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(Table A1) Stable isotope ratios and paleotemperature calculation of selected...
Paleotemperature estimates were calculated using the equation of Erez and Luz (1983), with seawater delta18O = -1.2 per mil PDB corresponding to a continental ice-free world... -
Planktic foraminiferal biostratigraphy of ODP Hole 171-1052E (Table S3)
Dataset showing numerical abundance counts on microsplits of the >150 micron fraction (non-zero numbers) and presence-absence observations (“0” and “x” entries) from the... -
Planktic foraminiferal biostratigraphy of ODP Hole 171-1050C (TAble S2)
Dataset showing numerical abundance counts on microsplits of the >150 micron fraction (non-zero numbers) and presence-absence observations (“0” and “x” entries) from the... -
Planktic foraminiferal biostratigraphy of ODP Hole 171-1049C (Table S1)
Dataset showing numerical abundance counts on microsplits of the >150 micron fraction (non-zero numbers) and presence-absence observations (“0” and “x” entries) from the... -
(Table 1b) Relative percent abundance of planktic foraminiferal species at DS...
This dataset has no description
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(Table A1) Stable isotope ratios and paleotemperature calculation of selected...
Isotope data for sample 74-525A-40-2,104-106 of the following species: Abathomphalus mayaroensis, Globotruncana arca, Gublerina cuvillieri, Heterohelix globulosa, Heterohelix... -
(Appendix C) Stable isotope ratios and paleotemperature calculation of select...
Absolute age estimates were determined based on average sedimentation rates within each planktonic foraminiferal biozone and magnetochron. Paleotemperature estimates were... -
(Appendix B) Relative abundances of larger size planktonic foraminifera in la...
Absolute age estimates were determined based on average sedimentation rates within each planktonic foraminiferal biozone and magnetochron
