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Major climatic changes in surface waters of the Japan Sea since the early middle Miocene

Conference · · EOS, Transactions, American Geophysical Union; (United States)
OSTI ID:6883999
 [1];  [2];  [3];  [4];
  1. Center for Marine Sciences, MS (United States)
  2. Univ. of Utah, Salt Lake (United States)
  3. Osaka Univ. (Japan)
  4. Univ. of California, Santa Cruz (United States)
The Japan Sea cooled from a subtropical to a temperature and subpolar biogeographic province during the early middle Miocene based on assemblages of planktonic foraminifers and calcareous nannofossils. High productivity persisted from 8 to 2 Ma as in other marginal basins of the Pacific rim based on the presence of diatom ooze, diatom clays, and diatom silty clays. Sea ice formed in the northern Japan Sea in short episode 4.5 and 4.0 Ma prior to the onset of extensive Northern Hemisphere glaciation 2.5 Ma. Sea ice reappeared between 2.7 and 2.4 Ma, 2.3 Ma, and between 0.9 and 0.7 Ma based on occurences of sea ice diatoms. Conditions in late Quaternary watermasses fluctuated in response to glacial cycles based on variable in assemblage composition, preservation, and abundance of radiolarians, planktonic foraminifers, and calcareous nannofossils. The relationship between surficial watermass conditions and cyclic deposition of dark brown, carbon-rich sediments constrains several hypotheses on depositional environment of the unusual lithology.
OSTI ID:
6883999
Report Number(s):
CONF-9002174--
Conference Information:
Journal Name: EOS, Transactions, American Geophysical Union; (United States) Journal Volume: 71:2
Country of Publication:
United States
Language:
English

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