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Volume 2012 (2012), Article ID 843539, 23 pages
Low Rates of Lateral Gene Transfer among Metabolic Genes Define the Evolving Biogeochemical Niches of Archaea through Deep Time
Department of Geosciences, University of Montana, 32 Campus Drive no. 1296, Missoula, MT 59812-1296, USA
Received 31 May 2012; Revised 2 September 2012; Accepted 2 October 2012
Academic Editor: Yoshizumi Ishino
Copyright © 2012 Carrine E. Blank. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
Phylogenomic analyses of archaeal genome sequences are providing windows into the group’s evolutionary past, even though most archaeal taxa lack a conventional fossil record. Here, phylogenetic analyses were performed using key metabolic genes that define the metabolic niche of microorganisms. Such genes are generally considered to have undergone high rates of lateral gene transfer. Many gene sequences formed clades that were identical, or similar, to the tree constructed using large numbers of genes from the stable core of the genome. Surprisingly, such lateral transfer events were readily identified and quantifiable, occurring only a relatively small number of times in the archaeal domain of life. By placing gene acquisition events into a temporal framework, the rates by which new metabolic genes were acquired can be quantified. The highest lateral transfer rates were among cytochrome oxidase genes that use oxygen as a terminal electron acceptor (with a total of 12–14 lateral transfer events, or 3.4–4.0 events per billion years, across the entire archaeal domain). Genes involved in sulfur or nitrogen metabolism had much lower rates, on the order of one lateral transfer event per billion years. This suggests that lateral transfer rates of key metabolic proteins are rare and not rampant.
Although there are still active debates over the extent of lateral gene transfer (LGT) in prokaryotic genomes , phylogenomic analyses using large sets of slowly evolving universally present genes have been producing an increasingly clearer picture of the core evolutionary signal in prokaryotic genomes, particularly for the archaeal domain of life [2, 3]. The actual rates of lateral gene transfer (in terms of number of events per billion years) are largely unknown, yet there is a growing recognition that lateral transfer among some sets of genes, particularly metabolic genes, appears to be higher than in other sets of genes [4–7]. Such lateral transfer events have no doubt led to the acquisition of new traits that help to redefine the metabolic niche of microorganisms, and these events have therefore had a profound influence on the evolving biogeochemical cycles on the Earth [8, 9]. Previous work on the archaeal domain of life has suggested an emerging evolutionary conservation between the habitat preference and metabolic traits . These niches have been changing through deep time as biogeochemical cycles gradually became more complex, particularly once oxygen became available in the biosphere.
This work is set about explicitly quantifying the rate of lateral gene acquisition events amongst key metabolic genes in the archaeal domain of life, using a phylogenetic approach. Phylogenetic trees of metabolic genes were constructed, and clades that were congruent with the slowly evolving core phylogenomic signal were identified in order to quantify the number of lateral gene transfer events (gains in new metabolic traits) for each gene. Inferred node ages were then used to identify when, in deep time, new metabolic traits could have been acquired via lateral gene transfer. This study shows that lateral transfer rates were highest among the genes using oxygen as a terminal electron acceptor, and lowest amongst genes involved in redox reactions between sulfur and sulfide. Nevertheless, the overall rate of metabolic gene acquisition in the archaeal domain appears to have been low—with cytochrome oxidase having the highest average rate of 3.4–4.0 events per billion years.
2.1. Concatenated Genomic Phylogeny, Node Ages, and Ancestral State Reconstruction
The methods for calculating the genomic tree and converting the branch lengths to ages have been published in detail elsewhere [10, 11]. In brief, the backbone genomic tree topology for the archaeal domain of life was calculated with Bayesian and maximum parsimony methods using a concatenated genomic dataset containing 98 protein and 2 ribosomal RNA sequences. The genomic dataset contained 119 taxa from cultured representatives of the Crenarchaeota and Euryarchaeota. The dataset contained a diverse suite of protein and ribosomal RNA sequences that sampled the core functioning of the cell. Ribosomal RNA sequences were aligned using secondary structure in order to align homologous nucleotides . Protein sequences were aligned using CLUSTALW  and hand edited in Se-Al , and character sets were defined such that only unambiguously aligned regions were used to construct the phylogenetic trees. Bayesian trees were calculated using MrBayes (v. 3.1.2 and 3.2.1; ) and maximum parsimony trees using PAUP* . These trees formed the core set of branching relationships that defined the consensus genome tree.
In order to scale branch lengths to time in Figure 1, branch lengths for the tree were estimated with the maximum likelihood method in PAUP*, using the large and small ribosomal RNA sequences, were the maximum likelihood parameters (pinvar, gamma distribution, nucleotide frequencies, and the substitution rate matrix) were estimated from the data using the model. The genome tree (calculated using all 100 protein and rRNA sequences) was used as a backbone constraint tree. Branch lengths were then converted to geologic ages using the penalized likelihood method in r8s [17, 18] using multiple age constraints. The maximum and minimum ages of the root of the archaeal domain were set at 3.8 Ga and 2.7 Ga, and the minimum age of the Euryarchaeota was 2.7 Ga . Oxygen age constraints were used to constrain the maximum age (2.32 Ga) of the Thermoplasmatales, Sulfolobales, Thermoproteales, Pyrobaculum-Thermoproteus, and the Halobacteriales . The oxygen age constraint of 2.32 Ga (the time by which free oxygen appeared in the atmosphere) was applied for archaeal clades that have the ability to use oxygen as a terminal electron acceptor, likely had an ancestor that metabolized oxygen, had an ancestor with a likely gene for metabolizing oxygen, and lived in an environment where cyanobacteria (a local source of oxygen) could not have been present. Chitin maximum age constraints (1.0 Ga, when chitin first appeared in the biosphere) were set for the Halobacteriales and Thermococcales, and the lignin maximum age constraints (475 Ma, when lignin from land plants first appeared) were set for the Sulfolobus solfataricus-Sulfolobus islandicus clade . Chitin maximum age constraints were applied for clades that currently have the ability to metabolize chitin and that likely had an ancestor with the ability to metabolize chitin. Lignin maximum age constraints were applied for clades that currently have the ability to metabolize phenolic compounds derived from lignin and that likely had an ancestor with the ability to metabolize phenolic compounds derived from lignin. The presence of cytochrome oxidase subunit I (or subunit I+III) was coded in Mesquite v. 2.75  such that of cytochrome oxidase in the genome and . Ancestral state reconstruction was performed in Mesquite using the likelihood method MK1 model, using the tree where branch lengths were scaled according to geologic time (Figure 1). Such an analysis shows the estimated geologic time where archaeal clades have acquired the ability to metabolize oxygen using a cytochrome oxidase gene. Such nodes are strong candidates for acquisition of metabolic genes via the process of lateral gene transfer.
2.2. Functional Gene Phylogenies and Topology Tests
The metabolic genes chosen for this study were a subset of those that play fundamental roles in the biogeochemical cycling of oxygen, sulfur, nitrogen, and carbon through the biosphere. Phylogenetic trees of metabolic genes were constructed by obtaining protein sequences from microbial genome sequences in GenBank using TBLASTN against the NCBI Chromosome and WGS databases. Database searches began using metabolic genes with demonstrated biochemical activity (from either bacteria or archaea, where available) and homologs were obtained from GenBank using TBLASTN against the nonredundant database. Orthology assessment was made using a pairwise orthology approach . Genes sequences were chosen if they showed BLAST scores that were significantly better than the highest scores to other annotated orthologs or genes with a different demonstrated biochemical activity. Next, phylogenetic trees of metabolic protein alignments were carried out using Clustal W, hand edited, and exported as nexus files, and phylogenetic trees were constructed using the maximum parsimony method in PAUP* v. 4.0b10  and the Bayesian method in MrBayes v.3.1.2 and 3.2.1 . Congruence testing of nitrogenase topologies was carried out using the approximately unbiased (AU) test in CONSEL , where site likelihoods were calculated with MrBayes.
2.3. Quantifying Lateral Transfer Rates
Candidate lateral gene transfer events (in this study, the acquisition of novel metabolic genes) were first identified using ancestral state reconstruction. Potential lateral transfer events can be identified if a clade has an ancestor that likely lacked a particular trait and then later gained the trait higher up in tree (e.g., cytochrome oxidase subunit I in Figure 1). Next, transfer events were confirmed if phylogenetic analysis of the protein sequencing underlying the trait exhibited moderately or well-supported branching relationships (as determined by bootstrap analyses or posterior probabilities greater than 70%) that were inconsistent with the concatenated genomic phylogeny. Relationships within clades were also examined; clades with internal relationships consistent with the genome phylogeny, yet showing an alternative rooting (e.g., CoxA1 and CoxA3 in Figure 2(a)), were also considered to have likely undergone lateral gene transfer, possibly from a donor outside of the archaeal domain of life. Next, the position of each gene was examined in relation to other subunits in the enzyme, or in other enzymes in a pathway that could have been transferred in a single transfer event. Genomic positional linkages were noted so as to conservatively estimate lateral transfer rates. If two genes were located in an operon that coded for a multienzyme complex or proteins in the same metabolic pathway, they were likely acquired in a singular lateral transfer event.
The overall rates of lateral gene transfer for the archaeal domain of life were calculated by summing up the total number of inferred lateral transfer events (the gains of new metabolic genes involved in key biogeochemical cycles) over the estimated age of the archaeal domain of life. These inferred LGT acquisition rates are summed up for the entire domain of life, assuming that the domain is comprised of the 119 cultured archaeal taxa in the Crenarchaeota and Euryarchaeota that make up this study.
3. Results and Discussion
3.1. Genome Phylogeny, Ancestral State Reconstruction, and Relaxed Clock
Figure 1 is a phylogenetic tree constructed using a 100-gene concatenated dataset. The branch lengths are scaled to geologic time, using age constraints for the archaeal domain of life developed by Blank [11, 19], and the likelihood that the ancestral genomes have cytochrome oxidase is indicated on the nodes of the tree using ancestral state reconstruction. This approach inferred that the ancestor to the Halobacteriales likely contained cytochrome oxidase in its genome. It also infers a high likelihood that the ancestor to Ferroplasma-Picrophilus and the Sulfolobales contained cytochrome oxidase. There is a high likelihood that the ancestor to Thermoproteus-Pyrobaculum contained cytochrome oxidase, yet it is less likely that cytochrome oxidase traces further back in the Thermoproteales. This demonstrates how ancestral state reconstruction can be used to identify potential lateral gene transfer (LGT) events in terms of the acquisition of novel metabolic genes that help define the metabolic niche of an organism (in this case, aerobic respiration). Ultimately, however, to quantify the number of lateral transfer events, one must also closely examine the phylogenetic trees that underlie the trait in question in order to confirm the hypothesis that these ancestors likely did acquire the cytochrome oxidase gene.
3.2. Cytochrome Oxidase
In the Euryarchaeota, phylogenetic analysis of cytochrome oxidase subunit I (and the cytochrome oxidase I portion of genes with fused I and III subunits; Figure 2(a)) shows four well-supported clades. One clade is comprised of CoxAC (where cytochrome oxidase subunits I and III are fused) from Picrophilus and Ferroplasma (labeled as node 1 in the figure). Sequence characteristics and phylogenetic relationships show that these proteins belong to the Heme-copper oxygen reductase family A1 . This phylogenetic pattern, in addition to ancestral state reconstruction (Figure 1), suggests that CoxAC was likely gained by an LGT event in the ancestor to Picrophilus and Ferroplasma. Three additional clades of cytochrome oxidase were observed in the Halobacteriales: CoxA1 (subunit I, family A1, node 2), CoxA2 (concatenated subunits I and III, family B, node 3), and CoxA3 (subunit I, family B, node 4). Most branching relationships within and between the clades showed moderate to poor support (Figure 2(a)). Ancestral state reconstruction suggests the presence of a cytochrome oxidase in the ancestor of the Halobacteriales (Figure 1). Ancestral state reconstruction using each form of the cytochrome oxidase genes predicts CoxA1 and CoxA3 (but not CoxA2, not shown) in the Halobacteriales ancestor. Halobacterium spp. formed the basal branch in the Halobacteriales in the genome tree. However, in the cytochrome oxidase tree, Halobacterium branched higher up in the CoxA1 and CoxA3 clades, suggesting that both sets of genes were acquired by independent lateral transfer events from donors outside the Euryarchaeota. A global phylogenetic tree containing families A and B sequences from Bacteria and Archaea (not shown; [23, 24]) shows CoxA1 and CoxA2 falling in a well-supported clade within family A1, and CoxA3 branching within family B. CoxA1 and CoxA2 did not branch as sister taxa with internal relationships consistent with the genome tree, which would be expected if the two were related by ancient gene duplication. CoxA2 homologs had a limited taxonomic distribution—only being observed in Halorubrum, Haloterrigena, Haloarcula, Haloferax, and Halogeometricum. Thus, CoxA2 was likely gained by an LGT event in the ancestor of these species (after the Halobacterium lineage diverged from the main Halobacteriales line of descent). Finally, one sequence from Natronomonas pharaonis (node 5) was rather divergent, branching with Magnetospirillum outside of any of the other archaeal clades. This is consistent with a recent lateral gene transfer event. In sum, five LGT events in the Euryarchaeota can be proposed to explain the phylogenetic pattern for cytochrome oxidase I and III (within the set of euryarchaeal taxa included in this study; Table 1).
Phylogenetic analysis of cytochrome oxidase subunit II in the Euryarchaeota (Figure 2(b)) similarly resulted in four clades. One clade contained Picrophilus and Ferroplasma (node 2). Examination of the physical location of the CoxB with CoxAC genes in the Picrophilus genome showed that they were linked, separated in the genome by a single open reading frame. The same observation was found for Ferroplasma. Thus, the LGT event that led to the acquisition of CoxAC also led to the acquisition of CoxB in the ancestor to Picrophilus and Ferroplasma. Three additional clades (CoxB1, CoxB2, and CoxB3; nodes 2–4) were found containing Halobacteriales taxa. Most branching relationships within and between the clades also showed moderate to poor support. Homologs to CoxB1 and CoxB3 (but not CoxB2) were observed in the two Halobacterium species. Again, Halobacterium CoxB1 and CoxB3 are found high up in the clade. Most genes in the CoxA1 and CoxB1 clades were physically linked, as were the genes for CoxA2 and CoxB2 and CoxA3 and CoxB3. Thus, the three LGT events that led to the acquisition of CoxA1, CoxA2, and CoxA3 also likely led to the acquisition of CoxB1, CoxB2, and CoxB3. The CoxB3 in Natronomonas (node 5) was also physically linked in the genome to CoxA3, that suggesting these two genes were acquired in a single LGT event as well. In sum, the total number of inferred LGT events for cytochrome oxidase subunits in the Euryarchaeota taxa included in this study is five (Table 1).
Phylogenetic analysis of cytochrome oxidase in the Crenarchaeota (Figure 3(a)) was somewhat more complex. In the Thermoproteales, a fused CoxAC was found in Pyrobaculum calidifontis, P. oguniense, P. sp. 1860, P. aerophilum, and Thermoproteus uzoniensis (node 1). This protein falls under the Heme-copper oxygen reductase family A1 . Another copy, CoxA, was found in Pyrobaculum calidifontis, P. oguniense, P. sp. 1860, and P. aerophilum (node 2). This second copy, a member of family B, branched separately from the CoxAC clade. Another CoxA in the family B was found in Caldivirga (node 3); however, this sequence did not branch with CoxA sequences from closely related Pyrobaculum spp. A global phylogenetic tree containing families A and B sequences from Bacteria and Archaea (not shown; ) showed Pyrobaculum CoxAC sequences branched with Sulfolobales SoxM sequences and family A1 sequences from Bacteria. Pyrobaculum CoxA sequences branched in a distinct location in the tree, in a well-supported clade with Aeropyrum, Halobacteriales CoxA3, and a wide diversity of bacterial family B sequences. The Caldivirga sequence branched with a phylogenetically distinct group of bacterial family B sequences from the Firmicutes and Proteobacteria. Relationships within the Pyrobaculum species of both clades, nevertheless, are congruent with the genome phylogeny (Figure 1). Thus, the simplest explanation for the observed phylogenetic pattern is three independent LGT events in the Thermoproteales: CoxA in Caldivirga, CoxA in the ancestor to Pyrobaculum spp., and CoxAC in the ancestor to Pyrobaculum-Thermoproteus. Three LGT events in the Thermoproteales were also inferred for Caldivirga and Pyrobaculum spp. using ancestral state reconstruction (Figure 1).
Four clades of cytochrome oxidases were observed in the Sulfolobales, corresponding to SoxM (fused subunits I and III, family A1, node 4), SoxB (subunit I, family B, node 5), DoxB (subunit I, family B, node 6), and a distinct clade in Sulfolobus tokodaii and Metallosphaera spp. (FoxA, family B, node 7). SoxM branched sister to Pyrobaculum-Thermoproteus CoxAC (65% and 100% support using MP and MB, resp.). This sister group relationship was also strongly supported in the global phylogeny containing Archaea and Bacteria (not shown), consistent with one LGT gain in the ancestor to the Sulfolobales. SoxB and DoxB formed a poorly to moderately well-supported clade with Pyrobaculum and Aeropyrum CoxA. However, branching relationships between and within the clades were often poorly or moderately supported. It is likely that SoxB and DoxB arose by a single LGT event followed by an ancestral gene duplication event (with subsequent duplications in Metallosphaera and S. tokodaii), given that branching relationships and the rooting of these two clades are consistent with the genome phylogeny. Nevertheless, phylogenetic trees with crenarchaeal cytochrome oxidases, crenarchaeal family B cytochrome oxidases, and the global family B tree are unresolved, and therefore, it cannot be formally ruled out that SoxB and DoxB were obtained by two independent LGT events. The FoxA clade is a newly identified clade of Heme-copper oxygen reductases found in Sulfolobus tokodaii and Metallosphaera spp. Transcriptional studies show that these genes are expressed under Fe(II)-oxidizing conditions . Phylogenetic analysis shows that this sequence belongs to the family B of Heme-copper oxygen reductases; however, branching relationships between Sulfolobales SoxB, DoxB, and other archaeal cytochrome oxidases are unresolved (Figure 3(a), not shown). Thus, it is possible that FoxB arose by ancient gene duplication from a SoxB or DoxB ancestor, or it could have been gained independently via LGT. Thus, the minimal total number of LGT events involving cytochrome oxidases in the Sulfolobales is 2, while the maximum number of events is 4.
In the Desulfurococcales, CoxA and CoxAC (members of Heme copper oxygen reductase families B and A1, resp., nodes 8 and 9) were found in Aeropyrum pernix. Both branched with their respective homologs in distantly related Pyrobaculum, suggestive of two independent LGT events leading to two copies of cytochrome oxidase in Aeropyrum. This scenario is also predicted using ancestral state reconstruction (Figure 1). In summary, a minimum of 7 LGT events, and a maximum of 9, can be proposed to explain the phylogenetic pattern for cytochrome oxidase I and III in the Crenarchaeota (Table 1).
The phylogenetic tree for crenarchaeal cytochrome oxidase subunit II was similar to that for subunit I. Two clades containing Pyrobaculum spp. (PoxH and PoxB) were comprised of the same species, with similar branching relationships, to CoxAC and CoxA (nodes 1 and 2). The PoxH and PoxB genes were also physically linked to CoxA and CoxAC genes in the genome; thus, the two LGT events that likely led to the acquisition of CoxA and CoxAC in the ancestor to Pyrobaculum also led to the acquisition of PoxH and PoxB. The Caldivirga homolog branched separately from the Pyrobaculum clades, and this gene was physically linked to CoxA (evidence that the LGT event leading to the acquisition of Caldivirga CoxA also led to the acquisition of CoxB, node 3). In the Sulfolobales, two cytochrome oxidase subunit II clades were found (SoxA and SoxH, nodes 4 and 5). Again, branching relationships within the clades were only moderately or poorly supported; however, most of the genes for SoxA are physically linked to SoxB; thus, the LGT event leading to the acquisition of SoxB in the Sulfolobales also likely led to the acquisition of SoxA. Similarly, homologs in the SoxH clade are physically linked to SoxM; thus, the LGT leading to SoxM acquisition also likely transferred SoxH. Two Aeropyrum lineages are also seen in the cytochrome oxidase II tree, with branching relationships seen in the subunit I+III tree (nodes 8 and 9). One copy branched sister to the PoxH from Pyrobaculum and thus was likely acquired in the same LGT event that led to the acquisition of CoxA in Aeropyrum. The branching position of the second homolog was poorly supported. Nevertheless, this homolog is physically linked to the CoxAC gene in Pyrobaculum, and so it was most likely acquired in the same LGT event that led to the acquisition of CoxAC. In summary, seven LGT events can be proposed to explain the phylogenetic pattern for cytochrome oxidase II in the Crenarchaeota; however, these genes were obtained in the same LGT events that lead to the acquisition of cytochrome oxidase I and III.
3.3. Cytochrome bd-Type Quinol Oxidase
In the Euryarchaeota, cytochrome bd quinol oxidase subunit 1 fell into five clades (Figure 4(a)). The first clade (node 1) contained Thermococcus gammatolerans and T. sp. AM4, consistent with an LGT event in the ancestor to these closely related species. The second clade contained Halobacteriales taxa (node 2). Halobacterium in this clade branched high up in the clade, suggesting either that the LGT donor came from outside the Euryarchaeota or that euryarchaeal taxa higher up in the tree then became the donor for other euryarchaeal groups. The third clade (node 3) contained Methanosarcina acetivorans and M. barkeri, consistent with another LGT gain in the ancestor to these closely related species. The fourth clade (node 4) was comprised of two adjacent quinol oxidase copies in the Archaeoglobus fulgidus genome, suggestive of a single LGT gain followed by a gene duplication event. The fifth clade was comprised of Thermoplasmatales taxa (node 5). The phylogenetic pattern of duplicate copies in this clade is consistent with a single LGT gain followed by a gene duplication event in the ancestor to Thermoplasma spp. and a second duplication in the ancestor to Ferroplasma and Picrophilus. Ancestral state reconstruction (not shown) was consistent with five gains in the Euryarchaeota.
In the Euryarchaeota, cytochrome bd quinol oxidase subunit 2 fell into three clades (Figure 4(b)). The first clade (node 1) was comprised of Thermococcus gammatolerans and T. sp. AM4, the second (node 2) contained Halobacteriales taxa with branching relationships that were identical to those seen in the quinol oxidase 1 tree, and the third clade (node 3) contained Methanosarcina acetivorans and M. barkeri. Physical linkage between quinol oxidase 1 and 2 was observed for all euryarchaeal taxa; thus, the LGT events leading to the acquisition of quinol oxidase 1 in the Euryarchaeota also led to the simultaneous acquisition of quinol oxidase 2.
In the Crenarchaeota, two copies of cytochrome bd quinol oxidase 1, forming sister clades, were found in Hyperthermus, Acidilobus, and most Thermoproteales taxa (Figure 5, nodes 1 and 2). Additional copies also were found in Vulcanisaeta distributa and V. moutnovskia (node 3). Phylogenetic analyses of the Thermoproteales taxa showed that neither sister clade was rooted with Thermofilum (as seen in the genome phylogeny); however, analyses of each sister clade in isolation (not shown) resulted in a tree that was congruent with the genome phylogeny. While this appears to be consistent with two independent LGT events in the ancestor to the Thermoproteales, examination of the genome positioning shows that both copies of quinol oxidase 1 in the Thermoproteales are adjacent in the genome. Thus, the most parsimonious explanation is a single LGT event that transferred two tandem, but distantly related, copies of quinol oxidase into the ancestor of the Thermoproteales. Two tandem copies of quinol oxidase 1 were also seen in Hyperthermus and Acidilobus (nodes 4 and 5), both branching sister to Thermofilum. The most likely explanation is a single LGT event, possibly from Thermofilum, which transferred the two tandem copies into Hyperthermus-Acidilobus (it is unlikely that the ancestor to Hyperthermus-Acidilobus was the donor for the Thermoproteales quinol oxidases, since the Thermoproteales clade is significantly older; Figure 1). One additional LGT event likely led to the acquisition of the third quinol oxidase copy in Vulcanisaeta spp. (node 3). Ancestral state reconstruction (not shown) was consistent with three independent LGT events in the Crenarchaeota.
3.4. Dissimilatory Sulfite Reduction
DsrA and DsrB are related proteins that derived from an ancient gene duplication event . The phylogeny of DsrA and DsrB (Figure 6) shows two well-supported clades in the archaeal domain, one containing Archaeoglobus spp. (nodes 1 and 6) and the second containing Caldivirga, Vulcanisaeta, Pyrobaculum, and Thermoproteus species (nodes 2 and 7). Genomic positioning shows that DsrA is linked to DsrB in all species, and one copy of DsrA and DsrB is found in Caldivirga and Vulcanisaeta spp. However, three copies are found in most of the genomes of Pyrobaculum and Thermoproteus spp., all forming a monophyletic group (nodes 3–5 and 8–10). This suggests that multiple gene duplication events occurred involving DsrAB in the ancestor to the Pyrobaculum-Thermoproteus clade, followed by later gene losses in some taxa. Thus, two LGT events are postulated for DsrAB in the archaea: once in the Archaeoglobales and once early in history of the Thermoproteales (Table 2). This is consistent with ancestral state reconstruction of the presence of DsrAB (not shown).
3.5. Thiosulfate Oxidation
Thiosulfate sulfurtransferase (SseA) catalyzes the oxidation of thiosulfate to sulfite, while reducing cyanide to thiocyanate . The phylogeny of the alpha subunit in the Euryarchaeota (Figure 7(a)) showed two clades of methanogen sequences (nodes 1–4) and two clades of sequences from the Halobacteriales (nodes 5 and 6). Little is known about thiosulfate metabolism in halophilic archaea; however, growing evidence suggests that many strains are able to oxidize it to sulfite and subsequently reduced to sulfide [28, 29]. The four methanogen sequences were found in distantly related euryarchaeal lineages. This provides evidence for four independent LGT events in the methanogens and is consistent to the pattern observed by ancestral state reconstruction (not shown). The Halobacteriales thiosulfate sulfurtransferase fell into two clades (copies 1 and 2), neither of which was rooted with Halobacterium. The sequences from copy 1 were found to be immediately adjacent to sequences from copy 2, suggesting that the two copies have been inherited as a single unit. Ancestral state reconstruction shows a high likelihood that SseA was present in the ancestor of the Halobacteriales (not shown).
In the Crenarchaeota (Figure 7(b)), thiosulfate sulfurtransferase was found in one member of the Desulfurococcales (Aeropyrum), many Thermoproteales, and many of the Sulfolobales. Thiosulfate stimulates growth in Aeropyrum and Pyrobaculum oguniense [30, 31], can be oxidized by Pyrobaculum aerophilum , and serves as an electron acceptor in Caldivirga, Thermoproteus uzoniensis, and many Pyrobaculum spp. [33, 34]. A single LGT event most likely led to the acquisition of SseA in Aeropyrum (node 1). The Thermoproteales sequences fell into three clades, one containing Caldivirga and P. aerophilum (node 2), another clade containing Caldivirga, Vulcanisaeta distributa, Thermoproteus uzoniensis, and Pyrobaculum spp. (node 3), and a clade containing P. sp. 1860 (node 4). Two LGT events may have led to the acquisition of two distantly related SseA copies in the ancestor to Caldivirga and Pyrobaculum, with a third acquisition in P. sp. 1860. The Sulfolobales sequences fell into two clades (nodes 5 and 6), both of which were rooted with Metallosphaera. Thus, two LGT events likely led to the acquisition of two distantly related SseA copies in the ancestor to the Sulfolobales. The inferred number of LGT events of thiosulfate oxidation in both the Euryarchaeota and Crenarchaeota is 11.
3.6. Sulfur Oxidation and Reduction
Sulfur oxygenase reductase (SOR) catalyzes the aerobic disproportionation of sulfur into sulfide and bisulfite. SOR activity in the archaea has been demonstrated for a number of Sulfolobales taxa  and more recently in Acidianus tengchongensis . Homologs were also found in Sulfolobus tokodaii, S. metallicus, Acidianus, and Desulfurolobus. Phylogenetic analysis (Figure 8(a)) shows that these sequences all form a monophyletic group, and thus, SOR was likely gained in the Sulfolobales (node 1). In the Euryarchaeota, putative homologs to SOR were found in the genomes of Ferroplasma and Picrophilus (node 2). Given that these two species are closely related, it is likely that SOR was also acquired via LGT in the ancestor to these two taxa.
Sulfur reductase catalyzes the reduction of sulfur or polysulfide to hydrogen sulfide. In the archaeal domain, the SreABCDE gene cluster has been demonstrated in Acidianus to carry out the reduction of sulfur . Putative homologs have been found in the members of Sulfolobus species (node 1). Their phylogenetic relationships (Figure 8(b)) were congruent with the genome phylogeny; thus, sulfur reductase was likely acquired in the ancestor to the Sulfolobales.
Flavocytochrome c sulfide dehydrogenase (FCSD) in Bacteria results in the anaerobic oxidation of sulfide to sulfur. Homologs to this FCSD have been identified in a number of Archaea (including Ignicoccus, Caldivirga, Pyrobaculum, Vulcanisaeta, Thermoproteus, Metallosphaera, Acidianus, and Sulfolobus tokodaii); however, FCSD activity has yet to be demonstrated in the archaeal domain. Phylogenetic analysis shows that archaeal FCSD forms a monophyletic group (node 1, Figure 8(c)) with a sister group relationship with bacterial proteins with demonstrated FCSD activity. Sequences from the Thermoproteales taxa Caldivirga, Pyrobaculum, Thermoproteus, and Vulcanisaeta formed a monophyletic group (node 2), with branching relationships consistent with the genome phylogeny, and ancestral state reconstruction predicted the presence of this gene in the ancestor of these taxa. An FCSD homolog was also found in Ignicoccus—this was likely gained by an independent LGT event (node 3). Similarly, the FCSD homolog in Acidianus, Metallosphaera, and Sulfolobus tokodaii formed a monophyletic group (node 4), so their common ancestor also likely gained this gene by LGT.
Sulfide quinone oxidoreductase (SQO) also catalyzes the anaerobic oxidation of sulfide to sulfur and shows sequence similarity to FCSD as well as to a large number of widely distributed putative homologs annotated as FAD-dependent pyridine-nucleotide disulfide oxidoreductases. In the Euryarchaeota, SQO is found in the Thermoplasmatales (node 1, Figure 9). Phylogenetic analyses and ancestral state reconstruction suggested that SQO was acquired by an LGT event in the ancestor of this group. In the Crenarchaeota, SQO (including the SQO from Acidianus with demonstrated activity) was found in the Sulfolobales, and the branching patterns in this group were congruent with the genome phylogeny (node 2). Thus, SQO in the Sulfolobales was likely gained in the ancestor to this group. Archaeal SQO homologs formed a monophyletic group sister to demonstrated SQO homologs in the bacterial domain, distinct from FCSD and the putative pyridine-dinucleotide disulfide oxidoreductases (not shown).
3.7. Nitrate and Nitrite Reduction
Nitrate reductase reduces nitrate to nitrite during anaerobic respiration. The catalytic and electron transfer subunits of nitrate reductase (Figures 10(a), and 10(b)) in the Euryarchaeota were found in Ferroglobus (node 1) and in a clade that contains several Halobacteriales taxa (node 2). In the Crenarchaeota nitrate, reductase subunits were found in the distantly related taxa Aeropyrum (node 3), Vulcanisaeta distributa (node 4), Metallosphaera yellowstonensis (node 5), two strains of Sulfolobus islandicus (node 6), and a clade containing Pyrobaculum spp. (node 7). Because nitrate reductase was not found in Halobacterium spp., it is likely that the latter acquisition occurred after diversification of Halobacterium. The phylogenetic patterning of the nitrate reductase catalytic subunit (Figure 10(a)) is consistent with seven LGT events. The phylogenies of NarG and NarH were identical, and the two genes were adjacent in the genomes of all taxa. Thus, the LGT events leading to the acquisition of NarG also likely led to the acquisition of NarH (Table 3).
Dissimilatory nitrite reductases (NirK) reduce nitrite to either nitric oxide or nitrous oxide. Copper-type nitrite reductases have been identified in some Halobacteriales taxa (Figure 11(a); ). Phylogenetic analyses show that they fall into a monophyletic group (node 1). The phylogenetic pattern suggests that they could have been acquired once, likely after the diversification of Halobacterium spp. However, ancestral state reconstruction suggests that two independent gains could have also occurred (nodes 1 and 2), once being in the ancestor to Haloferax and Halogeometricum.
Homologs to bacterial Heme-type nitrite reductases (NirS) have also been identified in the genomes of three Pyrobaculum species. These also formed a well-supported monophyletic group (node 1, Figure 11(b)). Each of the Pyrobaculum sequences is linked to cytochrome c proteins (not shown) that form part of the nitrite reductase complexes in bacteria. Thus, a single LGT event likely led to the acquisition of Heme-type nitrite reductases in the ancestor to Pyrobaculum spp.
Nitric oxide reductase (NorB) reduces nitric oxide to nitrous oxide. Phylogenetic analysis showed four well-supported clades of NorB in the archaeal domain (Figure 11(c)). One clade contained the Halobacteriales (but not Halobacterium, node 1), another contained S. solfataricus and S. islandicus species (node 2), a third contained the genus Acidilobus (node 3), and the fourth (ode 4) contained several taxa in the Thermoproteales (Caldivirga, Vulcanisaeta distributa, Thermoproteus uzoniensis, and several Pyrobaculum spp.).This is consistent with four lateral transfer events.
Finally, nitrous oxide reductase (NosZ) reduces nitrous oxide to nitrogen. NosZ homologues (Figure 11(d)) were found in only a few archaeal taxa: Haloarcula, Halobacterium, Halobiforma, Haloferax, Halogeometricum, Halopiger, and Halorubrum in the Halobacteriales (node 1), Ferroglobus (node 2), and two species of Pyrobaculum (node 3). The phylogenetic pattern was consistent with three lateral transfer events: once in the Halobacteriales, once in Ferroglobus, and once in the clade containing Pyrobaculum spp.
3.8. Nitrogen Fixation
As has been noted by many investigators, the distribution of nifH-like genes (making up “cluster 4”; Figure 12(a)) is widespread among methanogens, including the basal lineage Methanopyrus. These proteins have recently been shown to form a complex with NifD-like proteins, yet they have no apparent role in nitrogen fixation . True NifH genes involved in nitrogen fixation, however, show a much smaller taxonomic range. Indeed, the ability to fix nitrogen is found only in a small number of methanogens (Methanococcus maripaludis, M. thermolithotrophicus, M. aeolicus, M. vannielii, Methanothermobacter thermoautotrophicum, Methanosarcina barkeri, Methanospirillum, and Methanocaldococcus FS406-22 [32, 39, 40]). Many investigators have inferred a significant role for LGT as well as gene duplication events in the evolutionary history of archaeal nitrogen fixation genes, while a cursory look at the NifH phylogenetic tree (Figure 12(a)) is consistent with previous proposals that nitrogenase first arose in the methanogens . A more detailed analysis suggests that this may not be the case.
Nitrogenase reductases (NifH) fell into a well-supported clade comprising “clusters 2 and 3” (Figure 12(a), clades outlined in green) to the exclusion of proteins related to NifH that constitute “cluster 4” (clades outlined in gray). Within “cluster 2” sequences, an AU test showed that the genome phylogeny and the NifH phylogeny for the Methanococcales were not significantly different (). Relationships within and between the Methanomicrobiales and Methanosarcina were identical to the genome phylogeny. In contrast, an AU test showed that the “cluster 2” phylogeny (including Methanococcales, Methanobacteriales, Methanomicrobiales, and Methanosarcinales) was significantly different from the genome phylogeny (). The point of major incongruence was in the positioning of Methanobacteriales with respect to the Methanococcales and the rooting of the Methanococcales. In addition, “cluster 3” sequences showed positioning that was different from the genome tree. This suggests four lateral transfer events of nitrogenase: once in the ancestor to the Methanococcales (node 1), once in the Methanobacteriales (node 2), once in the ancestor to the Methanomicrobiales and Methanosarcinales (node 3), and once again in Methanosarcina spp. (resulting in the acquisition of the alternative nitrogenases of “cluster 3”; node 4).
The nitrogenase alpha subunit (NifD) and the FeMo cofactor subunit (NifE) are related to one another, likely as a result of an ancestral gene duplication event . Observations of relationships in these trees (Figure 12(b)) as well as AU tests (not shown) revealed relationships that were not significantly different from the relationships observed in the NifH tree. In terms of genomic positioning, “cluster 2” NifH is linked to “cluster 2” NifD and NifE. This suggests that when NifH was acquired by LGT, so were NifD and NifE (Table 3).
3.9. Degradation of Select Organocompounds
Most Thermococcales cultures have never been tested for chitin or chitosan (a form of deacetylated chitin) degradation [43, 44]; however, these organisms do inhabit deep sea hydrothermal vent ecosystems which harbor abundant chitin-containing metazoans (such as giant tube worms, crabs, and shrimp). Two genes with sequence similarity to known chitinases are present in the genomes of Pyrococcus furiosus and Thermococcus kodakarensis. Biochemical studies demonstrated that these genes exhibit chitinase activity [45, 46]. The chitinase genes are part of a unique chitin degradation pathway that includes at least three additional unique genes (exo-β-D-glucosaminidase, glucosamine-6-phosphate deaminase, and diacetylchitobiose deacetylase) [47, 48]. Phylogenetic analyses demonstrated that chitinases in the Thermococcales formed a well-supported monophyletic group (node 1, Figure 13), as did the three additional genes involved in chitin degradation (now shown). The chitinase and chitin degradation genes are all closely spaced along the genome. Thus, there was likely a single LGT event that led to the acquisition of chitin degradation genes in the ancestor to the Thermococcales (Table 4).
Many Halobacteriales also have chitinase-like genes. The halophilic archaea are not generally considered to be chitin degraders, however a recent study has demonstrated that Halobacterium sp. NRC-1 is capable of degrading chitin  and they live in environments where brine shrimp are often abundant. Thus, it is possible that, as in the Thermococcales, chitin degradation has been underestimated in the Halobacteriales. Several copies of chitinases are seen in the genomes of many Halobacteriales taxa (node 2, Figure 13), nevertheless they all appear to form a monophyletic group, and the multiple copies are often adjacent or nearby in the genome. Two subclades were seen to have mirror relationships, suggesting that two copies of chitinases were obtained by LGT in the ancestor of the Halobacteriales. Neither of these subclades, however, is rooted with Halobacterium (as seen in the genome phylogeny), and thus the two subclades likely did not arise as a result of ancestral or recent gene duplication. Rather the two copies were likely acquired by the same LGT event from a donor that came outside of the Thermococcales or Halobacteriales. This was then likely followed by losses of chitinase genes in other taxa in the Halobacteriales, including Natrialba, Halorubrum, Haloquadratum, Natronomonas, Halorhabdus, and Haloarcula.
Protein sequences related to those that catalyze the degradation of phenolic compounds, such as phenol, catechol, and phenylacetate, were found in the genomes of several archaeal groups (Figures 14 and 15). In the bacterial domain, members of class II extradiol dioxygenases have been shown to be capable of adding hydroxyl groups to the phenolic rings of catechol and hydroxyphenylacetate. Sulfolobus solfataricus P2 has been demonstrated to be able to use phenol, catechol, and toluene as sole carbon sources ; however, its close relative S. solfataricus 98/2 cannot be due to an insertion element in the operon containing phenol hydroxylase (which is also transcribed only in the presence of phenol; ). Archaeal relatives of multicomponent monooxygenases that hydroxylate phenol, toluene, and xylene have been observed in Pyrobaculum arsenaticum, Sulfolobus solfataricus strains, and several strains of Sulfolobus islandicus (Figure 14(a)). The phylogenetic pattern suggests a single LGT acquisition in Pyrobaculum arsenaticum (node 1), and a second acquisition in the ancestor to S. solfataricus-S. islandicus (node 2).
Relatives of monooxygenases that are involved in the hydroxylation of 4-hydroxyphenylacetate were also observed in the Sulfolobales, annotated as HpaH (Figure 14(b)). These sequences formed a well-supported clade and were found in Metallosphaera spp., S. tokodaii, S. acidocaldarius, one strain of S. solfataricus (P2), and all strains of S. islandicus. This suggests two LGT acquisition events: once in Pyrobaculum oguniense (node 1) and once again in the ancestor to the Sulfolobales (node 2).
Relatives of class II extradiol dioxygenases that are involved in cleavage of the phenolic rings of catechol and dihydroxyphenol acetate (Figure 15(a)) have been found in the genomes of the Sulfolobales. These sequences were observed to fall into two distinct well-supported clades. One clade (node 1) comprised both strains of Sulfolobus solfataricus and four strains of S. islandicus. Biochemical analyses have shown the proteins in both strains of S. solfataricus function as a catechol 2,3 dioxygenase and 4-chlorocatechol dioxygenase [50, 51]. The taxonomic distribution in this clade was identical to that found in the clade of phenol hydroxylases in the Sulfolobales (node 2, Figure 14(a)), their phylogenetic trees were identical, and, indeed, the proteins were found to be located nearby in the genome in all taxa. The second clade (node 2), annotated as HpaD, was more widespread in the Sulfolobales being present in Metallosphaera spp. (two to three copies), S. tokodaii, S. acidocaldarius, S. solfataricus P2,and all strains of S. islandicus. A third ortholog was identified in Pyrobaculum oguniense (node 3). Although the function of the archaeal HpaD ortholog has yet to be demonstrated, phylogenetic analyses suggest its functions as a 3,4-dihydroxyphenyl acetate dioxygenase . All HpaH sequences in the Sulfolobales genomes were adjacent to the HpaD sequences in class II extradiol dioxygenases (Figure 14(a)). Relationships within the catechol dioxygenase and HpaD clades showed only a moderate or poor support; branching relationships however were similar to those observed in the genome phylogeny.
Relatives of class III extradiol dioxygenases were also found in the genomes of the Sulfolobales, Thermoplasma acidophilum, Pyrobaculum arsenaticum, and three small groups of distantly related methanogens (Figure 15(b)). The biochemical function of these proteins in the archaeal domain is presently not known. A well-supported clade (node 1) contained relatives from Metallosphaera, S. tokodaii, S. acidocaldarius, S. solfataricus 98/2, and all strains of S. islandicus. Again, relationships within the clade were only moderately or poorly supported; however, branching relationships were similar to those in the genome phylogeny suggesting a single lateral transfer event in the ancestor to the Sulfolobales. Interestingly, the genes from all S. islandicus strains were found to be nearby the class II HpaD extradiol sequences, but such juxtaposition was not observed for any other taxa in the Sulfolobales. A homolog is also found in Thermoplasma acidophilum (node 3), consistent with a single gain in this taxon. A lone homolog to class III extradiol dioxygenase was also found in Pyrobaculum arsenaticum (node 3, Figure 15(b)), located in a similar location in the genome as the protein for phenol hydroxylase (node 1; Figure 14(b)), and both branch sisters suggesting they arose by a common LGT event followed by gene duplication. The phylogenetic distribution of the methanogen sequences suggests independent LGT events into three distantly related groups of methanogens (nodes 4–6). In sum, the phylogenetic pattern suggests six independent gains of class III extradiol dioxygenases by LGT events.
3.10. Rates of Lateral Transfer
Table 5 summarizes the number of LGT events per gene and converts this to a rate of number of LGT events over the age span of the archaeal domain (approximately 3.5 billion years). The gene with the highest transfer rate was thiosulfate sulfurtransferase (SseA), calculated to have been transferred 3.1 times per billion years across the entire archaeal domain of life. Cytochrome oxidase, quinol oxidase, and the genes coding for the oxidation of phenolic compounds were also transferred at higher rates (2.6–3.4 events per billion years). Most of other genes showed a small number of lateral transfer events, amounting to less than one transfer event per billion years. This suggests that gene acquisitions, and hence changes in the metabolic niches of archaea, have been slowly changing over geologic time. This observation is consistent with the complexity hypothesis [4–7].
Although metabolic genes are often considered to have been frequently swapped between prokaryotic lineages via the process of lateral gene transfer, a phylogenomic approach using explicit phylogenetic reconstruction and ancestral state reconstruction suggests that lateral transfer events involving metabolic genes are rare, across deep geologic time. These stable transfers likely occurred only a small number of times on the order of 1–3 transfer events per billions of years.
The author would like to thank Lara Smith, supported by an NSF Montana EPSCoR summer undergraduate fellowship, for assistance with data matrix construction and two anonymous reviewers for their helpful comments on the paper. This work was supported by funding from the NSF Assembling the Tree of Life Program (Grant no. 1208534).
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