Hydrological changes in the Laptev Sea during the Holocene inferred from the studies of aquatic palynomorphs
Based on the study of aquatic palynomorph assemblages in two Holocene sediment cores obtained from the eastern Laptev Sea shelf, the main stages in the postglacial transgression are reconstructed for the last 11.3 ky. During that period, the inner shelf of the Laptev Sea (sea depth of 51 m) was alre...
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Language: | English |
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Pleiades Publishing, Springer
2006
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Online Access: | https://oceanrep.geomar.de/id/eprint/31647/ https://oceanrep.geomar.de/id/eprint/31647/1/Klyuvitkina_Bauch.pdf https://doi.org/10.1134/S0001437006060117 |
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ftoceanrep:oai:oceanrep.geomar.de:31647 2023-05-15T17:07:06+02:00 Hydrological changes in the Laptev Sea during the Holocene inferred from the studies of aquatic palynomorphs Klyuvitkina, T. S. Bauch, H. A. 2006 text https://oceanrep.geomar.de/id/eprint/31647/ https://oceanrep.geomar.de/id/eprint/31647/1/Klyuvitkina_Bauch.pdf https://doi.org/10.1134/S0001437006060117 en eng Pleiades Publishing, Springer https://oceanrep.geomar.de/id/eprint/31647/1/Klyuvitkina_Bauch.pdf Klyuvitkina, T. S. and Bauch, H. A. (2006) Hydrological changes in the Laptev Sea during the Holocene inferred from the studies of aquatic palynomorphs. Oceanology, 46 (6). pp. 859-868. DOI 10.1134/S0001437006060117 <https://doi.org/10.1134/S0001437006060117>. doi:10.1134/S0001437006060117 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2006 ftoceanrep https://doi.org/10.1134/S0001437006060117 2023-04-07T15:23:56Z Based on the study of aquatic palynomorph assemblages in two Holocene sediment cores obtained from the eastern Laptev Sea shelf, the main stages in the postglacial transgression are reconstructed for the last 11.3 ky. During that period, the inner shelf of the Laptev Sea (sea depth of 51 m) was already flooded representing an area of intense freshwater sedimentation in the immediate proximity from the river mouth in the period of 11.3 to 10.3 ky B.P. Approximately 1.0–1.5 ky later, the inner shelf (sea depth of 32 m) was flooded, although it remained under the influence of the river runoff up to 7.4 ky B.P. The period of 10.3–7.4 ky B.P. was marked by the dominant dinoflagellate cysts Operculodinium centrocarpum among the aquatic palynomorphs, the appearance of more thermophilic dinoflagellate species, and elevated values of the AH ratio, which indicates an enhanced influx of relatively warm North Atlantic waters to the Laptev Sea shelf. The environment close to the present-day one became dominant on the outer and inner shelf of the Laptev Sea approximately 8.6 and 7.4 ky B.P., respectively. Article in Journal/Newspaper laptev Laptev Sea North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Laptev Sea Oceanology 46 6 859 868 |
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Open Polar |
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OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
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ftoceanrep |
language |
English |
description |
Based on the study of aquatic palynomorph assemblages in two Holocene sediment cores obtained from the eastern Laptev Sea shelf, the main stages in the postglacial transgression are reconstructed for the last 11.3 ky. During that period, the inner shelf of the Laptev Sea (sea depth of 51 m) was already flooded representing an area of intense freshwater sedimentation in the immediate proximity from the river mouth in the period of 11.3 to 10.3 ky B.P. Approximately 1.0–1.5 ky later, the inner shelf (sea depth of 32 m) was flooded, although it remained under the influence of the river runoff up to 7.4 ky B.P. The period of 10.3–7.4 ky B.P. was marked by the dominant dinoflagellate cysts Operculodinium centrocarpum among the aquatic palynomorphs, the appearance of more thermophilic dinoflagellate species, and elevated values of the AH ratio, which indicates an enhanced influx of relatively warm North Atlantic waters to the Laptev Sea shelf. The environment close to the present-day one became dominant on the outer and inner shelf of the Laptev Sea approximately 8.6 and 7.4 ky B.P., respectively. |
format |
Article in Journal/Newspaper |
author |
Klyuvitkina, T. S. Bauch, H. A. |
spellingShingle |
Klyuvitkina, T. S. Bauch, H. A. Hydrological changes in the Laptev Sea during the Holocene inferred from the studies of aquatic palynomorphs |
author_facet |
Klyuvitkina, T. S. Bauch, H. A. |
author_sort |
Klyuvitkina, T. S. |
title |
Hydrological changes in the Laptev Sea during the Holocene inferred from the studies of aquatic palynomorphs |
title_short |
Hydrological changes in the Laptev Sea during the Holocene inferred from the studies of aquatic palynomorphs |
title_full |
Hydrological changes in the Laptev Sea during the Holocene inferred from the studies of aquatic palynomorphs |
title_fullStr |
Hydrological changes in the Laptev Sea during the Holocene inferred from the studies of aquatic palynomorphs |
title_full_unstemmed |
Hydrological changes in the Laptev Sea during the Holocene inferred from the studies of aquatic palynomorphs |
title_sort |
hydrological changes in the laptev sea during the holocene inferred from the studies of aquatic palynomorphs |
publisher |
Pleiades Publishing, Springer |
publishDate |
2006 |
url |
https://oceanrep.geomar.de/id/eprint/31647/ https://oceanrep.geomar.de/id/eprint/31647/1/Klyuvitkina_Bauch.pdf https://doi.org/10.1134/S0001437006060117 |
geographic |
Laptev Sea |
geographic_facet |
Laptev Sea |
genre |
laptev Laptev Sea North Atlantic |
genre_facet |
laptev Laptev Sea North Atlantic |
op_relation |
https://oceanrep.geomar.de/id/eprint/31647/1/Klyuvitkina_Bauch.pdf Klyuvitkina, T. S. and Bauch, H. A. (2006) Hydrological changes in the Laptev Sea during the Holocene inferred from the studies of aquatic palynomorphs. Oceanology, 46 (6). pp. 859-868. DOI 10.1134/S0001437006060117 <https://doi.org/10.1134/S0001437006060117>. doi:10.1134/S0001437006060117 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1134/S0001437006060117 |
container_title |
Oceanology |
container_volume |
46 |
container_issue |
6 |
container_start_page |
859 |
op_container_end_page |
868 |
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1766062303313133568 |