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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... -
(Table S1) Relative abundance of planktic foraminifera species in the >150 mi...
DEPTH, sediment/rock [m] gives the depth below the Cretaceous-Paleogene boundary. <1 = present. -
(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... -
(Table Ia) Planktic foraminifera abundances in the latest Cretaceous sample i...
This dataset has no description
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(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 -
(Appendix) Distribution of planktonic foraminifers at DSDP Hole 72-516F, Coni...
During Leg 72 in the western South Atlantic, Cretaceous sediments were recovered only at Hole 516F (Rio Grande Rise). Late Cretaceous planktonic foraminifers were found in Cores...
