Cargando…

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...

Descripción completa

Detalles Bibliográficos
Autor principal: William Schopf, J.
Formato: Texto
Lenguaje:English
Publicado: Springer Netherlands 2010
Materias:
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
Descripción
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.