Organic-walled dinoflagellate cyst production in relation to upwelling intensity and lithogenic influx in the Cape Blanc region (off north-west Africa)

Fossil dinoflagellate cyst assemblages are increasingly used in paleoclimatic research to establish paleoenvi‐ronmental reconstructions. To obtain reliable reconstructions, it is essential to know which physical factors influence the cyst production. Most information about the relationship between variations in physical parameters and cyst production is known from middle and higher latitudes. Information from the (sub)tropics is rare. To increase this information, the temporal variation in cyst assemblages from the upwelling area off north‐west Africa (off Mauritania) has been compared to environmental conditions of the upper water column. Samples were collected by the sediment trap CB9, off north‐west Africa (Cape Blanc, 21°15′2″N, 20°42′2″W) between 11 June 1998 and 7 November 1999 at 27.5‐day intervals. Off Cape Blanc, upwelling occurs throughout the year with variable intensity. This region is also characterized by frequently occurring Saharan dust storms. Seasonal variations in dust input, upwelling intensity and sea surface temperature are reflected by the production of organic‐walled dinoflagellate cyst assemblages. Several cyst taxa are produced throughout the sampling interval, with the highest fluxes at times of strongest upwelling relaxation and/or dust input (Echinidinium aculeatum Zonneveld, Echini‐din ium delicatum Zonneveld, Echinidinium granulaturn Zonneveld, Echinidinium spp., Impagidinium aculeatum (Wall) Lentin et Williams, Impagidinium sphaeri‐cum (Wall) Lentin et Williams, Protoperidinium americanum (Gran et Braarud) Balech, Protoperidinium stellatum (Wall in Wall et Dale) Rochon etal., Protoperidinium spp., Selenopemphix nephroides (Benedek) Benedek et Sarjeant and Selenopemphix quanta (Bradford) Matsuoka). Species such as, for example, Bitectatodinium spongium (Zonneveld) Zonneveld et Jurkschat and Impagidinium patulum (Wall) Stover et Evitt do not show any production pattern related to a particular season of the year or to specific environmental conditions in the upper water column. The production of cysts of Protoperidinium monospinum (Paulsen) Zonneveld et Dale is restricted to intervals with increased nutrient concentrations in upper waters when sea surface temperatures at the sampling site is below approximately 24°C.     

A New Heterotrophic Dinoflagellate from the North‐eastern Pacific,Protoperidinium fukuyoi: Cyst–Theca Relationship,Phylogeny, Distribution and Ecology

The cyst–theca relationship of Protoperidinium fukuyoi n. sp. (Dinoflagellata, Protoperidiniaceae) is established by incubating resting cysts from estuarine sediments off southern Vancouver Island, British Columbia, Canada, and San Pedro Harbor, California, USA. The cysts have a brown‐coloured wall, and are characterized by a saphopylic archeopyle comprising three apical plates, the apical pore plate and canal plate; and acuminate processes typically arranged in linear clusters. We elucidate the phylogenetic relationship of P. fukuyoi through large and small subunit (LSU and SSU) rDNA sequences, and also report the SSU of the cyst‐defined species Islandinium minutum (Harland & Reid) Head et al. 2001. Molecular phylogenetic analysis by SSU rDNA shows that both species are closely related to Protoperidinium americanum (Gran & Braarud 1935) Balech 1974. Large subunit rDNA phylogeny also supports a close relationship between P. fukuyoi and P. americanum. Three subgroups in total are further characterized within the Monovela group. The cyst of P. fukuyoi shows a wide geographical range along the coastal tropical to temperate areas of the North‐east Pacific, its distribution reflecting optimal summer sea‐surface temperatures of ~14–18 °C and salinities of 22–34 psu.     

A further phylogenetic study of the heterotrophic dinoflagellate genus, Protoperidinium (Dinophyceae) based on small and large subunit ribosomal RNA gene sequences

The heterotrophic marine dinoflagellate genus Protoperidinium is the largest genus in the Dinophyceae. Previously, we reported on the intrageneric and intergeneric phylogenetic relationships of 10 species of Protoperidinium, from four sections, based on small subunit (SSU) rDNA sequences. The present paper reports on the impact of data from an additional 5 species and, therefore, an additional two sections, using the SSU rDNA data, but now also incorporating sequence data from the large subunit (LSU) rDNA. These sequences, in isolation and in combination, were used to reconstruct the evolutionary history of the genus. The LSU rDNA trees support a monophyletic genus, but the phylogenetic position within the Dinophyceae remains ambiguous. The SSU, LSU and SSU + LSU rDNA phylogenies support monophyly in the sections Avellana, Divergentia, Oceanica and Protoperidinium, but the section Conica is paraphyletic. Therefore, the concept of discrete taxonomic sections based on the shape of 1′ plate and 2a plate is upheld by molecular phylogeny. Furthermore, the section Oceanica is indicated as having an early divergence from other groups within the genus. The sections Avellana and Excentrica and a clade combining the sections Divergentia/Protoperidinium derived from Conica‐type dinoflagellates independently. Analysis of the LSU rDNA data resulted in the same phylogeny as that obtained using SSU rDNA data and, with increased taxon sampling, including members of new sections, a clearer idea of the evolution of morphological features within the genus Protoperidinium was obtained. Intraspecific variation was found in Protoperidinium conicum (Gran) Balech, Protoperidinium excentricum (Paulsen) Balech and Protoperidinium pellucidum Bergh based on SSU rDNA data and also in Protoperidinium claudicans (Paulsen) Balech, P. conicum and Protoperidinium denticulatum (Gran et Braarud) Balech based on LSU rDNA sequences. The common occurrence of base pair substitutions in P. conicum is indicative of the presence of cryptic species.     

Molecular phylogenetic study of the heterotrophic dinoflagellate genus Protoperidinium (Dinophyceae) inferred from small subunit rRNA gene sequences

In the present study, we investigated the intrageneric and intergeneric phylogenetic relationships of the heterotrophic marine dinoflagellate genus Protoperidinium. Using single‐cell polymerase chain reaction methods, we determined small subunit ribosomal RNA gene sequences for 10 Protoperidinium species belonging to four sections and two subgenera. Phylogenetic trees were constructed using maximum parsimony, neighbor joining and maximum likelihood methods. We found intraspecific variability of small subunit rDNA sequences in Protoperidinium conicum (Gran) Balech, Protoperidinium crassipes (Kofoid) Balech and Protoperidinium denticulatum (Gran et Braarud) Balech, but not in other species. The small subunit rDNA phylogeny revealed that the genus is monophyletic, but its phylogenetic position within the Dinophyceae could not be determined because of ambiguous basal topologies. Within the genus Protoperidinium, species of the subgenus Archaeperidinium with two anterior intercalary plates (2a) were shown to be monophyletic, but species of the subgenus Protoperidinium with three anterior intercalary plates (3a) were resolved as paraphyletic. The sections Avellana, Divergentia and Protoperidinium were shown to be monophyletic, while the section Conica was paraphyletic. Based on the trees obtained in the present study, most of the traditionally defined sections are supported by molecular phylogeny. It was also indicated that the section Avellana evolved from one of the Conica‐type dinoflagellates.     

MOLECULAR PHYLOGENY OF THE HETEROTROPHIC DINOFLAGELLATES,PROTOPERIDINIUM, DIPLOPSALIS AND PREPERIDINIUM (DINOPHYCEAE), INFERRED FROM LARGE SUBUNIT rDNA1

The genera Protoperidinium Bergh, Diplopsalis Bergh, and Preperidinium Mangin, comprised of species of marine, thecate, heterotrophic dinoflagellates in the family Protoperidinaceae Balech, have had a confused taxonomic history. To elucidate the validity of morphological groupings within the Protoperidinium and diplopsalids, and to determine the evolutionary relationships between these and other dinoflagellates, we undertook a study of molecular phylogeny using the D1–D3 domains of the large subunit (LSU) of the rDNA. Based on morphology, the 10 Protoperidinium species examined belonged to three subgenera and five morphological sections. Two diplopsalid species were also included. Single‐cell PCR, cloning, and sequencing revealed a high degree of intraindividual sequence variability in the LSU rDNA. The genus Protoperidinium appeared to be recently divergent in all phylogenetic analyses. In maximum parsimony and neighbor joining analyses, Protoperidinium formed a monophyletic group, evolving from diplopsalid dinoflagellates. In maximum likelihood and Bayesian analyses, however, Protoperidinium was polyphyletic, as the lenticular, diplopsalid heterotroph, Diplopsalis lenticula Bergh, was inserted within the Protoperidinium clade as basal to Protoperidinium excentricum (Paulsen) Balech, and Preperidinium meunieri (Pavillard) Elbrächter fell within a separate clade as a sister to the Oceanica and Protoperidinium steidingerae Balech. In all analyses, the Protoperidinium were divided into two major clades, with members in the Oceanica group and subgenus Testeria in one clade, and the Excentrica, Conica, Pellucida, Pyriforme and Divergens sections in the other clade. The LSU rDNA molecular phylogeny supported the historical morphologically determined sections, but not a simple morphology based model of evolution based on thecal plate shape.     

FLUORESCENCE IN SITU HYBRIDIZATION USING rRNA‐TARGETED PROBES FOR SIMPLE AND RAPID IDENTIFICATION OF THE TOXIC DINOFLAGELLATES ALEXANDRIUM TAMARENSE AND ALEXANDRIUM CATENELLA1

The toxic marine dinoflagellates Alexandrium tamarense (Lebor) Balech and A. catenella (Whedon and Kofoid) Taylor have been mainly responsible for paralytic shellfish poisoning in Japan. Rapid and precise identification of these algae has been difficult because this genus contains many morphologically similar toxic and nontoxic species. Here, we report a rapid, precise, and quantitative identification method using three fluorescent, rRNA‐targeted, oligonucleotide probes for A. tamarense (Atm1), A. catenella (Act1), and the nontoxic A. affine (Inoue et Fukuyo; Aaf1). Each probe was species specific when applied using fluorescence in situ hybridization (FISH). None of the probes reacted with three other Alexandrium spp., A. lusitanicum Balech, A. ostenfeldii (Paulsen) Balech & Tangen, and A. insuetum Balech, or with eight other microalgae, including Gymnodinium mikimotoi Miyake et Kominami ex Oda and Heterosigma akashiwo (Hada) Hara et Chihara, suggesting that the species specificity of each probe was very high. Cells labeled with fluorescein 5‐isothiocyanate–conjugated probes showed strong green fluorescence throughout the whole cell except for the nucleus. FISH could be completed within 1 h and largely eliminated the need for identifying species based on key morphological criteria. More than 80% of targeted cells of both species could be identified by microscopy and quantified during growth up to the early stationary phase; more than 70% of cells could be detected in the late stationary phase. The established FISH protocol was found to be a specific, rapid, precise, and quantitative method that might prove to be a useful tool to distinguish and quantify Alexandrium cells collected from Japanese coastal waters.     

Dinoflagellate cyst distribution in marine surface sediments off West Africa (17–6°N) in relation to sea-surface conditions, freshwater input and seasonal coastal upwelling

An organic-walled dinoflagellate cyst analysis was carried out on 53 surface sediment samples from West Africa (17–6°N) to obtain insight in the relationship between their spatial distribution and hydrological conditions in the upper water column as well as marine productivity in the study area.Multivariate analysis of the dinoflagellate cyst relative abundances and environmental parameters of the water column shows that sea-surface temperature, salinity, marine productivity and bottom water oxygen are the factors that relate significantly to the distribution patterns of individual species in the region.The composition of cyst assemblages and dinoflagellate cyst concentrations allows the identification of four hydrographic regimes; 1) the northern regime between 17 and 14°N characterized by high productivity associated with seasonal coastal upwelling, 2) the southern regime between 12 and 6°N associated with high-nutrient waters influenced by river discharge 3) the intermediate regime between 14 and 12°N influenced mainly by seasonal coastal upwelling additionally associated with fluvial input of terrestrial nutrients and 4) the offshore regime characterized by low chlorophyll-a concentrations in upper waters and high bottom water oxygen concentrations.Our data show that cysts of Polykrikos kofoidii, Selenopemphix quanta, Dubridinium spp., Echinidinium species, cysts of Protoperidinium monospinum and Spiniferites pachydermus are the best proxies to reconstruct the boundary between the NE trade winds and the monsoon winds in the subtropical eastern Atlantic Ocean. The association of Bitectatodinium spongium, Lejeunecysta oliva, Quinquecuspis concreta, Selenopemphix nephroides, Trinovantedinium applanatum can be used to reconstruct past river outflow variations within this region.     

ULTRASTRUCTURE OF THE FEEDING APPARATUS AND MYONEMAL SYSTEM OF THE HETEROTROPHIC DINOFLAGELLATE PROTOPERIDINIUM SPINULOSUM1

The feeding veil or pallium of the thecate heterotrophic dinoflagellate Protoperidinium spinulosum Schiller is a highly vesiculate membranous sac containing several arched, sometimes bifurcated microtubular ribbons. It originates from an internal microtubular basket, passes through a sphincter-like osmiophilic ring located inside the posterior flagellar pore, and emerges from the cell at that pore. The osmiophilic ring is part of an interconnected myonemal system (composed of two striated collars and several striated connectives) that is anchored to the pore plate and to two inward protrusions composed of minute sulcal plates. A related species, Protoperidinium punctulatum (Paulsen) Balech, also possesses a microtubular basket/osmiophilic ring complex. Elongate electron-dense bodies within the basket resemble digestive secretory granules found in other protists. Granular, electron-lucent microbodies clustered at the anterior end of the basket may also have a role in prey digestion. Dense membranous whorls observed within a P. spinulosum cell presented as it was preparing to initiate feeding indicate a condensed storage site for pallium membranes. A narrow microtubule-strengthened pseudopodal appendage found in two non-feeding cells constitutes the tow filament that serves as the initial linkage between the dinoflagellate and its food. The structures that constitute the pallium and pallium precursors, described here for the first time, are unlike those of other known protists, although some similarities with the dinoflagellate peduncle are evident. The existence of this unique system of organelles may have important ramifications in the search for evolutionary relationships among protists.     

Preservation of organic-walled dinoflagellate cysts in different oxygen regimes: a 10,000 year natural experiment

The occurrence of organic-walled dinoflagellate cysts in (fossil) sediments depends on several factors, including as the ecological preferences of the cyst-forming dinoflagellates, cyst production, transport and preservation. Although laboratory experiments have shown that several cyst species are sensitive to chemical treatment, no information about the selective preservation of dinoflagellate cyst species in natural environments has previously been presented. Here, we present data on the effects of oxygen availability in bottom sediments on a cyst assemblage from the ungraded Madeira Abyssal Plain f-turbidite of which only the upper layer has been oxidized. Based on differences in species composition between the oxidized and underlying, unoxidized layers of this turbidite, the influence of oxygen availability on the preservation of individual species has been estimated. Cyst species have been classified in ascending order of resistance to oxygen availability in sediments as: (1) highly sensitive (cysts formed by Protoperidinium species), (2) moderately sensitive (e.g. Spiniferites species), (3) moderately resistant (e.g. Impagidinium paradoxum and Nematosphaeropsis labyrinthus) and (4) resistant (e.g. Impagidinium aculeatum).     

WIDESPREAD PHAGOCYTOSIS OF CILIATES AND OTHER PROTISTS BY MARINE MIXOTROPHIC AND HETEROTROPHIC THECATE DINOFLAGELLATES1

An electron microscopic examination of large amorphous inclusions located in a variety of photosynthetic thecate dinoflagellates (Alexandrium ostenfeldii (Paulsen) Balech et Tangen, Gonyaulax diegensis Kofoid, Scrippsiella sp., Ceratium longipes (Bailey) Gran, and Prorocentrum micans Ehrenberg) and a nonphotosynthetic thecate species (Amylax sp.) revealed each inclusion to be a food vacuole, the majority of which were ingested ciliate prey. Recognizable features of these ciliates included linear arrays of basal bodies and cilia consistent with oligotrich polykinetid structure, characteristic macronuclei, chloroplasts (evidently kleptoplastids), cup-shaped starch plates, and cylindrical extrusomes. Three species contained (apparent) nonciliate prey: Scrippsiella sp., whose food vacuoles consistently contained unusual and complex extrusome-like cylindrical bodies having a distinctive six-lobed, multilayered structure; P. micans, which contained an unidentified encysted cell; and a single A. ostenfeldii cell, containing a Dinophysis sp. dinoflagellate cell. Several food vacuoles of ciliate origin had a red hue. This, together with the resemblance of A. ostenfeldii cells to planozygotes, suggests that similar structures previously identified as accumulation bodies may in fact be food vacuoles and that feeding may in some cases be associated with sexual processes.     

DINOFLAGELLATE HOST‐PARASITE STEROL PROFILES DICTATE KARLOTOXIN SENSITIVITY1

We examined the sterol profile of Karlodinium veneficum (D. Ballant.) J. Larsen, Akashiwo sanguinea (Hiraska) Ge. Hansen et Moestrup, Alexandrium tamarense (M. Lebour) Balech, Alexandrium affine (H. Inoue et Fukuyo) Balech, Gonyaulax polygramma F. Stein, and Gymnodinium instriatum (Freud. et J. J. Lee) Coats, along with their Amoebophyra parasites. There were no consistent sterol profiles that characterized the genus Amoebophyra. Instead, in five out of six comparisons, the host and parasite sterol profiles where highly correlated. The one exception, Amoebophyra sp. ex Alex. tamarense, was least like its host in sterol profile and also possessed the widest host range for infection. There was little correlation between host and parasite in fatty acid profiles, with the parasite being deficient in fatty acids characteristic of the plastid [e.g., 18:5(n‐3) associated with galactolipids of the thylakoids, as previously published by Adolf et al. (2007)]. Those hosts and parasites with sterol profiles dominated by desmethyl sterols were most sensitive to karlotoxin toxicity. In the host‐parasite pairs most sensitive to karlotoxin addition, recovery of the intact karlotoxin molecule was poorest. Given the sensitivity to karlotoxin, some species of Amoebophyra may avoid infection of K. veneficum.     

GROWTH AND PHOTOPROTECTION IN THREE DINOFLAGELLATES (INCLUDING TWO STRAINS OF ALEXANDRIUM TAMARENSE) AND ONE DIATOM EXPOSED TO FOUR WEEKS OF NATURAL AND ENHANCED ULTRAVIOLET‐B RADIATION1

Long‐term growth response to natural solar radiation with enhanced ultraviolet‐B (UVB) exposure was examined in two species of dinoflagellates [Alexandrium tamarense (M. Lebour) Balech, At, and Heterocapsa triquetra (Ehrenb.) F. Stein, Ht], including two strains of A. tamarense, one from Spain and another from UK, and one diatom species (Thalassiosira pseudonana Hasle et Heimdal). We examined whether variable photoprotection (mycosporine‐like amino acids [MAAs] and xanthophyll‐cycle pigments) affected photosynthetic performance, phytoplankton light absorption, and growth. Growth rate was significantly reduced under enhanced UVB for the UK strain of At and for Ht (both grew very little) as well as for the diatom (that maintained high growth rates), but there was no effect for the Spanish strain of At. MAA concentration was high in the dinoflagellates, but undetectable in the diatom, which instead used the xanthophyll cycle for photoprotection. The highest cell concentrations of MAAs and photoprotective pigments were observed in the UK strain of At, along with lowest growth rates and F_v/F_m, indicating high stress levels. In contrast, the Spanish strain showed progressive acclimation to the experimental conditions, with no significant difference in growth between treatments. Increase in total MAAs followed linearly the cumulative UVB of the preceding day, and both total and primary MAAs were maintained at higher constitutive levels in this strain. Acclimation to enhanced UVB in the diatom resulted in an increase in PSII activity and reduction in nonphotochemical quenching, indicating an increased resistance to photoinhibition after a few weeks. All four species showed increased phytoplankton light absorption under enhanced UVB. Large intrastrain differences suggest a need to consider more closely intraspecific variability in UV studies.     

CULTURE OF THE HETEROTROPHIC DINOFLAGELLATE PROTOPERIDINIUM CRASSIPES (DINOPHYCEAE) WITH NONCELLULAR FOOD ITEMS1

The genus Protoperidinium is an assemblage of heterotrophic dinoflagellates, several species of which have been successfully cultured in the past using various photosynthetic algae as a food source. We succeeded in culturing Protoperidinium crassipes (Kof.) Balech on three separate occasions for periods ranging from 2 to 21 months using rice flour as a food source. In these cultures, unusual small types of cells that were never observed to actively feed sometimes appeared. We confirmed that P. crassipes in culture exhibited bioluminescence.     

GROWTH INHIBITION AND TOXICITY OF THE DIATOM ALDEHYDE 2‐TRANS, 4‐TRANS‐DECADIENAL ON THALASSIOSIRA WEISSFLOGII (BACILLARIOPHYCEAE)1

A common aldehyde present in marine and freshwater diatoms, 2‐trans, 4‐trans‐decadienal (A3), is involved in the wound‐activated response of diatoms to copepod grazing. Upon breakage of the diatom cell membrane, aldehydes are enzymatically produced by the rapid conversion of precursors and strongly impact copepod reproduction by impairing egg production and hatching success, inducing teratogenic embryos modifications. In this study, A3 was assayed with the marine diatom Thalassiosira weissflogii (Grunow) Fryxell et Hasle. The aldehyde concentration necessary to reduce 50% growth rate (EC₅₀) was 0.29 mg·L^?1. Decadienal was found to inhibit T. weissflogii cell growth in a dose‐ and time‐dependent manner, with irreversible effects after 24 h of exposure. Decadienal induced a degenerative process, through modifications of cell membrane characteristics, interference with cell cycle progression, and with cell metabolic activity, leading to cell death. A preferential action of A3 on dividing cells was observed. Photosynthetic efficiency significantly decreased upon exposure to the aldehyde, paralleled by an increase in diatoxanthin, suggesting a protective role of this xanthophyll, usually involved in photoprotection. Dying cells exhibited the morphological and biochemical features that bear close resemblance to apoptosis of mammalian cells, including cell shrinkage, chromatin condensation, and degradation of nuclear DNA to nucleosomal size fragments. These data are the first direct evidence to show aldehydes are toxic to diatoms. We suggest a possible nontoxic role of such compounds as chemical signals of unfavorable conditions within the phytoplankton communities, which may be relevant for the population dynamics of diatoms during blooms.     

Identification of blood group A/A‐Leb/y and B/B‐Leb/y active glycotopes co‐expressed on the O‐glycans isolated from two distinct human ovarian cyst fluids

Although the individual human blood group A and B determinants are well defined, their co‐expression pattern on a particular glycan carrier in individuals of blood group AB status has not been delineated. To address this issue, complex O‐glycans were isolated from two distinct sources of human ovarian cyst glycoproteins (HOC 89 and Cyst 19) and profiled by advanced MS analyses, in conjunction with defining their binding characteristics against a panel of lectins and monoclonal antibodies. The major O‐glycans of HOC 89 were found to correspond to sialyl Tn, mono‐ and di‐sialyl T structures, whereas those of Cyst 19 were apparently more heterogeneous and extended to larger sizes. A minimal structure that carries both A and B determinants on the same molecule was identified, in which the A epitope is attached directly to the core GalNAc, whereas the B epitope is preferentially located on the six arms of a core 2 structure. Both arms can be further extended with internal fucosylation that appears to be restricted to those non‐sialylated chains already carrying the terminal ABH determinants, thus giving rise to rather prominent A/B‐Le^b/y glycotopes on larger O‐glycans.     

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.