Solovetsky Archipelago in the Late Pleistocene-Holocene: Correlation of Marine and Land Research Data

For the first time the data on Quaternary geology of land and sea were correlated by the example of the Solovetsky Archipelago and the adjacent shelf. Geomorphological analysis and the use of structural methods for studying moraines allowed reconstructing the pathways of glacier movement and revealing the role of the Bolshoi Solovetsky and Anzer Islands as ice lobe dividing zones formed on protrusions of the pre-Quaternary basement. It is shown that deglaciation in the area of the Solovetsky Archipelago was rapid, and as a result of Late Glacial transgression a proglacial basin was formed here, which rapidly turned into a glacio-marine basin, and already in the Early Holocene became purely marine. Earlier assumptions stating that in the Solovetsky inter-island in the Boreal and Atlantic periods there were unique hydrological conditions when the water temperature was increased by 1°–2° compared to the modern one, which in turn led to the blooming of malacofauna, are confirmed and substantiated.

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Publication Details

Journal
Doklady Earth Sciences
Published
2025-11-12
DOI
https://doi.org/10.1134/s1028334x25608727
Primary Topic
Geology and Paleoclimatology Research
Type
article
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article

Solovetsky Archipelago in the Late Pleistocene-Holocene: Correlation of Marine and Land Research Data

A. K. Krekhov, Oleg Vladimirovich Dron, Olga Korsakova, T. Yu. Repkina et al.
Doklady Earth Sciences
Geology and Paleoclimatology Research
article

Solovetsky Archipelago in the Late Pleistocene-Holocene: Correlation of Marine and Land Research Data

A. K. Krekhov, Oleg Vladimirovich Dron, Olga Korsakova, T. Yu. Repkina, Dmitry Subetto, M. Yu. Tokarev, P. A. Leontiev, Andrei A. Kudinov, А. Е. Рыбалко, Andrey Vashkov, Larissa A Savelieva, Yu. A. Kublitsky, N. E. Zaretskaya, Sergey Kotov, А. В. Орлов, P. Yu. Belyaev, M. I. Aleshin
article en

Abstract

For the first time the data on Quaternary geology of land and sea were correlated by the example of the Solovetsky Archipelago and the adjacent shelf. Geomorphological analysis and the use of structural methods for studying moraines allowed reconstructing the pathways of glacier movement and revealing the role of the Bolshoi Solovetsky and Anzer Islands as ice lobe dividing zones formed on protrusions of the pre-Quaternary basement. It is shown that deglaciation in the area of the Solovetsky Archipelago was rapid, and as a result of Late Glacial transgression a proglacial basin was formed here, which rapidly turned into a glacio-marine basin, and already in the Early Holocene became purely marine. Earlier assumptions stating that in the Solovetsky inter-island in the Boreal and Atlantic periods there were unique hydrological conditions when the water temperature was increased by 1°–2° compared to the modern one, which in turn led to the blooming of malacofauna, are confirmed and substantiated.

Doklady Earth SciencesVol. 525(2)
St Petersburg University (RU), Lomonosov Moscow State University (RU), Institute of Oceanology. PP Shirshov Russian Academy of Sciences (RU), Herzen University (RU), All Russian Research Institute of Geology and Mineral Resources of the World Ocean (RU), Institute of Geography (RU), A.P. Karpinsky Russian Geological Research Institute (RU), Kola Science Centre (RU), University of Split (HR)
Openalex Percentile: Top 61%
Geology and Paleoclimatology Research
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