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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... -
(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 S1) Diatom species richness from the Early Pleistocene to present
The extent to which the spatial distribution of marine planktonic microbes is controlled by local environmental selection or dispersal is poorly understood. Our ability to... -
Lithic grain and mineral composition of sand and sandstones from the North Pa...
Sand and sandstone compositions from different types of basins reflect provenance terranes governed by plate tectonics. One hundred and one thin sections of Upper Miocene 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... -
(Table 2) Analyses of prominent ash layers recovered at DSDP Site 18-178, Gul...
A sequence of ash layers recovered from site 178 of the Deep Sea Drilling Project in the Gulf of Alaska was studied to determine the nature of highly explosive volcanic... -
(Table 1) Argon dating of ash layers from DSDP Hole 18-178
Ash layers from Deep Sea Drilling Project site 178 in the northeast Pacific Ocean have been dated by the 40Ar-39Ar stepwise heating technique to resolve published discrepancies... -
(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... -
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... -
Calculated surface water paleotemperatures for the lower Pliocene at DSDP Sit...
The oxygen isotope record of the planktonic foraminifera Globigerina bulloides and Neogloboquadrina pachyderma from Pliocene and early Pleistocene sediments at both DSDP site... -
Minor-element chemical analyses of Hole 18-179
This dataset has no description
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Minor-element chemical analyses of Hole 18-178
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Minor-element chemical analyses of Hole 18-177A
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Minor-element chemical analyses of Hole 18-173
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Minor-element chemical analyses of Hole 18-172
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Major-element chemical analyses of Hole 18-179
This dataset has no description
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Major-element chemical analyses of Hole 18-178
This dataset has no description
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Major-element chemical analyses of Hole 18-177A
This dataset has no description
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Major-element chemical analyses of Hole 18-173
This dataset has no description
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Major-element chemical analyses of Hole 18-172
This dataset has no description