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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... -
(Supplement S1) Volcanic ash layer description and thickness analysis from di...
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(Table 1) Hf-Nd isotope ratios of marine sediments of the world's major subdu...
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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 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... -
Annotated record of the detailed examination of Mn deposits from DSDP Leg 31 ...
The major purpose of Leg 31 was the scrutiny of tectonic, sedimentologic, volcanic, paleontologic, and paleooceanographic processes operative in arc-marginal basin complexes... -
(Table 1) Estimated age for the last occurrence of Globoquadrina dehiscens
Ages were transfered to the timscale of Berggren et al. (1995) -
(Table 1) Results from XRD analysis as well as sediment type and selected res...
The location of the seaward tip of a subduction thrust controls material transfer at convergent plate margins, and hence global mass balances. At approximately half of those... -
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... -
Calcareous nannofossil events of DSDP Hole 31-292
Calcareous nannofossil assemblages from land sections of the Japanese Islands and DSDP Holes in the equatorial to high latitude regions of the Pacific Ocean were analyzed in an... -
(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). -
Chemical composition of bottom sediments from DSDP Hole 31-294
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Chemical composition of basal bottom sediments from DSDP Hole 31-293
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Chemical composition of bottom sediments and basalt from DSDP Hole 31-291
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(Table 5) Chemical composition of normal basalts from outer zones of deep-wat...
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(Appendix 1) Compilation of calcium carbonate concentrations from deep sea se...
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(Appendix 1) Compilation of calcium carbonate concentrations from deep sea se...
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(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... -
Calcium carbonate global LGM Burial rate data
Global databases of calcium carbonate concentrations and mass accumulation rates in Holocene and last glacial maximum sediments were used to estimate the deep-sea sedimentary...
