Late quaternary oceanographic conditions in the Western Bering Sea
The benthic and planktonic foraminiferal assemblages and the distribution of coarse grain-size factions were studied in the upper 4.5 m of the Core SO201-2-85KL (57A degrees 30.30' N, 170A degrees 24.79' E, water depth 968 m) retrieved from the Shirshov Ridge. This part of the core covers...
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2013
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Online Access: | https://oceanrep.geomar.de/id/eprint/21344/ https://oceanrep.geomar.de/id/eprint/21344/1/10.1134_S0001437013020136.pdf https://doi.org/10.1134/S0001437013020136 |
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ftoceanrep:oai:oceanrep.geomar.de:21344 2023-05-15T15:43:42+02:00 Late quaternary oceanographic conditions in the Western Bering Sea Ovsepyan, E. A. Ivanova, E. V. Max, L. Riethdorf, Jan-Rainer Nürnberg, Dirk Tiedemann, Ralf 2013 text https://oceanrep.geomar.de/id/eprint/21344/ https://oceanrep.geomar.de/id/eprint/21344/1/10.1134_S0001437013020136.pdf https://doi.org/10.1134/S0001437013020136 en eng Springer https://oceanrep.geomar.de/id/eprint/21344/1/10.1134_S0001437013020136.pdf Ovsepyan, E. A., Ivanova, E. V., Max, L., Riethdorf, J. R., Nürnberg, D. and Tiedemann, R. (2013) Late quaternary oceanographic conditions in the Western Bering Sea. Oceanology, 53 (2). pp. 211-222. DOI 10.1134/S0001437013020136 <https://doi.org/10.1134/S0001437013020136>. doi:10.1134/S0001437013020136 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2013 ftoceanrep https://doi.org/10.1134/S0001437013020136 2023-04-07T15:09:25Z The benthic and planktonic foraminiferal assemblages and the distribution of coarse grain-size factions were studied in the upper 4.5 m of the Core SO201-2-85KL (57A degrees 30.30' N, 170A degrees 24.79' E, water depth 968 m) retrieved from the Shirshov Ridge. This part of the core covers 7.5 to 50 kyr BP. The glacial period is established to be characterized by low surface water productivity, the wide distribution of sea ice and/or icebergs in this area, and a high oxygen concentration in the bottom layer. Enhanced productivity is inferred from the maximum abundance of planktonic foraminifers at the very beginning of the deglaciation. The late Bolling-Allerod interstadial and the early Holocene were marked by the further two-phase increase in the surface productivity and the weakened ventilation of the bottom water. Article in Journal/Newspaper Bering Sea Sea ice OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Bering Sea Shirshov Ridge ENVELOPE(171.000,171.000,57.500,57.500) Oceanology 53 2 211 222 |
institution |
Open Polar |
collection |
OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) |
op_collection_id |
ftoceanrep |
language |
English |
description |
The benthic and planktonic foraminiferal assemblages and the distribution of coarse grain-size factions were studied in the upper 4.5 m of the Core SO201-2-85KL (57A degrees 30.30' N, 170A degrees 24.79' E, water depth 968 m) retrieved from the Shirshov Ridge. This part of the core covers 7.5 to 50 kyr BP. The glacial period is established to be characterized by low surface water productivity, the wide distribution of sea ice and/or icebergs in this area, and a high oxygen concentration in the bottom layer. Enhanced productivity is inferred from the maximum abundance of planktonic foraminifers at the very beginning of the deglaciation. The late Bolling-Allerod interstadial and the early Holocene were marked by the further two-phase increase in the surface productivity and the weakened ventilation of the bottom water. |
format |
Article in Journal/Newspaper |
author |
Ovsepyan, E. A. Ivanova, E. V. Max, L. Riethdorf, Jan-Rainer Nürnberg, Dirk Tiedemann, Ralf |
spellingShingle |
Ovsepyan, E. A. Ivanova, E. V. Max, L. Riethdorf, Jan-Rainer Nürnberg, Dirk Tiedemann, Ralf Late quaternary oceanographic conditions in the Western Bering Sea |
author_facet |
Ovsepyan, E. A. Ivanova, E. V. Max, L. Riethdorf, Jan-Rainer Nürnberg, Dirk Tiedemann, Ralf |
author_sort |
Ovsepyan, E. A. |
title |
Late quaternary oceanographic conditions in the Western Bering Sea |
title_short |
Late quaternary oceanographic conditions in the Western Bering Sea |
title_full |
Late quaternary oceanographic conditions in the Western Bering Sea |
title_fullStr |
Late quaternary oceanographic conditions in the Western Bering Sea |
title_full_unstemmed |
Late quaternary oceanographic conditions in the Western Bering Sea |
title_sort |
late quaternary oceanographic conditions in the western bering sea |
publisher |
Springer |
publishDate |
2013 |
url |
https://oceanrep.geomar.de/id/eprint/21344/ https://oceanrep.geomar.de/id/eprint/21344/1/10.1134_S0001437013020136.pdf https://doi.org/10.1134/S0001437013020136 |
long_lat |
ENVELOPE(171.000,171.000,57.500,57.500) |
geographic |
Bering Sea Shirshov Ridge |
geographic_facet |
Bering Sea Shirshov Ridge |
genre |
Bering Sea Sea ice |
genre_facet |
Bering Sea Sea ice |
op_relation |
https://oceanrep.geomar.de/id/eprint/21344/1/10.1134_S0001437013020136.pdf Ovsepyan, E. A., Ivanova, E. V., Max, L., Riethdorf, J. R., Nürnberg, D. and Tiedemann, R. (2013) Late quaternary oceanographic conditions in the Western Bering Sea. Oceanology, 53 (2). pp. 211-222. DOI 10.1134/S0001437013020136 <https://doi.org/10.1134/S0001437013020136>. doi:10.1134/S0001437013020136 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1134/S0001437013020136 |
container_title |
Oceanology |
container_volume |
53 |
container_issue |
2 |
container_start_page |
211 |
op_container_end_page |
222 |
_version_ |
1766377896548499456 |