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Strontium isotope ratios of middle Eocene to Oligocene sediments from Maud Ri...
A 87Sr/86Sr isotope curve of the middle Eocene to Oligocene was produced from analysis of foraminifera in Ocean Drilling Program Hole 689B, Maud Rise, near the coast of... -
Helium isotope concentrations and ratios in sediments from ODP Hole 130-806B
We have determined the helium abundance and isotopic composition of seafloor carbonate sediments from the flanks of the Ontong Java Plateau, western equatorial Pacific Ocean... -
Lithium and strontium isotopic compositions of sediments and pore waters at O...
The distribution of Li isotopes in pore waters to a depth of 1157 m below seafloor is presented for ODP Sites 918 and 919 in the Irminger Basin, offshore Greenland. Lithium... -
Chemical composition of hydrous and other minerals and their chromian spinel ...
Primary hydrous and other minerals enriched with incompatible components were found in ocean-floor ultramafic-mafic plutonic rock suites recovered from two contrasting ridge... -
Revised geomagnetic polarity timescale for the late Oligocene to early Miocen...
At Ocean Drilling Program (ODP) Site 1090 (subantarctic South Atlantic), benthic foraminiferal stable isotope data (from Cibicidoides and Oridorsalis) span the late Oligocene... -
Phosphorus partition and acumulation rates in sediments of ODP Legs 130 and 138
Understanding phosphorus (P) geochemistry and burial in oceanic sediments is important because of the role of P for modulating oceanic productivity on long timescales. We... -
Sulphur contents and partition of iron in ODP Leg 112 sediments
Porewaters in site 680 Peru Margin sediments contain dissolved sulfide over a depth of approximately 70 m which, at a sedimentation rate of 0.005 cm/yr, gives a sediment... -
Chemical and strontium isotopic compositions of interstitial waters from sedi...
The depth variations in the major chemical components dissolved in interstitial waters from the Tonga margin (ODP Site 841) are much more pronounced than those usually observed... -
Age and oxygen isotope data for bulk carbonate from DSDP Sites 41-366 and 72-...
A numerical model which describes oxygen isotope exchange during burial and recrystallization of deep-sea carbonate is used to obtain information on how sea surface temperatures... -
Oligocene magnetostratigraphy for equatorial Pacific ODP Sites
An Oligocene magnetostratigraphy from ODP Sites 1218 and 1219 (Equatorial Pacific) has been obtained by measurements made on u-channel samples, augmented by about 221 discrete... -
Strontium and boron geochemistry of ODP sites at Hydrate Ridge, eastern Pacif...
ODP Leg 204, which drilled at Hydrate Ridge, provides unique insights into the fluid regime of an accretionary complex and delineates specific sub-seafloor pathways for fluid... -
Os isotope ratios of Late Eocene sediments from the tropical Pacific
High resolution records (ca. 100 kyr) of Os isotope composition (187Os/188Os) in bulk sediments from two tropical Pacific sites (ODP Sites 1218 and 1219) capture the complete... -
Stable oxygen isotope ratios of marine barite from Cenozoic sediments
We report new data on oxygen isotopes in marine sulfate (delta18O[SO4]), measured in marine barite (BaSO4), over the Cenozoic. The delta18O[SO4] varies by 6x over the Cenozoic,... -
Bromine and iodine concentrations in sediments and pore fluids of ODP Leg 112
At the Peruvian convergent margin, two distinct pore fluid regimes are recognized from differences in their Cl- concentrations. The slope pore fluids are characterized by low... -
Late Pliocene stable oxygen isotope and Mg/Ca record, and paleotemperature re...
The onset of Northern Hemisphere Glaciation (NHG) ~2.7 Ma ago coincided with prominent climate changes in the tropical regions such as the African and the Asian monsoons.... -
Major element concentrations in spinel, olivine and pyroxene from peridotites...
Serpentinized spinel peridotites of the Newfoundland margin drilled during ODP Leg 210 at Site 1277 have preserved, relic mineral compositions similar to the most depleted... -
Re-OS and Pb isotope ratios of sediments from Saanich Inlet, Western Canada
Re-Os and Pb-Pb isotopic analysis of reduced varved sediments cored in the deeper basin of Saanich Inlet (B.C.) are presented. From core top to 61 cm down-core, spanning... -
Geochemisty and Re-Os isotope ratios of peridotites from ODP Hole 209-1274A f...
Comprehensive major-, trace-element and rhenium-osmium (Re-Os) isotope data are presented for abyssal peridotites from Ocean Drilling Program (ODP) Leg 209, in the North... -
Contents, partition, and isotopic composition of sulphur in sediments from OD...
We have determined (1) the abundance and isotopic composition of pyrite, monosulphide, elemental sulphur, organically bound sulphur, and dissolved sulphide; (2) the partition of... -
Organic geochemistry of deep sea sediments from the Nankai Trough and the Sou...
Earth's largest reactive carbon pool, marine sedimentary organic matter, becomes increasingly recalcitrant during burial, making it almost inaccessible as a substrate for...
