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(Table S1) Calcium carbonate vein compositions
Depth, sediment = Curated depth (mbsf).K (Sr/Ca) (R), K (Mg/Ca) (R), Sr/Ca (R), Mg/Ca (R): calculated after Rimstidt et al. (1998), T-dependent.K (Sr/Ca) (G): calculated after... -
(Table 1) Summary of reconstructed seawater composition from Ca carbonate vei...
Sr/Ca (R), Mg/Ca (R): calculated after Rimstidt et al. (1998), T-dependentSr/Ca (M&B): calculated after Malone and Baker (1999), T-dependentSr/Ca (avg): average of both... -
Chemical composition of basaltic sand from DSDP Hole 49-413
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Chemical composition of bottom sediments from DSDP Hole 49-412
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Chemical composition of bottom sediments from DSDP Hole 49-410
This dataset has no description
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Chemical composition of bottom sediments from DSDP Hole 49-409
This dataset has no description
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Chemical composition of bottom sediments from DSDP Hole 49-408
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Chemical composition of bottom sediments from DSDP Hole 49-407
This dataset has no description
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(Table 3) Survey of Atlantic Ocean DSDP sites for hiatuses PH and NH 1 throug...
This dataset has no description
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(Table 4) Magnetic properties of titanomagnetite in MORB younger than 100 Ma,...
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Total organic carbon content in surface sediments, a compilation from differe...
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(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 5) Quaternary paleoproductivity of organic carbon in oceans based on D...
By analogy with the present-day ocean, primary productivity of paleoceans can be reconstructed using calculations based on content of organic carbon in sediments and their... -
Chemical composition of bottom sediments and rocks from DSDP Holes 3-14 throu...
Data on analyses of chemical composition of DSDP samples of bottom sediments and rocks carried out in P.P. Shirshov Institute of Oceanology are reported. Basal sediments and... -
Global compilation of benthic data sets I
Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary... -
Occurrence of hiatuses PH and NH 1 through NH 7 in DSDP holes
Miocene paleoceanographic evolution exhibits major changes resulting from the opening and closing of passages, the subsequent changes in oceanic circulation, and development of... -
Magnetic properties of Cenozoic MORB and Cretaceous MORB from DSDP and ODP holes
The fact that the natural remanent magnetization (NRM) intensity of mid-oceanic-ridge basalt (MORB) samples shows systematic variations as a function of age has long been... -
Planktic foraminifera abundance of Hole 49-410
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 49-407
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Occurrence of Globorotalia cavernula in the water column and sediments: globa...
Here, we present a global compilation of previously reported sightings of the rare planktic foraminifer Globorotalia cavernula Bé, 1967 as well as new observations of...
