@article {1420,
	title = {Response of free-living nitrogen-fixing microorganisms to land use change in the Amazon rainforest.},
	journal = {Appl Environ Microbiol},
	volume = {80},
	year = {2014},
	month = {2014 Jan},
	pages = {281-8},
	abstract = {<p>The Amazon rainforest, the largest equatorial forest in the world, is being cleared for pasture and agricultural use at alarming rates. Tropical deforestation is known to cause alterations in microbial communities at taxonomic and phylogenetic levels, but it is unclear whether microbial functional groups are altered. We asked whether free-living nitrogen-fixing microorganisms (diazotrophs) respond to deforestation in the Amazon rainforest, using analysis of the marker gene nifH. Clone libraries were generated from soil samples collected from a primary forest, a 5-year-old pasture originally converted from primary forest, and a secondary forest established after pasture abandonment. Although diazotroph richness did not significantly change among the three plots, diazotroph community composition was altered with forest-to-pasture conversion, and phylogenetic similarity was higher among pasture communities than among those in forests. There was also 10-fold increase in nifH gene abundance following conversion from primary forest to pasture. Three environmental factors were associated with the observed changes: soil acidity, total N concentration, and C/N ratio. Our results suggest a partial restoration to initial levels of abundance and community structure of diazotrophs following pasture abandonment, with primary and secondary forests sharing similar communities. We postulate that the response of diazotrophs to land use change is a direct consequence of changes in plant communities, particularly the higher N demand of pasture plant communities for supporting aboveground plant growth.</p>
},
	keywords = {Agriculture, Bacteria, Biota, Carbon, Cluster Analysis, Conservation of Natural Resources, Human Activities, Hydrogen-Ion Concentration, Molecular Sequence Data, Nitrogen, Nitrogen Fixation, Oxidoreductases, Phylogeny, Sequence Analysis, DNA, Soil, Soil Microbiology, South America, Trees},
	issn = {1098-5336},
	doi = {10.1128/AEM.02362-13},
	author = {Mirza, Babur S and Potisap, Chotima and N{\"u}sslein, Klaus and Bohannan, Brendan J M and Rodrigues, Jorge L M}
}
@article {744,
	title = {Salinity constraints on subsurface archaeal diversity and methanogenesis in sedimentary rock rich in organic matter.},
	journal = {Appl Environ Microbiol},
	volume = {73},
	year = {2007},
	month = {2007 Jul},
	pages = {4171-9},
	abstract = {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 CH(4) derived from biodegradation of sedimentary hydrocarbons. Shale pore waters collected from wells in the main CH(4)-producing zone lacked electron acceptors such as O(2), NO(3)(-), Fe(3+), or SO(4)(2-). Acetate was detected only in high-salinity waters, suggesting that acetoclastic methanogenesis is inhibited at Cl(-) concentrations above approximately 1,000 mM. Most-probable-number series revealed differences in methanogen substrate utilization (acetate, trimethylamine, or H(2)/CO(2)) 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, CH(4)-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.},
	keywords = {Archaea, Base Sequence, Cloning, Molecular, DNA Primers, Genes, Archaeal, Genetic Variation, Geologic Sediments, Methane, Michigan, Molecular Sequence Data, Organic Chemicals, Phylogeny, RNA, Archaeal, RNA, Ribosomal, 16S, Sodium Chloride, Soil, Soil Microbiology, Water Microbiology},
	issn = {0099-2240},
	doi = {10.1128/AEM.02810-06},
	author = {Waldron, Patricia J and Petsch, Steven T and Martini, Anna M and N{\"u}sslein, Klaus and N{\"u}slein, Klaus}
}
