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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 |
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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 |
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author | William Schopf, J. |
author_facet | William Schopf, J. |
author_sort | William Schopf, J. |
collection | PubMed |
description | 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. |
format | Text |
id | pubmed-3021713 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2010 |
publisher | Springer Netherlands |
record_format | MEDLINE/PubMed |
spelling | pubmed-30217132011-02-22 The paleobiological record of photosynthesis William Schopf, J. Photosynth Res Review 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. Springer Netherlands 2010-07-07 2011 /pmc/articles/PMC3021713/ /pubmed/20607406 http://dx.doi.org/10.1007/s11120-010-9577-1 Text en © The Author(s) 2010 https://creativecommons.org/licenses/by-nc/4.0/ This article is distributed under the terms of the Creative Commons Attribution Noncommercial License which permits any noncommercial use, distribution, and reproduction in any medium, provided the original author(s) and source are credited. |
spellingShingle | Review William Schopf, J. The paleobiological record of photosynthesis |
title | The paleobiological record of photosynthesis |
title_full | The paleobiological record of photosynthesis |
title_fullStr | The paleobiological record of photosynthesis |
title_full_unstemmed | The paleobiological record of photosynthesis |
title_short | The paleobiological record of photosynthesis |
title_sort | paleobiological record of photosynthesis |
topic | Review |
url | 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 |
work_keys_str_mv | AT williamschopfj thepaleobiologicalrecordofphotosynthesis AT williamschopfj paleobiologicalrecordofphotosynthesis |