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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... -
Oxygen and carbon isotopic composition in Eocene and Oligocene planktonic and...
Oxygen and carbon isotope ratios in Eocene and Oligocene planktonic and benthic foraminifera have been investigated from Atlantic, Indian, and Pacific Ocean locations. The major... -
Magnetic properties of Cenozoic MORB and Cretaceous MORB from DSDP and ODP holes
The fact that the natural remanent magnetization (NRM) intensity of mid-oceanic-ridge basalt (MORB) samples shows systematic variations as a function of age has long been... -
(Table 3) Lowermost occurrence of ice-rafted detritus clasts in selected DSDP...
Sediment depth is given in mbsf. Hole 28-266 was also investigated but no IRD clasts were present. -
(Table S2) Age control points used to derive Eocene-Oligocene chronologies fo...
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(Table 1) Calculated paleoelevations of drillhole points 35 million years ago
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(Table 2) Survey of Pacific Ocean DSDP sites for hiatuses PH and NH 1 through...
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(Table 1) Stable oxygen isotope ratios of benthic foraminifera from Pacific O...
The thermal structure of the Pacific Ocean between water depths of about 1 and 4.5 kilometers is estimated from the oxygen isotopic ratio of benthonic foraminifera from... -
Isotopic composition of carbon and oxygen from Paleogene deposits of some Pac...
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Neogene and Quaternary paleoenvironmental history at DSDP Leg 71 Holes
The Neogene and Quaternary sedimentary record of Leg 71 and previously drilled sequences from the Southern Ocean reveal evidence of a major late Miocene change of oceanic and... -
Global cooling during the Eocene Oligocene Transition
About 34 million years ago, Earth's climate shifted from a relatively ice-free world to one with glacial conditions on Antarctica characterized by substantial ice sheets. How... -
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... -
Foraminiferal oxygen and carbon isotopic measurements from 5 sites of souther...
The stratigraphy and paleoceanography of the late Miocene and early Pliocene have been examined at six sites in the South Atlantic and southwest Pacific oceans: Deep Sea... -
Ge/Si record of marine biogenic opal
We have determined germanium/silicon ratios in purified diatoms and radiolarians from siliceous sediments in Holocene core tops, one late Pleistocene piston core, and four... -
Strontium isotope ratios of pore waters and planktonic foraminifera from DSDP...
A detailed record of the strontium-87 to strontium-86 ratio in seawater during the last 100 million years was determined by measuring this ratio in 137 well-preserved and... -
Bolboforma abundance in sediment Hole 29-277
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Paleogene planktonic foraminifera of DSDP Hole 29-277
Stratigraphy of Paleogene deposits from high latitudes of the Pacific region (Koryak Highland, Kamchatka Peninsula, Karaginsky Island - in the northern hemisphere,... -
Nitrogen isotopic composition and chemical composition of altered oceanic cru...
Knowledge of the subduction input flux of nitrogen (N) in altered oceanic crust (AOC) is critical in any attempt to mass-balance N across arc-trench systems on a global or... -
Minor-element chemical analyses of Hole 29-282
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Minor-element chemical analyses of Hole 29-280A
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