@article {1737,
	title = {Methane cycling. Nonequilibrium clumped isotope signals in microbial methane.},
	journal = {Science},
	volume = {348},
	year = {2015},
	month = {2015 Apr 24},
	pages = {428-31},
	abstract = {<p>Methane is a key component in the global carbon cycle, with a wide range of anthropogenic and natural sources. Although isotopic compositions of methane have traditionally aided source identification, the abundance of its multiply substituted "clumped" isotopologues (for example, (13)CH3D) has recently emerged as a proxy for determining methane-formation temperatures. However, the effect of biological processes on methane{\textquoteright}s clumped isotopologue signature is poorly constrained. We show that methanogenesis proceeding at relatively high rates in cattle, surface environments, and laboratory cultures exerts kinetic control on (13)CH3D abundances and results in anomalously elevated formation-temperature estimates. We demonstrate quantitatively that H2 availability accounts for this effect. Clumped methane thermometry can therefore provide constraints on the generation of methane in diverse settings, including continental serpentinization sites and ancient, deep groundwaters.</p>},
	keywords = {Animals, Carbon Cycle, Carbon Isotopes, Cattle, Groundwater, Hydrogen, Methane, Methanomicrobiales, Temperature},
	issn = {1095-9203},
	doi = {10.1126/science.aaa4326},
	author = {Wang, David T and Gruen, Danielle S and Lollar, Barbara Sherwood and Hinrichs, Kai-Uwe and Stewart, Lucy C and Holden, James F and Hristov, Alexander N and Pohlman, John W and Morrill, Penny L and K{\"o}nneke, Martin and Delwiche, Kyle B and Reeves, Eoghan P and Sutcliffe, Chelsea N and Ritter, Daniel J and Seewald, Jeffrey S and McIntosh, Jennifer C and Hemond, Harold F and Kubo, Michael D and Cardace, Dawn and Hoehler, Tori M and Ono, Shuhei}
}
@article {1417,
	title = {Land use change alters functional gene diversity, composition and abundance in Amazon forest soil microbial communities.},
	journal = {Mol Ecol},
	volume = {23},
	year = {2014},
	month = {2014 Jun},
	pages = {2988-99},
	abstract = {<p>Land use change in the Amazon rainforest alters the taxonomic structure of soil microbial communities, but whether it alters their functional gene composition is unknown. We used the highly parallel microarray technology GeoChip 4.0, which contains 83,992 probes specific for genes linked nutrient cycling and other processes, to evaluate how the diversity, abundance and similarity of the targeted genes responded to forest-to-pasture conversion. We also evaluated whether these parameters were reestablished with secondary forest growth. A spatially nested scheme was employed to sample a primary forest, two pastures (6 and 38 years old) and a secondary forest. Both pastures had significantly lower microbial functional genes richness and diversity when compared to the primary forest. Gene composition and turnover were also significantly modified with land use change. Edaphic traits associated with soil acidity, iron availability, soil texture and organic matter concentration were correlated with these gene changes. Although primary and secondary forests showed similar functional gene richness and diversity, there were differences in gene composition and turnover, suggesting that community recovery was not complete in the secondary forest. Gene association analysis revealed that response to ecosystem conversion varied significantly across functional gene groups, with genes linked to carbon and nitrogen cycling mostly altered. This study indicates that diversity and abundance of numerous environmentally important genes respond to forest-to-pasture conversion and hence have the potential to affect the related processes at an ecosystem scale.</p>
},
	keywords = {Agriculture, Carbon Cycle, Ecosystem, Genes, Bacterial, Genes, Fungal, Genetic Variation, Metagenome, Multigene Family, Nitrogen Cycle, Oligonucleotide Array Sequence Analysis, Soil Microbiology, Trees, Tropical Climate},
	issn = {1365-294X},
	doi = {10.1111/mec.12786},
	author = {Paula, Fabiana S and Rodrigues, Jorge L M and Zhou, Jizhong and Wu, Liyou and Mueller, Rebecca C and Mirza, Babur S and Bohannan, Brendan J M and N{\"u}sslein, Klaus and Deng, Ye and Tiedje, James M and Pellizari, Vivian H}
}
@article {372,
	title = {Metagenomic analysis of a permafrost microbial community reveals a rapid response to thaw.},
	journal = {Nature},
	volume = {480},
	year = {2011},
	month = {2011 Dec 15},
	pages = {368-71},
	abstract = {Permafrost contains an estimated 1672 Pg carbon (C), an amount roughly equivalent to the total currently contained within land plants and the atmosphere. This reservoir of C is vulnerable to decomposition as rising global temperatures cause the permafrost to thaw. During thaw, trapped organic matter may become more accessible for microbial degradation and result in greenhouse gas emissions. Despite recent advances in the use of molecular tools to study permafrost microbial communities, their response to thaw remains unclear. Here we use deep metagenomic sequencing to determine the impact of thaw on microbial phylogenetic and functional genes, and relate these data to measurements of methane emissions. Metagenomics, the direct sequencing of DNA from the environment, allows the examination of whole biochemical pathways and associated processes, as opposed to individual pieces of the metabolic puzzle. Our metagenome analyses reveal that during transition from a frozen to a thawed state there are rapid shifts in many microbial, phylogenetic and functional gene abundances and pathways. After one week of incubation at 5 {\textdegree}C, permafrost metagenomes converge to be more similar to each other than while they are frozen. We find that multiple genes involved in cycling of C and nitrogen shift rapidly during thaw. We also construct the first draft genome from a complex soil metagenome, which corresponds to a novel methanogen. Methane previously accumulated in permafrost is released during thaw and subsequently consumed by methanotrophic bacteria. Together these data point towards the importance of rapid cycling of methane and nitrogen in thawing permafrost.},
	keywords = {Alaska, Arctic Regions, Bacteria, Carbon, Carbon Cycle, DNA, Freezing, Genes, rRNA, Metagenome, Metagenomics, Methane, Nitrogen, Nitrogen Cycle, Oxidation-Reduction, Phylogeny, RNA, Ribosomal, 16S, Soil, Soil Microbiology, Temperature, Time Factors},
	issn = {1476-4687},
	doi = {10.1038/nature10576},
	author = {Mackelprang, Rachel and Waldrop, Mark P and Deangelis, Kristen M and David, Maude M and Chavarria, Krystle L and Blazewicz, Steven J and Rubin, Edward M and Jansson, Janet K}
}
