Disentangling the record of diagenesis, local redox conditions, and global seawater chemistry during the latest Ordovician glaciation
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文摘
Persistent local deep water anoxia through the latest Ordovician. Intense modern weathering processes significantly affect Fe and S chemistry in outcrop samples. Ordovician glacio-eustasy drove spatial gradients in δ13CDIC decoupled from the open ocean.

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