Last-interglacial records from central Asia to the northern Black Sea shoreline: stratigraphy and correlation

  • A.E. Dodonov Geological Institute, Russian Academy of Sciences, Pyzhevsky 7, MOSCOW 109017, Russia
  • A.L. Tchepalyga Institute of Geography, Russian Academy of Sciences, Staromonetnyi 29, MOSCOW 109017, Russia
  • C.D. Mihailescu Institute of Geography, Moldavian Academy of Sciences, Academia Street 3, KISHINEV 2028, Moldova
  • L.P. Zhou The Godwin Laboratory, Department of Earth Sciences, University of Cambridge, Pembroke Street, CAMBRIDGE CB2 3SA, United Kingdom
  • A.K. Markova Institute of Geography, Russian Academy of Sciences, Staromonetnyi 29, MOSCOW 109017, Russia
  • V.M. Trubikhin Geological Institute, Russian Academy of Sciences, Pyzhevsky 7, MOSCOW 109017, Russia
  • A.N. Simakova Geological Institute, Russian Academy of Sciences, Pyzhevsky 7, MOSCOW 109017, Russia
  • E.G. Konikov Geological Department, Odessa University, Shampanskiy 2, ODESSA, Ukraine
Keywords: last interglacial, loess, marine transgression, mollusc fauna, palaeosol, stratigraphy

Abstract

The records of the last interglacial in several palaeogeographical zones and various sedimentary environments from Central Asia to the Black Sea shoreline are presented. The last interglacial is characterized in the study areas by a two- or three-unit stratigraphical complex with both terrestrial and marine formations. Finds of significant small mammalian remains, together with a characteristic mollusc fauna in the Karangatian marine sediments, provide key levels for biostratigraphical correlation between the marine and continental deposits. New U/Th dates allow the correlation of the Karangatian transgression with δ18O substage 5e.

Published
2000-08-01
How to Cite
A.E. Dodonov, A.L. Tchepalyga, C.D. Mihailescu, L.P. Zhou, A.K. Markova, V.M. Trubikhin, A.N. Simakova, & E.G. Konikov. (2000). Last-interglacial records from central Asia to the northern Black Sea shoreline: stratigraphy and correlation. Netherlands Journal of Geosciences, 79, 303 - 311. https://doi.org/10.1017/S0016774600021788
Section
Original Articles