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Pollen and spore abundance of Hole 18-175
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Pollen and spore abundance of Hole 18-174A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Pollen and spore abundance of Hole 18-174
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Pollen and spore abundance of Hole 18-173
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Annotated record of the detailed examination of Mn deposits from DSDP Site 17...
Site 172 was continuously cored to a depth of 24 meters in a sediment pond 140 kilometers south of the Murray fracture zone. The upper 9 meters consist of a moderate brown... -
(Supplement S3) Volcanic ash layer description and thickness analysis from di...
This dataset has no description
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(Table 1) Hf-Nd isotope ratios of marine sediments of the world's major subdu...
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... -
Geochemistry of marine sediments of the world's major subduction zones
This paper presents new major and trace-element data and Lu-Hf and Sm-Nd isotopic compositions for representative suites of marine sediment samples from 14 drill sites outboard... -
(Table 1) Major and trace element composition of marine sediments of the worl...
Sediment depth is given in mbsf. All concentrations reported relative to dry weight (110°C). -
(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... -
(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. -
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... -
(Table 1) Calculated paleoelevations of drillhole points 35 million years ago
This dataset has no description
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(Table 3) Petrological parameters of sands and sandstones from DSDP and ODP h...
Parameters and counted parameters used in the paper:Qpt = Polycrystalline quartz with tectonite fabricQpw = Polycrystalline quartz without tectonite fabricQm = Monocrystalline... -
(Table 2) Survey of Pacific Ocean DSDP sites for hiatuses PH and NH 1 through...
This dataset has no description
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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...
