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By Maurice E. Tucker

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Published by means of the yank Geophysical Union as a part of the Short classes in Geology Series.

This quantity assumes a basic wisdom of carbonate mineralogy in addition to a familiarity with the final rules of sedimentology and specializes in particular types of carbonate deposition and diagenesis. the final precept of uniformity of approach is principally broadly utilized in carbonate sedimentology. The editors therefore concentration first on versions in keeping with smooth settings. the appliance of those versions to historic carbonates completes the amount.


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1974, Reefs, platforms, and basins of Cretaceous in northeast Association of Petroleum 58, p. 800-809. G. F. frameworks' Sohl, Antillean Mexico' Geologists 1974, Cretaceous Verhandl. Naturi. American v. , geology, of References Ginsburg, State University, p. 131-173. , 1972, Paleoecologie des formations rudistes du Cretace Superior-lVexample du sud-est de la France' Palcogeography, Paleoclimatology, Palcoecology, v. 12, p. C. the lithification Sedimentology, v. 84, p. 399-467. G. 194-216. , 1979, Miocene bioherms and associated structures in the Upper Coralline rudist Ges.

A. 111-135. Pitcher, Publication Sedimentology, v. 17, p. 173-219. eontologica Polonica, v. 25, p. 655-668. P. R. , 1971, The conditions of growth of the Wenlock reefs of Shropshire, England' (reefs), Petroleum A western Geology, Canada: v. Bulletin of Canadian 28, p. 315-344. W. and R. Riding, 1981, Foreslope Renalcis-stromatoporoid 38 Copyright American Geophysical Union bioherm with evidence of Short Courses in Geology Carbonate Sedimentology and Petrology Vol. 4 JAMES early cementation, Devonian Ancient Wall reef complex' Sedimentology, v.

Reef-associatedorganisms were especially hard hit; stromatoporoids werereduced to a few genera; rugose corals were almost totally wiped out; tabulate corals disappeared; brachiopods were decimated and although they recovered, were never again as diverse (McLaren, 1982). The ecosystem of skeletal metazoans that had built the extensive middle Paleozoic reefs was gone. Late Paleozoic - Early Mesozoic Reef Mounds The early Mississippian has few if any "reef-building" taxa; the place of corals and stromatoporoids is taken by pelmatozoans and bryozoans.

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