Alkenone and alkenoic acid compositions of the membrane fractions of Emiliania huxleyi

The lipid classes and unsaturation ratios of long-chain alkenones (nC37-C39), related alkyl alkenoate compounds (nC37-C38) and alkenoic acids (nC14-C22) were determined in isolated membrane and organelle fractions of Emiliania huxleyi. The percentage distribution of these compounds was predominantly high in the endoplasmic reticulum (ER) and coccolith-producing compartment (CPC)-rich membrane fraction, although alkenones and alkenoates could be detected in all membrane fractions. In particular, the alkenones were mainly located in CPC, since their distribution was closely correlated with that of uronic acids which are markers of CPC. In contrast, the alkenoic acids seemed to be mainly located in chloroplast (thylakoid)-rich fractions. The alkenone unsaturation ratio and the ratio of alkenoates to alkenones were similar in all fractions, while the unsaturation ratio of alkenoic acids in the thylakoid-rich and plasma membrane (PM)/Golgi body-rich fractions was overwhelmingly higher than that in the ER/CPC-rich fractions. Thus, alkenoic acids seemed to be typical membrane-bound lipids, and could be closely related to photosynthesis and involved in regulating membrane fluidity and rigidity in E. huxleyi. It is presumed from these results that the alkenones and alkenoates were membrane-unbound lipids that might be associated with the function of CPC.     

Nitrate availability and calcite production in Emiliania huxleyi Lohmann

High-calcifying cells of Emiliania huxleyi were grown on a synthetic seawater medium and the effect of nitrate (NO^- ₃) concentration on growth, calcite accumulation, calcification rate and DIC (dissolved inorganic carbon) utilisation determined. The stoichiometry between NO^- ₃ utilisation and calcite production was 1:6·5 (mol/mol). Calcification and growth were tightly coupled: calcite production ceased when cultures entered the stationary phase due to NO^- ₃ depletion, but by adding a pulse of NO^- ₃ growth and calcification were restored. The initial C/N ratio in the medium was important in relation to calcification rate. At 20 µM NO^- ₃ the total DIC (2 mM) was rapidly depleted, the calcification rate subsequently declining, whereas at 5 and 10 µM NO^- ₃ rates of calcification were constant at 20 g carbon cell^-1 × 10¹⁴·h^-1 throughout culture growth, excess DIC being present relative to the available NO^- ₃. Calcite production per unit NO^- ₃ was similar for isolates of E. huxleyi from neritic, oligotrophic and nitrate-rich waters. In laboratory cultures, where the photon flux density is optimised for growth, the initial NO^- ₃ concentration is a reliable indicator of final calcite yield.     

Temperature-Induced Viral Resistance in Emiliania huxleyi (Prymnesiophyceae)

Annual Emiliania huxleyi blooms (along with other coccolithophorid species) play important roles in the global carbon and sulfur cycles. E. huxleyi blooms are routinely terminated by large, host-specific dsDNA viruses, (Emiliania huxleyi Viruses; EhVs), making these host-virus interactions a driving force behind their potential impact on global biogeochemical cycles. Given projected increases in sea surface temperature due to climate change, it is imperative to understand the effects of temperature on E. huxleyi’s susceptibility to viral infection and its production of climatically active dimethylated sulfur species (DSS). Here we demonstrate that a 3°C increase in temperature induces EhV-resistant phenotypes in three E. huxleyi strains and that successful virus infection impacts DSS pool sizes. We also examined cellular polar lipids, given their documented roles in regulating host-virus interactions in this system, and propose that alterations to membrane-bound surface receptors are responsible for the observed temperature-induced resistance. Our findings have potential implications for global biogeochemical cycles in a warming climate and for deciphering the particular mechanism(s) by which some E. huxleyi strains exhibit viral resistance.     

Intragenomic Spread of Plastid-Targeting Presequences in the Coccolithophore Emiliania huxleyi

Nucleus-encoded plastid-targeted proteins of photosynthetic organisms are generally equipped with an N-terminal presequence required for crossing the plastid membranes. The acquisition of these presequences played a fundamental role in the establishment of plastids. Here, we report a unique case of two non-homologous proteins possessing completely identical presequences consisting of a bipartite plastid-targeting signal in the coccolithophore Emiliania huxleyi. We further show that this presequence is highly conserved in five additional proteins that did not originally function in plastids, representing de novo plastid acquisitions. These are among the most recent cases of presequence spreading from gene to gene and shed light on important evolutionary processes that have been usually erased by the ancient history of plastid evolution. We propose a mechanism of acquisition involving genomic duplications and gene replacement through non-homologous recombination that may have played a more general role for equipping proteins with targeting information.     

A novel eukaryotic selenoprotein in the haptophyte alga Emiliania huxleyi

The diversity of selenoproteins raises the question of why many life forms require selenium. Especially in photosynthetic organisms, the biochemical basis for the requirement for selenium is unclear because there is little information on selenoproteins. We found six selenium-containing proteins in a haptophyte alga, Emiliania huxleyi, which requires selenium for growth. The 27-kDa protein EhSEP2 was isolated, and its cDNA was cloned. The deduced amino acid sequence revealed that EhSEP2 is homologous to protein disulfide isomerase (PDI) and contains a highly conserved thioredoxin domain. The nucleotide sequence contains an in-frame TGA codon encoding selenocysteine at the position corresponding to the cysteine residue in the reaction center of known PDIs. However, no typical selenocysteine insertion sequence was found in the EhSEP2 cDNA. The EhSEP2 mRNA level was related to the abundance of selenium. E. huxleyi possesses a novel PDI-like selenoprotein and may have a novel type of selenocysteine insertion machinery.     

Reduced calcification decreases photoprotective capability in the coccolithophorid Emiliania huxleyi

Intracellular calcification of coccolithophores generates CO? and consumes additional energy for acquisition of calcium and bicarbonate ions; therefore, it may correlate with photoprotective processes by influencing the energetics. To address this hypothesis, a calcifying Emiliania huxleyi strain (CS-369) was grown semi-continuously at reduced (0.1 mM, LCa) and ambient Ca2? concentrations (10 mM, HCa) for 150 d (>200 generations). The HCa-grown cells had higher photosynthetic and calcification rates and higher contents of Chl a and carotenoids compared with the naked (bearing no coccoliths) LCa-grown cells. When exposed to stressfull levels of photosynthetically active radiation (PAR), LCa-grown cells displayed lower photochemical yield and less efficient non-photochemical quenching (NPQ). When the LCa- or HCa-grown cells were inversely shifted to their counterpart medium, LCa to HCa transfer increased photosynthetic carbon fixation (P), calcification rate (C), the C/P ratio, NPQ and pigment contents, whereas those shifted from HCa to LCa exhibited the opposite effects. Increased NPQ, carotenoids and quantum yield were clearly linked with increased or sustained calcification in E. huxleyi. The calcification must have played a role in dissipating excessive energy or as an additional drainage of electrons absorbed by the photosynthetic antennae. This phenomenon was further supported by testing two non-calcifying strains, which showed insignificant changes in photosynthetic carbon fixation and NPQ when transferred to LCa conditions.     

Characterization of ectoenzyme activity and phosphate-regulated proteins in the coccolithophorid Emiliania huxleyi

Three phosphate-regulated proteins in the coccolithophorid Emilianiahuxleyi were detected by the biotinylation of cell-surface proteins.Two of these phosphate-regulated proteins have reduced denaturedmolecular weights near 110 000 Da (118 078 and 110 541, respectively),while the third, and most abundant, is 69 087 Da. Inductionof the three proteins and the common marker of phosphate stress,alkaline phosphatase activity, occur in the presence of <0.25µM inorganic phosphate in batch culture. Phosphate-regulatedproteins and enzyme activity differed among E. huxleyi strains.Alkaline phosphatase is an enzyme commonly induced by phytoplanktonin response to phosphate stress in order for cells to scavengeinorganic phosphate from organic sources. In E. huxleyi, thisenzyme activity and the phosphate-regulated proteins are rapidlylost when phosphate is added back to phosphate-stressed cultures.This contrasts with the slower loss of alkaline phosphataseactivity in the dinoflagellate Prorocentrum minimum. The presenceof the three phosphate-regulated proteins and enzyme activityappear to differ somewhat among E. huxleyi strains. Based onthese differences between strains, kinetic data, growth experimentsand enzyme activities, the 69 087 Da protein may be a phosphatasewith a high specificity for 5'-nucleotides.     

Lipid membrane with low proton permeability

This work reports the production of a liposomal formulation, having a lipidic membrane with known chemical composition and a low proton permeability, as confirmed by physicochemical characterization of the maintenance of a transmembranic pH gradient. These liposomes consist of DSPC, DSPE-PEG, DSPG and cholesterol, with low internal pH. To verify the low proton permeability of these liposomal bilayers, a study of proton migration according to the fluorescence quenching of 9-aminoacridine (9AA), as well as CPT-11 encapsulation, were used to monitor the acidification of the intravesicular space. Both experiments showed that this liposomal formulation is able to maintain a transmembranic proton gradient.     

Polymorphic microsatellite loci in global populations of the marine coccolithophorid Emiliania huxleyi

The marine coccolithophorid Emiliania huxleyi is an important component of the marine carbon cycle because bloom development results in the export of calcium carbonate from the ocean surface to the abyss. Laboratory and field studies demonstrate significant biogeographical, ecological, physiological and morphological plasticity in E. huxleyi and suggest high underlying genetic variability. Here we describe seven polymorphic microsatellite loci from the E. huxleyi genome and their degree of polymorphism in clonal isolates of different geographical origin. Our results indicate a high degree of genetic diversity within E. huxleyi.     

Bloom of Emiliania huxleyi (Prymnesiophyceae) in the western South Atlantic Ocean

A monospecific bloom of the coccolithophorid Emiliania huxleyi(Lohmann) Hay & Mohler (Prymnesiophyceae) was detected offRio de La Plata at 36°S and 54°W in November 1989. Thecell densities observed were up to 6x10⁵ cells I^–1. Thisis the first record of a bloom of E.huxleyi in the area.     

Substrate supply for calcite precipitation in Emiliania huxleyi: assessment of different model approaches

Over the last four decades, different hypotheses of Ca²⁺ and dissolved inorganic carbon transport to the intracellular site of calcite precipitation have been put forth for Emiliania huxleyi (Lohmann) Hay & Mohler. The objective of this study was to assess these hypotheses by means of mathematical models. It is shown that a vesicle‐based Ca²⁺ transport would require very high intravesicular Ca²⁺ concentrations, high vesicle fusion frequencies as well as a fast membrane recycling inside the cell. Furthermore, a kinetic model for the calcification compartment is presented that describes the internal chemical environment in terms of carbonate chemistry including calcite precipitation. Substrates for calcite precipitation are transported with different stoichiometries across the compartment membrane. As a result, the carbonate chemistry inside the compartment changes and hence influences the calcification rate. Moreover, the effect of carbonic anhydrase (CA) activity within the compartment is analyzed. One very promising model version is based on a Ca²⁺/H⁺ antiport, CO₂ diffusion, and a CA inside the calcification compartment. Another promising model version is based on an import of Ca²⁺ and HCO₃^? and an export of H⁺.     

The 24 hour recovery kinetics from n starvation in Phaeodactylum tricornutum and Emiliania huxleyi

The response of N (nitrate) starved cells of the diatom Phaeodactylum tricornutum and the coccolithophore Emiliania huxleyi to a pulse of new N were measured to investigate rapid cellular and photosynthetic recovery kinetics. The changes of multiple parameters were followed over 24 h. In P. tricornutum, the recovery of F_v/F_m (the maximum quantum yield of PS II) and σ_PSII (the functional absorption cross‐section for PSII) started within the first hour, much earlier than other parameters. Cellular pigments did not recover during the 24 h but the chlorophyll (chl) a/carotenoid ratios increased to levels measured in the controls. Cell division was independent of the recovery of chl a. In E. huxleyi, the recovery of F_v/F_m and σ_PSII started after an hour, synchronous with the increase in cellular organic N and chl a with pigments fully recovered within 14 h. P. tricornutum prioritized the recovery of its photosynthetic functions and cell divisions while E. huxleyi did not follow this pattern. We hypothesize that the different recovery strategies between the two species allow P. tricornutum to be more competitive when N pulses are introduced into N‐limited water while E. huxleyi is adapted to N scarce waters where such pulses are infrequent. These findings are consistent with successional patterns observed in coastal environments. This is one of only a few studies exploring recovery kinetics of cellular functions and photosynthesis after nitrogen stress in phytoplankton. Our results can be used to enhance ecological models linking phytoplankton traits to species diversity and community structure.     

Characterization of the selenite uptake mechanism in the coccolithophore Emiliania huxleyi (Haptophyta)

The marine coccolithophore Emiliania huxleyi (Haptophyta) requires selenium as an essential element for growth, and the active species absorbed is selenite, not selenate. This study characterized the selenite uptake mechanism using ??Se as a tracer. Kinetic analysis of selenite uptake showed the involvement of both active and passive transport processes. The active transport was suppressed by 0.5 mM vanadate, a membrane-permeable inhibitor of H?-ATPase, at pH 8.3. When the pH was lowered from 8.3 to 5.3, the selenite uptake activity greatly increased, even in the presence of vanadate, suggesting that the H? concentration gradient may be a motive force for selenite transport. [??Se]Selenite uptake at selenite-limiting concentrations was hardly affected by selenate, sulfate and sulfite, even at 100 μM. In contrast, 3 μM orthophosphate increased the K(m) 5-fold. These data showed that HSeO??, a dominant selenite species at acidic pH, is the active species for transport through the plasma membrane and transport is driven by ΔpH energized by H?-ATPase. Kinetic analysis showed that the selenite uptake activity was competitively inhibited by orthophosphate. Furthermore, the active selenite transport mechanism was shown to be induced de novo under Se-deficient conditions and induction was suppressed by the addition of either sufficient selenite or cycloheximide, an inhibitor of de novo protein synthesis. These results indicate that E. huxleyi cells developed an active selenite uptake mechanism to overcome the disadvantages of Se limitation in ecosystems, maintaining selenium metabolism and selenoproteins for high viability.     

CO2‐concentrating mechanisms in three southern hemisphere strains of Emiliania huxleyi

Rising global CO₂ is changing the carbonate chemistry of seawater, which is expected to influence the way phytoplankton acquire inorganic carbon. All phytoplankton rely on ribulose‐bisphosphate carboxylase oxygenase (RUBISCO) for assimilation of inorganic carbon in photosynthesis, but this enzyme is inefficient at present day CO₂ levels. Many algae have developed a range of energy demanding mechanisms, referred to as carbon concentrating mechanisms (CCMs), which increase the efficiency of carbon acquisition. We investigated CCM activity in three southern hemisphere strains of the coccolithophorid Emiliania huxleyi W. W. Hay & H. P. Mohler. Both calcifying and non‐calcifying strains showed strong CCM activity, with HCO₃^? as a preferred source of photosynthetic carbon in the non‐calcifying strain, but a higher preference for CO₂ in the calcifying strains. All three strains were characterized by the presence of pyrenoids, external carbonic anhydrase (CA) and high affinity for CO₂ in photosynthesis, indicative of active CCMs. We postulate that under higher CO₂ levels cocco‐lithophorids will be able to down‐regulate their CCMs, and re‐direct some of the metabolic energy to processes such as calcification. Due to the expected rise in CO₂ levels, photosynthesis in calcifying strains is expected to benefit most, due to their use of CO₂ for carbon uptake. The non‐calcifying strain, on the other hand, will experience only a 10% increase in HCO₃^?, thus making it less responsive to changes in carbonate chemistry of water.     

Effects of HCO-3 on Surface Calcification and CO2 Fixation in Marine Emiliania huxleyi

Emiliania huxleyi is a ubiquitous species with the largest biomass in marine planktonics. When cells of E. huxleyi were grown in ESM with additional 20 mmol/L HC03- , coccolith scales were formed on cell surface and the weight ratio of calcium carbonate fixed in coecoliths to organic substance in cells was about 2.47: 1. It was only about 0.05: 1 in cells grown in ESM without HCO3- addition, where no coccoliths were observed under scanning electron microscope, and the content of lipid reached 18.1% of dry. cell weight. It was demonstrated that the HCO3- concentration was the key factor to control the calcification on cell surface. Therefore, in addition to the pathway of photosynthesis for CO2 fixation, calcification on cell surface forming coccoliths is an alternative pathway for fixing dissolved inorganic carbon in E. huxleyi. Moreover, being rich in lipids, E. huxleyi cells produced high content of hydrocarbons including extractable organic matter, saturates and aromatics under pyrolysis at 300℃. Among those, the yield of saturates from E. huxleyi reached as high as 2.8%, 6-15 times that from other algae. All these suggest that E. huxleyi is a good experimental system for studies on the optimization of environment through carbon cycle and renewable energy in algal biomass.