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Bulk sedimentology of core GIK16992-1
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Sediment physics of core GIK16990-2 (Sonne 94-36), New Ireland Basin, Papua N...
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Sediment physics of box core GIK16990-1 (Sonne 94-35), New Ireland Basin, Pap...
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Sediment physics of box core GIK16989-2 (Sonne 94-32) New Irland Basin, Papua...
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Sediment physics of box core GIK 16989-1 (Sonne 94-31) New Irland Basin, Papu...
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Sediment physical parameters of box core GIK16994-2 (Sonne 94-75), sited betw...
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Sediment physical parameters of box core GIK16994-1 (Sonne 94-74), sited betw...
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Sediment physics of box core GIK16993-2 eastnortheast of Simbira Island, New ...
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Ostracode relative abundances and geochemistry in surface sediments from Lake...
Understanding the ecology of bioindicators such as ostracods is essential in order to reconstruct past environmental and climate change from analysis of fossil assemblages... -
Sediment physics of box core GIK16986-1 New Irland Basin, Papua New Guinea
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Sand fraction, organic carbon and nitrogen data, and calculated marine and te...
There is generally a lack of knowledge on how marine organic carbon accumulation is linked to vertical export and primary productivity patterns. In this study, a multi-proxy... -
(Table 1) Globigerinoides sacculifer oxygen and carbon isotopes at DSDP Site ...
The oxygen and carbon isotopic record of G. sacculifer in DSDP Holes 502 and 502B shows that the Quaternary interval is almost complete. A slight hiatus exists in the upper... -
(Table 1) CaCO3 content, grain size, and dissolution faces at DSDP Leg 73 Holes
The dissolution fades of 68 sediment samples from Leg 73 were determined by analyzing carbonate content and grain size. All sediments (Miocene to Pleistocene) from Site 519 and... -
(Table 1) Sediment characteristics at DSDP Hole 75-532A
Orientation and geometry of pores as well as sediment compressibility can be approximated by determining the shrinkage behavior of standardized samples. The sections... -
(Table 1) Proportions of clay minerals and mud, as well as description of sed...
The clay mineralogy of Lower Cretaceous deep-sea fan sediment in the western North Atlantic is dominated by smectite in most intervals, and by illite in samples from intervals... -
(Table T1) Granulometry of sediments from ODP Leg 168 sites
Sedimentary deposits of Cascadia Basin lap onto the Juan de Fuca Ridge to within 20 km of the spreading axis (Davis and Currie, 1993, doi:10.1139/e93-023). Collectively, these... -
(Table T1) Carbon geochemistry and coarse fraction content of ODP Sites 184-1...
The goal during Ocean Drilling Program Leg 184 was to reconstruct the long-term paleoenvironmental variability of the South China Sea (SCS) and the adjacent Asian continent. In... -
(Table 1) Population density and biomass of the foraminifer Rupertina, and gr...
Rupertina stabilis occupies a depth restricted biotope of suspension feeding animals situated at the Norwegian continental margin. It extends from the Voring plateau northwards... -
(Table T3) Granulometry of sediments from ODP Leg 190 sites
We present the results of grain-size analysis performed on hemipelagic sediment from Sites 1173, 1174, 1175, and 1177 at the Nankai Trough. Analyses of the <63-µm fraction... -
Median grain size and distribution of sand in ODP Hole 108-660A (Fig. 5)
50 m of Middle Eocene pure radiolarian ooze were drilled at ODP Site 660 in the equatorial East Atlantic, 80 km northeast of the Kane Gap. The oozes comprise a 10 m high and 2...