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Carbon and oxygen isotope literature data for foraminifera from ODP Site 113-690
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(Table S1) Relative abundances of planktic foraminifera in ODP Hole 113-690B
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(Table 5) Stratigraphic ranges and relative abundances of Paleogene planktoni...
Abundance: S = very rare or single specimen (1-3 specimens); R = rare (<3 %); F = few (3-15 %); C = common (15-30 %); A = abundant (>30 %); - = not present; ? = doubtful... -
(Table 4) Stratigraphic ranges and relative abundances of Paleogene planktoni...
Abundance: S = very rare or single specimen (1-3 specimens); R = rare (<3 %); F = few (3-15 %); C = common (15-30 %); A = abundant (>30 %); - = not present; ? = doubtful... -
(Table 3) Stratigraphic ranges and relative abundances of Paleogene planktoni...
Abundance: S = very rare or single specimen (1-3 specimens); R = rare (<3 %); F = few (3-15 %); C = common (15-30 %); A = abundant (>30 %); - = not present; ? = doubtful... -
(Table 2) Stratigraphic ranges and relative abundances of Paleogene planktoni...
Abundance: S = very rare or single specimen (1-3 specimens); R = rare (<3 %); F = few (3-15 %); C = common (15-30 %); A = abundant (>30 %); - = not present; ? = doubtful... -
(Appendix II) Planktonic foraminiferal biostratigraphy of ODP Site 113-690
Species abundance: A = abundant, C = common, F = few, R = rare, X = reworked?, ? = questionable, - = not present. -
(Appendix I) Planktonic foraminiferal biostratigraphy of ODP Hole 113-689B
Species abundance: A = abundant, C = common, F = few, R = rare, X = reworked?, ? = questionable, - = not present. -
(Table 2) Ranges of middle Eocene through Holocene planktonic foraminifera in...
Species abundance: A = abundant (>25%), C = common (16-25%), F = few (6-15%), R = rare (<1%), ? = questionable, - = absent. Size fraction = >63 µm -
(Table 1) Relative abundance of planktic foraminifera in Paleocene to Eocene ...
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Planktonic foraminiferal assemblages of the Paleocene-Eocene Thermal Maximum ...
High-resolution study of Antarctic planktonic foraminiferal assemblages (Ocean Drilling Program Site 690, Weddell Sea) shows that these microplankton underwent a stepwise series... -
(Fig. 1) Stable carbon and oxygen isotope ratios of foraminifera of ODP Hole ...
A remarkable oxygen and carbon isotope excursion occurred in Antarctic waters near the end of the Palaeocene (~57.33 Myr ago), indicating rapid global warming and oceanographic...