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Tropical Pacific benthic isotope record for 0-5 Ma. Depth used is Revised Meters Composite Depth.
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A data frame on the following variables.
Variables: | |
Core.section. | |
interval.cm. | |
Depth.mbsf. | |
Depth.mcd. | |
Age.ka. | |
Species | |
d13C.raw. | |
d13C_adjustment.factor | |
d18O.raw. | |
d18O_adjustment.factor | |
d13C.final. | |
d18O.final. | |
Site 1143 is located at 9d21.72'N, 113d11'E, at a water depth of 2772 m within a basin on the southern continental margin of the South China Sea. Three holes were cored at the site and combined into a composite (spliced) stratigraphic section that documents complete re- covery for the upper 190.85 meters composite depth, the interval of ad- vanced piston coring (Wang, Prell, Blum, et al., 2000; Wang et al., 2001). The early Pliocene to Holocene sediment sequence provided abundant and well-preserved calcareous microfossils and offered an ex- cellent opportunity to establish foraminiferal stable isotope records. Here, we present benthic and planktonic d18O and d13C records that cover the last 5 m.y. These data sets will provide an important basis for upcoming studies to generate an orbitally tuned oxygen isotope stratig- raphy and examine long- and short-term changes in deep and surface water mass signatures (temperature, salinity, and nutrients) with an av- erage sample spacing of ~2.9 k.y. for the benthic and ~2.6 k.y. for the planktonic records.
The record is very framentary, and difficult to use for dynamical system calibration purposes
See the file ‘PKG/orig/ODP/ODP1143.txt’ for details. Original version at http://www-odp.tamu.edu/publications/184_SR/VOLUME/TABLES/SR184221/221_T02.TXT
Xinrong Cheng,2 Jun Tian,2 and Pinxian Wang2 , 4. DATA REPORT: STABLE ISOTOPES FROM SITE 1143, in Prell, W.L., Wang, P., Blum, P., Rea, D.K., and Clemens, S.C. (Eds.) Proceedings of the Ocean Drilling Program, Scientific Results Volume 184 http://www-odp.tamu.edu/publications/184_SR/VOLUME/CHAPTERS/221.PDF
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