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• W1587412370 endingPage "680" @default.
• W1587412370 startingPage "669" @default.
• W1587412370 abstract "The unusual isotopic characteristics of the Lomagundi carbonates led Schidlowski and others (1976) to resample the Lomagundi Group for a new detailed study. They analyzed 67 dolomite samples, that yielded a mean δ13C of 8.2%. In addition, they demonstrated that the Lomagundi carbonates were well preserved and had most probably retained their primary carbon isotope compositions. Motivated by problems in applying a global carbon cycle model to explain the observed record, the authors changed their earlier view and suggested a local unusual sedimentary environment as the cause of the enrichment of heavy carbon isotopes in the Lomagundi carbonates. The notion of local conditions as the cause of the enrichment in 13C was challenged when new Paleoproterozoic carbonate successions with 13C-enriched carbon isotope signatures were found locally in Norway." @default.
• W1587412370 created "2016-06-24" @default.
• W1587412370 creator A5088271461 @default.
• W1587412370 date "2005-01-01" @default.
• W1587412370 modified "2023-10-14" @default.
• W1587412370 title "Chapter 16 Paleoppoterozoc carbonisotope excursion" @default.
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• W1587412370 doi "https://doi.org/10.1016/s0166-2635(05)80017-9" @default.
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