AEM
Home Help [Feedback] [For Subscribers] [Archive] [Search] [Contents]
This Article
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Other Versions of this Article:
AEM.00886-06v1
72/11/7218    most recent
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow Copyright Information
Right arrow Books from ASM Press
Right arrow MicrobeWorld
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Lloyd, K. G.
Right arrow Articles by Teske, A.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Lloyd, K. G.
Right arrow Articles by Teske, A.
Agricola
Right arrow Articles by Lloyd, K. G.
Right arrow Articles by Teske, A.
Applied and Environmental Microbiology, November 2006, p. 7218-7230, Vol. 72, No. 11
0099-2240/06/$08.00+0     doi:10.1128/AEM.00886-06
Copyright © 2006, American Society for Microbiology. All Rights Reserved.

An Anaerobic Methane-Oxidizing Community of ANME-1b Archaea in Hypersaline Gulf of Mexico Sediments{triangledown}

Karen G. Lloyd,* Laura Lapham, and Andreas Teske

Department of Marine Sciences, University of North Carolina at Chapel Hill, Chapel Hill, North Carolina 27599

Received 13 April 2006/ Accepted 1 September 2006

Sediments overlying a brine pool methane seep in the Gulf of Mexico (Green Canyon 205) were analyzed using molecular and geochemical approaches to identify geochemical controls on microbial community composition and stratification. 16S rRNA gene and rRNA clone libraries, as well as mcrA gene clone libraries, showed that the archaeal community consists predominantly of ANME-1b methane oxidizers; no archaea of other ANME subgroups were found with general and group-specific PCR primers. The ANME-1b community was found in the sulfate-methane interface, where undersaturated methane concentrations of ca. 100 to 250 µM coexist with sulfate concentrations around 10 mM. Clone libraries of dsrAB genes and bacterial 16S rRNA genes show diversified sulfate-reducing communities within and above the sulfate-methane interface. Their phylogenetic profiles and occurrence patterns are not linked to ANME-1b populations, indicating that electron donors other than methane, perhaps petroleum-derived hydrocarbons, drive sulfate reduction. The archaeal component of anaerobic oxidation of methane is comprised of an active population of mainly ANME-1b in this hypersaline sediment.


* Corresponding author. Mailing address: CB# 3300, Department of Marine Sciences, University of North Carolina—Chapel Hill, Chapel Hill, NC 27599. Phone: (919) 966-5965. Fax: (919) 962-1254. E-mail: klloyd{at}email.unc.edu.

{triangledown} Published ahead of print on 15 September 2006.


Applied and Environmental Microbiology, November 2006, p. 7218-7230, Vol. 72, No. 11
0099-2240/06/$08.00+0     doi:10.1128/AEM.00886-06
Copyright © 2006, American Society for Microbiology. All Rights Reserved.




This article has been cited by other articles:




Home Help [Feedback] [For Subscribers] [Archive] [Search] [Contents]
J. Bacteriol. Microbiol. Mol. Biol. Rev. Eukaryot. Cell All ASM Journals

Copyright © 2006 by the American Society for Microbiology. All rights reserved.