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(Table 2) Oxygen stable isotope values for Globigerinoides sacculifer and Pul...
This dataset has no description
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(Table 1) Pliocene calcareous nannofossil events of DSDP Hole 31-292
For 1.8 to 31.55 mbsf see Sato et al. (2002) data set: doi:10.1594/PANGAEA.706116 -
(Appendix 1) Estimated sea-surface temperatures of DSDP Hole in the western P...
FP-12E is the planktonic foraminiferal transfer function developed by Thompson (1981, doi:10.1016/0031-0182(81)90099-7) for the western Pacific. Time-slice: 1 = 1.8-2.0 Ma, 2 =... -
(Appendix 1) Estimated sea-surface temperatures of DSDP Hole in the western P...
FP-12E is the planktonic foraminiferal transfer function developed by Thompson (1981, doi:10.1016/0031-0182(81)90099-7) for the western Pacific. Time-slice: 1 = 1.8-2.0 Ma, 2 =... -
(Table 2) Sr, Nd and Pb isotope parameters for DSDP basalts from the West Phi...
This dataset has no description
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(Table 1) Major and trace element abundances in basalts and basaltic glasses ...
This dataset has no description
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(Table 1) Estimated age for the last occurrence of Globoquadrina dehiscens
Ages were transfered to the timscale of Berggren et al. (1995) -
(Table 2) Planktonic foraminiferal datum levels and paleoclimatic events of D...
This dataset has no description
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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) 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... -
(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) Biostratigraphic zonation and core depth of microtektite occurrence...
Microtektites have been recovered from three horizons in eight middle Eocene to middle Oligocene marine sediment sequences. Five of these occurrences are coeval and of latest... -
(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... -
(Table 1) Age determinations of basement rocks of DSDP Leg 31
The origin and development of the Phillipine Sea have been central issues in tectonic studies of a marginal sea: the deep-sea drilling project (DSDP), Leg 31, was primarily... -
(Table 2) Stable carbon and oxygen isotope ratios of foraminifera of DSDP Hol...
Oxygen isotopic studies both of benthic formanifera (Emiliani, 1954, doi:10.1126/science.119.3103.853; Savin et al., 1975, doi:10.1130/0016-7606(1975)86<1499:TMP>2.0.CO;2;... -
Lithic grain and mineral composition of sand and sandstones from the Japan an...
One hundred and twenty point counts of Oligocene to Recent sands and sandstones from DSDP sites in the Japan and Mariana intraoceanic forearc and backarc basins demonstrate that... -
Strontium, Rubidium and Neodymium isotopic composition of sediments of wester...
The Nd–Sr isotopic signature of fine-grained clastic strata from western Pacific marginal basins has been examined to test the applicability of isotopic fluctuations in basin... -
(Table 1) Compressional wave velocities for rocks from DSDP Hole 31-293 in th...
Compressional wave velocities measured in gabbroic rocks and metabasites recovered from Site 293 of Leg 31 in the Philippine Sea (on the Central Basin Fault) are correlative... -
(Table 1) Compositions of magnetites and ferric hydroxides from sediments fro...
Twenty-eight specimens of clastogenic magnetites and ferric hydroxides recovered by the “Glomar Challenger”. from Cenozoic deposits in the deep-sea basins of the Japan and... -
(Table 3) Aeolian component of North Pacific pelagic sediments
Isolation and analysis of the eolian component of late Cenozoic pelagic sediments from the North Pacific provides direct information concerning changes in atmospheric...
