Archaeal and bacterial communities across a chronosequence of drained lake basins in Arctic Alaska.

We examined patterns in soil microbial community composition across a successional gradient of drained lake basins in the Arctic Coastal Plain. Analysis of 16S rRNA gene sequences revealed that methanogens closely related to Candidatus 'Methanoflorens stordalenmirensis' were the dominant archaea, comprising >50% of the total archaea at most sites, with particularly high levels in the oldest basins and in the top 57 cm of soil (active and transition layers). Bacterial community composition was more diverse, with lineages from OP11, Actinobacteria, Bacteroidetes, and Proteobacteria found in high relative abundance across all sites. Notably, microbial composition appeared to converge in the active layer, but transition and permafrost layer communities across the sites were significantly different to one another. Microbial biomass using fatty acid-based analysis indicated that the youngest basins had increased abundances of gram-positive bacteria and saprotrophic fungi at higher soil organic carbon levels, while the oldest basins displayed an increase in only the gram-positive bacteria. While this study showed differences in microbial populations across the sites relevant to basin age, the dominance of Candidatus 'M. stordalenmirensis' across the chronosequence indicates the potential for changes in local carbon cycling, depending on how these methanogens and associated microbial communities respond to warming temperatures.

NUMTs in the sponge genome reveal conserved transposition mechanisms in metazoans.

The transposition of parts of the mitochondrial (mt) genetic material into the nuclear genome (NUMTs) occurs in a wide range of eukaryotes. Here, we show that NUMTs exist for nearly all regions of the mt genome in the demosponge Amphimedon queenslandica, a representative of the oldest phyletic lineage of animals. Because the sponge NUMTs are small and noncoding, and transposed via a DNA intermediate, as in eumetazoans, we infer that the transpositonal processes underlying NUMT formation in contemporary animals existed in their most recent common ancestor. In contrast to most bilaterians, Amphimedon NUMTs are inserted into regions of high gene density. Given the common features of metazoan NUMTs, the reduction in animal mt genome sizes relative to other eukaryotes may be the product of the mt DNA transposition mechanisms that evolved along the metazoan stem.