|Home | About | Journals | Submit | Contact Us | Français|
Conceived and designed the experiments: H-PK NK. Performed the experiments: IA CS MG KM SDH IP NI. Analyzed the data: IA CS MG IP NI. Contributed reagents/materials/analysis tools: KM SDH. Wrote the paper: IA MG NI.
The extremely halophilic archaea are present worldwide in saline environments and have important biotechnological applications. Ten complete genomes of haloarchaea are now available, providing an opportunity for comparative analysis.
We report here the comparative analysis of five newly sequenced haloarchaeal genomes with five previously published ones. Whole genome trees based on protein sequences provide strong support for deep relationships between the ten organisms. Using a soft clustering approach, we identified 887 protein clusters present in all halophiles. Of these core clusters, 112 are not found in any other archaea and therefore constitute the haloarchaeal signature. Four of the halophiles were isolated from water, and four were isolated from soil or sediment. Although there are few habitat-specific clusters, the soil/sediment halophiles tend to have greater capacity for polysaccharide degradation, siderophore synthesis, and cell wall modification. Halorhabdus utahensis and Haloterrigena turkmenica encode over forty glycosyl hydrolases each, and may be capable of breaking down naturally occurring complex carbohydrates. H. utahensis is specialized for growth on carbohydrates and has few amino acid degradation pathways. It uses the non-oxidative pentose phosphate pathway instead of the oxidative pathway, giving it more flexibility in the metabolism of pentoses.
These new genomes expand our understanding of haloarchaeal catabolic pathways, providing a basis for further experimental analysis, especially with regard to carbohydrate metabolism. Halophilic glycosyl hydrolases for use in biofuel production are more likely to be found in halophiles isolated from soil or sediment.
The organisms in the euryarchaeal order Halobacteriales are generally extreme halophiles requiring at least 1.5 M salt and growing optimally at 3.5–4.5 M salt , although some have recently been found to grow at lower salt concentrations , . The haloarchaea are found in the water and sediment of salt lakes and salterns, and also in saline soils. Their mechanism of adaptation to high salinity involves the accumulation of molar concentrations of KCl in the cytoplasm and the production of proteins with a higher number of negative charges than in other organisms. Bacteria of the order Halanaerobiales and the genus Salinibacter also accumulate KCl internally . Other halophilic organisms accumulate compatible solutes such as glycerol or glycine betaine to counter high external salt concentrations, but this is energetically more costly than accumulation of KCl .
The haloarchaea are heterotrophs, growing with amino acids and/or carbohydrates as carbon and energy sources. They are either aerobic or facultatively anaerobic using various electron acceptors . Glycerol is a particularly important nutrient for haloarchaea as it is produced by eukaryotic algae in high-salt environments . Dihydroxyacetone, produced by Salinibacter ruber, can also be present at high concentrations . While some haloarchaea are capable of growth on a wide range of compounds, others are very limited in their metabolism. The most extreme example of this is Haloquadratum walsbyi, which has only been found to grow well on pyruvate or dihydroxyacetone , .
Six haloarchaeal genomes have been sequenced previously, and analyses of the genomes have been published for Halobacterium salinarum NRC-1 , Halobacterium salinarum R1 , Haloarcula marismortui , Natronomonas pharaonis , Haloquadratum walsbyi , and Haloferax volcanii . Since the two H. salinarum genomes are very similar, we included only strain NRC-1 in the analysis. Here we present an analysis of these five genomes along with five new genomes, four of which (Halogeometricum borinquense, Halomicrobium mukohataei, Halorhabdus utahensis and Haloterrigena turkmenica) were sequenced as part of the Genomic Encyclopedia of Bacteria and Archaea (GEBA) project . The remaining genome, Halorubrum lacusprofundi, was sequenced as part of a Joint Genome Institute Community Sequencing Program project to sequence diverse archaeal genomes. With this work we are doubling the amount of genomic information from these extremophilic organisms and derive novel information and conclusions about the breadth of their metabolic capabilities.
Sequencing and annotation of H. borinquense, H. mukohataei, H. utahensis, and H. turkmenica have been previously described –. A publication describing the sequencing and annotation of H. lacusprofundi is in preparation. Genome sequences are available from GenBank. Genome analysis was carried out within the Integrated Microbial Genomes Expert Review (IMG-ER) system .
Protein sequences from 19 Halobacteria and outgroup (Methanomicrobia) genomes were retrieved from the IMG website (http://img.jgi.doe.gov/) or from NCBI (Methanocella paludicola SANAE; NC_013665). Methanomicrobia appear as sister group of Halobacteriaceae in a recent comprehensive 16S rRNA tree . Accession numbers for the genomes used in this study are listed in Table S5.
All-against-all protein BLAST was performed using mpiBLAST version 1.5 (http://www.mpiblast.org/), a parallel implementation of NCBI BLAST , using soft masking instead of complexity filtering. To determine orthologs, BLAST e-values were transformed using our own re-implementation of the OrthoMCL algorithm  in conjunction with MCL version 08-312 (http://micans.org/mcl/) using an inflation parameter of 3.0 (slightly deviating from the default, 2.0, thus yielding slightly more clusters). The transformation of the e-values corrects for genome-specific biases as, e.g., caused by a GC bias ; after transformation, the BLAST results are reduced to the reciprocal best hits for each pair of genomes, which are then clustered using the MCL algorithm. OrthoMCL clusters containing inparalogs were reduced by selecting the most ‘central’ of several sequences from the same genome, that is, the sequence with the highest sum of within-cluster BLAST scores. The reduced OrthoMCL clusters were aligned using MUSCLE version 3.7 under default settings . The program scan_orphanerrs from the RASCAL package version 1.3.4  was applied to detect orphan sequences (overall poorly aligned genes) within the alignments. After removal of orphan sequences (if present), poorly aligned columns and divergent regions were eliminated with GBLOCKS version 0.91b  using a minimum block length of two amino acids and allowing gap positions in all sequences. Each OrthoMCL cluster was also assigned to a COG category  using a majority-rule approach. Above-mentioned parameter settings for ortholog determination and alignment filtering had previously been optimized using a genome-scale dataset for Actinobacteria type strains (unpublished data). During this optimization, it also turned out that modifying the program parameters had comparatively little influence on the phylogenetic outcome.
Filtered OrthoMCL cluster alignments comprising at least four sequences were concatenated to form a supermatrix for phylogenetic analysis. Maximum likelihood (ML) phylogenetic trees were inferred from the supermatrix with the Pthreads-parallelized RAxML package  version 7.2.5, applying fast bootstrapping with subsequent search for the best tree , the autoMRE bootstopping criterion  and the LG model of amino acid evolution  in conjunction with gamma-distributed substitution rates  and empirical amino acid frequencies (F). Among all amino acid models implemented in RAxML (except GTR, which was rejected for performance reasons), LGF was the empirically preferred one, as it produced the highest likelihood if optimized on a RAxML parsimony starting tree. Tree searches under the maximum parsimony (MP) criterion were conducted with PAUP* version 4b10  using 100 rounds of random sequence addition and subsequent TBR branch swapping, saving no more than 10 best trees per round and collapsing potential zero-length branches during tree search. MP bootstrap support was calculated with PAUP* using 1,000 replicates with 10 rounds of heuristic search per replicate.
After reducing the OrthoMCL cluster alignments to ingroup sequences, congruence between gene trees and the species tree was assessed by calculating partitioned Bremer support (PBS) ,  for each OrthoMCL cluster using the newick.tcl script  in conjunction with PAUP*. The Bremer support value for a certain bipartition (split) in the tree topology is the difference between the score (number of steps) of the best-known MP tree in which this split does not occur (forced using a converse constraint) and the score of the unconstrained best-known MP tree. While the total Bremer support must be positive, PBS values may be positive, zero, or negative, indicating that the OrthoMCL cluster supports the split, contains no information, or prefers another topology, respectively . As the total PBS (summed over all branches) for each cluster positively correlated with both its number of genes and its number of informative characters, the residuals from a linear regression with these two independent variables were determined. The residuals were used to determine their correlation with the COG categories and classes  and the clusters most in conflict with the species tree (i.e., those with the most negative total PBS).
Protein sequences for the ten halophiles were downloaded from IMG-ER . We applied a spectral clustering procedure ,  for discriminating between groups of homologous proteins. The proteins are represented as nodes in a connected undirected graph with edges that carry weights based on node-to-node similarity according to the protein identity. The clustering procedure is analogous to a random walk of a particle moving on this graph from one node to another. In each node the particle moves to another node based on the probabilities corresponding to the weights of the edges. The amount of time the particle spends in a given subgraph will determine whether this is indeed a cluster of its own or not. After infinite time, the distinction between these subgraphs will become more clear, and to model this we calculated the normalized transition matrix at equilibrium. The eigenvalues of the transition matrix provide a measure of how distinct (or entwined) subgraphs are in relation to each other. An eigenvalue (or strength of partition) of 1 suggests a complete distinction between two subgraphs, while an eigenvalue of 0 suggests that no further partitions can be made. The eigenvectors are ordered by their eigenvalues in descending order, and the graph is successively partitioned while the second eigenvalue is greater than 0.8. As a result, a graph is partitioned into one or more subgraphs until the distinction between subgraphs becomes less clear. In this work, the choice of 0.8 as a cutoff suggests a balance between partitioning only fully non-homologous proteins and allowing proteins with weak similarities to be separated into subgraphs.
The heat maps and clustering of secreted proteases and glycosyl hydrolases were generated using hierarchical clustering with the program Cluster  and visualized with TreeView (http://rana.lbl.gov/EisenSoftware.htm). Glycosyl hydrolases were identified based on Pfam domains. Proteases were obtained from MEROPS . Non-peptidase homologues were eliminated from the analysis. Signal peptides were identified with SignalP .
The number of aligned and filtered OrthoMCL clusters containing at least four entries (i.e., genes from distinct genomes) was 3,853, their length ranging from 22 to 1650 amino acids (262.542 on average). The concatenated supermatrix thus comprised 1,011,575 columns, including 708,296 variable and 353,936 parsimony-informative characters.
The ML phylogeny inferred from the concatenated gene alignments is shown in Figure 1 (species tree) together with ML and MP bootstrap support values. The final highest log likelihood obtained was −12,342,390.79, whereas the single best MP tree (excluding uninformative sites) had a score of 1,409,187. ML and MP topologies were identical. Support was maximum (100%) for all branches under ML, and maximum for all but four branches under MP; only a single branch entirely lacked support under MP. As only one genome per genus was included in the sample, there is no taxonomic subdivision of Halobacteriaceae to compare the tree with. However, outgroup taxonomy was well recovered, the tree showing the monophyly of Methanomicrobiales, Methanosarcinales, and Methanosarcinaceae, each of which were represented with at least two genomes.
After reducing the dataset to the ingroup taxa and to the OrthoMCL clusters present in at least four ingroup genomes, total PBS per OrthoMCL cluster ranged between 142 and −219 (average: 4.941, standard deviation: 19.588, median: 1, MAD: 8.896). These data are plotted against the number of parsimony-informative characters in supplementary Figure S1. Within a total of 2,891 OrthoMCL clusters, 1,506 genes showed overall positive support and 764 showed overall negative support. Trees inferred from the five clusters least congruent with the species tree are depicted in Figure S2. They are uniformly characterized by high bootstrap support for groupings in conflict with the species tree estimate. Total PBS values per cluster vary between the COG categories (which could be assigned to 2,213 clusters; see Figure S1); on average, COGs related to information storage and processing display higher PBS than those associated with metabolism or cellular processes and signaling (Table S1); but individual COG categories may differ from this general trend (Table S1).
We used a spectral clustering method to generate gene clusters from the haloarchaeal genomes. There were 887 core clusters, those found in all of the haloarchaeal genomes, and these accounted for 40% to 50% of the genes in each genome (Table 1). As expected, the core clusters contain genes involved in basic cellular processes such as transcription, translation, DNA replication, DNA repair, RNA modification, protein modification, and protein secretion (Table S2). The core clusters also include many genes involved in biosynthesis of essential metabolites – amino acids, purines and pyrimidines, lipids, and cofactors. This is somewhat unexpected as the haloarchaea are heterotrophs, but they appear to be relatively self-sufficient in being able to make most essential metabolites. Biosynthetic pathways in the haloarchaea have recently been reviewed , so we will not go into more detail here. The number of genes in each genome belonging to all clusters ranges from 78% to 88% (Table 1), showing that 12% to 22% of the genes in each genome have no hits to genes in the other halophile genomes.
We also identified signature gene clusters, those that are shared by all haloarchaea but are not found in any other archaea. There are 112 of these clusters (Table S3), 89 of which contain proteins with completely unknown function. Of the clusters with a predicted function, two are protein kinases related to the Bacillus subtilis PrkA protein. These two kinase genes are adjacent to each other on the chromosome in all haloarchaeal genomes and are always found with two other genes: one with a domain of unknown function DUF444, and one related to B. subtilis SpoVR, the function of which is unknown. Proteins of these three families are found together on the chromosome in many other microbial genomes suggesting functional linkage.
Halophiles are known to accumulate gamma-glutamyl-cysteine , and two of the signature clusters may be involved in gamma-glutamyl-cysteine metabolism. Cluster 491.1× contains proteins related to glutamate-cysteine ligase, and the H. volcanii member of cluster 491.1× was recently shown to have glutamate-cysteine ligase activity . Cluster 1151× includes genes related to glutathione S-transferase, which inactivates toxic compounds by linking them to glutathione. In the halophiles, these may function as gamma-glutamylcysteine S-transferases.
Of the ten haloarchaea with sequenced genomes, four were isolated from water and four were isolated from soil or sediment. The ones isolated from water are H. walsbyi , N. pharaonis , H. marismortui , and H. borinquense . H. mukohataei and H. turkmenica were isolated from saline soils , , while H. volcanii and H. utahensis were isolated from lake sediments , . The water halophiles and soil/sediment halophiles do not form separate clades in the phylogenetic tree (Figure 1). We looked for clusters present in all water-isolated halophiles that are not present in soil/sediment halophiles and vice versa. There were no clusters specific to water halophiles and only three specific to soil/sediment haloarchaea (Table S4). Proteins belonging to two of the soil/sediment-specific clusters (326.1.0× and 2168×) are often found in the vicinity of nucleotide-sugar metabolic enzymes and glycosyl transferases, suggesting they are involved in cell wall biosynthesis .
Since there were few protein clusters completely specific to the water or soil/sediment halophiles, we looked for clusters present in three out of four organisms from one group and absent from the other group. There were 16 clusters present in three out of four water halophiles, of which 11 contain hypothetical proteins and four have only general functional annotations (Table S4). The only cluster with a specific annotation is cluster 1816×, formate-tetrahydrofolate ligase.
Of the 26 clusters found in three out of four soil/sediment halophiles and not present in water halophiles, 11 are hypothetical proteins (Table S4). Several of the clusters are involved in polysaccharide degradation. These include a glycosyl hydrolase of family GH4, an alpha-L-arabinofuranosidase of family GH51, a polysaccharide deacetylase and a trehalose utilization protein. Two additional clusters present in three out of four soil/sediment halophiles encode a monooxygenase and an acyltransferase, which are found adjacent to each other on the chromosome and flanked by two IucA/IucC family proteins. These proteins are likely to be involved in siderophore synthesis. H. borinquense has three IucA/IucC family proteins but lacks the monooxygenase and acyltransferase, thus it is unclear if it has a complete siderophore biosynthesis pathway.
We also looked for clusters conserved in all but one genome. These probably indicate recent gene losses in each species. The genomes fell into two groups – those that had 20 or less such clusters and those that had greater than 60 (Table 1). The three genomes that had greater than 60 clusters lost were H. salinarum, H. walsbyi, and H. utahensis. Many of the clusters lost from H. salinarum are involved in amino acid synthesis, including genes for the synthesis of glutamate, lysine, ornithine, methionine, and branched chain amino acids. To make up for this, H. salinarum does not have more amino acid transporters or secreted proteases than the other haloarchaea, but it is one of only two of the haloarchaea to have a putative peptide symporter of the OPT family (TC 2.A.67). Symporters have low affinity but high capacity, suggesting that H. salinarum may prefer to live where there is an ample supply of peptides. Of the clusters not present in H. walsbyi, many are involved in flagellum biosynthesis and chemotaxis. However, H. walsbyi has a set of gas vesicle proteins to enable motility in the absence of flagella. The clusters in all except H. utahensis include several enzymes involved in cobalamin synthesis and several enzymes of biotin utilization and propionate metabolism. H. utahensis appears to lack the enzymes for the early steps of cobalamin biosynthesis up to the incorporation of cobalt, but all of the halophiles, including H. utahensis, contain the enzymes for the later steps of cobalamin biosynthesis. Biotin and propionate metabolism are discussed further below.
Some haloarchaea are known to use the semi-phosphorylated Entner-Doudoroff (ED) pathway for glucose degradation , , and genes encoding enzymes of this pathway have been identified in several haloarchaea . With the addition of the new genomes, we find that the semi-phosphorylated Entner-Doudoroff pathway is likely to be present in all sequenced haloarchaea except N. pharaonis, which does not utilize carbohydrates. Aldolases belonging to two different protein families may be involved. All of the halophiles except H. salinarum and N. pharaonis have one or more bacterial-type 2-keto-3-deoxy-6-phosphogluconate (KDPGlc) aldolase (COG0800). Also all except N. pharaonis have at least one potential aldolase related to the characterized Sulfolobus aldolase (COG0329), which is active on KDPGlc and unphosphorylated 2-keto-3-deoxygluconate (KDGlc) . The enzymes of the semi-phosphorylated Entner-Doudoroff pathway are highly conserved in sequence among the haloarchaea, suggesting descent from a common ancestor.
The standard Embden-Meyerhof pathway of glycolysis appears to be incomplete in the halophiles as no 6-phosphofructokinase could be identified. This agrees with previous experimental studies and analysis . Gluconeogenesis is likely to be present in all of the halophile genomes with the possible exception of H. utahensis. All except H. utahensis have phosphoenolpyruvate (PEP) synthase and/or pyruvate, phosphate dikinase (COG0574). In addition, H. lacusprofundi and H. turkmenica have ATP-utilizing PEP carboxykinase (COG1866). In H. utahensis the only enzyme that potentially can generate PEP for gluconeogenesis is pyruvate kinase. All except H. utahensis have a fructose 1,6-bisphosphatase belonging to the same family as the E. coli Fbp enzyme (COG0158). All of the halophiles including H. utahensis have at least one gene belonging to COG0483, which includes inositol phosphatases and some archaeal fructose 1,6-bisphosphatases . H. utahensis has two genes belonging to this family, but they are weakly related to characterized fructose 1,6-bisphosphatases. These findings suggest that H. utahensis may lack the gluconeogenesis pathway or have an unusual gluconeogenesis pathway.
Unlike the rest of the archaea, halophiles are thought to use the oxidative pentose phosphate pathway for generation of pentoses . This pathway also generates NADPH for anabolic pathways. All except H. utahensis have a probable 6-phosphogluconate dehydrogenase (COG1023), the key enzyme of this pathway. In contrast, H. utahensis is the only sequenced haloarchaeon to have transaldolase (Huta_0859) and transketolase (Huta_0860 and Huta_0861), the enzymes of the non-oxidative pentose phosphate pathway. For NADPH generation, H. utahensis possesses genes encoding a NAD/NADP transhydrogenase (Huta_2005–2007). None of the other haloarchaea has the genes for this enzyme. The presence of these enzymes only in H. utahensis suggests that they may have been acquired through lateral transfer, but phylogenetic analysis was unable to identify the donor (data not shown).
Table 2 presents an overview of nutrient transport in the haloarchaea. All of the haloarchaea have at least five symporters for amino acids and at least two ABC transporters for peptides. Since all except H. salinarum can synthesize most or all amino acids, this suggests that amino acids are an important carbon and energy source even in the species that can grow on carbohydrates. All of the haloarchaea also have at least one symporter for nucleosides or nucleobases. Carbohydrate transport is variable. Only half of the halophiles have symporters for sugars, and either none or one ABC transporter for sugars is found in the non-carbohydrate-utilizing organisms. Surprisingly no transporters for sugars could be identified in the H. utahensis genome, suggesting that it uses uncharacterized families of sugar transporters.
There appears to be a connection between some transporters and universal stress protein A (UspA) family proteins. Most amino acid transporters of the amino acid-polyamine-organocation (APC) family are either fused to a UspA domain or adjacent on the chromosome to a UspA protein, and some are both fused and adjacent to UspA family proteins (e.g. Htur_0566). This appears to be specific for the APC family as other potential amino acid symporters of the neurotransmittersodium symporter (NSS) family and the dicarboxylate/amino acidcation symporter (DAACS) family are not associated with UspA family proteins. Several transporters of the formate-nitrite transporter (FNT) family are also fused or adjacent to UspA domains (Hmuk_1674, HQ1451A, NP6264A, Hlac_2299, and Htur_2705). The FNT family proteins with associated UspA domains are closely related to each other and to a transporter from H. marismortui that lacks a UspA domain (rrnAC0187). They are likely to be formate transporters as the H. marismortui and H. mukohataei proteins are adjacent to enzymes of folate metabolism. Another transporter with adjacent UspA proteins is a putative acetate transporter of the solutesodium symporter (SSS) family. This transporter is found in seven of the ten halophile genomes (e.g. NP5136A), and in all cases is followed by a UspA domain protein. In six of the seven genomes with this transporter, it is close on the chromosome to two acetyl-CoA synthetase genes (e.g. NP5128A and NP5132A). The transporter has highest similarity to subfamily 7 of the SSS family, which includes acetate, propionate, and phenylacetate transporters (see the Transporter Classification Database at www.tcdb.org). UspA family proteins are expressed during many stressful conditions, and they are known to bind ATP, but their exact molecular function is unknown . The UspA domains associated with transporters may play a regulatory role, or may be involved in maintaining transporter function during stressful conditions. A recent report shows that a UspA domain protein is involved in regulation of a transporter .
Since the halophiles have numerous transporters for amino acids and peptides, we analyzed the distribution of secreted proteases within their genomes. Only secreted proteases were considered because these are likely to be involved in the utilization of proteins as a nutrient source, while intracellular and integral membrane proteases are involved in a variety of cellular processes. We included proteases that have signal peptides as well as proteins that are likely to be attached to the membrane with the protease domain outside the cell. Signal peptidases (family S26) were excluded from the analysis since they have a specific cellular function. The numbers of secreted proteases in the genomes ranged from 3 to 11. Hierarchical clustering (Figure 2) shows that the halophiles fall into two groups with respect to protease distribution. The main feature separating these groups appears to be the presence or absence of secreted members of protease family S8, which includes subtilisin as well as halolysins from halophilic archaea. The organisms having secreted S8 proteases do not correspond to a habitat-specific or phylogenetic group. The presence of at least three secreted proteases in each genome suggests that all of the halophiles may be capable of degradation of extracellular proteins.
Since all of the halophiles have at least five amino acid symporters and two peptide ABC transporters, we investigated pathways of amino acid utilization to see if all of the halophiles are capable of using many amino acids. A summary is provided in Table 3. Three degradation pathways were found in all of the ten genomes. All of them had an alanine dehydrogenase similar to the enzyme characterized in Archaeoglobus fulgidus . This enzyme could potentially be involved in synthesis of alanine as well as its degradation. All had at least one asparaginase from COG0252 or COG1446. Finally all of them had a pyruvoyl-dependent arginine decarboxylase similar to the enzyme characterized in Methanocaldococcus jannaschii  and agmatinase. This combination of enzymes produces putrescine and urea from arginine. Additional enzymes of arginine utilization were present in some genomes. Six of the genomes have arginase, which produces ornithine and urea. None of the genomes had ornithine decarboxylase, but all of the ones that have arginase also have ornithine cyclodeaminase which produces proline.
Several other amino acid degradation pathways are found in a subset of the genomes. The glycine cleavage system is found in all genomes except those of H. walsbyi and H. utahensis. This enzyme complex produces CO2, NH3, methylene-tetrahydrofolate (THF), and NADH. Methylene-THF has a variety of possible uses within the cell. Another pathway found in all but H. walsbyi and H. utahensis is isoleucine degradation. A 2-oxoacid dehydrogenase complex involved in isoleucine degradation was recently identified in H. volcanii , and seven of the other halophiles have genes with at least 68% similarity to the H. volcanii genes, indicating that they probably have the same function. Five of the genomes have tryptophanase, which produces pyruvate from tryptophan. A histidine degradation pathway with formiminoglutamate as an intermediate is also found in five of the genomes. Seven have proline dehydrogenase, but only H. lacusprofundi has pyrroline-5-carboxylate dehydrogenase to complete proline conversion to glutamate. All of the genomes have threonine dehydratase, but this may be used only for biosynthesis. Five of the genomes in addition have threonine aldolase, which produces glycine and acetaldehyde. Finally, all of the genomes have glutamate dehydrogenase, which may have a biosynthetic role. Four of the genomes have glutamate mutase and methylaspartate ammonia-lyase. These are the first two enzymes of a four-step pathway that produces acetate and pyruvate from glutamate with mesaconate and citramalate as intermediates. However, these two enzymes are likely to be involved in a new pathway for acetate assimilation .
Many of the pathways for amino acid degradation are found in a subset of the genomes. They could have been acquired independently by lateral gene transfer or lost in some species. The genes for amino acid degradation in the halophiles are closely related in sequence, suggesting that the common ancestor of haloarchaea was able to degrade many amino acids and that some organisms have lost these pathways.
According to the distribution of glycosyl hydrolase domains and carbohydrate-binding modules, halophilic archaea can be divided into 3 groups: those that may be capable of degrading plant biomass (H. utahensis, H. turkmenica and to a lesser extent H. marismortui and H. volcanii), those harboring family 18 glycosyl hydrolases with possible chitinase activity (H. salinarum, H. mukohataei and H. borinquense) and organisms that are unlikely to degrade any externally provided polysaccharides (H. lacusprofundi, H. walsbyi and N. pharaonis) (Figure 3).
H. utahensis and H. turkmenica have the two largest sets of proteins with glycosyl hydrolase domains among halophilic archaea (43 and 44, respectively). However, their glycosyl hydrolase complements are markedly different. While H. utahensis has five proteins of GH10 family and two proteins of GH11 family, which probably have xylanase activity, H. turkmenica has only one GH10 protein and no GH11 members. The abundance of predicted xylanases in the H. utahensis genome is in agreement with experimental data that showed xylan-degrading activity of this archaeon . The H. utahensis genome contains seven GH5 family proteins and one GH9 family protein (as compared to three and zero in H. turkmenica genome). These proteins may have endo-beta-glucanase activity, thus enabling H. utahensis to degrade components of the plant cell wall. One of the GH5 proteins in H. utahensis (Huta_2387) has been shown experimentally to have cellulolytic activity (T. Zhang et al., in press). H. utahensis also has two GH94 proteins that may have cellobiose or cellodextrin phosphorylase activity. On the other hand, the H. turkmenica genome encodes four GH32 family proteins predicted to have beta-fructosidase (levanase or invertase) activity that are absent from the H. utahensis genome, while both genomes have several GH2 family proteins that may have beta-galactosidase activity.
Three of the genomes from haloarchaea isolated from soil or sediment encode enzymes involved in degradation of pectin. The backbone chains of pectin are made up of either homogalacturonan or rhamnogalacturonan with various side chains, and the main chains are linked together by α-1,5-arabinan chains . H. turkmenica has four family 1 polysaccharide lyases (PL) which likely have pectate lyase activity, three of which are close together on the chromosome (Htur_4783, Htur_4785, Htur_4789). Also in the vicinity of these three genes is a family 2 polysaccharide lyase related to pectate lyases (Htur_4786) and two glycosyl hydrolases, one of which may have polygalacturonase activity (Htur_4790). The other H. turkmenica PL1 family protein (Htur_4440) is close to one of two pectin methylesterases (Htur_4438) and a rhamnogalacturonan acetylesterase (Htur_4445). H. turkmenica also has two family 11 polysaccharide lyases (Htur_3890, Htur_3891) that are highly similar to a B. subtilis rhamnogalacturonan lyase and a GH105 protein similar to the RhiN protein of Dickeya (formerly Erwinia) chrysanthemi, which is involved in degradation of rhamnogalacturonate oligosaccharides . H. utahensis and H. volcanii have much lower capacity for pectin degradation: H. utahensis has two probable pectate lyases from family 1, while H. volcanii has one pectate lyase and one pectin methylesterase. In addition to enzymes capable of degrading the main chains of pectin, H. turkmenica, H. utahensis, and H. volcanii have GH43, GH51, and GH93 glycosyl hydrolases with similarity to endo- and exo-arabinases that may be capable of degrading the arabinan linking chains of pectin.
H. lacusprofundi and H. mukohataei have been shown to grow on galactose , , but the genome sequences suggest that other haloarchaea can also utilize galactose. Also the genome sequences show that two different pathways for galactose metabolism may exist in haloarchaea: the Leloir pathway in H. utahensis, and the De Ley-Doudoroff pathway in H. lacusprofundi, H. marismortui, H. volcanii, H. borinquense, H. mukohataei, and H. turkmenica. H. utahensis is the only haloarchaeon with genes encoding the three enzymes of the Leloir pathway. No other archaeon possesses a gene for hexose 1-phosphate uridylyltransferase (COG1085, Huta_2170), and H. volcanii is the only other haloarchaeon to have a probable galactokinase (HVO_1487). Six haloarchaea (listed above) have genes with high similarity (65–75%) to E. coli galactonate dehydratase, one of the enzymes of the De Ley-Doudoroff pathway. Phylogenetic analysis shows that the genes for galactonate dehydratase in the haloarchaea cluster together (data not shown). In the De Ley-Doudoroff pathway, after 2-dehydro-3-deoxygalactonate (KDGal) is formed by galactonate dehydratase, it is phosphorylated by KDGal kinase to form 2-dehydro-3-deoxy-6-phosphogalactonate (KDPGal). KDPGal is then split by KDPGal aldolase to form pyruvate and glyceraldehyde 3-phosphate . None of the halophiles has a gene related to known KDGal kinases (COG3734). KDPGal aldolases belong to the same family as bacterial-type KDPGlc aldolases of the Entner-Doudoroff pathway (COG0800). H. lacusprofundi has two proteins related to KDGlc kinase and two proteins related to bacterial-type KDPGlc aldolase. One kinase (Hlac_2870) and aldolase (Hlac_2860) are close on the chromosome to each other and to galactonate dehydratase (Hlac_2866), beta-galactosidase (Hlac_2868), and a probable alpha-galactosidase (Hlac_2869), suggesting that the kinase and aldolase may be involved in the utilization of galactose via the De Ley-Doudoroff pathway. Similarly, H. volcanii has three COG0800 proteins, one of which (HVO_A0329) is close on the chromosome to a KDPGlc kinase-related protein (HVO_A0328), galactonate dehydratase (HVO_A0331) and beta-galactosidase (HVO_A0326). Some of the halophiles that have galactonate dehydratase only have one protein related to KDGlc kinase and KDPGlc aldolase. It is possible that in these organisms the proteins are bifunctional, working with both KDGlc and KDGal, similar to the proteins of the Sulfolobus solfataricus ED pathway .
Fructose can be utilized by some haloarchaea: H. marismortui, H. borinquense, H. utahensis, and H. turkmenica have been shown to grow on fructose , , , , while H. mukohataei has been shown to grow on sucrose  and thus will likely also metabolize fructose. The enzyme ketohexokinase was characterized in Haloarcula vallismortis but the gene was not identified . H. marismortui, H. volcanii, and H. turkmenica each have one transporter of the phosphotransferase system (PTS), and operon evidence suggests that these are fructose transporters that produce fructose 1-phosphate. The PTS transporters from H. volcanii and H. turkmenica are close on the chromosome to putative fructose 1-phosphate kinases (COG1105), while in H. volcanii the PTS proteins are also close to fructose bisphosphate aldolase. In addition to the three haloarchaea with PTS transporters, H. utahensis and H. mukohataei also have putative fructose 1-phosphate kinases. In H. mukohataei the fructose 1-phosphate kinase (Hmuk_2661) is close on the chromosome to fructose bisphosphate aldolase (Hmuk_2663) and another putative sugar kinase (Hmuk_2662) which may be a ketohexokinase. Surprisingly H. borinquense does not have a member of COG1105, despite its known ability to grow on fructose. The protein sequences of all components of the PTS system transporter and fructose 1-phosphate kinase are strongly conserved among the halophiles.
The pathway by which H. volcanii utilizes xylose has recently been characterized . The pathway involves formation of xylonate, followed by two dehydratase steps to generate 2-oxoglutarate semialdehyde. This pathway also appears to be present in H. turkmenica and H. lacusprofundi, both of which were not previously known to utilize xylose. H. marismortui is known to produce acid from xylose, and it appears to have 2-dehydro-3-deoxyxylonate dehydratase and xylose dehydrogenase, but it does not have a gene with high similarity to the H. volcanii xylonate dehydratase. H. utahensis is known to degrade xylan and to be able to grow on xylose , , and it uses a different pathway for xylose degradation. It has a xylose isomerase (COG2115, Huta_2443) and xylulokinase (TIGR01312, Huta_2446). The resulting D-xylulose 5-phosphate then feeds into the non-oxidative pentose phosphate pathway. H. utahensis is the only one of the sequenced haloarchaea to have transaldolase and transketolase of the non-oxidative PPP, which allows it to use this pathway of xylose utilization. H. borinquense is known to utilize xylose , but it does not have identifiable genes for either of the pathways found in the other haloarchaea. Phylogenetic analysis of xylose isomerase using both neighbor joining (Clustal W) and Bayesian (MrBayes) methods show that H. utahensis xylose isomerase branches deeply within Firmicutes with high bootstrap support (not shown), but xylulokinase did not associate closely to any group of organisms.
Both H. utahensis and H. turkmenica have putative glucuronate isomerase (COG1904) and mannonate dehydratase (COG1312), suggesting that they may utilize glucuronate by the same pathway as found in E. coli . This pathway produces KDGlc which feeds into the Entner-Doudoroff pathway. H. utahensis also has a probable alpha-glucuronidase (Huta_0871) belonging to glycosyl hydrolase family 67, that is adjacent on the chromosome to glucuronate isomerase (Huta_0870) and mannonate dehydratase (Huta_0869). H. lacusprofundi has a putative mannonate dehydratase but no glucuronate isomerase, therefore it is unclear whether it has the capacity to break down glucuronate. Since H. lacusprofundi is known to grow on mannose , it is possible that mannonate dehydratase is used in a pathway for mannose degradation.
None of the haloarchaea have been shown to grow on L-arabinose, but the genomes suggest that it may be utilized by some haloarchaea. H. utahensis, H. volcanii, and H. turkmenica all have putative alpha-L-arabinofuranosidases (COG3534). In H. utahensis the arabinofuranosidase (Huta_1152) is close on the chromosome to L-arabinose isomerase (Huta_1154) and ribulose 5-phosphate 4-epimerase (Huta_1149), suggesting that H. utahensis uses the known bacterial pathway of L-arabinose degradation. A gene similar to ribulokinase was not found in H. utahensis, but there is a gene with similarity to xylulokinases (Huta_1150) close to the arabinose degradation genes. Huta_2446 is likely to be a xylulokinase in H. utahensis (see above), and Huta_1150 may be a ribulokinase, completing the pathway. This pathway produces D-xylulose 5-phosphate which enters the non-oxidative pentose phosphate pathway. H. utahensis is the only haloarchaeon to have the non-oxidative pentose phosphate pathway, which allows it to use this pathway, and it is also the only haloarchaeon to have L-arabinose isomerase.
Since the presence of family 18 glycosyl hydrolases in H. salinarum, H. mukohataei and H. borinquense indicates that they may possess chitinase activity and use chitin as a growth substrate, we attempted to identify enzymes for subsequent degradation of chitooligosaccharides, N-acetyl-glucosamine or glucosamine. We found that H. mukohataei likely possesses a beta-N-acetylhexosaminidase (Hmuk_3174) that has 51% similarity to characterized enzymes from Streptomyces thermoviolaceus  and Bacillus subtilis . A chitobiose deacetylase has been identified in Thermococcus kodakaraensis belonging to COG2120, which includes other carbohydrate deacetylases . Both H. mukohataei and H. borinquense have genes belonging to this family, although they are distantly related to the T. kodakaraensis enzyme. None of the organisms with family 18 glycosyl hydrolases has been tested for growth on N-acetylglucosamine or glucosamine , , so the presence of chitinase activity and chitinolytic pathway in haloarchaea needs further experimental elucidation.
The haloarchaea encode genes for two different glycerol utilization pathways. All except N. pharaonis have a glycerol kinase and glycerol 3-phosphate dehydrogenase, and the genes for both enzymes are found close together on the chromosome. Another pathway involving glycerol dehydrogenase and dihydroxyacetone kinase is present only in H. lacusprofundi. H. volcanii and H. walsbyi have a dihydroxyacetone kinase without glycerol dehydrogenase, and this may be used for metabolism of dihydroxyacetone from the environment . H. salinarum encodes a glycerol dehydrogenase but no dihydroxyacetone kinase.
Only H. mukohataei has an identifiable glycerol transporter within the genome. It encodes a member of the Major Intrinsic Protein (MIP) family adjacent to glycerol kinase, providing strong evidence for a glycerol transport function. All other haloarchaea that have a glycerol kinase have an uncharacterized membrane protein adjacent (e.g. rrnAC0550), and we predict that these genes encode a new family of glycerol transporters. H. borinquense has two glycerol kinases and both have this uncharacterized membrane protein family adjacent to the kinase gene. There are also bacterial homologs of this membrane protein family, and many of them are adjacent to genes involved in glycerol or propanediol metabolism.
H. lacusprofundi is the only halophile that has been shown to grow on propionate, but all of the haloarchaeal genomes, with the exception of H. utahensis, contain genes that may encode the methylmalonate pathway for conversion of propionate to succinyl-CoA. All except H. utahensis have methylmalonyl-CoA epimerase (TIGR03081) and methylmalonyl-CoA mutase (COG1884 and COG2185). Also they have a biotin carboxylase protein (COG4770) and a carboxyltransferase protein (pfam01039), subunits of a biotin-dependent carboxylase. All except H. utahensis also contain a biotin-protein ligase (COG0340) and a BioY family biotin transporter (pfam02632). Propionate or propionyl-CoA may be produced intracellularly from the breakdown of fatty acids, amino acids, or other compounds, or these organisms may be able to use propionate from the environment produced as a result of fermentation.
Glycine betaine is a compatible solute which is likely to be present in high-salt environments. All of the haloarchaeal genomes except that of H. mukohataei encode members of the betaine/carnitine/choline transporter (BCCT) family, which transport glycine betaine and related compounds. Most have one or two members of this family, but H. turkmenica has seven. In addition, H. turkmenica has an ABC transporter for compatible solutes. Four of the haloarchaeal genomes – H. marismortui, H. walsbyi, H. volcanii, and H. turkmenica – encode one or two genes with high similarity to dimethylglycine oxidase from Arthrobacter globiformis . In all four genomes these oxidase genes are close on the chromosome to BCCT family transporters. The presence of these enzymes and transporters raises the possibility that some of the halophiles may be able to utilize glycine betaine, dimethylglycine, and/or sarcosine. However, in H. walsbyi, betaine was not found to enhance growth  and H. utahensis could not grow on betaine .
Our analysis of the ten haloarchaeal genomes provided a phylogenetic tree in which all nodes were well-supported. We here followed the ‘total evidence’ approach for inferring the species tree, which dictates that the best phylogenetic hypothesis is the one based on all available data , and that conflict between the species tree and gene trees can at least as well as via inferring the gene trees be quantified after combined analysis , . Total evidence has been criticized as a ‘verificationist’ approach, particularly by researchers who question the concept of a microbial tree of life (TOL) in general . Other authors counter that concatenated analysis is well rooted in the ‘Popperian principles of background knowledge and corroboration’, and that whether a TOL exists can be assessed, among other means, by checking for high branch support, which would indicate a strong treelike signal, and by comparing previous phylogenetic or taxonomic hypotheses . These issues are of considerable importance for the future of Prokaryote classification . The mostly maximal bootstrap support observed here indicates that Halobacteriaceae have evolved in manner consistent with a TOL (Figure 1), which is supported by the majority of the genes (Table S1; Figure S1). Moreover, our supermatrix tree is fully in agreement with the current taxonomy of ingroup and outgroup, whereas considerable conflict was observed in a recent total evidence analysis of Pasteurellaceae . The single exception is the branch connecting H. borinquense and H. walsbyi, which is supported by 700 genes and contradicted by 565 ones, yielding a total positive support of 2,422 steps and a total negative support of −2,366 steps. Considerable incongruence between gene trees may thus be responsible for the low support under MP, but even this branch is maximally supported under ML (Figure 1).
While our results are in agreement with the optimistic view regarding TOL inference from supermatrices, they nevertheless also indicate that disagreement with the species tree is considerable for some genes (Figures S1 and S2). It is possible to distinguish the effects of artifacts of the phylogenetic inference method, caused e.g. by a low signal-to-noise-ratio, from those of horizontal gene transfer (HGT) because in the former case a correlation between gene length and the extent of disagreement between gene tree and species tree occurs . This correlation is significant in our analysis (Figure S1), but a number of genes appear as outliers of the regression, indicating distinct causes of incongruence such as HGT. The distribution of the median total PBS values over the COG categories reveals that genes related to information processing and storage are more in accordance with the species tree, corresponding to the view that such genes are less frequently horizontally transferred between organisms. However, many exceptions from this rule exist (Table S1; Figure S1), as also observed in a recent analysis of a comprehensive genomic dataset of Prokaryotes . In any case, total evidence analysis in conjunction with partitioned Bremer support  apparently worked well in identifying those genes most in disagreement with the species trees (Figure S2). Among the five ‘worst’ gene trees, those for L-lactate permease, Tyrosyl-tRNA synthetase and Cobalamin biosynthesis protein CobN did not comprise any ingroup paralogs in their OrthoMCL clusters; thus, horizontal gene transfer is the most likely explanation for their considerable incongruence with the species tree (Figure S2). HGT between Candidatus Desulforudis audaxviator and Archaea has been suggested in the literature for CobN  and between Opisthokonta and Archaea for Tyrosyl-tRNA synthetase . In contrast, the OrthoMCL clusters containing either Glucosamine 6-phosphate synthetase or Acyl-coenzyme A synthetase comprised a combination set of inparalogs and possible outparalogs; that is, their disagreement with our species tree estimate is most likely due to a complicated gene duplication/gene loss pattern which may not optimally have been resolved by the OrthoMCL algorithm.
While there were few habitat-specific clusters, soil/sediment halophiles were found to have more glycosyl hydrolases as well as genes involved in siderophore synthesis and cell wall metabolism. Some of the halophiles analyzed here were isolated from water (H. walsbyi, N. pharaonis, H. marismortui, H. borinquense), while others were isolated from soil (H. mukohataei, H. turkmenica) or lake sediment (H. volcanii, H. utahensis). We looked for gene clusters found exclusively in the water halophiles or in the soil/sediment halophiles, but very few clusters were found. There may be several explanations for this finding. One possibility is that the change from water to sediment or vice versa has happened several times independently, and different changes in the genome occurred during each round of adaptation. This explanation is supported by the fact that the water and soil/sediment halophiles do not form separate clades in the species phylogenetic tree (Figure 1). Another potential explanation is that the division between water and sediment is not clear-cut. Even though some of these organisms were isolated from water or sediment, they may live part of the time in both environments. Nevertheless, there were some clusters with known functions found in the soil/sediment group and not in the water group. The soil/sediment halophiles tend to have greater numbers of glycosyl hydrolases. Each of the four soil/sediment halophiles has between 15 and 44 glycosyl hydrolases, while the haloarchaea isolated from water have between zero and twelve glycosyl hydrolases. The soil/sediment halophiles also have clusters involved in siderophore synthesis that are missing from the water group. This may be explained by the fact that siderophores are less likely to diffuse away from the producing organism in soil or sediment. Finally the soil/sediment group has two clusters likely to be involved in cell wall metabolism. This may indicate a reaction to the more complex environments that they inhabit.
Differences in central metabolism in H. utahensis may make it easier for this organism to grow on pentoses. One of the findings from this study is that H. utahensis is substantially different from the other halophiles in its central metabolism. It may lack gluconeogenesis, and it appears to use the non-oxidative pentose phosphate pathway and a transhydrogenase instead of the oxidative pentose phosphate pathway used by other haloarchaea. It has the fewest amino acid degradation pathways of any of the sequenced haloarchaea, and thus appears to be the only one of the ten haloarchaea studied here that is specialized only for carbohydrate utilization.
The use of the non-oxidative pentose phosphate pathway may allow for more flexibility in the ability to utilize pentoses as carbon and energy sources. H. utahensis is known to degrade xylan and can grow on xylose , . The other halophiles have a different xylose degradation pathway that produces 2-oxoglutarate. The xylose and L-arabinose degradation pathways of H. utahensis are likely to feed into the pentose phosphate pathway, thus producing fructose 6-phosphate and glyceraldehyde 3-phosphate from phosphorylated pentoses. However, the fate of fructose 6-phosphate is unclear. Halophiles are thought to lack phosphofructokinase, but several including H. utahensis have putative fructose 1-phosphate kinase. A possible pathway for fructose utilization would involve the conversion of fructose 6-phosphate to fructose 1-phosphate, followed by phosphorylation to form fructose 1,6-bisphosphate, which would then enter the Embden-Meyerhof pathway. However, further experimental work will be needed to determine how pentoses are metabolized in H. utahensis.
The distribution of catabolic pathways and the protein sequence conservation of the associated enzymes suggest that the ancestor of haloarchaea could degrade many amino acids but few carbohydrates. The haloarchaea possess pathways for the utilization of amino acids, carbohydrates, and other compounds. The amino acid degradation pathways are found in four to ten of the genomes, and the sequences of the enzymes are closely related, suggesting that they were present in the ancestor of haloarchaea. Three of the genomes have five or fewer amino acid catabolic pathways (H. walsbyi, H. utahensis, and N. pharaonis), while the remaining genomes have at least seven pathways. H. walsbyi and N. pharaonis also have few glycosyl hydrolases and carbohydrate utilization pathways, and they use very few compounds as energy and carbon sources. H. utahensis on the other hand has a large number of glycosyl hydrolases and sugar utilization pathways, showing that it has become specialized for growth on carbohydrates.
In contrast to amino acid utilization pathways, alternative pathways are used for sugar catabolism. For example, H. utahensis uses a different xylose degradation pathway than the others, and fructose phosphorylation can occur via the phosphotransferase system or ketohexokinase. In addition, H. borinquense is known to grow on fructose and xylose, but it lacks the catabolic enzymes found in other haloarchaea. However, some genes and pathways are highly conserved. The enzymes of the semi-phosphorylated Entner-Doudoroff pathway are closely related in sequence, suggesting that glucose utilization by this pathway was present in the haloarchaeal ancestor. Fructose 1-phosphate kinase is found in five haloarchaeal genomes and is highly conserved. Similarly galactonate dehydratase is found in six of the ten genomes and forms a single phylogenetic group. Overall it appears that the ancestor of haloarchaea was able to use up to ten amino acids as energy and carbon sources, while its ability to use sugars was limited.
Halophilic glycosyl hydrolases have potential uses in polysaccharide degradation related to biofuel production. An unexpected result from this analysis was the high number of glycosyl hydrolases in two of the organisms. H. utahensis has numerous genes related to cellulases and xylanases, while H. turkmenica has a large number of predicted pectin-degrading enzymes. Salt-adapted glycosyl hydrolases from haloarchaea may have applications in the depolymerization of plant material for biofuel production. Plant material is pretreated in order to remove lignin and hemicellulose and to reduce the crystallinity of cellulose. Several different methods are used, some of which involve incubation with acid or base . After treatment with these chemicals, a neutralization step is required before further processing, and this produces a salty solution. Salt-adapted glycosyl hydrolases may be useful at this point in the process. Also, treatment of plant material with ionic liquids has been shown to reduce the crystallinity of cellulose and enhance its hydrolysis . One of the glycosyl hydrolase family 5 enzymes of H. utahensis has been shown to be a cellulase and to be active in an ionic liquid (T. Zhang et al., in press). Carrying out hydrolysis of lignocellulose under high-salt conditions has the advantage that the possibility of contamination is low.
Sum of partitioned Bremer support over all branches plotted against the number of parsimony-informative characters for all OrthoMCL clusters present in at least four ingroup genomes. Colors are according to the COG classes: blue, “Information Storage and Processing” (five categories); light blue, “Cellular Processes and Signaling” (ten categories); dark red, “Poorly characterized” (two categories); orange, “Metabolism” (eight categories). The solid line represents a robust-line fit, the dotted line the threshold between overall positive and negative support for the species tree.
Ingroup-only maximum likelihood (ML) phylogenetic trees inferred from the five OrthoMCL clusters with the most negative overall partitioned Bremer support, i.e., the five genes most in conflict with the species tree (Figure 1). The branches are scaled in terms of the expected number of substitutions per site. Numbers above branches are support values from ML (left) and maximum parsimony (MP; right) bootstrapping. Midpoint rooting  was applied to all trees. (A) COG1620 (L-lactate permease); (B) COG0449 (Glucosamine 6-phosphate synthetase, contains amidotransferase and phosphosugar isomerase domains); (C) COG1429 (Cobalamin biosynthesis protin CobN and related Mg-chelatases); (D) COG0162 (Tyrosyl-tRNA synthetase); (E) COG0365 (Acyl-coenzyme A synthetases/AMP-[fatty] acid ligases).
Sum of partitioned Bremer support (PBS) values for all OrthoMCL clusters in which at least four ingroup genomes were present, aggregated according to the corresponding COG categories and classes, after correcting for the effect of the number of genomes represented in each cluster and the number of parsimony-informative characters. Median support is positive for most categories; the fact that most mean support values are negative is most likely due to the presence of few outliers (see Figure S2).
Core clusters. Spectral clusters found in all haloarchaeal genomes. For each cluster the predicted function and list of locus tags are listed.
Signature clusters. Spectral clusters found in all haloarchaeal genomes and not found in any other sequenced archaeal genome. The predicted function and locus tags are listed.
Habitat-specific clusters. Spectral clusters found exclusively in one habitat type and not in the other habitat type. The predicted function and locus tags are listed.
Organisms used in this study and the RefSeq accession numbers for their genome sequences.
Competing Interests: The authors have declared that no competing interests exist.
Funding: This work was supported by the Office of Science of the United States Department of Energy (http://www.er.doe.gov/) under Contract No. DE-AC02-05CH112. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.