The discovery of ammonia-oxidizing archaea (AOA) of the phylum Thaumarchaeota and the high abundance of archaeal ammonia monooxygenase subunit A encoding gene sequences in many environments have extended our perception of nitrifying microbial communities. Moreover, AOA are the only aerobic ammonia oxidizers known to be active in geothermal environments. Molecular data indicate that in many globally distributed terrestrial high-temperature habits a thaumarchaeotal lineage within the Nitrosopumilus cluster (also called “marine” group I.1a) thrives, but these microbes have neither been isolated from these systems nor functionally characterized in situ yet. In this study, we report on the enrichment and genomic characterization of a representative of this lineage from a thermal spring in Kamchatka. This thaumarchaeote, provisionally classified as “Candidatus Nitrosotenuis uzonensis”, is a moderately thermophilic, non-halophilic, chemolithoautotrophic ammonia oxidizer. The nearly complete genome sequence (assembled into a single scaffold) of this AOA confirmed the presence of the typical thaumarchaeotal pathways for ammonia oxidation and carbon fixation, and indicated its ability to produce coenzyme F420 and to chemotactically react to its environment. Interestingly, like members of the genus Nitrosoarchaeum, “Candidatus N. uzonensis” also possesses a putative artubulin-encoding gene. Genome comparisons to related AOA with available genome sequences confirmed that the newly cultured AOA has an average nucleotide identity far below the species threshold and revealed a substantial degree of genomic plasticity with unique genomic regions in “Ca. N. uzonensis”, which potentially include genetic determinants of ecological niche differentiation.
Citation: Lebedeva EV, Hatzenpichler R, Pelletier E, Schuster N, Hauzmayer S, Bulaev A, et al. (2013) Enrichment and Genome Sequence of the Group I.1a Ammonia-Oxidizing Archaeon “Ca. Nitrosotenuis uzonensis” Representing a Clade Globally Distributed in Thermal Habitats. PLoS ONE 8(11): e80835. doi:10.1371/journal.pone.0080835
Editor: Leo Eberl, University of Zurich, Switzerland
Received: August 26, 2013; Accepted: October 14, 2013; Published: November 20, 2013
Copyright: © 2013 Lebedeva et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Funding: This research was funded by the Austrian Academy of Sciences via a DOC fellowship to RH, a Erwin Schrӧdinger postdoctoral fellowship by the Austrian Science Fund (FWF), J 3162-B20 to RH, by the Vienna Science and Technology Fund (WWTF) via grant LS09-040 to HD, the European Research Council [Advanced Grant Nitrification Reloaded (NITRICARE) 294343 to MW] and by the Russian Foundation for Basic Research No. 09-04-00502. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
The discovery of ammonia-oxidizing archaea revealed a new microbial group involved in nitrogen cycling [1-3]. All AOA recognized today are members of the phylum Thaumarchaeota [4,5], whose representatives in culture share ammonia oxidation as their only demonstrated pathway for energy conservation. However, at least some members of this phylum can obtain in the environment energy for growth from yet unidentified substrates other than ammonia . While until recently research on the first step of the nitrification process in the environment mainly focused on ammonia-oxidizing bacteria (AOB), which thrive in most terrestrial and aquatic systems [7,8], it has been shown during the last decade that thaumarchaeotes outnumber AOB in many ecosystems, including some soils [9–12], oceanic waters [13–15] and sediments [16,17].
In contrast to AOB, AOA also play a crucial role for nitrification in high temperature habitats [18-20]. In hot springs where ammonia is an abundant electron donor for chemolithotrophy high overall potential energy yields can be obtained from ammonia oxidation . Enrichment cultures of thermophilic (at 74°C)  and moderately thermophilic (at 46°C)  AOA have become available, and the widespread presence of archaeal ammonia monooxygenase subunit A (amoA)-like genes in high temperature habitats up to 97°C has been demonstrated. So far, such amoA-like gene sequences have been found in subsurface thermal springs [23,24], many terrestrial hot springs [19,20,25-27] and deep-sea hydrothermal vents [28,29]. Measurements of in situ nitrification [20,27] and of amoA gene transcription [19,30] in several hot springs further indicate an important role of thermophilic AOA in these systems. The presence of crenarchaeol (more accurately named thaumarchaeol ), which is a signature lipid component of both mesophilic [31,32] and thermophilic AOA [18,33], in terrestrial hot springs lends additional support to the importance of AOA in thermal habitats [34-37].
Despite the global distribution and ecological significance of AOA, knowledge of the physiology and genomic make-up of these organisms are still relatively sparse. This knowledge gap can partly be attributed to the difficulties of cultivating the slow-growing AOA under laboratory conditions. Thus, only few enrichment or pure cultures of AOA are currently available [18,22,38-44].
In this study, we inoculated mineral medium with samples from a hot spring located in the Uzon caldera on the Kamchatka peninsula (Russia). Stable ammonia-oxidizing enrichment cultures were established and grown at 46°C. We present evidence that in one of these cultures a novel, moderately thermophilic AOA strain is solely responsible for the observed oxidation of ammonia. We demonstrate that this thaumarchaeote, which we designate as “Candidatus Nitrosotenuis uzonensis”, represents a lineage of AOA that is globally distributed in terrestrial high temperature environments, but was not brought into culture previously. Furthermore, a near-complete genome sequence of “Candidatus Nitrosotenuis uzonensis” was obtained and we demonstrate the presence of (i) genes typically found in chemolithoautotrophic thaumarchaeotes, (ii) provide evidence for flagellation and chemotaxis, and (iii) confirm the status of “Candidatus Nitrosotenuis uzonensis” as a new species and member of a new genus by average nucleotide identity analyses.
Results and Discussion
An ammonia-oxidizing enrichment culture from a hot spring in the Uzon caldera
An ammonia-oxidizing enrichment culture seeded with material from a geothermal spring located in the Uzon caldera on the Kamchatka peninsula (Russia) was established and maintained in the laboratory for seven years. During the initial enrichment phase, different incubation temperatures were tested and the enrichment was observed to oxidize ammonia within a range of 28-52°C. For all further incubations 46°C was chosen, because it resulted in the highest ammonia removal rates. In later stages of the enrichment nitrite accumulated (Figure 1) and no nitrate was produced, indicating the absence of active nitrite-oxidizing bacteria (NOB). A parallel enrichment of NOB from the same primary enrichment recently resulted in the isolation of a novel thermophilic member of the genus Nitrospira .
Two replicate culture flasks (indicated by red and green symbols) were inoculated with 10 vol% of the parent culture, leading to an initial nitrite concentration of ~0.5 mM. Nitrate was not detectable during the whole experiment. Axis scaling is identical for the ammonia (triangles) and nitrite (squares) concentrations.
A highly enriched AOA culture, in the following referred to as “culture N4”, was obtained by consecutive application of vancomycin (100 mg L-1) and streptomycin (50 mg L-1) followed by inoculation into fresh medium (10 vol% of the culture). This procedure was repeated three times and subsequently the culture was further purified by repeated subculturing from diluted suspensions. At the time of manuscript submission, only one morphotype was visible in the enrichment culture by phase microscopy, but PCR screening with three different primer sets (Table S10 in File S1) targeting bacterial 16S rRNA genes revealed a cryptic bacterial contamination as these primer pairs still yielded an amplification product of the expected size. The very low number of bacterial contaminants was confirmed by fluorescence in situ hybridization (FISH) as no signals were observed after hybridization with the EUB338 probe set targeting almost all members of the bacteria (data not shown). Notably, ammonia oxidation of culture N4 was inhibited by addition of bacitracin (100 mg L-1) and rifampicin (20 mg L-1). While most archaea are resistant to rifampicin, many rifampicin-sensitive halobacterial and methanogenic species have been reported [46,47]. For some of these archaea a detergent-like effect of rifampicin has been suggested . The addition of low concentrations (20 mg L-1) of organic substrates, namely formate, acetate, succinate, and pyruvate (shown to have a growth-stimulating effect on N. viennensis EN76)  did not result in a greater rate of ammonia oxidation as compared to purely chemolithoautotrophic conditions (data not shown). Addition of HEPES-buffer (20 mM) to the growth medium inhibited ammonia oxidation. Culture N4 oxidized ammonia in the range of 0.05-1.0 g NaCl l-1 salinity with an optimum at 0.5 g salinity (data not shown). In contrast to the primary enrichment, culture N4 ceased to oxidize ammonia in the CaCl2-based medium as soon as the pH dropped below 6 (for comparison the pH at the sampling site was 6.5). Re-adjusting the pH did not restore ammonia-oxidizing activity. Consequently, culture N4 was till then maintained exclusively in CaCO3-based medium.
Absence of ammonia-oxidizing bacteria
Several molecular methods were applied to screen culture N4 for the presence of known AOB. Bacterial 16S rRNA genes were PCR-amplified with the broad-coverage primers 616F and 1492R (Table S1 in File S1) from the enrichment, cloned, sequenced, and subjected to phylogenetic analysis. None of the 30 analyzed bacterial 16S rRNA gene clones was affiliated to known AOB (data not shown). Consistent with these results, all attempts to PCR-amplify bacterial amoA genes from this culture were unsuccessful even when up to 40 PCR cycles were used. Similarly, no AOB were detected by fluorescence in situ hybridization (FISH) using established rRNA-targeted probes that are specific for betaproteobacterial AOB (Table S2 in File S1). These results are consistent with the absence of genomic sequences from AOB in the obtained metagenomic dataset (see below).
Molecular detection of a novel ammonia-oxidizing thaumarchaeote
During the early stages of culture N4 an archaeal 16S rRNA gene library was established using primers 21F and 1492R (Table S1 in File S1). Eight clones were randomly selected and sequenced. At a later stage of the culture, a second archaeal 16S rRNA gene library was established. Screening of 31 clones from this library by restriction fragment length polymorphism (RFLP) analysis yielded three band patterns. Ten nearly full-length 16S rRNA sequences representing these patterns were further analysed. All sequences obtained from these two libraries were highly similar to each other (>99.0%), fell within the Nitrosopumilus cluster  (also called group I.1a) of Thaumarchaeota, and were related to the 16S rRNA of the recently enriched strains “AOA-AC5” and “AOA-DW” obtained from freshwater sediment (~97% identity over the only partially [~800 nt] available 16S rRNA gene of these freshwater AOA) . The next closest relative (for which a full sequence is available) was Nitrosopumilus maritimus SCM1 (92.8% identity; Figure 2A).
All trees show only Nitrosopumilus cluster (also called group I.1a) sequences, while the respective sequences from the Nitrososphaera cluster (also called group I.1b), Nitrosotalea cluster (group I.1a-affiliated) and Nitrosocaldus cluster (ThAOA group) are contained within the outgroups. Circles on tree nodes indicate parsimony bootstrap support ≥90%. Numbers in parentheses indicate the number of sequences within a group. Dotted lines were used for short sequences that were added after construction of the overall tree. Scale bars show 10% estimated sequence divergence. SAGM, South African Gold Mine. For an extended AmoA tree please refer to Figure S1.
Clone libraries were also established for archaeal amoA and amoB (ammonia monooxygenase subunits A and B) genes, and 39 and 12 clones, respectively, were randomly picked and sequenced. All obtained amoA and amoB gene sequences were highly similar (≥99.1% nucleotide identity for each gene) and clearly differed from those of other identified AOA (Figure 2B, C), with enrichment “AOA-AC5” as the closest cultured relative (92% nucleotide identity of the amoA gene; amoB is not available for this strain). Intriguingly, the amoA sequence of the novel thaumarchaeote is closely related to sequences that have been obtained from various geographically distant high temperature terrestrial environments (Figure 2B and Figure S1), such as Austrian subsurface radioactive thermal springs , geothermal mine waters in the United States , and numerous hot springs in Asia, North America, and Iceland, which exhibit a wide range of physicochemical parameters (pH 3-8.4; 1.2-1,167 µM NH4+, listed in Figure S1) and temperatures up to 97°C [19,20,26,27,30]. The mere detection of archaeal amoA-like genes in an environment does not always prove nitrifying activity of the respective microbes, not even if these genes occur in high copy numbers and are transcribed . However, our ammonia-oxidizing enrichment of a thaumarchaeote from this cluster from a thermal spring and the global distribution of highly similar amoA-like genes in hot environments indicate that this particular lineage has at least the metabolic capability to perform nitrification in these habitats.
Furthermore, we established a clone library of the hcd gene encoding archaeal 4-hydroxybutyryl-CoA dehydratase, a key enzyme of the 3-hydroxypropionate/4-hydroxybutyrate cycle for autotrophic CO2 fixation . RFLP analysis of 25 hcd clones revealed two different band patterns, and six clones representing either pattern were sequenced and phylogenetically analyzed (Figure 2D). The sequences were highly similar (≥99.5% nucleotide identity) to each other, but showed only moderate similarity (<77% nucleotide identity) to thaumarchaeotal hcd sequences from other environments and cultures. However, it has to be considered that existing databases for this gene are much less exhaustive than 16S rRNA and amoA gene collections.
Taken together, the analyses of four molecular marker genes demonstrated that culture N4 contained a novel ammonia-oxidizing thaumarchaeote that is only distantly related to other cultured AOA.
When electron microscopic analyses were performed, the enrichment still contained cells that were detectable by FISH using the EUB338 probe set. However, the majority of the cells did not hybridize with these probes and most of them were thin rods. Some of these rods were clearly assigned to the novel AOA by CARD-FISH with probes Arch915 and Cren512 (Table S2 in File S1), but the hybridization signal was very weak and many cells neither hybridized with the bacterial nor the archaeal probes. Consistently, by electron microscopy thin rods were observed as the dominant morphotype in the enrichment and we thus assumed that these cells are the novel AOA. These cells appeared as slender, straight rods with a diameter of 0.2-0.3 µm and a length of 0.4-1.7 µm. One or two polar to subpolar tail-like cell projections were observed, which we assume to be flagella (Figure 3A). In whole cell preparations stained with uranyl acetate a network of hexagonal structures, typical for archaeal paracrystalline surface layers , was visible (Figure 3A).
(A) Intact cell stained with uranyl acetate, showing a subpolar tail-like cell projection, possibly a flagellum, and a network of hexagonal structures on the cell surface. (B) Organization of flagellar- and chemotaxis-associated genes in its genome. Genes encoding parts of the archaeal flagellum (fla genes) and chemotaxis apparatus (che genes) are given in red and green, respectively, whereas other genes are shown in grey. For details on these genes please refer to Table S8 in File S1. Black double bars indicate separate genomic regions, while blue bars display contig ends. MCP, putative methyl-accepting chemotaxis protein.
Genome reconstruction of the novel archaeon
The near-complete genome of the novel, moderately thermophilic AOA was reconstructed using an environmental genomics approach. At the time of sampling for genome sequencing, thaumarchaeotes constituted ~50% of cells in culture N4 according to visual quantification after catalyzed reporter deposition (CARD) FISH using probes Arch915 and Cren512 (Table S2 in File S1), but this number was likely an underestimate of the actual degree of enrichment as the CARD-FISH signals were very weak indicating either a very low ribosome content of the AOA or problems with cell permeabilization.
The genome of the novel AOA is represented by a single scaffold containing 14 contigs with a total length of 1,649,125 bp, mean sequence coverage of 39.4 and an average GC-content of 42.2%. Other key features of the genome are listed in Table 1 and Figure S2. The near completeness of the genome is indicated by the presence of all 138 clusters of orthologous groups (COGs) of proteins that are encoded in all sequenced archaeal genomes (archCOGs; Table S3 in File S1). The 16S rRNA, amoA, amoB, and hcd gene sequences in the genome were highly similar (>99% nucleotide identity for each gene) to the sequences retrieved from the aforementioned clone libraries. No sequence indicative of the presence of ammonia or nitrite oxidizing bacteria or other archaea was found in the metagenome.
|Genome size||1,649,125 bp|
|Average GC-content||42.25 %|
|Number of scaffolds||1|
|Number of contigs||14|
|Number of genomic objects (CDS, fCDS, tRNAs, rRNAs)||1,999|
|Number of CDS||1,958|
|Number of CDS with predicted function||411 (21.0%)|
|CDS density||1.19 CDS/kb|
|Average CDS length||766.3 bp|
|Average intergenic length||98.5 bp|
|Protein coding density||90.2 %|
|Number of 16S-23S rRNA operons||1|
|Number of 5S rRNAs||1|
|Number of tRNAs||38|
|Number of amoA, amoB, amoC genes||1 / 1 / 2|
|Number of accA/pccB and hcd genes||1 / 1|
The genome of the enriched thaumarchaeote encodes all proteins that have been hypothesized to be involved in the oxidation of ammonia and subsequent electron transport in N. maritimus SCM1 (Table S4 in File S1) . Considering the distant phylogenetic relationship and different habitat of the novel thaumarchaeote compared to the other genome-sequenced AOA, the conservation of this protein set in the novel and previously available genomes [38,43,51-54] supports the proposed key functional role in the metabolism of these organisms. Like the other genome-sequenced AOA, the analyzed thaumarchaeote possesses single copies of the amoA and amoB genes, whereas two copies of amoC (96.3% amino acid identity) are present. The amo genes are clustered with an arrangement identical to the order in the genomes of N. maritimus SCM1, “Ca. N. limnia” SFB1 and “Ca. N. koreensis” MY1 (amoA, amoX, amoC, amoB) [38,51,52,55].
Transport and use of alternative substrates
While two AmtB-type ammonia transporters were identified (Tables S4 and S5 in File S1), we found no genes coding for a urea transporter or a urease, which would enable the organism to conserve energy by oxidizing ammonia derived from the hydrolysis of urea. This finding is consistent with the absence of such genes in N. maritimus SCM1, “Ca. Nitrosopumilus Salaria” and “Ca. N. limnia” sp. [38,43,51-53]. In contrast, “Ca. Cenarchaeum symbiosum” A was reported to harbour all essential genes for ureolysis , but experimental support for this as well as its ammonia-oxidizing activity is lacking so far. However, ureolytic activity has been demonstrated in AOA from the Nitrososphaera cluster [44,54]. In addition, in the AOA enriched in our study, no genes for the uptake or utilization of cyanate as potential energy source, as recently hypothesized for “Ca. N. gargensis” , were found in the genome.
In contrast to the genome of “Ca. N. gargensis”, the archaeon enriched in this study only encodes a limited set of heavy metal transporters comparable to those of N. maritimus and ”Ca. N. limnia” (Table S5 in File S1). Unfortunately, no data on heavy metal concentrations in the thermal spring water used for inoculation are available and it remains unknown whether heavy metal exposure for strain N4 is lower than for “Ca. N. gargensis” from the Garga hot spring.
The genome of strain N4 encodes transporters of amino acids and oligo/dipeptides, as well as putative alanyl-, methionyl/ and leucyl-aminopeptidases (Table S5 in File S1). This suggests that strain N4 might be capable of mixotrophic growth on these substrates or at least can utilize them as an additional source of nitrogen. No systems for the uptake or degradation of glycerol or specific sugars, as found in other AOA [51,54], could be identified. Consistent with the finding that the addition of organic acids (formate, acetate, pyruvate, and succinate) to the culture did not result in a change of ammonia oxidation rates, no transporters for these compounds could be identified in the genome.
Recent data suggest that AOA grow autotrophically by fixing inorganic carbon via a modified 3-hydroxypropionate/4-hydroxybutyrate pathway (3HP/4HB) [50,51,56]. Two key enzymes of this cycle are 4-hydroxybutyryl-CoA dehydratase (Hcd) and acetyl-CoA/propionyl-CoA carboxylase (AccA/PccB), which recently have been used to study the distribution and abundance of autotrophic thaumarchaeotes in the environment [57-59]. The successful amplification of archaeal hcd gene sequences from culture N4 (Fig. 2D), which contained bicarbonate/carbon dioxide as the sole source of carbon, already indicated that the novel AOA uses this pathway for the fixation of inorganic carbon. This hypothesis was corroborated by the presence of a near complete 3HP/4HB cycle in the genome of the enriched AOA (Table S6 in File S1). This finding supports the proposed wide distribution of a 3HP/4HB-like cycle in AOA and is in agreement with the observed thermotolerance of this carbon fixation pathway . It should be noted that the primers recently developed for the detection of archaeal hcd  and accA  genes in environmental samples contain up to ten nucleotide mismatches to the respective genes of strain N4 and of “Ca. Nitrososphaera gargensis”. Although hcd gene fragments of strain N4 were amplifiable by using the published hcd-targeted primers and recommended PCR conditions, both primer sets could introduce strong biases in molecular analyses of thaumarchaeotal community structure.
Strain N4 encodes a cofactor F420-dependent NADP oxidoreductase as well as all key genes for F420-biosynthesis (Table S7 in File S1) that have recently been identified in all other available AOA genomes . However, in contrast to “Ca. N. gargensis” , but in accordance to all other AOA, the genome of strain N4 does not encode a F420-dependent glucose-6-phosphate dehydrogenase. While the role of F420 in AOA is yet unknown, this cofactor serves as electron carrier in methanogens  and in bacteria it has been shown to be involved in the protection from oxidants  and reactive nitrogen species . In contrast to “Ca. N. gargensis”, we could not microscopically observe the characteristic blue fluorescence of this cofactor in a highly active culture of strain N4. However, in this context it is important to note that F420 content also varies considerably in different methanogens  .
As all other genome-sequenced AOA, strain N4 encodes a polyhydroxyalkanoate synthase, the key enzyme for the production of polyhydroxyalkanoate (PHA), which most probably starts from the 3HP/4HB-cycle intermediate 3-hydroxybutyryl-CoA . Similar to all other thaumarchaeotes, with the exception of “Ca. N. gargensis” , the enzyme is encoded by a single locus of two partly overlapping genes (phaCE, encoded by Nituzv1_30469 and Nituzv1_30470). As in other AOA, canonical PHA depolymerases are absent from the strain N4 genome. In contrast to “Ca. N. gargensis”, Raman micro-spectroscopic analyses of strain N4 cells did not reveal signature bands of polyhydroxyalkanoates (data not shown), but this does not exclude the production of this storage polymer under different growth conditions.
Flagellation and chemotaxis
The novel AOA encodes a number of genes that have been associated with archaeal chemotaxis and flagellar assembly (Table S8 in File S1; Figure 3B). It comprises the full gene set required for the synthesis of an archaeal flagellum, and our observation of flagella-like structures during EM analyses (Figure 3A) suggest that these genes are actively expressed in the enrichment culture. Homologous genes are mostly absent from the genomes of N. maritimus SCM1 and “Ca. C. symbiosum” A, but were identified in “Ca. N. limnia” sp. as well as in the moderate thermophile “Ca. N. gargensis”, and are typically clustered in a single region (Figure 3B) [38,53,54]. As observed for the genomes of “Ca. N. limnia” species [38,53], the novel genome harbours more than one copy of flaB. The exact number is unknown, because the respective gene fragments are located at contig ends (Figure 3B). It should, however, be noted that in “Ca. N. limnia” sp. the four flaB genes are clustered in one locus, suggesting that the gaps between the respective contigs in the strain N4 genome are likely to be only very small.
In the genome of strain N4, the flagella genes are co-localized with a gene cluster harbouring the essential gene set for chemotaxis (i.e. cheA, cheB, cheC, cheD, cheR, cheW, cheY; Figure 3B, Table S8 in File S1). Furthermore, the genome contains 13 putative histidine kinases as well as 8 response regulator-like proteins (Table S8 in File S1). Chemotaxis and motility likely are beneficial to AOA living in heterogeneous habitats where they are exposed to shifts in substrate concentrations and/or to detrimental conditions. In contrast, these features seem to be less important in habitats of AOA lacking such genes like the open ocean, where N. maritimus-like archaea reside [15,66,67], or sponge tissue in which “Ca. C. symbiosum” thrives . As most other genome-sequenced thaumarchaeotes (the only exception is "Ca. N. gargensis" Ga9.2) , strain N4 does not encode gas vesicles.
Potential cell division system
As other genome-sequenced thaumarchaeotes, the enriched AOA encodes homologues of both crenarchaeotal (cdvABC) and euryarchaeotal/bacterial (ftsZ) cell division machinery components (Table S9 in File S1) [5,69]. In N. maritimus the ESCRTIII-related Cdv-system has been demonstrated to be the primary division system, while the role of FtsZ remains unknown [70,71]. Recently, an additional distant tubulin homologue was identified in the genomes of each “Ca. N. limnia” SFB1 and “Ca. Nitrosoarchaeum koreensis”  and named “artubulin” . It was suggested that these hypothetical thaumarchaeotal proteins may be evolutionary ancestral to eukaryotic tubulin , but the functionality of this protein as well as its sub-cellular localization is yet untested. Interestingly, the genome of strain N4 also encodes an “artubulin”-like protein (Table S9 in File S1) with ~79% amino acid identity to the homologues of the Nitrosoarchaeum species. The predicted protein contains all amino acid residues that are conserved in the majority of tubulins including the proposed “artubulins”, but which are not shared by the majority of FtsZ sequences . However, in contrast to the Nitrosoarchaeum species, strain N4’s “artubulin”-like protein is not found in proximity to one of its Snf7/CdvB-encoding genes (Table S9 in File S1) [52,53,72].
Genomic plasticity of AOA
The obtained genome sequence was compared to the genomes of its closest relatives, N. maritimus SCM1, “Ca. N. limnia” SFB1 and “Ca. C. symbiosum” A, to search for regions of genomic plasticity (RGP) that mainly contain genes specific for the novel thaumarchaeote. This analysis revealed numerous RGP with a total length of ~503 kb (Figure S2). Most genes in these regions encode hypothetical proteins or proteins of unknown function and lack homologs in the other AOA genomes, suggesting that they might be involved in habitat-specific adaptations such as life at elevated temperatures. The comparative genomic analysis between strain N4 and N. maritimus SCM1 also showed that 1,196 coding sequences (CDS; 61.1%) of the novel thaumarchaeote and 1,205 CDS (67.1%) of N. maritimus SCM1 are organized in 106 syntenic regions (syntons) with an average length of 11 CDS. A genome-wide dot plot (Figure S3A) confirmed a high degree of genomic synteny between these two AOA, which was also found in comparison to “Ca. N. limnia” SFB1 (Figure S3B). When compared to “Ca. C. symbiosum” A, in total 157 syntons were detected that contained 1,113 CDS (56.8%) of the novel thaumarchaeote and 1,125 CDS (55.5%) of “Ca. C. symbiosum” A. However, these syntons were shorter with an average length of 7 CDS and much more scattered, with genome-scale synteny being very low (Figure S3C). A low overall synteny to “Ca. C. symbiosum” A has also been reported for genomes of other AOA of the Nitrosopumilus cluster [38,51], indicating that numerous genomic rearrangements must have occurred during the evolution of “Ca. C. symbiosum” whose lifestyle as sponge symbiont differs markedly from that of free-living AOA.
A novel thaumarchaeotal species
The phylogenetic analyses of four marker genes (Figure 2) indicate that the enriched archaeon represents a new species, which can clearly be distinguished from all previously described AOA. This gains strong support from average nucleotide identity (ANI) analyses, which were based on the genome sequences of this organism and of its closest sequenced relatives, N. maritimus SCM1 and "Ca. C. symbiosum" A. The obtained ANI values of 67.1% (compared to N. maritimus SCM1) and 64.8% (compared to "Ca. C. symbiosum" A) are far below the threshold of 95-96%, which corresponds to DNA-DNA hybridization values of 60-70% and has been suggested as the ANI boundary for circumscribing archaeal and bacterial species . Tetranucleotide signature frequency correlation coefficients, also inferred from these three genome sequences, were 0.58 (compared to N. maritimus SCM1) and 0.55 (compared to "Ca. C. symbiosum" A). In general, much higher correlation coefficients (>0.99) correspond to ANI values above 96% . Thus, multiple lines of evidence support that strain N4 is a new thaumarchaeotal species.
Provisional classification and conclusion
In this study we demonstrate that strain N4, which we obtained in our moderately thermophilic enrichment culture, is a thaumarchaeote of the Nitrosopumilus cluster that is responsible for the observed oxidation of ammonia. We propose the following Candidatus status for this archaeon: “Nitrosotenuis uzonensis” fam et. gen. et sp. nov.
Nitrosus (Latin masculine adjective), nitrous; tenuis (Latin masculine adjective), small/slender; uzonensis (Latin neutrum genitive), from Uzon.
A terrestrial thermal spring located in the Uzon caldera on the Kamchatka peninsula, Russia.
A chemolithoauotrophic ammonia oxidizer affiliated with the Nitrosopumilus cluster as defined by  of the phylum Thaumarchaeota within the domain Archaea.
In addition to “Ca. N. yellowstonii”  of the Nitrosocaldus cluster and “Ca. N. gargensis”  of the Nitrososphaera cluster, this archaeon is the third identified species of AOA growing at elevated temperatures. “Ca. Nitrosotenius uzonensis” is the first cultured representative of Nitrosopumilus-cluster AOA with worldwide distribution in terrestrial geothermal habitats. Furthermore, as evidenced by the phylogenetic clustering of our AOA with the recently cultivated strains “AOA-AC5” and “AOA-DW” , this phylogenetic clade is not confined to habitats with elevated temperature, but also occurs in freshwater sediments. Their impact on biogeochemical cycling in these systems, however, has yet to be determined.
Materials and Methods
An ammonia-oxidizing enrichment culture, inoculated with water and sediment from a terrestrial thermal spring located in the Uzon caldera on the Kamchatka peninsula (Russia), was established in 2006 and maintained for seven years. A temperature of 45°C and a pH of 6.5 were measured at the sampling site. The concentration of ammonium was 34.4 µM, whereas nitrite and nitrate were not detectable at the time of sampling . At an early stage of the enrichment, different incubation temperatures were tested (28-52°C) in parallel to determine the optimal conditions for ammonia oxidation. The culture was grown aerobically in static 300 ml Erlenmeyer flasks or static 250 ml (Schott AG, Mainz, Germany) flasks. The cells were grown in medium containing (per litre) 54.4 mg KH2PO4, 74.4 mg KCl, 49.3 mg MgSO4 ×7H2O, 584 mg NaCl, 33.8 µg MnSO4, 49.4 µg H3BO3×7H2O, 43.1 µg ZnSO4×7H2O, 37.1 µg (NH4)6Mo7O24×4H2O, 97.3 µg FeSO4×5H2O, and 25.0 µg CuSO4×2H2O. Furthermore, either 147 mg CaCl2 or 4.0 g CaCO3 L-1 (which partially precipitated) was added. At late stages of the enrichment, only CaCO3-based medium was used. Typically, fresh medium contained 1 mM NH4Cl. In the case of CaCl2-medium, the pH was adjusted to 7.4-7.8 by adding 1% (w/v) NaHCO3 solution. To further enrich for AOA, consecutive application of vancomycin (100 mg L-1) and streptomycin (50 mg L-1) was performed, which was followed by inoculation into fresh medium (10 vol%). Sodium salts of either formate, acetate, pyruvate, or succinate were added (20 mg L-1) to test whether strain N4 used these organic substrates. The enrichment culture was regularly transferred by inoculation of flasks containing fresh medium with 10 vol% of the culture. The concentrations of nitrite and nitrate were regularly measured by using Merckoquant test stripes (Merck, Vienna, Austria). For recording substrate turnover, ammonium, nitrite, and nitrate concentrations were precisely measured as described recently [22,74].
Amplification, cloning, sequencing, and phylogenetic analyses of 16S rRNA, amo, and hcd genes
DNA was extracted from enrichment culture N4 either by phenol/chloroform-extraction including a bead-beating step (30 s, 6 m/s; adapted from ) or by using the PowerSoil kit (MOBio Laboratories, Darmstadt, Germany) according to the instructions of the manufacturer. PCR mixtures contained 2 mM MgCl2 and 1 U of Taq-polymerase (Fermentas Life Sciences, St. Leon-Rot, Germany) in combination with 50 pmol of the respective oligonucleotide primers. In all PCR 30 cycles were used to amplify the target DNA and a final elongation step of 10 min at 72 °C was performed. A list of all primers with the applied annealing temperatures is provided in Table S1 in File S1. Amplification of bacterial amoA genes was attempted by using primers amoA1F and amoA2R , and a plasmid carrying an amoA gene of Nitrosomonas sp. as template was used as positive control. Cloning and sequencing were performed as described elsewhere . The cloned 16S rRNA and hcd genes were screened, prior to sequencing, by RFLP analysis using the restriction endonucleases MspI and AluI (16S rRNA) or RsaI (hcd) (Fermentas Life Sciences, St. Leon-Rot, Germany), whereas amoA and amoB clones were randomly chosen for sequencing without RFLP analysis. For each unique RFLP pattern at least one representative clone was sequenced. Phylogenetic analyses were conducted using the programs ARB  and Phylip  with comprehensive databases. Automatic tools included in ARB were used to align sequences to the respective in-house databases. All alignments were manually refined. A 16S rRNA consensus tree was reconstructed based on Maximum-Likelihood (ML) calculation (using the Hasegawa, Kishino and Yano substitution model) and by collapsing all nodes with parsimony bootstrap (100 iterations) support below 70%. A sequence filter considering only positions conserved in ≥50% of all thaumarchaeotal and crenarchaeotal sequences in our database was used (resulting in 1,360 alignment positions for the tree calculations) and only sequences ≥1,300 nucleotides in length were considered. Shorter sequences were added later via the “parsimony interactive” tool within ARB without changing the overall topology of the tree. For the analyses of AmoA (176 considered amino acids), AmoB (152 amino acids) and Hcd (125 amino acids) sequences, Fitch-Margoliash distance trees (7 jumbles, Kimura substitution model, randomized sequence order) were reconstructed using Phylip  without the use of filters. In addition, parsimony bootstrapping (1,000 iterations) analyses were conducted using ARB, and its values projected onto the Fitch tree.
FISH and CARD-FISH
For the in situ detection and visualization of bacterial and archaeal cells in enrichment culture N4, FISH and CARD-FISH were performed as described elsewhere  with a hybridization time of 3 h and the probes listed in Table S2 in File S1. Fluorescein- and Cy3-labelled tyramides were synthesized according to Pernthaler et al.  and diluted 1:1,000 in amplification buffer. After FISH or CARD-FISH, cells were stained with 4’,6’-diamidino-2-phenylindole (DAPI, 1 µg ml-1) and were microscopically analyzed using a Zeiss LSM 510 confocal laser scanning microscope and the included software. The absence of unspecific fluorescence after CARD-FISH was confirmed by using probe NON-EUB (Table S2 in File S1) that does not bind to any known organism.
Negative staining of whole cells was performed using 1% uranyl acetate in distilled water for 10-20 s. Micrographs were recorded using a JEM-100CX II transmission electron microscope (JEOL, Tokyo, Japan).
Metagenomic sequencing and analyses
For obtaining biomass for metagenome sequencing, culture N4 was grown aerobically in 300 ml Erlenmeyer flaks as described above. Biomass was harvested by centrifugation (11,000 rpm, 10 min, room temperature) and frozen (-20 °C) until phenol/chloroform-based DNA extraction (see above) was performed. The genomic DNA was submitted to mechanical fragmentation through nebulization (hydroshear) with a 3 kb mean fragment size. After recircularization using an adapter, the DNA was fragmented using an E210 ultrasound DNA-shearer (Covaris, Woburn, MA), and 600 bp fragments containing the adapter were selected for sequencing. Three quarters of a 454 Titanium mate-paired run were performed, generating ~250 Mb of sequence in 796,942 reads. In addition, Illumina (GA-IIx) single read sequencing was performed, generating 34,689,904 reads of 36 bp each. The 454-reads were subjected to assembly by using the Newbler software package, generating 739 contigs on 41 scaffolds with a cumulative size of ~5.5 Mb. The largest of these scaffolds, containing 14 contigs with a total length of 1,649,125 bp and a mean contig coverage of 39.4, represents the genome of strain N4. The Illumina reads were used to correct 454 sequencing errors as described by Aury et al. . Corrected contigs assembled using the scaffold description were used to generate the final sequence. The MaGe annotation platform (Vallenet et al., 2006) was used for CDS prediction, automatic annotation, and manual annotation refinement according to guidelines as recently described . Statistics about syntons in compared genomes were generated by the respective tools of MaGe, where the gap parameter, which represents the maximum number of consecutive genes that are not involved in a synton, was set to five genes. Regions of genomic plasticity were identified by the respective tool of MaGe based on synteny breaks in the compared genomes and features of potential lateral gene transfer events, such as tRNA hotspots and DNA compositional biases, in the genome of strain N4. Genome-scale dot plots (Figure S3) were generated by using the PROmer and mummerplot programs contained in the MUMmer software package (version 3.22)  in combination with Gnuplot (version 4.4.3). The circular genome map (Figure S2) was generated using the software Circos (version 0.54) . Average nucleotide identity (ANI) values were calculated, based on whole-genome sequences of AOA and on the BLAST algorithm, by using the software JSpecies  with the default parameters. The same software was applied to determine tetranucleotide signature frequency correlation coefficients for the AOA genomes.
The genome sequence of “Ca. Nitrosotenuis uzonensis” has been deposited at the European Nucleotide Archive with the master reference number CBTY000000000.
Phylogenetic analysis of a selection of AmoA sequences obtained from geothermal sites that are closely related to the sequence of “Ca. Nitrosotenuis uzonensis”. The tree shows sequences affiliated with the Nitrosopumilus cluster, while sequences belonging to the Nitrososphaera, Nitrosotalea and Nitrosocaldus clusters have been used as outgroup. If available, temperature, pH and sample type are indicated for clones obtained from geothermal systems (in red font). Circles on tree nodes indicate parsimony bootstrap support ≥90%. Numbers in parentheses indicate the number of sequences within a group. The scale bar equals 10% estimated sequence divergence.
Circular representation of the “Ca. N. uzonensis” chromosome. Contigs are separated by white space in all rings. Predicted coding sequences (rings 1+2), RNA genes (ring 3), regions of genomic plasticity compared to N. maritimus SCM1 (ring 4) or “Ca. Cenarchaeum symbiosum” (ring 5), and local nucleotide composition measures (rings 6+7) are shown. Very short features were enlarged to enhance visibility.
Dot plots representing genome-wide alignments of “Ca. Nitrosotenuis uzonensis” to the genomes of (A) Nitrosopumilus maritimus SCM1, (B) “Ca. Nitrosoarchaeum limnia” SFB1, and (C) “Ca. Cenarchaeum symbiosum” A. Forward matches are shown in red, while reverse matches are shown in blue.
Combined file containing tables S1-S10.
We thank Valery Galchenko for providing samples from the terrestrial thermal spring, Christian Baranyi, Faris Behnam, Nadezda A. Kostrikina, and Gabriele Schwammel for help in the lab, Thomas Rattei for support with bioinformatic analyses, and Anja Spang for helpful discussions.
Conceived and designed the experiments: EVL RH HD MW. Performed the experiments: EVL RH EP NS SH AB NVG AG MS MP DLP. Analyzed the data: EVL RH NS SH AG MP MS HD MW. Contributed reagents/materials/analysis tools: EVL EP DLP HD MW. Wrote the manuscript: EVL RH HD MW.
- 1. Hatzenpichler R (2012) Diversity, physiology, and niche differentiation of ammonia-oxidizing archaea. Appl Environ Microbiol 78: 7501-7510. doi:10.1128/AEM.01960-12. PubMed: 22923400.
- 2. Schleper C, Nicol GW (2010) Ammonia-oxidising archaea - physiology, ecology and evolution. Adv Microb Physiol 57: 1-41. doi:10.1016/B978-0-12-381045-8.00001-1. PubMed: 21078440.
- 3. Stahl DA, de la Torre JR (2012) Physiology and diversity of ammonia-oxidizing archaea. Annu Rev Microbiol 66: 83-101. doi:10.1146/annurev-micro-092611-150128. PubMed: 22994489.
- 4. Brochier-Armanet C, Boussau B, Gribaldo S, Forterre P (2008) Mesophilic Crenarchaeota: proposal for a third archaeal phylum, the Thaumarchaeota. Nat Rev Microbiol 6: 245-252. doi:10.1038/nrmicro1852. PubMed: 18274537.
- 5. Spang A, Hatzenpichler R, Brochier-Armanet C, Rattei T, Tischler P et al. (2010) Distinct gene set in two different lineages of ammonia-oxidizing archaea supports the phylum Thaumarchaeota. Trends Microbiol 18: 331-340. doi:10.1016/j.tim.2010.06.003. PubMed: 20598889.
- 6. Mußmann M, Brito I, Pitcher A, Damste JSS, Hatzenpichler R et al. (2011) Thaumarchaeotes abundant in refinery nitrifying sludges express amoA but are not obligate autotrophic ammonia oxidizers. Proc Natl Acad Sci U S A 108: 16771-16776. doi:10.1073/pnas.1106427108. PubMed: 21930919.
- 7. Koops HP, Pommerening-Röser A (2001) Distribution and ecophysiology of the nitrifying bacteria emphasizing cultured species. FEMS Microbiol Ecol 37: 1-9. doi:10.1111/j.1574-6941.2001.tb00847.x.
- 8. Koops HP, Purkhold U, Pommerening-Röser A, Timmermann G, Wagner M (2003) The lithoautotrophic ammonia-oxidizing bacteria. In: D. Mea. The Procaryotes: An Evolving Electronic Resource for the Microbiological Community. Third edition. New York: Springer.
- 9. Adair KL, Schwartz E (2008) Evidence that ammonia-oxidizing archaea are more abundant than ammonia-oxidizing bacteria in semiarid soils of Northern Arizona, USA. Microb Ecol 56: 420-426. doi:10.1007/s00248-007-9360-9. PubMed: 18204798.
- 10. He JZ, Shen JP, Zhang LM, Zhu YG, Zheng YM et al. (2007) Quantitative analyses of the abundance and composition of ammonia-oxidizing bacteria and ammonia-oxidizing archaea of a Chinese upland red soil under long-term fertilization practices. Environ Microbiol 9: 2364-2374. doi:10.1111/j.1462-2920.2007.01358.x. PubMed: 17686032.
- 11. Leininger S, Urich T, Schloter M, Schwark L, Qi J et al. (2006) Archaea predominate among ammonia-oxidizing prokaryotes in soils. Nature 442: 806-809. doi:10.1038/nature04983. PubMed: 16915287.
- 12. Shen JP, Zhang LM, Zhu YG, Zhang JB, He JZ (2008) Abundance and composition of ammonia-oxidizing bacteria and ammonia-oxidizing archaea communities of an alkaline sandy loam. Environ Microbiol 10: 1601-1611. doi:10.1111/j.1462-2920.2008.01578.x. PubMed: 18336563.
- 13. Beman JM, Popp BN, Francis CA (2008) Molecular and biogeochemical evidence for ammonia oxidation by marine Crenarchaeota in the Gulf of California. ISME J 2: 429-441. doi:10.1038/ismej.2007.118. PubMed: 18200070.
- 14. Nakagawa T, Mori K, Kato C, Takahashi R, Tokuyama T (2007) Distribution of cold-adapted ammonia-oxidizing microorganisms in the deep-ocean of the Northeastern Japan Sea. Microbes Environ 22: 365-372. doi:10.1264/jsme2.22.365.
- 15. Wuchter C, Abbas B, Coolen MJ, Herfort L, van Bleijswijk J et al. (2006) Archaeal nitrification in the ocean. Proc Natl Acad Sci U S A 103: 12317-12322. doi:10.1073/pnas.0600756103. PubMed: 16894176.
- 16. Caffrey JM, Bano N, Kalanetra K, Hollibaugh JT (2007) Ammonia oxidation and ammonia-oxidizing bacteria and archaea from estuaries with differing histories of hypoxia. ISME J 1: 660-662. doi:10.1038/ismej.2007.79. PubMed: 18043673.
- 17. Park SJ, Park BJ, Rhee SK (2008) Comparative analysis of archaeal 16S rRNA and amoA genes to estimate the abundance and diversity of ammonia-oxidizing archaea in marine sediments. Extremophiles 12: 605-615. doi:10.1007/s00792-008-0165-7. PubMed: 18465082.
- 18. de la Torre JR, Walker CB, Ingalls AE, Könneke M, Stahl DA (2008) Cultivation of a thermophilic ammonia oxidizing archaeon synthesizing crenarchaeol. Environ Microbiol 10: 810–818. doi:10.1111/j.1462-2920.2007.01506.x. PubMed: 18205821.
- 19. Jiang H, Huang Q, Dong H, Wang P, Wang F et al. (2010) RNA-based investigation of ammonia-oxidizing archaea in hot springs of Yunnan Province, China. Appl Environ Microbiol 76: 4538-4541. doi:10.1128/AEM.00143-10. PubMed: 20435758.
- 20. Reigstad LJ, Richter A, Daims H, Urich T, Schwark L et al. (2008) Nitrification in terrestrial hot springs of Iceland and Kamchatka. FEMS Microbiol Ecol 64: 167–174. doi:10.1111/j.1574-6941.2008.00466.x. PubMed: 18355293.
- 21. Dodsworth JA, McDonald AI, Hedlund BP (2012) Calculation of total free energy yield as an alternative approach for predicting the importance of potential chemolithotrophic reactions in geothermal springs. FEMS Microbiol Ecol 81: 446-454. doi:10.1111/j.1574-6941.2012.01369.x. PubMed: 22443686.
- 22. Hatzenpichler R, Lebedeva EV, Spieck E, Stoecker K, Richter A et al. (2008) A moderately thermophilic ammonia-oxidizing crenarchaeote from a hot spring. Proc Natl Acad Sci U S A 105: 2134-2139. doi:10.1073/pnas.0708857105. PubMed: 18250313.
- 23. Spear JR, Barton HA, Robertson CE, Francis CA, Pace NR (2007) Microbial community biofabrics in a geothermal mine adit. Appl Environ Microbiol 73: 6172-6180. doi:10.1128/AEM.00393-07. PubMed: 17693567.
- 24. Weidler GW, Gerbl FW, Stan-Lotter H (2008) Crenarchaeota and their role in the nitrogen cycle in a subsurface radioactive thermal spring in the Austrian Central Alps. Appl Environ Microbiol 74: 5934-5942. doi:10.1128/AEM.02602-07. PubMed: 18723663.
- 25. Zhang T, Jin T, Yan Q, Shao M, Wells G et al. (2009) Occurrence of ammonia-oxidizing archaea in activated sludges of a laboratory scale reactor and two wastewater treatment plants. J Appl Microbiol 107: 970-977. doi:10.1111/j.1365-2672.2009.04283.x. PubMed: 19486399.
- 26. Zhao W, Song Z, Jiang H, Li W, Mou X et al. (2011) Ammonia-oxidzing archaea in Kamchatka hot springs. Geomicrobiol J 28: 149-159. doi:10.1080/01490451003753076.
- 27. Dodsworth JA, Hungate BA, Hedlund BP (2011) Ammonia oxidation, denitrification and dissimilatory nitrate reduction to ammonium in two US Great Basin hot springs with abundant ammonia-oxidizing archaea. Environ Microbiol 13: 2371-2386. doi:10.1111/j.1462-2920.2011.02508.x. PubMed: 21631688.
- 28. Wang F, Zhou H, Meng J, Peng X, Jiang L et al. (2009) GeoChip-based analysis of metabolic diversity of microbial communities at the Juan de Fuca Ridge hydrothermal vent. Proc Natl Acad Sci U S A 106: 4840-4845. doi:10.1073/pnas.0810418106. PubMed: 19273854.
- 29. Wang S, Xiao X, Jiang L, Peng X, Zhou H et al. (2009) Diversity and abundance of ammonia-oxidizing archaea in hydrothermal vent chimneys of the juan de fuca ridge. Appl Environ Microbiol 75: 4216-4220. doi:10.1128/AEM.01761-08. PubMed: 19395559.
- 30. Zhang CL, Ye Q, Huang ZY, Li WJ, Chen JQ et al. (2008) Global occurrence of archaeal amoA genes in terrestrial hot springs. Appl Environ Microbiol 74: 6417-6426. doi:10.1128/AEM.00843-08. PubMed: 18676703.
- 31. Pitcher A, Hopmans EC, Mosier AC, Park S-J, Rhee S-K et al. (2011) Core and intact polar glycerol dibiphytanyl glycerol tetraether lipids of ammonia-oxidizing archaea enriched from marine and estuarine sediments. Appl Environ Microbiol 77: 3468-3477. doi:10.1128/AEM.02758-10. PubMed: 21441324.
- 32. Schouten S, Hopmans EC, Baas M, Boumann H, Standfest S et al. (2008) Intact membrane lipids of Candidatus "Nitrosopumilus maritimus", a cultivated representative of the cosmopolitan mesophilic Group I Crenarchaeota. Appl Environ Microbiol 74: 2433-2440. doi:10.1128/AEM.01709-07. PubMed: 18296531.
- 33. Pitcher A, Rychlik N, Hopmans EC, Spieck E, Rijpstra WI, et al. (2009) Crenarchaeol dominates the membrane lipids of Candidatus Nitrososphaera gargensis, a thermophilic Group I.1b Archaeon. ISME J 4: 542–552. doi: 10.1038/ismej.2009.138
- 34. Pearson A, Pi YD, Zhao WD, Li WJ, Li YL et al. (2008) Factors controlling the distribution of archaeal tetraethers in terrestrial hot springs. Appl Environ Microbiol 74: 3523-3532. doi:10.1128/AEM.02450-07. PubMed: 18390673.
- 35. Pearson A, Huang Z, Ingalls AE, Romanek CS, Wiegel J et al. (2004) Nonmarine crenarchaeol in Nevada hot springs. Appl Environ Microbiol 70: 5229-5237. doi:10.1128/AEM.70.9.5229-5237.2004. PubMed: 15345404.
- 36. Pitcher A, Schouten S, Damste JSS (2009) In situ production of crenarchaeol in two California hot springs. Appl Environ Microbiol 75: 4443-4451. doi:10.1128/AEM.02591-08. PubMed: 19411420.
- 37. Schouten S, van der Meer MT, Hopmans EC, Rijpstra WI, Reysenbach AL et al. (2007) Archaeal and bacterial glycerol dialkyl glycerol tetraether lipids in hot springs of Yellowstone National Park (USA). Appl Environ Microbiol 73: 6181-6191. doi:10.1128/AEM.00630-07. PubMed: 17693566.
- 38. Blainey PC, Mosier AC, Potanina A, Francis CA, Quake SR (2011) Genome of a low-salinity ammonia-oxidizing archaeon determined by single-cell and metagenomic analysis. PLOS ONE 6: e16626. doi:10.1371/journal.pone.0016626. PubMed: 21364937.
- 39. French E, Kozlowski JA, Mukherjee M, Bullerjahn G, Bollmann A (2012) Ecophysiological characterization of ammonia-oxidizing archaea and bacteria from freshwater. Appl Environ Microbiol 78: 5773-6780. doi:10.1128/AEM.00432-12. PubMed: 22685142.
- 40. Jung MY, Park SJ, Min D, Kim JS, Rijpstra WI et al. (2011) Enrichment and characterization of an autotrophic ammonia-oxidizing archaeon of mesophilic crenarchaeal group I.1a from an agricultural soil. Appl Environ Microbiol 77: 8635–8647. doi:10.1128/AEM.05787-11. PubMed: 22003023.
- 41. Könneke M, Bernhard AE, de la Torre JR, Walker CB, Waterbury JB et al. (2005) Isolation of an autotrophic ammonia-oxidizing marine archaeon. Nature 437: 543-546. doi:10.1038/nature03911. PubMed: 16177789.
- 42. Lehtovirta-Morley LE, Stoecker K, Vilcinskas A, Prosser JI, Nicol GW (2011) Cultivation of an obligate acidophilic ammonia oxidizer from a nitrifying acid soil. Proc Natl Acad Sci U S A 108: 15892-15897. doi:10.1073/pnas.1107196108. PubMed: 21896746.
- 43. Mosier AC, Allen EE, Kim M, Ferriera S, Francis CA (2012) Genome sequence of "Candidatus Nitrosopumilus salaria" BD31, an ammonia-oxidizing archaeon from the San Francisco Bay estuary. J Bacteriol 194: 2121-2122. doi:10.1128/JB.00013-12. PubMed: 22461555.
- 44. Tourna M, Stieglmeier M, Spang A, Könneke M, Schintlmeister A et al. (2011) Nitrososphaera viennensis, an ammonia oxidizing archaeon from soil. Proc Natl Acad Sci U S A 108: 8420-8425. doi:10.1073/pnas.1013488108. PubMed: 21525411.
- 45. Lebedeva EV, Off S, Zumbrägel S, Kruse M, Shagzhina A et al. (2011) Isolation and characterization of a moderately thermophilic nitrite-oxidizing bacterium from a geothermal spring. FEMS Microbiol Ecol 75: 195-204. doi:10.1111/j.1574-6941.2010.01006.x. PubMed: 21138449.
- 46. Ellen AF, Zolghadr B, Driessen AM, Albers SV (2010) Shaping the archaeal cell envelope. Archaea doi:10.1155/2010/608243.
- 47. Jeanthon C, L'Haridon S, Reysenbach AL, Corre E, Vernet M et al. (1999) Methanococcus vulcanius sp. nov., a novel hyperthermophilic methanogen isolated from East Pacific Rise, and identification of Methanococcus sp. DSM 4213T as Methanococcus fervens sp. nov. Int J Syst Bacteriol 49 2: 583-589. doi:10.1099/00207713-49-2-583. PubMed: 10319479.
- 48. Pester M, Rattei T, Flechl S, Gröngröft A, Richter A et al. (2012) amoA-based consensus phylogeny of ammonia-oxidizing archaea and deep sequencing of amoA genes from soils of four different geographic regions. Environ Microbiol 14: 525-539. doi:10.1111/j.1462-2920.2011.02666.x. PubMed: 22141924.
- 49. Weidler GW, Dornmayr-Pfaffenhuemer M, Gerbl FW, Heinen W, Stan-Lotter H (2007) Communities of Archaea and Bacteria in a subsurface radioactive thermal spring in the Austrian central alps, and evidence of ammonia-oxidizing Crenarchaeota. Appl Environ Microbiol 73: 259-270. doi:10.1128/AEM.01570-06. PubMed: 17085711.
- 50. Berg IA, Kockelkorn D, Buckel W, Fuchs G (2007) A 3-hydroxypropionate/4-hydroxybutyrate autotrophic carbon dioxide assimilation pathway in archaea. Science 318: 1782-1786. doi:10.1126/science.1149976. PubMed: 18079405.
- 51. Walker CB, de la Torre JR, Klotz MG, Urakawa H, Pinel N et al. (2010) Nitrosopumilus maritimus genome reveals unique mechanisms for nitrification and autotrophy in globally distributed marine crenarchaea. Proc Natl Acad Sci U S A 107: 8818-8823. doi:10.1073/pnas.0913533107. PubMed: 20421470.
- 52. Kim BK, Jung MY, Yu DS, Park SJ, Oh TK et al. (2011) Genome sequence of an ammonia-oxidizing soil archaeon, "Candidatus Nitrosoarchaeum koreensis" MY1. J Bacteriol 193: 5539-5540. doi:10.1128/JB.05717-11. PubMed: 21914867.
- 53. Mosier AC, Allen EE, Kim M, Ferriera S, Francis CA (2012) Genome sequence of "Candidatus Nitrosoarchaeum limnia" BG20, a low-salinity ammonia-oxidizing archaeon from the San Francisco Bay estuary. J Bacteriol 194: 2119-2120. doi:10.1128/JB.00007-12. PubMed: 22461554.
- 54. Spang A, Poehlein A, Offre P, Zumbrägel S, Haider S et al. (2012) The genome of the ammonia-oxidizing Candidatus Nitrososphaera gargensis: Insights into metabolic versatility and environmental adaptations. Environ Microbiol 14: 3122–3145. doi:10.1111/j.1462-2920.2012.02893.x. PubMed: 23057602.
- 55. Bartossek R, Spang A, Weidler G, Lanzen A, Schleper C (2012) Metagenomic analysis of ammonia-oxidizing archaea affiliated with the soil group. Front Microbiol 3: 208. PubMed: 22723795.
- 56. Hallam SJ, Mincer TJ, Schleper C, Preston CM, Roberts K et al. (2006) Pathways of carbon assimilation and ammonia oxidation suggested by environmental genomic analyses of marine Crenarchaeota. PLoS Biol 4: e95. doi:10.1371/journal.pbio.0040095. PubMed: 16533068.
- 57. Offre P, Nicol GW, Prosser JI (2011) Community profiling and quantification of putative autotrophic thaumarchaeal communities in environmental samples. Environ Microbiol Rep 3: 245-253. doi:10.1111/j.1758-2229.2010.00217.x. PubMed: 23761257.
- 58. Pratscher J, Dumont MG, Conrad R (2011) Ammonia oxidation coupled to CO2 fixation by archaea and bacteria in an agricultural soil. Proc Natl Acad Sci U S A 108: 4170-4175. doi:10.1073/pnas.1010981108. PubMed: 21368116.
- 59. Zhang LM, Offre PR, He JZ, Verhamme DT, Nicol GW et al. (2010) Autotrophic ammonia oxidation by soil thaumarchaea. Proc Natl Acad Sci U S A 107: 17240-17245. doi:10.1073/pnas.1004947107. PubMed: 20855593.
- 60. Berg IA (2011) Ecological aspects of distribution of different autotrophic CO2 fixation pathways. Appl Environ Microbiol 77: 1925-1936. doi:10.1128/AEM.02473-10. PubMed: 21216907.
- 61. Yakimov MM, La Cono V, Denaro R (2009) A first insight into the occurrence and expression of functional amoA and accA genes of autotrophic and ammonia oxidizing bathypelagic Crenarchaeota of Tyrrhenian Sea. Deep Sea Res Part II Top Stud Oceanogr 56: 748–754. doi:10.1016/j.dsr2.2008.07.024.
- 62. Deppenmeier U (2002) Redox-driven proton translocation in methanogenic archaea. Cell Mol Life Sci 59: 1513-1533. doi:10.1007/s00018-002-8526-3. PubMed: 12440773.
- 63. Hasan MR, Rahman M, Jaques S, Purwantini E, Daniels L (2010) Glucose 6-phosphate accumulation in mycobacteria: implications for a novel F420-dependent anti-oxidant defense system. J Biol Chem 285: 19135-19144. doi:10.1074/jbc.M109.074310. PubMed: 20075070.
- 64. Purwantini E, Daniels L (1996) Purification of a novel coenzyme F420-dependent glucose-6-phosphate dehydrogenase from Mycobacterium smegmatis. J Bacteriol 178: 2861-2866. PubMed: 8631674.
- 65. Reynolds PJ, Colleran E (1987) Evaluation and improvement of methods for coenzyme F420 analysis in anaerobic sludges. Journal of Microbiological Methods 7: 115-130. doi:10.1016/0167-7012(87)90032-7.
- 66. Francis CA, Roberts KJ, Beman JM, Santoro AE, Oakley BB (2005) Ubiquity and diversity of ammonia-oxidizing archaea in water columns and sediments of the ocean. Proc Natl Acad Sci U S A 102: 14683-14688. doi:10.1073/pnas.0506625102. PubMed: 16186488.
- 67. Labrenz M, Sintes E, Toetzke F, Zumsteg A, Herndl GJ et al. (2010) Relevance of a crenarchaeotal subcluster related to Candidatus Nitrosopumilus maritimus to ammonia oxidation in the suboxic zone of the central Baltic Sea. ISME J 4: 1496-1508. doi:10.1038/ismej.2010.78. PubMed: 20535219.
- 68. Preston CM, Wu KY, Molinski TF, DeLong EF (1996) A psychrophilic crenarchaeon inhabits a marine sponge: Cenarchaeum symbiosum gen. nov., sp. nov. Proc Natl Acad Sci U S A 93: 6241-6246. doi:10.1073/pnas.93.13.6241. PubMed: 8692799.
- 69. Lindås AC, Karlsson EA, Lindgren MT, Ettema TJ, Bernander R (2008) A unique cell division machinery in the Archaea. Proc Natl Acad Sci U S A 105: 18942–18946. doi:10.1073/pnas.0809467105. PubMed: 18987308.
- 70. Pelve EA, Lindås AC, Martens-Habbena W, de la Torre JR, Stahl DA et al. (2011) Cdv-based cell division and cell cycle organization in the thaumarchaeon Nitrosopumilus maritimus. Mol Microbiol 82: 555-566. doi:10.1111/j.1365-2958.2011.07834.x. PubMed: 21923770.
- 71. Ng K-H, Srinivas V, Srinivasan R, Balasubramanian R (2013) The CdvB, but not FtsZ, assembles into polymers. Archaea 2013. Available: http://dx.doi.org/10.1155/2013/104147.
- 72. Yutin N, Koonin EV (2012) Archaeal origins of tubulin. Biology Direct 7. doi:10.1186/1745-6150-1187-1110.
- 73. Richter M, Rosselló-Móra R (2009) Shifting the genomic gold standard for the prokaryotic species definition. Proc Natl Acad Sci U S A 106: 19126-19131. doi:10.1073/pnas.0906412106. PubMed: 19855009.
- 74. Bollmann A, French E, Laanbroek HJ (2011) Isolation, cultivation, and characterization of ammonia-oxidizing bacteria and archaea adapted to low ammonium concentrations. Methods Enzymol 486: 55-88. doi:10.1016/B978-0-12-381294-0.00003-1. PubMed: 21185431.
- 75. Lueders T, Manefield M, Friedrich MW (2004) Enhanced sensitivity of DNA- and rRNA-based stable isotope probing by fractionation and quantitative analysis of isopycnic centrifugation gradients. Environ Microbiol 6: 73-78. PubMed: 14686943.
- 76. Rotthauwe JH, Witzel KP, Liesack W (1997) The ammonia monooxygenase structural gene amoA as a functional marker: molecular fine-scale analysis of natural ammonia-oxidizing populations. Appl Environ Microbiol 63: 4704-4712. PubMed: 9406389.
- 77. Ludwig W, Strunk O, Westram R, Richter L, Meier H et al. (2004) ARB: a software environment for sequence data. Nucleic Acids Res 32: 1363-1371. doi:10.1093/nar/gkh293. PubMed: 14985472.
- 78. Felsenstein J (1993) PHYLIP (Phylogeny Interference Package) version 3.5c. Department of Genetics, University of Washington, Seattle: distributed by the author.
- 79. Pernthaler A, Pernthaler P, Amann R (2004) Sensitive multi-color flourescence in situ hybridization for the identification of environmental microorganisms. Molecular Microbial Ecology Manual. 2 ed. Boston: Kluwer Academic Publishers. pp. 711-726.
- 80. Aury JM, Cruaud C, Barbe V, Rogier O, Mangenot S et al. (2008) High quality draft sequences for prokaryotic genomes using a mix of new sequencing technologies. BMC Genomics 9: 603. doi:10.1186/1471-2164-9-603. PubMed: 19087275.
- 81. Lücker S, Wagner M, Maixner F, Pelletier E, Koch H et al. (2010) A Nitrospira metagenome illuminates the physiology and evolution of globally important nitrite-oxidizing bacteria. Proc Natl Acad Sci U S A 107: 13479-13484. doi:10.1073/pnas.1003860107. PubMed: 20624973.
- 82. Kurtz S, Phillippy A, Delcher AL, Smoot M, Shumway M et al. (2004) Versatile and open software for comparing large genomes. Genome Biol 5: R12. doi:10.1186/gb-2004-5-6-p12. PubMed: 14759262.
- 83. Krzywinski M, Schein J, Birol I, Connors J, Gascoyne R et al. (2009) Circos: an information aesthetic for comparative genomics. Genome Res 19: 1639-1645. doi:10.1101/gr.092759.109. PubMed: 19541911.