Biostratigraphy of larger foraminifera in the Eocene (upper Ypresianlower Bartonian) sequences of the Southern Slope of the Western Caucasus (Russia, NE Black Sea). Correlation with regional and standard planktonic foraminiferal zones

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https://hdl.handle.net/2072/395073

Biostratigraphy of larger foraminifera in the Eocene (upper Ypresianlower Bartonian) sequences of the Southern Slope of the Western Caucasus (Russia, NE Black Sea). Correlation with regional and standard planktonic foraminiferal zones

Autor: Zakrevskaya, Federica, Stupin, S., Bugrova, E.M.

Publikováno v: Geologica Acta; Climate and biota of the early Paleogene: recent advances and new perspectives; 259-279
Geologica Acta; Vol. 7 No. 1-2 (2009): Climate and Biota of the Early Paleogene: Recent advances and new perspectives; 259-279
RCUB. Revistas Científicas de la Universidad de Barcelona
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Recercat. Dipósit de la Recerca de Catalunya
Recercat: Dipósit de la Recerca de Catalunya
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Dipòsit Digital de Documents de la UAB
Universitat Autònoma de Barcelona
Geologica Acta; 2009: Vol.: 7 Núm.: 1-2 Climate and biota of the early Paleogene: recent advances and new perspectives; p. 259-279

The biostratigraphic analysis of two Eocene (Upper Ypresian-Lower Bartonian) sections located on the Southern Slope of the Western Caucasus (Inal and Loo sections in the Tuapse and Sochi districts, respectively) was carried out using planktonic and l

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::ad7099348a2494144fb5cacea3c52c91
https://revistes.ub.edu/index.php/GEOACTA/article/view/105.000000277