Quaternary time scales for the Pontocaspian domain: interbasinal connectivity and faunal evolution

Krijgsman, W., Tesakov, A., Yanina, T., Lazarev, S., Danukalova, G., Van Baak, C.G.C., Agustí, J., Alçiçek, M.C., Aliyeva, E., Bista, D., Bruch, A., Büyükmeriç, Y., Bukhsianidze, M., Flecker, R., Frolov, P., Hoyle, T. M., Jorissen, E.L., Kirscher, U., Koriche, S. A. ORCID: https://orcid.org/0000-0003-1285-2035, Kroonenberg, S. B., Lordkipanidze, D., Oms, O., Rausch, L., Singarayer, J., Stoica, M., van de Velde, S., Titov, V. V. and Wesselingh, F. P. (2019) Quaternary time scales for the Pontocaspian domain: interbasinal connectivity and faunal evolution. Earth-Science Reviews, 188. pp. 1-40. ISSN 0012-8252 doi: 10.1016/j.earscirev.2018.10.013

Abstract/Summary

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.

Item Type	Article
URI	https://reading-clone.eprints-hosting.org/id/eprint/80093
Item Type	Article
Refereed	Yes
Divisions	Interdisciplinary centres and themes > Centre for Past Climate Change Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
Publisher	Elsevier
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