-
Paleoelevations in the Pacific Ocean 35 million years ago
Data from deep sea drilling, linear magnetic anomalies and bathymetric measurements together with age and morphometric characteristics of seamounts have been used to construct a... -
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... -
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... -
Foraminiferal oxygen and carbon isotope data for DSDP Sites 32-305 and 62-463...
Oxygen isotope analyses of well-preserved foraminifera from Blake Nose (30°N paleolatitude, North Atlantic) and globally distributed deep-sea sites provide a long-term... -
(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... -
TOC, TC, CaCO3 and Sr/Ca ratios of DSDP Hole 62-463 (Table 2)
There has been an interest in the application of Sr / Ca ratios in pelagic carbonates to reconstruct paleoceanographic conditions such as changes in the oceanic Ca and Sr... -
Annotated record of the detailed examination of Mn deposits from DSDP Leg 62 ...
The four sites drilled during Leg 62 were needed to establish better regional coverage of the North Pacific Ocean. Although paleoenvironments were to be stressed on Leg 62,... -
(Table 2) Major and trace elements of sulfide-rich layers from Unit II at DSD...
Fe, Ag, and Cu for 62-465A-40-2,18-20 by AA analysis. -
(Table 7) Geochemistry at DSDP Site 62-466
Sediment depth is given in mbsf. Analytical values for Mg and Na by atomic absorption were corrected for interstitial sea water. Empty cells indicate no analysis. -
(Table 5) Geochemistry at DSDP Site 62-465
Sediment depth is given in mbsf. Analytical values for Mg and Na by atomic absorption were corrected for interstitial sea water. -
(Table 3) Geochemistry at DSDP Hole 62-464
Sediment depth is given in mbsf. Analytical values for Mg and Na by atomic absorption were corrected for interstitial sea water. -
(Table 1) Geochemistry at DSDP Hole 62-463
Sediment depth is given in mbsf. Analytical values for Mg and Na by atomic absorption were corrected for interstitial sea water. -
(Table 2) Chemistry of bulk and <1-µm size fractions of altered volcanic ash,...
Other elements were scanned, but are below the limits of detection (listed in the parentheses in ppm): Ag (1.0), As (200), Au (10), Bi (10), Cd (2.0), Sb (15), Sn (2.0), Te... -
Chemical composition of basal sedimentary rocks from DSDP Hole 62-465A
This dataset has no description
-
Geochemistry of the oceanic crust from ocean drilling samples
This book presents new data on chemical and mineral compositions and on density of altered and fresh igneous rocks from key DSDP and ODP holes drilled on the following main... -
(Table 6) Mass accumulation rates for Jurassic to early Cretaceous sediments ...
This dataset has no description
-
(Table 1) Concentrations of platinum-group elements and rhenium in sediments ...
Concentrations are given for dry sediments. -
(Table 2) Distribution of kummerform and sinistral specimens the planktic for...
This dataset has no description
-
(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... -
K-T boundary in DSDP Holes 62-465 and 74-527 (Table 2)
The global extinctions linked to the Cretaceous-Tertiary (K-T) boundary severely affected marine pelagic organisms. The K-T boundary intervals at Deep Sea Drilling Project...
