Carbon isotope fractionation by an ancestral rubisco suggests that biological proxies for CO(2) through geologic time should be reevaluated

The history of Earth’s carbon cycle reflects trends in atmospheric composition convolved with the evolution of photosynthesis. Fortunately, key parts of the carbon cycle have been recorded in the carbon isotope ratios of sedimentary rocks. The dominant model used to interpret this record as a proxy...

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Detalles Bibliográficos
Autores principales: Wang, Renée Z., Nichols, Robert J., Liu, Albert K., Flamholz, Avi I., Artier, Juliana, Banda, Doug M., Savage, David F., Eiler, John M., Shih, Patrick M., Fischer, Woodward W.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2023
Materias:
Physical Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10193938/
https://www.ncbi.nlm.nih.gov/pubmed/37155899
http://dx.doi.org/10.1073/pnas.2300466120

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10193938/
https://www.ncbi.nlm.nih.gov/pubmed/37155899
http://dx.doi.org/10.1073/pnas.2300466120

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