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Microorganisms in the Zone of Submarine Volcanic Eruptions at 535-513 Ma
Diamond and Precious Metals Geology Institute, SB RAS, Yakutsk, Russia
Diamond and Precious Metals Geology Institute, SB RAS, Yakutsk, Russia
- 1 Diamond and Precious Metals Geology Institute, SB RAS, Yakutsk, Russia
- 2 Diamond and Precious Metals Geology Institute, SB RAS, Yakutsk, Russia
American Journal of Plant Sciences·Volume 05 (2014)·Pages 2464–2471·Published 4 July 2014·DOI10.4236/ajps.2014.515261
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Abstract
New anatomical features revealed in some Early Cambrian calcareous microfossils suggest comparison with Rhodophyta (red algae), which makes it possible to define their taxonomic position. A taxonomically rich Early Cambrian paleobiocoenosis has been discovered in northern Tien Shan, which exemplifies the existence on earth at 535-513 Ma (million years) of morphologically complex fungiform microorganisms and red algae in a shallow-water biotope where environmental conditions favorable for life were created as a result of submarine volcanic eruptions.
KeywordsCalcareous MicrofossilTetrasporeTetrasporangiumRhodophytaCambrianVolcanicityPaleobiocoenosisTien Shan
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