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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... -
(Table 6) Mass accumulation rates for Jurassic to early Cretaceous sediments ...
This dataset has no description
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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... -
(Table DR1) Biogenic silica and chert in the Pacific Ocean, DSDP and ODP data
Evidence for the dissolution of biogenic silica at the base of pelagic sections supports the hypothesis that much of the chert formed in the Pacific derives from the dissolution... -
Benthic foraminiferal number of specimens in Cretaceous samples of various DS...
Benthic foraminifera from 24 DSDP/ODP sites were investigated to assess their global horizontal and vertical distribution in the deep-sea environment at the end of the... -
Paleomagnetic properties of igneous rocks from several DSDP and ODP sites, we...
Oceanic basalts and other related igneous rocks are considered excellent recorders of the Earth's paleomagnetic field. Consequently, basalt core paleomagnetic data are valuable... -
Chemistry and accumulation rates of Jurassic to early Cretaceous sediments fr...
Sedimentation in the central Pacific during the Jurassic and Early Cretaceous was dominated by abundant biogenic silica. A synthesis of the stratigraphy, lithology, petrology,... -
Compilation of global mid-Miocene opal distribution
This is a virtual data set that comprises several other real data sets. -
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... -
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... -
Oxygen and carbon isotopic composition in Eocene and Oligocene planktonic and...
Oxygen and carbon isotope ratios in Eocene and Oligocene planktonic and benthic foraminifera have been investigated from Atlantic, Indian, and Pacific Ocean locations. The major... -
(Table T1) Paleomagnetic properties of igneous samples from DSDP Leg 17 sites
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Cadmium contents in bottom sediments and sedimentary rocks from DSDP Holes 3-...
This dataset has no description
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CaCO3 contents in bottom sediments from DSDP Holes 9-80A, 9-81, 17-167, 30-28...
This dataset has no description
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Chemical composition of basal bottom sediments from DSDP Hole 17-170
This dataset has no description
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Chemical composition of bottom sediments from DSDP Holes 17-165A and 17-167
This dataset has no description
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(Table 1) Calculated paleoelevations of drillhole points 35 million years ago
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(Table 11) Distribution of radiolaria in Oligocene to Pliocene sediments of D...
Species abundaces: A = abundant, C = common, F = few, R = rare, - = absent. -
(Table 3) Rubidium and strontium concentrations and isotope ratios of DSDP ho...
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(Figure 2b) Distribution of age indicator species of planktic foraminifera at...
This dataset has no description