Phosphate (PO4) is an important limiting nutrient in marine environments. Marine cyanobacteria scavenge PO4 using the high-affinity periplasmic phosphate binding protein PstS. The pstS gene has recently been identified in genomes of cyanobacterial viruses as well. Here, we analyse genes encoding transporters in genomes from viruses that infect eukaryotic phytoplankton. We identified inorganic PO4 transporter-encoding genes from the PHO4 superfamily in several virus genomes, along with other transporter-encoding genes. Homologues of the viral pho4 genes were also identified in genome sequences from the genera that these viruses infect. Genome sequences were available from host genera of all the phytoplankton viruses analysed except the host genus Bathycoccus. Pho4 was recovered from Bathycoccus by sequencing a targeted metagenome from an uncultured Atlantic Ocean population. Phylogenetic reconstruction showed that pho4 genes from pelagophytes, haptophytes and infecting viruses were more closely related to homologues in prasinophytes than to those in what, at the species level, are considered to be closer relatives (e.g. diatoms). We also identified PHO4 superfamily members in ocean metagenomes, including new metagenomes from the Pacific Ocean. The environmental sequences grouped with pelagophytes, haptophytes, prasinophytes and viruses as well as bacteria. The analyses suggest that multiple independent pho4 gene transfer events have occurred between marine viruses and both eukaryotic and bacterial hosts. Additionally, pho4 genes were identified in available genomes from viruses that infect marine eukaryotes but not those that infect terrestrial hosts. Commonalities in marine host-virus gene exchanges indicate that manipulation of host-PO4 uptake is an important adaptation for viral proliferation in marine systems. Our findings suggest that PO4-availability may not serve as a simple bottom-up control of marine phytoplankton.
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Marine phytoplankton play a major role in global photosynthesis and CO2 capture from Earth's atmosphere (Field et al., 1998). Phytoplankton populations are controlled by grazing and viral mortality as well as nutrient availability and other biological and physico-chemical factors. How these different forces control individual taxa remains poorly understood, see, e.g. (Azam et al., 1983; Rohwer and Thurber, 2009). A major challenge for understanding eukaryotic phytoplankton controls is their tremendous diversity and the fact that many remain uncultured. The smallest of these are the picoeukaryotes (≤ 2–3 µm diameter), a broad assemblage composed of picoprasinophytes, small haptophytes and stramenopiles (Worden and Not, 2008; Shi et al., 2009; Cuvelier et al., 2010). Picoprasinophytes in the order Mamiellales are widespread and genome sequences are available for two common genera, Ostreococcus (Derelle et al., 2006; Palenik et al., 2007) and Micromonas (Worden et al., 2009), but not yet for Bathycoccus. Ostreococcus is seen in tropical and temperate waters while Bathycoccus and Micromonas extend to polar systems (Not et al., 2005; Worden et al., 2009). While complete genome sequences are not yet available for haptophyte and stramenopilepicoplankton, the picoprasinophyte genomes provide information on the molecular underpinnings of nutrient uptake and insights on the relative importance of bottom-up controls.
Concentrations of the major nutrients nitrate, ammonium and phosphate (PO4) vary seasonally in the euphotic zone where they influence the dynamics and successional patterns of resident phytoplankton communities. PO4 depletion in particular is thought to cause intense competition between different taxa in the North Atlantic Ocean and to have influenced gene content in different strains of the picocyanobacteria Prochlorococcus and Synechococcus through selective adaptations (Scanlan et al., 2009). Indeed, Prochlorococcus populations were recently reported to have different frequencies of PO4-uptake related genes depending on whether they were from the North Pacific or the North Atlantic Gyre characterized by much lower PO4 concentrations (Coleman and Chisholm, 2010). Similar results were reported for the SAR11 clade, a lineage of widely distributed marine heterotrophic bacteria. These findings were hypothesized to reflect the influence of water mass characteristics on the gene repertoires of resident taxa (Coleman and Chisholm, 2010).
The two main types of inorganic PO4 transporters in cultured microbial taxa are encoded by genes in the PHO4 superfamily (Pfam PF01384) and Pst genes. Many eukaryotes and bacteria encode PHO4 superfamily members. This superfamily includes high- and low-affinity inorganic phosphate transporters. In eukaryotic phytoplankton a pho4 gene has been identified in expressed sequence tags from the haptophyte Emiliania huxleyi (Dyhrman et al., 2006a) as well as in the genome sequence of a virus that infects it, EhV-86 (Wilson et al., 2005). Comparative analysis of putative transporter-encoding genes in Micromonas and Ostreococcus indicate that PHO4 superfamily members are present in these taxa as well (Worden et al., 2009), but their relatedness and PO4 affinities are not yet known. The marine picocyanobacteria use the Pst system, a multi-unit high-affinity inorganic PO4 transport system that depends on the high-affinity periplasmic PO4-binding protein encoded by the gene pstS/phoS (Diaz et al., 2005). PstS homologues are present in all sequenced Prochlorococcus and Synechococcus genomes, sometimes in multiple copies (Martiny et al., 2006; Scanlan et al., 2009). Interestingly, some marine cyanophages also encode pstS genes and the presence of pstS in cyanophage genomes appears to be linked to whether the phage source waters were PO4-deplete or not (Sullivan et al., 2005; Sullivan et al., 2010). Phage-mediated gene transfer has been hypothesized to be responsible for the fact that many PO4-uptake related genes in Prochlorococcus ecotypes do not appear to follow the ‘species’ tree (Martiny et al., 2006).
Here, we analyse phosphate and other transporter-encoding genes in published genomes from viruses that infect eukaryotic phytoplankton. Ecological and evolutionary aspects of PHO4 superfamily members were investigated in the viruses and their hosts, including a ‘wild’Bathycoccus population. The distribution and diversity of this transporter gene was evaluated in metagenomes from a North Pacific Ocean transect and other marine environments.
Results and discussion
Virally encoded transporter genes
We analysed viruses infecting unicellular and/or marine eukaryotes for transporter-encoding genes, including the pho4 gene previously reported in EhV-86 (Wilson et al., 2005). Analysis of open reading frames (ORFs) in published viral genomes showed that several eukaryotic viruses encoded pho4 genes, as well as other putative transporter genes (Table 1). Apart from the amoeba-infecting mimivirus, all of these viruses belong to the Phycodnaviridae (Wilson et al., 2005; Derelle et al., 2008; Weynberg et al., 2009; 2011; Moreau et al., 2010), a family of nucleocytoplasmic large double-stranded DNA viruses. Genes from the different viruses that encoded PHO4 superfamily members had higher overall similarities to each other (ranging from 59% to 94% at the amino-acid level) than did the genes that encoded each of the other transporter types identified in the viral genomes (Table 1). Apart from EhV-86, the other identified pho4 genes were in Mamiellales-infecting viruses. Specifically, they were found in one of the two viruses infecting Bathycoccus, two of the four infecting Ostreococcus but not in MpV-1, which infects Micromonas. Some of these Mamiellales-infecting viruses contained the pho4 gene but no other known transporter genes (Table 1). Although genomic data are limited, it is possible that the presence or absence of pho4 genes reflects the influence of the environment, or environmental stresses acting on their hosts, in shaping viral genomes. For example, the pho4 gene-encoding virus OtV-2 infects Ostreococcus RCC393 (Weynberg et al., 2011), a strain that belongs to an Ostreococcus clade (OII) known to inhabit warm, oligotrophic waters where PO4 is often depleted (Demir-Hilton et al., 2011). In contrast, the Ostreococcus viruses OtV-1 and OtV-5 do not encode pho4 and their host, O. tauri, appears to be restricted to higher nutrient systems, such as bays, lagoons and brackish waters. Two different Bathycoccus viruses, BpV-1 and BpV-2, were isolated against the same Bathycoccus strain (RCC1105), but the source waters the viruses came from were collected at different times of the year (fall and winter). Hence, different nutrient conditions associated with seasonal changes may explain the fact that only BpV-1 encodes the pho4 gene. Different Micromonas clades also vary along environmental gradients (Foulon et al., 2008) and the distribution of the strain infected by MpV-1 is unknown. Lack of pho4 in MpV-1 is however consistent with Micromonas being most abundant in coastal settings, at least in temperate and subtropical systems (Foulon et al., 2008), that are usually PO4 replete.
Table 1. Transporter and phoH sequences detected in all published Mamiellales viruses, other representative eukaryotic viruses and mimivirus (as an outgroup).
The asterisk indicates a non-marine host; – indicates not found. Accessions provided were retrieved by blasting predicted ORFs against GenBank NR.
Putative functions of other virally encoded transporters were broader and more difficult to interpret ecologically. A single member of the ATP-Binding Cassette superfamily was found in the Paramecium bursaria Chlorella virus (PbCV-1, which infects a Chlorella alga that lives in a symbiotic association with P. bursaria) and one Major Facilitator Superfamily (small solute transporters) member was identified (Table 1). The latter was found in EhV-86 and an apparently unrelated Major Facilitator Superfamily member has been reported in a dsDNA virus infecting the moth Helicoverpa zea. A putative ion channel transporter gene (belonging to the VIC Superfamily) was detected in several of the Mamiellales viruses (Table 1). A homologue of this gene was first reported in PbCV-1 where it was shown to act as a potassium selective channel and appeared to be essential to the viral life cycle (Plugge et al., 1999). It was later described in EsV-1, which infects the multicellular brown alga Ectocarpus siliculosus (Chen et al., 2005). Members of the Cation Channel-forming Heat Shock Protein-70 family were also identified in the Bathycoccus viruses (YP_004061438, ADQ91175) and mimivirus (YP_003986897, YP_003986752). A putative ATPase-encoding gene, phoH, was also identified in most of the viral genomes (Table 1, see below).
The only viral sequence included in the full PHO4 Pfam alignment at the time of our analysis was from EhV-86. Pho4 was not present in the 50 nucleocytoplasmic large double-stranded DNA viruses (Asfarviridae, Iridoviridae, Mimiviridae, Phycodnaviridae and Poxviridae) and 46 herpesvirus genomes sequences available when that Pfam alignment was generated. The majority of these viruses infect terrestrial hosts including mammals, non-mammalian vertebrates and invertebrates. Furthermore, pho4 genes were not detected in newly available genomes from viruses that infect other hosts, including non-marine unicellular eukaryotes. In environments like the mammalian cellular milieu or many freshwater systems, PO4 is not considered limiting and therefore selection pressure favouring viruses that encode a PO4 transporter (or retention of this gene) is presumably weak. In contrast, manipulation of PO4-uptake in marine hosts that often encounter PO4-deplete conditions could ensure enough PO4 is available for viral replication.
Origins of virally encoded pho4 genes
Many previous studies have suggested that viruses acquire genes from their hosts (studies by, for example, Monier et al., 2007; Sharon et al., 2009; Colson and Raoult, 2010). We screened eukaryotic algal genomes for the pho4 gene, including hosts for the analysed viruses. In addition to the previously described E. huxleyi pho4 gene (Dyhrman et al., 2006a), genes containing the PHO4 Pfam domain were found in Aureococcus anophagefferens (a pelagophyte) and all genome sequenced Ostreococcus strains (O. tauri, O. lucimarinus and Ostreococcus RCC809). They were also found in Micromonas RCC299 and CCMP1545 but with low similarity to the Ostreococcus pho4 genes (see discussion below).
To better understand the distribution of pho4 genes in the Mamiellales and potential gene exchanges between viruses and hosts, we generated and screened a targeted metagenome for Bathycoccus. A natural population was sorted by flow cytometry (Fig. S1) from PO4-deplete waters (Fig. 1, Table 2) and the 18S rDNA clone library built from the sorted and multiple displacement amplification (MDA)-amplified material was composed solely of Bathycoccus sequences (Fig. S2; 99% nucleotide identity to Bathycoccus prasinos BLA77). Results for 16S rDNA clone sequences were less clear and an unknown endosymbiont or other material may have been present (Table S1). Therefore, only scaffolds with ≥ half of predicted ORFs with best BLASTp hits to predicted protein sequences in other Mamiellales genomes (i.e. Micromonas and Ostreococcus), that fit other criteria as well (see Experimental procedures), were considered derived from the Bathycoccus nuclear genome and used in subsequent analyses. Two distinct G + C signatures were observed in the Bathycoccus nuclear metagenome similar to what has been seen in whole genome sequences from cultured members of the Mamiellales. The ‘anomalously low-G + C’ region of 38% G + C was about 10% lower than the overall metagenome average of 48%. These regions of considerably lower G + C content were first observed in O. tauri (58% for the whole genome and 52% for the low G + C region) and Micromonas sp. RCC299 (64% and 50% respectively) and have been hypothesized to serve as a sex chromosome that encodes convergent, overlapping genes (Derelle et al., 2006; Worden et al., 2009). The specificity of recovered ORFs, as well as detection of low G + C scaffolds with a differential from the overall average within range of that observed in Ostreococcus and Micromonas, indicating that the assembled and filtered metagenome is specific to the Bathycoccus nuclear genome.
Table 2. Summary of water samples from which metagenomes were sequenced and corresponding metadata.
Location (lat.; long.)
Chl a (mg m−3)
For Atlantic samples reported NO3 measurements reflect NO3 + NO2.
T, temperature; S, salinity.
Sta. 13 Sort
A pho4 gene was identified in the Bathycoccus metagenome, with highest amino-acid sequence similarity to that of Ostreococcus (65%, O. lucimarinus XP_001422167). Similarities between pho4 genes from these Mamiellales and those in Micromonas were low (Bathycoccus had 29% similarity to Micromonas RCC299 ACO69637 and 27% to M. CCMP1545 XP_003062965). Surprisingly, the similarities between pho4 from Ostreococcus or Bathycoccus were lower to Micromonas than to Tetraselmis chui (50% similarity with Bathycoccus), a more distant prasinophyte. Bathycoccus and Ostreococcus also appeared more closely related to each other than to Micromonas based on 18S rDNA analyses (Fig. S2), see also (Guillou et al., 2004; Worden, 2006).
Recovery of pho4 genes from host genera and other eukaryotes allowed us to construct a robust phylogeny for the corresponding viral and host pho4 protein sequences. BpV-1, OlV-1 and OtV-2 pho4 sequences branched with those of Bathycoccus and Ostreococcus while the EhV-86 pho4 gene branched with its host E. huxleyi (Fig. 2). The analysis suggests that multiple horizontal gene transfer (HGT) events occurred – although the direction of those events is still unclear (whether from host to virus, or virus to host). Phylogenetic analysis supports the hypothesis that the EhV-86 and Ostreococcus viral pho4 genes were derived from their respective host genera, rather than a common viral ancestor. Still, other gene exchange scenarios are possible. For instance, the exchange could have occurred from host to virus, virus to virus and then virus to another host lineage, explaining the presence of ‘green’-like pho4 genes in, e.g. the haptophytes. The pattern of multiple exchanges, resulting in an indirect virally mediated exchange of host genes to another host has been hypothesized for the photosynthetic reaction centre genes psbA and psbD in cyanobacteria and cyanophages (Sullivan et al., 2006). Two pho4 genes from Ostreococcus viruses branched together and have higher similarity (across all positions) to one another than to homologues from Ostreococcus itself. A pho4 sequence is not available from Ostreococcus RCC393, the host strain against which OtV-2 was isolated, although a sequence from another Ostreococcus Clade OII member (Ostreococcus RCC809) was included. The fact that OlV-1 and OtV-2 sequences branched together could indicate they originated from a common ancestor rather than from their respective hosts. Without an OtV-2 host-encoded pho4 sequence in the tree it is not possible to determine if placement of the OtV-2 version would differ if the host sequence was included. Finally, host cross-infectivity levels of Phycodnaviridae family members are not well known and could influence acquisition and retention patterns.
Horizontal gene transfer events similar to those hypothesized here for the pho4 gene in marine systems have been reported for E. huxleyi and EhV-86 sphingolipid biosynthesis genes. Sphingolipid biosynthesis genes were hypothesized to have been acquired by the virus from its host (Monier et al., 2009) and viral glycosphingolipid molecules have been shown to be synthesized by the haptophyte during infection (Vardi et al., 2009). These molecules have been detected in the natural environment and are possibly related to bloom dynamics of the host (Vardi et al., 2009). In contrast to the broad distribution of pho4 genes in viruses that each infect different marine eukaryotic taxa or lineages, the hypothesized sphingolipid pathway HGT has so far only been reported between E. huxleyi and EhV. In addition to the pho4 homologues present in various algae and their viruses, we found a close homologue of the BpV-1 and BpV-2 encoded Cation Channel-forming hsp70 family gene in the Bathycoccus metagenome (scaffold C503; this gene is also present in O. lucimarinus and Micromonas RCC299), suggesting this gene may have been acquired through HGT and is sufficiently advantageous to be retained by the recipient genome. Homology has been reported between 11 predicted genes in OtV-1 and host-encoded (O. tauri) genes (Weynberg et al., 2009). Studies exploring the expression of virally encoded pho4 genes and other putatively exchanged genes should enhance our understanding of viral impacts on oceanic phytoplankton as well as environmental factors controlling viral proliferation.
Phylogenetic relationships between algal pho4 genes and implications for function
The phylogenetic relationships of phytoplankton pho4 homologues inferred from the protein sequences (Fig. 2) were inconsistent with ‘species phylogenies’ based on 18S rDNA and chloroplast gene trees (Andersen, 2004; Keeling et al., 2005; Worden and Not, 2008). In our analysis, a ‘green-clade’ consisting of pho4 homologues from the prasinophytes Bathycoccus, Ostreococcus and T. chui formed a sister group to other members of the Plantae, especially green algae. However, this ‘green-clade’ also included pho4 homologues from stramenopiles (E. siliculosus and A. anophagefferens) and the haptophyte E. huxleyi. High representation of green algal or plant-like genes in haptophytes has been reported previously (Hampl et al., 2009; Cuvelier et al., 2010). Interestingly, E. siliculosus appeared to only have the ‘green’pho4 gene-version and Aureococcus (Gobler et al., 2011) had multiple versions, three of which were ‘green’-like (Fig. 2). In contrast, pho4 genes from the diatoms Thalassiosira pseudonana and Phaeodactylum tricornutum (Armbrust et al., 2004; Bowler et al., 2008) grouped together in a position outside of the ‘green-clade’, as would be expected based on their evolutionary history inferred by chloroplast gene trees. Anomalous phylogenetic patterns have also been reported for phytoplankton ammonium transporters (McDonald et al., 2010). However, in most cases, each different picoprasinophyte AMT type (i.e. forming distinct clades within the AMT-gene tree) was present in all of the sequenced picoprasinophyte genomes. In contrast, despite the presence of ‘green’-like PHO4 superfamily members in disparate lineages, this version was not found in the picoprasinophyte Micromonas; their pho4 genes branched in an unsupported position basal to metazoans (not shown). There are several possible explanations for the observed phylogenetic distribution of pho4 genes in eukaryotic algae. The fact that the stramenopile and haptophyte pho4 homologues grouped with green algae may have been influenced by taxon undersampling, particularly the lack of available homologues from red algae apart from C. merolae. However, it may also reflect ancestral characteristics with differential loss or divergence in some taxa (e.g. diatoms) or gain from a proposed cryptic green algal endosymbiont in the chromalveolates (Moustafa et al., 2009). Alternatively, HGT events may have occurred between distantly related organisms, possibly involving virally mediated exchange, leading to the observed phylogenetic relationships. HGT events have been reported between distant eukaryotic organisms, e.g. carotenoid production related genes in fungi and aphids (Moran and Jarvik, 2010).
All of the pho4 genes within the ‘green-clade’ that have been experimentally characterized serve as high-affinity transporters. The T. chui encoded protein (AAO47330) acts as a high-affinity PO4 permease and the gene is specifically upregulated in P-deplete conditions (Chung et al., 2003). Its branching position was basal to pho4 genes from several of the algae and viruses analysed, suggesting it represents a more ancestral version of the gene (Fig. 2); it showed a high degree of similarity to the algae at terminal nodes of the ‘green-clade’. The E. huxleyi pho4 gene is expressed under PO4 depletion (Dyhrman et al., 2006a) and similar results have been reported for an Aureococcus version (Wurch et al., 2011), both of which are embedded within this clade (Fig. 2). Thus, we hypothesize that the other algal pho4 genes branching within this region of the tree are also high-affinity PO4 transporters. Notably, in the Ostreococcus viruses, a 54-amino-acid segment was missing from the pho4 gene that is present in host versions. In the same region 19 amino acids were absent from BpV-1 that were present in the host version. How these deletions affect function is still unclear; deletions are seen in this region in some eukaryotic taxa as well, although involving fewer amino acids.
Most of the eukaryotic viral genomes analysed herein also encoded the gene phoH (Table 1). Although not a transporter this is relevant because phoH is found in the PHO (phosphate) regulon of E. coli and other bacteria, although its precise role is unclear (see discussions in Martiny et al., 2006; Sullivan et al., 2010). We identified phoH homologues in all available Mamiellales-virus genomes (OtV-1, OtV-2, OtV-5, OlV-1, BpV1, BpV-2 and MpV-1) but not EhV-86 (Table 1). Unlike the phoH genes in cyanobacteria and cyanophages (present in both hosts and viruses) or pstS and pho4 genes, which were found in all sequenced hosts, phoH genes appeared to be present only in the O. tauri and E. huxleyi genomes, based on BLASTp and tBLASTn similarity searches against available proteomes and genomes. In addition, the O. tauri-encoded version did not appear to be closely related to versions in viruses infecting Ostreococcus.
PHO4 superfamily members in the natural environment
We scanned metagenomes from three Pacific Ocean environments (Fig. 3), coastal (high PO4), mesotrophic (moderate PO4) and oligotrophic (moderate PO4 and low nitrogen) for members of the PHO4 superfamily (Table S2a) as well as Global Ocean Sampling (GOS) data (Rusch et al., 2007) using a HMM (Fig. S3, Table S2b). The detected PHO4 sequences were assigned to branches on a fixed maximum-likelihood reference tree built from the overall Pfam alignment (Fig. 4). A large fraction of environmental sequences were assigned to two groups containing Gammaproteobacteria. One of these groups contained sequences from cultured Shewanella strains and some cyanobacterial gene sequences (Arthrospira and Synechococcus WH5701) branched in the same region of the tree. WH5701 is a halotolerant strain and some environmental sequences assigned to this group might be from the nitrogen fixing cyanobacterium Crocosphaera. The Crocosphaera gene model containing the PHO4 domain (ZP_00517140) appeared to be missing a section of the conserved C-terminal domain that is part of the PHO4 Pfam model and was therefore not included in the tree, but had high similarity to the WH5701 version (ZP_01085811; 69% identity at the amino-acid level). Prochlorococcus and Synechococcus do not appear to encode genes containing the PHO4 Pfam domain. Environmental sequences were assigned to other bacterial groups as well (Fig. 4). The PHO4 Pfam model is composed of both high- and some low-affinity transporters and affinities could not be inferred based on placement in the overall Pfam analysis (Fig. 4). Although there appear to be numerous bacterial pho4 homologues in environmental community DNA (Fig. 4), if bacteriophages exchange this gene with their hosts, as eukaryotic viruses appear to, then any number might belong to phage rather than bacteria. Indeed, the flanking region of a Sanger sequenced shotgun clone from the Pacific Ocean deep chlorophyll maximum (DCM, 86 m) metagenome, recognized by our PHO4 superfamily HMM, indicated it was phage derived. In our phylogenetic analysis of this clone, the pho4-encoding ORF branched in an unsupported position with several bacterial taxa, close to the marine alphaproteobacterium strain HIMB59 (Fig. 5). In contrast, the flanking ORF in this cloned sequence encoded a hypothetical protein so far only seen in cyanophages.
Three hundred and nineteen environmental sequences were assigned to branches within the region of the PHO4 superfamily tree containing cultured eukaryotic algae, the Bathycoccus targeted metagenome pho4 gene sequence and the viral versions discussed above (Fig. 4). These environmental sequences were then assigned placements on the refined-eukaryotic pho4 tree (Fig. 2), which included more positions than the superfamily tree. The majority of eukaryotic environmental sequences grouped with prasinophytes, stramenopiles, haptophytes or corresponding viruses. A large number of those assigned to the Mamiellales (Bathycoccus/Ostreococcus) clade appeared to be from viral DNA templates (i.e. those assigned to OlV-1/OtV-2 or BpV-1) rather than host-derived templates. For the haptophyte lineage, environmental sequences were not placed with E. huxleyi or its virus EhV-86, but rather branched in a position basal to the E. huxleyi-EhV-86 node, suggesting they may have originated from other prymnesiophyte taxa, which include widespread uncultured marine groups (Worden and Not, 2008; Liu et al., 2009; Shi et al., 2009; Cuvelier et al., 2010), or potentially their viruses. Sequenced genomes are not available for Pelagomonas (or Pelagomonas-infecting viruses); therefore, a pho4 gene from this taxon (assuming it contains the pho4 gene) was not included in our analysis. Several Pelagomonas, but not Aureococcus, SSU rDNA sequences were present in clone libraries (data not shown) from the Pacific sites (Table 2). Hence, environmental pho4 sequences assigned to the Aureococcus node were likely from its more oceanic relative Pelagomonas. The analysis showed that eukaryotic algae and viruses inhabiting both PO4 replete (Fig. 3) and deplete (Figs. 1 and S3, and some cultured taxon isolation sites) environments contained the putatively high-affinity inorganic PO4 transporter gene (Fig. 2). Given the high degree of homology between host and respective viral pho4 sequences, unambiguous assignment to either host- or infecting virus branches was not always possible, particularly for short-metagenomic reads with limited phylogenetic information. The fact that our Pacific Ocean metagenome sequences came from larger size fractions (0.1 to ≤ 0.8, 0.8 to ≤ 3.0 and 3.0 to ≤ 20 µm) as opposed to sampling protocols that target the viral size fraction (e.g. tangential flow filtration for < 0.1 µm sized particles), indicates that the virally derived environmental sequences were present in infected hosts, especially for the two largest size fractions we sequenced. The proportion of viruses in nature that encode the pho4 gene is still not known.
In marine environments, P-availability is linked to primary production levels and shifts in phytoplankton community composition. PO4-uptake via different molecular mechanisms mitigates P-starvation and is important for survival in oligotrophic waters (e.g. Dyhrman et al., 2006b; Coleman and Chisholm, 2010). The distribution of the ‘green’-like pho4 homologues across green algae, haptophytes and some stramenopiles, indicates this putatively high-affinity transporter is important to physiological success. Together with previously hypothesized pstS HGT from cyanobacteria to cyanophages (Sullivan et al., 2010), the host-virus exchanges hypothesized herein show unexpected commonalities in the retention of PO4-uptake related genes in viral genomes from both viruses that infect eukaryotic hosts and bacteriophages.
Experimentally, E. huxleyi viral lysis rates are reportedly higher in P-replete than P-deplete conditions (Bratbak et al., 1993). Similar observations were reported for Synechococcus grown in P-deplete conditions, in which they appear to be infected and lysed at significantly lower rates by the bacteriophage S-PM2, than in P-replete conditions (Wilson et al., 1996). The presence or absence of PO4-uptake related genes in the genome of the infecting virus might mechanistically underpin these observations. For example, the S-PM2 genome does not appear to encode pstS (Mann et al., 2005), consistent with its low lysis rates in P-deplete conditions. Viral nutrient requirements and the ability of a virus, or lack thereof, to increase host nutrient uptake under limiting conditions could explain many such results. Moreover, presence of PO4-uptake related genes in a significant fraction of sequenced viral genomes, but not known nitrogen-uptake related genes, supports the hypothesis that viruses are more susceptible to PO4-limitation than nitrogen limitation due to a high nucleic acid to protein ratio. The prevalence of pho4 in marine viral genomes indicates it may alleviate bottom-up control of viruses by PO4-limitation, allowing them to propagate even under low PO4 conditions. This in turn could influence phytoplankton top-down controls, enhancing the ability of eukaryotic viruses and bacteriophages alike to replicate and induce host mortality. Thus, expression and manipulation of PO4-uptake related genes presumably influence both the fitness and demise of multiple marine microbial taxa. Our data reveal evolutionary pressures felt by marine viruses and highlight the complex influences of nutrient bioavailability on microbial interactions and dynamics.
Identification of transporter genes in virus genomes
Transporter protein sequences and corresponding annotations were retrieved from TransportDB (Ren et al., 2007). To avoid biases resulting from different gene prediction methods we predicted ORFs for all the eukaryotic viral genomes investigated (Table 1). Viral genome sequences were downloaded from GenBank, and stop-stop ORFs with a minimum size of 60-amino-acid residues were retrieved. A combination of BLASTx and BLASTp searches against TransportDB were performed and BLAST hits having an e-value less than 0.001 were considered for further analysis. Results were controlled using BLASTp searches against NR and searches against Pfam-A using the hmmscan module of HMMer 3 (Eddy, 2009).
Environmental sample collection and contextual analyses
Samples were collected using a rosette equipped with Niskin bottles, a CTD and fluorometer on two research expeditions, one aboard the R/V Seward Johnson (July 2006) and the other on R/V Western Flyer (October 2007). The first cruise was in the tropical Atlantic Ocean and the sample sequenced here was collected on 12 July 2006 at Station 13 (SJ0609) from the deep chlorophyll maximum (Fig. 1, Table 2). One L of water was filtered by gravity onto a 0.45 µm pore size Supor filter until reduced (concentrated) to a volume of 10 ml, this concentrated sample was then used for flow sorting as below. The second cruise was performed in the eastern North Pacific and samples collected at three sites (Table 2). In both cases samples for phosphate and nitrate analysis were collected at multiple depths from the surface to the base of the euphotic zone. For DNA for traditional bulk metagenomic sequencing, approximately 200 l of water were filtered first through a 20 µm mesh, and then sequentially through 293 mm diameter, 3 µm pore size filters (Pall Sciences Versapor-3000T), a 0.8 µm pore size filters (Pall Sciences Supor-800) and finally a 0.1 µm pore size filters (Pall Sciences Supor-100). Surface ocean chlorophyll concentrations (Figs 1 and 3; Fig. S3) were derived from the MODIS instrument carried on NASA's Aqua satellite (http://oceancolor.gsfc.nasa.gov).
Metagenome templates and construction
Processing for materials used to construct the targeted metagenome (sorted population) and the traditional metagenomes (size fractionated filters) was different. For the former, a 454-FLX and Sanger blended metagenomic assembly was generated for Bathycoccus. The analysed cells were first sorted by flow cytometry based on distinctive scatter and chlorophyll signals (Fig. S1) using an InFlux cell sorter (BD), directly after water collection. To avoid contamination, the instrument was cleaned extensively. Sheath fluid was 0.2 µm filtered, autoclaved PBS made in 18.2 MegaOhm H2O and 750 ml were run through the instrument after cleaning (immediately before sorting). Contamination control materials were from left and right test deflections run for 1 min (sample flow rate ∼25 µl min−1). All sort droplets were immediately frozen cryogenically. Upon return to land the population sort was resorted to enhance purity levels (Fig. S1). The sample and controls were then amplified by MDA and the products debranched and precipitated prior to sequencing according to methods in Cuvelier and colleagues (2010). Universal 16S rRNA gene primers were used to verify the absence of product in controls (indicating the instrument provided no prokaryotic contamination). A combination of Sanger shotgun sequencing and 454 pyrosequencing was then performed on the DNA as detailed in Cuvelier and colleagues (2010). For Sanger sequencing, 3 Kbp shotgun libraries were constructed using debranched MDA products and end-sequencing yielded 71 328 reads (totalling 52.83 Mbp). Pyrosequencing was also performed on debranched MDA products using the Genome Sequencer FLX System (454 Life Sciences) according to the manufacturer protocol and resulted in 118 Mbp of sequence. Pyrosequence reads were assembled using the 454 Newbler assembler version 1.1.02.15 and the consensus sequence shredded into 1 Kbp shreds with 100 bp overlaps. The 454 shred data were assembled with Sanger sequences using the lucy trimmer, to remove vector and low-quality sequence, and the Paracel Genome Assembler (lucy version 1.19p, PGA version 2.6.2). The assembly process generated 1929 contigs containing 9 859 508 bp.
To assess purity of the Bathycoccus sort we constructed 18S rDNA clone libraries using universal 18S rDNA primers (Moon-van der Staay et al., 2000). The resulting 741 sequences were analysed using Mothur v1.17 (Schloss et al., 2009). Sequences were first aligned against the SILVA 18S rRNA gene reference alignment (Pruesse et al., 2007). After end-trimming, clustering at 99% sequence identity resulted in six clusters and representatives of these were used for phylogenetic analysis. The maximum-likelihood tree was constructed using phyML v2.4 (Guindon and Gascuel, 2003) using an alignment where all gap-containing positions were removed and the TrNG substitution model was selected by AIC criterion (MrAIC script, distributed by J.A.A. Nylander, Uppsala University), and 100 bootstrap replicates. Because mitochondrial 16S rDNA databases are limited, BLASTn was performed against two databases, NCBI reference genomes and NCBI non-redundant nucleotide database (NT) using the 16S rDNA clones generated herein as query sequences.
In order to further insure that only scaffolds originating from Bathycoccus were analysed, ORFs spanning at least 180 nucleotides (between two stop codons) were retrieved using EMBOSS GetORF (Rice et al., 2000). The resulting putative ORFs were used as BLASTp queries (Altschul et al., 1997) against the NCBI non-redundant database (NR-DB). Taxonomic information for each of the best BLASTp hit (E-value cutoff: 1e−3) was retrieved using the NCBI taxonomy database and assigned to the corresponding ORF. A scaffold was classified as Bathycoccus-like if more than half of its predicted ORFs had their best BLASTp hits (E-value cutoff: 1e−3) against a protein sequence originating from any of the five available prasinophyte genomes (Derelle et al., 2006; Palenik et al., 2007; Worden et al., 2009), including the publically available but unpublished genome from Ostreococcus RCC809. That is, at least three ORFs had to be detected on the scaffold, and two or more of these had to have best BLASTp hits to prasinophytes in order to be included in subsequent analyses. Additionally, scaffolds smaller than 7 kb were discarded. Of 10 Mb total assembly, scaffolds composing 7.1 Mb fit the criteria of more than half the ORFs being prasinophyte-like (with a minimum of three predicted ORFs), and among these 5.1 Mb were scaffolds of 7 kb or more (183 scaffolds).
For each Pacific Ocean traditional metagenome, three different size fractions were extracted and sequenced independently. The nominal size fractions were 0.1 to < 0.8 µm, 0.8 to < 3 µm and 3 to < 20 µm. DNA was extracted from a fragment of each 293 mm filter using a sucrose protocol as described in Cuvelier and colleagues (2010). These materials were then divided and sequenced using the 454-FLX platform and Sanger sequencing.
PHO4 homologue searches
The PHO4 model alignment from Pfam (PF01384) was retrieved and used to build a hidden Markov (HMM) model based on amino-acid sequences using hmmbuild [part of HMMer 3 (Eddy, 2009)]. This HMM was then used with hmmsearch (also part of HMMer 3) to detect PHO4 homologues not yet integrated in the PF01384 model alignment. Searches were conducted against microbial eukaryotic proteomes not yet published or released in NR-DB and Uniprot (Apweiler et al., 2010) but publicly available (i.e. E. huxleyi, A. anophagefferens, Ostreococcus sp. RCC809) and NR-DB, allowing the detection of E. siliculosus (Cock et al., 2010), Chlorella sp. NC64A and Volvox carteri f. nagariensis homologues. The detected putative PHO4 sequences were then manually validated using BLASTp searches against NR-DB. It should be noted that the gene name pho4 has also been used to refer to genes that are not directly related to PO4 transport.
Environmental PHO4 sequences were identified from GOS [ORFs were retrieved from CAMERA (Seshadri et al., 2007)] and CN207 [after stop-stop ORF predictions with a minimum size of 40 amino-acid residues, as implemented by ORF_finder, part of the RAMMCAP analysis pipeline (Li, 2009)] datasets using the PF01384 HMM enriched with other detected PHO4 sequences (added to the model alignment with hmmalign) using hmmsearch with an E-value threshold of 1e−10 and gathering cutoff. The percentage of pho4 genes detected in our 454-FLX reads was lower than from GOS samples (Sanger sequences) or some of our Sanger libraries (Table S2). Frequency differences for PHO4 superfamily members in different samples were not compared since they could be a function of (i) the two data types (Sanger and 454-FLX) used or (ii) the fact that short reads encode less information for successful domain detection. Furthermore, differences in nominal pore sizes, samples and relative depth of sequencing compound difficulties in interpreting frequency results.
The overall PHO4 superfamily phylogenetic tree reconstruction (Fig. 4) was based on a non-redundant Pfam model alignment PF01384 with the addition of newly identified PHO4 amino-acid sequences (see above paragraph), which were aligned using hmmalign (HMMer 3). To reduce the number of taxa in the alignment prior to phylogenetic analysis representative sequences were selected from a 95% similarity clustering using Uclust (Edgar, 2010). In addition, short sequences (i.e. smaller than 200-amino-acid residues) were removed from the multiple sequence alignment. The final alignment was composed of 954 protein sequences. The maximum-likelihood PHO4 tree was reconstructed using RAxML 7.0.4 (Stamatakis, 2006), an estimate gamma shape parameter, a WAG matrix and empirical amino-acid frequencies. Statistical support was not computed for this reference tree due to the computational time needed with the large number of sequences and positions in the Pfam alignment, as well as the use of maximum-likelihood methods.
From the overall PHO4 superfamily protein tree, a region of the tree where most eukaryotic algal PHO4 protein sequences branched was identified and corresponding eukaryotic sequences were extracted from the alignment. This allowed us to construct an alignment that retained more informative positions than the entire Pfam alignment. Sequences were aligned using clustal W2 and the alignment was curated manually. A few additional sequences were added using T_Coffee v. 8.91 (Notredame et al., 2000). The majority of gap-containing sites were removed prior tophylogenetic analysis. This alignment served for a maximum-likelihood phylogenetic reconstruction using phyML v. 3 (Guindon and Gascuel, 2003) using Jones-Taylor-Thornton (JTT) matrix and 100 bootstrap replicates.
Homologues to the hypothetical protein and PHO4 superfamily protein sequences encoded on a potential marine bacteriophage metagenomic Sanger-sequenced shotgun clone were retrieved using a combination of BLASTp and tBLASTn searches against NR-DB and NCBI reference genomes and genomes of the Moore Marine Microbial Genomics Initiative. Sequences were aligned using T_Coffee v.8.91. Resulting multiple sequence alignments were cleaned using Gblocks (Castresana, 2000) allowing 50% of gapped-positions and was manually inspected using seaview 4 (Gouy et al., 2010). Phylogenetic reconstructions were conducted using phyML v. 3 with JTT matrix and 100 bootstrap replicates.
Placement of metagenomic PHO4 superfamily sequences
PHO4 superfamily members detected in traditional metagenomes from the Pacific (as well as in GOS data) using our HMM search were then assigned to branches or nodes on the PHO4 protein family tree using pplacer (Matsen et al., 2010). A WAG matrix was used and Bayesian posterior probabilities computed to establish statistical support of the placements. The resulting tree with mapped environmental sequences was visualized and edited with Dendroscope (Huson et al., 2007) and taxonomic information for each of the tree node was retrieved through UniProtKB identifiers (Apweiler et al., 2010). Environmental sequences assigned to the eukaryotic/algal region of the superfamily tree (Fig. 4) were extracted and used for a second round of phylogenetic placement (with same parameters as the initial run) on the manually curated eukaryotic PHO4 phylogenetic tree. Only environmental PHO4 sequences assigned placements that retained statistical support (i.e. P ≥ 0.75) were considered further.
Nucleotide sequence accession numbers
Traditional metagenome Sanger sequences from this study have been deposited in GenBank under Accession Numbers JF837193-JF837211 and 454-FLX sequences are in the CAMERA database (https://portal.camera.calit2.net/gridsphere/gridsphere). The targeted Bathycoccus metagenome was deposited in NCBI genomes under accession AFUW00000000.
We thank the captain and crews of the R/V Seward Johnson and R/V Western Flyer as well as J Zehr and J Montoya for cruise space on SJ0609. We are deeply grateful to A Engman, E Demir-Hilton, ML Cuvelier and MP Simmons for providing invaluable assistance with cruise sampling, H Wilcox for performing traditional metagenomic extractions as well as T Ishoey, T Woyke and SG Tringe for help with the population metagenome. C Suttle and MB Sullivan provided helpful discussions. H Moreau and E Derelle kindly confirmed Bathycoccus genome characteristics reported herein by comparison with a genome project for Bathycoccus. This work was supported by the David and Lucille Packard Foundation, NSF OCE-083672 and a Gordon and Betty Moore Foundation (GBMF) Young Investigator award to AZW; a DOE Community Sequencing Program award to AZW and JAE; and a GBMF Grant 1668 to AZW, EVA and GW.