-
(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 foraminifera abundance of Hole 2-10
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(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 2) Planktic foraminiferal species and number of specimens present in 5...
Preservation is poor with strong dissolution in predominantly volcanic sediments. -
(Table 1b) Relative percent abundance of planktic foraminiferal species at DS...
This dataset has no description
-
(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 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 1) Relative abundances of planktic foraminifera across the K/T transit...
size fraction >63 µm except for the laminated interval with 1 cm sample intervals across the K/T boundary, where the >38 µm size fraction was used -
(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 -
(Appendix A) Relative abundances of smaller size planktonic foraminifera in l...
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... -
Distribution of foraminiferal fauna from ODP Hole 122-762C (Table 1)
Planktonic foraminiferal diversity, equitability and biostratigraphic analysis of samples from Ocean Drilling Program (ODP) Leg 122, Hole 762C show that in general, cool water...
