作者: Hemmo Bosscher , Wolfgang Schlager
DOI: 10.1086/648228
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摘要: The growth potential of carbonate platforms, i.e., the maximum rate at which they can aggrade vertically, is difficult to assess. To estimate from conservative side and search for variations with time, we have compiled published accumulation rates Phanerozoic. Accumulation vary in a pattern, up 200 m/Ma or more (not corrected compaction) late Devonian, Permian, Triassic, Jurassic mid-Cretaceous, separated by intervals reduced (e.g., Carboniferous, early Cretaceous). most dramatic drop occurs Permo-Triassic boundary, after there no documented platform growth. This pattern resembles evolutionary rhythm bloom demise reefs reef-builders. observed (over $10^{6}-10^{7} yr$), probably imposed long-term relative sea level rise on passive margins, favorable site deve...