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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 S4) Modern SST at the site location, backtracked for plate movement, O...
This dataset has no description
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(Table S4) Modern SST at the site location, backtracked for plate movement, O...
This dataset has no description
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(Table 3) Carbonate accumulation and paleobathymetry of eastern Pacific DSDP ...
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Pacific Neogene carbonate accumulation rates
I have compiled CaCO3 mass accumulation rates (MARs) for the period 0–25 Ma for 144 Deep Sea Drilling Project and Ocean Drilling Program drill sites in the Pacific in order to... -
SST gradient and reconstructed Antarctic Circumpolar Current latitude changes...
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(Table 1) Paleocoordinates of deep-sea drilling sites in Neogene
Reconstruction of climatic zonation and features of surface water circulation in the Indian Ocean for seven selected time intervals is presented based on DSDP/ODP data on... -
(Table S4) Modern SST at the site location, backtracked for plate movement, O...
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(Table 2) Paleolatitude and reconstructed temperatures for Cretaceous samples...
AGE [ka BP] is an estimated age. Absolute ages of samples are estimated from sedimentation rate curves for the Leg 207 sites (Erbacher et al., 2004) and have an estimated... -
(Table T14) Paleolatitudes for ODP Leg 173 and Leg 149 sites
AGE is given as the mean of minimum and maximum age. -
(Table 6) Mass accumulation rates for Jurassic to early Cretaceous sediments ...
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(Table T3) Mean inclinations and paleolatitudes of ODP Holes 210-1276A and 21...
Sediment depth is given in mbsf. Approximate age estimates from Hart and Blusztajn (2006, doi:10.1016/j.chemgeo.2006.07.001), Jagoutz et al. (2007, doi:10.1130/G23613A.1) and... -
(Appendix A) Paleomegnetic of ODP Hole 162-983C
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(Appendix A) Paleomegnetic of ODP Hole 162-983B
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(Table 1) Oxygen and carbon isotopic values of benthic foraminifera from the ...
Stable isotopic data from benthic foraminifera indicate the occurrence of at least three deepwater masses in the late Maastrichtian ocean. Given mean oceanic d18Ow of -1.0 per... -
Chert intervals in DSDP and ODP sites (Table 1)
Radiolarian cherts in the Tethyan realm of Jurassic age were recently interpreted as resulting from high biosiliceous productivity along upwelling zones in subequatorial... -
LPEE reconstructions of oxygen and hydrogen isotope compositions of precipita...
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(Table S4) Modern SST at the site location, backtracked for plate movement, s...
This dataset has no description
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(Table S4) Modern SST at the site location, backtracked for plate movement, D...
This dataset has no description
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(Table S4) Modern SST at the site location, backtracked for plate movement, I...
This dataset has no description