TY - JOUR AU - Lehmkuhl, F AU - Nett, J AU - Pötter, S AU - Schulte, P AU - Sprafke, T AU - Jary, Z AU - Antoine, P AU - Wacha, L AU - Wolf, D AU - Zerboni, A AU - Hošek, J AU - Slobodan, Marković AU - Obreht, I AU - Sümegi, Pál AU - Veres, D AU - Zeeden, C AU - Boemke, B AU - Schaubert, V AU - Viehweger, J AU - Hambach, U TI - Loess landscapes of Europe – Mapping, geomorphology, and zonal differentiation JF - EARTH-SCIENCE REVIEWS J2 - EARTH-SCI REV VL - 215 PY - 2021 PG - 82 SN - 0012-8252 DO - 10.1016/j.earscirev.2020.103496 UR - https://m2.mtmt.hu/api/publication/31826687 ID - 31826687 N1 - Funding Agency and Grant Number: Deutsche Forschungsgemeinschaft (DFG, German Research Foundation)German Research Foundation (DFG) [57444011 - SFB 806] Funding text: The investigations were carried out in the frame of the 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", funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) - Projektnummer57444011 - SFB 806). We thank D. Haase for sharing shapefiles of the loess distribution map, P. Bertran for providing the shapefiles of the distribution of aeolian sediments modeled by his team, P. Ludwig for providing the data of the LGM regional dust model, and A. Weber for help with compiling the supplementary material. We thank G. Ujv ' ari and two anonymous reviewers for their suggestions that helped to improve the manuscript. LA - English DB - MTMT ER - TY - JOUR AU - Molnár, Dávid AU - Sümegi, Pál AU - Makó, László AU - Cseh, Péter AU - Zeeden, C AU - Nett, J AU - Lehmkuhl, F AU - Törőcsik, Tünde AU - Sümegi, BP. TI - Palaeoecological background of the Upper Palaeolithic site of Ságvár, Hungary: radiocarbon‐dated malacological and sedimentological studies on the Late Pleistocene environment JF - JOURNAL OF QUATERNARY SCIENCE J2 - J QUATERNARY SCI VL - 36 PY - 2021 IS - 8. szám Spec. Iss. SP - 1353 EP - 1363 PG - 11 SN - 0267-8179 DO - 10.1002/jqs.3306 UR - https://m2.mtmt.hu/api/publication/32017843 ID - 32017843 N1 - Funding Agency and Grant Number: Hungarian Human Resource Development Operational Programme [EFOP-3.6.1-16-2016-00008]; Ministry of Human Capacities, Hungary [20391-3/2018/FEKUSTRAT]; European Regional Development Fund [GINOP-2.3.2-15-2016- 00009] Funding text: This research was supported by the Hungarian Human Resource Development Operational Programme under project code: EFOP-3.6.1-16-2016-00008, Ministry of Human Capacities, Hungary grant 20391-3/2018/FEKUSTRAT, European Regional Development Fund grant GINOP-2.3.2-15-2016- 00009 'ICER'. 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 - Kovács, János AU - Újvári, Gábor AU - Varga, György AU - Seelos, K AU - Szabó, Péter AU - Dezső, József AU - Gammoudi, Nadia TI - Plio-Pleistocene dust traps on paleokarst surfaces: a case study from the Carpathian Basin JF - FRONTIERS IN EARTH SCIENCE J2 - FRONT EARTH SC-SWITZ VL - 8 PY - 2020 PG - 10 SN - 2296-6463 DO - 10.3389/feart.2020.00189 UR - https://m2.mtmt.hu/api/publication/31342357 ID - 31342357 N1 - Cited By :1 Export Date: 6 April 2021 Correspondence Address: Kovács, J.; Department of Geology and Meteorology, Hungary; email: jones@gamma.ttk.pte.hu Correspondence Address: Kovács, J.; Environmental Analytical and Geoanalytical Research Group, Hungary; email: jones@gamma.ttk.pte.hu AB - Plio-Pleistocene silt/clay-rich deposits and paleo-karst fissure sediments from sites of the northern and southern parts of the Carpathian Basin were investigated. These materials were supposed to be mixed during transport before being captured in karstified fissures. Evidence that the eolian fissure sediments of Plio-Pleistocene age in the older Triassic-Cretaceous limestones are derived from eolian silt and clay includes compositional and textural matches, especially decreasing grain-size trends observed downwards from the paleo-surface of the former landscape. Various environmental factors could be recognized by the statistical evaluation of grain-size distribution curves of fissure fillings sediments, such as the effects of eolian transport, parent rock type, weathering, and other sediment transport processes. Grain-size distribution curves with a single maximum in the silt size range are typical for the overlying siltstone debris, for the redeposited loess and red paleosol underlying the loess. Red clay fissure fillings yield bimodal grain-size distribution curves with maxima both in the clay and silt fractions. The research reported in this paper identifies for the first time the presence of eolian deposits in karst fissures of the Carpathian Basin and investigates the characteristics and origin. LA - English DB - MTMT ER - TY - JOUR AU - Stevens, T AU - Sechi, D AU - Bradák, Balázs AU - Orbe, R AU - Baykal, Y AU - Cossu, G AU - Tziavaras, C AU - Andreucci, S AU - Pascucci, V TI - Abrupt last glacial dust fall over southeast England associated with dynamics of the British-Irish ice sheet JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 250 PY - 2020 SN - 0277-3791 DO - 10.1016/j.quascirev.2020.106641 UR - https://m2.mtmt.hu/api/publication/31647185 ID - 31647185 LA - English DB - MTMT ER - TY - JOUR AU - Szeberényi, József AU - Kovács, József AU - Bradák, Balázs AU - Barta, Gabriella AU - Csonka, Diána AU - Medveďová, A. AU - Rostinsky, P. AU - Kiss, Klaudia AU - Varga, György TI - Experiencing new perspectives in the application of reflectance spectroscopy in loess research JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 552 PY - 2020 SP - 36 EP - 49 PG - 14 SN - 1040-6182 DO - 10.1016/j.quaint.2019.09.035 UR - https://m2.mtmt.hu/api/publication/30819668 ID - 30819668 N1 - Geographical Institute, Research Centre for Astronomy and Earth Sciences, Budaörsi út 45, Budapest, H-1112, Hungary Department of Physical and Applied Geology, Eötvös Loránd University, Pázmány Péter sétány 1/C, Budapest, H-1117, Hungary Research Center for Inland Seas, Kobe University, Nada, Kobe, 657-8501, Japan Department of Physics, University of Burgos, Av. De Cantabria, s/n, Burgos, 09006, Spain Department of Physical Geography, Eötvös Loránd University, Pázmány Péter sétány 1/C, Budapest, H-1117, Hungary University of Matej Bel Faculty of Natural Science, Tajovského 40, Banská Bystrica, 974 01, Slovakia Institute of Geonics AS CR, v.v.i., Ostrava-Poruba, Studentska 1768708 00, Czech Republic Cited By :2 Export Date: 26 October 2020 Correspondence Address: Szeberényi, J.; Geographical Institute, Research Centre for Astronomy and Earth Sciences, Budaörsi út 45, Hungary; email: szeberenyi.jozsef@csfk.mta.hu LA - English DB - MTMT ER - TY - JOUR AU - Wilczyński, J AU - Žaár, O AU - Nemergut, A AU - Kufel-Diakowska, B AU - Hoyo, MM AU - Morczek, P AU - Páll-Gergely, Barna AU - Oberc, T AU - Lengyel, György TI - The Upper Palaeolithic at Trenčianske Bohuslavice, Western Carpathians, Slovakia JF - JOURNAL OF FIELD ARCHAEOLOGY J2 - J FIELD ARCHAEOL VL - 45 PY - 2020 IS - 4 SP - 270 EP - 292 PG - 23 SN - 0093-4690 DO - 10.1080/00934690.2020.1733334 UR - https://m2.mtmt.hu/api/publication/31229840 ID - 31229840 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 - Újvári, Gábor AU - Kele, Sándor AU - Bernasconi, SM AU - Haszpra, László AU - Novothny, Ágnes AU - Bradák, Balázs TI - Clumped isotope paleotemperatures from MIS 5 soil carbonates in southern Hungary JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 518 PY - 2019 SP - 72 EP - 81 PG - 10 SN - 0031-0182 DO - 10.1016/j.palaeo.2019.01.002 UR - https://m2.mtmt.hu/api/publication/30399128 ID - 30399128 N1 - Funding Agency and Grant Number: National Research Development and Innovation Office in Hungary (NKFI Alap) [KH-125584]; Bolyai Janos Research Scholarship of the Hungarian Academy of Sciences; European Union; State of Hungary; European Regional Development Fund [GINOP-2.3.2-15-2016-00009] Funding text: This work was funded by the National Research Development and Innovation Office in Hungary (NKFI Alap KH-125584 project). Additional financial support provided by the Bolyai Janos Research Scholarship of the Hungarian Academy of Sciences (to GU) is gratefully acknowledged. The research was supported by the European Union and the State of Hungary, co-financed by the European Regional Development Fund in the project of GINOP-2.3.2-15-2016-00009 'ICER'. Constructive and insightful comments made by two anonymous reviewers greatly improved the paper. Export Date: 25 November 2019 CODEN: PPPYA Correspondence Address: Újvári, G.; Department of Lithospheric Research, University of Vienna, Althantrsasse 14 (UZA II), Austria; email: ujvari.gabor@csfk.mta.hu Cited By :3 Export Date: 25 October 2020 CODEN: PPPYA Correspondence Address: Újvári, G.; Department of Lithospheric Research, University of Vienna, Althantrsasse 14 (UZA II), Austria; email: ujvari.gabor@csfk.mta.hu Funding Agency and Grant Number: National Research Development and Innovation Office in Hungary (NKFI Alap) [KH-125584]; Bolyai Janos Research Scholarship of the Hungarian Academy of SciencesHungarian Academy of Sciences; European UnionEuropean Union (EU); State of Hungary; European Regional Development FundEuropean Union (EU) [GINOP-2.3.2-15-2016-00009] Funding text: This work was funded by the National Research Development and Innovation Office in Hungary (NKFI Alap KH-125584 project). Additional financial support provided by the Bolyai Janos Research Scholarship of the Hungarian Academy of Sciences (to GU) is gratefully acknowledged. The research was supported by the European Union and the State of Hungary, co-financed by the European Regional Development Fund in the project of GINOP-2.3.2-15-2016-00009 'ICER'. Constructive and insightful comments made by two anonymous reviewers greatly improved the paper. Cited By :5 Export Date: 16 February 2021 CODEN: PPPYA Correspondence Address: Újvári, G.; Department of Lithospheric Research, Althantrsasse 14 (UZA II), Austria; email: ujvari.gabor@csfk.mta.hu Funding details: European Commission, EC Funding details: Magyar Tudományos Akadémia, MTA Funding details: National Kidney Foundation of Iowa, NKFI Funding details: European Regional Development Fund, FEDER, GINOP-2.3.2-15-2016-00009 Funding text 1: This work was funded by the National Research Development and Innovation Office in Hungary ( NKFI Alap KH-125584 project). Additional financial support provided by the Bolyai János Research Scholarship of the Hungarian Academy of Sciences (to GÚ) is gratefully acknowledged. The research was supported by the European Union and the State of Hungary , co-financed by the European Regional Development Fund in the project of GINOP-2.3.2-15-2016-00009 ‘ICER’. Constructive and insightful comments made by two anonymous reviewers greatly improved the paper. 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 - Marković, SB AU - Stevens, T AU - Mason, J AU - Vandenberghe, J AU - Yang, S AU - Veres, D AU - Újvári, Gábor AU - Timar-Gabor, A AU - Zeeden, C AU - Guo, Z AU - Hao, Q AU - Obreht, I AU - Hambach, U AU - Wu, H AU - Gavrilov, MB AU - Rolf, C AU - Tomić, N AU - Lehmkuhl, F TI - Loess correlations – Between myth and reality JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 509 PY - 2018 SP - 4 EP - 23 PG - 20 SN - 0031-0182 DO - 10.1016/j.palaeo.2018.04.018 UR - https://m2.mtmt.hu/api/publication/3365644 ID - 3365644 AB - Abstract The correlation of loess sequences across global, hemispheric, regional and local scales is one of the most fundamental aspects to loess research. However, despite recent progress in stratigraphic and chronometric methods, the correlation of many loess sequences is often still based on untested assumptions over loess deposition, preservation, soil type and age. As such, the aim of this overview is to provide an adequate framework for evaluation of the accuracy of loess correlations applied on different temporal and spatial scales across Eurasia. This opens up possibilities for detailed temporal and spatial environmental reconstructions across the huge loess provinces of the Eurasia and provides a framework for future extension of this to North America. Additionally, we evaluate the potential development of appropriate sub-millennial scale loess correlations, as well as essentially important chronological approaches for establishing valid correlations between different loess records, such as current improvements in tephrochronology, 14C and luminescence dating techniques. LA - English DB - MTMT ER - TY - JOUR AU - Slobodan, B Marković AU - Sümegi, Pál AU - Thomas, Stevens AU - Randall, J Schaetzl AU - Igor, Obreht6 AU - Wei, Chu AU - Björn, Buggle AU - Michael, Zech AU - Roland, Zech AU - Christian, Zeeden AU - Milivoj, B Gavrilov AU - Zoran, Perić AU - Zorica, Svirčev AU - Frank, Lehmkuhl TI - The Crvenka loess-paleosol sequence. a record of continuous grassland domination in the southern Carpathian Basin during the Late Pleistocene TS - a record of continuous grassland domination in the southern Carpathian Basin during the Late Pleistocene JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 509 PY - 2018 SP - 33 EP - 46 PG - 14 SN - 0031-0182 DO - 10.1016/j.palaeo.2018.03.019 UR - https://m2.mtmt.hu/api/publication/3379923 ID - 3379923 N1 - Funding Agency and Grant Number: Serbian Ministry of Education and Science [176020]; Serbian Academy of Sciences and Arts [F-178]; Collaborative Research Center (CRC) 806 grant of the German Research Foundation (DFG); [GINOP-2.3.2-15-2016-00009] Funding text: This research was financially supported by Project 176020 of the Serbian Ministry of Education and Science and grant F-178 of Serbian Academy of Sciences and Arts. F.L., C.Z., W.C., and I.O. acknowledge the financial support from a grant the Collaborative Research Center (CRC) 806 grant of the German Research Foundation (DFG). The malacological research of P.S. was supported by the GINOP-2.3.2-15-2016-00009. We thank to Stevan Savic, Djordjije Vasiljevic, Mladjen Jovanovic, Biljana Basarin and Nemanja Basarin for their help during the laboratory and fieldwork. LA - English DB - MTMT ER - TY - JOUR AU - Nykamp, M AU - Knitter, D AU - Timár, Gábor AU - Krause, J AU - Heeb, B S AU - Szentmiklosi, A AU - Schütt, B TI - Estimation of wind-driven soil erosion of a loess-like sediment and its implications for the occurrence of archaeological surface and subsurface finds. An example from the environs of Corneşti-Iarcuri, western Romania TS - An example from the environs of Corneşti-Iarcuri, western Romania JF - JOURNAL OF ARCHAEOLOGICAL SCIENCE: REPORTS J2 - J ARCHAEOL SCI REP VL - 12 PY - 2017 SP - 601 EP - 612 PG - 12 SN - 2352-409X DO - 10.1016/j.jasrep.2017.03.030 UR - https://m2.mtmt.hu/api/publication/3201895 ID - 3201895 LA - English DB - MTMT ER - TY - JOUR AU - Újvári, Gábor AU - Stevens, T AU - Molnár, Mihály AU - Demény, Attila AU - Fabrice, L AU - Varga, György AU - Jull, Timothy AJ AU - Páll-Gergely, Barna AU - Buylaert, JP AU - Kovács, János TI - Coupled European and Greenland last glacial dust activity driven by North Atlantic climate JF - PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA J2 - P NATL ACAD SCI USA VL - 114 PY - 2017 IS - 50 SP - E10632 EP - E10638 PG - 7 SN - 0027-8424 DO - 10.1073/pnas.1712651114 UR - https://m2.mtmt.hu/api/publication/3296802 ID - 3296802 N1 - Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budapest, H-1112, Hungary Center for Nuclear Technologies, Technical University of Denmark, Roskilde, 4000, Denmark Department of Earth Sciences, Uppsala University, Uppsala, 75236, Sweden Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Hungarian Academy of Sciences, Debrecen, H-4026, Hungary Geography Institute, Pontificia Universidad Católica de Chile, Santiago, 7810000, Chile Geographical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budapest, H-1112, Hungary Department of Geosciences, University of Arizona, Tucson, AZ 85721, United States University of Arizona Accelerator Mass Spectrometry Facility, University of Arizona, Tucson, AZ 85721, United States Plant Protection Institute, Centre for Agricultural Research, Hungarian Academy of Sciences, Budapest, H-1022, Hungary Nordic Laboratory for Luminescence Dating, Department of Geoscience, University of Aarhus, Roskilde, 4000, Denmark Department of Geology and Meteorology, University of Pécs, Pécs, H-7624, Hungary Environmental Analytical and Geoanalytical Research Group, Szentágothai Research Centre, Pécs, H-7624, Hungary Cited By :10 Export Date: 24 September 2019 CODEN: PNASA Correspondence Address: Újvári, G.; Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of SciencesHungary; email: ujvari.gabor@csfk.mta.hu Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budapest, H-1112, Hungary Center for Nuclear Technologies, Technical University of Denmark, Roskilde, 4000, Denmark Department of Earth Sciences, Uppsala University, Uppsala, 75236, Sweden Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Hungarian Academy of Sciences, Debrecen, H-4026, Hungary Geography Institute, Pontificia Universidad Católica de Chile, Santiago, 7810000, Chile Geographical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budapest, H-1112, Hungary Department of Geosciences, University of Arizona, Tucson, AZ 85721, United States University of Arizona Accelerator Mass Spectrometry Facility, University of Arizona, Tucson, AZ 85721, United States Plant Protection Institute, Centre for Agricultural Research, Hungarian Academy of Sciences, Budapest, H-1022, Hungary Nordic Laboratory for Luminescence Dating, Department of Geoscience, University of Aarhus, Roskilde, 4000, Denmark Department of Geology and Meteorology, University of Pécs, Pécs, H-7624, Hungary Environmental Analytical and Geoanalytical Research Group, Szentágothai Research Centre, Pécs, H-7624, Hungary Export Date: 22 February 2021 CODEN: PNASA Correspondence Address: Újvári, G.; Institute for Geological and Geochemical Research, Hungary; email: ujvari.gabor@csfk.mta.hu LA - English DB - MTMT ER - TY - JOUR AU - Újvári, Gábor AU - Kok, J F AU - Varga, György AU - Kovács, János TI - The physics of wind-blown loess: Implications for grain size proxy interpretations in Quaternary paleoclimate studies JF - EARTH-SCIENCE REVIEWS J2 - EARTH-SCI REV VL - 154 PY - 2016 SP - 247 EP - 278 PG - 32 SN - 0012-8252 DO - 10.1016/j.earscirev.2016.01.006 UR - https://m2.mtmt.hu/api/publication/3011427 ID - 3011427 N1 - Funding Agency and Grant Number: Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [OTKA PD-108639]; Bolyai Janos Research Scholarship of the Hungarian Academy of SciencesHungarian Academy of Sciences [BO/00326/15/10]; Directorate For GeosciencesNational Science Foundation (NSF)NSF - Directorate for Geosciences (GEO) [1358621] Funding Source: National Science Foundation; Div Atmospheric & Geospace SciencesNational Science Foundation (NSF)NSF - Directorate for Geosciences (GEO) [1358621] Funding Source: National Science Foundation Funding text: This work has been funded by a post doc project from the Hungarian Scientific Research Fund to GU (OTKA PD-108639). Additional financial support provided by the Bolyai Janos Research Scholarship of the Hungarian Academy of Sciences (BO/00326/15/10) (GU, GV) is gratefully acknowledged. Constructive and insightful comments by Joe Mason and Thomas Stevens improved this paper substantially. Editorial handling and comments by Ian Candy is appreciated. Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi u. 45., Budapest, H-1112, Hungary Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Acaemy of Sciences, Csatkai E. u. 6-8., Sopron, H-9400, Hungary Department of Atmospheric and Oceanic Sciences, University of California, 405 Hilgard Ave, Los Angeles, CA 90095, United States Geographical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi út 45., Budapest, H-1112, Hungary Department of Geology and Meteorology, University of Pécs, Ifjúság u. 6., Pécs, H-7624, Hungary Environmental Analytical and Geoanalytical Laboratory, Szentágothai Research Centre, University of Pécs, Ifjúság u. 20., Pécs, H-7624, Hungary Cited By :87 Export Date: 16 February 2021 Correspondence Address: Újvári, G.; Institute for Geological and Geochemical Research, Budaörsi u. 45., Hungary; email: ujvari.gabor@csfk.mta.hu Funding details: Magyar Tudományos Akadémia, MTA, BO/00326/15/10 ) Funding details: Hungarian Scientific Research Fund, OTKA Funding details: Hungarian Scientific Research Fund, OTKA, PD-108639 Funding text 1: This work has been funded by a post doc project from the Hungarian Scientific Research Fund to GÚ ( OTKA PD-108639 ). Additional financial support provided by the Bolyai János Research Scholarship of the Hungarian Academy of Sciences ( BO/00326/15/10 ) (GÚ, GV) is gratefully acknowledged. Constructive and insightful comments by Joe Mason and Thomas Stevens improved this paper substantially. Editorial handling and comments by Ian Candy is appreciated. AB - Loess deposits are recorders of aeolian activity during past glaciations. Since the size distribution of loess deposits depends on distance to the dust source, and environmental conditions at the source, during transport, and at deposition, loess particle size distributions and derived statistical measures are widely used proxies in Quaternary paleoenvironmental studies. However, the interpretation of these proxies often only considers dust transport processes. To move beyond such overly simplistic proxy interpretations, and toward proxy interpretations that consider the range of environmental processes that determine loess particle size distribution variations we provide a comprehensive review on the physics of dust particle mobilization and deposition. Furthermore, using high-resolution bulk loess and quartz grain size datasets from a last glacial/interglacial sequence, we show that, because grain size distributions are affected by multiple, often stochastic processes, changes in these distributions over time allow multiple interpretations for the driving processes. Consequently, simplistic interpretations of proxy variations in terms of only one factor (e.g. wind speed) are likely to be inaccurate. Nonetheless using loess proxies to understand temporal changes in the dust cycle and environmental parameters requires (i) a careful site selection, to minimize the effects of topography and source distance, and (ii) the joint use of bulk and quartz grain size proxies, together with high resolution mass accumulation rate calculations if possible. © 2016 Elsevier B.V. LA - English DB - MTMT ER - TY - JOUR AU - Marković, SB AU - Stevens, T AU - Kukla, GJ AU - Hambach, U AU - Fitzsimmons, KE AU - Gibbard, P AU - Buggle, B AU - Zech, M AU - Guo, Z AU - Hao, Q AU - Wu, H AU - O'Hara, Dhand K AU - Smalley, IJ AU - Újvári, Gábor AU - Sümegi, Pál AU - Timar-Gabor, A AU - Veres, D AU - Sirocko, F AU - Vasiljević, DA AU - Jary, Z AU - Svensson, A AU - Jović, V AU - Lehmkuhl, F AU - Kovács, János AU - Svirčev, Z TI - Danube loess stratigraphy - Towards a pan-European loess stratigraphic model JF - EARTH-SCIENCE REVIEWS J2 - EARTH-SCI REV VL - 148 PY - 2015 SP - 228 EP - 258 PG - 31 SN - 0012-8252 DO - 10.1016/j.earscirev.2015.06.005 UR - https://m2.mtmt.hu/api/publication/2920426 ID - 2920426 N1 - Laboratory for Palaeoenvironmental Reconstruction, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 2, Novi Sad, 21000, Serbia Department of Earth Sciences, Uppsala University, Villavägen 16, Uppsala, 75236, Sweden Lamont-Doherty Earth Observatory of Columbia University, Rt. 9W, Palisades, NY 10964, United States BayCEER and Chair of Geomorphology, University of Bayreuth, Bayreuth, D-95440, Germany Department of Human Evolution, Max Planck Institute for Evolutionary Anthropology, Deutscher Platz 6, Leipzig, D-04103, Germany Cambridge Quaternary, Department of Geography, University of Cambridge, Downing Place, Cambridge, England, CB2 3EN, United Kingdom Geological Institute, ETH Zürich, Sonneggstr. 5, Zürich, 8092, Switzerland Soil Physics Department, University of Bayreuth, Bayreuth, D-95440, Germany Key laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 10029, China Giotto Loess Research Group, Geography Department, Leicester University, Leicester, LE1 7RH, United Kingdom Geodetic and Geophysical Research Institute of the Hungarian Academy of Sciences, Csatkai Endre u. 6-8., Sopron, H-9400, Hungary Department of Geology and Palaeontology, University of Szeged, Egyetem u. 2-6, Szeged, H-6722, Hungary Faculty of Environmental Science, Babes-Bolyai University, Fantanele, 30, Cluj Napoca, 400294, Romania Romanian Academy, Institute of Speleology, Clinicilor 5, Cluj-Napoca, 400006, Romania Institute of GeoSciences, University of Mainz, J.-J. Becher-Weg 21, Mainz, D-55128, Germany Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 2, Novi Sad, 21000, Serbia Institute of Geography and Regional Development, University of Wrocław, Pl. Uniwersytecki 1, Wrocław, 50-137, Poland Ice and Climate Research, Niels Bohr Institute, University of Copenhagen, Juliane Maries Vej 30, Copenhagen, 2100, Denmark Serbian Academy of Sciences and Arts, Knez Mihajlova 35, Belgrade, 11000, Serbia Department of Geography, RWTH Aachen University, Wüllnertsr. 5b, Aachen, D-52056, Germany Department of Geology and Meteorology And Environmental Analytical and oGeoanalytical Research Group, Szentágothai Research Centre, University of Pecs, Hungary Cited By :193 Export Date: 25 May 2022 Correspondence Address: Marković, S.B.; Laboratory for Palaeoenvironmental Reconstruction, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 2, Serbia AB - The Danube River drainage basin is the second largest river catchment in Europe and contains a significant and extensive region of thick loess deposits that preserve a record of a wide variety of recent and past environments. Indeed, the Danube River and tributaries may themselves be responsible for the transportation of large volumes of silt that ultimately drive loess formation in the middle and lower reaches of this large catchment. However, this vast loess province lacks a unified stratigraphic scheme. European loess research started in the late 17th century in the Danube Basin with the work of Count Luigi Ferdinand Marsigli. Since that time numerous investigations provided the basis for the pioneering stratigraphic framework proposed initially by Kukla (1970, 1977) in his correlations of loess with deep-sea sediments. Loess-palaeosol sequences in the middle and lower reaches of the Danube River basin were a key part of this framework and contain some of the longest and most complete continental climate records in Europe, covering more than the last million years. However, the very size of the Danube loess belt and the large number of countries it covers presents a major limiting factor in developing a unified approach that enables continental scale analysis of the deposits. Local loess-palaeosol stratigraphic schemes have been defined separately in different countries and the difficulties in correlating such schemes, which often change significantly with advances in age-dating, have limited the number of basin-wide studies. A unified basin-wide stratigraphic model would greatly alleviate these difficulties and facilitate research into the wider significance of these loess records. Therefore we review the existing stratigraphic schemes and define a new Danube Basin wide loess stratigraphy based around a synthetic type section of the Mošorin and Stari Slankamen sites in Serbia. We present a detailed comparison with the sedimentological and palaeoclimatic records preserved in sediments of the Chinese Loess Plateau, with the oxygen isotope records from deep-sea sediments, and with classic European Pleistocene stratigraphic subdivisions. The hierarchy of Danubian stratigraphic units is determined by climatically controlled environmental shifts, in a similar way to the Chinese loess stratigraphic scheme. A new unified Danube loess stratigraphic model has a number of advantages, including preventing confusion resulting from the use of multiple national schemes, a more transparent basis, and the potential to set Pleistocene palaeoenvironmental changes recorded in the Danube catchment area into a global context. The use of a very simple labelling system based on the well-established Chinese loess scheme facilitates interpretation of palaeoenvironmental information reported from the Danube Basin loess sites in a wider more accessible context that can be readily correlated world-wide. This stratigraphic approach also provides, for the first time, an appropriate framework for the development of an integrated, pan-European and potentially pan-Eurasian loess stratigraphic scheme. © 2015 Elsevier B.V. LA - English DB - MTMT ER - TY - JOUR AU - Constantin, D AU - Begy, Róbert-Csaba AU - Vasiliniuc, S AU - Panaiotu, C AU - Necula, C AU - Codrea, V AU - Timar-Gabor, A TI - High-resolution OSL dating of the Costineşti section (Dobrogea, SE Romania) using fine and coarse quartz JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 334 PY - 2014 SP - 20 EP - 29 PG - 10 SN - 1040-6182 DO - 10.1016/j.quaint.2013.06.016 UR - https://m2.mtmt.hu/api/publication/2999019 ID - 2999019 AB - Previous studies on the application of optically stimulated luminescence dating on quartz extracted from Romanian loess yielded inconsistent age estimates between different grain sizes. The present work reports a high-resolution SAR-OSL chronology for the L1 (MIS 2-4), S1 (MIS 5) and L2 (MIS 6) units of the loess-palaeosol profile from Costineşti, that contains at least five loess-palaeosol alternations and is located on the Black Sea Shore (Dobrogea, SE Romania). Analysis were performed on fine (4-11μm) and coarse (63-90μm) quartz grains extracted from 25 samples collected at very high resolution (10-20cm). Luminescence investigations confirm the reliability of the SAR-OSL dating protocol previously applied to Romanian loess (preheat at 220°C for 10s, cutheat to 180°C and elevated temperature OSL (ETOSL). The dose-response curve is best described by the sum of two saturating exponential functions. The results confirm the different saturation characteristics of fine and coarse grains of quartz, as reported in previous studies on loess sections in SE Romania. The equivalent doses obtained for coarse grains are higher than those obtained for fine grains, for all samples. The fine quartz OSL age estimates are significantly younger than the coarse quartz age results, as in the case of previous studies on the Mircea-Vodǎ and Mostiştea loess sections. Coarse quartz in samples collected from the upper part of S1 yielded ages of 94±11ka, 116±11ka and 120±10ka that do not seem to underestimate the true burial age. The same observation applies to the upper part of L2. Overall, from the luminescence results it can be concluded that the S1 palaeosol formed during the MIS 5, and the discrepancy observed on coarse and fine quartz OSL ages is a general feature of SE Romanian loess. © 2013 Elsevier Ltd and INQUA. LA - English DB - MTMT ER - TY - JOUR AU - Markovic, S B AU - Korac, Miomir AU - Mrdic, Nemanja AU - Buylaert, Jan-Pieter AU - Thiel, Christine AU - McLaren, Sue J AU - Stevens, Thomas AU - Tomic, Nemanja AU - Petic, Nikola AU - Jovanovic, Mladjen AU - Vasiljevic, D A AU - Sümegi, Pál AU - Gavrilov, Milivoj B. AU - Obreht, Igor TI - Palaeoenvironment and geoconservation of mammoths from the Nosak loess-palaeosol sequence (Drmno, northeastern Serbia): Initial results and perspectives. JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 334-335 PY - 2014 SP - 30 EP - 39 PG - 10 SN - 1040-6182 DO - 10.1016/j.quaint.2013.05.047 UR - https://m2.mtmt.hu/api/publication/2798781 ID - 2798781 N1 - WoS:hiba:000338817800005 2020-08-29 09:16 kötet nem egyezik 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 - Újvári, Gábor AU - Raucsikné Varga, Andrea Beáta AU - Ramos, F C AU - Kovács, János AU - Németh, Tibor AU - Stevens, T TI - Evaluating the use of clay mineralogy, Sr-Nd isotopes and zircon U-Pb ages in tracking dust provenance: An example from loess of the Carpathian Basin JF - CHEMICAL GEOLOGY J2 - CHEM GEOL VL - 304-305 PY - 2012 SP - 83 EP - 96 PG - 14 SN - 0009-2541 DO - 10.1016/j.chemgeo.2012.02.007 UR - https://m2.mtmt.hu/api/publication/1934996 ID - 1934996 N1 - Megjegyzés-22375086 WC: Geochemistry & Geophysics LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Gulyás, Sándor AU - Persaits, Gergő AU - Páll, Dávid Gergely AU - Molnár, Dávid TI - The loess-paleosol sequence of Basaharc (Hungary) revisited: Mollusc-based paleoecological results for the Middle and Upper Pleistocene JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 240 PY - 2011 IS - 1-2 SP - 181 EP - 192 PG - 12 SN - 1040-6182 DO - 10.1016/j.quaint.2011.05.005 UR - https://m2.mtmt.hu/api/publication/1943041 ID - 1943041 AB - The present study discusses the findings of detailed stratigraphical, sedimentological, geochemical and paleoecological investigations implemented as part of a 1990 campaign to Pécsi's studied profile at Hungary's important Danubian loess profile at Basaharc. In older studies, there were major discrepancies between the old lithostratigraphic classifications and the numerical ages. According to the findings of this study, the Basaharc Double Paleosol Complex, described formerly from the lower brickyard as a stratotype of Middle Würmian, is an isochronous heterotype of the Mende Upper Paleosol Complex from Profile #1 due to reworking. However, the lower member of the Mende Upper Paleosol Complex must have formed not at the boundary of the Upper and Middle Würmian as originally presumed, but during the Riss-Würmian interglacial. Conversely, the upper member of this same complex developed during an interglacial between the Upper and Middle Würmian, implying the presence of a huge erosional hiatus between the two members of the paleosol complex. The genetics of the individual paleosol layers needs a re-evaluation as well. The majority of the soils formerly conceived to be of steppe and forest steppe origin developed among closed woodland conditions. © 2011 Elsevier Ltd and INQUA. 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 - 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 -