TY - JOUR AU - Cruz‐Silva, E AU - Harrison, S P AU - Prentice, I C AU - Marinova, E TI - Holocene vegetation dynamics of the Eastern Mediterranean region : old controversies addressed by a new analysis JF - JOURNAL OF BIOGEOGRAPHY J2 - J BIOGEOGR VL - 51 PY - 2024 IS - 2 SP - 294 EP - 310 PG - 17 SN - 0305-0270 DO - 10.1111/jbi.14749 UR - https://m2.mtmt.hu/api/publication/34267763 ID - 34267763 N1 - School of Archaeology, Geography & Environmental Science, Reading University, Reading, United Kingdom Department of Life Sciences, Georgina Mace Centre for the Living Planet, Imperial College London, Ascot, United Kingdom Laboratory for Archaeobotany, Baden-Württemberg State Office for Cultural Heritage Management, Hemmenhofen-Gaienhofen, Germany Export Date: 1 December 2023 CODEN: JBIOD Correspondence Address: Cruz-Silva, E.; School of Archaeology, Whiteknights, United Kingdom; email: e.cruz-silva@pgr.reading.ac.uk LA - English DB - MTMT ER - TY - JOUR AU - Badino, Federica AU - Pini, Roberta AU - Ravazzi, Cesare AU - Chytry, Milan AU - Bertuletti, Paolo AU - Bortolini, Eugenio AU - Dudova, Lydie AU - Peresani, Marco AU - Romandini, Matteo AU - Benazzi, Stefano TI - High-resolution ecosystem changes pacing the millennial climate variability at the Middle to Upper Palaeolithic transition in NE-Italy JF - SCIENTIFIC REPORTS J2 - SCI REP VL - 13 PY - 2023 IS - 1 PG - 17 SN - 2045-2322 DO - 10.1038/s41598-023-38081-1 UR - https://m2.mtmt.hu/api/publication/34608221 ID - 34608221 N1 - Department of Cultural Heritage, University of Bologna, Ravenna, 48121, Italy CNR-Institute of Environmental Geology and Geoengineering, Lab. of Palynology and Palaeoecology, Research Group on Vegetation, Climate and Human Stratigraphy, Milan, 20126, Italy Department of Botany and Zoology, Faculty of Science, Masaryk University, Brno, Czech Republic Department of Paleoecology, Institute of Botany, Czech Academy of Sciences, Brno, Czech Republic Department of Humanities, Prehistoric and Anthropology Sciences, University of Ferrara, Ferrara, 44100, Italy Cited By :1 Export Date: 19 March 2024 Correspondence Address: Badino, F.; Department of Cultural Heritage, Italy; email: federica.badino@igag.cnr.it AB - Observation of high-resolution terrestrial palaeoecological series can decipher relationships between past climatic transitions, their effects on ecosystems and wildfire cyclicity. Here we present a new radiocarbon dated record from Lake Fimon (NE-Italy) covering the 60-27 ka interval. Palynological, charcoal fragments and sediment lithology analysis were carried out at centennial to sub-centennial resolutions. Identification of the best modern analogues for MIS 3 ecosystems further enabled to thoroughly reconstruct structural changes in the vegetation through time. This series also represents an öff-site" reference record for chronologically well-constrained Palaeolithic sites documenting Neanderthal and Homo sapiens occupations within the same region. Neanderthals lived in a mosaic of grasslands and woodlands, composed of a mixture of boreal and broad-leaved temperate trees analogous to those of the modern Central-Eastern Europe, the Southern Urals and central-southern Siberia. Dry and other grassland types expanded steadily from 44 to 43 ka and peaked between 42 and 39 ka, i.e., about the same time when Sapiens reached this region. This vegetation, which finds very few reliable modern analogues in the adopted Eurasian calibration set, led to the expansion of ecosystems able to sustain large herds of herbivores. During 39-27 ka, the landscape was covered by steppe, desert-steppe and open dry boreal forests similar to those of the modern Altai-Sayan region. Both Neanderthal and Sapiens lived in contexts of expanded fire-prone ecosystems modulated by the high-frequency climatic cycles of MIS 3. LA - English DB - MTMT ER - TY - JOUR AU - Darabos, Gabriella AU - Magyari, Enikő Katalin AU - Szabó, Zoltán AU - Lisztes-Szabó, Zsuzsa AU - Veres, D AU - Haliuc, A AU - Reitmeyer, B AU - Pálfi, Ivett TI - Erdő- és fahatár változás a Déli-Kárpátokban a késő glaciális és kora holocén gyors felmelegedési hullámai idején: korai erdőexpanzió és a fiatal driász lehűlés csillapított hatása JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 153 PY - 2023 IS - 2 SP - 143 EP - 163 PG - 21 SN - 0015-542X DO - 10.23928/foldt.kozl.2023.153.2.143 UR - https://m2.mtmt.hu/api/publication/34105792 ID - 34105792 N1 - Eötvös Loránd Tudományegyetem, Környezet-és Tájföldrajzi Tanszék, Hungary MTA-MTM-ELTE Paleontológiai Kutatócsoport ELKH Atommagkutató Intézet, Izotópklimatológiai és Környezettudományi Központ, Hungary Institute of Speleology, Romanian Academy, Romania Csillagászati és Földtudományi Kutatóközpont, Földtani és Geokémiai Intézet Export Date: 27 October 2023 Correspondence Address: Darabos, G.; Eötvös Loránd Tudományegyetem, Hungary; email: gabriella.darabos@ttk.elte.hu AB - A Páreng-hegységcsoportban (Munții Parâng, Déli-Kárpátok) lévő magashegyi tó (Latorica-tó, Iezerul Latorița, 1530 m) üledékének késő glaciális és kora holocén korú szakaszán növényi makrofosszília és pollen analitikai elemzéseket végeztünk, hogy megállapítsuk a fahatár, az erdőhatár és a szubalpi vegetáció éghajlatváltozásra adott válaszreakcióit. A Latorica-tó vízgyűjtőjén és partján 15 510–14 765 kal. BP évek (Grönlandi 2-es oxigénizotóp fázis (GS-2) vége) között a gleccserek visszahúzódása nyomán nem volt, vagy csak ritka növényborítás lehetett, tehát a fahatár valószínűleg a tó alatt húzódott. Az ezt követő GI-1 fázisban (kormodellünk alapján 14 765–13 340 kal. BP évek között) bekövetkező felmelegedés hatására a tó körül kialakuló fahatár ökoton zónában törpefenyő, lucfenyő és szálanként vörösfenyő (Pinus mugo–Picea abies–Larix decidua) keveredésével jellemezhető, boreális nyílt erdő expanzióját rekonstruáltuk. A fahatár fokozatosan magasabbra húzódott, majd a GI-1 végén (13 340–12 930 kal BP évek közt) nagy intenzitású erdőtűz következhetett be a tó körül, annak vízgyűjtőjére is kiterjedve. A fiatal driász lehűlés a jelenlegi kormodell szerint 12 930 és 11 995 kal. BP évek között a tó szerves anyag produkciójának csökkenéséhez vezetett, ugyanakkor a lehűlés csak kis mértékben hatott a tó menti vegetációra. A legjelentősebb változás a havasi cirbolyafenyő (Pinus cembra) megjelenése és előretörése volt ebben az időszakban. A kora holocénben (11 995–11 300 kal. BP évek közt) a fa- és erdőhatár folyamatosan emelkedhetett, az erdőszerkezet zárult és tovább diverzifikálódott a molyhos nyír (Betula pubescens) megjelenésével: luc- (P. abies), vörösfenyő (L. decidua) és törpefenyő (P. mugo) alkotta nyílt, de a késő glaciálisnál zártabb erdők uralták a tó körüli tájat. Eredményeink alapján elmondhatjuk, hogy a késő glaciális erdőexpanzió gyorsasága közeli refúgiális populációkra utal a fenyőfélék esetében, valamint eredményeink megerősítik a Déli-Kárpátok Retyezát vonulatában kapott eredményeket, miszerint a fiatal driász lehűlés a vegetációs időszak hőösszegét csak kis mértékben csökkentette ebben a régióban (szemben Nyugat-Európával). Az éghajlatváltozás kompetíciós előnybe hozta a Déli-Kárpátok szubalpin zónájában a havasi cirbolyafenyőt (P. cembra), mely ekkor terjedt el a fahatár ökoton zónában. A kora holocén felmelegedés során a mainál kontinentálisabb klímán a vörösfenyő széles körben elterjedt a Déli-Kárpátokban a szubalpin zónában. LA - Hungarian DB - MTMT ER - TY - JOUR AU - Farkas, Beáta AU - Sipos, György AU - Bartyik, Tamás AU - Józsa, Edina AU - Czigány, Szabolcs AU - Balogh, Richárd AU - Varga, Gábor AU - Kovács, János AU - Fábián, Szabolcs Ákos TI - Characterization and mapping of MIS‐2 thermal contraction crack polygons in Western Transdanubia, Hungary JF - PERMAFROST AND PERIGLACIAL PROCESSES J2 - PERMAFROST PERIGLAC VL - 34 PY - 2023 IS - 3 SP - 417 EP - 427 PG - 11 SN - 1045-6740 DO - 10.1002/ppp.2190 UR - https://m2.mtmt.hu/api/publication/33777210 ID - 33777210 N1 - Special Issue: Cryopedology Across Scales:Integrating Experiments, Observations And Models LA - English DB - MTMT ER - TY - BOOK ED - Karátson, Dávid ED - Veres, D. ED - Gertisser, R. ED - Magyari, Enikő Katalin ED - Jánosi, C. ED - Hambach, U. TI - A Kárpátok legfiatalabb tűzhányója, a Csomád. Vulkánosság, őskörnyezet, ember és táj. PB - Tortoma Könyvkiadó CY - Barót PY - 2023 SN - 9786069716472 UR - https://m2.mtmt.hu/api/publication/33733446 ID - 33733446 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Lisztes-Szabó, Zsuzsa AU - Tóth, Albert AU - Buró, Botond AU - Braun, Ádám AU - Csík, Attila AU - Filep, Anna Fruzsina AU - Kuneš, Petr AU - Braun, Mihály TI - Well-preserved Norway spruce needle phytoliths in sediments can be a new paleoenvironmental indicator JF - HOLOCENE J2 - HOLOCENE VL - 33 PY - 2023 IS - 4 SP - 471 EP - 477 PG - 7 SN - 0959-6836 DO - 10.1177/09596836221145361 UR - https://m2.mtmt.hu/api/publication/33550234 ID - 33550234 N1 - Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Hungary Institute of Nature Conservation and Environmental Management, Hungarian University of Agriculture and Life Sciences, Hungary Laboratory of Materials Science, Institute for Nuclear Research, Hungary Pál Juhász-Nagy Doctoral School of Biology and Environmental Sciences, University of Debrecen, Hungary Department of Botany, Faculty of Science, Charles University, Czech Republic Export Date: 4 September 2023 CODEN: HOLOE Correspondence Address: Lisztes-Szabó, Z.; Isotope Climatology and Environmental Research Centre, Hungary; email: lisztes-szabo.zsuzsanna@atomki.hu AB - Analysis of phytoliths (plant silica bodies) still may have an unrevealed potential in paleoenvironmental reconstruction studies. This can provide novel findings in research on environmental change as phytoliths play an important role in the silicon biogeochemical cycle. In favorable environmental conditions, Picea abies [L.] H. Karst (Norway spruce) needles develop a phytolith layer consisting of more or less cubical or cuboid (blocky) phytoliths in their transfusion tissue that becomes continuous toward the apex of the needle. This can be studied in situ in fossil (subfossil) needles under a stereomicroscope. This study reports the blocky-type phytolith preservation in fossil spruce needles in sediment sections of the lake Černé jezero (Bohemian Forest, Czech Republic). The oldest needle containing phytoliths was 7.8 cal ka BP. Despite differences in the Energy Dispersive X-ray (EDX) spectra of different age phytoliths, the studied subfossil phytoliths did not lose their globular ultrastructure in the needle tissue, proving the stability of this phytolith morphotype. As the tissue of the needle fossils can preserve phytoliths in situ, further micro-analytical measurements will make these needles promising tools for paleoenvironmental reconstructions. The most favorable period for spruce phytolith formation for the studied region appears to be the period 6.0–4.5 cal ka BP, within the Holocene Climate Optimum period. In order to use these phytoliths as a terrestrial climate proxy, the next step is to refine their sensitivity to environmental changes. LA - English DB - MTMT ER - TY - JOUR AU - Milinkó, István AU - Novothny, Ágnes AU - Pető, Ákos TI - Lösz-paleotalaj sorozatokban megőrződött fitolitkészletek környezettörténeti és környezet régészeti vonatkozású kutatási lehetőségei JF - ARCHEOMETRIAI MŰHELY J2 - ARCHEOMETRIAI MŰHELY VL - 20 PY - 2023 IS - 1 SP - 93 EP - 114 PG - 22 SN - 1786-271X DO - 10.55023/issn.1786-271X.2023-006 UR - https://m2.mtmt.hu/api/publication/34007320 ID - 34007320 N1 - Eötvös Loránd Tudományegyetem, Természetföldrajzi Tanszék, 1117, Pázmány P. sétány 1/C., Budapest, Hungary Magyar Agrár- és Élettudományi Egyetem, Vadgazdálkodási és Természetvédelmi Intézet, Természetvédelmi és Tájgazdálkodási Tanszék, Páter K. u. 1, Gödöllő, 2100, Hungary Export Date: 5 January 2024 Correspondence Address: Pető, Á.; Magyar Agrár- és Élettudományi Egyetem, Páter K. u. 1, Hungary; email: Peto.Akos@uni-mate.hu AB - A fitolitok növények által termelt opálszemcsék, amelyek bizonyos tulajdonságaiknak köszönhetően (pl. nagy mennyiségben termelődnek, diagnosztikai értékkel bíró morfotípusok létezése, viszonylag nagy ellenállóképesség) az egykori (lokális) vegetáció indikátorai. Talajokból, üledékekből, üledékes kőzetekből kinyert fitolitkészlet értékes proxy adatot jelenthet a környezetrekonstrukciós vizsgálatokhoz. Régészeti kontextusból gyűjtött fitolitok az ember táj- és növényhasznosításának rekonstrukciójában játszhatnak fontos szerepet. A fitolitkészlet megfelelő kiértékeléséhez elengedhetetlen a fitolitkészletet ért tafonómiai folyamatok ismerete, hatásuk becslése. Lösz-paleotalaj sorozatok jelentős kiterjedésben és vastagságban borítják a szárazföldek felszínét. A lösz-paleotalaj sorozatokból kinyert fitolitkészleteket ennélfogva nagy kiterjedésű területen, jelentős időtávot (elsősorban a negyedidőszakot) átfogva lehet felhasználni a környezetrekonstrukciós vizsgálatok során. A fitolitkészlet környezetrekonstrukciós vizsgálatokban történő megfelelő kiértékeléséhez szükséges ismerni a lösz-paleotalaj sorozatok esetében érvényesülő főbb tafonómiai folyamatokat. A fitolitok lösz-paleotalaj sorozatokban történő megőrződését befolyásoló folyamatok jobb megismerése megbízhatóbb környezetrekonstrukciót tesz lehetővé. LA - Hungarian DB - MTMT ER - TY - JOUR AU - Mitka, Jozef AU - Wroblewaka, Ada AU - Boron, Piotr AU - Kucharzyk, Stanislaw AU - Stachurska-Swakon, Alina TI - Perhaps there were northern refugia in LGM? The phylogeographic structure of the thermophilic tree Carpinus betulus in the Carpathian region JF - SCIENCE OF THE TOTAL ENVIRONMENT J2 - SCI TOTAL ENVIRON VL - 905 PY - 2023 PG - 13 SN - 0048-9697 DO - 10.1016/j.scitotenv.2023.167214 UR - https://m2.mtmt.hu/api/publication/34243231 ID - 34243231 N1 - Funding Agency and Grant Number: NCN [N N304 071940] Funding text: We dedicate this manuscript to the memory of Kazimierz Szczepanek (1931-2021), a Polish paleobotanist - researcher of glacial and Holocene floras in the Carpathian Mountains. The paper was financially supported by an NCN grant no. N N304 071940. The authors thank Ewelina Klichowska (Institute of Botany, Jagiellonian University) for modelling the species' European LGM refugia and Jacqueline Trojan (New Mexico State University) for language revision. AB - Carpinus betulus L., the hornbeam, is a component of lowland and highland forests in Europe. By examining the postglacial migratory history of thermophilic tree species, the study aimed to unravel their putative glacial microrefugia in the Carpathian region. The present study points to the two distinct genetic AFLP groups of C. betulus in the Carpathian region that represent different genetic lineages based on Bayesian analysis. They differed in Nei's gene diversity index h, and the analysis of molecular variance AMOVA showed a percentage variation of the populations between the groups of 13.74 %. Principal coordinate analysis (PCoA) of 368 AFLP tree samples confirmed the presence of two genetic groups. Ninety-five populations underwent principal component analysis (PCA) to show the main correlations between genetic diversity indices and bioclimatic/ climate variables (WorldClim and Carpatclim). The generalized logistic model (GLM) showed the significance of Nei's genetic index h in delimiting genetic groups. The results of population-genetic and multivariate analyses determined that the two genetic groups nowadays are spatially diffused and do not show a clear geographic pattern, pointing to a genetic melting pot. We found ecological links between genetic diversity and bioclimatic characteristics, especially the precipitation in the coldest quarter - Bio19. The refugial Maxent model indicates a significant contribution of the Bio7 variable (both linked with a continental type of climate) to the occurrence of the species during the LGM in Europe. We suggest the relict character of hornbeam populations in a specific climatic-terrain niche in the northern part of the Carpathian Basin. LA - English DB - MTMT ER - TY - JOUR AU - Molnár, Ábel Péter AU - Demeter, László AU - Biró, Marianna AU - Chytrý, Milan AU - Bartha, Sándor AU - Batdelger, Gantuya AU - Molnár, Zsolt TI - Is there a massive glacial–Holocene flora continuity in Central Europe? JF - BIOLOGICAL REVIEWS J2 - BIOL REV VL - 98 PY - 2023 IS - 6 SP - 2307 EP - 2319 PG - 13 SN - 1464-7931 DO - 10.1111/brv.13007 UR - https://m2.mtmt.hu/api/publication/34119273 ID - 34119273 N1 - Hungarian University of Agriculture and Life Sciences, Institute for Wildlife Management and Nature Conservation, Páter Károly u. 1., Gödöllő, 2100, Hungary Doctoral School of Biological Sciences, Hungarian University of Agriculture and Life Sciences, Páter Károly u. 1., Gödöllő, 2100, Hungary Centre for Ecological Research, Institute of Ecology and Botany, Alkotmány u. 2–4., Vácrátót, 2163, Hungary Department of Botany and Zoology, Faculty of Science, Masaryk University, Kotlářská 2, Brno, 611 37, Czech Republic Botanic Garden and Research Institute, Mongolian Academy of Sciences, 13th Street, Peace Avenue 54a, Bayanzurkh district, Ulaanbaatar, 13330, Mongolia Doctoral School of Biology, Eötvös Lorand University, Budapest, Pázmány P. stny. 1/C., Budapest, 1117, Hungary Export Date: 13 November 2023 Correspondence Address: Molnár, Z.; Centre for Ecological Research, Alkotmány u. 2–4., Hungary; email: molnar.zsolt@ecolres.hu AB - The prevailing paradigm about the Quaternary ecological and evolutionary history of Central European ecosystems is that they were repeatedly impoverished by regional extinctions of most species during the glacial periods, followed by massive recolonizations from southern and eastern refugia during interglacial periods. Recent literature partially contradicts this view and provides evidence to re‐evaluate this Postglacial Recolonization Hypothesis and develop an alternative one. We examined the long‐term history of the flora of the Carpathian (Pannonian) Basin by synthesising recent advances in ecological, phylogeographical, palaeoecological and palaeoclimatological research, and analysing the cold tolerance of the native flora of a test area (Hungary, the central part of the Carpathian Basin). We found that (1) many species have likely occurred there continuously since before the Last Glacial Maximum (LGM); (2) most of the present‐day native flora (1404 species, about 80%) can occur in climates as cold as or colder than the LGM (mean annual temperature ≤+3.5°C); and (3) grasslands and forests can be species‐rich under an LGM‐like cold climate. These arguments support an alternative hypothesis, which we call the Flora Continuity Hypothesis. It states that long‐term continuity of much of the flora in the Carpathian Basin is more plausible than regional extinctions during the LGM followed by massive postglacial recolonizations. The long‐term continuity of the region's flora may have fundamental implications not only for understanding local biogeography and ecology (e.g. the temporal scale of processes), but also for conservation strategies focusing on protecting ancient species‐rich ecosystems and local gene pools. LA - English DB - MTMT ER - TY - JOUR AU - Prach, Jindrich AU - Hosek, Jan AU - Pokorna, Adela AU - Hoskova, Kristyna AU - Pokorny, Petr TI - Well-hidden forests? Modern pollen spectra from Central Yakutia (Eastern Siberia) contribute to the interpretation of the last glacial vegetation in Central Europe JF - FOLIA GEOBOTANICA J2 - FOLIA GEOBOT PY - 2023 PG - 19 SN - 1211-9520 DO - 10.1007/s12224-023-09435-4 UR - https://m2.mtmt.hu/api/publication/34608222 ID - 34608222 N1 - Export Date: 19 March 2024 Correspondence Address: Prach, J.; Centre for Theoretical Study, Jilská 1, Czech Republic; email: jindraprach@gmail.com AB - The landscape of central Europe is thought to have been dominated by steppe, forest-steppe, or tundra during the Last Glacial. This classical view is mostly based on the pollen records. However, as the pollen production and taphonomy during the cold periods are largely unknown, modern analogies of past landscapes need to be involved to provide more plausible vegetation reconstructions. Here we performed pollen analyses of recent samples from small lakes in Yakutia, eastern Siberia, a cold region where larch taiga forest is maintained by water from cyclically melting permafrost. We compared the pollen samples using multivariate (PCA) and analogue matching techniques with 830 fossil pollen samples from central Europe dated to MIS3-MIS1 (ca 35,000-11,700 cal BP). We have shown that the non-arboreal pollen proportion is around 50% in the lakes within Yakutian forested landscape, while such proportions have been interpreted as an indication of forestless landscape in European fossil records. Some central European fossil samples are more similar to samples from present-day Yakutia than to the South Siberian steppes so far considered analogous; this is especially true for samples from areas on unconsolidated bedrock with water-saturated permafrost from the Late Glacial, Bolling-Allerod interstadials. We advocate the idea of extending existing interpretations of past landscapes. The fossil pollen might not only reflect steppe-tundra vegetation, but, in addition to that, at least the Late Glacial pollen samples from central Europe may reflect a landscape forested by 'invisible' larch with spatially limited steppe patches, like the one found in present-day Yakutia. LA - English DB - MTMT ER - TY - JOUR AU - Semerikov, N. V. AU - Petrova, I. V. TI - Demographic History of Scots Pine in the Pleistocene in Northern Eurasia and the Caucasus Region Based on an Analysis of Nuclear Microsatellite Loci JF - CONTEMPORARY PROBLEMS OF ECOLOGY J2 - CONTEMP PROBL ECOL VL - 16 PY - 2023 IS - 5 SP - 549 EP - 563 PG - 15 SN - 1995-4255 DO - 10.1134/S1995425523050116 UR - https://m2.mtmt.hu/api/publication/34172601 ID - 34172601 N1 - Export Date: 8 February 2024 Correspondence Address: Semerikov, N.V.; Botanical Garden, Russian Federation; email: semerikov2014@mail.ru LA - English DB - MTMT ER - TY - JOUR AU - Večeřa, Martin AU - Axmanová, Irena AU - Chytrý, Milan AU - Divíšek, Jan AU - Ndiribe, Charlotte AU - Velasco Mones, Gonzalo AU - Čeplová, Natálie AU - Aćić, Svetlana AU - Bahn, Michael AU - Bergamini, Ariel AU - Boenisch, Gerhard AU - Biurrun, Idoia AU - Bruun, Hans Henrik AU - Byun, Chaeho AU - Catford, Jane A. AU - Cerabolini, Bruno E. L. AU - Cornelissen, Johannes H. C. AU - Dengler, Jürgen AU - Jansen, Florian AU - Jansen, Steven AU - Kattge, Jens AU - Kozub, Łukasz AU - Kuzemko, Anna AU - Minden, Vanessa AU - Mitchell, Rachel M. AU - Moeslund, Jesper E. AU - Mori, Akira S. AU - Niinemets, Ülo AU - Ruprecht, Eszter AU - Rūsiņa, Solvita AU - Šilc, Urban AU - Soudzilovskaia, Nadejda A. AU - van Bodegom, Peter M. AU - Vassilev, Kiril AU - Weiher, Evan AU - Wright, Ian J. AU - Lososová, Zdeňka TI - Decoupled phylogenetic and functional diversity in European grasslands JF - PRESLIA J2 - PRESLIA VL - 95 PY - 2023 IS - 4 SP - 413 EP - 445 PG - 33 SN - 0032-7786 DO - 10.23855/preslia.2023.413 UR - https://m2.mtmt.hu/api/publication/34450692 ID - 34450692 N1 - Department of Botany and Zoology, Faculty of Science, Masaryk University, Kotlářská 2, Brno, CZ-61137, Czech Republic Department of Geography, Faculty of Science, Masaryk University, Kotlářská 2, Brno, CZ-61137, Czech Republic Department of Cell Biology and Genetics, University of Lagos, Tafawa Balewa Way, Lagos, NG-101245, Nigeria Department of Biology, Faculty of Education, Masaryk University, Poříčí 7, Brno, CZ-60300, Czech Republic Department of Botany, Faculty of Agriculture, University of Belgrade, Nemanjina 6, Zemun, Belgrade, RS-11000, Serbia Department of Ecology, University of Innsbruck, Sternwartestrasse 15, Innsbruck, AT-6020, Austria WSL Swiss Federal Research Institute, Zürcherstrasse 111, Birmensdorf, CH-8903, Switzerland Max Planck Institute for Biogeochemistry, Hans-Knöll-Strasse 10, Jena, DE-07745, Germany Department of Plant Biology and Ecology, Faculty of Science and Technology, University of the Basque Country UPV/EHU, Barrio Sarriena s/n, Leioa, Bilbao, ES-48940, Spain Depart-ment of Biology, University of Copenhagen, Ole Maalřes Vej 5, Copenhagen, DK-2200, Denmark Department of Biological Sciences, Andong National University, Gyeongdong-ro, Songcheon-dong, Andong, KR-1375, South Korea Department of Geography, King’s College London, Strand, London, UK-WC2R 2LS, United Kingdom Department of Biotechnologies and Life Sciences, University of Insubria, Via J. H. Dunant 3, Varese, IT-21100, Italy Systems Ecology, Department of Ecological Science, Vrije Universiteit Amsterdam, De Boelelaan 1085, Amsterdam, NL-1081 HV, Netherlands Vegetation Ecology, Institute of Natural Resource Sciences (IUNR), Zurich University of Applied Sciences (ZHAW), Grüentalstrasse 14, Wädenswil, CH-8820, Switzerland Plant Ecology, Bayreuth Center of Ecology and Environmental Research (BayCEER), University of Bayreuth, Dr. Hans-Frisch-Strasse 1-3, Bayreuth, DE-95448, Germany German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Puschstrasse 4, Leipzig, DE-04103, Germany Faculty of Agricultural and Environmental Sciences, University of Rostock, Justusvon-Liebig-Weg 6, Rostock, DE-18059, Germany Institute of Botany, Ulm University, Albert-Einstein-Allee 11, Ulm, Baden-Württemberg, DE-89081, Germany Department of Ecology and Environmental Conservation, Institute of Environmental Biology, Faculty of Biology, University of Warsaw, Ilji Miecznikowa 1, Warsaw, PL-02096, Poland M. G. Kholodny Institute of Botany, National Academy of Sciences of Ukraine, Tereshchenkivska 2, Kyiv, UA-01601, Ukraine De-partment of Biology, Vrije Universiteit Brussel, Pleinlaan 2, Elsene, Brussels, BE-1050, Belgium School of Natural Resources and the Environment, University of Arizona, E. Lowell Street 1064, Tucson, AZ-85721, United States Department of Ecoscience, Faculty of Technical Sciences, Aarhus University, C. F. M řllers Allé 6-8, Aarhus C, DK-8000, Denmark Research Center for Advanced Science and Technology, University of Tokyo, Tokyo, 153-8904, Japan Chair of Crop Science and Plant Biology, Estonian University of Life Sciences, Kreutzwaldi 1, Tartu, EE-51006, Estonia Hungarian Department of Biology and Ecology, Babeş-Bolyai University, Strada Republicii 44, Cluj-Napoca, RO-400000, Romania Faculty of Geography and Earth Sciences, University of Latvia, Jelgavas iela 1, Riga, LV-1004, Latvia Institute of Biology, Research Centre of the Slovenian Academy of Sciences and Arts, Novi trg 2, Ljubljana, SI-1000, Slovenia Centre for Environmental Sciences, Hasselt Univeristy, Martelarenlaan 42, Hasselt, BE-3500, Belgium Insti-tute of Environmental Sciences, Leiden University, Rapenburg 70, Leiden, NL-2311 EZ, Netherlands Department of Plant and Fungal Diversity and Resources, Institute of Biodiversity and Ecosystem Research, Bulgarian Academy of Sciences, Gagarin Street 2, Sofia, BG-1113, Bulgaria Department of Biology, University of Wisconsin – Eau Claire, Roosevelt Avenue 101, Eau Claire, WI-54701, United States Hawkesbury Institute for the Environment, Western Sydney University, Richmond, NSW-2753, Australia School of Natural Sciences, Macquarie University, Sydney, NSW-2109, Australia Cited By :1 Export Date: 19 March 2024 Correspondence Address: Večeřa, M.; Department of Botany and Zoology, Kotlářská 2, Czech Republic; email: martinvec@seznam.cz LA - English DB - MTMT ER - TY - JOUR AU - Bertran, P TI - Distribution and characteristics of Pleistocene ground thermal contraction polygons in Europe from satellite images JF - PERMAFROST AND PERIGLACIAL PROCESSES J2 - PERMAFROST PERIGLAC VL - 33 PY - 2022 IS - 2 SP - 9 EP - 113 PG - 15 SN - 1045-6740 DO - 10.1002/ppp.2137 UR - https://m2.mtmt.hu/api/publication/32633606 ID - 32633606 N1 - Inrap, Bègles, France PACEA, Université de Bordeaux – CNRS, Pessac, France Export Date: 25 May 2022 CODEN: PEPPE Correspondence Address: Bertran, P.; InrapFrance; email: pascal.bertran@inrap.fr LA - English DB - MTMT ER - TY - JOUR AU - Bertran, Pascal AU - Stadelmaier, Kim H. AU - Ludwig, Patrick TI - Last Glacial Maximum active layer thickness in Western Europe, and the issue of ‘tundra gleys’ in loess sequences JF - JOURNAL OF QUATERNARY SCIENCE J2 - J QUATERNARY SCI VL - 2022 PY - 2022 SN - 0267-8179 DO - 10.1002/jqs.3434 UR - https://m2.mtmt.hu/api/publication/32894529 ID - 32894529 N1 - Export Date: 19 October 2022 Correspondence Address: Bertran, P.; Inrap, France; email: pascal.bertran@inrap.fr LA - English DB - MTMT ER - TY - JOUR AU - Degen, Bernd AU - Yanbaev, Yulai AU - Ianbaev, Ruslan AU - Blanc-Jolivet, Celine AU - Mader, Malte AU - Bakhtina, Svetlana AU - Heinze, Berthold TI - Large-scale genetic structure of Quercus robur in its eastern distribution range enables assignment of unknown seed sources JF - FORESTRY J2 - FORESTRY PY - 2022 SN - 0015-752X DO - 10.1093/forestry/cpac009 UR - https://m2.mtmt.hu/api/publication/32771050 ID - 32771050 N1 - Thuenen-Institute of Forest Genetics, Sieker Landstrasse 2, Grosshansdorf, 22927, Germany Bashkir State Agrarian University, 50-letiya Oktyabrya str.-34, Ufa, 450001, Russian Federation Export Date: 27 February 2023 CODEN: FRSTA Correspondence Address: Degen, B.; Thuenen-Institute of Forest Genetics, Sieker Landstrasse 2, Germany; email: bernd.degen@thuenen.de LA - English DB - MTMT ER - TY - JOUR AU - Divíšek, Jan AU - Večeřa, Martin AU - Welk, Erik AU - Danihelka, Jiří AU - Chytrý, Kryštof AU - Douda, Jan AU - Chytrý, Milan TI - Origin of the central European steppe flora: insights from palaeodistribution modelling and migration simulations JF - ECOGRAPHY J2 - ECOGRAPHY VL - 2022 PY - 2022 IS - 12 PG - 17 SN - 0906-7590 DO - 10.1111/ecog.06293 UR - https://m2.mtmt.hu/api/publication/33195593 ID - 33195593 N1 - Funding Agency and Grant Number: Czech Science Foundation [18-03028S] Funding text: This study was supported by the Czech Science Foundation (project no. 18-03028S). LA - English DB - MTMT ER - TY - JOUR AU - Gębica, P AU - Michno, A AU - Sobucki, M AU - Wacnik, A AU - Superson, S TI - Chronology and dynamics of fluvial style changes in the Younger Dryas and Early Holocene in Central Europe (lower San River, SE Poland) JF - SCIENCE OF THE TOTAL ENVIRONMENT J2 - SCI TOTAL ENVIRON VL - 830 PY - 2022 SN - 0048-9697 DO - 10.1016/j.scitotenv.2022.154700 UR - https://m2.mtmt.hu/api/publication/32760471 ID - 32760471 N1 - Institute of Archaeology, University of Rzeszow, Moniuszki 10, Rzeszów, 35-015, Poland Institute of Geography and Spatial Management, Faculty of Geography and Geology, Jagiellonian University, Gronostajowa 7, Kraków, 30-387, Poland W. Szafer Institute of Botany, Polish Academy of Sciences, Lubicz 46, Kraków, 31-512, Poland Vocational Secondary School no. 2 in Rzeszow, Rejtana 3, Rzeszów, 35-326, Poland Export Date: 25 May 2022 CODEN: STEVA Correspondence Address: Gębica, P.; Institute of Archaeology, Moniuszki 10, Poland; email: pgebica@ur.edu.pl LA - English DB - MTMT ER - TY - JOUR AU - Geng, Rongwei AU - Andreev, Andrei AU - Kruse, Stefan AU - Heim, Birgit AU - van Geffen, Femke AU - Pestryakova, Luidmila AU - Zakharov, Evgenii AU - Troeva, Elena AU - Shevtsova, Iuliia AU - Li, Furong AU - Zhao, Yan AU - Herzschuh, Ulrike TI - Modern Pollen Assemblages From Lake Sediments and Soil in East Siberia and Relative Pollen Productivity Estimates for Major Taxa JF - FRONTIERS IN ECOLOGY AND EVOLUTION J2 - FRONT ECOL EVOL VL - 10 PY - 2022 PG - 17 SN - 2296-701X DO - 10.3389/fevo.2022.837857 UR - https://m2.mtmt.hu/api/publication/33000462 ID - 33000462 N1 - Section of Polar Terrestrial Environmental Systems, Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam, Germany Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, China Institute of Biochemistry and Biology, University of Potsdam, Potsdam, Germany Institute of Natural Sciences, North-Eastern Federal University of Yakutsk, Yakutsk, Russian Federation Institute for Biological Problems of Cryolithozone, Russian Academy of Sciences, Yakutsk, Russian Federation School of Ecology, Sun Yat-sen University, Shenzhen, China Cited By :2 Export Date: 27 February 2023 Correspondence Address: Herzschuh, U.; Section of Polar Terrestrial Environmental Systems, Germany; email: ulrike.herzschuh@awi.de AB - Modern pollen-vegetation-climate relationships underpin palaeovegetation and palaeoclimate reconstructions from fossil pollen records. East Siberia is an ideal area for investigating the relationships between modern pollen assemblages and near natural vegetation under cold continental climate conditions. Reliable pollen-based quantitative vegetation and climate reconstructions are still scarce due to the limited number of modern pollen datasets. Furthermore, differences in pollen representation of samples from lake sediments and soils are not well understood. Here, we present a new pollen dataset of 48 moss/soil and 24 lake surface-sediment samples collected in Chukotka and central Yakutia in East Siberia. The pollen-vegetation-climate relationships were investigated by ordination analyses. Generally, tundra and taiga vegetation types can be well distinguished in the surface pollen assemblages. Moss/soil and lake samples contain generally similar pollen assemblages as revealed by a Procrustes comparison with some exceptions. Overall, modern pollen assemblages reflect the temperature and precipitation gradients in the study areas as revealed by constrained ordination analysis. We estimate the relative pollen productivity (RPP) of major taxa and the relevant source area of pollen (RSAP) for moss/soil samples from Chukotka and central Yakutia using Extended R-Value (ERV) analysis. The RSAP of the tundra-forest transition area in Chukotka and taiga area in central Yakutia are ca. 1300 and 360 m, respectively. For Chukotka, RPPs relative to both Poaceae and Ericaceae were estimated while RPPs for central Yakutia were relative only to Ericaceae. Relative to Ericaceae (reference taxon, RPP = 1), Larix, Betula, Picea, and Pinus are overrepresented while Alnus, Cyperaceae, Poaceae, and Salix are underrepresented in the pollen spectra. Our estimates are in general agreement with previously published values and provide the basis for reliable quantitative reconstructions of East Siberian vegetation. LA - English DB - MTMT ER - TY - BOOK ED - Karátson, Dávid ED - Veres, D. ED - Gertisser, R. ED - Magyari, Enikő Katalin ED - Jánosi, C. ED - Hambach, U. TI - Ciomadul (Csomád), The Youngest Volcano in the Carpathians PB - Springer Netherlands CY - Cham (Németország) PY - 2022 SP - 296 SN - 9783030891404 DO - 10.1007/978-3-030-89140-4 UR - https://m2.mtmt.hu/api/publication/32186131 ID - 32186131 LA - English DB - MTMT ER - TY - JOUR AU - Kobiv, Y. AU - Koutecký, P. AU - Štech, M. AU - Pachschwöll, C. TI - First records of Calamagrostis purpurea (Poaceae) in the Carpathians, a relict species new to the flora of Slovakia, Ukraine, and Romania JF - BIOLOGIA (BRATISLAVA) J2 - BIOLOGIA PY - 2022 SN - 0006-3088 DO - 10.1007/s11756-022-01083-x UR - https://m2.mtmt.hu/api/publication/32843008 ID - 32843008 N1 - Institute of Ecology of the Carpathians, National Academy of Sciences of Ukraine, Lviv, Ukraine Department of Botany, Faculty of Science, University of South Bohemia, České Budějovice, Czech Republic Department of Botany and Biodiversity Research, University of Vienna, Vienna, Austria Export Date: 25 May 2022 Correspondence Address: Pachschwöll, C.; Department of Botany and Biodiversity Research, Austria; email: clemens.pachschwoell@univie.ac.at LA - English DB - MTMT ER - TY - JOUR AU - Magyari, Enikő Katalin AU - Gasparik, Mihály AU - Major, István AU - Lengyel, György AU - Pál, Ilona AU - Virág, Attila AU - Korponai, János AU - Haliuc, Aritina AU - Szabó, Zoltán AU - Pazonyi, Piroska TI - Mammal extinction facilitated biome shift and human population change during the last glacial termination in East-Central Europe JF - SCIENTIFIC REPORTS J2 - SCI REP VL - 12 PY - 2022 IS - 1 PG - 14 SN - 2045-2322 DO - 10.1038/s41598-022-10714-x UR - https://m2.mtmt.hu/api/publication/32795556 ID - 32795556 N1 - A publikáció a Nemzeti Közszolgálati Egyetem 2020. évi Tématerületi Kiválóság Program keretében, a Fenntartható biztonság és társadalmi környezet elnevezésű projekt támogatásával valósult meg, az Innovációs és Technológiai Minisztérium Nemzeti Kutatási, Fejlesztési és Innovációs Alapból nyújtott támogatásával, a Nemzeti Kutatási, Fejlesztési és Innovációs Hivatal által kibocsátott támogatói okirat alapján. AB - The study of local extinction times, together with the associated environmental and human population changes in the last glacial termination, provides insights into the causes of mega- and microfauna extinctions. In East-Central (EC) Europe, groups of Palaeolithic humans were present throughout the last glacial maximum, but disappeared suddenly around 15,200 cal BP. In this study cave sediment profiles dated using radiocarbon techniques and a large set of mammal bones dated directly by AMS 14C were used to determine local extinction times. These were, in turn, compared to changes in the total megafauna population of EC Europe derived from coprophilous fungi, the Epigravettian population decline, quantitative climate models, pollen and plant macrofossil inferred climate, as well as to biome reconstructions. The results suggest that the population size of large herbivores decreased in the area after 17,700 cal BP, when temperate tree abundance and warm continental steppe cover both increased in the lowlands. Boreal forest expansion started around 16,200 cal BP. Cave sediments show the decline of narrow-headed vole and arctic lemming populations specifically associated with a tundra environment at the same time and the expansion of the common vole, an inhabitant of steppes. The last dated appearance of arctic lemming was at ~ 16,640 cal BP, while that of the narrow-headed vole at ~ 13,340, and the estimated extinction time of woolly mammoth was either at 13,830 (GRIWM) or 15,210 (PHASE), and reindeer at 11,860 (GRIWM) or 12,550 cal BP (PHASE). The population decline of the large herbivore fauna slightly preceded changes in terrestrial vegetation, and likely facilitated it via a reduction in the intensity of grazing and the concomitant accumulation of plant biomass. Furthermore, it is possible to conclude that the Late Epigravettian population had high degree of quarry-fidelity; they left the basin when these mammals vanished. LA - English DB - MTMT ER - TY - CHAP AU - Oliva, M AU - Fernández-Fernández, JM. AU - Nývlt, D ED - Fernández-Fernández, José M ED - Nývlt, Daniel ED - Oliva, Marc TI - The Periglaciation of Europe T2 - Periglacial Landscapes of Europe PB - Springer Netherlands CY - Cham SN - 9783031148958 PY - 2022 SP - 477 EP - 523 PG - 47 DO - 10.1007/978-3-031-14895-8_16 UR - https://m2.mtmt.hu/api/publication/33600537 ID - 33600537 N1 - Export Date: 19 March 2024 Correspondence Address: Oliva, M.; Department of Geography, Spain; email: marcoliva@ub.edu LA - English DB - MTMT ER - TY - JOUR AU - Seidl, Anna AU - Tremetsberger, Karin AU - Pfanzelt, Simon AU - Lindhuber, Lisa AU - Kropf, Matthias AU - Neuffer, Barbara AU - Blattner, Frank R. AU - Király, Botond Gergely AU - Smirnov, Sergey V. AU - Friesen, Nikolai AU - Shmakov, Alexander I. AU - Plenk, Kristina AU - Batlai, Oyuntsetseg AU - Hurka, Herbert AU - Bernhardt, Karl-Georg TI - Genotyping-by-sequencing reveals range expansion of Adonis vernalis (Ranunculaceae) from Southeastern Europe into the zonal Euro-Siberian steppe JF - SCIENTIFIC REPORTS J2 - SCI REP VL - 12 PY - 2022 IS - 1 PG - 13 SN - 2045-2322 DO - 10.1038/s41598-022-23542-w UR - https://m2.mtmt.hu/api/publication/33245558 ID - 33245558 AB - The Euro-Siberian steppe flora consists of warm- and cold-adapted species, which may have responded differently to Pleistocene glacials and interglacials. Genotyping-by-sequencing individuals from across the distribution range of the pheasant’s eye ( Adonis vernalis ), we aimed to gain insight into steppe florogenesis based on the species’ evolutionary history. Although the primary area of origin of the species group comprising A. vernalis , A. villosa and A. volgensis is in Asia, our results indicate that recent populations of A. vernalis are not of Asian origin but evolved in the southern part of Europe during the Pleistocene, with Spanish populations clearly genetically distinct from the Southeastern European populations. We inferred that A. vernalis migrated eastwards from the sub-Mediterranean forest-steppes of Southeastern Europe into the continental forest-steppe zone. Eastern European populations had the highest private allelic richness, indicating long-term large population sizes in this region. As a thermophilic species, A. vernalis seems unlikely to have survived in the cold deserts of the Last Glacial Maximum in Western Siberia, so this region was likely (re)colonized postglacially. Overall, our results reinforce the importance of identifying the area of origin and the corresponding ecological requirements of steppe plants in order to understand the composition of today’s steppe flora. LA - English DB - MTMT ER - TY - JOUR AU - Smycka, Jan AU - Roquet, Cristina AU - Boleda, Marti AU - Alberti, Adriana AU - Boyer, Frederic AU - Douzet, Rolland AU - Perrier, Christophe AU - Rome, Maxime AU - Valay, Jean-Gabriel AU - Denoeud, France AU - Semberova, Kristyna AU - Zimmermann, Niklaus E. AU - Thuiller, Wilfried AU - Wincker, Patrick AU - Alsos, Inger G. AU - Coissac, Eric AU - Layergne, Sebastien TI - Tempo and drivers of plant diversification in the European mountain system JF - NATURE COMMUNICATIONS J2 - NAT COMMUN VL - 13 PY - 2022 IS - 1 PG - 13 SN - 2041-1723 DO - 10.1038/s41467-022-30394-5 UR - https://m2.mtmt.hu/api/publication/33000463 ID - 33000463 N1 - Univ. Grenoble Alpes, Univ. Savoie Mont Blanc, CNRS, LECA, Grenoble, FR-38000, France Center for Theoretical Study, Charles University and the Academy of Sciences of the Czech Republic, Prague, CZ-11000, Czech Republic Department of Botany, Faculty of Science, Charles University, Prague, CZ-12801, Czech Republic Systematics and Evolution of Vascular Plants (UAB) – Associated Unit to CSIC, Departament de Biologia Animal, Biologia Vegetal i Ecologia, Facultat de Biociències, Universitat Autònoma de Barcelona, Bellaterra, ES-08193, Spain Génomique Métabolique, Genoscope, Institut François Jacob, CEA, CNRS, Université Evry, Université Paris-Saclay, Evry, FR-91057, France Université Paris-Saclay, CEA, CNRS, Institute for Integrative Biology of the Cell (I2BC), Gif-sur-Yvette, FR-91190, France CNRS, Lautaret, Jardin du Lautaret, Université Grenoble Alpes, Grenoble, FR-38000, France Czech Academy of Sciences, Institute of Botany, Průhonice, CZ-25243, Czech Republic Swiss Federal Research Institute WSL, Birmensdorf, CH-8903, Switzerland UiT – The Arctic University of Norway, The Arctic University Museum of Norway, Tromsø, N-9037, Norway Cited By :1 Export Date: 27 February 2023 Correspondence Address: Smyčka, J.; Univ. Grenoble Alpes, France; email: smyckaj@gmail.com AB - Here, the authors use full-plastome phylogenomics and multiclade comparative models to reconstruct the tempo and drivers of six European Alpine angiosperm lineages before and during the Pleistocene. They find that geographic divergence and bedrock shifts drive speciation events, while diversification rates remained steady.There is still limited consensus on the evolutionary history of species-rich temperate alpine floras due to a lack of comparable and high-quality phylogenetic data covering multiple plant lineages. Here we reconstructed when and how European alpine plant lineages diversified, i.e., the tempo and drivers of speciation events. We performed full-plastome phylogenomics and used multi-clade comparative models applied to six representative angiosperm lineages that have diversified in European mountains (212 sampled species, 251 ingroup species total). Diversification rates remained surprisingly steady for most clades, even during the Pleistocene, with speciation events being mostly driven by geographic divergence and bedrock shifts. Interestingly, we inferred asymmetrical historical migration rates from siliceous to calcareous bedrocks, and from higher to lower elevations, likely due to repeated shrinkage and expansion of high elevation habitats during the Pleistocene. This may have buffered climate-related extinctions, but prevented speciation along elevation gradients as often documented for tropical alpine floras. LA - English DB - MTMT ER - TY - JOUR AU - Stancikaite, Migle AU - Zernitskaya, Valentina AU - Kluczynska, Grazyna AU - Valunas, Darius AU - Gedminiene, Laura AU - Uogintas, Domas AU - Skuratovic, Zana AU - Vlasov, Boris AU - Gasteviciene, Neringa AU - Ezerinskis, Zilvinas AU - Sapolaite, Justina AU - Seiriene, Vaida TI - The Lateglacial and Early Holocene vegetation dynamics: New multi-proxy data from the central Belarus JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 630 PY - 2022 SP - 121 EP - 136 PG - 16 SN - 1040-6182 DO - 10.1016/j.quaint.2021.05.004 UR - https://m2.mtmt.hu/api/publication/33000461 ID - 33000461 N1 - Funding Agency and Grant Number: Research Council of Lithuania [S-MIP-17-133]; State Program of Scientific Research in Belarus "Natural resources and the environment" (SPSR) [1.03] Funding text: The authors are indebted to anonymous reviewers for constructive comments and remarks on the manuscript. Investigations were financed by the grant (No. S-MIP-17-133) from the Research Council of Lithuania and State Program of Scientific Research in Belarus "Natural resources and the environment" (SPSR No.1.03). AB - Detailed knowledge of the periglacial flora is essential to assess the vegetation dynamics in deglaciated regions of northern and north eastern Europe, previously covered by the ice sheet of the Late Weichselian Glaciation. Therefore, the territory of Belarus, which stretches in the periglacial zone of the Last Glaciation and the most part of which was free of ice during the Last Glacial maximum, is off particular importance in analysing the post-glacial floral establishment and the subsequent vegetation dynamics in this part of the continent. In this study, results of palaeobotanical (pollen and plant macrofossil), lithological (measurements of magnetic susceptibility, MS) and isotopic (C-14) investigations were obtained to fill the existing gap in reconstructing the peculiarities of the terrestrial and aquatic vegetation dynamics throughout the Lateglacial - Early Holocene period in the central Belarus. The investigated sediment profile, comprising organically enriched gyttja at 13,400-13,100 cal yr BP, carbon enriched and sandy gyttja at 13,100-9700 cal yr BP and unconsolidated mud after 9500 cal yr BP, provides clear evidence proving the flourishing of a pine-birch predominated forest with occasional spruce stands during the Allerod in area. Three occasions of change in the vegetation structure were noted within the Younger Dryas, i.e. 12,900-12,700 cal yr BP, 12,200-12,000 cal yr BP and 11,900-11,700 cal yr BP, suggesting negative climatic excursion taken place in area and facilitating flourishing of a Picea-predominating forest that culminated at about 12,300 and 12,000 cal yr BP. Pollen record suggests the Early Holocene vegetation shifts occurring at about 11,300-11,200 cal yr BP, 10,800-10,600 cal yr BP and 10,300-10,100 cal yr BP evidence the general response to the global-scale climatic events i.e. Preborael Oscillation or "10,2 ka " while fluctuations triggered by local or regional-scale climatic events have been identified as well. About 10,800-10,700 cal yr BP, formation of the forest with an increasing representation of thermophilous taxa (Ulmus, Tilia, Quercus) started in area. LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Molnár, Dávid AU - Náfrádi, Katalin AU - Makó, László AU - Cseh, Péter AU - Törőcsik, Tünde AU - Molnár, Mihály AU - Zhou, Liping TI - Vegetation and land snail-based reconstruction of the palaeocological changes in the forest steppe eco-region of the Carpathian Basin during last glacial warming JF - GLOBAL ECOLOGY AND CONSERVATION J2 - GLOB ECOL CONSERV VL - 33 PY - 2022 PG - 28 SN - 2351-9894 DO - 10.1016/j.gecco.2021.e01976 UR - https://m2.mtmt.hu/api/publication/32544836 ID - 32544836 N1 - Funding Agency and Grant Number: Hungarian Government, Ministry of Human Capacities [20391-3/2018/FEKUSTRAT]; European Regional Development Fund [GINOP-2.3.2-15-2016-00009 'ICER']; University of Szeged Open Access Fund [5386]; Hungarian National Excellence Programme grant [NTP-NFTOd-19-B-0158] Funding text: This research was supported by the Hungarian Government, Ministry of Human Capacities (20391-3/2018/FEKUSTRAT) and the European Regional Development Fund (GINOP-2.3.2-15-2016-00009 'ICER') and the University of Szeged Open Access Fund (no. 5386) . D. Molnar would like to thank the support of the Hungarian National Excellence Programme grant (NTP-NFTOd-19-B-0158) . LA - English DB - MTMT ER - TY - JOUR AU - Szatmari, P-M AU - Hurdu, B-I TI - Low altitude glacial relicts in the Romanian flora JF - CONTRIBUTII BOTANICE J2 - CONTR BOTANICE VL - 57 PY - 2022 SP - 19 EP - 51 PG - 33 SN - 0069-9616 DO - 10.24193/Contrib.Bot.57.2 UR - https://m2.mtmt.hu/api/publication/33538348 ID - 33538348 N1 - Babeș-Bolyai University, Biological Research Center-Botanic Garden “Vasile Fati”, 16, Wesselényi Miklós St., Jibou, RO-455200, Romania Babeș-Bolyai University, Faculty of Biology and Geology, Doctoral School of Integrative Biology, 44, Republicii St., Cluj-Napoca, RO-400015, Romania Institute of Biological Research Cluj-Napoca, National Institute for Research and Development in Biological Sciences, 48, Republicii St., Cluj-Napoca, RO-400015, Romania Export Date: 3 January 2023 Correspondence Address: Hurdu, B.-I.; Institute of Biological Research Cluj-Napoca, 48, Republicii St., Romania; email: bogdan.hurdu@icbcluj.ro AB - Glacial relicts represent isolated populations of cold-adapted species, remnants of their past extensive distribution at southern latitudes that have survived in situ far from their current main areal since the Ice Age ended. We hereby aim to identify, based on a numerical evaluation that uses a scoring system applied for 14 ecological and biogeographic criteria, putative glacial relicts occurring in lowland wetlands from the Romanian part of the Carpathian Region. Our selection of (sub) species for evaluation includes mainly cold-adapted plants occurring in wetland areas of the intra-mountain depressions and peripheral lowland areas, while those occurring mostly in the high mountain areas of the Carpathians were excluded. As a result, of 171 evaluated taxa, 74 are considered to possess stronger lowland glacial relict features in the Romanian flora. Furthermore, based on the evaluation of their distribution in Romania, we highlight the hotspots of richness, rarity and range limit for these taxa. Both richness and rarity indices calculated for the 74 glacial relicts displayed the highest values in the Eastern Carpathians, probably linked to the wider development in this region of intra-mountain depressions harboring extensive wetlands. In addition, several potential refugia have been identified based on the distribution of very rare taxa in the north-eastern part of the Apuseni Mountains and the eastern part of the Southern Carpathians (Bucegi Mountains). The distribution of range limit populations of glacial relicts in Romania outlines two well-demarcated areas, one in the southern part of the Eastern Carpathians and the second in the western part of the Southern Carpathians, along deep intra-mountain valleys and depressions. Due to their limited, isolated distribution and the fragility of wetland habitats in which they occur, populations of glacial relicts are more prone to be affected by impacts generated by human activities and climate change. Therefore, our study can also serve as a useful tool for enhancing conservation efforts by highlighting the lowland wetland areas harboring a high number of cold-adapted relict populations that require careful monitoring and urgent protection measures. LA - English DB - MTMT ER - TY - JOUR AU - Tóth, Mónika AU - Heiri, O AU - Vincze, Ildikó AU - Braun, Mihály AU - Szabó, Zoltán AU - Magyari, Enikő Katalin TI - Limnological changes and chironomid-inferred summer air temperature from the Late Pleniglacial to the Early Holocene in the East Carpathians JF - QUATERNARY RESEARCH J2 - QUATERNARY RES VL - 105 PY - 2022 SP - 151 EP - 165 PG - 15 SN - 0033-5894 DO - 10.1017/qua.2021.36 UR - https://m2.mtmt.hu/api/publication/32133278 ID - 32133278 LA - English DB - MTMT ER - TY - JOUR AU - Bertran, P AU - Bosq, M AU - Borderie, Q AU - Coussot, C AU - Coutard, S AU - Deschodt, L AU - Franc, O AU - Gardère, P AU - Liard, M AU - Wuscher, P TI - Revised map of European aeolian deposits derived from soil texture data JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 266 PY - 2021 IS - 3 PG - 16 SN - 0277-3791 DO - 10.1016/j.quascirev.2021.107085 UR - https://m2.mtmt.hu/api/publication/32102652 ID - 32102652 N1 - Inrap, 140 Avenue du Maréchal Leclerc, Bègles, 33130, France PACEA, Université de Bordeaux-CNRS, Bâtiment B2, Allée Geoffroy-Saint-Hilaire, Pessac, 33605, France Direction de l'aménagement, Conseil départemental d'Eure-et-Loir, Chartres, 28028, France Inrap, 3-5 Rue René Cassin, Chartres, 28000, France UMR 8591 CNRS, Laboratoire de Géographie Physique, Environnements Quaternaires et Actuels, 1 Place A. Briand, Meudon, Cedex, 92195, France Inrap, 32 Avenue de l'Etoile du Sud, Glisy, 80440, France Inrap, 11 Rue des Champs, Villeneuve-d'Ascq, 59650, France Inrap, 12 Rue MaggioriniBron 69500, France Inrap, 148 Avenue André Maginot, Tours, 37100, France UMR 7324 CNRS Citères – LAT, 35 Allée Ferdinand de Lesseps, Tours, 37200, France Inrap, 525 Avenue de la Pomme de PinSaint-Cyr-en-Val 45590, France Archéologie Alsace, 11 Rue Jean-François Champollion, Sélestat, 67600, France Laboratoire Image Ville Environnement, Université de Strasbourg-CNRS, 3 Rue de l'ArgonneStrasbourg 67000, France Cited By :3 Export Date: 25 May 2022 CODEN: QSRED Correspondence Address: Bertran, P.; Inrap, 140 Avenue du Maréchal Leclerc, France; email: pascal.bertran@inrap.fr LA - English DB - MTMT ER - TY - JOUR AU - Degen, Bernd AU - Yanbaev, Yulai AU - Mader, Malte AU - Ianbaev, Ruslan AU - Bakhtina, Svetlana AU - Schroeder, Hilke AU - Blanc-Jolivet, Celine TI - Impact of Gene Flow and Introgression on the Range Wide Genetic Structure of Quercus robur (L.) in Europe JF - FORESTS J2 - FORESTS VL - 12 PY - 2021 IS - 10 PG - 17 SN - 1999-4907 DO - 10.3390/f12101425 UR - https://m2.mtmt.hu/api/publication/32746070 ID - 32746070 N1 - Funding Agency and Grant Number: Russian Science FoundationRussian Science Foundation (RSF) [19-16-00084]; German Federal Ministry of Food and Agriculture [WKF-WF04-22WC4111 01]; German Federal German Ministry for the Environment, Nature Conservation and Nuclear Safety Funding text: The study was funded through the grant No 19-16-00084 from the Russian Science Foundation (project members: B. Degen, Y. Yanbaev, R. Ianbaev and S. Bakhtina) and by the grant WKF-WF04-22WC4111 01 from the German Federal Ministry of Food and Agriculture and German Federal German Ministry for the Environment, Nature Conservation and Nuclear Safety. AB - As for most other temperate broadleaved tree species, large-scale genetic inventories of pedunculate oak (Quercus robur L.) have focused on the plastidial genome, which showed the impact of post-glacial recolonization and manmade seed transfer. However, how have pollen mediated gene flow and introgression impacted the large-scale genetic structure? To answer these questions, we did a genetic inventory on 1970 pedunculate oak trees from 197 locations in 13 European countries. All samples were screened with a targeted sequencing approach on a set of 381 polymorphic loci (356 nuclear SNPs, 3 nuclear InDels, 17 chloroplast SNPs, and 5 mitochondrial SNPs). In a former analysis with additional 1763 putative Quercus petraea trees screened for the same gene markers we obtained estimates on the species admixture of all pedunculate oak trees. We identified 13 plastidial haplotypes, which showed a strong spatial pattern with a highly significant autocorrelation up to a range of 1250 km. Significant spatial genetic structure up to 1250 km was also observed at the nuclear loci. However, the differentiation at the nuclear gene markers was much lower compared to the organelle gene markers. The matrix of genetic distances among locations was partially correlated between nuclear and organelle genomes. Bayesian clustering analysis revealed the best fit to the data for a sub-division into two gene pools. One gene pool is dominating the west and the other is the most abundant in the east. The western gene pool was significantly influenced by introgression from Quercus petraea in the past. In Germany, we identified a contact zone of pedunculate oaks with different introgression intensity, likely resulting from different historical levels of introgression in glacial refugia or during postglacial recolonization. The main directions of postglacial recolonization were south to north and south to northwest in West and Central Europe, and for the eastern haplotypes also east to west in Central Europe. By contrast, the pollen mediated gene flow and introgression from Q. petraea modified the large-scale structure at the nuclear gene markers with significant west-east direction. LA - English DB - MTMT ER - TY - JOUR AU - Longo, Laura AU - Altieri, Simona AU - Birarda, Giovanni AU - Cagnato, Clarissa AU - Graziani, Valerio AU - Obada, Theodor AU - Pantyukhina, Irina AU - Ricci, Paola AU - Skakun, Natalia AU - Sorrentino, Giusi AU - Terekhina, Vera AU - Tortora, Luca AU - Vaccari, Lisa AU - Lubritto, Carmine TI - A Multi-Dimensional Approach to Investigate Use-Related Biogenic Residues on Palaeolithic Ground Stone Tools JF - ENVIRONMENTAL ARCHAEOLOGY J2 - ENVIRON ARCHAEOL PY - 2021 PG - 29 SN - 1461-4103 DO - 10.1080/14614103.2021.1975252 UR - https://m2.mtmt.hu/api/publication/32746071 ID - 32746071 N1 - Funding Agency and Grant Number: Elettra-Sincrotrone Trieste [20170057]; Singapore, NTU [M4081669.090]; Russian Academy of SciencesRussian Academy of Sciences [0184-2014-0008] Funding text: This work was supported by Elettra-Sincrotrone Trieste: [Proposal Number 20170057]; Singapore, NTU: [Grant Number M4081669.090]; Russian Academy of Sciences: [Grant Number 0184-2014-0008]. AB - Recent advances in the role played by dietary carbohydrates in human food webs during the Palaeolithic highlight that starchy foods were part of the diet well before crop domestication. Although certain plants can be eaten raw, intentional processing such as mechanical reduction using stone tools and thermal treatment readily increases the assimilation of nutrients for metabolic functions and for storing. We present a multi-techniques approach designed to combine micro to nanoscale analyses applied to percussive stones to identify their function using micro-wear traces and use-related biogenic residues. The starch grains extracted from functionally active areas of the ground stone tools were scanned using optical microscopy (OM) down to the nanoscale (SEM) and by applying different spectroscopic and spectrometric techniques like FTIR, ToF-SIMS, and IRMS. The combined analyses carried out at different resolutions - morpho-structural and molecular levels - contribute to an unprecedented methodological refinement regarding the intentional processing of starch-rich plants as early as 40,000 years ago at the boreal latitudes. Our preliminary data on pestles and grinding stones from Early Upper Palaeolithic sites of the Pontic steppe (Moldova and Russia) show the suitability of the analytical techniques involved and also the difficulties encountered in detailing authentication procedures of ancient starch candidates. LA - English DB - MTMT ER - TY - JOUR AU - Maier, A AU - Stojakowits, P AU - Mayr, C AU - Pfeifer, S AU - Preusser, F AU - Zolitschka, B AU - Anghelinu, M AU - Bobak, D AU - Duprat-Oualid, F AU - Einwögerer, T AU - Hambach, U AU - Händel, M AU - Kaminská, L AU - Kämpf, L AU - Łanczont, M AU - Lehmkuhl, F AU - Ludwig, P AU - Magyari, Enikő Katalin AU - Mroczek, P AU - Nemergut, A AU - Nerudová, Z AU - Niţă, L AU - Polanská, M AU - Połtowicz-Bobak, M AU - Rius, D AU - Römer, W AU - Simon, U AU - Škrdla, P AU - Újvári, Gábor AU - Veres, D TI - Cultural evolution and environmental change in Central Europe between 40 and 15 ka JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 581-582 PY - 2021 SP - 225 EP - 240 PG - 16 SN - 1040-6182 DO - 10.1016/j.quaint.2020.09.049 UR - https://m2.mtmt.hu/api/publication/31969601 ID - 31969601 N1 - Funding Agency and Grant Number: Friedrich-Alexander-Universitat Erlangen-Nurnberg Funding text: We thank the Friedrich-Alexander-Universitat Erlangen-Nurnberg for funding a workshop on the Last Glacial Maximum in Europe, which sparked the idea for this article and Robin John (University of Cologne) for graphic support. We also thank Olaf Joris (Archaologisches Forschungszentrum und Museum fur menschliche Verhaltensevolution Monrepos) and a second anonymous reviewer for constructive comments of the original manuscript. LA - English DB - MTMT ER - TY - JOUR AU - Peresani, M AU - Monegato, G AU - Ravazzi, C AU - Bertola, S AU - Margaritora, D AU - Breda, M AU - Fontana, A AU - Fontana, F AU - Janković, I AU - Karavanić, I AU - Komšo, D AU - Mozzi, P AU - Pini, R AU - Furlanetto, G AU - Maria De Amicis, MG AU - Perhoč, Z AU - Posth, C AU - Ronchi, L AU - Rossato, S AU - Vukosavljević, N AU - Zerboni, A TI - Hunter-gatherers across the great Adriatic-Po region during the Last Glacial Maximum: Environmental and cultural dynamics JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 581-582 PY - 2021 SP - 128 EP - 163 PG - 36 SN - 1040-6182 DO - 10.1016/j.quaint.2020.10.007 UR - https://m2.mtmt.hu/api/publication/31637303 ID - 31637303 N1 - Funding Agency and Grant Number: Ferrara University (FAR2019); Croatian Science Foundation [IP-2019-04-7821] Funding text: This paper is a contribution to the CNR-IGAG research line DTA. AD001.112 -Quaternary paleoenvironments and palaeoclimate. Studies and analyses were supported by the Ferrara University (FAR2019) and by the Croatian Science Foundation (grant no: IP-2019-04-7821). The authors are grateful to Andreas Maier and Christopher Mayr for invitation to the workshop in Erlangen, to Mauro Marchetti (University of Modena and Reggio Emilia) for fruitful discussions on palaeohydrography of the Po Plain and to Federica Badino (University of Bologna) for advices on MIS 3 terrestrial ecology at the southern Italian foreland. The GAPR palaeoenvironmental mapping included in this paper is part of a PhD project developed at University of Ferrara by one of us (D.M.). Authors contributions: M.P. and G.M. conceived the study; S.B. and M.P. produced original petroarchaeological data, A.F., G.M., P. M., L.R., S.R. and A.Z. geomorphological framework, C.R., R.P. and G.F. plant ecological framework, M.B. vertebrate palaeontology framework, M.P., F.F., I.J., I.K. and N.V. cultural framework, S.B., M.P. and Z.P. chert petroarchaeological framework; C.P. curated chapter 6.6; D.M. drawn the maps of figures 1, 2, 3, 9 with inputs by M. DeA., A.F., G.M., P. M., M.P., R.P., C.R., A.Z.; C.R. drawn Fig. 4; DK provided the unpublished radiocarbon date of Pe ' cina Cave near Rovinjsko Selo 1. LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Gulyás, Sándor AU - Molnár, Dávid AU - Bozsó, Gábor AU - Fekete, István AU - Makó, László AU - Cseh, Péter AU - Molnár, Mihály AU - Sümegi, Balázs P. AU - Almond, Peter AU - Zeeden, Christian AU - Törőcsik, Tünde AU - Nett, Janina J. AU - Markó, András AU - Lehmkuhl, Frank TI - New chronology and extended palaeoenvironmental data to the 1975 loess profile of Madaras brickyard, South Hungary JF - JOURNAL OF QUATERNARY SCIENCE J2 - J QUATERNARY SCI VL - 36 PY - 2021 IS - 8 SP - 1364 EP - 1381 PG - 18 SN - 0267-8179 DO - 10.1002/jqs.3382 UR - https://m2.mtmt.hu/api/publication/32471189 ID - 32471189 N1 - Special Issue: Pleistocene geoarchaeology and palaeoenvironments in European loess LA - English DB - MTMT ER - TY - JOUR AU - Szabó, Bence AU - Pazonyi, Piroska AU - Tóth, Emőke AU - Magyari, Enikő Katalin AU - Kiss, Gabriella Ilona AU - Rinyu, László AU - Futó, István AU - Virág, Attila TI - Pleistocene and holocene palaeoenvironmental reconstruction of the carpathian basin based on multiproxy analysis of cervid teeth JF - HISTORICAL BIOLOGY J2 - HIST BIOL VL - 33 PY - 2021 IS - 12 SP - 3307 EP - 3325 PG - 19 SN - 0891-2963 DO - 10.1080/08912963.2020.1863960 UR - https://m2.mtmt.hu/api/publication/31797540 ID - 31797540 N1 - Eötvös Loránd University, Department of Palaeontology, Budapest, Hungary Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Debrecen, Hungary MTA-MTM-ELTE Research Group for Paleontology, Budapest, Hungary Eötvös Loránd University, Department of Environmental and Landscape Geography, Budapest, Hungary Export Date: 29 January 2021 Correspondence Address: Szabó, B.; Eötvös Loránd University, Hungary; email: szabobence.pal@gmail.com Eötvös Loránd University, Department of Palaeontology, Budapest, Hungary Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Debrecen, Hungary MTA-MTM-ELTE Research Group for Paleontology, Budapest, Hungary Eötvös Loránd University, Department of Environmental and Landscape Geography, Budapest, Hungary Export Date: 28 May 2021 Correspondence Address: Szabó, B.; Eötvös Loránd University, Hungary; email: szabobence.pal@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Tapody, Réka Orsolya AU - Sümegi, Pál AU - Molnár, Dávid AU - Karlik, Máté AU - Törőcsik, Tünde AU - Cseh, Péter AU - Makó, László TI - Sedimentological-Geochemical Data Based Reconstruction of Climate Changes and Human Impacts from the Peat Sequence of Round Lake in the Western Foothill Area of the Eastern Carpathians, Romania JF - QUATERNARY J2 - Quaternary VL - 4 PY - 2021 IS - 2 PG - 29 SN - 2571-550X DO - 10.3390/quat4020018 UR - https://m2.mtmt.hu/api/publication/32064831 ID - 32064831 N1 - Department of Geology and Palaeontology, University of Szeged, Egyetem Str. 2-6, Szeged, H-6722, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Bem Square 18/c, Debrecen, H-4026, Hungary Institute for Geological and Geochemical Research, RCAES, Budaörsi Str. 45, Budapest, H-1112, Hungary Export Date: 23 May 2022 Correspondence Address: Sümegi, P.; Department of Geology and Palaeontology, Egyetem Str. 2-6, Hungary; email: sumegi@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - Újvári, Gábor AU - Bernasconi, SM. AU - Stevens, T AU - Kele, Sándor AU - Páll-Gergely, Barna AU - Surányi, Gergely AU - Demény, Attila TI - Stadial‐interstadial temperature and aridity variations in East Central Europe preceding the Last Glacial Maximum JF - PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY J2 - PALEOCEANOGR PALEOCL VL - 36 PY - 2021 IS - 8 PG - 20 SN - 2572-4517 DO - 10.1029/2020PA004170 UR - https://m2.mtmt.hu/api/publication/32131406 ID - 32131406 N1 - Funding Agency and Grant Number: Hungarian National Research, Development, and Innovation OfficeNational Research, Development & Innovation Office (NRDIO) - Hungary [OTKA PD-108639, OTKA KH-125584, OTKA FK-135262]; Bolyai Janos Research Scholarship of the Hungarian Academy of SciencesHungarian Academy of Sciences [BO/00326/15]; Public Limited Company for Radioactive Waste Management, Hungary (RHK Kft.); Swedish Research CouncilSwedish Research CouncilEuropean Commission [2017-03888] Funding text: This study was funded by the Hungarian National Research, Development, and Innovation Office to GU (OTKA PD-108639), SK (OTKA KH-125584), and PGB (OTKA FK-135262). Additional financial support provided by the Bolyai Janos Research Scholarship of the Hungarian Academy of Sciences (BO/00326/15-Gu and BPG) is gratefully acknowledged. The study on the PK-6 flowstone was financially supported by the Public Limited Company for Radioactive Waste Management, Hungary (RHK Kft.). TS is grateful for the support of the Swedish Research Council (2017-03888). Zoltan Kern and Istvan Gabor Hatvani provided essential help with the delta18O-temperature gradient calculations, which is gratefully acknowledged. Constructive and insightful comments of three anonymous reviewers improved the paper substantially. LA - English DB - MTMT ER - TY - THES AU - Večeřa, M TI - Diversity patterns in European vegetation: Linking community ecology and macroecology PY - 2021 UR - https://m2.mtmt.hu/api/publication/32498048 ID - 32498048 LA - English DB - MTMT ER - TY - JOUR AU - Velasquez, P AU - Kaplan, JO. AU - Messmer, M AU - Ludwig, P AU - Raible, CC. TI - The role of land cover in the climate of glacial Europe JF - CLIMATE OF THE PAST J2 - CLIM PAST VL - 17 PY - 2021 IS - 3 SP - 1161 EP - 1180 PG - 20 SN - 1814-9324 DO - 10.5194/cp-17-1161-2021 UR - https://m2.mtmt.hu/api/publication/32076826 ID - 32076826 N1 - Funding Agency and Grant Number: Schweizerischer Nationalfonds zur Forderung der Wissenschaftlichen ForschungAustrian Science Fund (FWF) [200021-162444, P2BEP_181837] Funding text: This research has been supported by the Schweizerischer Nationalfonds zur Forderung der Wissenschaftlichen Forschung (grant nos. 200021-162444 and P2BEP_181837). LA - English DB - MTMT ER - TY - JOUR AU - Badino, F AU - Pini, R AU - Bertuletti, P AU - Ravazzi, C AU - Delmonte, B AU - Monegato, G AU - Reimer, P AU - Vallé, F AU - Arrighi, S AU - Bortolini, E AU - Figus, C AU - Lugli, F AU - Maggi, V AU - Marciani, G AU - Margaritora, D AU - Oxilia, G AU - Romandini, M AU - Silvestrini, S AU - Benazzi, S TI - The fast-acting “pulse” of Heinrich Stadial 3 in a mid-latitude boreal ecosystem JF - SCIENTIFIC REPORTS J2 - SCI REP VL - 10 PY - 2020 IS - 1 SN - 2045-2322 DO - 10.1038/s41598-020-74905-0 UR - https://m2.mtmt.hu/api/publication/31648339 ID - 31648339 N1 - Department of Cultural Heritage, University of Bologna, Ravenna, 48121, Italy Research Group on Vegetation, Climate and Human Stratigraphy, Laboratory of Palynology and Palaeoecology, CNR-Institute of Environmental Geology and Geoengineering (IGAG), Milan, 20126, Italy Department of Environmental and Earth Sciences, University of Milano-Bicocca, Milan, 20126, Italy CNR-Institute of Geosciences and Earth Resources (IGG), Padua, 35131, Italy School of Natural and Built Environment, Queen’s University Belfast, Belfast, BT7 1NN, United Kingdom Dipartimento di Scienze Fisiche, della Terra e dell’Ambiente, Università di Siena, Siena, 53100, Italy Dipartimento di Scienze Chimiche e Geologiche, Università di Modena e Reggio Emilia, Modena, 41125, Italy Dipartimento di Studi Umanistici, Sezione di Scienze Preistoriche e Antropologiche, Università di Ferrara, Ferrara, 44100, Italy Department of Human Evolution Max Planck Institute for Evolutionary Anthropology, Leipzig, 04103, Germany Cited By :4 Export Date: 25 May 2022 Correspondence Address: Badino, F.; Department of Cultural Heritage, Italy; email: federica.badino@unibo.it LA - English DB - MTMT ER - TY - JOUR AU - Gałka, Mariusz AU - Tantau, Ioan AU - Carter, Vachel A. AU - Feurdean, Angelica TI - The Holocene dynamics of moss communities in subalpine wetland ecosystems in the Eastern Carpathian Mountains, Central Europe JF - BRYOLOGIST J2 - BRYOLOGIST VL - 123 PY - 2020 IS - 1 SP - 84 EP - 97 PG - 14 SN - 0007-2745 DO - 10.1639/0007-2745-123.1.084 UR - https://m2.mtmt.hu/api/publication/31251874 ID - 31251874 N1 - Export Date: 26 April 2022 CODEN: BRYOA Correspondence Address: Gałka, M.; University of Lodz, 12/16 Banacha Str., Poland; email: mariusz.galka@biol.uni.lodz.pl LA - English DB - MTMT ER - TY - JOUR AU - Haesaerts, P. AU - Gerasimenko, N. AU - Damblon, F. AU - Yurchenko, T. AU - Kulakovska, L. AU - Usik, V AU - Ridush, B. TI - The Upper Palaeolithic site Doroshivtsi III: A new chronostratigraphic and environmental record of the Late Pleniglacial in the regional context of the Middle Dniester-Prut loess domain (Western Ukraine) JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 546 PY - 2020 SP - 196 EP - 215 PG - 20 SN - 1040-6182 DO - 10.1016/j.quaint.2019.12.018 UR - https://m2.mtmt.hu/api/publication/31434574 ID - 31434574 N1 - Royal Belgian Institute of Natural Sciences, Vautier str. 29, Brussels, B-1000, Belgium Taras Shevshenko National University of Kyiv, Department of Earth Sciences and Geomorphology, Volodymyrska str. 64/13, Kyiv, 01601, Ukraine Institute of Archaeology of National Academy of Sciences of Ukraine, pr. Geroiv Stalingrada 12, Kyiv, 04210, Ukraine Yuriy Fedkovych National University of Chernivtsi, Department of Physical Geography, Geomorphology and Paleogeography, Kotsubynskogo str. 2, Chernivtsi, 58012, Ukraine Cited By :11 Export Date: 25 May 2022 Correspondence Address: Gerasimenko, N.; Earth Science and Geomorphology Department, Akademika Glushkova ave. 2, Ukraine; email: n.garnet2@gmail.com AB - A multidisciplinary study of the Upper Palaeolithic site Doroshivtsi III (Western Ukraine) allows the establishment of a high-resolution chronostratigraphic and environmental record of short climatic oscillations during the Late Pleniglacial (from ca. 23 ka uncal BP to the Late Glacial). Chronostratigraphic records, radiocarbon dating, palynology and anthracology were used in parallel with archaeological studies. Palaeoenvironmental interpretations based on pedostratigraphy and pollen data show a remarkable concordance. The Doroshivtsi III sequence provides a succession of 12 short-time interstadial events. In the lower part of the sequence, they are separated by very cold and wet stadials, represented by tundra gleys. In the middle part of the sequence, interstadial events are separated by episodes of loess accumulation under cold and dry climate, whereas the upper part of the sequence almost completely consists of loesses. The sum of pollen of arcto-alpine and arcto-boreal plants was the largest during the periods of tundra gley formation, whereas few pollen grains of broad-leaved taxa occurred during formation of some soil horizons. The latter allows the preliminary suggestion that during the Late Pleniglacial some temperate trees persisted to the south from the Middle Dniester Valley. The Doroshivtsi III sequence is well correlated with the other East Carpathian records (Molodova, Mitoc and Cosautsi), and allows the establishment of a very complete record of climatic oscillations in this area from 33 ka BP to the beginning of the Holocene. It also provides a link for the correlation with the interstadial events 8 to 1 of the Greenland Ice Sequence. LA - English DB - MTMT ER - TY - JOUR AU - Horsak, Michal AU - Limondin-Lozouet, Nicole AU - Granai, Salome AU - Dabkowski, Julie AU - Divisek, Jan AU - Hajkova, Petra TI - Colonisation dynamic and diversity patterns of Holocene forest snail fauna across temperate Europe: The imprint of palaeoclimate changes JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 240 PY - 2020 PG - 13 SN - 0277-3791 DO - 10.1016/j.quascirev.2020.106367 UR - https://m2.mtmt.hu/api/publication/31463346 ID - 31463346 N1 - Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, 611 37, Czech Republic CNRS, Université Paris 1, UPEC, UMR 8591, Laboratoire de Géographie Physique, 1 Place Aristide Briand, Meudon Cedex, 92195, France GéoArchéon, 30 rue de la Victoire, Viéville-sous-les-Côtes55210, France Department of Geography, Masaryk University, Kotlářská 2, Brno, 611 37, Czech Republic Laboratory of Paleoecology, Institute of Botany, The Czech Academy of Sciences, Lidická 25/27, Brno, 602 00, Czech Republic Cited By :2 Export Date: 25 May 2022 CODEN: QSRED Correspondence Address: Horsák, M.; Department of Botany and Zoology, Kotlářská 2, Czech Republic; email: horsak@sci.muni.cz AB - The development of biotic communities since the last glaciation has been shaped by both dramatic climate changes and pathways of species colonisation from glacial refugia. Although the growing body of literature has emerged recently on possible scenarios of postglacial colonisation, less is known about the effect of climate. We analysed the dynamics of Holocene mollusc succession with an undetected human impact using three well-dated sequences from spring tufa deposits across temperate Europe. For the first time, the detailed Holocene mollusc successions can be compared with climate parameters in the corresponding time windows. High-resolution palaeoclimate data accompanied the species data, and the data derived from stable isotope analyses. The number of closed-canopy forest species that colonised the sites until 5000 cal BP and the maximum number of species per sample systematically increased towards the interior of the continent. We also observed earlier colonisation of forest snail species in the Western Carpathians. While the aridity index was the best predictor of local species richness in Normandy and Luxembourg, minimum January temperature drove the variation in snail data in Slovakia. The short period of an abrupt cooling and drying around 8500 cal BP was found to stop the colonisation, sharply reducing the number of local species across the continent. Our results document the importance of climate for the colonisation and development of forest biota during the first half of the Holocene, both at continental and local scales. They also elucidate processes shaping the current distribution of forest snail fauna across the European temperate zone. (C) 2020 Elsevier Ltd. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Jakovljevic, Ksenija AU - Tomovic, Gordana AU - Djordjevic, Vladan AU - Niketic, Marjan AU - Stevanovic, Vladimir TI - Steppe flora in Serbia - distribution, ecology, centres of diversity and conservation status JF - FOLIA GEOBOTANICA J2 - FOLIA GEOBOT VL - 55 PY - 2020 IS - 1 SP - 1 EP - 14 PG - 14 SN - 1211-9520 DO - 10.1007/s12224-019-09361-4 UR - https://m2.mtmt.hu/api/publication/31454382 ID - 31454382 N1 - Institute of Botany and Botanical Garden ‘Jevremovac’, University of Belgrade, Takovska 43, Belgrade, 11000, Serbia Natural History Museum, Njegoševa 51, Belgrade, 11000, Serbia Export Date: 5 May 2021 Correspondence Address: Jakovljević, K.; Institute of Botany and Botanical Garden ‘Jevremovac’, Takovska 43, Serbia; email: kjakovljevic@bio.bg.ac.rs AB - The steppe flora and vegetation represents a significant part of the Eurasian temperate grassland biome. In Serbia, this flora is a part of the biome's western border zone and its characteristics therefore may be modified. The aim of this study was to determine the number of steppe taxa in Serbia and to conduct a chorological and ecological analysis of this flora. The results of diversity analysis and summary distribution of steppe taxa were presented on 50 x 50 km grids using the Universal Transverse Mercator projection. Regression analysis was used to explore the relationship between steppe species richness and the altitude. Floristic similarity between the geographical groups were analysed using the clustering method and species fidelity to each cluster was calculated. The species conservation status is also presented. In total, the presence of 233 steppe taxa in the investigated area was recorded. The most frequent families are Asteraceae, Fabaceae, Poaceae and Caryophyllaceae with Dianthus, Astragalus, Allium, Stipa, Cytisus, Centaurea and Silene as genera that contribute the most to steppe flora in Serbia. According to the chorological and life form spectra, Pontic European taxa and hemicryptophytes are the most numerous. Geological substrate like loess, sand, and other unbound sediment, as well as the lower altitudinal ranges proved to be most suitable for the development of steppe flora in Serbia. The distribution of steppe flora in Serbia indicates Deliblato Sand and Mt Fruska Gora as centres of diversity. The study suggests that the cumulative effect of environmental factors is important to consider in the planning of steppe species conservation. LA - English DB - MTMT ER - TY - JOUR AU - Lisztes-Szabó, Zsuzsa AU - Filep, Anna Fruzsina AU - Csík, Attila AU - Pető, Ákos AU - Kertész, Gréta Titanilla AU - Braun, Mihály TI - pH-dependent silicon release from phytoliths of Norway spruce (Picea abies) JF - JOURNAL OF PALEOLIMNOLOGY J2 - J PALEOLIMNOL VL - 63 PY - 2020 IS - 1 SP - 65 EP - 81 PG - 17 SN - 0921-2728 DO - 10.1007/s10933-019-00103-2 UR - https://m2.mtmt.hu/api/publication/30947384 ID - 30947384 N1 - Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Hungarian Academy of Sciences, Debrecen, Hungary Institute for Nuclear Research, Hungarian Academy of Sciences, Debrecen, Hungary Institute of Nature Conservation and Landscape Management, Szent István University, Gödöllő, Hungary Export Date: 9 December 2019 CODEN: JOUPE Correspondence Address: Lisztes-Szabó, Z.; Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Hungarian Academy of SciencesHungary; email: lisztes-szabo.zsuzsanna@atomki.mta.hu LA - English DB - MTMT ER - TY - JOUR AU - Molnár, Ábel Péter AU - Demeter, László TI - Egy Kárpát-medencei síkság–hegység flóragrádiens – A Tisza és a Bihar-csúcs közötti gyepek jellemzése, zonációs és vegetációtörténeti kontextusba helyezése = A lowland–mountain floristic gradient from the Carpathian Basin – The characterization of grasslands between the Tisza River and the Bihor Peak, and their positioning in a zonation and vegetation history context JF - CRISICUM: A KÖRÖS - MAROS NEMZETI PARK IGAZGATÓSÁG IDŐSZAKI KIADVÁNYA J2 - CRISICUM VL - 2020 PY - 2020 IS - 11 SP - 7 EP - 40 PG - 33 SN - 1419-2853 UR - https://m2.mtmt.hu/api/publication/31786740 ID - 31786740 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Steiner, Bigna L. AU - Alonso, Natalia AU - Grillas, Patrick AU - Jorda, Christophe AU - Piques, Gael AU - Tillier, Margaux AU - Rovira, Nuria TI - Languedoc lagoon environments and man: Building a modern analogue botanical macroremain database for understanding the role of water and edaphology in sedimentation dynamics of archaeobotanical remains at the Roman port ofLattara(Lattes, France) JF - PLOS ONE J2 - PLOS ONE VL - 15 PY - 2020 IS - 6 PG - 25 SN - 1932-6203 DO - 10.1371/journal.pone.0234853 UR - https://m2.mtmt.hu/api/publication/31485073 ID - 31485073 N1 - Department of Environmental Sciences, Integrative Prehistory and Archaeological Science (IPAS), University of Basel, Basel, Switzerland Archéologie des Sociétés Méditerranéennes (ASM), UMR5140, CNRS, Paul Valéry University of Montpellier, Montpellier, France Departament d'História, Grup d'Investigaciò Prehistòrica, Universitat de Lleida, Lleida, Catalonia, Spain Tour du Valat, Research Institute for the Conservation of Mediterranean Wetlands, Arles, France Inrap-Méditerranée, Parc Actipolis, Villeneuve-lès-Béziers, France Institut des Sciences de l'Evolution de Montpellier (ISEM), Montpellier, France Export Date: 25 May 2022 CODEN: POLNC Correspondence Address: Steiner, B.L.; Department of Environmental Sciences, Switzerland; email: bigna.steiner@unibas.ch AB - A new method to evaluate archaeological wetland sites in a more objective way was tested. Different wetland environments have been sampled in areas of a nature reserve and their macroremain content analysed to build a modern analogue dataset. This dataset was then used to characterise archaeological samples from a navigation channel from the Roman port cityLattara. In the modern analogue samples, the different wetland types (saline/brackish or fresh water) could be differentiated in the correspondence analysis. Within these groups, the sampled area of the littoral (submerged, shoreline, unsubmerged) could also be differentiated. This dataset can therefore provide a basis for the interpretation of the nature and degree of aquatic influence and layer formation processes in archaeobotanical records of coastal sites. In the tested archaeological samples from the navigation channel ofLattara, changes in space and time could be tracked using the modern analogue dataset and geoarchaeological information. The channel lost its fresh water supply and silted up over a short period of time (approx. 100 years). LA - English DB - MTMT ER - TY - CHAP AU - Sümegi, Pál AU - Náfrádi, Katalin AU - Törőcsik, Tünde AU - Jakab, Gusztáv AU - Bodor, Elvira AU - Molnár, Mihály AU - Pál Sümegi, Balázs AU - Tapody, Réka Orsolya AU - Knipl, István AU - Kustár, Rozália AU - Bánffy, Eszter ED - Bánffy, Eszter TI - Prehistoric environment of the Sárköz region in the Danube Valley, Southern Hungary. case studies from infilled oxbow lakes TS - case studies from infilled oxbow lakes T2 - The environmental history of the prehistoric Sárköz region in Southern Hungary PB - Magyar Tudományos Akadémia Bölcsészettudományi Kutatóközpont Régészeti Intézet CY - Langenweissbach SN - 9783957411334 T3 - Confinia et horizontes ; 1. PY - 2020 SP - 83 EP - 159 PG - 77 UR - https://m2.mtmt.hu/api/publication/31780003 ID - 31780003 LA - English DB - MTMT ER - TY - JOUR AU - Tugya, Beáta AU - Náfrádi, Katalin AU - Gulyás, Sándor AU - Törőcsik, Tünde AU - Sümegi, Balázs Pál AU - Pomázi, Péter AU - Sümegi, Pál TI - Environmental Historical Analysis of the Sarmatian and Gepids Settlement of Rákóczifalva JF - ACTA ARCHAEOLOGICA ACADEMIAE SCIENTIARUM HUNGARICAE J2 - ACTA ARCHAEOL ACAD SCI HUNG VL - 71 PY - 2020 IS - 1 SP - 101 EP - 156 PG - 56 SN - 0001-5210 DO - 10.1556/072.2020.00005 UR - https://m2.mtmt.hu/api/publication/31623610 ID - 31623610 AB - We present the results of the environmental historical and geoarchaeological analysis of Rákóczifalva-Bagiföldek and Rákóczifalva-Rokkant-földek archeological sites in Jász-Nagykun-Szolnok County. They were discovered in the course of several hectares of archaeological excavations related to the Roman Age and Migration Period, especially the Sarmatian and the Gepids era. A significant number of Gepids sites and finds were found in both the investigated areas and the wider area of the site, in the middle reach of the Tisza valley. So the geoarchaeological and environmental historical analysis of the Sarmatian and Late-Sarmatian and Gepids sites in Rákóczifalva can also provide a model for the settling strategy and lifestyle of the Sarmatian and Gepids communities. The purpose of our work is to present how geoarchaeological and environmental historical factors impacted local settling and lifestyles in the Gepids communities and Sarmatian-Late Sarmatian communities as well during the Roman Age and the Migration Period. In addition, to demonstrate the relationship of the Sarmatian and Gepids communities and their environment in the Rákóczifalva site compared to other Gepids and Sarmatian and Late Sarmatian communities in the Great Hungarian Plain. Based on the number of objects containing animal bones and the amount of bones found in them, we can reconstruct considerable settling in the Celtic, Sarmatian, Gepids, Avar and Arpadian periods. The number of objects from the Linear Pottery culture (Great Hungarian Plain) and the Bodrogkeresztúr culture is high; however, the number of animal bones is low. On the basis of the bones discovered, we can count on a smaller settlement during the Tiszapolgár culture, the Hunyadihalom group, the Halomíros culture, the Gava culture and during the Scythians period. In this paper, we present the results of the Sarmatian, Late Sarmatian and the Gepid findings since the largest number of animal bones (except the Avar period) turned up from these periods. Our aim was to compare the animal husbandry, meat consumption and hunting habits of the Oriental origin Sarmatians and the Germanic Gepids communities. Bone artefacts and bone anvils have been found in the archaeological material of both ethnic groups. LA - English DB - MTMT ER - TY - JOUR AU - Buró, Botond AU - Lóki, József AU - Győri, Erika AU - Nagy, Richárd AU - Molnár, Mihály AU - Négyesi, Gábor TI - New radiocarbon data from the paleosols of the Nyírség blown sand area, Hungary JF - RADIOCARBON J2 - RADIOCARBON VL - 61 PY - 2019 IS - 6 SP - 1983 EP - 1995 PG - 13 SN - 0033-8222 DO - 10.1017/RDC.2019.137 UR - https://m2.mtmt.hu/api/publication/30933157 ID - 30933157 N1 - Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Hungarian Academy of Sciences, Bem tér 18/c., Debrecen, H-4026, Hungary Department of Physical Geography and Geoinformatics, University of Debrecen, Debrecen, Hungary Export Date: 10 January 2020 CODEN: RACAA Correspondence Address: Buró, B.; Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Hungarian Academy of Sciences, Bem tér 18/c., Hungary; email: bbotond86@gmail.com Part number: 2 Isotope Climatology and Environmental Research Centre (ICER), Institute for Nuclear Research, Hungarian Academy of Sciences, Bem tér 18/c., Debrecen, H-4026, Hungary Department of Physical Geography and Geoinformatics, University of Debrecen, Debrecen, Hungary Export Date: 22 February 2021 CODEN: RACAA Correspondence Address: Buró, B.; Isotope Climatology and Environmental Research Centre (ICER), Bem tér 18/c., Hungary; email: bbotond86@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Chytry, Milan AU - Horsak, Michal AU - Danihelka, Jiri AU - Ermakov, Nikolai AU - German, Dmitry A. AU - Hajek, Michal AU - Hajkova, Petra AU - Koci, Martin AU - Kubesova, Svatava AU - Lustyk, Pavel AU - Nekola, Jeffrey C. AU - Ricankova, Vera Pavelkova AU - Preislerova, Zdenka AU - Resl, Philipp AU - Valachovic, Milan TI - A modern analogue of the Pleistocene steppe-tundra ecosystem in southern Siberia JF - BOREAS J2 - BOREAS VL - 48 PY - 2019 IS - 1 SP - 36 EP - 56 PG - 21 SN - 0300-9483 DO - 10.1111/bor.12338 UR - https://m2.mtmt.hu/api/publication/30542158 ID - 30542158 N1 - Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, 611 37, Czech Republic Institute of Botany of the Czech Academy of Sciences, Zámek 1, Průhonice, 252 43, Czech Republic Nikitsky Botanical Garden, Nikitsky Spusk 52, Nikita, Yalta, Ukraine Department of Biodiversity and Plant Systematics, Centre for Organismal Studies (COS) Heidelberg, Heidelberg University, Im Neuenheimer Feld 345, Heidelberg, 69120, Germany South-Siberian Botanical Garden, Altai State University, Lenina 61, Barnaul, 656049, Russian Federation Laboratory of Paleoecology, Institute of Botany of the Czech Academy of Sciences, Lidická 25/27, Brno, 602 00, Czech Republic Department of Botany, Moravian Museum, Hviezdoslavova 29a, Brno, 627 00, Czech Republic Biology Department, University of New Mexico, Albuquerque, NM 87131, United States Department of Zoology, Faculty of Science, University of South Bohemia, Branišovská 31, České Budějovice, 370 05, Czech Republic Montis Centrum, 330 36, Čerňovice, 238, Czech Republic Institute of Plant Sciences, NAWI Graz, University of Graz, Holteigasse 6, Graz, 8010, Austria Faculty of Biology, Department I, Systematic Botany and Mycology, University of Munich, Menzinger Str. 67, Munich, 80638, Germany Milan Valachovič, Plant Science and Biodiversity Center, Institute of Botany, Slovak Academy of Sciences, Dúbravská cesta 9, Bratislava, 845 23, Slovakia Cited By :31 Export Date: 25 May 2022 Correspondence Address: Chytrý, M.; Department of Botany and Zoology, Kotlářská 2, Czech Republic; email: chytry@sci.muni.cz AB - Steppe-tundra is considered to have been a dominant ecosystem across northern Eurasia during the Last Glacial Maximum. As the fossil record is insufficient for understanding the ecology of this vanished ecosystem, modern analogues have been sought, especially in Beringia. However, Beringian ecosystems are probably not the best analogues for more southern variants of the full-glacial steppe-tundra because they lack many plant and animal species of temperate steppes found in the full-glacial fossil record from various areas of Europe and Siberia. We present new data on flora, land snails and mammals and characterize the ecology of a close modern analogue of the full-glacial steppe-tundra ecosystem in the southeastern Russian Altai Mountains, southern Siberia. The Altaian steppe-tundra is a landscape mosaic of different habitat types including steppe, mesic and wet grasslands, shrubby tundra, riparian scrub, and patches of open woodland at moister sites. Habitat distribution, species diversity, primary productivity and nutrient content in plant biomass reflect precipitation patterns across a broader area and the topography-dependent distribution of soil moisture across smaller landscape sections. Plant and snail species considered as glacial relicts occur in most habitats of the Altaian steppe-tundra, but snails avoid the driest types of steppe. A diverse community of mammals, including many species typical of the full-glacial ecosystems, also occurs there. Insights from the Altaian steppe-tundra suggest that the full-glacial steppe-tundra was a heterogeneous mosaic of different habitats depending on landscape-scale moisture gradients. Primary productivity of this habitat mosaic combined with shallow snow cover that facilitated winter grazing was sufficient to sustain rich communities of large herbivores. LA - English DB - MTMT ER - TY - JOUR AU - Herbert, Hurka AU - Nikolai, Friesen AU - Karl-Georg, Bernhardt AU - Barbara, Neuffer AU - Sergej, Smirnov AU - Alexander, Shmakov AU - Frank, Blattner TI - The Eurasian steppe belt: Status quo, origin and evolutionary history JF - Turczaninowia J2 - Turczaninowia VL - 22 PY - 2019 IS - 3 SP - 5 EP - 71 PG - 67 SN - 1560-7259 DO - 10.14258/turczaninowia.22.3.1 UR - https://m2.mtmt.hu/api/publication/30833952 ID - 30833952 N1 - Department of Botany, University of Osnabrueck, Barbarastrasse 11, Osnabrueck, 49076, Germany Botanical Garden, University of Osnabrueck, Albrechtstr. 29, Osnabrueck, 490776, Germany I. M. Sechenov First Moscow State Medical University, Ministry of Health of the Russian Federation, Department of Pharmaceutical and Natural Sciences, Izmailovsky Boulevard, 8, Moscow, 105043, Russian Federation Institute of Botany, University of Natural Resources and Life Sciences, Vienna, Gregor-Mendel-Straße 33, Vienna, 1180, Austria South-Siberian Botanical Garden, Altai State University, Lenina Str., 61, Barnaul, 656049, Russian Federation Leibniz Institute of Plant Genetics and Crop Plant Research (IPK), Corrensstrasse 3, Gatersleben, 06466, Germany Cited By :12 Export Date: 14 April 2021 LA - English DB - MTMT ER - TY - JOUR AU - Hodková, Eva AU - Doudová, Jana AU - Douda, Jan AU - Krak, Karol AU - Mandák, Bohumil TI - On the road: Postglacial history and recent expansion of the annual Atriplex tatarica in Europe JF - JOURNAL OF BIOGEOGRAPHY J2 - J BIOGEOGR VL - 46 PY - 2019 IS - 11 SP - 2609 EP - 2621 PG - 13 SN - 0305-0270 DO - 10.1111/jbi.13687 UR - https://m2.mtmt.hu/api/publication/30773293 ID - 30773293 N1 - Cited By :3 Export Date: 25 May 2022 CODEN: JBIOD Correspondence Address: Mandák, B.; Faculty of Environmental Sciences, Czech Republic; email: mandak@fzp.czu.cz LA - English DB - MTMT ER - TY - JOUR AU - Houfkova, Petra AU - Horak, Jan AU - Pokorna, Adela AU - Besta, Tomas AU - Pravcova, Ivana AU - Novak, Jan AU - Klir, Tomas TI - The dynamics of a non-forested stand in the Krusne Mts.: the effect of a short-lived medieval village on the local environment JF - VEGETATION HISTORY AND ARCHAEOBOTANY J2 - VEG HIST ARCHAEOBOT VL - 28 PY - 2019 IS - 6 SP - 607 EP - 621 PG - 15 SN - 0939-6314 DO - 10.1007/s00334-019-00718-5 UR - https://m2.mtmt.hu/api/publication/30968646 ID - 30968646 N1 - Laboratory of Archaeobotany and Palaeoecology, Faculty of Science, University of South Bohemia, Branišovská 1760, Ceske Budejovice, 37005, Czech Republic Department of Archaeology, Faculty of Arts, Charles University, Celetná 20, Prague 1, 116 36, Czech Republic Department of Ecology, Faculty of Environmental Sciences, Czech University of Life Sciences, Kamýcká 129, Prague 6, Suchdol 165 21, Czech Republic Institute of Archaeology of the CAS, Prague, v.v.i., Letenská 4, Prague 1, 11801, Czech Republic Department of Botany, Faculty of Science, Charles University in Prague, Benátská 2, Prague 2, 128 01, Czech Republic Institute of Archaeology, Faculty of Philosophy, University of South Bohemia, Branišovská 31a, Ceske Budejovice, 37005, Czech Republic Cited By :6 Export Date: 25 May 2022 Correspondence Address: Houfková, P.; Laboratory of Archaeobotany and Palaeoecology, Branišovská 1760, Czech Republic; email: petra.houfkova@gmail.com AB - Medieval vegetation-human-climate interactions were studied from a sediment profile situated in the centre of a short-lived medieval village located above 800 m a.s.l. on the ridge of the Krusne Mts., NW Bohemia, Central Europe. Analyses of pollen, seeds/fruits, micro- and macro-charcoals, diatoms and concentrations of microelements in connection with written sources revealed a significant human-induced deforestation in the second half of the 14th century. This deforestation occurred sooner than supposed and the area did not revert after ad 1347 as elsewhere in Europe. Arable fields probably enabled basic self-sustaining cultivation of winter cereals even at such elevations in the climatically favourable years of the Medieval Warm Period. The village presumably collapsed due to a combination of weather fluctuations at the onset of the Little Ice Age, simultaneous socioeconomic stagnation in the Czech Lands and exploitation of the surrounding forest. The dynamics of wet stand vegetation and Calthion palustris montane wet meadows were driven by fluctuating human and grazing impacts. Annual and biennial herbaceous species that peaked after village abandonment were rapidly replaced by Filipendula ulmaria and Salix stands. The secondary forest developed towards Picea stands. Only later, mesic montane meadows of medium tall grasses combined with Meum athamanticum and mountain dry pastures developed on nutrient poor patches. LA - English DB - MTMT ER - TY - JOUR AU - Lisztes-Szabó, Zsuzsa AU - Braun, Mihály AU - Csík, Attila AU - Pető, Ákos TI - Phytoliths of six woody species important in the Carpathians: characteristic phytoliths in Norway spruce needles JF - VEGETATION HISTORY AND ARCHAEOBOTANY J2 - VEG HIST ARCHAEOBOT VL - 28 PY - 2019 IS - 6 SP - 649 EP - 662 PG - 14 SN - 0939-6314 DO - 10.1007/s00334-019-00720-x UR - https://m2.mtmt.hu/api/publication/30599658 ID - 30599658 LA - English DB - MTMT ER - TY - JOUR AU - Magyari, Enikő Katalin AU - Pál, Ilona AU - Vincze, Ildikó AU - Veres, D AU - Jakab, Gusztáv AU - Braun, Mihály AU - Szalai, Zoltán AU - Szabó, Zoltán AU - Korponai, János TI - Warm Younger Dryas summers and early late glacial spread of temperate deciduous trees in the Pannonian Basin during the last glacial termination (20-9 kyr cal BP) JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 225 PY - 2019 PG - 22 SN - 0277-3791 DO - 10.1016/j.quascirev.2019.105980 UR - https://m2.mtmt.hu/api/publication/30859762 ID - 30859762 N1 - Szalai Zoltánnál a második affiliáció a szerző közlése alapján Export Date: 28 October 2019 CODEN: QSRED Correspondence Address: Magyari, E.K.; ELTE Department of Environmental and Landscape Geography, Pázmány Péter str. 1/C, Hungary; email: emagyari@caesar.elte.hu Cited By :1 Export Date: 25 November 2019 CODEN: QSRED Correspondence Address: Magyari, E.K.; ELTE Department of Environmental and Landscape Geography, Pázmány Péter str. 1/C, Hungary; email: emagyari@caesar.elte.hu WoS:hiba:000498754500010 2020-08-30 06:06 cikkazonosító nem egyezik AB - This paper focuses on the last glacial termination vegetation and climate reorganization of the Eastern Pannonian Plain via the multi-proxy paleoecological analysis of Kokad mire in Eastern Hungary. Grains size, sediment chemistry and magnetic susceptibility records are compared with the pollen and plant macrofossil records on the basis of which biome and quantitative summer mean temperature reconstructions are provided and discussed with other climate records of the region. Biome assignments indicated (graminoid and forb) tundra vegetation from 19,440 cal yr BP with the local presence of Betula pendula, B. pubescens, B. nana, and Pinus sylvestris. A rapid biome shift to cool coniferous forest took place at 16,200 cal yr BP, and a second biome shift was identified at 14,740 cal yr BP when cool mixed forest developed and persisted into the Early Holocene. The most prominent feature of the record was the early post last glacial maximum (LGM) establishment (17,700 cal yr BP) and expansion (14,700 cal yr BP) of elm (Ulmus) and hazel (Corylus) supporting the phylogeographical evidence for extra-Mediterranean refugia in the Pannonian Basin. The fungal spore record indicated the presence of large grazing mammals locally after the LGM until ∼16,780 cal yr BP. Their disappearance predated the biome shift to cold coniferous forest and the final increase of forest fires. Pollen based summer temperature reconstruction suggested relatively warm summers (∼14.5 °C) by 19,440 cal yr BP, and buffered July mean temperature fluctuations throughout the last glacial termination in this region with < 1 °C decrease in summer mean temperatures during the Younger Dryas stadial, and ∼2.2 °C warming in the Early Holocene. Our comprehensive summary of the basin’s Late Pleniglacial (24,000–14,600 cal yr BP) and late glacial paleoenvironmental and paleoclimate records showed a partially wooded landscape with higher woody cover in Western Hungary. Several loess and lake archives confirmed that in this region of Europe the warming after Heinrich event 1 (around 16,200 cal yr BP) had similar amplitude to the late glacial warming. LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Molnár, Dávid AU - Gulyás, Sándor AU - Náfrádi, Katalin AU - Sümegi, B P AU - Törőcsik, Tünde AU - Persaits, G AU - Molnár, Mihály AU - Vandenberghe, J AU - Zhou, L TI - High-resolution proxy record of the environmental response to climatic variations during transition MIS3/MIS2 and MIS2 in Central Europe. the loess-paleosol sequence of Katymár brickyard (Hungary) TS - the loess-paleosol sequence of Katymár brickyard (Hungary) JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 504 PY - 2019 SP - 40 EP - 55 PG - 16 SN - 1040-6182 DO - 10.1016/j.quaint.2018.03.030 UR - https://m2.mtmt.hu/api/publication/3361435 ID - 3361435 LA - English DB - MTMT ER - TY - JOUR AU - Tóth, Endre György AU - Bede-Fazekas, Ákos AU - Vendramin, G G AU - Bagnoli, F AU - Höhn, Mária Margit TI - Mid-Pleistocene and Holocene demographic fluctuation of Scots pine (Pinus sylvestris L.) in the Carpathian Mountains and the Pannonian Basin: Signs of historical expansions and contractions JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 504 PY - 2019 SP - 202 EP - 213 PG - 12 SN - 1040-6182 DO - 10.1016/j.quaint.2017.11.024 UR - https://m2.mtmt.hu/api/publication/3299580 ID - 3299580 N1 - Funding Agency and Grant Number: European Union's ProCoGen grant [289841]; National Research, Development and Innovation Office, Hungary by Hungarian Scientific Research Fund [OTKA K101600]; [GINOP-2.3.2-15-2016-00019] Funding text: We wish to thank the Editor for helpful comments and the Anonymous Reviewers who helped us improve the manuscript. The authors are also grateful to Tamas Pocs (Hungary), Ivan Iliev (Bulgaria), Tibor Baranec (Slovakia) for collection of plant material and for valuable discussions. GGV and FB were supported by the European Union's ProCoGen grant, under grant agreement no 289841. EGyT and MH was supported by the National Research, Development and Innovation Office, Hungary by the grant of the Hungarian Scientific Research Fund [OTKA K101600]. ABF was supported by the GINOP-2.3.2-15-2016-00019 grant. Country borders were provided by EuroGeographics (original product (with terms of the licence) is available at www.eurogeographics.org/). Szent István University, Dept. of Botany, 1118, Ménesi út 44, Budapest, Hungary MTA Centre for Ecological Research, Inst. of Ecology and Botany, Alkotmány u. 2-4, Vácrátót, 2163, Hungary MTA Centre for Ecological Research, GINOP Sustainable Ecosystems Group, Klebelsberg Kuno u. 3, Tihany, 8237, Hungary CNR Institute of Biosciences and Bioresources, Via Madonna del Piano 10, Sesto Fiorentino (FI), 50019, Italy Cited By :1 Export Date: 10 December 2019 Correspondence Address: Höhn, M.; Szent István University, Dept. of Botany, 1118, Ménesi út 44, Hungary; email: hohn.maria@kertk.szie.hu AB - Climate fluctuations of the Quaternary caused radical changes in distribution of tree species and resulted in large-scale range shifts, population contractions and expansions. Scots pine (Pinus sylvestris L.) a widely distributed conifer of the boreal regions underwent spatio-temporal changes, which shaped the modern-day genetic structure and phylogeographic pattern of the species. By applying independent approaches, including molecular genetic data and historical climate models we aimed to describe demography and past distribution patterns of Scots pine populations from the highly fragmented southern periphery, the Carpathians and the Pannonian Basin. We used Approximate Bayesian Computation (ABC) approach based on nuclear microsatellite markers (nSSRs) and Maximum Entropy distribution modelling (MaxEnt) with temperature- and precipitation-related bioclimatic data. ABC results indicated that from an ancestral Scots pine population two genetic lineages have diverged that in the Mid-Pleistocene due to the favourable climatic conditions underwent population expansion leading to an admixture event. The outcome of the hindcasting confirmed the expansion that leaded to the admixture event revealed by the ABC analysis. This can be dated to the Late Glacial period (14,160–11,800 yrs BP), in which widespread distribution of Scots pine in accordance with palynological proxies was detected. Predictions for the Mid-Holocene period have shown large-scale reduction in distribution of Scots pine and low probability of its occurrence, leading to disjunction and population fragmentation. LA - English DB - MTMT ER - TY - JOUR AU - Törőcsik, Tünde AU - Gulyás, Sándor AU - Sümegi, Pál AU - Sümegi, B AU - Molnár, Dávid AU - Benyó-Korcsmáros, Réka TI - Environmental history of the Csorna plain (Western Danube plain, NW Hungary) from the late glacial to the late Holocene as seen from data of multiproxy geoarchaeological investigations JF - STUDIA QUATERNARIA J2 - STUD QUATER VL - 36 PY - 2019 IS - 1 SP - 19 EP - 43 PG - 25 SN - 1641-5558 DO - 10.24425/sq.2019.126377 UR - https://m2.mtmt.hu/api/publication/30741579 ID - 30741579 N1 - Funding Agency and Grant Number: OTKA [K-112318]; Ministry of Human Capacities, Hungary [20391-3/2018/FEKUSTRAT] Funding text: The research was supported by OTKA grant K-112318 (An Environmental History of the Carpathian Basin in the Middle Ages), the Principal Leader is Prof. Elek Benko, academic director (Institute of Archaeology, Hungarian Academy of Sciences, Budapest). Research has been carried out within the framework of University of Szeged, Interdisciplinary Excellence Centre, Institute of Geography and Earth Sciences, Long Environmental Changes Research Team. Support of the Ministry of Human Capacities, Hungary grant 20391-3/2018/FEKUSTRAT is acknowledged. LA - English DB - MTMT ER - TY - JOUR AU - Tugya, Beáta AU - Sümegi, Pál AU - Náfrádi, Katalin AU - Törőcsik, Tünde AU - Sümegi, Balázs Pál AU - Pomázi, Péter AU - Gulyás, Sándor TI - A dark age settlement and its environment at Rákóczifalva in the Middle Tisza region, Hungary [Egy népvándorlás kori település és környezete a középső-tiszavidékről, Rákóczifalvánál] JF - ARCHEOMETRIAI MŰHELY J2 - ARCHEOMETRIAI MŰHELY VL - 16 PY - 2019 IS - 3 SP - 215 EP - 244 PG - 30 SN - 1786-271X UR - https://m2.mtmt.hu/api/publication/32662708 ID - 32662708 N1 - Thúry György Museum, Zrínyi street 62, Nagykanizsa, H-8800, Hungary University of Szeged, Interdisciplinary Excellence Centre, Institute of Geography and Earth Sciences, Long-Term Environmental Changes Research Team, Department of Geology and Palaeontology, Egyetem street 2, Szeged, H-6722, Hungary Hungarian Academy of Sciences, Research Centre for the Humanities Institute of Archaeology, Tóth Kálmán street 4, Budapest, H-1097, Hungary Export Date: 22 May 2022 Correspondence Address: Tugya, B.; Thúry György Museum, Zrínyi street 62, Hungary; email: tbea82@gmail.com Correspondence Address: Sümegi, P.; University of Szeged, Egyetem street 2, Hungary; email: sumegi@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - Vincze, Ildikó AU - Finsinger, W AU - Jakab, Gusztáv AU - Braun, Mihály AU - Hubay, Katalin AU - Veres, D AU - Deli, T AU - Szalai, Zoltán AU - Szabó, Zoltán AU - Magyari, Enikő Katalin TI - Paleoclimate reconstruction and mire development in the Eastern Great Hungarian Plain for the last 20,000 years JF - REVIEW OF PALAEOBOTANY AND PALYNOLOGY J2 - REV PALAEOBOT PALYNO VL - 271 PY - 2019 PG - 15 SN - 0034-6667 DO - 10.1016/j.revpalbo.2019.104112 UR - https://m2.mtmt.hu/api/publication/30798788 ID - 30798788 N1 - Export Date: 25 October 2020 CODEN: RPPYA Correspondence Address: Vincze, I.; Eötvös Loránd University, Department of Physical and Applied Geology, Pázmány Péter sétány 1/C, Hungary; email: ildi_vincze@yahoo.com LA - English DB - MTMT ER - TY - JOUR AU - Dite, Daniel AU - Hajek, Michal AU - Svitkova, Ivana AU - Kosuthova, Alica AU - Soltes, Rudolf AU - Kliment, Jan TI - Glacial-relict symptoms in the Western Carpathian flora JF - FOLIA GEOBOTANICA J2 - FOLIA GEOBOT VL - 53 PY - 2018 IS - 3 SP - 277 EP - 300 PG - 24 SN - 1211-9520 DO - 10.1007/s12224-018-9321-8 UR - https://m2.mtmt.hu/api/publication/30341722 ID - 30341722 N1 - Institute of Botany, Plant Science and Biodiversity Center, Slovak Academy of Sciences, Dúbravská cesta 9, Bratislava, SK-84523, Slovakia Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, CZ-61137, Czech Republic Department of Botany, Swedish Museum of Natural History, P.O. Box 50007, Stockholm, SE-104 05, Sweden Institute of High Mountains Biology, University of Žilina, Tatranská Javorina 7, Tatranská Javorina, SK-059 56, Slovakia Botanical Garden of Comenius University, Blatnica 315, Blatnica, SK-038 15, Slovakia Cited By :4 Export Date: 9 December 2018 Correspondence Address: Dítě, D.; Institute of Botany, Plant Science and Biodiversity Center, Slovak Academy of Sciences, Dúbravská cesta 9, Slovakia; email: daniel.dite@savba.sk Cited By :11 Export Date: 20 February 2020 AB - Glacial relicts have been regionally more common in glacial than in recent times. A rigorous assessment of which species are indeed glacial relicts is extremely difficult because direct evidence is untraceable or equivocal for many species. We aimed to identify species of the Western Carpathian flora (vascular plants, bryophytes and terrestrial lichens) that display apparent biogeographical and ecological symptoms, suggesting a wider regional or supra-regional distribution during glacial times, or at least before the middle-Holocene climate optimum. We worked with the premise that exemplary relict species should tolerate continental and/or arctic climates, should have large distribution ranges with disjunctions, being regionally rare and ecologically conservative nowadays, should be associated with habitats that occurred during glacial times (tundra, steppe, peatland, open coniferous forest) and should display a restriction of ecological niches in the study region. The assessed species were primarily those with boreo-continental or artcic-alpine distribution. We demonstrated a conspicuous gradient of glacial-relict symptoms, with Carex vaginata, Betula nana, Trichophorum pumilum, Nephroma arcticum, Saxifraga hirculus and Cladonia stellaris topping the ranking. Based on the arbitrary ranking, 289 taxa can be considered high-probability relicts. For only a minority of them, there are any phylogeographical and/or palaeoecological data available from the study area. Biogeographical and ecological symptoms of 144 taxa suggest that they retreated rapidly after the Last Glacial Maximum whereas other species probably retreated later. The first principal component of biogeographical symptoms sorted species from circumpolar arctic-alpine species of acidic peatlands and wet tundra to strongly continental species of steppe, steppe-tundra and mineral-rich fens. This differentiation may mirror the altitudinal zonation of glacial vegetation in the Western Carpathians. LA - English DB - MTMT ER - TY - JOUR AU - Drag, Lukas AU - Hauck, David AU - Rican, Oldrich AU - Schmitt, Thomas AU - Shovkoon, Dmitri F. AU - Godunko, Roman J. AU - Curletti, Gianfranco AU - Cizek, Lukas TI - Phylogeography of the endangered saproxylic beetle Rosalia longicorn, Rosalia alpina (Coleoptera, Cerambycidae), corresponds with its main host, the European beech (Fagus sylvatica, Fagaceae) JF - JOURNAL OF BIOGEOGRAPHY J2 - J BIOGEOGR VL - 45 PY - 2018 IS - 12 SP - 2631 EP - 2644 PG - 14 SN - 0305-0270 DO - 10.1111/jbi.13429 UR - https://m2.mtmt.hu/api/publication/30473686 ID - 30473686 N1 - Faculty of Science, University of South Bohemia, Ceske Budejovice, Czech Republic Institute of Entomology, Biology Centre CAS, Ceske Budejovice, Czech Republic Department of Taxonomy and Biogeography, Senckenberg German Entomological Institute, Müncheberg, Germany Faculty of Natural Sciences I, Zoology, Institute of Biology, Martin Luther University Halle-Wittenberg, Halle, Germany Institute of Steppe of the Ural branch of the Russian Academy of Sciences, Orenburg, Russian Federation Laboratory of Animal Systematic and Faunistic, Samara State University, Samara, Russian Federation Department of Entomology, Museo Civico di Storia Naturale, Carmagnola, Italy Cited By :8 Export Date: 25 May 2022 CODEN: JBIOD Correspondence Address: Drag, L.; Faculty of Science, Czech Republic; email: lukasdrag@gmail.com AB - Aim The Rosalia longicorn (Rosalia alpina) is an internationally protected icon of biodiversity associated with old trees and dead wood. Although the beetle regularly exploits several marginal hosts, its preferred main host is European beech (Fagus sylvatica s.l.). Moreover, the geographical ranges of R. alpina and beech closely overlap. To assess whether their spatial association is mirrored in the genetic patterns of both species, we investigated the phylogeography of Rosalia alpina over its entire geographical range and compared it with the known genetic patterns of its hosts. Location Methods Europe and western Asia. Using both mitochondrial (COI) and nuclear (14 microsatellite loci) markers, we analysed 148 (444, respectively) individuals from 31 (30, respectively) sites. We constructed a Bayesian Inference tree and a haplotype network, calculated the spatial analysis of molecular variance and assessed the population structure of our dataset using two Bayesian clustering methods (STRUCTURE and BAPS). Results Main conclusions Mitochondrial markers suggested existence of five clades in R. alpina populations. Two of them were endemic to the Italian mainland, one to Sicily, and another to southern Turkey. The remaining clade probably originated in the Balkans and colonized the rest of the species' range. Nuclear markers supported this division. They also suggested two main recolonization routes from the Balkans; one heading north and then both west and east, the second expanding eastwards as far as the Caucasus. The observed genetic patterns were largely congruent with those of European beech. The results of both markers were mostly congruent, suggesting at least four potential refugia for R. alpina located in the southernmost parts of its geographical range. Its populations from a large part of Europe and western Asia, however, were genetically poor, dominated by a single haplotype. Phylogeographies of the beetle and its main host seem to be tightly matched, reflecting their common history. LA - English DB - MTMT ER - TY - JOUR AU - Feurdean, Angelica AU - Ruprecht, Eszter AU - Molnár, Zsolt AU - Hutchinson, Simon M. AU - Hickler, Thomas TI - Biodiversity-rich European grasslands: Ancient, forgotten ecosystems JF - BIOLOGICAL CONSERVATION J2 - BIOL CONSERV VL - 228 PY - 2018 SP - 224 EP - 232 PG - 9 SN - 0006-3207 DO - 10.1016/j.biocon.2018.09.022 UR - https://m2.mtmt.hu/api/publication/30323831 ID - 30323831 N1 - Funding Agency and Grant Number: German Research Foundation [FE-1096/4-1]; Janos Bolyai Research Scholarship of the Hungarian Academy of Sciences; National Research, Development and Innovation Office [GINOP-2.3.2-15-2016-00019] Funding text: This work was supported by the German Research Foundation [FE-1096/4-1]. E.R. was supported by the Janos Bolyai Research Scholarship of the Hungarian Academy of Sciences. Z.M. was supported by the National Research, Development and Innovation Office (GINOP-2.3.2-15-2016-00019 project). Funding sources had no involvement in study design; in the collection, analysis and interpretation of data; in the writing of the report; and in the decision to submit the article for publication. Cited By :8 Export Date: 24 September 2019 CODEN: BICOB Correspondence Address: Feurdean, A.; Senckenberg Biodiversity and Climate Research Centre (BiK-F), Senckenberganlage, 25, Germany; email: angelica.feurdean@senckenberg.de Cited By :11 Export Date: 18 November 2019 CODEN: BICOB Correspondence Address: Feurdean, A.; Senckenberg Biodiversity and Climate Research Centre (BiK-F), Senckenberganlage, 25, Germany; email: angelica.feurdean@senckenberg.de Cited By :19 Export Date: 28 May 2020 CODEN: BICOB Correspondence Address: Feurdean, A.; Senckenberg Biodiversity and Climate Research Centre (BiK-F), Senckenberganlage, 25, Germany; email: angelica.feurdean@senckenberg.de Funding Agency and Grant Number: German Research FoundationGerman Research Foundation (DFG) [FE-1096/4-1]; Janos Bolyai Research Scholarship of the Hungarian Academy of SciencesHungarian Academy of Sciences; National Research, Development and Innovation Office [GINOP-2.3.2-15-2016-00019] Funding text: This work was supported by the German Research Foundation [FE-1096/4-1]. E.R. was supported by the Janos Bolyai Research Scholarship of the Hungarian Academy of Sciences. Z.M. was supported by the National Research, Development and Innovation Office (GINOP-2.3.2-15-2016-00019 project). Funding sources had no involvement in study design; in the collection, analysis and interpretation of data; in the writing of the report; and in the decision to submit the article for publication. LA - English DB - MTMT ER - TY - JOUR AU - Frodlova, Jitka AU - Hajkova, Petra AU - Horsak, Michal TI - Effect of sample size and resolution on palaeomalacological interpretation: a case study from Holocene calcareous-fen deposits JF - JOURNAL OF QUATERNARY SCIENCE J2 - J QUATERNARY SCI VL - 33 PY - 2018 IS - 1 SP - 68 EP - 78 PG - 11 SN - 0267-8179 DO - 10.1002/jqs.2999 UR - https://m2.mtmt.hu/api/publication/27332356 ID - 27332356 N1 - Department of Botany and Zoology, Faculty of Science, Masaryk University, Brno, Czech Republic Laboratory of Paleoecology, Institute of Botany, Czech Academy of Sciences, Lidická, Brno, Czech Republic Cited By :7 Export Date: 25 May 2022 Correspondence Address: Frodlová, J.; Department of Botany and Zoology, Czech Republic; email: jitka.moutelikova@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Horsak, Michal AU - Jurickova, Lucie AU - Horsakova, Veronika AU - Pokorna, Adela AU - Pokorny, Petr AU - Sizling, Arnost L AU - Chytry, Milan TI - Forest snail diversity and its environmental predictors along a sharp climatic gradient in southern Siberia JF - ACTA OECOLOGICA: INTERNATIONAL JOURNAL OF ECOLOGY J2 - ACTA OECOL VL - 88 PY - 2018 SP - 1 EP - 8 PG - 8 SN - 1146-609X DO - 10.1016/j.actao.2018.02.009 UR - https://m2.mtmt.hu/api/publication/27587274 ID - 27587274 N1 - Department of Botany and Zoology, Faculty of Science, Masaryk University, Kotlářská 2, Brno, CZ-61137, Czech Republic Department of Zoology, Faculty of Science, Charles University, Viničná 7, Praha 2, CZ-128 44, Czech Republic Center for Theoretical Study, Charles University and The Czech Academy of Sciences, Jilská 1, Praha 1, CZ-110 00, Czech Republic Department of Botany, Faculty of Science, Charles University, Benátská 2, Praha 2, CZ-128 01, Czech Republic Cited By :4 Export Date: 25 May 2022 CODEN: ACOEE Correspondence Address: Horsák, M.; Department of Botany and Zoology, Kotlářská 2, Czech Republic; email: horsak@sci.muni.cz LA - English DB - MTMT ER - TY - JOUR AU - Jimenez-Alfaro, Borja AU - Girardello, Marco AU - Chytry, Milan AU - Svenning, Jens-Christian AU - Willner, Wolfgang AU - Gegout, Jean-Claude AU - Agrillo, Emiliano AU - Antonio, Campos Juan AU - Jandt, Ute AU - Kacki, Zygmunt AU - Silc, Urban AU - Slezak, Michal AU - Tichy, Lubomir AU - Tsiripidis, Ioannis AU - Turtureanu, Pavel Dan AU - Ujhazyova, Mariana AU - Wohlgemuth, Thomas TI - History and environment shape species pools and community diversity in European beech forests JF - NATURE ECOLOGY & EVOLUTION J2 - NAT ECOL EVOL VL - 2 PY - 2018 IS - 3 SP - 483 EP - 490 PG - 8 SN - 2397-334X DO - 10.1038/s41559-017-0462-6 UR - https://m2.mtmt.hu/api/publication/27340969 ID - 27340969 N1 - German Centre for Integrative Biodiversity Research (IDiv) Halle-Jena-Leipzig, Leipzig, Germany Institute of Biology/Geobotany and Botanical Garden, Martin Luther University Halle-Wittenberg, Halle, Germany Department of Botany and Zoology, Masaryk University, Brno, Czech Republic Section for Ecoinformatics and Biodiversity, Department of Bioscience, Aarhus University, Aarhus, Denmark CE3c-Centre for Ecology, Evolution and Environmental Changes, Azorean Biodiversity Group, Angra do Heroísmo, Portugal Center for Biodiversity Dynamics in A Changing World (BIOCHANGE), Aarhus University, Aarhus, Denmark VINCA - Vienna Institute for Nature Conservation and Analyses, Wien, Austria Department of Botany and Biodiversity Research, University of Vienna, Vienna, Austria LERFoB, INRA, AgroParisTech, Nancy, France Department of Environmental Biology, Sapienza University of Rome, Rome, Italy Department of Plant Biology and Ecology, University of Basque Country UPV/EHU, Bilbao, Spain Department of Vegetation Ecology, Botanical Garden, University of Wroclaw, Wrocław, Poland ZRC SAZU, Institute of Biology, Ljubljana, Slovenia Institute of Forest Ecology, Slovak Academy of Sciences, Zvolen, Slovakia Plant Science and Biodiversity Center, Institute of Botany, Slovak Academy of Sciences, Bratislava, Slovakia Department of Botany, School of Biology, Aristotle University of Thessaloniki, Thessaloniki, Greece Alexandru Borza Botanical Garden, Babeş-Bolyai University, Cluj-Napoca, Romania Department of Applied Ecology, Faculty of Ecology and Environmental Sciences, Technical University in Zvolen, Zvolen, Slovakia WSL Swiss Federal Research Institute, Birmensdorf, Switzerland Cited By :2 Export Date: 16 December 2018 Correspondence Address: Jiménez-Alfaro, B.; German Centre for Integrative Biodiversity Research (IDiv) Halle-Jena-LeipzigGermany; email: jimenezalfaro.borja@gmail.com German Centre for Integrative Biodiversity Research (IDiv) Halle-Jena-Leipzig, Leipzig, Germany Institute of Biology/Geobotany and Botanical Garden, Martin Luther University Halle-Wittenberg, Halle, Germany Department of Botany and Zoology, Masaryk University, Brno, Czech Republic Section for Ecoinformatics and Biodiversity, Department of Bioscience, Aarhus University, Aarhus, Denmark CE3c-Centre for Ecology, Evolution and Environmental Changes, Azorean Biodiversity Group, Angra do Heroísmo, Portugal Center for Biodiversity Dynamics in A Changing World (BIOCHANGE), Aarhus University, Aarhus, Denmark VINCA - Vienna Institute for Nature Conservation and Analyses, Wien, Austria Department of Botany and Biodiversity Research, University of Vienna, Vienna, Austria LERFoB, INRA, AgroParisTech, Nancy, France Department of Environmental Biology, Sapienza University of Rome, Rome, Italy Department of Plant Biology and Ecology, University of Basque Country UPV/EHU, Bilbao, Spain Department of Vegetation Ecology, Botanical Garden, University of Wroclaw, Wrocław, Poland ZRC SAZU, Institute of Biology, Ljubljana, Slovenia Institute of Forest Ecology, Slovak Academy of Sciences, Zvolen, Slovakia Plant Science and Biodiversity Center, Institute of Botany, Slovak Academy of Sciences, Bratislava, Slovakia Department of Botany, School of Biology, Aristotle University of Thessaloniki, Thessaloniki, Greece Alexandru Borza Botanical Garden, Babeş-Bolyai University, Cluj-Napoca, Romania Department of Applied Ecology, Faculty of Ecology and Environmental Sciences, Technical University in Zvolen, Zvolen, Slovakia WSL Swiss Federal Research Institute, Birmensdorf, Switzerland Cited By :15 Export Date: 18 November 2019 Correspondence Address: Jiménez-Alfaro, B.; German Centre for Integrative Biodiversity Research (IDiv) Halle-Jena-LeipzigGermany; email: jimenezalfaro.borja@gmail.com German Centre for Integrative Biodiversity Research (IDiv) Halle-Jena-Leipzig, Leipzig, Germany Institute of Biology/Geobotany and Botanical Garden, Martin Luther University Halle-Wittenberg, Halle, Germany Department of Botany and Zoology, Masaryk University, Brno, Czech Republic Section for Ecoinformatics and Biodiversity, Department of Bioscience, Aarhus University, Aarhus, Denmark CE3c-Centre for Ecology, Evolution and Environmental Changes, Azorean Biodiversity Group, Angra do Heroísmo, Portugal Center for Biodiversity Dynamics in A Changing World (BIOCHANGE), Aarhus University, Aarhus, Denmark VINCA - Vienna Institute for Nature Conservation and Analyses, Wien, Austria Department of Botany and Biodiversity Research, University of Vienna, Vienna, Austria LERFoB, INRA, AgroParisTech, Nancy, France Department of Environmental Biology, Sapienza University of Rome, Rome, Italy Department of Plant Biology and Ecology, University of Basque Country UPV/EHU, Bilbao, Spain Department of Vegetation Ecology, Botanical Garden, University of Wroclaw, Wrocław, Poland ZRC SAZU, Institute of Biology, Ljubljana, Slovenia Institute of Forest Ecology, Slovak Academy of Sciences, Zvolen, Slovakia Plant Science and Biodiversity Center, Institute of Botany, Slovak Academy of Sciences, Bratislava, Slovakia Department of Botany, School of Biology, Aristotle University of Thessaloniki, Thessaloniki, Greece Alexandru Borza Botanical Garden, Babeş-Bolyai University, Cluj-Napoca, Romania Department of Applied Ecology, Faculty of Ecology and Environmental Sciences, Technical University in Zvolen, Zvolen, Slovakia WSL Swiss Federal Research Institute, Birmensdorf, Switzerland Cited By :33 Export Date: 13 April 2021 Correspondence Address: Jiménez-Alfaro, B.; German Centre for Integrative Biodiversity Research (IDiv) Halle-Jena-LeipzigGermany; email: jimenezalfaro.borja@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Kolaczek, Piotr AU - Galka, Mariusz AU - Apolinarska, Karina AU - Plociennik, Mateusz AU - Gasiorowski, Michal AU - Brooks, Stephen J AU - Hutchinson, Simon M AU - Karpinska-Kolaczek, Monika TI - A multi-proxy view of exceptionally early postglacial development of riparian woodlands with Ulmus in the Dniester River valley, updates western Ukraine JF - REVIEW OF PALAEOBOTANY AND PALYNOLOGY J2 - REV PALAEOBOT PALYNO VL - 250 PY - 2018 SP - 27 EP - 43 PG - 17 SN - 0034-6667 DO - 10.1016/j.revpalbo.2017.12.001 UR - https://m2.mtmt.hu/api/publication/27332353 ID - 27332353 N1 - Cited By :14 Export Date: 25 May 2022 CODEN: RPPYA Correspondence Address: Kołaczek, P.; Department of Biogeography and Paleoecology, Krygowskiego 10, Poland; email: pkolacz@amu.edu.pl LA - English DB - MTMT ER - TY - JOUR AU - Ricankova, Vera Pavelkova AU - Horsak, Michal AU - Hais, Martin AU - Robovsky, Jan AU - Chytry, Milan TI - Environmental correlates of the Late Quaternary regional extinctions of large and small Palaearctic mammals JF - ECOGRAPHY J2 - ECOGRAPHY VL - 41 PY - 2018 IS - 3 SP - 516 EP - 527 PG - 12 SN - 0906-7590 DO - 10.1111/ecog.02851 UR - https://m2.mtmt.hu/api/publication/27332354 ID - 27332354 N1 - Faculty of Science, Univ. of South Bohemia, České, Budějovice, Czech Republic Dept of Botany and Zoology, Masaryk Univ., Brno, Czech Republic Cited By :12 Export Date: 25 May 2022 CODEN: ECOGE LA - English DB - MTMT ER - TY - CHAP AU - Törőcsik, Tünde AU - Sümegi, Balázs Pál AU - Sümegi, Pál ED - Korda, Márton TI - Az ócsai Selyem-rét környezettörténete a jégkor végétől [Environmental history from the terminal phase of the ice age on the Selyemrét area at Ócsa] T2 - Természetvédelem és kutatás a Turjánvidék északi részén PB - Duna-Ipoly Nemzeti Park Igazgatóság CY - Budapest SN - 9786155241253 T3 - Rosalia, ISSN 1787-825X ; 10. PY - 2018 SP - 81 EP - 118 PG - 38 UR - https://m2.mtmt.hu/api/publication/3411767 ID - 3411767 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Chytry, Milan AU - Horsak, Michal AU - Syrovatka, Vit AU - Danihelka, Jiri AU - Ermakov, Nikolai AU - German, Dmitry A AU - Hajek, Michal AU - Hajek, Ondrej AU - Hajkova, Petra AU - Horsakova, Veronika AU - Koci, Martin AU - Kubegova, Svatava AU - Lustyk, Pavel AU - Nekola, Jeffrey C AU - Preislerova, Zdenka AU - Resl, Philipp AU - Valachovic, Milan TI - Refugial ecosystems in central Asia as indicators of biodiversity change during the Pleistocene-Holocene transition JF - ECOLOGICAL INDICATORS J2 - ECOL INDIC VL - 77 PY - 2017 SP - 357 EP - 367 PG - 11 SN - 1470-160X DO - 10.1016/j.ecolind.2016.12.033 UR - https://m2.mtmt.hu/api/publication/26929802 ID - 26929802 N1 - Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, 611 37, Czech Republic Department of Vegetation Ecology, Institute of Botany, The Czech Academy of Sciences, Lidická 25/27, Brno, 602 00, Czech Republic Central Siberian Botanical Garden, Russian Academy of Sciences, Zolotodolinskaya 101, Novosibirsk, 630090, Russian Federation Department of Biodiversity and Plant Systematics, Centre for Organismal Studies (COS) Heidelberg, Heidelberg University, Im Neuenheimer Feld 345, Heidelberg, 69120, Germany South-Siberian Botanical Garden, Altai State University, Lenina 61, Barnaul, 656049, Russian Federation Department of Botany, Moravian Museum, Hviezdoslavova 29a, Brno, 627 00, Czech Republic Biology Department, University of New Mexico, Albuquerque, NM 87131, United States Institute of Plant Sciences, NAWI Graz, University of Graz, Holteigasse 6, Graz, 8010, Austria Institute of Botany, Slovak Academy of Sciences, Dúbravská cesta 9, Bratislava, 845 23, Slovakia Cited By :13 Export Date: 25 May 2022 Correspondence Address: Chytrý, M.; Department of Botany and Zoology, Kotlářská 2, Czech Republic; email: chytry@sci.muni.cz LA - English DB - MTMT ER - TY - CHAP AU - Feurdean, A AU - Tantau, I ED - Radoane, Maria ED - Vespremeanu-Stroe, Alfred TI - The Evolution of Vegetation from the last Glacial Maximum until the Present T2 - Landform Dynamics and Evolution in Romania PB - Springer Netherlands CY - Cham SN - 9783319325897 T3 - Springer Geography, ISSN 2194-315X PB - Springer Netherlands PY - 2017 SP - 67 EP - 83 PG - 17 DO - 10.1007/978-3-319-32589-7_4 UR - https://m2.mtmt.hu/api/publication/26500362 ID - 26500362 N1 - Senckenberg Research Institute and Natural History Museum, Biodiversity and Climate Research Centre, Frankfurt Am Main, Germany Emil Racoviţă Institute of Speleology, Romanian Academy, Clinicilor 5, Cluj-Napoca, Cluj, 400006, Romania Department of Geology, Babeş-Bolyai University, M. Kogălniceanu, 1, Cluj-Napoca, 400084, Romania Institute of Biological Research, Cluj-Napoca, Cluj, Romania Cited By :7 Export Date: 25 May 2022 Correspondence Address: Feurdean, A.; Senckenberg Research Institute and Natural History Museum, Germany; email: angelica.feurdean@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Haliuc, A AU - Veres, D AU - Brauer, A AU - Hubay, Katalin AU - Hutchinson, S AU - Begy, R AU - Braun, Mihály TI - Palaeohydrological changes during the mid and late Holocene in the Carpathian area, central-eastern Europe JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 152 PY - 2017 SP - 99 EP - 114 PG - 16 SN - 0921-8181 DO - 10.1016/j.gloplacha.2017.02.010 UR - https://m2.mtmt.hu/api/publication/3217479 ID - 3217479 N1 - Stefan cel Mare University of Suceava, Department of Geography, Suceava, Romania Institute of Speleology, Romanian Academy, Cluj-Napoca, Romania GFZ German Research Centre for Geosciences, Section 5.2 Climate Dynamics and Landscape Evolution, Potsdam, Germany Hertelendi Laboratory of Environmental Studies, Atomki, Debrecen, Hungary School of Environment and Life Sciences, Peel Building, University of Salford, Salford, United Kingdom Interdisciplinary Research Institute on Bio-Nano-Science, Babes-Bolyai University, Cluj-Napoca, Romania Export Date: 15 October 2019 CODEN: GPCHE Correspondence Address: Haliuc, A.; Stefan cel Mare University of Suceava, Department of Geography, 13 Universitatii str, Romania Stefan cel Mare University of Suceava, Department of Geography, Suceava, Romania Institute of Speleology, Romanian Academy, Cluj-Napoca, Romania GFZ German Research Centre for Geosciences, Section 5.2 Climate Dynamics and Landscape Evolution, Potsdam, Germany Hertelendi Laboratory of Environmental Studies, Atomki, Debrecen, Hungary School of Environment and Life Sciences, Peel Building, University of Salford, Salford, United Kingdom Interdisciplinary Research Institute on Bio-Nano-Science, Babes-Bolyai University, Cluj-Napoca, Romania Export Date: 22 February 2021 CODEN: GPCHE Correspondence Address: Haliuc, A.; Stefan cel Mare University of Suceava, 13 Universitatii str, Romania LA - English DB - MTMT ER - TY - JOUR AU - Janska, Veronika AU - Jimenez-Alfaro, Borja AU - Chytry, Milan AU - Divisek, Jan AU - Anenkhonov, Oleg AU - Korolyuk, Andrey AU - Lashchinskyi, Nikolai AU - Culek, Martin TI - Palaeodistribution modelling of European vegetation types at the Last Glacial Maximum using modern analogues from Siberia: Prospects and limitations JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 159 PY - 2017 SP - 103 EP - 115 PG - 13 SN - 0277-3791 DO - 10.1016/j.quascirev.2017.01.011 UR - https://m2.mtmt.hu/api/publication/26576765 ID - 26576765 N1 - Department of Geography, Masaryk University, Kotlářská 2, Brno, CZ-611 37, Czech Republic Department of Botany and Zoology, Masaryk University, Kotlářská 2, Brno, CZ-611 37, Czech Republic Geobotany and Botanical Garden, Institute of Biology, Martin Luther University Halle Wittenberg, Am Kirchtor 1, Halle (Saale), 06108, Germany German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Deutscher Platz 5e, Leipzig, 04103, Germany Institute of General and Experimental Biology, Siberian Branch of the Russian Academy of Sciences, Sakhyanovoi 6, Ulan-Ude, RU-670047, Russian Federation Central Siberian Botanical Garden, Siberian Branch of the Russian Academy of Sciences, Zolotodolinskya 101, Novosibirsk, RU-630090, Russian Federation Cited By :43 Export Date: 25 May 2022 CODEN: QSRED Correspondence Address: Jiménez-Alfaro, B.; Geobotany and Botanical Garden, Am Kirchtor 1, Germany; email: jimenezalfaro.borja@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Kolaczek, Piotr AU - Margielewski, Modzimierz AU - Galka, Mariusz AU - Apolinarska, Karina AU - Plociennik, Mateusz AU - Gasiorowski, Michal AU - Buczek, Krzysztof AU - Karpinska-Kolaczek, Monika TI - Five centuries of the Early Holocene forest development and its interactions with palaeoecosystem of small landslide lake in the Beskid Makowski Mountains (Western Carpathians, Poland) - High resolution multi-proxy study JF - REVIEW OF PALAEOBOTANY AND PALYNOLOGY J2 - REV PALAEOBOT PALYNO VL - 244 PY - 2017 SP - 113 EP - 127 PG - 15 SN - 0034-6667 DO - 10.1016/j.revpalbo.2017.05.002 UR - https://m2.mtmt.hu/api/publication/26929800 ID - 26929800 N1 - Department of Biogeography and Palaeoecology, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University in Poznań, Krygowskiego 10, Poznań, 61-680, Poland Institute of Nature Conservation, Polish Academy of Sciences, Adama Mickiewicza Ave. 33, Kraków, 31-120, Poland Institute of Geology, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University in Poznań, Krygowskiego 12, Poznań, 61-680, Poland Department of Invertebrate Zoology and Hydrobiology, University of Lodz, Banacha 12/16, Łódź, 90-237, Poland Institute of Geological Sciences, Polish Academy of Sciences, Twarda 51/55, Warszawa, 00-818, Poland Laboratory of Wetland Ecology and Monitoring, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University in Poznań, Krygowskiego 10, Poznań, 61-680, Poland Centre for the Study of Demographic and Economic Structures in Preindustrial Central and Eastern Europe, University of Bialystok, Plac Uniwersytecki 1, Białystok, 15-420, Poland Cited By :13 Export Date: 25 May 2022 CODEN: RPPYA Correspondence Address: Kołaczek, P.; Department of Biogeography and Palaeoecology, Krygowskiego 10, Poland; email: pkolacz@amu.edu.pl LA - English DB - MTMT ER - TY - JOUR AU - McLaughlin, B.C. AU - Ackerly, D.D. AU - Klos, P.Z. AU - Natali, J. AU - Dawson, T.E. AU - Thompson, S.E. TI - Hydrologic refugia, plants, and climate change JF - GLOBAL CHANGE BIOLOGY J2 - GLOBAL CHANGE BIOL VL - 23 PY - 2017 IS - 8 SP - 2941 EP - 2961 PG - 21 SN - 1354-1013 DO - 10.1111/gcb.13629 UR - https://m2.mtmt.hu/api/publication/26762177 ID - 26762177 N1 - Funding Agency and Grant Number: National Science Foundation [IOS-1441396]; National Institute of Food and Agriculture, U.S. Department of Agriculture, McIntire Stennis project [1006829] Funding text: We thank the National Science Foundation IOS-1441396, and National Institute of Food and Agriculture, U.S. Department of Agriculture, McIntire Stennis project under 1006829. Cited By :28 Export Date: 3 December 2018 Correspondence Address: McLaughlin, B.C.; Department of Natural Resources and Society, University of IdahoUnited States; email: bcmclaughlin@gmail.com AB - Climate, physical landscapes, and biota interact to generate heterogeneous hydrologic conditions in space and over time, which are reflected in spatial patterns of species distributions. As these species distributions respond to rapid climate change, microrefugia may support local species persistence in the face of deteriorating climatic suitability. Recent focus on temperature as a determinant of microrefugia insufficiently accounts for the importance of hydrologic processes and changing water availability with changing climate. Where water scarcity is a major limitation now or under future climates, hydrologic microrefugia are likely to prove essential for species persistence, particularly for sessile species and plants. Zones of high relative water availability - mesic microenvironments - are generated by a wide array of hydrologic processes, and may be loosely coupled to climatic processes and therefore buffered from climate change. Here, we review the mechanisms that generate mesic microenvironments and their likely robustness in the face of climate change. We argue that mesic microenvironments will act as species-specific refugia only if the nature and space/time variability in water availability are compatible with the ecological requirements of a target species. We illustrate this argument with case studies drawn from California oak woodland ecosystems. We posit that identification of hydrologic refugia could form a cornerstone of climate-cognizant conservation strategies, but that this would require improved understanding of climate change effects on key hydrologic processes, including frequently cryptic processes such as groundwater flow. LA - English DB - MTMT ER - TY - CHAP AU - Mîndrescu, M AU - Florescu, G AU - Grădinaru, I AU - Haliuc, A ED - Radoane, Maria ED - Vespremeanu-Stroe, Alfred TI - Lakes, Lacustrine Sediments, and Palaeoenvironmental Reconstructions T2 - Landform Dynamics and Evolution in Romania PB - Springer Netherlands CY - Cham SN - 9783319325897 T3 - Springer Geography, ISSN 2194-315X PB - Springer Netherlands PY - 2017 SP - 699 EP - 734 PG - 36 DO - 10.1007/978-3-319-32589-7_30 UR - https://m2.mtmt.hu/api/publication/26099775 ID - 26099775 N1 - Cited By :5 Export Date: 25 May 2022 Correspondence Address: Mîndrescu, M.; Cirques and Lakes Research Group, Universității 13, Romania; email: marcel.mindrescu@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Reinecke, Jennifer AU - Troeva, Elena AU - Wesche, Karsten TI - Extrazonal steppes and other temperate grasslands of northern Siberia-Phytosociological classification and ecological characterization JF - PHYTOCOENOLOGIA J2 - PHYTOCOENOLOGIA VL - 47 PY - 2017 IS - 2 SP - 167 EP - 196 PG - 30 SN - 0340-269X DO - 10.1127/phyto/2017/0175 UR - https://m2.mtmt.hu/api/publication/26933773 ID - 26933773 N1 - Senckenberg Museum of Natural History Görlitz, P.O. Box 300154, Görlitz, 02806, Germany Internationales Hochschulinstitut Zittau, Technische Universität Dresden, Markt 23, Zittau, 02763, Germany Laboratory of Genesis and Ecology of Soil-Vegetation Cover, Institute for Biological Problems of the Cryolithozone, Siberian Branch of the Russian Academy of Sciences, Yakutsk, Russian Federation German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-Leipzig, Deutscher Platz 5e, Leipzig, 04103, Germany Cited By :6 Export Date: 25 May 2022 Correspondence Address: Reinecke, J.; Senckenberg Museum of Natural HistoryGermany; email: jennifer.reinecke@senckenberg.de LA - English DB - MTMT ER - TY - JOUR AU - Tóth, Endre György AU - Köbölkuti, Zoltán Attila AU - Pedryc, A. AU - Höhn, Mária Margit TI - Evolutionary history and phylogeography of Scots pine (Pinus sylvestris L.) in Europe based on molecular markers JF - JOURNAL OF FOREST RESEARCH J2 - J FOREST RES-JPN VL - 28 PY - 2017 IS - 4 SP - 637 EP - 651 PG - 15 SN - 1341-6979 DO - 10.1007/s11676-017-0393-8 UR - https://m2.mtmt.hu/api/publication/3212261 ID - 3212261 N1 - Department of Botany, Szent István University, Ménesi út 44, Budapest, 1118, Hungary Department of Genetics and Plant Breeding, Szent István University, Ménesi út 44, Budapest, 1118, Hungary Cited By :2 Export Date: 9 December 2018 Correspondence Address: Tóth, E.G.; Department of Botany, Szent István University, Ménesi út 44, Hungary; email: toth.endre@kertk.szie.hu WoS:hiba:000404234900001 2019-03-14 01:54 folyóirat nem egyezik AB - In this review we summarized recent historical records and molecular studies on evolutionary history and phylogeography of Scots pine with focus on the European highly fragmented distribution area of the species. Fossilized pollen, plant micro- and macrofossil records provided evidences on the large-scale species' range shifts and demographic changes during the Quaternary. Populations of Scots pine were documented both in the glacial (incl. full glaciation) and interglacial periods. Recolonization of Europe after the glaciation originated from the (Sub) Mediterranean areas like the Balkan Peninsula but also from around the Eastern Alps and the surroundings of the Danube plain. Fennoscandia and northern European Baltic regions were most probably colonized from two main directions, from Western Europe and from the Russian Plain. Modern history of Scots pine was hardly affected by anthropogenic activities that started to strengthen in the Bronze and Iron Age. Along with the fossil records, molecular genetic tools were used to infer the origin and putative history including migration, differentiation and demography of the species. In this paper we compiled the major publications (30) of molecular genetic studies of the past 20 years derived from distinctly inherited organelle genomes (mitochondrial, chloroplast, nuclear) revealed by different marker systems (mtDNA-cox1, -nad1, -nad3, -nad7, ISSR, cpSSR, nSSR, B-SAP, SNP). It is important to consider that different phylogeographic patterns can be drawn by the analysis of different DNA marker types. Accordingly the use of more than one marker simultaneously outlines the most sophisticated phylogeographical pattern on the genetic lineages and can reveal high differentiation of the European distribution. Combined marker systems and markers derived from coding sequences have also been used to detect species' phylogeographic patterns, but these were rarely applied to Scots pine. Although new molecular techniques can provide higher resolution data for populations, the reviewed results can shape the direction of further studies. LA - English DB - MTMT ER - TY - JOUR AU - Tóth, Endre György AU - Vendramin, G G AU - Bagnoli, F AU - Cseke, Klára AU - Höhn, Mária Margit TI - High genetic diversity and distinct origin of recently fragmented Scots pine (Pinus sylvestris L.) populations along the Carpathians and the Pannonian Basin JF - TREE GENETICS & GENOMES J2 - TREE GENET GENOMES VL - 13 PY - 2017 IS - 47 PG - 12 SN - 1614-2942 DO - 10.1007/s11295-017-1137-9 UR - https://m2.mtmt.hu/api/publication/3212241 ID - 3212241 N1 - Department of Botany, Szent István University, 1118, Ménesi út 44, Budapest, Hungary CNR Institute of Biosciences and Bioresources, Via Madonna del Piano 10, Sesto Fiorentino, FI 50019, Italy Forest Research Institute, Sárvár Experimental Station, 9600, Várkerület u. 30/A, Sárvár, Hungary Cited By :2 Export Date: 9 December 2018 Correspondence Address: Tóth, E.G.; Department of Botany, Szent István University, 1118, Ménesi út 44, Hungary; email: toth.endre@kertk.szie.hu WoS:hiba:000400497600017 2019-03-14 01:54 füzet nem egyezik AB - Historical evolutionary events highly affect the modern-day genetic structure of natural populations. Scots pine (Pinus sylvestris L.), as a dominant tree species of the Eurasian taiga communities following the glacial cycles of the Pleistocene, has survived in small, scattered populations at the range limits of its south-eastern European distribution. In this study, we examined genetic relationships, genetic divergence and demographic history of peripheral populations from central-eastern Europe, the Carpathian Mountains and the Pannonian Basin. Four hundred twenty-one individuals from 20 populations were sampled and characterized with both nuclear and chloroplast simple sequence repeat (SSR) markers. Standard population genetic indices, the degree of genetic differentiation and spatial genetic structure were analysed. Our results revealed that peripheral Scots pine populations retained high genetic diversity despite the recently ongoing fragmentation and isolation of the persisting relict populations. Analysis of molecular variance (AMOVA) showed 7% among-population genetic differentiation, and there was no isolation by distance among the island-like occurrences. Genetic discontinuities with strong barriers (99-100% bootstrap support) were identified in the Carpathians. Based on both marker types, populations of the Western Carpathians were delimited from those inhabiting the Eastern Carpathians, and two main genetic lineages were traced that most probably originate from two main refugia. One refugium presumably existed in the region of the Eastern Alps with the Hungarian Plain, while the other was probably found in the Eastern Carpathians. These findings are supported by recent palynological records. The strongest genetic structure was revealed within the Romanian Carpathians on the basis of both marker types. With only some exceptions, no signs of recent bottlenecks or inbreeding were detected. However, Carpathian natural populations of Scots pine are highly fragmented and have a small census size, though they have not yet been affected by genetic erosion induced by isolation. LA - English DB - MTMT ER - TY - JOUR AU - Van, Geel Bas AU - Protopopov, Albert AU - Protopopova, Victoria AU - Pavlov, Innokenti AU - Van, Der Plicht Johannes AU - Van, Reenen Guido B A TI - Larix during the Mid-Pleniglacial (Greenland Interstadial 8) on Kotelny Island, northern Siberia JF - BOREAS J2 - BOREAS VL - 46 PY - 2017 IS - 2 SP - 338 EP - 345 PG - 8 SN - 0300-9483 DO - 10.1111/bor.12216 UR - https://m2.mtmt.hu/api/publication/26576764 ID - 26576764 N1 - Institute for Biodiversity and Ecosystem Dynamics, University of Amsterdam, Science Park 904, Amsterdam, 1098 XH, Netherlands Academy of Sciences of the Republic of Sakha (Yakutia), 33 Lenina ave, Yakutsk, 677007, Russian Federation Institute for Biological Problems of Cryolithozone, Siberian Branch of RAS, 41 Lenina ave, Yakutsk, 677980, Russian Federation Centre for Isotope Research, University of Groningen, Nijenborgh 4, Groningen, 9747 AG, Netherlands Cited By :7 Export Date: 25 May 2022 LA - English DB - MTMT ER - TY - JOUR AU - Bernhardsson, C AU - Floran, V AU - Ganea, S L AU - Garcia-Gil, M R TI - Present genetic structure is congruent with the common origin of distant Scots pine populations in its Romanian distribution JF - FOREST ECOLOGY AND MANAGEMENT J2 - FOREST ECOL MANAG VL - 361 PY - 2016 SP - 131 EP - 143 PG - 13 SN - 0378-1127 DO - 10.1016/j.foreco.2015.10.047 UR - https://m2.mtmt.hu/api/publication/27496819 ID - 27496819 N1 - Department of Forest Genetics and Plant Physiology, SLU, SE-901 83, Umeå, Sweden Faculty of Horticulture, University of Agriculture Science and Veterinary Medicine, Cluj Napoca, 400372, Romania Faculty of Agriculture, University of Agriculture Science and Veterinary Medicine, Cluj Napoca, 400372, Romania Cited By :16 Export Date: 25 May 2022 CODEN: FECMD Correspondence Address: García-Gil, M.R.; Department of Forest Genetics and Plant Physiology, SE-90183, Sweden; email: m.rosario.garcia@slu.se AB - Owing to the fact that mitochondrial, chloroplast and nuclear genomes are differently affected by evolutionary forces, the comparative study of all three genomes in combination with paleobotanical evidences allows for a more accurate interpretation of present genetic make-up. In this study, we analyzed the nad1-nad7 mitotype, 14 cpSSR loci and 10 nSSR loci in 13 Romanian Scots pine (Pious sylvestris L.) populations from the Romanian Carpathians and two Hungarian populations. Previous analysis of the macro fossil records supports the presence of Scots pine and Swiss stone pine (Pinus cembra L.) during the glacial period in Hungary and Romania. For a better image into the population structure in the studied area we also included in the data analysis two outgroup populations (north and south of Sweden) of known post glacial origin, which resulted in a more defined genetic structure. Our study reveals that relatively high genetic diversity is preserved at all the Romanian and Hungarian populations, with no distinction among naturally regenerated, managed autochthonous and introduced populations. Furthermore, genetic differentiation analysis fails to distinguish the two introduced populations from the Romanian ones. AMOVA clustering is congruent with the paleobotanical-based evidences of contraction of Scots pine range since the Holocene to its present fragmented distribution. (C) 2015 Elsevier B.V. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Dawson, MN AU - Axmacher, JC AU - Beierkuhnlein, C AU - Blois, J AU - Bradley, BA AU - Cord, AF AU - Dengler, J AU - He, KS AU - Heaney, LR AU - Jansson, R AU - Mahecha, MD AU - Myers, C AU - Nogués-Bravo, D AU - Papadopoulou, A AU - Reu, B AU - Rodríguez-Sánchez, F AU - Steinbauer, MJ AU - Stigall, A AU - Tuanmu, M-N AU - Gavin, DG TI - A second horizon scan of biogeography: Golden ages, Midas touches, and the Red Queen JF - FRONTIERS OF BIOGEOGRAPHY J2 - FRONT BIOGEOGRAPHY VL - 8 PY - 2016 IS - 4 SN - 1948-6596 DO - 10.21425/F58429770 UR - https://m2.mtmt.hu/api/publication/27120550 ID - 27120550 N1 - School of Natural Sciences, University of California, 5200 North Lake Road, Merced, CA 95343, United States UCL Department of Geography, University College London, London, WC1E 6BT, United Kingdom Biogeography, Bayreuth Center of Ecology and Environmental Research (BayCEER), University of Bayreuth, Universitätstr. 30, Bayreuth, 95447, Germany Department of Environmental Conservation, University of Massachusetts, Amherst, MA 01003, United States Department of Computational Landscape Ecology, Helmholtz Centre for Environmental Research - UFZ, Permoserstr. 15, Leipzig, 04318, Germany Plant Ecology, Bayreuth Center of Ecology and Environmental Research (BayCEER), University of Bayreuth, Universitätstr. 30, Bayreuth, 95447, Germany German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena- Leipzig, Deutscher Platz 5e, Leipzig, 04103, Germany Department of Biological Sciences, Murray State University, Murray, KY 42071, United States Field Museum of Natural History, 1400 S Lake Shore Drive, Chicago, IL 60605, United States Department of Ecology and Environmental Science, Umeå University, Umeå, SE-901 87, Sweden Max Planck Institute for Biogeochemistry, Jena, 07745, Germany German Centre for Integrative Biodiversity Research (iDiv), Halle-Jena-Leipzig, Leipzig, 04103, Germany Department of Earth and Planetary Sciences, University of New Mexico, 1 Northrop Hall, Albuquerque, NM 87131, United States Center for Macroecology, Evolution and Climate, Natural History Museum of Denmark, University of Copenhagen, Universitetsparken 15, Copenhagen Ø, DK-2100, Denmark Integrative Ecology Group, Estación Biológica de Doñana, Consejo Superior de Investigaciones Científicas (EBD-CSIC), Avenida Américo Vespucio s/n, Sevilla, E-41092, Spain Institute of Biology, University of Leipzig, Leipzig, 04103, Germany Section Ecoinformatics and Biodiversity, Department of Bioscience, Aarhus University, Aarhus, DK-8000, Denmark Ohio University, Department of Geological Sciences, OHIO Center for Ecology and Evolutionary Studies, 316 Clippinger Laboratories, Athens, OH 45701, United States Department of Ecology and Evolutionary Biology, Yale University, 165 Prospect Street, New Haven, CT 06520, United States Biodiversity Research Center, Academia Sinica, Taipei, 115, Taiwan Department of Geography, University of Oregon, Eugene, OR 97403, United States Cited By :5 Export Date: 25 May 2022 Correspondence Address: Dawson, M.N.; School of Natural Sciences, 5200 North Lake Road, United States; email: mdawson@ucmerced.edu LA - English DB - MTMT ER - TY - JOUR AU - Hochheimer, J AU - Hoffmann, MH TI - Footprints of the Last Glacial: Past competition may have shaped strongly disjunct distribution ranges in Artemisia rupestris and A. laciniata JF - FLORA J2 - FLORA VL - 224 PY - 2016 SP - 203 EP - 210 PG - 8 SN - 0367-2530 DO - 10.1016/j.flora.2016.08.004 UR - https://m2.mtmt.hu/api/publication/27120975 ID - 27120975 N1 - Cited By :3 Export Date: 25 May 2022 CODEN: FLRAB Correspondence Address: Hoffmann, M.H.; Martin-Luther Universität Halle-Wittenberg, Geobotanik und Botanischer Garten, Am Kirchtor 3, Germany; email: matthias.hoffmann@botanik.uni-halle.de LA - English DB - MTMT ER - TY - JOUR AU - Kajtoch, Łukasz AU - Elżbieta, Cieślak AU - Varga, Zoltán Sándor AU - Wojciech, Paul AU - Miłosz A, Mazur AU - Sramkó, Gábor AU - Daniel, Kubisz TI - Phylogeographic patterns of steppe species in Eastern Central Europe: a review and the implications for conservation JF - BIODIVERSITY AND CONSERVATION J2 - BIODIVERS CONSERV VL - 25 PY - 2016 IS - 12 SP - 2309 EP - 2339 PG - 31 SN - 0960-3115 DO - 10.1007/s10531-016-1065-2 UR - https://m2.mtmt.hu/api/publication/3024279 ID - 3024279 N1 - Institute of Systematics and Evolution of Animals, Polish Academy of Sciences, Krakow, Poland W. Szafer Institute of Botany, Polish Academy of Sciences, Krakow, Poland Department of Evolutionary Zoology, University of Debrecen, Debrecen, Hungary Center for Biodiversity Studies, Opole University, Opole, Poland Department of Botany, University of Debrecen, Debrecen, Hungary MTA-ELTE-MTM Ecology Research Group, Budapest, Hungary Cited By :71 Export Date: 3 January 2023 CODEN: BONSE Correspondence Address: Kajtoch, Ł.; Institute of Systematics and Evolution of Animals, Poland; email: lukasz.kajtoch@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Mraz, Patrik AU - Ronikier, Michal TI - Biogeography of the Carpathians: evolutionary and spatial facets of biodiversity JF - BIOLOGICAL JOURNAL OF THE LINNEAN SOCIETY J2 - BIOL J LINN SOC VL - 119 PY - 2016 IS - 3 SP - 528 EP - 559 PG - 32 SN - 0024-4066 DO - 10.1111/bij.12918 UR - https://m2.mtmt.hu/api/publication/26242202 ID - 26242202 N1 - Cited By :20 Export Date: 9 December 2018 CODEN: BJLSB Correspondence Address: Ronikier, M.; W. Szafer Institute of Botany, Polish Academy of Sciences, Lubicz 46, Poland; email: m.ronikier@botany.pl Cited By :19 Export Date: 12 December 2018 CODEN: BJLSB Correspondence Address: Ronikier, M.; W. Szafer Institute of Botany, Polish Academy of Sciences, Lubicz 46, Poland; email: m.ronikier@botany.pl Cited By :42 Export Date: 20 February 2020 CODEN: BJLSB Funding Agency and Grant Number: Switzerland through the Swiss Contribution [PSPB-161/2010]; Committee of Botany of the Polish Academy of Sciences; Foundation for Polish Botany; Switzerland through the Swiss Contribution to the enlarged European Union (Polish-Swiss Research Program) [PSPB-161/2010]; W. Szafer Institute of Botany, Polish Academy of Sciences in Krakow Funding text: The First Interdisciplinary Symposium Biogeography of the Carpathians: Evolution of biodiversity in a spatiotemporal context (http://bio.botany.pl/carpathiansbiogeography) and related outputs was financially supported by a grant from Switzerland through the Swiss Contribution to the enlarged European Union (Polish-Swiss Research Program, project no. PSPB-161/2010), by the Committee of Botany of the Polish Academy of Sciences, and by the Foundation for Polish Botany. We are indebted to John Allen, Editor of the Biological Journal of the Linnean Society, for the possibility of publishing this special issue, his invaluable help and advice during editorial work, and for his comments on earlier versions of this manuscript, as well as to Charlene Lim, Production Editor, for excellent assistance with technical aspects of the publication. We also thank A. Ronikier, P. Schonswetter, P. Sklenar, and T. Suchan for their useful comments on the first draft, as well as V. Mrazova, A. Ronikier, and P. Turis, for their kind help with preparing maps and plates. A. Guttova, B. Hurdu, L. Kajtoch, L'. Kovac, A. Kristin, K. Misikova, L. Sliwa, T. Schmitt, P. Turis, and J. Vana provided some literature sources and/or consultations. Colleagues who kindly provided their original photographs are acknowledged in captions of Figures 2 and 3. P. Mraz was supported by institutional funding by the Charles University. M. Ronikier was financially supported by a grant from Switzerland through the Swiss Contribution to the enlarged European Union (Polish-Swiss Research Program, project no. PSPB-161/2010) and by statutory funds of the W. Szafer Institute of Botany, Polish Academy of Sciences in Krakow. Cited By :55 Export Date: 16 December 2020 CODEN: BJLSB Correspondence Address: Ronikier, M.; W. Szafer Institute of Botany, Polish Academy of Sciences, Lubicz 46, Poland; email: m.ronikier@botany.pl Cited By :62 Export Date: 22 April 2021 CODEN: BJLSB Correspondence Address: Ronikier, M.; W. Szafer Institute of Botany, Lubicz 46, Poland; email: m.ronikier@botany.pl AB - The Carpathians are the largest mountain range in Central Europe. Their geographical position, extent, isolation, landscape heterogeneity, well-preserved environment, and relatively low impact of Quaternary glaciations make them of utmost importance for studies on European biodiversity and biogeography. In this review, introducing a Special Issue of the Biological Journal of the Linnean Society, we provide an overview of current research and focus on three main aspects: (1) distribution patterns and species richness including endemism; (2) phylogeographical patterns, inference of major barriers, and divergence areas; and (3) cytological studies and cytogeography inferred from vascular plant polyploid complexes. Our survey shows that, although accurate estimation is not possible for several important taxonomic entities because of unavailable or dispersed data, the Carpathians are a clear hotspot of European diversity for many groups of organisms, such as mammals, breeding birds, amphibians, lichens, and vascular plants. Certain groups, not necessarily those with high species richness, are rich in endemic taxa. This holds mainly for subterranean invertebrates, molluscs, grasshoppers, beetles, spiders, and vascular plants. Distribution patterns of endemic richness vary across taxonomic groups, as well as geographically, reflecting both history and habitat features. In general, the South-Eastern Carpathians have a significantly higher proportion of endemic taxa than the northerly-situated Western Carpathians. Molecular clock-based estimations have provided some insight into the diversification age of the Carpathian biota, including a Tertiary origin for some endemic taxa and lineages, especially those confined to environmentally stable habitats. Distribution patterns, as well as phylogeographical and phylogenetic data, corroborate the persistence of many high-mountain and forest taxa during the Quaternary climatic oscillations, often in multiple spatially delimited areas isolated by physical barriers. Several studies show that the Carpathian massifs played an important role as refugia for rare lineages and/or as stepping stones in migrations. Phylogeographical analysis reveals clear patterns of biogeographical breaks, as well as links, although clear exceptions also confirm that extant distribution patterns are often shaped more by idiosyncratic processes acting at different geological times. Cytogeographical data also uncover several consistent patterns, which probably reflect a deeper evolutionary history. In conclusion, the available data highlight the unique position of the Carpathians in the evolution and preservation of European biota within the European Alpine System. LA - English DB - MTMT ER - TY - JOUR AU - Nerudova, Z AU - Dolakova, N AU - Novak, J TI - New information augmenting the picture of local environment at the LGM/LGT in the context of the Middle Danube region JF - HOLOCENE J2 - HOLOCENE VL - 26 PY - 2016 IS - 9 SP - 1345 EP - 1354 PG - 10 SN - 0959-6836 DO - 10.1177/0959683616640051 UR - https://m2.mtmt.hu/api/publication/26204591 ID - 26204591 N1 - Cited By :7 Export Date: 25 May 2022 CODEN: HOLOE Correspondence Address: Nerudová, Z.; Moravian Museum, Zelný trh 6, Czech Republic; email: znerudova@mzm.cz LA - English DB - MTMT ER - TY - JOUR AU - Pryor, A J E AU - Pullen, A AU - Beresford-Jones, D G AU - Svoboda, J A AU - Gamble, C S TI - Reflections on Gravettian firewood procurement near the Pavlov Hills, Czech Republic JF - JOURNAL OF ANTHROPOLOGICAL ARCHAEOLOGY J2 - J ANTHROPOL ARCHAEOL VL - 43 PY - 2016 SP - 1 EP - 12 PG - 12 SN - 0278-4165 DO - 10.1016/j.jaa.2016.05.003 UR - https://m2.mtmt.hu/api/publication/26207192 ID - 26207192 N1 - Department of Archaeology, Faculty of Humanities, University of Southampton, Avenue Campus, Highfield, Southampton, SO17 1BF, United Kingdom McDonald Institute for Archaeological Research, University of Cambridge, Downing Street, Cambridge, CB2 3ER, United Kingdom Department of Anthropology, Faculty of Sciences, Masaryk University, Kotlářská 2, Brno, 61137, Czech Republic Cited By :8 Export Date: 25 May 2022 Correspondence Address: Pryor, A.J.E.; Department of Archaeology, Avenue Campus, Highfield, United Kingdom; email: Alex.Pryor@soton.ac.uk LA - English DB - MTMT ER - TY - JOUR AU - Skrdla, Petr AU - Nejman, Ladislav AU - Bartik, Jaroslav AU - Rychtarikova, Tereza AU - Nikolajev, Pavel AU - Eigner, Jan AU - Fisakova, Miriam Nyvltova AU - Novak, Jan AU - Polanska, Michaela TI - Mohelno - A terminal Last Glacial Maximum industry with microlithic tools made on carenoidal blanks JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 406 PY - 2016 IS - Part A SP - 184 EP - 194 PG - 11 SN - 1040-6182 DO - 10.1016/j.quaint.2015.05.055 UR - https://m2.mtmt.hu/api/publication/26033190 ID - 26033190 N1 - Part number: A LA - English DB - MTMT ER - TY - JOUR AU - Újvári, Gábor AU - Kok, J F AU - Varga, György AU - Kovács, János TI - The physics of wind-blown loess: Implications for grain size proxy interpretations in Quaternary paleoclimate studies JF - EARTH-SCIENCE REVIEWS J2 - EARTH-SCI REV VL - 154 PY - 2016 SP - 247 EP - 278 PG - 32 SN - 0012-8252 DO - 10.1016/j.earscirev.2016.01.006 UR - https://m2.mtmt.hu/api/publication/3011427 ID - 3011427 N1 - Funding Agency and Grant Number: Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [OTKA PD-108639]; Bolyai Janos Research Scholarship of the Hungarian Academy of SciencesHungarian Academy of Sciences [BO/00326/15/10]; Directorate For GeosciencesNational Science Foundation (NSF)NSF - Directorate for Geosciences (GEO) [1358621] Funding Source: National Science Foundation; Div Atmospheric & Geospace SciencesNational Science Foundation (NSF)NSF - Directorate for Geosciences (GEO) [1358621] Funding Source: National Science Foundation Funding text: This work has been funded by a post doc project from the Hungarian Scientific Research Fund to GU (OTKA PD-108639). Additional financial support provided by the Bolyai Janos Research Scholarship of the Hungarian Academy of Sciences (BO/00326/15/10) (GU, GV) is gratefully acknowledged. Constructive and insightful comments by Joe Mason and Thomas Stevens improved this paper substantially. Editorial handling and comments by Ian Candy is appreciated. Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi u. 45., Budapest, H-1112, Hungary Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Acaemy of Sciences, Csatkai E. u. 6-8., Sopron, H-9400, Hungary Department of Atmospheric and Oceanic Sciences, University of California, 405 Hilgard Ave, Los Angeles, CA 90095, United States Geographical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi út 45., Budapest, H-1112, Hungary Department of Geology and Meteorology, University of Pécs, Ifjúság u. 6., Pécs, H-7624, Hungary Environmental Analytical and Geoanalytical Laboratory, Szentágothai Research Centre, University of Pécs, Ifjúság u. 20., Pécs, H-7624, Hungary Cited By :87 Export Date: 16 February 2021 Correspondence Address: Újvári, G.; Institute for Geological and Geochemical Research, Budaörsi u. 45., Hungary; email: ujvari.gabor@csfk.mta.hu Funding details: Magyar Tudományos Akadémia, MTA, BO/00326/15/10 ) Funding details: Hungarian Scientific Research Fund, OTKA Funding details: Hungarian Scientific Research Fund, OTKA, PD-108639 Funding text 1: This work has been funded by a post doc project from the Hungarian Scientific Research Fund to GÚ ( OTKA PD-108639 ). Additional financial support provided by the Bolyai János Research Scholarship of the Hungarian Academy of Sciences ( BO/00326/15/10 ) (GÚ, GV) is gratefully acknowledged. Constructive and insightful comments by Joe Mason and Thomas Stevens improved this paper substantially. Editorial handling and comments by Ian Candy is appreciated. AB - Loess deposits are recorders of aeolian activity during past glaciations. Since the size distribution of loess deposits depends on distance to the dust source, and environmental conditions at the source, during transport, and at deposition, loess particle size distributions and derived statistical measures are widely used proxies in Quaternary paleoenvironmental studies. However, the interpretation of these proxies often only considers dust transport processes. To move beyond such overly simplistic proxy interpretations, and toward proxy interpretations that consider the range of environmental processes that determine loess particle size distribution variations we provide a comprehensive review on the physics of dust particle mobilization and deposition. Furthermore, using high-resolution bulk loess and quartz grain size datasets from a last glacial/interglacial sequence, we show that, because grain size distributions are affected by multiple, often stochastic processes, changes in these distributions over time allow multiple interpretations for the driving processes. Consequently, simplistic interpretations of proxy variations in terms of only one factor (e.g. wind speed) are likely to be inaccurate. Nonetheless using loess proxies to understand temporal changes in the dust cycle and environmental parameters requires (i) a careful site selection, to minimize the effects of topography and source distance, and (ii) the joint use of bulk and quartz grain size proxies, together with high resolution mass accumulation rate calculations if possible. © 2016 Elsevier B.V. LA - English DB - MTMT ER - TY - JOUR AU - Feurdean, A AU - Marinova, E AU - Nielsen, AB AU - Liakka, J AU - Veres, D AU - Hutchinson, SM AU - Braun, Mihály AU - Timar-Gabor, A AU - Astalos, C AU - Mosburgger, V AU - Hickler, T TI - Origin of the forest steppe and exceptional grassland diversity in Transylvania (central-eastern Europe) JF - JOURNAL OF BIOGEOGRAPHY J2 - J BIOGEOGR VL - 42 PY - 2015 IS - 5 SP - 951 EP - 963 PG - 13 SN - 0305-0270 DO - 10.1111/jbi.12468 UR - https://m2.mtmt.hu/api/publication/2970162 ID - 2970162 LA - English DB - MTMT ER - TY - JOUR AU - Hais, Martin AU - Komprdova, Klara AU - Ermakov, Nikolai AU - Chytry, Milan TI - Modelling the Last Glacial Maximum environments for a refugium of Pleistocene biota in the Russian Altai Mountains, Siberia JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 438 PY - 2015 SP - 135 EP - 145 PG - 11 SN - 0031-0182 DO - 10.1016/j.palaeo.2015.07.037 UR - https://m2.mtmt.hu/api/publication/25326642 ID - 25326642 N1 - Cited By :23 Export Date: 25 May 2022 CODEN: PPPYA Correspondence Address: Chytrý, M.; Department of Botany and Zoology, Kotlářská 2, Czech Republic LA - English DB - MTMT ER - TY - JOUR AU - Horsak, Michal AU - Chytry, Milan AU - Hajkova, Petra AU - Hajek, Michal AU - Danihelka, Jiri AU - Horsakova, Veronika AU - Ermakov, Nikolai AU - German, Dmitry A AU - Koci, Martin AU - Lustyk, Pavel AU - Nekola, Jeffrey C AU - Preislerova, Zdenka AU - Valachovic, Milan TI - European glacial relict snails and plants: environmental context of their modern refugial occurrence in southern Siberia JF - BOREAS J2 - BOREAS VL - 44 PY - 2015 IS - 4 SP - 638 EP - 657 PG - 20 SN - 0300-9483 DO - 10.1111/bor.12133 UR - https://m2.mtmt.hu/api/publication/25326643 ID - 25326643 N1 - Funding Agency and Grant Number: Czech Science Foundation [P504/11/0454]; [RVO 67985939]; Russian Science Foundation [14-14-00453] Funding Source: Russian Science Foundation Funding text: Many thanks go to our Russian colleagues for their logistic support and help in the field and Ondrej Hajek for preparing the climate data and the map. We are very grateful to Olivier Moine, John Birks and Richard Preece for many valuable comments and improvements of the manuscript. This study was supported by the Czech Science Foundation (P504/11/0454), the institutional support of Masaryk University, and the longterm research development project no. RVO 67985939. LA - English DB - MTMT ER - TY - JOUR AU - Kołaczek, P AU - Gałka, M AU - Karpińska-Kołaczek, M TI - Succession of arboreal taxa during the Late Glacial in south-eastern Poland: Climatic implications JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 421 PY - 2015 SP - 1 EP - 14 PG - 14 SN - 0031-0182 DO - 10.1016/j.palaeo.2015.01.007 UR - https://m2.mtmt.hu/api/publication/24428501 ID - 24428501 N1 - Cited By :8 Export Date: 25 May 2022 CODEN: PPPYA Correspondence Address: Kołaczek, P.; Department of Biogeography and Palaeoecology, Faculty of Geographical and Geological Sciences, Adam Mickiewicz University, Dziegielowa 27, Poland LA - English DB - MTMT ER - TY - JOUR AU - Łanczont, M AU - Madeyska, T AU - Mroczek, P AU - Komar, M AU - Łacka, B AU - Bogucki, A AU - Sobczyk, K AU - Wilczyński, J TI - The loess-palaeosol sequence in the upper palaeolithic site at Kraków spadzista: A palaeoenvironmental approach JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 365 PY - 2015 SP - 98 EP - 113 PG - 16 SN - 1040-6182 DO - 10.1016/j.quaint.2014.11.033 UR - https://m2.mtmt.hu/api/publication/25145421 ID - 25145421 N1 - Department of Geoecology and Palaeogeography, Maria Curie-Skłodowska University, Lublin, Kraśnicka 2cd, Lublin, 20-718, Poland Institute of Geological Sciences, Polish Academy of Sciences, Warsaw, Twarda 51/55, Warszawa, 00-818, Poland Institute of Geological Sciences, National Academy of Sciences of Ukraine, Gonchara 55B, Kyiv, 01601, Ukraine National Museum of Natural History, National Academy of Sciences of Ukraine, 15 Bohdan Khmelnitsky, Kyiv, 01601, Ukraine Department of Geomorphology and Palaeogeography, Ivan Franko National University, Doroshenka 41, Lviv, 79000, Ukraine Institute of Archaeology, Jagiellonian University, Gołebia 11, Kraków, 31-007, Poland Institute of Systematics and Evolution of Animals, Polish Academy of Sciences, Sławkowska 17, Kraków, 31-016, Poland Cited By :11 Export Date: 25 May 2022 Correspondence Address: Mroczek, P.; Department of Geoecology and Palaeogeography, Kraśnicka 2cd, Poland; email: przemyslaw.mroczek@umcs.pl LA - English DB - MTMT ER - TY - JOUR AU - Mitka, Józef AU - Wróblewska, Ada AU - Bąba, Wojciech AU - Watrak, Grzegorz AU - Wątroba, Marta AU - Boroń, Piotr TI - Pochodzenie Galium schultesii i Stellaria holostea w Bieszczadach (Karpaty Wschodnie) : refugium glacjalne czy genetyczny tygiel? [The origins of Galium schultesii and Stellaria holostea in the Bieszczady Mts (Eastern Carpathians) : glacial refugium or genetic melting pot?] JF - Roczniki Bieszczadzkie J2 - Roczniki Bieszczadzkie VL - 23 PY - 2015 IS - 17 SP - 54 SN - 1233-1910 UR - https://m2.mtmt.hu/api/publication/32266984 ID - 32266984 LA - Polish DB - MTMT ER - TY - JOUR AU - Monegato, G AU - Ravazzi, C AU - Culiberg, M AU - Pini, R AU - Bavec, M AU - Calderoni, G AU - Jez, J AU - Perego, R TI - Sedimentary evolution and persistence of open forests between the south-eastern Alpine fringe and the Northern Dinarides during the Last Glacial Maximum JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 436 PY - 2015 SP - 23 EP - 40 PG - 18 SN - 0031-0182 DO - 10.1016/j.palaeo.2015.06.025 UR - https://m2.mtmt.hu/api/publication/27496786 ID - 27496786 N1 - CNR, Institute of Geosciences and Earth Resources, Via Valperga Caluso 35, Torino, 10125, Italy CNR, Institute for the Dynamics of Environmental Processes, Lab. of Palynology and Palaeoecology, Piazza della Scienza 1, Milano, 20126, Italy Jovan Hadži Institute of Biology, Slovenian Academy of Sciences, Novi trg 5, Ljubljana, 1000, Slovenia Geological Survey of Slovenia, Dimičeva ulica 14, Ljubljana, 1000, Slovenia Dept. of Earth Sciences, University La Sapienza, Piazzale A. Moro 5, Roma, 00185, Italy CNR, Institute of Environmental Geology and Geoengineering, Area della Ricerca Roma 1, Montelibretti, Monterotondo, 00015, Italy Integrative Prehistory and Archaeological Science, University of Basel, Spalenring 145, Basel, 4055, Switzerland Cited By :26 Export Date: 25 May 2022 CODEN: PPPYA Correspondence Address: Monegato, G.; CNR, Institute of Geosciences and Earth Resources, Via Valperga Caluso 35, Italy LA - English DB - MTMT ER - TY - JOUR AU - Pokorny, Petr AU - Chytry, Milan AU - Jurickova, Lucie AU - Sadlo, Jiri AU - Novak, Jan AU - Lozek, Vojen TI - Mid-Holocene bottleneck for central European dry grasslands: Did steppe survive the forest optimum in northern Bohemia, Czech Republic? JF - HOLOCENE J2 - HOLOCENE VL - 25 PY - 2015 IS - 4 SP - 716 EP - 726 PG - 11 SN - 0959-6836 DO - 10.1177/0959683614566218 UR - https://m2.mtmt.hu/api/publication/25644183 ID - 25644183 N1 - Megjegyzés-24582728 N1 10.1177/0959683614566218 LA - English DB - MTMT ER - TY - JOUR AU - Feurdean, A AU - Perşoiu, A AU - Tanţău, I AU - Stevens, T AU - Magyari, Enikő Katalin AU - Onac, BP AU - Marković, S AU - Andrič, M AU - Connor, S AU - Fărcaş, S AU - Gałka, M AU - Gaudenyi, Tivadar AU - Hoek, W AU - Kolaczek, P AU - Kuneš, P AU - Lamentowicz, M AU - Marinova, E AU - Michczyńska, DJ AU - Perşoiu, I AU - Płóciennik, M AU - Słowiński, M AU - Stancikaite, M AU - Sümegi, Pál AU - Svensson, A AU - Tămaş, T AU - Timar, A AU - Tonkov, S AU - Tóth, Mónika AU - Veski, S AU - Willis, KJ AU - Zernitskaya, V TI - Climate variability and associated vegetation response throughout Central and Eastern Europe (CEE) between 60 and 8 ka JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 106 PY - 2014 SP - 206 EP - 224 PG - 19 SN - 0277-3791 DO - 10.1016/j.quascirev.2014.06.003 UR - https://m2.mtmt.hu/api/publication/2706681 ID - 2706681 N1 - Available online 1 July 2014 AB - Abstract Records of past climate variability and associated vegetation response exist in various regions throughout Central and Eastern Europe (CEE). To date, there has been no coherent synthesis of the existing palaeo-records. During an INTIMATE meeting (Cluj Napoca, Romania) focused on identifying CEE paleo-records, it was decided to address this gap by presenting the palaeo-community with a compilation of high-quality climatic and vegetation records for the past 60–8 ka. The compilation should also serve as a reference point for the use in the modelling community working towards the INTIMATE project goals, and in data-model inter-comparison studies. This paper is therefore a compilation of up to date, best available quantitative and semi-quantitative records of past climate and biotic response from CEE covering this period. It first presents the proxy and archive used. Speleothems and loess mainly provide the evidences available for the 60–20 ka interval, whereas pollen records provide the main source of information for the Lateglacial and Holocene. It then examines the temporal and spatial patterns of climate variability inferred from different proxies, the temporal and spatial magnitude of the vegetation responses inferred from pollen records and highlights differences and similarities between proxies and sub-regions and the possible mechanisms behind this variability. Finally, it identifies weakness in the proxies and archives and their geographical distribution. This exercise also provides an opportunity to reflect on the status of research in the area and to identify future critical areas and subjects of research. LA - English DB - MTMT ER - TY - JOUR AU - Magyari, Enikő Katalin AU - Veres, D AU - Wennrich, V AU - Wagner, B AU - Braun, Mihály AU - Jakab, Gusztáv AU - Karátson, Dávid AU - Pál, Z AU - Ferenczy, Gy AU - St-Onge, G AU - Rethemeyer, J AU - Francois, J-P AU - von Reumont, F AU - Schäbitz, F TI - Vegetation and environmental responses to climate forcing during the last glacial maximum and deglaciation in the East Carpathians: attenuated response to maximum cooling and increased biomass burning JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 106 PY - 2014 SP - 278 EP - 298 PG - 21 SN - 0277-3791 DO - 10.1016/j.quascirev.2014.09.015 UR - https://m2.mtmt.hu/api/publication/2743488 ID - 2743488 LA - English DB - MTMT ER -