Stable isotopic and mineralogical investigations of an arid Quaternary lacustrine palaeoenvironment, Western Qaidam, China

Bojar, A. V.; Rieser, A.; Neubauer, F.; Bojar, H. P.; Genser, J.; Liu, Y.; Ge, X. H.

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Tytuł artykułu

Stable isotopic and mineralogical investigations of an arid Quaternary lacustrine palaeoenvironment, Western Qaidam, China

Autorzy

Bojar A. V. , Rieser A. , Neubauer F. , Bojar H. P. , Genser J. , Liu Y. , Ge X. H.

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Warianty tytułu

Konferencja

Stable isotope records of environmental change. European Society for Isotope Research. VII Isotope Workshop, Graz 2004

Języki publikacji

Abstrakty

Stable isotope analyses on carbonates from lake evaporites collected from the non-marine western Qaidam basin yield a positive excursion from Pliocene to Quaternary times. At Dafeng Shan, the Quaternary sequences are composed of alternating layers of celestine/dolomite and aragonite/calcite/barite with distinct isotopic compositions. The sequence described at Dafeng Shan formed in a low energy, hypersaline lacustrine environment as indicated by the microstructures and evaporitic minerals as well as by the absence of lithoclasts. The peloids, ooids and oncoids described are related to microbialactivities in saline lake. The oxygen isotopic composition of the carbonates vary between +34.4 and +39.8‰ (SMOW), representing the heaviest values measured until now. The δ¹⁸ O and the δ³⁴ S isotopic composition of the celestine range between 20.1 to 22.3‰ (SMOW) and +19 to +22‰ (CDT) respectively, suggesting sulfur recycling via sulfide oxidation. The carbon isotopic compositions of the carbonates show a large negative excursion of up to -30‰. The microstructures, mineralogy and isotopic compositions as well as the geological context suggest oxidation of methane from a deep source.

Słowa kluczowe

Qaidam Quaternary stable isotopes celestine carbonates hypersaline lacustrine environment

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2005

Tom

Vol. 49, No. 2

Strony

173--184

Opis fizyczny

Bibliogr. 82 poz., rys., tab.

Twórcy

autor

Bojar A. V.

ana-voica.bojar@uni-graz.at

Institute of Earth Science, Geology and Paleontology, Karl-Franzens University, A-8010 Graz, Austria

autor

Rieser A.

Department of Geography, Geology and Mineralogy, Divison General Geology and Geodynamics, Paris-Lodron University, A-5020 Salzburg, Austria

autor

Neubauer F.

Department of Geography, Geology and Mineralogy, Divison General Geology and Geodynamics, Paris-Lodron University, A-5020 Salzburg, Austria

autor

Bojar H. P.

Depar ment of Mineralogy, Landesmuseum Joanneum, A-8010 Graz, Austria

autor

Genser J.

Department of Geography, Geology and Mineralogy, Divison General Geology and Geodynamics, Paris-Lodron University, A-5020 Salzburg, Austria

autor

Liu Y.

Faculty of Earth Sciences, Jilin University, 130061 Changchun, China

autor

Ge X. H.

Faculty of Earth Sciences, Jilin University, 130061 Changchun, China

Bibliografia

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