Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum
Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and oc...
Ausführliche Beschreibung
Autor*in: |
Matul, A. G. [verfasserIn] |
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Sprache: |
Englisch |
Erschienen: |
2015 |
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Anmerkung: |
© Pleiades Publishing, Inc. 2015 |
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Übergeordnetes Werk: |
Enthalten in: Oceanology - Pleiades Publishing, 1966, 55(2015), 1 vom: Feb., Seite 91-99 |
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Übergeordnetes Werk: |
volume:55 ; year:2015 ; number:1 ; month:02 ; pages:91-99 |
Links: |
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DOI / URN: |
10.1134/S0001437015010130 |
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OLC2071618114 |
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10.1134/S0001437015010130 doi (DE-627)OLC2071618114 (DE-He213)S0001437015010130-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Matul, A. G. verfasserin aut Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2015 Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. Last Glacial Maximum Glacial Maximum Intermediate Water Radiolaria Lithostratigraphy Abelmann, A. aut Gersonde, R. aut Nürnberg, D. aut Tiedemann, R. aut Kruglikova, S. B. aut Enthalten in Oceanology Pleiades Publishing, 1966 55(2015), 1 vom: Feb., Seite 91-99 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:55 year:2015 number:1 month:02 pages:91-99 https://doi.org/10.1134/S0001437015010130 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 55 2015 1 02 91-99 |
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10.1134/S0001437015010130 doi (DE-627)OLC2071618114 (DE-He213)S0001437015010130-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Matul, A. G. verfasserin aut Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2015 Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. Last Glacial Maximum Glacial Maximum Intermediate Water Radiolaria Lithostratigraphy Abelmann, A. aut Gersonde, R. aut Nürnberg, D. aut Tiedemann, R. aut Kruglikova, S. B. aut Enthalten in Oceanology Pleiades Publishing, 1966 55(2015), 1 vom: Feb., Seite 91-99 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:55 year:2015 number:1 month:02 pages:91-99 https://doi.org/10.1134/S0001437015010130 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 55 2015 1 02 91-99 |
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10.1134/S0001437015010130 doi (DE-627)OLC2071618114 (DE-He213)S0001437015010130-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Matul, A. G. verfasserin aut Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2015 Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. Last Glacial Maximum Glacial Maximum Intermediate Water Radiolaria Lithostratigraphy Abelmann, A. aut Gersonde, R. aut Nürnberg, D. aut Tiedemann, R. aut Kruglikova, S. B. aut Enthalten in Oceanology Pleiades Publishing, 1966 55(2015), 1 vom: Feb., Seite 91-99 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:55 year:2015 number:1 month:02 pages:91-99 https://doi.org/10.1134/S0001437015010130 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 55 2015 1 02 91-99 |
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10.1134/S0001437015010130 doi (DE-627)OLC2071618114 (DE-He213)S0001437015010130-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Matul, A. G. verfasserin aut Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2015 Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. Last Glacial Maximum Glacial Maximum Intermediate Water Radiolaria Lithostratigraphy Abelmann, A. aut Gersonde, R. aut Nürnberg, D. aut Tiedemann, R. aut Kruglikova, S. B. aut Enthalten in Oceanology Pleiades Publishing, 1966 55(2015), 1 vom: Feb., Seite 91-99 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:55 year:2015 number:1 month:02 pages:91-99 https://doi.org/10.1134/S0001437015010130 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 55 2015 1 02 91-99 |
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10.1134/S0001437015010130 doi (DE-627)OLC2071618114 (DE-He213)S0001437015010130-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Matul, A. G. verfasserin aut Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Pleiades Publishing, Inc. 2015 Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. Last Glacial Maximum Glacial Maximum Intermediate Water Radiolaria Lithostratigraphy Abelmann, A. aut Gersonde, R. aut Nürnberg, D. aut Tiedemann, R. aut Kruglikova, S. B. aut Enthalten in Oceanology Pleiades Publishing, 1966 55(2015), 1 vom: Feb., Seite 91-99 (DE-627)130005363 (DE-600)417045-3 (DE-576)9130005361 0001-4370 nnns volume:55 year:2015 number:1 month:02 pages:91-99 https://doi.org/10.1134/S0001437015010130 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_201 AR 55 2015 1 02 91-99 |
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Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum |
abstract |
Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. © Pleiades Publishing, Inc. 2015 |
abstractGer |
Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. © Pleiades Publishing, Inc. 2015 |
abstract_unstemmed |
Abstract A comparison of micropaleontological data on the distribution of the Cycladophora davisiana radiolarian species in the surface sediment layer and the Late Quaternary sediments from the Subarctic Pacific and Far East marginal seas allowed conclusions concerning the possible conditions and occurrence of intermediate waters during the last glacial maximum. We used the modern data on the C. davisiana species, which is a micro-paleontological indicator of the cold oxygen-rich upper intermediate water mass, which is now forming only in the Sea of Okhotsk. The high amount of C. davisiana in sediments of the last glacial maximum may point to the possible formation and expansion of the ventilated intermediate water in the most part of the Subarctic paleo-Pacific: the Bering Sea, the Sea of Okhotsk, within the NW Gyre, and in the Gulf of Alaska. © Pleiades Publishing, Inc. 2015 |
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title_short |
Late quaternary distribution of the Cycladophora davisiana radiolarian species: Reflection of possible ventilation of the North Pacific intermediate water during the Last Glacial Maximum |
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https://doi.org/10.1134/S0001437015010130 |
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Abelmann, A. Gersonde, R. Nürnberg, D. Tiedemann, R. Kruglikova, S. B. |
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Abelmann, A. Gersonde, R. Nürnberg, D. Tiedemann, R. Kruglikova, S. B. |
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up_date |
2024-07-04T03:51:15.804Z |
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