Return of the coral reef hypothesis
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Differences in the rate of coral reef carbonate deposition from the Pleistocene to the Holocene may account for the Quaternary variation of atmospheric CO 2 . Sea-level change shifts the locus of carbonate deposition from the deep sea to the shelves as the normal glacial-interglacial pattern of deposition for Quaternary global carbonates. To assess the impact of these changes on atmospheric CO 2 , a simple numerical simulation of the global carbon cycle was developed. -from Authors
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Geology