Suppressive Subtractive Hybridization of and Differences in Gene Expression Content of Calcifying and Noncalcifying Cultures of Emiliania huxleyi Strain 1516

The marine coccolithophorid Emiliania huxleyi is a cosmopolitan alga intensely studied in relation to global carbon cycling, biogeochemistry, marine ecology, and biomineralization processes. The biomineralization capabilities of coccolithophorids have attracted the attention of scientists interested in exploiting this ability for the development of materials science and biomedical and biotechnological applications. Although it has been well documented that biomineralization in E. huxleyi is promoted by growth under phosphate-limited conditions, the genes and proteins that govern the processes of calcification and coccolithogenesis remain unknown. Suppressive subtractive hybridization (SSH) libraries were constructed from cultures grown in phosphate-limited and phosphate-replete media as tester and driver populations for reciprocal SSH procedures. Positive clones from each of the two libraries were randomly selected, and dot blotting was performed for the analysis of expression patterns. A total of 513 clones from the phosphate-replete library and 423 clones from the phosphate-limited library were sequenced, assembled, and compared to sequences in GenBank using BLASTX. Of the 103 differentially expressed gene fragments from the phosphate-replete library, 34% showed significant homology to other known proteins, while only 23% of the 65 differentially expressed gene fragments from the phosphate-limited library showed homology to other proteins. To further assess mRNA expression, real-time RT-PCR analysis was employed and expression profiles were generated over a 14-day time course for three clones from the phosphate-replete library and five clones from the phosphate-limited library. The fragments isolated provide the basis for future cloning of full-length genes and functional analysis.     

Transcriptome analysis of functional differentiation between haploid and diploid cells of Emiliania huxleyi, a globally significant photosynthetic calcifying cell

Background  

Eukaryotes are classified as either haplontic, diplontic, or haplo-diplontic, depending on which ploidy levels undergo mitotic cell division in the life cycle. Emiliania huxleyi is one of the most abundant phytoplankton species in the ocean, playing an important role in global carbon fluxes, and represents haptophytes, an enigmatic group of unicellular organisms that diverged early in eukaryotic evolution. This species is haplo-diplontic. Little is known about the haploid cells, but they have been hypothesized to allow persistence of the species between the yearly blooms of diploid cells. We sequenced over 38,000 expressed sequence tags from haploid and diploid E. huxleyi normalized cDNA libraries to identify genes involved in important processes specific to each life phase (2N calcification or 1N motility), and to better understand the haploid phase of this prominent haplo-diplontic organism.     

Metolachlor-Mediated Selection of a Microalgal Strain Producing Novel Polyunsaturated Fatty Acids

Long-chain (≥ C₂₀) polyunsaturated fatty acids, such as docosahexaenoic acid and eicosapentaenoic acid, are nutritionally important and provide protection against cardiovascular disease, stroke, and cancer. Structural variants of these compounds may have the potential to be used as pharmaceuticals. Marine microalgae are the key producers of long-chain polyunsaturated fatty acids in the global food web. Assuming vast biological and biochemical diversity, we devised a screen to identify microalgae that produce novel fatty acids. The herbicide metolachlor, an inhibitor of long-chain fatty acid biosynthesis, was used in microcosms containing field-collected microalgae to identify naturally resistant strains. We show that one diatom, Melosira cf. moniliformis, is naturally resistant to concentrations of metolachlor, which were cytostatic or lethal to all the other microalgae. Gas chromatography and gas chromatography-mass spectrometry revealed three fatty acids that have not previously been described-18:4 (Δ5,8,11,14), 18:4 (Δ5,9,12,15), and 18:5 (Δ5,8,11,14,17). We propose that this type of screen may be generally applicable to the search of novel compounds produced by marine microorganisms.     

Gene expression changes in the coccolithophore Emiliania huxleyi after 500 generations of selection to ocean acidification

Coccolithophores are unicellular marine algae that produce biogenic calcite scales and substantially contribute to marine primary production and carbon export to the deep ocean. Ongoing ocean acidification particularly impairs calcifying organisms, mostly resulting in decreased growth and calcification. Recent studies revealed that the immediate physiological response in the coccolithophore Emiliania huxleyi to ocean acidification may be partially compensated by evolutionary adaptation, yet the underlying molecular mechanisms are currently unknown. Here, we report on the expression levels of 10 candidate genes putatively relevant to pH regulation, carbon transport, calcification and photosynthesis in E. huxleyi populations short-term exposed to ocean acidification conditions after acclimation (physiological response) and after 500 generations of high CO₂ adaptation (adaptive response). The physiological response revealed downregulation of candidate genes, well reflecting the concomitant decrease of growth and calcification. In the adaptive response, putative pH regulation and carbon transport genes were up-regulated, matching partial restoration of growth and calcification in high CO₂-adapted populations. Adaptation to ocean acidification in E. huxleyi likely involved improved cellular pH regulation, presumably indirectly affecting calcification. Adaptive evolution may thus have the potential to partially restore cellular pH regulatory capacity and thereby mitigate adverse effects of ocean acidification.     

The Complete Plastid Genome Sequence of the Haptophyte Emiliania huxleyi: a Comparison to Other Plastid Genomes

The complete nucleotide sequence of the plastid genome of thehaptophyte Emiliania huxleyi has been determined. E. huxleyiis the most abundant coccolithophorid and has a key role inthe carbon cycle. It is also implicated in the production ofdimethylsulphide (DMS), which is involved in cloud nucleationand may affect the global climate. Here, we report the plastidgenome sequence of this ecologically and economically importantspecies and compare its gene content and arrangement to otherknown plastid genomes. The genome is circular and consists of105,309 bp with an inverted repeat of 4,841 bp. In terms ofboth genome size and gene content E. huxleyi cpDNA is substantiallysmaller than any other from the red plastid lineage. The geneticinformation is densely packed, with 86.8% of the genome specifying110 identified protein-coding genes, 9 open reading frames,28 different tRNAs, and 3 rRNAs. A detailed comparison to otherplastid genomes, based on gene content, gene function, and genecluster analysis is discussed. These analyses suggest a closerelationship of the E. huxleyi cpDNA to the chlorophyll c-containingplastids from heterokonts and cryptophytes, and they supportthe origin of the chromophyte plastids from the red algal lineage.     

Evidence for the Involvement of Mitochondrial Respiration in Calcification in a Marine Coccolithophorid, Emiliania huxleyi

In the marine coccolithophorid, Emiliania huxleyi, CaCO₃ productionunder illumination showed a lag phase for about 3 h and thenincreased greatly. During the lag phase the rate of CaCO₃ productionin the light was similar to that in the dark. The productionof CaCO₃ in the dark was inhibited by the addition of 170 µMCCCP, 1 mM KCN and 1 mM SHAM. These results suggest that a littleproduction of CaCO₃ is supported by energy from mitochondrialrespiration, but that large amount of CaCO₃ production requiresphotosynthesis. ¹Present address: SDS Biotech K.K., Tsukuba Technology Center,Midorigahara 2-1, Tsukuba, Ibaraki, 300-26 Japan     

Application of the major capsid protein as a marker of the phylogenetic diversity of Emiliania huxleyi viruses

Studies of the Phycodnaviridae have traditionally relied on the DNA polymerase (pol) gene as a biomarker. However, recent investigations have suggested that the major capsid protein (MCP) gene may be a reliable phylogenetic biomarker. We used MCP gene amplicons gathered across the North Atlantic to assess the diversity of Emiliania huxleyi-infecting Phycodnaviridae. Nucleotide sequences were examined across >6000 km of open ocean, with comparisons between concentrates of the virus-size fraction of seawater and of lysates generated by exposing host strains to these same virus concentrates. Analyses revealed that many sequences were only sampled once, while several were over-represented. Analyses also revealed nucleotide sequences distinct from previous coastal isolates. Examination of lysed cultures revealed a new richness in phylogeny, as MCP sequences previously unrepresented within the existing collection of E. huxleyi viruses (EhV) were associated with viruses lysing cultures. Sequences were compared with previously described EhV MCP sequences from the North Sea and a Norwegian Fjord, as well as from the Gulf of Maine. Principal component analysis indicates that location-specific distinctions exist despite the presence of sequences common across these environments. Overall, this investigation provides new sequence data and an assessment on the use of the MCP gene.     

Elemental stoichiometry of the key calcifying marine phytoplankton Emiliania huxleyi under ocean climate change: A meta-analysis

The elemental composition of marine microorganisms (their C:N:P ratio, or stoichiometry) is central to understanding the biotic and biogeochemical processes underlying key marine ecosystem functions. Phytoplankton C:N:P is species specific and flexible to changing environmental conditions. However, bulk or fixed phytoplankton stoichiometry is usually assumed in biogeochemical and ecological models because more realistic, environmentally responsive C:N:P ratios have yet to be defined for key functional groups. Here, a comprehensive meta-analysis of experimental laboratory data reveals the variable C:N:P stoichiometry of Emiliania huxleyi, a globally significant calcifying phytoplankton species. Mean C:N:P of E. huxleyi is 124C:16N:1P under control conditions (i.e. growth not limited by one or more environmental stressors) and shows a range of responses to changes in nutrient and light availability, temperature and pCO₂. Macronutrient limitation caused strong shifts in stoichiometry, increasing N:P and C:P under P deficiency (by 305% and 493% respectively) and doubling C:N under N deficiency. Responses to light, temperature and pCO₂ were mixed but typically shifted cellular elemental content and C:N:P stoichiometry by ca. 30% or less. Besides these independent effects, the interactive effects of multiple environmental changes on E. huxleyi stoichiometry under future ocean conditions could be additive, synergistic or antagonistic. To synthesise our meta-analysis results, we explored how the cellular elemental content and C:N:P stoichiometry of E. huxleyi may respond to two hypothetical future ocean scenarios (increased temperature, irradiance and pCO₂ combined with either N deficiency or P deficiency) if an additive effect is assumed. Both future scenarios indicate decreased calcification (which is predominantly sensitive to elevated pCO₂), increased C:N, and up to fourfold shifts in C:P and N:P. Our results strongly suggest that climate change will significantly alter the role of E. huxleyi (and potentially other calcifying phytoplankton species) in marine biogeochemical processes.     

Coccolith volume of the Southern Ocean coccolithophore Emiliania huxleyi as a possible indicator for palaeo‐cell volume

Coccolithophores are a key functional phytoplankton group and produce minute calcite plates (coccoliths) in the sunlit layer of the pelagic ocean. Coccoliths significantly contribute to the sediment record since the Triassic and their geometry have been subject to palaeoceanographic and biological studies to retrieve information on past environmental conditions. Here, we present a comprehensive analysis of coccolith, coccosphere and cell volume data of the Southern Ocean Emiliania huxleyi ecotype A, subject to gradients of temperature, irradiance, carbonate chemistry and macronutrient limitation. All tested environmental drivers significantly affect coccosphere, coccolith and cell volume with driver‐specific sensitivities. However, a highly significant correlation emerged between cell and coccolith volume with V_coccolith = 0.012 ± 0.001 * V_cell + 0.234 ± 0.066 (n = 23, r² = .85, p < .0001, σ_est = 0.127), indicating a primary control of coccolith volume by physiological modulated changes in cell volume. We discuss the possible application of fossil coccolith volume as an indicator for cell volume/size and growth rate and, additionally, illustrate that macronutrient limitation of phosphorus and nitrogen has the predominant influence on coccolith volume in respect to other environmental drivers. Our results provide a solid basis for the application of coccolith volume and geometry as a palaeo‐proxy and shed light on the underlying physiological reasons, offering a valuable tool to investigate the fossil record of the coccolithophore E. huxleyi.     

Dynamics and genotypic composition of Emiliania huxleyi and their co-occurring viruses during a coccolithophore bloom in the North Sea

We studied the temporal succession of vertical profiles of Emiliania huxleyi and their specific viruses (EhVs) during the progression of a natural phytoplankton bloom in the North Sea in June 1999. Genotypic richness was assessed by exploiting the variations in a gene encoding a protein with calcium-binding motifs (GPA) for E.?huxleyi and in the viral major capsid protein gene for EhVs. Using denaturing gradient gel electrophoresis and sequencing analysis, we showed at least three different E.?huxleyi and EhV genotypic profiles during the period of study, revealing a complex, and changing assemblage at the molecular level. Our results also indicate that the dynamics of EhV genotypes reflect fluctuations in abundance of potential E.?huxleyi host cells. The presence and concentration of specific EhVs in the area prior to the bloom, or EhVs transported into the area by different water masses, are significant factors affecting the structure and intraspecific succession of E.?huxleyi during the phytoplankton bloom.     

Role of Coccoliths in the Utilization of Inorganic Carbon by a Marine Unicellular Coccolithophorid, Emiliania huxleyi: a Survey Using Intact Cells and Protoplasts

The utilization of inorganic carbon and role of the coccolithswere investigated in intact cells and protoplasts of a marineunicellular calcareous alga, Emiliania huxleyi. Protoplastswith high photosynthetic activity were obtained by artificialdecalcification with 50 mM MES-NaOH (pH5.5). (1) The kineticsof the photosynthetic evolution of O₂ at various concentrationsof externally added NaHCO₃ were the same for intact cells andprotoplasts, indicating that the kinetic properties with respectto dissolved inorganic carbon (DIC) were not affected by thepresence or absence of the coccoliths on the cell surface. Double-reciprocalplots and plots of the concentration of substrate divided byvelocity (s/v) against the concentration of substrate (s) werebiphasic in the case of both intact cells and protoplasts. TheCO₂-utilization reaction was, therefore, considered to involvetwo processes with different values of K_m and V_max. From thekinetic analyses, K_m and V_max [µmoles O₂ (ml PCV)^–1h^–1] were deduced to be 92 µM and 76.3 for a "low-K_m"reaction and 4.1 mM and 252 for a "high-K_m" reaction, respectively.(2) In short-term (40-min) experiments, time courses of thetotal uptake of ¹⁴C-DIC and the incorporation of ¹⁴C into acid-stableproducts of photosynthesis and the internal pool of DIC, determinedas acid-labile compounds, under CO₂-limiting conditions (80µM) were very similar for intact cells and protoplasts.However, incorporation of ¹⁴C into CaCO₃ apparently occurredmore slowly in protoplasts than in intact cells. (3) In longterm (24-h) experiments, patterns of incorporation of ¹⁴C werealmost same for intact cells and protoplasts, with the exceptionthat the amount of ¹⁴C incorporated into CaCO₃ was much smallerin the former than the latter. The production of Ca¹⁴CO₃ increasedduring the course of 10 h after a 4-h lag. However, after 10h the level of Ca¹⁴CCO₃ started to decrease. The decrease wasaccompanied by an increase in ¹⁴C in the products of photosynthesis,suggesting that CaCO₃ was reutilized for the photosyntheticfixation of CO₂ and, therefore, that the coccoliths functionas sites of storage of DIC. However, the internal level of DICremained at the same level even after the supply of externalDIC has been almost completely depleted. (Received July 25, 1995; Accepted December 11, 1995)     

Characterization of NADH: nitrate reductase from the coccolithophorid Emiliania huxleyi (Lohman) Hay & Mohler (Haptophyceae)

Abstract Nitrate reductase was purified from and characterized in a bloom-forming unicellular calcifying alga, Emiliania huxleyi (Haptophyceae). The molecular masses of the native form and the subunit were 514 and 85 kDa, respectively, showing that the enzyme is a hexamer composed of 6 homologous subunits. The K _m values for NADH and NO3− were 40 μM and 104 μM, respectively. Activity of the reduction of nitrate was very high with reduced methylviologen and NADH, but no activity was observed with NADPH or reduced flavin mononucleotide; oxidation of NADH was very high with cytochrome c but did not occur with ferricyanide. These results indicate that Emiliania nitrate reductase is NADH-specific (EC 1.6.6.1), and that among algae and plants its subunit structure and kinetic properties are unique.     

Enzymological evidence for the function of a plastid-located pyruvate carboxylase in the Haptophyte alga Emiliania huxleyi: a novel pathway for the production of C4 compounds

Pyruvate carboxylase (PYC) catalyzes the β-carboxylation of pyruvate to yield oxaloacetate (OAA). We previously isolated a cDNA encoding a putative PYC (EhPYC1) from the haptophyte alga Emiliania huxleyi and then proposed that EhPYC1 contributes to active anaplerotic β-carboxylation during photosynthesis although PYC activity was not detected in the cell extracts. Involvement of PYC in photosynthetic carbon metabolism is unique, since PYC generally functions in non-photosynthetic organisms. In the present study, we demonstrate that EhPYC1 is highly sensitive to endogenous proteases and therefore is easily degraded in cell extracts. By avoiding proteolytic degradation, PYC activity can be detected in the cell extracts of E. huxleyi. The activity of a recombinant His-tagged EhPYC1 expressed in Streptomyces lividans was inhibited by l-malate in a mixed non-competitive manner. Immunofluorescence labeling showed that EhPYC1 is located in the plastid. This result agrees with the prediction that a bipartite plastid-targeting signal is present that functions to deliver proteins into the four-membrane plastid of haptophyte algae. This is the first finding of a plastid-located PYC. These results indicate that E. huxleyi possesses a unique pathway to produce OAA catalyzed by PYC, and the pathway may provide carbon skeletons for amino acid biosynthesis in the plastid. A database search indicates that PYC genes are widespread in green algae, diatoms and brown algae, suggesting the crucial role of PYC in various aquatic phototrophs.     

Development and validation of a molecular technique for the analysis of archived formalin-preserved phytoplankton samples permits retrospective assessment of Emiliania huxleyi communities

The coccolithophores, particularly the species Emiliania huxleyi (Lohmann) Hay & Mohler, account for the bulk of global calcium carbonate production and as such play a fundamental role in global CO2 cycling and the carbonate chemistry of the oceans. To evaluate the response of this functional group to the effects of climate change, we undertook a feasibility study to determine whether a retrospective approach could be used on archived coccolithophore datasets. We demonstrate for the first time a technique for the extraction of E. huxleyi nucleic acids from archived formalin-fixed samples of the long-term Continuous Plankton Recorder. Molecular analysis of a nine year old formalin-fixed sample reveals the presence of a diverse population of E. huxleyi genotypes within a developing coccolithophore bloom. In addition, E. huxleyi sequences were amplified from a number of formalin-fixed samples, the earliest of which was collected in August 1972. This molecular assay promises the possibility of studying global variations in the distribution and genetic make-up of E. huxleyi communities over extensive periods of time.