The fatty acid and sterol composition of two marine dinoflagellates

The fatty acid, sterol and chlorophyll pigment compositions of the marine dinoflagellates Gymnodinium wilczeki and Prorocentrum cordatum are reported. The fatty acids of both algae show a typical dinoflagellate distribution pattern with a predominance of C₁₈, C₂₀ and C₂₂ unsaturated components. The acid 18:5ω3 is present at high concentration in these two dinoflagellates. G. wilczeki contains a high proportion (93.4%) of 4-methyl-5α-stanols including 4,23,24-trimethyl-5α-cholest-22E-en-3β-ol (dinosterol), dinostanol and 4,23,24-trimethyl-5α-cholest-7-en-3β-ol reported for the first time in dinoflagellates. The role of this sterol in the biosynthesis of 5α-stanols in dinoflagellates is discussed. P. cordatum contains high concentrations of a number of δ ²⁴⁽²⁸⁾-sterols with dinosterol, 24-methylcholesta-5,24(28)-dien-3β-ol, 23,24-dimethylcholesta-5,22E-dien-3β-ol, 4,24-dimethyl-5α-cholest-24(28)-en-3β-ol and a sterol identified as either 4,23,24-trimethyl- or 4-methyl-24-ethyl-5α-cholest-24(28)-en-3β-ol present as the five major components. The role of marine dinoflagellates in the input of both 4-methyl- and 4-desmethyl-5α-stanols to marine sediments is discussed.     

A SURVEY OF THE STEROL COMPOSITION OF THE MARINE DINOFLAGELLATES KARENIA BREVIS,KARENIA MIKIMOTOI,AND KARLODINIUM MICRUM: DISTRIBUTION OF STEROLS WITHIN OTHER MEMBERS OF THE CLASS DINOPHYCEAE1

The sterol composition of different marine microalgae has been examined to determine the utility of sterols as biomarkers to distinguish members of various algal classes. For example, members of the class Dinophyceae possess certain 4‐methyl sterols, such as dinosterol, which are rarely found in other classes of algae. The ability to use sterol biomarkers to distinguish certain dinoflagellates such as the toxic species Karenia brevis Hansen and Moestrup, responsible for red tide events in the Gulf of Mexico, from other species within the same class would be of considerable scientific and economic value. Karenia brevis has been shown by others to possess two major sterols, (24S)‐4α‐methyl‐5α‐ergosta‐8(14),22‐dien‐3β‐ol (ED) and its 27‐nor derivative (NED), having novel structures not previously known to be present in other dinoflagellates. This prompted the present study of the sterol signatures of more than 40 dinoflagellates. In this survey, sterols with the properties of ED and NED were found in cultures of K. brevis and shown also to be the principal sterols of Karenia mikimotoi Hansen and Moestrup and Karlodinium micrum Larsen, two dinoflagellates closely related to K. brevis. They are also found as minor components of the more complex sterol profiles of other members of the Gymnodinium/Peridinium/Prorocentrum (GPP) taxonomic group. The distribution of these sterols is consistent with the known close relationship between K. brevis, K. mikimotoi, and K. micrum and serves to limit the use of these sterols as lipid biomarkers to a few related species of dinoflagellates.     

FATTY ACID AND LIPID COMPOSITION OF THE ACIDOPHILIC GREEN ALGA CHLAMYDOMONAS SP.1

The lipid and fatty acid compositions of Chlamydomonas sp. isolated from a volcanic acidic lake and C. reinhardtii were compared, and the effects of pH of the medium on lipid and fatty acid components of Chlamydomonas sp. were studied. The fatty acids in polar lipids from Chlamydomonas sp. were more saturated than those of C. reinhardtii. The relative percentage of triacylglycerol to the total lipid content in Chlamydomonas sp. grown in medium at pH 1 was higher than that in other cells grown at higher pH. A probable explanation might be that Chlamydomonas sp. has two low pH adaptation mechanisms. One mechanism is the saturation of fatty acids in membrane lipids to decrease membrane lipid fluidity, and the other is the accumulation of triacylglycerol, as a storage lipid, to prevent the osmotic imbalance caused by high concentrations of H₂SO₄.     

LIPID COMPOSITION OF A PROCHLOROPHYTE1

A lipid analysis is reported of a symbiont Prochloron sp. associated with the ascidian Lissorclinum patella collected from Rodda Reef, North Queensland, Australia. Phosphatidyl glycerol, monogalacosyl diglyceride, digalacosyl diglyceride and sulfoquinovasyl diglyceride were identified. These lipids together with their fatty acid profiles, the limited range of hydrocargons (nC₁₃-nC₁₇), and sterol analysis (chlesterol 27%) are consistent with a firm relaionship fot the new genus Prochloron with he Cyanophya.     

COLONIZATION OF THE EPINEUSTON BY CYSTODINIUM BATAVIENSE(DINOPHYCEAE): BEHAVIOR OF THE ZOOSPORE1

Cystodinium bataviense Klebs is the first dinoflagellate observed to exhibit specialized zoospore behavior which results in colonization of the epineuston. The zoospore: (1) is strongly phototactic; (2) changes shape rapidly upon release; (3) possesses at least two types of swimming behavior, including a “stop mechanism”; and, (4) sheds its theca as the new cell wall asymmetrically elongates into the immobile vegetative stage. These features working in concert facilitate the entrance of Cystodinium into the epineuston. Detailed observations of zoospore morphology and analysis of its behavior are used as new characters to further delimit C. bataviense. Since vegetative morphology has proven unsatisfactory in circumscribing other Cystodinium species, the study of variation in zoospore characters will help to clarify taxonomic units within the genus.     

ANTARCTIC DISTRIBUTION,PIGMENT AND LIPID COMPOSITION,AND MOLECULAR IDENTIFICATION OF THE BRINE DINOFLAGELLATE POLARELLA GLACIALIS (DINOPHYCEAE)1

Polarella glacialis (Montresor et al.) was identified in Davis Station sea ice by morphological and DNA sequence comparison of cultures with those of the authentic strain P. glacialis CCMP 1383 isolated from McMurdo Sound. Cells and cysts of the Davis isolate (FL1B) were morphologically indistinguishable from P. glacialis, and comparison of the large subunit rDNA of both cultures demonstrated only 0.2% sequence divergence over 1366 base pairs. The photosynthetic pigments of P. glacialis (strains FL1B and CCMP 1383) were typical of dinoflagellates, with peridinin (contributing up to 31%) as the major accessory pigment. Extremely high levels of polyunsaturated fatty acids (PUFA, up to 76.3%) were characteristic of P. glacialis isolate FL1B. The high PUFA concentration of this species is thought to be an adaptation to survive the cold temperatures of the upper fast ice. The sterol profile of FL1B was atypical of dinoflagellates, with 4‐desmethylsterols (up to 79%) in greater abundance than 4α‐methyl sterols (up to 24%). 27‐Nor‐24‐methylcholest‐5,22E‐dien‐3β‐ol was identified as the principle sterol in P. glacialis, contributing up to 64% of the total sterol composition.     

THE FATTY ACID AND STEROL COMPOSITION OF FIVE MARINE DINOFLAGELLATES

The fatty acid and sterol compositions of five species of marine dinoflagellates (Scrippsiella sp. Symbiodinium microadriaticum Freud, Gymnodinium sp., Gymnodinium sanguineum Hirasaki, and Fragilidium sp.) are reported. All contained the major fatty acids that are considered common in dinoflagellates, but the proportions were quite variable, and some species contained low contents of some polyunsaturated fatty acids. Concentration ranges for the major fatty acids were: 16:0 (9.0%–24.8%), 18:4(n-3) (2.5%–11.5%), 18:5(n-3) (7.0%–43.1%), 20:5(n-3) (EPA) (1.8%–20.9%), and 22:6(n-3) (DHA) (9.9%– 26.3%). Small amounts of novel very-long-chain highly unsaturated C₂₈ fatty acids occurred in all species. Each dinoflagellate contained a complex mixture of 4-methyl sterols and 4-desmethyl sterols. Four species contained cholesterol, although the amounts were highly variable (from 0.2% of total sterols in Scrippsiella sp. to 45.6% in Fragilidium sp.). All but G. sanguineum contained the 4-methyl sterol dinosterol, and all species contained sterols lacking a double bond in the ring system (i.e. stanols); in Scrippsiella sp. cholestanol composed 24.3% of the total sterols. Other common features of the 4-methylsterol profiles were the presence of 23,24-dimethyl alkylation and unsaturation at Δ²² in the side chain. In Scrippsiella sp., four steroidal ketones were identified: cholestanone, dinosterone, 4α,23,24-trimethyl-5α-cholest-8(14)-en-3-one, and dinostanone. The structures of these corresponded to the major sterols in this species, suggesting that the sterols and steroidal ketones are biosynthetically linked. Steroidal ketones were not detected in the other species. Although fatty acid profiles can be used to distinguish among algal classes, they were not useful for differentiating among dinoflagellate species. In contrast, whereas some taxonomic groupings of dinoflagellates display similar sterol patterns, others, such as the gymnodinoids studied here, clearly do not. The combination of fatty acid, sterol, and steroidal ketone profiles may be useful complementary chemotaxonomic tools for distinguishing morphologically similar species. The identification of steroidal ketones supports earlier suggestions that certain dinoflagellates might be a significant source of such components in marine environments.     

THE FLAGELLAR APPARATUS OF GYMNODINIUM SP. (DINOPHYCEAE)1

The detailed structure of the flagellar apparatus has been determined in a small dinoflagellate of the genus Gymnodinium. Although diminutive, this dinoflagellate possesses a complex flagellar apparatus consisting of a posteriorly directed microtubular root, a transverse striated fibrous root, several striated fibrous connectives that attach the basal bodies to one another as well as to the different roots, and a conspicuous non-striated fibrous connective that directly links the posteriorly directded microtubular root with the extended lobe of the nucleus. This represents the second discovery of a nuclear connective linked to the flagellar apparatus in the Dinophyceae but is the first report to elucidate the spatial relationships of the connective with the flagellar apparatus and the cell. A detailed diagrammatic reconstruction is provided and the similarities between these flagellar apparatus features are compared with those known for other dinoflagellates. Additionally, the structure and displacement of the nuclear connective are compared with nuclear connectives described in other protists.     

EVIDENCE A PHOTOPROTECTIVE FOR SECONDARY CAROTENOIDS OF SNOW ALGAE1

Snow algae occupy a unique habitat in high altitude and polar environments. These algae are often subject to extremes in nutrient availability, acidity, solar irradiance, desiccation, and ambient temperature. This report documents the accumulation of secondary carotenoids by snow algae in response to the availability of nitrogenous nutrients. Unusually large accumulations of astaxanthin esters in extra-chloroplastic lipid globules produce the characteristics red pigmentation typical of some snow algae (e.g. Chlamydomonas nivalis (Bauer) Wille). Consequently these compounds greatly reduce the amount of light available for absorption by the light-harvesting pigment-protein complexes, thus potentially limiting photoinhibition and photodamage caused by intense solar radiation. The esterification of astaxnthin with fatty acids represents a possible mechanism by which this chromophore can be concentrated within cytoplasmic globules to maximize its photoprotective efficiency.     

UTEX 1336: PERIDINIUM CINCTUM OR PERIDINIUM VOLZII (DINOPHYCEAE)?1

Plate pattern variation in UTEX clone 1336 and published photographs using this clone indicate the presence of two taxa: Peridinium cinctum and Peridinium volzii. All subclones established from UTEX 1336 contain the same two cell types. The identification of UTEX 1336 and its future use by researchers are discussed.     

EFFECT OF NUTRIENT LIMITATION ON FATTY ACID AND LIPID CONTENT OF MARINE MICROALGAE1

Phaeodactylum tricornutum and Chaetoceros sp. (Badllariophyceae), Isochrysis galbana (clone T-Iso) and Pavlova lutheri (Prymnesiophyceae), Nannochloris atomus (Chlorophyceae), Tetraselmis sp. (Prasinophyceae), and Gymnodinum sp. (Dinophyceae) were cultured at different extents of nutrient-limited growth: 50 and 5% of μ_max. The lipid content of the algae was in the range 8.3–29.5% of dry matter and was generally higher in the Prymnesiophyceae than in the Prasinophyceae and the Chlorophyceae. Increasing extent of phosphorus limitation resulted in increased lipid content in the Bacillariophyceae and Prymnesiophyceae and decreased lipid content in the green flagellates N. atomus and Tetraselmis sp. The fatty acid composition of the algae showed taxonomic conformity, especially for the Bacillariophyceae, where the major fatty adds were 14:0, 16:0, 16:1, and 20:5n-3. These fatty acids were dominant also in the Prymnesiophyceae together with 22:6n-3. An exception was I. galbana, in which 18:1 was the major monounsaturated fatty add and 20:5n-3 was absent. The fatty acids of N. atomus and Tetraselmis sp. varied somewhat, but 16:0, 16:1, 18:1, 18:3n-3, and 20:5n-3 were most abundant. Gymnodinum sp. contained mainly 16:0, 18:4n-3, 20: 5n-3, and 22:6n-3. An increased level of nutrient limitation (probably phosphorus) resulted in a higher relative content of 16:0 and 18:1 and a lower relative content of 18:4n-3, 20:5n-3, and 22:6n-3. The nutrient limitation probably reduced the synthesis of n-3 polyunsaturated fatty acids.     

LIPID CLASS,CAROTENOID, AND TOXIN DYNAMICS OF KARENIA BREVIS (DINOPHYCEAE) DURING DIEL VERTICAL MIGRATION1

The internal lipid, carotenoid, and toxin concentrations of Karenia brevis (C. C. Davis) Gert Hansen and Moestrup are influenced by its ability to use ambient light and nutrients for growth and reproduction. This study investigated changes in K. brevis toxicity, lipid class, and carotenoid concentrations in low‐light, nitrate‐replete (250 μmol quanta · m^?2 · s^?1, 80 μM NO₃); high‐light, nitrate‐replete (960 μmol quanta · m^?2 · s^?1, 80 μM NO₃); and high‐light, nitrate‐reduced (960 μmol quanta · m^?2 · s^?1, <5 μM NO₃) mesocosms. Reverse‐phase HPLC quantified the epoxidation state (EPS) of the xanthophyll‐cycle pigments diadinoxanthin and diatoxanthin, and a Chromarod Iatroscan thin layer chromatography/flame ionization detection (TLC/FID) system quantified changes in lipid class concentrations. EPS did not exceed 0.20 in the low‐light mesocosm, but increased to 0.65 in the high‐light mesocosms. Triacylglycerol and monogalactosyldiacylglycerol (MGDG) were the largest lipid classes consisting of 9.3% to 48.7% and 37.3% to 69.7% of total lipid, respectively. Both lipid classes also experienced the greatest concentration changes in high‐light experiments. K. brevis increased EPS and toxin concentrations while decreasing its lipid concentrations under high light. K. brevis may mobilize its toxins into the surrounding environment by reducing lipid concentrations, such as sterols, limiting competition, or toxins are released because lipids are decreased in high light, reducing any protective mechanism against their own toxins.     

EFFECTS OF SILICON DEFICIENCY ON LIPID COMPOSITION AND METABOLISM IN THE DIATOM CYCLOTELLA CRYPTICA1

The effects of silicon deficiency on the metabolism and composition of lipids in Cyclotella cryptica T13L Reimann, Lewin, and Guillard were examined. Silicon-deficient cells had higher levels of neutral lipids (primarily triacylglycerols) and higher proportions of saturated and monounsaturated fatty acids than silicon-replete cells. After 4 h of silicon deficiency, the percentage of newly assimilated NaH¹⁴CO₃ partitioned into lipids increased from 27.6% to 54.1%, whereas the percentage partitioned into chrysolaminarin decreased from 21.6% to 10.6%. In addition, pulse-chase experiments with NaH¹⁴CO₃ indicated that the amount of ¹⁴C in the total cellular lipid fraction increased by 32% after 12 h of silicon deficiency despite the absence of additional photoassimilable ¹⁴C. Therefore, the accumulation of lipids in response to silicon deficiency appears to be due to two distinct processes: (a) an increase in the proportion of newly assimilated carbon partioned into lipids, and (2) a slow conversion of previously assimilated carbon from non-lipid compounds into lipids     

A NEW LARVAL FISH BIOASSAY FOR TESTING THE PATHOGENICITY OF PFIESTERIA SPP. (DINOPHYCEAE)1

Water quality, microbial contamination, prior fish health, and variable results have been major impediments to identifying the cause and mechanism of fish mortality in standard aquarium‐format Pfiesteria bioassays. Therefore, we developed a sensitive 96‐h larval fish bioassay for assessing Pfiesteria spp. pathogenicity using six‐well tissue culture plates and 7‐day‐old larval cyprinodontid fish. We used the assay to test pathogenicity of several clonal lines of Pfiesteria piscicida Steidinger and Burkholder and P. shumwayae Glasgow and Burkholder that had been cultured with algal prey for 2 to 36 months. The P. shumwayae cultures exhibited 80%–100% cumulative mortality in less than 96 h at initial zoospore densities of approximately 1000 cells·mL^?1. No fish mortalities occurred with P. piscicida at identical densities or in controls. In a dose‐response assay, we demonstrated a strong positive correlation between dinospore density and fish mortality in a highly pathogenic culture of P. shumwayae, generating a 96‐h LD₅₀ of 108 zoospores·mL^?1. Additionally, we applied the assay to evaluate a 38‐L P. shumwayae bioassay that was actively killing fish and compared results with those from exposures of juvenile tilapia (Oreochromis niloticus) in a 500‐mL assay system. Water from the fish‐killing 38‐L assay was filtered and centrifuged to produce fractions dominated by dinoflagellates, bacteria, or presumed ichthyotoxin (cell‐free fraction). After 96 h, the larval fish assay exhibited 50%–100% cumulative mortality only in fractions containing dinoflagellates, with no mortalities occurring in the other fractions. The 500‐mL bioassay with tilapia produced inconsistent results and demonstrated no clear correlation between mortality and treatment. The new larval fish bioassay was demonstrated as a highly effective method to verify and evaluate dinoflagellate pathogenicity.     

STEROL DISTRIBUTION IN THE GENUS HETEROCAPSA (PYRRHOPHYTA)1

The sterol composition of seven strains of marine peridinioid dinoflagellates comprising the four known species of Heterocapsa Stein was examined by gas chromatography-mass spectrometry to determine the utility of these compounds in systematics. Cholest-5-en-3β-ol (cholesterol), 24-methyl-cholest-5-en-3β-ol (24-methylcholesterol), 4α,24(S)-dimethyl-5α-cholestan-3β-ol (4,24-dimethylcholestanol), 4α,23,24(R)-trimethyl-5α-cholest-22-en-3β-ol (dinosterol), 4α,23ξ,24ξ-trimethyl-5α-cholestan-3β-ol (dihydrodinosterol), and an unknown sterol were detected. Sterol composition does not vary significantly from species to species within the genus Heterocapsa and thus cannot be used for species differentiation. Sterols may, however, have value in defining the properties of dinoflagellate taxa above the family level. Over the course of the growth curve for Heterocapsa niei (Loeblich) Morrill & Loeblich 4,24-dimethylcholestanol and dinosterol covaried, suggesting that 4,24-dimethylcholestanol is converted into dinosterol by a previously proposed bioalkylation scheme.     

LIPID,FATTY ACID,AND STEROL COMPOSITION OF EIGHT SPECIES OF KARENIACEAE (DINOPHYTA): CHEMOTAXONOMY AND PUTATIVE LIPID PHYCOTOXINS1

The lipid class, fatty acid, and sterol composition of eight species of ichthyotoxic marine gymnodinioid dinoflagellate (Karenia, Karlodinium, and Takayama) species was examined. The major lipid class in all species was phospholipid (78%–95%), with low levels of triacylglycerol (TAG; 0%–16%) and free fatty acid (FFA; 1%–11%). The common dinoflagellate polyunsaturated fatty acids (PUFA), octadecapentaenoic acid (OPA 18:5ω3), and docosahexaenoic acid (DHA 22:6ω3), were present in all species in varying amounts (14%–35% and 8%–23%, respectively). The very‐long‐chain PUFA (VLC‐PUFA) 28:7ω6 and 28:8ω3 were present at low levels (<1%), and the ratio of these fatty acids may be a useful chemotaxonomic marker at the species level. The typical dinoflagellate sterol dinosterol was absent from all species tested. A predominance of the 4‐methyl and 4‐desmethyl Δ⁸⁽¹⁴⁾ sterols in all dinoflagellate species included 23‐methyl‐27‐norergosta‐8(14),22‐dien‐3β‐ol (Karenia papilionacea A. J. Haywood et Steid, 59%–66%); 27‐nor‐(24R)‐4α‐methyl‐5α‐ergosta‐8(14),22‐dien‐3β‐ol, brevesterol, (Takayama tasmanica de Salas, Bolch et Hallegraeff 84%, Takayama helix de Salas, Bolch, Botes et Hallegraeff 71%, Karenia brevis (C. C. Davis) G. Hansen et Moestrup 45%, Karlodinium KDSB01 40%, Karenia mikimotoi (Miyake et Kominami ex Oda) G. Hansen et Moestrup 38%); and (24R)‐4α‐methyl‐5α‐ergosta‐8(14),22‐dien‐3β‐ol, gymnodinosterol, (K. mikimotoi 48%, Karenia umbella de Salas, Bolch et Hallegraeff 59%, Karlodinium veneficum (D. L. Ballant.) J. Larsen 71%–83%). In Takayama species, five steroid ketones were identified, including for the first time the 3‐keto form of brevesterol and gymnodinosterol. These results indicate a biochemical link between sterol and steroid ketone biosynthesis, suggesting that selected dinoflagellates can make a significant contribution to ketones in marine sediments. The presence of steroid ketones, specific sterols, and fatty acids, and the ratio of VLC‐PUFA may prove to be a useful chemotaxonomic tool for distinguishing between morphologically similar species. The relative levels of the PUFA, OPA, and DHA, coupled with the potential inhibitory action of Δ⁸⁽¹⁴⁾ sterols, may provide an insight into the ichthyotoxicity of these bloom‐forming dinoflagellates.     

LIPID CLASS DISTRIBUTION OF HIGHLY UNSATURATED LONG CHAIN FATTY ACIDS IN MARINE DINOFLAGELLATES

The very long chain highly unsaturated C₂₈ fatty acids, octacosaheptaenoic [28:7(n-6)] and octacosaoctaenoic acid [28:8(n-3)], were found to be associated with phospholipids, obtained by fractionation of total lipid extracts into distinct lipid classes, in 4 and 6, respectively, of 16 examined dinoflagellates. An interfraction comparison of fatty acids associated with phospholipids and glycolipids has also shown that the phospholipid fractions contained the majority (over 75% in 12 of 16 strains) of docosahexaenoic acid [22:6(n-3)] and traces of tetracosanoic acid (24:0). By contrast, the highly unsaturated C₁₈ fatty acids octadecatetraenoic [18:4(n-3)] and octadecapentaenoic acid [18:5(n-3)] were primarily recovered from a chloroplast-associated glycolipid fraction comprised of monogalactosyldiacylglycerol, digalactosyldiacylglycerol, and sulfoquinovosyldiacylglycerol. In 12 of 16 strains, an interfraction comparison showed that over 90% of 18:5(n-3) was found to be associated with glycolipids. These findings indicate that the C₂₈ fatty acids are located and probably synthesized in the cytoplasm or in an organelle other than the chloroplast, possibly with 22:6(n-3) and 24:0 as precursors, whereas the C₁₈ fatty acids 18:4(n-3) and 18:5(n-3) are glycolipid constituents apparently synthesized within the chloroplast. The function(s) of these C₂₈ fatty acids as components of phospholipids in cellular membranes is currently unknown.     

INVESTIGATION OF 4-METHYL STEROLS FROM CULTURED DINOFLAGELLATE ALGAL STRAINS

The marine dinoflagellates Prorocentrum micans, Gonyaulax polyedra, Gymnodinium sp., and Alexandrium tamarense, collected from the Adriatic Sea during red-tide blooms, were cultured to investigate the 4-methyl sterol constituents. To ascertain a possible influence of cell age on the 4-methyl sterol content, for one strain (Gymnodinium sp.)we investigated the composition of these constituents at exponential and stationary growing phases. The lipid material extracted with acetone from the lyophilized algal samples was fractionated by thin-layer chromatography. The 4-methyl sterols recovered from the layer were converted into the corresponding OTMS derivatives. Nine of 11 constituents were identified by gas chromatography and gas chromatography-mass spectrometry; only two minor constituents were characterized by their gas chromatographic parameters. All free methyl sterols identified in the algal samples had been detected previously in various dinoflagellates. The 4-methyl sterol fractions generally contained very few constituents. Except for the Gymnodinium sp. sample, collected at the exponential growing phase (GyD2 exp), which contains 4,24-dimethylcholestan-3-ol as a unique constituent, dinosterol was the major component. Moreover, 4,24-ethylcholestan-3-ol was also an important constituent of both Prorocentrum and Gonyaulax strains, whereas considerable amounts of dinostanol characterized all the Gymnodinium sp. strains. In addition, the latter contained several minor constituents such as 4-methylcholestan-3-ol, 4,24-dimethylcholesta-22-en-3-ol, and 4-methyl-24-ethylcholestan-3-ol. 4-Methyl-24-methylene-cholestan-3-ol was a constituent of the Gymnodinium sp. sample, collected at the stationary growing phase (GyD2 stat)only, whereas 4-methylgorgostanol was identified only in the Alexandrium tamarense Gt4 strain. Except for 4-methyl-24-ethylcholesta-8(14)-en-3-ol, all the methyl sterol constituents from our algae show a saturated polynuclear system. The pathways by which side-chain modifications occur in dinoflagellate 4-methyl sterols are considered, and a map of the fragmentation pattern of the trimethylsilyl-4-methyl sterols under electronic impact is also reported.     

THE BIOCHEMICAL COMPOSITION OF MARINE MICROALGAE FROM THE CLASS EUSTIGMATOPHYCEAE1

The biochemical composition of four strains of microalgae from the class Eustigmatophyceae was determined to assess their usefulness as live feeds for mariculture and to establish characteristic features for use in chemotaxonomic studies. We studied Nannochloropsis salina (strain CS-190) from Scotland, two strains of Nannochloropsis oculata (CS-179 and CS-216) from Japan, and an unnamed eustigmatophyte (CS-246) isolated from Queensland waters that appears to be closely related to N. oculata. Gross compositional features were similar: total carbohydrate ranged from 5.2% (N. oculata CS-179) to 8.9% (N. salina) of cell dry weight. Polysaccharide comprised 74% (N. oculata CS-179) to 88% (CS-246) of this total. Glucose was the principal polysaccharide sugar (45.2–66.2% of total sugars). Other sugars included fucose, galactose, mannose, rhamnose, ribose, and xylose (2.0–14.0%). Arabinose was a minor constituent in all species (0.6–1.7%). Protein varied from 17.8% (N. salina) to 22.1% (N. oculata CS-216) of the cell dry weight. The major amino acids were arginine, glutamate, and asparatate (7.2–10.4% of total amino acids), with methionine, cystine, histidine, tryptophan, hydroxy-proline, ornithine, and γ-aminobutyric acid much less abundant (0.03–2.6%). Lipid content ranged from 8.2% (N. oculata CS-216) to 16.9% (N. salina) of cell dry weight, the latter value reflecting enhanced concentrations of triacylglycerols in N. salina. The major fatty acids were palmitic acid (16:0), palmitoleic acid [16:1(n-7)], and eicosapentaenoic acid [20:5(n-3)] with lesser amounts of lauric acid (14:0), linoleic acid [18:2(n-6)], and others. The sterols consisted almost entirely of cholesterol, which is an essential constituent of crustacean diets. Chlorophyll a ranged from 0.6% (N. oculata CS-216) to 1.7% (N. oculata CS-179 and N. salina) of cell dry weight. Chlorophylls b and c were not detected. All strains contained a characteristic pattern of carotenoid pigments, which included violaxanthin, β-carotene, zeaxanthin, and a pigment tentatively identified as vaucheriaxanthin-ester. The distinctive pigment and lipid compositional data can be used as chemotaxonomic markers for Nannochloropsis and for assigning microalgae to the class Eustigmatophyceae. Nannochloropsis oculata is widely used as an algal feed in mariculture, and based on the similarity of the biochemical data, both N. salina and the unnamed tropical species should also prove to be nutritionally valuable live algal feedstocks. Feeding trials will be needed to confirm this.     

THE RELATIONSHIP OF LIPIDS WITH LIGHT AND CHLOROPHYLL MEASUREMENTS IN FRESHWATER ALGAE AND PERIPHYTON1

Lipid content and lipid class composition were determined in stream periphyton and the filamentous green algae Cladophora sp. and Spirogyra sp, Sterols and phospholipids were compared to chlorophyll a (chl a) as predictors of biomass for stream periphyton and algae. Chlorophyll a, phospholipids, and sterols were each highly correlated with ash-free dry mass (AFDM) (r² > 0.98). Stream periphyton exposed naturally to high light (HL) and low light (LL) had chl a concentrations (μg chl a-mg^?1AFDM) of 7.9± 0.7 and 12.4 ± 2.9, respectively, while the sterol concentrations of these HL and LL stream periphyton (1.6 ± 0.4) were not significantly different (P > 0.05). Periphyton exposed to an irradiance of 300 μmol photons·m^?2s^?1 in the laboratory for 60 h had 5.6 ± 0.55 μg chl a·mg^?1 AFDM, but the same periphyton exposed to 2% incident light for the same amount of time had 11.0 ± 0.56 μg chl a·mg^?1 AFDM. Sterol concentrations in these periphyton communities remained unchanged (1.5 ± 0.3 μg·mg^?1AFDM), Similar results (i.e. changes in chl a but stability of sterol concentrations in response to irradiance changes) were also found for Cladophora and Spirogyra in laboratory experiments. Sterols can be quantified rapidly from a few milligrams of algae and appear to be a useful predictor of eukaryote biomass, whereas cellular levels of chl a vary substantially with light conditions. Phospholipids (or phospholipid fatty acids) are considered to be a reliable measure of viable microbial biomass. Nevertheless, phospholipid content varied substantially and unpredictably among algae and periphyton under different light regimes. Irradiance also had a significant effect on storage lipids: HL Cladophora and HL periphyton had 2 × and 5 × greater concentrations of triacylglycerols, respectively, compared to their LL forms. HL and LL algae also differed in the concentration of several major fatty acids. These light-induced changes in algal lipids and fatty acids have important implications for grazers.