@article{MTMT:3298445,
	title = {Middle Bronze Age humidity and temperature variations, and societal changes in East-Central Europe},
	url = {https://m2.mtmt.hu/api/publication/3298445},
	author = {Demény, Attila and Kern, Zoltán and Czuppon, György and Németh, Alexandra and Schöll-Barna, G and Siklósy, Z and Leél-Őssy, Szabolcs and Cook, G and Serlegi, Gábor and Bajnóczi, Bernadett and Sümegi, Pál and Király, Ágnes and Kiss, Viktória and Kulcsár, Gabriella and Bondár, Mária (Ködmönné)},
	doi = {10.1016/j.quaint.2017.11.023},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {504},
	unique-id = {3298445},
	issn = {1040-6182},
	year = {2019},
	eissn = {1873-4553},
	pages = {80-95},
	orcid-numbers = {Demény, Attila/0000-0003-0522-9018; Kern, Zoltán/0000-0003-4900-2587; Czuppon, György/0000-0002-7231-6042; Bajnóczi, Bernadett/0000-0003-0006-7611; Sümegi, Pál/0000-0003-1755-4440; Bondár, Mária (Ködmönné)/0000-0002-6526-0570}
}

@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:31279285,
	title = {Pollen-based reconstruction of the plant cultivation in the Carpathian basin from the Migration Age to the end of the Medieval Age [Pollen alapú növénytermesztési rekonstrukció a Kárpát-medencében a népvándorlás korától a középkor végéig]},
	url = {https://m2.mtmt.hu/api/publication/31279285},
	author = {Törőcsik, Tünde and Sümegi, Pál},
	journal-iso = {ARCHEOMETRIAI MŰHELY},
	journal = {ARCHEOMETRIAI MŰHELY},
	volume = {16},
	unique-id = {31279285},
	issn = {1786-271X},
	abstract = {From the beginning of the Migration period to the end of the Ottoman period, from the turn of the IV-Vth century until to the XVI-XVIIth century, we examined the changes of 1300 years of grain production throughout the Carpathian Basin in a centennial resolution, through 13 centuries, and 137 pollen sites. Based on the spatial distribution of the total cereal pollen ratio, which is related to cultivation, agriculture, population density, and headcount, the following statements were made regarding the age of the Migration period, the Hungarian conquest, the Middle Ages and the Ottoman period. Our analysis is only the beginning of a comprehensive environmental history analysis, which, together with significant material and time investment, archaeological data, historical analyses, pollen data, and other archaeobotanical, archaeozoological data, allows us to conduct an almost complete economic history analysis of the Carpathian Basin.},
	year = {2019},
	pages = {245-270},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:3320438,
	title = {Timing of major forest compositional changes and tree expansions in the Retezat Mts during the last 16,000 years},
	url = {https://m2.mtmt.hu/api/publication/3320438},
	author = {Magyari, Enikő Katalin and Vincze, Ildikó and Orbán, Ildikó and Biró, Tamás and Pál, Ilona},
	doi = {10.1016/j.quaint.2017.12.054},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {477},
	unique-id = {3320438},
	issn = {1040-6182},
	keywords = {POLLEN ANALYSIS; conservation management; EASTERN-EUROPE; GLACIAL REFUGIA; Plant macrofossils; ENVIRONMENTAL-CHANGES; Climate changes; Holocene vegetation history; Carpathian Mountains; EVENT STRATIGRAPHY; CARPATHIAN MOUNTAINS ROMANIA; ABIES-ALBA MILL.; Expansion times; Postglacial forest succession},
	year = {2018},
	eissn = {1873-4553},
	pages = {40-58},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Orbán, Ildikó/0000-0003-1547-675X; Biró, Tamás/0000-0001-5198-7210}
}

@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:2719067,
	title = {Evolution of the Pannonian basin and its geothermal resources},
	url = {https://m2.mtmt.hu/api/publication/2719067},
	author = {Horváth, Ferenc and Musitz, Balázs and Balázs, Attila and Végh, Andor and Uhrin, András and Nádor, Annamária and Koroknai, B and Pap, Norbert and Tóth, Tamás and Wórum, G},
	doi = {10.1016/j.geothermics.2014.07.009},
	journal-iso = {GEOTHERMICS},
	journal = {GEOTHERMICS},
	volume = {53},
	unique-id = {2719067},
	issn = {0375-6505},
	keywords = {Pannonian Basin; Tectonics; Geothermal installations; Thermal water reservoirs},
	year = {2015},
	eissn = {1879-3576},
	pages = {328-352},
	orcid-numbers = {Balázs, Attila/0000-0003-2948-0397; Pap, Norbert/0000-0001-8243-4213}
}

@article{MTMT:2706681,
	title = {Climate variability and associated vegetation response throughout Central and Eastern Europe (CEE) between 60 and 8 ka},
	url = {https://m2.mtmt.hu/api/publication/2706681},
	author = {Feurdean, A and Perşoiu, A and Tanţău, I and Stevens, T and Magyari, Enikő Katalin and Onac, BP and Marković, S and Andrič, M and Connor, S and Fărcaş, S and Gałka, M and Gaudenyi, Tivadar and Hoek, W and Kolaczek, P and Kuneš, P and Lamentowicz, M and Marinova, E and Michczyńska, DJ and Perşoiu, I and Płóciennik, M and Słowiński, M and Stancikaite, M and Sümegi, Pál and Svensson, A and Tămaş, T and Timar, A and Tonkov, S and Tóth, Mónika and Veski, S and Willis, KJ and Zernitskaya, V},
	doi = {10.1016/j.quascirev.2014.06.003},
	journal-iso = {QUATERN SCI REV},
	journal = {QUATERNARY SCIENCE REVIEWS},
	volume = {106},
	unique-id = {2706681},
	issn = {0277-3791},
	abstract = {Abstract Records of past climate variability and associated vegetation response exist in various regions throughout Central and Eastern Europe (CEE). To date, there has been no coherent synthesis of the existing palaeo-records. During an INTIMATE meeting (Cluj Napoca, Romania) focused on identifying CEE paleo-records, it was decided to address this gap by presenting the palaeo-community with a compilation of high-quality climatic and vegetation records for the past 60–8 ka. The compilation should also serve as a reference point for the use in the modelling community working towards the INTIMATE project goals, and in data-model inter-comparison studies. This paper is therefore a compilation of up to date, best available quantitative and semi-quantitative records of past climate and biotic response from CEE covering this period. It first presents the proxy and archive used. Speleothems and loess mainly provide the evidences available for the 60–20 ka interval, whereas pollen records provide the main source of information for the Lateglacial and Holocene. It then examines the temporal and spatial patterns of climate variability inferred from different proxies, the temporal and spatial magnitude of the vegetation responses inferred from pollen records and highlights differences and similarities between proxies and sub-regions and the possible mechanisms behind this variability. Finally, it identifies weakness in the proxies and archives and their geographical distribution. This exercise also provides an opportunity to reflect on the status of research in the area and to identify future critical areas and subjects of research.},
	keywords = {climate; POLLEN; Holocene; vegetation response; LATITUDINAL GRADIENTS; Glacial; INTIMATE; Terrestrial records},
	year = {2014},
	eissn = {1873-457X},
	pages = {206-224},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:2594039,
	title = {Late Pleniglacial vegetation in eastern-central Europe: are there modern analogues in Siberia?},
	url = {https://m2.mtmt.hu/api/publication/2594039},
	author = {Magyari, Enikő Katalin and Kunes, P and Jakab, Gusztáv and Sümegi, Pál and Pelánková, B and Schabitz, F and Braun, Mihály and Chytry, M},
	doi = {10.1016/j.quascirev.2014.04.020},
	journal-iso = {QUATERN SCI REV},
	journal = {QUATERNARY SCIENCE REVIEWS},
	volume = {95},
	unique-id = {2594039},
	issn = {0277-3791},
	year = {2014},
	eissn = {1873-457X},
	pages = {60-79},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Jakab, Gusztáv/0000-0002-2569-5967; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:1979868,
	title = {Using linear discriminant analysis (LDA) of bulk lake sediment geochemical data to reconstruct lateglacial climate changes in the South Carpathian Mountains},
	url = {https://m2.mtmt.hu/api/publication/1979868},
	author = {Braun, Mihály and Hubay, Katalin and Magyari, Enikő Katalin and Veres, D and Papp, István and Bálint, M},
	doi = {10.1016/j.quaint.2012.03.025},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {293},
	unique-id = {1979868},
	issn = {1040-6182},
	year = {2013},
	eissn = {1873-4553},
	pages = {114-122},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Papp, István/0000-0002-0006-9919}
}

@article{MTMT:2402859,
	title = {Status Report of the New AMS 14C Sample Preparation Lab of the Hertelendi Laboratory of Environmental Studies (Debrecen, Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2402859},
	author = {Molnár, Mihály and Janovics, Róbert and Major, István and Orsovszki, J and Gönczi, R and Veres, Mihály and Leonard, A G and Castle, S M and Lange, T E and Wacker, L and Hajdas, I and T Jull, A J},
	doi = {10.2458/azu_js_rc.55.16394},
	journal-iso = {RADIOCARBON},
	journal = {RADIOCARBON},
	volume = {55},
	unique-id = {2402859},
	issn = {0033-8222},
	year = {2013},
	eissn = {1945-5755},
	pages = {665-676},
	orcid-numbers = {Major, István/0000-0003-4675-9875}
}

@article{MTMT:2333500,
	title = {Future Climate Impacts in Woodland and Forest Steppe Based on Holocene Paleoclimatic Trends, Paleobotanical Change in Central Part of the Carpathian Basin (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/2333500},
	author = {Náfrádi, Katalin and Jakab, Gusztáv and Sümegi, Pál and Szelepcsényi, Zoltán and Törőcsik, Tünde},
	doi = {10.4236/ajps.2013.46147},
	journal-iso = {AM J PLANT SCI},
	journal = {AMERICAN JOURNAL OF PLANT SCIENCES (AJPS)},
	volume = {4},
	unique-id = {2333500},
	issn = {2158-2742},
	abstract = {The Sirok Nyírjes-tó peat bog provides an almost full Holocene climatic record reconstructed by bog surface wetness investigations based on plant macrofossil analysis. We compared our macrofossil data to anthracological material derived from archaeological sites and to the newest bioclimatological models of the Carpathian basin. On the basis of environ-mental historical and climatic data we aimed to reconstruct the expected changes of forested areas in the Carpathian Basin. The results indicate that the surface wetness decreases in long term. Parallel to the Sphagnum-peat decline an open forest and forest steppe developed surrounding the bog. The complete disappearance of Sphagna from the area must be linked to a steady drop in rainfall, resulting in at least 50 mm deficit in the local water balance. This could have been achieved by an increased evapotranspiration as a result of elevated temperatures of the summer growth season. This deficit value must have exceeded even 100 mm during the Middle Holocene Transition.},
	year = {2013},
	eissn = {2158-2750},
	pages = {1187-1203},
	orcid-numbers = {Jakab, Gusztáv/0000-0002-2569-5967; Sümegi, Pál/0000-0003-1755-4440; Szelepcsényi, Zoltán/0000-0002-9844-4958}
}

@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}
}

@book{MTMT:2154565,
	title = {Prehistoric wagon models in the Carpathian Basin (3500-1500 BC)},
	url = {https://m2.mtmt.hu/api/publication/2154565},
	isbn = {9789639911345},
	author = {Bondár, Mária (Ködmönné)},
	publisher = {Archaeolingua Alapítvány és Kiadó},
	unique-id = {2154565},
	year = {2012},
	orcid-numbers = {Bondár, Mária (Ködmönné)/0000-0002-6526-0570}
}

@article{MTMT:30864769,
	title = {Immigration and transhumance in the Early Bronze Age Carpathian Basin: the occupants of a kurgan},
	url = {https://m2.mtmt.hu/api/publication/30864769},
	author = {Gerling, C and Bánffy, Eszter and Dani, János and Köhler, Kitti and Kulcsár, Gabriella and Pike, AWG and Szeverényi, Vajk and Heyd, V},
	doi = {10.1017/S0003598X00048274},
	journal-iso = {ANTIQUITY},
	journal = {ANTIQUITY: A QUARTERLY REVIEW OF WORLD ARCHAEOLOGY},
	volume = {86},
	unique-id = {30864769},
	issn = {0003-598X},
	abstract = {You never know until you look. The authors deconstruct a kurgan burial mound in the Great Hungarian Plain designated to the Yamnaya culture, to find it was actually shared by a number of different peoples. The Yamnaya were an influential immigrant group of the Late Copper Age/Early Bronze Age transition. The burials, already characterised by their grave goods, were radiocarbon elated and further examined using stable isotope analysis on the human teeth. The revealing sequence began with a young person of likely local origin buried around or even before the late fourth millennium BC-a few centuries before the arrival of the Yamnaya. It ended around 500 years later with a group of different immigrants, apparently from the eastern mountains. These are explained as contacts built up between the mountains and the plain through the practice of transhumance.},
	year = {2012},
	eissn = {1745-1744},
	pages = {1097-1111},
	orcid-numbers = {Bánffy, Eszter/0000-0001-5156-826X}
}

@article{MTMT:1846857,
	title = {Rapid vegetation response to lateglacial and early Holocene climatic fluctuation in the South Carpathian Mountains (Romania).},
	url = {https://m2.mtmt.hu/api/publication/1846857},
	author = {Magyari, Enikő Katalin and Jakab, Gusztáv and Bálint, M and Kern, Zoltán and Buczkó, Krisztina and Braun, Mihály},
	doi = {10.1016/j.quascirev.2012.01.006},
	journal-iso = {QUATERN SCI REV},
	journal = {QUATERNARY SCIENCE REVIEWS},
	volume = {35},
	unique-id = {1846857},
	issn = {0277-3791},
	year = {2012},
	eissn = {1873-457X},
	pages = {116-130},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Jakab, Gusztáv/0000-0002-2569-5967; Kern, Zoltán/0000-0003-4900-2587}
}

@article{MTMT:1792003,
	title = {Climatic variability in the Late Copper Age: Stable isotope fluctuation of prehistoric Unio pictorum (Unionidae) shells from Lake Balaton (Hungary)},
	url = {https://m2.mtmt.hu/api/publication/1792003},
	author = {Schöll-Barna, Gabriella and Demény, Attila and Serlegi, Gábor and Fábián, Szilvia and Sümegi, Pál and Fórizs, István and Bajnóczi, Bernadett},
	doi = {10.1007/s10933-011-9561-6},
	journal-iso = {J PALEOLIMNOL},
	journal = {JOURNAL OF PALEOLIMNOLOGY},
	volume = {47},
	unique-id = {1792003},
	issn = {0921-2728},
	year = {2012},
	eissn = {1573-0417},
	pages = {87-100},
	orcid-numbers = {Demény, Attila/0000-0003-0522-9018; Sümegi, Pál/0000-0003-1755-4440; Fórizs, István/0000-0003-0813-6079; Bajnóczi, Bernadett/0000-0003-0006-7611}
}

@article{MTMT:1943039,
	title = {Farming and/or foraging? New environmental data to the life and economic transformation of Late Neolithic tell communities (Tisza Culture) in SE Hungary},
	url = {https://m2.mtmt.hu/api/publication/1943039},
	author = {Gulyás, Sándor and Sümegi, Pál},
	doi = {10.1016/j.jas.2011.07.019},
	journal-iso = {J ARCHAEOL SCI},
	journal = {JOURNAL OF ARCHAEOLOGICAL SCIENCE},
	volume = {38},
	unique-id = {1943039},
	issn = {0305-4403},
	abstract = {The turn of the 6th and 5th millennia BC witnessed probably the largest economic and cultural transformation of SE Europe giving rise to a new techno-complex occupying the alluvial plains of the Tisza River and its tributaries in the southern parts of the Carpathian Basin. Representatives of the Tisza Culture were engaged in intensive farming complemented with foraging creating a complex system of hierarchical multi-layered settlements (tells). The favorable endowments of the sites with a large variety of multiple ecotones ideal for multifocal subsistence, as well as the introduction of new farming techniques ensured the establishment of long-term sedentary lifeways. However, according to the archeology, a major shift in subsistence happened toward the end of the Late Neolithic marking the terminal part of the evolution of the culture. Traditional crop cultivation was increasingly complemented with hunting, animal husbandry gaining importance. Other second-line resources like fish and shellfish followed the same pattern. Finally, tells were disintegrated and a new cultural group of the Copper Age emerged. The exact background of these transformations is still unknown. In order to see whether or not potential transformations in the local riparian environment had some role in shaping human behavior, a multiproxy paleoecological analysis was implemented on mollusk material of one of the largest tell sites of SE Hungary. Freshwater mollusks collected by humans in themselves characterize the quality of the water body from which they derive. They are also an excellent marker of socioeconomic response to environmental stress. According to our findings the emergence of new settlement phases and the intensified foraging could have been correlated with alteration of stream properties yielding successively higher floods. This was initially beneficial creating lush pasturelands for large bodied prey infiltrating the area during the referred period like aurochs, red-deer. But ultimately it might have reduced areas suitable for agriculture and living most likely leading to social disruption besides other cultural, social processes. © 2011 Elsevier Ltd.},
	keywords = {Hungary; Cultivation; Animalia; Cervus elaphus; Mollusca; Mollusks; Animal Husbandry; foraging behavior; Carpathian Basin; Tisza river; crop production; socioeconomic conditions; paleoecology; intensive agriculture; farming system; economic activity; alluvial plain; mollusc; Foraging; Bos primigenius; Neolithic; human settlement; economic history; cultural history; Social & economic crisis; Riparian environment; Multiproxy paleoecological analysis; Late Neolithic},
	year = {2011},
	eissn = {1095-9238},
	pages = {3323-3339},
	orcid-numbers = {Gulyás, Sándor/0000-0002-3384-2381; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:1943040,
	title = {Riparian environment in shaping social and economic behavior during the first phase of the evolution of Late Neolithic tell complexes in SE Hungary (6th/5th millennia BC)},
	url = {https://m2.mtmt.hu/api/publication/1943040},
	author = {Gulyás, Sándor and Sümegi, Pál},
	doi = {10.1016/j.jas.2011.06.005},
	journal-iso = {J ARCHAEOL SCI},
	journal = {JOURNAL OF ARCHAEOLOGICAL SCIENCE},
	volume = {38},
	unique-id = {1943040},
	issn = {0305-4403},
	abstract = {The period corresponding to the initial phase of cultural evolution in the Late Neolithic of SE Hungary (turn of the 6th and 5th millennia) is characterized by a major transformation recorded both in settlement structure and strategy, as well as material culture of the agrarian societies settled in the SE part of the Great Hungarian Plains. According to the available chronological data and archeology from the sites of multi-layered settlement complexes (tells) located on natural highs of the floodplain of the River Tisza, during the initial phase of its evolution representatives of the Tisza Culture were mainly confined to the SE part of the Great Hungarian Plains south of the Körös River. This period was followed by a relatively stable phase lasting about 150 years which hallmarked the greatest northward expansion of the culture. Some studies noticed strange features in connection with the first settlement complexes dated to the first period especially along the northern borderline of the culture's distribution; i.e. a loose cluster of distinct settlement nuclei instead of concentration of settlements to a confined area characteristic of tells. Furthermore, by the end of the first phase, in the evolution of some settlements a northward shift of the houses away from the water was recorded. Most likely these reflect a socioeconomic response to some transformation in the local and/or regional riparian environment. As shown by our data gained from the paleoecological analysis of freshwater mollusks from a tell site, the referred pre-transitional period was characterized by pronounced floods causing major perturbations in the regional riparian environment. At the same time, the introduction of new subsistence strategies including shellfishing and fishing and the reordering of settlement structure was also recorded at several sites implying a successful adaptation to such most likely climate-induced perturbation, which is contemporary with the 5.1 ky event known in the literature. © 2011 Elsevier Ltd.},
	keywords = {Hungary; climate change; Mollusca; chronology; Carpathian Basin; Tisza river; paleoecology; floodplain; climate variation; mollusc; PERTURBATION; settlement history; riparian zone; Social and economic development; Multi-proxy paleoecological analysis; Freshwater mollusks; Neolithic; cultural history; Riparian environment},
	year = {2011},
	eissn = {1095-9238},
	pages = {2683-2695},
	orcid-numbers = {Gulyás, Sándor/0000-0002-3384-2381; Sümegi, Pál/0000-0003-1755-4440}
}

@{MTMT:2877642,
	title = {Introduction. The paleo-environment and settlement context of Polgár-10},
	url = {https://m2.mtmt.hu/api/publication/2877642},
	author = {Magyari, Enikő Katalin and Robert, Shiel and David, Passmore},
	booktitle = {The Upper Tisza Project, Studies in Hungarian Landscape Archaeology, Book 4: Lowland Settlement in North East Hungary: Excavations at the Neolithic Settlement Site Polgár-10},
	unique-id = {2877642},
	year = {2010},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937}
}

@article{MTMT:2588298,
	title = {Miocene facies associations and sedimentary evolution of the Southern Transylvanian Basin (Romania): Implications for hydrocarbon exploration},
	url = {https://m2.mtmt.hu/api/publication/2588298},
	author = {Krezsek, C and Filipescu, S and Silye, Lóránd and Matenco, L and Doust, H},
	doi = {10.1016/j.marpetgeo.2009.07.009},
	journal-iso = {MAR PETROL GEOL},
	journal = {MARINE AND PETROLEUM GEOLOGY},
	volume = {27},
	unique-id = {2588298},
	issn = {0264-8172},
	abstract = {The Transylvanian Basin is a mature hydrocarbon province of Romania characterized by two petroleum systems: Mesozoic (thermogenic) and Miocene (biogenic). An extensive outcrop-based sedimentological and micropaleontological study correlated to seismic and well data discusses the elements of the Miocene petroleum system. The facies associations are indicative of alluvial, fandelta, shallow- and deep-marine settings. These are grouped into four different depositional systems (evaporite, mud-carbonate, sand-mud and sand-gravel). Their evolution in time and space shows large differences between various parts of the basin that have important consequences for exploration. The Transylvanian gas is formed by more than 99% methane of bacterial origin. This is sourced by low quality (<1% TOC) deep-marine shales. The shales contain Type II and Type III kerogen. The organic material is thermally immature. The best source rocks were deposited during major transgressions in the central-eastern parts of the basin. In general, reservoir quality is the best (porosity < 20%, permeability < 1 D) in the basin center, where reservoirs are deep-marine turbidite sandstones. Lower quality reservoirs are conglomerate-rich slope channels and various shallow-marine sandstones located near the basin margins. The seals are formed by shales that hold gas columns of up to 60 m. The most common structural traps are in 4-way dip closures related to salt-cored folds. Their timing is coeval with the late (post-Pannonian) exhumation of the basin and strongly linked to coeval salt tectonics. This requires a late charge and migration. The largest traps typically have multistory (up to 20) pay zones with a total of 100 BCF to 1 TCF reserves. Exploration to date has focused on structural traps, but most of the obvious structures have been drilled. It is argued that significant exploration potential lies in stratigraphic plays, including confined submarine fans, slope channels, detached lowstand prograding wedges, incised valleys, diapir flanks, salt-tectonics related unconformities and various sub-volcanic plays. Risks of the petroleum system elements associated to these plays in different areas of the basin are discussed. (C) 2009 Elsevier Ltd. All rights reserved.},
	keywords = {SYSTEM; history; Pannonian Basin; Middle Miocene; Sequence stratigraphy; Transylvanian Basin; CENTRAL PARATETHYS; Hydrocarbon system; Fission-track; FOREDEEP; THRUST BELT; CARPATHIANS ROMANIA; DENSITY TURBIDITY CURRENTS; Exploration potential; Biogenic gas; Facies associations},
	year = {2010},
	eissn = {1873-4073},
	pages = {191-214},
	orcid-numbers = {Silye, Lóránd/0000-0001-7306-6041}
}

@article{MTMT:1431870,
	title = {Holocene persistence of wooded steppe in the Great Hungarian Plain},
	url = {https://m2.mtmt.hu/api/publication/1431870},
	author = {Magyari, Enikő Katalin and Chapman, J C and Passmore, D G and Allen, J R M and Huntley, J P and Huntley, B},
	doi = {10.1111/j.1365-2699.2009.02261.x},
	journal-iso = {J BIOGEOGR},
	journal = {JOURNAL OF BIOGEOGRAPHY},
	volume = {37},
	unique-id = {1431870},
	issn = {0305-0270},
	year = {2010},
	eissn = {1365-2699},
	pages = {915-935},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937}
}

@article{MTMT:1803133,
	title = {Palaeolimnology of the last crater lake in the Eastern Carpathian Mountains: a multiproxy study of Holocene hydrological changes},
	url = {https://m2.mtmt.hu/api/publication/1803133},
	author = {Magyari, Enikő Katalin and Buczkó, Krisztina and Jakab, Gusztáv and Braun, Mihály and Pal, Z and Karátson, Dávid and Papp, István},
	doi = {10.1007/s10750-009-9801-1},
	journal-iso = {HYDROBIOLOGIA},
	journal = {HYDROBIOLOGIA},
	volume = {631},
	unique-id = {1803133},
	issn = {0018-8158},
	abstract = {A multi-proxy investigation (loss-on-ignition, major and trace elements, pollen, plant macrofossil and siliceous algae) was carried out on the sediment of a crater lake (Lake Saint Ana, 950 m a.s.l.) from the Eastern Carpathian Mountains. Diatom-based transfer functions were applied to estimate the lake's trophic status and pH, while reconstruction of the water-depth changes was based on the plant macrofossil and diatom records. The lowest Holocene water depths were found between 9000 and 7400 calibrated BP years, when the crater was occupied by Sphagnum-bog. Significant increases in water depth were found from 5350(1), 3300(2) and 2700 cal yr BP. Of these, the first two coincided with major terrestrial vegetation changes, namely (1) the establishment of Carpinus betulus on the crater slope and (2) the replacement of the lakeshore Picea abies forest by Fagus sylvatica. The chemical record indicated significant soil changes along with the canopy changes (from coniferous to deciduous) that led to increased in-lake productivity and pH. A further increase in water depth around 2700 cal yr BP resulted in stable thermal stratification and hypolimnetic anoxia that via P-release further increased in-lake productivity and eventually led to phytoplankton blooms with large populations of Scenedesmus. High productivity was depressed by anthropogenic lakeshore forest clearances from ca. 1000 cal yr BP that led to the re-establishment of P. abies on the lakeshore and consequent acidification of the lake water. On the whole, these data suggest that Lake Saint Ana is a vulnerable ecosystem: in-lake productivity is higher under deciduous canopy and litter, and considerably repressed by coniferous canopy and litter. The lake today subsists in a managed environment that is far from its natural state. This would be a dense F. sylvatica forest supplying more nutrients and keeping up a more productive in-lake flora and fauna.},
	keywords = {POLLEN; Romania; VEGETATION HISTORY; CLIMATE VARIABILITY; GUTAIULUI MOUNTAINS; NORTHWESTERN ROMANIA; ENVIRONMENTAL HISTORY; POSTGLACIAL COLONIZATION; POLLEN ANALYSIS; NW ROMANIA; CAL YR BP; SPRUCE PICEA-ABIES; Sediment chemistry; Siliceous algae; Macrofossil; Lake level change},
	year = {2009},
	eissn = {1573-5117},
	pages = {29-63},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Jakab, Gusztáv/0000-0002-2569-5967; Karátson, Dávid/0000-0003-0386-1239; Papp, István/0000-0002-0006-9919}
}

@article{MTMT:1951407,
	title = {Middle Age paleoecological and paleoclimatological reconstruction in the Carpathian Basin},
	url = {https://m2.mtmt.hu/api/publication/1951407},
	author = {Sümegi, Pál and Jakab, Gusztáv and Majkut, P and Törőcsik, Tünde and Zatykó, Csilla},
	journal-iso = {IDŐJÁRÁS},
	journal = {IDŐJÁRÁS / QUARTERLY JOURNAL OF THE HUNGARIAN METEOROLOGICAL SERVICE},
	volume = {113},
	unique-id = {1951407},
	issn = {0324-6329},
	year = {2009},
	eissn = {0324-6329},
	pages = {265-298},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440; Jakab, Gusztáv/0000-0002-2569-5967}
}

@article{MTMT:1255465,
	title = {Review of the present-day geodynamics of the Pannonian basin: progress},
	url = {https://m2.mtmt.hu/api/publication/1255465},
	author = {Bada, G and Horváth, Ferenc and Gerner, P and Fejes, I},
	doi = {10.1016/S0264-3707(98)00013-1},
	journal-iso = {J GEODYN},
	journal = {JOURNAL OF GEODYNAMICS},
	volume = {27},
	unique-id = {1255465},
	issn = {0264-3707},
	abstract = {We present a comprehensive review on what we have learned during the
		last decade and what we need to know in the future about the
		present-day crustal deformation and geodynamics of the Pannonian basin
		and its surroundings,
		The recent tectonic activity of the region is controlled primarily by
		the counterclockwise rotation of the Adriatic microplate relative to
		Europe around a pole in the Western Alps. Due to the indentation of
		this crustal block against the Southern Alpine-Dinaric fold and thrust
		belt, intense shortening is effecting these orogens as evidenced by the
		general seismicity pattern and crustal deformation. The present-day
		kinematics of the Pannonian basin shows that the area is pushed from
		the south-southwest. As a result, strike-slip to compressive faulting
		is observed well inside the Pannonian basin and, furthermore, the
		nearly complete absence of normal faulting in the whole study area
		suggests that extension in the Pannonian basin has been finished and
		structural inversion is in progress. Due to an increase of intraplate
		compressional stress the Pannonian lithosphere exhibits large-scale
		bending manifested by the Quaternary subsidence and uplift history.
		The orientation of the modern tectonic stress field in and around the
		Pannonian basin shows a remarkable radial pattern of maximum horizontal
		stress around the Adriatic microplate. N-S directed compression
		observed at its northern tip in the Southern Alps gradually becomes
		NE-SW oriented along the Dinaric belt. This pattern is further
		traceable well inside the Pannonian basin, while in the Vrancea zone of
		the southeastern Carpathians E-W to ESE-WNW directed compression can be
		determined. Finite element stress modelling suggests that the stress
		regime in the Pannonian basin is governed by distinct tectonic factors
		in the overall convergent setting associated with the Africa-Europe
		collision. The most important stress source appears to be the active
		push of the Adriatic microplate, Additional boundary conditions, such
		as the deformation of crustal blocks with different geometry and
		rigidity at the margin of the Pannonian-Carpathian area and the effect
		of active compression in the Vrancea zone, significantly influence the
		stress regime and pattern.
		Finally, with a brief overview about the principal aims of the Central
		Europe Regional Geodynamic Project (CERGOP), we argue for the need of
		further investigations applying the latest techniques of space geodesy
		(GPS). This international cooperation can provide an excellent
		opportunity to further develop our understanding of the recent crustal
		deformation in Central Europe and to refine concepts and models about
		the tectonic inversion of sedimentary basins with back-are origin. (C)
		1999 Elsevier Science Ltd. All rights reserved.},
	year = {1999},
	pages = {501-527}
}

@article{MTMT:170374,
	title = {Palynological and plant macrofossil data on late Quaternary short term climatic oscillations in North-East Hungary},
	url = {https://m2.mtmt.hu/api/publication/170374},
	author = {Magyari, Enikő Katalin and Jakab, Gusztáv and Rudner, Edina and Sümegi, Pál},
	journal-iso = {ACTA PALAEOBOT},
	journal = {ACTA PALAEOBOTANICA},
	volume = {Suppl},
	unique-id = {170374},
	issn = {0001-6594},
	year = {1999},
	eissn = {2082-0259},
	pages = {491-502},
	orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Jakab, Gusztáv/0000-0002-2569-5967; Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:1177753,
	title = {Prehistoric land degradation in Hungary: who, how and why?},
	url = {https://m2.mtmt.hu/api/publication/1177753},
	author = {Willis, K J and Sümegi, Pál and Braun, Mihály and Bennett, K D and Tóth, Albert},
	doi = {10.1017/S0003598X00086312},
	journal-iso = {ANTIQUITY},
	journal = {ANTIQUITY: A QUARTERLY REVIEW OF WORLD ARCHAEOLOGY},
	volume = {72},
	unique-id = {1177753},
	issn = {0003-598X},
	year = {1998},
	eissn = {1745-1744},
	pages = {101-113},
	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:146539,
	title = {Re-evaluation of the Neolithic in Eastern Hungary based on calibrated radiocarbon dates},
	url = {https://m2.mtmt.hu/api/publication/146539},
	author = {Hertelendi, Ede and Kalicz, N and Raczky, Pál and Horváth, F and Veres, Mihály and Sudár Sándorné Svingor, Éva and Futó, István and Bartosiewicz, László},
	doi = {10.1017/S0033822200030691},
	journal-iso = {RADIOCARBON},
	journal = {RADIOCARBON},
	volume = {37},
	unique-id = {146539},
	issn = {0033-8222},
	year = {1995},
	eissn = {1945-5755},
	pages = {239-244},
	orcid-numbers = {Raczky, Pál/0000-0001-5556-723X}
}

@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:1255446,
	title = {TOWARDS A MECHANICAL MODEL FOR THE FORMATION OF THE PANNONIAN BASIN},
	url = {https://m2.mtmt.hu/api/publication/1255446},
	author = {Horváth, Ferenc},
	doi = {10.1016/0040-1951(93)90126-5},
	journal-iso = {TECTONOPHYSICS},
	journal = {TECTONOPHYSICS},
	volume = {226},
	unique-id = {1255446},
	issn = {0040-1951},
	abstract = {New maps showing crustal and lithospheric thickness variations in the
		Pannonian basin and the surrounding East Alpine, Carpathian and Dinaric
		mountains have been prepared on the basis of recent seismic,
		seismologic and electromagnetic data. A map presenting Miocene faults
		of regional significance has been also constructed for the same region
		by using a wealth of recently available national and/or more local
		studies. It is suggested that observed crustal and lithospheric
		structural contrasts have been controlled primarily by Neogene
		kinematic history of the region. Kinematic history is characterized by
		the following main patterns: (1) indentation by Adria and large-scale
		backthrusting in the Southern Alps; (2) eastward escape and extension
		of the Eastern Alps; (3) extensional collapse in the Pannonian basin
		area; (4) formation of broad wrench fault systems along strike in the
		Dinarides and Southern Carpathians, and the Western Carpathians with
		dextral and sinistral shear, respectively; (5) compression and
		accretion of the external thrust and fold belt in the Eastern
		Carpathians. These kinematic patterns are thought to be interrelated
		and all are manifestations of the late-stage evolution of an
		overthickened orogenic wedge.
		In order to arrive at a better understanding of the mechanism of
		extension, which formed the Pannonian basin, deep crustal seismic
		profiles, hydrocarbon exploration reflection lines and borehole data
		have been analyzed in the Little Hungarian Plain. This plain represents
		the transition zone between the Alps and the Pannonian lowlands, and
		the results are illustrated by eight interpreted cross-sections. One
		result of regional importance is the clear recognition that the
		Transdanubian Central Range at the southeastern flank of the Little
		Hungarian Plain is composed of Alpine (pre-Senonian) thrust sheets.
		This finding marks the end of a century of debate: the allochthony of
		the substrata of the Pannonian basin can be now considered proven.
		Another result of more general interest is that these cross-sections
		document the mode of lithospheric extension. Preexisting compressional
		detachment planes reactivate as low-angle normal faults and lead to
		tectonic unroofing of deeply buried metamorphic terranes characterized
		by ductile flow along subhorizontal lineation.},
	year = {1993},
	eissn = {1879-3266},
	pages = {333-357}
}

@article{MTMT:1177724,
	title = {Geochronologic and paleoclimatic characterization of Quaternary sediments in the Great Hungarian Plain},
	url = {https://m2.mtmt.hu/api/publication/1177724},
	author = {Hertelendi, Ede and Sümegi, Pál and Szöőr, Gy},
	doi = {10.1017/S0033822200064146},
	journal-iso = {RADIOCARBON},
	journal = {RADIOCARBON},
	volume = {34},
	unique-id = {1177724},
	issn = {0033-8222},
	year = {1992},
	eissn = {1945-5755},
	pages = {833-839},
	orcid-numbers = {Sümegi, Pál/0000-0003-1755-4440}
}

@article{MTMT:1659829,
	title = {A counter system for high-precision 14C dating},
	url = {https://m2.mtmt.hu/api/publication/1659829},
	author = {Hertelendi, Ede and Csongor, Éva and Záborszky, László and Molnár, József and Dajkó, Gábor and Győrffy, Miklós and Nagy, S},
	journal-iso = {RADIOCARBON},
	journal = {RADIOCARBON},
	volume = {31},
	unique-id = {1659829},
	issn = {0033-8222},
	keywords = {Software; radiocarbon dating; Carbon-14; DETECTOR; counter system; carbon-14 dating},
	year = {1989},
	eissn = {1945-5755},
	pages = {399-406}
}