Quaternary time scales for the Pontocaspian domain

Interbasinal connectivity and faunal evolution

Review (2019)

Authors

W. Krijgsman Universiteit Utrecht
A. Tesakov Geological Institute of the Russian Academy of Sciences
Tamara A. Yanina Chemistry Faculty of M. V. Lomonosov Moscow State University
Sergei Lazarev Universiteit Utrecht
G. Danukalova Institute of Geology of the Ufimian Scientific Centre
J. Agustí Universitat Rovira i Virgili
R. Flecker University of Bristol
S.B. Kroonenberg Applied Geology - CEG
More Authors... External organisation
Research Group
Applied Geology (CEG) (TU Delft)
Copyright: © 2019 W. Krijgsman, A. Tesakov, T. Yanina, S. Lazarev, G. Danukalova, C. G.C. Van Baak, J. Agustí, R. Flecker, S.B. Kroonenberg, More Authors
DOI: https://doi.org/10.1016/j.earscirev.2018.10.013
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Published Date

01-01-2019

Language

English

Faculty

Civil Engineering & Geosciences

Department

Geoscience and Engineering

Research Group

Applied Geology

Abstract

The Pontocaspian (Black Sea - Caspian Sea) region has a very dynamic history of basin development and biotic evolution. The region is the remnant of a once vast Paratethys Sea. It contains some of the best Eurasian geological records of tectonic, climatic and paleoenvironmental change. The Pliocene-Quaternary co-evolution of the Black Sea-Caspian Sea is dominated by major changes in water (lake and sea) levels resulting in a pulsating system of connected and isolated basins. Understanding the history of the region, including the drivers of lake level and faunal evolution, is hampered by indistinct stratigraphic nomenclature and contradicting time constraints for regional sedimentary successions. In this paper we review and update the late Pliocene to Quaternary stratigraphic framework of the Pontocaspian domain, focusing on the Black Sea Basin, Caspian Basin, Marmara Sea and the terrestrial environments surrounding these large, mostly endorheic lake-sea systems.