New luminescence-based geochronology framing the last two glacial cycles at the southern limit of European Pleistocene loess in Stalać (Serbia)

Bösken, J.; Klasen, N.; Zeeden, Ch.; Obreht, I.; Marković, S. B.; Hambach, U.; Lehmkuhl, F.

doi:10.1515/geochr-2015-0062

Artykuł - szczegóły

Tytuł artykułu

New luminescence-based geochronology framing the last two glacial cycles at the southern limit of European Pleistocene loess in Stalać (Serbia)

Autorzy

Bösken J. , Klasen N. , Zeeden Ch. , Obreht I. , Marković S. B. , Hambach U. , Lehmkuhl F.

Wybrane pełne teksty z tego czasopisma

Identyfikatory

DOI

10.1515/geochr-2015-0062

Warianty tytułu

Języki publikacji

Abstrakty

A new geochronology was established for the Stalać loess-paleosol sequence (LPS) in Serbia. The section is located in the interior of the Central Balkan region, south of the typical loess distribution, in a zone of paleoclimatic shifts between continental and Mediterranean climate regimes. The sampled sequence contains four well-developed paleosol and loess layers, a crypto tephra and one visible tephra layer. Optically stimulated luminescence measurements showed a strong dependency of preheat temperature on equivalent dose for one fine-grained quartz sample, which makes it unsuitable for dating. A firm chronology framing the last two glacial cycles was established using finegrained polyminerals and the post-infrared infrared stimulated luminescence (pIR50IR290) protocol instead. The characteristics of dated paleosols indicate similar climatic conditions during the last interstadial and interglacial phases, which were different from the penultimate interglacial period. The tephra within the L2 loess, probably related to tephra layers also found in other sections in Southeastern Europe, was sandwich-dated. The results indicate an age between 118 ka and 141 ka. Furthermore, a weak pedogenic layer dated to between 126 ka and 148 ka gives a first numerical age to this soil formation in Southeastern Europe.

Słowa kluczowe

post-infrared infrared stimulated luminescence (pIRIR) dating Pleistocene loesspaleosol sequences preheat plateau quartz and polymineral fine grains Serbia

Wydawca

De Gruyter

Czasopismo

Geochronometria

Rocznik

2017

Tom

Vol. 44, no. 1

Strony

150--161

Opis fizyczny

Bibliogr. 75 poz., rys.

Twórcy

autor

Bösken J.

Janina.boesken@geo.rwth-aachen.de

Department of Geography, RWTH Aachen University, Templergraben 55, D-52056 Aachen, Germany

autor

Klasen N.

Institute of Geography, University of Cologne, Albertus-Magnus-Platz, D-50923 Cologne, Germany

autor

Zeeden Ch.

Department of Geography, RWTH Aachen University, Templergraben 55, D-52056 Aachen, Germany

autor

Obreht I.

Department of Geography, RWTH Aachen University, Templergraben 55, D-52056 Aachen, Germany

autor

Marković S. B.

Laboratory for Paleoenvironmental Reconstruction, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 2, 21000 Novi Sad, Serbia

autor

Hambach U.

BayCEER & Chair of Geomorphology, University of Bayreuth, D-94450 Bayreuth, Germany
Laboratory for Paleoenvironmental Reconstruction, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 2, 21000 Novi Sad, Serbia

autor

Lehmkuhl F.

Department of Geography, RWTH Aachen University, Templergraben 55, D-52056 Aachen, Germany

Bibliografia

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Uwagi

Opracowanie ze środków MNiSW w ramach umowy 812/P-DUN/2016 na działalność upowszechniającą naukę (zadania 2017).

Typ dokumentu

Bibliografia

Identyfikator YADDA

bwmeta1.element.baztech-bd862609-d0a2-4d8c-8643-4604a441c1d9