Saved in:
| Main Authors: | , , , , |
|---|---|
| Format: | Dataset Open Access |
| Language: | en |
| Published: |
PANGAEA
2008
|
| Subjects: | |
| Online Access: | https://doi.org/10.1594/PANGAEA.778845 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| _version_ | 1867169044211171328 |
|---|---|
| author | Chekhovskaya, Maria P Basov, Ivan A Matul, Alexander G Khusid, Tatyana A Gorbarenko, Sergey A |
| author_facet | Chekhovskaya, Maria P Basov, Ivan A Matul, Alexander G Khusid, Tatyana A Gorbarenko, Sergey A |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Taxonomic composition and distribution of planktonic foraminifera are studied in section of Core GC-11 penetrated through Upper Quaternary sediments of the Bowers Ridge western slope, south Bering Sea. It is shown that structure of foraminiferal assemblage and productivity varied substantially during the last 32000 calendar years in response to changes in surface water temperatures and water mass circulation in the North Pacific including the Bering Sea. Productivity was maximal during the deglaciation epoch, being notably lower in Holocene and minimal at glaciation time. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_778845 |
| institution | PANGAEA |
| language | en |
| publishDate | 2008 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Sediment age, abundance of planktonic foraminifera shells, degree of their dissolution, percentage of benthic foraminifera in total foram fauna, Core GC-11, Sea of Okhotsk Chekhovskaya, Maria P Basov, Ivan A Matul, Alexander G Khusid, Tatyana A Gorbarenko, Sergey A Age, 14C conventional; Archive of Ocean Data; ARCOD; Benthic foraminifera of total foram fauna; Bering Sea; Calculated; Calendar age; Counting, foraminifera, planktic; DEPTH, sediment/rock; Epoch; Foraminifera; Foraminifera, planktic; GC; GC-11; Gravity corer; Sample comment Taxonomic composition and distribution of planktonic foraminifera are studied in section of Core GC-11 penetrated through Upper Quaternary sediments of the Bowers Ridge western slope, south Bering Sea. It is shown that structure of foraminiferal assemblage and productivity varied substantially during the last 32000 calendar years in response to changes in surface water temperatures and water mass circulation in the North Pacific including the Bering Sea. Productivity was maximal during the deglaciation epoch, being notably lower in Holocene and minimal at glaciation time. |
| title | Sediment age, abundance of planktonic foraminifera shells, degree of their dissolution, percentage of benthic foraminifera in total foram fauna, Core GC-11, Sea of Okhotsk |
| topic | Age, 14C conventional; Archive of Ocean Data; ARCOD; Benthic foraminifera of total foram fauna; Bering Sea; Calculated; Calendar age; Counting, foraminifera, planktic; DEPTH, sediment/rock; Epoch; Foraminifera; Foraminifera, planktic; GC; GC-11; Gravity corer; Sample comment |
| url | https://doi.org/10.1594/PANGAEA.778845 |