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(Table 2) Terrigenous, authigenic and biogenic composition of sediments at DS...
Pelagic sedimentation during the Early Cretaceous at Site 603 produced alternations of laminated marly limestone and bioturbated limestone--a facies typical of the "Blake-Bahama... -
(Table 1) Ages of planktonic foraminiferal datums at Leg 94 Sites
The six Leg 94 sites have produced a unique data set from a north-south transect of sites, all with good paleomagnetic records, and all but one with above-average accumulation... -
Planktonic foraminifera and microfossil composition of IODP Hole 302-M0004C
Calcareous microfossils are widely used by paleoceanographers to investigate past sea-surface hydrology. Among these microfossils, planktonic foraminifera are probably the most... -
Core-section summary from IODP Hole 317-U1353B
This dataset has no description
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(Table 1) Summary of maximum clast size and bed thickness of ODP Leg 126 samples
Subaerial debris flows, with water contents ranging from as little as 10 wt% up to no more than about 25 wt% (Pierson, 1986; Pierson and Costa, 1987), are non-Newtonian fluids... -
Geochemical analyses of chert nodules and beds from deep-sea sediments (Table 1)
Concentrations of Fe, Mg, Ca, Sr, Mn, Zn, and other heavy metals were analyzed by atomic absorption spectrometry in 27 chert samples from the Pacific deep sea, 17 chert samples... -
(Table 1) Age and depth of reflectors of the 3.5-kHz and airgun seismic recor...
DSDP cores from areas of low (Site 505) and high heat flow (Site 504 B) near the Costa Rica Rift, together with seismic profiles from the Panama Basin, have been studied to... -
Geotechnical and physical properties from whole-round consolidations samples ...
Sediments cored from the Barbados Ridge accretionary complex at ODP Sites 671, 672, and 676 are progressively underconsolidated with depth. Very low measured intergranular... -
Age determination of ODP Site 165-1002
An expanded Cariaco Basin 14C chronology is tied to 230Th-dated Hulu Cave speleothem records in order to provide detailed marine-based 14C calibration for the past 50,000 years.... -
(Table 1) Element enrichment in dark versus light layers of the ''Zebra'' int...
Analysis focuses on the upper part of subunit 1/6, subunit 1/5, and the lower part of subunit 1/4 (cores M0002A-47X 3W to M0002A-44X 1W) extending from 203.70 to 191.99 mcd. -
Trace element composition of IODP Site 304-U1309 and 305-U1309 (Table A2)
IODP Site U1309 was drilled at Atlantis Massif, an oceanic core complex, at 30°N on the Mid-Atlantic Ridge (MAR). We present the results of a bulk rock geochemical study (major... -
Spacing and amplitude of IR temperature anomalies and hydrate content of sedi...
Large uncertainties about the energy resource potential and role in global climate change of gas hydrates result from uncertainty about how much hydrate is contained in marine... -
Particel size distribution and microstructures of sediments from ODP Leg 205 ...
Ocean Drilling Program Legs 170 and 205 offshore Costa Rica provide structural observations which support a new model for the geometry and deformation response to the seismic... -
Occurrence of tethyan radiolarian species in early Cretaceous sediments of OD...
During ODP Leg 123, abundant and well-preserved Neocomian radiolarians were recovered at Site 765 (Argo Abyssal Plain) and Site 766 (lower Exmouth Plateau). Assemblages are... -
(Appendix I) Stable isotope measurements of benthic and planktonic foraminife...
Isotopic analysis was performed at the Leibniz-Laboratory for radiometric dating and stable isotope research at Christian-Albrechts-University Kiel, Germany using a Finnigan MAT... -
Stable water isotope data from ice wedges at Mamontovy Khayata
This dataset has no description
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Stable water isotope data from snow patches
This dataset has no description
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Stable water isotope data from ice wedges at Kurungnakh
This dataset has no description
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Stable water isotope data from ice wedges at Nagym
This dataset has no description
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(Table 2h) Planktic and benthic 14C and 14C reservoir ages of sediment core M...
All 14C dates are rounded to decades. Planktic plateau boundaries were either defined at or in between single 14C ages of the records. For reasons of specimen availability...
