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The evolution of the marine carbonate factory - Nature

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The evolution of the marine carbonate factory - Nature

Calcium carbonate formation is the primary pathway by which carbon is returned from the ocean–atmosphere system to the solid Earth1,2. The removal of dissolved inorganic carbon from seawater by precipitation of carbonate minerals—the marine carbonate factory—plays a critical role in shaping marine biogeochemical cycling1,2. A paucity of empirical constraints has led to widely divergent views on how the marine carbonate factory has changed over time3–5.

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The evolution of the marine carbonate factory - Nature

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The evolution of the marine carbonate factory - Nature

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