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(Figure 2b) Distribution of age indicator species of planktic foraminifera at...
This dataset has no description
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(Table A1) Stable isotope ratios and paleotemperature calculation of selected...
Paleotemperature estimates were calculated using the equation of Erez and Luz (1983), with seawater delta18O = -1.2 per mil PDB corresponding to a continental ice-free world... -
Diatom abundance of Hole 62-466
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Diatom abundance of Hole 62-464
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Table 1) Occurrence and abundance of late Early Cretaceous radiolarians at D...
G = good; M = moderate; P = poor; PM = poor to moderate; - = looked for but not found; + = one specimen; A = abundant; C = common; F = few; R = rare; ? = uncertain... -
Relative abundances of benthic foraminifera at the Cretaceous/Paleogene bound...
Uppermost Maastrichtian benthic foraminiferal assemblages (>63 µm) are diverse, indicating mesotrophic conditions in lower bathyal DSDP Hole 465A (Hess Rise, central North... -
Late Cretaceous and Cainozoic bathyal Ostracoda of DSDP Site 62-463 in the Ce...
Cainozoic deep-sea ostracod assemblages from the summits of Mid-Pacific guyots point to high levels of endemism possibly as a result of their bathymetric separation from the... -
Stable oxygen and carbon isotope ratios for Early to Middle Cretaceous benthi...
Stable isotopic measurements have been made on planktonic and benthic foraminifera of Early to mid-Cretaceous (Early Albian-Cenomanian) age from DSDP site 463 located in the... -
Planktic foraminifera abundance of Hole 62-466
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 62-463
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 62-465A
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
Planktic foraminifera abundance of Hole 62-465
Relative abundance: D = dominant, A = abundant, C = common, F = few, R = rare, T = trace, P = present (numerical values are abundance in percent) -
(Table 2) Elastic constants and shear-wave velocities at DSDP Hole 62-465A
This dataset has no description
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(Table 1) Compressional-wave velocities at DSDP Hole 62-465A
This dataset has no description
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(Table 3) Anisotropy velocity (Pc = 0.2 kbar) at DSDP Holes 62-463 and 62-465A
This dataset has no description
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(Table 1) Summary of acoustic properties at DSDP Holes 62-463 and 62-465A
Sediment depth is given in mbsf. Empty cells = no data. -
(Table 2) Clinopyroxene chemistry at DSDP Hole 62-466
Number of cations on the basis of 6 oxygens. -
(Table 1) Petrography of volcanic clasts in upper Cretaceous sediments at DSD...
Empty cells = no data. Small clasts from 11-CC had 100 points counted. Remainder had 400 to 500 points counted. Iddingsite, calcite, and smectite replace olivine; smectite... -
(Table 2) Geochemical data and pyrolysis at DSDP Hole 62-463
Sediment depth is given in mbsf. Empty cells = no data, ? = value uncertain. -
(Table 1) Mineralogy at DSDP Hole 62-463
?1 = presence uncertain epmty cells = no data.
