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Solovetsky Archipelago in the Late Pleistocene-Holocene: Correlation of Marine and Land Research Data. / Rybalko, AE; Repkina, TY; Korsakova, OP; Vashkov, AA; Zaretskaya, NE; Tokarev, MY; Subetto, DA; Aleshin, MI; Belyaev, PY; Dron, OV; Kotov, SR; Krekhov, AK; Kublitsky, YA; Kudinov, AA; Leontiev, PA; Orlov, AV; Savelieva, LA.

In: Doklady Earth Sciences, Vol. 525, No. 2, 2025.

Research output: Contribution to journal › Article › peer-review

Harvard

Rybalko, AE, Repkina, TY, Korsakova, OP, Vashkov, AA, Zaretskaya, NE, Tokarev, MY, Subetto, DA, Aleshin, MI, Belyaev, PY, Dron, OV, Kotov, SR, Krekhov, AK, Kublitsky, YA, Kudinov, AA, Leontiev, PA, Orlov, AV & Savelieva, LA 2025, 'Solovetsky Archipelago in the Late Pleistocene-Holocene: Correlation of Marine and Land Research Data', Doklady Earth Sciences, vol. 525, no. 2. https://doi.org/10.1134/S1028334X25608727

APA

Rybalko, AE., Repkina, TY., Korsakova, OP., Vashkov, AA., Zaretskaya, NE., Tokarev, MY., Subetto, DA., Aleshin, MI., Belyaev, PY., Dron, OV., Kotov, SR., Krekhov, AK., Kublitsky, YA., Kudinov, AA., Leontiev, PA., Orlov, AV., & Savelieva, LA. (2025). Solovetsky Archipelago in the Late Pleistocene-Holocene: Correlation of Marine and Land Research Data. Doklady Earth Sciences, 525(2). https://doi.org/10.1134/S1028334X25608727

Vancouver

Rybalko AE, Repkina TY, Korsakova OP, Vashkov AA, Zaretskaya NE, Tokarev MY et al. Solovetsky Archipelago in the Late Pleistocene-Holocene: Correlation of Marine and Land Research Data. Doklady Earth Sciences. 2025;525(2). https://doi.org/10.1134/S1028334X25608727

Author

Rybalko, AE ; Repkina, TY ; Korsakova, OP ; Vashkov, AA ; Zaretskaya, NE ; Tokarev, MY ; Subetto, DA ; Aleshin, MI ; Belyaev, PY ; Dron, OV ; Kotov, SR ; Krekhov, AK ; Kublitsky, YA ; Kudinov, AA ; Leontiev, PA ; Orlov, AV ; Savelieva, LA. / Solovetsky Archipelago in the Late Pleistocene-Holocene: Correlation of Marine and Land Research Data. In: Doklady Earth Sciences. 2025 ; Vol. 525, No. 2.

BibTeX

@article{a96f9cdcfc2b4c74a8ec76ed9f824d4c,
title = "Solovetsky Archipelago in the Late Pleistocene-Holocene: Correlation of Marine and Land Research Data",
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 degrees-2 degrees compared to the modern one, which in turn led to the blooming of malacofauna, are confirmed and substantiated.",
keywords = "White Sea, Onega Bay, Valdai glaciation, seismoacoustic profiling, glacial ridges",
author = "AE Rybalko and TY Repkina and OP Korsakova and AA Vashkov and NE Zaretskaya and MY Tokarev and DA Subetto and MI Aleshin and PY Belyaev and OV Dron and SR Kotov and AK Krekhov and YA Kublitsky and AA Kudinov and PA Leontiev and AV Orlov and LA Savelieva",
note = "Times Cited in Web of Science Core Collection: 0 Total Times Cited: 0 Cited Reference Count: 20",
year = "2025",
doi = "10.1134/S1028334X25608727",
language = "Английский",
volume = "525",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - Solovetsky Archipelago in the Late Pleistocene-Holocene: Correlation of Marine and Land Research Data

AU - Rybalko, AE

AU - Repkina, TY

AU - Korsakova, OP

AU - Vashkov, AA

AU - Zaretskaya, NE

AU - Tokarev, MY

AU - Subetto, DA

AU - Aleshin, MI

AU - Belyaev, PY

AU - Dron, OV

AU - Kotov, SR

AU - Krekhov, AK

AU - Kublitsky, YA

AU - Kudinov, AA

AU - Leontiev, PA

AU - Orlov, AV

AU - Savelieva, LA

N1 - Times Cited in Web of Science Core Collection: 0 Total Times Cited: 0 Cited Reference Count: 20

PY - 2025

Y1 - 2025

N2 - 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 degrees-2 degrees compared to the modern one, which in turn led to the blooming of malacofauna, are confirmed and substantiated.

AB - 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 degrees-2 degrees compared to the modern one, which in turn led to the blooming of malacofauna, are confirmed and substantiated.

KW - White Sea

KW - Onega Bay

KW - Valdai glaciation

KW - seismoacoustic profiling

KW - glacial ridges

U2 - 10.1134/S1028334X25608727

DO - 10.1134/S1028334X25608727

M3 - статья

VL - 525

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 147943293