Changes in the Ostracod Assemblages of the Northeastern Black Sea Shelf during the Late Pleistocene and Holocene


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Distribution of 57 ostracod species is investigated in the Quaternary sediment samples from the borehole RBH-16, drilled at the north-eastern Black Sea shelf edge off the town of Anapa. Among them, 52 species of the Caspian type and 5 species of the Mediterranean type were found. Four distinct assemblage zones are identified: the Caspian type one typical for Chaudian basin (Early Neopleistocene) (I) in interval 15.55–14.11 m; the Caspian type one dominating from the Late Pleistocene to the early Holocene (II), according to species composition closed to Khvalynian basin, at the depth 13.4–3.84 m (from 13.6 to 8.7 cal. ka BP), the mixed one of Caspian type and Mediterranean type species (III) in interval 3.84–0.95 m (younger than 8.7 cal. ka BP), and the assemblage with progressively increasing dominance of Mediterranean species (IV) in interval above 0.75 m (after 7.4 cal. ka BP).

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M. Zenina

Shirshov Institute of Oceanology, Russian Academy of Sciences

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Email: maria_zenina@mail.ru
俄罗斯联邦, Moscow

A. Chepalyga

Institute of Geography, Russian Academy of Sciences

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Email: tchepalyga@mail.ru
俄罗斯联邦, Moscow

I. Murdmaa

Shirshov Institute of Oceanology, Russian Academy of Sciences

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Email: murdmaa@mail.ru
俄罗斯联邦, Moscow

G. Malgezini

RINA Consulting S.p.A.

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Email: giuseppe.malgesini@rina.org
意大利, Genova

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