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


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Аннотация

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.

Авторлар туралы

V. Kolka

Geological Institute, Kola Science Center, Russian Academy of Sciences

Хат алмасуға жауапты Автор.
Email: kolka@geoksc.apatity.ru
Ресей, Apatity, Murmansk oblast, 184209

O. Korsakova

Geological Institute, Kola Science Center, Russian Academy of Sciences

Email: kolka@geoksc.apatity.ru
Ресей, Apatity, Murmansk oblast, 184209

N. Lavrova

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

Email: kolka@geoksc.apatity.ru
Ресей, Petrozavodsk, 185910

T. Shelekhova

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

Email: kolka@geoksc.apatity.ru
Ресей, Petrozavodsk, 185910

N. Zaretskaya

Geological Institute, Russian Academy of Sciences

Email: kolka@geoksc.apatity.ru
Ресей, Moscow, 119017

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