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Last Glacial Maximum seawater temperature estimates based on planktonic foram...
Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS... -
(Table 2) Nitrogen concentrations and isotopic compositions of samples from D...
This dataset has no description
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(Table 2) Chlorine geochemistry and mineralogy of altered oceanic crust samples
Bulk chlorine concentrations and chlorine stable isotope compositions were determined for hydrothermally altered basalt (extrusive lavas and sheeted dikes) and gabbro samples (n... -
Geochemistry of the oceanic crust from ocean drilling samples
This book presents new data on chemical and mineral compositions and on density of altered and fresh igneous rocks from key DSDP and ODP holes drilled on the following main... -
Nitrogen isotopic composition and chemical composition of altered oceanic cru...
Knowledge of the subduction input flux of nitrogen (N) in altered oceanic crust (AOC) is critical in any attempt to mass-balance N across arc-trench systems on a global or... -
(Table 3) Age determination of eastern equatorial Pacific sediment cores
Sediment depth is given in mbsf. Measured on Neogloboquadrina dutertrei >200 µm. 14C results were calibrated to calendar ages considering a one standard deviation uncertainty... -
(Table 2) Age models and isotope analyses for eastern equatorial Pacific sedi...
This dataset has no description
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(Table S6) Published Pliocene-Pleistocene Mg/Ca-SST data for DSDP Hole 70-509...
AGE [ka] from original Mg/Ca publication. -
(Table 10) Trace elements in DSDP Sample 70-504B-36-1,91-110
The nine laboratories are the Woods Hole Oceanographic Institution (WHOI), the Vernadsky Institute of Geochemistry and Analytical Chemistry, Moscow (VIG), the Department of... -
(Table 9) Trace elements in DSDP Sample 70-504B-36-1,91-110
The nine laboratories are the Woods Hole Oceanographic Institution (WHOI), the Vernadsky Institute of Geochemistry and Analytical Chemistry, Moscow (VIG), the Department of... -
(Table 7) Deviations from the mean value for all major elements for the diffe...
The nine laboratories are the Woods Hole Oceanographic Institution (WHOI), the Vernadsky Institute of Geochemistry and Analytical Chemistry, Moscow (VIG), the Department of... -
(Table 6) Major element composition of DSDP 70-504B-40-2,72-88 when recalcula...
The nine laboratories are the Woods Hole Oceanographic Institution (WHOI), the Vernadsky Institute of Geochemistry and Analytical Chemistry, Moscow (VIG), the Department of... -
(Table 5) Major element composition of DSDP 70-504B-36-1,91-110 when recalcul...
The nine laboratories are the Woods Hole Oceanographic Institution (WHOI), the Vernadsky Institute of Geochemistry and Analytical Chemistry, Moscow (VIG), the Department of... -
(Table 3) Major element composition of DSDP Sample 70-504B-40-2,72-88
The nine laboratories are the Woods Hole Oceanographic Institution (WHOI), the Vernadsky Institute of Geochemistry and Analytical Chemistry, Moscow (VIG), the Department of... -
(Table 2) Major element composition of DSDP Sample 70-504B-36-1,91-110
The nine laboratories are the Woods Hole Oceanographic Institution (WHOI), the Vernadsky Institute of Geochemistry and Analytical Chemistry, Moscow (VIG), the Department of... -
(Table 11) Geochemistry of plagioclases at DSDP Legs 68-70
Structural formulae calculated on the basis of 32 oxygens. -
(Table 10) Geochemistry of olivine at DSDP Legs 68-70
Structural formulae calculated on the basis of 4 oxygens. -
(Table 9) Geochemistry of Cr-spinels at DSDP Holes 70-504B and 68-501
Structural formulae computed from stoichiometry on the basis of 32 oxygens. -
(Table 7) Geochemistry of clinopyroxenes at DSDP Legs 69-70 Holes
Structural formulae calculated on the basis of 6 oxygens. Empty cells mean no data. -
(Table 6) Geochemistry of plagioclases at DSDP Legs 69-70 Holes
Structural formulae calculated on the basis of 32 oxygens.