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- W62023835 endingPage "394" @default.
- W62023835 startingPage "297" @default.
- W62023835 abstract "Hemipelagic sediments in the SCS often register higher depositional rates. Carbonate compensation depth (CCD) in this marginal ocean basin is generally deeper than neighboring sea basins. Thus the SCS offers an ideal locality for paleoceanographic studies in the low-latitude western Pacific (Wang P. 1999). The first several cores in the world ocean used for high-resolution stratigraphy using accelerator mass spectrometer (AMS) 14C dating technique were from the southern part of this basin (Andree et al. 1986; Broecker et al. 1988). This is particularly significant for the western Pacific region where high-resolution paleo-studies are hampered by poor carbonate preservation and low sedimentation rates." @default.
- W62023835 created "2016-06-24" @default.
- W62023835 creator A5017303956 @default.
- W62023835 creator A5072936902 @default.
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- W62023835 date "2009-01-01" @default.
- W62023835 modified "2023-09-26" @default.
- W62023835 title "Upper Water Structure and Paleo-Monsoon5" @default.
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