Central European Geology
Volume/Issue:
Volume 55: Issue 4
Stable isotope compositions of bivalve shells and geochemistry of bulk sediments in a 5–20 ky fluvial section at Körösladány, SE Hungary: Sedimentary changes vs. climate signals
Authors:
Attila Demény Institute for Geological and Geochemical Research Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, H-1112, Budapet, Budaörsi út 45, Hungary

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Gabriella Schöll-Barna Institute for Geological and Geochemical Research Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, H-1112, Budapet, Budaörsi út 45, Hungary

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Pál Sümegi Department of Geology and Palaeontology, University of Szeged, H-6722, Szeged, Egyetem u. 2, Hungary

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Péter Sipos Institute for Geological and Geochemical Research Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, H-1112, Budapet, Budaörsi út 45, Hungary

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István Fórizs Institute for Geological and Geochemical Research Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, H-1112, Budapet, Budaörsi út 45, Hungary

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Brigitta Réka Balázs Institute for Geological and Geochemical Research Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, H-1112, Budapet, Budaörsi út 45, Hungary

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Bernadett Bajnóczi Institute for Geological and Geochemical Research Research Centre for Astronomy and Earth Sciences, Hungarian Academy of Sciences, H-1112, Budapet, Budaörsi út 45, Hungary

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Gordon Cook Scottish Universities Environmental Research Centre, Rankine Avenue, Scottish Enterprise Technology Park, East Kilbride, Glasgow, Scotland, G75 0QF, UK

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Pages:
417–439
Online Publication Date:
01 Dec 2012
Publication Date:
01 Dec 2012
Article Category:
Research Article
DOI:
https://doi.org/10.1556/ceugeol.55.2012.4.4
Keywords:
Pleistocene-Holocene transition; Late Glacial; stable isotopes; geochemistry; fluvial sediments; Unio crassus ; Sphaerium rivicola
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Abstract

In this paper we present sedimentological and geochemical data for a section of fluvial deposits from SE Hungary covering the period from about 20 to 5 ky BP. Major and trace element geochemistry of bulk sediments as well as stable C and O isotope compositions of the carbonate content indicate significant changes in depositional facies and/or sediment provenance as well as climate conditions. Variations in bulk sediment Sr, TiO2 and P2O5 concentrations were correlated with major climate change events following the Late Glacial Maximum that support the age model established on the basis of AMS 14C age data. Bulk sediment Sr concentrations and stable C and O isotope compositions of bulk sediment carbonate were determined by changes in denudation of carbonate rocks in the recharge area. The Sr and C-O isotope patterns show correlations with global temperature changes during the Pleistocene-Holocene transition. However, TiO2 and P2O5 contents show correspondence with humidity changes, suggesting variations in chemical weathering. In addition to the sedimentological effects, C and O isotope compositions of Unio crassus shell fragments show strong changes at the Pleistocene-Holocene transition, indicating that the bivalve shells can reflect climate conditions. On the other hand, shorter climate change events were difficult to track in the isotope records due to the competing fractionation processes. The combined evaluation of chemical and isotopic compositions revealed that beside the globally important Younger Dryas and Bølling/Allerød periods, the Ságvár-Lascaux interstadial was of local importance, in accordance with earlier studies.

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Central European Geology
Print ISSN:
1788-2281
Online ISSN:
1789-3348

Senior editors

Editor(s)-in-Chief: Attila DEMÉNY

Deputy Editor(s)-in-Chief: Béla RAUCSIK

Co-ordinating Editor(s): Gábor SCHMIEDL

Editorial Board

  • Zsolt BENKÓ (Geochemistry, Ar dating; Institute for Nuclear Research, Debrecen)
  • Szabolcs HARANGI (Petrology, geochemistry, volcanology; Eötvös Loránd University, Budapest)
  • Anette GÖTZ (Sedimentology; Landesamt für Bergbau, Energie und Geologie, Hannover)
  • János HAAS (Regional Geology and Sedimentology; Eötvös Loránd University, Budapest)
  • István Gábor HATVANI (Geomathematics; Institute for Geological and Geochemical Research, Budapest)
  • Henry M. LIEBERMAN (Language Editor; Salt Lake City)
  • János KOVÁCS (Quaternary geology; University of Pécs)
  • Szilvia KÖVÉR (Sedimentology; Eötvös Loránd University, Budapest)
  • Tivadar M. TÓTH (Mineralogy; Petrology    University of Szeged)
  • Stephen J. MOJZSIS (Petrology, geochemistry and planetology; University of Colorado Boulder)
  • Norbert NÉMETH (Structural geology; University of Miskolc)
  • Attila ŐSI (Paleontology; Eötvös Loránd University, Budapest)
  • József PÁLFY (Fossils and Stratigraphic Records; Eötvös Loránd University, Budapest)
  • György POGÁCSÁS (Petroleum Geology; Eötvös Loránd University, Budapest)
  • Krisztina SEBE (Tectonics, sedimentology, geomorphology University of Pécs)
  • Ioan SEGHEDY (Petrology and geochemistry; Institute of Geodynamics, Bucharest)
  • Lóránd SILYE (Paleontology; Babeș-Bolyai University, Cluj-Napoca)
  • Ákos TÖRÖK (Applied and Environmental Earth Sciences; Budapest University of Technology and Economics, Budapest)
  • Norbert ZAJZON (Petrology and geochemistry; University of Miskolc)
  • Ferenc MOLNÁR (ore geology, geochemistry, geochronology, archaeometry; Geological Survey of Finland, Espoo)

Advisory Board

Due to the changes in editorial functions, the Advisory Board has been terminated. The participation of former Advisory Board members is highly appreciated and gratefully thanked.

CENTRAL EUROPEAN GEOLOGY
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Central European Geology
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Vol 64- : A4
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