Algae with secondary plastids of a red algal origin, such as ochrophytes (photosynthetic stramenopiles), are diverse and ecologically important, yet their evolutionary history remains controversial. We sequenced plastid genomes of two ochrophytes, Ochromonas sp. CCMP1393 (Chrysophyceae) and Trachydiscus minutus (Eustigmatophyceae). A shared split of the clpC gene as well as phylogenomic analyses of concatenated protein sequences demonstrated that chrysophytes and eustigmatophytes form a clade, the Limnista, exhibiting an unexpectedly elevated rate of plastid gene evolution. Our analyses also indicate that the root of the ochrophyte phylogeny falls between the recently redefined Khakista and Phaeista assemblages. Taking advantage of the expanded sampling of plastid genome sequences, we revisited the phylogenetic position of the plastid of Vitrella brassicaformis, a member of Alveolata with the least derived plastid genome known for the whole group. The results varied depending on the dataset and phylogenetic method employed, but suggested that the Vitrella plastids emerged from a deep ochrophyte lineage rather than being derived vertically from a hypothetical plastid-bearing common ancestor of alveolates and stramenopiles. Thus, we hypothesize that the plastid in Vitrella and potentially in other alveolates, may have been acquired by an endosymbiosis of an early ochrophyte.
The evolutionary history of photosynthetic eukaryotes is astonishingly complex. One of the most puzzling aspects is the evolution of plastids derived from red algae (rhodophytes) by eukaryote-to-eukaryote endosymbioses1,2. Phylogenetic analyses and a number of shared features indicate a single origin of these plastids, implying a scenario in which an early red alga became integrated into a heterotrophic eukaryotic host cell and ultimately gave rise to diverse algal lineages as well as non-photosynthetic lineages that subsequently lost their plastids. However, how the distribution of red alga-derived plastids was achieved across these various lineages remains controversial.
The Ochrophyta, a monophyletic phylum within the Stramenopiles (or Heterokonta), are the most diverse algal group with secondary plastids of algal origin in terms of morphology, pigmentation and phylogeny3,4. Diatoms (Bacillariophyceae) and multicellular brown algae (Phaeophyceae) are the best characterized ochrophytes, but at least 15 separate “classes”, plus several isolated smaller lineages of uncertain taxonomic status exist4,5,6,7,8. Several groups within the ochrophytes have important ecological roles, particularly in terms of marine photosynthesis and uptake of CO29.
Understanding relationships among the ochrophytes is important for both ecological and evolutionary studies. Phylogenetic studies of nuclear SSU rRNA gene sequences proposed the existence of several higher-order clades, specifically: diatoms plus the Bolidophyceae; the Chrysophyceae plus the Synchromophyceae; and the large “PX” clade comprising brown algae, the Xanthophyceae and other less well-known groups4,5,6,7,8. Multi-gene datasets including various combinations of nuclear, plastid and mitochondrial genes have improved resolution of ochrophyte phylogenetic relationships, yet some relationships are still unresolved5,7,10. Most notably, the position of the root of the ochrophyte phylogeny remains unknown. Despite these uncertainties and sometimes lack of statistical support, many different putative groupings of ochrophyte classes have been proposed11. This includes the Limnista, which contain the classes Eustigmatophyceae and Chrysophyceae along with a few minor lineages.
Regardless occasional horizontal movement of plastids between different eukaryotic lineages (see below), it is generally assumed that within most algal and plant lineages plastids are inherited vertically. The growing list of completely sequenced plastid genomes of various algal and plant lineages is thus a resource for inferring relationships among both plastids and host cell lineages12,13,14. Given the lack of evidence for non-vertical inheritance of ochrophyte plastids, plastid genome sequences could be also very helpful in resolving the ochrophyte phylogeny, but only seven of the approximately 15 known ochrophyte classes are represented by completely sequenced plastid genomes (Table S1). Furthermore, sampling is limited to a single genus in the case of eustigmatophytes and to a single species in the raphidophytes and xanthophytes. Representatives of other classes, such as the Chrysophyceae, Pinguiophyceae and Dichtyochophyceae, are yet to be sequenced.
Two different conceptual frameworks are often used to explain the emergence of ochrophytes. One is the “chromalveolate hypothesis”, which posits that all extant groups with red-algal derived plastids, namely the Ochrophyta, Myzozoa (a subgroup of the Alveolata that includes the Apicomplexa, Dinoflagellata, “chromerid” algae and a few additional minor lineages), Haptophyta and Cryptophyta (a subgroup of the Cryptista along with some non-photosyntetic lineages), inherited their plastids vertically from a common ancestor15,16. Plastid-lacking lineages closely related to any of these groups (i.e. plastid-lacking stramenopiles, alveolates and cryptists) would have lost the plastid secondarily. However, phylogenetic and phylogenomic analyses have failed to provide evidence for the monophyly of the proposed “chromalveolate” lineages. Whereas stramenopiles and alveolates are specifically related to the Rhizaria17,18, cryptists and haptophytes do not show any robustly supported affiliation and in some analyses are even found nested among eukaryotes with the primary plastid (Archaeplastida)18,19,20.
The second conceptual framework builds on a growing amount of data suggesting that a red algal plastid was acquired by one “chromalveolate” lineage, from which it spread to others through a series of higher-order tertiary or even quaternary endosymbioses (see, e.g.,21,22,23,24,25). This scenario has recently been dubbed the “rhodoplex hypothesis”26. However, higher-order endosymbiotic gains of plastids postulated by the rhodoplex hypothesis have only been conclusively demonstrated for some dinoflagellate lineages2,27.
Here, we sequenced and analyzed plastid genomes from two unrepresented ochrophyte groups. Trachydiscus minutus CCALA 838 belongs to a newly recognized eustigmatophyte subgroup (Goniochloridales)28,29 and is deeply diverged from the biotechnologically significant genus Nannochloropsis. Ochromonas sp. CCMP1393 is a marine member of the Chrysophyceae (Fig. S1), a group long known from freshwater habitats, but recently shown to be widely distributed in marine environments and important for primary production30,31. We performed comparative and phylogenetic analyses of these genomes in the context of existing plastid sequence data to address questions on relationships among ochrophytes as well as on the plastid evolution in “chromalveolates”.
Material and methods
Sequencing and annotation of the plastid genomes
Cultivation of the algae and DNA isolation followed standard protocols. Sequencing of total DNA preparations employed the 454 and Illumina platforms. Initial assemblies of the reads were searched to identify scaffolds corresponding to the plastid genome and the final assembly of the plastid genome sequences was achieved by manual gap filling and polishing. MFannot (http://megasun.bch.umontreal.ca/cgi-bin/mfannot/mfannotInterface.pl) was used for obtaining an initial automated annotation of the assembled plastid genome sequences, which was checked and improved manually. Details on the cultivation, DNA isolation, sequencing, assembly and annotation are provided in Supplementary methods. Annotated plastid genome sequences from T. minutus and Ochromonas sp. CCMP1393 are deposited in the GenBank database (accession numbers KJ624065 and KJ877675, respectively).
68 orthologous protein sequences encoded by plastid genomes were aligned and concatenated, leaving 16,948 reliably aligned amino acid (aa) positions in the main (“Full”) alignment (hereafter referred to as dataset F). Removal of the fastest-evolving category of sites from the full dataset F yielded the dataset SP (“Slow Positions”) comprising 11,208 aa positions. The dataset SG (“Slow Genes” comprising 14,699 reliably aligned aa positions was built by aligning only protein sequences encoded by 34 slowly evolving plastid genes defined in a previous study12.
Phylogenetic trees were inferred using two different methods: ML (RAxML 7.4.8a)32 with the site-homogeneous GTRGAMMA model of amino acid substitution and Bayesian inference (PhyloBayes 3.3f)33 with the site-heterogeneous CAT-GTR model. A detailed description of the procedures used to build the alignments and infer trees is available in Supplementary methods.
Results and Discussion
The plastid genomes of Trachydiscus minutus and Ochromonas sp. CCMP1393 reveal split clpC genes and rapid gene evolution shared by eustigmatophytes and chrysophytes
The newly sequenced plastid genomes exhibit size, GC content and gene content similar to previously sequence plastid genomes (see1,34; Tables 1 and S2, Fig. S2). Both genomes also display the typical circular-mapping architecture and the presence of inverted repeat (IR) regions separated by a large single copy and a small single copy region. The IR copies are identical at the nucleotide sequence level except for one-nucleotide deletion in one of the psaC copies in Trachydiscus introducing a frame-shift into the coding sequence; this copy is thus probably a non-functional pseudogene. The IR region of the Ochromonas plastid genome is the second longest among ochrophyte plastid genomes sequenced so far, while the small single copy region is exceptionally short (805 bp) and includes only two protein-coding genes.
The set of genes in the plastid genomes of Trachydiscus and Ochromonas is similar to other ochrophytes in terms of both their number and identity (Tables 1, S2 and S3). The most significant observations concerning the gene complement are discussed below, while additional details are provided in Supplementary Note 1.
One notable feature is the presence of a predicted group I intron in one of the three tRNA-Leu genes in the Trachydiscus genome. A tRNA-Leu gene intron has been postulated to have been present in the cyanobacterial ancestor of plastids and in time was lost, presumably independently, in many plastid-containing lineages35. Although overlooked in previous publications, we identified a tRNA-Leu gene in Nannochloropsis plastid genomes that also contains a group I intron (Fig. S3). This suggests that the intron may be a common feature in eustigmatophytes. In contrast, no introns were identified in Ochromonas plastid tRNA-Leu genes. This result is in accord with the previous indication that the intron was lost in the chrysophyte ancestor35.
Other interesting features were observed as well. For example, plastid genomes of Trachydiscus and Nannochloropsis spp. share possession of the gene ycf49. This gene codes for small uncharacterized proteins possessing the DUF2499 domain of an unknown function and is also found in primary plastid genomes from cyanidiophyte red algae and the glaucophyte Cyanophora paradoxa, but no other published plastid genomes (primary or secondary; Table S4). This is the case even when sensitive PSI-BLAST searches are employed. In both cyanidiophytes and eustigmatophytes ycf49 genes are located in the same conserved plastid gene block petL-ycf49-ycf4-trnG-psbE-psbF-psbL-psbJ. Thus, the ycf49 genes in the eustigmatophyte plastid genomes were apparently inherited directly from the plastid genome of the red algal ancestor of the “chromalveolate” plastids, while most “chromalveolate” lineages lost the ycf49 gene from their plastid genomes independently on several occasions.
Additionally, results were interesting for the gene clpC, which encodes a member of the Clp/Hsp100 family of AAA+ proteins involved in the protein degradation pathway mediated by the ClpP protease. Starkenburg et al.36 recently demonstrated that in Nannochloropsis spp. clpC is split into three separate genes, annotated as clpN (encoding the N-terminal domain of a typical ClpC protein), clpC1 (encoding the first AAA ATPase domain) and clpC2 (encoding the second AAA ATPase domain). We identified these three genes in the Trachydiscus plastid genome (with clpC2 gene present in two identical copies, since it resides in the IR region). This indicates that the split of clpC into three genes must have occurred before the radiation of known eustigmatophytes. Furthermore, the Ochromonas plastid genome exhibits an intermediate state, as it harbours a separate clpN gene, but the rest of the clpC gene is intact and codes for both AAA ATPase domains. Our results demonstrate that the split of the 5’-end of the clpC gene most likely predates the divergence of eustigmatophytes and chrysophytes, but without a plastid genome from the Pinguiophyceae, a putative sister group of the Limnista7, it cannot yet be ascertained whether this split is exclusive (i.e. synapomorphic) for the Limnista.
While inspecting multiple alignments of protein sequences encoded by the plastid genes we also noted that the sequences from eustigmatophytes and/or Ochromonas tend to harbour unusual indels in regions otherwise well conserved among ochrophytes (see Fig. S4), which may be an indication that the evolutionary rates of plastid genes in eustigmatophytes and Ochromonas are elevated compared to the rates exhibited by other ochrophytes. Indeed, phylogenetic analyses using individual genes revealed noticeably longer branches for eustigmatophyte and Ochromonas than for other ochrophytes (Fig. S5), indicating an increased rate of substitutions in the former lineages.
Phylogenomic analyses of plastid genomes support the Limnista clade
The most recent phylogenomic analyses of algal plastid genomes12,23,34,37 did not include data from chrysophytes and eustigmatophytes. Therefore, we conducted analyses using genes encoded by the new plastid genome sequences along with other recently published sequences. We used three different concatenated alignments (F, SG and SP) and two methods of phylogenetic inference (ML and Bayesian inference). These employed site-homogeneous and site-heterogeneous substitution models to evaluate the robustness of the results (see Material and Methods and Supplementary methods for technical details).
The six trees obtained from the three different datasets and two methods were generally congruent with the previous analyses and with each other (Fig. 1, S6 and S7, Table 2; informative aspects of our analyses that are not directly related to ochrophytes are provided in Supplementary Note 2). Both ML and Bayesian trees were consistent with a common origin of plastids of all “chromalveolates” from a deep red algal lineage and showed strong to maximal statistical support for the monophyly of ochrophyte plastids. Likewise, haptophyte plastids, including the haptophyte-derived tertiary plastid of the dinoflagellate Karlodinium veneficum, were monophyletic, as were those of cryptophytes. Among ochrophyte classes, all those represented by more than one species were monophyletic with maximal support in all trees.
Notably, the chrysophyte Ochromonas and eustigmatophytes formed a clade with maximal support in all trees (Fig. 1, S6 and S7). The chrysophyte and eustigmatophyte branches are considerably longer than those of most other taxa included in our analyses, apparently as a result of the generally increased evolutionary rate of individual plastid genes (see above). Such long branches are known to be prone to misplacement due to long-branch attraction, especially when the substitution model employed does not sufficiently capture the actual substitution process38,39,40. However, the clade uniting the Ochromonas plastid sequences with those of eustigmatophytes is consistently recovered even with the CAT-GTR substitution model, which is considered effective in coping with long-branch attraction39. Together with the unique trait shared by the plastid genome of Ochromonas and eustigmatophytes, i.e. the split clpC gene (see the previous section), the specific relationship observed between chrysophytes and eustigmatophytes is strongly supported by our analyses.
Our results thus corroborate the existence of the Limnista, a group originally proposed to be comprised of the Chrysophyceae (including Synurophyceae), the Eustigmatophyceae and two enigmatic organisms – the alga Chlamydomyxa labyrinthuloides (now known to represent a broader group called the Synchromophyceae41) and the minute marine flagellate Picophagus flagellatus11. While some analyses have supported such a grouping5,7, others have not10. Although our analysis does not include data from the other proposed Limnista lineages (i.e., synchromophytes and Picophagus), their affinity to the Chrysophyceae is consistently supported by other phylogenetic analyses7,8,41,42. Thus, our results can be interpreted as direct evidence for the monophyly of the Limnista sensu Cavalier-Smith and Chao11. Whether the Limnista should be expanded to also include the marine class Pinguiophyceae as recently suggested8, is a matter for future investigations.
Identifying the root of the ochrophyte phylogeny
In addition to resolving the Limnista, our analyses provide insights into other parts of the ochrophyte phylogeny. All trees provided maximal support for the sisterhood of brown algae and Vaucheria litorea representing the Xanthophyceae. This result agrees with previous single-gene and multi-gene analyses that established the existence of the so-called “PX” clade5,7. Diatoms and pelagophytes consistently formed sister groups within a single clade, generally with strong support (Table 2). The same clade was seen in plastid phylogenies reported by previous analyses lacking representatives of Limnista12,14,34. This clade likely also includes two additional classes with no sequenced plastid genome to date – the Bolidophyceae and Dictyochophyceae7 and was proposed by Riisberg10 to be termed the Khakista (expanding the original meaning of this name coined for a grouping of diatoms and bolidophytes only11). Our results thus add support to an emerging consensus on the existence of this major ochrophyte subclade united by some potential synapomorphies on the ultrastructural and biochemical level, e.g. by the presence of chlorophyll c37,10.
Further relationships within ochrophytes were less clearly resolved and appeared to be more sensitive to the method of inference and dataset employed. Least stable was the relative position of the PX clade, the raphidophyte Heterosigma and the Limnista clade (Fig. 1, S6 and S7, Table 2). All three PhyloBayes analyses provided maximal support for grouping of each of these three lineages, but ML analyses provided only low support or, in the case of the SP dataset, the Limnista clade moved to a position sister to all ochrophytes. The SP dataset yielded another inconsistent result: when analysed with PhyloBayes, it recovered (with high support) the Limnista in a position sister to Heterosigma, disrupting the monophyly of the Heterosigma+PX clade. This conflicts with previous multi-gene analyses that provided strong evidence for the sisterhood of raphidophytes and the PX clade (to the exclusion of limnistan lineages)7,10. It also conflicts with groupings observed in the five remaining trees generated herein (although with only moderate or low support in two of them, Table 2).
The unstable position of the Limnista clade in the different analyses may relate to significantly longer branch lengths for members of this clade compared to most other algal species (Fig. 1, 2, S6-S13), apart from the extremely long branch of the tertiary haptophyte-derived plastid of the dinoflagellate Karlodinium veneficum43. As already mentioned, long branches are known to be difficult to place reliably in phylogenetic trees, but considering that the more complex CAT-GTR model should provide more accurate inferences on the correct phylogenetic position of the rapidly-evolving limnistan branch than the site-homogeneous model39, we posit that branching of Limnista with the expanded PX clade is the appropriate working hypothesis.
Overall, these results point to an ochrophyte root positioned between the expanded Khakista (diatoms, pelagophytes, most likely also dictyochophytes and bolidophytes) and all other ochrophytes collectively termed the Phaeista10. Previous phylogenetic analyses provided conflicting and generally poorly supported results regarding the root position presumably due to the more limited phylogenetic information available at the time5,6,8,10,42. Notably, our inference on the position of the root of the ochrophyte phylogeny is consistent with the recently published phylogenomic analysis based on sequences of 85 nuclear genome-encoded proteins44. That study was not focused on ochrophytes and hence its sampling is relatively sparse, but the inferred phylogeny places the root with maximal support between diatoms and a pelagophyte on the one side and a phaeophyte and a eustigmatophyte on the other side. Our analyses suggest that further sampling of ochrophyte plastid genomes will help to completely resolve evolutionary relationships between algae within this immensely important group.
Revisiting the phylogenetic position of plastids in “chromerid” algae
The phylogenetic analyses described above omit data from plastid-bearing alveolates (i.e., myzozoans). Plastid genomes of two prominent myzozoan subgroups – apicomplexans and dinoflagellates – are extremely divergent and have a highly reduced gene content, whereas plastids of some other myzozoans, e.g. of the oyster parasite Perkinsus marinus and various “colpodellids” have lost a plastid genome entirely44,45. The situation is additionally complicated by the fact that several dinoflagellate lineages have more recently acquired algal endosymbionts or plastids from other groups via a higher-order (tertiary or quaternary) endosymbiosis or kleptoplastidy2,27.
However, two recently discovered myzozoan algae, Chromera velia46 and especially Vitrella brassicaformis47, have plastid genomes that are more similar to conventional plastid genomes12. These two species, together hereafter called “chromerid algae” or simply “chromerids” (put in quotation marks, because they are not monophyletic within Myzozoa44), have several unusual characteristics that are present in dinoflagellate and apicomplexan plastids as well, supporting the notion that plastids of the different myzozoan lineages (except the dinoflagellates with plastids representing recent replacements, see above) are monophyletic. Furthermore, the lesser divergence of the plastid genome in “chromerids”, particularly Vitrella, allowed phylogenomic analyses of conserved plastid genes, which showed this lineage as a sister branch of ochrophyte plastids as a whole12. This echoes the close relationship of stramenopiles and alveolates established on the basis of nuclear genes19 and suggests that a plastid was present in a common ancestor of stramenopiles and alveolates, in agreement with the chromalveolate hypothesis.
Here, we used the expanded sampling of plastid genomes to reanalyze these relationships. We used the same methodology as above to analyze the F, SG and SP datasets with the addition of Vitrella plastid protein sequences. We also analyzed variants of all three datasets from which data from the divergent tertiary plastid of the dinoflagellate K. veneficum were excluded. All ML trees consistently recovered the Vitrella lineage nested within ochrophytes, specifically related to the Eustigmatophyceae (Fig. 2A, S8-S12). Bootstrap support (BS) values for the Vitrella+Eustigmatophyceae clade varied from 97% (F dataset including K. veneficum) to 17% (SG dataset including K. veneficum, Table 2). Most analyses nevertheless provided strong support for a clade comprising the Eustigmatophyceae and Vitrella plus Ochromonas (Table 2). Hence, the ML analyses very consistently showed the Vitrella plastid as branching with the Limnista.
Interestingly, Vitrella and eustigmatophytes have high similarities in their pigment composition, including violaxanthin as the dominant xanthophyll and the shared absence of chlorophyll c (missing also from Chromera), which has previously led to speculation that a specific evolutionary connection between these taxa might exist47. However, Vitrella plastid gene sequences are still quite divergent, resulting in a long branch in the inferred phylogenetic trees, longer than even that of the tertiary plastid of K. veneficum (Fig. 2, S10-S12). Given the inherent difficulties in placing rapidly evolving lineages in phylogenies the accuracy of these inferences are uncertain, especially since members of the Limnista clade also exhibit relatively divergent plastid genome-encoded proteins.
Indeed, using PhyloBayes and the site-heterogeneous CAT-GTR model, which should be much more effective in coping with long-branch attraction39, we recovered the monophyletic Limnista excluding Vitrella with posterior probabilities (PP) of 0.97 to 1.0, depending on the dataset (Fig. 2B, S8-S12, Table 2). In three cases the Vitrella plastid lineage moved to a position sister to all ochrophytes, but the monophyly of ochrophytes to the exclusion of Vitrella was never strongly supported (maximal support was PP of 0.84 in the F dataset including K. veneficum; Table 2, Figs. S8, S10 and S11). However, in the remaining three trees the Vitrella plastid lineage moved from the base of ochrophytes to different positions within them, either sister to diatoms and pelagophytes or sister to the Limnista clade, but support was not attained for specific branching with any ochrophyte lineage (Fig. 2B, S9 and S12, Table 2). Except for the varying position of Vitrella, the topology of the ochrophyte subtree in these analyses was congruent with the results obtained by analyzing the datasets without Vitrella.
We additionally performed an analysis of an expanded SG dataset including not only sequences from Vitrella, but also Chromera (SG+V+C dataset). The resulting trees are portrayed as Fig. S13. As expected, plastids of the two myzozoan algae branch together with maximal support in both the ML and PhyloBayes analayses. However, the branch length of Chromera is more than three times as long as the branch length of the already quite divergent Vitrella (measured from the node representing their last common ancestor). In the ML analysis the Vitrella+Chromera clade is sister to Eustigmatophyceae with BS value of 80% (Fig. S13A), consistent with the results of the ML analyses of the SG+V dataset. In the PhyloBayes analysis, the Limnista clade (to the exclusion of Vitrella and Chromera) is recovered with PP of 0.98, but the Vitrella+Chromera clade is sister to Limnista with maximal support (Fig. S13B). Given the extreme divergence of the Chromera plastid protein sequences evident from the analysis of the SG dataset, we did not perform analyses of the other alignment variants (F, SP).
Did the plastid in alveolates emerge from an ochrophyte endosymbiont?
Understanding the actual nature of the relationship of plastids in ochrophytes and “chromerids” is relevant to the evolutionary history of plastids in “chromalveolates” in general. Our ML phylogenetic analyses that included Vitrella (or both “chromerid” algae) could suggest a tertiary endosymbiosis of a limnistan (possibly eustigmatophyte-related) alga in an alveolate host cell as the evolutionary origin of the Vitrella plastid. However, the clustering of the divergent “chromerid” plastid genome-encoded proteins with the relatively rapidly evolving sequences of Limnista may be a phylogenetic artifact, as suggested by the results of most analyses with the more realistic site-heterogeneous CAT-GTR model.
Some of these analyses show the Vitrella plastid sister to all ochrophyte plastids. This result seems consistent with the idea that Vitrella and ochrophytes and by extension all alveolates and stramenopiles, share a plastid-bearing ancestor, as implied by the chromalveolate hypothesis12,16. However, the ochrophyte stem branch in all such trees is very short and poorly supported (Figs. S8, S10 and S11). This is somewhat surprising, since one would expect a relatively long and well-supported stem branch of ochrophyte plastids if the plastids of Vitrella and ochrophytes were vertically inherited from a common ancestor of stramenopiles and alveolates. This is because the phylogenetic distance between the last common ancestor of stramenopiles and alveolates and the last common ancestor of ochrophyte lineages seems to be rather large. Eukaryote SSU rRNA phylogenies with relaxed molecular clock models suggested that the last common ancestor of stramenopiles and alveolates may be older than the last common ancestor of ochrophytes by 250-500 million years6,48. Dating of the main diversification events in the eukaryote phylogeny based on multigene molecular clocks inferred an even higher difference in the age of these nodes – around 750 million years49.
Although these numbers must be interpreted with caution, it is established that the ochrophyte radiation happened hundreds of millions of years after the stramenopile stem lineage separated from the stem lineage of alveolates. Thus, under this scenario, it is unclear why monophyly of ochrophyte plastids to the exclusion of Vitrella is not recovered consistently. Our logic is in principle similar to that of Baurain et al.23, who pointed to the discrepancy between the strong phylogenetic signal in “chromalveolate” plastid genomes that was suggestive of common ancestry and the weak, or perhaps non-existent, phylogenetic signal in nuclear genomes for the monophyly of the “chromalveolates” as such. All these observations argue against a simple vertical inheritance of a plastid from a common ancestor of stramenopiles and alveolates, or from a hypothetical common ancestor of “chromalveolates”.
Therefore, the results of our phylogenetic analyses appear more compatible with the idea that the “chromerid” lineage gained its plastid from an early ochrophyte. The ML analyses and some PhyloBayes analyses (see Fig. 2 and S13) suggest that the donor might have been a Limnista-related alga, although these results may well result from an artefactual attraction of the very divergent protein sequences encoded by “chromerid” plastid genomes to the relatively divergent sequences of the limnistan algae. Regardless of the actual donor ochrophyte lineage, we posit that the “chromerid” plastid represents a tertiary acquisition. The derived nature of the “chromerid” plastid genomes, especially that of Chromera, may then be explained as a consequence of this origin by a higher-order endosymbiosis, in analogy to the highly divergent plastid genome of K. veneficum (note that the plastid genomes of both Chromera and K. veneficum are linear rather than circular50) established by a (presumably) tertiary endosymbiosis of a haptophyte in a dinoflagellate host43.
The actual nature of the “chromerid” plastid depends on whether the plastid in the putative ochrophyte donor is derived from a secondary endosymbiosis itself, which has been challenged21,22,23,51. Most recently, Stiller and co-workers used novel statistical analyses of the gene content in “chromalveolate” genomes to conclude that the results are incompatible with the presence of a red algal endosymbiont in an ancestor of all “chromalveolates”25. They instead suggested an explicit scenario, in which a secondary red-algal plastid originated in the cryptophyte lineage, from which it moved by serial endosymbioses first into an ancestor of ochrophytes and subsequently from an early ochrophyte into an ancestor of haptophytes (alveolates were not analyzed in their study). If the ochrophyte plastid really emerged from a tertiary endosymbiosis, we would modify our interpretation above such that the “chromerid” plastid is not tertiary, but quaternary, as previously speculated by Bodył and co-workers22. This putative endosymbiosis must have been a different event than the quaternary origin of the haptophyte plastid suggested by Stiller et al..25, since haptophytes and alveolates never branch together in phylogenomic analyses of both plastid and nuclear genes (our results and, e.g.,18). Furthermore, the putative ochrophyte donor for the haptophyte plastid must have represented a very deep ochrophyte lineage preceding the radiation of extant ochrophytes, as our phylogenomic analyses leave no doubt on the monophyly of ochrophyte plastids to the exclusion of haptophyte plastids.
Previously, several lines of evidence suggested that plastids of “chromerid” algae are monophyletic with plastids of other myzozoans, i.e. apicomplexans and peridinin-containing dinoflagellates12. Hence, our inference of an ochrophyte origin of the “chromerid” plastid would by extension apply to the plastids in the Myzozoa as a whole. Anecdotal evidence for such a notion was actually available before, for example a phylogenetic analysis of five concatenated plastid genes carried out by Yoon et al. recovered peridinin-containing plastids of dinoflagellates nested within ochrophytes52. Our own multi-gene phylogenetic analyses that included sequences from plastid genomes of apicomplexans and peridinin-containing dinoflagellates indeed showed their grouping with “chromerids” (data not shown), but it cannot be excluded that this results is an artifact stemming from the extremely divergent nature of all these plastid genomes. Furthermore, Petersen et al. recently cast some doubt on the common origin of myzozoan plastids based on phylogenies of several nucleus-encoded plastid-targeted proteins26. While the significance of their observations remains unclear, we cautiously refrain from making definitive statements concerning all myzozoan plastids on the basis of results obtained by analyzing Vitrella and Chromera only.
Our newly sequenced ochrophyte plastid genomes enabled us to improve our understanding of the ochrophyte phylogeny by providing convincing support for the existence of the Limnista clade (comprised of the classes Chrysophyceae and Eustigmatophyceae). Our studies also support positioning of the root of the ochrophyte phylogeny between the groups Khakista (diatom, bolidophytes, pelagophytes, dictyochophytes) and Phaeista (i.e. raphidophytes, phaeophytes, xanthophytes, eustigmatophytes, chrysophytes and pinguiophytes along with a few other, smaller lineages) as redefined by Riisberg et al.10. Sampling of plastid genomes from ochrophyte classes that are as yet unsequenced and additional taxa for those like chrysophytes, for which the Ochromonas plastid genome sequenced herein is the sole representative, will allow testing of hypotheses on other relationships among the ochrophyte classes, such as the sisterhood of chrysophytes and synchromophytes and the probable sister relationship of the Limnista and Pinguiophyceae7.
The introduction of chrysophyte and additional eustigmatophyte plastid genome sequences provides a new impetus for revisiting the current ideas about the evolutionary origin of plastids in the Myzozoa. Our analyses suggest that a valid alternative hypothesis is horizontal transfer of a plastid, via endosymbiosis or kleptoplastidy, from an early ochrophyte lineage to an ancestor of “chromerid” algae. Whether this ancestor was a progenitor of the whole Myzozoa groups remains contentious due to the extremely divergent nature of all myzozoan plastid genomes characterized so far. This question may eventually be answered by additional improvements in the methodology of phylogenetic inference, new data from the nuclear genomes of Vitrella and Chromera, and/or characterization of the presently enigmatic additional plastid-bearing myzozoan lineages known by their plastid 16S rRNA genes sequences in environmental surveys53.
Finally, the gain of a plastid by one of the major “chromalveolate” lineages (Myzozoa) from another such lineages (Ochrophyta) suggested here does not support the chromalveolate hypothesis, but is consistent with an alternative scenario, ”the rhodoplex hypothesis”26. This scenario explains, for example, why plastids are not observed in non-myzozoan alveolates (ciliates, Colponema and Acavomonas54,55): because they were never acquired by their ancestors (while the chromalveolate hypothesis requires multiple plastid losses from these lineages). The upcoming wealth of genomic data and new genome-scale comparative and phylogenetic analyses should soon enable us to critically test this newly emerging view of the evolutionary history of “chromalveolates” and their plastids.
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We thank Jan Janouškovec for sharing data on Acavomonas prior to publication. This work was supported by grants from the Gordon and Betty Moore Foundation (GBMF3788) and DOE-DE-SC0004765 (to. A.Z.W) and from the the Czech Science Foundation (13-33039S to M.O. and P506-12-P931 to A.H.). The work conducted by the U.S. Department of Energy Joint Genome Institute is supported by the Office of Science of the U.S. Department of Energy under Contract No. DE-AC02-05CH11231. Funds also came from the Lucile and David Packard Foundation (to A.Z.W.). T.Š. and M.E. acknowledge support of the Project CZ.1.05/2.1.00/03.0100 (IET) financed by the Structural Funds of the EU and of the Project LO1208 of the National Feasibility Programme I of the Czech Republic.
The authors declare no competing financial interests.
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Ševčíková, T., Horák, A., Klimeš, V. et al. Updating algal evolutionary relationships through plastid genome sequencing: did alveolate plastids emerge through endosymbiosis of an ochrophyte?. Sci Rep 5, 10134 (2015). https://doi.org/10.1038/srep10134
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