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(Table 1) Spacing of diatom abundance index and opal index at ODP Site 175-1084
An important discovery during Ocean Drilling Program Leg 175, when investigating the record of upwelling off Namibia, was the finding of a distinct Late Pliocene diatom maximum... -
(Appendix 1) Age, Ge/Si ratio, aluminium and opal contents in ODP Sites 175-1...
As a result of both culture and sediment core studies, the ratio of germanium (Ge) to silicon (Si) in diatom shells has been proposed as a proxy for monitoring whole-ocean... -
Clay mineralogy of ODP Leg 103 sites (Table 1)
Samples from Cenozoic and Mesozoic sediments drilled during ODP Leg 103 were analyzed for clay mineralogy. Kaolinite, chlorite, illite, and smectite occur in most of the samples... -
Grain size analysis on Site 208-1262
This dataset has no description
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Grain size analysis on Site 208-1267
This dataset has no description
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Grain size analysis on Site 208-1266
This dataset has no description
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Grain size analysis on ODP Hole 208-1265A
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Concentrations of trace elements and stable carbon and oxygen isotope record ...
Trace element contents (Sr, Mg, Mn, and Fe) and the composition of oxygen and carbon isotopes show that late burial diagenesis did not play an important role in pelagic... -
Age models, stable isotope record, and physical properties of ODP Hole 154-926B
We extend existing high-resolution Oligocene–Miocene proxy records from Ocean Drilling Program (ODP) Leg 154. The extended record spans the time interval from ~17.86 to 26.5... -
Age determination of sediment core NP90-52 (Table 1)
Data on glacial erosion have been compiled and synthesised using a wide range of sediment budget and sediment yield studies from the Svalbard-Barents Sea region. The data... -
Physical-property data of turbidites and periplatform ooze of ODP Leg 101 hol...
Along the slopes and in adjacent basinal areas of Bahamian platforms, periplatform ooze forms the host sediment for variable proportions of carbonate turbidites. In unlithified... -
Age determination of ODP Hole 108-658C (Table 1)
A detailed (ca. 100 yr resolution) and well-dated (18 AMS 14C dates to 23 cal. ka BP) record of latest Pleistocene–Holocene variations in terrigenous (eolian) sediment... -
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.... -
U and Th concentrations and U-TH ages for bulk carbonate samples from ODP Hol...
Thirty-one new bulk-sediment U–Th dates are presented, together with an improved d18O stratigraphy, for ODP Site 1008A on the slopes of the Bahamas Banks. These ages supplement... -
Isotopic measurements of 3 foraminifer species from ODP Hole 171-1050C
Analysis of 944 single specimens of three species of late Maastrichtian planktonic foraminifera (Racemiguembelina fructicosa, Contusotruncana contusa, and Rugoglobigerina... -
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... -
Geochemical measurements of the Tasmanian Gateway from ODP Hole 189-1172A
Tectonic changes that produced a deep Tasmanian Gateway between Australia and Antarctica are widely invoked as the major mechanism for Antarctic cryosphere growth and Antarctic... -
(Table 1) Age determination of ODP Leg 166 holes
Thick, late Quaternary sediment sections were recovered at several sites on the leeward slope of Great Bahama Bank during Leg 166 of the Ocean Drilling Program. These sections... -
(Table 1) Facies classification for ODP Site 174-1072
Commonly accepted models for the evolution of continental margins link sediment erosion, transport and deposition to eustasy. To test these models, we constructed an oxygen... -
Neodymium isotopic ratios and clay mineral composition from ODP Hole 1147A an...
Ocean Drilling Program sampling of the distal passive margin of South China at Sites 1147 and 1148 has yielded clay-rich hemipelagic sediments dating to 32 Ma (Oligocene), just...
