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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) -
(Figure 10) Relative abundance of nannoliths at DSDP Hole 62-466
0 = species that were not observed in the particular sample during counting. -
(Figure 9) Relative abundance of nannoliths at DSDP Hole 62-465A
0 = species that were not observed in the particular sample during counting. -
(Figure 8) Relative abundance of nannoliths at DSDP Hole 62-464
0 = species that were not observed in the particular sample during counting. -
(Figure 7) Relative abundance of nannoliths at DSDP Hole 62-463
0 = species that were not observed in the particular sample during counting. -
(Table 5) Distribution and abundance of calcareous-nannoplankton species in t...
Sediment depth is given in mbsf. A = abundant, C= common, F = few, R = rare, VR = very rare, G = good, M = moderate, P = poor, + = present, X = cf., ? = questionable, - = not... -
(Table 6) Distribution and abundance of calcareous-nannoplankton species in t...
Sediment depth is given in mbsf. A = abundant, C= common, F = few, R = rare, VR = very rare, G = good, M = moderate, P = poor, + = present, X = cf., ? = questionable, - = not... -
(Table 4) Distribution and abundance of calcareous-nannoplankton species in t...
Sediment depth is given in mbsf. A = abundant, C= common, F = few, R = rare, VR = very rare, G = good, M = moderate, P = poor, + = present, X = cf., ? = questionable, - = not... -
(Table 3) Distribution and abundance of calcareous-nannoplankton species in t...
Sediment depth is given in mbsf. A = abundant, C= common, F = few, R = rare, VR = very rare, G = good, M = moderate, P = poor, + = present, X = cf., ? = questionable, - = not... -
(Table 2) Distribution and abundance of calcareous-nannoplankton species in t...
Sediment depth is given in mbsf. A = abundant, C= common, F = few, R = rare, VR = very rare, G = good, M = moderate, P = poor, + = present, X = cf., ? = questionable, - = not... -
(Tab. 15) Distribution of benthic foraminifera in Lower Cretaceous sediments ...
A = abundant, C = common, R = rare, - = absent. Samples 62-463-71-3,53-55, 62-463-79-1,34-35 radiolarians, samples 62-463-59-2, 62-463-59-CC, 62-463-70-1,41-42,... -
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... -
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... -
Concentrations and accumulation rates of platinum-group elements and rhenium ...
The nature of Re-platinum-group element (PGE; Pt, Pd, Ir, Os, Ru) transport in the marine environment was investigated by means of marine sediments at and across the... -
(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... -
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...
