Oxygen isotope effects during microbial sulfate reduction: applications to sediment cell abundances

The majority of anaerobic biogeochemical cycling occurs within marine sediments. To understand these processes, quantifying the distribution of active cells and gross metabolic activity is essential. We present an isotope model rooted in thermodynamics to draw quantitative links between cell-specifi...

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Detalles Bibliográficos
Autores principales: Bertran, E., Waldeck, A., Wing, B. A., Halevy, I., Leavitt, W. D., Bradley, A. S., Johnston, D. T.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7242377/
https://www.ncbi.nlm.nih.gov/pubmed/32152390
http://dx.doi.org/10.1038/s41396-020-0618-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7242377/
https://www.ncbi.nlm.nih.gov/pubmed/32152390
http://dx.doi.org/10.1038/s41396-020-0618-2

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