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Sedimentary bulk organic matter and various molecular organic components exhibit strong CO2-dependent carbon isotope fractionation relative to dissolved inorganic carbon sources. This fractionation (εp) has been employed as proxy for paleo-pCO2. Yet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::739b70a52acb6c1387fb5cc5fd310654
https://bg.copernicus.org/preprints/bg-2022-118/
https://bg.copernicus.org/preprints/bg-2022-118/