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Applied and Environmental Microbiology, July 2007, p. 4171-4179, Vol. 73, No. 13
0099-2240/07/$08.00+0     doi:10.1128/AEM.02810-06
Copyright © 2007, American Society for Microbiology. All Rights Reserved.

Salinity Constraints on Subsurface Archaeal Diversity and Methanogenesis in Sedimentary Rock Rich in Organic Matter{triangledown}

Patricia J. Waldron,1,{dagger} Steven T. Petsch,2* Anna M. Martini,3 and Klaus Nüsslein1

Department of Microbiology, University of Massachusetts Amherst, Amherst, Massachusetts 01003,1 Department of Geosciences, University of Massachusetts Amherst, Amherst, Massachusetts 01003,2 Department of Geology, Amherst College, Amherst, Massachusetts 010023

Received 1 December 2006/ Accepted 17 April 2007

The diversity of microorganisms active within sedimentary rocks provides important controls on the geochemistry of many subsurface environments. In particular, biodegradation of organic matter in sedimentary rocks contributes to the biogeochemical cycling of carbon and other elements and strongly impacts the recovery and quality of fossil fuel resources. In this study, archaeal diversity was investigated along a salinity gradient spanning 8 to 3,490 mM Cl– in a subsurface shale rich in CH4 derived from biodegradation of sedimentary hydrocarbons. Shale pore waters collected from wells in the main CH4-producing zone lacked electron acceptors such as O2, NO3–, Fe3+, or SO42–. Acetate was detected only in high-salinity waters, suggesting that acetoclastic methanogenesis is inhibited at Cl– concentrations above ~1,000 mM. Most-probable-number series revealed differences in methanogen substrate utilization (acetate, trimethylamine, or H2/CO2) associated with chlorinity. The greatest methane production in enrichment cultures was observed for incubations with salinity at or close to the native pore water salinity of the inoculum. Restriction fragment length polymorphism analyses of archaeal 16S rRNA genes from seven wells indicated that there were links between archaeal communities and pore water salinity. Archaeal clone libraries constructed from sequences from 16S rRNA genes isolated from two wells revealed phylotypes similar to a halophilic methylotrophic Methanohalophilus species and a hydrogenotrophic Methanoplanus species at high salinity and a single phylotype closely related to Methanocorpusculum bavaricum at low salinity. These results show that several distinct communities of methanogens persist in this subsurface, CH4-producing environment and that each community is adapted to particular conditions of salinity and preferential substrate use and each community induces distinct geochemical signatures in shale formation waters.

* Corresponding author. Mailing address: Department of Geosciences, University of Massachusetts, 611 N. Pleasant St., Amherst, MA 01003. Phone: (413) 545-4413. Fax: (413) 545-1200. E-mail: spetsch{at}geo.umass.edu

{triangledown} Published ahead of print on 27 April 2007.

{dagger} Present address: Department of Microbiology, University of Oklahoma, Norman, OK.

Applied and Environmental Microbiology, July 2007, p. 4171-4179, Vol. 73, No. 13
0099-2240/07/$08.00+0     doi:10.1128/AEM.02810-06
Copyright © 2007, American Society for Microbiology. All Rights Reserved.



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