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Geochemistry of sediment core Kinneret_AA3
Long-term fire histories provide insight into the effects of climate, ecology and humans on fire activity; they can be generated using accumulation rates of charcoal and soot... -
Basal age, surface accumulation, basal melting, geothermal flux and Lliboutry...
Ice sheets provide exceptional archives of past changes in polar climate, regional environment and global atmospheric composition. The oldest dated deep ice core drilled in... -
Size normalized planktic foraminifera weight and coccolith diameter from DSDP...
As a result of anthropogenic pCO2 increases, future oceans are growing warmer and lower in pH and oxygen, conditions that are likely to impact planktic communities. Past... -
Mass accumulation rates of IODP Hole 320-U1333C
Understanding changes in export production through time provides insight into the response of the biological pump to global climate change, particularly during periods of rapid... -
(Table 1) Mass-accumulation rates for the non-authigenic, inorganic, crystall...
Elevated regions in the central parts of ocean basins are excellent for study of accumulation of eolian material. The mass-accumulation rates of this sediment component appear... -
(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) Components and accumulation rates of sediments from ODP Leg 165 sites
Records of long-term sediment deposition in the Caribbean Sea were recovered during Ocean Drilling Program Leg 165. Samples from the Cayman Rise (Site 998), the Colombian Basin... -
(Table T1) Sedimentation rate, bulk density and mass accumulation rate of ODP...
Ocean Drilling Program Leg 198 Site 1208 is located on the Central High of Shatsky Rise (36°7.6301'N, 158°12.0952'E) in the North Pacific Ocean at a water depth of 3346 m. A... -
(Table 2) Age-depth datums, sedimentation rate and accumulation rates of ODP ...
Results of preliminary pollen analyses of 280 samples from selected intervals of cores from Hole 798 on the Oki Ridge in the Sea of Japan (Sections 798A-1H-1 through... -
(Table 1) Radiolarian accumulation rates and geochemistry of ODP Site 184-1143
Late Miocene–Recent micropaleontological and geochemical records from Ocean Drilling Program (ODP) Site 1143 in the southern South China Sea (SCS) indicate that increase and... -
Age and accumulation rates of bottom sediments from Core AMK21-2179, Woodlark...
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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) Sedimentation and accumulation rates of DSDP Holes 38-337 and 38-338
The modern depositional environment of the deep Norwegian-Greenland Sea is highly asymmetric in an E–W direction because of the hydrography of the surface water masses and... -
Major and trace element concentrations, accumulation rates and carbonate cont...
Statistical analyses of sediment geochemical data from a Cretaceous/Tertiary (KT) boundary section at Broken Ridge indicate that the sediments here are composed of three major... -
(Table 2) Actual and synthetic mass accumulation rate data and their absolute...
Synthetic mass accumulation rates have been calculated for ODP Site 707 using depth-density and depth-porosity functions to estimate values for these parameters with increasing... -
Organic carbon chemistry of ODP Hole 151-909C (Table 1)
Organic-rich sediments were recognized in early Miocene strata from the Norwegian-Greenland Sea during ODP Leg 151. Three organic-geochemical subunits were distinguished in Hole... -
(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... -
Linear sedimentation rates and mass accumulation rates of detritus and Kosa o...
In order to reconstruct past variations in the east Asian monsoon and to establish a direct link between terrestrial and marine climatic records, we evaluated the temporal... -
(Appendix A) Sedimentation rate, geochemical and environmental magnetic proxi...
The upper Tortonian Metochia marls on the island of Gavdos provide an ideal geological archive to trace variations in Aegean sediment supply as well as changes in the North... -
Osmium concentration and isotope composition of ODP Hole 165-1002C (Table 1)
A high resolution record of seawater osmium isotopic composition (35 samples over the past 191,000 yr) has been obtained from sediments from Ocean Drilling Program (ODP) Leg 165...