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Ice-rafted debris record in the Prydz Bay
Ice-rafted debris mass accumulation rates (IRD MAR) at a drill site on the Antarctic continental margin are investigated to evaluate the linkages between East Antarctic Ice... -
Organic matter C and N composition and N. pachyderma stable isotope ratios of...
We report the results of downhole stable isotopic (d13Corg [organic carbon] and d15N) and elemental measurements (total organic carbon [TOC], total nitrogen [TN], and... -
Sulphate and d34S in pore waters and δ¹³C, δ¹⁸O and mineral composition of ca...
Carbon and oxygen isotopic compositions of authigenic carbonate nodules or layers reflect the diagenetic conditions at the time of nodule growth. The shallowest samples of... -
Biostratigraphy, magnetostratigraphy, granulometry, isotopes and clay mineral...
During Ocean Drilling Program Leg 188 to Prydz Bay, East Antarctica, several of the shipboard scientists formed the High-Resolution Integrated Stratigraphy Committee (HiRISC).... -
P-wave velocities and applied bed thickness and velocity changes for syntheti...
Synthetic seismograms provide a crucial link between lithologic variations within a drill hole and reflectors on seismic profiles crossing the site. In essence, they provide a... -
Granulometry, biogenic silica content, magnetic susceptibility and bulk densi...
The Prydz Bay area is a key region for studying and understanding the history of the eastern Antarctic Continental Ice Sheet (O'Brien, Cooper, Richter, et al., 2001,... -
Calcium carbonate content, brightness and color reflectance of ODP Site 188-1...
We measured and analyzed near-ultraviolet/visible/near-infrared spectral data from core samples recovered from Ocean Drilling Program Sites 1165 (Wild Drift) and 1167 (Prydz... -
Diatom datums and abundance in ODP Hole 188-1165B and 188-1166A sediments
The biostratigraphic distribution and qualitative relative abundance of Quaternary-Pliocene diatoms from Ocean Drilling Program Leg 188, Sites 1165 (64.380°S, 67.219°E) and 1166... -
Palynology, source vegetation, environment and age of ODP Site 188-1166 sedim...
Twenty-three core catcher samples from Site 1166 (Hole 1166A) in Prydz Bay were analyzed for their palynomorph content, with the aims of determining the ages of the sequence... -
Dinoflagellate cyst and pollen/spore abundance and preservation of ODP Leg 18...
Sites 1165 and 1167 were drilled on the continental slope and rise seaward of Prydz Bay, East Antarctica. The sediments penetrated are glacigene and independently dated as... -
Distribution of foraminifera and other components in ODP Leg 188 sites
During Leg 188 of the Ocean Drilling Program (ODP), employing JOIDES Resolution, we drilled holes at three sites in the southern Indian Ocean in and near Prydz Bay, East... -
Geochemistry and age determination of zircons in Cretaceous to Quaternary sed...
In central Antarctica, drainage today and earlier back to the Paleozoic radiates from the Gamburtsev Subglacial Mountains (GSM). Proximal to the GSM past the Permian-Triassic... -
Clay mineralogy of ODP Site 188-1165
The Ocean Drilling Program Leg 188 Site 1165 was drilled on the Wild Drift on the Continental Rise off Prydz Bay, East Antarctica to a total depth of 999.1 meters below seafloor... -
Quantitative silicoflagellate data from the southern Indic Ocean from ODP Hol...
In the modern marine environment the silicoflagellate genus Dictyocha is rare, or absent, south of the Antarctic polar front (APF); the genus Distephanus, in contrast, is... -
P-wave velocity (PWS split-core system) on ODP Hole 188-1167A
This dataset has no description
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P-wave velocity (PWS split-core system) on ODP Hole 188-1166A
This dataset has no description
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P-wave velocity (PWS split-core system) on ODP Hole 188-1165C
This dataset has no description
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P-wave velocity (PWS split-core system) on ODP Hole 188-1165B
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Thermal conductivity of ODP Hole 188-1167A
This dataset has no description
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Thermal conductivity of ODP Hole 188-1166A
This dataset has no description