Some features of the evolution of carbonate accumulation in the earth’s history: Communication 1. Evolution of the intensity, mechanism, and setting of carbonate accumulation |
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Authors: | V G Kuznetsov |
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Institution: | (1) Institute of Oil and Gas Problems, Russian Academy of Sciences, Leninskii pr. 65, 117917 Moscow, Russia |
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Abstract: | Marine and oceanic carbonate accumulation during the Vendian-Cambrian was mostly controlled by the life activity of organisms,
which either constructed skeletons and directly transferred carbonates into sediments or created geochemical environments
favorable for the precipitation of the carbonate substance. During the first third of the Paleozoic, the chemogenic and biochemogenic
mechanisms of limestone formation were replaced by the biogenic one. In the dolomite formation, to the contrary, the chemogenic
mechanism progressively replaced the biochemogenic mechanism and its pseudobiogenic modification. The carbonate accumulation
occurred in the cyclic mode and its intensity increased with time to reach its peak in the Late Cretaceous. The main paleogeographic
domains of carbonate accumulation also experienced changes. They were mainly represented by spacious shelf seas in the Paleozoic;
by intraoceanic shoals, reefs and pelagic realm in the Mesozoic; and by the pelagic realm and, to a lesser extent, reefs in
the main Cenozoic. |
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