T. Alwyn V. Rees

Metabolic interactions between algal symbionts and invertebrate hosts

Some invertebrates have enlisted autotrophic unicellular algae to provide a competitive metabolic advantage in nutritionally demanding habitats. These symbioses exist primarily but not exclusively in shallow tropical oceanic waters where clear water and low nutrient levels provide maximal advantage to the association. Mostly, the endosymbiotic algae are localized in host cells surrounded by a host-derived membrane (symbiosome). This anatomy has required adaptation of the host biochemistry to allow transport of the normally excreted inorganic nutrients (CO2, NH3 and PO43-) to the alga. In return, the symbiont supplies photosynthetic products to the host to meet its energy demands. Most attention has focused on the metabolism of CO2 and nitrogen sources. Carbon-concentrating mechanisms are a feature of all algae, but the products exported to the host following photosynthetic CO2 fixation vary. Identification of the stimulus for release of algal photosynthate in hospite remains elusive. Nitrogen assimilation within the symbiosis is an essential element in the hosts control over the alga. Recent studies have concentrated on cnidarians because of the impact of global climate change resulting in coral bleaching. The loss of the algal symbiont and its metabolic contribution to the host has the potential to result in the transition from a coral-dominated to an algal-dominated ecosystem.

Allometry and stoichiometry of unicellular, colonial and multicellular phytoplankton

Phytoplankton life forms, including unicells, colonies, pseudocolonies, and multicellular organisms, span a huge size range. The smallest unicells are less than 1 microm3 (e.g. cyanobacteria), while large unicellular diatoms may attain 10(9) microm3, being visible to the naked eye. Phytoplankton includes chemo-organotrophic unicells, colonies and multicellular organisms that depend on symbionts or kleptoplastids for their capacity to photosynthesize. Analyses of physical (transport within cells, diffusion boundary layers, package effect, turgor, and vertical movements) and biotic (grazing, viruses and other parasitoids) factors indicate potential ecological constraints and opportunities that differ among the life forms. There are also variations among life forms in elemental stoichiometry and in allometric relations between biovolume and specific growth. While many of these factors probably have ecological and evolutionary significance, work is needed to establish those that are most important, warranting explicit description in models. Other factors setting limitations on growth rate (selecting slow-growing species) await elucidation.

IS THE GROWTH RATE HYPOTHESIS APPLICABLE TO MICROALGAE?1

The growth rate hypothesis (GRH) asserts, from known biochemistry, that maintaining high growth rates requires high concentrations of ribosomes. Since ribosomes are rich in phosphorus (P), the GRH predicts a positive correlation between growth rate and P content; this correlation is observed in some organisms. We consider the application of the GRH to phytoplankton and identify several key problems that require further research before the hypothesis can be accepted for these organisms. There are severe methodological problems that confound interpretation of data for testing the GRH. These problems include the measurement of protein and nucleic acids (such that ratio of these components carries a high level of uncertainty), studies of steady‐state versus dynamic systems, and the presentation of data per cell (especially as cell size varies with growth rate limitations) and the calculation of growth rates. In addition, because of the short generation times and rapid responses of these organisms to perturbations, ribosome and RNA content is expected to vary in response to (de)repression of various systems; content may increase on application of growth‐limiting stress. Finally, that most phytoplankton accumulate P when not P stressed conflicts with the GRH. In consequence, the value of the GRH for any sort of predictive role in nature appears to be severely limited. We conclude that the GRH cannot be assumed to apply to phytoplankton taxa without first performing experimental tests under transient conditions.

CHANGES IN CELL COMPOSITION AND LIPID METABOLISM MEDIATED BY SODIUM AND NITROGEN AVAILABILITY IN THE MARINE DIATOM PHAEODACTYLUM TRICORNUTUM (BACILLARIOPHYCEAE)1

The effects of nitrogen starvation in the presence or absence of sodium in the culture medium were monitored in batch cultures of the marine diatom Phaeodactylum tricornutum Bohlin. During nitrogen starvation in the presence of sodium, cell nitrogen and chlorophyll a decreased, mainly as a consequence of continued cell division. These decreases were accompanied by decreases in the rates of photosynthesis and respiration. There was no change in either cell volume or carbohydrate, but both carbon and lipid increased. During nitrogen starvation in the absence of sodium, cell division ceased. Cell nitrogen and chlorophyll a remained constant, and respiration did not decrease, but the changes in the photosynthetic rate and the lipid content per cell were similar to cultures that were nitrogen‐starved in the presence of sodium. The carbon‐to‐nitrogen ratio increased in both cultures. Nitrogen, in the form of nitrate, and sodium were resupplied to cultures that had been preconditioned in nitrogen‐ and sodium‐deficient medium for 5 d. Control cultures to which neither nitrate or sodium were added remained in a static state with respect to cell number, volume, and carbohydrate but showed slight increases in lipid. Cells in cultures to which 10 mM nitrate alone was added showed a similar response to cultures where no additions were made. Cells in cultures to which 50 mM sodium alone was added divided for 2 d, with concomitant small decreases in all measured constituents. Cell division resumed in cultures to which both sodium and nitrate were added. The lipid content fell dramatically in these cells and was correlated to metabolic oxidation via measured increases in the activity of the glyoxylate cycle enzyme, isocitrate lyase. We conclude that lipids are stored as a function of decreased growth rate and are metabolized to a small extent when cell division resumes. However, much higher rates of metabolism occur if cell division resumes in the presence of a nitrogen source.

KINETICS OF AMMONIUM ASSIMILATION IN TWO SEAWEEDS, ENTEROMORPHA SP. (CHLOROPHYCEAE) AND OSMUNDARIA COLENSOI (RHODOPHYCEAE)

The kinetics of ammonium assimilation were investigated in two seaweeds from northeastern New Zealand, Enteromorpha sp. (Chlorophyceae, Ulvales) and Osmundaria colensoi (Hook. f. et Harvey) R.E. Norris (Rhodophyceae, Ceramiales), with the use of a recently developed method for measuring assimilation. In contrast to ammonium uptake, which was nonsaturable, ammonium assimilation exhibited Michaelis–Menten kinetics in both species. Maximum rates of assimilation (Vmax) were 27 and 12 μmol·(g DW)−1·h−1 for Enteromorpha sp. and O. colensoi, respectively, with half‐saturation (Km) constants for assimilation of 18 and 41 μM. At environmentally relevant concentrations, assimilation accounted for all of the ammonium taken up by both species. The maximum rate of assimilation in Enteromorpha sp. resembled very closely that of the ammonium assimilatory enzyme, glutamine synthetase, when activities of the latter were measured in the presence of subsaturating substrate (glutamate and ATP) concentrations. Moreover, the initial rate of glutamine production (measured with HPLC) following ammonium enrichment was almost identical to the rates determined above. The rate of ammonium assimilation was therefore determined by three independent methods, two of which involve in vivo measurements, and it is suggested that the use of assimilation kinetics may be useful when examining the nutrient relations of seaweeds.

MEASURING RATES OF AMMONIUM ASSIMILATION IN MARINE ALGAE: USE OF THE PROTONOPHORE CARBONYL CYANIDE m‐CHLOROPHENYLHYDRAZONE TO DISTINGUISH BETWEEN UPTAKE AND ASSIMILATION

A method for determining rates of ammonium assimilation in marine algae is described. Ammonium assimilation is defined as the decrease in total (medium + cellular) ammonium. The protonophore carbonyl cyanide m‐chlorophenylhydrazone (CCCP) was used to distinguish between uptake and assimilation of ammonium. Ammonium uptake by nitrogen‐replete and nitrogen‐starved cells of the diatom Phaeodactylum tricornutum Bohlin and the green macroalga Enteromorpha sp. was completely (98%–99%) inhibited in the presence of 100 μM CCCP. In addition to inhibiting further uptake of ammonium, CCCP promoted the release of unassimilated ammonium by nitrogen‐replete and nitrogen‐starved P. tricornutum and Enteromorpha that had been allowed to take up ammonium for a period. Most (97.5%) of preaccumulated 14C‐methylammonium was released by nitrogen‐starved P. tricornutum in the presence of CCCP. Specific rates of ammonium assimilation in nitrogen‐replete cultures of P. tricornutum were identical to the maximum growth rate, but specific rates in nitrogen‐starved cultures were fourfold greater. Rates of ammonium assimilation in Enteromorpha during both the surge and the internally controlled uptake phases were the same as the internally controlled rate of uptake, suggesting that the latter is a reliable measure of the maximum rate of assimilation.

Changes in amino acid composition of Ulva intestinalis (Chlorophyceae) following addition of ammonium or nitrate

M.W. Taylor, N.G. Barr, C.M. Grant and T.A.V. Rees. 2006. Changes in amino acid composition of Ulva intestinalis (Chlorophyceae) following addition of ammonium or nitrate. Phycologia 45: 270–276. DOI: 10.2216/05-15.1 Nitrogen assimilation was investigated in the marine macroalga Ulva intestinalis. Following incubation of the alga in the presence of ammonium or nitrate, resulting changes in free amino acid content were determined. After 10 h, the largest changes by far occurred in the levels of glutamine and asparagine, which both increased more than 10-fold regardless of nitrogen source. Other amino acids increased slightly, but these two – together with their precursors glutamate and aspartate – comprised 83 and 76% of the total free protein amino acid-N pool upon addition of ammonium or nitrate, respectively. In subsequent time-course experiments, with ammonium as nitrogen source, glutamate initially decreased (with a concomitant increase in glutamine) before recovering to at least its original level. Asparagine levels began to increase after 1 h. Saturation of the glutamine and glutamate pools occurred after approximately 6 h, and coincided with the transition from the surge phase of ammonium uptake to the internally controlled uptake phase. This study represents the first investigation into how levels of specific amino acids change during ammonium assimilation in macroalgae, and as such extends our current knowledge of this poorly understood process.

CONTRASTING EFFECTS OF METHIONINE SULFOXIMINE ON UPTAKE AND ASSIMILATION OF AMMONIUM IN ULVA INTESTINALIS (CHLOROPHYCEAE)

Ammonium is assimilated in algae by the glutamine synthetase (GS)–glutamine:2‐oxoglutarate aminotransferase pathway. In addition to the assimilation of external ammonium taken up across the cell membrane, an alga may have to reassimilate ammonium derived from endogenous sources (i.e. nitrate reduction, photorespiration, and amino acid degradation). Methionine sulfoximine (MSX), an irreversible inhibitor of GS, completely inhibited GS activity in Ulva intestinalis L. after 12 h. However, assimilation of externally derived ammonium was completely inhibited after only 1–2 h in the presence of MSX and was followed by production of endogenous ammonium. However, endogenous ammonium production in U. intestinalis represented only a mean of 4% of total assimilation attributable to GS. The internally controlled rate of ammonium uptake (Vi) was almost completely inhibited in the presence of MSX, suggesting that Vi is a measure of the maximum rate of ammonium assimilation. After complete inhibition of ammonium assimilation in the presence of MSX, the initial or surge (Vs) rate of ammonium uptake in the presence of 400 μM ammonium chloride decreased by only 17%. However, the amount that the rate of ammonium uptake decreased by was very similar to the uninhibited rate of ammonium assimilation. In addition, the decrease in the rate of ammonium uptake in darkness (in the absence of MSX) in the presence of 400 μM ammonium chloride matched the decrease in the rate of ammonium assimilation. However, in the presence of 10 μM ammonium chloride, MSX completely inhibited ammonium assimilation but had no effect on the rate of uptake.

Arrest of cell division but not protein synthesis in sodium-deficient cells of the marine diatom Phaeodactylum tricornutum Bohlin

Cell division in the marine diatom Phaeodactylum tricornutum was prevented when cultures were maintained in the absence of sodium, regardless of the nitrogen status of the cells or medium. Addition of 10 mM ammonium and 50 mM sodium to cultures preconditioned in nitrogen and sodium-deficient medium for 5 d led to a recovery in cell division and chlorophyll a, and net protein synthesis. Sodium added in the absence of ammonium led to a recovery in cell division, but not net protein synthesis. Ammonium added in the absence of sodium was partially assimilated (as NH3) and resulted in a small amount of protein synthesis, but without cell division. This effect was enhanced if the cells had lower protein quotas prior to ammonium addition, with total consumption of the added 1 mM ammonium and appreciable net protein synthesis. Respiration was enhanced by 1 or 10 mM ammonium or 10 mM methylammonium addition to nitrogen-deficient cultures maintained in the presence or absence of sodium. In contrast to respiration, photosynthesis was inhibited by these additions in sodium-replete cultures, but was enhanced in sodium-deficient cultures.

EFFECT OF OLIGOMYCIN ON DARK RESPIRATION IN THE MARINE DIATOM PHAEODACTYLUM TRICORNUTUM (BACILLARIOPHYCEAE): IMPLICATIONS FOR DETERMINATION OF MAINTENANCE RESPIRATION

Oligomycin is an inhibitor of the mitochondrial ATP synthase. In nitrogen‐replete cells of the marine diatom Phaeodactylum tricornutum Bohlin, the rate of dark respiration was high and markedly inhibited (62%–74%) in the presence of oligomycin. In contrast, the rate of dark respiration in nitrogen‐deprived cells was about half that in nitrogen‐replete cells but was only slightly inhibited (16%–30%) by oligomycin. Consistent with these effects on rates of dark respiration, oligomycin decreased the ATP level and the ATP:ADP ratio by about 40% in nitrogen‐replete cells incubated in darkness but had a negligible effect on the ATP level and ATP:ADP ratio in nitrogen‐deprived cells. In sodium and nitrogen‐deprived cells, the rate of dark respiration was greater than that in nitrogen‐replete cells, but there was little effect of oligomycin on the rate of dark respiration. In light‐limited cells, the rate of dark respiration was similar to that in nitrogen‐deprived cells, but the inhibition (57%) in the presence of oligomycin was greater. These results suggest that most of the O2 consumption by nitrogen‐replete cells was linked to mitochondrial ATP synthesis and that the rate of mitochondrial ATP synthesis in nitrogen‐deprived and sodium and nitrogen‐deprived cells was low. The potential implications of these results for our understanding of maintenance respiration are discussed.