Data for: Carbonate-rich sequences in the deep sea of the eastern South Sea subbasin (IODP Hole U1431D) during the last 600 kyr
Published: 26 May 2020| Version 1 | DOI: 10.17632/v3hhs28ycn.1
Contributors:
AMANDA GEROTTO, Rubens Figueira, Annette Hahn, Renata Hanae Nagai, Iván Hernández Almeida, Paulo FerreiraDescription
Planktonic foraminiferal total abundance, fragmentation (FI%) and foraminiferal dissolution (FDX) indexes, and FTIR inferred total organic carbon content (TOC) in the first 20 m of the sedimentary column of the Hole U1431D (15o22’N, 117o00’E, 4240 m water depth, 617 m of sediment recovery) retrieved from the South China Sea East Subbasin during the IODP Expedition 349 on board the R/V JOIDES Resolution.
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Categories
Oceanography, Geochemistry, Micropaleontology, Geological Oceanography, Chemical Oceanography, Paleoceanography