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(Table S1, S4) Campanian-Maastrichtian benthic foraminifera from ODP Hole 113...
During the latest Cretaceous cooling phase, a positive shift in benthic foraminiferal d18O values lasting about 1.5 Myr (71.5-70 Ma) can be observed at a global scale... -
(Appendix 2) Late Cretaceous benthic foraminifera of ODP Site 207-1259
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(Appendix 1) Late Cretaceous benthic foraminifera of ODP Hole 207-1257A
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Foraminifera abundance of Hole 17-167
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Low-resolution census data of Extinction Group species in the Cenozoic of ODP...
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(Table S2) Benthic foraminiferal counts from ODP Hole 113-690C
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(Appendix Table 2) Percentages of benthic foraminiferal taxa, and number of s...
Sediment depth is given in mbsf. The top line corresponds to mbsf (meters below sea floor) for each sample. -
Total fauna of benthic foraminifera of sediment core Kronsmoor, Late Cretaceous
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Benthic foraminiferal abundances at the Cretaceous/Paleogene boundary of ODP ...
Sediments recovered at lower bathyal ODP Site 1049 on Blake Nose (Northwestern Atlantic) offer an opportunity to study environmental changes at the Cretaceous/Paleogene (K/P)... -
Relative abundances of benthic foraminifera at the Cretaceous/Paleogene bound...
Uppermost Maastrichtian benthic foraminiferal assemblages (>63 µm) are diverse, indicating mesotrophic conditions in lower bathyal DSDP Hole 465A (Hess Rise, central North... -
Benthic foraminiferal assemblages across the Cretaceous Paleogene boundray of...
Sediments recovered at ODP Site 1262 on Walvis Ridge (eastern South Atlantic Ocean, paleodepth ~2500–3000 m) offer an opportunity to look into the nature and cause(s) of the... -
Range table from benthic foraminifers in ODP Hole 159-959D
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