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Benthic foraminiferal, Mg/Ca-based, paleotemperatures spanning the Cenozoic f...
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(Appendix 1) Sulphur isotope ratios barite and carbonate associated sulphates...
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(Appendix 2) Average Mg/Ca ratios of Cibicidoides spp. from ODP Site 113-689
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(Table 2) Stable oxygen isotope ratios of marine barite from ODP Hole 113-689B
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Mg/Ca ratios of Cenozoic benthic foraminifera from the Indian and South Atlan...
We investigate the evolution of Cenozoic climate and ice volume as evidenced by the oxygen isotopic composition of seawater (delta18Osw) derived from benthic foraminiferal Mg/Ca... -
Stable oxygen isotope ratios of marine barite from Cenozoic sediments
We report new data on oxygen isotopes in marine sulfate (delta18O[SO4]), measured in marine barite (BaSO4), over the Cenozoic. The delta18O[SO4] varies by 6x over the Cenozoic,... -
Late middle Eocene to late Oligocene radiolarian biostratigraphy of ODP Hole ...
We propose a new biostratigraphic scheme comprising the Eucyrtidium spinosum, Eucyrtidium antiquum (new), Lychnocanoma conica (emended), Clinorhabdus robusta (emended) and... -
High-resolution census data of Extinction Group species in the Cenozoic of OD...
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(Table S2) Benthic foraminiferal counts from ODP Hole 113-690C
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(Appendix 4) Calcareous nannofossils in ODP Hole 113-689B
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(Appendix 3) Calcareous nannofossils in ODP Hole 113-690B
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(Table 10) Stratigraphic occurrences of selected diatom species from the Neog...
A = abundant (>30% of total assemblage); C = common (15%-30%); F = few (3%-15%); R = rare (<3%); and T = trace (species encountered only sporadically); * = reworking or... -
Nitrogen isotope ratio and oxygen isotope ratio from Arabian Sea IODP Site 35...
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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... -
Peak areas and heights for minerals of ODP Leg 113-696B (Table 1)
Seismic data acquired over the eastern shelf and margin of the South Orkney microcontinent, Antarctica, have shown a high-amplitude reflection lying at a sub-bottom two-way... -
Late Cretaceous ostracods recorded from ODP Hole 113-689B
Twenty-six deep-sea ostracod species are described from the late Campanian to late Maastrichtian of ODP Site 689 in the Southern Ocean. Three are described as new:... -
Occurrence of late Aptian/earliest Albian radiolaria from ODP Hole 113-693A (...
Unusually well preserved Cretaceous radiolarians are observed in the subsurface sections from two drilled sites in the Weddell Sea collected during Leg 113 of the Ocean Drilling... -
(Appendix 2) Abundances of benthic forminifera in ODP Hole 113-690B
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(Appendix 1) Abundances of benthic forminifera in ODP Hole 113-689B
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(Table 7) Abundance of silicoflagellates and ebridians in ODP Hole 113-693A
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