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Cenozoic TEX86-derived global SST compilation including new data from ODP/DSD...
Cenozoic global TEX86-derived sea surface temperature (SST) compilation from all published marine TEX86 records and new data measured in this study (ODP/DSDP Sites 516, 588,... -
(Table 3) Lowermost occurrence of ice-rafted detritus clasts in selected DSDP...
Sediment depth is given in mbsf. Hole 28-266 was also investigated but no IRD clasts were present. -
(Table 2) Occurrence of ice-rafted detritus clasts in DSDP Holes 71-513 and 7...
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(Table 1) Major zones of ice-rafted detritus accumulation in DSDP Holes 71-51...
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(Table S2) Age control points used to derive Eocene-Oligocene chronologies fo...
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(Table 5) Geochemistry from DSDP Hole 71-514
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(Table 5) Geochemistry from DSDP Hole 71-513A
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(Table 6) Strontium isotope data of some benthic and planktonic foraminiferal...
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(Table 2) Oxygen and carbon isotope values for planktonic and benthic foramin...
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(Table 3) Rare earth and trace element contents in DSDP and ODP cherts
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(Table 1-2) Sample summary and major element contents in DSDP and ODP cherts
Contents are given on volatile free base -
(Data Set S1) Compiled benthic foraminiferal stable isotopic values
d13C_adj: carbon isotopic value adjusted to Cibicidoides equivalent.d18O_adj: oxygen isotopic value adjusted to Cibicidoides equivalent. -
(Table S1) Diatom species richness from the Early Pleistocene to present
The extent to which the spatial distribution of marine planktonic microbes is controlled by local environmental selection or dispersal is poorly understood. Our ability to... -
Neogene and Quaternary paleoenvironmental history at DSDP Leg 71 Holes
The Neogene and Quaternary sedimentary record of Leg 71 and previously drilled sequences from the Southern Ocean reveal evidence of a major late Miocene change of oceanic and... -
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... -
Ge/Si record of marine biogenic opal
We have determined germanium/silicon ratios in purified diatoms and radiolarians from siliceous sediments in Holocene core tops, one late Pleistocene piston core, and four... -
O, C and Sr isotopic data for plankton and benthic foraminifera from DSDP Leg...
A detailed d18O and d13C stratigraphy has been generated from analysis of well-preserved Albian - Early Maastrichtian foraminifera from Deep Sea Drilling Project (DSDP) Sites... -
Chemical composition of DSDP and ODP cherts
Rare earth element (REE), major, and trace element abundances and relative fractionations in forty nodular cherts sampled by the Deep Sea Drilling Project (DSDP) and Ocean... -
(Appendix) Benthic foraminiferal abundance at DSDP Hole 71-511
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(Figure 4) Distribution of benthic foraminifers in the Upper Cretaceous of DS...
X = present, - = absent.