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Paleoecology of Cambrian Reef Ecosystems

Chapter
Part of the Topics in Geobiology book series (TGBI, volume 17)

Abstract

Modern tropical reefs, together with tropical rain forests, comprise the principal centers of biodiversity. The tropical rain forest, however, is a relatively fresh phenomenon in a geological time sense. Therefore, to estimate ancient biodiversity, we first of all look to fossil reefs. Mutual intergrowths as well as processes of marine lithification and minor diagenetic alternation allow us to study many aspects of interaction between organisms in long-ago vanished ecosystems, which are poorly preserved in other settings. All these turn fossil reefs into highly attractive areas for scientific exploration. Cambrian reefs, which formed between 545 Ma and 490 Ma, are especially interesting among fossil reefs because they retain their history. They recall the blooming and are a testament to the failure of the earliest metazoan reef ecosystem.

Keywords

Coral Reef Mass Extinction Siberian Platform Lower Cambrian Reef Community 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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© Academic/Plenum Publishers, New York 2001

Authors and Affiliations

  1. 1.Paleontological InstituteAcademy of Russian SciencesMoscowRussia

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