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(Table T1) Planktonic and benthic foraminifer abundance of ODP Hole 183-1138A
Dominance is defined as the percentage of the benthic fauna constituted by the dominant species. Diversity is the number of species that constitute 95% of the benthic fauna. One... -
(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. -
(Figure 4) Distribution of benthic foraminifers in the Upper Cretaceous of DS...
X = present, - = absent. -
(Table 1) Relative abundances of Maastrichtian benthic foraminifera at El Kef...
Depth, sediment is depth below K/T boundary. -
(Table 1) Relative abundances of Maastrichtian benthic foraminifera at El Kef...
Depth, sediment is depth below K/T boundary. -
(Appendix 2, Part 4) Distribution of Maestrichtian to Paleocene benthic foram...
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(Appendix 2, Part 3) Distribution of Eocene to Recent benthic foraminifera in...
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(Appendix 2, Part 2) Distribution of Maestrichtian to Paleocene benthic foram...
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(Table 1) Occurrence of upper Maestrichtian to Eocene benthic foraminifers in...
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(Table S1) Benthic foraminifera at Ancora, Millville and Bass River drill sites
We describe seven Paleocene to lowermost Eocene sequences in core holes at Island Beach, Bass River, Ancora, Millville, and Sea Girt, NJ (Ocean Drilling Program Leg 150X, 174AX)... -
(Appendix) Benthic foraminifera distribution of upper Creatceous and Paleocen...
Benthic foraminifers of the Coniacian-Santonian through the Paleocene were recovered from a continuous pelagic carbonate section from Hole 516F on the Rio Grande Rise.... -
(Table 1) Distribution of Cretaceous-Tertiary benthic foraminifers in ODP Hol...
Reworked shallow-water larger and deep-water calcareous benthic foraminifers were recovered from foraminiferal packstones and nannofossil chalks in Hole 802A. The autochthonous... -
(Table DR1) Abundance of benthonic foraminifera in sediments from ODP Hole 11...
A mass extinction of deep-sea benthic foraminifera has been documented globally, coeval with the negative carbon isotope excursion (CIE) at the Paleocene-Eocene boundary, which... -
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 foraminifera in ODP Hole 199-1220B
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Range table from benthic foraminifers in ODP Hole 171-1052E
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Range table from benthic foraminifers in ODP Hole 171-1049A
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Range table from benthic foraminifers in ODP Hole 159-959D
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