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Mounting evidence suggests that ammonia-oxidizing archaea (AOA) may play important roles in nitrogen cycling in geothermal environments. In this study, the diversity, distribution and ecological significance of AOA in terrestrial hot springs in Kamchatka (Far East Russia) were explored using amoA genes complemented by analysis of glycerol dialkyl glycerol tetraethers (GDGTs) of archaea. PCR amplification of functional genes (amoA) from AOA and ammonia-oxidizing bacteria (AOB) was performed on microbial mats/streamers and sediments collected from three hot springs (42°C to 87°C and pH 5.5-7.0). No amoA genes of AOB were detected. The amoA genes of AOA formed three distinct phylogenetic clusters with Cluster 3 representing the majority (∼59%) of OTUs. Some of the sequences from Cluster 3 were closely related to those from acidic soil environments, which is consistent with the predominance of low pH (<7.0) in these hot springs. Species richness (estimated by Chao1) was more frequently higher at temperatures below 75°C than above it, indicating that AOA may be favored in the moderately high temperature environments. Quantitative PCR of 16S rRNA genes showed that crenarchaeota counted for up to 80% of total archaea. S-LIBSHUFF separated all samples into two phylogenetic groups. The profiles of GDGTs were well separated among the studied springs, suggesting a spatial patterning of archaeal lipid biomarkers. However, this patterning did not correlate significantly with variation in archaeal amoA, suggesting that AOA are not the predominant archaeal group in these springs producing the observed GDGTs. [ABSTRACT FROM AUTHOR]

Objective: Crenarchaeota is a major archaeal lineage in terrestrial hot springs and important in biogeochemical cycles of life-essential elements. In this study, we investigated the diversity of Crenarchaeota in hot springs and the surrounding environments in Kamchatka, Russia. In addition, we compared crenarchaeotal community structures in Kamchatka, Russia and Yunnan province, China., Methods: Crenarchaeal 16S rRNA gene clone libraries were constructed and the sequences and abundances of representational clone were obtained. Phylogenetic analysis was then performed and the community structures in different samples were compared., Results: The high temperature spring Burlyashi Liza (BSL, 89 degrees C) comprised Thermoprotei. The moderate temperature spring TF Vent 2 (TFV, 49 degrees C) harbored unidentified Thermoprotei group, unidentified crenarchaeal group, HWCG-II (hot water crenarchaeotal group II), and Group1. 1b (one thaumarchaeotal subgroup). Most of sequences that obtained from surrounding environments ( <15 degrees C) are closely with the representational clone pJP from a Yellowstone hot spring. Jackknife cluster and Principal coordinates analysis (PCoA) showed that the samples have more similarity in crenarchaeal communities at similar temperatures., Conclusion: The diversities of Crenarchaeota in Kamchatka hot springs are somewhat different from those in Yunnan province. Terrestrial hot springs obviously affect the crenarchaeotal communities in surrounding environments. Temperature is the major factor controlling the community structure in terrestrial hot springs.

Background: Genetic analyses of human lice have shown that the current taxonomic classification of head lice (Pediculus humanus capitis) and body lice (Pediculus humanus humanus) does not reflect their phylogenetic organization. Three phylotypes of head lice A, B and C exist but body lice have been observed only in phylotype A. Head and body lice have different behaviours and only the latter have been involved in outbreaks of infectious diseases including epidemic typhus, trench fever and louse borne recurrent fever. Recent studies suggest that body lice arose several times from head louse populations., Methods and Findings: By introducing a new genotyping technique, sequencing variable intergenic spacers which were selected from louse genomic sequence, we were able to evaluate the genotypic distribution of 207 human lice. Sequence variation of two intergenic spacers, S2 and S5, discriminated the 207 lice into 148 genotypes and sequence variation of another two intergenic spacers, PM1 and PM2, discriminated 174 lice into 77 genotypes. Concatenation of the four intergenic spacers discriminated a panel of 97 lice into 96 genotypes. These intergenic spacer sequence types were relatively specific geographically, and enabled us to identify two clusters in France, one cluster in Central Africa (where a large body louse outbreak has been observed) and one cluster in Russia. Interestingly, head and body lice were not genetically differentiated., Conclusions: We propose a hypothesis for the emergence of body lice, and suggest that humans with both low hygiene and head louse infestations provide an opportunity for head louse variants, able to ingest a larger blood meal (a required characteristic of body lice), to colonize clothing. If this hypothesis is ultimately supported, it would help to explain why poor human hygiene often coincides with outbreaks of body lice. Additionally, if head lice act as a reservoir for body lice, and that any social degradation in human populations may allow the formation of new populations of body lice, then head louse populations are potentially a greater threat to humans than previously assumed.

Despite the ubiquity of ammonium in geothermal environments and the thermodynamic favorability of aerobic ammonia oxidation, thermophilic ammonia-oxidizing microorganisms belonging to the crenarchaeota kingdom have only recently been described. In this study, we analyzed microbial mats and surface sediments from 21 hot spring samples (pH 3.4 to 9.0; temperature, 41 to 86 degrees C) from the United States, China, and Russia and obtained 846 putative archaeal ammonia monooxygenase large-subunit (amoA) gene and transcript sequences, representing a total of 41 amoA operational taxonomic units (OTUs) at 2% identity. The amoA gene sequences were highly diverse, yet they clustered within two major clades of archaeal amoA sequences known from water columns, sediments, and soils: clusters A and B. Eighty-four percent (711/846) of the sequences belonged to cluster A, which is typically found in water columns and sediments, whereas 16% (135/846) belonged to cluster B, which is typically found in soils and sediments. Although a few amoA OTUs were present in several geothermal regions, most were specific to a single region. In addition, cluster A amoA genes formed geographic groups, while cluster B sequences did not group geographically. With the exception of only one hot spring, principal-component analysis and UPGMA (unweighted-pair group method using average linkages) based on the UniFrac metric derived from cluster A grouped the springs by location, regardless of temperature or bulk water pH, suggesting that geography may play a role in structuring communities of putative ammonia-oxidizing archaea (AOA). The amoA genes were distinct from those of low-temperature environments; in particular, pair-wise comparisons between hot spring amoA genes and those from sympatric soils showed less than 85% sequence identity, underscoring the distinctness of hot spring archaeal communities from those of the surrounding soil system. Reverse transcription-PCR showed that amoA genes were transcribed in situ in one spring and the transcripts were closely related to the amoA genes amplified from the same spring. Our study demonstrates the global occurrence of putative archaeal amoA genes in a wide variety of terrestrial hot springs and suggests that geography may play an important role in selecting different assemblages of AOA.