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 - Szilágyi, Gábor AU - Gulyás, Sándor AU - Vári, Tamás Zsolt AU - Sümegi, Pál TI - Late Quaternary Paleoecology and Environmental History of the Hortobágy, an Alkaline Steppe in Central Europe JF - DIVERSITY (BASEL) J2 - DIVERSITY-BASEL VL - 16 PY - 2024 IS - 1 SP - 67 SN - 1424-2818 DO - 10.3390/d16010067 UR - https://m2.mtmt.hu/api/publication/34427009 ID - 34427009 LA - English DB - MTMT ER - TY - JOUR AU - Antic, Aleksandar AU - Radakovic, Milica G. AU - Marjanovic, Milos AU - Markovic, Slobodan B. AU - Peric, Zoran M. AU - Spalevic, Velibor AU - Momcilovic, Oliver AU - Kostadinovic, Milica AU - Markovic, Rastko AU - Tomic, Nemanja TI - Loess and geotourism potential of the Braničevo District (NE Serbia): From overexploitation to paleoclimate interpretation JF - OPEN GEOSCIENCES J2 - OPEN GEOSCI VL - 15 PY - 2023 IS - 1 PG - 18 SN - 2391-5447 DO - 10.1515/geo-2022-0546 UR - https://m2.mtmt.hu/api/publication/34611598 ID - 34611598 AB - The use of loess as a resource for paleoclimatic research is quite well established. In Serbia, a significant number of loess sequences have been preserved in old brickyards. The results of the previously conducted research indicate extremely valuable data that enable a better understanding of the mid- to late Pleistocene climatic evolution in this part of Europe, as well as human dispersal from Africa to Europe via the so-called Danubian migration corridor. The aim of this study is to evaluate the geotourism potentials of the loess profiles in Pozarevac (northeastern Serbia). The goal is to determine their geotourism potential for paleoclimate interpretation. The Modified Geoheritage Assessment Model method has identified exceptional geotourism potentials that can be implemented in the tourism market. Paleoclimatic data can serve as indicators for the development of scientific visitor centers for the promotion and popularization of paleoclimate science and museums, which will affirm sustainable socio-economic development through multidisciplinary interpretation. By combining geological, paleoclimatic, archaeological, biological, and other values that reveal natural and anthropogenic events from the distant past, it is possible to create a very competitive geotourism destination, whose sustainability can be passed on to future generations. LA - English DB - MTMT ER - TY - JOUR AU - Marković, Slobodan B. AU - Vandenberghe, Jef AU - Perić, Zoran M. AU - Filyó, Dávid AU - Bartyik, Tamás AU - Radaković, Milica G. AU - Hao, Qingzhen AU - Marković, Rastko S. AU - Lukić, Tin AU - Tomić, Nemanja AU - Gavrilov, Milivoj B. AU - Antić, Aleksandar AU - Cvijanović, Ivana AU - Sipos, György TI - Local Differentiation in the Loess Deposition as a Function of Dust Source. Key Study Novo Orahovo Loess Paleosol Sequence (Vojvodina, Serbia) TS - Key Study Novo Orahovo Loess Paleosol Sequence (Vojvodina, Serbia) JF - QUATERNARY J2 - Quaternary VL - 6 PY - 2023 IS - 1 PG - 15 SN - 2571-550X DO - 10.3390/quat6010023 UR - https://m2.mtmt.hu/api/publication/33705061 ID - 33705061 AB - Typical patterns of the Late Pleistocene loess–paleosol units are preserved in the Novo Orahovo brickyard, Northern Serbia. Presented preliminary luminescence chronology supports the chronostratigraphic interpretations of global isotopic marine climate reconstructions. Magnetic susceptibility and sedimentological evidence exhibit general similarities with the marine oxygen-isotope stratigraphy. These records provide new insights into the dust accumulation regimes over the eastern side of the Bačka loess plateau and offer new paleoenvironmental information for the region. They represent an important step forward towards the establishment of a catena from the thin loess-like sediments of the Banat foothills in the east towards the thicker and seemingly more complete loess sections of the southeastern and central Carpathian Basin. Grain-size data from the loess record of Nova Orahovo explain the regional differentiation in dust deposition. LA - English DB - MTMT ER - TY - JOUR AU - Radaković, MG. AU - Oches, EA. AU - Hughes, PD. AU - Marković, RS. AU - Hao, Q AU - Perić, ZM. AU - Gavrilović, B AU - Ludwig, P AU - Lukić, T AU - Gavrilov, MB. AU - Marković, SB. TI - Reconstructed Malacothermometer July Paleotemperatures from the Last Nine Glacials over the South-Eastern Carpathian Basin (Serbia) JF - ATMOSPHERE J2 - ATMOSPHERE-BASEL VL - 14 PY - 2023 IS - 5 SN - 2073-4433 DO - 10.3390/atmos14050791 UR - https://m2.mtmt.hu/api/publication/33784551 ID - 33784551 N1 - ISSN:2073-4433 AB - In this study, the compiled malacological record of the two most important loess–palaeosol sequences (LPS) in Serbia was used to reconstruct the Malacothermometer July Paleotemperature (MTJP) of the last nine glacials. The sieved loess samples yielded shells of 11 terrestrial gastropod species that were used to estimate the MTJP. Veliki Surduk (covering the last three glacial cycles) and Stari Slankamen (covering the last fourth to ninth glacial cycle) LPSs previously lacked the malacological investigations. After the sieving, a total of 66,871 shells were found, from which 48,459 shells were used for the estimation of the MTJP. Through the studied period, the reconstructed MTJP was ranging from 14.4 °C to 21.5 °C. The lowest temperature was recorded during the formation of the loess unit L5, equivalent to the Marine Isotope Stage (MIS) 12. The second-coldest summers were occurring during the MIS 16 glacial. Although the warmest glacial was L8 (MIS 20) according to MTJP, these July temperatures might be overestimated due to only two samples from the poorly preserved L8 unit. The malacological material derived from the loess units at Veliki Surduk and Stari Slankamen LPSs showed great potential for July temperature reconstruction, as the comparison with other regional records showed similar climate changes. Further work is necessary to validate the age scale of the oldest samples, and a higher resolution sampling could lead to more detailed July temperature fluctuations, as was shown for the youngest glacial in this study. Likewise, estimating the July temperature using different proxies (e.g., pollen) from the same LPSs could be used to confirm the observed climate trends. LA - English DB - MTMT ER - TY - JOUR AU - Fenn, K AU - Millar, I L AU - Durcan, J A AU - Thomas, D S G AU - Banak, A AU - Marković, S B AU - Veres, D AU - Stevens, Th TI - The provenance of Danubian loess JF - EARTH-SCIENCE REVIEWS J2 - EARTH-SCI REV VL - 226 PY - 2022 SN - 0012-8252 DO - 10.1016/j.earscirev.2022.103920 UR - https://m2.mtmt.hu/api/publication/32596596 ID - 32596596 N1 - Department of Geography and Planning, University of Liverpool, Liverpool, UK L69 7ZT, United Kingdom Oxford University Centre for the Environment, South Parks Road, Oxford, UK OX1 3QY, United Kingdom Geochronology and Tracers Facility, British Geological Survey, Keyworth, Nottingham, UK NG12 5GG, United Kingdom Croatian Geological Survey, Department of Geology, Sachsova 2, Zagreb, HR-10000, Croatia Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, Novi Sad, 21000, Serbia Romanian Academy, Institute of Speleology, Clinicilor 5, Cluj-Napoca, 400006, Romania Department of Earth Sciences, Uppsala University, Villavägen 16, Uppsala, 752 36, Sweden Export Date: 30 April 2022 Correspondence Address: Fenn, K.; Department of Geography and Planning, United Kingdom; email: kaja.fenn@liverpool.ac.uk LA - English DB - MTMT ER - TY - JOUR AU - Kalkan, K AU - Forkapic, S AU - Markovic, S AU - Bikit, K AU - Tosic, R AU - Mrdja, D AU - Milentijevic, N TI - Study of hanging valley in loess-paleosoil sediments with soil erosion assessment using nuclear and erosion potential methods JF - NUCLEAR TECHNOLOGY & RADIATION PROTECTION J2 - NUCL TECHNOL RADIAT VL - 37 PY - 2022 IS - 1 SP - 65 EP - 77 PG - 13 SN - 1451-3994 DO - 10.2298/NTRP2201065K UR - https://m2.mtmt.hu/api/publication/33034354 ID - 33034354 LA - English DB - MTMT ER - TY - JOUR AU - Perić, ZM. AU - Stevens, T AU - Obreht, I AU - Hambach, U AU - Lehmkuhl, Frank AU - Marković, SB. TI - Detailed luminescence dating of dust mass accumulation rates over the last two glacial-interglacial cycles from the Irig loess-palaeosol sequence, Carpathian Basin JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 215 PY - 2022 SN - 0921-8181 DO - 10.1016/j.gloplacha.2022.103895 UR - https://m2.mtmt.hu/api/publication/33036742 ID - 33036742 N1 - Cited by: 0 AB - Mineral dust records distant from dust sources are crucial in establishing wider atmospheric dust loads in the past. However, detailed, independent chronologies for loess-palaeosol sequences distant from local dust sources are still rare in Europe. In this study we present a high-resolution OSL and pIRIR290 chronology and multi-proxy investigation of the Irig loess-palaeosol sequence (LPS), Vojvodina, Serbia. Our results show that 4–11 μm quartz is a reliable dosimeter only up to 59 ka (179 Gy), after which the OSL ages underestimate the expected ages based on stratigraphy. The pIRIR290 signal displays generally good luminescence behaviour and resultant ages show good agreement with the expected stratigraphic ages, although with apparent 15 kyr and 35 kyr age underestimations at the L2-S2 and S2-L3 boundaries, respectively. The calculated dust mass accumulation rates (MAR) reveal large fluctuations during the last two glacial-interglacial cycles. During the penultimate glacial, the highest MARs were observed between 171 and 181 ka, subsequently decreasing rapidly during MIS 5. During the last glacial period, dust MARs display maximum values during MIS 2 and MIS 4, while the lowest dust input was observed during the Holocene, followed by MIS 3. Dust MAR and grain-size shifts appear to lead changes in magnetic susceptibility by several kyr. Our results imply that changes in dust availability and wind dynamics occurred prior to changes in climate-controlled soil moisture conditions at the Irig LPS. Moreover, our results reveal a close coupling of the dust MAR and grain-size variations during the Mid-Late Pleistocene. These patterns suggest that the Irig site is likely representative of regional dust dynamics, which separates it from more source proximal loess sites, such as those close to major rivers, which are likely more affected by local dust availability and river discharge. © 2022 The Author(s) LA - English DB - MTMT ER - TY - JOUR AU - Perić, ZM. AU - Marković, SB. AU - Avram, A AU - Timar-Gabor, A AU - Zeeden, C AU - Nett, JJ. AU - Fischer, P AU - Fitzsimmons, KE. AU - Gavrilov, MB. TI - Initial quartz OSL and dust mass accumulation rate investigation of the Kisiljevo loess sequence in north-eastern Serbia JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 620 PY - 2022 SP - 13 EP - 23 PG - 11 SN - 1040-6182 DO - 10.1016/j.quaint.2020.10.040 UR - https://m2.mtmt.hu/api/publication/31636099 ID - 31636099 N1 - Összes idézések száma a WoS-ban: 0 LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Molnár, Dávid AU - Náfrádi, Katalin AU - Makó, László AU - Cseh, Péter AU - Törőcsik, Tünde AU - Molnár, Mihály AU - Zhou, Liping TI - Vegetation and land snail-based reconstruction of the palaeocological changes in the forest steppe eco-region of the Carpathian Basin during last glacial warming JF - GLOBAL ECOLOGY AND CONSERVATION J2 - GLOB ECOL CONSERV VL - 33 PY - 2022 PG - 28 SN - 2351-9894 DO - 10.1016/j.gecco.2021.e01976 UR - https://m2.mtmt.hu/api/publication/32544836 ID - 32544836 N1 - Funding Agency and Grant Number: Hungarian Government, Ministry of Human Capacities [20391-3/2018/FEKUSTRAT]; European Regional Development Fund [GINOP-2.3.2-15-2016-00009 'ICER']; University of Szeged Open Access Fund [5386]; Hungarian National Excellence Programme grant [NTP-NFTOd-19-B-0158] Funding text: This research was supported by the Hungarian Government, Ministry of Human Capacities (20391-3/2018/FEKUSTRAT) and the European Regional Development Fund (GINOP-2.3.2-15-2016-00009 'ICER') and the University of Szeged Open Access Fund (no. 5386) . D. Molnar would like to thank the support of the Hungarian National Excellence Programme grant (NTP-NFTOd-19-B-0158) . LA - English DB - MTMT ER - TY - JOUR AU - Bertran, P AU - Bosq, M AU - Borderie, Q AU - Coussot, C AU - Coutard, S AU - Deschodt, L AU - Franc, O AU - Gardère, P AU - Liard, M AU - Wuscher, P TI - Revised map of European aeolian deposits derived from soil texture data JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 266 PY - 2021 IS - 3 PG - 16 SN - 0277-3791 DO - 10.1016/j.quascirev.2021.107085 UR - https://m2.mtmt.hu/api/publication/32102652 ID - 32102652 N1 - Inrap, 140 Avenue du Maréchal Leclerc, Bègles, 33130, France PACEA, Université de Bordeaux-CNRS, Bâtiment B2, Allée Geoffroy-Saint-Hilaire, Pessac, 33605, France Direction de l'aménagement, Conseil départemental d'Eure-et-Loir, Chartres, 28028, France Inrap, 3-5 Rue René Cassin, Chartres, 28000, France UMR 8591 CNRS, Laboratoire de Géographie Physique, Environnements Quaternaires et Actuels, 1 Place A. Briand, Meudon, Cedex, 92195, France Inrap, 32 Avenue de l'Etoile du Sud, Glisy, 80440, France Inrap, 11 Rue des Champs, Villeneuve-d'Ascq, 59650, France Inrap, 12 Rue MaggioriniBron 69500, France Inrap, 148 Avenue André Maginot, Tours, 37100, France UMR 7324 CNRS Citères – LAT, 35 Allée Ferdinand de Lesseps, Tours, 37200, France Inrap, 525 Avenue de la Pomme de PinSaint-Cyr-en-Val 45590, France Archéologie Alsace, 11 Rue Jean-François Champollion, Sélestat, 67600, France Laboratoire Image Ville Environnement, Université de Strasbourg-CNRS, 3 Rue de l'ArgonneStrasbourg 67000, France Cited By :3 Export Date: 25 May 2022 CODEN: QSRED Correspondence Address: Bertran, P.; Inrap, 140 Avenue du Maréchal Leclerc, France; email: pascal.bertran@inrap.fr LA - English DB - MTMT ER - TY - JOUR AU - Csámer, Árpád AU - Papp, Lajos AU - Kristály, Ferenc AU - Szakáll, Sándor AU - Rózsa, Péter TI - Vivianite formation as indicator of human impact in porous sediments JF - ENVIRONMENTAL EARTH SCIENCES J2 - ENVIRON EARTH SCI VL - 80 PY - 2021 IS - 17 PG - 18 SN - 1866-6280 DO - 10.1007/s12665-021-09866-2 UR - https://m2.mtmt.hu/api/publication/32173613 ID - 32173613 N1 - "A cikkben/előadásban/tanulmányban ismertetett kutató munka az EFOP-3.6.1-16-2016-00011 jelű „Fiatalodó és Megújuló Egyetem – Innovatív Tudásváros – a Miskolci Egyetem intelligens szakosodást szolgáló intézményi fejlesztése” projekt részeként – a Széchenyi 2020 keretében – az Európai Unió támogatásával, az Európai Szociális Alap társfinanszírozásával valósul meg" = “The described article/presentation/study was carried out as part of the EFOP-3.6.1-16-00011 “Younger and Renewing University – Innovative Knowledge City – institutional development of the University of Miskolc aiming at intelligent specialisation” project implemented in the framework of the Szechenyi 2020 program. The realization of this project is supported by the European Union, co-financed by the European Social Fund.” AB - Environmental geological survey of a chemical works situated in NE Hungary has been performed for decades. Up till now, several hundreds of drillings of different depths as well as engineering geological soundings have been carried out in the area. Vivianite has been found in a discrete part of a drilling in a gray, silty bed at the depth 6.8-8.5 m. Vivianite was analyzed using X-ray powder diffraction (XRPD), thermal analysis (TG/DTG), and scanning electron microscopic and energy dispersive spectrometry (SEM-EDS) techniques. To demonstrate the spatial distribution of hydrochemical parameters and selected chemical constituents the available data concerning drillings and hydrochemical analyses were collected and evaluated, and field measurements were also performed. For mapping the distribution of relevant physico-chemical parameters and chemical constituents kriging interpolation method was used. Archive aerial photographs demonstrate that a coffered, earth-bedded reservoir for storing huge amounts of extracted plant debris is situated in the vicinity of the drilling. Our study suggests that orthophosphate derived from decomposing biomass entered the groundwater and accumulated within the lowest permeability zone of the intact bedrock. Therefore, the discrete appearance of vivianite in the drilling can be regarded, at least partly, the result of a man-induced mineralogical process. 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 - Fu, Y AU - Hao, Q AU - Peng, S AU - Markovic, SB AU - Gao, X AU - Han, L AU - Wu, X AU - Namier, N AU - Zhang, W AU - Gavrilov, MB AU - Markovic, R AU - Guo, Z TI - Clay mineralogy of the Stari Slankamen (Serbia) loess-paleosol sequence during the last glacial cycle — Implications for dust provenance and interglacial climate JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 263 PY - 2021 PG - 14 SN - 0277-3791 DO - 10.1016/j.quascirev.2021.106990 UR - https://m2.mtmt.hu/api/publication/32057844 ID - 32057844 N1 - Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China University of Chinese Academy of Sciences, Beijing, 100049, China Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Beijing, 100044, China Key Laboratory of Tourism and Resources Environment in Universities of Shandong, Taishan University, Taian, 271021, China Department of Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, Novi Sad, 21000, Serbia Export Date: 25 May 2022 CODEN: QSRED Correspondence Address: Hao, Q.; Key Laboratory of Cenozoic Geology and Environment, China; email: haoqz@mail.iggcas.ac.cn Correspondence Address: Peng, S.; Key Laboratory of Tourism and Resources Environment in Universities of Shandong, China; email: pengshuzhen@tsu.edu.cn LA - English DB - MTMT ER - TY - THES AU - Kalkan, K TI - Primena radioaktivnih metoda u geomorfološkim istraživanjima Titelskog brega [Application of radioactive methods in geomorphological research of Titelski breg] PB - University of Novi Sad PY - 2021 SP - 248 SN - 9798762123068 UR - https://m2.mtmt.hu/api/publication/32911094 ID - 32911094 LA - Serbian 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 - Ludwig, P AU - Gavrilov, MB AU - Radakovic, MG AU - Markovic, SB TI - Malaco temperature reconstructions and numerical simulation of environmental conditions in the southeastern Carpathian Basin during the Last Glacial Maximum JF - JOURNAL OF QUATERNARY SCIENCE J2 - J QUATERNARY SCI VL - 36 PY - 2021 IS - 8 SP - 1426 EP - 1435 PG - 10 SN - 0267-8179 DO - 10.1002/jqs.3318 UR - https://m2.mtmt.hu/api/publication/32009766 ID - 32009766 N1 - Funding Agency and Grant Number: Helmholtz Climate Initiative REKLIM; DKRZ project [965] Funding text: PL thanks the German Climate Computing Centre (DKRZ, Hamburg) for hosting the MPI-ESM-P data and providing computing resources within DKRZ project 965 `Our Way to Europe -Palaeoclimate and Palaeoenvironmental reconstructions'. PL is supported by the Helmholtz Climate Initiative REKLIM (regional climate change; https://www.reklim.de/en).This study is a contribution to the PALEOLINK project within the PAGES 2k Network. The idea for this study emerges at the CRC 806 (https://www.sfb806.uni-koeln.de/) supported international workshop `Loess and Archaeology' in Aachen in 2019. LA - English DB - MTMT ER - TY - JOUR AU - Ludwig, P AU - Gavrilov, MB AU - Markovic, SB AU - Újvári, Gábor AU - Lehmkuhl, F. TI - Simulated regional dust cycle in the Carpathian Basin and the Adriatic Sea region during the Last Glacial Maximum JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 581-582 PY - 2021 SP - 114 EP - 127 PG - 14 SN - 1040-6182 DO - 10.1016/j.quaint.2020.09.048 UR - https://m2.mtmt.hu/api/publication/31969595 ID - 31969595 N1 - Cited By :2 Export Date: 3 May 2021 Correspondence Address: Ludwig, P.; Institute of Meteorology and Climate Research, Germany; email: patrick.ludwig@kit.edu Funding details: Deutsche Forschungsgemeinschaft, DFG, 57444011 – SFB 806 Funding text 1: PL thanks the German Climate Computing Centre (DKRZ, Hamburg) for providing the MPI-ESM-P data and computing resources within DKRZ project 965 “Our Way to Europe – Palaeoclimate and Palaeoenvironmental reconstructions”. PL is supported by the Helmholtz Climate Initiative REKLIM (regional climate change; https://www.reklim.de/en ). FL acknowledge funding by the CRC 806 "Our way to Europe", subproject B1 "The Eastern Trajectory: Last Glacial Palaeogeography and Archaeology of the Eastern Mediterranean and of the Balkan Peninsula", by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) – Projekt-ID 57444011 – SFB 806 . MBG and SBM are grateful to the First Program of the Chinese-Serbian Developing Projects (Project title: “A Comparative Study of Past Climate Change in the East Asian Monsoon Region and the Westerly Zone Using Multiple Timescales”). The authors thank two anonymous reviewers for their comments that improved the manuscript. LA - English DB - MTMT ER - TY - JOUR AU - Markovic, SB. AU - Vandenberghe, J AU - Stevens, T AU - Mihailovic, D AU - Gavrilov, MB. AU - Radakovic, MG. AU - Zeeden, C AU - Obreht, I AU - Peric, ZM. AU - Nett, JJ. AU - Lehmkuhl, F TI - Geomorphological evolution of the Petrovaradin Fortress Palaeolithic site (Novi Sad, Serbia) JF - QUATERNARY RESEARCH J2 - QUATERNARY RES VL - 103 PY - 2021 SP - 21 EP - 34 PG - 14 SN - 0033-5894 DO - 10.1017/qua.2020.88 UR - https://m2.mtmt.hu/api/publication/31678166 ID - 31678166 N1 - Department of Geography, Tourism and Hotel Management, Faculty of Science, University of Novi Sad, Trg Dositeja Obradovicá 3, Novi Sad, 21000, Serbia Department of Earth Sciences, Faculty of Science, Vrije Universiteit, De Boelelaan 1085, Amsterdam, 1081 HV, Netherlands Department of Earth Sciences, Uppsala University, Villavägen 16, Uppsala, 75236, Sweden Department of Archaeology, Faculty of Philosophy, University of Belgrade, Čika Ljubina 18-20, Belgrade, 11000, Serbia Leibniz Institute for Applied Geophysics, Geozentrum Hannover, Stilleweg 2, Hannover, , 30655, Germany Organic Geochemistry Group, Center for Marine Environmental Sciences and Department of Geosciences, University of Bremen, Leobener Str. 8,MARUM, Bremen, 28359, Germany Research Group for Terrestrial Paleoclimates, Max Planck Institute for Chemistry, Hahn-Meitner Weg 1, Mainz, 55128, Germany Department of Geography, Rwth Aachen University, Wüllnerstr. 5b, Aachen, 52056, Germany Cited By :2 Export Date: 12 October 2021 Correspondence Address: Marković, S.B.; Department of Geography, Trg Dositeja Obradovicá 3, Serbia; email: baca.markovic@gmail.com Funding details: Deutsche Forschungsgemeinschaft, DFG, 57444011 – SFB 806 Funding details: Vetenskapsrådet, VR, 2017-03888 Funding details: Ministarstvo Prosvete, Nauke i Tehnološkog Razvoja, MPNTR, 177023 Funding text 1: The authors are very grateful to Claire Tye (Gallant), Radovan Bunardžić and MihajloLesjak for help during the fieldwork, and to Vladica Cvetković for stimulating discussion. Slobodan Marković, Milivoj Gavrilov and Milica Radaković were supported by grant # 176020, financed by the Serbian Ministry of Education, Science and Technological Development and the First Program of the Chinese-Serbian Developing Projects (Project title: “A Comparative Study of Past Climate Change in the East Asian Monsoon Region and the Westerly Zone using Multiple Timescales”). Christian Zeeden, Igor Obreht, Janina Nett and Frank Lehmkuhl acknowledge funding by the CRC 806 “Our Way to Europe”, subproject B1 – “The Eastern Trajectory: Last Glacial Palaeogeography and Archaeology of the Eastern Mediterranean and of the Balkan Peninsula” – by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) – Projektnummer 57444011 – SFB 806. Thomas Stevens gratefully acknowledges the support of the Swedish Research Council (2017-03888). The work of Dušan Mihailović was supported by Ministry of Culture and Information, and the Ministry of Education, Science and Technological Development of the Republic of Serbia (project # 177023). AB - Two phases of archaeological investigation were performed in the Novi Sad City Museum at Petrovaradin Fortress. In this study, we summarize the results of geo-archaeological investigations of the second period of excavation inside the Novi Sad City Museum building. The fortress is situated on a Danube terrace with the top of the bedrock at ca.123 m asl. The investigated section consists of undisturbed fine-sandy silt. The grain-size distribution of the sediments indicates clearly its alluvial reworking but shows also a general similarity with typical primary loess in the region. All analyzed proxies indicate slightly stronger weathering in the upper part of the profile. Luminescence ages suggest that the investigated sequence covers the last glacial period and the terrace presumably formed during MIS 4. Subsequently, the Danube started its incision at the start of the next warmer period (MIS 3) onward. This terrace age and elevation enable us to derive an uplift rate of the terrace of ca. 0.73 mm/a for the last 60 ka, which seems to increase towards the present. Basal loessic material, in which artifacts occur, likely in the reworked position, indicate that the area close to today's Petrovaradin Fortress was already inhabited in MIS 5. LA - English DB - MTMT ER - TY - JOUR AU - Marković, SB. AU - Oches, EA. AU - Perić, ZM. AU - Gaudenyi, T AU - Jovanović, M AU - Sipos, Gy AU - Thiel, C AU - Buylaert, JP AU - Savić, S AU - McCoy, WD. AU - Radaković, MG. AU - Marković, RS. AU - Gavrilov, MB. TI - The Požarevac loess–paleosol sequence: a record of increased aridity in the south‐eastern margin of the Carpathian Basin during the last 350 ka JF - JOURNAL OF QUATERNARY SCIENCE J2 - J QUATERNARY SCI VL - 36 PY - 2021 IS - 8 SP - 1436 EP - 1447 PG - 12 SN - 0267-8179 DO - 10.1002/jqs.3327 UR - https://m2.mtmt.hu/api/publication/32062161 ID - 32062161 N1 - Department of Geography, Tourism and Hotel management, Faculty of Science, University of Novi Sad, Novi Sad, Serbia Serbian Academy of Arts and Sciences, Belgrade, Serbia Department of Natural and Applied Sciences, Bentley University, Waltham, MA, United States Research Group for Terrestrial Paleoclimates, Max Planck Institute for Chemistry, Mainz, Germany Geographical Institute SASA “Jovan Cvijić”, Belgrade, Serbia Department of Physical Geography, University of Szeged, Szeged, Hungary Department B4.3: Federal Seismological Survey, Nuclear-Test Ban, Federal Institute for Geosciences and Natural Resources, Hannover, Germany Department of Physics, Technical University of Denmark, RisøCampus, Roskilde, Denmark Department of Geosciences, University of Massachusetts, Amherst, MA, United States Cited By :2 Export Date: 12 October 2021 Correspondence Address: Radaković, M.G.; Department of Geography, Serbia; email: milica.radakovic.95@gmail.com Funding details: Ministarstvo Prosvete, Nauke i Tehnološkog Razvoja, MPNTR, 451‐03‐9/2021‐14/200125 Funding details: Serbian Academy of Sciences and Arts, SASA, F‐178 Funding text 1: We thank the Požarevac Brick factory for allowing the team to work in the quarry. This study was supported by the First Program of the Chinese–Serbian Developing Projects (Project title: ‘A Comparative Study of Past Climate Change in the East Asian Monsoon Region and the Westerly Zone Using Multiple Timescales’). The authors acknowledge financial support of the Ministry of Education, Science and Technological Development of the Republic of Serbia (grant no. 451‐03‐9/2021‐14/200125) and Serbian Academy of Sciences and Arts (grant no. F‐178). AB - The loess sequence preserved in the Pozarevac brickyard in north-eastern Serbia comprises eight loess units separated by seven paleosols. Geochronological investigation using amino acid racemization and luminescence dating support stratigraphic correlations of loess units L3, S2LL1 and L1 at the Pozarevac section with loess of glacial cycles E [Marine Isotope Stage (MIS) 10], D (MIS 9-8), C (MIS 7-6) and B (MIS 5-2) across central Europe. Correlation with the marine oxygen-isotope stratigraphy and associated paleoclimatic inferences are further supported by magnetic susceptibility, particle size and carbonate content measured in Pozarevac sediments. Malacological investigations at the Pozarevac section reveal the continuous presence of the Chondrula tridens and Helicopsis striata faunal assemblages throughout the last 350 ka. The loess malacological fauna, which is characterized by the complete absence of cold-resistant and cold-preferring species, suggests a stable, dry and relatively warm glacial and interglacial climate, compared with other central European loess localities. Together these data suggest that the south-eastern part of the Carpathian (Pannonian, Middle Danube) Basin was a refugium for warm-preferring and xerophilous land-snails during the generally unfavorable glacial climates of the late Middle and Late Pleistocene. LA - English DB - MTMT ER - TY - JOUR AU - Perić, ZM. AU - Marković, SB. AU - Filyó, Dávid AU - Thiel, C AU - Murray, AS. AU - Gavrilov, MB. AU - Nett, JJ. AU - Sipos, György TI - Quartz OSL and polymineral post IR–IRSL dating of the Požarevac loess–palaeosol sequence in north–eastern Serbia JF - QUATERNARY GEOCHRONOLOGY J2 - QUAT GEOCHRONOL VL - 66 PY - 2021 PG - 14 SN - 1871-1014 DO - 10.1016/j.quageo.2021.101216 UR - https://m2.mtmt.hu/api/publication/32151522 ID - 32151522 N1 - Cited By :2 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 - Potter, S AU - Veres, D AU - Baykal, Y AU - Nett, JJ AU - Schulte, P AU - Hambach, U AU - Lehmkuhl, F TI - Disentangling Sedimentary Pathways for the Pleniglacial Lower Danube Loess Based on Geochemical Signatures JF - FRONTIERS IN EARTH SCIENCE J2 - FRONT EARTH SC-SWITZ VL - 9 PY - 2021 SN - 2296-6463 DO - 10.3389/feart.2021.600010 UR - https://m2.mtmt.hu/api/publication/32036727 ID - 32036727 N1 - Funding Agency and Grant Number: Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) [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 Palaeogeography and Archaeology of the Eastern Mediterranean and of the Balkan Peninsula," funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation)-Projektnummer 57444011-SFB 806. LA - English DB - MTMT ER - TY - JOUR AU - Pötter, S AU - Schmitz, A AU - Lücke, A AU - Schulte, P AU - Obreht, I AU - Zech, M AU - Wissel, H AU - Marković, SB. AU - Lehmkuhl, F TI - Middle to Late Pleistocene environments based on stable organic carbon and nitrogen isotopes of loess‐palaeosol sequences from the Carpathian Basin JF - BOREAS J2 - BOREAS VL - 50 PY - 2021 IS - 1 SP - 184 EP - 204 PG - 21 SN - 0300-9483 DO - 10.1111/bor.12470 UR - https://m2.mtmt.hu/api/publication/31626828 ID - 31626828 LA - English DB - MTMT ER - TY - JOUR AU - Zeeden, C AU - Hambach, U TI - Magnetic Susceptibility Properties of Loess From the Willendorf Archaeological Site: Implications for the Syn/Post-Depositional Interpretation of Magnetic Fabric JF - FRONTIERS IN EARTH SCIENCE J2 - FRONT EARTH SC-SWITZ VL - 8 PY - 2021 SN - 2296-6463 DO - 10.3389/feart.2020.599491 UR - https://m2.mtmt.hu/api/publication/31908801 ID - 31908801 N1 - Cited By :2 Export Date: 23 May 2022 Correspondence Address: Zeeden, C.; Leibniz Institute for Applied GeophysicsGermany; email: christian.zeeden@leibniz-liag.de Correspondence Address: Zeeden, C.; BayCEER and Chair of Geomorphology, Germany; email: christian.zeeden@leibniz-liag.de LA - English DB - MTMT ER - TY - JOUR AU - Zeeden, C AU - Hambach, U AU - Klasen, N AU - Fischer, P AU - Schulte, P AU - Nett, JJ. AU - Veres, D AU - Obreht, I AU - Chu, W AU - Papadopoulou, M AU - Viehberg, F AU - SchÄBitz, F AU - Gavrilov, MB. AU - Markovic, SB. AU - Vött, A AU - Lehmkuhl, F TI - Sedimentology of a Late Quaternary lacustrine record from the south‐eastern Carpathian Basin JF - JOURNAL OF QUATERNARY SCIENCE J2 - J QUATERNARY SCI VL - 36 PY - 2021 IS - 8 SP - 1414 EP - 1425 PG - 12 SN - 0267-8179 DO - 10.1002/jqs.3297 UR - https://m2.mtmt.hu/api/publication/32006908 ID - 32006908 N1 - Funding Agency and Grant Number: Deutsche Forschungsgemeinschaft (DFG, German Research Foundation)German Research Foundation (DFG) [CRC 806, 57444011 - SFB 806]; Serbian Ministry of Education, Science and Technological DevelopmentMinistry of Education, Science & Technological Development, Serbia [176020]; EEA-RO-NO-2018 Grant [0126]; Projekt DEAL 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 Palaeogeography and Archaeology of the Eastern Mediterranean and of the Balkan Peninsula', and subproject F2 `Application of Luminescence and Electron-SpinResonance Dating Techniques in Geoarchaeological Contexts', funded by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) -Projektnummer 57444011 - SFB 806. S.B.M. and M.B.G. acknowledge the financial support from grant 176020 of the Serbian Ministry of Education, Science and Technological Development. D.V. acknowledges support financed through the EEA-RO-NO-2018 Grant #0126 (KARSTHIVES2). We are grateful to Lea Obrocki and Jan Hosek for their help in the field. Radionuclide concentrations were measured using high purity germanium gamma spectrometry at VKTA Rossendorf (Dr D. Degering). Bruno Boemke, Janek Walk and Jonas Viehweger are thanked for support with maps. We thank the two reviewers for their constructive and helpful feedback. Open access funding enabled and organized by Projekt DEAL. LA - English DB - MTMT ER - TY - JOUR AU - Badino, F AU - Pini, R AU - Ravazzi, C AU - Margaritora, D AU - Arrighi, S AU - Bortolini, E AU - Figus, C AU - Giaccio, B AU - Lugli, F AU - Marciani, G AU - Monegato, G AU - Moroni, A AU - Negrino, F AU - Oxilia, G AU - Peresani, M AU - Romandini, M AU - Ronchitelli, A AU - Spinapolice, EE. AU - Zerboni, A AU - Benazzi, S TI - An overview of Alpine and Mediterranean palaeogeography, terrestrial ecosystems and climate history during MIS 3 with focus on the Middle to Upper Palaeolithic transition JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 551 PY - 2020 SP - 7 EP - 28 PG - 22 SN - 1040-6182 DO - 10.1016/j.quaint.2019.09.024 UR - https://m2.mtmt.hu/api/publication/30817326 ID - 30817326 N1 - Dipartimento di Beni Culturali, Università di Bologna, Ravenna, 48121, Italy C.N.R, Istituto di Geologia Ambientale e Geoingegneria, Milano, 20126, Italy Dipartimento di Scienze Fisiche Della Terra e Dell'Ambiente, Università di Siena, Siena, 53100, Italy Centro Studi sul Quaternario, Sansepolcro, 52037, Italy C.N.R., Istituto di Geologia Ambientale e Geoingegneria, Rome, 00015, Italy Dipartimento di Scienze Chimiche e Geologiche, Università di Modena e Reggio Emilia, Modena, 41125, Italy C.N.R, Istituto di Geoscienze e Georisorse, Padova, 35131, Italy Dipartimento Antichità, Filosofia e Storia, Università di Genova, Genova, 16126, Italy Dipartimento di Studi Umanistici, Sezione di Scienze Preistoriche e Antropologiche, Università di Ferrara, Ferrara, 44100, Italy Dipartimento di Scienze Dell'Antichità, Università Sapienza, Roma, 00185, Italy Dipartimento di Scienze Della Terra “A. Desio”, Università Degli Studi di Milano, Milano, 20133, Italy Department of Human Evolution Max Planck Institute for Evolutionary Anthropology, Leipzig, 04103, Germany Cited By :7 Export Date: 25 October 2020 Correspondence Address: Badino, F.; Università di Bologna, Dipartimento di Beni Culturali, Via degli Ariani 1, Italy; email: federica.badino@unibo.it LA - English DB - MTMT ER - TY - JOUR AU - Chen, J. AU - Yang, T. AU - Qiang, M. AU - Matishov, G.G. AU - Velichko, A.A. AU - Zeng, B. AU - Xu, M. AU - Shi, P. TI - Interpretation of sedimentary subpopulations extracted from grain size distributions in loess deposits at the Sea of Azov, Russia JF - AEOLIAN RESEARCH J2 - AEOLIAN RES VL - 45 PY - 2020 SN - 1875-9637 DO - 10.1016/j.aeolia.2020.100597 UR - https://m2.mtmt.hu/api/publication/31277488 ID - 31277488 N1 - Export Date: 13 April 2020 School of Geography Sciences, South China Normal University, Guangzhou, 510631, China Institute of Glaciology and Ecogeography, College of Earth and Environmental Sciences, Lanzhou University, Lanzhou, 730000, China South Scientific Centre, Russian Academy of Sciences, Chekhov Av. 41, Rostov-on-Don, 344006, Russian Federation Institute of Geography, Russian Academy of Sciences, Staromonetny 29, Moscow, 119017, Russian Federation College of Tourism and Environment, Shananxi Normal University, Xi'an, 710119, China Export Date: 26 October 2020 Correspondence Address: Yang, T.; Institute of Glaciology and Ecogeography, College of Earth and Environmental Sciences, Lanzhou UniversityChina; email: yangtb@lzu.edu.cn LA - English DB - MTMT ER - TY - JOUR AU - Willmes, Christian AU - Niedziolka, Kamil AU - Serbe, Benjamin AU - Grimm, Sonja B. AU - Gross, Daniel AU - Miebach, Andrea AU - Marker, Michael AU - Henselowsky, Felix AU - Gamisch, Alexander AU - Rostami, Masoud AU - Mateos, Ana AU - Rodriguez, Jesus AU - Limberg, Heiko AU - Schmidt, Isabell AU - Mueller, Martin AU - Hoelzchen, Ericson AU - Holthausen, Michael AU - Klein, Konstantin AU - Wegener, Christian AU - Weninger, Bernhard AU - Nielsen, Trine Kellberg AU - Otto, Taylor AU - Weniger, Gerd-Christian AU - Bubenzer, Olaf AU - Bareth, Georg TI - State of the Art in Paleoenvironment Mapping for Modeling Applications in Archeology-Summary, Conclusions, and Future Directions from the PaleoMaps Workshop JF - QUATERNARY J2 - Quaternary VL - 3 PY - 2020 IS - 2 PG - 25 SN - 2571-550X DO - 10.3390/quat3020013 UR - https://m2.mtmt.hu/api/publication/31498579 ID - 31498579 AB - In this report, we present the contributions, outcomes, ideas, discussions and conclusions obtained at the PaleoMaps Workshop 2019, that took place at the Institute of Geography of the University of Cologne on 23 and 24 September 2019. The twofold aim of the workshop was: (1) to provide an overview of approaches and methods that are presently used to incorporate paleoenvironmental information in human-environment interaction modeling applications, and building thereon; (2) to devise new approaches and solutions that might be used to enhance the reconstruction of past human-environmental interconnections. This report first outlines the presented papers, and then provides a joint protocol of the often extensive discussions that came up following the presentations or else during the refreshment intervals. It concludes by adressing the open points to be resolved in future research avenues, e.g., implementation of open science practices, new procedures for reviewing of publications, and future concepts for quality assurance of the often complex paleoenvironmental data. This report may serve as an overview of the state of the art in paleoenvironment mapping and modeling. It includes an extensive compilation of the basic literature, as provided by the workshop attendants, which will itself facilitate the necessary future research. 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 - Hao, Q. AU - Zeeden, C. AU - Moska, P. AU - Tomić, N. TI - Loess2M - Modelling and Mapping JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 502 PY - 2019 SP - 1 EP - 3 PG - 3 SN - 1040-6182 DO - 10.1016/j.quaint.2019.02.030 UR - https://m2.mtmt.hu/api/publication/30613177 ID - 30613177 N1 - Export Date: 27 March 2019 LA - English DB - MTMT ER - TY - JOUR AU - Obreht, I. AU - Zeeden, C. AU - Hambach, U. AU - Veres, D. AU - Marković, S.B. AU - Lehmkuhl, F. TI - A critical reevaluation of palaeoclimate proxy records from loess in the Carpathian Basin JF - EARTH-SCIENCE REVIEWS J2 - EARTH-SCI REV VL - 190 PY - 2019 SP - 498 EP - 520 PG - 23 SN - 0012-8252 DO - 10.1016/j.earscirev.2019.01.020 UR - https://m2.mtmt.hu/api/publication/30429893 ID - 30429893 N1 - Export Date: 11 February 2019 Organic Geochemistry Group, MARUM-Center for Marine Environmental Sciences and Department of Geosciences, University of Bremen, Leobener Str. 8, Bremen, 28359, Germany IMCCE, Observatoire de Paris, PSL Research University, CNRS, Sorbonne Universités, UPMC Univ Paris 06, Univ Lille, Paris, 75014, France LIAG, Leibniz Institute for Applied Geophysics, Stilleweg 2, Hannover, 30655, Germany BayCEER & Chair of Geomorphology, University of Bayreuth, Bayreuth, 95440, Germany Romanian Academy, Institute of Speleology, Cluj-Napoca, 400006, Romania Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, Novi Sad, 21000, Serbia Department of Geography, RWTH Aachen University, Templergraben 55, Aachen, 52056, Germany Cited By :1 Export Date: 13 June 2019 Correspondence Address: Obreht, I.; Organic Geochemistry Group, MARUM-Center for Marine Environmental Sciences and Department of Geosciences, University of Bremen, Leobener Str. 8, Germany; email: iobreht@marum.de Organic Geochemistry Group, MARUM-Center for Marine Environmental Sciences and Department of Geosciences, University of Bremen, Leobener Str. 8, Bremen, 28359, Germany IMCCE, Observatoire de Paris, PSL Research University, CNRS, Sorbonne Universités, UPMC Univ Paris 06, Univ Lille, Paris, 75014, France LIAG, Leibniz Institute for Applied Geophysics, Stilleweg 2, Hannover, 30655, Germany BayCEER & Chair of Geomorphology, University of Bayreuth, Bayreuth, 95440, Germany Romanian Academy, Institute of Speleology, Cluj-Napoca, 400006, Romania Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, Novi Sad, 21000, Serbia Department of Geography, RWTH Aachen University, Templergraben 55, Aachen, 52056, Germany Cited By :4 Export Date: 30 August 2019 Correspondence Address: Obreht, I.; Organic Geochemistry Group, MARUM-Center for Marine Environmental Sciences and Department of Geosciences, University of Bremen, Leobener Str. 8, Germany; email: iobreht@marum.de Organic Geochemistry Group, MARUM-Center for Marine Environmental Sciences and Department of Geosciences, University of Bremen, Leobener Str. 8, Bremen, 28359, Germany IMCCE, Observatoire de Paris, PSL Research University, CNRS, Sorbonne Universités, UPMC Univ Paris 06, Univ Lille, Paris, 75014, France LIAG, Leibniz Institute for Applied Geophysics, Stilleweg 2, Hannover, 30655, Germany BayCEER & Chair of Geomorphology, University of Bayreuth, Bayreuth, 95440, Germany Romanian Academy, Institute of Speleology, Cluj-Napoca, 400006, Romania Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, Novi Sad, 21000, Serbia Department of Geography, RWTH Aachen University, Templergraben 55, Aachen, 52056, Germany Cited By :5 Export Date: 24 September 2019 Correspondence Address: Obreht, I.; Organic Geochemistry Group, MARUM-Center for Marine Environmental Sciences and Department of Geosciences, University of Bremen, Leobener Str. 8, Germany; email: iobreht@marum.de 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 -