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(Table 2) Age model control points, and CaCO3 and TOC accumulation rates of O...
Recent modeling studies call on increased ocean heat transport to explain high-latitude warming observed for intervals throughout the middle Pliocene. Possible vehicles for... -
(Table 4) Mass accumulation rates of selected components in red, green, and b...
Deep-water sedimentary sequences of mid-Cretaceous age, rich in organic carbon, have been recovered at many DSDP sites in the Atlantic Ocean. Most of these sequences have a... -
(Table 1) Geochemistry, accumulation rates and sea surface temperature estima...
We analyzed the unsaturation ratio (Uk37) of long-chain ketones - a molecular sea-surface temperature (SST) indicator û concentrations of carbonate and organic carbon in... -
(Appendix A) Geochemistry for Units 1/6, 2, and the upper part of Unit 3 of I...
Integrated Ocean Drilling Program (IODP) Expedition 302 Arctic Coring Expedition (ACEX) obtained the first relatively continuous long sediment cores from the Lomonosov Ridge in... -
(Appendix) Different accumulation rates from ODP Hole 189-1172A
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(Appendix) Different accumulation rates from ODP Hole 189-1168A
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(Table 1) Geochemistry of Sapropels of the Mediterranean Sea
Sapropels -organic-matter rich layers- are common in Neogene sediments of the eastern Mediterranean Sea. The formation of these layers has been attributed to climate-related... -
(Table 2) Age interval and accumulation rates of organic and inorganic carbon...
The Ocean Drilling Program Leg 175 recovered a unique series of stratigraphically continuous sedimentary sections along the SW African margin, an area which is presently... -
Carbon contents and isotopic compositions from the ODP Hole 161-974C near the...
The modern Mediterranean Sea is oligotrophic, yet its sediment record contains layers of organic-carbon-rich sapropels at 21 ky (precessional) spacing that imply periods of... -
Stable carbon isotope ratios and accumulation rates of organic carbon and nut...
Future warming is predicted to shift the Earth system into a mode with progressive increase and vigour of extreme climate events possibly stimulating other mechanisms that... -
Sedimentology and geochemical analyses of Pliocene to Holocene sediments of O...
A multiproxy geochemical study of nine sapropel layers from ODP Hole 964A, ODP Leg 160 in the eastern Mediterranean spanning the Pliocene-Holocene time interval provides new... -
Accumulation rate of Site 177-1089 (Table A-12)
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Geochemistry of black-shale cycles at Hole 159-959D
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(Table 1) Sample identification and bulk properties, Hole 175-1084A
The major biomarker compounds in surface (0.95 meters below seafloor [mbsf]) and deep (579.92 mbsf) sediment samples from the Benguela Current coastal upwelling system off... -
Tab.A.3.5. Sediment composition and accumulation rates of ODP Hole 105-646A
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Tab.A.3.4. Sediment composition and accumulation rates of ODP Hole 104-644A
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Tab.A.3.3. Sediment composition and accumulation rates of ODP Hole 104-643A
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Tab.A.3.2. Sediment composition and accumulation rates of ODP Hole 104-642D
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Tab.A.3.2. Sediment composition and accumulation rates of ODP Hole 104-642B
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Tab.A.3.1. Sediment composition and accumulation rates of Hole 49-408
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