Cyanophages are viruses that infect cyanobacteria. An interesting feature of many of them is the presence of psbA and psbD, genes that encode D1 and D2 proteins, respectively. The D1 and D2 are core proteins of the photosystem II (PSII) in cyanobacteria, algae and plants and influence the proper function of oxygenic photosynthesis (OP) in all oxyphototrophs on Earth. The frequent occurrence of psbA and psbD in cyanophages raises the question whether these genes coevolved with hosts during the early stages of cyanophage and cyanobacterial evolution, or whether they are direct descendants of genes adopted from the genomes of cyanobacterial hosts. The phylogeny of D1/D2 proteins encoded in the genomes of selected cyanophages and oxyphototrophs was reconstructed. In addition, common ancestral sequences of D1 and D2 proteins were predicted for cyanophages and oxyphototrophs. Based on this, the reconstruction of the 3D structures of D1 and D2 proteins was performed. In addition, the ratio of non-synonymous to synonymous (dN/dS) nucleotide substitutions in the coding sequences (CDSs) of psbA and psbD was determined. The results of the predicted spatial structures of the D1 and D2 proteins and purifying selection for the CDSs of psbA and psbD suggest that they belong to the ancient proteins, which may have formed the primordial PSII. It cannot be ruled out that they involved in water oxidation in cyanobacteria-like organisms at early stages of the evolution of life on Earth and coevolved with ancient cyanophages. The data are also discussed in the context of the origin of viruses.
Cyanophages, or bacteriophages (phages) that infect cyanobacteria, were first described in the 1990s1,2. To date, the genomes of more than 70 cyanophages, mainly living in marine environments, have been identified and sequenced3. Interestingly, the vast majority of described cyanophages mainly infect cyanobacteria from the two genera Prochlorococcus and Synechococcus, which in turn are the dominant oxyphototrophs on Earth, as they inhabit all oceans4,5,6,7. Cyanophages are among most abundant ‘semi-life’ forms that play a crucial role in global biogeochemical cycles of carbon, oxygen and nitrogen8,9.
A particularly interesting feature of cyanophages is the presence of genes in their genome that encode proteins involved in the photosynthetic activity of cyanobacteria. The best known in this context are the genes coding the PSII core proteins that are most abundant in cyanophages, namely psbA for protein D1 and psbD for protein D23,10,11. The first photosynthetic gene identified in cyanophages was psbA12,13. 80% of the cyanophage genomes sequenced so far have psbA, and 42% have both psbA and psbD genes3. The function of the cyanophage genes psbA and psbD is not yet fully understood, but it is likely that they play a key role in infection under changing light conditions that cause photoinhibition of host D1/D2 proteins14. Light-induced photoinhibition causes a more rapid degradation of D1/D2 than the completion of the cyanophage developmental cycle. Thus, providing copies of psbA (D1) and psbD (D2) during viral infection allows the infected cell to be photosynthetically active for as long as is required for full viral particle replication3,15,16,17.
The relatively wide distribution of psbA and psbD in cyanophages raises the question of whether these genes evolved in co-evolution with hosts in the early stages of cyanophage and cyanobacterial evolution or whether they are direct descendants of genes that cyanophages later adopted from the genomes of cyanobacterial hosts. The answer to this question relates to at least two interrelated issues. First, it concerns the origin of viruses in general and cyanophages in particular. Second, it sheds light on the evolution of oxygenic photosynthesis (OP) too, since cyanobacteria-like organisms are generally considered to be the first oxyphototrophs on Earth18,19,20. According to the most widely held view, the ancestor of cyanobacteria did not possess photosynthetic genes encoding proteins involved in O2 production. OP probably arose about 2.3–2.6 billion years ago during the so-called Great Oxidation Event (GOE) through lateral gene transfer and the fusion of two photosynthetic systems derived from primordial, non-oxygen evolving bacteria21,22,23. Some recent phylogenetic analyses suggest that OP may have arisen at very early stages of the evolution of life on Earth24,25,26. Therefore, the molecular evolution of proteins at the coding sequence (CDS) level for psbA and psbD was also studied here in the context of nucleotide substitutions in codons. Most nucleotide substitutions occur at the 3rd position in the codon, less frequently at the 1st and 2nd positions27. A nucleotide substitution in a codon can be synonymous and we usually find it at the 3rd position. Generally, synonymous substitutions do not lead to a change in the encoded amino acid in the protein. As a result, the protein retains its biological function. In other words, such a change is neutral and invisible to natural selection. Non-synonymous nucleotide substitutions at the codon lead to a change in the amino acid in the protein. The altered protein can in turn affect the fitness of an organism. Determining the number of non-synonymous (dN) and synonymous (dS) nucleotide substitutions therefore allows us to estimate what type of selection we are dealing with within the CDS under study27,28,29. By comparing the dN/dS ratio, we were thus able to determine which type of selection acts on the CDS for psbA and psbD in cyanophages and selected oxyphototrophs (see "Methods" for details).
Our data are presented in the context of the various hypotheses that concern origin of viruses. It cannot be ruled out that cyanophages carrying psbA/psbD genes are ancient remnants and "living fossils" from the earliest stages of the evolution of life, when a mixture of protocyanobacterial and virus-like replicators existed.
Phylogenetic analysis of D1 and D2 proteins
Phylogenetic trees were reconstructed for D1 and D2 proteins, highlighting cyanophages that have only the gene for the D1 protein (psbA) and/or D2 protein (psbD) in the genome. In the group of cyanophages examined, no case was found in which only psbD was present; when psbD was present, it was only together with psbA (Fig. 1). In contrast, in some cyanophages psbA was present as the only gene for the PSII core protein (Fig. 1).
The phylogenetic tree reconstructed for the D1 protein showed several distinct clades: for plants, algae and most of the cyanobacteria analysed (Fig. 1A). One of these clades, with the exception of the Synechococcus T7-like phage S-TIP37, includes cyanophages that have psbD for the D2 protein in their genome in addition to the psbA gene for D1 (Fig. 1A). This entire group of cyanophages most likely shares a common ancestor with D1 for other cyanobacteria, algae and plants.
A separate cyanophage clade is formed by cyanophages that only possess D1. Interestingly, 3 species of cyanobacteria also belong to this clade: Synechococcus elongatus PCC 7942, Geitlerinema sp. PCC 7407 and Prochlorococcus marinus MIT 9301 (Fig. 1). The localisation of the D1 protein in P. marinus suggests that psbA is derived from cyanophage ancestors of psbA. D1 in this group in turn shares a common ancestor with D1 in S. elongatus and Geitlerinema sp. (Fig. 1A).
Phylogenetic analysis of D2 protein
In contrast to the phylogenetic tree for D1, the tree reconstructed for D2 contains fewer protein sequences. This is due to the fact that many fewer cyanophages contain psbD, which codes for the D2 protein, in their genome. Moreover, if psbD is already present in the cyanophage genome, it is accompanied by psbA for the D1 protein (Fig. 1B). Similar to the tree for D1, plants, algae and cyanobacteria form separate clades. However, it is worth noting that D2 occurs in two algal species: Galdieria sulphuraria and Vaucheria litorea between the D2 sequences for cyanobacteria (Fig. 1B). This result suggests that horizontal gene transfer for psbD may have occurred in the past between selected groups of algae and cyanobacteria. This possibility cannot be ruled out, as HGT between bacteria, cyanobacteria, viruses and algae, including the red alga G. sulphuraria, has already been observed30.
Ancestral sequence reconstruction and prediction of spatial structure
The algorithm in the workspace SWISS-MODEL used the D1 template (PDB: 6w1p.1.U), which is 10 amino acids shorter at the N-terminus than the full D1 sequence (UniProt: P0A444, Supplementary Information Notes S5). Homology modelling performed by SWISS-MODEL showed that the predicted and ancestral D1 protein (model_D1) is 37 and 27 amino acids shorter than the full D1 sequence (UniProt: P0A444) and the D1 template (PDB: 6w1p.1.U) from Thermosynechococcus elongatus, respectively. The D1 model lacks the first 26 amino acids and is missing D308 (Fig. 2, Supplementary Information Notes S5). D1 belongs to proteins that play a key role in binding the Mn4O5Ca cluster24,25,32. In T. elongatus, the following amino acids of D1 are involved in this binding and the proper function of the oxygen evolving complex (OEC): D170, E189, H332, E333, D342, and A34433, https://www.rcsb.org/3d-view/6W1P, Supplementary Information Notes S5]. These 6 amino acid residues of the D1 protein are present in all modern organisms that carry out OP34. Although the predicted model protein is shorter than the template, namely only shifted by 37 amino acid residues, there is an identical set and pattern of amino acids required for the functioning of OEC: D144, E163, H305, E306, D315 and A317 (Fig. 2, Supplementary Information Notes S5). In general, the identity between the template and the model is ~ 83%. The results indicate that the amino acid sequence of a potentially ancestral D1 protein has not changed significantly compared to the extant D1 proteins found in oxyphototrophs and encoded in cyanophage genomes.
In the case of the D2 protein, the template was also the D2 protein from T. elongatus (6dhe.1.D). We obtained a much more similar, almost identical 3D model of the predicted, probably ancestral D2 (Fig. 3, Supplementary Information Notes S6). The differences concern substitutions of only 22 amino acids with similar physicochemical properties (Supplementary Information Notes S6). Although the amino acids of the D2 protein are not directly involved in the binding of the Mn4O5Ca cluster, they play an important role in proper functioning of PSII25. It should be noted that the amino acid residues involved in Mn4O5Ca binding (Fig. 2) appear to be very conservative and probably occurred in an ancient D1-like protein at a very early stage of OP evolution.
Determination of dN/dS values
Analysis of CDSs for psbA and psbD, encoding D1 and D2 proteins respectively, showed that the dN/dS values for cyanophages, cyanobacteria, algae and plants were lower than 1 (dN/dS < 1) (Fig. 4, for details see “Methods”). The results show that the CDSs tested are subject to purifying (negative) selection. Interestingly, the dN/dS values for psbA and psbD were much more similar in both cyanophages and cyanobacteria than the dN/dS values in algae and plants (Fig. 4). These results suggest a close co-evolution of psbA/psbD in cyanophages and cyanobacteria.
The D1/D2 proteins are homologues formed by duplication of the original gene, and this duplication must have occurred long before the appearance of cyanobacteria24,25. The occurrence of early branched cyanobacterial D1 and D2 in clades dominated by cyanophage sequences also suggests an early and continuous gene exchange between cyanophages and their hosts (Figs. 1 and 5). Furthermore, it has already been confirmed that cyanophage genomes encode only D1 or both D1 and D2 proteins. According to our knowledge, no cyanophages have yet been found that have only psbD (D2) in their genome3,10. It is likely that psbD was later lost in some cyanophages. The results also show that purifying selection CDSs of psbA and psbD, early branching in the trees for D1/D2 proteins, and separate clades with dominance of cyanophage proteins indicate that the psbA and psbD genes for D1 and D2, respectively, must have evolved very early in both cyanophages and cyanobacteria. It cannot be excluded that the genes psbA and psbD had a common ancestor prior appearance of cyanobacteria-like organisms. Moreover, the reconstructed spatial structures for the predicted hypothetical ancestral D1 and D2 proteins suggest that they may have been functionally similar enough to the modern forms. The ability to bind the Mn4O5Ca cluster may even have been present in the case of the ancient form of the D1 protein. The common ancestor of the psbA/psbD genes and the corresponding D1 and D2 protein products proposed here is made plausible by previous data that the D1/D2 heterodimer may have preceded the homodimeric form D025. The predicted structure of the hypothetical D0 protein suggests that it was more similar to the existing D1 than to the D2 sequences, and contained almost the same amino acids as D1, which are responsible for binding the Mn4O5Ca cluster. The only predicted mutation was at position 170, where D replaces E (D170E)25. Another important point related to the evolution of OP is also the structural similarity of the Ca-binding site between the homodimeric type I reaction centre (RCI) of green sulphur bacteria and heliobacteria and the Mn-binding site with the D/E residues in PSII35,36,37. Taken together, all these common structural features and the data based on molecular phylogeny provide further evidence for an early evolution of PSII and OEC.
As far as the origin of viruses is concerned, in connection with the phylogeny of psbA and psbD in cyanobacteria and cyanophages, one can ask whether it can not only be a rough model for the evolution of cyanobacteria and cyanophages, but whether it can also give an indication of how the evolution of viruses has proceeded in general. In the case of cyanophages and D1/D2 proteins, the results obtained indicate that the primordiality hypothesis of viruses in relation to their cellular hosts can be considered38,39,40,41. Our phylogenetic data showed that both the cyanophage and cyanobacterial D1/D2 proteins are deeply related, suggesting that the cyanophage and cyanobacterial ancestral sequences of psbA and psbD arose at least at the same time. This also suggests close co-evolution of psbA and psbD between hosts and their cyanophages. Therefore, the data seem to fit, at least in part, the 'virus early' hypothesis38,39,41,42. However, a certain problem with this virus/cyanophage origin scenario is the question of the origin of the proteins that build their capsids. Viral capsid proteins have no obvious homologues among the proteins of modern cells43,44. An analysis of cyanophage capsid proteins is beyond the scope of this study. Nevertheless, following new comparative analyses of capsid proteins, it has been hypothesised that protoviruses, the first replicons or mobile genetic elements, originated with the first cellular forms, i.e. the last universal common ancestor (LUCA), but that the capsid proteins were recruited from later primordial cellular forms39,44. All analysed here cyanophages belong to the realm Duplodnaviria that possess double-stranded DNA (dsDNA) (data form https://www.ncbi.nlm.nih.gov, October 2022). Comparative analyses of viruses and their hosts suggest that Duplodnaviria-like dsDNA viruses may have evolved from a population of replicators in the pre-LUCA era, which later gave rise to dsDNA viruses and cellular forms39.
At this point, a hypothetical scenario about the origin of viruses and cyanophages in particular is linked to the advent of OP. Cyanophages must have co-evolved with their hosts, as evidenced by the relatively abundant presence of psbA and psbD within them. Purifying selection for CDSs of psbA/psbD has already been described for the major groups of oxyphototrophs26. This fact, together with the conserved 3D structure of D1/D2 proteins predicted here, suggests that the ability to bind Mn4O5Ca clusters and to oxidise water may have arisen very early.
In summary, the D1/D2 proteins and the genomes of the cyanophages that code for them arose in very early stages of the evolution of cyanobacteria and must have been in close relationship with the cyanophages (co-evolution). The in silico reconstructed 3D structures of the D1 and D2 proteins and the purifying selection estimated for the CDSs of psbA and psbD in the studied groups of oxyphototrophs and cyanophages suggest that D1/D2 are ancient proteins that may have formed the primordial PSII that could oxidise water at very early stages of the evolution of life on Earth.
Phylogenetic analysis of D1/D2 proteins
The molecular phylogenetic analysis was based on D1 and D2 amino acid sequences from selected group of organisms: cyanobacteria, algae, and plants. The latter are defined here as vascular and land plants. Moreover, D1/D2 proteins from cyanophages were also analysed. All sequences were derived from GenBank (www.ncbi.nlm.nih.gov) and UniProt (uniprot.org) databases (for details see Supplementary Information Notes S1 and Notes S2). The sequences were aligned with the default parameters of ClustalW implemented in MEGA645. The evolutionary history was inferred by using the Maximum Likelihood method based on the Le and Gascuel46 model. A discrete Gamma distribution was used to model evolutionary rate differences among sites. The bootstrap consensus tree was inferred from 1000 replicates47. The tree is drawn to scale, with branch lengths measured in the number of substitutions per site. This analysis involved 48 and 39 proteins for D1 and D2, respectively.
Ancestral sequence reconstruction and prediction of spatial structure
Based on the phylogenetic trees for D1 and D2 proteins, the deepest nodes were selected, designated ID1 and IID1 for D1 proteins and ID2 and IID2 for D2 proteins (Fig. 1). The ancestral amino acid sequences reconstructed for these nodes were pairwise aligned by the programme Cons (EMBOSS explorer, https://www.bioinformatics.nl/cgi-bin/emboss/cons) and the consensus sequences were determined (Fig. 5, Supplementary Information Notes S3 and Notes S4). A 3D structure for D1 and D2 was then predicted for the consensus sequences based on the SWISS-MODELL workspace on March 202248. From the list of known PSII protein structures suggested as templates by the SWISS-MODEL algorithm, the protein structures of D1 (6w1p.1.U) and D2 (6dhe.1.D) for T. elongatus were used. The accession numbers, i.e.: 6w1p and 6dhe correspond to the 3D protein structures of PSII deposited in the Protein Data Bank (PDB) (https://www.rcsb.org). The selection was based on the fact that the 3D structures of the D1 and D2 proteins were determined by X-ray diffraction with a resolution of 2.26 and 2.05 Å, respectively33,49. The templates and the obtained models were pairwise alignment by EMBOSS needle software (Supplementary Information Notes S5 and Notes S6). The 3D protein structures were visualised and analysed with the software UCSF ChimeraX31.
Coding sequences (CDSs) for psbA/psbD and determination of the values of non-synonymous (dN) and synonymous (dS) substitutions
The molecular phylogenetic analysis was based on CDSs for psbA and psbD taken from selected group of organisms: cyanobacteria, algae, and plants. Moreover, CDSs for these genes from cyanophages were also analysed. All sequences were derived from GenBank (www.ncbi.nlm.nih.gov), UniProt (www.uniprot.org), Kyoto Encyclopedia of Genes and Genomes (KEGG, www.genome.jp/kegg/), and European Nucleotide Archive (ENA, www.ebi.ac.uk/ena/browser/home) databases for details see Supplementary Information Notes S7 and Notes S8). The number of non-synonymous (dN) and synonymous (dS) nucleotide substitutions was determined in the analysed CDSs. The ratio of dN to dS (dN/dS) was calculated to estimate the type of selection. According to the dN/dS method, dN/dS = 1 means neutral evolution, dN/dS < 1 indicates purifying (negative) selection, and dN/dS > 1 means positive selection29. The sequences were aligned using the default parameters of ClustalW implemented in MEGA645. The dN and dS values were calculated using the software DnaSP v. 6.12.0350, then dN/dS values were determined.
The datasets generated during and/or analysed during the current study are available from the corresponding author on reasonable request.
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This research was supported by The Franciszek Górski Institute of Plant Physiology Polish Academy of Sciences in Kraków, Poland.
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Ślesak, I., Ślesak, H. Cyanophages as an important factor in the early evolution of oxygenic photosynthesis. Sci Rep 12, 20581 (2022). https://doi.org/10.1038/s41598-022-24795-1