Phylogenetic analyses indicate that the 19'Hexanoyloxy-fucoxanthin-containing dinoflagellates have tertiary plastids of haptophyte origin

The three anomalously pigmented dinoflagellates Gymnodinium galatheanum, Gyrodinium aureolum, and Gymnodinium breve have plastids possessing 19'-hexanoyloxy-fucoxanthin as the major carotenoid rather than peridinin, which is characteristic of the majority of the dinoflagellates. Analyses of SSU rDNA from the plastid and the nuclear genome of these dinoflagellate species indicate that they have acquired their plastids via endosymbiosis of a haptophyte. The dinoflagellate plastid sequences appear to have undergone rapid sequence evolution, and there is considerable divergence between the three species. However, distance, parsimony, and maximum-likelihood phylogenetic analyses of plastid SSU rRNA gene sequences place the three species within the haptophyte clade. Pavlova gyrans is the most basal branching haptophyte and is the outgroup to a clade comprising the dinoflagellate sequences and those of other haptophytes. The haptophytes themselves are thought to have plastids of a secondary origin; hence, these dinoflagellates appear to have tertiary plastids. Both molecular and morphological data divide the plastids into two groups, where G. aureolum and G. breve have similar plastid morphology and G. galatheanum has plastids with distinctive features.     

The Monophyletic Origin of the Peridinin‐, and Fucoxanthin‐Containing Dinoflagellate Plastid Through Tertiary Replacement

The dinoflagellates contain diverse plastids of uncertain origin. To determine the origin of the peridinin‐ and fucoxanthin‐containing dinoflagellate plastid, we sequenced the plastid‐encoded psaA, psbA, and rbcL genes from various red and dinoflagellate algae. The psbA gene phylogeny, which was made from a dataset of 15 dinoflagellates, 22 rhodophytes, five cryptophytes, seven haptophytes, seven stramenopiles, two chlorophytes, and a glaucophyte as the outgroup, supports monophyly of the peridinin‐, and fucoxanthin‐containing dinoflagellates, as a sister group to the haptophytes. The monophyletic relationship with the haptophytes is recovered in the psbA + psaA phylogeny, with stronger support. The rubisco tree utilized the ‘Form I’ red algal type of rbcL and included fucoxanthin‐containing dinoflagellates. The dinoflagellate + haptophyte sister relationship is also recovered in this analysis. Peridinium foliaceum is shown to group with the diatoms in all the phylogenies. Based on our analyses of plastid sequences, we postulate that: (1) the plastid of peridinin‐, and fucoxanthin‐containing dinoflagellates originated from a common ancestor; (2) the ancestral dinoflagellate acquired its plastid from a haptophyte though a tertiary plastid replacement; (3) ‘Form II’ rubisco replaced the ancestral rbcL after the divergence of the peridinin‐, and fucoxanthin‐containing dinoflagellates; and (4) we confirm that the plastid of P. foliaceum originated from a Stramenopiles endosymbiont.     

Phylogeny of Dinoflagellate Plastid Genes Recently Transferred to the Nucleus Supports a Common Ancestry with Red Algal Plastid Genes

It is generally accepted that peridinin-containing dinoflagellate plastids are derived from red alga, but whether they are secondary plastids equivalent to plastids of stramenopiles, haptophytes, or cryptophytes, or are tertiary plastids derived from one of the other secondary plastids, has not yet been completely resolved. As secondary plastids, plastid gene phylogeny should mirror that of nuclear genes, while incongruence in the two phylogenies should be anticipated if their origin was as tertiary plastids. We have analyzed the phylogeny of plastid-encoded genes from Lingulodinium as well as that of nuclear-encoded dinoflagellate homologues of plastid-encoded genes conserved in all other plastid genome sequences. Our analyses place the dinoflagellate, stramenopile, haptophyte, and cryptophyte plastids firmly in the red algal lineage, and in particular, the close relationship between stramenopile plastid genes and their dinoflagellate nuclear-encoded homologues is consistent with the hypothesis that red algal-type plastids have arisen only once in evolution.     

Genome evolution of a tertiary dinoflagellate plastid

The dinoflagellates have repeatedly replaced their ancestral peridinin-plastid by plastids derived from a variety of algal lineages ranging from green algae to diatoms. Here, we have characterized the genome of a dinoflagellate plastid of tertiary origin in order to understand the evolutionary processes that have shaped the organelle since it was acquired as a symbiont cell. To address this, the genome of the haptophyte-derived plastid in Karlodinium veneficum was analyzed by Sanger sequencing of library clones and 454 pyrosequencing of plastid enriched DNA fractions. The sequences were assembled into a single contig of 143 kb, encoding 70 proteins, 3 rRNAs and a nearly full set of tRNAs. Comparative genomics revealed massive rearrangements and gene losses compared to the haptophyte plastid; only a small fraction of the gene clusters usually found in haptophytes as well as other types of plastids are present in K. veneficum. Despite the reduced number of genes, the K. veneficum plastid genome has retained a large size due to expanded intergenic regions. Some of the plastid genes are highly diverged and may be pseudogenes or subject to RNA editing. Gene losses and rearrangements are also features of the genomes of the peridinin-containing plastids, apicomplexa and Chromera, suggesting that the evolutionary processes that once shaped these plastids have occurred at multiple independent occasions over the history of the Alveolata.     

Origins of plastids and glyceraldehyde-3-phosphate dehydrogenase genes in the green-colored dinoflagellate Lepidodinium chlorophorum

The dinoflagellate Lepidodinium chlorophorum possesses "green" plastids containing chlorophylls a and b (Chl a+b), unlike most dinoflagellate plastids with Chl a+c plus a carotenoid peridinin (peridinin-containing plastids). In the present study we determined 8 plastid-encoded genes from Lepidodinium to investigate the origin of the Chl a+b-containing dinoflagellate plastids. The plastid-encoded gene phylogeny clearly showed that Lepidodinium plastids were derived from a member of Chlorophyta, consistent with pigment composition. We also isolated three different glyceraldehyde-3-phosphate dehydrogenase (GAPDH) genes from Lepidodinium-one encoding the putative cytosolic "GapC" enzyme and the remaining two showing affinities to the "plastid-targeted GapC" genes. In a GAPDH phylogeny, one of the plastid-targeted GapC-like sequences robustly grouped with those of dinoflagellates bearing peridinin-containing plastids, while the other was nested in a clade of the homologues of haptophytes and dinoflagellate genera Karenia and Karlodinium bearing "haptophyte-derived" plastids. Since neither host nor plastid phylogeny suggested an evolutionary connection between Lepidodinium and Karenia/Karlodinium, a lateral transfer of a plastid-targeted GapC gene most likely took place from a haptophyte or a dinoflagellate with haptophyte-derived plastids to Lepidodinium. The plastid-targeted GapC data can be considered as an evidence for the single origin of plastids in haptophytes, cryptophytes, stramenopiles, and alveolates. However, in the light of Lepidodinium GAPDH data, we need to closely examine whether the monophyly of the plastids in the above lineages inferred from plastid-targeted GapC genes truly reflects that of the host lineages.     

Did some red alga‐derived plastids evolve via kleptoplastidy? A hypothesis

The evolution of plastids has a complex and still unresolved history. These organelles originated from a cyanobacterium via primary endosymbiosis, resulting in three eukaryotic lineages: glaucophytes, red algae, and green plants. The red and green algal plastids then spread via eukaryote–eukaryote endosymbioses, known as secondary and tertiary symbioses, to numerous heterotrophic protist lineages. The number of these horizontal plastid transfers, especially in the case of red alga‐derived plastids, remains controversial. Some authors argue that the number of plastid origins should be minimal due to perceived difficulties in the transformation of a eukaryotic algal endosymbiont into a multimembrane plastid, but increasingly the available data contradict this argument. I suggest that obstacles in solving this dilemma result from the acceptance of a single evolutionary scenario for the endosymbiont‐to‐plastid transformation formulated by Cavalier‐Smith & Lee (1985). Herein I discuss data that challenge this evolutionary scenario. Moreover, I propose a new model for the origin of multimembrane plastids belonging to the red lineage and apply it to the dinoflagellate peridinin plastid. The new model has several general and practical implications, such as the requirement for a new definition of cell organelles and in the construction of chimeric organisms.     

EVOLUTIONARY ANALYSES OF THE NUCLEAR‐ENCODED PHOTOSYNTHETIC GENE psbO FROM TERTIARY PLASTID‐CONTAINING ALGAE IN DINOPHYTA1

Although the dinophytes generally possess red‐algal‐derived secondary plastids, tertiary plastids originating from haptophyte and diatom ancestors are recognized in some lineages within the Dinophyta. However, little is known about the nuclear‐encoded genes of plastid‐targeted proteins from the dinophytes with diatom‐derived tertiary plastids. We analyzed the sequences of the nuclear psbO gene encoding oxygen‐evolving enhancer protein from various algae with red‐algal‐derived secondary and tertiary plastids. Based on our sequencing of 10 new genes and phylogenetic analysis of PsbO amino acid sequences from a wide taxon sampling of red algae and organisms with red‐algal‐derived plastids, dinophytes form three separate lineages: one composed of peridinin‐containing species with secondary plastids, and the other two having haptophyte‐ or diatom‐derived tertiary plastids and forming a robust monophyletic group with haptophytes and diatoms, respectively. Comparison of the N‐terminal sequences of PsbO proteins suggests that psbO genes from a dinophyte with diatom‐derived tertiary plastids (Kryptoperidinium) encode proteins that are targeted to the diatom plastid from the endosymbiotic diatom nucleus as in the secondary phototrophs, whereas the fucoxanthin‐containing dinophytes (Karenia and Karlodinium) have evolved an additional system of psbO genes for targeting the PsbO proteins to their haptophyte‐derived tertiary plastids from the host dinophyte nuclei.     

A tertiary plastid uses genes from two endosymbionts

The origin and subsequent spread of plastids by endosymbiosis had a major environmental impact and altered the course of a great proportion of eukaryotic biodiversity. The ancestor of dinoflagellates contained a secondary plastid that was acquired in an ancient endosymbiotic event, where a eukaryotic cell engulfed a red alga. This is known as secondary endosymbiosis and has happened several times in eukaryotic evolution. Certain dinoflagellates, however, are unique in having replaced this secondary plastid in an additional (tertiary) round of endosymbiosis. Most plastid proteins are encoded in the nucleus of the host and are targeted to the organelle. When secondary or tertiary endosymbiosis takes place, it is thought that these genes move from nucleus to nucleus, so the plastid retains the same proteome. We have conducted large-scale expressed sequence tag (EST) surveys from Karlodinium micrum, a dinoflagellate with a tertiary haptophyte-derived plastid, and two haptophytes, Isochrysis galbana and Pavlova lutheri. We have identified all plastid-targeted proteins, analysed the phylogenetic origin of each protein, and compared their plastid-targeting transit peptides. Many plastid-targeted genes in the Karlodinium nucleus are indeed of haptophyte origin, but some genes were also retained from the original plastid (showing the two plastids likely co-existed in the same cell), in other cases multiple isoforms of different origins exist. We analysed plastid-targeting sequences and found the transit peptides in K.micrum are different from those found in either dinoflagellates or haptophytes, pointing to a plastid with an evolutionarily chimeric proteome, and a massive remodelling of protein trafficking during plastid replacement.     

A novel type of kleptoplastidy in Dinophysis (Dinophyceae): presence of haptophyte-type plastid in Dinophysis mitra

Red-fluorescent, non-phycobilin-containing plastids were found in the heterotrophic dinoflagellate, Dinophysis mitra. Transmission electron microscopy showed that they contained a three-layer thylakoid, the absence of girdle lamella, and an embedded pyrenoid with thylakoid intrusions. These characteristics all coincide with haptophyte plastids. Phylogenetic analysis of the plastid small-subunit ribosomal DNA (SSU rDNA) revealed that the Dinophysis mitra sequences are distantly related to those of phycobilin-containing Dinophysis species and are positioned within a lineage of haptophytes belonging to Prymnesiophyceae. Because the plastid SSU rDNA sequences of Dinophysis mitra showed significant heterogeneity, despite being derived from a single species, it is highly likely that they were not established as plastids through an evolutionary process but are "kleptoplastids" (temporally stolen plastids) from multiple sources of haptophytes in the environment. We deduced that Dinophysis mitra takes up haptophytes myzocytotically and selectively retains the plastid with surrounding plastidal membranes, whereas other haptophyte cell components are degraded. This represents another type of kleptoplastidy in the Dinophysis species, which mostly harbor cryptophyte plastids, and is the first evidence of kleptoplastidy originating from haptophytes.     

Combined heat shock protein 90 and ribosomal RNA sequence phylogeny supports multiple replacements of dinoflagellate plastids

Dinoflagellates harbour diverse plastids obtained from several algal groups, including haptophytes, diatoms, cryptophytes, and prasinophytes. Their major plastid type with the accessory pigment peridinin is found in the vast majority of photosynthetic species. Some species of dinoflagellates have other aberrantly pigmented plastids. We sequenced the nuclear small subunit (SSU) ribosomal RNA (rRNA) gene of the "green" dinoflagellate Gymnodinium chlorophorum and show that it is sister to Lepidodinium viride, indicating that their common ancestor obtained the prasinophyte (or other green alga) plastid in one event. As the placement of dinoflagellate species that acquired green algal or haptophyte plastids is unclear from small and large subunit (LSU) rRNA trees, we tested the usefulness of the heat shock protein (Hsp) 90 gene for dinoflagellate phylogeny by sequencing it from four species with aberrant plastids (G. chlorophorum, Karlodinium micrum, Karenia brevis, and Karenia mikimotoi) plus Alexandrium tamarense, and constructing phylogenetic trees for Hsp90 and rRNAs, separately and together. Analyses of the Hsp90 and concatenated data suggest an ancestral origin of the peridinin-containing plastid, and two independent replacements of the peridinin plastid soon after the early radiation of the dinoflagellates. Thus, the Hsp90 gene seems to be a promising phylogenetic marker for dinoflagellate phylogeny.     

Plastid genome sequence of the cryptophyte alga Rhodomonas salina CCMP1319: lateral transfer of putative DNA replication machinery and a test of chromist plastid phylogeny

Cryptophytes are a group of unicellular algae with chlorophyll c-containing plastids derived from the uptake of a secondary (i.e., eukaryotic) endosymbiont. Biochemical and molecular data indicate that cryptophyte plastids are derived from red algae, yet the question of whether or not cryptophytes acquired their red algal plastids independent of those in heterokont, haptophyte, and dinoflagellate algae is of long-standing debate. To better understand the origin and evolution of the cryptophyte plastid, we have sequenced the plastid genome of Rhodomonas salina CCMP1319: at 135,854 bp, it is the largest secondary plastid genome characterized thus far. It also possesses interesting features not seen in the distantly related cryptophyte Guillardia theta or in other red secondary plastids, including pseudogenes, introns, and a bacterial-derived gene for the tau/gamma subunit of DNA polymerase III (dnaX), the first time putative DNA replication machinery has been found encoded in any plastid genome. Phylogenetic analyses indicate that dnaX was acquired by lateral gene transfer (LGT) in an ancestor of Rhodomonas, most likely from a firmicute bacterium. A phylogenomic survey revealed no additional cases of LGT, beyond a noncyanobacterial type rpl36 gene similar to that recently characterized in other cryptophytes and haptophytes. Rigorous concatenated analysis of 45 proteins encoded in 15 complete plastid genomes produced trees in which the heterokont, haptophyte, and cryptophyte (i.e., chromist) plastids were monophyletic, and heterokonts and haptophytes were each other's closest relatives. However, statistical support for chromist monophyly disappears when amino acids are recoded according to their chemical properties in order to minimize the impact of composition bias, and a significant fraction of the concatenate appears consistent with a sister-group relationship between cryptophyte and haptophyte plastids.     

Review

Most photosynthetic dinoflagellates harbour the peridinin plastid. This plastid is surrounded by three membranes and its characteristic pigments are chlorophyll c and the carotenoid peridinin. The evolutionary origin of this peculiar plastid remains controversial and is hotly debated. On the recently published tree of concatenated plastid-encoded proteins, dinoflagellates emerge from within the Chromista (clade containing cryptophytes, heterokonts, and haptophytes) and cluster specifically with Heterokonta. These data inspired a new version of the ‘chromalveolate’ model, according to which the peridinin plastid evolved by ‘descent with modification’ from a heterokont-like plastid that had been acquired from a rhodophyte by an ancestral chromalveolate. However, this model of plastid evolution encounters serious obstacles. Firstly, the heterokont plastid is surrounded by four membranes, which means that the ancestral peridinin plastid must have lost one of these primary membranes. However, such a loss could be traumatic, because it could potentially disturb protein import into and/or within the plastid. Secondly, on the phylogenetic tree of Dinoflagellata and Heterokonta, the first to diverge are not plastid, but heterotrophic, aplastidal taxa. Thus, when accepting the single origin of the heterokont and peridinin plastids, we would have to postulate multiple plastid losses, but such a scenario is highly doubtful when the numerous non-photosynthetic functions of plastids and their existence in heterotrophic protists, including parasitic lineages, are considered. Taking these obstacles into account, we suggest an alternative interpretation of the concatenated tree of plastid-encoded proteins. According to our hypothesis, the peridinin plastid evolved from a heterokont alga through tertiary endosymbiosis.     

Origin of the plastid in the anomalously pigmented dinoflagellate Gymnodinium mikimotoi (Gymnodiniales, Dinophyta) as inferred from phylogenetic analysis based on the gene encoding the large subunit of form I-type RuBisCO

The dinoflagellate Gymnodinium mikimotoi Miyake et Kominami ex Oda possesses an anomalously pigmented plastid which contains 19′‐hexanoyloxyfucoxanthin, 19′‐butanoyloxyfucoxanthin and fucoxanthin instead of peridinin as the major carotenoids. Previously, we have shown that the plastid of G. mikimotoi belongs to the rhodoplast lineage as inferred from phylogenetic analyses based on the amino acid sequences deduced from psbA and psaA and the nucleotide sequence of the plastid small subunit ribosomal RNA. Furthermore, in the present study, we cloned and sequenced an additional representative plastid gene, rbcL, encoding the large subunit of ribulose 1–5 bisphosphate carboxylase/oxygenase (RuBisCO LSU) from G. mikimotoi. The amino acid sequence deduced from the rbcL gene of G. mikimotoi apparently revealed the conventional form I RuBisCO LSU, which is present in most photosynthetic organisms, and not the divergent form II existing in typically pigmented dinofl age Nates with plastids containing peridinin as the main carotenoid. This finding supports the hypothesis that the origins of the plastids in G. mikimotoi and peridinin‐type dinoflagellates are not related to each other. Molecular phylogenetic analysis based on the amino acid sequence deduced from the rbcL gene further showed that the plastid of G. mikimotoi belongs to the rhodoplast lineage. In particular, G. mikimotoi clustered with haptophytes in the phylogenetic tree. From this result, two hypotheses with respect to the origin of the plastid in G. mikimotoi can be proposed: G. mikimotoi may have engulfed a haptophyte‐like cell (tertiary symbiosis) or englulfed a rhodophyte‐like cell that was closely related to the origin of the plastid in the haptophyte (secondary symbiosis).     

Diversity and evolutionary history of plastids and their hosts

By synthesizing data from individual gene phylogenies, large concatenated gene trees, and other kinds of molecular, morphological, and biochemical markers, we begin to see the broad outlines of a global phylogenetic tree of eukaryotes. This tree is apparently composed of five large assemblages, or "supergroups." Plants and algae, or more generally eukaryotes with plastids (the photosynthetic organelle of plants and algae and their nonphotosynthetic derivatives) are scattered among four of the five supergroups. This is because plastids have had a complex evolutionary history involving several endosymbiotic events that have led to their transmission from one group to another. Here, the history of the plastid and of its various hosts is reviewed with particular attention to the number and nature of the endosymbiotic events that led to the current distribution of plastids. There is accumulating evidence to support a single primary origin of plastids from a cyanobacterium (with one intriguing possible exception in the little-studied amoeba Paulinella), followed by the diversification of glaucophytes, red and green algae, with plants evolving from green algae. Following this, some of these algae were themselves involved in secondary endosymbiotic events. The best current evidence indicates that two independent secondary endosymbioses involving green algae gave rise to euglenids and chlorarachniophytes, whereas a single endosymbiosis with a red algae gave rise to the chromalveolates, a diverse group including cryptomonads, haptophytes, heterokonts, and alveolates. Dinoflagellates (alveolates) have since taken up other algae in serial secondary and tertiary endosymbioses, raising a number of controversies over the origin of their plastids, and by extension, the recently discovered cryptic plastid of the closely related apicomplexan parasites.     

Phylogeny of nuclear-encoded plastid-targeted GAPDH gene supports separate origins for the peridinin- and the fucoxanthin derivative-containing plastids of dinoflagellates

Although most photosynthetic dinoflagellates have plastids with peridinin, the three dinoflagellate genera Karenia, Karlodinium, and Takayama possess anomalously pigmented plastids that contain fucoxanthin and its derivatives (19′-hexanoyloxy-fucoxanthin and 19′-butanoyloxy-fucoxanthin) instead of the peridinin. This pigment composition is similar to that of haptophytes. All peridinin-containing dinoflagellates investigated so far have at least two types of glyceraldehyde-3-phosphate dehydrogenase (GAPDH): cytosolic and plastid-targeted forms. In the present study, we cloned and sequenced genes encoding cytosolic and plastid-targeted GAPDH proteins from three species of the fucoxanthin derivative-containing dinoflagellates. Based on the molecular phylogeny, the plastid-targeted GAPDH genes of the fucoxanthin derivative-containing dinoflagellates were closely related to those of haptophyte algae rather than to the peridinin-containing dinoflagellates, while one of several cytosolic versions from the peridinin- and the fucoxanthin derivative-containing dinoflagellates are closely related to each other. Considering a previously reported theory that the plastid-targeted GAPDH from the peridinin-containing dinoflagellates originated by a gene duplication of the cytosolic form before the splitting of the dinoflagellate lineage, it is highly likely that the plastid-targeted GAPDH gene of the peridinin-containing dinoflagellates is original in this algal group and that in the fucoxanthin-containing dinoflagellates, the original plastid-targeted GAPDH was replaced by that of a haptophyte endosymbiont during a tertiary endosymbiosis. The present results strongly support the hypothesis that the plastids of the peridinin- and the fucoxanthin derivative-containing dinoflagellates are of separate origin.     

Phylogenetic artifacts can be caused by leucine, serine, and arginine codon usage heterogeneity: dinoflagellate plastid origins as a case study

Phylogenetic analyses of first and second codon positions (DNA1 + 2 analysis) and amino acid sequences (protein analysis) are often thought to provide similar estimates of deep-level phylogeny. However, here we report a novel artifact influencing DNA level phylogenetic inference of protein-coding genes introduced by codon usage heterogeneity that causes significant incongruities between DNA1 + 2 and protein analyses. DNA1 + 2 analyses of plastid-encoded psbA genes (encoding of photosystem II D1 proteins) strongly suggest a relationship between haptophyte plastids and typical (peridinin-containing) dinoflagellate plastids. The psbA genes from haptophytes and a subset of the peridinin-type plastids display similar codon usage patterns for Leu, Ser, and Arg, which are each encoded by two separated codon sets that differ at first or first plus second codon positions. Our detailed analyses clearly indicate that these unusual preferences shared by haptophyte and some peridinin-type plastid genes are largely responsible for their strong affinity in DNA analyses. In particular, almost all of the support from DNA level analyses for the monophyly of haptophyte and peridinin-type plastids is lost when the codons corresponding to constant Leu, Ser, and Arg amino acids are excluded, suggesting that this signal comes from rapidly evolving synonymous substitutions, rather than from substitutions that result in amino acid changes. Indeed, protein maximum-likelihood analyses of concatenated PsaA and PsbA amino acid sequences indicate that, although 19' hexanoyloxyfucoxanthin-type (19' HNOF-type) plastids in dinoflagellates group with haptophyte plastids, peridinin-type plastids group weakly with those of stramenopiles. Consequently our results cast doubt on the single origin of peridinin-type and 19' HNOF-type plastids in dinoflagellates previously suggested on the basis of psaA and psbA concatenated gene phylogenetic analyses. We suggest that codon usage heterogeneity could be a more general problem for DNA level analyses of protein-coding genes, even when third codon positions are excluded.     

Genome fragmentation is not confined to the peridinin plastid in dinoflagellates

When plastids are transferred between eukaryote lineages through series of endosymbiosis, their environment changes dramatically. Comparison of dinoflagellate plastids that originated from different algal groups has revealed convergent evolution, suggesting that the host environment mainly influences the evolution of the newly acquired organelle. Recently the genome from the anomalously pigmented dinoflagellate Karlodinium veneficum plastid was uncovered as a conventional chromosome. To determine if this haptophyte-derived plastid contains additional chromosomal fragments that resemble the mini-circles of the peridin-containing plastids, we have investigated its genome by in-depth sequencing using 454 pyrosequencing technology, PCR and clone library analysis. Sequence analyses show several genes with significantly higher copy numbers than present in the chromosome. These genes are most likely extrachromosomal fragments, and the ones with highest copy numbers include genes encoding the chaperone DnaK(Hsp70), the rubisco large subunit (rbcL), and two tRNAs (trnE and trnM). In addition, some photosystem genes such as psaB, psaA, psbB and psbD are overrepresented. Most of the dnaK and rbcL sequences are found as shortened or fragmented gene sequences, typically missing the 3'-terminal portion. Both dnaK and rbcL are associated with a common sequence element consisting of about 120 bp of highly conserved AT-rich sequence followed by a trnE gene, possibly serving as a control region. Decatenation assays and Southern blot analysis indicate that the extrachromosomal plastid sequences do not have the same organization or lengths as the minicircles of the peridinin dinoflagellates. The fragmentation of the haptophyte-derived plastid genome K. veneficum suggests that it is likely a sign of a host-driven process shaping the plastid genomes of dinoflagellates.     

64 Nucleus-encoded, plastid-targeted glyceraldehyde-3-phosphate dehydrogenase (GAPDH) indicates a single origin for chromalveolate plastids

Plastids (the photosynthetic organelles of plants and algae) ultimately originated through an endosymbiosis between a cyanobacterium and a eukaryote. Subsequently, plastids spread to other eukaryotes by secondary endosymbioses that took place between a eukaryotic alga and a second eukaryote. Recently, evidence has mounted in favour of a single origin for plastids of apicomplexans, cryptophytes, dinoflagellates, haptophytes, and heterokonts (together with their non-photosynthetic relatives, collectively termed chromalveolates). As of yet, however, no single molecular marker has been described which supports a common origin for all of these plastids. One piece of the evidence for a single origin of chromalveolate plastids came from plastid-targeted glyceraldehyde-3-phosphate dehydrogenase (GAPDH), which originated by a gene duplication of the cytosolic form. However, no plastid GAPDH has been characterized from haptophytes, leaving an important piece of the puzzle missing. We have sequenced genes encoding cytosolic, mitochondrial-targeted, and plastid-targeted GAPDH proteins from a number of haptophytes and heterokonts, and found the haptophyte homologues to branch within the strongly supported clade of chromalveolate plastid-targeted GAPDH genes. Interestingly, plastid-targeted GAPDH genes from the haptophytes were more closely related to apicomplexan genes than was expected. Overall, the evolution of plastid-targeted GAPDH reinforces other data for a red algal ancestry of apicomplexan plastids, and raises a number of questions about the importance of plastid loss and the possibility of cryptic plastids in non-photosynthetic lineages such as ciliates.     

Nucleus-encoded,plastid-targeted glyceraldehyde-3-phosphate dehydrogenase (GAPDH) indicates a single origin for chromalveolate plastids

Plastids (the photosynthetic organelles of plants and algae) originated through endosymbiosis between a cyanobacterium and a eukaryote and subsequently spread to other eukaryotes by secondary endosymbioses between two eukaryotes. Mounting evidence favors a single origin for plastids of apicomplexans, cryptophytes, dinoflagellates, haptophytes, and heterokonts (together with their nonphotosynthetic relatives, termed chromalveolates), but so far, no single molecular marker has been described that supports this common origin. One piece of evidence comes from plastid-targeted glyceraldehyde-3-phosphate dehydrogenase (GAPDH), which originated by a gene duplication of the cytosolic form. However, no plastid GAPDH has been characterized from haptophytes, leaving an important piece of the puzzle missing. We have sequenced genes encoding cytosolic, mitochondrion-targeted, and plastid-targeted GAPDH proteins from a number of haptophytes and heterokonts and found haptophyte homologs that branch within a strongly supported clade of chromalveolate plastid-targeted genes, being more closely related to an apicomplexan homolog than was expected. The evolution of plastid-targeted GAPDH supports red algal ancestry of apicomplexan plastids and raises a number of questions about the importance of plastid loss and the possibility of cryptic plastids in nonphotosynthetic lineages such as ciliates.     

PIGMENT COMPOSITION AND rbcL SEQUENCE DATA FROM THE SILICOFLAGELLATE DICTYOCHA SPECULUM: A HETEROKONT ALGA WITH PIGMENTS SIMILAR TO SOME HAPTOPH Y TES

Monophyly of plastids in the morphologically diverse heterokont algae has rarely been questioned. However, HPLC analysis revealed that the pigment composition of the silicoflagellate Dictyocha speculum Ehrenberg is similar to that observed in a group of haptophytes (“type 4”sensu Jeffrey and Wright 1994 . Dictyocha speculum and type 4 haptophytes possess acylfucoxanthins (19′-butanoyloxy- and 19′-hexanoyloxyfucoxanthin) in addition to fuco-, diadino-, and diatoxanthin and chl a, c, and c₃. The pigment composition of two pedinellids (Apedinella radians[Lohmann] Campbell and Mesopedinella arctica Daugbjerg), a sister group to D. speculum, deviates from D. speculum by lack of chl c ₃ and acylfucoxanthins. The distinct pigment composition suggested that plastid evolution in D. speculum differs from that of other heterokont algae. This prompted determination of the plastid-encoded rbcL gene from D. speculum to gain further insight into the evolutionary history of plastids in heterokont algae and haptophytes. A phylogenetic inference based on parsimony, maximum likelihood, and LogDet transformation methods included 35 heterokonts, 19 haptophytes, 8 red algae, and 1 cryptomonad. Three proteobacteria possessing type I RUBISCO were used to root the tree. In phylogenetic analyses, D. speculum was closely related to Rhizochromulina sp. and pedinellids, despite the latter possessing a different pigment composition. Surprisingly, the Dictyochophyceae clustered outside the lineage of heterokont algae but not within the haptophytes. Hence, analyses deduced from rbcL sequences indicated that the plastids in heterokont algae might have a more complex evolutionary history and that the shared pigment composition in D. speculum and type 4 haptophytes could be explained by convergent evolution or gene transfer. The pigment composition in D. speculum may have implications for pigment-based characterization of phytoplankton community structure in natural samples.