TY - JOUR AU - Makó, László AU - Cseh, P AU - Nagy, Balázs AU - Sümegi, Pál AU - Molnár, Dávid TI - Development History of the Loess–Paleosol Profiles of Pécel, Kisdorog and Bonyhádvarasd, Hungary JF - QUATERNARY J2 - Quaternary VL - 6 PY - 2023 IS - 3 PG - 21 SN - 2571-550X DO - 10.3390/quat6030038 UR - https://m2.mtmt.hu/api/publication/34047615 ID - 34047615 AB - This study covers the examination of four loess–paleosol profiles in Hungary through grain size composition, organic matter, carbonate content and magnetic susceptibility measurements. One of the profiles (with a thickness of 25.72 m) can be found in the Gödöllő hills, on the border of town Pécel, and the other three profiles (Kisdorog-West—5.60 m, Kisdorog-East—6.40 and Bonyhádvarasd—8.16 m) are located in the Tolna hills of the Transdanubia region. The sections were continuously sampled with an interval of 4 cm. The same interval was also applied to the other three profiles. During the field exploration of the Pécel profile, we were able to study the complete loess wall, which was deposited on the sediment of the nearby Rákos stream. Based on the Ostracod fauna of the clay sediment beneath, the fluvial deposit can be considered as originating from the Upper Miocene. In the case of the Transdanubian sections, a significant change can be observed in the prevailing wind direction based on the grain size analyses. In addition, the results of magnetic susceptibility measurements suggest that the development of the Pécel profile took place during MIS 9–10, while the age of the three Transdanubian sections can be assumed to be the MIS 2–4. 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 - Almond, PC. AU - Gulyás, Sándor AU - Sümegi, Pál AU - Sümegi, BP. AU - Covey-Crump, S AU - Jones, M AU - Shaw, J AU - Parker, A TI - A palaeoenvironmental record of the Southern Hemisphere last glacial maximum from the Mount Cass loess section, North Canterbury, Aotearoa/New Zealand JF - QUATERNARY RESEARCH J2 - QUATERNARY RES VL - 102 PY - 2021 SP - 115 EP - 129 PG - 15 SN - 0033-5894 DO - 10.1017/qua.2020.95 UR - https://m2.mtmt.hu/api/publication/31816012 ID - 31816012 LA - English DB - MTMT ER - TY - JOUR AU - Makó, László AU - Molnár, Dávid AU - Cseh, Péter AU - Sümegi, Pál TI - MAR comparisons between different chronometric methods for two profiles in the Bodrogkeresztúr area JF - STUDIA QUATERNARIA J2 - STUD QUATER VL - 38 PY - 2021 IS - 1 SP - 67 EP - 73 PG - 7 SN - 1641-5558 DO - 10.24425/sq.2020.133761 UR - https://m2.mtmt.hu/api/publication/31817980 ID - 31817980 N1 - Department of Geology and Paleontology, University of Szeged, Egyetem u. 2-6, Szeged, H-6722, Hungary University of Szeged, Interdisciplinary Excellence Centre, Institute of Geography and Earth Sciences, Long Environmental Changes research team, Egyetem u. 2-6, Szeged, H-6722, Hungary Cited By :2 Export Date: 22 May 2022 Correspondence Address: Makó, L.; Department of Geology and Paleontology, Egyetem u. 2-6, Hungary; email: makol@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - Molnár, Dávid AU - Makó, László AU - Cseh, Péter AU - Sümegi, Pál AU - Fekete, István AU - Galović, L TI - Middle and Late Pleistocene loess-palaeosol archives in East Croatia: multi-proxy palaeoecological studies on Zmajevac and Šarengrad II sequences JF - STUDIA QUATERNARIA J2 - STUD QUATER VL - 38 PY - 2021 IS - 1 SP - 3 EP - 17 PG - 15 SN - 1641-5558 DO - 10.24425/sq.2020.133758 UR - https://m2.mtmt.hu/api/publication/31962092 ID - 31962092 N1 - Funding Agency and Grant Number: Ministry of Human Capacities, Hungary [20391-3/2018/FEKUSTRAT]; Croatian Science Foundation [SAPIQ 4425] Funding text: This work has been supported in part Ministry of Human Capacities, Hungary grant 20391-3/2018/FEKUSTRAT and Croatian Science Foundation under the project SAPIQ 4425. Authors would like to thank the reviewers' efforts for making the manuscript better and reach its final form. 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 - Trájer, Attila János TI - The changing malaria risk patterns in East‐Central Europe and the North Balkans in the last 27 000 years JF - JOURNAL OF QUATERNARY SCIENCE J2 - J QUATERNARY SCI VL - 2021 PY - 2021 SN - 0267-8179 DO - 10.1002/jqs.3357 UR - https://m2.mtmt.hu/api/publication/32165831 ID - 32165831 N1 - Funding Agency and Grant Number: Szechenyi 2020 project of the Hungarian Ministry of Innovation and Technology [GINOP-2.3.2-15-2016-00016, NKFIH-872] Funding text: This work was supported by the Szechenyi 2020 project of the Hungarian Ministry of Innovation and Technology under grant no. GINOP-2.3.2-15-2016-00016. The research presented in this article was carried out with the support of the NKFIH-872 project. LA - English DB - MTMT ER - TY - JOUR AU - Rózsa, Péter AU - Incze, József AU - Balogh, Szabolcs AU - Novák, Tibor József TI - A novel approach to quantifying the degree of anthropogenic surface transformation – the concept of ‘hemeromorphy’ JF - ERDKUNDE J2 - ERDKUNDE VL - 74 PY - 2020 IS - 1 SP - 45 EP - 57 PG - 13 SN - 0014-0015 DO - 10.3112/erdkunde.2020.01.03 UR - https://m2.mtmt.hu/api/publication/31259838 ID - 31259838 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 - Bösken, J AU - Obreht, I AU - Zeeden, C AU - Klasen, N AU - Hambach, U AU - Sümegi, Pál AU - Lehmkuhl, F TI - High-resolution paleoclimatic proxy data from the MIS3/2 transition recorded in northeastern Hungarian loess JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 502/PartA PY - 2019 SP - 95 EP - 107 PG - 13 SN - 1040-6182 DO - 10.1016/j.quaint.2017.12.008 UR - https://m2.mtmt.hu/api/publication/3331516 ID - 3331516 N1 - Funding Agency and Grant Number: DFG (Deutsche Forschungsgemeinschaft) [INST 216/596-2, CRC 806] Funding text: The investigations were carried out within CRC 806 "Our way to Europe", subproject B1 "The Eastern Trajectory: Last Glacial Paleogeography and Archaeology 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 CRC806 database (see Bosken et al., 2017c). We thank Anja Zander for the assessment of the radionuclide concentrations and her help in the Cologne Luminescence Laboratory. We thank Marianne Dohms and her team from the sedimentological Laboratory at the RWTH Aachen University for the measurements of the sedimentological and geochemical samples. Further, the authors would like to thank David Molnar and Balazs Sumegi for help during fieldwork, and Philipp Schulte and Daniel Veres for fruitful discussions. Finally, we thank Wei Chu for his assistance in the field, his advice on the manuscript and the preparation of the radiocarbon sample. Part number: A AB - The Bodrogkeresztúr loess-paleosol sequence in northeastern Hungary was investigated to improve our understanding of the paleoenvironmental conditions at the foothills of the Carpathians and their impact on the Gravettian population. The main part of the section is comprised of eolian deposits that enable the reconstruction of the paleoenvironmental conditions. This study comprises grain size, geochemical, color and rock magnetic analysis, as well as luminescence and radiocarbon dating. The chronological data place this section from later MIS 3 until present, but also suggest erosion of the sediment in the late MIS 2 and the (early) Holocene. Moreover, generally more humid conditions during late MIS3 and early MIS2 are observed, in comparison to other regions in the Carpathian Basin. Main dust source was most likely the Tisza floodplain, and the material was probably transported to the site from a northeastern wind direction. Increased weathering led to the formation of a well-developed MIS3 paleosol. The loess exhibits elevated values of frequency dependent magnetic susceptibility that highlight the relatively mild conditions during loess formation. Nevertheless, two loess layers with high sand abundance in the profile indicate colder and dryer conditions with increased eolian dynamics during short periods within MIS2. Finally, the Bodrogkeresztúr section highlights the unique microclimatic conditions at the foothill areas of the Carpathian Basin, which may have offered a favorable environment for the Gravettian population. © 2017 Elsevier Ltd and INQUA. LA - English DB - MTMT ER - TY - JOUR AU - Molnár, Dávid AU - Sümegi, Pál AU - Fekete, István AU - Makó, László AU - P. Sümegi, B TI - Radiocarbon dated malacological records of two Late Pleistocene loess-paleosol sequences from SW-Hungary. Paleoecological inferences TS - Paleoecological inferences JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 504 PY - 2019 SP - 108 EP - 117 PG - 10 SN - 1040-6182 DO - 10.1016/j.quaint.2018.01.018 UR - https://m2.mtmt.hu/api/publication/3327732 ID - 3327732 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 - Szilágyi, Gábor AU - Náfrádi, Katalin AU - Sümegi, Pál TI - A preliminary chronological study to understand the construction phases of a Late Copper–Early Bronze Age kurgan (kunhalom) JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 62 PY - 2019 IS - 1 SP - 27 EP - 55 PG - 29 SN - 1788-2281 DO - 10.1556/24.61.2018.11 UR - https://m2.mtmt.hu/api/publication/30413691 ID - 30413691 N1 - Import hibák 2019-01-29 10:46 {"M3":"doi: 10.1556/24.61.2018.11"} doi: 10.1556/24.61.2018.11 Cited By :1 Export Date: 12 February 2021 Correspondence Address: Szilágyi, G.; Department of Nature Protection, Sumen Utca 2, Hungary; email: szilagyigabor@hnp.hu Funding text 1: The authors would like to thank Balázs Pál Sümegi and Tünde Töro˝csik for assisting in the sedimentological and magnetic susceptibility measurements, as well as Dr. Dávid Gergely Pál for assisting in the geochemical measurements. They would also like to express their special thanks to the Hortobágy National Park Directorate for the financial support provided. AB - The aim of this study is to identify the milestones of landscape evolution around the Ecse Mound (Karcag-Kunmadaras, Hortobágy National Park, Hungary) in the Holocene period by sedimentological and malacological analysis of strata underneath and within the body of the kurgan concerned, including that of the same characteristics of the artificially piled layers. An undisturbed core drilling was carried out and the sedimentological properties of both the mound and of the substrate baserock were revealed, analysis of which has been supported by three radiocarbon (AMS) measurements. The baserock formation during the last phase of the Ice Age, Middle and Upper Pleniglacial, and Late Glacial phases was followed by soil development in the Holocene, while the mound was constructed in two phases at the end of the Copper Age by the communities of the Pit Grave (Yamna or Ochre Grave) Culture. By publishing these preliminary data, it is also intended to draw attention to the need of focused research efforts by standardized methodology in kurgan research, in order to make the results of different studies consistent and comparable. 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 - Chu, Wei AU - Lengyel, György AU - Zeeden, Christian AU - Péntek, Attila AU - Kaminská, Ľubomíra AU - Mester, Zsolt TI - Early Upper Paleolithic surface collections from loess-like sediments in the northern Carpathian Basin JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 485 PY - 2018 SP - 167 EP - 182 PG - 16 SN - 1040-6182 DO - 10.1016/j.quaint.2017.05.017 UR - https://m2.mtmt.hu/api/publication/3244739 ID - 3244739 AB - The way in which modern humans first entered Europe has been a recent focus of Upper Paleolithic research. A leading theory posits that the Danube served as a conduit for migration from Southeastern into Central and Western Europe. However, a challenge to this has been the scarcity of Early Upper Paleolithic sites along the Middle Danube (Carpathian) Basin. Though several sites with Early Upper Paleolithic features (Szeletian, Aurignacian) are known from surface prospections, few have been archeologically investigated in detail. 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 - Martin, Schumacher AU - Dobos, Anna AU - Wolfram, Schier AU - Brigitta, Schütt TI - Holocene valley incision in the southern Bükk foreland: Climate-human-environment interferences in northern Hungary JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 463 PY - 2018 IS - A SP - 91 EP - 109 PG - 19 SN - 1040-6182 DO - 10.1016/j.quaint.2016.10.021 UR - https://m2.mtmt.hu/api/publication/3200317 ID - 3200317 LA - English DB - MTMT ER - TY - JOUR AU - Nadachowski, A. AU - Lipecki, G. AU - Baca, M. AU - Zmihorski, M. AU - Wilczyński, J. TI - Impact of climate and humans on the range dynamics of the woolly mammoth (Mammuthus primigenius) in Europe during MIS 2 JF - QUATERNARY RESEARCH J2 - QUATERNARY RES VL - 90 PY - 2018 IS - 3 SP - 439 EP - 456 PG - 18 SN - 0033-5894 DO - 10.1017/qua.2018.54 UR - https://m2.mtmt.hu/api/publication/30363709 ID - 30363709 N1 - Institute of Systematics and Evolution of Animals, Polish Academy of Sciences, Sławkowska 17, Kraków, 31-016, Poland Center of New Technologies, University of Warsaw, Banacha 2c, Warsaw, 02-097, Poland Institute of Nature Conservation, Polish Academy of Sciences, Mickiewicza 33, Kraków, 31-120, Poland Export Date: 27 December 2018 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 - 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 - Novák, Tibor József AU - Csámer, Árpád AU - Incze, József AU - Papp, I AU - Rózsa, Péter TI - Szekunder karbonátok mennyisége és vertikális eloszlása tokaji talajszelvényekben JF - AGROKÉMIA ÉS TALAJTAN J2 - AGROKÉMIA ÉS TALAJTAN VL - 65 PY - 2016 IS - 2 SP - 193 EP - 206 PG - 14 SN - 0002-1873 DO - 10.1556/0088.2016.65.2.2 UR - https://m2.mtmt.hu/api/publication/3146640 ID - 3146640 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Törőcsik, Tünde AU - Náfrádi, Katalin AU - Sümegi, Balázs Pál AU - Majkut, Péter AU - Molnár, Dávid AU - Tapody, Réka Orsolya TI - Radiocarbon dated complex paleoecological and geoarcheological analyses at the Bodrogkeresztúr – Henye Gravettian site (NE Hungary) [A bodrogkeresztrúi Henye tetői Gravetti lelőhely komplex paleoökológiai és geoarcheológiai elemzése (ÉK Magyarország)] JF - ARCHEOMETRIAI MŰHELY J2 - ARCHEOMETRIAI MŰHELY VL - 13 PY - 2016 IS - 1 SP - 31 EP - 41 PG - 11 SN - 1786-271X UR - https://m2.mtmt.hu/api/publication/3158287 ID - 3158287 N1 - Szegedi Tudományegyetem Földtani és Oslénytani Tanszék, Egyetem utca 2., Szeged, 6722, Hungary MTA BTK Régészeti Intézet, Úri utca 49, Budapest, 1014, Hungary Cited By :5 Export Date: 22 May 2022 LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Náfrádi, Katalin TI - A radiocarbon-dated cave sequence and the Pleistocene/Holocene transition in Hungary JF - OPEN GEOSCIENCES J2 - OPEN GEOSCI VL - 7 PY - 2015 IS - 1 SP - 783 EP - 798 PG - 16 SN - 2391-5447 DO - 10.1515/geo-2015-0051 UR - https://m2.mtmt.hu/api/publication/3045359 ID - 3045359 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 - Schatz, AK AU - Qi, Y AU - Siebel, W AU - Wu, J AU - Zoeller, L TI - Tracking potential source areas of Central European loess: examples from Tokaj (HU), Nussloch (D) and Grub (AT) JF - OPEN GEOSCIENCES J2 - OPEN GEOSCI VL - 7 PY - 2015 IS - 1 SP - 678 EP - 720 PG - 43 SN - 2391-5447 DO - 10.1515/geo-2015-0048 UR - https://m2.mtmt.hu/api/publication/27496789 ID - 27496789 N1 - Soil Science and Geomorphology Group, Department of Geosciences, University of Tübingen, Rümelinstr. 19-23, Tubingen, 72072, Germany School of Earth and Space Sciences, University of Science and Technology of China, Hefei, 230026, China State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, China Department of Geosciences, University of Tübingen, Wilhelmstr. 56, Tubingen, 72074, Germany Research School of Earth Sciences, Australian National University, Canberra, ACT, Australia Department of Geomorphology, University of Bayreuth, Universitätsstr. 30, Bayreuth, 95440, Germany Cited By :5 Export Date: 24 September 2019 Correspondence Address: Schatz, A.-K.; Soil Science and Geomorphology Group, Department of Geosciences, University of Tübingen, Rümelinstr. 19-23, Germany; email: ann.schatz@uni-tuebingen.de 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 - Alexandrowicz, Witold Pawel TI - Malacological sequence of Weichselian (MIS 5-2) loess series from a profile in Grodzisko Dolne (southern Poland) and its palaeogeographic significance JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 319 PY - 2014 SP - 109 EP - 118 PG - 10 SN - 1040-6182 DO - 10.1016/j.quaint.2013.08.048 UR - https://m2.mtmt.hu/api/publication/24810332 ID - 24810332 N1 - Funding Agency and Grant Number: AGH University of Science and Technology [11.11.140.173] Funding text: This study has been sponsored by the AGH University of Science and Technology through University grant no. 11.11.140.173. LA - English DB - MTMT ER - TY - JOUR AU - Kemencei, Zita AU - Farkas, Roland Tibor AU - Páll-Gergely, B AU - Vilisics, Ferenc AU - Nagy, Antal AU - Hornung, Erzsébet AU - Sólymos, Péter TI - Microhabitat associations of land snails in forested dolinas: implications for coarse filter conservation JF - COMMUNITY ECOLOGY J2 - COMMUNITY ECOL VL - 15 PY - 2014 IS - 2 SP - 180 EP - 186 PG - 7 SN - 1585-8553 DO - 10.1556/comec.15.2014.2.6 UR - https://m2.mtmt.hu/api/publication/2485324 ID - 2485324 LA - English DB - MTMT ER - TY - JOUR AU - Novák, Tibor József AU - Incze, József AU - Spohn, M AU - Glina, B AU - Giani, L TI - Soil and vegetation transformation in abandoned vineyards of the Tokaj Nagy-Hill JF - CATENA J2 - CATENA VL - 123 PY - 2014 SP - 88 EP - 98 PG - 10 SN - 0341-8162 DO - 10.1016/j.catena.2014.07.017 UR - https://m2.mtmt.hu/api/publication/2723923 ID - 2723923 N1 - Megjegyzés-27496825 Megjegyzés-26852040 OA No LA - English DB - MTMT ER - TY - JOUR AU - Újvári, Gábor AU - Molnár, Mihály AU - Novothny, Ágnes AU - Páll-Gergely, Barna AU - Kovács, János AU - Várhegyi, András TI - AMS 14C and OSL/IRSL dating of the Dunaszekcső loess sequence (Hungary): chronology for 20 to 150 ka and implications for establishing reliable age–depth models for the last 40 ka JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 106 PY - 2014 IS - SI SP - 140 EP - 154 PG - 15 SN - 0277-3791 DO - 10.1016/j.quascirev.2014.06.009 UR - https://m2.mtmt.hu/api/publication/2790432 ID - 2790432 N1 - Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Csatkai E. u. 6-8., Sopron, H-9400, Hungary Hertelendi Laboratory of Environmental Studies, Institute for Nuclear Research, Hungarian Academy of Sciences, Bem tér 18/C, Debrecen, H-4026, Hungary Department of Physical Geography, Eötvös Loránd University, Pazmany Peter setany 1/c, Budapest, H-1117, Hungary Department of Biology, Shinshu University, Matsumoto, 390-8621, Japan Department of Geology and Meteorology, University of Pécs, Ifjúság u. 6., Pécs, 7624, Hungary Environmental Analytical and Geoanalytical Research Group, Szentágothai Research Centre, University of Pécs, Ifjúság útja 20., Pécs, H-7624, Hungary Department of Environmental Engineering, Polláck Mihály Faculty of Engineering and Information Technology, University of Pécs, Rozmaring u. 17., Pécs, H-7634, Hungary Export Date: 15 October 2019 CODEN: QSRED Correspondence Address: Újvári, G.; Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Csatkai E. u. 6-8., Hungary; email: ujvari@ggki.hu Funding Agency and Grant Number: Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [OTKA PD-108639, OTKA PD-100315]; Bolyai Janos Research Scholarship of the Hungarian Academy of SciencesHungarian Academy of Sciences; EUEuropean Union (EU) [TAMOP-4.2.2.C-11/1/KONV-2012-0015, SROP-4.2.1.B-10/2/KONV-2010-0002, TAMOP-4.2.2.A-11/1/KONV-2012-0043] Funding text: This work has been funded by post doc projects from the Hungarian Scientific Research Fund to GU (OTKA PD-108639) and to AN (OTKA PD-100315). Additional financial support provided by the Bolyai Janos Research Scholarship of the Hungarian Academy of Sciences (GU) and the EU through the TAMOP-4.2.2.C-11/1/KONV-2012-0015 Earth System, the SROP-4.2.1.B-10/2/KONV-2010-0002 and ENVIKUT (TAMOP-4.2.2.A-11/1/KONV-2012-0043) projects is gratefully acknowledged. Special thanks to Christine Thiel, Jan-Pieter Buylaert and Andrew Murray for the fruitful discussions on post-IR IRSL dating and for the possibility to etching fine-grained samples at the Nordic Laboratory for Luminescence Dating, Riso National Laboratory, Roskilde, Denmark. Guest editor Achim Brauer and the two anonymous referees are thanked for their valuable input which helped us to refine the original manuscript substantially. Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Csatkai E. u. 6-8., Sopron, H-9400, Hungary Hertelendi Laboratory of Environmental Studies, Institute for Nuclear Research, Hungarian Academy of Sciences, Bem tér 18/C, Debrecen, H-4026, Hungary Department of Physical Geography, Eötvös Loránd University, Pazmany Peter setany 1/c, Budapest, H-1117, Hungary Department of Biology, Shinshu University, Matsumoto, 390-8621, Japan Department of Geology and Meteorology, University of Pécs, Ifjúság u. 6., Pécs, 7624, Hungary Environmental Analytical and Geoanalytical Research Group, Szentágothai Research Centre, University of Pécs, Ifjúság útja 20., Pécs, H-7624, Hungary Department of Environmental Engineering, Polláck Mihály Faculty of Engineering and Information Technology, University of Pécs, Rozmaring u. 17., Pécs, H-7634, Hungary Cited By :46 Export Date: 16 February 2021 CODEN: QSRED Correspondence Address: Újvári, G.; Geodetic and Geophysical Institute, Csatkai E. u. 6-8., Hungary; email: ujvari@ggki.hu Funding details: European Commission, EC Funding details: Magyar Tudományos Akadémia, MTA Funding details: Hungarian Scientific Research Fund, OTKA, PD-100315, OTKA PD-108639 Funding text 1: This work has been funded by post doc projects from the Hungarian Scientific Research Fund to GÚ ( OTKA PD-108639 ) and to ÁN ( OTKA PD-100315 ). Additional financial support provided by the Bolyai János Research Scholarship of the Hungarian Academy of Sciences (GÚ) and the EU through the TÁMOP-4.2.2.C-11/1/KONV‒2012-0015 Earth System, the SROP-4.2.1.B-10/2/KONV-2010-0002 and ENVIKUT (TÁMOP-4.2.2.A-11/1/KONV-2012-0043) projects is gratefully acknowledged. Special thanks to Christine Thiel, Jan-Pieter Buylaert and Andrew Murray for the fruitful discussions on post-IR IRSL dating and for the possibility to etching fine-grained samples at the Nordic Laboratory for Luminescence Dating, Risø National Laboratory, Roskilde, Denmark. Guest editor Achim Brauer and the two anonymous referees are thanked for their valuable input which helped us to refine the original manuscript substantially. Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Csatkai E. u. 6-8., Sopron, H-9400, Hungary Hertelendi Laboratory of Environmental Studies, Institute for Nuclear Research, Hungarian Academy of Sciences, Bem tér 18/C, Debrecen, H-4026, Hungary Department of Physical Geography, Eötvös Loránd University, Pazmany Peter setany 1/c, Budapest, H-1117, Hungary Department of Biology, Shinshu University, Matsumoto, 390-8621, Japan Department of Geology and Meteorology, University of Pécs, Ifjúság u. 6., Pécs, 7624, Hungary Environmental Analytical and Geoanalytical Research Group, Szentágothai Research Centre, University of Pécs, Ifjúság útja 20., Pécs, H-7624, Hungary Department of Environmental Engineering, Polláck Mihály Faculty of Engineering and Information Technology, University of Pécs, Rozmaring u. 17., Pécs, H-7634, Hungary Export Date: 22 February 2021 CODEN: QSRED Correspondence Address: Újvári, G.; Geodetic and Geophysical Institute, Csatkai E. u. 6-8., Hungary; email: ujvari@ggki.hu AB - Abstract As revealed by 18 AMS radiocarbon and 24 OSL/IRSL ages the Dunaszekcső loess-paleosol sequence is an excellent terrestrial record of paleoenvironmental change in the Carpathian Basin for the last 130 ka, with significant soil forming episodes during the Eemian interglacial (130–115 ka, MIS 5e) and in some subsequent MIS 5 stages, and distinct periods of loess accumulations during the MIS 4 and MIS 2. Charcoals from the sequence made it possible to test the accuracy of 14C ages from mollusc shells. This approach revealed that 14C ages from some gastropods having small shells (<10 mm) (Succinella oblonga, Vitrea crystallina) are statistically indistinguishable from the ages of charcoals, while others (Clausiliidae sp., Chondrula tridens) show age anomalies up to 600–800 years. OSL and pIRIR@290 ages are found to be consistently older, while post-IR OSL ages are younger than the 14C ages from charcoals and molluscs by some thousands of years, except for pIRIR@225 ages that match the radiocarbon ages quite well. OSL and IRSL ages have scatters up to 7–10 thousand years within 40 ka, while charcoals and small molluscs yield consistent ages with relatively low variability. Beyond the observation that some small molluscs seem to yield reliable 14C ages, calibrated 2σ age ranges of the radiocarbon data (ca 500–800 years for 20 to 30 ka) are an order of magnitude narrower than those of the OSL/IRSL methods (1800–4000 years for 25 to 35 ka). Thus, for establishing chronologies within 40 ka, which are both accurate and precise enough to address issues like synchroneity of millennial-scale paleoenvironmental events across regions (e.g. North Atlantic and Europe), AMS radiocarbon dating of shells of specific loess molluscs and charcoals may probably be a powerful chronological tool. However, additional work is definitely required involving 14C and OSL/IRSL dates from other loess sequences to further test the performance of these two supposedly robust chronometers. 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 - 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 - Kovács, János TI - Radiocarbon chronology of Late Pleistocene large mammal faunas from the Pannonian basin (Hungary) JF - BULLETIN OF GEOSCIENCES J2 - B GEOSCI VL - 87 PY - 2012 IS - 1 SP - 13 EP - 19 PG - 7 SN - 1214-1119 DO - 10.3140/bull.geosci.1282 UR - https://m2.mtmt.hu/api/publication/1925602 ID - 1925602 N1 - Megjegyzés-22302044 RID: A-8807-2010 WC: Geosciences, Multidisciplinary; Paleontology LA - English DB - MTMT ER - TY - JOUR AU - Páll, Dávid Gergely AU - Persaits, Gergő AU - Náfrádi, Katalin AU - Sümegi, Pál TI - Középső-würm végi fosszilis talaj- és löszréteg átmeneti szintjének komplex paleoökológiai vizsgálata a tokaji Kopasz-hegyen JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 142 PY - 2012 IS - 3 SP - 251 EP - 268 PG - 18 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/2197608 ID - 2197608 N1 - SZTE Földtani és Oslénytani Tanszék, 6722 Szeged Egyetem u. 2, Hungary MTA Régészeti Intézet, 1014 Budapest Úri u. 49, Hungary Export Date: 22 May 2022 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Schatz, AK AU - Buylaert, JP AU - Murray, A AU - Stevens, T AU - Scholten, T TI - Establishing a luminescence chronology for a palaeosol-loess profile at Tokaj (Hungary): A comparison of quartz OSL and polymineral IRSL signals JF - QUATERNARY GEOCHRONOLOGY J2 - QUAT GEOCHRONOL VL - 10 PY - 2012 IS - SI SP - 68 EP - 74 PG - 7 SN - 1871-1014 DO - 10.1016/j.quageo.2012.02.018 UR - https://m2.mtmt.hu/api/publication/27496830 ID - 27496830 N1 - Cited By :43 Export Date: 26 May 2022 Correspondence Address: Schatz, A.-K.; Soil Science and Geomorphology Work Group, Rümelinstrasse 19-23, D-72070 Tübingen, Germany; email: ann.schatz@uni-tuebingen.de LA - English DB - MTMT ER - TY - CHAP AU - Sümegi, Pál AU - Persaits, G AU - Gulyás, Sándor ED - Myster, Randall W TI - Woodland-Grassland Ecotonal Shifts in Environmental Mosaics: Lessons Learnt from the Environmental History of the Carpathian Basin (Central Europe) During the Holocene and the Last Ice Age Based on Investigation of Paleobotanical and Mollusk Remains. T2 - Ecotones Between Forest and Grassland PB - Springer New York CY - New York, New York SN - 9781461437970 PY - 2012 SP - 17 EP - 57 PG - 41 DO - 10.1007/978-1-4614-3797-0_2 UR - https://m2.mtmt.hu/api/publication/2044262 ID - 2044262 N1 - Cited By :34 Export Date: 22 May 2022 Correspondence Address: Sümegi, P.; Department of Geology and Paleontology, Egyetem u.2-6, Hungary LA - English DB - MTMT ER - TY - JOUR AU - Varga, György AU - Kovács, János AU - Újvári, Gábor TI - Late Pleistocene variations of the background aeolian dust concentration in the Carpathian Basin: An estimate using decomposition of grain-size distribution curves of loess deposits JF - NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW J2 - NETH J GEOSCI VL - 91 PY - 2012 IS - 1-2 SP - 159 EP - 171 PG - 13 SN - 0016-7746 DO - 10.1017/S0016774600001566 UR - https://m2.mtmt.hu/api/publication/2104731 ID - 2104731 N1 - Megjegyzés-23636471 : Gyorgy/F-1039-2012 Geographical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaòrsi út 45, H-1112 Budapest Hungary, Hungary Department of Geology, University of Pees, Ifjúság u. 6, H-7624 Pecs, Hungary Institute of Applied Geology, BOKU, Peter Jordan Str. 70, A-1190 Vienna, Austria Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Csatkai E. u. 6-8, H-9400 Sopron, Hungary Cited By :18 Export Date: 24 September 2019 Correspondence Address: Kovács, J.; Department of Geology, University of Pees, Ifjúság u. 6, H-7624 Pecs, Hungary; email: jones@gamma.ttk.pte.hu AB - Aeolian dust deposits can be considered as one of the most important archives of past climatic changes. Alternating loess and paleosol strata display variations of the dust load in the Pleistocene atmosphere. By using the observations of recent dust storms, we are able to employ Late Pleistocene stratigraphie datasets (with accurate chronological framework) and detailed granulometric data for making conclusions on the atmospheric dust load in the past. Age-depths models, created from the absolute age data and stratigraphie interpretation, allow us to calculate sedimentation rates and dust fluxes, while grain-size specifies the dry-deposition velocity, i.e. the atmospheric residence time of mineral particles. Thus, the dust concentration can be expressed as the quotient of the dust flux and gravitational settling velocity. Recent observations helped to clarify the mechanisms behind aeolian sedimentation and the physical background of this process has nowadays been well established. Based on these two, main contrasting sedimentary modes of dust transport and deposition can be recognised: the short suspension episodes of the coarse (silt and very fine sand) fraction and the long-range transport of a fine (clay and fine silt) component. Using parametric curve fitting the basic statistical properties of these two sediment populations can be revealed for Pleistocene aeolian dust deposits, as it has been done for loess in Hungary. As we do not have adequate information on the magnitude and frequency of the Pleistocene dust storms, conclusions could only be made on the magnitude of continuous background dust load. The dust concentration can be set in the range between 1100 and 2750 ug/m3. These values are mostly higher than modern dust concentrations, even in arid regions. Another interesting proxy of past atmospheric conditions could be the visibility, being proportional to the dust concentration. According to the known empirical dust concentration - visibility equations, its value is around 6.5 to 26 kilometres. 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 AU - Lócskai, T AU - Hupuczi, Júlia TI - Late Quaternary palaeoenvironment and palaeoclimate of the Lake Fehér (Fehér-tó) sequence at Kardoskút (South Hungary), based on preliminary mollusc records JF - CENTRAL EUROPEAN JOURNAL OF GEOSCIENCES J2 - CENT EUR J GEOSCI VL - 3 PY - 2011 IS - 1 SP - 43 EP - 52 PG - 10 SN - 2081-9900 DO - 10.2478/s13533-011-0007-5 UR - https://m2.mtmt.hu/api/publication/1951396 ID - 1951396 N1 - Funding Agency and Grant Number: [TAMOP-4.2.1/B-09/1/KONV-2010-0005] Funding text: This project is currently funded by the research grant TAMOP-4.2.1/B-09/1/KONV-2010-0005. LA - English DB - MTMT ER - TY - JOUR AU - Újvári, Gábor AU - Kovács, János AU - Varga, György AU - Raucsik, Béla AU - Markovic, SB TI - Dust flux estimates for the Last Glacial Period in East Central Europe based on terrestrial records of loess deposits: a review JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 29 PY - 2010 IS - 23-24 SP - 3157 EP - 3166 PG - 10 SN - 0277-3791 DO - 10.1016/j.quascirev.2010.07.005 UR - https://m2.mtmt.hu/api/publication/1361069 ID - 1361069 N1 - Geodetic and Geophysical Research Institute of the Hungarian Academy of Sciences, Csatkai Endre u. 6-8., H-9400 Sopron, Hungary Department of Geology, University of Pécs, Ifjúság u. 6., H-7624 Pécs, Hungary Department of Earth and Environmental Sciences, University of Pannonia, Egyetem u. 10., H-8200 Veszprém, Hungary Department of Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, 21000 Novi Sad, Serbia Cited By :76 Export Date: 22 May 2022 CODEN: QSRED Correspondence Address: Újvári, G.; Geodetic and Geophysical Research Institute of the Hungarian Academy of Sciences, Csatkai Endre u. 6-8., H-9400 Sopron, Hungary; email: ujvari@ggki.hu LA - English DB - MTMT ER - TY - JOUR AU - Pazonyi, Piroska TI - A Kárpát-medence felső-pliocén és kvarter emlősfauna közösségeinek paleoökológiai vizsgálata. Palaeoecological investigations of upper pliocene and quaternary mammalian communities in the Carpathian Basin TS - Palaeoecological investigations of upper pliocene and quaternary mammalian communities in the Carpathian Basin JF - FÖLDTANI KÖZLÖNY J2 - FÖLDTANI KÖZLÖNY VL - 139 PY - 2009 IS - 3 SP - 283 EP - 304 PG - 22 SN - 0015-542X UR - https://m2.mtmt.hu/api/publication/1393294 ID - 1393294 N1 - idézve: p. 284. LA - Hungarian DB - MTMT ER - TY - JOUR AU - Pendea, I F AU - Gray, J T AU - Ghaleb, B AU - Tantau, I AU - Badarau, A S AU - Nicorici, C TI - Episodic build-up of alluvial fan deposits during the Weichselian Pleniglacial in the western Transylvanian Basin, Romania and their paleoenvironmental significance JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 198 PY - 2009 IS - 1-2 SP - 98 EP - 112 PG - 15 SN - 1040-6182 DO - 10.1016/j.quaint.2008.05.002 UR - https://m2.mtmt.hu/api/publication/27496836 ID - 27496836 N1 - Department of Geography, Babes-Bolyai University, Str. Clinicilor no. 5-7, 400006 Cluj-Napoca, Romania Department of Geography, University of Montréal, 520, Côte Sainte-Catherine, Outremont, Que. H2V 2B8, Canada Centre de recherche en géochimie et en géodynamique, GEOTOP, CP 8888, Succursale Centre-Ville Montreal, Que., H3C 3P8, Canada Department of Geology, Babes-Bolyai University, Str. Bilascu no. 44, 400015 Cluj-Napoca, Romania Department of Environmental Sciences, Babes-Bolyai University, Piata Stefan cel Mare no. 4, 400192 Cluj-Napoca, Romania Cited By :11 Export Date: 29 May 2022 Correspondence Address: Pendea, I.F.; Department of Geography, Str. Clinicilor no. 5-7, 400006 Cluj-Napoca, Romania; email: ionel.pendea@mail.mcgill.ca 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 - Gábris, Gyula AU - Nádor, Annamária TI - Long-term fluvial archives in Hungary: response of the Danube and Tisza rivers to tectonic movements and climatic changes during the Quaternary: a review and new synthesis JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 26 PY - 2007 IS - 22-24 SP - 2758 EP - 2782 PG - 25 SN - 0277-3791 DO - 10.1016/j.quascirev.2007.06.030 UR - https://m2.mtmt.hu/api/publication/1135543 ID - 1135543 AB - The paper discusses the Quaternary evolution of the Danube and Tisza rivers and their main tributaries in the context of evolution of the entire Pannonian Basin, which is Europe's largest intramontane basin, within the Alp-Carpathian orogen. The palaeo-drainage reconstruction of the Pannonian Basin for the pre-Quaternary period is Outlined in connection with the gradual regression of Lake Pannon since the Late Miocene. Deltas of rivers that entered the basin from the northwest and northeast were gradually transformed into extended alluvial plains; thus, the earliest possible ancestor of the Danube coming southeastwards from the Alps could be as old as Late Miocene. By the Pliocene the whole Lake Parnnon was infilled. The former extensional basin formation was replaced by a compresional stress field, which resulted in an uplift of the marginal flanks and late-stage subsidence anomalies. The increasing relief led to the formation of the Quaternary drainage pattern. The actively subsiding young basins were filled by fluvial sediments, transported by the Danube and Tisza river systems from the uplifting mountains. Between the subsiding regions of the Little and Great Plains, the Danube has formed an antecedent valley with terrace staircases between the uplifting sections of the Transdanubian Range and the North Midmountains. The formation of the terraces is attributed to periodic climate changes during the Pleistocene combined with differences in the uplift rate. The paper gives a complex overview of the classical chronology of the six terraces based on various data sources: mostly dating of loess/paleosol sequences, travertines, aeolian sand, and tephra strata overlying the fluvial sediments, complemented by scattered vertebrate faunal data and archaeological evidence directly from the terrace sediments. The Quaternary drainage pattern evolution of the Great Plain, with a strong tectonic control, is discussed in detail. Rivers originating from the uplifting marginal areas were drawn towards the subsiding depressions which served as local base level. Changes in subsidence rates in space and time throughout the Quaternary resulted in the evolution of a complex drainage pattern. A special emphasis is placed on the Late Pleistocene-Holocene development of the Middle-Tisza region and the Koros basin, where the Berettyo-Koros Rivers form an eastern tributary system of the Tisza River. A comparative evaluation of these two areas is especially relevant, as they provide insights into large-scale Late Pleistocene avulsion of the Tisza River. OSL dating, complemented with inferred transport directions determined from heavy mineral analysis of fluvial sediments in the Koros basin, has revealed an ancient large meandering river system that can be identified with the palaeo-Tisza, which was flowing along a tectonically controlled depression during the Late Pleniglacial. Successions in the Middle Tisza region have allowed differentiation between the older channels of the palaeo-Bodrog River and the Sajo-Hernad alluvial fan and the younger meander belts of the new course of the Tisza. In the Tisza system, changes in river style (braided to various scales of meandering) show correspondence to millennial-scale climate changes of the last 25 ka, while in the Koros basin the effects of tectonics are overprinted onto the regional climatic signals. (c) 2007 Elsevier Ltd. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Nádor, Annamária AU - Thamóné Bozsó, Edit AU - Magyari, A AU - Babinszki, Edit TI - Fluvial responses to tectonics and climate change during the Late Weichselian in the eastern part of the Pannonian Basin (Hungary) JF - SEDIMENTARY GEOLOGY J2 - SEDIMENT GEOL VL - 202 PY - 2007 IS - 1-2 SP - 174 EP - 192 PG - 19 SN - 0037-0738 DO - 10.1016/j.sedgeo.2007.03.001 UR - https://m2.mtmt.hu/api/publication/1333818 ID - 1333818 AB - Fine-grained sandy-silty channel-belt and floodplain deposits of the Berettyo-Koros Rivers, a main eastern transverse tributary system of the modem Tisza River in the eastern part of the Pannonian Basin, were deposited during the Late Pleistocene under net subsiding conditions. The palaeo-drainage network pattern of a 2500 km 2 large part of the alluvial plain was reconstructed based on interpretation of airborne photographs and analysis of 18th century topographic maps, which show the natural river patterns that predate the introduction of river regulation schemes. The investigation showed that a large meandering river system, with two main channel belts surrounding a floodbasin, entered the alluvial plain from the northeast, and a braided river entered the alluvial plain from the southeast. Detailed sedimentary logs of seven continuous corings and several sand and clay-pit sections were used to characterize different alluvial units. Optical luminescence dating (OSL) of 25 quartz samples and four C-14 datings showed that the sediments are of Late Pleniglacial to Late Glacial age. Transport directions inferred from heavy mineral analyses combined with the OSL ages strongly suggest that the large meandering system represents the palaeo-Tisza River, which supposedly flowed along the northeast-southwest striking Ermellek depression during the Late Pleniglacial. The braided river can be regarded as a precursor to the Fekete and Feher-Koros Rivers, which entered the alluvial plain from the southeast during the Late Glacial. The interpretation of seismic profiles, field measurements of neotectonic activity, and variations in thickness of sediments along the studied profile revealed that river development was largely controlled by subsidence along the Ermellek depression until 14 to 16 ky, and by uplift of the southeastern part of the catchment area. The studied fluvial successions also document the response of the palaeo-Tisza and Koros system to the climate changes of the Weichselian Late Pleniglacial-Late Glacial period. Much of the sand from the meandering zones was deposited during the Bolling-Allerod and Sagvar-Lascaux interstadials, whereas some dated sand units from the braided zone represent the Older and Younger Dryas. The error ranges of OSL dates, which often exceed the duration of Weichselian substages and subdivisions, prevented an unambiguous correlation of the studied sections with the millennial-scale climate changes of the last 25 ky. Meandering and braided river activity coexisted under different climate conditions, whereas locations of the main channel belts are related to subsidence anomalies. The results of A our study thus clearly indicate that tectonics was the primary control on river development. (c) 2007 Elsevier B.V. All rights reserved. LA - English DB - MTMT ER - TY - JOUR AU - Sólymos, Péter AU - Fehér, Zoltán TI - Conservation prioritization based on distribution of land snails in Hungary JF - CONSERVATION BIOLOGY J2 - CONSERV BIOL VL - 19 PY - 2005 SP - 1084 EP - 1094 PG - 11 SN - 0888-8892 DO - 10.1111/j.1523-1739.2005.00193.x UR - https://m2.mtmt.hu/api/publication/1070503 ID - 1070503 LA - English DB - MTMT ER - TY - CHAP AU - Sudár Sándorné Svingor, Éva AU - Molnár, Mihály AU - Szántó, Andrea Zsuzsanna TI - Appendix I: Radiocarbon data from Upper Paleolithic sites and Late Quaternary paleoecological sites in Hungary T2 - Loess and Upper Paleolithic environment in Hungary PB - Aurea Kiadó CY - Nagykovácsi SN - 963218212X PY - 2005 SP - 295 UR - https://m2.mtmt.hu/api/publication/149557 ID - 149557 N1 - [P19179 ATKI2005/0030] Megjegyzés-10226583 [H30672->P08540ATKI2005/0004] 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 - Viczián, I TI - Clay mineralogy of Quaternary sediments covering mountainous and hilly areas of Hungary JF - ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES J2 - ACTA GEOL HUNG VL - 45 PY - 2002 IS - 3 SP - 265 EP - 286 PG - 22 SN - 0236-5278 DO - 10.1556/AGeol.45.2002.3.5 UR - https://m2.mtmt.hu/api/publication/10291454 ID - 10291454 N1 - Cited By :9 Export Date: 29 May 2022 Correspondence Address: Viczián, I.; Geological Institute of Hungary, Stefánia út 14, Budapest H-1143, Hungary; email: viczian@mafi.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 - 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 -