Comparisons between the oxygen isotopic composition of pore water and Globigerinoides ruber in sediments from Hole 817C

Research output: Contribution to journalArticle

2 Scopus citations

Abstract

The variations in the δ18O may reflect original variations in the waters, the magnitude of which has been subsequently reduced by process of diffusion. Second, these may reflect recrystallization of the precursor sediment and isotopic exchange between the fluids and the recrystallized sediment. The correlation between the Cl- and the δ18O data may suggest that these values reflect the original composition modified by diffusion. -from Author

Original languageEnglish (US)
Pages (from-to)481-487
Number of pages7
JournalUnknown Journal
DOIs
StatePublished - 1993
Externally publishedYes

ASJC Scopus subject areas

  • Environmental Science(all)
  • Earth and Planetary Sciences(all)

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