Of the 257
P. infestans proteins identified as resembling flagellar components of other eukaryotes, most are connected firmly to the biology of that organelle since 77% of the corresponding genes are up-regulated during the life-stages when zoospore components are synthesized, and 82% are absent from the non-flagellated sister taxon
H. arabidopsidis. While it was not our intention to identify the complete flagellar proteome of
P. infestans, the 257 proteins are close in number to the roughly 250 estimated by 2-dimensional gel analysis to comprise the
C. reinhardtii flagellar axoneme
[49]. Reflecting diversification of flagella during the eukaryotic radiation, about 45 proteins assigned to
C. reinhardtii flagella lacked orthologs in
P. infestans, while 7
P. infestans sequences lacked orthologs in
C. reinhardtii. The latter were likely part of the ancestral organelle, since they match proteins in other lower eukaryotes such as
N. gruberi. Oomycetes may also have evolved novel flagellar proteins, but identifying them is problematic due to an inability to purify enough flagella for analysis.
The highest confidence flagella-focused dataset from
P. infestans includes about 185 proteins, based on the fraction that were up-regulated during spore formation and lacked orthologs in aflagellates. Combining both criteria reduces false positives, but at the expense of excluding proteins with multiple functions. This is especially true for proteins that may reside in both basal bodies and centrioles, which in many but not all species interconvert during the life cycle
[1],
[45]. While most basal body proteins have unknown functions, hints may come from their patterns of expression. Constitutive genes may encode proteins present in both basal bodies and centrioles, such as PITG_09512, which encodes the ortholog of a
T. thermophila basal body protein, BBC30
[27]. In contrast, up-regulated genes might influence the disappearance of centrioles and genesis of basal bodies during zoospore development. An example is sporulation-induced gene PITG_14588 (MKS1), which encodes the ortholog of a human protein needed for the migration of centrosomes to the sites of basal body formation
[50]. Although most oomycetes are known to use centrioles to nucleate the spindle at mitosis, their fate during the cell cycle and flagella-forming stages is not well-understood
[51]. Strikingly,
H. arabidopsidis lacks orthologs of all centriole-associated proteins covered by this study, including POC1 which is otherwise widely distributed in eukaryotes. It is unknown whether
H. arabidopsidis has centrioles.
The up-regulated
P. infestans genes exhibited diverse kinetics of mRNA induction and persistence, which likely reflects the role of each gene and biology of the spores. Sporangia are an intermediate between hyphae and zoospores. While sporangia can make zoospores soon after maturation, sporangia may remain quiescent for days until zoosporogenesis is stimulated by environment (cold temperatures and free water). Zoospore release can take less than an hour after stimulation, which is consistent with studies using actinomycin-D and cycloheximide that suggested that sporangia already contain all necessary proteins
[40],
[52]. Matching that earlier finding is our observation that virtually all genes for axonemal proteins (dynein arms, radial spokes, etc.) were induced early in sporulation. Why most RNAs persist through later stages may be explained by the need to replenish proteins broken down during sporangial quiescence, and to preserve motility, which can last a day under ideal conditions. Many late-induced genes may not be needed directly to form zoospores but may instead enable prolonged swimming and chemotaxis. Adenylate kinase PITG_03419 (CPC1), for example, may help maintain ATP levels during the motile period. The need for such functions may extend into subsequent life-stages, such as during encystment of the zoospore, extension of a germ tube from the cyst, or appressorium formation
[22].
Why and how the zoospore stage was lost from
H. arabidopsidis is unknown. The ability of most oomycetes to form zoospores is considered to aid survival by helping them reach nutrients or optimal host infection sites. However, zoospores were lost several times during oomycete speciation, particularly in obligately pathogenic clades such as
Hyaloperonospora, Bremia, and most
Peronospora spp.
[53]. Aflagellates germinate by extending a hyphal tube directly from the asexual spore (conidium), and this also occurs in
Phytophthora when conditions are too warm to favor zoospore release
[22]. Presumably the need to maintain genes for both germination pathways represented a heavy load for some obligately pathogenic oomycetes, providing positive selection for their loss. In this regard, the elimination of zoospores parallels the trend of metabolic pathway loss seen in many obligately pathogenic bacteria and protists
[7],
[54]. It should be noted that zoospores are maintained in some obligately pathogenic oomycetes, including the
Albugo white rusts and certain downy mildews within
Peronospora.
One may speculate that destruction of the pathway began in one allele of a flagellar gene that experienced a spontaneous mutation or insertion of a transposable element. The latter are common in most oomycete genomes, and have influenced the evolution of several gene families;
H. arabidopsidis has a 100 Mb genome, with 42% repetitive DNA content
[23],
[32],
[55]. Considering that oomycetes are diploid, how the remaining functional allele was lost is intriguing. Loss of heterozygosity due to mitotic crossing-over appears frequent in some oomycetes
[56], but this might have been ecologically deleterious if the elimination of the remaining functional allele was the result. Alternatively, the first step in zoospore loss could have been a dominant-negative regulatory mutation.
Regardless of the nature of the event that initiated zoospore loss from
H. arabidopsidis, examining the fate of its remaining flagellar genes was of interest in light of the complexity of oomycete genomes, and the dearth of information about their evolution outside of effector families, retroelements, and occasional gene fusions
[23],
[57],
[58],
[59]. A fair degree of shared synteny between
Phytophthora and
H. arabidopsidis allowed us to identify remnants of many flagella genes and observe a higher propensity for loss of synteny at the affected regions. One factor maintaining gene order in oomycetes is probably their small intergenic distances, most commonly 400–500 nt; this likely restricts the viability of illegitimate recombination events such as unequal crossovers or transposon insertions. Degradation of a flagella gene presumably results in a larger target for viable recombination.
We also observed compaction of the
H. arabidopsidis genome at most affected loci. Such changes are estimated to account for a reduction of about 1 Mb; overall shrinkage is likely greater since some metabolic genes, protein kinases, and effectors are also reported to be absent in
H. arabidopsidis
[23],
[60]. Most other obligately parasitic eukaryotes such as
Cryptosporidium and
Entamoeba have more dramatically reduced genomes as a consequence of gene loss or fusion, intron reduction, and a diminution of intergenic distances
[54]. Compaction, however, is not restricted to obligates. For example, the
O. tauri genome is much smaller than its relatives
[61].
It is interesting to note that the loss from
H. arabidopsidis of a gene seemed to be a better predictor of its flagellar role than whether
O. tauri lacked an ortholog of a
C. reinhardtii gene; the fraction of retained flagellar genes was 35% greater in
O. tauri than in the downy mildew. A recent survey showed that other plants that lack a flagella stage have also retained multiple flagella-associated proteins
[62]. Retention of a flagella gene is likely explained by its acquisition of additional roles prior to the loss of the organelle. The fraction of retained genes also may reflect the time of divergence of
H. arabidopsidis and
O. tauri from their flagellated sister taxa, as well as from plants and the Stramenopile kingdom, which includes oomycetes, from their shared ancestor. Plants and Stramenopiles diverged more than one billion years ago during the Mesoproterozoic era, the two algae from each other 0.5 to 1 billion years ago during the Neoproterozoic (although flagellar loss is probably more recent), and downy mildews from
Phytophthora less than 65 million years ago with oomycetes themselves having a Neoproterozoic origin
[5],
[63],
[64]. Our understanding of oomycete evolution is still developing, and current phylogenetic schemes nest many of the non-flagellated plant pathogens within
Phytophthora
[33]. Dating the oomycete radiation is challenging in the absence of a clear fossil record, and it is interesting to consider that gene remnants as reported here for
H. arabidopsidis may inform us about the timing of key events. The fact that gene remnants can still be detected suggests that flagella loss in
Hyaloperonospora was relatively recent.