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Global and regional controls on marine redox changes across the Ordovician-Silurian boundary in South China
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文摘

Comparative Fe-S-C study was conducted on O-S transitional strata in South China.

Strong spatial heterogeneity of oceanic redox evolution was observed between sites.

Large perturbation of the carbon and sulfur cycle was observed for study sections.

A dual-control involving Hirnantian glaciation and Kwangsian Orogeny is proposed.

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