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 - Kustár, Rozália AU - Molnár, Dávid AU - Sümegi, Pál AU - Törőcsik, Tünde AU - Sávai, Szilvia TI - Preliminary paleoecological reconstruction of long-term relationship between human and environment in the northern part of Danube-along Plain, Hungary JF - OPEN GEOSCIENCES J2 - OPEN GEOSCI VL - 8 PY - 2016 IS - 1 SP - 405 EP - 419 PG - 15 SN - 2391-5447 DO - 10.1515/geo-2016-0026 UR - https://m2.mtmt.hu/api/publication/3159156 ID - 3159156 N1 - Visky Károly Museum, Szent István krt. 25, Kalocsa, H-6300, Hungary Department of Geology and Palaeontolgy, University of Szeged, Egyetem u. 2-6, Szeged, H-6722, Hungary Institute of Archaeology, Hungarian Academy of Sciences, Úri u. 49, Budapest, H-1014, Hungary Cited By :4 Export Date: 25 May 2022 Correspondence Address: Kustár, R.; Visky Károly Museum, Szent István krt. 25, Hungary; email: rozina_kustar@t-online.hu LA - English DB - MTMT ER - TY - JOUR AU - Ruszkiczay-Rüdiger, Zsófia AU - Kern, Zoltán TI - Permafrost or seasonal frost? A review of paleoclimate proxies of the last glacial cycle in the East Central European lowlands JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 415 PY - 2016 SP - 241 EP - 252 PG - 12 SN - 1040-6182 DO - 10.1016/j.quaint.2015.07.027 UR - https://m2.mtmt.hu/api/publication/2932988 ID - 2932988 N1 - Export Date: 14 December 2020 Correspondence Address: Ruszkiczay-Rüdiger, Z.; Institute for Geological and Geochemical Research, Research Centre for Astronomy and Earth Sciences, MTA, Budaörsi út 45, Hungary; email: rrzsofi@geochem.hu AB - Our critical revision of the sedimentological characteristics and genetic interpretation of relict periglacial soil deformation features (cryoturbations and sand wedges) suggests that the continuous permafrost zone did not necessarily reached the lowland areas of the Pannonian Basin, as suggested by previous studies. The discontinuous permafrost zone most probably penetrated the north-western part of the study area for a certain period, but most of the lowlands might have been affected only by sporadic/isolated permafrost and/or deep seasonal frost. The re-evaluated climate conditions implied by the periglacial soil structures and other proxies for a periglacial environment of the area do not constrain such a narrow zone of extremely low mean annual air temperature (MAAT) and mean annual precipitation (MAP). The compilation of the climate thresholds suggested by the observed and revised interpretation cryoturbation features and thermal contraction cracks with other paleoclimate proxies converge on 0 +/- 2 degrees C MAAT and 300-490 mm MAP on the lowland areas of the Pannonian Basin during the coldest phase of the last glacial. These values indicate a temperature drop of congruent to 10 +/- 2 C degrees and a precipitation decrease of 30-50% relative to modern conditions. (C) 2015 Elsevier Ltd and INQUA. All rights reserved. LA - English DB - MTMT ER -