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(Table 4) Stable carbon and oxygen isotope ratios of foraminifera from DSDP L...
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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(Appendix 1) Oxygen and carbon isotopic composition in foraminifera from DSDP...
This dataset has no description
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(Table 3) Relative percent abundance of planktic Foraminifera at DSDP Site 10...
Also examined samples: 10-95-12-4,72, 10-95-12-4,144, 10-95-13-1,63, Danian assemblage Zone P1c. 10-95-13-2,106, dissolution, mostly benthics present. 10-95-13-3,100, Middle... -
(Table 3) Rare earth and trace element contents in DSDP and ODP cherts
This dataset has no description
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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 -
Carbon isotope records from seven globally distributed marine sediment cores
Stable carbon isotope values of higher-plant leaf wax lipids were extracted, isolated, and measured from seven sediments cores. Sediment cores from DSDP/ODP Sites 94, 354, 511,... -
Age model parameters from seven globally distributed marine sediment cores
Stable carbon isotope values of higher-plant leaf wax lipids were extracted, isolated, and measured from seven sediments cores. Sediment cores from DSDP/ODP Sites 94, 354, 511,... -
Trace elemental data from the Cretaceous–Paleogene boundary (K-Pg boundary)
Trace elemental data from the K-Pg boundary -
Annotated record of the detailed examination of Mn deposits from DSDP Site 86...
The origin of the Campeche Escarpment in the Gulf of Mexico has been attributed to several causes. Some suggest that the scarp represents a fault scarp, others suggest that its... -
(Table 1) n-alkane distribution, and stable carbon and deuterium isotope rati...
Hydrology, source region, and timing of precipitation are important controls on the climate of the Great Plains of North America and the composition of terrestrial ecosystems.... -
(Table 1) Biostratigraphic zonation and core depth of microtektite occurrence...
Microtektites have been recovered from three horizons in eight middle Eocene to middle Oligocene marine sediment sequences. Five of these occurrences are coeval and of latest... -
Cretaceous ostracods of DSDP Hole 10-95 (Figure 2)
The ostracoda fauna recovered from site 95, JOIDES leg 10, consists of Albian and Senonian species, some of which have previously been described from the southeastern United... -
(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... -
Nannofossil datums and occurrence of microspherules in Upper Eocene sediments...
Upper Eocene microspherules (microtektites and microkrystites) have been found in deep-sea sediments from the western North Atlantic, Caribbean, Gulf of Mexico, equatorial... -
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... -
Radiolaria abundance of Hole 10-96
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Radiolaria abundance of Hole 10-95
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Radiolaria abundance of Hole 10-94
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Radiolaria abundance of Hole 10-86
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent)