Mackinawite and greigite in ancient alkaline hydrothermal chimneys: Identifying potential key catalysts for emergent life
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We use Raman Spectroscopy to study ancient hydrothermal iron sulfide formation <100 °C.

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We show hydrothermal formation of mackinawite and greigite iron sulfide phases.

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Greigite is observed at 70&ndash;75 °C under anoxic conditions.

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We suggest a FeIII-mackinawite intermediate in the mackinawite&ndash;greigite transition.

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Mackinawite is suggested as the dominant catalyst in ancient pre-biotic chemistry.

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