Benthic Foraminifera in Upper Pleistocene - Holocene bottom sediments from the southeastern Sea of Okhotsk
A comparative analysis of benthic foraminiferal assemblages in the last glacial sediments obtained by gravity cores from the southern Kamchatka slope (Vulk-34-98) and from the eastern slope of the Akademii Nauk Rise in the central Sea of Okhotsk (Vulk-34-90) revealed, along with their undoubted simi...
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2002
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.761778 2023-05-15T16:59:11+02:00 Benthic Foraminifera in Upper Pleistocene - Holocene bottom sediments from the southeastern Sea of Okhotsk Basov, Ivan A Khusid, Tatyana A MEDIAN LATITUDE: 49.470833 * MEDIAN LONGITUDE: 151.830000 * SOUTH-BOUND LATITUDE: 48.831667 * WEST-BOUND LONGITUDE: 150.460000 * NORTH-BOUND LATITUDE: 50.110000 * EAST-BOUND LONGITUDE: 153.200000 2002-06-16 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.761778 https://doi.org/10.1594/PANGAEA.761778 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.761778 https://doi.org/10.1594/PANGAEA.761778 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Basov, Ivan A; Khusid, Tatyana A (2002): Benthic foraminiferal assemblages of the southeastern Sea of Okhotsk during the last glacial period. Translated from Okeanologiya, 2002, 42(4), 592-599, Oceanology, 42(4), 567-574 Archive of Ocean Data ARCOD GC Gravity corer Sea of Okhotsk Vulk-34-90 Vulk-34-98 Dataset 2002 ftpangaea https://doi.org/10.1594/PANGAEA.761778 2023-01-20T07:32:12Z A comparative analysis of benthic foraminiferal assemblages in the last glacial sediments obtained by gravity cores from the southern Kamchatka slope (Vulk-34-98) and from the eastern slope of the Akademii Nauk Rise in the central Sea of Okhotsk (Vulk-34-90) revealed, along with their undoubted similarity, substantial differences caused by hydrological regime in these areas during the considered period. It is shown that during the last glacial period bottom waters near the northern Kuril Islands were warmer and less aerated than those in the Akademii Nauk Rise area. As is evident from low-amplitude variations in proportions of dominant species, hydrological parameters in the bottom layer of the latter area at that time were relatively more stable than in the former area. Dataset Kamchatka PANGAEA - Data Publisher for Earth & Environmental Science Akademii Nauk Rise ENVELOPE(150.000,150.000,49.500,49.500) Okhotsk ENVELOPE(150.460000,153.200000,50.110000,48.831667) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Archive of Ocean Data ARCOD GC Gravity corer Sea of Okhotsk Vulk-34-90 Vulk-34-98 |
spellingShingle |
Archive of Ocean Data ARCOD GC Gravity corer Sea of Okhotsk Vulk-34-90 Vulk-34-98 Basov, Ivan A Khusid, Tatyana A Benthic Foraminifera in Upper Pleistocene - Holocene bottom sediments from the southeastern Sea of Okhotsk |
topic_facet |
Archive of Ocean Data ARCOD GC Gravity corer Sea of Okhotsk Vulk-34-90 Vulk-34-98 |
description |
A comparative analysis of benthic foraminiferal assemblages in the last glacial sediments obtained by gravity cores from the southern Kamchatka slope (Vulk-34-98) and from the eastern slope of the Akademii Nauk Rise in the central Sea of Okhotsk (Vulk-34-90) revealed, along with their undoubted similarity, substantial differences caused by hydrological regime in these areas during the considered period. It is shown that during the last glacial period bottom waters near the northern Kuril Islands were warmer and less aerated than those in the Akademii Nauk Rise area. As is evident from low-amplitude variations in proportions of dominant species, hydrological parameters in the bottom layer of the latter area at that time were relatively more stable than in the former area. |
format |
Dataset |
author |
Basov, Ivan A Khusid, Tatyana A |
author_facet |
Basov, Ivan A Khusid, Tatyana A |
author_sort |
Basov, Ivan A |
title |
Benthic Foraminifera in Upper Pleistocene - Holocene bottom sediments from the southeastern Sea of Okhotsk |
title_short |
Benthic Foraminifera in Upper Pleistocene - Holocene bottom sediments from the southeastern Sea of Okhotsk |
title_full |
Benthic Foraminifera in Upper Pleistocene - Holocene bottom sediments from the southeastern Sea of Okhotsk |
title_fullStr |
Benthic Foraminifera in Upper Pleistocene - Holocene bottom sediments from the southeastern Sea of Okhotsk |
title_full_unstemmed |
Benthic Foraminifera in Upper Pleistocene - Holocene bottom sediments from the southeastern Sea of Okhotsk |
title_sort |
benthic foraminifera in upper pleistocene - holocene bottom sediments from the southeastern sea of okhotsk |
publisher |
PANGAEA |
publishDate |
2002 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.761778 https://doi.org/10.1594/PANGAEA.761778 |
op_coverage |
MEDIAN LATITUDE: 49.470833 * MEDIAN LONGITUDE: 151.830000 * SOUTH-BOUND LATITUDE: 48.831667 * WEST-BOUND LONGITUDE: 150.460000 * NORTH-BOUND LATITUDE: 50.110000 * EAST-BOUND LONGITUDE: 153.200000 |
long_lat |
ENVELOPE(150.000,150.000,49.500,49.500) ENVELOPE(150.460000,153.200000,50.110000,48.831667) |
geographic |
Akademii Nauk Rise Okhotsk |
geographic_facet |
Akademii Nauk Rise Okhotsk |
genre |
Kamchatka |
genre_facet |
Kamchatka |
op_source |
Supplement to: Basov, Ivan A; Khusid, Tatyana A (2002): Benthic foraminiferal assemblages of the southeastern Sea of Okhotsk during the last glacial period. Translated from Okeanologiya, 2002, 42(4), 592-599, Oceanology, 42(4), 567-574 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.761778 https://doi.org/10.1594/PANGAEA.761778 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.761778 |
_version_ |
1766051395730931712 |