-
Cadmium contents in bottom sediments and sedimentary rocks from DSDP Holes 3-...
This dataset has no description
-
(Table S3) Mean sea surface temperture values of the Eocene-Oligocene Transit...
Estimated values at ~33-34 Ma (EOT) and at ~34-37 Ma (pre-EOT). With consideration of chronology uncertainty, we allowed time intervals over which mean SST values were... -
(Table S2) Age control points used to derive Eocene-Oligocene chronologies fo...
This dataset has no description
-
Magnetic properties of the oceanic igneous rocks (Table 1)
Hysteresis measurements have been carried out on a suite of ocean-floor basalts with ages ranging from Quaternary to Cretaceous. Approximately linear, yet separate,... -
(Table 1) Average aluminium accumulation rate at 40 DSDP Sites for the time i...
A six-fold increase in the rate of accumulation of Al in north and central Atlantic and Pacific Ocean sediments indicates vastly increased denudation of the continents during... -
Compilation of global mid-Miocene opal distribution
This is a virtual data set that comprises several other real data sets. -
Geochemistry and geological ages for organic-rich black shales of the Quatern...
This dataset has no description
-
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 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... -
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... -
(Appendix Table 1) Hf isotope ratios of basalts from the North Atlantic Igneo...
Lu and Hf concentrations determined by ICP-MS at the Univ. of Durham, except for the samples from Goban Spur (Leg 80), which were determined by INAA at Leicester University.... -
(Appendix A) Palynofacies absoulte abundances of DSDP Hole 38-338
This dataset has no description
-
Annotated record of the detailed examination of Mn deposits from DSDP Leg 38 ...
Because of its position between the North Atlantic and the Arctic oceans, its young age, small size, and diversity of geological structures, the Norwegian-Greenland Sea provided... -
Chemical composition of basal bottom sediments from DSDP Hole 38-348
This dataset has no description
-
Chemical composition of basal sedimentary rocks from DSDP Hole 38-345
This dataset has no description
-
Chemical composition of bottom sediments from DSDP Hole 38-338
This dataset has no description
-
Chemical composition of bottom sediments from DSDP Hole 38-336
This dataset has no description
-
(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 interstitial waters from DSDP Si...
Six Deep Sea Drilling Project (DSDP) Sites (252, 285, 315, 317, 336, 386) were examined for the chemical composition of the dissolved salts in interstitial waters, the oxygen...