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Examples
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Delineating primary and secondary organic carbon in neoproterozoic glacial sediments
innovations-report 2010
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Actually, I think organic carbon burial to rock is about 20\% of the total geologic sequestration of C - typically, with large excursions in the paleoproterozoic and neoproterozoic (in between, it is thought that as the surface and atmospheric environments became oxic, the deep ocean remained anoxic and became sulfidic, due to changes in the sulfur cycle caused by changes in the oxygen cycle due to the increasing atmospheric oxygen levels).
RealClimate 2009
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