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The Fossil Record of Cyanobacteria

  • J. William Schopf
Chapter

Summary

Fossil evidence of cyanobacteria, represented in the geological record by microbially laminated stromatolites, cyanobacterial and cyanobacterium-like microscopic fossils, and carbon isotopic data consistent with the presence of Rubisco-mediated CO2-fixation, extends back to ∼3,500 million years ago. The most abundant and best-documented fossil cyanobacteria, known from thousands of specimens preserved in several hundred geological units, belong to five taxonomic families: the Oscillatoriaceae, Nostocaceae, Chroococcaceae, Entophysalidaceae and Pleurocapsaceae. As documented by the essentially identical morphologies, life cycles, and ecologic settings of such fossils and their modern counterparts, members of these families have exhibited extreme evolutionary stasis over enormous segments of geological time. Because of the incompleteness of the fossil record, however, such data do not resolve the time of origin of O2-producing cyanobacteria from their anoxygenic, bacterial, evolutionary precursors. Though it is well established that Earth’s ecosystem has included autotrophs since its very early stages, available data indicate only that O2-producing photoautotrophic cyanobacteria originated earlier than the Great Oxidation Event at ∼2,450 million years ago; that such microbes were evidently extant by ∼2,700 million years ago; and that the origin of oxygenic photosynthesis may date from as early as, or even earlier than, 3,500 million years ago.

Keywords

Fossil Record Carbon Isotopic Composition Oxygenic Photosynthesis Carbonaceous Matter Rock Record 
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.

Abbreviations

BIF

banded iron-formation

CLSM

confocal laser scanning microscopy

GOE

Grand Oxidation Event

Ma

million years

NMR

solid-state 13C nuclear magnetic resonance

RIP

Raman Index of Preservation

Rubisco

ribulose bisphospate carboxylase/oxygenase

XANES

X-ray absorption near-edge spectroscopy

Notes

Acknowledgments

Based in part on Schopf (2009), preparation of this article has been supported by the Center for the Study of Evolution and the Origin of Life at UCLA. I thank J. Shen-Miller for a helpful review of the manuscript.

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© Springer Science+Business Media B.V. 2012

Authors and Affiliations

  1. 1.Department of Earth and Space Sciences, Center for the Study of Evolution and the Origin of Life, Institute of Geophysics and Planetary Physics, Molecular Biology InstituteUniversity of CaliforniaLos AngelesUSA

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