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Age model of sediment core Q859
This dataset has no description
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(Table 2) Duration of the polarity change process at DSDP Holes 72-515A and 7...
A study has been made of downhole declination changes of the horizontal component of the natural remanent magnetization of unopened whole-core sections recovered by use of the... -
(Table 1) Magnetostratigraphy and sedimentation rates of the K/T boundary int...
The results of two separate magnetic investigations are discussed in this paper. The first study produced a magnetostratigraphy from the K/T boundary interval of Hole 1001A from... -
(Table A) Radiocarbon datings and sedimentation rates of bottom sediments fro...
1-4 - speciation forms: 1 - bound with CaCO3 and sorbed; 2 - bound with hydroxides of Fe and Mn; 3 - bound with organic matter and sulfides; 4 - bound with lithogenic matter; 5... -
(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... -
(Table 3) Sedimentation rates of stage 1 and last glacial maximum from differ...
Within the Scotia Sea, the axis of the Antarctic Circumpolar Current (ACC) is geographically confined, and sediments therefore contain a record of palaeo-flow speed... -
(Table 1) Sapropel analysis from ODP Sites 160-964, 160-966, 160-967 and 160-969
Seventeen eastern Mediterranean Pliocene sapropels from ODP Sites 964, 966, 967 and 969, some of which are coeval, have been analysed for their geochemistry. The sapropels are... -
(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... -
Linear sedimentation rates of ODP Hole 68-503B and sediment core KK75-02 (Tab...
The mass accumulation rate and grain size of the total colian component isolated from pelagic sediment in two North Pacific cores, piston core KK75-02 under the prevailing... -
(Table 2-3) Radiocarbon datings of organic matter from sediments of Core PSh-...
Core PSh-2510 (4.76 m long) recovered mud and clay of the Baltic Ice Lake and of all subsequent stages of the Baltic Sea. Grain size, mineral and chemical compositions, as well... -
(Table 1) Thickness of the Holocene layer and sedimentation rates in the Atla...
On the basis of planktonic foraminifera study, thickness of Holocene sediments has been ascertained in 60 sediment cores from various regions of the Atlantic Ocean. Ratios of... -
Milankovitch frequency peaks of ODP Site 113-693 (Table 3)
The first well logs collected below the Antarctic circle were obtained during Leg 113 at Site 693 on the Dronning Maud Land Margin (Antarctica) in the Weddell Sea. Gamma-ray,... -
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... -
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... -
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...
