Paleoceanological Conditions on the Northern Segment of the Mohns Ridge (Norwegian Sea) at the End of the Middle Pleistocene Based on the Dinocyst Analysis.

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Title: Paleoceanological Conditions on the Northern Segment of the Mohns Ridge (Norwegian Sea) at the End of the Middle Pleistocene Based on the Dinocyst Analysis.
Authors: Klyuvitkina, T. S.1 (AUTHOR) t.klyuvitkina@mail.ru, Novichkova, E. A.2 (AUTHOR), Matul, A. G.2 (AUTHOR), Mohan, R.3 (AUTHOR), Tiwari, M.3 (AUTHOR), Lozinskaia, L. A.2 (AUTHOR), Kravchishina, M. D.2 (AUTHOR)
Source: Doklady Earth Sciences. Dec2025, Vol. 525 Issue 2, p1-5. 5p.
Subjects: Paleoceanography, Dinoflagellate cysts, Fronts (Meteorology), Ocean, Sea ice, Oxygen isotopes, Mid-ocean ridges, Pleistocene Epoch
Geographic Terms: Norwegian Sea
Abstract: New paleoceanological data for the northern part of the Norwegian Sea were obtained for the marine oxygen isotope stages (MIS) 8–6. Dinocyst analysis, performed on the sediment core AMK-5536, showed that during cold MIS 6 and MIS 8, the local environments were formed in close proximity to the Arctic Front with probable presence of sea ice. In the warm MIS 7, the dramatic increase in dinocyst concentrations with high species diversity, and the appearance of warm-water taxa with typical species Spiniferites septentrionalis were noted. The MIS 7 optimum corresponds to the time of ~240–236 ka. The warming was short-lived and strongly pronounced. The influence of the North Atlantic warm and saline sea-surface waters was greater than at present; the Arctic Front shifted northward. The reconstructed sea-surface temperature was approximately 2.9–3.6°C higher than the modern one. [ABSTRACT FROM AUTHOR]
Copyright of Doklady Earth Sciences is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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  Data: Paleoceanological Conditions on the Northern Segment of the Mohns Ridge (Norwegian Sea) at the End of the Middle Pleistocene Based on the Dinocyst Analysis.
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  Data: New paleoceanological data for the northern part of the Norwegian Sea were obtained for the marine oxygen isotope stages (MIS) 8–6. Dinocyst analysis, performed on the sediment core AMK-5536, showed that during cold MIS 6 and MIS 8, the local environments were formed in close proximity to the Arctic Front with probable presence of sea ice. In the warm MIS 7, the dramatic increase in dinocyst concentrations with high species diversity, and the appearance of warm-water taxa with typical species Spiniferites septentrionalis were noted. The MIS 7 optimum corresponds to the time of ~240–236 ka. The warming was short-lived and strongly pronounced. The influence of the North Atlantic warm and saline sea-surface waters was greater than at present; the Arctic Front shifted northward. The reconstructed sea-surface temperature was approximately 2.9–3.6°C higher than the modern one. [ABSTRACT FROM AUTHOR]
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  Data: <i>Copyright of Doklady Earth Sciences is the property of Springer Nature and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract.</i> (Copyright applies to all Abstracts.)
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