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

Research output: Contribution to journalArticle

  • Wout Krijgsman
  • A Tesakov
  • T Yanina
  • S Lazarev
  • G Danukalova
  • Christiaan G.C. van Baak
  • J Agusti
  • M.C. Alçiçek
  • E Aliyeva
  • Diksha Bista
  • A Bruch
  • Y Büyükmeriç
  • M Bukhsianidze
  • Rachel Flecker
  • P Frolov
  • T.M. Hoyle
  • E.L. Jorissen
  • U Kirscher
  • S.A. Koriche
  • S.B. Kroonenberg
  • D. Lordkipanidze
  • O Oms
  • L Rausch
  • Joy Singarayer
  • M Stoica
  • S. van de Velde
  • V.V. Titov
  • Frank P Wesselingh
Original languageEnglish
Pages (from-to)1-40
Number of pages40
JournalEarth-Science Reviews
Volume188
Early online date18 Oct 2018
DOIs
DateAccepted/In press - 16 Oct 2018
DateE-pub ahead of print (current) - 18 Oct 2018
DatePublished - Jan 2019

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.

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