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The paleobiological record of photosynthesis
Fossil evidence of photosynthesis, documented in Precambrian sediments by microbially laminated stromatolites, cyanobacterial microscopic fossils, and carbon isotopic data consistent with the presence of Rubisco-mediated CO(2)-fixation, extends from the present to ~3,500 million years ago. Such data...
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Formato: | Texto |
Lenguaje: | English |
Publicado: |
Springer Netherlands
2010
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Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3021713/ https://www.ncbi.nlm.nih.gov/pubmed/20607406 http://dx.doi.org/10.1007/s11120-010-9577-1 |
Sumario: | Fossil evidence of photosynthesis, documented in Precambrian sediments by microbially laminated stromatolites, cyanobacterial microscopic fossils, and carbon isotopic data consistent with the presence of Rubisco-mediated CO(2)-fixation, extends from the present to ~3,500 million years ago. Such data, however, do not resolve time of origin of O(2)-producing photoautotrophy from its anoxygenic, bacterial, evolutionary precursor. Though it is well established that Earth’s ecosystem has been based on autotrophy since its very early stages, the time of origin of oxygenic photosynthesis, more than 2,450 million years ago, has yet to be established. |
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