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Triple oxygen and multiple sulfur isotope constraints on the evolution of the post-Marinoan sulfur cycle
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文摘

We present new Δ17O and coeval 33,34,36S data of Neoproterozoic aged barite from NW Canada.

Through a dynamic 1-box model we demonstrate the sulfate source to global barites was global seawater.

Results suggest a diminished marine sulfate reservoir in the aftermath of the Marinoan glaciation.

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