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Mineralogical composition of tested samples measured by X-Ray diffraction (XR...
This dataset has no description
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Rate- and state friction (RSF) parameters obtained from inverse modelling of ...
This dataset has no description
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(Appendix 2) Stable carbon and hydrogen data of different desoprtion methods
w.m.: values are given as weighted mean of seperate aliquots extracted over time, n.m.: not measured, n.d.: not detected / hydrocarbon gases were extracted using hot solution of... -
(Appendix 1) Stable carbon and hydrogen data of different settings
w.m.: values are given as weighted mean of seperate aliquots extracted over time, n.m.: not measured, n.d.: not detected, Depth, sediment=mbsf: meter below seafloor -
(Appendix 7) Tabulated data of hydrocarbon gases from different oceanographic...
n.m.: not measured, n.d.: not detected, Depth, sediment=meter below seafloor -
(Appendix 7) Tabulated data of hydrocarbon gases from different oceanographic...
n.m.: not measured, n.d.: not detected, Depth, sediment=meter below seafloor -
(Appendix 1-4) Geochemistry, desorption methods, TOC, TC, and mineral content...
Sorption of volatile hydrocarbon gases (VHCs) to marine sediments is a recognized phenomenon that has been investigated in the context of petroleum exploration. However, little... -
Studies of the microbial diversity on analyzed samples from from Peru Margin,...
Marine sediments harbor an enormous quantity of microorganisms, including a multitude of novel species. The habitable zone of the marine sediment column begins at the... -
Methane concentration and porewater acetate of sediment cores from the IODP E...
In deep subsurface sediments of the Juan de Fuca Ridge Flank, porewater acetate that is depleted in 13C relative to sedimentary organic matter indicates an acetogenic component... -
(Table 3) Concentrations and relative proportions of PLFAs and bacterial IPLs
This dataset has no description
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(Table 1) Geochemical parameters of analyzed samples from from Peru Margin, E...
This dataset has no description
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Dipicolinic acid concentration in sediment samples
Marine sediments host an unexpectedly large microbial biosphere, suggesting unique microbial mechanisms for surviving burial and slow metabolic turnover. Although dormancy is... -
(Table 4) Multiple sulfur isotope compositions for altered basalt and glass s...
This dataset has no description
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Porewater acetate concentrations of sediment cores from IODP Expedition 301 S...
BD = below detection limit, ND = not determined -
Methane concentrations and carbon isotopic compositions of methane in sedimen...
BD = below detection limit, ND = not determinedFor CH4 see also doi:10.2204/iodp.proc.301.106.2005 -
(Table S2) Relative abundance of archaeal 16S rRNA genes in sediment cores
Deep drilling into the marine sea floor has uncovered a vast sedimentary ecosystem of microbial cells (Parkes et al., 1994, doi:10.1038/371410a0; D'Hondt et al., 2004,... -
(Table 1) Heavy minerals in silt and sand samples of IODP Site 301-U1301
The northwestern Cascadia Basin of western North America accumulated high-sedimentation-rate sequences during the Pleistocene sea-level low-stands. The continental shelf was... -
Cohesion coefficients, coefficients of peak friction, and coefficients of sli...
This dataset has no description
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(Table S9) Isotopic composition of IODP Hole 301-U1301B
Sediment-covered basalt on the flanks of mid-ocean ridges constitutes most of Earth's oceanic crust, but the composition and metabolic function of its microbial ecosystem are...
