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Phanerozoic Cycling of Sedimentary Carbonates

SEDIMENTARY CARBONATES IN THE EVOLUTION OF EARTH S SURFACE ENVIRONMENT [Pg.578]

In contrast to the total sedimentary carbonate mass, oceanic carbonate oozes have a decay constant of 0.02 ma 1, about 10 times that of the global carbonate mass. The pelagic oozes compose about 8% of the global sedimentary carbonate mass but presently account for about 60% of carbonate deposition. [Pg.578]

Synopsis of the origin and evolution of the hydrosphere-atmosphere-sedimentary lithosphere [Pg.582]

Garrels R.M. and Lerman A. (1981) Phanerozoic cycles of sedimentary carbon and sulfur. National Academy of Sciences Proceedings 78,4652-4656. [Pg.630]

Wilkinson, B. H. Walker, J. C. G. 1989. Phanerozoic cycling of sedimentary carbonate. American Journal of Science, 289, 525-548. [Pg.257]

No remarkable alterations were shown in carbon and sulfur cycles or in atmospheric oxygen concentrations since the Latest Proterozoic. The coupling of carbon and sulfur biogeochemical cycles is supported by systematic covariations in the isotopic records of sedimentary rocks over Phanerozoic time. [Pg.57]

See other pages where Phanerozoic Cycling of Sedimentary Carbonates is mentioned: [Pg.225]    [Pg.577]    [Pg.677]    [Pg.225]    [Pg.577]    [Pg.677]    [Pg.577]    [Pg.578]    [Pg.516]    [Pg.565]    [Pg.571]    [Pg.580]    [Pg.582]    [Pg.3969]    [Pg.4395]    [Pg.4406]    [Pg.4410]    [Pg.56]    [Pg.261]    [Pg.228]    [Pg.530]    [Pg.551]   


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Phanerozoic

Phanerozoic carbonates

Sedimentary cycle

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