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pro vyhledávání: '"Sean Gazdewich"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 3, Pp n/a-n/a (2024)
Abstract Stable carbon isotope ratios (δ13C values) of marine carbonates are widely used to infer the relative burial rates of organic carbon, a source of oxygen to the ocean‐atmosphere system. This inference, however, is based on the assumption t
Externí odkaz:
https://doaj.org/article/e198ee63f1774b84939d6602ff7f06e5
