Cold Stress Stimulates Intracellular Calcification by the Coccolithophore, Emiliania huxleyi (Haptophyceae) Under Phosphate-Deficient Conditions

Intracellular calcification by the coccolith-producing haptophyte Emiliania huxleyi (NIES 837) is regulated by various environmental factors. This study focused on the relationship between cold and phosphate-deficient stresses to elucidate how those factors control coccolith production. (45)Ca incorporation into coccoliths was more than 97% of the total (45)Ca incorporation by whole cells. In a batch culture, orthophosphate in the medium (final concentration, 28.7 muM) was rapidly depleted within 3 days, and then extracellular alkaline phosphatase (AP) activity, an indicator of phosphate deprivation, increased during the stationary growth phase. The increase in AP activity was slightly higher at 20 degrees C than at 12 degrees C. The calcification started to increase earlier than AP activity, and the increase was much higher at 12 degrees C than at 20 degrees C. Such enhancement of calcification was suppressed by the addition of phosphate, while AP activity was also suppressed after a transient increase. These results suggest that phosphate deprivation is a trigger for calcification and that a rather long induction period is needed for calcification compared to the increase in AP activity. While calcification was greatly stimulated by cold stress, other cellular activities such as growth, phosphate utilization, and the induction of AP activity were suppressed. The stimulation of coccolith production by cold stress was minimal under phosphate-sufficient conditions. The high calcification activity estimated by (45)Ca incorporation was confirmed by morphological observations of coccoliths on the cell surface under bright-field and polarization microscopy. These results indicate that phosphate deprivation is the primary factor for stimulating coccolith production, and cold stress is a secondary acceleration factor that stimulates calcification under conditions of phosphate deprivation.     

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.     

Cytochemical and X-ray microanalysis studies of intracellular calcium pools in scale-bearing cells of the coccolithophoridEmiliania huxleyi

Summary Emiliania huxleyi is a coccolithophorid with a life cycle including a stage characterized by the occurrence of a scale-bearing cell type. The scales are composed of organic material and are produced in the cisternae of the Golgi apparatus. The present report deals with the ultrastructural calcium localization in scale-bearing cells using cation-precipitating agents. Cations were precipitated either with potassium pyroantimonate alone or according to a combined procedure in which cells are treated first with potassium oxalate, or potassium carbonate, or potassium phosphate, and then with potassium pyroantimonate. The distribution of electron-opaque deposits was the same when visualized by all four techniques. The most extensive deposits occurred in the Golgi apparatus, the peripheral space (a cellular compartment totally encompassing the protoplast), the multivesicular bodies, and the cell vacuole. X-ray microanalysis revealed that calcium was a constituent of the electron-opaque deposits. The uptake and transport of calcium, as universal functions of the Golgi apparatus, are discussed.     

Physiological regulation of carbon fixation in the photosynthesis and calcification of coccolithophorids

Emiliania huxleyi and Gephyrocapsa oceanica are the predominant coccolithophorid species that produce blooms in the ocean and affect the global environment. These species are capable of carbon fixation by both photosynthesis for organic matter production and by intracellular calcification for coccolith production. Both processes were strongly affected by the nutrient status in a laboratory culture. The coccolith production was stimulated by the addition of a high concentration of sodium bicarbonate and by the depletion of phosphate. Interestingly, when the calcification was stimulated, the increase in cell number during algal growth was greatly suppressed and then the cell volume increased. When the growth rate was increased under nutrient-sufficient conditions, the cells became very small in size and most of them bore few or no coccoliths. The data from laboratory experiments show that the cell growth and calcification proceeded apparently independently at different phases. We, therefore, assume that the coccolithophorid blooms in the ocean might be separated into two phases; firstly, the increase in cell population might be triggered by an adequate supply of nutrients to enhance algal growth and then the calcification might subsequently be stimulated when the nutrients become depleted by substantial algal growth.     

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.     

Identification and functional characterisation of genes encoding the omega-3 polyunsaturated fatty acid biosynthetic pathway from the coccolithophore Emiliania huxleyi

The Prymnesiophyceae coccolithophore Emiliania huxleyi is one of the most abundant alga in our oceans and therefore plays a central role in marine foodwebs. E. huxleyi is notable for the synthesis and accumulation of the omega-3 long chain polyunsaturated fatty acid docosahexaenoic acid (DHA; 22:6Δ^{4,7,10,13,16,19}, n − 3) which is accumulated in fish oils and known to have health-beneficial properties to humans, preventing cardiovascular disease and related pathologies. Here we describe the identification and functional characterisation of the five E. huxleyi genes which direct the synthesis of docosahexaenoic acid in this alga. Surprisingly, E. huxleyi does not use the conventional Δ6-pathway, instead using the alternative Δ8-desaturation route which has previously only been observed in a few unrelated microorganisms. Given that E. huxleyi accumulates significant levels of the Δ6-desaturated fatty acid stearidonic acid (18:4Δ^6,9,12,15, n − 3), we infer that the biosynthesis of DHA is likely to be metabolically compartmentalised from the synthesis of stearidonic acid.     

Regulation of CaCO(3) formation in coccolithophores

Coccolithophores impact the ocean carbon cycle principally through the generation of CO₂ during CaCO₃ production. Coccolithophore biomineralization has been examined most extensively in Pleurochrysis carterae and Emiliania huxleyi both of which produce mineralized scales—coccoliths—composed of elaborate calcite crystals attached to an underlying organic base plate. Calcification of preformed base plates is mediated by acidic polysaccharides and occurs in Golgi-derived structures known as mineralizing vesicles. In Pleurochrysis a high capacity calcium-binding polysaccharide PS2 is required for efficient nucleation of calcitic protocrystals. A galacturonomannan PS3 is required for the growth and transformation of the protocrystals into a massive double disc of calcite. The genes that regulate expression of the glycans have not yet been identified. In addition to the coccolith-bearing diploid phases, Pleurochrysis and Emiliania possess both haploid and diploid non-calcifying stages, which are self-perpetuating via binary fission. One non-calcifying Pleurochrysis phase fails to synthesis PS2 and spontaneously reverts to the mineralizing morphotype in laboratory cultures. As yet, there is little information on environmental factors that effect the expression or silencing of calcifying genes or favor the growth of calcifying over non-calcifying phases. These issues will need extensive investigation, if we are to appreciate the role of coccolithophores in the regulation of atmospheric CO₂ levels.     

Cryopreservation of the coccolithophore, <Emphasis Type="Italic">Emiliania huxleyi</Emphasis> (Haptophyta,Prymnesiophyceae)

We studied the cryopreservation of the most common coccolithophore, Emiliania huxleyi which is considered as one of the main global carbon cycle participants. Both stages of this complex life cycle species were submitted to gradual addition of three distinct cryoprotectants: dimethylsulfoxide (7.5% v/v), methanol (5% v/v) and proline (0.5 M). They were then control-rate cooled (−5 °C min⁻¹) to −50 °C before plunging into liquid nitrogen. Free radical oxygen species have been proposed to occur in cells subjected to pre-freezing manipulation or to cooling. Therefore, catalase (preventing accumulation of hydroxyl radicals) was evaluated for its ability to improve cell viability before and after freezing-thawing challenge. With the exception of proline which induced a decrease in diploid cell proliferation, cryoprotectants had no deleterious effects. On the contrary, growth of the haploid stage was enhanced by each CPA treatment, suggesting mixotrophic growth. Cryopreservation succeeded when dimethylsulfoxide was used, and the late exponential phase was obtained as soon as the 15th post-thawing day. Cell densities were then similar to the unfrozen controls. Catalase had no beneficial effect on the ability of cells to grow, neither prior freezing nor after thawing. In comparison with former attempts to cryopreserve E. huxleyi in other culture collection centers, our protocols allowed faster recovery.     

Effects of the diatom-Emiliana huxleyi succession on photosynthesis, calcification and carbon metabolism by size-fractioned phytoplankton

Changes in the species composition, photosynthesis, calcification and size-fractionated carbon metabolism by natural phytoplankton assemblages were monitored in three mesocosms under different nutrient conditions during May 1993. In the 3 enclosures, the decline of the diatom-dominated assemblages was followed by the development of a bloom of the coccolithoporid Emiliania huxleyi. Highest growth of E. huxleyi was observed in the mesocosm with a high N : P ratio, suggesting this species is a good competitor at low phosphate concentrations. The transition from diatom- to E. huxleyi-dominated assemblages brought about a sharp reduction of the phytoplankton standing stock and carbon-specific photosynthetic rate. The relative contribution of the smaller size fraction to total photosynthesis increased as the succession progressed. Calcification rate and E. huxleyi cell-specified calcite production were highest during the early stages of development of the E. huxleyi bloom. Distinct changes in the patterns of ¹⁴C allocation into biomolecules were noticed during the diatom-E. huxleyi succession. The diatom-dominated assemblage showed high relative ¹⁴C incorporation into low molecular weight metabolites (LMWM), whereas proteins and, specially, lipids accounted for the largest proportion of carbon incorporation in the E. huxleyi bloom. The patterns of photoassimilated carbon metabolism proved to be strongly dependent on cellular size, as protein relative synthesis was significantly higher in the smaller than in the larger size fraction, irrespective of the nutrient regime and the successional stage. These results are discussed in relation to the ecological and physiological features of small phytoplankton.     

Changes in sodium,calcium and magnesium ion concentrations in sturgeon (Huso huso) urine and in kidney morphology

During adaptation to brackish water the young great sturgeon Huso huso is able to regulate its serum osmolarity and ion concentrations. After transfer from fresh water to brackish water the ion concentrations in the urine increase and the urine becomes isoosmotic to the blood serum after 24h. The Na⁺ and K⁺ concentrations in the urine increase during the first 12 h by 4.4 and 7.7 times, respectively, later decreasing again. The Mg²⁺ and Ca²⁺ concentrations in the urine increase by 3.4 and 14 times during the first 72h in brackish water and remain high thereafter. These results suggest that the kidneys play an important part in the regulation of serum osmolarity and in the removal of Ca²⁺; however, in contrast to teleosts, Mg²⁺ must be removed extrarenally. During adaptation to a hyperosmotic medium the diameters of the Malpighian bodies, the glomeruli and the diameter of the tubules initially all decrease, but the distal tubules become morphologically differentiated into two regions and the diameter of the distal section later increases again. It is suggested that this is the site of Ca²⁺ secretion into the urine.     

Isoforms of Glutamine Synthetase in the Marine Coccolithophorid Emiliania huxleyi (Prymnesiophyceae)

Two isoenzymes of glutamine synthetase (EC 6.3.1.2), GS₁ and GS₂, have been purified from cells of Emiliania huxleyi using Cibacron blue dye ligand chromatography and gel filtration, separated by ion-exchange chromatography on Mono-Q and partly characterized. Each enzyme is a homohexamer with a molecular mass of 402 kDa for GS₁ and 501 kDa for GS₂. The molecular mass of the subunits of GS₁ and GS₂ was estimated to be 61 and 78 kDa, respectively. As in higher plants, GS₁ is slightly more thermostable than GS₂ and much less stimulated by thiols than GS₂. For these reasons, GS₁ was designated as the cytosolic enzyme and GS₂ as the chloroplastic one. Although the K_ms for NH₂OH are about the same, GS₂ possesses a much higher affinity for glutamine than GS₁. As in bacteria, ATP appears to play an important role in the allosteric regulation of GS₂. l-Ala and CTP are potent inhibitors of GS₁ activity. CTP, carbamoyl-phosphate and l-Ala exert a cumulative inhibitory effect on GS₁ activity. GS₂ is also inhibited to some extent by l-Ala and l-His. NH₂-terminal sequence analysis of GS₂ did not show any homology with bacteria, cyanobacteria or higher plants.     

Seasonal variation in Emiliania huxleyi coccolith morphology and calcification in the Aegean Sea (Eastern Mediterranean)

A seasonal morphological variability is observed in Emiliania huxleyi var. huxleyi specimens, collected from discrete water samples in the Aegean Sea. Biometric analyses reveal a consistent pattern of increase in the size of coccoliths and coccospheres, including the thickness of the inner tube elements (INT), in winter/spring time low sea surface temperature and moderate productivity samples when compared with summer time high temperature-low productivity samples. The small range of salinity change in the Aegean Sea and the absence of seasonal pattern in nutrient content do not support any association with the observed increase in E. huxleyi coccolith size. A relatively increased [HCO₃^-] content is observed during spring-time interval related with the increase in the coccolith size, however it remains unclear which parameter of the carbonate system causes the observed effects.     

Genetic delineation between and within the widespread coccolithophore morpho‐species Emiliania huxleyi and Gephyrocapsa oceanica (Haptophyta)

Emiliania huxleyi and Gephyrocapsa oceanica are abundant coccolithophore morpho‐species that play key roles in ocean carbon cycling due to their importance as both primary producers and cal‐cifiers. Global change processes such as ocean acidification impact these key calcifying species. The physiology of E. huxleyi, a developing model species, has been widely studied, but its genetic delineation from G. oceanica remains unclear due to a lack of resolution in classical genetic markers. Using nuclear (18S rDNA and 28S rDNA), mitochondrial (cox1, cox2, cox3, rpl16, and dam), and plastidial (16S rDNA, rbcL, tufA, and petA) DNA markers from 99 E. huxleyi and 44 G. oceanica strains, we conducted a multigene/multistrain survey to compare the suitability of different markers for resolving phylogenetic patterns within and between these two morpho‐species. The nuclear genes tested did not provide sufficient resolution to discriminate between the two morpho‐species that diverged only 291Kya. Typical patterns of incomplete lineage sorting were generated in phylogenetic analyses using plastidial genes. In contrast, full morpho‐species delineation was achieved with mitochondrial markers and common intra‐morpho‐species phylogenetic patterns were observed despite differing rates of DNA substitution. Mitochondrial genes are thus promising barcodes for distinguishing these coccolithophore morpho‐species, in particular in the context of environmental monitoring.     

Free radical oxidation (autoxidation) of alkenones and other lipids in cells of Emiliania huxleyi

Cells of the coccolithophorid Emiliania huxleyi strain CS-57 grown under an atmosphere of air+0.5% CO(2) showed oxidative damage after 10 days growth with concomitant and major changes to the lipid composition. The fatty acid profile was strongly altered and lacked appreciable amounts of the polyunsaturated fatty acids (PUFA: C(18:5), C(18:3) and C(22:6)) typical of healthy cells. Oxidation products of these PUFA could not be detected, but monounsaturated fatty acids proved to be good indicators of oxidative processes. The presence (after NaBH(4)-reduction) of a high proportion of 11-hydroxyoctadec-cis-9-enoic and 8-hydroxyoctadec-cis-9-enoic acids showed that the degradation of oleic acid involved mainly free radical oxidation processes (70-75% autoxidation and 20-25% photooxidation). We also detected large amounts of degradation products of the oxidation product 9,10-epoxyoctadecanoic acid including diols, methoxyhydrins and chlorohydrins. These oxidative effects were found in all the lipid classes examined. Products included significant amounts of chlorophyll side-chain autooxidation products Z- and E-3,7,11,15-tetramethylhexadec-3-ene-1,2-diols and Z-and E-3,7,11,15-tetramethylhexadec-2-ene-1,4-diols, while phytyldiol was present in relatively low proportions. Delta(5)-3beta,7-epimeric unsaturated steroidal diols arising from the autooxidation of the Delta(5) double bond of epi-brassicasterol and minor amounts of Delta(4)-3beta,6-diols were also detected. Long-chain unsaturated ketone (alkenone) content per cell was much higher in the presence of 0.5% CO(2) likely due to carbon storage under these conditions. The proportions of di- and tri-unsaturated alkenones was relatively stable throughout the growth cycle in the absence of additional CO(2), but not when grown with 0.5% CO(2). The detection of characteristic alkenone autoxidation products in cells grown under these latter conditions allowed us to attribute the significant increase in index observed to the involvement of free radical oxidation processes.