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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 3) Accumulation rates and residence times of iridium, osmium and rheni...
Concentrations are given for dry sediments. -
Revised Cenozoic hiatus database
The differential effects of climate change, sea level, and water mass circulation on deposition/erosion of marine sediments can be constrained from the distribution of... -
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 T1) Mineralogy of ODP Leg 199 and DSDP Hole 16-162 sediments - compari...
During Ocean Drilling Program Leg 199 in the equatorial Pacific, visible and near-infrared spectroscopy (VNIS) was used to measure the reflectance spectra (350-2500 nm) of 1343... -
(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... -
Os and Re concentrations and Os isotope ratios for DSDP and ODP metalliferous...
We report new 187Os/186Os data and Re and Os concentrations in metalliferous sediments from the Pacific to construct a composite Os isotope seawater evolution curve over the... -
Concentrations and accumulation rates of platinum-group elements and rhenium ...
The nature of Re-platinum-group element (PGE; Pt, Pd, Ir, Os, Ru) transport in the marine environment was investigated by means of marine sediments at and across the... -
Compilation of global mid-Miocene opal distribution
This is a virtual data set that comprises several other real data sets. -
Revised chronology of Neogene DSDP holes from the World Ocean
After nearly 30 years of growth in geochronologic knowledge, the originally published age models for many older deep sea marine sections have become badly outdated. In this... -
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... -
Ferromanganese nodules and crusts chemical analyses from SIO outside of the I...
The data encoded in the Scripps Institute of Oceanography Nodule Data Bank (SNDB) was used as a model for the publication of USGS Ferromanganese Crusts Data Bank. The chemical... -
Cadmium contents in bottom sediments and sedimentary rocks from DSDP Holes 3-...
This dataset has no description
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Chemical composition of transition and metalliferous bottom sediments from DS...
This dataset has no description
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Chemical composition of bottom sediments from DSDP Hole 16-162
This dataset has no description
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Chemical composition of basal transition and metalliferous bottom sediments f...
This dataset has no description
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Chemical composition of basal bottom sediments from DSDP Hole 16-160
This dataset has no description
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Chemical composition of basal bottom sediments from DSDP Hole 16-157
This dataset has no description
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(Table 1) Calculated paleoelevations of drillhole points 35 million years ago
This dataset has no description
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Coiling ratios of Pulleniatina spp. in sediments from DSDP Hole 16-157
This dataset has no description