Modelled deep-sea carbonate sediment thickness since 120 million years ago. Subduction zones (black hatched lines), other plate boundaries (black lines), shallow-water carbonate platforms from Kiessling et al. (2003) (magenta), and paleo- coastlines (white outlines) on continents (gray) are shown. Cool-water carbonates are not included.

Reference: Dutkiewicz, A., Müller, R.D., Cannon, J., Vaughan, S. and Zahirovic, S., 2019, Sequestration and subduction of deep-sea carbonate in the global ocean since the Early Cretaceous, Geology, [ Ссылка ]

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