Feng-ye, L., Yu-lan, S. Study of Okinawa Trough sedimentation rates and paleoenvironment based on uranium series isotope., Chin. J. Ocean. Limnol. 14, 373–377 (1996). https://doi.org/10.1007/BF02850559
DOI:
Feng-ye, L., Yu-lan, S. Study of Okinawa Trough sedimentation rates and paleoenvironment based on uranium series isotope., Chin. J. Ocean. Limnol. 14, 373–377 (1996). https://doi.org/10.1007/BF02850559DOI:
Study of Okinawa Trough sedimentation rates and paleoenvironment based on uranium series isotope
摘要
Abstract
Spectrometry of238U
234U
230Th and
232Th in three Okinawa Trough cores showed that
based on the230Th/232Th activity ratio
the sedimentation rates were about 2.5cm/ka
2.8cm/ka and 8.5cm/ka respectively during the Holocene and about 20.1cm/ka
12.29cm/ka
8.8cm/ka and 12.6cm/ka respectively during the Würm glacial. To examine the past global climatic and oceanographic changes
the stable oxygen isotopes δ18O and CaCO3 were measured. The Th content and Th/U ratio showed that variations of terrigenous material input from the continental shelf were associated with glacial and interglacial changes and sea level fluctuations.
关键词
Keywords
references
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Phylogenetic diversity and bioactivity of culturable deepsea-derived fungi from Okinawa Trough
Palynological and algal assemblages from the sediments of Okinawa Trough
Major features and variability of the Kuroshio in the East China Sea
Geochemical studies of U, Th, Ra,40K in seciments of the China Sea and adjacent sea area, and lower reaches of several Chinese Rivers
A strategy for studying shelf circulation in China Seas —Interannual variability of shelf circulation
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Related Institution
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