@article{MTMT:34047615, title = {Development History of the Loess–Paleosol Profiles of Pécel, Kisdorog and Bonyhádvarasd, Hungary}, url = {https://m2.mtmt.hu/api/publication/34047615}, author = {Makó, László and Cseh, P and Nagy, Balázs and Sümegi, Pál and Molnár, Dávid}, doi = {10.3390/quat6030038}, journal-iso = {Quaternary}, journal = {QUATERNARY}, volume = {6}, unique-id = {34047615}, issn = {2571-550X}, abstract = {This study covers the examination of four loess–paleosol profiles in Hungary through grain size composition, organic matter, carbonate content and magnetic susceptibility measurements. One of the profiles (with a thickness of 25.72 m) can be found in the Gödöllő hills, on the border of town Pécel, and the other three profiles (Kisdorog-West—5.60 m, Kisdorog-East—6.40 and Bonyhádvarasd—8.16 m) are located in the Tolna hills of the Transdanubia region. The sections were continuously sampled with an interval of 4 cm. The same interval was also applied to the other three profiles. During the field exploration of the Pécel profile, we were able to study the complete loess wall, which was deposited on the sediment of the nearby Rákos stream. Based on the Ostracod fauna of the clay sediment beneath, the fluvial deposit can be considered as originating from the Upper Miocene. In the case of the Transdanubian sections, a significant change can be observed in the prevailing wind direction based on the grain size analyses. In addition, the results of magnetic susceptibility measurements suggest that the development of the Pécel profile took place during MIS 9–10, while the age of the three Transdanubian sections can be assumed to be the MIS 2–4.}, year = {2023}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741} } @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:31816012, title = {A palaeoenvironmental record of the Southern Hemisphere last glacial maximum from the Mount Cass loess section, North Canterbury, Aotearoa/New Zealand}, url = {https://m2.mtmt.hu/api/publication/31816012}, author = {Almond, PC. and Gulyás, Sándor and Sümegi, Pál and Sümegi, BP. and Covey-Crump, S and Jones, M and Shaw, J and Parker, A}, doi = {10.1017/qua.2020.95}, journal-iso = {QUATERNARY RES}, journal = {QUATERNARY RESEARCH}, volume = {102}, unique-id = {31816012}, issn = {0033-5894}, year = {2021}, eissn = {1096-0287}, pages = {115-129}, orcid-numbers = {Almond, PC./0000-0003-4203-1529; Gulyás, Sándor/0000-0002-3384-2381; Sümegi, Pál/0000-0003-1755-4440} } @article{MTMT:31817980, title = {MAR comparisons between different chronometric methods for two profiles in the Bodrogkeresztúr area}, url = {https://m2.mtmt.hu/api/publication/31817980}, author = {Makó, László and Molnár, Dávid and Cseh, Péter and Sümegi, Pál}, doi = {10.24425/sq.2020.133761}, journal-iso = {STUD QUATER}, journal = {STUDIA QUATERNARIA}, volume = {38}, unique-id = {31817980}, issn = {1641-5558}, year = {2021}, eissn = {2300-0384}, pages = {67-73}, orcid-numbers = {Molnár, Dávid/0000-0001-5304-0741; Sümegi, Pál/0000-0003-1755-4440} } @article{MTMT:31962092, title = {Middle and Late Pleistocene loess-palaeosol archives in East Croatia: multi-proxy palaeoecological studies on Zmajevac and Šarengrad II sequences}, url = {https://m2.mtmt.hu/api/publication/31962092}, author = {Molnár, Dávid and Makó, László and Cseh, Péter and Sümegi, Pál and Fekete, István and Galović, L}, doi = {10.24425/sq.2020.133758}, journal-iso = {STUD QUATER}, journal = {STUDIA QUATERNARIA}, volume = {38}, unique-id = {31962092}, issn = {1641-5558}, year = {2021}, eissn = {2300-0384}, pages = {3-17}, orcid-numbers = {Molnár, Dávid/0000-0001-5304-0741; Sümegi, Pál/0000-0003-1755-4440} } @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:32165831, title = {The changing malaria risk patterns in East‐Central Europe and the North Balkans in the last 27 000 years}, url = {https://m2.mtmt.hu/api/publication/32165831}, author = {Trájer, Attila János}, doi = {10.1002/jqs.3357}, journal-iso = {J QUATERNARY SCI}, journal = {JOURNAL OF QUATERNARY SCIENCE}, volume = {2021}, unique-id = {32165831}, issn = {0267-8179}, year = {2021}, eissn = {1099-1417}, orcid-numbers = {Trájer, Attila János/0000-0003-3248-6474} } @article{MTMT:31259838, title = {A novel approach to quantifying the degree of anthropogenic surface transformation – the concept of ‘hemeromorphy’}, url = {https://m2.mtmt.hu/api/publication/31259838}, author = {Rózsa, Péter and Incze, József and Balogh, Szabolcs and Novák, Tibor József}, doi = {10.3112/erdkunde.2020.01.03}, journal-iso = {ERDKUNDE}, journal = {ERDKUNDE}, volume = {74}, unique-id = {31259838}, issn = {0014-0015}, year = {2020}, eissn = {0014-0015}, pages = {45-57}, orcid-numbers = {Novák, Tibor József/0000-0002-5514-9035} } @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:3331516, title = {High-resolution paleoclimatic proxy data from the MIS3/2 transition recorded in northeastern Hungarian loess}, url = {https://m2.mtmt.hu/api/publication/3331516}, author = {Bösken, J and Obreht, I and Zeeden, C and Klasen, N and Hambach, U and Sümegi, Pál and Lehmkuhl, F}, doi = {10.1016/j.quaint.2017.12.008}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {502/PartA}, unique-id = {3331516}, issn = {1040-6182}, abstract = {The Bodrogkeresztúr loess-paleosol sequence in northeastern Hungary was investigated to improve our understanding of the paleoenvironmental conditions at the foothills of the Carpathians and their impact on the Gravettian population. The main part of the section is comprised of eolian deposits that enable the reconstruction of the paleoenvironmental conditions. This study comprises grain size, geochemical, color and rock magnetic analysis, as well as luminescence and radiocarbon dating. The chronological data place this section from later MIS 3 until present, but also suggest erosion of the sediment in the late MIS 2 and the (early) Holocene. Moreover, generally more humid conditions during late MIS3 and early MIS2 are observed, in comparison to other regions in the Carpathian Basin. Main dust source was most likely the Tisza floodplain, and the material was probably transported to the site from a northeastern wind direction. Increased weathering led to the formation of a well-developed MIS3 paleosol. The loess exhibits elevated values of frequency dependent magnetic susceptibility that highlight the relatively mild conditions during loess formation. Nevertheless, two loess layers with high sand abundance in the profile indicate colder and dryer conditions with increased eolian dynamics during short periods within MIS2. Finally, the Bodrogkeresztúr section highlights the unique microclimatic conditions at the foothill areas of the Carpathian Basin, which may have offered a favorable environment for the Gravettian population. © 2017 Elsevier Ltd and INQUA.}, keywords = {Magnetic susceptibility; loess; luminescence dating; Wind directions derived from AMS measurements; Weathering indices; Grain size analysis}, year = {2019}, eissn = {1873-4553}, pages = {95-107}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440} } @article{MTMT:3327732, title = {Radiocarbon dated malacological records of two Late Pleistocene loess-paleosol sequences from SW-Hungary. Paleoecological inferences}, url = {https://m2.mtmt.hu/api/publication/3327732}, author = {Molnár, Dávid and Sümegi, Pál and Fekete, István and Makó, László and P. Sümegi, B}, doi = {10.1016/j.quaint.2018.01.018}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {504}, unique-id = {3327732}, issn = {1040-6182}, year = {2019}, eissn = {1873-4553}, pages = {108-117}, orcid-numbers = {Molnár, Dávid/0000-0001-5304-0741; Sümegi, Pál/0000-0003-1755-4440} } @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:30413691, title = {A preliminary chronological study to understand the construction phases of a Late Copper–Early Bronze Age kurgan (kunhalom)}, url = {https://m2.mtmt.hu/api/publication/30413691}, author = {Szilágyi, Gábor and Náfrádi, Katalin and Sümegi, Pál}, doi = {10.1556/24.61.2018.11}, journal-iso = {CENT EUR GEOL}, journal = {CENTRAL EUROPEAN GEOLOGY}, volume = {62}, unique-id = {30413691}, issn = {1788-2281}, abstract = {The aim of this study is to identify the milestones of landscape evolution around the Ecse Mound (Karcag-Kunmadaras, Hortobágy National Park, Hungary) in the Holocene period by sedimentological and malacological analysis of strata underneath and within the body of the kurgan concerned, including that of the same characteristics of the artificially piled layers. An undisturbed core drilling was carried out and the sedimentological properties of both the mound and of the substrate baserock were revealed, analysis of which has been supported by three radiocarbon (AMS) measurements. The baserock formation during the last phase of the Ice Age, Middle and Upper Pleniglacial, and Late Glacial phases was followed by soil development in the Holocene, while the mound was constructed in two phases at the end of the Copper Age by the communities of the Pit Grave (Yamna or Ochre Grave) Culture. By publishing these preliminary data, it is also intended to draw attention to the need of focused research efforts by standardized methodology in kurgan research, in order to make the results of different studies consistent and comparable.}, year = {2019}, eissn = {1789-3348}, pages = {27-55}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440} } @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:3244739, title = {Early Upper Paleolithic surface collections from loess-like sediments in the northern Carpathian Basin}, url = {https://m2.mtmt.hu/api/publication/3244739}, author = {Chu, Wei and Lengyel, György and Zeeden, Christian and Péntek, Attila and Kaminská, Ľubomíra and Mester, Zsolt}, doi = {10.1016/j.quaint.2017.05.017}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {485}, unique-id = {3244739}, issn = {1040-6182}, abstract = {The way in which modern humans first entered Europe has been a recent focus of Upper Paleolithic research. A leading theory posits that the Danube served as a conduit for migration from Southeastern into Central and Western Europe. However, a challenge to this has been the scarcity of Early Upper Paleolithic sites along the Middle Danube (Carpathian) Basin. Though several sites with Early Upper Paleolithic features (Szeletian, Aurignacian) are known from surface prospections, few have been archeologically investigated in detail.}, keywords = {Carpathian Basin; GRAIN-SIZE ANALYSIS; Aurignacian; Szeletian; Danube corridor hypothesis}, year = {2018}, eissn = {1873-4553}, pages = {167-182}, orcid-numbers = {Lengyel, György/0000-0002-7803-3043; Mester, Zsolt/0000-0001-5874-5935} } @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:3200317, title = {Holocene valley incision in the southern Bükk foreland: Climate-human-environment interferences in northern Hungary}, url = {https://m2.mtmt.hu/api/publication/3200317}, author = {Martin, Schumacher and Dobos, Anna and Wolfram, Schier and Brigitta, Schütt}, doi = {10.1016/j.quaint.2016.10.021}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {463}, unique-id = {3200317}, issn = {1040-6182}, year = {2018}, eissn = {1873-4553}, pages = {91-109}, orcid-numbers = {Dobos, Anna/0000-0001-6864-7052} } @article{MTMT:30363709, title = {Impact of climate and humans on the range dynamics of the woolly mammoth (Mammuthus primigenius) in Europe during MIS 2}, url = {https://m2.mtmt.hu/api/publication/30363709}, author = {Nadachowski, A. and Lipecki, G. and Baca, M. and Zmihorski, M. and Wilczyński, J.}, doi = {10.1017/qua.2018.54}, journal-iso = {QUATERNARY RES}, journal = {QUATERNARY RESEARCH}, volume = {90}, unique-id = {30363709}, issn = {0033-5894}, year = {2018}, eissn = {1096-0287}, pages = {439-456} } @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: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:3146640, title = {Szekunder karbonátok mennyisége és vertikális eloszlása tokaji talajszelvényekben}, url = {https://m2.mtmt.hu/api/publication/3146640}, author = {Novák, Tibor József and Csámer, Árpád and Incze, József and Papp, I and Rózsa, Péter}, doi = {10.1556/0088.2016.65.2.2}, journal-iso = {AGROKÉMIA ÉS TALAJTAN}, journal = {AGROKÉMIA ÉS TALAJTAN}, volume = {65}, unique-id = {3146640}, issn = {0002-1873}, year = {2016}, eissn = {1588-2713}, pages = {193-206}, orcid-numbers = {Novák, Tibor József/0000-0002-5514-9035; Csámer, Árpád/0000-0003-2374-2413} } @article{MTMT:3158287, title = {Radiocarbon dated complex paleoecological and geoarcheological analyses at the Bodrogkeresztúr – Henye Gravettian site (NE Hungary) [A bodrogkeresztrúi Henye tetői Gravetti lelőhely komplex paleoökológiai és geoarcheológiai elemzése (ÉK Magyarország)]}, url = {https://m2.mtmt.hu/api/publication/3158287}, author = {Sümegi, Pál and Törőcsik, Tünde and Náfrádi, Katalin and Sümegi, Balázs Pál and Majkut, Péter and Molnár, Dávid and Tapody, Réka Orsolya}, journal-iso = {ARCHEOMETRIAI MŰHELY}, journal = {ARCHEOMETRIAI MŰHELY}, volume = {13}, unique-id = {3158287}, issn = {1786-271X}, year = {2016}, pages = {31-41}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Molnár, Dávid/0000-0001-5304-0741} } @article{MTMT:3045359, title = {A radiocarbon-dated cave sequence and the Pleistocene/Holocene transition in Hungary}, url = {https://m2.mtmt.hu/api/publication/3045359}, author = {Sümegi, Pál and Náfrádi, Katalin}, doi = {10.1515/geo-2015-0051}, journal-iso = {OPEN GEOSCI}, journal = {OPEN GEOSCIENCES}, volume = {7}, unique-id = {3045359}, issn = {2391-5447}, year = {2015}, eissn = {2391-5447}, pages = {783-798}, orcid-numbers = {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:27496789, title = {Tracking potential source areas of Central European loess: examples from Tokaj (HU), Nussloch (D) and Grub (AT)}, url = {https://m2.mtmt.hu/api/publication/27496789}, author = {Schatz, AK and Qi, Y and Siebel, W and Wu, J and Zoeller, L}, doi = {10.1515/geo-2015-0048}, journal-iso = {OPEN GEOSCI}, journal = {OPEN GEOSCIENCES}, volume = {7}, unique-id = {27496789}, issn = {2391-5447}, year = {2015}, eissn = {2391-5447}, pages = {678-720}, orcid-numbers = {Schatz, AK/0000-0003-4900-8217} } @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:24810332, title = {Malacological sequence of Weichselian (MIS 5-2) loess series from a profile in Grodzisko Dolne (southern Poland) and its palaeogeographic significance}, url = {https://m2.mtmt.hu/api/publication/24810332}, author = {Alexandrowicz, Witold Pawel}, doi = {10.1016/j.quaint.2013.08.048}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {319}, unique-id = {24810332}, issn = {1040-6182}, year = {2014}, eissn = {1873-4553}, pages = {109-118} } @article{MTMT:2485324, title = {Microhabitat associations of land snails in forested dolinas: implications for coarse filter conservation}, url = {https://m2.mtmt.hu/api/publication/2485324}, author = {Kemencei, Zita and Farkas, Roland Tibor and Páll-Gergely, B and Vilisics, Ferenc and Nagy, Antal and Hornung, Erzsébet and Sólymos, Péter}, doi = {10.1556/comec.15.2014.2.6}, journal-iso = {COMMUNITY ECOL}, journal = {COMMUNITY ECOLOGY}, volume = {15}, unique-id = {2485324}, issn = {1585-8553}, year = {2014}, eissn = {1588-2756}, pages = {180-186}, orcid-numbers = {Sólymos, Péter/0000-0001-7337-1740} } @article{MTMT:2723923, title = {Soil and vegetation transformation in abandoned vineyards of the Tokaj Nagy-Hill}, url = {https://m2.mtmt.hu/api/publication/2723923}, author = {Novák, Tibor József and Incze, József and Spohn, M and Glina, B and Giani, L}, doi = {10.1016/j.catena.2014.07.017}, journal-iso = {CATENA}, journal = {CATENA}, volume = {123}, unique-id = {2723923}, issn = {0341-8162}, year = {2014}, eissn = {1872-6887}, pages = {88-98}, orcid-numbers = {Novák, Tibor József/0000-0002-5514-9035} } @article{MTMT:2790432, title = {AMS 14C and OSL/IRSL dating of the Dunaszekcső loess sequence (Hungary): chronology for 20 to 150 ka and implications for establishing reliable age–depth models for the last 40 ka}, url = {https://m2.mtmt.hu/api/publication/2790432}, author = {Újvári, Gábor and Molnár, Mihály and Novothny, Ágnes and Páll-Gergely, Barna and Kovács, János and Várhegyi, András}, doi = {10.1016/j.quascirev.2014.06.009}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {106}, unique-id = {2790432}, issn = {0277-3791}, abstract = {Abstract As revealed by 18 AMS radiocarbon and 24 OSL/IRSL ages the Dunaszekcső loess-paleosol sequence is an excellent terrestrial record of paleoenvironmental change in the Carpathian Basin for the last 130 ka, with significant soil forming episodes during the Eemian interglacial (130–115 ka, MIS 5e) and in some subsequent MIS 5 stages, and distinct periods of loess accumulations during the MIS 4 and MIS 2. Charcoals from the sequence made it possible to test the accuracy of 14C ages from mollusc shells. This approach revealed that 14C ages from some gastropods having small shells (<10 mm) (Succinella oblonga, Vitrea crystallina) are statistically indistinguishable from the ages of charcoals, while others (Clausiliidae sp., Chondrula tridens) show age anomalies up to 600–800 years. OSL and pIRIR@290 ages are found to be consistently older, while post-IR OSL ages are younger than the 14C ages from charcoals and molluscs by some thousands of years, except for pIRIR@225 ages that match the radiocarbon ages quite well. OSL and IRSL ages have scatters up to 7–10 thousand years within 40 ka, while charcoals and small molluscs yield consistent ages with relatively low variability. Beyond the observation that some small molluscs seem to yield reliable 14C ages, calibrated 2σ age ranges of the radiocarbon data (ca 500–800 years for 20 to 30 ka) are an order of magnitude narrower than those of the OSL/IRSL methods (1800–4000 years for 25 to 35 ka). Thus, for establishing chronologies within 40 ka, which are both accurate and precise enough to address issues like synchroneity of millennial-scale paleoenvironmental events across regions (e.g. North Atlantic and Europe), AMS radiocarbon dating of shells of specific loess molluscs and charcoals may probably be a powerful chronological tool. However, additional work is definitely required involving 14C and OSL/IRSL dates from other loess sequences to further test the performance of these two supposedly robust chronometers.}, keywords = {Hungary; radiocarbon dating; mollusc; paleosol; loess; OSL and IRSL dating}, year = {2014}, eissn = {1873-457X}, pages = {140-154}, orcid-numbers = {Újvári, Gábor/0000-0002-2816-6155; Novothny, Ágnes/0000-0003-3513-0406; Páll-Gergely, Barna/0000-0002-6167-7221; Kovács, János/0000-0001-7742-5515} } @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: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:1925602, title = {Radiocarbon chronology of Late Pleistocene large mammal faunas from the Pannonian basin (Hungary)}, url = {https://m2.mtmt.hu/api/publication/1925602}, author = {Kovács, János}, doi = {10.3140/bull.geosci.1282}, journal-iso = {B GEOSCI}, journal = {BULLETIN OF GEOSCIENCES}, volume = {87}, unique-id = {1925602}, issn = {1214-1119}, year = {2012}, eissn = {1802-8225}, pages = {13-19}, orcid-numbers = {Kovács, János/0000-0001-7742-5515} } @article{MTMT:2197608, title = {Középső-würm végi fosszilis talaj- és löszréteg átmeneti szintjének komplex paleoökológiai vizsgálata a tokaji Kopasz-hegyen}, url = {https://m2.mtmt.hu/api/publication/2197608}, author = {Páll, Dávid Gergely and Persaits, Gergő and Náfrádi, Katalin and Sümegi, Pál}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {142}, unique-id = {2197608}, issn = {0015-542X}, year = {2012}, eissn = {2559-902X}, pages = {251-268}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440} } @article{MTMT:27496830, title = {Establishing a luminescence chronology for a palaeosol-loess profile at Tokaj (Hungary): A comparison of quartz OSL and polymineral IRSL signals}, url = {https://m2.mtmt.hu/api/publication/27496830}, author = {Schatz, AK and Buylaert, JP and Murray, A and Stevens, T and Scholten, T}, doi = {10.1016/j.quageo.2012.02.018}, journal-iso = {QUAT GEOCHRONOL}, journal = {QUATERNARY GEOCHRONOLOGY}, volume = {10}, unique-id = {27496830}, issn = {1871-1014}, year = {2012}, eissn = {1878-0350}, pages = {68-74}, orcid-numbers = {Schatz, AK/0000-0003-4900-8217; Buylaert, JP/0000-0003-0587-8077; Stevens, T/0000-0002-6662-6650; Scholten, T/0000-0002-4875-2602} } @inbook{MTMT:2044262, title = {Woodland-Grassland Ecotonal Shifts in Environmental Mosaics: Lessons Learnt from the Environmental History of the Carpathian Basin (Central Europe) During the Holocene and the Last Ice Age Based on Investigation of Paleobotanical and Mollusk Remains.}, url = {https://m2.mtmt.hu/api/publication/2044262}, author = {Sümegi, Pál and Persaits, G and Gulyás, Sándor}, booktitle = {Ecotones Between Forest and Grassland}, doi = {10.1007/978-1-4614-3797-0_2}, unique-id = {2044262}, year = {2012}, pages = {17-57}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Gulyás, Sándor/0000-0002-3384-2381} } @article{MTMT:2104731, title = {Late Pleistocene variations of the background aeolian dust concentration in the Carpathian Basin: An estimate using decomposition of grain-size distribution curves of loess deposits}, url = {https://m2.mtmt.hu/api/publication/2104731}, author = {Varga, György and Kovács, János and Újvári, Gábor}, doi = {10.1017/S0016774600001566}, journal-iso = {NETH J GEOSCI}, journal = {NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW}, volume = {91}, unique-id = {2104731}, issn = {0016-7746}, abstract = {Aeolian dust deposits can be considered as one of the most important archives of past climatic changes. Alternating loess and paleosol strata display variations of the dust load in the Pleistocene atmosphere. By using the observations of recent dust storms, we are able to employ Late Pleistocene stratigraphie datasets (with accurate chronological framework) and detailed granulometric data for making conclusions on the atmospheric dust load in the past. Age-depths models, created from the absolute age data and stratigraphie interpretation, allow us to calculate sedimentation rates and dust fluxes, while grain-size specifies the dry-deposition velocity, i.e. the atmospheric residence time of mineral particles. Thus, the dust concentration can be expressed as the quotient of the dust flux and gravitational settling velocity. Recent observations helped to clarify the mechanisms behind aeolian sedimentation and the physical background of this process has nowadays been well established. Based on these two, main contrasting sedimentary modes of dust transport and deposition can be recognised: the short suspension episodes of the coarse (silt and very fine sand) fraction and the long-range transport of a fine (clay and fine silt) component. Using parametric curve fitting the basic statistical properties of these two sediment populations can be revealed for Pleistocene aeolian dust deposits, as it has been done for loess in Hungary. As we do not have adequate information on the magnitude and frequency of the Pleistocene dust storms, conclusions could only be made on the magnitude of continuous background dust load. The dust concentration can be set in the range between 1100 and 2750 ug/m3. These values are mostly higher than modern dust concentrations, even in arid regions. Another interesting proxy of past atmospheric conditions could be the visibility, being proportional to the dust concentration. According to the known empirical dust concentration - visibility equations, its value is around 6.5 to 26 kilometres.}, keywords = {grain-size; PLEISTOCENE; loess; Dust concentration; Aeolian dust}, year = {2012}, eissn = {1573-9708}, pages = {159-171}, orcid-numbers = {Varga, György/0000-0003-4784-6372; Kovács, János/0000-0001-7742-5515; Újvári, Gábor/0000-0002-2816-6155} } @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:1951396, title = {Late Quaternary palaeoenvironment and palaeoclimate of the Lake Fehér (Fehér-tó) sequence at Kardoskút (South Hungary), based on preliminary mollusc records}, url = {https://m2.mtmt.hu/api/publication/1951396}, author = {Sümegi, Pál and Lócskai, T and Hupuczi, Júlia}, doi = {10.2478/s13533-011-0007-5}, journal-iso = {CENT EUR J GEOSCI}, journal = {CENTRAL EUROPEAN JOURNAL OF GEOSCIENCES}, volume = {3}, unique-id = {1951396}, issn = {2081-9900}, year = {2011}, eissn = {1896-1517}, pages = {43-52}, orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440} } @article{MTMT:1361069, title = {Dust flux estimates for the Last Glacial Period in East Central Europe based on terrestrial records of loess deposits: a review}, url = {https://m2.mtmt.hu/api/publication/1361069}, author = {Újvári, Gábor and Kovács, János and Varga, György and Raucsik, Béla and Markovic, SB}, doi = {10.1016/j.quascirev.2010.07.005}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {29}, unique-id = {1361069}, issn = {0277-3791}, year = {2010}, eissn = {1873-457X}, pages = {3157-3166}, orcid-numbers = {Újvári, Gábor/0000-0002-2816-6155; Kovács, János/0000-0001-7742-5515; Varga, György/0000-0003-4784-6372; Raucsik, Béla/0000-0002-1951-5974} } @article{MTMT:1393294, title = {A Kárpát-medence felső-pliocén és kvarter emlősfauna közösségeinek paleoökológiai vizsgálata. Palaeoecological investigations of upper pliocene and quaternary mammalian communities in the Carpathian Basin}, url = {https://m2.mtmt.hu/api/publication/1393294}, author = {Pazonyi, Piroska}, journal-iso = {FÖLDTANI KÖZLÖNY}, journal = {FÖLDTANI KÖZLÖNY}, volume = {139}, unique-id = {1393294}, issn = {0015-542X}, year = {2009}, eissn = {2559-902X}, pages = {283-304} } @article{MTMT:27496836, title = {Episodic build-up of alluvial fan deposits during the Weichselian Pleniglacial in the western Transylvanian Basin, Romania and their paleoenvironmental significance}, url = {https://m2.mtmt.hu/api/publication/27496836}, author = {Pendea, I F and Gray, J T and Ghaleb, B and Tantau, I and Badarau, A S and Nicorici, C}, doi = {10.1016/j.quaint.2008.05.002}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {198}, unique-id = {27496836}, issn = {1040-6182}, year = {2009}, eissn = {1873-4553}, pages = {98-112} } @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:1135543, title = {Long-term fluvial archives in Hungary: response of the Danube and Tisza rivers to tectonic movements and climatic changes during the Quaternary: a review and new synthesis}, url = {https://m2.mtmt.hu/api/publication/1135543}, author = {Gábris, Gyula and Nádor, Annamária}, doi = {10.1016/j.quascirev.2007.06.030}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {26}, unique-id = {1135543}, issn = {0277-3791}, abstract = {The paper discusses the Quaternary evolution of the Danube and Tisza rivers and their main tributaries in the context of evolution of the entire Pannonian Basin, which is Europe's largest intramontane basin, within the Alp-Carpathian orogen. The palaeo-drainage reconstruction of the Pannonian Basin for the pre-Quaternary period is Outlined in connection with the gradual regression of Lake Pannon since the Late Miocene. Deltas of rivers that entered the basin from the northwest and northeast were gradually transformed into extended alluvial plains; thus, the earliest possible ancestor of the Danube coming southeastwards from the Alps could be as old as Late Miocene. By the Pliocene the whole Lake Parnnon was infilled. The former extensional basin formation was replaced by a compresional stress field, which resulted in an uplift of the marginal flanks and late-stage subsidence anomalies. The increasing relief led to the formation of the Quaternary drainage pattern. The actively subsiding young basins were filled by fluvial sediments, transported by the Danube and Tisza river systems from the uplifting mountains. Between the subsiding regions of the Little and Great Plains, the Danube has formed an antecedent valley with terrace staircases between the uplifting sections of the Transdanubian Range and the North Midmountains. The formation of the terraces is attributed to periodic climate changes during the Pleistocene combined with differences in the uplift rate. The paper gives a complex overview of the classical chronology of the six terraces based on various data sources: mostly dating of loess/paleosol sequences, travertines, aeolian sand, and tephra strata overlying the fluvial sediments, complemented by scattered vertebrate faunal data and archaeological evidence directly from the terrace sediments. The Quaternary drainage pattern evolution of the Great Plain, with a strong tectonic control, is discussed in detail. Rivers originating from the uplifting marginal areas were drawn towards the subsiding depressions which served as local base level. Changes in subsidence rates in space and time throughout the Quaternary resulted in the evolution of a complex drainage pattern. A special emphasis is placed on the Late Pleistocene-Holocene development of the Middle-Tisza region and the Koros basin, where the Berettyo-Koros Rivers form an eastern tributary system of the Tisza River. A comparative evaluation of these two areas is especially relevant, as they provide insights into large-scale Late Pleistocene avulsion of the Tisza River. OSL dating, complemented with inferred transport directions determined from heavy mineral analysis of fluvial sediments in the Koros basin, has revealed an ancient large meandering river system that can be identified with the palaeo-Tisza, which was flowing along a tectonically controlled depression during the Late Pleniglacial. Successions in the Middle Tisza region have allowed differentiation between the older channels of the palaeo-Bodrog River and the Sajo-Hernad alluvial fan and the younger meander belts of the new course of the Tisza. In the Tisza system, changes in river style (braided to various scales of meandering) show correspondence to millennial-scale climate changes of the last 25 ka, while in the Koros basin the effects of tectonics are overprinted onto the regional climatic signals. (c) 2007 Elsevier Ltd. All rights reserved.}, keywords = {Europe; EVOLUTION; SITE; Pannonian Basin; Carpathian Basin; MIDDLE; PLAIN}, year = {2007}, eissn = {1873-457X}, pages = {2758-2782} } @article{MTMT:1333818, title = {Fluvial responses to tectonics and climate change during the Late Weichselian in the eastern part of the Pannonian Basin (Hungary)}, url = {https://m2.mtmt.hu/api/publication/1333818}, author = {Nádor, Annamária and Thamóné Bozsó, Edit and Magyari, A and Babinszki, Edit}, doi = {10.1016/j.sedgeo.2007.03.001}, journal-iso = {SEDIMENT GEOL}, journal = {SEDIMENTARY GEOLOGY}, volume = {202}, unique-id = {1333818}, issn = {0037-0738}, abstract = {Fine-grained sandy-silty channel-belt and floodplain deposits of the Berettyo-Koros Rivers, a main eastern transverse tributary system of the modem Tisza River in the eastern part of the Pannonian Basin, were deposited during the Late Pleistocene under net subsiding conditions. The palaeo-drainage network pattern of a 2500 km 2 large part of the alluvial plain was reconstructed based on interpretation of airborne photographs and analysis of 18th century topographic maps, which show the natural river patterns that predate the introduction of river regulation schemes. The investigation showed that a large meandering river system, with two main channel belts surrounding a floodbasin, entered the alluvial plain from the northeast, and a braided river entered the alluvial plain from the southeast. Detailed sedimentary logs of seven continuous corings and several sand and clay-pit sections were used to characterize different alluvial units. Optical luminescence dating (OSL) of 25 quartz samples and four C-14 datings showed that the sediments are of Late Pleniglacial to Late Glacial age. Transport directions inferred from heavy mineral analyses combined with the OSL ages strongly suggest that the large meandering system represents the palaeo-Tisza River, which supposedly flowed along the northeast-southwest striking Ermellek depression during the Late Pleniglacial. The braided river can be regarded as a precursor to the Fekete and Feher-Koros Rivers, which entered the alluvial plain from the southeast during the Late Glacial. The interpretation of seismic profiles, field measurements of neotectonic activity, and variations in thickness of sediments along the studied profile revealed that river development was largely controlled by subsidence along the Ermellek depression until 14 to 16 ky, and by uplift of the southeastern part of the catchment area. The studied fluvial successions also document the response of the palaeo-Tisza and Koros system to the climate changes of the Weichselian Late Pleniglacial-Late Glacial period. Much of the sand from the meandering zones was deposited during the Bolling-Allerod and Sagvar-Lascaux interstadials, whereas some dated sand units from the braided zone represent the Older and Younger Dryas. The error ranges of OSL dates, which often exceed the duration of Weichselian substages and subdivisions, prevented an unambiguous correlation of the studied sections with the millennial-scale climate changes of the last 25 ky. Meandering and braided river activity coexisted under different climate conditions, whereas locations of the main channel belts are related to subsidence anomalies. The results of A our study thus clearly indicate that tectonics was the primary control on river development. (c) 2007 Elsevier B.V. All rights reserved.}, year = {2007}, eissn = {1879-0968}, pages = {174-192} } @article{MTMT:1070503, title = {Conservation prioritization based on distribution of land snails in Hungary}, url = {https://m2.mtmt.hu/api/publication/1070503}, author = {Sólymos, Péter and Fehér, Zoltán}, doi = {10.1111/j.1523-1739.2005.00193.x}, journal-iso = {CONSERV BIOL}, journal = {CONSERVATION BIOLOGY}, volume = {19}, unique-id = {1070503}, issn = {0888-8892}, year = {2005}, eissn = {1523-1739}, pages = {1084-1094}, orcid-numbers = {Sólymos, Péter/0000-0001-7337-1740; Fehér, Zoltán/0000-0002-4888-1156} } @inbook{MTMT:149557, title = {Appendix I: Radiocarbon data from Upper Paleolithic sites and Late Quaternary paleoecological sites in Hungary}, url = {https://m2.mtmt.hu/api/publication/149557}, author = {Sudár Sándorné Svingor, Éva and Molnár, Mihály and Szántó, Andrea Zsuzsanna}, booktitle = {Loess and Upper Paleolithic environment in Hungary}, unique-id = {149557}, year = {2005}, pages = {295} } @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:10291454, title = {Clay mineralogy of Quaternary sediments covering mountainous and hilly areas of Hungary}, url = {https://m2.mtmt.hu/api/publication/10291454}, author = {Viczián, I}, doi = {10.1556/AGeol.45.2002.3.5}, journal-iso = {ACTA GEOL HUNG}, journal = {ACTA GEOLOGICA HUNGARICA: A QUARTERLY OF THE HUNGARIAN ACADEMY OF SCIENCES}, volume = {45}, unique-id = {10291454}, issn = {0236-5278}, year = {2002}, pages = {265-286} } @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: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} }