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Abstract

The timing and nature of changes in the chemistry of the early oceans are intensely debated. Geochemical analyses show that a prominent transition to sulphidic marine conditions 1.8 billion years ago may have been restricted to near-shore environments.

Original languageEnglish
Pages (from-to)453-454
Number of pages2
JournalNature Geoscience
Volume3
Issue number7
DOIs
StatePublished - Jul 2010

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