Stratigraphy and major paleoenvironmental changes in the Sea of Okhotsk during the last million years inferred from radiolarian data

The radiolarian distribution is studied in Core IMAGES MD01-2415(46-m-long) from the central Sea of Okhotsk. The obtained data made it possible to refine the regional biostratigraphy and document the major paleoenvironmental changes in the basin in the last million years. In total, 17 radiolarian da...

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Bibliographic Details
Published in:Oceanology
Main Authors: Matul, A. G., Abelmann, A., Nürnberg, Dirk, Tiedemann, R.
Format: Article in Journal/Newspaper
Language:English
Published: Pleiades Publishing, Springer 2009
Subjects:
Okhotsk
Pacific
Subarctic
Online Access:https://oceanrep.geomar.de/id/eprint/13342/
https://oceanrep.geomar.de/id/eprint/13342/1/Matul.pdf
https://doi.org/10.1134/S0001437009010111
Description
Summary:The radiolarian distribution is studied in Core IMAGES MD01-2415(46-m-long) from the central Sea of Okhotsk. The obtained data made it possible to refine the regional biostratigraphy and document the major paleoenvironmental changes in the basin in the last million years. In total, 17 radiolarian datum planes are defined with 12 of them being new. Their number exceeds that previously established for different fossil groups in the Subarctic Pacific for this period. Radiolarian datum planes are usually confined to the main boundaries and Quaternary climatic events. The analysis of the radiolaria distribution reveals several major paleoenvironmental shifts in the sea that occurred 950, 700, and 420-280 ka ago and are correlative with regional and global phases of the Middle Pleistocene climatic revolution.

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