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Abstract The deep continental biosphere hosts microbial communities employing ancient metabolisms such as methanogenesis. Yet, it is one of Earth’s least explored ecosystems with its long-term history remaining poorly constrained.
Stable C, O and clumped isotope systematics and 14C geochronology of carbonates from the Quaternary Chewaucan closed-basin lake system, Great Basin, USA: Implications for paleoenvironmental reconstructions using carbonates Geochimica et Cosmochimica Acta By: Adam Hudson, Jay Quade, Guleed Ali, Douglas P. Boyle, Scott Bassett, Katharine W. Huntington, Marie G. De los Santos, Andrew S.
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