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seaweeds ( Knoll 1994 , Knoll & Golubic 1992 ). A job for micrometazoans in this initial decline is extra speculative, but the Ediacaran and Cambrian radiations of huge animals undoubtedly contributed to the further, terminal Proterozoic-Cambrian decline of stromatolites ( Awramik 1971 ). Additional support for the function of algae and animals in limiting stromatolite-building mat communities to restricted coastal environments comes from carbonates deposited within the immediate aftermath of mass extinctions.

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