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Stable isotope ratios of Maestrichtian foraminifera of DSDP Hole 44-390
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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... -
Stable isotope ratios of Maestrichtian foraminifera of DSDP Hole 39-357
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(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. -
(Figure 3) Distribution of planktonic foraminifers in the Upper Cretaceous of...
Species abundance: C = common, F = few, R = rare,VR = very rare, - = not observed. -
(Figure 2) Distribution chart of creatceous planktonic foraminifera of ODP Ho...
species abundance: A = abundant, C = common, F = few, R = rare, P = present, - = absent -
(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 -
Range table from planktonic foraminifers in ODP Hole 192-1186A
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Range table from planktonic foraminifers in ODP Hole 192-1183A
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Range table from planktonic foraminifers in ODP Hole 171-1052E
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Range table from planktonic foraminifers in ODP Hole 171-1050C
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Range table from planktonic foraminifers in ODP Hole 144-875C
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