@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:34427009,
	title = {Late Quaternary Paleoecology and Environmental History of the Hortobágy, an Alkaline Steppe in Central Europe},
	url = {https://m2.mtmt.hu/api/publication/34427009},
	author = {Szilágyi, Gábor and Gulyás, Sándor and Vári, Tamás Zsolt and Sümegi, Pál},
	doi = {10.3390/d16010067},
	journal-iso = {DIVERSITY-BASEL},
	journal = {DIVERSITY (BASEL)},
	volume = {16},
	unique-id = {34427009},
	year = {2024},
	eissn = {1424-2818},
	pages = {67},
	orcid-numbers = {Gulyás, Sándor/0000-0002-3384-2381; Vári, Tamás Zsolt/0000-0002-1763-614X; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:34611598,
	title = {Loess and geotourism potential of the Braničevo District (NE Serbia): From overexploitation to paleoclimate interpretation},
	url = {https://m2.mtmt.hu/api/publication/34611598},
	author = {Antic, Aleksandar and Radakovic, Milica G. and Marjanovic, Milos and Markovic, Slobodan B. and Peric, Zoran M. and Spalevic, Velibor and Momcilovic, Oliver and Kostadinovic, Milica and Markovic, Rastko and Tomic, Nemanja},
	doi = {10.1515/geo-2022-0546},
	journal-iso = {OPEN GEOSCI},
	journal = {OPEN GEOSCIENCES},
	volume = {15},
	unique-id = {34611598},
	issn = {2391-5447},
	abstract = {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.},
	keywords = {loess; paleoclimatic interpretation; sustainable geotourism; Brani & ccaron;evo District (Serbia)},
	year = {2023},
	eissn = {2391-5447},
	orcid-numbers = {Marjanovic, Milos/0000-0003-0412-6615; Spalevic, Velibor/0000-0002-7800-2909}
}

@article{MTMT:33705061,
	title = {Local Differentiation in the Loess Deposition as a Function of Dust Source. Key Study Novo Orahovo Loess Paleosol Sequence (Vojvodina, Serbia)},
	url = {https://m2.mtmt.hu/api/publication/33705061},
	author = {Marković, Slobodan B. and Vandenberghe, Jef and Perić, Zoran M. and Filyó, Dávid and Bartyik, Tamás and Radaković, Milica G. and Hao, Qingzhen and Marković, Rastko S. and Lukić, Tin and Tomić, Nemanja and Gavrilov, Milivoj B. and Antić, Aleksandar and Cvijanović, Ivana and Sipos, György},
	doi = {10.3390/quat6010023},
	journal-iso = {Quaternary},
	journal = {QUATERNARY},
	volume = {6},
	unique-id = {33705061},
	issn = {2571-550X},
	abstract = {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.},
	year = {2023},
	orcid-numbers = {Vandenberghe, Jef/0000-0001-9910-1319; Perić, Zoran M./0000-0003-0116-8895; Radaković, Milica G./0000-0002-5916-4187; Hao, Qingzhen/0000-0002-6281-5817; Lukić, Tin/0000-0001-5398-0928; Antić, Aleksandar/0000-0002-6973-7671; Sipos, György/0000-0001-6224-2361}
}

@article{MTMT:33784551,
	title = {Reconstructed Malacothermometer July Paleotemperatures from the Last Nine Glacials over the South-Eastern Carpathian Basin (Serbia)},
	url = {https://m2.mtmt.hu/api/publication/33784551},
	author = {Radaković, MG. and Oches, EA. and Hughes, PD. and Marković, RS. and Hao, Q and Perić, ZM. and Gavrilović, B and Ludwig, P and Lukić, T and Gavrilov, MB. and Marković, SB.},
	doi = {10.3390/atmos14050791},
	journal-iso = {ATMOSPHERE-BASEL},
	journal = {ATMOSPHERE},
	volume = {14},
	unique-id = {33784551},
	abstract = {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.},
	keywords = {Serbia; loess; Middle Pleistocene; malacofauna; Titel loess plateau; July temperature; Veliki Surduk; Stari Slankamen},
	year = {2023},
	eissn = {2073-4433}
}

@article{MTMT:32596596,
	title = {The provenance of Danubian loess},
	url = {https://m2.mtmt.hu/api/publication/32596596},
	author = {Fenn, K and Millar, I L and Durcan, J A and Thomas, D S G and Banak, A and Marković, S B and Veres, D and Stevens, Th},
	doi = {10.1016/j.earscirev.2022.103920},
	journal-iso = {EARTH-SCI REV},
	journal = {EARTH-SCIENCE REVIEWS},
	volume = {226},
	unique-id = {32596596},
	issn = {0012-8252},
	year = {2022},
	eissn = {1872-6828}
}

@article{MTMT:33034354,
	title = {Study of hanging valley in loess-paleosoil sediments with soil erosion assessment using nuclear and erosion potential methods},
	url = {https://m2.mtmt.hu/api/publication/33034354},
	author = {Kalkan, K and Forkapic, S and Markovic, S and Bikit, K and Tosic, R and Mrdja, D and Milentijevic, N},
	doi = {10.2298/NTRP2201065K},
	journal-iso = {NUCL TECHNOL RADIAT},
	journal = {NUCLEAR TECHNOLOGY & RADIATION PROTECTION},
	volume = {37},
	unique-id = {33034354},
	issn = {1451-3994},
	year = {2022},
	eissn = {1452-8185},
	pages = {65-77},
	orcid-numbers = {Markovic, S/0000-0002-4977-634X}
}

@article{MTMT:33036742,
	title = {Detailed luminescence dating of dust mass accumulation rates over the last two glacial-interglacial cycles from the Irig loess-palaeosol sequence, Carpathian Basin},
	url = {https://m2.mtmt.hu/api/publication/33036742},
	author = {Perić, ZM. and Stevens, T and Obreht, I and Hambach, U and Lehmkuhl, Frank and Marković, SB.},
	doi = {10.1016/j.gloplacha.2022.103895},
	journal-iso = {GLOBAL PLANET CHANGE},
	journal = {GLOBAL AND PLANETARY CHANGE},
	volume = {215},
	unique-id = {33036742},
	issn = {0921-8181},
	abstract = {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)},
	keywords = {LUMINESCENCE; Soil moisture; Soil moisture; SEDIMENTS; STRATIGRAPHY; PLEISTOCENE; Quaternary; Quaternary; Grain size and shape; chronology; DUST; Magnetic susceptibility; Magnetic susceptibility; Glacial geology; Carpathian Basin; Serbia; Serbia; paleosol; marine isotope stage; loess; loess; loess; luminescence dating; MINERAL DUST; MINERAL DUST; MINERAL DUST; Moisture control; VOJVODINA; OSL; OSL; Loess-palaeosol sequences; Geoaccumulation; dust sources; dendrochronology; Glacial-interglacial cycle; Glacial-interglacial cycles; Serbium; Mass accumulation rates; pIRIR290; pIRIR290},
	year = {2022},
	eissn = {1872-6364}
}

@article{MTMT:31636099,
	title = {Initial quartz OSL and dust mass accumulation rate investigation of the Kisiljevo loess sequence in north-eastern Serbia},
	url = {https://m2.mtmt.hu/api/publication/31636099},
	author = {Perić, ZM. and Marković, SB. and Avram, A and Timar-Gabor, A and Zeeden, C and Nett, JJ. and Fischer, P and Fitzsimmons, KE. and Gavrilov, MB.},
	doi = {10.1016/j.quaint.2020.10.040},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {620},
	unique-id = {31636099},
	issn = {1040-6182},
	year = {2022},
	eissn = {1873-4553},
	pages = {13-23},
	orcid-numbers = {Perić, ZM./0000-0003-0116-8895; Avram, A/0000-0002-6631-311X; Nett, JJ./0000-0001-8431-0484; Fitzsimmons, KE./0000-0002-9337-0793}
}

@article{MTMT:32544836,
	title = {Vegetation and land snail-based reconstruction of the palaeocological changes in the forest steppe eco-region of the Carpathian Basin during last glacial warming},
	url = {https://m2.mtmt.hu/api/publication/32544836},
	author = {Sümegi, Pál and Molnár, Dávid and Náfrádi, Katalin and Makó, László and Cseh, Péter and Törőcsik, Tünde and Molnár, Mihály and Zhou, Liping},
	doi = {10.1016/j.gecco.2021.e01976},
	journal-iso = {GLOB ECOL CONSERV},
	journal = {GLOBAL ECOLOGY AND CONSERVATION},
	volume = {33},
	unique-id = {32544836},
	issn = {2351-9894},
	year = {2022},
	eissn = {2351-9894},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741}
}

@article{MTMT:32102652,
	title = {Revised map of European aeolian deposits derived from soil texture data},
	url = {https://m2.mtmt.hu/api/publication/32102652},
	author = {Bertran, P and Bosq, M and Borderie, Q and Coussot, C and Coutard, S and Deschodt, L and Franc, O and Gardère, P and Liard, M and Wuscher, P},
	doi = {10.1016/j.quascirev.2021.107085},
	journal-iso = {QUATERN SCI REV},
	journal = {QUATERNARY SCIENCE REVIEWS},
	volume = {266},
	unique-id = {32102652},
	issn = {0277-3791},
	keywords = {Europe; loess; cartography; coversand stratigraphy; LUCAS 2009 topsoil database},
	year = {2021},
	eissn = {1873-457X},
	orcid-numbers = {Bertran, P/0000-0003-3334-9869; Bosq, M/0000-0003-0963-212X; Borderie, Q/0000-0002-2199-4038}
}

@article{MTMT:32173613,
	title = {Vivianite formation as indicator of human impact in porous sediments},
	url = {https://m2.mtmt.hu/api/publication/32173613},
	author = {Csámer, Árpád and Papp, Lajos and Kristály, Ferenc and Szakáll, Sándor and Rózsa, Péter},
	doi = {10.1007/s12665-021-09866-2},
	journal-iso = {ENVIRON EARTH SCI},
	journal = {ENVIRONMENTAL EARTH SCIENCES},
	volume = {80},
	unique-id = {32173613},
	issn = {1866-6280},
	abstract = {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.},
	keywords = {GROUNDWATER; Vivanite; Organic debris; Orthophosphate release; Human-induced mineralization},
	year = {2021},
	eissn = {1866-6299},
	orcid-numbers = {Csámer, Árpád/0000-0003-2374-2413; Kristály, Ferenc/0000-0002-0075-5994; Rózsa, Péter/0000-0002-6820-3563}
}

@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:32057844,
	title = {Clay mineralogy of the Stari Slankamen (Serbia) loess-paleosol sequence during the last glacial cycle — Implications for dust provenance and interglacial climate},
	url = {https://m2.mtmt.hu/api/publication/32057844},
	author = {Fu, Y and Hao, Q and Peng, S and Markovic, SB and Gao, X and Han, L and Wu, X and Namier, N and Zhang, W and Gavrilov, MB and Markovic, R and Guo, Z},
	doi = {10.1016/j.quascirev.2021.106990},
	journal-iso = {QUATERN SCI REV},
	journal = {QUATERNARY SCIENCE REVIEWS},
	volume = {263},
	unique-id = {32057844},
	issn = {0277-3791},
	year = {2021},
	eissn = {1873-457X}
}

@mastersthesis{MTMT:32911094,
	title = {Primena radioaktivnih metoda u geomorfološkim istraživanjima Titelskog brega [Application of radioactive methods in geomorphological research of Titelski breg]},
	url = {https://m2.mtmt.hu/api/publication/32911094},
	isbn = {9798762123068},
	author = {Kalkan, K},
	publisher = {Univerzitet u Novom Sadu},
	unique-id = {32911094},
	year = {2021}
}

@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:32009766,
	title = {Malaco temperature reconstructions and numerical simulation of environmental conditions in the southeastern Carpathian Basin during the Last Glacial Maximum},
	url = {https://m2.mtmt.hu/api/publication/32009766},
	author = {Ludwig, P and Gavrilov, MB and Radakovic, MG and Markovic, SB},
	doi = {10.1002/jqs.3318},
	journal-iso = {J QUATERNARY SCI},
	journal = {JOURNAL OF QUATERNARY SCIENCE},
	volume = {36},
	unique-id = {32009766},
	issn = {0267-8179},
	year = {2021},
	eissn = {1099-1417},
	pages = {1426-1435}
}

@article{MTMT:31969595,
	title = {Simulated regional dust cycle in the Carpathian Basin and the Adriatic Sea region during the Last Glacial Maximum},
	url = {https://m2.mtmt.hu/api/publication/31969595},
	author = {Ludwig, P and Gavrilov, MB and Markovic, SB and Újvári, Gábor and Lehmkuhl, F.},
	doi = {10.1016/j.quaint.2020.09.048},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {581-582},
	unique-id = {31969595},
	issn = {1040-6182},
	year = {2021},
	eissn = {1873-4553},
	pages = {114-127},
	orcid-numbers = {Újvári, Gábor/0000-0002-2816-6155}
}

@article{MTMT:31678166,
	title = {Geomorphological evolution of the Petrovaradin Fortress Palaeolithic site (Novi Sad, Serbia)},
	url = {https://m2.mtmt.hu/api/publication/31678166},
	author = {Markovic, SB. and Vandenberghe, J and Stevens, T and Mihailovic, D and Gavrilov, MB. and Radakovic, MG. and Zeeden, C and Obreht, I and Peric, ZM. and Nett, JJ. and Lehmkuhl, F},
	doi = {10.1017/qua.2020.88},
	journal-iso = {QUATERNARY RES},
	journal = {QUATERNARY RESEARCH},
	volume = {103},
	unique-id = {31678166},
	issn = {0033-5894},
	abstract = {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.},
	keywords = {Danube; loess; Last glacial; Paleolithic; Petrovaradin; Tectonic uplift; Fruska Gora Mountain},
	year = {2021},
	eissn = {1096-0287},
	pages = {21-34}
}

@article{MTMT:32062161,
	title = {The Požarevac loess–paleosol sequence: a record of increased aridity in the south‐eastern margin of the Carpathian Basin during the last 350 ka},
	url = {https://m2.mtmt.hu/api/publication/32062161},
	author = {Marković, SB. and Oches, EA. and Perić, ZM. and Gaudenyi, T and Jovanović, M and Sipos, Gy and Thiel, C and Buylaert, JP and Savić, S and McCoy, WD. and Radaković, MG. and Marković, RS. and Gavrilov, MB.},
	doi = {10.1002/jqs.3327},
	journal-iso = {J QUATERNARY SCI},
	journal = {JOURNAL OF QUATERNARY SCIENCE},
	volume = {36},
	unique-id = {32062161},
	issn = {0267-8179},
	abstract = {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.},
	year = {2021},
	eissn = {1099-1417},
	pages = {1436-1447},
	orcid-numbers = {Marković, SB./0000-0002-4977-634X; Oches, EA./0000-0001-6930-7017; Perić, ZM./0000-0003-0116-8895; Gaudenyi, T/0000-0002-1843-2384; Thiel, C/0000-0003-1671-9987; Buylaert, JP/0000-0003-0587-8077; Savić, S/0000-0002-4297-129X; Radaković, MG./0000-0002-5916-4187}
}

@article{MTMT:32151522,
	title = {Quartz OSL and polymineral post IR–IRSL dating of the Požarevac loess–palaeosol sequence in north–eastern Serbia},
	url = {https://m2.mtmt.hu/api/publication/32151522},
	author = {Perić, ZM. and Marković, SB. and Filyó, Dávid and Thiel, C and Murray, AS. and Gavrilov, MB. and Nett, JJ. and Sipos, György},
	doi = {10.1016/j.quageo.2021.101216},
	journal-iso = {QUAT GEOCHRONOL},
	journal = {QUATERNARY GEOCHRONOLOGY},
	volume = {66},
	unique-id = {32151522},
	issn = {1871-1014},
	year = {2021},
	eissn = {1878-0350},
	orcid-numbers = {Perić, ZM./0000-0003-0116-8895; Thiel, C/0000-0003-1671-9987; Nett, JJ./0000-0001-8431-0484; Sipos, György/0000-0001-6224-2361}
}

@article{MTMT:32036727,
	title = {Disentangling Sedimentary Pathways for the Pleniglacial Lower Danube Loess Based on Geochemical Signatures},
	url = {https://m2.mtmt.hu/api/publication/32036727},
	author = {Potter, S and Veres, D and Baykal, Y and Nett, JJ and Schulte, P and Hambach, U and Lehmkuhl, F},
	doi = {10.3389/feart.2021.600010},
	journal-iso = {FRONT EARTH SC-SWITZ},
	journal = {FRONTIERS IN EARTH SCIENCE},
	volume = {9},
	unique-id = {32036727},
	year = {2021},
	eissn = {2296-6463}
}

@article{MTMT:31626828,
	title = {Middle to Late Pleistocene environments based on stable organic carbon and nitrogen isotopes of loess‐palaeosol sequences from the Carpathian Basin},
	url = {https://m2.mtmt.hu/api/publication/31626828},
	author = {Pötter, S and Schmitz, A and Lücke, A and Schulte, P and Obreht, I and Zech, M and Wissel, H and Marković, SB. and Lehmkuhl, F},
	doi = {10.1111/bor.12470},
	journal-iso = {BOREAS},
	journal = {BOREAS},
	volume = {50},
	unique-id = {31626828},
	issn = {0300-9483},
	year = {2021},
	eissn = {1502-3885},
	pages = {184-204},
	orcid-numbers = {Pötter, S/0000-0003-0059-5270; Lehmkuhl, F/0000-0002-6876-7377}
}

@article{MTMT:31908801,
	title = {Magnetic Susceptibility Properties of Loess From the Willendorf Archaeological Site: Implications for the Syn/Post-Depositional Interpretation of Magnetic Fabric},
	url = {https://m2.mtmt.hu/api/publication/31908801},
	author = {Zeeden, C and Hambach, U},
	doi = {10.3389/feart.2020.599491},
	journal-iso = {FRONT EARTH SC-SWITZ},
	journal = {FRONTIERS IN EARTH SCIENCE},
	volume = {8},
	unique-id = {31908801},
	year = {2021},
	eissn = {2296-6463}
}

@article{MTMT:32006908,
	title = {Sedimentology of a Late Quaternary lacustrine record from the south‐eastern Carpathian Basin},
	url = {https://m2.mtmt.hu/api/publication/32006908},
	author = {Zeeden, C and Hambach, U and Klasen, N and Fischer, P and Schulte, P and Nett, JJ. and Veres, D and Obreht, I and Chu, W and Papadopoulou, M and Viehberg, F and SchÄBitz, F and Gavrilov, MB. and Markovic, SB. and Vött, A and Lehmkuhl, F},
	doi = {10.1002/jqs.3297},
	journal-iso = {J QUATERNARY SCI},
	journal = {JOURNAL OF QUATERNARY SCIENCE},
	volume = {36},
	unique-id = {32006908},
	issn = {0267-8179},
	year = {2021},
	eissn = {1099-1417},
	pages = {1414-1425},
	orcid-numbers = {Zeeden, C/0000-0002-8617-0443; Fischer, P/0000-0002-8410-5824; Nett, JJ./0000-0001-8431-0484; Veres, D/0000-0003-3932-577X; Chu, W/0000-0002-4595-388X; Viehberg, F/0000-0003-0253-2222}
}

@article{MTMT:30817326,
	title = {An overview of Alpine and Mediterranean palaeogeography, terrestrial ecosystems and climate history during MIS 3 with focus on the Middle to Upper Palaeolithic transition},
	url = {https://m2.mtmt.hu/api/publication/30817326},
	author = {Badino, F and Pini, R and Ravazzi, C and Margaritora, D and Arrighi, S and Bortolini, E and Figus, C and Giaccio, B and Lugli, F and Marciani, G and Monegato, G and Moroni, A and Negrino, F and Oxilia, G and Peresani, M and Romandini, M and Ronchitelli, A and Spinapolice, EE. and Zerboni, A and Benazzi, S},
	doi = {10.1016/j.quaint.2019.09.024},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {551},
	unique-id = {30817326},
	issn = {1040-6182},
	year = {2020},
	eissn = {1873-4553},
	pages = {7-28},
	orcid-numbers = {Negrino, F/0000-0001-7539-2959}
}

@article{MTMT:31277488,
	title = {Interpretation of sedimentary subpopulations extracted from grain size distributions in loess deposits at the Sea of Azov, Russia},
	url = {https://m2.mtmt.hu/api/publication/31277488},
	author = {Chen, J. and Yang, T. and Qiang, M. and Matishov, G.G. and Velichko, A.A. and Zeng, B. and Xu, M. and Shi, P.},
	doi = {10.1016/j.aeolia.2020.100597},
	journal-iso = {AEOLIAN RES},
	journal = {AEOLIAN RESEARCH},
	volume = {45},
	unique-id = {31277488},
	issn = {1875-9637},
	year = {2020},
	eissn = {2212-1684}
}

@article{MTMT:31498579,
	title = {State of the Art in Paleoenvironment Mapping for Modeling Applications in Archeology-Summary, Conclusions, and Future Directions from the PaleoMaps Workshop},
	url = {https://m2.mtmt.hu/api/publication/31498579},
	author = {Willmes, Christian and Niedziolka, Kamil and Serbe, Benjamin and Grimm, Sonja B. and Gross, Daniel and Miebach, Andrea and Marker, Michael and Henselowsky, Felix and Gamisch, Alexander and Rostami, Masoud and Mateos, Ana and Rodriguez, Jesus and Limberg, Heiko and Schmidt, Isabell and Mueller, Martin and Hoelzchen, Ericson and Holthausen, Michael and Klein, Konstantin and Wegener, Christian and Weninger, Bernhard and Nielsen, Trine Kellberg and Otto, Taylor and Weniger, Gerd-Christian and Bubenzer, Olaf and Bareth, Georg},
	doi = {10.3390/quat3020013},
	journal-iso = {Quaternary},
	journal = {QUATERNARY},
	volume = {3},
	unique-id = {31498579},
	issn = {2571-550X},
	abstract = {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.},
	keywords = {open science; Paleoclimate modeling; Human-environment interaction; paleoenvironment reconstruction; paleoenvironment modeling; archeological modeling},
	year = {2020},
	orcid-numbers = {Serbe, Benjamin/0000-0001-5134-758X; Gross, Daniel/0000-0002-1328-1134; Mateos, Ana/0000-0002-0676-9836; Rodriguez, Jesus/0000-0002-2834-0694; Otto, Taylor/0000-0002-1717-7879}
}

@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:30613177,
	title = {Loess2M - Modelling and Mapping},
	url = {https://m2.mtmt.hu/api/publication/30613177},
	author = {Hao, Q. and Zeeden, C. and Moska, P. and Tomić, N.},
	doi = {10.1016/j.quaint.2019.02.030},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {502},
	unique-id = {30613177},
	issn = {1040-6182},
	year = {2019},
	eissn = {1873-4553},
	pages = {1-3}
}

@article{MTMT:30429893,
	title = {A critical reevaluation of palaeoclimate proxy records from loess in the Carpathian Basin},
	url = {https://m2.mtmt.hu/api/publication/30429893},
	author = {Obreht, I. and Zeeden, C. and Hambach, U. and Veres, D. and Marković, S.B. and Lehmkuhl, F.},
	doi = {10.1016/j.earscirev.2019.01.020},
	journal-iso = {EARTH-SCI REV},
	journal = {EARTH-SCIENCE REVIEWS},
	volume = {190},
	unique-id = {30429893},
	issn = {0012-8252},
	year = {2019},
	eissn = {1872-6828},
	pages = {498-520}
}

@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}
}