A Glacial–Interglacial Malacofauna Record from the Titel Loess Plateau, Serbia, between ~350 and 250 ka

Author:

Radaković Milica G.1ORCID,Gavrilović Bojan2,Gavrilov Milivoj B.1,Marković Rastko S.3,Hao Qingzhen4ORCID,Schaetzl Randall J.5,Zeeden Christian6,Cai Binggui78,Perić Zoran M.9ORCID,Antić Aleksandar110ORCID,Lukić Tin1ORCID,Marković Slobodan B.11112

Affiliation:

1. Department of Geography, Tourism and Hotel Management, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, 21000 Novi Sad, Serbia

2. Institute of Forestry, Kneza Višeslava 3, 11030 Belgrade, Serbia

3. Department of Geography, Faculty of Science, University of Niš, Višegradska 11, 18000 Niš, Serbia

4. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

5. Department of Geography, Environment, and Spatial Sciences, Michigan State University, East Lansing, MI 48824, USA

6. Leibniz Institute for Applied Geophysics (LIAG), Stilleweg 2, 30655 Hannover, Germany

7. Fujian Provincial Key Laboratory for Subtropical Resources and Environment, Fujian Normal University, Fuzhou 350117, China

8. Key Laboratory for Humid Subtropical Eco-Geographical Processes of the Ministry of Education, Fujian Normal University, Fuzhou 350117, China

9. Lund Luminescence Laboratory, Department of Geology, Lund University, Sölvegatan 12, SE-223 62 Lund, Sweden

10. Institute of Geography and Sustainability, University of Lausanne, 1967 Sion, Switzerland

11. Serbian Academy of Sciences and Arts, Kneza Mihaila 35, 11000 Belgrade, Serbia

12. Biotechnical Faculty, University of Montenegro, Mihaila Lalića 15, 81000 Podgorica, Montenegro

Abstract

We present data on molluscan fauna within the L3 loess unit (and partially within the S3 paleosol) from the key loess section of Veliki Surduk in Serbia. The section correlates to Marine Isotope Stage (MIS) 8 and late MIS 9 and, thus, spans the time frame from ~350 to 250 ka. The Veliki Surduk loess–paleosol sequence (LPS) is located on the northwestern margin of the Titel loess plateau and comprises ~30 m of sediments. Our focus is on a 5.4 m thick sedimentary interval, which was sampled at 20 cm increments, each sample covering approximately 2 ky. Nine mollusk species were identified in the loess sequence: Granaria frumentum, Helicopsis striata, Pupilla triplicata, Chondrula tridens, Pupilla muscorum, Succinella oblonga, Punctum pygmaeum, Vallonia costata, and Vitrina pellucida, as well as a few unidentified slug taxa (Limacidae, Agriolimacidae, and Milacidae). The majority of the snail assemblage occurs at the transition between MIS 9 and MIS 8, suggesting a mostly dry climate and an open and steppe-like habitat. The fauna identified in the upper part of the paleosol layer S3, below the L3 unit, indicated aridification.

Funder

Ministry of Science, Technological Development and Innovation of the Republic of Serbia

Provincial Secretariat for Higher Education and Scientific Research of Vojvodina

Publisher

MDPI AG

Reference114 articles.

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