TY - JOUR AU - Gulyás, Sándor AU - Sümegi, Pál TI - Late Pleistocene to Holocene Palaeohydrological History of the Thermal-Spring-Fed Lake Pețea (NW Romania) Revealed by Radiocarbon Dating and Complex Sedimentological Investigations JF - QUATERNARY J2 - Quaternary VL - 6 PY - 2023 IS - 2 PG - 20 SN - 2571-550X DO - 10.3390/quat6020037 UR - https://m2.mtmt.hu/api/publication/34019976 ID - 34019976 N1 - Export Date: 4 September 2023 Correspondence Address: Gulyás, S.; Department of Geology and Paleontology, Hungary; email: gulyas.sandor@geo.u-szeged.hu AB - Understanding sedimentation processes in response to past hydrogeological and climatic changes and capturing millennial-scale variations is a key focus of lacustrine paleoenvironmental research. This study presents the first high-resolution chronology and sedimentary data for the small thermal-spring-fed Lake Pețea, NW Romania, and unravels the evolutionary history of the lake harboring a unique endemic fauna. Its small size and single source of water make it particularly sensitive to hydrological changes. In the recent past, over-exploitation of the thermal water has led to the complete drying up of the lake and the extinction of its fauna. Nevertheless, past spatio-temporal variation of environmental factors, in particular the fluctuation of lake levels and water temperature, must have had a significant impact on the survival and evolution of the endemic mollusk fauna. This fact makes this study particularly important. Based on our results, a three-stage sedimentary evolution occurred, mainly controlled by major climate-driven hydrological changes also seen in regional records, i.e., 17.5–14.5 ka shallow eutrophic lake, 14.5–5.5 ka oligotrophic carbonate-rich lake, and 5.5–0.5 ka shallow eutrophic lake. A major lowstand at 11.7–10.2 ka due to drier climate was followed by progressively rising water levels up to 5 ka followed by a drop. The main control on lake level fluctuations and sedimentary phases was the varying input of thermal water due to recurring increased/decreased recharge of the underground shallow karst water system. The driving factor of thermal water discharge was different during the Late Glacial than the Holocene. It was the warming of the climate at 14.5 ka cal BP and melting of regional ice sheets in addition to increased precipitation that created an oligotrophic lake by recharging the underground thermal water system. Conversely, during the Holocene, increasing/decreasing moisture availability driven by major climate forcings was in control of thermal water recharge, erosion, and fluctuating lake levels. LA - English DB - MTMT ER - TY - JOUR AU - Radaković, MG. AU - Oches, EA. AU - Hughes, PD. AU - Marković, RS. AU - Hao, Q AU - Perić, ZM. AU - Gavrilović, B AU - Ludwig, P AU - Lukić, T AU - Gavrilov, MB. AU - Marković, SB. TI - Reconstructed Malacothermometer July Paleotemperatures from the Last Nine Glacials over the South-Eastern Carpathian Basin (Serbia) JF - ATMOSPHERE J2 - ATMOSPHERE-BASEL VL - 14 PY - 2023 IS - 5 SN - 2073-4433 DO - 10.3390/atmos14050791 UR - https://m2.mtmt.hu/api/publication/33784551 ID - 33784551 N1 - ISSN:2073-4433 AB - In this study, the compiled malacological record of the two most important loess–palaeosol sequences (LPS) in Serbia was used to reconstruct the Malacothermometer July Paleotemperature (MTJP) of the last nine glacials. The sieved loess samples yielded shells of 11 terrestrial gastropod species that were used to estimate the MTJP. Veliki Surduk (covering the last three glacial cycles) and Stari Slankamen (covering the last fourth to ninth glacial cycle) LPSs previously lacked the malacological investigations. After the sieving, a total of 66,871 shells were found, from which 48,459 shells were used for the estimation of the MTJP. Through the studied period, the reconstructed MTJP was ranging from 14.4 °C to 21.5 °C. The lowest temperature was recorded during the formation of the loess unit L5, equivalent to the Marine Isotope Stage (MIS) 12. The second-coldest summers were occurring during the MIS 16 glacial. Although the warmest glacial was L8 (MIS 20) according to MTJP, these July temperatures might be overestimated due to only two samples from the poorly preserved L8 unit. The malacological material derived from the loess units at Veliki Surduk and Stari Slankamen LPSs showed great potential for July temperature reconstruction, as the comparison with other regional records showed similar climate changes. Further work is necessary to validate the age scale of the oldest samples, and a higher resolution sampling could lead to more detailed July temperature fluctuations, as was shown for the youngest glacial in this study. Likewise, estimating the July temperature using different proxies (e.g., pollen) from the same LPSs could be used to confirm the observed climate trends. LA - English DB - MTMT ER - TY - JOUR AU - Cseh, Péter AU - Molnár, Dávid AU - Makó, László AU - Sümegi, Pál TI - Geoarchaeological Analyses of a Late-Copper-Age Kurgan on the Great Hungarian Plain JF - QUATERNARY J2 - Quaternary VL - 5 PY - 2022 IS - 2 SN - 2571-550X DO - 10.3390/quat5020020 UR - https://m2.mtmt.hu/api/publication/32776652 ID - 32776652 N1 - Department of Geology and Paleontology, University of Szeged, Szeged, H-6722, Hungary Long Environmental Changes Research Team, Interdisciplinary Excellence Centre, Institute of Geography and Earth Sciences, University of Szeged, Szeged, H-6722, Hungary Export Date: 23 May 2022 Correspondence Address: Cseh, P.; Department of Geology and Paleontology, Hungary; email: cspeter@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - Gulyás, Sándor AU - Torma, Andrea AU - Pap, Norbert AU - Fodor, Pál AU - Kitanics, Máté AU - Gyenizse, Péter AU - Molnár, Mihály AU - Sümegi, Pál TI - Tackling erosion-accumulation events in a moat sequence from a unique Ottoman memorial place (Szigetvár, SW Hungary) using 14C and geoarcheological data JF - ARCHAEOLOGICAL AND ANTHROPOLOGICAL SCIENCES J2 - ARCHAEO ANTHROP SCI VL - 14 PY - 2022 IS - 1 PG - 12 SN - 1866-9557 DO - 10.1007/s12520-021-01479-x UR - https://m2.mtmt.hu/api/publication/32596336 ID - 32596336 N1 - Department of Geology and Paleontology, University of Szeged, 2-6 Egyetem u, Szeged, H-6722, Hungary Szentágothai János Research Center, University of Pécs, Historical and Political Geography Research Centre H-7624, 20 Ifjúság útja, Pécs, Hungary Eötvös Lorand Research Network, Research Centre for the Humanities, 4 Tóth Kálmán Utca, Budapest, H-1097, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Eötvös Lóránd Research Network, Bem square 18/c, Debrecen, 4026, Hungary Export Date: 23 May 2022 Correspondence Address: Gulyás, S.; Department of Geology and Paleontology, 2-6 Egyetem u, Hungary; email: gulyas.sandor@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Molnár, Dávid AU - Gulyás, Sándor AU - Stevens, T AU - Makó, László AU - Cseh, P AU - Molnár, Mihály AU - Fitzsimmons, K AU - Nett, JJ. AU - Hlavatskyi, D AU - Lehmkuhl, F TI - Comparison of High-Resolution 14C and Luminescence-Based Chronologies of the MIS 2 Madaras Loess/Paleosol Sequence, Hungary: Implications for Chronological Studies JF - QUATERNARY J2 - Quaternary VL - 5 PY - 2022 IS - 4 SN - 2571-550X DO - 10.3390/quat5040047 UR - https://m2.mtmt.hu/api/publication/33240955 ID - 33240955 N1 - Department of Geology and Paleontology, University of Szeged, Szeged, H-6722, Hungary Interdisciplinary Excellence Centre, Institute of Geography and Earth Sciences, Long Environmental Changes Research Team, University of Szeged, Szeged, H-6722, Hungary Department of Earth Sciences, University of Uppsala, Uppsala, 75236, Sweden Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Eötvös Lóránd Research Network, Bem square 18/c, Debrecen, H-4026, Hungary Department of Geosciences, University of Tübingen, Tübingen, 72076, Germany Physical Geography and Geoecology, Department of Geography, RWTH Aachen University, Aachen, 52062, Germany Institute of Geophysics, National Academy of Sciences of Ukraine, Kyiv, 01030, Ukraine Export Date: 4 January 2023 Correspondence Address: Sümegi, P.; Department of Geology and Paleontology, Hungary; email: sumegi@geo.u-szeged.hu AB - Numerous loess/paleosol sequences (LPS) in the Carpathian Basin span the period of Marine Isotope Stage (MIS) 2 and the last glacial maximum (LGM). Nevertheless, only two known records—Madaras and Dunaszekcső—preserve highly resolved records with absolute chronologies with minimal uncertainties, which enable the meaningful assessment of feedbacks and short-term climatic fluctuations over this period. The Madaras profile is located at the northern margin fringe of the Bácska loess plateau; Dunaszekcső, located on the Danube to its west, yields a chronology built on over 100 14C dates yet spans only part of MIS 2, missing half of the LGM including its peak. Here, we add to the previously published 14C chronology for Madaras (15 dates) with an additional 17 14C and luminescence ages. Resulting age models built solely on quartz OSL and feldspar pIRIRSL data underestimate the 14C based chronology, which is likely based on inaccuracies related to luminescence signal behavior; we observe age underestimations associated with unusual quartz behavior and significant signal loss, a phenomenon also observed in Serbian and Romanian loess, which may relate to non-sensitized grains from proximal sources. Our new chronology provides higher resolution than hitherto possible, yielding consistent 2 sigma uncertainties of ~150–200 years throughout the entire sequence. Our study indicates that the addition of further dates may not increase the chronological precision significantly. Additionally, the new age model is suitable for tackling centennial-scale changes. The mean sedimentation rate based on our new age-depth model (10.78 ± 2.34 years/cm) is the highest yet recorded in the Carpathian Basin for MIS 2. The resolution of our age model is higher than that for the Greenland NGRIP ice core record. The referred horizons in our profile are all characterized by a drop in accumulation and a higher sand input, the latter most likely deriving from nearby re-exposed sand dunes. LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Molnár, Dávid AU - Náfrádi, Katalin AU - Makó, László AU - Cseh, Péter AU - Törőcsik, Tünde AU - Molnár, Mihály AU - Zhou, Liping TI - Vegetation and land snail-based reconstruction of the palaeocological changes in the forest steppe eco-region of the Carpathian Basin during last glacial warming JF - GLOBAL ECOLOGY AND CONSERVATION J2 - GLOB ECOL CONSERV VL - 33 PY - 2022 PG - 28 SN - 2351-9894 DO - 10.1016/j.gecco.2021.e01976 UR - https://m2.mtmt.hu/api/publication/32544836 ID - 32544836 N1 - Funding Agency and Grant Number: Hungarian Government, Ministry of Human Capacities [20391-3/2018/FEKUSTRAT]; European Regional Development Fund [GINOP-2.3.2-15-2016-00009 'ICER']; University of Szeged Open Access Fund [5386]; Hungarian National Excellence Programme grant [NTP-NFTOd-19-B-0158] Funding text: This research was supported by the Hungarian Government, Ministry of Human Capacities (20391-3/2018/FEKUSTRAT) and the European Regional Development Fund (GINOP-2.3.2-15-2016-00009 'ICER') and the University of Szeged Open Access Fund (no. 5386) . D. Molnar would like to thank the support of the Hungarian National Excellence Programme grant (NTP-NFTOd-19-B-0158) . LA - English DB - MTMT ER - TY - JOUR AU - Kempf, M TI - Take a seed! Revealing Neolithic landscape and agricultural development in the Carpathian Basin through multivariate statistics and environmental modelling JF - PLOS ONE J2 - PLOS ONE VL - 16 PY - 2021 IS - 10 PG - 34 SN - 1932-6203 DO - 10.1371/journal.pone.0258206 UR - https://m2.mtmt.hu/api/publication/32474023 ID - 32474023 N1 - Department of Archaeology and Museology, Faculty of Arts, Masaryk University, Brno, Czech Republic Physical Geography, Institute of Environmental Social Science and Geography, University of Freiburg, Freiburg, Germany Export Date: 27 November 2021 CODEN: POLNC Correspondence Address: Kempf, M.; Department of Archaeology and Museology, Czech Republic; email: kempf@phil.muni.cz LA - English DB - MTMT ER - TY - JOUR AU - Ludwig, P AU - Gavrilov, MB AU - Radakovic, MG AU - Markovic, SB TI - Malaco temperature reconstructions and numerical simulation of environmental conditions in the southeastern Carpathian Basin during the Last Glacial Maximum JF - JOURNAL OF QUATERNARY SCIENCE J2 - J QUATERNARY SCI VL - 36 PY - 2021 IS - 8 SP - 1426 EP - 1435 PG - 10 SN - 0267-8179 DO - 10.1002/jqs.3318 UR - https://m2.mtmt.hu/api/publication/32009766 ID - 32009766 N1 - Funding Agency and Grant Number: Helmholtz Climate Initiative REKLIM; DKRZ project [965] Funding text: PL thanks the German Climate Computing Centre (DKRZ, Hamburg) for hosting the MPI-ESM-P data and providing computing resources within DKRZ project 965 `Our Way to Europe -Palaeoclimate and Palaeoenvironmental reconstructions'. PL is supported by the Helmholtz Climate Initiative REKLIM (regional climate change; https://www.reklim.de/en).This study is a contribution to the PALEOLINK project within the PAGES 2k Network. The idea for this study emerges at the CRC 806 (https://www.sfb806.uni-koeln.de/) supported international workshop `Loess and Archaeology' in Aachen in 2019. LA - English DB - MTMT ER - TY - JOUR AU - Marković, SB. AU - Oches, EA. AU - Perić, ZM. AU - Gaudenyi, T AU - Jovanović, M AU - Sipos, Gy AU - Thiel, C AU - Buylaert, JP AU - Savić, S AU - McCoy, WD. AU - Radaković, MG. AU - Marković, RS. AU - Gavrilov, MB. TI - The Požarevac loess–paleosol sequence: a record of increased aridity in the south‐eastern margin of the Carpathian Basin during the last 350 ka JF - JOURNAL OF QUATERNARY SCIENCE J2 - J QUATERNARY SCI VL - 36 PY - 2021 IS - 8 SP - 1436 EP - 1447 PG - 12 SN - 0267-8179 DO - 10.1002/jqs.3327 UR - https://m2.mtmt.hu/api/publication/32062161 ID - 32062161 N1 - Department of Geography, Tourism and Hotel management, Faculty of Science, University of Novi Sad, Novi Sad, Serbia Serbian Academy of Arts and Sciences, Belgrade, Serbia Department of Natural and Applied Sciences, Bentley University, Waltham, MA, United States Research Group for Terrestrial Paleoclimates, Max Planck Institute for Chemistry, Mainz, Germany Geographical Institute SASA “Jovan Cvijić”, Belgrade, Serbia Department of Physical Geography, University of Szeged, Szeged, Hungary Department B4.3: Federal Seismological Survey, Nuclear-Test Ban, Federal Institute for Geosciences and Natural Resources, Hannover, Germany Department of Physics, Technical University of Denmark, RisøCampus, Roskilde, Denmark Department of Geosciences, University of Massachusetts, Amherst, MA, United States Cited By :2 Export Date: 12 October 2021 Correspondence Address: Radaković, M.G.; Department of Geography, Serbia; email: milica.radakovic.95@gmail.com Funding details: Ministarstvo Prosvete, Nauke i Tehnološkog Razvoja, MPNTR, 451‐03‐9/2021‐14/200125 Funding details: Serbian Academy of Sciences and Arts, SASA, F‐178 Funding text 1: We thank the Požarevac Brick factory for allowing the team to work in the quarry. This study was supported by the First Program of the Chinese–Serbian Developing Projects (Project title: ‘A Comparative Study of Past Climate Change in the East Asian Monsoon Region and the Westerly Zone Using Multiple Timescales’). The authors acknowledge financial support of the Ministry of Education, Science and Technological Development of the Republic of Serbia (grant no. 451‐03‐9/2021‐14/200125) and Serbian Academy of Sciences and Arts (grant no. F‐178). AB - The loess sequence preserved in the Pozarevac brickyard in north-eastern Serbia comprises eight loess units separated by seven paleosols. Geochronological investigation using amino acid racemization and luminescence dating support stratigraphic correlations of loess units L3, S2LL1 and L1 at the Pozarevac section with loess of glacial cycles E [Marine Isotope Stage (MIS) 10], D (MIS 9-8), C (MIS 7-6) and B (MIS 5-2) across central Europe. Correlation with the marine oxygen-isotope stratigraphy and associated paleoclimatic inferences are further supported by magnetic susceptibility, particle size and carbonate content measured in Pozarevac sediments. Malacological investigations at the Pozarevac section reveal the continuous presence of the Chondrula tridens and Helicopsis striata faunal assemblages throughout the last 350 ka. The loess malacological fauna, which is characterized by the complete absence of cold-resistant and cold-preferring species, suggests a stable, dry and relatively warm glacial and interglacial climate, compared with other central European loess localities. Together these data suggest that the south-eastern part of the Carpathian (Pannonian, Middle Danube) Basin was a refugium for warm-preferring and xerophilous land-snails during the generally unfavorable glacial climates of the late Middle and Late Pleistocene. LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Gulyás, Sándor TI - Some notes on the interpretation and reliability of malacological proxies in paleotemperature reconstructions from loess- comments to Obreht et al.'s “A critical reevaluation of paleoclimate proxy records from loess in the Carpathian Basin” JF - EARTH-SCIENCE REVIEWS J2 - EARTH-SCI REV VL - 221 PY - 2021 PG - 10 SN - 0012-8252 DO - 10.1016/j.earscirev.2021.103675 UR - https://m2.mtmt.hu/api/publication/32058723 ID - 32058723 N1 - Cited By :1 Export Date: 22 May 2022 Correspondence Address: Gulyás, S.; University of Szeged, Egyetem u.2-6, Hungary; email: gulyas.sandor@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Gulyás, Sándor AU - Molnár, Dávid AU - Bozsó, Gábor AU - Fekete, István AU - Makó, László AU - Cseh, Péter AU - Molnár, Mihály AU - Sümegi, Balázs P. AU - Almond, Peter AU - Zeeden, Christian AU - Törőcsik, Tünde AU - Nett, Janina J. AU - Markó, András AU - Lehmkuhl, Frank TI - New chronology and extended palaeoenvironmental data to the 1975 loess profile of Madaras brickyard, South Hungary JF - JOURNAL OF QUATERNARY SCIENCE J2 - J QUATERNARY SCI VL - 36 PY - 2021 IS - 8 SP - 1364 EP - 1381 PG - 18 SN - 0267-8179 DO - 10.1002/jqs.3382 UR - https://m2.mtmt.hu/api/publication/32471189 ID - 32471189 N1 - Special Issue: Pleistocene geoarchaeology and palaeoenvironments in European loess LA - English DB - MTMT ER - TY - JOUR AU - Tapody, Réka Orsolya AU - Sümegi, Pál AU - Molnár, Dávid AU - Karlik, Máté AU - Törőcsik, Tünde AU - Cseh, Péter AU - Makó, László TI - Sedimentological-Geochemical Data Based Reconstruction of Climate Changes and Human Impacts from the Peat Sequence of Round Lake in the Western Foothill Area of the Eastern Carpathians, Romania JF - QUATERNARY J2 - Quaternary VL - 4 PY - 2021 IS - 2 PG - 29 SN - 2571-550X DO - 10.3390/quat4020018 UR - https://m2.mtmt.hu/api/publication/32064831 ID - 32064831 N1 - Department of Geology and Palaeontology, University of Szeged, Egyetem Str. 2-6, Szeged, H-6722, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Bem Square 18/c, Debrecen, H-4026, Hungary Institute for Geological and Geochemical Research, RCAES, Budaörsi Str. 45, Budapest, H-1112, Hungary Export Date: 23 May 2022 Correspondence Address: Sümegi, P.; Department of Geology and Palaeontology, Egyetem Str. 2-6, Hungary; email: sumegi@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - Gavrilović, B AU - Sümegi, Pál AU - Ćirić, M AU - Radaković, MG. AU - Gavrilov, MB. AU - Mlađan, D AU - Marković, SB. TI - The Middle and Late Pleniglacial (Weichselian) malacofauna of the Zemun loess–paleosol sequence, Serbia JF - PALAEONTOLOGISCHE ZEITSCHRIFT J2 - PALAEONTOL Z VL - 94 PY - 2020 IS - 3 SP - 519 EP - 531 PG - 13 SN - 0031-0220 DO - 10.1007/s12542-019-00465-y UR - https://m2.mtmt.hu/api/publication/30757439 ID - 30757439 N1 - Department of Physical Geography, Geographical Institute “Jovan Cvijić”, Serbian Academy of Sciences and Arts, Djure Jakšića 9, Belgrade, Serbia Department of Geology and Paleontology, University of Szeged, Egyetem ut. 2-6., Szeged, 6222, Hungary Department of Ecology and Technoeconomics, Institute of Chemistry, Technology and Metallurgy, University of Belgrade, Njegoševa 12, Belgrade, Serbia Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, Novi Sad, Serbia The Academy of Criminalistics and Police Studies, Cara Dušana 196, Belgrade, Serbia Cited By :3 Export Date: 22 May 2022 Correspondence Address: Gavrilović, B.; Department of Physical Geography, Djure Jakšića 9, Serbia; email: b.gavrilovic@gi.sanu.ac.rs AB - The aim of our study was to describe the succession of malacological assemblages along the exposed loess profile located in Belgrade, along the banks of the Danube River (municipality of Zemun). Deposits that belong to the composite loess unit L1 were sampled. Loess unit L1 included two subunits: L1SS1 (a Middle Pleniglacial subunit with two weakly developed initial pedogenic horizons) and L1LL1 (a Late Pleniglacial loess subunit). Three malacological zones were distinguished. Malacological results imply a change in climatic conditions and subsequently in vegetation structure. The molluscs indicate an environment with a moderate (warm and dry) climate and a mosaic vegetation type composed of grasslands and forest steppe. Gradual cooling was inferred within the Late Pleniglacial period. Our findings concur with the results of earlier studies indicating that the Zemun site and the adjacent area served as a transition zone between the refuge areas within the southeastern part of the Carpathian Basin during the Late Pleistocene. LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Gulyás, Sándor AU - Molnár, Dávid AU - Szilágyi, Gábor AU - Sümegi, Balázs P AU - Törőcsik, Tünde AU - Molnár, Mihály TI - 14C Dated Chronology of the Thickest and Best Resolved Loess/Paleosol Record of the LGM from SE Hungary Based on Comparing Precision and Accuracy of Age-Depth Models JF - RADIOCARBON J2 - RADIOCARBON VL - 62 PY - 2020 IS - 2 SP - 403 EP - 417 PG - 15 SN - 0033-8222 DO - 10.1017/RDC.2019.154 UR - https://m2.mtmt.hu/api/publication/31124193 ID - 31124193 N1 - Funding Agency and Grant Number: European Union [20391-3/2018/FEKUSTRAT, GINOP-2.3.2-15-201600009]; State of Hungary, Ministry of Human Capacities [20391-3/2018/FEKUSTRAT, GINOP-2.3.2-15-201600009]; European Regional Development Fund [20391-3/2018/FEKUSTRAT, GINOP-2.3.2-15-201600009] Funding text: Research has been carried out within the framework of University of Szeged, Interdisciplinary Excellence Centre, Institute of Geography and Earth Sciences, Long Environmental Changes Research Team. Support of Grants 20391-3/2018/FEKUSTRAT and GINOP-2.3.2-15-201600009 `ICER' are acknowledged by the European Union and the State of Hungary, Ministry of Human Capacities, co-financed by the European Regional Development Fund. LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Molnár, Dávid AU - Gulyás, Sándor AU - Náfrádi, Katalin AU - Sümegi, B P AU - Törőcsik, Tünde AU - Persaits, G AU - Molnár, Mihály AU - Vandenberghe, J AU - Zhou, L TI - High-resolution proxy record of the environmental response to climatic variations during transition MIS3/MIS2 and MIS2 in Central Europe. the loess-paleosol sequence of Katymár brickyard (Hungary) TS - the loess-paleosol sequence of Katymár brickyard (Hungary) JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 504 PY - 2019 SP - 40 EP - 55 PG - 16 SN - 1040-6182 DO - 10.1016/j.quaint.2018.03.030 UR - https://m2.mtmt.hu/api/publication/3361435 ID - 3361435 LA - English DB - MTMT ER - TY - JOUR AU - Törőcsik, Tünde AU - Gulyás, Sándor AU - Sümegi, Pál AU - Sümegi, B AU - Molnár, Dávid AU - Benyó-Korcsmáros, Réka TI - Environmental history of the Csorna plain (Western Danube plain, NW Hungary) from the late glacial to the late Holocene as seen from data of multiproxy geoarchaeological investigations JF - STUDIA QUATERNARIA J2 - STUD QUATER VL - 36 PY - 2019 IS - 1 SP - 19 EP - 43 PG - 25 SN - 1641-5558 DO - 10.24425/sq.2019.126377 UR - https://m2.mtmt.hu/api/publication/30741579 ID - 30741579 N1 - Funding Agency and Grant Number: OTKA [K-112318]; Ministry of Human Capacities, Hungary [20391-3/2018/FEKUSTRAT] Funding text: The research was supported by OTKA grant K-112318 (An Environmental History of the Carpathian Basin in the Middle Ages), the Principal Leader is Prof. Elek Benko, academic director (Institute of Archaeology, Hungarian Academy of Sciences, Budapest). Research has been carried out within the framework of University of Szeged, Interdisciplinary Excellence Centre, Institute of Geography and Earth Sciences, Long Environmental Changes Research Team. Support of the Ministry of Human Capacities, Hungary grant 20391-3/2018/FEKUSTRAT is acknowledged. LA - English DB - MTMT ER - TY - JOUR AU - Chu, W TI - The Danube Corridor Hypothesis and the Carpathian Basin: Geological, Environmental and Archaeological Approaches to Characterizing Aurignacian Dynamics JF - JOURNAL OF WORLD PREHISTORY J2 - J WORLD PREHIST VL - 31 PY - 2018 IS - 2 SP - 117 EP - 178 PG - 62 SN - 0892-7537 DO - 10.1007/s10963-018-9115-1 UR - https://m2.mtmt.hu/api/publication/27595356 ID - 27595356 N1 - Export Date: 3 March 2019 Cited By :7 Export Date: 22 November 2019 Correspondence Address: Chu, W.; Institute for Prehistory, University of Cologne, Weyertal, 125, Germany; email: wchu@uni-koeln.de Cited By :7 Export Date: 27 November 2019 Correspondence Address: Chu, W.; Institute for Prehistory, University of Cologne, Weyertal, 125, Germany; email: wchu@uni-koeln.de LA - English DB - MTMT ER - TY - JOUR AU - Janina, Bösken AU - Sümegi, Pál AU - Christian, Zeeden AU - Nicole, Klasen AU - Gulyás, Sándor AU - Frank, Lehmkuhl TI - Investigating the last glacial Gravettian site ‘Ságvár Lyukas Hill’ (Hungary) and its paleoenvironmental and geochronological context using a multi-proxy approach JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 509 PY - 2018 SP - 77 EP - 90 PG - 43 SN - 0031-0182 DO - 10.1016/j.palaeo.2017.08.010 UR - https://m2.mtmt.hu/api/publication/3298855 ID - 3298855 N1 - Funding Agency and Grant Number: DFG (Deutsche Forschungsgemeinschaft) [INST 216/596-2] Funding text: The investigations were carried out in the context of the CRC 806 "Our way to Europe", subproject B1 "The Eastern Trajectory: Last Glacial Paleogeography and Archeology of the Eastern Mediterranean and of the Balkan Peninsula", supported by the DFG (Deutsche Forschungsgemeinschaft, Grant number INST 216/596-2). All physical and chemical data obtained in this study are available in the Pangaea database at https://doi.pangaea.de/10.1594/PANGAEA.868368. Rock magnetic data were measured in the Laboratory for Palaeo- and Environmental Magnetism (PUM), Bayreuth. We thank Ulrich Hambach for supervision and discussing the data. The luminescence samples were measured at the Cologne Luminescence Lab. We thank Anja Zander for the assessment of the radionuclide concentrations and her help in the laboratory. We thank Marianne Dohms and her team from the sedimentological Lab at the RWTH Aachen University for the measurements of the sedimentological and geochemical samples. Further, the authors would like to thank Christa Loibl for help during fieldwork, and Igor Obreht and Philipp Schulte for fruitful discussions. Moreover, we thank Kathrin Emunds and Heiko Lindner for the compilation of Fig. 1. LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Gulyás, Sándor AU - Molnár, Dávid AU - Sümegi, B P AU - Almond, P C AU - Vandenberghe, J AU - Zhou, L AU - Pál-Molnár, Elemér AU - Törőcsik, Tünde AU - Hao, Q AU - Smalley, I AU - Molnár, Mihály AU - Marsi, István TI - New chronology of the best developed loess/paleosol sequence of Hungary capturing the past 1.1 ma. Implications for correlation and proposed pan-Eurasian stratigraphic schemes TS - Implications for correlation and proposed pan-Eurasian stratigraphic schemes JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 191 PY - 2018 SP - 144 EP - 166 PG - 23 SN - 0277-3791 DO - 10.1016/j.quascirev.2018.04.012 UR - https://m2.mtmt.hu/api/publication/3374753 ID - 3374753 N1 - Megjegyzés-27405538 N1 Funding details: GINOP-2.3.2-15-2016-00009, FEDER, European Regional Development Fund N1 Funding text: The research was supported by the European Union and the State of Hungary, co-financed by the gs1:European Regional Development Fund in the project of GINOP-2.3.2-15-2016-00009 'ICER'. We are grateful for the two anonymous reviewers whose comments helped improving the content of the manuscript to its present form. Appendix A University of Szeged, Department of Geology and Paleontology, Szeged, Hungary Institute of Archeology, Hungarian Academy of Science, Budapest, Hungary Lincoln University, Lincoln, Northern Canterbury, New Zealand Vrije Universiteit Amsterdam, Institute of Earth Sciences, Netherlands University of Beijing, Department of Geomorphology and Quaternary Geology, China University of Szeged, Department of Minerology, Petrology and Geochemistry, Szeged, Hungary Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China University of Leicester, Department of Geography, United Kingdom Institute of Nuclear Research, Hertelendi Laboratory of Environmental Sciences, Debrecen, Hungary ICER Center, Institute of Nuclear Research, Hungarian Academy of Sciences, Debrecen, Hungary Hungarian Geological and Geophysical Institute, Budapest, Hungary Cited By :2 Export Date: 24 September 2019 CODEN: QSRED Correspondence Address: Gulyás, S.; University of Szeged, Department of Geology and PaleontologyHungary; email: gulyas.sandor@geo.u-szeged.hu Funding details: European Regional Development Fund, GINOP-2.3.2-15-2016-00009 Funding text 1: The research was supported by the European Union and the State of Hungary, co-financed by the gs1:European Regional Development Fund in the project of GINOP-2.3.2-15-2016-00009 'ICER'. We are grateful for the two anonymous reviewers whose comments helped improving the content of the manuscript to its present form. Appendix A LA - English DB - MTMT ER - TY - JOUR AU - Szilágyi, Gábor AU - Sümegi, Pál AU - Gulyás, Sándor AU - Molnár, Dávid TI - Revision of the Age of Construction Phases of a Mound Dated to the Late Copper–Early Bronze Age in Eastern Hungary Relying on 14C-Based Chronologies JF - RADIOCARBON J2 - RADIOCARBON VL - 60 PY - 2018 IS - 5 SP - 1403 EP - 1412 PG - 10 SN - 0033-8222 DO - 10.1017/RDC.2018.107 UR - https://m2.mtmt.hu/api/publication/30330204 ID - 30330204 N1 - University of Szeged, Department of Geology and Paleontology, Egyetem street 2, Szeged, H-6722, Hungary Hortobágyi National Park Directorate, Sumen street 2, Debrecen, H-4024, Hungary Hungarian Academy of Sciences, Research Centre for the Humanities Institute of Archaeology, Tóth Kálmán street 4, Budapest, 1097, Hungary Export Date: 12 February 2021 CODEN: RACAA Correspondence Address: Szilágyi, G.; University of Szeged, Egyetem street 2, Hungary; email: szilagyigabor@hnp.hu LA - English DB - MTMT ER - TY - JOUR AU - Tapody, Réka Orsolya AU - Gulyás, Sándor AU - Törőcsik, Tünde AU - Sümegi, Pál AU - Molnár, Dávid AU - Sümegi, B P AU - Molnár, Mihály TI - Radiocarbon-dated peat development. anthropogenic and climatic signals in a Holocene raised bog and lake profile from the Eastern part of the Carpathian Basin TS - anthropogenic and climatic signals in a Holocene raised bog and lake profile from the Eastern part of the Carpathian Basin JF - RADIOCARBON J2 - RADIOCARBON VL - 60 PY - 2018 IS - 4 SP - 1215 EP - 1226 PG - 12 SN - 0033-8222 DO - 10.1017/RDC.2018.38 UR - https://m2.mtmt.hu/api/publication/3388045 ID - 3388045 N1 - \n Department of Geology and Palaeontology, University of Szeged, Egyetem street 2, Szeged, 6722, Hungary \n Archaeological Institute of Hungarian Academy of Sciences, Úri street 49, Budapest, Hungary \n Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Hungarian Academy of Sciences (Atomki), Bem tér 18/c, Debrecen, 4026, Hungary \n Export Date: 6 November 2018 \n CODEN: RACAA \n Correspondence Address: Tapody, R.O.; Department of Geology and Palaeontology, University of Szeged, Egyetem street 2, Hungary; email: tapody@geo.u-szeged.hu Department of Geology and Palaeontology, University of Szeged, Egyetem street 2, Szeged, 6722, Hungary Archaeological Institute of Hungarian Academy of Sciences, Úri street 49, Budapest, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Hungarian Academy of Sciences (Atomki), Bem tér 18/c, Debrecen, 4026, Hungary Export Date: 22 February 2021 CODEN: RACAA Correspondence Address: Tapody, R.O.; Department of Geology and Palaeontology, Egyetem street 2, Hungary; email: tapody@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - Törőcsik, Tünde AU - Gulyás, Sándor AU - Molnár, Dávid AU - Tapody, Réka Orsolya AU - Sümegi, BP AU - Szilágyi, Gábor AU - Molnár, Mihály AU - Jakab, Gusztáv AU - Sümegi, Pál AU - Novák, Zsolt TI - Probabilistic 14C Age-Depth Models Aiding the Reconstruction of Holocene Paleoenvironmental Evolution of a Marshland from Southern Hungary JF - RADIOCARBON J2 - RADIOCARBON VL - 60 PY - 2018 IS - 5 SP - 1301 EP - 1315 PG - 15 SN - 0033-8222 DO - 10.1017/RDC.2018.112 UR - https://m2.mtmt.hu/api/publication/30338111 ID - 30338111 N1 - Department of Geology and Paleontology, University of Szeged, Egyetem street 2, Szeged, 6722, Hungary Archaeological Institute of Hungarian Academy of Sciences, Úri street 49, Budapest, Hungary Hortobágy National Park, Sumen u. 2, Debrecen, 4024, Hungary Institute of Nuclear Research of HAS, Bem tér 18/c, Debrecen, 4026, Hungary Tessedik Campus, Szabadság út 1-3, Szarvas, 5540, Hungary Department of Physical Geography and Geoinformatics, University of Szeged, Egyetem street 2, Szeged, 6722, Hungary Export Date: 7 January 2019 CODEN: RACAA Correspondence Address: Törå'csik, T.; Department of Geology and Paleontology, University of Szeged, Egyetem street 2, Hungary; email: t.torocsik@geo.u-szeged.hu Department of Geology and Paleontology, University of Szeged, Egyetem street 2, Szeged, 6722, Hungary Archaeological Institute of Hungarian Academy of Sciences, Úri street 49, Budapest, Hungary Hortobágy National Park, Sumen u. 2, Debrecen, 4024, Hungary Institute of Nuclear Research of HAS, Bem tér 18/c, Debrecen, 4026, Hungary Tessedik Campus, Szabadság út 1-3, Szarvas, 5540, Hungary Department of Physical Geography and Geoinformatics, University of Szeged, Egyetem street 2, Szeged, 6722, Hungary Export Date: 22 February 2021 CODEN: RACAA Correspondence Address: Törå'csik, T.; Department of Geology and Paleontology, Egyetem street 2, Hungary; email: t.torocsik@geo.u-szeged.hu AB - This paper presents first chronological results for a Holocene marshland system from the southern part of the Danube-Tisza Interfluve. Radiocarbon (C-14) ages were used to build age-depth models relying of probabilistic tools. Four models have been built: a linear one using dates gained via simple calibration, a P_Sequence model, fitting a polynomial function to calibrated dates; a Gamma_Sequence considering priori given and posterior accumulation rates have been constructed. As there was no significant difference between the mean values of individual models all seem suitable for establishing a reliable chronology despite differences in 95% CI ranges. While P_Sequence models underestimated SR, values calculated from the polynomial model were not significantly different from those of the G_Sequence. Based on multiproxy geochemical, sedimentological, paleoecological data the evolution of the system was reconstructed, covering a timespan of ca. 13,000 years starting from 12,000 BC and lasting until 1300 AD. Highest accumulation rates are dated to the Early Middle Ages from the 11th century. Several climate changes could have been identified which are present in other Hungarian and Western European records too, such as the 5b IRD event at ca. 5800 BC, a humid phase around 1600 BC, and a cool humid phase around the 6th century AD. LA - English DB - MTMT ER - TY - JOUR AU - Kustár, Rozália AU - Molnár, Dávid AU - Sümegi, Pál AU - Törőcsik, Tünde AU - Sávai, Szilvia TI - Preliminary paleoecological reconstruction of long-term relationship between human and environment in the northern part of Danube-along Plain, Hungary JF - OPEN GEOSCIENCES J2 - OPEN GEOSCI VL - 8 PY - 2016 IS - 1 SP - 405 EP - 419 PG - 15 SN - 2391-5447 DO - 10.1515/geo-2016-0026 UR - https://m2.mtmt.hu/api/publication/3159156 ID - 3159156 N1 - Visky Károly Museum, Szent István krt. 25, Kalocsa, H-6300, Hungary Department of Geology and Palaeontolgy, University of Szeged, Egyetem u. 2-6, Szeged, H-6722, Hungary Institute of Archaeology, Hungarian Academy of Sciences, Úri u. 49, Budapest, H-1014, Hungary Cited By :4 Export Date: 25 May 2022 Correspondence Address: Kustár, R.; Visky Károly Museum, Szent István krt. 25, Hungary; email: rozina_kustar@t-online.hu LA - English DB - MTMT ER - TY - JOUR AU - Schatz, AK AU - Scholten, T AU - Kuehn, P TI - Paleoclimate and weathering of the Tokaj (Hungary) loess-paleosol sequence JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 426 PY - 2015 SP - 170 EP - 182 PG - 13 SN - 0031-0182 DO - 10.1016/j.palaeo.2015.03.016 UR - https://m2.mtmt.hu/api/publication/27496822 ID - 27496822 N1 - Export Date: 14 December 2020 CODEN: PPPYA Correspondence Address: Schatz, A.-K.; Soil Science and Geomorphology Group, Department of Geosciences, Faculty of Science, University of Tübingen, Rümelinstraße 19-23, Germany LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Molnár, Dávid AU - Sávai, Szilvia AU - Náfrádi, Katalin AU - Novák, Z AU - Szelepcsényi, Zoltán AU - Törőcsik, Tünde TI - First radiocarbon dated paleoecological data from the freshwater carbonates of the Danube-Tisza Interfluve JF - OPEN GEOSCIENCES J2 - OPEN GEOSCI VL - 7 PY - 2015 IS - 1 SP - 40 EP - 52 PG - 13 SN - 2391-5447 DO - 10.1515/geo-2015-0003 UR - https://m2.mtmt.hu/api/publication/2846935 ID - 2846935 N1 - Cited By :4 Export Date: 25 May 2022 Correspondence Address: Sümegi, P.; Department of Geology and Paleontology, Egyetem u. 2-6., Hungary; email: sumegi@geo.u-szeged.hu AB - The first radiocarbon dates available on the evolution of the freshwater carbonates of the Danube-Tisza Interfluve are presented in this work along with their possible uses to precisely date paleoecological and paleoenvironmental changes. This work also gives the basis of a comparative analysis of the Holocene radiocarbon-dated profile of Csólyospálos with other Hungarian radiocarbondated profiles of the same age (Bátorliget, the Sárrét, etc.) and the implementation of a detailed chronological and regional paleoenvironmental study. Furthermore, our findings clearly demonstrate the importance of radiocarbon analysis in the study of terminal Pleistocene and Holocene Hungarian sedimentary sequences for accurately dating and reconstructing the chronological order of paleoenvironmental changes as well as the evolution of the natural endowments plus the regional comparison of the various profiles. LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Náfrádi, Katalin AU - Molnár, Dávid AU - Sávai, Szilvia TI - Results of paleoecological studies in the loess region of Szeged-Öthalom (SE Hungary) JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 372 PY - 2015 SP - 66 EP - 78 PG - 13 SN - 1040-6182 DO - 10.1016/j.quaint.2014.09.003 UR - https://m2.mtmt.hu/api/publication/2755798 ID - 2755798 N1 - Funding Agency and Grant Number: European Union; State of Hungary; European Social Fund [TAMOP-4.2.4.A/2-11/1-2012-0001] Funding text: The research of Pal Sumegi was supported by the European Union and the State of Hungary, co-financed by the European Social Fund in the framework of TAMOP-4.2.4.A/2-11/1-2012-0001 'National Excellence Program'. LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Magyari, Enikő Katalin AU - Dániel, Péter AU - Molnár, Mihály AU - Törőcsik, Tünde TI - Responses of terrestrial ecosystems to Dansgaard–Oeshger cycles and Heinrich-events: A 28,000-year record of environmental changes from SE Hungary JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 293 PY - 2013 SP - 34 EP - 50 PG - 17 SN - 1040-6182 DO - 10.1016/j.quaint.2012.07.032 UR - https://m2.mtmt.hu/api/publication/2203162 ID - 2203162 N1 - Available online 5 August 2012 AB - According to the findings of a complex sedimentological, geochemical, malacological and pollen study implemented on a core sequence of an alkaline lake (Fehér Lake), interstadials in the SE Great Hungarian Plain were characterized by increased boreal woodland cover during Marine Isotope Stage 2 (MIS 2: 29,700–14,500 cal BP). These interstadials were dated to 26,420–27,970, 23,185–24,880, and 18,810–20,770 cal BP, and correlate well with the Dansgaard-Oeschger (DO) interstadials 2 and 3 and the post LGM warm interval seen in the Greenland ice core oxygen isotope records. Intervening cold phases, on the other hand, were found between 24,880–26,420 and 20,770–23,185 cal BP, correlating with Heinrich event 2 and the LGM. These data overall confirm that millennial scale climate variability during Marine Isotope Stage 2 had profound effect on the terrestrial ecosystems in the continental interior of SE Europe, leading to periodic boreal woodland expansions and contractions and wildfires. LA - English DB - MTMT ER - TY - JOUR AU - Vlačiky, M AU - Michalík, T AU - Nyvltova, Fisakova M AU - Nývlt, D AU - Moravcová, M AU - Králík, M AU - Kovanda, J AU - Péková, K AU - Přichystal, A AU - Dohnalová, A TI - Gravettian occupation of the Beckov Gate in Western Slovakia as viewed from the interdisciplinary research of the Trenčianske Bohuslavice-Pod Tureckom site JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 294 PY - 2013 SP - 41 EP - 60 PG - 20 SN - 1040-6182 DO - 10.1016/j.quaint.2011.09.004 UR - https://m2.mtmt.hu/api/publication/23393664 ID - 23393664 N1 - State Geological Inst. of Dionýz Štúr, Mlynská dolina 1, 817 04 Bratislava 11, Slovakia Department of Geological Sciences, Faculty of Science, Masaryk University, Kotlářská 2, 611 37 Brno, Czech Republic Department of Archaeology, Faculty of Arts, Comenius University in Bratislava, Gondova 2, 818 01 Bratislava, Slovakia Institute of Archaeology in Brno, Academy of Sciences of the Czech Republic, V.v.i., Královopolská 147, 612 00 Brno, Czech Republic Czech Geological Survey, Leitnerova 22, 658 69 Brno, Czech Republic Department of Anthropology, Faculty of Sciences, Masaryk University, Vinařská 5, 60 200 Brno, Czech Republic not available, Dobropolská 26, 102 00 Praha 10, Czech Republic not available, Podzáhradná 3, 821 06 Bratislava, Slovakia Cited By :20 Export Date: 29 May 2022 Correspondence Address: Vlačiky, M.; State Geological Inst. of Dionýz Štúr, Mlynská dolina 1, 817 04 Bratislava 11, Slovakia; email: martin.vlaciky@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Demény, Attila AU - Schöll-Barna, Gabriella AU - Sümegi, Pál AU - Sipos, Péter AU - Fórizs, István AU - Balázs, Réka AU - Bajnóczi, Bernadett AU - Cook, G TI - Stable isotope compositions of bivalve shells and geochemistry of bulk sediments in a 5-20 ky fluvial section at Körösladány, SE Hungary: Sedimentary changes vs. climate signals JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 55 PY - 2012 IS - 4 SP - 417 EP - 439 PG - 23 SN - 1788-2281 DO - 10.1556/CEuGeol.55.2012.4.4 UR - https://m2.mtmt.hu/api/publication/2517245 ID - 2517245 N1 - Hungarian Academy of Sciences, Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Budaörsi út 45, H-1112 Budapet, Hungary University of Szeged, Department of Geology and Palaeontology, Egyetem u. 2, H-6722 Szeged, Hungary Scottish Universities Environmental Research Centre Rankine Avenue, Scottish Enterprise Technology Park, East Kilbride Glasgow, G75 0QF, United Kingdom Export Date: 14 December 2020 Correspondence Address: Hungarian Academy of Sciences, Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Budaörsi út 45, H-1112 Budapet, Hungary LA - English DB - MTMT ER - TY - JOUR AU - Fitzsimmons, KE AU - Markovic, SB AU - Hambach, U TI - Pleistocene environmental dynamics recorded in the loess of the middle and lower Danube basin JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 41 PY - 2012 SP - 104 EP - 118 PG - 15 SN - 0277-3791 DO - 10.1016/j.quascirev.2012.03.002 UR - https://m2.mtmt.hu/api/publication/27496831 ID - 27496831 N1 - Cited By :99 Export Date: 24 September 2019 CODEN: QSRED Correspondence Address: Fitzsimmons, K.E.; Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Deutscher Platz 6, D-04103 Leipzig, Germany; email: kathryn_fitzsimmons@eva.mpg.de Cited By :115 Export Date: 27 October 2020 CODEN: QSRED Correspondence Address: Fitzsimmons, K.E.; Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Deutscher Platz 6, D-04103 Leipzig, Germany; email: kathryn_fitzsimmons@eva.mpg.de LA - English DB - MTMT ER - TY - JOUR AU - Schatz, A -K AU - Zech, M AU - Buggle, B AU - Gulyás, Sándor AU - Hambach, U AU - Marković, S B AU - Sümegi, Pál AU - Scholten, T TI - The late Quaternary loess record of Tokaj, Hungary: Reconstructing palaeoenvironment, vegetation and climate using stable C and N isotopes and biomarkers JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 240 PY - 2011 IS - 1-2 SP - 52 EP - 61 PG - 10 SN - 1040-6182 DO - 10.1016/j.quaint.2010.10.009 UR - https://m2.mtmt.hu/api/publication/1943042 ID - 1943042 N1 - Funding Agency and Grant Number: Geographical Institute, University of Tubingen; Alexander von Humboldt-Foundation Funding text: The authors would like to thank G.D. Pall and G. Persaits (University of Szeged) for help during fieldwork, Prof G. Gebauer and his team (Biogeochemistry Group, BayCEER, University of Bayreuth) for stable isotope and elemental concentration measurements, A. Mergner (University of Bayreuth) for support in the laboratory and K. Schmidt (University of Tubingen) for help with graphs and figures. We also appreciated the comments of the editor and the anonymous reviewer. A. Schatz received financial support from the Geographical Institute, University of Tubingen. M. Zech greatly acknowledges the support provided by the Alexander von Humboldt-Foundation. AB - Large areas of Southeast Europe are covered by Pleistocene loess deposits with interbedded palaeosol layers, reflecting interglacials or -stadials. These loess-palaeosol sequences are valuable terrestrial archives for continuous palaeoclimatic and palaeoenvironmental information. In recent years, the traditional paradigm of treeless full-glacial palaeoenvironments has increasingly been called into question, as there is palynological, anthracological and malacological evidence for the continuous presence of trees from loess-palaeosol sequences in the Carpathian Basin. This paper aims at contributing to this discussion by applying biogeochemical, geophysical and sedimentological methods to a late Quaternary loess-palaeosol profile at Tokaj, NE Hungary. Previous studies at the same location have focused on molluscs and charcoal, while this study concentrated on stable C and N isotopes and lipid biomarkers. Long-chain n-alkanes (C 23-C 33), which form major constituents of plant leaf waxes, have successfully been used as biomarkers over the last years and allow for a reconstruction of palaeovegetation based on the differentiation of grassland vs. shrubs and trees. Stable carbon isotopes were used to further differentiate between C 3 and C 4 palaeovegetation, and stable N isotopes to reconstruct the N cycle and climatic variations. Magnetic susceptibility (MS), organic carbon and grain size distribution, which may serve as proxies for e.g. the intensity of pedegenesis, weathering and palaeowind strength, were measured to complement the biogeochemical results and to establish a pedo- and biostratigraphy. Although the results do not agree in every detail with previous studies, there are surprising matches and similarities in the data. Alkane and stable N isotopic data indicate that, pedogenesis occurred under productive, fertile steppe-grasslands, probably in an intensified seasonal climate, and during reduced sedimentation. Two short treeless-steppe periods were found between 26 and 12 ka BP. However, periods characterised by a cooler climate in which trees and shrubs expanded were also found. This interpretation is also supported by previous mollusc data that provide evidence for several periods of favourable conditions for tree growth. © 2010 Elsevier Ltd and INQUA. LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál TI - Archeomalakológiai vizsgálatok Magyarországon. Archaeomalacological research in Hungary TS - Archaeomalacological research in Hungary JF - ARCHEOMETRIAI MŰHELY J2 - ARCHEOMETRIAI MŰHELY VL - 8 PY - 2011 IS - 2 SP - 101 EP - 116 PG - 16 SN - 1786-271X UR - https://m2.mtmt.hu/api/publication/1951422 ID - 1951422 N1 - Szegedi Tudományegyetem, Földtani es Oslénytani Tanszék, 6722 Szeged Egyetem u. 2, Hungary MTA Régészeti Intézet, 1014 Budapest Úri u. 49, Hungary Export Date: 22 May 2022 Correspondence Address: Sümegi, P.; Szegedi Tudományegyetem, 6722 Szeged Egyetem u. 2, Hungary; email: sumegi@geo.u-szeged.hu LA - Hungarian DB - MTMT ER - TY - JOUR AU - Sümegi, Pál TI - Kis-balatoni és balatoni fúrások archeomalakológiai vizsgálatának eredményei. The results of the archaeomalacological investigaton of the core sequences from Balaton and Little Balaton basins TS - The results of the archaeomalacological investigaton of the core sequences from Balaton and Little Balaton basins JF - ARCHEOMETRIAI MŰHELY J2 - ARCHEOMETRIAI MŰHELY VL - 8 PY - 2011 IS - 2 SP - 137 EP - 156 PG - 20 SN - 1786-271X UR - https://m2.mtmt.hu/api/publication/1951428 ID - 1951428 N1 - Szegedi Tudományegyetem, Földtani és Oslénytani Tanszék, Egyetem u. 2, 6722 Szeged, Hungary MTA Régészeti Intézet, Úri u. 49, 1014 Budapest, Hungary Export Date: 22 May 2022 Correspondence Address: Sümegi, P.; Szegedi Tudományegyetem, Egyetem u. 2, 6722 Szeged, Hungary; email: sumegi@geo.u-szeged.hu LA - Hungarian DB - MTMT ER - TY - JOUR AU - Veres, Z AU - Sümegi, Pál AU - Törőcsik, Tünde TI - First radiocarbon-dated holocene record of Pomatias elegans in Hungary - Results of complex archeomalacological investigations from the Marshland of Ócsa. Az ócsai láp archeomalakológiai vizsgálata - A Pomatias elegans elso{combining double acute accent} radiokarbon adatokkal korolt holocén elo{combining double acute accent}fordulása Magyarországon TS - Az ócsai láp archeomalakológiai vizsgálata - A Pomatias elegans elso{combining double acute accent} radiokarbon adatokkal korolt holocén elo{combining double acute accent}fordulása Magyarországon JF - ARCHEOMETRIAI MŰHELY J2 - ARCHEOMETRIAI MŰHELY VL - 8 PY - 2011 IS - 2 SP - 181 EP - 196 PG - 16 SN - 1786-271X UR - https://m2.mtmt.hu/api/publication/24439174 ID - 24439174 N1 - Szegedi Tudományegyetem, Földtani és Oslénytani Tanszék, Egyetem u. 2, 6722 Szeged, Hungary MTA Régészeti Intézete, Úri utca 49, 1014 Budapest, Hungary Export Date: 29 May 2022 Correspondence Address: Veres, Z.; Szegedi Tudományegyetem, Egyetem u. 2, 6722 Szeged, Hungary; email: vereszsolti@gmail.com LA - Hungarian DB - MTMT ER - TY - JOUR AU - Hammouti, Nasera AU - Schmitt, Thomas AU - Seitz, Alfred AU - Kosuch, Joachim AU - Veith, Michael TI - Combining mitochondrial and nuclear evidences: a refined evolutionary history of Erebia medusa (Lepidoptera: Nymphalidae: Satyrinae) in Central Europe based on the COI gene JF - JOURNAL OF ZOOLOGICAL SYSTEMATICS AND EVOLUTIONARY RESEARCH J2 - J ZOOL SYST EVOL RES VL - 48 PY - 2010 IS - 2 SP - 115 EP - 125 PG - 11 SN - 0947-5745 DO - 10.1111/j.1439-0469.2009.00544.x UR - https://m2.mtmt.hu/api/publication/27496796 ID - 27496796 LA - English DB - MTMT ER - TY - JOUR AU - Konrád, Gyula AU - Kovács, János AU - Halász, Amadé AU - Sebe, Krisztina AU - Palffy, H TI - Late Quaternary woolly mammoth (Mammuthus primigenius Blum) remains from southern Transdanubia, Hungary JF - COMPTES RENDUS PALEVOL J2 - CR PALEVOL VL - 9 PY - 2010 IS - 1-2 SP - 47 EP - 54 PG - 8 SN - 1631-0683 DO - 10.1016/j.crpv.2009.08.001 UR - https://m2.mtmt.hu/api/publication/1344146 ID - 1344146 N1 - Megjegyzés-21914561 : FN Thomson Reuters Web of Knowledge LA - English DB - MTMT ER - TY - CHAP AU - Varga, Zoltán Sándor ED - Habel, J C ED - Assmann, T TI - Extra-mediterranean refugia, post-glacial vegetation history and area dynamics in Eastern Central Europe T2 - Relict Species: Phylogeography and Conservation Biology PB - Springer Netherlands CY - Berlin CY - Heidelberg SN - 9783540921592 PY - 2010 SP - 57 EP - 87 PG - 31 DO - 10.1007/978-3-540-92160-8_3 UR - https://m2.mtmt.hu/api/publication/25104120 ID - 25104120 AB - Evidences from fossil records and genetic research suggest that the arboreal refugia were not restricted to Southern Europe and in particular to the Mediterranean peninsulas during the full-glacials. Fossil pollen data and macrofossil remains indicate that several tree species have survived also at the Southern edge of the cold-dry steppe-tundra area in Central and Eastern Europe. Recent results of surveys on the Late Pleistocene Mammalian fauna clearly contradict to the "tree-less tundra" models for Europe North of the transverse mountain ranges of the Pyrenees, Alps and Carpathians. It was pointed out that the carrying capacity to feed the herds of large herbivores demands a rather productive environment. The presence of Northern temperate refugia is also supported by the "nonanalogue" assemblages of small mammals discovered from the Late Pleistocene of unglaciated areas of Eastern Central Europe. The assembly of species today typifying the tundra, steppe and semi-desert habitats seems to include also species from deciduous woodland. Extra-Mediterranean core areas were identified also in widely dispersed cold-tolerant frogs and reptiles. Some of their core areas had been at least near the Carpathians and/or marginal areas of the Carpathian Basin. The close faunal connections of the Carpathians suggest the existence of highly dynamic contacts and exchanges with mountains of the Balkan Peninsula during the climatic fluctuations of the Upper Pleistocene. The Eastern and Southern Carpathians, together with the mountains of Western Transylvania, can be considered as core areas of survival and autochtonous evolution in some invertebrate groups with limited mobility. The post-glacial re-population of the Carpathian Basin from different directions has been supported by Illyrian versus Dacian vicarious pairs of sister species/subspecies. In mobile insect groups, peripherically isolated sibling species/subspecies have only been evolved, which display manifold biogeographic connections, e.g. to the Balkan Peninsula, Asia Minor or Southern Russia. The organisation of community-complexes of the Pannonian forest-steppe connected by habitat ecotones resulted in the overlap of several different faunal types, e.g. Mediterranean, Balkanic, Siberian, Ponto-Caspian, Ponto-Pannonian, Turano-Eremic and Xeromontane elements. LA - English DB - MTMT ER - TY - JOUR AU - Timár, Gábor AU - Gábris, Gyula TI - Estimation of the water conducting capacity of the natural flood conducting channels of the Tisza floodplain, the Great Hungarian Plain JF - GEOMORPHOLOGY J2 - GEOMORPHOLOGY VL - 98 PY - 2008 IS - 3-4 SP - 250 EP - 261 PG - 12 SN - 0169-555X DO - 10.1016/j.geomorph.2006.12.031 UR - https://m2.mtmt.hu/api/publication/1138107 ID - 1138107 AB - The rapidly subsiding central part of the Pannonian Basin, the flood-plain system of the Tisza River, is analyzed. Natural flood-conducting channels that were functioning prior to the construction of the water control measures of the 19th century have been identified and mapped. By now these channels have mostly disappeared; only small traces of them can be found on modern maps. The identification of these channels was achieved by studying historical maps of the region and by geomorphologic studies. Drawing the outline of the channels and the estimation of their initial meander size was supported by elevation models and satellite imagery. Eight flood breakout points and five independent channel systems were identified. The flood conveying capacity of each channel was also estimated, based on meander wavelengths. The reliability of this estimation is discussed. The channels functioned as anabranches, conducting the floods of the Tisza to its tributary, the Körös River. The efficiency of the flood control system could be increased by regeneration of these natural channels. The summarized water conveying capacity of the abandoned channels is estimated as 1000 m3/s, a value that is slightly under a half of the flood discharge of the Tisza River. LA - English DB - MTMT ER - TY - JOUR AU - Jenei, M AU - Gulyás, Sándor AU - Sümegi, Pál AU - Molnár, Mihály TI - Holocene lacustrine carbonate formation: old ideas in the light of new radiocarbon data from a single site in Central Hungary JF - RADIOCARBON J2 - RADIOCARBON VL - 49 PY - 2007 IS - 2 SP - 1017 EP - 1021 PG - 5 SN - 0033-8222 DO - 10.1017/S0033822200042879 UR - https://m2.mtmt.hu/api/publication/1183251 ID - 1183251 LA - English DB - MTMT ER - TY - JOUR AU - Marković, SB AU - Oches, EA AU - McCoy, WD AU - Frechen, M AU - Gaudenyi, Tivadar TI - Malacological and sedimentological evidence for "warm" glacial climate from the Irig loess sequence, Vojvodina, Serbia JF - GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS J2 - GEOCHEM GEOPHY GEOSY VL - 8 PY - 2007 IS - 9 PG - 12 SN - 1525-2027 DO - 10.1029/2006GC001565 UR - https://m2.mtmt.hu/api/publication/2972519 ID - 2972519 LA - English DB - MTMT ER - TY - JOUR AU - Schmitt, Thomas TI - Molecular biogeography of Europe: Pleistocene cycles and postglacial trends JF - FRONTIERS IN ZOOLOGY J2 - FRONT ZOOL VL - 4 PY - 2007 PG - 13 SN - 1742-9994 DO - 10.1186/1742-9994-4-11 UR - https://m2.mtmt.hu/api/publication/27496798 ID - 27496798 N1 - Cited By :648 Export Date: 29 May 2022 Correspondence Address: Schmitt, T.; Biogeographie, Fachbereich VI, Wissenschaftspark Trier-Petrisberg, D - 54286 Trier, Germany; email: thsh@uni-trier.de LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Molnár, Mihály AU - Sudár Sándorné Svingor, Éva AU - Szántó, Andrea Zsuzsanna AU - Hum, L AU - Gulyás, Sándor TI - Results of radiocarbon analysis of Upper Weichselian loess sequences from Hungary JF - RADIOCARBON J2 - RADIOCARBON VL - 49 PY - 2007 IS - 2 SP - 1023 EP - 1030 PG - 6 SN - 0033-8222 DO - 10.1017/S0033822200042880 UR - https://m2.mtmt.hu/api/publication/1183257 ID - 1183257 N1 - University of Szeged, Department of Geology and Paleontology, Egyetem u. 2-6, 6722 Szeged, Hungary Institute of Nuclear Research of Hungarian Academy of Sciences, Laboratory of Environmental Studies, Bem tér 18/C, 4026 Debrecen, Hungary Cited By :10 Export Date: 22 May 2022 CODEN: RACAA Correspondence Address: Sümegi, P.; University of Szeged, Egyetem u. 2-6, 6722 Szeged, Hungary; email: sumegi@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - Schmitt, Thomas AU - Habel, Jan Christian AU - Zimmermann, Marco AU - Mueller, Paul TI - Genetic differentiation of the marbled white butterfly, Melanargia galathea, accounts for glacial distribution patterns and postglacial range expansion in southeastern Europe JF - MOLECULAR ECOLOGY J2 - MOL ECOL VL - 15 PY - 2006 IS - 7 SP - 1889 EP - 1901 PG - 13 SN - 0962-1083 DO - 10.1111/j.1365-294X.2006.02900.x UR - https://m2.mtmt.hu/api/publication/27496800 ID - 27496800 N1 - Department VI-Biogeography, University of Trier, Am Wissenschaftspark 25-27, D-54296 Trier, Germany Department of Biogeography, University of Trier, Germany Cited By :52 Export Date: 29 May 2022 CODEN: MOECE Correspondence Address: Schmitt, T.; Department VI-Biogeography, Am Wissenschaftspark 25-27, D-54296 Trier, Germany; email: thsh@uni-trier.de LA - English DB - MTMT ER - TY - JOUR AU - Pazonyi, Piroska TI - Mammalian ecosystem dynamics in the Carpathian Basin during the last 27,000 years JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 212 PY - 2004 IS - 3-4 SP - 295 EP - 314 PG - 20 SN - 0031-0182 DO - 10.1016/j.palaeo.2004.06.008 UR - https://m2.mtmt.hu/api/publication/1393291 ID - 1393291 LA - English DB - MTMT ER - TY - JOUR AU - Nádor, Annamária AU - Lantos, M AU - Tóth-Makk, Á AU - Thamóné Bozsó, Edit TI - Milankovitch-scale multi-proxy records from fluvial sediments of the last 2.6 Ma, Pannonian Basin, Hungary. JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 22 PY - 2003 SP - 2157 EP - 2175 PG - 19 SN - 0277-3791 DO - 10.1016/S0277-3791(03)00134-3 UR - https://m2.mtmt.hu/api/publication/2702559 ID - 2702559 LA - English DB - MTMT ER - TY - JOUR AU - Schmitt, T AU - Giessl, A AU - Seitz, A TI - Did Polyommatus icarus (Lepidoptera: Lycaenidae) have distinct glacial refugia in southern Europe? Evidence from population genetics JF - BIOLOGICAL JOURNAL OF THE LINNEAN SOCIETY J2 - BIOL J LINN SOC VL - 80 PY - 2003 IS - 3 SP - 529 EP - 538 PG - 10 SN - 0024-4066 DO - 10.1046/j.1095-8312.2003.00261.x UR - https://m2.mtmt.hu/api/publication/23393680 ID - 23393680 LA - English DB - MTMT ER - TY - JOUR AU - Schmitt, T AU - Gießl, A AU - Seitz, A TI - Postglacial colonisation of western Central Europe by Polyommatus coridon (Poda 1761) (Lepidoptera: Lycaenidae): Evidence from population genetics JF - HEREDITY J2 - HEREDITY VL - 88 PY - 2002 IS - 1 SP - 26 EP - 34 PG - 9 SN - 0018-067X DO - 10.1038/sj/hdy/6800003 UR - https://m2.mtmt.hu/api/publication/23393682 ID - 23393682 LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Krolopp, E TI - Quatermalacological analyses for modeling of the Upper Weichselian palaeoenvironmental changes in the Carpathian Basin JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 91 PY - 2002 IS - 1 SP - 53 EP - 63 PG - 11 SN - 1040-6182 DO - 10.1016/S1040-6182(01)00102-1 UR - https://m2.mtmt.hu/api/publication/231404 ID - 231404 N1 - Department of Geology and Palaeontology, University of Szeged, Egyetem u.2, 6722, Szeged, Hungary Archaeological Institute of Hungarian Academy Sciences, Úri u. 51, 1024, Budapest, Hungary Hungarian Geological Institute, Stefánia u. 14, 1143, Budapest, Hungary Cited By :136 Export Date: 22 May 2022 Correspondence Address: Sümegi, P.; Department of Geology/Palaeontology, , Szeged Egyetem u.2. 6722, Hungary; email: sumegi@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - Magyari, Enikő Katalin AU - Sümegi, Pál AU - Braun, Mihály AU - Jakab, Gusztáv AU - Molnár, Mihály TI - Retarded wetland succession: anthropogenic and climatic signals in a Holocene peat bog profile from north-east Hungary JF - JOURNAL OF ECOLOGY J2 - J ECOL VL - 89 PY - 2001 IS - 6 SP - 1019 EP - 1032 PG - 14 SN - 0022-0477 DO - 10.1046/j.0022-0477.2001.00624.x UR - https://m2.mtmt.hu/api/publication/1177778 ID - 1177778 N1 - Department of Mineralogy and Geology, University of Debrecen, PO Box 4, H-4010 Debrecen, Hungary Department of Geology and Palaeontology, University of Szeged, PO Box 658, H-6701 Szeged, Hungary Department of Inorganic and Analytical Chemistry, University of Debrecen, PO Box 21, H-4010 Debrecen, Hungary Institute of Nuclear Research, Hungarian Academy of Sciences, PO Box 51, H-4001, Hungary Cited By :63 Export Date: 29 May 2022 CODEN: JECOA Correspondence Address: Magyari, E.; Department of Mineralogy, P.O. Box 4, H-4010 Debrecen, Hungary; email: magyari@tigris.klte.hu LA - English DB - MTMT ER - TY - JOUR AU - Rudner, Edina AU - Sümegi, Pál TI - Recurring Taiga forest-steppe habitats in the Carpathian Basin in the Upper Weichselian JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 76-77 PY - 2001 SP - 177 EP - 189 PG - 13 SN - 1040-6182 DO - 10.1016/S1040-6182(00)00101-4 UR - https://m2.mtmt.hu/api/publication/1177772 ID - 1177772 N1 - Cited By :76 Export Date: 22 May 2022 Correspondence Address: Rudner, Z.E.; Geographical Research Institute, Budaörsi u. 43-45, Budapest, H-1112, Hungary; email: rze@freemail.hu LA - English DB - MTMT ER - TY - JOUR AU - Schmitt, T AU - Seitz, A TI - Intraspecific allozymatic differentiation reveals the glacial refugia and the postglacial expansions of European Erebia medusa (Lepidoptera: Nymphalidae) JF - BIOLOGICAL JOURNAL OF THE LINNEAN SOCIETY J2 - BIOL J LINN SOC VL - 74 PY - 2001 IS - 4 SP - 429 EP - 458 PG - 30 SN - 0024-4066 DO - 10.1006/bijl.2001.0584 UR - https://m2.mtmt.hu/api/publication/23393685 ID - 23393685 LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Rudner, Edina TI - In situ charcoal fragments as remains of natural wild fires in the upper Würm of the Carpathian Basin JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 76/77 PY - 2001 SP - 165 EP - 176 PG - 12 SN - 1040-6182 DO - 10.1016/S1040-6182(00)00100-2 UR - https://m2.mtmt.hu/api/publication/1177775 ID - 1177775 N1 - Department of Mineralogy and Geology, L. Kossuth University, P.O. Box 4, 4010 Debrecen, Hungary Institute of Geography, Hungarian Academy of Sciences, Budaörsi U. 43-45, Budapest, 1112, Hungary Department of Geology and Palaeontology, University of Szeged, Egyetem U. 2, Szeged, H-6722, Hungary Cited By :34 Export Date: 22 May 2022 Correspondence Address: Sümegi, P.; Dept. of Mineralogy and Geology, P.O. Box 4, 4010 Debrecen, Hungary; email: sumegi@tigris.kltc.hu LA - English DB - MTMT ER - TY - JOUR AU - Willis, KJ AU - Rudner, Edina AU - Sümegi, Pál TI - The full-glacial forests of central and southeastern Europe JF - QUATERNARY RESEARCH J2 - QUATERNARY RES VL - 53 PY - 2000 IS - 2 SP - 203 EP - 213 PG - 11 SN - 0033-5894 DO - 10.1006/qres.1999.2119 UR - https://m2.mtmt.hu/api/publication/1177762 ID - 1177762 N1 - Nincs jelölve a levelező szerzőség a közleményen. (SE SZTE admin5) LA - English DB - MTMT ER - TY - JOUR AU - Sólymos, Péter AU - Sümegi, Pál TI - The shell morpho-thermometer method and its application in palaeoclimatic reconstruction JF - ANNALES UNIVERSITATIS SCIENTIARUM BUDAPESTINENSIS DE ROLANDO EÖTVÖS NOMINATAE - SECTIO GEOLOGICA J2 - ANN UNIV SCI BP R EÖTVÖS NOM SECT GEOL VL - 32 PY - 1999 SP - 137 EP - 148 PG - 12 SN - 0365-0634 UR - https://m2.mtmt.hu/api/publication/1184524 ID - 1184524 N1 - Nincs jelölve a levelező szerzőség a közleményen. (SE SZTE admin5) LA - English DB - MTMT ER - TY - JOUR AU - Tóth, C TI - The identification of the palaeoclimatic and palaeo-ecological development of Hortobagy National Park in the Pleistocene/Holocene transition period JF - PETERMANNS GEOGRAPHISCHE MITTEILUNGEN J2 - PETERMANNS GEOGR MITT VL - 143 PY - 1999 IS - 3 SP - 219 EP - 227 PG - 9 SN - 0031-6229 UR - https://m2.mtmt.hu/api/publication/23393688 ID - 23393688 LA - German DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Hertelendi, Ede TI - Reconstruction of Microenvironmental Changes in the Kopasz Hill Loess Area at Tokaj (Hungary) Between 15 and 70 ka BP JF - RADIOCARBON J2 - RADIOCARBON VL - 40 PY - 1998 IS - 2 SP - 855 EP - 863 PG - 9 SN - 0033-8222 DO - 10.1017/s0033822200018828 UR - https://m2.mtmt.hu/api/publication/1177756 ID - 1177756 N1 - Megjegyzés-24810524 Megjegyzés-21827259 PN: Part 2 Megjegyzés-23377741 PN 2 Megjegyzés-21827197 PN: Part 2 Nincs jelölve a levelező szerzőség a közleményen. (SE SZTE admin5) LA - English DB - MTMT ER - TY - JOUR AU - Willis, K J AU - Braun, Mihály AU - Sümegi, Pál AU - Tóth, Albert TI - Does soil change cause vegetation change or vice versa? A temporal perspective from Hungary JF - ECOLOGY J2 - ECOLOGY VL - 78 PY - 1997 IS - 3 SP - 740 EP - 750 PG - 11 SN - 0012-9658 DO - 10.1890/0012-9658(1997)078[0740:DSCCVC]2.0.CO;2 UR - https://m2.mtmt.hu/api/publication/1177751 ID - 1177751 N1 - Nincs jelölve a levelező szerzőség a közleményen. (SE SZTE admin5) LA - English DB - MTMT ER - TY - JOUR AU - Dergachev, V AU - Chistyakov, V TI - Cosmogenic radiocarbon and cyclical natural processes JF - RADIOCARBON J2 - RADIOCARBON VL - 37 PY - 1995 IS - 2 SP - 417 EP - 424 PG - 8 SN - 0033-8222 DO - 10.1017/S0033822200030897 UR - https://m2.mtmt.hu/api/publication/21632091 ID - 21632091 N1 - [H09009->P08041] LA - English DB - MTMT ER - TY - JOUR AU - Krolopp, E AU - Sümegi, Pál TI - Palaeoecological reconstruction of the Late Pleistocene, Based on Loess Malacofauna in Hungary JF - GEOJOURNAL J2 - GEOJOURNAL VL - 36 PY - 1995 IS - 2-3 SP - 213 EP - 222 PG - 10 SN - 0343-2521 DO - 10.1007/BF00813173 UR - https://m2.mtmt.hu/api/publication/1177739 ID - 1177739 N1 - Nincs jelölve a levelező szerzőség a közleményen. (SE SZTE admin5) LA - English DB - MTMT ER - TY - JOUR AU - Willis, K J AU - Sümegi, Pál AU - Braun, Mihály AU - Tóth, Albert TI - The Late Quaternary environmental history of Bátorliget, N.E. Hungary JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 118 PY - 1995 IS - 1-2 SP - 25 EP - 47 PG - 23 SN - 0031-0182 DO - 10.1016/0031-0182(95)00004-6 UR - https://m2.mtmt.hu/api/publication/1177745 ID - 1177745 N1 - Nincs jelölve a levelező szerzőség a közleményen. (SE SZTE admin5) LA - English DB - MTMT ER - TY - JOUR AU - Goodfriend, GA TI - The use of land snail shells in paleoenvironmental reconstruction JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 11 PY - 1992 IS - 6 SP - 665 EP - 685 PG - 21 SN - 0277-3791 DO - 10.1016/0277-3791(92)90076-K UR - https://m2.mtmt.hu/api/publication/21632090 ID - 21632090 N1 - [H07925->P08041] LA - English DB - MTMT ER -