@article{MTMT:34019976,
	title = {Late Pleistocene to Holocene Palaeohydrological History of the Thermal-Spring-Fed Lake Pețea (NW Romania) Revealed by Radiocarbon Dating and Complex Sedimentological Investigations},
	url = {https://m2.mtmt.hu/api/publication/34019976},
	author = {Gulyás, Sándor and Sümegi, Pál},
	doi = {10.3390/quat6020037},
	journal-iso = {Quaternary},
	journal = {QUATERNARY},
	volume = {6},
	unique-id = {34019976},
	issn = {2571-550X},
	abstract = {Understanding sedimentation processes in response to past hydrogeological and climatic changes and capturing millennial-scale variations is a key focus of lacustrine paleoenvironmental research. This study presents the first high-resolution chronology and sedimentary data for the small thermal-spring-fed Lake Pețea, NW Romania, and unravels the evolutionary history of the lake harboring a unique endemic fauna. Its small size and single source of water make it particularly sensitive to hydrological changes. In the recent past, over-exploitation of the thermal water has led to the complete drying up of the lake and the extinction of its fauna. Nevertheless, past spatio-temporal variation of environmental factors, in particular the fluctuation of lake levels and water temperature, must have had a significant impact on the survival and evolution of the endemic mollusk fauna. This fact makes this study particularly important. Based on our results, a three-stage sedimentary evolution occurred, mainly controlled by major climate-driven hydrological changes also seen in regional records, i.e., 17.5–14.5 ka shallow eutrophic lake, 14.5–5.5 ka oligotrophic carbonate-rich lake, and 5.5–0.5 ka shallow eutrophic lake. A major lowstand at 11.7–10.2 ka due to drier climate was followed by progressively rising water levels up to 5 ka followed by a drop. The main control on lake level fluctuations and sedimentary phases was the varying input of thermal water due to recurring increased/decreased recharge of the underground shallow karst water system. The driving factor of thermal water discharge was different during the Late Glacial than the Holocene. It was the warming of the climate at 14.5 ka cal BP and melting of regional ice sheets in addition to increased precipitation that created an oligotrophic lake by recharging the underground thermal water system. Conversely, during the Holocene, increasing/decreasing moisture availability driven by major climate forcings was in control of thermal water recharge, erosion, and fluctuating lake levels.},
	year = {2023},
	orcid-numbers = {Gulyás, Sándor/0000-0002-3384-2381; Sümegi, Pál/0000-0003-1755-4440}
}

@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:32776652,
	title = {Geoarchaeological Analyses of a Late-Copper-Age Kurgan on the Great Hungarian Plain},
	url = {https://m2.mtmt.hu/api/publication/32776652},
	author = {Cseh, Péter and Molnár, Dávid and Makó, László and Sümegi, Pál},
	doi = {10.3390/quat5020020},
	journal-iso = {Quaternary},
	journal = {QUATERNARY},
	volume = {5},
	unique-id = {32776652},
	issn = {2571-550X},
	year = {2022},
	orcid-numbers = {Molnár, Dávid/0000-0001-5304-0741; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:32596336,
	title = {Tackling erosion-accumulation events in a moat sequence from a unique Ottoman memorial place (Szigetvár, SW Hungary) using 14C and geoarcheological data},
	url = {https://m2.mtmt.hu/api/publication/32596336},
	author = {Gulyás, Sándor and Torma, Andrea and Pap, Norbert and Fodor, Pál and Kitanics, Máté and Gyenizse, Péter and Molnár, Mihály and Sümegi, Pál},
	doi = {10.1007/s12520-021-01479-x},
	journal-iso = {ARCHAEO ANTHROP SCI},
	journal = {ARCHAEOLOGICAL AND ANTHROPOLOGICAL SCIENCES},
	volume = {14},
	unique-id = {32596336},
	issn = {1866-9557},
	year = {2022},
	eissn = {1866-9565},
	orcid-numbers = {Gulyás, Sándor/0000-0002-3384-2381; Pap, Norbert/0000-0001-8243-4213; Kitanics, Máté/0000-0003-0073-7451; Gyenizse, Péter/0000-0002-8175-9734; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:33240955,
	title = {Comparison of High-Resolution 14C and Luminescence-Based Chronologies of the MIS 2 Madaras Loess/Paleosol Sequence, Hungary: Implications for Chronological Studies},
	url = {https://m2.mtmt.hu/api/publication/33240955},
	author = {Sümegi, Pál and Molnár, Dávid and Gulyás, Sándor and Stevens, T and Makó, László and Cseh, P and Molnár, Mihály and Fitzsimmons, K and Nett, JJ. and Hlavatskyi, D and Lehmkuhl, F},
	doi = {10.3390/quat5040047},
	journal-iso = {Quaternary},
	journal = {QUATERNARY},
	volume = {5},
	unique-id = {33240955},
	issn = {2571-550X},
	abstract = {Numerous loess/paleosol sequences (LPS) in the Carpathian Basin span the period of Marine Isotope Stage (MIS) 2 and the last glacial maximum (LGM). Nevertheless, only two known records—Madaras and Dunaszekcső—preserve highly resolved records with absolute chronologies with minimal uncertainties, which enable the meaningful assessment of feedbacks and short-term climatic fluctuations over this period. The Madaras profile is located at the northern margin fringe of the Bácska loess plateau; Dunaszekcső, located on the Danube to its west, yields a chronology built on over 100 14C dates yet spans only part of MIS 2, missing half of the LGM including its peak. Here, we add to the previously published 14C chronology for Madaras (15 dates) with an additional 17 14C and luminescence ages. Resulting age models built solely on quartz OSL and feldspar pIRIRSL data underestimate the 14C based chronology, which is likely based on inaccuracies related to luminescence signal behavior; we observe age underestimations associated with unusual quartz behavior and significant signal loss, a phenomenon also observed in Serbian and Romanian loess, which may relate to non-sensitized grains from proximal sources. Our new chronology provides higher resolution than hitherto possible, yielding consistent 2 sigma uncertainties of ~150–200 years throughout the entire sequence. Our study indicates that the addition of further dates may not increase the chronological precision significantly. Additionally, the new age model is suitable for tackling centennial-scale changes. The mean sedimentation rate based on our new age-depth model (10.78 ± 2.34 years/cm) is the highest yet recorded in the Carpathian Basin for MIS 2. The resolution of our age model is higher than that for the Greenland NGRIP ice core record. The referred horizons in our profile are all characterized by a drop in accumulation and a higher sand input, the latter most likely deriving from nearby re-exposed sand dunes.},
	year = {2022},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741; Gulyás, Sándor/0000-0002-3384-2381; Stevens, T/0000-0002-6662-6650; Hlavatskyi, D/0000-0002-9901-7827}
}

@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:32474023,
	title = {Take a seed! Revealing Neolithic landscape and agricultural development in the Carpathian Basin through multivariate statistics and environmental modelling},
	url = {https://m2.mtmt.hu/api/publication/32474023},
	author = {Kempf, M},
	doi = {10.1371/journal.pone.0258206},
	journal-iso = {PLOS ONE},
	journal = {PLOS ONE},
	volume = {16},
	unique-id = {32474023},
	issn = {1932-6203},
	year = {2021},
	eissn = {1932-6203},
	orcid-numbers = {Kempf, M/0000-0002-9474-4670}
}

@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: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:32058723,
	title = {Some notes on the interpretation and reliability of malacological proxies in paleotemperature reconstructions from loess- comments to Obreht et al.'s “A critical reevaluation of paleoclimate proxy records from loess in the Carpathian Basin”},
	url = {https://m2.mtmt.hu/api/publication/32058723},
	author = {Sümegi, Pál and Gulyás, Sándor},
	doi = {10.1016/j.earscirev.2021.103675},
	journal-iso = {EARTH-SCI REV},
	journal = {EARTH-SCIENCE REVIEWS},
	volume = {221},
	unique-id = {32058723},
	issn = {0012-8252},
	year = {2021},
	eissn = {1872-6828},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Gulyás, Sándor/0000-0002-3384-2381}
}

@article{MTMT:32471189,
	title = {New chronology and extended palaeoenvironmental data to the 1975 loess profile of Madaras brickyard, South Hungary},
	url = {https://m2.mtmt.hu/api/publication/32471189},
	author = {Sümegi, Pál and Gulyás, Sándor and Molnár, Dávid and Bozsó, Gábor and Fekete, István and Makó, László and Cseh, Péter and Molnár, Mihály and Sümegi, Balázs P. and Almond, Peter and Zeeden, Christian and Törőcsik, Tünde and Nett, Janina J. and Markó, András and Lehmkuhl, Frank},
	doi = {10.1002/jqs.3382},
	journal-iso = {J QUATERNARY SCI},
	journal = {JOURNAL OF QUATERNARY SCIENCE},
	volume = {36},
	unique-id = {32471189},
	issn = {0267-8179},
	year = {2021},
	eissn = {1099-1417},
	pages = {1364-1381},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Gulyás, Sándor/0000-0002-3384-2381; Molnár, Dávid/0000-0001-5304-0741; Zeeden, Christian/0000-0002-8617-0443; Nett, Janina J./0000-0001-8431-0484; Markó, András/0000-0002-7556-0091}
}

@article{MTMT:32064831,
	title = {Sedimentological-Geochemical Data Based Reconstruction of Climate Changes and Human Impacts from the Peat Sequence of Round Lake in the Western Foothill Area of the Eastern Carpathians, Romania},
	url = {https://m2.mtmt.hu/api/publication/32064831},
	author = {Tapody, Réka Orsolya and Sümegi, Pál and Molnár, Dávid and Karlik, Máté and Törőcsik, Tünde and Cseh, Péter and Makó, László},
	doi = {10.3390/quat4020018},
	journal-iso = {Quaternary},
	journal = {QUATERNARY},
	volume = {4},
	unique-id = {32064831},
	issn = {2571-550X},
	year = {2021},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741}
}

@article{MTMT:30757439,
	title = {The Middle and Late Pleniglacial (Weichselian) malacofauna of the Zemun loess–paleosol sequence, Serbia},
	url = {https://m2.mtmt.hu/api/publication/30757439},
	author = {Gavrilović, B and Sümegi, Pál and Ćirić, M and Radaković, MG. and Gavrilov, MB. and Mlađan, D and Marković, SB.},
	doi = {10.1007/s12542-019-00465-y},
	journal-iso = {PALAEONTOL Z},
	journal = {PALAEONTOLOGISCHE ZEITSCHRIFT},
	volume = {94},
	unique-id = {30757439},
	issn = {0031-0220},
	abstract = {The aim of our study was to describe the succession of malacological assemblages along the exposed loess profile located in Belgrade, along the banks of the Danube River (municipality of Zemun). Deposits that belong to the composite loess unit L1 were sampled. Loess unit L1 included two subunits: L1SS1 (a Middle Pleniglacial subunit with two weakly developed initial pedogenic horizons) and L1LL1 (a Late Pleniglacial loess subunit). Three malacological zones were distinguished. Malacological results imply a change in climatic conditions and subsequently in vegetation structure. The molluscs indicate an environment with a moderate (warm and dry) climate and a mosaic vegetation type composed of grasslands and forest steppe. Gradual cooling was inferred within the Late Pleniglacial period. Our findings concur with the results of earlier studies indicating that the Zemun site and the adjacent area served as a transition zone between the refuge areas within the southeastern part of the Carpathian Basin during the Late Pleistocene.},
	year = {2020},
	eissn = {1867-6812},
	pages = {519-531},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:31124193,
	title = {14C Dated Chronology of the Thickest and Best Resolved Loess/Paleosol Record of the LGM from SE Hungary Based on Comparing Precision and Accuracy of Age-Depth Models},
	url = {https://m2.mtmt.hu/api/publication/31124193},
	author = {Sümegi, Pál and Gulyás, Sándor and Molnár, Dávid and Szilágyi, Gábor and Sümegi, Balázs P and Törőcsik, Tünde and Molnár, Mihály},
	doi = {10.1017/RDC.2019.154},
	journal-iso = {RADIOCARBON},
	journal = {RADIOCARBON},
	volume = {62},
	unique-id = {31124193},
	issn = {0033-8222},
	year = {2020},
	eissn = {1945-5755},
	pages = {403-417},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Gulyás, Sándor/0000-0002-3384-2381; Molnár, Dávid/0000-0001-5304-0741; Molnár, Mihály/0000-0003-4382-9508}
}

@article{MTMT:3361435,
	title = {High-resolution proxy record of the environmental response to climatic variations during transition MIS3/MIS2 and MIS2 in Central Europe. the loess-paleosol sequence of Katymár brickyard (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/3361435},
	author = {Sümegi, Pál and Molnár, Dávid and Gulyás, Sándor and Náfrádi, Katalin and Sümegi, B P and Törőcsik, Tünde and Persaits, G and Molnár, Mihály and Vandenberghe, J and Zhou, L},
	doi = {10.1016/j.quaint.2018.03.030},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {504},
	unique-id = {3361435},
	issn = {1040-6182},
	year = {2019},
	eissn = {1873-4553},
	pages = {40-55},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741; Gulyás, Sándor/0000-0002-3384-2381}
}

@article{MTMT:30741579,
	title = {Environmental history of the Csorna plain (Western Danube plain, NW Hungary) from the late glacial to the late Holocene as seen from data of multiproxy geoarchaeological investigations},
	url = {https://m2.mtmt.hu/api/publication/30741579},
	author = {Törőcsik, Tünde and Gulyás, Sándor and Sümegi, Pál and Sümegi, B and Molnár, Dávid and Benyó-Korcsmáros, Réka},
	doi = {10.24425/sq.2019.126377},
	journal-iso = {STUD QUATER},
	journal = {STUDIA QUATERNARIA},
	volume = {36},
	unique-id = {30741579},
	issn = {1641-5558},
	year = {2019},
	eissn = {2300-0384},
	pages = {19-43},
	orcid-numbers = {Gulyás, Sándor/0000-0002-3384-2381; Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741}
}

@article{MTMT:27595356,
	title = {The Danube Corridor Hypothesis and the Carpathian Basin: Geological, Environmental and Archaeological Approaches to Characterizing Aurignacian Dynamics},
	url = {https://m2.mtmt.hu/api/publication/27595356},
	author = {Chu, W},
	doi = {10.1007/s10963-018-9115-1},
	journal-iso = {J WORLD PREHIST},
	journal = {JOURNAL OF WORLD PREHISTORY},
	volume = {31},
	unique-id = {27595356},
	issn = {0892-7537},
	year = {2018},
	eissn = {1573-7802},
	pages = {117-178}
}

@article{MTMT:3298855,
	title = {Investigating the last glacial Gravettian site ‘Ságvár Lyukas Hill’ (Hungary) and its paleoenvironmental and geochronological context using a multi-proxy approach},
	url = {https://m2.mtmt.hu/api/publication/3298855},
	author = {Janina, Bösken and Sümegi, Pál and Christian, Zeeden and Nicole, Klasen and Gulyás, Sándor and Frank, Lehmkuhl},
	doi = {10.1016/j.palaeo.2017.08.010},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {509},
	unique-id = {3298855},
	issn = {0031-0182},
	year = {2018},
	eissn = {1872-616X},
	pages = {77-90},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Gulyás, Sándor/0000-0002-3384-2381}
}

@article{MTMT:3374753,
	title = {New chronology of the best developed loess/paleosol sequence of Hungary capturing the past 1.1 ma. Implications for correlation and proposed pan-Eurasian stratigraphic schemes},
	url = {https://m2.mtmt.hu/api/publication/3374753},
	author = {Sümegi, Pál and Gulyás, Sándor and Molnár, Dávid and Sümegi, B P and Almond, P C and Vandenberghe, J and Zhou, L and Pál-Molnár, Elemér and Törőcsik, Tünde and Hao, Q and Smalley, I and Molnár, Mihály and Marsi, István},
	doi = {10.1016/j.quascirev.2018.04.012},
	journal-iso = {QUATERN SCI REV},
	journal = {QUATERNARY SCIENCE REVIEWS},
	volume = {191},
	unique-id = {3374753},
	issn = {0277-3791},
	year = {2018},
	eissn = {1873-457X},
	pages = {144-166},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Gulyás, Sándor/0000-0002-3384-2381; Molnár, Dávid/0000-0001-5304-0741; Pál-Molnár, Elemér/0000-0002-9606-0133}
}

@article{MTMT:30330204,
	title = {Revision of the Age of Construction Phases of a Mound Dated to the Late Copper–Early Bronze Age in Eastern Hungary Relying on 14C-Based Chronologies},
	url = {https://m2.mtmt.hu/api/publication/30330204},
	author = {Szilágyi, Gábor and Sümegi, Pál and Gulyás, Sándor and Molnár, Dávid},
	doi = {10.1017/RDC.2018.107},
	journal-iso = {RADIOCARBON},
	journal = {RADIOCARBON},
	volume = {60},
	unique-id = {30330204},
	issn = {0033-8222},
	year = {2018},
	eissn = {1945-5755},
	pages = {1403-1412},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Gulyás, Sándor/0000-0002-3384-2381; Molnár, Dávid/0000-0001-5304-0741}
}

@article{MTMT:3388045,
	title = {Radiocarbon-dated peat development. anthropogenic and climatic signals in a Holocene raised bog and lake profile from the Eastern part of the Carpathian Basin},
	url = {https://m2.mtmt.hu/api/publication/3388045},
	author = {Tapody, Réka Orsolya and Gulyás, Sándor and Törőcsik, Tünde and Sümegi, Pál and Molnár, Dávid and Sümegi, B P and Molnár, Mihály},
	doi = {10.1017/RDC.2018.38},
	journal-iso = {RADIOCARBON},
	journal = {RADIOCARBON},
	volume = {60},
	unique-id = {3388045},
	issn = {0033-8222},
	year = {2018},
	eissn = {1945-5755},
	pages = {1215-1226},
	orcid-numbers = {Gulyás, Sándor/0000-0002-3384-2381; Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741}
}

@article{MTMT:30338111,
	title = {Probabilistic 14C Age-Depth Models Aiding the Reconstruction of Holocene Paleoenvironmental Evolution of a Marshland from Southern Hungary},
	url = {https://m2.mtmt.hu/api/publication/30338111},
	author = {Törőcsik, Tünde and Gulyás, Sándor and Molnár, Dávid and Tapody, Réka Orsolya and Sümegi, BP and Szilágyi, Gábor and Molnár, Mihály and Jakab, Gusztáv and Sümegi, Pál and Novák, Zsolt},
	doi = {10.1017/RDC.2018.112},
	journal-iso = {RADIOCARBON},
	journal = {RADIOCARBON},
	volume = {60},
	unique-id = {30338111},
	issn = {0033-8222},
	abstract = {This paper presents first chronological results for a Holocene marshland system from the southern part of the Danube-Tisza Interfluve. Radiocarbon (C-14) ages were used to build age-depth models relying of probabilistic tools. Four models have been built: a linear one using dates gained via simple calibration, a P_Sequence model, fitting a polynomial function to calibrated dates; a Gamma_Sequence considering priori given and posterior accumulation rates have been constructed. As there was no significant difference between the mean values of individual models all seem suitable for establishing a reliable chronology despite differences in 95% CI ranges. While P_Sequence models underestimated SR, values calculated from the polynomial model were not significantly different from those of the G_Sequence. Based on multiproxy geochemical, sedimentological, paleoecological data the evolution of the system was reconstructed, covering a timespan of ca. 13,000 years starting from 12,000 BC and lasting until 1300 AD. Highest accumulation rates are dated to the Early Middle Ages from the 11th century. Several climate changes could have been identified which are present in other Hungarian and Western European records too, such as the 5b IRD event at ca. 5800 BC, a humid phase around 1600 BC, and a cool humid phase around the 6th century AD.},
	year = {2018},
	eissn = {1945-5755},
	pages = {1301-1315},
	orcid-numbers = {Gulyás, Sándor/0000-0002-3384-2381; Molnár, Dávid/0000-0001-5304-0741; Jakab, Gusztáv/0000-0002-2569-5967; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:3159156,
	title = {Preliminary paleoecological reconstruction of long-term relationship between human and environment in the northern part of Danube-along Plain, Hungary},
	url = {https://m2.mtmt.hu/api/publication/3159156},
	author = {Kustár, Rozália and Molnár, Dávid and Sümegi, Pál and Törőcsik, Tünde and Sávai, Szilvia},
	doi = {10.1515/geo-2016-0026},
	journal-iso = {OPEN GEOSCI},
	journal = {OPEN GEOSCIENCES},
	volume = {8},
	unique-id = {3159156},
	issn = {2391-5447},
	year = {2016},
	eissn = {2391-5447},
	pages = {405-419},
	orcid-numbers = {Molnár, Dávid/0000-0001-5304-0741; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:27496822,
	title = {Paleoclimate and weathering of the Tokaj (Hungary) loess-paleosol sequence},
	url = {https://m2.mtmt.hu/api/publication/27496822},
	author = {Schatz, AK and Scholten, T and Kuehn, P},
	doi = {10.1016/j.palaeo.2015.03.016},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {426},
	unique-id = {27496822},
	issn = {0031-0182},
	year = {2015},
	eissn = {1872-616X},
	pages = {170-182},
	orcid-numbers = {Schatz, AK/0000-0003-4900-8217; Scholten, T/0000-0002-4875-2602}
}

@article{MTMT:2846935,
	title = {First radiocarbon dated paleoecological data from the freshwater carbonates of the Danube-Tisza Interfluve},
	url = {https://m2.mtmt.hu/api/publication/2846935},
	author = {Sümegi, Pál and Molnár, Dávid and Sávai, Szilvia and Náfrádi, Katalin and Novák, Z and Szelepcsényi, Zoltán and Törőcsik, Tünde},
	doi = {10.1515/geo-2015-0003},
	journal-iso = {OPEN GEOSCI},
	journal = {OPEN GEOSCIENCES},
	volume = {7},
	unique-id = {2846935},
	issn = {2391-5447},
	abstract = {The first radiocarbon dates available on the evolution of the freshwater carbonates of the Danube-Tisza Interfluve are presented in this work along with their possible uses to precisely date paleoecological and paleoenvironmental changes. This work also gives the basis of a comparative analysis of the Holocene radiocarbon-dated profile of Csólyospálos with other Hungarian radiocarbondated profiles of the same age (Bátorliget, the Sárrét, etc.) and the implementation of a detailed chronological and regional paleoenvironmental study. Furthermore, our findings clearly demonstrate the importance of radiocarbon analysis in the study of terminal Pleistocene and Holocene Hungarian sedimentary sequences for accurately dating and reconstructing the chronological order of paleoenvironmental changes as well as the evolution of the natural endowments plus the regional comparison of the various profiles.},
	keywords = {WATER; Hungary; Carbonates; Comparative analysis; Cesium; dolomite; sedimentary sequence; Radiocarbon analysis; Terminal Pleistocene; Paleoenvironmental study; Paleoenvironmental change; freshwater limestone; Csólyospálos village; alkaline lake},
	year = {2015},
	eissn = {2391-5447},
	pages = {40-52},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741; Szelepcsényi, Zoltán/0000-0002-9844-4958}
}

@article{MTMT:2755798,
	title = {Results of paleoecological studies in the loess region of Szeged-Öthalom (SE Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2755798},
	author = {Sümegi, Pál and Náfrádi, Katalin and Molnár, Dávid and Sávai, Szilvia},
	doi = {10.1016/j.quaint.2014.09.003},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {372},
	unique-id = {2755798},
	issn = {1040-6182},
	year = {2015},
	eissn = {1873-4553},
	pages = {66-78},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741}
}

@article{MTMT:2203162,
	title = {Responses of terrestrial ecosystems to Dansgaard–Oeshger cycles and Heinrich-events: A 28,000-year record of environmental changes from SE Hungary},
	url = {https://m2.mtmt.hu/api/publication/2203162},
	author = {Sümegi, Pál and Magyari, Enikő Katalin and Dániel, Péter and Molnár, Mihály and Törőcsik, Tünde},
	doi = {10.1016/j.quaint.2012.07.032},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {293},
	unique-id = {2203162},
	issn = {1040-6182},
	abstract = {According to the findings of a complex sedimentological, geochemical, malacological and pollen study implemented on a core sequence of an alkaline lake (Fehér Lake), interstadials in the SE Great Hungarian Plain were characterized by increased boreal woodland cover during Marine Isotope Stage 2 (MIS 2: 29,700–14,500 cal BP). These interstadials were dated to 26,420–27,970, 23,185–24,880, and 18,810–20,770 cal BP, and correlate well with the Dansgaard-Oeschger (DO) interstadials 2 and 3 and the post LGM warm interval seen in the Greenland ice core oxygen isotope records. Intervening cold phases, on the other hand, were found between 24,880–26,420 and 20,770–23,185 cal BP, correlating with Heinrich event 2 and the LGM. These data overall confirm that millennial scale climate variability during Marine Isotope Stage 2 had profound effect on the terrestrial ecosystems in the continental interior of SE Europe, leading to periodic boreal woodland expansions and contractions and wildfires.},
	year = {2013},
	eissn = {1873-4553},
	pages = {34-50},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Magyari, Enikő Katalin/0000-0002-2844-8937}
}

@article{MTMT:23393664,
	title = {Gravettian occupation of the Beckov Gate in Western Slovakia as viewed from the interdisciplinary research of the Trenčianske Bohuslavice-Pod Tureckom site},
	url = {https://m2.mtmt.hu/api/publication/23393664},
	author = {Vlačiky, M and Michalík, T and Nyvltova, Fisakova M and Nývlt, D and Moravcová, M and Králík, M and Kovanda, J and Péková, K and Přichystal, A and Dohnalová, A},
	doi = {10.1016/j.quaint.2011.09.004},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {294},
	unique-id = {23393664},
	issn = {1040-6182},
	year = {2013},
	eissn = {1873-4553},
	pages = {41-60}
}

@article{MTMT:2517245,
	title = {Stable isotope compositions of bivalve shells and geochemistry of bulk sediments in a 5-20 ky fluvial section at Körösladány, SE Hungary: Sedimentary changes vs. climate signals},
	url = {https://m2.mtmt.hu/api/publication/2517245},
	author = {Demény, Attila and Schöll-Barna, Gabriella and Sümegi, Pál and Sipos, Péter and Fórizs, István and Balázs, Réka and Bajnóczi, Bernadett and Cook, G},
	doi = {10.1556/CEuGeol.55.2012.4.4},
	journal-iso = {CENT EUR GEOL},
	journal = {CENTRAL EUROPEAN GEOLOGY},
	volume = {55},
	unique-id = {2517245},
	issn = {1788-2281},
	year = {2012},
	eissn = {1789-3348},
	pages = {417-439},
	orcid-numbers = {Demény, Attila/0000-0003-0522-9018; Sümegi, Pál/0000-0003-1755-4440; Sipos, Péter/0000-0002-8746-0573; Fórizs, István/0000-0003-0813-6079; Bajnóczi, Bernadett/0000-0003-0006-7611}
}

@article{MTMT:27496831,
	title = {Pleistocene environmental dynamics recorded in the loess of the middle and lower Danube basin},
	url = {https://m2.mtmt.hu/api/publication/27496831},
	author = {Fitzsimmons, KE and Markovic, SB and Hambach, U},
	doi = {10.1016/j.quascirev.2012.03.002},
	journal-iso = {QUATERN SCI REV},
	journal = {QUATERNARY SCIENCE REVIEWS},
	volume = {41},
	unique-id = {27496831},
	issn = {0277-3791},
	year = {2012},
	eissn = {1873-457X},
	pages = {104-118}
}

@article{MTMT:1943042,
	title = {The late Quaternary loess record of Tokaj, Hungary: Reconstructing palaeoenvironment, vegetation and climate using stable C and N isotopes and biomarkers},
	url = {https://m2.mtmt.hu/api/publication/1943042},
	author = {Schatz, A -K and Zech, M and Buggle, B and Gulyás, Sándor and Hambach, U and Marković, S B and Sümegi, Pál and Scholten, T},
	doi = {10.1016/j.quaint.2010.10.009},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {240},
	unique-id = {1943042},
	issn = {1040-6182},
	abstract = {Large areas of Southeast Europe are covered by Pleistocene loess deposits with interbedded palaeosol layers, reflecting interglacials or -stadials. These loess-palaeosol sequences are valuable terrestrial archives for continuous palaeoclimatic and palaeoenvironmental information. In recent years, the traditional paradigm of treeless full-glacial palaeoenvironments has increasingly been called into question, as there is palynological, anthracological and malacological evidence for the continuous presence of trees from loess-palaeosol sequences in the Carpathian Basin. This paper aims at contributing to this discussion by applying biogeochemical, geophysical and sedimentological methods to a late Quaternary loess-palaeosol profile at Tokaj, NE Hungary. Previous studies at the same location have focused on molluscs and charcoal, while this study concentrated on stable C and N isotopes and lipid biomarkers. Long-chain n-alkanes (C 23-C 33), which form major constituents of plant leaf waxes, have successfully been used as biomarkers over the last years and allow for a reconstruction of palaeovegetation based on the differentiation of grassland vs. shrubs and trees. Stable carbon isotopes were used to further differentiate between C 3 and C 4 palaeovegetation, and stable N isotopes to reconstruct the N cycle and climatic variations. Magnetic susceptibility (MS), organic carbon and grain size distribution, which may serve as proxies for e.g. the intensity of pedegenesis, weathering and palaeowind strength, were measured to complement the biogeochemical results and to establish a pedo- and biostratigraphy. Although the results do not agree in every detail with previous studies, there are surprising matches and similarities in the data. Alkane and stable N isotopic data indicate that, pedogenesis occurred under productive, fertile steppe-grasslands, probably in an intensified seasonal climate, and during reduced sedimentation. Two short treeless-steppe periods were found between 26 and 12 ka BP. However, periods characterised by a cooler climate in which trees and shrubs expanded were also found. This interpretation is also supported by previous mollusc data that provide evidence for several periods of favourable conditions for tree growth. © 2010 Elsevier Ltd and INQUA.},
	keywords = {Hungary; Mollusca; VEGETATION; Sedimentology; Quaternary; Tokaj-Eperjes Mountains; Tokaj Mountains; biomarker; paleoclimate; Sequence stratigraphy; Carpathian Basin; paleoenvironment; BIOGEOCHEMISTRY; climate variation; paleosol; loess; carbon isotope; palynology; nitrogen isotope; geological record},
	year = {2011},
	eissn = {1873-4553},
	pages = {52-61},
	orcid-numbers = {Gulyás, Sándor/0000-0002-3384-2381; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:1951422,
	title = {Archeomalakológiai vizsgálatok Magyarországon. Archaeomalacological research in Hungary},
	url = {https://m2.mtmt.hu/api/publication/1951422},
	author = {Sümegi, Pál},
	journal-iso = {ARCHEOMETRIAI MŰHELY},
	journal = {ARCHEOMETRIAI MŰHELY},
	volume = {8},
	unique-id = {1951422},
	issn = {1786-271X},
	year = {2011},
	pages = {101-116},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:1951428,
	title = {Kis-balatoni és balatoni fúrások archeomalakológiai vizsgálatának eredményei. The results of the archaeomalacological investigaton of the core sequences from Balaton and Little Balaton basins},
	url = {https://m2.mtmt.hu/api/publication/1951428},
	author = {Sümegi, Pál},
	journal-iso = {ARCHEOMETRIAI MŰHELY},
	journal = {ARCHEOMETRIAI MŰHELY},
	volume = {8},
	unique-id = {1951428},
	issn = {1786-271X},
	year = {2011},
	pages = {137-156},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:24439174,
	title = {First radiocarbon-dated holocene record of Pomatias elegans in Hungary - Results of complex archeomalacological investigations from the Marshland of Ócsa. Az ócsai láp archeomalakológiai vizsgálata - A Pomatias elegans elso{combining double acute accent} radiokarbon adatokkal korolt holocén elo{combining double acute accent}fordulása Magyarországon},
	url = {https://m2.mtmt.hu/api/publication/24439174},
	author = {Veres, Z and Sümegi, Pál and Törőcsik, Tünde},
	journal-iso = {ARCHEOMETRIAI MŰHELY},
	journal = {ARCHEOMETRIAI MŰHELY},
	volume = {8},
	unique-id = {24439174},
	issn = {1786-271X},
	year = {2011},
	pages = {181-196},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:27496796,
	title = {Combining mitochondrial and nuclear evidences: a refined evolutionary history of Erebia medusa (Lepidoptera: Nymphalidae: Satyrinae) in Central Europe based on the COI gene},
	url = {https://m2.mtmt.hu/api/publication/27496796},
	author = {Hammouti, Nasera and Schmitt, Thomas and Seitz, Alfred and Kosuch, Joachim and Veith, Michael},
	doi = {10.1111/j.1439-0469.2009.00544.x},
	journal-iso = {J ZOOL SYST EVOL RES},
	journal = {JOURNAL OF ZOOLOGICAL SYSTEMATICS AND EVOLUTIONARY RESEARCH},
	volume = {48},
	unique-id = {27496796},
	issn = {0947-5745},
	year = {2010},
	eissn = {1439-0469},
	pages = {115-125}
}

@article{MTMT:1344146,
	title = {Late Quaternary woolly mammoth (Mammuthus primigenius Blum) remains from southern Transdanubia, Hungary},
	url = {https://m2.mtmt.hu/api/publication/1344146},
	author = {Konrád, Gyula and Kovács, János and Halász, Amadé and Sebe, Krisztina and Palffy, H},
	doi = {10.1016/j.crpv.2009.08.001},
	journal-iso = {CR PALEVOL},
	journal = {COMPTES RENDUS PALEVOL},
	volume = {9},
	unique-id = {1344146},
	issn = {1631-0683},
	year = {2010},
	eissn = {1777-571X},
	pages = {47-54},
	orcid-numbers = {Kovács, János/0000-0001-7742-5515; Halász, Amadé/0000-0003-4582-8883; Sebe, Krisztina/0000-0002-4647-2199}
}

@{MTMT:25104120,
	title = {Extra-mediterranean refugia, post-glacial vegetation history and area dynamics in Eastern Central Europe},
	url = {https://m2.mtmt.hu/api/publication/25104120},
	author = {Varga, Zoltán Sándor},
	booktitle = {Relict Species: Phylogeography and Conservation Biology},
	doi = {10.1007/978-3-540-92160-8_3},
	unique-id = {25104120},
	abstract = {Evidences from fossil records and genetic research suggest that the arboreal refugia were not restricted to Southern Europe and in particular to the Mediterranean peninsulas during the full-glacials. Fossil pollen data and macrofossil remains indicate that several tree species have survived also at the Southern edge of the cold-dry steppe-tundra area in Central and Eastern Europe. Recent results of surveys on the Late Pleistocene Mammalian fauna clearly contradict to the "tree-less tundra" models for Europe North of the transverse mountain ranges of the Pyrenees, Alps and Carpathians. It was pointed out that the carrying capacity to feed the herds of large herbivores demands a rather productive environment. The presence of Northern temperate refugia is also supported by the "nonanalogue" assemblages of small mammals discovered from the Late Pleistocene of unglaciated areas of Eastern Central Europe. The assembly of species today typifying the tundra, steppe and semi-desert habitats seems to include also species from deciduous woodland. Extra-Mediterranean core areas were identified also in widely dispersed cold-tolerant frogs and reptiles. Some of their core areas had been at least near the Carpathians and/or marginal areas of the Carpathian Basin. The close faunal connections of the Carpathians suggest the existence of highly dynamic contacts and exchanges with mountains of the Balkan Peninsula during the climatic fluctuations of the Upper Pleistocene. The Eastern and Southern Carpathians, together with the mountains of Western Transylvania, can be considered as core areas of survival and autochtonous evolution in some invertebrate groups with limited mobility. The post-glacial re-population of the Carpathian Basin from different directions has been supported by Illyrian versus Dacian vicarious pairs of sister species/subspecies. In mobile insect groups, peripherically isolated sibling species/subspecies have only been evolved, which display manifold biogeographic connections, e.g. to the Balkan Peninsula, Asia Minor or Southern Russia. The organisation of community-complexes of the Pannonian forest-steppe connected by habitat ecotones resulted in the overlap of several different faunal types, e.g. Mediterranean, Balkanic, Siberian, Ponto-Caspian, Ponto-Pannonian, Turano-Eremic and Xeromontane elements.},
	year = {2010},
	pages = {57-87}
}

@article{MTMT:1138107,
	title = {Estimation of the water conducting capacity of the natural flood conducting channels of the Tisza floodplain, the Great Hungarian Plain},
	url = {https://m2.mtmt.hu/api/publication/1138107},
	author = {Timár, Gábor and Gábris, Gyula},
	doi = {10.1016/j.geomorph.2006.12.031},
	journal-iso = {GEOMORPHOLOGY},
	journal = {GEOMORPHOLOGY},
	volume = {98},
	unique-id = {1138107},
	issn = {0169-555X},
	abstract = {The rapidly subsiding central part of the Pannonian Basin, the flood-plain system of the Tisza River, is analyzed. Natural flood-conducting channels that were functioning prior to the construction of the water control measures of the 19th century have been identified and mapped. By now these channels have mostly disappeared; only small traces of them can be found on modern maps. The identification of these channels was achieved by studying historical maps of the region and by geomorphologic studies. Drawing the outline of the channels and the estimation of their initial meander size was supported by elevation models and satellite imagery. Eight flood breakout points and five independent channel systems were identified. The flood conveying capacity of each channel was also estimated, based on meander wavelengths. The reliability of this estimation is discussed. The channels functioned as anabranches, conducting the floods of the Tisza to its tributary, the Körös River. The efficiency of the flood control system could be increased by regeneration of these natural channels. The summarized water conveying capacity of the abandoned channels is estimated as 1000 m3/s, a value that is slightly under a half of the flood discharge of the Tisza River.},
	keywords = {MODEL; climate; Hungary; river; AREA; SEDIMENTS; Pannonian Basin; DISCHARGE; Tisza river; flood control; Flood-plains; flood conducting channels},
	year = {2008},
	eissn = {1872-695X},
	pages = {250-261},
	orcid-numbers = {Timár, Gábor/0000-0001-9675-6192}
}

@article{MTMT:1183251,
	title = {Holocene lacustrine carbonate formation: old ideas in the light of new radiocarbon data from a single site in Central Hungary},
	url = {https://m2.mtmt.hu/api/publication/1183251},
	author = {Jenei, M and Gulyás, Sándor and Sümegi, Pál and Molnár, Mihály},
	doi = {10.1017/S0033822200042879},
	journal-iso = {RADIOCARBON},
	journal = {RADIOCARBON},
	volume = {49},
	unique-id = {1183251},
	issn = {0033-8222},
	year = {2007},
	eissn = {1945-5755},
	pages = {1017-1021},
	orcid-numbers = {Gulyás, Sándor/0000-0002-3384-2381; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:2972519,
	title = {Malacological and sedimentological evidence for "warm" glacial climate from the Irig loess sequence, Vojvodina, Serbia},
	url = {https://m2.mtmt.hu/api/publication/2972519},
	author = {Marković, SB and Oches, EA and McCoy, WD and Frechen, M and Gaudenyi, Tivadar},
	doi = {10.1029/2006GC001565},
	journal-iso = {GEOCHEM GEOPHY GEOSY},
	journal = {GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS},
	volume = {8},
	unique-id = {2972519},
	year = {2007},
	eissn = {1525-2027}
}

@article{MTMT:27496798,
	title = {Molecular biogeography of Europe: Pleistocene cycles and postglacial trends},
	url = {https://m2.mtmt.hu/api/publication/27496798},
	author = {Schmitt, Thomas},
	doi = {10.1186/1742-9994-4-11},
	journal-iso = {FRONT ZOOL},
	journal = {FRONTIERS IN ZOOLOGY},
	volume = {4},
	unique-id = {27496798},
	issn = {1742-9994},
	year = {2007},
	eissn = {1742-9994}
}

@article{MTMT:1183257,
	title = {Results of radiocarbon analysis of Upper Weichselian loess sequences from Hungary},
	url = {https://m2.mtmt.hu/api/publication/1183257},
	author = {Sümegi, Pál and Molnár, Mihály and Sudár Sándorné Svingor, Éva and Szántó, Andrea Zsuzsanna and Hum, L and Gulyás, Sándor},
	doi = {10.1017/S0033822200042880},
	journal-iso = {RADIOCARBON},
	journal = {RADIOCARBON},
	volume = {49},
	unique-id = {1183257},
	issn = {0033-8222},
	year = {2007},
	eissn = {1945-5755},
	pages = {1023-1030},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Gulyás, Sándor/0000-0002-3384-2381}
}

@article{MTMT:27496800,
	title = {Genetic differentiation of the marbled white butterfly, Melanargia galathea, accounts for glacial distribution patterns and postglacial range expansion in southeastern Europe},
	url = {https://m2.mtmt.hu/api/publication/27496800},
	author = {Schmitt, Thomas and Habel, Jan Christian and Zimmermann, Marco and Mueller, Paul},
	doi = {10.1111/j.1365-294X.2006.02900.x},
	journal-iso = {MOL ECOL},
	journal = {MOLECULAR ECOLOGY},
	volume = {15},
	unique-id = {27496800},
	issn = {0962-1083},
	year = {2006},
	eissn = {1365-294X},
	pages = {1889-1901}
}

@article{MTMT:1393291,
	title = {Mammalian ecosystem dynamics in the Carpathian Basin during the last 27,000 years},
	url = {https://m2.mtmt.hu/api/publication/1393291},
	author = {Pazonyi, Piroska},
	doi = {10.1016/j.palaeo.2004.06.008},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {212},
	unique-id = {1393291},
	issn = {0031-0182},
	year = {2004},
	eissn = {1872-616X},
	pages = {295-314}
}

@article{MTMT:2702559,
	title = {Milankovitch-scale multi-proxy records from fluvial sediments of the last 2.6 Ma, Pannonian Basin, Hungary.},
	url = {https://m2.mtmt.hu/api/publication/2702559},
	author = {Nádor, Annamária and Lantos, M and Tóth-Makk, Á and Thamóné Bozsó, Edit},
	doi = {10.1016/S0277-3791(03)00134-3},
	journal-iso = {QUATERN SCI REV},
	journal = {QUATERNARY SCIENCE REVIEWS},
	volume = {22},
	unique-id = {2702559},
	issn = {0277-3791},
	year = {2003},
	eissn = {1873-457X},
	pages = {2157-2175}
}

@article{MTMT:23393680,
	title = {Did Polyommatus icarus (Lepidoptera: Lycaenidae) have distinct glacial refugia in southern Europe? Evidence from population genetics},
	url = {https://m2.mtmt.hu/api/publication/23393680},
	author = {Schmitt, T and Giessl, A and Seitz, A},
	doi = {10.1046/j.1095-8312.2003.00261.x},
	journal-iso = {BIOL J LINN SOC},
	journal = {BIOLOGICAL JOURNAL OF THE LINNEAN SOCIETY},
	volume = {80},
	unique-id = {23393680},
	issn = {0024-4066},
	year = {2003},
	eissn = {1095-8312},
	pages = {529-538}
}

@article{MTMT:23393682,
	title = {Postglacial colonisation of western Central Europe by Polyommatus coridon (Poda 1761) (Lepidoptera: Lycaenidae): Evidence from population genetics},
	url = {https://m2.mtmt.hu/api/publication/23393682},
	author = {Schmitt, T and Gießl, A and Seitz, A},
	doi = {10.1038/sj/hdy/6800003},
	journal-iso = {HEREDITY},
	journal = {HEREDITY},
	volume = {88},
	unique-id = {23393682},
	issn = {0018-067X},
	year = {2002},
	eissn = {1365-2540},
	pages = {26-34}
}

@article{MTMT:231404,
	title = {Quatermalacological analyses for modeling of the Upper Weichselian palaeoenvironmental changes in the Carpathian Basin},
	url = {https://m2.mtmt.hu/api/publication/231404},
	author = {Sümegi, Pál and Krolopp, E},
	doi = {10.1016/S1040-6182(01)00102-1},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {91},
	unique-id = {231404},
	issn = {1040-6182},
	year = {2002},
	eissn = {1873-4553},
	pages = {53-63},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:1177778,
	title = {Retarded wetland succession: anthropogenic and climatic signals in a Holocene peat bog profile from north-east Hungary},
	url = {https://m2.mtmt.hu/api/publication/1177778},
	author = {Magyari, Enikő Katalin and Sümegi, Pál and Braun, Mihály and Jakab, Gusztáv and Molnár, Mihály},
	doi = {10.1046/j.0022-0477.2001.00624.x},
	journal-iso = {J ECOL},
	journal = {JOURNAL OF ECOLOGY},
	volume = {89},
	unique-id = {1177778},
	issn = {0022-0477},
	year = {2001},
	eissn = {1365-2745},
	pages = {1019-1032},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Sümegi, Pál/0000-0003-1755-4440; Jakab, Gusztáv/0000-0002-2569-5967}
}

@article{MTMT:1177772,
	title = {Recurring Taiga forest-steppe habitats in the Carpathian Basin in the Upper Weichselian},
	url = {https://m2.mtmt.hu/api/publication/1177772},
	author = {Rudner, Edina and Sümegi, Pál},
	doi = {10.1016/S1040-6182(00)00101-4},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {76-77},
	unique-id = {1177772},
	issn = {1040-6182},
	year = {2001},
	eissn = {1873-4553},
	pages = {177-189},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:23393685,
	title = {Intraspecific allozymatic differentiation reveals the glacial refugia and the postglacial expansions of European Erebia medusa (Lepidoptera: Nymphalidae)},
	url = {https://m2.mtmt.hu/api/publication/23393685},
	author = {Schmitt, T and Seitz, A},
	doi = {10.1006/bijl.2001.0584},
	journal-iso = {BIOL J LINN SOC},
	journal = {BIOLOGICAL JOURNAL OF THE LINNEAN SOCIETY},
	volume = {74},
	unique-id = {23393685},
	issn = {0024-4066},
	year = {2001},
	eissn = {1095-8312},
	pages = {429-458}
}

@article{MTMT:1177775,
	title = {In situ charcoal fragments as remains of natural wild fires in the upper Würm of the Carpathian Basin},
	url = {https://m2.mtmt.hu/api/publication/1177775},
	author = {Sümegi, Pál and Rudner, Edina},
	doi = {10.1016/S1040-6182(00)00100-2},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {76/77},
	unique-id = {1177775},
	issn = {1040-6182},
	year = {2001},
	eissn = {1873-4553},
	pages = {165-176},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:1177762,
	title = {The full-glacial forests of central and southeastern Europe},
	url = {https://m2.mtmt.hu/api/publication/1177762},
	author = {Willis, KJ and Rudner, Edina and Sümegi, Pál},
	doi = {10.1006/qres.1999.2119},
	journal-iso = {QUATERNARY RES},
	journal = {QUATERNARY RESEARCH},
	volume = {53},
	unique-id = {1177762},
	issn = {0033-5894},
	year = {2000},
	eissn = {1096-0287},
	pages = {203-213},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:1184524,
	title = {The shell morpho-thermometer method and its application in palaeoclimatic reconstruction},
	url = {https://m2.mtmt.hu/api/publication/1184524},
	author = {Sólymos, Péter and Sümegi, Pál},
	journal-iso = {ANN UNIV SCI BP R EÖTVÖS NOM SECT GEOL},
	journal = {ANNALES UNIVERSITATIS SCIENTIARUM BUDAPESTINENSIS DE ROLANDO EÖTVÖS NOMINATAE - SECTIO GEOLOGICA},
	volume = {32},
	unique-id = {1184524},
	issn = {0365-0634},
	year = {1999},
	pages = {137-148},
	orcid-numbers = {Sólymos, Péter/0000-0001-7337-1740; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:23393688,
	title = {The identification of the palaeoclimatic and palaeo-ecological development of Hortobagy National Park in the Pleistocene/Holocene transition period},
	url = {https://m2.mtmt.hu/api/publication/23393688},
	author = {Tóth, C},
	journal-iso = {PETERMANNS GEOGR MITT},
	journal = {PETERMANNS GEOGRAPHISCHE MITTEILUNGEN},
	volume = {143},
	unique-id = {23393688},
	issn = {0031-6229},
	year = {1999},
	pages = {219-227}
}

@article{MTMT:1177756,
	title = {Reconstruction of Microenvironmental Changes in the Kopasz Hill Loess Area at Tokaj (Hungary) Between 15 and 70 ka BP},
	url = {https://m2.mtmt.hu/api/publication/1177756},
	author = {Sümegi, Pál and Hertelendi, Ede},
	doi = {10.1017/s0033822200018828},
	journal-iso = {RADIOCARBON},
	journal = {RADIOCARBON},
	volume = {40},
	unique-id = {1177756},
	issn = {0033-8222},
	year = {1998},
	eissn = {1945-5755},
	pages = {855-863},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:1177751,
	title = {Does soil change cause vegetation change or vice versa? A temporal perspective from Hungary},
	url = {https://m2.mtmt.hu/api/publication/1177751},
	author = {Willis, K J and Braun, Mihály and Sümegi, Pál and Tóth, Albert},
	doi = {10.1890/0012-9658(1997)078[0740:DSCCVC]2.0.CO;2},
	journal-iso = {ECOLOGY},
	journal = {ECOLOGY},
	volume = {78},
	unique-id = {1177751},
	issn = {0012-9658},
	year = {1997},
	eissn = {1939-9170},
	pages = {740-750},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:21632091,
	title = {Cosmogenic radiocarbon and cyclical natural processes},
	url = {https://m2.mtmt.hu/api/publication/21632091},
	author = {Dergachev, V and Chistyakov, V},
	doi = {10.1017/S0033822200030897},
	journal-iso = {RADIOCARBON},
	journal = {RADIOCARBON},
	volume = {37},
	unique-id = {21632091},
	issn = {0033-8222},
	year = {1995},
	eissn = {1945-5755},
	pages = {417-424}
}

@article{MTMT:1177739,
	title = {Palaeoecological reconstruction of the Late Pleistocene, Based on Loess Malacofauna in Hungary},
	url = {https://m2.mtmt.hu/api/publication/1177739},
	author = {Krolopp, E and Sümegi, Pál},
	doi = {10.1007/BF00813173},
	journal-iso = {GEOJOURNAL},
	journal = {GEOJOURNAL},
	volume = {36},
	unique-id = {1177739},
	issn = {0343-2521},
	year = {1995},
	eissn = {1572-9893},
	pages = {213-222},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:1177745,
	title = {The Late Quaternary environmental history of Bátorliget, N.E. Hungary},
	url = {https://m2.mtmt.hu/api/publication/1177745},
	author = {Willis, K J and Sümegi, Pál and Braun, Mihály and Tóth, Albert},
	doi = {10.1016/0031-0182(95)00004-6},
	journal-iso = {PALAEOGEOGR PALAEOCL},
	journal = {PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY},
	volume = {118},
	unique-id = {1177745},
	issn = {0031-0182},
	year = {1995},
	eissn = {1872-616X},
	pages = {25-47},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:21632090,
	title = {The use of land snail shells in paleoenvironmental reconstruction},
	url = {https://m2.mtmt.hu/api/publication/21632090},
	author = {Goodfriend, GA},
	doi = {10.1016/0277-3791(92)90076-K},
	journal-iso = {QUATERN SCI REV},
	journal = {QUATERNARY SCIENCE REVIEWS},
	volume = {11},
	unique-id = {21632090},
	issn = {0277-3791},
	year = {1992},
	eissn = {1873-457X},
	pages = {665-685}
}