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Local and Global Controls on Carbon Isotope Chemostratigraphy

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Over million-year timescales, the geologic cycling of carbon controls long- term climate and the oxidation of Earth's surface. Inferences about the carbon cycle can be made from time series of carbon isotopic ratios measured from sedimentary rocks.

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Local and Global Controls on Carbon Isotope Chemostratigraphy, Anne-Sofie Ahm, Jon Husson

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2022
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