Digital recordings of gas-vesicle collapse used to measure turgor pressure and cell-water relations of cyanobacterial cells.

The gas vesicles of the cyanobacterium Microcystis sp. collapse under pressures ranging from 0.65-1.

Cyanobacterial heterocysts: terminal pores proposed as sites of gas exchange.

In many filamentous cyanobacteria, oxygenic photosynthesis is restricted to vegetative cells, whereas N(2) fixation is confined to microoxic heterocysts. The heterocyst has an envelope that provides a barrier to gas exchange: N(2) and O(2) diffuse into heterocysts at similar rates, which ensures that concentrations of N(2) are high enough to saturate N(2) fixation while respiration maintains O(2) at concentrations low enough to prevent nitrogenase inactivation. I propose that the main gas-diffusion pathway is through the terminal pores that connect heterocysts with vegetative cells.

Changes in cell turgor pressure related to uptake of solutes by Microcystis sp. strain 8401.

Uptake of several naturally occurring organic solutes by the unicellular cyanobacterium Microcystis sp. caused changes in cell turgor pressure (p(t)), which was determined by measuring the mean critical pressure (p(c)) of gas vesicles in the cells. Cells had an initial p(t) of 0.

The uptake of amino acids by the cyanobacterium Planktothrix rubescens is stimulated by light at low irradiances.

The rates of uptake of five amino acids--alanine, glutamate, glycine, leucine and serine--by axenic cultures of the cyanobacterium Planktothrix rubescens were measured over a range of irradiances using the (14)C-labelled amino acids at the nanomolar concentrations observed in Lake Zürich. The rates in the light exceeded the dark rates by as much as two- to ninefold. The light-affinity constants for stimulation were similar, indicating a similar process for each of the five amino acids.

Sinking velocities of phytoplankton measured on a stable density gradient by laser scanning.

Two particular difficulties in measuring the sinking velocities of phytoplankton cells are preventing convection within the sedimenting medium and determining the changing depth of the cells. These problems are overcome by using a density-stabilized sedimentation column scanned by a laser. For freshwater species, a suspension of phytoplankton is layered over a vertical density gradient of Percoll solution; as the cells sink down the column their relative concentration is measured by the forward scattering of light from a laser beam that repeatedly scans up and down the column.

Analysis of tryptic digests indicates regions of GvpC that bind to gas vesicles of Anabaena flos-aquae.

The gas vesicles of the cyanobacterium Anabaena flos-aquae contain two main proteins: GvpA, which forms the ribs of the hollow cylindrical shell, and GvpC, which occurs on the outer surface. Analysis by MALDI-TOF MS shows that after incubating Anabaena gas vesicles in trypsin, GvpA was cleaved only at sites near the N-terminus, whereas GvpC was cleaved at most of its potential tryptic sites. Many of the resulting tryptic peptides from GvpC remained attached to the underlying GvpA shell: the pattern of attachment indicated that there are binding sites to GvpA at both ends of the 33-residue repeats (33RRs) in GvpC, although one of the tryptic peptides within the 33RR did not remain attached.

Gas vesicles in actinomycetes?

Gas vesicles encoded by gvp genes provide buoyancy in many prokaryotes. In a recent Trends in Microbiology article entitled 'Gas vesicles in actinomycetes: old buoys in novel habitats?' van Keulen et al. documented the occurrence of gvp genes in soil-inhabiting actinomycetes but questioned whether any of them produce gas vesicles.

The Burgundy-blood phenomenon: a model of buoyancy change explains autumnal waterblooms by Planktothrix rubescens in Lake Zürich.

Buoyancy changes of the cyanobacterium Planktothrix rubescens- the Burgundy-blood alga - were modelled from its buoyancy response to light and irradiance changes in Lake Zürich during autumnal mixing. The daily insolation received by filaments at fixed depths and circulating to different depths was calculated from the measured light attenuation and surface irradiance. The active mixing depth, za5, was determined from the vertical turbulent diffusion coefficient, Kz, calculated from the wind speed, heat flux and temperature gradients.

Stratification by cyanobacteria in lakes: a dynamic buoyancy model indicates size limitations met by Planktothrix rubescens filaments.

The ability of the Planktothrix rubescens to stratify in Lake Zürich is related to the size and shape of the cyanobacterial filaments. Detailed measurements made in the lake are used in a dynamic computer model of buoyancy regulation to investigate the vertical movements of filaments tracking the depth at which the irradiance would support neutral buoyancy. The movement of the filament lags behind the constantly changing target depth owing to (a) the time taken for the filament to respond to the irradiance by changing its density and (b) the time it takes to move by sinking down or floating up through the water column.

The diameter and critical collapse pressure of gas vesicles in Microcystis are correlated with GvpCs of different length.

In cyanobacteria the protein on the outside of the gas vesicle, GvpC, is characterised by the presence of a 33 amino acid residue repeat (33RR), which in some genera is highly conserved. The number of 33RRs correlates with the diameter of the gas vesicle and inversely with its strength. Gas vesicles isolated from Microcystis aeruginosa strain PCC 7806 were found to be wider and have a lower critical collapse pressure than those from Microcystis sp.

Archaea with square cells.

Two groups of microbiologists have independently isolated 'Walsby's square bacterium' from salt crystallizer ponds; its growth depends on pyruvate. Genetic analysis shows that the squares, discovered 25 years ago on the Sinai Peninsula, are archaea rather than bacteria. These transparent tile-like cells might have been dismissed as surface artefacts of salt crystals but for their gas vesicles--structures peculiar to prokaryotic organisms.

Different gvpC length variants are transcribed within single filaments of the cyanobacterium Planktothrix rubescens.

Transcripts of the gas vesicle genes gvpA and gvpC were detected in single filaments of the cyanobacterium Planktothrix rubescens using reverse transcription and quantitative real-time PCR. Primers were designed to amplify short sequences within gvpA and three length variants of gvpC. With genomic template DNA, and using Sybr Green to monitor product accumulation, similar amplification efficiencies were observed for each of these genes.

Spontaneous mutations in gas vesicle genes of Planktothrix spp. affect gas vesicle production and critical pressure.

Wild-type strains of the cyanobacterium Planktothrix rubescens have a cluster of gas vesicle (gvp) genes with repeats of alternating gvpA and gvpC. The gvpC occurs in three length variants, all with the same 3'-sequence, OmegaC. Spontaneous non-buoyant mutants had lost some of the alternating gvpAC copies and their gvpC genes had a novel 3'-end sequence, PsiC; additional gvpC genes terminating in this sequence were also found in the wild-type and representatives of other GV genotypes.

The sequence of the major gas vesicle protein, GvpA, influences the width and strength of halobacterial gas vesicles.

Transformation experiments with Haloferax volcanii show that the amino acid sequence of the gas vesicle protein GvpA influences the morphology and strength of gas vesicles produced by halophilic archaea. A modified expression vector containing p-gvpA was used to complement a Vac(-) strain of Hfx. volcanii that harboured the entire p-vac region (from Halobacterium salinarum PHH1) except for p-gvpA.

The daily integral of growth by Planktothrix rubescens calculated from growth rate in culture and irradiance in Lake Zürich.

In Lake Zürich, populations of the cyanobacterium Planktothrix rubescens develop in the metalimnion during the summer and become gradually entrained in the deepening surface mixed layer during the autumn. It had previously been demonstrated that the daily integrals of photosynthetic production accounted for the growth observed in the metalimnion and greatly exceeded the smaller increase during the autumn. We have now determined the relationship between growth rate (μ) and irradiance (I) in cultures of P.

The selective advantage of buoyancy provided by gas vesicles for planktonic cyanobacteria in the Baltic Sea.

Observations were made on the vertical distribution of colonies of Aphanizomenon flos-aquae for 9 d at a drift-station east of Bornholm Island in the Baltic Sea. The buoyant colonies were dispersed in the upper layers of the water column during periods of wind-induced mixing but floated up during calm periods. From measurements of the vertical light extinction, surface irradiance and the photosynthesis versus irradiance curve, calculations were made of the changes in the daily integral of photosynthesis with respect to time and depth throughout the water column.

Growth competition between strain PHH1 and mutants affected in gas vesicle synthesis.

To investigate the role of the buoyancy provided by gas vesicles in the facultative anaerobe PHH1, the growth of a gas-vacuolate (Gv) strain in competition with two gas-vesicle-defective (Gv) mutants was examined. The Gv strain synthesized gas vesicles throughout its growth cycle, and floated up to form a thick surface scum during the exponential growth phase in static culture. Mutant Gv produced significantly fewer gas vesicles than the Gv strain in corresponding stages of growth, although in late stationary phase a small proportion of cells floated up to the surface of static cultures.