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(Table 1) Carbon and nitrogen chemistry of ODP Hole 183-1138A
We have conducted elemental, isotopic, and Rock-Eval analyses of Cenomanian-Santonian sediment samples from ODP Site 1138 in the southern Indian Ocean to assess the origin and... -
(Table 2) Chlorine geochemistry and mineralogy of altered oceanic crust samples
Bulk chlorine concentrations and chlorine stable isotope compositions were determined for hydrothermally altered basalt (extrusive lavas and sheeted dikes) and gabbro samples (n... -
(Table 1) Summary of horizon, lithology, and paleomagnetic of ODP Hole 126-79...
A paleomagnetic study was made on the highly vesiculated basaltic tuff breccia (the basaltic mousse) drilled by Ocean Drilling Program Leg 126 from the Izu-Bonin backarc, Sumisu... -
(Table 1) Color, Fe-C-S chemistry and carbonate content from ODP Sites 172-10...
Reflectance spectra collected during ODP Leg 172 were used in concert with solid phase iron chemistry, carbonate content, and organic carbon content measurements to evaluate the... -
(Table 1) Upper Carboniferous spores abundances from ODP Holes 172-1062B, 172...
Color variations were interpreted in paleoceanographic terms for the late Pliocene-Pleistocene sediments recovered by ODP Leg 172 on deep-sea drifts at Blake-Bahama Outer Ridge... -
Median grain size and distribution of sand in ODP Hole 108-660A (Fig. 5)
50 m of Middle Eocene pure radiolarian ooze were drilled at ODP Site 660 in the equatorial East Atlantic, 80 km northeast of the Kane Gap. The oozes comprise a 10 m high and 2... -
(Appendix A) Oxygen and carbon isotope results of detrital carbonate grains o...
We report oxygen and carbon isotope results of detrital carbonate grains from Heinrich layers at three sites in the North Atlantic located along a transect from the Labrador Sea... -
(Table 3) Oxygen isotope ratios of benthic foraminifera from DSDP Hole 80-548
Presently, the intermediate depths of the North Atlantic Ocean are occupied by a great lens of warm, saline water whose source is the Mediterranean Sea. This water flows both... -
(Table 1) Depth and revised depth from ODP Sites 169-1033 and 169-1034
The Holocene section in Saanich Inlet, Vancouver Island, British Columbia, is 50-70 m thick. Cores from Saanich Inlet obtained during Leg 169S of the Ocean Drilling Program... -
(Table 1) Phosphorus and carbon chemistry of ODP Holes 169-1033B and 169-1034B
Uncertainty currently exists about the removal of carbon (C) and phosphorus (P) from the oceanic reservoir, especially in low oxygen settings. In this paper, the cycling of C... -
(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... -
Apatite fission track analytical data for samples from ODP Leg 152
We test a new approach to understanding the tectonic evolution of passive margins by using fission-track analysis on detrital apatites from sediments deposited offshore East... -
Calculation of paleoproductivity during the Eocene-Oligocene transition of OD...
High-resolution records of carbon and oxygen isotopes and benthic foraminiferal accumulation rates for the Eocene-Oligocene section at Ocean Drilling Program Site 689 (Maud... -
(Table 2) Age controls used to derive a time scale for DSDP Site 73-522
The stratotype section for the base of the Miocene is at a reversed (below) to normal (above) magnetic transition that is claimed to represent magnetic chron C6Cn.2n (o). Deep... -
(Table 1) Sr-Nd-Pb isotopic compositions of samples from ODP Hole 183-1137
Basalts forming the floor of the Indian Ocean are geochemically distinct from those of the Atlantic and Pacific Oceans. These differences have been attributed to a deeply... -
(Table 1) Hydrocarbon (C1-C5) and carbon dioxide content of interstitial gas ...
Interstitial gases from the Deep-Sea Drilling Project (DSDP-IPOD) Leg-64 Sites 474, 477-479 and 481 in the Gulf of California have been analyzed by gas chromatography and... -
(Table 1) Age, thickness of sedimentary cover, depth into volcanic basement, ...
Textural and DNA studies of pillow lavas in DSDP/ODP cores from the Atlantic Ocean, the Lau Basin and the Costa Rica Rift indicate that microbes had a significant role in the... -
Calcium and iron of ODP Hole 113-690B
The late Paleocene thermal maximum (LPTM) is associated with a brief, but intense, interval of global warming and a massive perturbation of the global carbon cycle. We have... -
Lithium and osmium isotopes, and trace element ratios in bulk carbonates of d...
The Middle Eocene Climatic Optimum (MECO) was a ~400,000-year-long global warming event which occurred ~40 million years ago and interrupted the Eocene's long-term cooling... -
Cenozoic foraminifera-bound nitrogen isotope records, TEX86-derived global SS...
Over recent decades, the oxygen-deficient zones (ODZs) of the ocean have expanded, affecting marine ecosystems. However, their response to future global warming is poorly...
