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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 S4) Relative abundance of planktic foraminifera species in the 63-150 ...
DEPTH, sediment/rock [m] gives the depth below the Cretaceous-Paleogene boundary. -
(Table S3) Relative abundance of planktic foraminifera species in the >150 mi...
DEPTH, sediment/rock [m] gives the depth below the Cretaceous-Paleogene boundary. -
(Table S2) Relative abundance of planktic foraminifera species in the 63-150 ...
DEPTH, sediment/rock [m] gives the depth below the Cretaceous-Paleogene boundary. -
(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. -
(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
