Genome evolution of microbes involves parent-to-offspring descent, and lateral genetic transfer that convolutes the phylogenomic signal. This study investigated phylogenomic signals among thousands of microbial genomes based on short subsequences without using multiple-sequence alignment. The signal from ribosomal RNAs is strong across all taxa, and the signal of plasmids is strong only in closely related groups, particularly Proteobacteria. However, the signal from other chromosomal regions (∼99% of the genomes) is remarkably restricted in breadth. The similarity of subsequences is found to correlate with taxonomic rank and informs on conserved and differential core functions relative to niche specialization and evolutionary diversification of microbes. These results provide a comprehensive, alignment-free view of microbial genome evolution as a network, beyond a tree-like structure.
KEYWORDS: core functions, k-mers, networks, phylogenetic analysis, phylogenomics
ABSTRACT
Microbial genomes have been shaped by parent-to-offspring (vertical) descent and lateral genetic transfer. These processes can be distinguished by alignment-based inference and comparison of phylogenetic trees for individual gene families, but this approach is not scalable to whole-genome sequences, and a tree-like structure does not adequately capture how these processes impact microbial physiology. Here we adopted alignment-free approaches based on k-mer statistics to infer phylogenomic networks involving 2,783 completely sequenced bacterial and archaeal genomes and compared the contributions of rRNA, protein-coding, and plasmid sequences to these networks. Our results show that the phylogenomic signal arising from ribosomal RNAs is strong and extends broadly across all taxa, whereas that from plasmids is strong but restricted to closely related groups, particularly Proteobacteria. However, the signal from the other chromosomal regions is restricted in breadth. We show that mean k-mer similarity can correlate with taxonomic rank. We also link the implicated k-mers to genome annotation (thus, functions) and define core k-mers (thus, core functions) in specific phyletic groups. Highly conserved functions in most phyla include amino acid metabolism and transport as well as energy production and conversion. Intracellular trafficking and secretion are the most prominent core functions among Spirochaetes, whereas energy production and conversion are not highly conserved among the largely parasitic or commensal Tenericutes. These observations suggest that differential conservation of functions relates to niche specialization and evolutionary diversification of microbes. Our results demonstrate that k-mer approaches can be used to efficiently identify phylogenomic signals and conserved core functions at the multigenome scale.
IMPORTANCE Genome evolution of microbes involves parent-to-offspring descent, and lateral genetic transfer that convolutes the phylogenomic signal. This study investigated phylogenomic signals among thousands of microbial genomes based on short subsequences without using multiple-sequence alignment. The signal from ribosomal RNAs is strong across all taxa, and the signal of plasmids is strong only in closely related groups, particularly Proteobacteria. However, the signal from other chromosomal regions (∼99% of the genomes) is remarkably restricted in breadth. The similarity of subsequences is found to correlate with taxonomic rank and informs on conserved and differential core functions relative to niche specialization and evolutionary diversification of microbes. These results provide a comprehensive, alignment-free view of microbial genome evolution as a network, beyond a tree-like structure.
INTRODUCTION
For nearly 100 years following the discovery of diverse bacteria by Pasteur, Koch, Cohn, and others in the latter decades of the 19th century (1), little was known of how these organisms might be related among themselves or to the rest of the living world. This began to change with the recognition that ribosomal RNAs are present in all living cells and contain structural domains that, by virtue of their differential entanglements with core molecular functions and their interactions with greater or lesser numbers of other components of the translational apparatus, can inform on evolutionary history across a range of temporal scales “much as the hands of a clock separately indicate hours, minutes, and seconds” (2). Given the central role of translation in the emergence of phenotype from genotype and the number and interrelatedness of these structural and functional constrains, it was assumed that statistical analysis of rRNA sequences would recover the tree of vertical descent not merely of the corresponding genes but also, much more interestingly, of the host organisms. As it happened, the PCR method was invented at about the same time (3), and the presence of conserved 5′ and 3′ regions made the rRNA gene an attractive target for amplification and sequencing. Thus, Darwin’s Great Tree of Life quickly became universal, and, as a bonus, Archaebacteria (Archaea) were recognized as a distinct domain of living organisms.
As molecular evolutionary studies were extended into families of protein-coding genes, congruent topologies were often (but not always) recovered (4). In contrast to expectation, instances of incongruence often failed to be resolved as data sets grew larger and statistical methodology for phylogenetic inference improved. It also became clear that many microbes can exchange genetic material through the mediation of plasmids or phage and/or take up DNA from their environment. Depending on the breadth and granularity of the data, phylogenetic trees inferred for regions of lateral origin may thus contain edges that directly connect lineages that are nonadjacent in the rRNA tree. That is, lateral genetic transfer creates phylogenomic networks. Plasmid and phage sequences in particular are expected to increase the connectivity of phylogenomic networks, although any genetic material that becomes established in a new host genome after transmission by such a vector can contribute.
The resulting pattern of phylogenomic relationships has been described (by the use of diverse metaphors) as fundamentally treelike (5, 6), as a tree overgrown with tiny vines (7), as a ring (8, 9), as a coral (10), as a web (7, 11), as a network with some treelike regions (12), or simply as a network (13, 14). Networks of lateral genetic transfer (11, 13) highlighted the need to visualize contributions of different genomic regions on a broad scale.
Complete genome sequences are now available for thousands of bacterial and archaeal species, making it possible to assess microbial evolution globally and, often, at considerable phyletic depth. However, until recently these studies were necessarily biased in favor of alignable regions, i.e., genes, as classical phylogenomic workflows are based on multiple-sequence alignment (MSA) of putative orthogroups. Recently, so-called alignment-free (AF) approaches have been shown to perform well in phylogenetic inference from simulated and empirical (microbial genome) data sets (15; see references 16, 17, and 18 for recent reviews).
An important class of AF methods consists of approaches based on subsequences of fixed length, known as k-mers. These methods typically compute a matrix of distances on the basis of, e.g., the number of shared k-mers, which can then be used to generate a tree by the use of, e.g., neighbor joining (19) or a similarity network (20). Alternatively, k-mers of lateral origin can be recognized (11, 21, 22) and used to generate a directional network in which the edges natively represent inferred lateral relationships. The use of k-mers in phylogenetics is biologically intuitive (23, 24); the earlier works of Carl Woese and colleagues (25–27) showed that short (enzymatically digested) oligonucleotides of 16S/18S ribosomal RNAs carry significant phylogenetic (and thus, homology) signal and reveal the three domains of life. AF approaches can recover homology signal among molecular sequences at the genome scale and have been successfully applied to genomes of bacteria and archaea (15, 28–30), organelles (31), plants (31), and primates (30) as well as to microbial metagenomes (30).
AF methods can be more robust than MSA-based approaches to among-site rate heterogeneity, compositional bias, rearrangement, and insertion-deletion events (15, 32) and are scalable for very large data sets (32, 33). We earlier generated an AF phylogenetic network for 143 bacterial and archaeal genomes (29) using pairwise k-mer distances computed using the D2S statistic (34, 35). By varying similarity thresholds, we could easily display changes of network structure, e.g., the progressive separation of genomic lineages (29) or the disappearance of cliques (putative “genetic exchange communities” [11, 36]).
Here we used k-mer methods and the D2S statistic to infer phylogenomic networks for 2,783 complete prokaryote genomes and investigated the contribution of different components of the data to the phylogenetic signals captured by AF methods. Specifically, we compared AF networks inferred using (i) complete genomic data sets, including plasmids, if any; (ii) chromosomal sequences without rRNA genes; (iii) only rRNA genes; and (iv) only plasmid sequences. Using an advanced database approach, we investigated the core functions that are specific to particular phyletic groups or genera on the basis of the shared k-mers.
RESULTS
For each subset of the data (see above), we first calculated a distance d between the genomes in a given pair (a and b) using the D2S distance measure and k = 25 (see Materials and Methods). The value of k = 25 was found to capture an adequate level of uniqueness among 1,121 complete bacterial genome sequences and is thus suitable for deriving a metric of relatedness among bacterial genomes (37). We transformed the distance between genome a and genome b (dab) into a similarity value (Sab) and generated a similarity network using a method that we described previously (29). These networks capture the relatedness among these genomes, i.e., are phylogenomic, although the relative contributions of the vertical and lateral components (which may be admixed) depend on the subset of data used as input. Here we define a threshold t for which only edges with S values that are ≥t are considered in the network. To compare our results at the genome and phylum levels, we generated I-networks in which nodes represent distinct genome isolates and edges indicate evidence of shared k-mers and also generated P-networks in which nodes represent distinct phyla and edges represent the number of isolates (summed over both nodes) that share k-mers with isolates of the other phylum (see Materials and Methods). Given the taxon richness of Proteobacteria, we evaluated its subgroups (e.g., Alphaproteobacteria and Betaproteobacteria) as individual phyla. We then compared the k-mer networks based on the topological differences between them at different t values. All I- and P-networks of these 2,705 genome isolates are available at https://doi.org/10.14264/uql.2017.436.
AF networks of microbial evolution.
We first inferred phylogenomic networks based on a data set of 2,783 completely sequenced microbial genomes (2,618 bacterial genomes and 165 archaeal genomes [total of 9,582,718,896 bases]) downloaded from NCBI on 31 January 2016 (see Data Set S1 in the supplemental material), including plasmid sequences if present. Where two or more genomes had identical contents of 25-mers (D2S distance = 0), only one was retained. We also removed edges for which the D2S distance was >10; these genomes share ≤0.01% of 25-mers with any other genome. Following this filtering step, we took 2,705 genomes forward into subsequent analyses. For each network, we systematically assessed the number of nonsingleton nodes (c) (i.e., the number of nodes with one or more edges), the size of the maximal clique (i.e., the clique with the largest number of genomes) (z), and the number of cliques (n) across various levels of the similarity score threshold (t). We required a clique to contain three or more edges and defined D as the density of a network, i.e., the proportion of edges among all possible edges in a network (Fig. 1; see also Materials and Methods).
The network topology changes substantially with similarity threshold: at t = 0, c = 2,705 and z = 2,704, compared to c = 1,358 and z = 48 at t = 9 (Table 1). As we increase the stringency of the threshold of shared similarity, the network becomes less connected, and distinct subsets corresponding to diverse taxa (i.e., phyla, classes, and genera) start to emerge. In this network, many bacterial phyla are represented in a single subgraph at t = 4, most phyla can be identified as distinct sets at t = 5, and all proteobacterial classes are separate from each other at t > 5.
TABLE 1.
Threshold | No. of nonsingleton nodes, c | Density, D | Size of the maximal clique, z | No. of cliques, n |
---|---|---|---|---|
0 | 2,705 | 0.998 | 2,704 | 10 |
1 | 2,705 | 0.989 | 2,701 | Not available |
2 | 2,705 | 0.513 | 860 | Not available |
3 | 2,680 | 0.079 | 339 | 1,662,785 |
4 | 2,378 | 0.019 | 211 | 6,181 |
5 | 2,091 | 0.008 | 124 | 3,344 |
6 | 1,860 | 0.005 | 82 | 525 |
7 | 1,676 | 0.003 | 64 | 229 |
8 | 1,538 | 0.003 | 61 | 224 |
9 | 1,358 | 0.002 | 48 | 232 |
The I-network is very densely connected at t = 0, with the maximum number of cliques n = 10. The value n is too great to be computed at t =1 or t = 2, but n = 1,662,785 at t = 3 and decreases to 232 at t = 9 (Table 1). Most isolates are members of a single large clique at t = 0 and t = 1 (D > 0.98 in both cases); at t = 2, D = 0.513. The network becomes less dense at t = 3 (D = 0.079; Table 1). As this network of 2,705 nodes remains too densely connected to be visualized and analyzed directly, we generated the P-network using the same data, with each node representing a phylum. Figure 2 shows the P-network of the 2,705 genomes at t = 3 (dynamic view available at http://bioinformatics.org.au/tools/AFmicrobes/). The width (thickness) of each edge represents the number of instances in which any two genomes (one from each phylum connected by the edge) have similarity S≥t; the width is relative to the number of connected genome pairs between two phyla. Major phyla (e.g., Betaproteobacteria and Gammaproteobacteria, Firmicutes, Actinobacteria, and Tenericutes) are clearly separated at t = 3. The thickest edge (in red) is between the Betaproteobacteria and Gammaproteobacteria (7,568 connected genome pairs; see Fig. S1A in the supplemental material), suggesting a high similarity among genomes between these groups. In addition, we also observed a large proportion of shared 25-mers between Firmicutes and each of the proteobacterial classes.
Phylogenomic signal contributed by rRNA genes.
To determine the contribution of the rRNA genes to our AF networks, we first excluded from our set of 2,705 unique genomes (see above) the 89 genomes that did not have gene annotation, and we excluded from the remaining 2,616 all rRNA gene sequences based on annotated start and stop coordinates (see Materials and Methods). The density of the I-network of genomes from which rRNA genes have been removed was lower than in the I-network inferred using the whole data set. Similarly to what we observed for the I-networks described in the previous section, here, at t = 0, c = 2,615 and z = 1,226, and these values decreased to c = 1,290 and z = 47 at t = 9 (Table 2). At t = 3, the I-network of the rRNA gene-free network had a network density of D = 0.026, 3-fold lower than the D = 0.079 in the whole-genome network (Table 1). Figure 3 shows the P-network of these 2,616 genomes at t = 3 (dynamic view available at http://bioinformatics.org.au/tools/AFmicrobes/). As in Fig. 2, the thickest edge (in red), between Betaproteobacteria and Gammaproteobacteria (Fig. 3), indicates the largest number of instances of shared k-mers between genomes from these two groups. This P-network is less dense than the equivalent network based on the whole data set (shown in Fig. 2). Although we observed fewer connections between phyla after removal of rRNA sequences from the genome data, many of the major connections observed in Fig. 2 remained, e.g., the connections between Betaproteobacteria and Gammaproteobacteria (404 connected genome pairs) and between Actinobacteria and Gammaproteobacteria (57 connected genome pairs) (see Fig. S1B). Thus, the sharing of 25-mers contributing to these major connections extends beyond the rRNA genes commonly used as phylogenetic markers.
TABLE 2.
Threshold | No. of nonsingleton nodes, c | Density, D | Size of the maximal clique, z | No. of cliques, n |
---|---|---|---|---|
0 | 2,615 | 0.490 | 1,226 | Not available |
1 | 2,597 | 0.219 | 548 | Not available |
2 | 2,555 | 0.072 | 367 | 164,221 |
3 | 2,394 | 0.026 | 220 | 5,379 |
4 | 2,182 | 0.012 | 159 | 5,139 |
5 | 1,959 | 0.006 | 117 | 631 |
6 | 1,761 | 0.004 | 74 | 299 |
7 | 1,591 | 0.003 | 62 | 120 |
8 | 1,460 | 0.003 | 59 | 117 |
9 | 1,290 | 0.002 | 47 | 131 |
A network computed using only the rRNA sequences was denser than the two corresponding I-networks described above. At t = 6, D was high at 0.635 (z = 1,321; see Table S1 in the supplemental material) compared to 0.005 (z = 82) and 0.004 (z = 74) in the I-networks based on whole-genome and rRNA gene-removed data, respectively. Figure S2 shows the P-network of 2,616 genome isolates based solely on rRNA genes at t = 6. Although almost all phyla were connected to each other (c = 2,613 and z = 1,321 at t = 6), we observed a clear separation between the Archaea and Bacteria. These results imply that rRNA gene sequences contain sufficient information to distinguish Archaea from Bacteria by the use of a k-mer approach, but separation of bacterial phyla would require further tuning of k and t.
Phylogenomic signal contributed by plasmid genomes.
Among the genome data records available to this study, 921 (representing 26 phyla) include sequence annotated as arising from one or more extrachromosomal plasmids. To examine the phylogenomic signal contributed by these plasmids, we computed I- and P-networks using only the plasmid sequences for these 921 isolates (see Materials and Methods). Figure 4 shows the I-network of the 921 plasmid genomes at t = 0, in which D = 0.025 (c = 745 and z = 48; Table 3); a dynamic view is available at http://bioinformatics.org.au/tools/AFmicrobes/. Most phyla appear as distinct cliques, but, notably, there are edges between Proteobacteria and Actinobacteria and between Proteobacteria and Firmicutes. At t = 4, most phyla are separated as distinct cliques, with the exception of Epsilonproteobacteria and Firmicutes; the other Proteobacteria (Alphaproteobacteria, Betaproteobacteria, Deltaproteobacteria, and Gammaproteobacteria) are in a distinct paraclique. The Euryarchaeota, connected only to the bacterial phylum Planctomycetes at t = 0, is separated from Bacteria at t ≥ 1. All phyla are disjoint at t = 7. These results are not surprising, as the plasmid genomes can have a narrow host range (38, 39) and are known to evolve faster than the core genomes (40); in combination with their smaller genome size, fewer shared k-mers are observed at a given similarity threshold (41).
TABLE 3.
Threshold | No. of nonsingleton nodes, c | Density, D | Size of the maximal clique, z | No. of cliques, n |
---|---|---|---|---|
0 | 745 | 0.025 | 48 | 20,557 |
1 | 718 | 0.021 | 46 | 13,272 |
2 | 680 | 0.017 | 45 | 3,925 |
3 | 648 | 0.014 | 39 | 1,406 |
4 | 601 | 0.011 | 34 | 800 |
5 | 556 | 0.009 | 30 | 589 |
6 | 499 | 0.006 | 25 | 368 |
7 | 439 | 0.004 | 13 | 122 |
8 | 353 | 0.002 | 11 | 26 |
9 | 245 | 0.001 | 9 | 14 |
For each genome pair, we further compared its D2S distance derived from whole genome data set to those derived from distinct genome components (Fig. S3). Distances derived from rRNA sequences are almost always smaller than the distances derived from the overall data set. The reverse trend is observed for distances derived from chromosomal sequences with rRNAs removed (although a one-to-one relationship is observed) and to a greater extent for those derived from plasmid sequences.
Network comparison.
Figure 5 shows the density D for all four I-networks as a function of threshold t. For all networks, the network density decreases as t increases. At t > 2, the rRNA gene-only network is denser than the others, with D remaining >0.63 through t = 6, compared to D < 0.02 for the others at t > 3. As expected, the highest density of the complete-genome network is observed at t < 2; D > 0.98 and decreases rapidly at 2 < t < 5. The network without rRNA genes exhibits a lower density, D < 0.5, at t = 0, and by t = 5, D has decreased to a level similar to that calculated for the complete-genome network (D < 0.01). Together with our observed pairwise genome distances based on distinct genome components (Fig. S3), these results confirm that rRNA sequences (as captured by 25-mers) are more highly conserved than are the genome sequences overall. The data corresponding to the whole-genome and rRNA-free networks differ through a similar range of network densities, whereas data corresponding to the rRNA gene network differ at a higher threshold (i.e., t > 5). The plasmid network shows the lowest density, with D < 0.03 at t ≥ 0 (Fig. 5), indicating that these plasmid genomes are more diverse in 25-mer composition than are the corresponding main genomes. The results presented in Fig. 5 provide a guide for visualization and comparison of these networks at the appropriate t values. In this study, we chose t values that would yield a clear separation of Bacteria and Archaea; thus, we used t = 3 for visualizing the two networks shown in Fig. 2 and 3 (i.e., the use of the same t value for both networks is purely coincidental) and t = 0 for the plasmid network shown in Fig. 4.
To assess the (individual) contributions of rRNA genes and plasmids to the relatedness among the distinct phyla, we calculated for each phylum pair a connectedness value C, representing the proportion of genome pairs that share one or more k-mers over all possible genome pairs in the two phyla (see Materials and Methods). As shown in the heat map summaries (Fig. 6), the hierarchical clustering of C values does not conform to known phyletic relationships; e.g., proteobacterial groups are not unified a single cluster. In the all-inclusive genome network (Fig. 6A), the archaeal phyla (Crenarchaeota and Euryarchaeota) are not clearly separated from the Bacteria phylum and show substantial connectedness with Tenericutes (C > 0.63) and Chlamydiae (C > 0.54). The highest mean C value (0.85) was observed in the network consisting only of rRNA genes (Fig. 6B), with Archaea and Bacteria clearly separated. Crenarchaeota shows substantial connectedness (C > 0.5) with 11 bacterial phyla, compared to Euryarchaeota with 6; both cases include Deinococcus-Thermus, Aquificae, and Thermotogae. The removal of rRNA genes from the genome sequences appears to have removed most of the connectedness among phyla (mean C = 0.05 in Fig. 6C), with the maximum C = 0.59 between Betaproteobacteria and Gammaproteobacteria. Even less phylum-level connectedness was observed in the plasmid-only network (Fig. 6D; mean C = 0.002), with maximum C = 0.029 between Betaproteobacteria and Gammaproteobacteria. These results indicate the complications of inferring a tree-like structure among these taxa using genome-wide k-mers and that whole-genome and plasmid sequences capture phyletic relatedness that is distinct from that captured by the rRNA genes. Remarkably, chromosomal sequences, apart from rRNA genes, although usually representing more than 99% of the genome sequences, contribute little to overall phylogenetic signal.
Core k-mers of microbial genera.
We define a core k-mer in a group of interest as a k-mer that is present in every genome within the group, e.g., a core 25-mer in Proteobacteria is present in all proteobacterial genomes in our database (see Materials and Methods). We identified core 25-mers for each genus in our 2,783-genome data set. Of these 699 genera, 497 are represented by only a single genome isolate, and a further 51 consist of highly divergent genomes for which no core 25-mers were identified; we exclude these data from this part of analysis. The remaining 151 genera for which core 25-mers were identified are listed in Table S2. As these genera are represented in our data set by different numbers of isolates, we define K as the number of distinct core k-mers per isolate for each genus; this value can help describe the extent of genome divergence (and thus the evolutionary rate of these genomes) within each of these genera. Thus, the three genomes representing genus Azotobacter show the highest number of core k-mers, and K = 1,722,079; these genomes represent distinct isolates of the same species, Azotobacter vinelandii. This is in contrast to the 123 Streptococcus genomes (in 27 described species), which share only one core k-mer (K = 0.01). Among the 20 genera with the greatest K values, Shigella is represented here by the greatest number of distinct isolates (10 from four species), and K = 33,698. This number compares to K = 4.82 among the 11 Ralstonia genome isolates from three species. Thus, these Shigella genomes have diverged much less from their common ancestor than have these Ralstonia genomes from theirs, as assessed by shared 25-mers. This result also lends support to the earlier discovery of extensive gene dispersal among six genomes of Ralstonia solanacearum (of the 11 Ralstonia isolates in our data set) (42).
Core functions of microbial phyla.
To relate the shared k-mers to biological functions, for all 25-mers in these 2,783 genomes we organized the genome coordinates of each instance, and the biological function annotated for the gene product encoded at those coordinates, in a relational database. Functional annotation was based on Clusters of Orthologous Groups (COGs) (43). Then, using the list of core 25-mers described above, we grouped these 25-mers by taxon, focusing on protein-coding sequences (i.e., rRNA sequences were discarded; see Materials and Methods). This yielded a set of core 25-mers for 112 genera in 16 phyla; the corresponding COG functional categories for these core 25-mers are shown in Table S3. The noninformative functional categories R (general function prediction only) and S (function unknown) were excluded from subsequent analyses. No core k-mer in our data set was found to be associated with functional category Y (nuclear structure). Functional categories represented at <1% of core k-mers in each genus included category A (RNA processing and modification), category B (chromatin structure and dynamics), category W (extracellular structure), and category Z (cytoskeleton).
We found core k-mers associated with functional category A only in the proteobacterial classes Alphaproteobacteria, Betaproteobacteria, Gammaproteobacteria, and Deltaproteobacteria (i.e., not in the Epsilonproteobacteria) and in phylum Actinobacteria and those associated with functional category B only in phyla Chloroflexi, Euryarchaeota and Thaumarchaeota. Figure 7 shows the proportions of the five most-frequent COG categories associated with core 25-mers across the 23 COG categories for 16 phyla. Categories E (amino acid metabolism and transport) and C (energy production and conversion) are among the five most abundant categories in 15 and 13 phyla, respectively. The Epsilonproteobacteria, Thaumarchaeota, Euryarchaeota, Actinobacteria, Cyanobacteria, and Chloroflexi represent the only phyla with category H (coenzyme metabolism) among the five most abundant. For the phyla Tenericutes, Deinococcus-Thermus, Firmicutes and Crenarchaeota, the most-represented functional categories include P (inorganic ion transport and metabolism), L (replication and repair), J (translation), E (amino acid transport and metabolism), and G (carbohydrate metabolism and transport). Bacteroidetes is the only phylum for which categories O (posttranslational modification, protein turnover, and chaperone functions), Q (secondary structure), and F (nucleotide metabolism and transport) are among the top five. Phylum Spirochaetes is the only one with U (intracellular trafficking and secretion) and T (signal transduction) among the five most abundant, but very few COGs are associated with core 25-mers.
Comparing the annotated core k-mers in each phylum to all annotated core k-mers, 11 of the 25 COG functional categories are significantly enriched in Gammaproteobacteria (Fisher’s exact test, Benjamini-Hochberg [44]-adjusted P ≤ 0.05), 9 in Alphaproteobacteria, 9 in Actinobacteria, 8 in Deltaproteobacteria, and 7 in Firmicutes (Table S4). This observation may be due to the large (73.6%) representation of taxa of these phyla in the overall 2,783 data set: 1,163 (41.8%) Proteobacteria, 601 (21.6%) Firmicutes, and 285 (10.2%) Actinobacteria (Data Set S1). In comparison, category L (replication and repair) is enriched (P = 7.55 × 10−6) among the core k-mers of Tenericutes and category M (cell wall/membrane/envelop biogenesis; P = 4.88 × 10−9) in Euryarchaeota. These results suggest a more prominent conservation of these functions in these phyla than in the others, indicating their importance.
In order to determine whether the phyla can be clustered based on their COG-category profiles, we performed a series of principal-component analyses (PCA). PCA of the raw data (e.g., of nonnormalized counts of COG number) did not reveal any particular clustering (Fig. S4A), nor did PCA of the clusters of genera classified according to the number of isolates (Fig. S4B). Figure S4C shows the results of PCA performed on the normalized counts of COG numbers in a centered scale (e.g., COG categories with equal weights). In this analysis, Nitrosopumilus, the only genus in phylum Thaumarchaeota represented in this data set, is isolated from the other genera, as is genus Dehalococcoides, a member of phylum Chloroflexi. These results confirm that the different numbers of isolates per genus do not bias our analysis of functional categories but that some phyla can be distinguished from others.
DISCUSSION
Phylogenetic studies have long been based on multiple-sequence alignment (thus the implicit assumption of full-length contiguity), from which a phylogenetic tree is inferred. A tree-like structure is an unrealistic representation of microbial evolution due to complications of horizontal signal caused by genome rearrangements and lateral genetic transfer (33, 45, 46). In this study, we demonstrated that AF approaches can be used to infer phylogenetic networks quickly for large-scale microbial whole-genome data (see also Text S1 in the supplemental material). Our results provide a comprehensive, alignment-free view of microbial genome evolution as a network, beyond a tree-like structure. We introduce for the first time the concept of a k-mer similarity network and two types of AF networks, the I- and P-networks. We show that by combining a k-mer approach with the use of a relational database, biological information can be accessed efficiently for large-scale data. Finally, we define core k-mers as consisting of those k-mers present in every isolate genome of a genus (or other taxon), following the concept of core genes (47, 48).
We examined the contributions of rRNA genes and plasmids to the phylogenomic signal among microbial genomes. As expected, rRNA genes contribute to the signal captured by 25-mers, as they do in MSA-based approaches. However, the pattern of network density versus threshold (Fig. 5) clearly indicates the different extents of sequence conservation in the distinct genomic regions. Our demonstration that, in general, the signal contributed by rRNA genes is not by itself sufficient to resolve relationships among (and sometimes within) bacterial phyla is in line with many previous studies (2, 6, 49, 50). The low density of the plasmid k-mer network also confirms that plasmids tend to be taxon specific (41). In all our AF networks, phyletic relatedness based on shared k-mers is often strongest between proteobacterial classes, in particular, between the Betaproteobacteria and Gammaproteobacteria, and many 25-mers are shared between the Actinobacteria and Proteobacteria or Firmicutes across all networks. Lateral genetic transfer between lineages of Betaproteobacteria and Gammaproteobacteria (14), identified in earlier studies based on MSA (14, 51) and k-mers (11), partly explains this strong similarity in our networks.
Overall, the I- and P-networks provide a quick overview of the evolutionary relationships among whole genomes, or subsets of genomes, in large-scale data sets. The I-networks capture evolutionary dynamics (e.g., divergence and lateral genetic transfer) and relatedness among individual genomes, providing a fine-scale overview of shared genetic elements among these genomes. The P-networks capture phyletic relatedness and illustrate the magnitude of the sharing of k-mers (and genetic elements) among these groups at a deeper evolutionary timescale.
Assignment of taxonomic rank to groups of bacteria has long been considered fraught (52–54), and there is no generally accepted way to extract taxonomic rank from trees. This undertaking is further complicated by the imbalance in the number of isolates per higher taxon. Our k-mer similarity networks provide an alternative way to explore the evolutionary dynamics of microbial genomes that tracks taxonomic rank. In our phylogenomic network based on 2,705 complete genomic data sets, at threshold at t < 3, domains Archaea and Bacteria appear as separate regions of dense connection within the AF graph. At 3 ≤ t ≤ 5, phyla (e.g., Proteobacteria and Firmicutes) emerge. We see classes (e.g., of Proteobacteria) at 4 ≤ t ≤ 6 and structure between and/or within genera (e.g., Escherichia coli and Shigella) at t > 6. Our k-mer phylogenomic network allows dynamic genome-scale exploration of the taxonomic rank.
Relating the identified core 25-mers for each genus to annotated functions of the corresponding genes identifies highly conserved functions. Although we took great care to use only 2,873 completely sequenced and annotated prokaryote genomes (and excluded draft, fragmented genomes with suboptimal annotations), we cannot dismiss entirely the possible impact of technical errors or inconsistencies of the genome annotation process (e.g., due to chains of functional inference) on these data sets. However, the annotated functions of core k-mers represent conservation at a finer scale than those based on full-length sequence comparisons and remain biologically relevant. Across the phyla represented in our data set, functions (identified on this basis) associated with the metabolism and transport of amino acids, and with the production and conversion of energy, are the ones most frequently encountered. Perhaps not surprisingly, we observed that phyla that share many 25-mers also exhibit similar core functional profiles. Our analysis reveals that the core functions highly conserved in Epsilonproteobacteria and in Deltaproteobacteria are distinct from those conserved in the other proteobacterial classes. Except for the two most highly conserved categories (see above), the Epsilonproteobacteria do not share highly conserved functions with the other classes of Proteobacteria; indeed, the Epsilonproteobacteria share more 25-mers with the Firmicutes and with the Actinobacteria than with other Proteobacteria. These results support those of previous single-gene phylogenetic analyses revealing Epsilonproteobacteria to be the most basal proteobacterial lineage and are consistent with Epsilonproteobacteria having been the last class in this phylum to have been recognized (55). Finally, we also observed that phylum Tenericutes is among the only phyla that do not have highly conserved functions related to energy production and conversion; this can be related to their parasitic or commensal lifestyle (56). These results demonstrate that analysis of conserved k-mers can identify molecular mechanisms and functions that characterize evolutionary diversification within and among microbial taxa.
No core 25-mers were recovered for 51 of these 699 genera, particularly those represented by genome sequences for many isolates from different species. For such genera, a core k-mer set might be sought at lower values of k, although at the potential risk of including signal from false positives and background noise (i.e., nonhomologous k-mers). Similarly, some phyla that we pointed out as sharing highly conserved functions have few distinct COGs related to core 25-mers.
MATERIALS AND METHODS
Data.
In total, 2,785 completely sequenced genomes of Bacteria and Archaea were downloaded from NCBI on 31 January 2016 (Data Set S1); two of these were identified as “multispecies” and “multi-isolate” and were thus excluded. Functional annotation of the remaining 2,783 genomes was obtained through the corresponding RefSeq records. Genes encoding ribosomal RNAs were identified based on annotation. Genomes with no annotation information were excluded from our rRNA-gene network. Of the 2,783 isolates, 921 contained plasmids; these plasmid genomes were used in the plasmid-only network.
Relational database of k-mers and genome features.
We extracted 10,059,526,408 distinct 25-mers from the genomes of 4,401 bacterial and archaeal isolates (present as of 31 January 2016 in NCBI RefSeq), of which 2,783 genomes were complete and included in our subsequent analysis (see above). We organized these k-mers, and their genomic locations and features (based on RefSeq annotations), in a relational database using SQL, following the method of Greenfield and Roehm (37). Tables in the database contain a list of isolates, lists of genes and their sequences, coherent taxonomic information for each isolate, an indexed list of all 25-mers, an indexed list of gene-by-gene comparisons for each pair of genes, and an indexed list of genome-by-genome comparisons for each pair of genomes.
Alignment-free (AF) network.
We followed the method of Bernard et al. (29) in generating the AF networks. We first computed pairwise comparisons for the 2,783 isolates and generated for each comparison the corresponding D2S distance (15) value d, using 25-mers across parallel central processing units (CPUs). For a pair of genomes a and b, we transformed d into a similarity measure Sab, where Sab=10- d. For instance, considering two highly similar genomes of a and b for which distance dab = 0.001, the similarity measure Sab = 9.999. Likewise, considering two highly dissimilar genomes of a and b for which dab = 9.925, Sab = 0.075. We ignored any edge for which d > 10 (i.e., for which the S value was negative), as the corresponding pair of sequences shares only ≤0.01% of 25-mers (i.e., 25-mers capture little evidence of homology). We then generated the networks using JSON files containing the S values as input for a Javascript script using the D3 library (https://d3js.org/). Here, we present two types of AF networks. For a phylum-level depiction of the network (P-network), we grouped all sequences of the same phylum as a single entity prior to calculating the distance; each phylum is represented by a node in the network. The width of the edge between two nodes represents the number of connections between isolates from these two phyla, and the size of each node is proportional to the number of isolates in the phylum. For an isolate-level depiction of the network (I-network) we treated each genome isolate as a single entity (i.e., node). In this network, an edge between two nodes indicates evidence of shared k-mers. The AF networks include a similarity-score threshold t, for which only edges with S>t are displayed; changing t therefore can dynamically change the structure of the network (29). The resulting dynamic networks can be visualized using any web browser. All of the networks are available at https://doi.org/10.14264/uql.2017.436.
Network density and phylum connectedness.
For a network with x nodes, there are e possible edges (potential connections), where . For a network containing y edges (actual connections), the density value D was calculated as (Fig. 1). For a pair of phyla a and b, their connectedness value Cab is, where g is the number of genome pairs (between phyla a and b) that share one or more k-mers and G is the number of all possible genome pairs between phyla a and b. In this case, G = Na × Nb, where Na and Nb represent the number of genomes or isolates in phylum a and phylum b, respectively. For each network, C values were calculated at the optimal threshold t for which the connectedness signal is neither too strong nor too weak across all phylum pair comparisons. To avoid potential biases of incomplete taxon sampling, here we restricted our comparisons to phyla that have ≥10 genomes.
Core k-mers and COG categories.
For a specific group of microbial isolates (representing, e.g., a genus or a phylum), we extracted the set of the 25-mers that are found in all isolates within the group; we define this set of 25-mers as the core k-mers for the corresponding group. Using the relational database of k-mers (see above), we identified for these core 25-mers their corresponding genome locations and function based on COG (Clusters of Orthologous Groups) (57) annotations in RefSeq records. We generated profiles of COG functional categories for each of the 151 genera, for each of the 11 phyla, and for the five proteobacterial classes in which core k-mers were identified using our approach.
ACKNOWLEDGMENTS
This project was supported by an Australian Research Council grant (DP150101875) awarded to M.A.R. and C.X.C. and by a James S. McDonnell Foundation grant awarded to M.A.R. This work was supported by computational resources of the National Computational Infrastructure (NCI) National Facility systems through the NCI Merit Allocation Scheme (Project d85). The funders had no role in study design, data collection and interpretation, or the decision to submit the work for publication.
G.B. implemented the analysis workflow, conducted the experiments, and prepared the first draft of the manuscript. G.B. and C.X.C. prepared all figures and tables. P.G. provided the k-mer database and contributed to analyses using this database. G.B., C.X.C., and M.A.R. conceived the study, designed the experiments, and analyzed and interpreted the results. All of us prepared, wrote, reviewed, commented on, and approved the final manuscript.
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