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Age determination of ODP Hole 182-1127B (Table 1)
In Northern Hemisphere deglaciation records, the transition from the last glacial to the Holocene indicates a rapid return to near-glacial conditions during the Younger Dryas,... -
(Appendix 1) Crustal helium-4 abundance and flux data for ODP Hole 130-806B
The mass accumulation rates (MARs) of aeolian dust in the ocean basins provide an important record of climate in the continental source regions of atmospheric dust and of the... -
Osmium concentrations and isotope ratios of ODP Site 146-893A
The Pleistocene deposits of Santa Barbara Basin (SBB) show laminations during interglacial periods typical of an anoxic or suboxic depositional environment and more sporadically... -
Neodymium isotope ratios of fish teeth from ODP Site 113-689 (Appendix A)
Long-term records of neodymium (Nd) isotopes from sedimentary archives can be influenced by both changes in water mass mixing and continental weathering. Results of Nd isotopic... -
(Table 1) Chemical compositions of beryllium in sediments and pore waters of ...
Studies of Be distributions in subduction zone sediments will help to understand questions regarding the enrichments of cosmogenic Be-10 in arc volcanic rocks. Analyses of Be-10... -
(Table 1) B content, d11B, δ¹⁸O, degree of alteration, and lithology of basal...
Boron contents and boron isotopic compositions were determined for the uppermost 1.3 km section of typical 6.2 Ma oceanic crust from DSDP/ODP Hole 504B, Costa Rica Rift,... -
Isotope record of Nd-Sr-Pb in deep sea sediments from the Pacific (Table 2)
Pelagic clay of the east-central Pacific province is shown to be a mixture of three primary detrital components, reflecting continental source areas in Asia, North America, and... -
(Table 1) Sulfur contents and isotope composition in rocks and minerals from ...
DSDP Hole 504B is the only hole in oceanic crust to penetrate through the volcanic section and into hydrothermally altered sheeted dikes. We have carried out petrologic and... -
(Table 1) Organic carbon and hydrogen index data for sediment samples from OD...
The extractable organic matter in Holocene to early Miocene deep-sea sediments from Site 645 (ODP Leg 105) in Baffin Bay contains almost exclusively biological markers of... -
Magnetostratigraphy of ODP Site 177-1092 (Table 1)
Ocean Drilling Program (ODP) Site 1092 from the sub-Antarctic South Atlantic produced a clear magnetic stratigraphy for the Late Miocene [Evans et al., 2003,... -
Age control points and sedimentation rates of ODP Hole 145-887B (Table 1)
Hole 887B of the Ocean Drilling Program (ODP) comprises a 44 m (750 kyr) long continuous section recovered from the Patton-Murray Rise, an elevated plateau that is largely... -
(Table 1) Composition of rocks from ODP Hole 140-504B before and after leachi...
Hydrothermally altered rocks from the base metal depleted reaction zone in the lower sheeted dyke complex (ODP Hole 504B) show significant losses of rare earth elements (REE) in... -
Occurrence of microtextures recorded from quartz sand grains of ODP Hole 178-...
Sediment drifts on the continental rise are located proximal to the western side of the Antarctic Peninsula and recorded changes in glacial volume and thermal regime over the... -
Pliocene-Pleistocene biostratigraphic datums of ODP Site 184-1148
Based on the stable isotopic analysis of planktonic and benthic foraminifers from Ocean Drilling Program Core 1148 of the northern South China Sea (SCS), Pliocene-Pleistocene... -
Mid-Pliocene polarity zones of ODP Site 177-1092 (Table 2)
We present mid-Pliocene (4.3-2.6 Ma) benthic stable oxygen and carbon isotope data from Ocean Drilling Program Site 1092 (ODP Leg 177) drilled in the sub-Antarctic sector of the... -
(Table 1) Rock type and summary of alteration after component minerals in thi...
This dataset has no description
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Biostratigraphy and average linear sedimentation rate and accumulation rate o...
Reconstructing the long-term evolution of organic sedimentation in the eastern Equatorial Atlantic (ODP Leg 159) provides information about the history of the climate/ocean... -
(Table 1) Forms of iron, organic and inorganic carbon, aluminium, molybdenum,...
An abrupt transition from oxic to anoxic-sulfidic (euxinic) marine bottom waters occurred in the Cariaco Basin in response to increasing productivity resulting from the late... -
Composite stratigraphy of ODP Site 177-1094 and sediment core TTN057-13-PC4 (...
Visual counts of ice-rafted debris (IRD), foraminifera, and radiolaria were made for ~1500 samples in Site 1094 spanning the last four climatic cycles (marine isotope stages... -
(Table 6) Sb isotope composition of bottom sediments from ODP Hole 185-1149A
Multiple-collector inductively coupled plasma mass spectrometry (MC-ICP-MS) has been used for the precise measurement of Sb isotopic composition in geological samples, as well...
