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A soil actinobacterium scavenges atmospheric H(2) using two membrane-associated, oxygen-dependent [NiFe] hydrogenases
In the Earth’s lower atmosphere, H(2) is maintained at trace concentrations (0.53 ppmv/0.40 nM) and rapidly turned over (lifetime ≤ 2.1 y(−1)). It is thought that soil microbes, likely actinomycetes, serve as the main global sink for tropospheric H(2). However, no study has ever unambiguously proven...
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| Main Authors: | , , , , |
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| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
National Academy of Sciences
2014
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| Fag: | |
| Online adgang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3964045/ https://ncbi.nlm.nih.gov/pubmed/24591586 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1320586111 |
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