Lithology, Biostratigraphy, and Geochronology of the Late Pleistocene–Holocene Sediments on the Coast of Onega Bay of the White Sea


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This paper reports on the lithological, micropaleontological, and chronometric data (radiocarbon dating) for one of the areas of the White Sea coast. The sedimentary sequences were studied in the current lake basins, which were separated from the large basin at different times. The basin was situated in the head of the current Onega Bay. On the basis of these data, the bottom sediments were stratified and the Late Pleistocene–Holocene paleogeographic settings were reconstructed for the southeastern part of Onega Bay.

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V. Kolka

Geological Institute, Kola Science Center, Russian Academy of Sciences

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Email: kolka@geoksc.apatity.ru
俄罗斯联邦, Apatity, Murmansk oblast, 184209

O. Korsakova

Geological Institute, Kola Science Center, Russian Academy of Sciences

Email: kolka@geoksc.apatity.ru
俄罗斯联邦, Apatity, Murmansk oblast, 184209

N. Lavrova

Institute of Geology, Karelian Research Center,
Russian Academy of Sciences

Email: kolka@geoksc.apatity.ru
俄罗斯联邦, Petrozavodsk, 185910

T. Shelekhova

Institute of Geology, Karelian Research Center,
Russian Academy of Sciences

Email: kolka@geoksc.apatity.ru
俄罗斯联邦, Petrozavodsk, 185910

N. Zaretskaya

Geological Institute, Russian Academy of Sciences

Email: kolka@geoksc.apatity.ru
俄罗斯联邦, Moscow, 119017

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