@article{MTMT:34267763, title = {Holocene vegetation dynamics of the Eastern Mediterranean region : old controversies addressed by a new analysis}, url = {https://m2.mtmt.hu/api/publication/34267763}, author = {Cruz‐Silva, E and Harrison, S P and Prentice, I C and Marinova, E}, doi = {10.1111/jbi.14749}, journal-iso = {J BIOGEOGR}, journal = {JOURNAL OF BIOGEOGRAPHY}, volume = {51}, unique-id = {34267763}, issn = {0305-0270}, year = {2024}, eissn = {1365-2699}, pages = {294-310}, orcid-numbers = {Harrison, S P/0000-0001-5687-1903; Prentice, I C/0000-0002-1296-6764} } @article{MTMT:34608221, title = {High-resolution ecosystem changes pacing the millennial climate variability at the Middle to Upper Palaeolithic transition in NE-Italy}, url = {https://m2.mtmt.hu/api/publication/34608221}, author = {Badino, Federica and Pini, Roberta and Ravazzi, Cesare and Chytry, Milan and Bertuletti, Paolo and Bortolini, Eugenio and Dudova, Lydie and Peresani, Marco and Romandini, Matteo and Benazzi, Stefano}, doi = {10.1038/s41598-023-38081-1}, journal-iso = {SCI REP}, journal = {SCIENTIFIC REPORTS}, volume = {13}, unique-id = {34608221}, issn = {2045-2322}, abstract = {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.}, year = {2023}, eissn = {2045-2322}, orcid-numbers = {Dudova, Lydie/0000-0002-0610-0630; Peresani, Marco/0000-0001-6562-6336} } @article{MTMT:34105792, title = {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}, url = {https://m2.mtmt.hu/api/publication/34105792}, author = {Darabos, Gabriella and Magyari, Enikő Katalin and Szabó, Zoltán and Lisztes-Szabó, Zsuzsa and Veres, D and Haliuc, A and Reitmeyer, B and Pálfi, Ivett}, doi = {10.23928/foldt.kozl.2023.153.2.143}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {153}, unique-id = {34105792}, issn = {0015-542X}, abstract = {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.}, year = {2023}, eissn = {2559-902X}, pages = {143-163}, orcid-numbers = {Darabos, Gabriella/0000-0001-8070-5630; Magyari, Enikő Katalin/0000-0002-2844-8937; Lisztes-Szabó, Zsuzsa/0000-0002-6322-8542; Veres, D/0000-0003-3932-577X; Haliuc, A/0000-0002-5681-8210; Pálfi, Ivett/0000-0001-9814-3410} } @article{MTMT:33777210, title = {Characterization and mapping of MIS‐2 thermal contraction crack polygons in Western Transdanubia, Hungary}, url = {https://m2.mtmt.hu/api/publication/33777210}, author = {Farkas, Beáta and Sipos, György and Bartyik, Tamás and Józsa, Edina and Czigány, Szabolcs and Balogh, Richárd and Varga, Gábor and Kovács, János and Fábián, Szabolcs Ákos}, doi = {10.1002/ppp.2190}, journal-iso = {PERMAFROST PERIGLAC}, journal = {PERMAFROST AND PERIGLACIAL PROCESSES}, volume = {34}, unique-id = {33777210}, issn = {1045-6740}, year = {2023}, pages = {417-427}, orcid-numbers = {Farkas, Beáta/0000-0002-7026-8980; Sipos, György/0000-0001-6224-2361; Czigány, Szabolcs/0000-0002-9158-3162; Kovács, János/0000-0001-7742-5515; Fábián, Szabolcs Ákos/0000-0001-9127-2113} } @book{MTMT:33733446, title = {A Kárpátok legfiatalabb tűzhányója, a Csomád. Vulkánosság, őskörnyezet, ember és táj.}, url = {https://m2.mtmt.hu/api/publication/33733446}, isbn = {9786069716472}, editor = {Karátson, Dávid and Veres, D. and Gertisser, R. and Magyari, Enikő Katalin and Jánosi, C. and Hambach, U.}, publisher = {Tortoma Könyvkiadó}, unique-id = {33733446}, year = {2023}, orcid-numbers = {Karátson, Dávid/0000-0003-0386-1239; Magyari, Enikő Katalin/0000-0002-2844-8937} } @article{MTMT:33550234, title = {Well-preserved Norway spruce needle phytoliths in sediments can be a new paleoenvironmental indicator}, url = {https://m2.mtmt.hu/api/publication/33550234}, author = {Lisztes-Szabó, Zsuzsa and Tóth, Albert and Buró, Botond and Braun, Ádám and Csík, Attila and Filep, Anna Fruzsina and Kuneš, Petr and Braun, Mihály}, doi = {10.1177/09596836221145361}, journal-iso = {HOLOCENE}, journal = {HOLOCENE}, volume = {33}, unique-id = {33550234}, issn = {0959-6836}, abstract = {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.}, year = {2023}, eissn = {1477-0911}, pages = {471-477}, orcid-numbers = {Lisztes-Szabó, Zsuzsa/0000-0002-6322-8542; Csík, Attila/0000-0002-8173-9653; Kuneš, Petr/0000-0001-9605-8204} } @article{MTMT:34007320, title = {Lösz-paleotalaj sorozatokban megőrződött fitolitkészletek környezettörténeti és környezet régészeti vonatkozású kutatási lehetőségei}, url = {https://m2.mtmt.hu/api/publication/34007320}, author = {Milinkó, István and Novothny, Ágnes and Pető, Ákos}, doi = {10.55023/issn.1786-271X.2023-006}, journal-iso = {ARCHEOMETRIAI MŰHELY}, journal = {ARCHEOMETRIAI MŰHELY}, volume = {20}, unique-id = {34007320}, issn = {1786-271X}, abstract = {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.}, year = {2023}, pages = {93-114}, orcid-numbers = {Novothny, Ágnes/0000-0003-3513-0406} } @article{MTMT:34243231, title = {Perhaps there were northern refugia in LGM? The phylogeographic structure of the thermophilic tree Carpinus betulus in the Carpathian region}, url = {https://m2.mtmt.hu/api/publication/34243231}, author = {Mitka, Jozef and Wroblewaka, Ada and Boron, Piotr and Kucharzyk, Stanislaw and Stachurska-Swakon, Alina}, doi = {10.1016/j.scitotenv.2023.167214}, journal-iso = {SCI TOTAL ENVIRON}, journal = {SCIENCE OF THE TOTAL ENVIRONMENT}, volume = {905}, unique-id = {34243231}, issn = {0048-9697}, abstract = {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.}, keywords = {Carpathian Mountains; LGM; hornbeam; Diffused microrefugia; Genetic melting pot}, year = {2023}, eissn = {1879-1026}, orcid-numbers = {Stachurska-Swakon, Alina/0000-0003-0381-4520} } @article{MTMT:34119273, title = {Is there a massive glacial–Holocene flora continuity in Central Europe?}, url = {https://m2.mtmt.hu/api/publication/34119273}, author = {Molnár, Ábel Péter and Demeter, László and Biró, Marianna and Chytrý, Milan and Bartha, Sándor and Batdelger, Gantuya and Molnár, Zsolt}, doi = {10.1111/brv.13007}, journal-iso = {BIOL REV}, journal = {BIOLOGICAL REVIEWS}, volume = {98}, unique-id = {34119273}, issn = {1464-7931}, abstract = {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.}, year = {2023}, eissn = {1469-185X}, pages = {2307-2319}, orcid-numbers = {Demeter, László/0000-0003-2343-2570; Bartha, Sándor/0000-0001-6331-7521} } @article{MTMT:34608222, title = {Well-hidden forests? Modern pollen spectra from Central Yakutia (Eastern Siberia) contribute to the interpretation of the last glacial vegetation in Central Europe}, url = {https://m2.mtmt.hu/api/publication/34608222}, author = {Prach, Jindrich and Hosek, Jan and Pokorna, Adela and Hoskova, Kristyna and Pokorny, Petr}, doi = {10.1007/s12224-023-09435-4}, journal-iso = {FOLIA GEOBOT}, journal = {FOLIA GEOBOTANICA}, unique-id = {34608222}, issn = {1211-9520}, abstract = {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.}, keywords = {VEGETATION HISTORY; POLLEN ANALYSIS; late glacial; Larix; modern analogues}, year = {2023}, eissn = {1874-9348} } @article{MTMT:34172601, title = {Demographic History of Scots Pine in the Pleistocene in Northern Eurasia and the Caucasus Region Based on an Analysis of Nuclear Microsatellite Loci}, url = {https://m2.mtmt.hu/api/publication/34172601}, author = {Semerikov, N. V. and Petrova, I. V.}, doi = {10.1134/S1995425523050116}, journal-iso = {CONTEMP PROBL ECOL}, journal = {CONTEMPORARY PROBLEMS OF ECOLOGY}, volume = {16}, unique-id = {34172601}, issn = {1995-4255}, year = {2023}, eissn = {1995-4263}, pages = {549-563} } @article{MTMT:34450692, title = {Decoupled phylogenetic and functional diversity in European grasslands}, url = {https://m2.mtmt.hu/api/publication/34450692}, author = {Večeřa, Martin and Axmanová, Irena and Chytrý, Milan and Divíšek, Jan and Ndiribe, Charlotte and Velasco Mones, Gonzalo and Čeplová, Natálie and Aćić, Svetlana and Bahn, Michael and Bergamini, Ariel and Boenisch, Gerhard and Biurrun, Idoia and Bruun, Hans Henrik and Byun, Chaeho and Catford, Jane A. and Cerabolini, Bruno E. L. and Cornelissen, Johannes H. C. and Dengler, Jürgen and Jansen, Florian and Jansen, Steven and Kattge, Jens and Kozub, Łukasz and Kuzemko, Anna and Minden, Vanessa and Mitchell, Rachel M. and Moeslund, Jesper E. and Mori, Akira S. and Niinemets, Ülo and Ruprecht, Eszter and Rūsiņa, Solvita and Šilc, Urban and Soudzilovskaia, Nadejda A. and van Bodegom, Peter M. and Vassilev, Kiril and Weiher, Evan and Wright, Ian J. and Lososová, Zdeňka}, doi = {10.23855/preslia.2023.413}, journal-iso = {PRESLIA}, journal = {PRESLIA}, volume = {95}, unique-id = {34450692}, issn = {0032-7786}, year = {2023}, eissn = {2570-950X}, pages = {413-445} } @article{MTMT:32633606, title = {Distribution and characteristics of Pleistocene ground thermal contraction polygons in Europe from satellite images}, url = {https://m2.mtmt.hu/api/publication/32633606}, author = {Bertran, P}, doi = {10.1002/ppp.2137}, journal-iso = {PERMAFROST PERIGLAC}, journal = {PERMAFROST AND PERIGLACIAL PROCESSES}, volume = {33}, unique-id = {32633606}, issn = {1045-6740}, year = {2022}, pages = {9-113}, orcid-numbers = {Bertran, P/0000-0003-3334-9869} } @article{MTMT:32894529, title = {Last Glacial Maximum active layer thickness in Western Europe, and the issue of ‘tundra gleys’ in loess sequences}, url = {https://m2.mtmt.hu/api/publication/32894529}, author = {Bertran, Pascal and Stadelmaier, Kim H. and Ludwig, Patrick}, doi = {10.1002/jqs.3434}, journal-iso = {J QUATERNARY SCI}, journal = {JOURNAL OF QUATERNARY SCIENCE}, volume = {2022}, unique-id = {32894529}, issn = {0267-8179}, year = {2022}, eissn = {1099-1417}, orcid-numbers = {Bertran, Pascal/0000-0003-3334-9869; Stadelmaier, Kim H./0000-0003-2023-0797; Ludwig, Patrick/0000-0003-3655-7890} } @article{MTMT:32771050, title = {Large-scale genetic structure of Quercus robur in its eastern distribution range enables assignment of unknown seed sources}, url = {https://m2.mtmt.hu/api/publication/32771050}, author = {Degen, Bernd and Yanbaev, Yulai and Ianbaev, Ruslan and Blanc-Jolivet, Celine and Mader, Malte and Bakhtina, Svetlana and Heinze, Berthold}, doi = {10.1093/forestry/cpac009}, journal-iso = {FORESTRY}, journal = {FORESTRY}, unique-id = {32771050}, issn = {0015-752X}, year = {2022}, eissn = {1464-3626}, orcid-numbers = {Degen, Bernd/0000-0001-9082-3163} } @article{MTMT:33195593, title = {Origin of the central European steppe flora: insights from palaeodistribution modelling and migration simulations}, url = {https://m2.mtmt.hu/api/publication/33195593}, author = {Divíšek, Jan and Večeřa, Martin and Welk, Erik and Danihelka, Jiří and Chytrý, Kryštof and Douda, Jan and Chytrý, Milan}, doi = {10.1111/ecog.06293}, journal-iso = {ECOGRAPHY}, journal = {ECOGRAPHY}, volume = {2022}, unique-id = {33195593}, issn = {0906-7590}, year = {2022}, eissn = {1600-0587}, orcid-numbers = {Divíšek, Jan/0000-0002-5127-5130; Večeřa, Martin/0000-0001-8507-791X; Welk, Erik/0000-0002-2685-3795; Danihelka, Jiří/0000-0002-2640-7867; Douda, Jan/0000-0002-1205-364X; Chytrý, Milan/0000-0002-8122-3075} } @article{MTMT:32760471, title = {Chronology and dynamics of fluvial style changes in the Younger Dryas and Early Holocene in Central Europe (lower San River, SE Poland)}, url = {https://m2.mtmt.hu/api/publication/32760471}, author = {Gębica, P and Michno, A and Sobucki, M and Wacnik, A and Superson, S}, doi = {10.1016/j.scitotenv.2022.154700}, journal-iso = {SCI TOTAL ENVIRON}, journal = {SCIENCE OF THE TOTAL ENVIRONMENT}, volume = {830}, unique-id = {32760471}, issn = {0048-9697}, year = {2022}, eissn = {1879-1026} } @article{MTMT:33000462, title = {Modern Pollen Assemblages From Lake Sediments and Soil in East Siberia and Relative Pollen Productivity Estimates for Major Taxa}, url = {https://m2.mtmt.hu/api/publication/33000462}, author = {Geng, Rongwei and Andreev, Andrei and Kruse, Stefan and Heim, Birgit and van Geffen, Femke and Pestryakova, Luidmila and Zakharov, Evgenii and Troeva, Elena and Shevtsova, Iuliia and Li, Furong and Zhao, Yan and Herzschuh, Ulrike}, doi = {10.3389/fevo.2022.837857}, journal-iso = {FRONT ECOL EVOL}, journal = {FRONTIERS IN ECOLOGY AND EVOLUTION}, volume = {10}, unique-id = {33000462}, issn = {2296-701X}, abstract = {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.}, keywords = {Tundra; Modern pollen assemblages; East Siberia; taiga; pollen-vegetation-climate relationships; relative pollen productivity; quantitative vegetation reconstruction}, year = {2022}, eissn = {2296-701X} } @book{MTMT:32186131, title = {Ciomadul (Csomád), The Youngest Volcano in the Carpathians}, url = {https://m2.mtmt.hu/api/publication/32186131}, isbn = {9783030891398}, doi = {10.1007/978-3-030-89140-4}, editor = {Karátson, Dávid and Veres, D. and Gertisser, R. and Magyari, Enikő Katalin and Jánosi, C. and Hambach, U.}, publisher = {Springer Netherlands}, unique-id = {32186131}, year = {2022}, orcid-numbers = {Karátson, Dávid/0000-0003-0386-1239; Magyari, Enikő Katalin/0000-0002-2844-8937} } @article{MTMT:32843008, title = {First records of Calamagrostis purpurea (Poaceae) in the Carpathians, a relict species new to the flora of Slovakia, Ukraine, and Romania}, url = {https://m2.mtmt.hu/api/publication/32843008}, author = {Kobiv, Y. and Koutecký, P. and Štech, M. and Pachschwöll, C.}, doi = {10.1007/s11756-022-01083-x}, journal-iso = {BIOLOGIA}, journal = {BIOLOGIA (BRATISLAVA)}, unique-id = {32843008}, issn = {0006-3088}, year = {2022}, eissn = {1336-9563} } @article{MTMT:32795556, title = {Mammal extinction facilitated biome shift and human population change during the last glacial termination in East-Central Europe}, url = {https://m2.mtmt.hu/api/publication/32795556}, author = {Magyari, Enikő Katalin and Gasparik, Mihály and Major, István and Lengyel, György and Pál, Ilona and Virág, Attila and Korponai, János and Haliuc, Aritina and Szabó, Zoltán and Pazonyi, Piroska}, doi = {10.1038/s41598-022-10714-x}, journal-iso = {SCI REP}, journal = {SCIENTIFIC REPORTS}, volume = {12}, unique-id = {32795556}, issn = {2045-2322}, abstract = {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.}, year = {2022}, eissn = {2045-2322}, orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Major, István/0000-0003-4675-9875; Lengyel, György/0000-0002-7803-3043; Virág, Attila/0000-0002-5530-0065; Korponai, János/0000-0003-0211-192X} } @{MTMT:33600537, title = {The Periglaciation of Europe}, url = {https://m2.mtmt.hu/api/publication/33600537}, author = {Oliva, M and Fernández-Fernández, JM. and Nývlt, D}, booktitle = {Periglacial Landscapes of Europe}, doi = {10.1007/978-3-031-14895-8_16}, unique-id = {33600537}, year = {2022}, pages = {477-523} } @article{MTMT:33245558, title = {Genotyping-by-sequencing reveals range expansion of Adonis vernalis (Ranunculaceae) from Southeastern Europe into the zonal Euro-Siberian steppe}, url = {https://m2.mtmt.hu/api/publication/33245558}, author = {Seidl, Anna and Tremetsberger, Karin and Pfanzelt, Simon and Lindhuber, Lisa and Kropf, Matthias and Neuffer, Barbara and Blattner, Frank R. and Király, Botond Gergely and Smirnov, Sergey V. and Friesen, Nikolai and Shmakov, Alexander I. and Plenk, Kristina and Batlai, Oyuntsetseg and Hurka, Herbert and Bernhardt, Karl-Georg}, doi = {10.1038/s41598-022-23542-w}, journal-iso = {SCI REP}, journal = {SCIENTIFIC REPORTS}, volume = {12}, unique-id = {33245558}, issn = {2045-2322}, abstract = {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.}, year = {2022}, eissn = {2045-2322}, orcid-numbers = {Király, Botond Gergely/0000-0002-8439-2616} } @article{MTMT:33000463, title = {Tempo and drivers of plant diversification in the European mountain system}, url = {https://m2.mtmt.hu/api/publication/33000463}, author = {Smycka, Jan and Roquet, Cristina and Boleda, Marti and Alberti, Adriana and Boyer, Frederic and Douzet, Rolland and Perrier, Christophe and Rome, Maxime and Valay, Jean-Gabriel and Denoeud, France and Semberova, Kristyna and Zimmermann, Niklaus E. and Thuiller, Wilfried and Wincker, Patrick and Alsos, Inger G. and Coissac, Eric and Layergne, Sebastien}, doi = {10.1038/s41467-022-30394-5}, journal-iso = {NAT COMMUN}, journal = {NATURE COMMUNICATIONS}, volume = {13}, unique-id = {33000463}, issn = {2041-1723}, abstract = {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.}, year = {2022}, eissn = {2041-1723}, orcid-numbers = {Roquet, Cristina/0000-0001-8748-3743; Alberti, Adriana/0000-0003-3372-9423; Boyer, Frederic/0000-0003-0021-9590; Denoeud, France/0000-0001-8819-7634; Zimmermann, Niklaus E./0000-0003-3099-9604} } @article{MTMT:33000461, title = {The Lateglacial and Early Holocene vegetation dynamics: New multi-proxy data from the central Belarus}, url = {https://m2.mtmt.hu/api/publication/33000461}, author = {Stancikaite, Migle and Zernitskaya, Valentina and Kluczynska, Grazyna and Valunas, Darius and Gedminiene, Laura and Uogintas, Domas and Skuratovic, Zana and Vlasov, Boris and Gasteviciene, Neringa and Ezerinskis, Zilvinas and Sapolaite, Justina and Seiriene, Vaida}, doi = {10.1016/j.quaint.2021.05.004}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {630}, unique-id = {33000461}, issn = {1040-6182}, abstract = {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.}, keywords = {POLLEN; VEGETATION HISTORY; Lake sediments; Belarus; Plant macro; Periglacial zone}, year = {2022}, eissn = {1873-4553}, pages = {121-136} } @article{MTMT:32544836, title = {Vegetation and land snail-based reconstruction of the palaeocological changes in the forest steppe eco-region of the Carpathian Basin during last glacial warming}, url = {https://m2.mtmt.hu/api/publication/32544836}, author = {Sümegi, Pál and Molnár, Dávid and Náfrádi, Katalin and Makó, László and Cseh, Péter and Törőcsik, Tünde and Molnár, Mihály and Zhou, Liping}, doi = {10.1016/j.gecco.2021.e01976}, journal-iso = {GLOB ECOL CONSERV}, journal = {GLOBAL ECOLOGY AND CONSERVATION}, volume = {33}, unique-id = {32544836}, issn = {2351-9894}, year = {2022}, eissn = {2351-9894}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741} } @article{MTMT:33538348, title = {Low altitude glacial relicts in the Romanian flora}, url = {https://m2.mtmt.hu/api/publication/33538348}, author = {Szatmari, P-M and Hurdu, B-I}, doi = {10.24193/Contrib.Bot.57.2}, journal-iso = {CONTR BOTANICE}, journal = {CONTRIBUTII BOTANICE}, volume = {57}, unique-id = {33538348}, issn = {0069-9616}, abstract = {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.}, year = {2022}, eissn = {2067-3094}, pages = {19-51}, orcid-numbers = {Szatmari, P-M/0000-0002-1393-6540; Hurdu, B-I/0000-0002-3165-108X} } @article{MTMT:32133278, title = {Limnological changes and chironomid-inferred summer air temperature from the Late Pleniglacial to the Early Holocene in the East Carpathians}, url = {https://m2.mtmt.hu/api/publication/32133278}, author = {Tóth, Mónika and Heiri, O and Vincze, Ildikó and Braun, Mihály and Szabó, Zoltán and Magyari, Enikő Katalin}, doi = {10.1017/qua.2021.36}, journal-iso = {QUATERNARY RES}, journal = {QUATERNARY RESEARCH}, volume = {105}, unique-id = {32133278}, issn = {0033-5894}, year = {2022}, eissn = {1096-0287}, pages = {151-165}, orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937} } @article{MTMT:32102652, title = {Revised map of European aeolian deposits derived from soil texture data}, url = {https://m2.mtmt.hu/api/publication/32102652}, author = {Bertran, P and Bosq, M and Borderie, Q and Coussot, C and Coutard, S and Deschodt, L and Franc, O and Gardère, P and Liard, M and Wuscher, P}, doi = {10.1016/j.quascirev.2021.107085}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {266}, unique-id = {32102652}, issn = {0277-3791}, keywords = {Europe; loess; cartography; coversand stratigraphy; LUCAS 2009 topsoil database}, year = {2021}, eissn = {1873-457X}, orcid-numbers = {Bertran, P/0000-0003-3334-9869; Bosq, M/0000-0003-0963-212X; Borderie, Q/0000-0002-2199-4038} } @article{MTMT:32746070, title = {Impact of Gene Flow and Introgression on the Range Wide Genetic Structure of Quercus robur (L.) in Europe}, url = {https://m2.mtmt.hu/api/publication/32746070}, author = {Degen, Bernd and Yanbaev, Yulai and Mader, Malte and Ianbaev, Ruslan and Bakhtina, Svetlana and Schroeder, Hilke and Blanc-Jolivet, Celine}, doi = {10.3390/f12101425}, journal-iso = {FORESTS}, journal = {FORESTS}, volume = {12}, unique-id = {32746070}, issn = {1999-4907}, abstract = {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.}, keywords = {DIFFERENTIATION; PATTERNS; DIVERSITY; Software; POLLEN; haplotype; STANDS; HYBRIDIZATION; gene flow; Quercus petraea; local adaptation; CHLOROPLAST DNA VARIATION; POLLEN DISPERSAL; white oaks; spatial genetic autocorrelation}, year = {2021}, eissn = {1999-4907}, orcid-numbers = {Degen, Bernd/0000-0001-9082-3163} } @article{MTMT:32746071, title = {A Multi-Dimensional Approach to Investigate Use-Related Biogenic Residues on Palaeolithic Ground Stone Tools}, url = {https://m2.mtmt.hu/api/publication/32746071}, author = {Longo, Laura and Altieri, Simona and Birarda, Giovanni and Cagnato, Clarissa and Graziani, Valerio and Obada, Theodor and Pantyukhina, Irina and Ricci, Paola and Skakun, Natalia and Sorrentino, Giusi and Terekhina, Vera and Tortora, Luca and Vaccari, Lisa and Lubritto, Carmine}, doi = {10.1080/14614103.2021.1975252}, journal-iso = {ENVIRON ARCHAEOL}, journal = {ENVIRONMENTAL ARCHAEOLOGY}, unique-id = {32746071}, issn = {1461-4103}, abstract = {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.}, keywords = {EXTRACTION; ACID; Starch; CONSUMPTION; ARCHAEOLOGY; FOOD; SEM; Raman; exploitation; HUMAN SKIN; GRAINS; Environmental Sciences; OM; Starch granules; Wear-traces; Ground stones}, year = {2021}, eissn = {1749-6314}, orcid-numbers = {Longo, Laura/0000-0001-6562-3047; Altieri, Simona/0000-0001-8673-8812; Cagnato, Clarissa/0000-0002-2010-1437; Pantyukhina, Irina/0000-0001-6206-5799} } @article{MTMT:31969601, title = {Cultural evolution and environmental change in Central Europe between 40 and 15 ka}, url = {https://m2.mtmt.hu/api/publication/31969601}, author = {Maier, A and Stojakowits, P and Mayr, C and Pfeifer, S and Preusser, F and Zolitschka, B and Anghelinu, M and Bobak, D and Duprat-Oualid, F and Einwögerer, T and Hambach, U and Händel, M and Kaminská, L and Kämpf, L and Łanczont, M and Lehmkuhl, F and Ludwig, P and Magyari, Enikő Katalin and Mroczek, P and Nemergut, A and Nerudová, Z and Niţă, L and Polanská, M and Połtowicz-Bobak, M and Rius, D and Römer, W and Simon, U and Škrdla, P and Újvári, Gábor and Veres, D}, doi = {10.1016/j.quaint.2020.09.049}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {581-582}, unique-id = {31969601}, issn = {1040-6182}, year = {2021}, eissn = {1873-4553}, pages = {225-240}, orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Újvári, Gábor/0000-0002-2816-6155} } @article{MTMT:31637303, title = {Hunter-gatherers across the great Adriatic-Po region during the Last Glacial Maximum: Environmental and cultural dynamics}, url = {https://m2.mtmt.hu/api/publication/31637303}, author = {Peresani, M and Monegato, G and Ravazzi, C and Bertola, S and Margaritora, D and Breda, M and Fontana, A and Fontana, F and Janković, I and Karavanić, I and Komšo, D and Mozzi, P and Pini, R and Furlanetto, G and Maria De Amicis, MG and Perhoč, Z and Posth, C and Ronchi, L and Rossato, S and Vukosavljević, N and Zerboni, A}, doi = {10.1016/j.quaint.2020.10.007}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {581-582}, unique-id = {31637303}, issn = {1040-6182}, year = {2021}, eissn = {1873-4553}, pages = {128-163}, orcid-numbers = {Peresani, M/0000-0001-6562-6336; Margaritora, D/0000-0003-1436-4588; Karavanić, I/0000-0003-1452-8394; Ronchi, L/0000-0003-0245-7074; Rossato, S/0000-0002-1075-2586} } @article{MTMT:32471189, title = {New chronology and extended palaeoenvironmental data to the 1975 loess profile of Madaras brickyard, South Hungary}, url = {https://m2.mtmt.hu/api/publication/32471189}, author = {Sümegi, Pál and Gulyás, Sándor and Molnár, Dávid and Bozsó, Gábor and Fekete, István and Makó, László and Cseh, Péter and Molnár, Mihály and Sümegi, Balázs P. and Almond, Peter and Zeeden, Christian and Törőcsik, Tünde and Nett, Janina J. and Markó, András and Lehmkuhl, Frank}, doi = {10.1002/jqs.3382}, journal-iso = {J QUATERNARY SCI}, journal = {JOURNAL OF QUATERNARY SCIENCE}, volume = {36}, unique-id = {32471189}, issn = {0267-8179}, year = {2021}, eissn = {1099-1417}, pages = {1364-1381}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Gulyás, Sándor/0000-0002-3384-2381; Molnár, Dávid/0000-0001-5304-0741; Zeeden, Christian/0000-0002-8617-0443; Nett, Janina J./0000-0001-8431-0484; Markó, András/0000-0002-7556-0091} } @article{MTMT:31797540, title = {Pleistocene and holocene palaeoenvironmental reconstruction of the carpathian basin based on multiproxy analysis of cervid teeth}, url = {https://m2.mtmt.hu/api/publication/31797540}, author = {Szabó, Bence and Pazonyi, Piroska and Tóth, Emőke and Magyari, Enikő Katalin and Kiss, Gabriella Ilona and Rinyu, László and Futó, István and Virág, Attila}, doi = {10.1080/08912963.2020.1863960}, journal-iso = {HIST BIOL}, journal = {HISTORICAL BIOLOGY}, volume = {33}, unique-id = {31797540}, issn = {0891-2963}, year = {2021}, eissn = {1029-2381}, pages = {3307-3325}, orcid-numbers = {Pazonyi, Piroska/0000-0002-8256-8577; Tóth, Emőke/0000-0002-1733-7828; Magyari, Enikő Katalin/0000-0002-2844-8937; Virág, Attila/0000-0002-5530-0065} } @article{MTMT:32064831, title = {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}, url = {https://m2.mtmt.hu/api/publication/32064831}, author = {Tapody, Réka Orsolya and Sümegi, Pál and Molnár, Dávid and Karlik, Máté and Törőcsik, Tünde and Cseh, Péter and Makó, László}, doi = {10.3390/quat4020018}, journal-iso = {Quaternary}, journal = {QUATERNARY}, volume = {4}, unique-id = {32064831}, issn = {2571-550X}, year = {2021}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741} } @article{MTMT:32131406, title = {Stadial‐interstadial temperature and aridity variations in East Central Europe preceding the Last Glacial Maximum}, url = {https://m2.mtmt.hu/api/publication/32131406}, author = {Újvári, Gábor and Bernasconi, SM. and Stevens, T and Kele, Sándor and Páll-Gergely, Barna and Surányi, Gergely and Demény, Attila}, doi = {10.1029/2020PA004170}, journal-iso = {PALEOCEANOGR PALEOCL}, journal = {PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY}, volume = {36}, unique-id = {32131406}, issn = {2572-4517}, year = {2021}, eissn = {2572-4525}, orcid-numbers = {Újvári, Gábor/0000-0002-2816-6155; Bernasconi, SM./0000-0001-7672-8856; Stevens, T/0000-0002-6662-6650; Kele, Sándor/0000-0002-8607-7636; Páll-Gergely, Barna/0000-0002-6167-7221; Demény, Attila/0000-0003-0522-9018} } @mastersthesis{MTMT:32498048, title = {Diversity patterns in European vegetation: Linking community ecology and macroecology}, url = {https://m2.mtmt.hu/api/publication/32498048}, author = {Večeřa, M}, unique-id = {32498048}, year = {2021} } @article{MTMT:32076826, title = {The role of land cover in the climate of glacial Europe}, url = {https://m2.mtmt.hu/api/publication/32076826}, author = {Velasquez, P and Kaplan, JO. and Messmer, M and Ludwig, P and Raible, CC.}, doi = {10.5194/cp-17-1161-2021}, journal-iso = {CLIM PAST}, journal = {CLIMATE OF THE PAST}, volume = {17}, unique-id = {32076826}, issn = {1814-9324}, year = {2021}, eissn = {1814-9332}, pages = {1161-1180}, orcid-numbers = {Velasquez, P/0000-0002-7835-9094; Kaplan, JO./0000-0001-9919-7613; Messmer, M/0000-0001-6835-4508; Ludwig, P/0000-0003-3655-7890} } @article{MTMT:31648339, title = {The fast-acting “pulse” of Heinrich Stadial 3 in a mid-latitude boreal ecosystem}, url = {https://m2.mtmt.hu/api/publication/31648339}, author = {Badino, F and Pini, R and Bertuletti, P and Ravazzi, C and Delmonte, B and Monegato, G and Reimer, P and Vallé, F and Arrighi, S and Bortolini, E and Figus, C and Lugli, F and Maggi, V and Marciani, G and Margaritora, D and Oxilia, G and Romandini, M and Silvestrini, S and Benazzi, S}, doi = {10.1038/s41598-020-74905-0}, journal-iso = {SCI REP}, journal = {SCIENTIFIC REPORTS}, volume = {10}, unique-id = {31648339}, issn = {2045-2322}, year = {2020}, eissn = {2045-2322} } @article{MTMT:31251874, title = {The Holocene dynamics of moss communities in subalpine wetland ecosystems in the Eastern Carpathian Mountains, Central Europe}, url = {https://m2.mtmt.hu/api/publication/31251874}, author = {Gałka, Mariusz and Tantau, Ioan and Carter, Vachel A. and Feurdean, Angelica}, doi = {10.1639/0007-2745-123.1.084}, journal-iso = {BRYOLOGIST}, journal = {BRYOLOGIST}, volume = {123}, unique-id = {31251874}, issn = {0007-2745}, year = {2020}, eissn = {1938-4378}, pages = {84-97} } @article{MTMT:31434574, title = {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)}, url = {https://m2.mtmt.hu/api/publication/31434574}, author = {Haesaerts, P. and Gerasimenko, N. and Damblon, F. and Yurchenko, T. and Kulakovska, L. and Usik, V and Ridush, B.}, doi = {10.1016/j.quaint.2019.12.018}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {546}, unique-id = {31434574}, issn = {1040-6182}, abstract = {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.}, keywords = {palynology; loess stratigraphy; Doroshivtsi III site; Late pleniglacial; Gravettian chronology; Middle Dniester}, year = {2020}, eissn = {1873-4553}, pages = {196-215} } @article{MTMT:31463346, title = {Colonisation dynamic and diversity patterns of Holocene forest snail fauna across temperate Europe: The imprint of palaeoclimate changes}, url = {https://m2.mtmt.hu/api/publication/31463346}, author = {Horsak, Michal and Limondin-Lozouet, Nicole and Granai, Salome and Dabkowski, Julie and Divisek, Jan and Hajkova, Petra}, doi = {10.1016/j.quascirev.2020.106367}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {240}, unique-id = {31463346}, issn = {0277-3791}, abstract = {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.}, keywords = {stable isotopes; Diversity changes; Woodland gastropods; Colonisation pattern; Holocene development; Palaeoclimate effects; Temperate Europe}, year = {2020}, eissn = {1873-457X} } @article{MTMT:31454382, title = {Steppe flora in Serbia - distribution, ecology, centres of diversity and conservation status}, url = {https://m2.mtmt.hu/api/publication/31454382}, author = {Jakovljevic, Ksenija and Tomovic, Gordana and Djordjevic, Vladan and Niketic, Marjan and Stevanovic, Vladimir}, doi = {10.1007/s12224-019-09361-4}, journal-iso = {FOLIA GEOBOT}, journal = {FOLIA GEOBOTANICA}, volume = {55}, unique-id = {31454382}, issn = {1211-9520}, abstract = {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.}, keywords = {Biodiversity; Mapping; BALKAN PENINSULA; Richness; Phytogeography; Pontic area}, year = {2020}, eissn = {1874-9348}, pages = {1-14}, orcid-numbers = {Jakovljevic, Ksenija/0000-0002-1457-6807; Djordjevic, Vladan/0000-0002-3389-5176} } @article{MTMT:30947384, title = {pH-dependent silicon release from phytoliths of Norway spruce (Picea abies)}, url = {https://m2.mtmt.hu/api/publication/30947384}, author = {Lisztes-Szabó, Zsuzsa and Filep, Anna Fruzsina and Csík, Attila and Pető, Ákos and Kertész, Gréta Titanilla and Braun, Mihály}, doi = {10.1007/s10933-019-00103-2}, journal-iso = {J PALEOLIMNOL}, journal = {JOURNAL OF PALEOLIMNOLOGY}, volume = {63}, unique-id = {30947384}, issn = {0921-2728}, year = {2020}, eissn = {1573-0417}, pages = {65-81}, orcid-numbers = {Lisztes-Szabó, Zsuzsa/0000-0002-6322-8542; Csík, Attila/0000-0002-8173-9653} } @article{MTMT:31786740, title = {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}, url = {https://m2.mtmt.hu/api/publication/31786740}, author = {Molnár, Ábel Péter and Demeter, László}, journal-iso = {CRISICUM}, journal = {CRISICUM: A KÖRÖS - MAROS NEMZETI PARK IGAZGATÓSÁG IDŐSZAKI KIADVÁNYA}, volume = {2020}, unique-id = {31786740}, issn = {1419-2853}, year = {2020}, pages = {7-40}, orcid-numbers = {Demeter, László/0000-0003-2343-2570} } @article{MTMT:31485073, title = {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)}, url = {https://m2.mtmt.hu/api/publication/31485073}, author = {Steiner, Bigna L. and Alonso, Natalia and Grillas, Patrick and Jorda, Christophe and Piques, Gael and Tillier, Margaux and Rovira, Nuria}, doi = {10.1371/journal.pone.0234853}, journal-iso = {PLOS ONE}, journal = {PLOS ONE}, volume = {15}, unique-id = {31485073}, issn = {1932-6203}, abstract = {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).}, year = {2020}, eissn = {1932-6203} } @inbook{MTMT:31780003, title = {Prehistoric environment of the Sárköz region in the Danube Valley, Southern Hungary. case studies from infilled oxbow lakes}, url = {https://m2.mtmt.hu/api/publication/31780003}, author = {Sümegi, Pál and Náfrádi, Katalin and Törőcsik, Tünde and Jakab, Gusztáv and Bodor, Elvira and Molnár, Mihály and Pál Sümegi, Balázs and Tapody, Réka Orsolya and Knipl, István and Kustár, Rozália and Bánffy, Eszter}, booktitle = {The environmental history of the prehistoric Sárköz region in Southern Hungary}, unique-id = {31780003}, year = {2020}, pages = {83-159}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Jakab, Gusztáv/0000-0002-2569-5967; Bánffy, Eszter/0000-0001-5156-826X} } @article{MTMT:31623610, title = {Environmental Historical Analysis of the Sarmatian and Gepids Settlement of Rákóczifalva}, url = {https://m2.mtmt.hu/api/publication/31623610}, author = {Tugya, Beáta and Náfrádi, Katalin and Gulyás, Sándor and Törőcsik, Tünde and Sümegi, Balázs Pál and Pomázi, Péter and Sümegi, Pál}, doi = {10.1556/072.2020.00005}, journal-iso = {ACTA ARCHAEOL ACAD SCI HUNG}, journal = {ACTA ARCHAEOLOGICA ACADEMIAE SCIENTIARUM HUNGARICAE}, volume = {71}, unique-id = {31623610}, issn = {0001-5210}, abstract = {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.}, keywords = {POLLEN ANALYSIS; Sarmatian; geoarchaeology; archaeozoology; Bone anvil; Gepids; Late Sarmatian; Macrobotanical analysis; Rákóczifalva}, year = {2020}, eissn = {1588-2551}, pages = {101-156}, orcid-numbers = {Gulyás, Sándor/0000-0002-3384-2381; Sümegi, Pál/0000-0003-1755-4440} } @article{MTMT:30933157, title = {New radiocarbon data from the paleosols of the Nyírség blown sand area, Hungary}, url = {https://m2.mtmt.hu/api/publication/30933157}, author = {Buró, Botond and Lóki, József and Győri, Erika and Nagy, Richárd and Molnár, Mihály and Négyesi, Gábor}, doi = {10.1017/RDC.2019.137}, journal-iso = {RADIOCARBON}, journal = {RADIOCARBON}, volume = {61}, unique-id = {30933157}, issn = {0033-8222}, year = {2019}, eissn = {1945-5755}, pages = {1983-1995}, orcid-numbers = {Buró, Botond/0000-0002-2173-1537} } @article{MTMT:30542158, title = {A modern analogue of the Pleistocene steppe-tundra ecosystem in southern Siberia}, url = {https://m2.mtmt.hu/api/publication/30542158}, author = {Chytry, Milan and Horsak, Michal and Danihelka, Jiri and Ermakov, Nikolai and German, Dmitry A. and Hajek, Michal and Hajkova, Petra and Koci, Martin and Kubesova, Svatava and Lustyk, Pavel and Nekola, Jeffrey C. and Ricankova, Vera Pavelkova and Preislerova, Zdenka and Resl, Philipp and Valachovic, Milan}, doi = {10.1111/bor.12338}, journal-iso = {BOREAS}, journal = {BOREAS}, volume = {48}, unique-id = {30542158}, issn = {0300-9483}, abstract = {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.}, year = {2019}, eissn = {1502-3885}, pages = {36-56}, orcid-numbers = {Chytry, Milan/0000-0002-8122-3075} } @article{MTMT:30833952, title = {The Eurasian steppe belt: Status quo, origin and evolutionary history}, url = {https://m2.mtmt.hu/api/publication/30833952}, author = {Herbert, Hurka and Nikolai, Friesen and Karl-Georg, Bernhardt and Barbara, Neuffer and Sergej, Smirnov and Alexander, Shmakov and Frank, Blattner}, doi = {10.14258/turczaninowia.22.3.1}, journal-iso = {Turczaninowia}, journal = {Turczaninowia}, volume = {22}, unique-id = {30833952}, issn = {1560-7259}, year = {2019}, pages = {5-71} } @article{MTMT:30773293, title = {On the road: Postglacial history and recent expansion of the annual Atriplex tatarica in Europe}, url = {https://m2.mtmt.hu/api/publication/30773293}, author = {Hodková, Eva and Doudová, Jana and Douda, Jan and Krak, Karol and Mandák, Bohumil}, doi = {10.1111/jbi.13687}, journal-iso = {J BIOGEOGR}, journal = {JOURNAL OF BIOGEOGRAPHY}, volume = {46}, unique-id = {30773293}, issn = {0305-0270}, year = {2019}, eissn = {1365-2699}, pages = {2609-2621}, orcid-numbers = {Douda, Jan/0000-0002-1205-364X; Mandák, Bohumil/0000-0002-9545-7497} } @article{MTMT:30968646, title = {The dynamics of a non-forested stand in the Krusne Mts.: the effect of a short-lived medieval village on the local environment}, url = {https://m2.mtmt.hu/api/publication/30968646}, author = {Houfkova, Petra and Horak, Jan and Pokorna, Adela and Besta, Tomas and Pravcova, Ivana and Novak, Jan and Klir, Tomas}, doi = {10.1007/s00334-019-00718-5}, journal-iso = {VEG HIST ARCHAEOBOT}, journal = {VEGETATION HISTORY AND ARCHAEOBOTANY}, volume = {28}, unique-id = {30968646}, issn = {0939-6314}, abstract = {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.}, keywords = {Central Europe; Succession; Environmental reconstruction; Bioarchaeology; Deserted medieval village; Peripheral mountain area}, year = {2019}, eissn = {1617-6278}, pages = {607-621}, orcid-numbers = {Horak, Jan/0000-0001-5589-7124} } @article{MTMT:30599658, title = {Phytoliths of six woody species important in the Carpathians: characteristic phytoliths in Norway spruce needles}, url = {https://m2.mtmt.hu/api/publication/30599658}, author = {Lisztes-Szabó, Zsuzsa and Braun, Mihály and Csík, Attila and Pető, Ákos}, doi = {10.1007/s00334-019-00720-x}, journal-iso = {VEG HIST ARCHAEOBOT}, journal = {VEGETATION HISTORY AND ARCHAEOBOTANY}, volume = {28}, unique-id = {30599658}, issn = {0939-6314}, year = {2019}, eissn = {1617-6278}, pages = {649-662}, orcid-numbers = {Lisztes-Szabó, Zsuzsa/0000-0002-6322-8542; Csík, Attila/0000-0002-8173-9653} } @article{MTMT:30859762, title = {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)}, url = {https://m2.mtmt.hu/api/publication/30859762}, author = {Magyari, Enikő Katalin and Pál, Ilona and Vincze, Ildikó and Veres, D and Jakab, Gusztáv and Braun, Mihály and Szalai, Zoltán and Szabó, Zoltán and Korponai, János}, doi = {10.1016/j.quascirev.2019.105980}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {225}, unique-id = {30859762}, issn = {0277-3791}, abstract = {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.}, year = {2019}, eissn = {1873-457X}, orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Jakab, Gusztáv/0000-0002-2569-5967; Szalai, Zoltán/0000-0001-5267-411X; Korponai, János/0000-0003-0211-192X} } @article{MTMT:3361435, title = {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)}, url = {https://m2.mtmt.hu/api/publication/3361435}, author = {Sümegi, Pál and Molnár, Dávid and Gulyás, Sándor and Náfrádi, Katalin and Sümegi, B P and Törőcsik, Tünde and Persaits, G and Molnár, Mihály and Vandenberghe, J and Zhou, L}, doi = {10.1016/j.quaint.2018.03.030}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {504}, unique-id = {3361435}, issn = {1040-6182}, year = {2019}, eissn = {1873-4553}, pages = {40-55}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741; Gulyás, Sándor/0000-0002-3384-2381} } @article{MTMT:3299580, title = {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}, url = {https://m2.mtmt.hu/api/publication/3299580}, author = {Tóth, Endre György and Bede-Fazekas, Ákos and Vendramin, G G and Bagnoli, F and Höhn, Mária Margit}, doi = {10.1016/j.quaint.2017.11.024}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {504}, unique-id = {3299580}, issn = {1040-6182}, abstract = {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.}, year = {2019}, eissn = {1873-4553}, pages = {202-213}, orcid-numbers = {Bede-Fazekas, Ákos/0000-0002-2905-338X; Höhn, Mária Margit/0000-0002-8587-8271} } @article{MTMT:30741579, title = {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}, url = {https://m2.mtmt.hu/api/publication/30741579}, author = {Törőcsik, Tünde and Gulyás, Sándor and Sümegi, Pál and Sümegi, B and Molnár, Dávid and Benyó-Korcsmáros, Réka}, doi = {10.24425/sq.2019.126377}, journal-iso = {STUD QUATER}, journal = {STUDIA QUATERNARIA}, volume = {36}, unique-id = {30741579}, issn = {1641-5558}, year = {2019}, eissn = {2300-0384}, pages = {19-43}, orcid-numbers = {Gulyás, Sándor/0000-0002-3384-2381; Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741} } @article{MTMT:32662708, title = {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]}, url = {https://m2.mtmt.hu/api/publication/32662708}, author = {Tugya, Beáta and Sümegi, Pál and Náfrádi, Katalin and Törőcsik, Tünde and Sümegi, Balázs Pál and Pomázi, Péter and Gulyás, Sándor}, journal-iso = {ARCHEOMETRIAI MŰHELY}, journal = {ARCHEOMETRIAI MŰHELY}, volume = {16}, unique-id = {32662708}, issn = {1786-271X}, year = {2019}, pages = {215-244}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Gulyás, Sándor/0000-0002-3384-2381} } @article{MTMT:30798788, title = {Paleoclimate reconstruction and mire development in the Eastern Great Hungarian Plain for the last 20,000 years}, url = {https://m2.mtmt.hu/api/publication/30798788}, author = {Vincze, Ildikó and Finsinger, W and Jakab, Gusztáv and Braun, Mihály and Hubay, Katalin and Veres, D and Deli, T and Szalai, Zoltán and Szabó, Zoltán and Magyari, Enikő Katalin}, doi = {10.1016/j.revpalbo.2019.104112}, journal-iso = {REV PALAEOBOT PALYNO}, journal = {REVIEW OF PALAEOBOTANY AND PALYNOLOGY}, volume = {271}, unique-id = {30798788}, issn = {0034-6667}, year = {2019}, eissn = {1879-0615}, orcid-numbers = {Jakab, Gusztáv/0000-0002-2569-5967; Szalai, Zoltán/0000-0001-5267-411X; Magyari, Enikő Katalin/0000-0002-2844-8937} } @article{MTMT:30341722, title = {Glacial-relict symptoms in the Western Carpathian flora}, url = {https://m2.mtmt.hu/api/publication/30341722}, author = {Dite, Daniel and Hajek, Michal and Svitkova, Ivana and Kosuthova, Alica and Soltes, Rudolf and Kliment, Jan}, doi = {10.1007/s12224-018-9321-8}, journal-iso = {FOLIA GEOBOT}, journal = {FOLIA GEOBOTANICA}, volume = {53}, unique-id = {30341722}, issn = {1211-9520}, abstract = {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.}, keywords = {Central Europe; bryophytes; biogeography; Vascular plants; Habitat preferences; Glacial relict; Macroscopic terrestrial lichens}, year = {2018}, eissn = {1874-9348}, pages = {277-300} } @article{MTMT:30473686, title = {Phylogeography of the endangered saproxylic beetle Rosalia longicorn, Rosalia alpina (Coleoptera, Cerambycidae), corresponds with its main host, the European beech (Fagus sylvatica, Fagaceae)}, url = {https://m2.mtmt.hu/api/publication/30473686}, author = {Drag, Lukas and Hauck, David and Rican, Oldrich and Schmitt, Thomas and Shovkoon, Dmitri F. and Godunko, Roman J. and Curletti, Gianfranco and Cizek, Lukas}, doi = {10.1111/jbi.13429}, journal-iso = {J BIOGEOGR}, journal = {JOURNAL OF BIOGEOGRAPHY}, volume = {45}, unique-id = {30473686}, issn = {0305-0270}, abstract = {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.}, keywords = {CONSERVATION; refugium; biogeography; Insect-plant interactions; Spatial genetic structure; postglacial recolonization}, year = {2018}, eissn = {1365-2699}, pages = {2631-2644}, orcid-numbers = {Godunko, Roman J./0000-0003-2196-3327; Cizek, Lukas/0000-0002-6447-2002} } @article{MTMT:30323831, title = {Biodiversity-rich European grasslands: Ancient, forgotten ecosystems}, url = {https://m2.mtmt.hu/api/publication/30323831}, author = {Feurdean, Angelica and Ruprecht, Eszter and Molnár, Zsolt and Hutchinson, Simon M. and Hickler, Thomas}, doi = {10.1016/j.biocon.2018.09.022}, journal-iso = {BIOL CONSERV}, journal = {BIOLOGICAL CONSERVATION}, volume = {228}, unique-id = {30323831}, issn = {0006-3207}, year = {2018}, eissn = {1873-2917}, pages = {224-232} } @article{MTMT:27332356, title = {Effect of sample size and resolution on palaeomalacological interpretation: a case study from Holocene calcareous-fen deposits}, url = {https://m2.mtmt.hu/api/publication/27332356}, author = {Frodlova, Jitka and Hajkova, Petra and Horsak, Michal}, doi = {10.1002/jqs.2999}, journal-iso = {J QUATERNARY SCI}, journal = {JOURNAL OF QUATERNARY SCIENCE}, volume = {33}, unique-id = {27332356}, issn = {0267-8179}, year = {2018}, eissn = {1099-1417}, pages = {68-78} } @article{MTMT:27587274, title = {Forest snail diversity and its environmental predictors along a sharp climatic gradient in southern Siberia}, url = {https://m2.mtmt.hu/api/publication/27587274}, author = {Horsak, Michal and Jurickova, Lucie and Horsakova, Veronika and Pokorna, Adela and Pokorny, Petr and Sizling, Arnost L and Chytry, Milan}, doi = {10.1016/j.actao.2018.02.009}, journal-iso = {ACTA OECOL}, journal = {ACTA OECOLOGICA: INTERNATIONAL JOURNAL OF ECOLOGY}, volume = {88}, unique-id = {27587274}, issn = {1146-609X}, year = {2018}, eissn = {1873-6238}, pages = {1-8}, orcid-numbers = {Chytry, Milan/0000-0002-8122-3075} } @article{MTMT:27340969, title = {History and environment shape species pools and community diversity in European beech forests}, url = {https://m2.mtmt.hu/api/publication/27340969}, author = {Jimenez-Alfaro, Borja and Girardello, Marco and Chytry, Milan and Svenning, Jens-Christian and Willner, Wolfgang and Gegout, Jean-Claude and Agrillo, Emiliano and Antonio, Campos Juan and Jandt, Ute and Kacki, Zygmunt and Silc, Urban and Slezak, Michal and Tichy, Lubomir and Tsiripidis, Ioannis and Turtureanu, Pavel Dan and Ujhazyova, Mariana and Wohlgemuth, Thomas}, doi = {10.1038/s41559-017-0462-6}, journal-iso = {NAT ECOL EVOL}, journal = {NATURE ECOLOGY & EVOLUTION}, volume = {2}, unique-id = {27340969}, issn = {2397-334X}, year = {2018}, eissn = {2397-334X}, pages = {483-490}, orcid-numbers = {Jimenez-Alfaro, Borja/0000-0001-6601-9597} } @article{MTMT:27332353, title = {A multi-proxy view of exceptionally early postglacial development of riparian woodlands with Ulmus in the Dniester River valley, updates western Ukraine}, url = {https://m2.mtmt.hu/api/publication/27332353}, author = {Kolaczek, Piotr and Galka, Mariusz and Apolinarska, Karina and Plociennik, Mateusz and Gasiorowski, Michal and Brooks, Stephen J and Hutchinson, Simon M and Karpinska-Kolaczek, Monika}, doi = {10.1016/j.revpalbo.2017.12.001}, journal-iso = {REV PALAEOBOT PALYNO}, journal = {REVIEW OF PALAEOBOTANY AND PALYNOLOGY}, volume = {250}, unique-id = {27332353}, issn = {0034-6667}, year = {2018}, eissn = {1879-0615}, pages = {27-43} } @article{MTMT:27332354, title = {Environmental correlates of the Late Quaternary regional extinctions of large and small Palaearctic mammals}, url = {https://m2.mtmt.hu/api/publication/27332354}, author = {Ricankova, Vera Pavelkova and Horsak, Michal and Hais, Martin and Robovsky, Jan and Chytry, Milan}, doi = {10.1111/ecog.02851}, journal-iso = {ECOGRAPHY}, journal = {ECOGRAPHY}, volume = {41}, unique-id = {27332354}, issn = {0906-7590}, year = {2018}, eissn = {1600-0587}, pages = {516-527} } @inbook{MTMT:3411767, title = {Az ócsai Selyem-rét környezettörténete a jégkor végétől [Environmental history from the terminal phase of the ice age on the Selyemrét area at Ócsa]}, url = {https://m2.mtmt.hu/api/publication/3411767}, author = {Törőcsik, Tünde and Sümegi, Balázs Pál and Sümegi, Pál}, booktitle = {Természetvédelem és kutatás a Turjánvidék északi részén}, unique-id = {3411767}, year = {2018}, pages = {81-118}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440} } @article{MTMT:26929802, title = {Refugial ecosystems in central Asia as indicators of biodiversity change during the Pleistocene-Holocene transition}, url = {https://m2.mtmt.hu/api/publication/26929802}, author = {Chytry, Milan and Horsak, Michal and Syrovatka, Vit and Danihelka, Jiri and Ermakov, Nikolai and German, Dmitry A and Hajek, Michal and Hajek, Ondrej and Hajkova, Petra and Horsakova, Veronika and Koci, Martin and Kubegova, Svatava and Lustyk, Pavel and Nekola, Jeffrey C and Preislerova, Zdenka and Resl, Philipp and Valachovic, Milan}, doi = {10.1016/j.ecolind.2016.12.033}, journal-iso = {ECOL INDIC}, journal = {ECOLOGICAL INDICATORS}, volume = {77}, unique-id = {26929802}, issn = {1470-160X}, year = {2017}, eissn = {1872-7034}, pages = {357-367}, orcid-numbers = {Chytry, Milan/0000-0002-8122-3075} } @{MTMT:26500362, title = {The Evolution of Vegetation from the last Glacial Maximum until the Present}, url = {https://m2.mtmt.hu/api/publication/26500362}, author = {Feurdean, A and Tantau, I}, booktitle = {Landform Dynamics and Evolution in Romania}, doi = {10.1007/978-3-319-32589-7_4}, publisher = {Springer Netherlands}, unique-id = {26500362}, year = {2017}, pages = {67-83} } @article{MTMT:3217479, title = {Palaeohydrological changes during the mid and late Holocene in the Carpathian area, central-eastern Europe}, url = {https://m2.mtmt.hu/api/publication/3217479}, author = {Haliuc, A and Veres, D and Brauer, A and Hubay, Katalin and Hutchinson, S and Begy, R and Braun, Mihály}, doi = {10.1016/j.gloplacha.2017.02.010}, journal-iso = {GLOBAL PLANET CHANGE}, journal = {GLOBAL AND PLANETARY CHANGE}, volume = {152}, unique-id = {3217479}, issn = {0921-8181}, year = {2017}, eissn = {1872-6364}, pages = {99-114} } @article{MTMT:26576765, title = {Palaeodistribution modelling of European vegetation types at the Last Glacial Maximum using modern analogues from Siberia: Prospects and limitations}, url = {https://m2.mtmt.hu/api/publication/26576765}, author = {Janska, Veronika and Jimenez-Alfaro, Borja and Chytry, Milan and Divisek, Jan and Anenkhonov, Oleg and Korolyuk, Andrey and Lashchinskyi, Nikolai and Culek, Martin}, doi = {10.1016/j.quascirev.2017.01.011}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {159}, unique-id = {26576765}, issn = {0277-3791}, year = {2017}, eissn = {1873-457X}, pages = {103-115} } @article{MTMT:26929800, title = {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}, url = {https://m2.mtmt.hu/api/publication/26929800}, author = {Kolaczek, Piotr and Margielewski, Modzimierz and Galka, Mariusz and Apolinarska, Karina and Plociennik, Mateusz and Gasiorowski, Michal and Buczek, Krzysztof and Karpinska-Kolaczek, Monika}, doi = {10.1016/j.revpalbo.2017.05.002}, journal-iso = {REV PALAEOBOT PALYNO}, journal = {REVIEW OF PALAEOBOTANY AND PALYNOLOGY}, volume = {244}, unique-id = {26929800}, issn = {0034-6667}, year = {2017}, eissn = {1879-0615}, pages = {113-127} } @article{MTMT:26762177, title = {Hydrologic refugia, plants, and climate change}, url = {https://m2.mtmt.hu/api/publication/26762177}, author = {McLaughlin, B.C. and Ackerly, D.D. and Klos, P.Z. and Natali, J. and Dawson, T.E. and Thompson, S.E.}, doi = {10.1111/gcb.13629}, journal-iso = {GLOBAL CHANGE BIOL}, journal = {GLOBAL CHANGE BIOLOGY}, volume = {23}, unique-id = {26762177}, issn = {1354-1013}, abstract = {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.}, keywords = {ECOLOGY; climate change; CONSERVATION; GROUNDWATER; WATER-UPTAKE; Biodiversity conservation; fog; NATIONAL-PARK; RANGE SHIFTS; microrefugia; hydrologic niche; hydrologic refugia; BIOLOGICAL SOIL CRUSTS; CALIFORNIA REDWOOD FOREST; SEMPERVIRENS D. DON; HYDRAULIC LIFT; GROUNDWATER USE; CLOUD FOREST}, year = {2017}, eissn = {1365-2486}, pages = {2941-2961} } @{MTMT:26099775, title = {Lakes, Lacustrine Sediments, and Palaeoenvironmental Reconstructions}, url = {https://m2.mtmt.hu/api/publication/26099775}, author = {Mîndrescu, M and Florescu, G and Grădinaru, I and Haliuc, A}, booktitle = {Landform Dynamics and Evolution in Romania}, doi = {10.1007/978-3-319-32589-7_30}, publisher = {Springer Netherlands}, unique-id = {26099775}, year = {2017}, pages = {699-734} } @article{MTMT:26933773, title = {Extrazonal steppes and other temperate grasslands of northern Siberia-Phytosociological classification and ecological characterization}, url = {https://m2.mtmt.hu/api/publication/26933773}, author = {Reinecke, Jennifer and Troeva, Elena and Wesche, Karsten}, doi = {10.1127/phyto/2017/0175}, journal-iso = {PHYTOCOENOLOGIA}, journal = {PHYTOCOENOLOGIA}, volume = {47}, unique-id = {26933773}, issn = {0340-269X}, year = {2017}, eissn = {2363-7153}, pages = {167-196} } @article{MTMT:3212261, title = {Evolutionary history and phylogeography of Scots pine (Pinus sylvestris L.) in Europe based on molecular markers}, url = {https://m2.mtmt.hu/api/publication/3212261}, author = {Tóth, Endre György and Köbölkuti, Zoltán Attila and Pedryc, A. and Höhn, Mária Margit}, doi = {10.1007/s11676-017-0393-8}, journal-iso = {J FOREST RES-JPN}, journal = {JOURNAL OF FOREST RESEARCH}, volume = {28}, unique-id = {3212261}, issn = {1341-6979}, abstract = {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.}, keywords = {QUATERNARY HISTORY; Phylogeography; Pinus Sylvestris; Refugia; molecular genetic markers}, year = {2017}, eissn = {1610-7403}, pages = {637-651}, orcid-numbers = {Höhn, Mária Margit/0000-0002-8587-8271} } @article{MTMT:3212241, title = {High genetic diversity and distinct origin of recently fragmented Scots pine (Pinus sylvestris L.) populations along the Carpathians and the Pannonian Basin}, url = {https://m2.mtmt.hu/api/publication/3212241}, author = {Tóth, Endre György and Vendramin, G G and Bagnoli, F and Cseke, Klára and Höhn, Mária Margit}, doi = {10.1007/s11295-017-1137-9}, journal-iso = {TREE GENET GENOMES}, journal = {TREE GENETICS & GENOMES}, volume = {13}, unique-id = {3212241}, issn = {1614-2942}, abstract = {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.}, keywords = {MICROSATELLITES; carpathians; GLACIAL REFUGIA; Phylogeography; Pinus Sylvestris}, year = {2017}, eissn = {1614-2950}, orcid-numbers = {Höhn, Mária Margit/0000-0002-8587-8271} } @article{MTMT:26576764, title = {Larix during the Mid-Pleniglacial (Greenland Interstadial 8) on Kotelny Island, northern Siberia}, url = {https://m2.mtmt.hu/api/publication/26576764}, author = {Van, Geel Bas and Protopopov, Albert and Protopopova, Victoria and Pavlov, Innokenti and Van, Der Plicht Johannes and Van, Reenen Guido B A}, doi = {10.1111/bor.12216}, journal-iso = {BOREAS}, journal = {BOREAS}, volume = {46}, unique-id = {26576764}, issn = {0300-9483}, year = {2017}, eissn = {1502-3885}, pages = {338-345} } @article{MTMT:27496819, title = {Present genetic structure is congruent with the common origin of distant Scots pine populations in its Romanian distribution}, url = {https://m2.mtmt.hu/api/publication/27496819}, author = {Bernhardsson, C and Floran, V and Ganea, S L and Garcia-Gil, M R}, doi = {10.1016/j.foreco.2015.10.047}, journal-iso = {FOREST ECOL MANAG}, journal = {FOREST ECOLOGY AND MANAGEMENT}, volume = {361}, unique-id = {27496819}, issn = {0378-1127}, abstract = {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.}, keywords = {Genetic Diversity; Hungary; Romania; Pinus Sylvestris; Spatial genetic structure; Nad1/nad7 mitotype; Chloroplast SSR; Nuclear SSR}, year = {2016}, eissn = {1872-7042}, pages = {131-143} } @article{MTMT:27120550, title = {A second horizon scan of biogeography: Golden ages, Midas touches, and the Red Queen}, url = {https://m2.mtmt.hu/api/publication/27120550}, author = {Dawson, MN and Axmacher, JC and Beierkuhnlein, C and Blois, J and Bradley, BA and Cord, AF and Dengler, J and He, KS and Heaney, LR and Jansson, R and Mahecha, MD and Myers, C and Nogués-Bravo, D and Papadopoulou, A and Reu, B and Rodríguez-Sánchez, F and Steinbauer, MJ and Stigall, A and Tuanmu, M-N and Gavin, DG}, doi = {10.21425/F58429770}, journal-iso = {FRONT BIOGEOGRAPHY}, journal = {FRONTIERS OF BIOGEOGRAPHY}, volume = {8}, unique-id = {27120550}, issn = {1948-6596}, year = {2016} } @article{MTMT:27120975, title = {Footprints of the Last Glacial: Past competition may have shaped strongly disjunct distribution ranges in Artemisia rupestris and A. laciniata}, url = {https://m2.mtmt.hu/api/publication/27120975}, author = {Hochheimer, J and Hoffmann, MH}, doi = {10.1016/j.flora.2016.08.004}, journal-iso = {FLORA}, journal = {FLORA}, volume = {224}, unique-id = {27120975}, issn = {0367-2530}, year = {2016}, eissn = {1618-0585}, pages = {203-210} } @article{MTMT:3024279, title = {Phylogeographic patterns of steppe species in Eastern Central Europe: a review and the implications for conservation}, url = {https://m2.mtmt.hu/api/publication/3024279}, author = {Kajtoch, Łukasz and Elżbieta, Cieślak and Varga, Zoltán Sándor and Wojciech, Paul and Miłosz A, Mazur and Sramkó, Gábor and Daniel, Kubisz}, doi = {10.1007/s10531-016-1065-2}, journal-iso = {BIODIVERS CONSERV}, journal = {BIODIVERSITY AND CONSERVATION}, volume = {25}, unique-id = {3024279}, issn = {0960-3115}, year = {2016}, eissn = {1572-9710}, pages = {2309-2339}, orcid-numbers = {Sramkó, Gábor/0000-0001-8588-6362} } @article{MTMT:26242202, title = {Biogeography of the Carpathians: evolutionary and spatial facets of biodiversity}, url = {https://m2.mtmt.hu/api/publication/26242202}, author = {Mraz, Patrik and Ronikier, Michal}, doi = {10.1111/bij.12918}, journal-iso = {BIOL J LINN SOC}, journal = {BIOLOGICAL JOURNAL OF THE LINNEAN SOCIETY}, volume = {119}, unique-id = {26242202}, issn = {0024-4066}, abstract = {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.}, keywords = {Europe; SPECIATION; polyploidy; Biodiversity; Species richness; Phylogeography; biogeography; Distribution patterns; Endemism; Cryptic diversity; cytogeography; mountainous areas}, year = {2016}, eissn = {1095-8312}, pages = {528-559} } @article{MTMT:26204591, title = {New information augmenting the picture of local environment at the LGM/LGT in the context of the Middle Danube region}, url = {https://m2.mtmt.hu/api/publication/26204591}, author = {Nerudova, Z and Dolakova, N and Novak, J}, doi = {10.1177/0959683616640051}, journal-iso = {HOLOCENE}, journal = {HOLOCENE}, volume = {26}, unique-id = {26204591}, issn = {0959-6836}, year = {2016}, eissn = {1477-0911}, pages = {1345-1354} } @article{MTMT:26207192, title = {Reflections on Gravettian firewood procurement near the Pavlov Hills, Czech Republic}, url = {https://m2.mtmt.hu/api/publication/26207192}, author = {Pryor, A J E and Pullen, A and Beresford-Jones, D G and Svoboda, J A and Gamble, C S}, doi = {10.1016/j.jaa.2016.05.003}, journal-iso = {J ANTHROPOL ARCHAEOL}, journal = {JOURNAL OF ANTHROPOLOGICAL ARCHAEOLOGY}, volume = {43}, unique-id = {26207192}, issn = {0278-4165}, year = {2016}, eissn = {1090-2686}, pages = {1-12} } @article{MTMT:26033190, title = {Mohelno - A terminal Last Glacial Maximum industry with microlithic tools made on carenoidal blanks}, url = {https://m2.mtmt.hu/api/publication/26033190}, author = {Skrdla, Petr and Nejman, Ladislav and Bartik, Jaroslav and Rychtarikova, Tereza and Nikolajev, Pavel and Eigner, Jan and Fisakova, Miriam Nyvltova and Novak, Jan and Polanska, Michaela}, doi = {10.1016/j.quaint.2015.05.055}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {406}, unique-id = {26033190}, issn = {1040-6182}, year = {2016}, eissn = {1873-4553}, pages = {184-194} } @article{MTMT:3011427, title = {The physics of wind-blown loess: Implications for grain size proxy interpretations in Quaternary paleoclimate studies}, url = {https://m2.mtmt.hu/api/publication/3011427}, author = {Újvári, Gábor and Kok, J F and Varga, György and Kovács, János}, doi = {10.1016/j.earscirev.2016.01.006}, journal-iso = {EARTH-SCI REV}, journal = {EARTH-SCIENCE REVIEWS}, volume = {154}, unique-id = {3011427}, issn = {0012-8252}, abstract = {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.}, keywords = {Quaternary; Quartz; wind; loess; Grain size proxy; Aeolian dynamics}, year = {2016}, eissn = {1872-6828}, pages = {247-278}, orcid-numbers = {Újvári, Gábor/0000-0002-2816-6155; Varga, György/0000-0003-4784-6372; Kovács, János/0000-0001-7742-5515} } @article{MTMT:2970162, title = {Origin of the forest steppe and exceptional grassland diversity in Transylvania (central-eastern Europe)}, url = {https://m2.mtmt.hu/api/publication/2970162}, author = {Feurdean, A and Marinova, E and Nielsen, AB and Liakka, J and Veres, D and Hutchinson, SM and Braun, Mihály and Timar-Gabor, A and Astalos, C and Mosburgger, V and Hickler, T}, doi = {10.1111/jbi.12468}, journal-iso = {J BIOGEOGR}, journal = {JOURNAL OF BIOGEOGRAPHY}, volume = {42}, unique-id = {2970162}, issn = {0305-0270}, year = {2015}, eissn = {1365-2699}, pages = {951-963} } @article{MTMT:25326642, title = {Modelling the Last Glacial Maximum environments for a refugium of Pleistocene biota in the Russian Altai Mountains, Siberia}, url = {https://m2.mtmt.hu/api/publication/25326642}, author = {Hais, Martin and Komprdova, Klara and Ermakov, Nikolai and Chytry, Milan}, doi = {10.1016/j.palaeo.2015.07.037}, journal-iso = {PALAEOGEOGR PALAEOCL}, journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY}, volume = {438}, unique-id = {25326642}, issn = {0031-0182}, year = {2015}, eissn = {1872-616X}, pages = {135-145} } @article{MTMT:25326643, title = {European glacial relict snails and plants: environmental context of their modern refugial occurrence in southern Siberia}, url = {https://m2.mtmt.hu/api/publication/25326643}, author = {Horsak, Michal and Chytry, Milan and Hajkova, Petra and Hajek, Michal and Danihelka, Jiri and Horsakova, Veronika and Ermakov, Nikolai and German, Dmitry A and Koci, Martin and Lustyk, Pavel and Nekola, Jeffrey C and Preislerova, Zdenka and Valachovic, Milan}, doi = {10.1111/bor.12133}, journal-iso = {BOREAS}, journal = {BOREAS}, volume = {44}, unique-id = {25326643}, issn = {0300-9483}, year = {2015}, eissn = {1502-3885}, pages = {638-657} } @article{MTMT:24428501, title = {Succession of arboreal taxa during the Late Glacial in south-eastern Poland: Climatic implications}, url = {https://m2.mtmt.hu/api/publication/24428501}, author = {Kołaczek, P and Gałka, M and Karpińska-Kołaczek, M}, doi = {10.1016/j.palaeo.2015.01.007}, journal-iso = {PALAEOGEOGR PALAEOCL}, journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY}, volume = {421}, unique-id = {24428501}, issn = {0031-0182}, year = {2015}, eissn = {1872-616X}, pages = {1-14} } @article{MTMT:25145421, title = {The loess-palaeosol sequence in the upper palaeolithic site at Kraków spadzista: A palaeoenvironmental approach}, url = {https://m2.mtmt.hu/api/publication/25145421}, author = {Łanczont, M and Madeyska, T and Mroczek, P and Komar, M and Łacka, B and Bogucki, A and Sobczyk, K and Wilczyński, J}, doi = {10.1016/j.quaint.2014.11.033}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {365}, unique-id = {25145421}, issn = {1040-6182}, year = {2015}, eissn = {1873-4553}, pages = {98-113} } @article{MTMT:32266984, title = {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?]}, url = {https://m2.mtmt.hu/api/publication/32266984}, author = {Mitka, Józef and Wróblewska, Ada and Bąba, Wojciech and Watrak, Grzegorz and Wątroba, Marta and Boroń, Piotr}, journal-iso = {Roczniki Bieszczadzkie}, journal = {Roczniki Bieszczadzkie}, volume = {23}, unique-id = {32266984}, issn = {1233-1910}, year = {2015}, pages = {54} } @article{MTMT:27496786, title = {Sedimentary evolution and persistence of open forests between the south-eastern Alpine fringe and the Northern Dinarides during the Last Glacial Maximum}, url = {https://m2.mtmt.hu/api/publication/27496786}, author = {Monegato, G and Ravazzi, C and Culiberg, M and Pini, R and Bavec, M and Calderoni, G and Jez, J and Perego, R}, doi = {10.1016/j.palaeo.2015.06.025}, journal-iso = {PALAEOGEOGR PALAEOCL}, journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY}, volume = {436}, unique-id = {27496786}, issn = {0031-0182}, year = {2015}, eissn = {1872-616X}, pages = {23-40} } @article{MTMT:25644183, title = {Mid-Holocene bottleneck for central European dry grasslands: Did steppe survive the forest optimum in northern Bohemia, Czech Republic?}, url = {https://m2.mtmt.hu/api/publication/25644183}, author = {Pokorny, Petr and Chytry, Milan and Jurickova, Lucie and Sadlo, Jiri and Novak, Jan and Lozek, Vojen}, doi = {10.1177/0959683614566218}, journal-iso = {HOLOCENE}, journal = {HOLOCENE}, volume = {25}, unique-id = {25644183}, issn = {0959-6836}, year = {2015}, eissn = {1477-0911}, pages = {716-726}, orcid-numbers = {Chytry, Milan/0000-0002-8122-3075} } @article{MTMT:2706681, title = {Climate variability and associated vegetation response throughout Central and Eastern Europe (CEE) between 60 and 8 ka}, url = {https://m2.mtmt.hu/api/publication/2706681}, author = {Feurdean, A and Perşoiu, A and Tanţău, I and Stevens, T and Magyari, Enikő Katalin and Onac, BP and Marković, S and Andrič, M and Connor, S and Fărcaş, S and Gałka, M and Gaudenyi, Tivadar and Hoek, W and Kolaczek, P and Kuneš, P and Lamentowicz, M and Marinova, E and Michczyńska, DJ and Perşoiu, I and Płóciennik, M and Słowiński, M and Stancikaite, M and Sümegi, Pál and Svensson, A and Tămaş, T and Timar, A and Tonkov, S and Tóth, Mónika and Veski, S and Willis, KJ and Zernitskaya, V}, doi = {10.1016/j.quascirev.2014.06.003}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {106}, unique-id = {2706681}, issn = {0277-3791}, abstract = {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.}, keywords = {climate; POLLEN; Holocene; vegetation response; LATITUDINAL GRADIENTS; Glacial; INTIMATE; Terrestrial records}, year = {2014}, eissn = {1873-457X}, pages = {206-224}, orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Sümegi, Pál/0000-0003-1755-4440} } @article{MTMT:2743488, title = {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}, url = {https://m2.mtmt.hu/api/publication/2743488}, author = {Magyari, Enikő Katalin and Veres, D and Wennrich, V and Wagner, B and Braun, Mihály and Jakab, Gusztáv and Karátson, Dávid and Pál, Z and Ferenczy, Gy and St-Onge, G and Rethemeyer, J and Francois, J-P and von Reumont, F and Schäbitz, F}, doi = {10.1016/j.quascirev.2014.09.015}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {106}, unique-id = {2743488}, issn = {0277-3791}, year = {2014}, eissn = {1873-457X}, pages = {278-298}, orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Jakab, Gusztáv/0000-0002-2569-5967; Karátson, Dávid/0000-0003-0386-1239} }