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Methane- and Sulfur-Metabolizing Microbial Communities Dominate the Lost City Hydrothermal Field Ecosystem

Hydrothermal venting and the formation of carbonate chimneys in the Lost City hydrothermal field (LCHF) are driven predominantly by serpentinization reactions and cooling of mantle rocks, resulting in a highly reducing, high-pH environment with abundant dissolved hydrogen and methane. Phylogenetic a...

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Bibliografische gegevens
Hoofdauteurs: Brazelton, William J., Schrenk, Matthew O., Kelley, Deborah S., Baross, John A.
Formaat: Artigo
Taal:Inglês
Gepubliceerd in: American Society for Microbiology 2006
Onderwerpen:
Online toegang:https://ncbi.nlm.nih.gov/pmc/articles/PMC1563643/
https://ncbi.nlm.nih.gov/pubmed/16957253
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1128/AEM.00574-06
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