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P-wave velocity (PWS split-core system) on ODP Hole 160-964A
This dataset has no description
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P-wave velocity (PWS split-core system) on ODP Hole 160-963A
This dataset has no description
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Shear strength of ODP Hole 160-971A
This dataset has no description
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(Table 1) Revised and corrected composite depth sections of ODP Site 160-964
High-resolution color reflectance records of KC01 and KC01B (Calabrian Ridge, Ionian Sea) are presented and compared with a modified spliced high-resolution color reflectance... -
Downhole temperature in ODP Hole 160-971D
Sediment depth is given in mbsf. Temperature data not available. -
Downhole temperature in ODP Hole 160-970B
Sediment depth is given in mbsf. Temperature data not available. -
Downhole temperature in ODP Hole 160-969E
Sediment depth is given in mbsf. Temperature data not available. -
Downhole temperature in ODP Hole 160-969C
Sediment depth is given in mbsf. Temperature data not available. -
(Appendix) Carbon and nitrogen isotope ratios of ODP Site 160-964
Nitrogen isotopes of chlorins, degradation products of chlorophyll, reflect the isotopic composition of nutrient N utilized by marine phytoplankton communities. Here we show... -
(Table 1) Geochemistry of ODP Site 160-963 sediments
The Mediterranean Sea acts as a miniature ocean with the development of its own conveyor belt. It constitutes an ideal location to study and forecast how the marine environment... -
(Table 1) Geochemistry of Sapropels of the Mediterranean Sea
Sapropels -organic-matter rich layers- are common in Neogene sediments of the eastern Mediterranean Sea. The formation of these layers has been attributed to climate-related... -
(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 1) Porewater analysis with respect to gypsum from different ODP holes
The stability of gypsum in marine sediments has been investigated through the calculation of its saturation index at the sediment in situ temperature and pressure, using the... -
(Table 967ARMCD) Color reflectance data sets of Hole 160-967A
We have developed revised postcruise composite depth sections over the ~100-m-long, Pliocene-Holocene sediment sequences at four paleoceanographic sites (Site 964: Ionian Basin;... -
Concentrations of major and minor constituents of samples from the lower end ...
The pore water chemistry of mud volcanoes from the Olimpi Mud Volcano Field and the Anaximander Mountains in the eastern Mediterranean Sea have been studied for three major... -
Grain-size distribution, and calcium carbonate and organic carbon concentrati...
Grain size distributions of the <63 µm terrigenous fraction of closely spaced sediment samples were measured across an interrupted sapropel sequence at ODP Site 969 on the... -
Sedimentology and geochemical analyses of Pliocene to Holocene sediments of O...
A multiproxy geochemical study of nine sapropel layers from ODP Hole 964A, ODP Leg 160 in the eastern Mediterranean spanning the Pliocene-Holocene time interval provides new... -
Global shallow sediment diagenesis survey results based on all available IODP...
Global shallow sediment diagenesis survey results based on all available IODP sediment core images.
