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Lithotrophic iron-oxidizing bacteria produce organic stalks to control mineral growth: implications for biosignature formation

Neutrophilic Fe-oxidizing bacteria (FeOB) are often identified by their distinctive morphologies, such as the extracellular twisted ribbon-like stalks formed by Gallionella ferruginea or Mariprofundus ferrooxydans. Similar filaments preserved in silica are often identified as FeOB fossils in rocks....

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Detalhes bibliográficos
Main Authors: Chan, Clara S, Fakra, Sirine C, Emerson, David, Fleming, Emily J, Edwards, Katrina J
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group 2011
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC3105749/
https://ncbi.nlm.nih.gov/pubmed/21107443
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ismej.2010.173
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