The identification of sulfide oxidation as a potential metabolism driving primary production on late Noachian Mars

The transition of the martian climate from the wet Noachian era to the dry Hesperian (4.1–3.0 Gya) likely resulted in saline surface waters that were rich in sulfur species. Terrestrial analogue environments that possess a similar chemistry to these proposed waters can be used to develop an understa...

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Bibliographic Details
Published in:Scientific Reports
Main Authors: Macey, M. C., Fox-Powell, M., Ramkissoon, N. K., Stephens, B. P., Barton, T., Schwenzer, S. P., Pearson, V. K., Cousins, C. R., Olsson-Francis, K.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2020
Subjects:
Online Access:https://oro.open.ac.uk/71126/
https://oro.open.ac.uk/71126/1/s41598-020-67815-8.pdf
https://doi.org/10.1038/s41598-020-67815-8