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- W1460528305 abstract "This chapter discusses the carbonate turnover and deposition by metazoa. Although there are potentially a large number of carbonate minerals that might be formed by metazoan, the only important ones are the polymorphic forms of calcium carbonate: high and low magnesian calcites, aragonite, and much less commonly, vaterite. The occurrence of calcium carbonate as the major mineral of invertebrate skeletons has two important consequences for the relationship of biogenic mineralization to inorganic processes of the environment. The first concerns natural cycles. The second effect of metazoa on inorganic processes of the environment relates to their capacity for rapid deposition of calcium carbonate as compared to inorganic precipitation in natural waters. This comparison between inorganic processes and the more complex systems found in organisms serve as a framework in the discussion of biological mineralization. The coelenterates playing a major role in marine carbonate deposition include the Hydrozoa, specifically the Stylasterina and Milleporina, the Octocorallia and the Scleractinia (Zooantharia)." @default.
- W1460528305 created "2016-06-24" @default.
- W1460528305 creator A5034353823 @default.
- W1460528305 creator A5081934457 @default.
- W1460528305 date "1979-01-01" @default.
- W1460528305 modified "2023-09-24" @default.
- W1460528305 title "Chapter 2.3 Carbonate Turnover and Deposition by Metazoa" @default.
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