{ "labelLang" : "hun", "responseDate" : "2024-03-29 06:22", "content" : { "otype" : "JournalArticle", "mtid" : 2790432, "status" : "VALIDATED", "published" : true, "comment" : "Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Csatkai E. u. 6-8., Sopron, H-9400, Hungary \n Hertelendi Laboratory of Environmental Studies, Institute for Nuclear Research, Hungarian Academy of Sciences, Bem tér 18/C, Debrecen, H-4026, Hungary \n Department of Physical Geography, Eötvös Loránd University, Pazmany Peter setany 1/c, Budapest, H-1117, Hungary \n Department of Biology, Shinshu University, Matsumoto, 390-8621, Japan \n Department of Geology and Meteorology, University of Pécs, Ifjúság u. 6., Pécs, 7624, Hungary \n Environmental Analytical and Geoanalytical Research Group, Szentágothai Research Centre, University of Pécs, Ifjúság útja 20., Pécs, H-7624, Hungary \n Department of Environmental Engineering, Polláck Mihály Faculty of Engineering and Information Technology, University of Pécs, Rozmaring u. 17., Pécs, H-7634, Hungary \n Export Date: 15 October 2019 \n CODEN: QSRED \n Correspondence Address: Újvári, G.; Geodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Csatkai E. u. 6-8., Hungary; email: ujvari@ggki.hu\nFunding Agency and Grant Number: Hungarian Scientific Research FundOrszagos Tudomanyos Kutatasi Alapprogramok (OTKA) [OTKA PD-108639, OTKA PD-100315]; Bolyai Janos Research Scholarship of the Hungarian Academy of SciencesHungarian Academy of Sciences; EUEuropean Union (EU) [TAMOP-4.2.2.C-11/1/KONV-2012-0015, SROP-4.2.1.B-10/2/KONV-2010-0002, TAMOP-4.2.2.A-11/1/KONV-2012-0043]\n Funding text: This work has been funded by post doc projects from the Hungarian Scientific Research Fund to GU (OTKA PD-108639) and to AN (OTKA PD-100315). Additional financial support provided by the Bolyai Janos Research Scholarship of the Hungarian Academy of Sciences (GU) and the EU through the TAMOP-4.2.2.C-11/1/KONV-2012-0015 Earth System, the SROP-4.2.1.B-10/2/KONV-2010-0002 and ENVIKUT (TAMOP-4.2.2.A-11/1/KONV-2012-0043) projects is gratefully acknowledged. Special thanks to Christine Thiel, Jan-Pieter Buylaert and Andrew Murray for the fruitful discussions on post-IR IRSL dating and for the possibility to etching fine-grained samples at the Nordic Laboratory for Luminescence Dating, Riso National Laboratory, Roskilde, Denmark. Guest editor Achim Brauer and the two anonymous referees are thanked for their valuable input which helped us to refine the original manuscript substantially.\nGeodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Csatkai E. u. 6-8., Sopron, H-9400, Hungary \n Hertelendi Laboratory of Environmental Studies, Institute for Nuclear Research, Hungarian Academy of Sciences, Bem tér 18/C, Debrecen, H-4026, Hungary \n Department of Physical Geography, Eötvös Loránd University, Pazmany Peter setany 1/c, Budapest, H-1117, Hungary \n Department of Biology, Shinshu University, Matsumoto, 390-8621, Japan \n Department of Geology and Meteorology, University of Pécs, Ifjúság u. 6., Pécs, 7624, Hungary \n Environmental Analytical and Geoanalytical Research Group, Szentágothai Research Centre, University of Pécs, Ifjúság útja 20., Pécs, H-7624, Hungary \n Department of Environmental Engineering, Polláck Mihály Faculty of Engineering and Information Technology, University of Pécs, Rozmaring u. 17., Pécs, H-7634, Hungary \n Cited By :46 \n Export Date: 16 February 2021 \n CODEN: QSRED \n Correspondence Address: Újvári, G.; Geodetic and Geophysical Institute, Csatkai E. u. 6-8., Hungary; email: ujvari@ggki.hu \n Funding details: European Commission, EC \n Funding details: Magyar Tudományos Akadémia, MTA \n Funding details: Hungarian Scientific Research Fund, OTKA, PD-100315, OTKA PD-108639 \n Funding text 1: This work has been funded by post doc projects from the Hungarian Scientific Research Fund to GÚ ( OTKA PD-108639 ) and to ÁN ( OTKA PD-100315 ). Additional financial support provided by the Bolyai János Research Scholarship of the Hungarian Academy of Sciences (GÚ) and the EU through the TÁMOP-4.2.2.C-11/1/KONV‒2012-0015 Earth System, the SROP-4.2.1.B-10/2/KONV-2010-0002 and ENVIKUT (TÁMOP-4.2.2.A-11/1/KONV-2012-0043) projects is gratefully acknowledged. Special thanks to Christine Thiel, Jan-Pieter Buylaert and Andrew Murray for the fruitful discussions on post-IR IRSL dating and for the possibility to etching fine-grained samples at the Nordic Laboratory for Luminescence Dating, Risø National Laboratory, Roskilde, Denmark. Guest editor Achim Brauer and the two anonymous referees are thanked for their valuable input which helped us to refine the original manuscript substantially.\nGeodetic and Geophysical Institute, Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, Csatkai E. u. 6-8., Sopron, H-9400, Hungary \n Hertelendi Laboratory of Environmental Studies, Institute for Nuclear Research, Hungarian Academy of Sciences, Bem tér 18/C, Debrecen, H-4026, Hungary \n Department of Physical Geography, Eötvös Loránd University, Pazmany Peter setany 1/c, Budapest, H-1117, Hungary \n Department of Biology, Shinshu University, Matsumoto, 390-8621, Japan \n Department of Geology and Meteorology, University of Pécs, Ifjúság u. 6., Pécs, 7624, Hungary \n Environmental Analytical and Geoanalytical Research Group, Szentágothai Research Centre, University of Pécs, Ifjúság útja 20., Pécs, H-7624, Hungary \n Department of Environmental Engineering, Polláck Mihály Faculty of Engineering and 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change in the Carpathian Basin for the last 130 ka, with significant soil forming episodes during the Eemian interglacial (130–115 ka, MIS 5e) and in some subsequent MIS 5 stages, and distinct periods of loess accumulations during the MIS 4 and MIS 2. Charcoals from the sequence made it possible to test the accuracy of 14C ages from mollusc shells. This approach revealed that 14C ages from some gastropods having small shells (<10 mm) (Succinella oblonga, Vitrea crystallina) are statistically indistinguishable from the ages of charcoals, while others (Clausiliidae sp., Chondrula tridens) show age anomalies up to 600–800 years. OSL and pIRIR@290 ages are found to be consistently older, while post-IR OSL ages are younger than the 14C ages from charcoals and molluscs by some thousands of years, except for pIRIR@225 ages that match the radiocarbon ages quite well. OSL and IRSL ages have scatters up to 7–10 thousand years within 40 ka, while charcoals and small molluscs yield consistent ages with relatively low variability. Beyond the observation that some small molluscs seem to yield reliable 14C ages, calibrated 2σ age ranges of the radiocarbon data (ca 500–800 years for 20 to 30 ka) are an order of magnitude narrower than those of the OSL/IRSL methods (1800–4000 years for 25 to 35 ka). Thus, for establishing chronologies within 40 ka, which are both accurate and precise enough to address issues like synchroneity of millennial-scale paleoenvironmental events across regions (e.g. North Atlantic and Europe), AMS radiocarbon dating of shells of specific loess molluscs and charcoals may probably be a powerful chronological tool. 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