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(Table 1) Occurrences of fossil Chaetoceros resting spore species in DSDP Hol...
Sediment depth is given in mbsf. Numbers indicate individuals encountered during 100 counts of resting spore valves; <1 indicates epivalves encountered after the count. -
(Appendix B) Dinoflagellate cysts eco-groups of DSDP Hole 38-338
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(Appendix B) Dinoflagellate cysts occurrence in DSDP Hole 38-338
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(Table S2) Age control points used to derive Eocene-Oligocene chronologies fo...
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Diatom abundance of Hole 38-338, Part 2
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Diatom abundance of Hole 38-338, Part 1
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 38-349
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 38-343
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 38-338
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 38-337
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Nannofossil abundance of Hole 38-336
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Silicoflagellate abundance of Hole 38-338
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Dinoflagellate abundance of Hole 38-338
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Global cooling during the Eocene Oligocene Transition
About 34 million years ago, Earth's climate shifted from a relatively ice-free world to one with glacial conditions on Antarctica characterized by substantial ice sheets. How... -
(Appendix A) Palynofacies absoulte abundances of DSDP Hole 38-338
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(Appendix A) Palynofacies raw counts of DSDP Hole 38-338
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(Table 3) Cr-rich spinel geochemistry of DSDP Hole 38-338 and ODP Hole 152-917A
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(Appendix) Geochemistry of samples from DSDP Hole 38-338, ODP Hole 152-917A a...
This dataset has no description
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(Table 4) Inferred melt compositions of DSDP Hole 38-338 and ODP Hole 152-917A
This dataset has no description
