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(Table 3) Chlorine stable isotope ratios of water-soluble (WSC) and structura...
Fractionation was determined using the average value where several values are presented. -
(Table 3) Noble gas composition of dissociated gas hydrate specimens from ODP...
Fractionation of the noble gases should occur during formation of a Structure I gas hydrate from water and CH4 such that CH4 hydrate is greatly enriched in Xenon. Noble gas... -
(Table 1) Stable oxygen isotope ratios of clinoptilolites from ODP Hole 127-797B
For d18O data of pore water see Brumsack et al. (1992) dataset: doi:10.1594/PANGAEA.711476 -
(Table 1) Stable oxygen isotope ratios of clinoptilolites from ODP Site 122-762
This dataset has no description
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(Table 3) Chlorine stable isotope ratios of water-soluble (WSC) and structura...
Fractionation was determined using the average value where several values are presented. -
(Table 3) Chlorine stable isotope ratios of water-soluble (WSC) and structura...
Fractionation was determined using the average value where several values are presented. -
(Table 3) Chlorine stable isotope ratios of water-soluble (WSC) and structura...
Fractionation was determined using the average value where several values are presented. -
(Table 3) Chlorine stable isotope ratios of water-soluble (WSC) and structura...
Fractionation was determined using the average value where several values are presented. -
Hydrogen isotope fractions of long-chain alkenones produced by Emiliania huxl...
Over the last decade, hydrogen isotopes of long-chain alkenones have been shown to be a promising proxy for reconstructing paleo sea surface salinity due to a strong hydrogen... -
The effects of growth phase and salinity on the hydrogen isotopic composition...
The isotopic fractionation of hydrogen during the biosynthesis of alkenones produced by marine haptophyte algae has been shown to depend on salinity and, as such, the hydrogen...
