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Dynamic sulfur and carbon cycling through the end-Ordovician extinction revealed by paired sulfate–pyrite δ34S

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Could land‐based early photosynthesizing ecosystems have bioengineered the planet in mid‐Palaeozoic times?

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Controlling Factors on Organic Matter Accumulation of Marine Shale across the Ordovician-Silurian Transition in South China: Constraints from Trace-Element Geochemistry

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Untitled work

(2004) · doi:10.1130/1052-5173(2004)014<4:caapdo>2.0.co;2