@article{MTMT:34802068, title = {Modelling the paleopedological development of loess/palaeosol sections using discriminant function analysis of compositional geoscience data, case study in Eastern Croatia}, url = {https://m2.mtmt.hu/api/publication/34802068}, author = {Galović, L and Šorša, A and Peh, Z}, doi = {10.1016/j.gexplo.2024.107473}, journal-iso = {J GEOCHEM EXPLOR}, journal = {JOURNAL OF GEOCHEMICAL EXPLORATION}, volume = {262}, unique-id = {34802068}, issn = {0375-6742}, year = {2024}, eissn = {1879-1689} } @article{MTMT:34611429, title = {Loess formation and chronology at the Palaeolithic key site Rheindahlen, Lower Rhine Embayment, Germany}, url = {https://m2.mtmt.hu/api/publication/34611429}, author = {Kehl, M and Seeger, K and Pötter, S and Schulte, P and Klasen, N and Zickel, M and Pastoors, A and Claßen, E}, doi = {10.5194/egqsj-73-41-2024}, journal-iso = {E G QUATERN SCI J}, journal = {EISZEITALTER UND GEGENWART / E&G QUATERNARY SCIENCE JOURNAL}, volume = {73}, unique-id = {34611429}, issn = {0424-7116}, abstract = {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.}, year = {2024}, eissn = {2199-9090}, pages = {41-67}, orcid-numbers = {Seeger, K/0000-0003-0766-9818; Schulte, P/0000-0001-8956-669X; Zickel, M/0000-0002-4473-1759} } @article{MTMT:34557195, title = {The relationship between the loess stratigraphy in the Vojvodina region of northern Serbia and the Saalian and Rissian Stage glaciations – a review}, url = {https://m2.mtmt.hu/api/publication/34557195}, author = {Marković, SB and Hughes, PD and Schaetzl, R and Gibbard, PL and Hao, Q and Radaković, MG and Vandenberghe, J and Obreht, I and Sipos, György and Laag, C and Gavrilov, MB and Antić, A and Marković, RS and Krsmanović, P and Fenn, K and Lukić, T and Perić, ZM}, doi = {10.1111/bor.12646}, journal-iso = {BOREAS}, journal = {BOREAS}, volume = {In press}, unique-id = {34557195}, issn = {0300-9483}, abstract = {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.}, year = {2024}, eissn = {1502-3885}, orcid-numbers = {Sipos, György/0000-0001-6224-2361} } @article{MTMT:33336800, title = {Distal tephras along the SE European margin date powerful explosive eruptions from the Elbrus volcanic center (Greater Caucasus)}, url = {https://m2.mtmt.hu/api/publication/33336800}, author = {Ponomareva, V and Portnyagin, M and Danišík, M and Konstantinov, E and Zelenin, E and Tkach, N and Hauff, F and Schmitt, A K and Friedrichs, B and Romanyuk, B and Guillong, M and Kirkland, C L and Rankenburg, K and Müller, S and Garbe-Schönberg, D}, doi = {10.1016/j.quascirev.2022.107910}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {300}, unique-id = {33336800}, issn = {0277-3791}, year = {2023}, eissn = {1873-457X}, orcid-numbers = {Ponomareva, V/0000-0001-6771-9923; Danišík, M/0000-0002-0885-4938; Zelenin, E/0000-0003-3733-1922; Hauff, F/0000-0001-9503-9714; Schmitt, A K/0000-0002-9029-4211; Friedrichs, B/0000-0001-8555-128X; Guillong, M/0000-0002-6920-3362; Rankenburg, K/0000-0003-3708-9304} } @article{MTMT:34047637, title = {Pleniglacial dynamics in an oceanic central European loess landscape}, url = {https://m2.mtmt.hu/api/publication/34047637}, author = {Pötter, S and Seeger, K and Richter, C and Brill, D and Knaak, M and Lehmkuhl, F and Schulte, P}, doi = {10.5194/egqsj-72-77-2023}, journal-iso = {E G QUATERN SCI J}, journal = {EISZEITALTER UND GEGENWART / E&G QUATERNARY SCIENCE JOURNAL}, volume = {72}, unique-id = {34047637}, issn = {0424-7116}, abstract = {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.}, year = {2023}, eissn = {2199-9090}, pages = {77-94}, orcid-numbers = {Seeger, K/0000-0003-0766-9818; Richter, C/0000-0003-2365-2899; Brill, D/0000-0001-8637-4641; Lehmkuhl, F/0000-0002-6876-7377; Schulte, P/0000-0001-8956-669X} } @article{MTMT:34001105, title = {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}, url = {https://m2.mtmt.hu/api/publication/34001105}, author = {Püspöki, Zoltán and Gibbard, P.L. and Kiss, László Ferenc and McIntosh, Richard William and Thamó-Bozsó, E. and Krassay, Z. and Szappanos, B. and Maigut, V. and Kovács, Péter Gábor and Karácsony, Dominik Ádám and Stercel, F. and Visnovitz, Ferenc and Demény, K. and Bereczki, L. and Szőcs, T. and Rotár-Szalkai, Á. and Fancsik, Tamás}, doi = {10.1111/bor.12618}, journal-iso = {BOREAS}, journal = {BOREAS}, volume = {52}, unique-id = {34001105}, issn = {0300-9483}, abstract = {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.}, year = {2023}, eissn = {1502-3885}, pages = {402-426}, orcid-numbers = {Visnovitz, Ferenc/0000-0002-7040-0080} } @article{MTMT:33034927, title = {The myth of ‘Bohunician soil’: A re-evaluation of the MIS 3 palaeosol record at the Brno-Bohunice site (Czechia)}, url = {https://m2.mtmt.hu/api/publication/33034927}, author = {Adameková, K. and Petřík, J.}, doi = {10.1016/j.catena.2022.106510}, journal-iso = {CATENA}, journal = {CATENA}, volume = {217}, unique-id = {33034927}, issn = {0341-8162}, year = {2022}, eissn = {1872-6887} } @mastersthesis{MTMT:34461852, title = {Reconstructing High-Resolution Paleoclimate for Portions of the Last 250,000 Years from Cave of the Mounds Speleothems}, url = {https://m2.mtmt.hu/api/publication/34461852}, isbn = {9798790654107}, author = {Batchelor, CJ}, publisher = {The University of Wisconsin - Madison}, unique-id = {34461852}, year = {2022} } @article{MTMT:32705034, title = {Revisiting Late Pleistocene Loess–Paleosol Sequences in the Azov Sea Region of Russia: Chronostratigraphy and Paleoenvironmental Record}, url = {https://m2.mtmt.hu/api/publication/32705034}, author = {Chen, J and Stevens, T and Yang, T and Qiang, M and Matishov, G and Konstantinov, E and Kurbanov, R and Zeng, B and Shi, P}, doi = {10.3389/feart.2021.808157}, journal-iso = {FRONT EARTH SC-SWITZ}, journal = {FRONTIERS IN EARTH SCIENCE}, volume = {9}, unique-id = {32705034}, year = {2022}, eissn = {2296-6463} } @article{MTMT:32870584, title = {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}, url = {https://m2.mtmt.hu/api/publication/32870584}, author = {Chen, Q. and Liu, X. and Zhao, G. and Jia, J. and Ye, W. and Bin, L.Ü. and Meadows, M. and Guan, J.}, doi = {10.1029/2021GL097510}, journal-iso = {GEOPHYS RES LETT}, journal = {GEOPHYSICAL RESEARCH LETTERS}, volume = {49}, unique-id = {32870584}, issn = {0094-8276}, abstract = {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.}, keywords = {Rivers; CHINA; SEDIMENTS; MAGNETISM; Grain size and shape; grain size; grain size; ACCUMULATION RATES; paleosol; loess; loess; rock magnetism; rock magnetism; eolian deposit; Loess-palaeosol sequences; Loess Plateau; Yellow River; the Yellow River; the Yellow River; Timing circuits; Palaeosols; Palaeosols; Tectonic structure; Grainsize; Lower reaches of the yellow rivers; The sanmen gorge; The sanmen gorge}, year = {2022}, eissn = {1944-8007} } @article{MTMT:32800573, title = {A remarkable last glacial loess sedimentation at Roxolany in the Dniester Liman (Southern Ukraine)}, url = {https://m2.mtmt.hu/api/publication/32800573}, author = {Łanczont, M and Mroczek, P and Komar, M and Fedorowicz, S and Woronko, B and Nawrocki, J and Frankowski, Z and Standzikowski, K}, doi = {10.1016/j.quascirev.2022.107521}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {285}, unique-id = {32800573}, issn = {0277-3791}, year = {2022}, eissn = {1873-457X}, orcid-numbers = {Mroczek, P/0000-0003-2702-5577} } @article{MTMT:33222920, title = {Reply to the comment on “A remarkable last glacial loess sedimentation at Roxolany in the Dniester Liman (Southern Ukraine)” by}, url = {https://m2.mtmt.hu/api/publication/33222920}, author = {Łanczont, M and Mroczek, P and Komar, M and Fedorowicz, S and Woronko, B and Nawrocki, J and Frankowski, Z and Standzikowski, K}, doi = {10.1016/j.quascirev.2022.107835}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {297}, unique-id = {33222920}, issn = {0277-3791}, year = {2022}, eissn = {1873-457X}, orcid-numbers = {Mroczek, P/0000-0003-2702-5577} } @misc{MTMT:32800560, title = {Análise granulométrica, de suscetibilidade magnética e de paleoambiente através de sedimentos do tipo loess do Quaternário, seção Remizovka, Sul do Cazaquistão}, url = {https://m2.mtmt.hu/api/publication/32800560}, author = {Tomaoka, L K O}, unique-id = {32800560}, year = {2022} } @article{MTMT:31665653, title = {Late Pleistocene loess-paleosol sequence at the Belovo section, south of Western Siberia, Russia: Preliminary results}, url = {https://m2.mtmt.hu/api/publication/31665653}, author = {Zykina, V.S. and Zykin, V.S. and Volvakh, A.O. and Radaković, M.G. and Gavrilov, M.B. and Marković, S.B.}, doi = {10.1016/j.quaint.2020.10.069}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {620}, unique-id = {31665653}, issn = {1040-6182}, year = {2022}, eissn = {1873-4553}, pages = {75-84} } @article{MTMT:31883643, title = {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)}, url = {https://m2.mtmt.hu/api/publication/31883643}, author = {Adameková, K and Lisá, L and Neruda, P and Petřík, J and Doláková, N and Novák, J and Volánek, J}, doi = {10.1016/j.catena.2021.105174}, journal-iso = {CATENA}, journal = {CATENA}, volume = {200}, unique-id = {31883643}, issn = {0341-8162}, year = {2021}, eissn = {1872-6887}, orcid-numbers = {Neruda, P/0000-0001-5017-9107; Volánek, J/0000-0003-3629-4971} } @article{MTMT:32469640, title = {The past in dust: current trends and future directions in Pleistocene geoarcheology of European loess}, url = {https://m2.mtmt.hu/api/publication/32469640}, author = {Chu, W. and Nett, J.J.}, doi = {10.1002/jqs.3388}, journal-iso = {J QUATERNARY SCI}, journal = {JOURNAL OF QUATERNARY SCIENCE}, volume = {36}, unique-id = {32469640}, issn = {0267-8179}, year = {2021}, eissn = {1099-1417}, pages = {1279-1292} } @article{MTMT:32493346, title = {A tale of two signals: Global and local influences on the Late Pleistocene loess sequences in Bulgarian Lower Danube}, url = {https://m2.mtmt.hu/api/publication/32493346}, author = {Fenn, K and Thomas, DSG. and Durcan, JA. and Millar, IL. and Veres, D and Piermattei, A and Lane, CS.}, doi = {10.1016/j.quascirev.2021.107264}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {274}, unique-id = {32493346}, issn = {0277-3791}, year = {2021}, eissn = {1873-457X} } @article{MTMT:31618911, title = {Millennial-scale terrestrial ecosystem responses to Upper Pleistocene climatic changes: 4D-reconstruction of the Schwalbenberg Loess-Palaeosol-Sequence (Middle Rhine Valley, Germany)}, url = {https://m2.mtmt.hu/api/publication/31618911}, author = {Fischer, P and Jöris, O and Fitzsimmons, KE. and Vinnepand, M and Prud'homme, C and Schulte, P and Hatté, C and Hambach, U and Lindauer, S and Zeeden, C and Peric, Z and Lehmkuhl, F and Wunderlich, T and Wilken, D and Schirmer, W and Vött, A}, doi = {10.1016/j.catena.2020.104913}, journal-iso = {CATENA}, journal = {CATENA}, volume = {196}, unique-id = {31618911}, issn = {0341-8162}, year = {2021}, eissn = {1872-6887}, orcid-numbers = {Fischer, P/0000-0002-8410-5824; Schulte, P/0000-0001-8956-669X; Lindauer, S/0000-0001-5363-2755; Lehmkuhl, F/0000-0002-6876-7377} } @article{MTMT:32528518, title = {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}, url = {https://m2.mtmt.hu/api/publication/32528518}, author = {Hlavatskyi, D and Bakhmutov, V}, doi = {10.3390/quat4040043}, journal-iso = {Quaternary}, journal = {QUATERNARY}, volume = {4}, unique-id = {32528518}, issn = {2571-550X}, year = {2021}, orcid-numbers = {Hlavatskyi, D/0000-0002-9901-7827} } @article{MTMT:32159640, title = {Significance of the Ukrainian loess-palaeosol sequences for Pleistocene climate reconstructions: rock magnetic, palaeosol and pollen proxies}, url = {https://m2.mtmt.hu/api/publication/32159640}, author = {Hlavatskyi, D. V. and Gerasimenko, N.P. and Bakhmutov, V.G. and Bonchkovskyi, O.S. and Poliachenko, I.B. and Shpyra, V.V. and Mychak, S.V. and Kravchuk, I.V. and Cherkes, S.I.}, doi = {10.24028/gzh.v43i3.236378}, journal-iso = {GEOPHYS J}, journal = {GEOFIZICHESKIY ZHURNAL / GEOPHYSICAL JOURNAL}, volume = {43}, unique-id = {32159640}, issn = {0203-3100}, year = {2021}, eissn = {2524-1052}, pages = {3-26} } @article{MTMT:31816862, title = {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}, url = {https://m2.mtmt.hu/api/publication/31816862}, author = {Kehl, M and Vlaminck, S and Köhler, T and Laag, C and Rolf, C and Tsukamoto, S and Frechen, M and Sumita, M and Schmincke, HU and Khormali, F}, doi = {10.1016/j.quascirev.2020.106774}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {253}, unique-id = {31816862}, issn = {0277-3791}, year = {2021}, eissn = {1873-457X}, orcid-numbers = {Kehl, M/0000-0003-4587-5858; Laag, C/0000-0002-6012-1029; Khormali, F/0000-0001-6805-7343} } @article{MTMT:32036570, title = {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}, url = {https://m2.mtmt.hu/api/publication/32036570}, author = {Laag, C and Hambach, U and Zeeden, C and Lagroix, F and Guyodo, Y and Veres, D and Jovanović, M and Marković, SB.}, doi = {10.3389/feart.2021.600086}, journal-iso = {FRONT EARTH SC-SWITZ}, journal = {FRONTIERS IN EARTH SCIENCE}, volume = {9}, unique-id = {32036570}, year = {2021}, eissn = {2296-6463} } @article{MTMT:31826687, title = {Loess landscapes of Europe – Mapping, geomorphology, and zonal differentiation}, url = {https://m2.mtmt.hu/api/publication/31826687}, author = {Lehmkuhl, F and Nett, J and Pötter, S and Schulte, P and Sprafke, T and Jary, Z and Antoine, P and Wacha, L and Wolf, D and Zerboni, A and Hošek, J and Slobodan, Marković and Obreht, I and Sümegi, Pál and Veres, D and Zeeden, C and Boemke, B and Schaubert, V and Viehweger, J and Hambach, U}, doi = {10.1016/j.earscirev.2020.103496}, journal-iso = {EARTH-SCI REV}, journal = {EARTH-SCIENCE REVIEWS}, volume = {215}, unique-id = {31826687}, issn = {0012-8252}, year = {2021}, eissn = {1872-6828}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440} } @article{MTMT:32871573, title = {Optically stimulated luminescence dating using quartz}, url = {https://m2.mtmt.hu/api/publication/32871573}, author = {Murray, A and Arnold, LJ. and Buylaert, JP and Guérin, G and Qin, J and Singhvi, AK. and Smedley, R and Thomsen, KJ.}, doi = {10.1038/s43586-021-00068-5}, journal-iso = {NATURE REV METHOD PRIM}, journal = {NATURE REVIEWS METHODS PRIMERS}, volume = {1}, unique-id = {32871573}, year = {2021}, eissn = {2662-8449}, orcid-numbers = {Murray, A/0000-0001-5559-1862; Arnold, LJ./0000-0001-9603-3824; Qin, J/0000-0002-2024-5975; Smedley, R/0000-0001-7773-5193; Thomsen, KJ./0000-0002-4883-1220} } @article{MTMT:31306984, title = {Testing polymineral post‐ IR IRSL and quartz SAR ‐ OSL protocols on Middle to Late Pleistocene loess at Batajnica, Serbia}, url = {https://m2.mtmt.hu/api/publication/31306984}, author = {Avram, A and Constantin, D and Veres, D and Kelemen, Sz and Obreht, I and Hambach, U and Marković, SB. and Timar‐Gabor, A}, doi = {10.1111/bor.12442}, journal-iso = {BOREAS}, journal = {BOREAS}, volume = {49}, unique-id = {31306984}, issn = {0300-9483}, year = {2020}, eissn = {1502-3885}, pages = {615-633} } @article{MTMT:31335994, title = {Re‐analysis of late Quaternary dust mass accumulation rates in Serbia using new luminescence chronology for loess–palaeosol sequence at Surduk}, url = {https://m2.mtmt.hu/api/publication/31335994}, author = {Fenn, K and Durcan, JA. and Thomas, DSG. and Millar, IL. and Marković, SB.}, doi = {10.1111/bor.12445}, journal-iso = {BOREAS}, journal = {BOREAS}, volume = {49}, unique-id = {31335994}, issn = {0300-9483}, year = {2020}, eissn = {1502-3885}, pages = {634-652}, orcid-numbers = {Fenn, K/0000-0002-6322-0540; Durcan, JA./0000-0001-8724-8022} } @article{MTMT:31366792, title = {Exploring the use of a low temperature preheat in IRSL dating of feldspar in Beringian archaeological contexts}, url = {https://m2.mtmt.hu/api/publication/31366792}, author = {Forget Brisson, L. and Lamothe, M. and Hardy, F. and Graf, K.E.}, doi = {10.1016/j.radmeas.2020.106387}, journal-iso = {RADIAT MEAS}, journal = {RADIATION MEASUREMENTS}, volume = {136}, unique-id = {31366792}, issn = {1350-4487}, year = {2020}, eissn = {1879-0925} } @article{MTMT:31390072, title = {A post‐ IR IRSL chronology and dust mass accumulation rates of the Nosak loess‐palaeosol sequence in northeastern Serbia}, url = {https://m2.mtmt.hu/api/publication/31390072}, author = {Perić, ZM. and Marković, SB. and Sipos, György and Gavrilov, MB. and Thiel, C and Zeeden, C and Murray, AS.}, doi = {10.1111/bor.12459}, journal-iso = {BOREAS}, journal = {BOREAS}, volume = {49}, unique-id = {31390072}, issn = {0300-9483}, year = {2020}, eissn = {1502-3885}, pages = {841-857}, orcid-numbers = {Perić, ZM./0000-0003-0116-8895; Sipos, György/0000-0001-6224-2361; Murray, AS./0000-0001-5559-1862} } @article{MTMT:31329058, title = {Pedostratigraphy and chronology of the Late Pleistocene for the extra glacial area in the Central Russian Upland (reference section Aleksandrov quarry)}, url = {https://m2.mtmt.hu/api/publication/31329058}, author = {Sycheva, S. and Frechen, M. and Terhorst, B. and Sedov, S. and Khokhlova, O.}, doi = {10.1016/j.catena.2020.104689}, journal-iso = {CATENA}, journal = {CATENA}, volume = {194}, unique-id = {31329058}, issn = {0341-8162}, year = {2020}, eissn = {1872-6887} } @article{MTMT:31276824, title = {Revisiting the chronostratigraphy of Late Pleistocene loess-paleosol sequences in southwestern Ukraine: OSL dating of Kurortne section}, url = {https://m2.mtmt.hu/api/publication/31276824}, author = {Tecsa, V and Gerasimenko, N and Veres, D and Hambach, U and Lehmkuhl, F and Schulte, P and Timar-Gabor, A}, doi = {10.1016/j.quaint.2020.03.001}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {542}, unique-id = {31276824}, issn = {1040-6182}, year = {2020}, eissn = {1873-4553}, pages = {65-79}, orcid-numbers = {Veres, D/0000-0003-3932-577X; Lehmkuhl, F/0000-0002-6876-7377} } @article{MTMT:31337645, title = {Progress in Danube Loess and Paleoenvironment Study}, url = {https://m2.mtmt.hu/api/publication/31337645}, author = {Wu, X and Hao, Q and Marković, S and Fu, Y and Namira, Y and Song, Y and Guo, Z}, doi = {10.11867/j.issn.1001-8166.2020.035}, journal-iso = {ADV EARTH SCI}, journal = {DIQIU KEXUE JINZHAN / ADVANCES IN EARTH SCIENCE}, volume = {35}, unique-id = {31337645}, issn = {1001-8166}, year = {2020}, pages = {363-377} } @article{MTMT:31634392, title = {Soil moisture estimation for the Chinese loess plateau using MODIS-derived ATI and TVDI}, url = {https://m2.mtmt.hu/api/publication/31634392}, author = {Yuan, L. and Li, L. and Zhang, T. and Chen, L. and Zhao, J. and Hu, S. and Cheng, L. and Liu, W.}, doi = {10.3390/RS12183040}, journal-iso = {REMOTE SENS-BASEL}, journal = {REMOTE SENSING}, volume = {12}, unique-id = {31634392}, year = {2020}, eissn = {2072-4292} } @article{MTMT:31276499, title = {Smoothed millennial-scale palaeoclimatic reference data as unconventional comparison targets: Application to European loess records}, url = {https://m2.mtmt.hu/api/publication/31276499}, author = {Zeeden, C. and Obreht, I. and Veres, D. and Kaboth-Bahr, S. and Hošek, J. and Marković, S.B. and Bösken, J. and Lehmkuhl, F. and Rolf, C. and Hambach, U.}, doi = {10.1038/s41598-020-61528-8}, journal-iso = {SCI REP}, journal = {SCIENTIFIC REPORTS}, volume = {10}, unique-id = {31276499}, issn = {2045-2322}, year = {2020}, eissn = {2045-2322} } @article{MTMT:30710244, title = {On the reliability and comparability of laser diffraction grain size measurements of paleosols in loess records}, url = {https://m2.mtmt.hu/api/publication/30710244}, author = {Varga, György and Gresina, Fruzsina and Újvári, Gábor and Kovács, János and Szalai, Zoltán}, doi = {10.1016/j.sedgeo.2019.05.011}, journal-iso = {SEDIMENT GEOL}, journal = {SEDIMENTARY GEOLOGY}, volume = {389}, unique-id = {30710244}, issn = {0037-0738}, year = {2019}, eissn = {1879-0968}, pages = {42-53}, orcid-numbers = {Varga, György/0000-0003-4784-6372; Újvári, Gábor/0000-0002-2816-6155; Kovács, János/0000-0001-7742-5515; Szalai, Zoltán/0000-0001-5267-411X} } @article{MTMT:31011788, title = {High resolution OSL dating of the late quaternary loess from Central Shandong Mountains in eastern China and the paleoclimatic implications}, url = {https://m2.mtmt.hu/api/publication/31011788}, author = {Zhao, Q. and Ding, M. and Peng, S. and Zhang, W. and Song, B. and Zhou, R. and Yue, J. and Liang, M. and Zhang, D.}, doi = {10.1088/1755-1315/349/1/012037}, journal-iso = {IOP CONF SER EARTH AND ENVIRON SCI}, journal = {IOP CONFERENCE SERIES: EARTH AND ENVIRONMENTAL SCIENCE}, volume = {349}, unique-id = {31011788}, issn = {1755-1307}, year = {2019}, eissn = {1755-1315} } @article{MTMT:30953310, title = {Eurasian loess records Preface}, url = {https://m2.mtmt.hu/api/publication/30953310}, author = {Markovic, SB. and Yang, S and Mason, J}, doi = {10.1016/j.palaeo.2018.05.041}, journal-iso = {PALAEOGEOGR PALAEOCL}, journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY}, volume = {509}, unique-id = {30953310}, issn = {0031-0182}, keywords = {Eurasia; loess}, year = {2018}, eissn = {1872-616X}, pages = {1-3}, orcid-numbers = {Mason, J/0000-0003-2287-8247} }