Neogene geochemical cycles: implications concerning phosphogenesis

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Abstract

Notable changes in continental weathering rates, depositional settings for sediments, and global climate are indicated by the isotopic records of strontium and oxygen and the eustatic sea-level curve for the Neogene, and support the notion that the Neogene was the culmination of a number of important Tertiary trends in global geochemical cycling. -from Author

Original languageEnglish (US)
Pages (from-to)273-282
Number of pages10
JournalUnknown Journal
StatePublished - Jan 1 1990

All Science Journal Classification (ASJC) codes

  • General Environmental Science
  • General Earth and Planetary Sciences

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