TY - JOUR AU - Demény, Attila AU - Kern, Zoltán AU - Czuppon, György AU - Németh, Alexandra AU - Schöll-Barna, G AU - Siklósy, Z AU - Leél-Őssy, Szabolcs AU - Cook, G AU - Serlegi, Gábor AU - Bajnóczi, Bernadett AU - Sümegi, Pál AU - Király, Ágnes AU - Kiss, Viktória AU - Kulcsár, Gabriella AU - Bondár, Mária (Ködmönné) TI - Middle Bronze Age humidity and temperature variations, and societal changes in East-Central Europe JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 504 PY - 2019 SP - 80 EP - 95 PG - 16 SN - 1040-6182 DO - 10.1016/j.quaint.2017.11.023 UR - https://m2.mtmt.hu/api/publication/3298445 ID - 3298445 N1 - Available online 24 November 2017 Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi Str 45, Budapest, H-1112, Hungary Hertelendi Laboratory of Environmental Studies, Institute for Nuclear Research, MTA, Bem Tér, 18/c, Debrecen, H-4026, Hungary Department of Physical and Applied Geology, Eötvös Loránd University, Pázmány Péter Sétány. 1/C, Budapest, H-1117, Hungary Scottish Universities Environmental Research Centre, Rankine Avenue, Scottish Enterprise Technology Park, East Kilbride, Glasgow, Scotland G75 0QF, United Kingdom Institute of Archaeology, Research Centre for the Humanities, Hungarian Academy of Sciences, Tóth Kálmán Str 4, Budapest, H-1019, Hungary Department of Geology and Paleontology, University of Szeged, Egyetem Str 2, Szeged, H-6722, Hungary Export Date: 13 January 2021 Correspondence Address: Demény, A.; Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Budaörsi Str 45, Hungary; email: demeny@geochem.hu LA - English DB - MTMT ER - TY - JOUR AU - Szilágyi, Gábor AU - Náfrádi, Katalin AU - Sümegi, Pál TI - A preliminary chronological study to understand the construction phases of a Late Copper–Early Bronze Age kurgan (kunhalom) JF - CENTRAL EUROPEAN GEOLOGY J2 - CENT EUR GEOL VL - 62 PY - 2019 IS - 1 SP - 27 EP - 55 PG - 29 SN - 1788-2281 DO - 10.1556/24.61.2018.11 UR - https://m2.mtmt.hu/api/publication/30413691 ID - 30413691 N1 - Import hibák 2019-01-29 10:46 {"M3":"doi: 10.1556/24.61.2018.11"} doi: 10.1556/24.61.2018.11 Cited By :1 Export Date: 12 February 2021 Correspondence Address: Szilágyi, G.; Department of Nature Protection, Sumen Utca 2, Hungary; email: szilagyigabor@hnp.hu Funding text 1: The authors would like to thank Balázs Pál Sümegi and Tünde Töro˝csik for assisting in the sedimentological and magnetic susceptibility measurements, as well as Dr. Dávid Gergely Pál for assisting in the geochemical measurements. They would also like to express their special thanks to the Hortobágy National Park Directorate for the financial support provided. AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Törőcsik, Tünde AU - Sümegi, Pál TI - 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] JF - ARCHEOMETRIAI MŰHELY J2 - ARCHEOMETRIAI MŰHELY VL - 16 PY - 2019 IS - 3 SP - 245 EP - 270 PG - 26 SN - 1786-271X UR - https://m2.mtmt.hu/api/publication/31279285 ID - 31279285 N1 - Cited By :4 Export Date: 22 May 2022 Correspondence Address: Törőcsik, T.; University of Szeged, Egyetem street 2, Hungary; email: ttorocsik63@gmail.com AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Magyari, Enikő Katalin AU - Vincze, Ildikó AU - Orbán, Ildikó AU - Biró, Tamás AU - Pál, Ilona TI - Timing of major forest compositional changes and tree expansions in the Retezat Mts during the last 16,000 years JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 477 PY - 2018 SP - 40 EP - 58 PG - 19 SN - 1040-6182 DO - 10.1016/j.quaint.2017.12.054 UR - https://m2.mtmt.hu/api/publication/3320438 ID - 3320438 N1 - MTA-MTM-ELTE Research Group for Paleontology, Pázmány Péter stny. 1/C, Budapest, H-1117, Hungary Department of Environmental and Landscape Geography, Eötvös Loránd University, Pázmány Péter stny. 1/C, Budapest, H-1117, Hungary MTA Centre for Ecological Research, GINOP Sustainable Ecosystems Group, Klebelsberg Kuno u. 3, Tihany, 8237, Hungary Department of Physical and Applied Geology, Eötvös Loránd University, Pázmány Péter stny. 1/C, Budapest, H-1117, Hungary Department of Plant Systematics, Ecology and Theoretical Biology, Eötvös Loránd University, Pázmány Péter stny. 1/C, Budapest, 1117, Hungary Department of Physical Geography, Eötvös Loránd University, Pázmány Péter stny. 1/C, Budapest, H-1117, Hungary MTA ATOMKI, Bem tér 18/C., Debrecen, 4026, Hungary Cited By :7 Export Date: 14 November 2019 Correspondence Address: Magyari, E.; MTA-MTM-ELTE Research Group for Paleontology, Pázmány Péter stny. 1/C, Hungary; email: emagyari@caesar.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Szilágyi, Gábor AU - Sümegi, Pál AU - Gulyás, Sándor AU - Molnár, Dávid TI - 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 JF - RADIOCARBON J2 - RADIOCARBON VL - 60 PY - 2018 IS - 5 SP - 1403 EP - 1412 PG - 10 SN - 0033-8222 DO - 10.1017/RDC.2018.107 UR - https://m2.mtmt.hu/api/publication/30330204 ID - 30330204 N1 - University of Szeged, Department of Geology and Paleontology, Egyetem street 2, Szeged, H-6722, Hungary Hortobágyi National Park Directorate, Sumen street 2, Debrecen, H-4024, Hungary Hungarian Academy of Sciences, Research Centre for the Humanities Institute of Archaeology, Tóth Kálmán street 4, Budapest, 1097, Hungary Export Date: 12 February 2021 CODEN: RACAA Correspondence Address: Szilágyi, G.; University of Szeged, Egyetem street 2, Hungary; email: szilagyigabor@hnp.hu LA - English DB - MTMT ER - TY - JOUR AU - Tapody, Réka Orsolya AU - Gulyás, Sándor AU - Törőcsik, Tünde AU - Sümegi, Pál AU - Molnár, Dávid AU - Sümegi, B P AU - Molnár, Mihály TI - Radiocarbon-dated peat development. anthropogenic and climatic signals in a Holocene raised bog and lake profile from the Eastern part of the Carpathian Basin TS - anthropogenic and climatic signals in a Holocene raised bog and lake profile from the Eastern part of the Carpathian Basin JF - RADIOCARBON J2 - RADIOCARBON VL - 60 PY - 2018 IS - 4 SP - 1215 EP - 1226 PG - 12 SN - 0033-8222 DO - 10.1017/RDC.2018.38 UR - https://m2.mtmt.hu/api/publication/3388045 ID - 3388045 N1 - \n Department of Geology and Palaeontology, University of Szeged, Egyetem street 2, Szeged, 6722, Hungary \n Archaeological Institute of Hungarian Academy of Sciences, Úri street 49, Budapest, Hungary \n Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Hungarian Academy of Sciences (Atomki), Bem tér 18/c, Debrecen, 4026, Hungary \n Export Date: 6 November 2018 \n CODEN: RACAA \n Correspondence Address: Tapody, R.O.; Department of Geology and Palaeontology, University of Szeged, Egyetem street 2, Hungary; email: tapody@geo.u-szeged.hu Department of Geology and Palaeontology, University of Szeged, Egyetem street 2, Szeged, 6722, Hungary Archaeological Institute of Hungarian Academy of Sciences, Úri street 49, Budapest, Hungary Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research, Hungarian Academy of Sciences (Atomki), Bem tér 18/c, Debrecen, 4026, Hungary Export Date: 22 February 2021 CODEN: RACAA Correspondence Address: Tapody, R.O.; Department of Geology and Palaeontology, Egyetem street 2, Hungary; email: tapody@geo.u-szeged.hu LA - English DB - MTMT ER - TY - JOUR AU - Horváth, Ferenc AU - Musitz, Balázs AU - Balázs, Attila AU - Végh, Andor AU - Uhrin, András AU - Nádor, Annamária AU - Koroknai, B AU - Pap, Norbert AU - Tóth, Tamás AU - Wórum, G TI - Evolution of the Pannonian basin and its geothermal resources JF - GEOTHERMICS J2 - GEOTHERMICS VL - 53 PY - 2015 SP - 328 EP - 352 PG - 25 SN - 0375-6505 DO - 10.1016/j.geothermics.2014.07.009 UR - https://m2.mtmt.hu/api/publication/2719067 ID - 2719067 N1 - Geomega Ltd., Mester u. 4, H-1095 Budapest, Hungary Department of Geophysics and Space Sciences, Eötvös Loránd University, Pázmány Péter st. 1/c, H-1117 Budapest, Hungary Geological and Geophysical Institute of Hungary, Stefánia út 14, H-1442 Budapest, Hungary Department of Political Geography and Regional Development, University of Pécs, Vasvári Pál u. 4., H-7622 Pécs, Hungary Eriksfiord AS, Prof. Olav Hanssens vei 7A, Ipark, N-4021 Stavanger, Norway Utrecht University, Faculty of Geosciences, Utrecht, Netherlands Cited By :74 Export Date: 18 December 2018 CODEN: GTMCA Correspondence Address: Horváth, F.; MOL Hungarian Oil and Gas Company Plc, Október huszonharmadika u. 18, H-1117, Hungary; email: frankh@ludens.elte.hu LA - English DB - MTMT ER - TY - JOUR AU - Feurdean, A AU - Perşoiu, A AU - Tanţău, I AU - Stevens, T AU - Magyari, Enikő Katalin AU - Onac, BP AU - Marković, S AU - Andrič, M AU - Connor, S AU - Fărcaş, S AU - Gałka, M AU - Gaudenyi, Tivadar AU - Hoek, W AU - Kolaczek, P AU - Kuneš, P AU - Lamentowicz, M AU - Marinova, E AU - Michczyńska, DJ AU - Perşoiu, I AU - Płóciennik, M AU - Słowiński, M AU - Stancikaite, M AU - Sümegi, Pál AU - Svensson, A AU - Tămaş, T AU - Timar, A AU - Tonkov, S AU - Tóth, Mónika AU - Veski, S AU - Willis, KJ AU - Zernitskaya, V TI - Climate variability and associated vegetation response throughout Central and Eastern Europe (CEE) between 60 and 8 ka JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 106 PY - 2014 SP - 206 EP - 224 PG - 19 SN - 0277-3791 DO - 10.1016/j.quascirev.2014.06.003 UR - https://m2.mtmt.hu/api/publication/2706681 ID - 2706681 N1 - Available online 1 July 2014 AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Magyari, Enikő Katalin AU - Kunes, P AU - Jakab, Gusztáv AU - Sümegi, Pál AU - Pelánková, B AU - Schabitz, F AU - Braun, Mihály AU - Chytry, M TI - Late Pleniglacial vegetation in eastern-central Europe: are there modern analogues in Siberia? JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 95 PY - 2014 SP - 60 EP - 79 PG - 20 SN - 0277-3791 DO - 10.1016/j.quascirev.2014.04.020 UR - https://m2.mtmt.hu/api/publication/2594039 ID - 2594039 LA - English DB - MTMT ER - TY - JOUR AU - Braun, Mihály AU - Hubay, Katalin AU - Magyari, Enikő Katalin AU - Veres, D AU - Papp, István AU - Bálint, M TI - Using linear discriminant analysis (LDA) of bulk lake sediment geochemical data to reconstruct lateglacial climate changes in the South Carpathian Mountains JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 293 PY - 2013 SP - 114 EP - 122 PG - 9 SN - 1040-6182 DO - 10.1016/j.quaint.2012.03.025 UR - https://m2.mtmt.hu/api/publication/1979868 ID - 1979868 N1 - Available online 21 March 2012 LA - English DB - MTMT ER - TY - JOUR AU - Molnár, Mihály AU - Janovics, Róbert AU - Major, István AU - Orsovszki, J AU - Gönczi, R AU - Veres, Mihály AU - Leonard, A G AU - Castle, S M AU - Lange, T E AU - Wacker, L AU - Hajdas, I AU - T Jull, A J TI - Status Report of the New AMS 14C Sample Preparation Lab of the Hertelendi Laboratory of Environmental Studies (Debrecen, Hungary) JF - RADIOCARBON J2 - RADIOCARBON VL - 55 PY - 2013 IS - 2-3 SP - 665 EP - 676 PG - 12 SN - 0033-8222 DO - 10.2458/azu_js_rc.55.16394 UR - https://m2.mtmt.hu/api/publication/2402859 ID - 2402859 N1 - Institute of Nuclear Research of the Hungarian Academy of Sciences (ATOMKI), Debrecen, Hungary Isotoptech Zrt, Debrecen, Hungary NSF Arizona AMS Laboratory, University of Arizona, Tucson, AZ, United States Laboratory of Ion Beam Physics, ETHZ, Zürich, Switzerland Export Date: 15 October 2019 CODEN: RACAA Correspondence Address: Molnár, M.; Institute of Nuclear Research of the Hungarian Academy of Sciences (ATOMKI), Debrecen, Hungary; email: molnar.mihaly@atomki.mta.hu WoS:hiba:000325752100054 2020-12-10 18:46 DOI azonosító nem egyezik Institute of Nuclear Research of the Hungarian Academy of Sciences (ATOMKI), Debrecen, Hungary Isotoptech Zrt, Debrecen, Hungary NSF Arizona AMS Laboratory, University of Arizona, Tucson, AZ, United States Laboratory of Ion Beam Physics, ETHZ, Zürich, Switzerland Export Date: 3 May 2021 CODEN: RACAA Correspondence Address: Molnár, M.; Institute of Nuclear Research of the Hungarian Academy of Sciences (ATOMKI), Debrecen, Hungary; email: molnar.mihaly@atomki.mta.hu LA - English DB - MTMT ER - TY - JOUR AU - Náfrádi, Katalin AU - Jakab, Gusztáv AU - Sümegi, Pál AU - Szelepcsényi, Zoltán AU - Törőcsik, Tünde TI - Future Climate Impacts in Woodland and Forest Steppe Based on Holocene Paleoclimatic Trends, Paleobotanical Change in Central Part of the Carpathian Basin (Hungary) JF - AMERICAN JOURNAL OF PLANT SCIENCES (AJPS) J2 - AM J PLANT SCI VL - 4 PY - 2013 IS - 6 SP - 1187 EP - 1203 PG - 17 SN - 2158-2742 DO - 10.4236/ajps.2013.46147 UR - https://m2.mtmt.hu/api/publication/2333500 ID - 2333500 AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Magyari, Enikő Katalin AU - Dániel, Péter AU - Molnár, Mihály AU - Törőcsik, Tünde TI - Responses of terrestrial ecosystems to Dansgaard–Oeshger cycles and Heinrich-events: A 28,000-year record of environmental changes from SE Hungary JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 293 PY - 2013 SP - 34 EP - 50 PG - 17 SN - 1040-6182 DO - 10.1016/j.quaint.2012.07.032 UR - https://m2.mtmt.hu/api/publication/2203162 ID - 2203162 N1 - Available online 5 August 2012 AB - 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. LA - English DB - MTMT ER - TY - BOOK AU - Bondár, Mária (Ködmönné) TI - Prehistoric wagon models in the Carpathian Basin (3500-1500 BC) T3 - Varia Archaeologica Hungarica, ISSN 1216-6847 ; 32. ET - 0 PB - Archaeolingua CY - Budapest PY - 2012 SP - 142 SN - 9789639911345 UR - https://m2.mtmt.hu/api/publication/2154565 ID - 2154565 LA - English DB - MTMT ER - TY - JOUR AU - Gerling, C AU - Bánffy, Eszter AU - Dani, János AU - Köhler, Kitti AU - Kulcsár, Gabriella AU - Pike, AWG AU - Szeverényi, Vajk AU - Heyd, V TI - Immigration and transhumance in the Early Bronze Age Carpathian Basin: the occupants of a kurgan JF - ANTIQUITY: A QUARTERLY REVIEW OF WORLD ARCHAEOLOGY J2 - ANTIQUITY VL - 86 PY - 2012 IS - 334 SP - 1097 EP - 1111 PG - 15 SN - 0003-598X DO - 10.1017/S0003598X00048274 UR - https://m2.mtmt.hu/api/publication/30864769 ID - 30864769 AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Magyari, Enikő Katalin AU - Jakab, Gusztáv AU - Bálint, M AU - Kern, Zoltán AU - Buczkó, Krisztina AU - Braun, Mihály TI - Rapid vegetation response to lateglacial and early Holocene climatic fluctuation in the South Carpathian Mountains (Romania). JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 35 PY - 2012 SP - 116 EP - 130 PG - 15 SN - 0277-3791 DO - 10.1016/j.quascirev.2012.01.006 UR - https://m2.mtmt.hu/api/publication/1846857 ID - 1846857 N1 - Funding Agency and Grant Number: European Commission [MERG-CT-2006-041088]; Bolyai Scholarship [BO/00518/07]; OTKA [PD73234, NF 101362]; LOEWE - Landes-Offensive zur Entwicklung Wissen-schaftlich-okonomischer Exzellenz of Hesse's Ministry of Higher Education, Research, and the Arts Funding text: This research was supported by the European Commission through a Marie Curie Reintegration Grant held by E. K. Magyari (MERG-CT-2006-041088: Combining Palaeoecology and Palaeogenetics), the Bolyai Scholarship (BO/00518/07) and OTKA Research Fund (PD73234, NF 101362). This is MTA-MTM Paleo Contribution No. 145. M. Mint is supported by the research funding program LOEWE - Landes-Offensive zur Entwicklung Wissen-schaftlich-okonomischer Exzellenz of Hesse's Ministry of Higher Education, Research, and the Arts. We would like to thank the help of the Retezat National Park. Aron Nemes and Zoltan Kohan are acknowledged for drawing Fig. 1. LA - English DB - MTMT ER - TY - JOUR AU - Schöll-Barna, Gabriella AU - Demény, Attila AU - Serlegi, Gábor AU - Fábián, Szilvia AU - Sümegi, Pál AU - Fórizs, István AU - Bajnóczi, Bernadett TI - Climatic variability in the Late Copper Age: Stable isotope fluctuation of prehistoric Unio pictorum (Unionidae) shells from Lake Balaton (Hungary) JF - JOURNAL OF PALEOLIMNOLOGY J2 - J PALEOLIMNOL VL - 47 PY - 2012 IS - 1 SP - 87 EP - 100 PG - 14 SN - 0921-2728 DO - 10.1007/s10933-011-9561-6 UR - https://m2.mtmt.hu/api/publication/1792003 ID - 1792003 N1 - Megjegyzés-23475523 FN: Thomson Reuters Web of Knowledge LA - English DB - MTMT ER - TY - JOUR AU - Gulyás, Sándor AU - Sümegi, Pál TI - Farming and/or foraging? New environmental data to the life and economic transformation of Late Neolithic tell communities (Tisza Culture) in SE Hungary JF - JOURNAL OF ARCHAEOLOGICAL SCIENCE J2 - J ARCHAEOL SCI VL - 38 PY - 2011 IS - 12 SP - 3323 EP - 3339 PG - 17 SN - 0305-4403 DO - 10.1016/j.jas.2011.07.019 UR - https://m2.mtmt.hu/api/publication/1943039 ID - 1943039 N1 - Megjegyzés-22302347 WC: Anthropology; Archaeology; Geosciences, Multidisciplinary AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Gulyás, Sándor AU - Sümegi, Pál TI - 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) JF - JOURNAL OF ARCHAEOLOGICAL SCIENCE J2 - J ARCHAEOL SCI VL - 38 PY - 2011 IS - 10 SP - 2683 EP - 2695 PG - 13 SN - 0305-4403 DO - 10.1016/j.jas.2011.06.005 UR - https://m2.mtmt.hu/api/publication/1943040 ID - 1943040 N1 - Funding Agency and Grant Number: Departments of Geology and Geography, University of Szeged, Hungary [TAMOP-4.2.1/B-09/1/KONV-2010-0005] Funding text: The authors would like to express their gratitude to all colleagues working at the Department of Geology and Paleontology, University of Szeged for assisting in the technical part of the paper preparation and a part of the labwork. Special thanks to Ferenc Horvath at the Mora Museum of Szeged for granting access to the material subjected to analysis. Also to Robert Kovacs in his assistance in labwork. Work was supported from the research fund of Departments of Geology and Geography, University of Szeged, Hungary no. TAMOP-4.2.1/B-09/1/KONV-2010-0005. Finally, thanks are due to the editorial board of The Journal of Archaeological Science and the two reviewers whose comments made the final version of this paper stronger and clearer than early drafts. AB - 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. LA - English DB - MTMT ER - TY - CHAP AU - Magyari, Enikő Katalin AU - Robert, Shiel AU - David, Passmore TI - Introduction. The paleo-environment and settlement context of Polgár-10 TS - The paleo-environment and settlement context of Polgár-10 T2 - 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 PB - Archaeopress Publishing Ltd CY - Oxford T3 - BAR International Series, ISSN 0143-3059 PY - 2010 UR - https://m2.mtmt.hu/api/publication/2877642 ID - 2877642 LA - English DB - MTMT ER - TY - JOUR AU - Krezsek, C AU - Filipescu, S AU - Silye, Lóránd AU - Matenco, L AU - Doust, H TI - Miocene facies associations and sedimentary evolution of the Southern Transylvanian Basin (Romania): Implications for hydrocarbon exploration JF - MARINE AND PETROLEUM GEOLOGY J2 - MAR PETROL GEOL VL - 27 PY - 2010 IS - 1 SP - 191 EP - 214 PG - 24 SN - 0264-8172 DO - 10.1016/j.marpetgeo.2009.07.009 UR - https://m2.mtmt.hu/api/publication/2588298 ID - 2588298 AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Magyari, Enikő Katalin AU - Chapman, J C AU - Passmore, D G AU - Allen, J R M AU - Huntley, J P AU - Huntley, B TI - Holocene persistence of wooded steppe in the Great Hungarian Plain JF - JOURNAL OF BIOGEOGRAPHY J2 - J BIOGEOGR VL - 37 PY - 2010 IS - 5 SP - 915 EP - 935 PG - 21 SN - 0305-0270 DO - 10.1111/j.1365-2699.2009.02261.x UR - https://m2.mtmt.hu/api/publication/1431870 ID - 1431870 N1 - idézet a 917.és a 925. oldalon LA - English DB - MTMT ER - TY - JOUR AU - Magyari, Enikő Katalin AU - Buczkó, Krisztina AU - Jakab, Gusztáv AU - Braun, Mihály AU - Pal, Z AU - Karátson, Dávid AU - Papp, István TI - Palaeolimnology of the last crater lake in the Eastern Carpathian Mountains: a multiproxy study of Holocene hydrological changes JF - HYDROBIOLOGIA J2 - HYDROBIOLOGIA VL - 631 PY - 2009 IS - 1 SP - 29 EP - 63 PG - 35 SN - 0018-8158 DO - 10.1007/s10750-009-9801-1 UR - https://m2.mtmt.hu/api/publication/1803133 ID - 1803133 N1 - Cited By :73 Export Date: 26 May 2022 CODEN: HYDRB Correspondence Address: Magyari, E.; Hungarian Natural History Museum, P.O. Box 222, Budapest 1476, Hungary; email: magyari@bot.nhmus.hu AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Sümegi, Pál AU - Jakab, Gusztáv AU - Majkut, P AU - Törőcsik, Tünde AU - Zatykó, Csilla TI - Middle Age paleoecological and paleoclimatological reconstruction in the Carpathian Basin JF - IDŐJÁRÁS / QUARTERLY JOURNAL OF THE HUNGARIAN METEOROLOGICAL SERVICE J2 - IDŐJÁRÁS VL - 113 PY - 2009 IS - 4 SP - 265 EP - 298 PG - 34 SN - 0324-6329 UR - https://m2.mtmt.hu/api/publication/1951407 ID - 1951407 N1 - Megjegyzés-24810357 Admin megjegyzés-24439248 #JournalID1# Name: Ido;; járás QJ Hungarian Meteorol. Service ISSN: 0324-6329 #JournalID2# LA - English DB - MTMT ER - TY - JOUR AU - Bada, G AU - Horváth, Ferenc AU - Gerner, P AU - Fejes, I TI - Review of the present-day geodynamics of the Pannonian basin: progress JF - JOURNAL OF GEODYNAMICS J2 - J GEODYN VL - 27 PY - 1999 IS - 4-5 SP - 501 EP - 527 PG - 27 SN - 0264-3707 DO - 10.1016/S0264-3707(98)00013-1 UR - https://m2.mtmt.hu/api/publication/1255465 ID - 1255465 N1 - Dept. of Appl. and Environ. Geology, Eötvös University, Múzeum krt. 4/A, H-1088 Budapest, Hungary Department of Geophysics, Eötvös University, Ludovika tér 2, H-1083 Budapest, Hungary FÖMI Satellite Geodetic Observ., P.O. Box 546, H-1373 Budapest, Hungary Cited By :108 Export Date: 11 November 2022 Correspondence Address: Bada, G.; Dept. of Appld. and Env'l. Geology, Muzeum krt, 4/A, H-1088 Budapest, Hungary; email: bada@iris.elte.hu Funding details: Hungarian Science Foundation, T 019393 Funding text 1: We acknowledge the help ofÁ. Simon and T. Borza (both FÖMI Satellite Geodetic Observatory, Hungary) in the course of this study. Editorial help and patience of W. Jacoby (Mainz, Germany) is greatly appreciated. Reviews of K. Rebenauer-Lieb (Auckland, New-Zealand) and three journal reviewers helped us to significantly improve the quality of this paper. G. Bada is grateful for the advises and encouragement of S. Cloetingh and M. Gölke (Amsterdam, the Netherlands). This work has been financially supported by the CERGOP project (contracts CIPA-CT94-0114 and MUI/TP/18/1995), the IBS (Integrated Basin Studies) project of the European Community (contract JOU2-CT92-0110), and the Hungarian Science Foundation OTKA (T 019393). AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Magyari, Enikő Katalin AU - Jakab, Gusztáv AU - Rudner, Edina AU - Sümegi, Pál TI - Palynological and plant macrofossil data on late Quaternary short term climatic oscillations in North-East Hungary JF - ACTA PALAEOBOTANICA J2 - ACTA PALAEOBOT VL - Suppl PY - 1999 IS - 2 SP - 491 EP - 502 PG - 12 SN - 0001-6594 UR - https://m2.mtmt.hu/api/publication/170374 ID - 170374 LA - English DB - MTMT ER - TY - JOUR AU - Willis, K J AU - Sümegi, Pál AU - Braun, Mihály AU - Bennett, K D AU - Tóth, Albert TI - Prehistoric land degradation in Hungary: who, how and why? JF - ANTIQUITY: A QUARTERLY REVIEW OF WORLD ARCHAEOLOGY J2 - ANTIQUITY VL - 72 PY - 1998 IS - 275 SP - 101 EP - 113 PG - 13 SN - 0003-598X DO - 10.1017/S0003598X00086312 UR - https://m2.mtmt.hu/api/publication/1177753 ID - 1177753 N1 - Nincs jelölve a levelező szerzőség a közleményen. (SE SZTE admin5) LA - English DB - MTMT ER - TY - JOUR AU - Willis, K J AU - Braun, Mihály AU - Sümegi, Pál AU - Tóth, Albert TI - Does soil change cause vegetation change or vice versa? A temporal perspective from Hungary JF - ECOLOGY J2 - ECOLOGY VL - 78 PY - 1997 IS - 3 SP - 740 EP - 750 PG - 11 SN - 0012-9658 DO - 10.1890/0012-9658(1997)078[0740:DSCCVC]2.0.CO;2 UR - https://m2.mtmt.hu/api/publication/1177751 ID - 1177751 N1 - Nincs jelölve a levelező szerzőség a közleményen. (SE SZTE admin5) LA - English DB - MTMT ER - TY - JOUR AU - Hertelendi, Ede AU - Kalicz, N AU - Raczky, Pál AU - Horváth, F AU - Veres, Mihály AU - Sudár Sándorné Svingor, Éva AU - Futó, István AU - Bartosiewicz, László TI - Re-evaluation of the Neolithic in Eastern Hungary based on calibrated radiocarbon dates JF - RADIOCARBON J2 - RADIOCARBON VL - 37 PY - 1995 IS - 2 SP - 239 EP - 244 PG - 6 SN - 0033-8222 DO - 10.1017/S0033822200030691 UR - https://m2.mtmt.hu/api/publication/146539 ID - 146539 LA - English DB - MTMT ER - TY - JOUR AU - Willis, K J AU - Sümegi, Pál AU - Braun, Mihály AU - Tóth, Albert TI - The Late Quaternary environmental history of Bátorliget, N.E. Hungary JF - PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY J2 - PALAEOGEOGR PALAEOCL VL - 118 PY - 1995 IS - 1-2 SP - 25 EP - 47 PG - 23 SN - 0031-0182 DO - 10.1016/0031-0182(95)00004-6 UR - https://m2.mtmt.hu/api/publication/1177745 ID - 1177745 N1 - Nincs jelölve a levelező szerzőség a közleményen. (SE SZTE admin5) LA - English DB - MTMT ER - TY - JOUR AU - Horváth, Ferenc TI - TOWARDS A MECHANICAL MODEL FOR THE FORMATION OF THE PANNONIAN BASIN JF - TECTONOPHYSICS J2 - TECTONOPHYSICS VL - 226 PY - 1993 IS - 1-4 SP - 333 EP - 357 PG - 25 SN - 0040-1951 DO - 10.1016/0040-1951(93)90126-5 UR - https://m2.mtmt.hu/api/publication/1255446 ID - 1255446 AB - 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. LA - English DB - MTMT ER - TY - JOUR AU - Hertelendi, Ede AU - Sümegi, Pál AU - Szöőr, Gy TI - Geochronologic and paleoclimatic characterization of Quaternary sediments in the Great Hungarian Plain JF - RADIOCARBON J2 - RADIOCARBON VL - 34 PY - 1992 IS - 3 SP - 833 EP - 839 PG - 7 SN - 0033-8222 DO - 10.1017/S0033822200064146 UR - https://m2.mtmt.hu/api/publication/1177724 ID - 1177724 LA - English DB - MTMT ER - TY - JOUR AU - Hertelendi, Ede AU - Csongor, Éva AU - Záborszky, László AU - Molnár, József AU - Dajkó, Gábor AU - Győrffy, Miklós AU - Nagy, S TI - A counter system for high-precision 14C dating JF - RADIOCARBON J2 - RADIOCARBON VL - 31 PY - 1989 SP - 399 EP - 406 PG - 8 SN - 0033-8222 UR - https://m2.mtmt.hu/api/publication/1659829 ID - 1659829 N1 - [P06935] ATKI1989/0241 LA - English DB - MTMT ER -