Global aspects of C/N interactions determining plant-environment interactions

The atomic C:N ratio in photolithotrophs is a function of their content of nucleic acids, proteins, lipids, polysaccharides, and other organic materials, and varies from about 5 in some protein-rich microalgae to much higher values in macroalgae and in higher plants with relatively more structural and energy storage materials. These differences in C:N ratios among organisms means that there is more N assimilation by photosynthetic organisms in the oceans than on land despite the near equality of global photosynthetic C assimilation rates in the two environments. Aquatic organisms obtain inorganic C and inorganic N from the surrounding water. Terrestrial photolithotrophs obtain inorganic C, dinitrogen (by diazotrophy) and some combined N from the atmosphere, with the remaining combined N coming from the soil. The nitrogen cost of growth (biomass production rate per unit plant N) varies with the C:N ratio and specific growth rate of the organism. The C:N ratio of plants can be increased with no, or minimal, decrease in growth rate by switching from N-containing to N-free solutes involved in, for example, UV-B screening or by reducing the content of particular proteins. The water cost of growth (water lost per unit biomass gain) in terrestrial plants is a function of N supply and of C supply; water cost is lower with higher N and C availability. Water supply is also important in determining denitrification rates on land and on N (and C) fluxes from terrestrial to aquatic systems.     

Cardiopulmonary baroreflex is reset during dynamic exercise.

The purpose of this study was to examine the hypothesis that the operating point of the cardiopulmonary baroreflex resets to the higher cardiac filling pressure of exercise associated with the increased cardiac filling volumes. Eight men (age 26 +/- 1 yr; height 180 +/- 3 cm; weight 86 +/- 6 kg; means +/- SE) participated in the present study. Lower body negative pressure (LBNP) was applied at 8 and 16 Torr to decrease central venous pressure (CVP) at rest and during steady-state leg cycling at 50% peak oxygen uptake (104 +/- 20 W). Subsequently, two discrete infusions of 25% human serum albumin solution were administered until CVP was increased by 1.8 +/- 0.6 and 2.4 +/- 0.4 mmHg at rest and 2.9 +/- 0.9 and 4.6 +/- 0.9 mmHg during exercise. During all protocols, heart rate, arterial blood pressure, and CVP were recorded continuously. At each stage of LBNP or albumin infusion, forearm blood flow and cardiac output were measured. During exercise, forearm vascular conductance increased from 7.5 +/- 0.5 to 8.7 +/- 0.6 U (P = 0.024) and total systemic vascular conductance from 7.2 +/- 0.2 to 13.5 +/- 0.9 l.min(-1).mmHg(-1) (P < 0.001). However, there was no significant difference in the responses of both forearm vascular conductance and total systemic vascular conductance to LBNP and the infusion of albumin between rest and exercise. These data indicate that the cardiopulmonary baroreflex had been reset during exercise to the new operating point associated with the exercise-induced change in cardiac filling volume.     

Cerebral autoregulation is preserved during orthostatic stress superimposed with systemic hypotension.

We sought to determine whether cerebral autoregulation (CA) is compromised during orthostatic stress superimposed with systemic hypotension. Transient systemic hypotension was produced by deflation of thigh cuffs previously inflated to suprasystolic pressure, combined with or without lower body negative pressure (LBNP). Cardiac output (CO) decreased from a baseline of 5.0+/-0.5 l/min by -8.3+/-1.7, -19.2+/-2.0, and -30.6+/-3.4% during LBNP of -15, -30, and -50 Torr, respectively. Mean arterial pressure (MAP) was maintained during LBNP, despite decreases in systolic and pulse pressures. Middle cerebral arterial blood flow velocity (VMCA) decreased significantly from a baseline of 64+/-3 to 58+/-4 cm/s (-9.7+/-2.4%) at -50 Torr of LBNP. The reduction in VMCA was associated with a decrease in regional cerebral O2 saturation. However, the percent decrease in VMCA was markedly less than that of CO. This suggests that the magnitude of the change in VMCA (an index of cerebral blood flow) is less than would be predicted, given the decrease in CO. Transient systemic hypotension decreased MAP by -21+/-2, -24+/-2, -28+/-3, and -26+/-3% at rest and during LBNP of -15, -30, and -50 Torr, respectively. Likewise, this acute hypotension resulted in decreases in VMCA of -20+/-2, -21+/-2, -24+/-25, and -19+/-2% and regional cerebral O2 saturation of -5+/-1, -6+/-1, -6+/-1, and -7+/-2% at rest and during LBNP of -15, -30, and -50 Torr, respectively. Complete recovery of VMCA to baseline values following transient hypotension (ranging from 5 to 8 s) occurred significantly earlier compared with MAP (from 10 to 12 s). No subjects experienced syncope during acute hypotension. We conclude that CA is preserved during LBNP, superimposed with transient systemic hypotension, despite the decrease in VMCA associated with sustained central hypovolemia in normal healthy individuals. This preserved CA is vital for the prevention of orthostatic syncope.     

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.     

Development of species-specific PCR primer sets for the detection of Leptospira

Spirochetes of the genus Leptospira infect animals and humans and are the causative agents for the emerging infectious disease leptospirosis. Rapid and simple assays for the identification of individual Leptospira species are currently not available. For identification of individual Leptospira species, PCR primers that detect the ompL1 gene sequence for the majority of pathogenic leptospires were developed in this study. The primer pairs detect Leptospira interrogans, Leptospira borgpetersenii, Leptospira kirschneri, Leptospira santarosai, Leptospira weilii and Leptospira noguchii, without cross-reacting with other Leptospira species. The development of the primers revealed a divergence of the ompL1 gene within L. interrogans, splitting this species into two separate groups. The species-specific primers will be especially useful in epidemiological studies and disease outbreak investigations for the detection of Leptospira species in human, animal and environmental samples.     

Limitations on microalgal growth at very low photon fluence rates: the role of energy slippage

The lower limits of photosynthetically useable radiation at which growth and photosynthesis can occur establish the lower boundaries for the extent of photolithotrophy in the biosphere. Photolithotrophic growth denotes the capacity to grow with photons as the sole energy input. Slippage in terms of photosynthetic energy conversion implies a less than theoretical stoichiometry of energy-transduction process(es) such as the dissipation of intermediates of O₂ evolution and of ATP synthesis (H⁺/e⁻ and H⁺/ATP ratios). Slippage is particularly important in limiting the growth of photolithotrophic organisms at very low photon fluence rates. We found that Dunaliella tertiolecta and Phaeodactylum tricornutum avoid such reductions in photon use efficiency by increasing the size and number of their photosynthetic units, respectively, and by altering Q_A reduction kinetics on the reducing side of PS II. P. tricornutum is also less susceptible to slippage in terms of the breakdown of intermediates in its O₂ evolution pathway than D. tertiolecta. Minimizing H⁺ leakage through the CF₀–CF₁ ATP synthetase (and other H⁺ porters) is also discussed briefly. In combination, strategies employed by P.␣tricornutum effectively allow it to grow and photosynthesize at lower rates of energy input than D. tertiolecta, consistent with our observations. Differences in the responses of the photosynthetic apparatus of these two marine microalgae are mechanistic and probably representative of evolutionary divergences associated with strategies for dealing with environmental perturbations.     

Occurrence of 1-glyceryl-1-myo-inosityl phosphate in hyperthermophiles

The accumulation of compatible solutes was studied in the hyperthermophilic bacterium Aquifex pyrophilus as a function of the temperature and the NaCl concentration of the growth medium. Nuclear magnetic resonance analysis of cell extracts revealed the presence of alpha- and beta-glutamate, di-mannosyl-di-myo-inositol phosphate, di-myo-inositol phosphate, and an additional compound here identified as 1-glyceryl-1-myo-inosityl phosphate. All solutes accumulated by A. pyrophilus are negatively charged at physiological pH. The intracellular levels of di-myo-inositol phosphate increased in response to supraoptimal growth temperature, while alpha- and beta-glutamate accumulated in response to osmotic stress, especially at growth temperatures below the optimum. The newly discovered compound, 1-glyceryl-1-myo-inosityl phosphate, appears to play a double role in osmo- and thermoprotection, since its intracellular pool increased primarily in response to a combination of osmotic and heat stresses. This work also uncovered the nature of the unknown compound, previously detected in Archaeoglobus fulgidus (L. O. Martins et al., Appl. Environ. Microbiol. 63:896-902, 1997). The curious structural relationship between diglycerol phosphate (found only in Archaeoglobus species), di-myo-inositol phosphate (a canonical solute of hyperthermophiles), and the newly identified solute is highlighted. This is the first report on the occurrence of 1-glyceryl-1-myo-inosityl phosphate in living systems.     

Occurrence of 1-Glyceryl-1-myo-Inosityl Phosphate in Hyperthermophiles

The accumulation of compatible solutes was studied in the hyperthermophilic bacterium Aquifex pyrophilus as a function of the temperature and the NaCl concentration of the growth medium. Nuclear magnetic resonance analysis of cell extracts revealed the presence of α- and β-glutamate, di-mannosyl-di-myo-inositol phosphate, di-myo-inositol phosphate, and an additional compound here identified as 1-glyceryl-1-myo-inosityl phosphate. All solutes accumulated by A. pyrophilus are negatively charged at physiological pH. The intracellular levels of di-myo-inositol phosphate increased in response to supraoptimal growth temperature, while α- and β-glutamate accumulated in response to osmotic stress, especially at growth temperatures below the optimum. The newly discovered compound, 1-glyceryl-1-myo-inosityl phosphate, appears to play a double role in osmo- and thermoprotection, since its intracellular pool increased primarily in response to a combination of osmotic and heat stresses. This work also uncovered the nature of the unknown compound, previously detected in Archaeoglobus fulgidus (L. O. Martins et al., Appl. Environ. Microbiol. 63:896-902, 1997). The curious structural relationship between diglycerol phosphate (found only in Archaeoglobus species), di-myo-inositol phosphate (a canonical solute of hyperthermophiles), and the newly identified solute is highlighted. This is the first report on the occurrence of 1-glyceryl-1-myo-inosityl phosphate in living systems.     

Mechanisms of compound I formation in heme peroxidases

The formation of compound I is the first step in the reaction mechanism of plant heme peroxidases. This intermediate stores two oxidizing equivalents from hydrogen peroxide as an oxyferryl iron center and a radical, either on the porphyrin ring or on a tryptophan residue. Site-directed mutagenesis has proved to be a most useful tool for the identification of the intermediates involved and the resulting nature of the compound I formed. Although there is no doubt that an acid-base mechanism operates in heme peroxidase during the formation of compound I, the roles of several distal pocket residues are currently the subject of intensive research. It is now generally accepted that the conserved distal histidine in the active site of heme peroxidases is the acid-base catalyst that promotes the heterolytic cleavage of hydrogen peroxide. Other residues, such as the distal arginine and asparagine, participate in a range of roles assisting catalysis by the distal histidine. Recent advances in the elucidation of the mechanism at the molecular level are discussed. Another aspect related to the nature of compound I is the location of the radical center. Novel radical species have been detected in the reactions of ascorbate peroxidase, lignin peroxidase and several mutants of horseradish peroxidase. Detailed kinetic and spectroscopic studies of these radical species have provided important insights about the factors that control porphyrin-protein radical exchange. The wide range of data being obtained on compound I will lead to an understanding of its vital function in peroxidase catalysis and the physiological roles played by these enzymes.     

Algal biogeography: metagenomics shows distribution of a picoplanktonic pelagophyte

How can we determine the distribution of uncultured marine microorganisms? Targeted metagenomics has provided the complete chloroplast genome sequence, and the distribution, for a picoplanktonic pelagophyte alga.