Local and Global Controls on Carbon Isotope Chemostratigraphy - Ahm, Anne-Sofie (Princeton University, New Jersey); Husson, Jon (University of Victoria, British Columbia)
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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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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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