TY - JOUR AU - Galović, L AU - Šorša, A AU - Peh, Z TI - Modelling the paleopedological development of loess/palaeosol sections using discriminant function analysis of compositional geoscience data, case study in Eastern Croatia JF - JOURNAL OF GEOCHEMICAL EXPLORATION J2 - J GEOCHEM EXPLOR VL - 262 PY - 2024 SN - 0375-6742 DO - 10.1016/j.gexplo.2024.107473 UR - https://m2.mtmt.hu/api/publication/34802068 ID - 34802068 LA - English DB - MTMT ER - TY - JOUR AU - Kehl, M AU - Seeger, K AU - Pötter, S AU - Schulte, P AU - Klasen, N AU - Zickel, M AU - Pastoors, A AU - Claßen, E TI - Loess formation and chronology at the Palaeolithic key site Rheindahlen, Lower Rhine Embayment, Germany JF - EISZEITALTER UND GEGENWART / E&G QUATERNARY SCIENCE JOURNAL J2 - E G QUATERN SCI J VL - 73 PY - 2024 IS - 1 SP - 41 EP - 67 PG - 27 SN - 0424-7116 DO - 10.5194/egqsj-73-41-2024 UR - https://m2.mtmt.hu/api/publication/34611429 ID - 34611429 AB - Abstract. The loess–palaeosol sequence and intercalated Palaeolithic find layers at the former brickyard of Rheindahlen are matters of ongoing scientific dispute. The age of different palaeosols and loess layers, hence their correlation with the global climate cycles, and the timing of repeated Neanderthal occupations have been hotly debated. These disagreements should be solved because the exceptional sedimentary and Palaeolithic sequences at Rheindahlen provide a unique opportunity to study diachronic changes in Neanderthal behaviour within the context of past climate change. We thus revisited one of the key loess sections of the Rheindahlen site to improve our understanding of loess formation processes and provide a more reliable chronostratigraphic framework for the sequence. High-resolution grain size analyses and micromorphology show that the Erkelenz Soil and the Rheindahlen Soil are characterized by more strongly developed Bt horizons than the modern soil. While these soils represent interglacial phases, the lowermost palaeosol likely formed during an interstadial and has been overprinted by weak clay illuviation during the formation of the Rheindahlen Soil. Sedimentary features of prolonged frost characterize loess and palaeosols below the modern soil and give indirect evidence for a Holocene age of the uppermost part of the sequence. Our luminescence dating approach corroborates this correlation and adds several Last Glacial deposition ages for the upper metres of the sequence. Previous correlation of this part of the sedimentary sequence with the penultimate glacial is thus rejected, whereas placing the Middle Palaeolithic inventories A3, B1, and B2 into the Last Glacial is confirmed. Luminescence measurements for the parental loess of the Erkelenz Soil and for loess layers below did not provide reliable ages probably related to signal saturation. The age of this part of the sequence thus remains open, hence the timing of human occupation testified by Palaeolithic inventories B3, B4/5, C1, and D1. The new findings provide an improved base for stratigraphic correlation of the Rheindahlen loess sequence and for investigating diachronic change in Neanderthal behaviour against the background of past climate change. LA - English DB - MTMT ER - TY - JOUR AU - Marković, SB AU - Hughes, PD AU - Schaetzl, R AU - Gibbard, PL AU - Hao, Q AU - Radaković, MG AU - Vandenberghe, J AU - Obreht, I AU - Sipos, György AU - Laag, C AU - Gavrilov, MB AU - Antić, A AU - Marković, RS AU - Krsmanović, P AU - Fenn, K AU - Lukić, T AU - Perić, ZM TI - The relationship between the loess stratigraphy in the Vojvodina region of northern Serbia and the Saalian and Rissian Stage glaciations – a review JF - BOREAS J2 - BOREAS VL - In press PY - 2024 SN - 0300-9483 DO - 10.1111/bor.12646 UR - https://m2.mtmt.hu/api/publication/34557195 ID - 34557195 AB - The regional loess stratigraphy in the Vojvodina region, in the southeastern Carpathian Basin, has often been successfully correlated to the global palaeoclimate. This is a quasi-continuous sedimentary record that provides detailed environmental reconstruction during the last four glacial/interglacial cycles. In this study, we present a standardized loess stratigraphy and illustrate how it correlates with the marine oxygen isotope and Chinese loess stratigraphical records. We argue that the loess stratigraphy in Vojvodina region is an important link in the integration of European terrestrial stratigraphical schemes and the deep-sea stratigraphical model. We highlight how the loess record can better illustrate terrestrial environmental change through multiple glacial cycles than other records, such as glacial records. The investigated loess record enables direct links to be made between the loess sediments and their glacial sources. This reveals evidence of glaciations during every glacial cycle of the Saalian Stage complex, equivalent to Marine Isotope Stage (MIS) 10, 8 and 6. Therefore, Serbian loess has the potential to provide a direct link between terrestrial glaciations and wider records of global climate change, which is an enigma for many other continental records. These loess records display a strong relationship with the intensity of European glaciations during different glacial cycles. Loess sedimentation rates are highest in the most intensive European glaciation of the Saalian complex (MIS 6) and much lower during the weaker ?missing? glaciations equivalent to MIS 8 and 10. A key observation from the Vojvodina loess is the gradual increase in interglacial aridity through the late Middle Pleistocene. The explanation for the progressively increasing aridity in the investigated region at this time is still unclear. However, this trend is consistent with the idea of the Saalian complex as representing a 400?ka mega glacial cycle modulated by shorter classic 100?ka glacial cycles. LA - English DB - MTMT ER - TY - JOUR AU - Ponomareva, V AU - Portnyagin, M AU - Danišík, M AU - Konstantinov, E AU - Zelenin, E AU - Tkach, N AU - Hauff, F AU - Schmitt, A K AU - Friedrichs, B AU - Romanyuk, B AU - Guillong, M AU - Kirkland, C L AU - Rankenburg, K AU - Müller, S AU - Garbe-Schönberg, D TI - Distal tephras along the SE European margin date powerful explosive eruptions from the Elbrus volcanic center (Greater Caucasus) JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 300 PY - 2023 PG - 18 SN - 0277-3791 DO - 10.1016/j.quascirev.2022.107910 UR - https://m2.mtmt.hu/api/publication/33336800 ID - 33336800 LA - English DB - MTMT ER - TY - JOUR AU - Pötter, S AU - Seeger, K AU - Richter, C AU - Brill, D AU - Knaak, M AU - Lehmkuhl, F AU - Schulte, P TI - Pleniglacial dynamics in an oceanic central European loess landscape JF - EISZEITALTER UND GEGENWART / E&G QUATERNARY SCIENCE JOURNAL J2 - E G QUATERN SCI J VL - 72 PY - 2023 IS - 1 SP - 77 EP - 94 PG - 18 SN - 0424-7116 DO - 10.5194/egqsj-72-77-2023 UR - https://m2.mtmt.hu/api/publication/34047637 ID - 34047637 AB - Abstract. Loess–palaeosol sequences (LPSs) of the oceanic-influenced European loess belt underwent frequent post-depositional processes induced by surface runoff or periglacial processes. The interpretation of such atypical LPSs isnot straightforward, and they cannot be easily used for regional tocontinental correlations. Within the last few years, however, such sequencesgained increased attention, as they are valuable archives for regionallandscape dynamics. In this study, the Siersdorf LPS was analysed using amulti-proxy approach using sedimentological, geochemical, andspectrophotometric methods combined with luminescence dating and tentativemalacological tests to unravel Pleniglacial dynamics of the Lower RhineEmbayment. A marshy wetland environment for the late Middle Pleniglacial tothe early Upper Pleniglacial was shown by colour reflectance and grain sizedistribution. Age inversions from luminescence dating paired withgeochemical and sedimentological data reveal long-lasting erosionalprocesses during the early Upper Pleniglacial, which were constrained to arelatively small catchment with short transport ranges. The upper sequenceshows typical marker horizons for the study area and indicate harsh,cold-arid conditions for the late Upper Pleniglacial. In comparison withother terrestrial archives, the Siersdorf LPS shows that the Lower RhineEmbayment was more diverse than previously assumed, regarding not only itsgeomorphological settings and related processes but also its ecosystems andenvironments. LA - English DB - MTMT ER - TY - JOUR AU - Püspöki, Zoltán AU - Gibbard, P.L. AU - Kiss, László Ferenc AU - McIntosh, Richard William AU - Thamó-Bozsó, E. AU - Krassay, Z. AU - Szappanos, B. AU - Maigut, V. AU - Kovács, Péter Gábor AU - Karácsony, Dominik Ádám AU - Stercel, F. AU - Visnovitz, Ferenc AU - Demény, K. AU - Bereczki, L. AU - Szőcs, T. AU - Rotár-Szalkai, Á. AU - Fancsik, Tamás TI - Obliquity-driven mountain permafrost-related fluvial magnetic susceptibility cycles in the Quaternary mid-latitude long-term (2.5 Ma) fluvial Maros Fan in the Pannonian Basin JF - BOREAS J2 - BOREAS VL - 52 PY - 2023 IS - 3 SP - 402 EP - 426 PG - 25 SN - 0300-9483 DO - 10.1111/bor.12618 UR - https://m2.mtmt.hu/api/publication/34001105 ID - 34001105 N1 - Supervisory Authority for Regulatory Affairs, Alkotás út 50, Budapest, H-1123, Hungary Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, CB2 1ER, United Kingdom Wigner Research Centre for Physics, Konkoly-Thege Miklós u. 29-33, Budapest, H-1121, Hungary Department of Mineralogy and Geology, University of Debrecen, Egyetem tér 1, Debrecen, H-4032, Hungary Németh László u. 2/C, Dunakeszi, H-2120, Hungary Petőfi Lutheran Grammar School of Aszód, Régész u. 34, Aszód, H-2170, Hungary Western Balkans Green Center, Naphegy tér 8, Budapest, H-1016, Hungary Faculty of Earth Science and Engineering, University of Miskolc, Egyetemváros, Miskolc, H-3515, Hungary István út 21. IV/36, Debrecen, H-4031, Hungary Department of Geophysics and Space Science, Eötvös Lóránd University, Pázmány Péter sétány 1/c, Budapest, H-1117, Hungary Middle-Danube-Valley Water Directorate, Rákóczi u. 41, Budapest, H-1088, Hungary Export Date: 7 July 2023 Correspondence Address: Gibbard, P.L.; Scott Polar Research Institute, Lensfield Road, United Kingdom; email: plg1@cam.ac.uk AB - Magnetic susceptibility (MS) of the Quaternary long-term mid-latitude Maros fluvial fan (Pannonian Basin) was recorded to understand the stratigraphical features of source-proximal fluvial depositional settings. Three fully cored 500-m-deep boreholes were sampled at 0.5-m intervals; low-field and frequency dependent MS were measured, and complementary hysteresis and SEM-EDAX investigationswere performed on selected samples. Logged susceptibility data were also used to log correlations established by a simultaneous comparison of wireline log and laboratory measurements. Time-series analyses of the susceptibility records reveal a ∼41-ka and ∼100-ka cyclicity. Towards the source-distal sections the intensity of the ∼41-ka cycles decreases, while that of the ∼100-ka cycles remains strong. Stratigraphical and spectral similarities were observed between the Maros fluvial fan and Chinese loess records; however, based on complementary magnetic data, the magnetic phase of the Maros Fan sections is related to the detrital magnetite that originates from the catchment during early postglacial permafrost degradations. The amplification of the ∼41-ka cycles can be attributed to the very high susceptibility values in source-proximal settings and to the special stratigraphical feature of the distributive fluvial systems. This comprises the increased avulsion frequency on the fluvial fans in ‘glacial recession periods’, in concert with the ‘early postglacial’ occurrence of the permafrost-related magnetite originating from the catchment. As a local phenomenon, this is significant since it records the obliquity-driven variations in permafrost development in a catchment. However, fluvial and alluvial fans are widespread depositional landforms within the Eurasian mountain range and were possibly the same during the Quaternary deglaciations. Thus, obliquity-driven magnetic susceptibility variations in source-proximal fan deposits attached or adjacent to regions of loess deposition should also be considered when scanning for potential source material of aeolian deposits. LA - English DB - MTMT ER - TY - JOUR AU - Adameková, K. AU - Petřík, J. TI - The myth of ‘Bohunician soil’: A re-evaluation of the MIS 3 palaeosol record at the Brno-Bohunice site (Czechia) JF - CATENA J2 - CATENA VL - 217 PY - 2022 SN - 0341-8162 DO - 10.1016/j.catena.2022.106510 UR - https://m2.mtmt.hu/api/publication/33034927 ID - 33034927 N1 - Export Date: 01 August 2022; CODEN: CIJPD LA - English DB - MTMT ER - TY - THES AU - Batchelor, CJ TI - Reconstructing High-Resolution Paleoclimate for Portions of the Last 250,000 Years from Cave of the Mounds Speleothems PB - The University of Wisconsin - Madison PY - 2022 SN - 9798790654107 UR - https://m2.mtmt.hu/api/publication/34461852 ID - 34461852 LA - English DB - MTMT ER - TY - JOUR AU - Chen, J AU - Stevens, T AU - Yang, T AU - Qiang, M AU - Matishov, G AU - Konstantinov, E AU - Kurbanov, R AU - Zeng, B AU - Shi, P TI - Revisiting Late Pleistocene Loess–Paleosol Sequences in the Azov Sea Region of Russia: Chronostratigraphy and Paleoenvironmental Record JF - FRONTIERS IN EARTH SCIENCE J2 - FRONT EARTH SC-SWITZ VL - 9 PY - 2022 PG - 17 SN - 2296-6463 DO - 10.3389/feart.2021.808157 UR - https://m2.mtmt.hu/api/publication/32705034 ID - 32705034 N1 - School of Geography, South China Normal University, Guangzhou, China Department of Earth Sciences, Uppsala University, Uppsala, Sweden Institute of Glaciology and Ecogeography, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou, China Southern Scientific Center, Russian Academy of Sciences, Rostov-on-Don, Russian Federation Institute of Geography, Russian Academy of Sciences, Moscow, Russian Federation Faculty of Geography, Lomonosov Moscow State University, Moscow, Russian Federation College of Tourism and Environment, Shaanxi Normal University, Xi’an, China Export Date: 25 February 2022 Correspondence Address: Yang, T.; Institute of Glaciology and Ecogeography, China; email: yangtb@lzu.edu.cn LA - English DB - MTMT ER - TY - JOUR AU - Chen, Q. AU - Liu, X. AU - Zhao, G. AU - Jia, J. AU - Ye, W. AU - Bin, L.Ü. AU - Meadows, M. AU - Guan, J. TI - 0.2 Ma or 1.2 Ma? Timing of the Linking of the Middle and Lower Reaches of the Yellow River Inferred From Loess-Palaeosol Sequences JF - GEOPHYSICAL RESEARCH LETTERS J2 - GEOPHYS RES LETT VL - 49 PY - 2022 IS - 6 SN - 0094-8276 DO - 10.1029/2021GL097510 UR - https://m2.mtmt.hu/api/publication/32870584 ID - 32870584 N1 - College of Geography and Environmental Sciences, Zhejiang Normal University, Jinhua, China State Key Laboratory for Subtropical Mountain Ecology of the Ministry of Science and Technology and Fujian, Fujian Normal University, Fuzhou, China Department of Earth and Environmental Sciences, Macquarie University, Sydney, NSW, Australia School of Geographical Sciences, Xinyang Normal University, Xinyang, China Department of Environmental and Geographical Science, University of Cape Town, Rondebosch, South Africa School of Geographical and Oceanographic Sciences, Nanjing University, Nanjing, China Department of Educational Technology, Zhejiang Normal University, Jinhua, China Export Date: 10 June 2022; Cited By: 0; Correspondence Address: Q. Chen; College of Geography and Environmental Sciences, Jinhua, China; email: chenqu@zjnu.cn; CODEN: GPRLA AB - Variations in susceptibility, grain size or accumulation rates of eolian sequences in the Sanmen Gorge entry and exit points and on the Loess Plateau were compared at different time scales. Synchronous changes in multiple proxies occurred during the formation of S14/L14 at different locality. However, the accumulation rates and magnetic properties were different between the sections in S2 or above, implying that there was significant difference in the proximate source for the gorge entry and exit points. It is suggested that the linking of the middle and lower reaches of the Yellow River occurred at around 1.2 Ma (million years ago) after progressively incising the gorge, while the acceleration in loess accumulation at 0.2 Ma can be attributed to its strong incision in the middle reaches and further channelization in the study area. The entrenchment and terrace formation of the river may be associated with tectonic forcing. © 2022. American Geophysical Union. All Rights Reserved. LA - English DB - MTMT ER - TY - JOUR AU - Łanczont, M AU - Mroczek, P AU - Komar, M AU - Fedorowicz, S AU - Woronko, B AU - Nawrocki, J AU - Frankowski, Z AU - Standzikowski, K TI - A remarkable last glacial loess sedimentation at Roxolany in the Dniester Liman (Southern Ukraine) JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 285 PY - 2022 PG - 24 SN - 0277-3791 DO - 10.1016/j.quascirev.2022.107521 UR - https://m2.mtmt.hu/api/publication/32800573 ID - 32800573 LA - English DB - MTMT ER - TY - JOUR AU - Łanczont, M AU - Mroczek, P AU - Komar, M AU - Fedorowicz, S AU - Woronko, B AU - Nawrocki, J AU - Frankowski, Z AU - Standzikowski, K TI - Reply to the comment on “A remarkable last glacial loess sedimentation at Roxolany in the Dniester Liman (Southern Ukraine)” by JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 297 PY - 2022 SN - 0277-3791 DO - 10.1016/j.quascirev.2022.107835 UR - https://m2.mtmt.hu/api/publication/33222920 ID - 33222920 N1 - Funding Agency and Grant Number: Polish National Science Centre; [2018/31/B/ST10/01507] Funding text: Research carried out as part of the project No. 2018/31/B/ST10/01507 by the Polish National Science Centre. 3 M. ?anczont, P. Mroczek, M. Komar et al. LA - English DB - MTMT ER - TY - GEN AU - Tomaoka, L K O TI - Análise granulométrica, de suscetibilidade magnética e de paleoambiente através de sedimentos do tipo loess do Quaternário, seção Remizovka, Sul do Cazaquistão PY - 2022 PG - 86 UR - https://m2.mtmt.hu/api/publication/32800560 ID - 32800560 LA - Portuguese DB - MTMT ER - TY - JOUR AU - Zykina, V.S. AU - Zykin, V.S. AU - Volvakh, A.O. AU - Radaković, M.G. AU - Gavrilov, M.B. AU - Marković, S.B. TI - Late Pleistocene loess-paleosol sequence at the Belovo section, south of Western Siberia, Russia: Preliminary results JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 620 PY - 2022 SP - 75 EP - 84 PG - 10 SN - 1040-6182 DO - 10.1016/j.quaint.2020.10.069 UR - https://m2.mtmt.hu/api/publication/31665653 ID - 31665653 N1 - Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, Acad. Koptug Ave, 3, Novosibirsk, 630090, Russian Federation National Research Novosibirsk State University, Pirogova Str. 2, Novosibirsk, 630090, Russian Federation Chair of Physical Geography, Faculty of Science, University of Novi Sad, Trg Dositeja Obradovića 3, Novi Sad, Serbia Serbian Academy of Sciences and Arts, Kneza Miloša 35, Belgrade, 11000, Serbia Export Date: 18 November 2020 Correspondence Address: Zykina, V.S.Acad. Koptug Ave, 3, Russian Federation; email: zykina@igm.nsc.ru LA - English DB - MTMT ER - TY - JOUR AU - Adameková, K AU - Lisá, L AU - Neruda, P AU - Petřík, J AU - Doláková, N AU - Novák, J AU - Volánek, J TI - Pedosedimentary record of MIS 5 as an interplay of climatic trends and local conditions: Multi-proxy evidence from the Palaeolithic site of Moravský Krumlov IV (Moravia, Czech Republic) JF - CATENA J2 - CATENA VL - 200 PY - 2021 SN - 0341-8162 DO - 10.1016/j.catena.2021.105174 UR - https://m2.mtmt.hu/api/publication/31883643 ID - 31883643 N1 - Department of Geological Sciences, Faculty of Science, Masaryk University, Kotlářská 2, Brno, 611 37, Czech Republic Institute of Geology of the Czech Academy of Sciences, Rozvojová 269, Prague 6, 165 00, Czech Republic Anthropos Institute, The Moravian Museum, Zelný trh 6, Brno, 659 37, Czech Republic Department of Botany, Faculty of Science, Charles University, Prague, Benátská 2, Prague, Czech Republic Department of Geology and Soil Science, Faculty of Forestry and Wood Technology, Mendel University in Brno, Zemědělská 3, Brno, 613 00, Czech Republic Cited By :4 Export Date: 23 June 2023 CODEN: CIJPD Correspondence Address: Adameková, K.; Department of Geological Sciences, Kotlářská 2, Czech Republic; email: katu.adamekova@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Chu, W. AU - Nett, J.J. TI - The past in dust: current trends and future directions in Pleistocene geoarcheology of European loess JF - JOURNAL OF QUATERNARY SCIENCE J2 - J QUATERNARY SCI VL - 36 PY - 2021 IS - 8 SP - 1279 EP - 1292 PG - 14 SN - 0267-8179 DO - 10.1002/jqs.3388 UR - https://m2.mtmt.hu/api/publication/32469640 ID - 32469640 N1 - Export Date: 27 October 2021 LA - English DB - MTMT ER - TY - JOUR AU - Fenn, K AU - Thomas, DSG. AU - Durcan, JA. AU - Millar, IL. AU - Veres, D AU - Piermattei, A AU - Lane, CS. TI - A tale of two signals: Global and local influences on the Late Pleistocene loess sequences in Bulgarian Lower Danube JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 274 PY - 2021 PG - 21 SN - 0277-3791 DO - 10.1016/j.quascirev.2021.107264 UR - https://m2.mtmt.hu/api/publication/32493346 ID - 32493346 LA - English DB - MTMT ER - TY - JOUR AU - Fischer, P AU - Jöris, O AU - Fitzsimmons, KE. AU - Vinnepand, M AU - Prud'homme, C AU - Schulte, P AU - Hatté, C AU - Hambach, U AU - Lindauer, S AU - Zeeden, C AU - Peric, Z AU - Lehmkuhl, F AU - Wunderlich, T AU - Wilken, D AU - Schirmer, W AU - Vött, A TI - Millennial-scale terrestrial ecosystem responses to Upper Pleistocene climatic changes: 4D-reconstruction of the Schwalbenberg Loess-Palaeosol-Sequence (Middle Rhine Valley, Germany) JF - CATENA J2 - CATENA VL - 196 PY - 2021 SN - 0341-8162 DO - 10.1016/j.catena.2020.104913 UR - https://m2.mtmt.hu/api/publication/31618911 ID - 31618911 N1 - Funding Agency and Grant Number: German Research Foundation (Deutsche Forschungs-gemeinschaft, DFG)German Research Foundation (DFG) [FI 1941/5-1, FI 1918/4-1, VO 938/25-1]; DFGGerman Research Foundation (DFG)European Commission [57444011-SFB 806] Funding text: We appreciate funding by the German Research Foundation (Deutsche Forschungs-gemeinschaft, DFG) in the frame of the TERRACLIME-Project (FI 1941/5-1; FI 1918/4-1; VO 938/25-1). Sediment core REM 1 was drilled and analysed in the frame of the CRC 806 "Our Way to Europe", funded by the DFG (project number 57444011-SFB 806). We thank Barry Thornton for the determination of the TOC content at the James Hutton Institute, Scotland. We also thank Timo Willershauser (JGU Mainz) for taking the core pictures of REM 3 and REM 5. Intensive fieldwork conducted by the whole TERRACLIME-Team and associates, namely Aditi Dave (MPI-C, Mainz), Alexandra Nimmrichter (JGU Mainz), Aileen Klinger (JGU Mainz) build the base of this contribution, which we are grateful for. LA - English DB - MTMT ER - TY - JOUR AU - Hlavatskyi, D AU - Bakhmutov, V TI - Early–Middle Pleistocene Magnetostratigraphic and Rock Magnetic Records of the Dolynske Section (Lower Danube, Ukraine) and Their Application to the Correlation of Loess–Palaeosol Sequences in Eastern and South-Eastern Europe JF - QUATERNARY J2 - Quaternary VL - 4 PY - 2021 IS - 4 PG - 42 SN - 2571-550X DO - 10.3390/quat4040043 UR - https://m2.mtmt.hu/api/publication/32528518 ID - 32528518 N1 - Export Date: 26 December 2021 LA - English DB - MTMT ER - TY - JOUR AU - Hlavatskyi, D. V. AU - Gerasimenko, N.P. AU - Bakhmutov, V.G. AU - Bonchkovskyi, O.S. AU - Poliachenko, I.B. AU - Shpyra, V.V. AU - Mychak, S.V. AU - Kravchuk, I.V. AU - Cherkes, S.I. TI - Significance of the Ukrainian loess-palaeosol sequences for Pleistocene climate reconstructions: rock magnetic, palaeosol and pollen proxies JF - GEOFIZICHESKIY ZHURNAL / GEOPHYSICAL JOURNAL J2 - GEOPHYS J VL - 43 PY - 2021 IS - 3 SP - 3 EP - 26 PG - 24 SN - 0203-3100 DO - 10.24028/gzh.v43i3.236378 UR - https://m2.mtmt.hu/api/publication/32159640 ID - 32159640 LA - English DB - MTMT ER - TY - JOUR AU - Kehl, M AU - Vlaminck, S AU - Köhler, T AU - Laag, C AU - Rolf, C AU - Tsukamoto, S AU - Frechen, M AU - Sumita, M AU - Schmincke, HU AU - Khormali, F TI - Pleistocene dynamics of dust accumulation and soil formation in the southern Caspian Lowlands - New insights from the loess-paleosol sequence at Neka-Abelou, northern Iran JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 253 PY - 2021 SN - 0277-3791 DO - 10.1016/j.quascirev.2020.106774 UR - https://m2.mtmt.hu/api/publication/31816862 ID - 31816862 N1 - Institute of Geography, University of Cologne, Albertus-Magnus-Platz, Cologne, 50923, Germany Leibniz Institute for Applied Geophysics (LIAG), Stilleweg 2, Hannover, 30655, Germany GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstr. 1-3, Kiel, 24148, Germany Department of Soil Sciences, Gorgan University of Agricultural Sciences and Natural Resources, Gorgan, Iran Chair of Soil Physics, University of Bayreuth, Bayreuth Center of Ecology and Environmental Research (BayCEER), Universitätsstr. 30, Bayreuth, 95447, Germany Université de Paris, Institut de Physique du Globe de Paris, CNRS, 1 rue Jussieu, Paris, 75005, France Cited By :11 Export Date: 14 February 2023 CODEN: QSRED Correspondence Address: Kehl, M.; Institute of Geography, Albertus-Magnus-Platz, Germany; email: kehlm@uni-koeln.de LA - English DB - MTMT ER - TY - JOUR AU - Laag, C AU - Hambach, U AU - Zeeden, C AU - Lagroix, F AU - Guyodo, Y AU - Veres, D AU - Jovanović, M AU - Marković, SB. TI - A Detailed Paleoclimate Proxy Record for the Middle Danube Basin Over the Last 430 kyr: A Rock Magnetic and Colorimetric Study of the Zemun Loess-Paleosol Sequence JF - FRONTIERS IN EARTH SCIENCE J2 - FRONT EARTH SC-SWITZ VL - 9 PY - 2021 PG - 24 SN - 2296-6463 DO - 10.3389/feart.2021.600086 UR - https://m2.mtmt.hu/api/publication/32036570 ID - 32036570 N1 - Funding Agency and Grant Number: Alexander von Humboldt Foundation Funding text: We want to thank the Zemun sampling team. We want to thank Kathrin Worm (LIAG Grubenhagen) for the additional colorimetric measurements and Eva Meier (University of Bayreuth) for language improvements of this manuscript. DV was supported through a fellowship provided by Alexander von Humboldt Foundation. All data will be made available on the Pangaea Data Repository. This is IPGP contribution 4210. LA - English DB - MTMT ER - 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 - Murray, A AU - Arnold, LJ. AU - Buylaert, JP AU - Guérin, G AU - Qin, J AU - Singhvi, AK. AU - Smedley, R AU - Thomsen, KJ. TI - Optically stimulated luminescence dating using quartz JF - NATURE REVIEWS METHODS PRIMERS J2 - NATURE REV METHOD PRIM VL - 1 PY - 2021 IS - 1 SN - 2662-8449 DO - 10.1038/s43586-021-00068-5 UR - https://m2.mtmt.hu/api/publication/32871573 ID - 32871573 LA - English DB - MTMT ER - TY - JOUR AU - Avram, A AU - Constantin, D AU - Veres, D AU - Kelemen, Sz AU - Obreht, I AU - Hambach, U AU - Marković, SB. AU - Timar‐Gabor, A TI - Testing polymineral post‐ IR IRSL and quartz SAR ‐ OSL protocols on Middle to Late Pleistocene loess at Batajnica, Serbia JF - BOREAS J2 - BOREAS VL - 49 PY - 2020 IS - 3 SP - 615 EP - 633 PG - 19 SN - 0300-9483 DO - 10.1111/bor.12442 UR - https://m2.mtmt.hu/api/publication/31306984 ID - 31306984 N1 - Interdisciplinary Research Institute on Bio-Nano-Sciences, Babes-Bolyai University, Treboniu Laurian 42, Cluj-Napoca, 400271, Romania Faculty of Environmental Sciences and Engineering, Babes-Bolyai University, Fantanele 30, CLuj-Napoca, 400294, Romania Institute of Speleology, Romanian Academy, Clinicilor 5, Cluj-Napoca, 400006, Romania Organic Geochemistry Group, MARUM-Center for Marine Environmental Sciences and Department of Geosciences, University of Bremen, Leobener 8, Bremen, 28359, Germany BayCEER& Chair of Geomorphology, University of Bayreuth, Universitätsstrasse 30, Bayreuth, 95440, Germany Chair of Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovica 3Novi Sad 21000, Serbia Cited By :15 Export Date: 23 May 2022 Correspondence Address: Constantin, D.; Interdisciplinary Research Institute on Bio-Nano-Sciences, Treboniu Laurian 42, Romania; email: daniela.constantin1@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Fenn, K AU - Durcan, JA. AU - Thomas, DSG. AU - Millar, IL. AU - Marković, SB. TI - Re‐analysis of late Quaternary dust mass accumulation rates in Serbia using new luminescence chronology for loess–palaeosol sequence at Surduk JF - BOREAS J2 - BOREAS VL - 49 PY - 2020 IS - 3 SP - 634 EP - 652 PG - 19 SN - 0300-9483 DO - 10.1111/bor.12445 UR - https://m2.mtmt.hu/api/publication/31335994 ID - 31335994 N1 - Funding Agency and Grant Number: UK Natural Environmental Research CouncilUK Research & Innovation (UKRI)Natural Environment Research Council (NERC) [NE/L002612/1]; International Association of Sedimentologists; Hertford College Travel Fund; NERCUK Research & Innovation (UKRI)Natural Environment Research Council (NERC) [bgs06001] Funding Source: UKRI Funding text: This research was funded by the UK Natural Environmental Research Council (grant: NE/L002612/1), International Association of Sedimentologists, and Hertford College Travel Fund. We are grateful to Nemanja Tomi and Zoran Peri for the field assistance, to Jacek Skurzyski for geochemical discussion, and to Janina Bosken and two anonymous reviewers for their constructive comments. LA - English DB - MTMT ER - TY - JOUR AU - Forget Brisson, L. AU - Lamothe, M. AU - Hardy, F. AU - Graf, K.E. TI - Exploring the use of a low temperature preheat in IRSL dating of feldspar in Beringian archaeological contexts JF - RADIATION MEASUREMENTS J2 - RADIAT MEAS VL - 136 PY - 2020 SN - 1350-4487 DO - 10.1016/j.radmeas.2020.106387 UR - https://m2.mtmt.hu/api/publication/31366792 ID - 31366792 LA - English DB - MTMT ER - TY - JOUR AU - Perić, ZM. AU - Marković, SB. AU - Sipos, György AU - Gavrilov, MB. AU - Thiel, C AU - Zeeden, C AU - Murray, AS. TI - A post‐ IR IRSL chronology and dust mass accumulation rates of the Nosak loess‐palaeosol sequence in northeastern Serbia JF - BOREAS J2 - BOREAS VL - 49 PY - 2020 IS - 4 SP - 841 EP - 857 PG - 17 SN - 0300-9483 DO - 10.1111/bor.12459 UR - https://m2.mtmt.hu/api/publication/31390072 ID - 31390072 N1 - Research Group for Terrestrial Paleoclimates, Max Planck Institute for Chemistry, Hahn-Meitner Weg 1, Mainz, 55128, Germany Serbian Academy of Sciences and Arts, Knez Mihajlova 35, Belgrade, 11000, Serbia Chair of Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, Novi Sad, 21000, Serbia Department of Physical Geography and Geoinformatics, University of Szeged, Szeged, Hungary Centre for Nuclear Technologies, Technical University of Denmark, Risø Campus Frederiksborgvej 399, Roskilde, DK-4000, Denmark Federal Institute for Geosciences and Natural Resources, Stilleweg 2, Hannover, 30655, Germany Leibniz Institute for Applied Geophysics, Stilleweg 2, Hannover, 30655, Germany Nordic Laboratory for Luminescence Dating, Department of Geoscience, Aarhus University, Risø Campus, Roskilde, DK-4000, Denmark Cited By :6 Export Date: 25 May 2022 Correspondence Address: Perić, Z.M.; Research Group for Terrestrial Paleoclimates, Hahn-Meitner Weg 1, Germany; email: zoranperic.geo@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Sycheva, S. AU - Frechen, M. AU - Terhorst, B. AU - Sedov, S. AU - Khokhlova, O. TI - Pedostratigraphy and chronology of the Late Pleistocene for the extra glacial area in the Central Russian Upland (reference section Aleksandrov quarry) JF - CATENA J2 - CATENA VL - 194 PY - 2020 SN - 0341-8162 DO - 10.1016/j.catena.2020.104689 UR - https://m2.mtmt.hu/api/publication/31329058 ID - 31329058 N1 - Export Date: 29 May 2020 CODEN: CIJPD LA - English DB - MTMT ER - TY - JOUR AU - Tecsa, V AU - Gerasimenko, N AU - Veres, D AU - Hambach, U AU - Lehmkuhl, F AU - Schulte, P AU - Timar-Gabor, A TI - Revisiting the chronostratigraphy of Late Pleistocene loess-paleosol sequences in southwestern Ukraine: OSL dating of Kurortne section JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 542 PY - 2020 SP - 65 EP - 79 PG - 15 SN - 1040-6182 DO - 10.1016/j.quaint.2020.03.001 UR - https://m2.mtmt.hu/api/publication/31276824 ID - 31276824 N1 - Export Date: 9 April 2020 LA - English DB - MTMT ER - TY - JOUR AU - Wu, X AU - Hao, Q AU - Marković, S AU - Fu, Y AU - Namira, Y AU - Song, Y AU - Guo, Z TI - Progress in Danube Loess and Paleoenvironment Study JF - DIQIU KEXUE JINZHAN / ADVANCES IN EARTH SCIENCE J2 - ADV EARTH SCI VL - 35 PY - 2020 IS - 4 SP - 363 EP - 377 PG - 15 SN - 1001-8166 DO - 10.11867/j.issn.1001-8166.2020.035 UR - https://m2.mtmt.hu/api/publication/31337645 ID - 31337645 N1 - Funding Agency and Grant Number: 国家自然科学基金基础科学中心项目; 国家重点研发计划项目 LA - Chinese DB - MTMT ER - TY - JOUR AU - Yuan, L. AU - Li, L. AU - Zhang, T. AU - Chen, L. AU - Zhao, J. AU - Hu, S. AU - Cheng, L. AU - Liu, W. TI - Soil moisture estimation for the Chinese loess plateau using MODIS-derived ATI and TVDI JF - REMOTE SENSING J2 - REMOTE SENS-BASEL VL - 12 PY - 2020 IS - 18 SN - 2072-4292 DO - 10.3390/RS12183040 UR - https://m2.mtmt.hu/api/publication/31634392 ID - 31634392 N1 - School of Public Policy and Management, China University of Mining and Technology, Daxue Road 1, Xuzhou, 221116, China Department of Geography, Earth System Science, Vrije Universiteit Brussel, Pleinlaan 2, Brussels, 1050, Belgium Department of Geology Engineering and Geomatics, Chang'an University, Yantalu 120, Xi'an, 710054, China School of Humanities and Law, Jiangsu Ocean University, Cangwu Road 59, Lianyungang, 222005, China Henry Fok College of Biology and Agriculture, Shaoguan University, Daxue Road 26, Shaoguan, 512005, China School of Environment and Spatial Informatics, China University of Mining and Technology, Daxue Road 1, Xuzhou, 221116, China Export Date: 19 October 2020 Correspondence Address: Chen, L.; School of Public Policy and Management, China University of Mining and Technology, Daxue Road 1, China; email: chenlq@cumt.edu.cn LA - English DB - MTMT ER - TY - JOUR AU - Zeeden, C. AU - Obreht, I. AU - Veres, D. AU - Kaboth-Bahr, S. AU - Hošek, J. AU - Marković, S.B. AU - Bösken, J. AU - Lehmkuhl, F. AU - Rolf, C. AU - Hambach, U. TI - Smoothed millennial-scale palaeoclimatic reference data as unconventional comparison targets: Application to European loess records JF - SCIENTIFIC REPORTS J2 - SCI REP VL - 10 PY - 2020 IS - 1 SN - 2045-2322 DO - 10.1038/s41598-020-61528-8 UR - https://m2.mtmt.hu/api/publication/31276499 ID - 31276499 N1 - Export Date: 10 April 2020 LA - English DB - MTMT ER - TY - JOUR AU - Varga, György AU - Gresina, Fruzsina AU - Újvári, Gábor AU - Kovács, János AU - Szalai, Zoltán TI - On the reliability and comparability of laser diffraction grain size measurements of paleosols in loess records JF - SEDIMENTARY GEOLOGY J2 - SEDIMENT GEOL VL - 389 PY - 2019 SP - 42 EP - 53 PG - 12 SN - 0037-0738 DO - 10.1016/j.sedgeo.2019.05.011 UR - https://m2.mtmt.hu/api/publication/30710244 ID - 30710244 N1 - Geographical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi út 45, Budapest, H-1112, Hungary Institute of Geography and Earth Sciences, Faculty of Science, Eötvös University, Pázmány Péter sétány 1/c, Budapest, H-1117, Hungary Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi u. 45, Budapest, H-1112, Hungary Department of Lithospheric Research, University of Vienna, Althanstraße 14, Wien, A-1090, Austria Environmental Analytical & Geoanalytical Research Group, Szentágothai Research Centre, University of Pécs, Ifjúság u. 20, Pécs, H-7624, Hungary Department of Geology & Meteorology, University of Pécs, Ifjúság u. 6, Pécs, H-7624, Hungary Export Date: 16 July 2019 Correspondence Address: Varga, G.; Geographical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi út 45, Hungary; email: varga.gyorgy@csfk.mta.hu Funding Agency and Grant Number: National Research, Development and Innovation Office [NKFIH K120620, KH130337]; MTA research fund [KEP-08/2018] Funding text: Support of the National Research, Development and Innovation Office NKFIH K120620 and KH130337 are gratefully acknowledged. The research was additionally supported by the MTA research fund KEP-08/2018. Geographical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi út 45, Budapest, H-1112, Hungary Institute of Geography and Earth Sciences, Faculty of Science, Eötvös University, Pázmány Péter sétány 1/c, Budapest, H-1117, Hungary Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi u. 45, Budapest, H-1112, Hungary Department of Lithospheric Research, University of Vienna, Althanstraße 14, Wien, A-1090, Austria Environmental Analytical & Geoanalytical Research Group, Szentágothai Research Centre, University of Pécs, Ifjúság u. 20, Pécs, H-7624, Hungary Department of Geology & Meteorology, University of Pécs, Ifjúság u. 6, Pécs, H-7624, Hungary Export Date: 24 September 2019 Correspondence Address: Varga, G.; Geographical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi út 45, Hungary; email: varga.gyorgy@csfk.mta.hu LA - English DB - MTMT ER - TY - JOUR AU - Zhao, Q. AU - Ding, M. AU - Peng, S. AU - Zhang, W. AU - Song, B. AU - Zhou, R. AU - Yue, J. AU - Liang, M. AU - Zhang, D. TI - High resolution OSL dating of the late quaternary loess from Central Shandong Mountains in eastern China and the paleoclimatic implications JF - IOP CONFERENCE SERIES: EARTH AND ENVIRONMENTAL SCIENCE J2 - IOP CONF SER EARTH AND ENVIRON SCI VL - 349 PY - 2019 IS - 1 SN - 1755-1307 DO - 10.1088/1755-1315/349/1/012037 UR - https://m2.mtmt.hu/api/publication/31011788 ID - 31011788 N1 - Key Laboratory of Tourism and Resources Environment in Universities of Shandong, Taishan University, Taian, 271000, China Beijing Jing Yuan School, Beijing, 100040, China Institute of Earthquake Science, CEA, Beijing, 100036, China Export Date: 17 December 2019 LA - English DB - MTMT ER - TY - JOUR AU - Markovic, SB. AU - Yang, S AU - Mason, J TI - Eurasian loess records Preface JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 509 PY - 2018 SP - 1 EP - 3 PG - 3 SN - 0031-0182 DO - 10.1016/j.palaeo.2018.05.041 UR - https://m2.mtmt.hu/api/publication/30953310 ID - 30953310 N1 - Funding Agency and Grant Number: Chinese Association for Quaternary Research; Chinese Academy of Sciences [XDA19050104]; National Natural Science Foundation of China [41725010] Funding text: We are very grateful to the Editors-in-Chief, Thomas Algeo and Paul Hesse, for unusual enthusiasm and kind support during the preparation of this special issue. We thank the Chinese Association for Quaternary Research, the "Strategic Priority Research Program" of the Chinese Academy of Sciences (Grant XDA19050104), and the National Natural Science Foundation of China (Grant 41725010) for financial support related to the organization of the ISADEH meeting. LA - English DB - MTMT ER -