CaCO3 nucleation by cyanobacteria: laboratory evidence for a passive, surface-induced mechanism

Calcite nucleation on the surface of cyanobacteria of the Synechococcus leopoliensis strain PCC 7942 was investigated to assess the influence of photosynthetic uptake of inorganic carbon and active ion exchange processes across the cell membrane on the nucleation and precipitation mechanisms. We performed long-term precipitation experiments at a constant CO₂ level in ambient air by adding suspensions of previously washed cyanobacteria to solutions of NaHCO₃/CaCl₂ which were supersaturated with respect to calcite. Induction times between 4 and 110 h were measured over a range of saturation states, Ω, between 8 and 4. The kinetics of CaCO₃ nucleation was compared between experiments: (i) with ongoing photosynthesis, (ii) with cells metabolizing but not undergoing photosynthetic uptake of inorganic carbon and (iii) in darkness without photosynthesis. No significant differences were observed between the three treatments. The results reveal that under low nutrient concentrations and permanent CO₂ supply, photosynthetic uptake of inorganic carbon predominantly uses CO₂ and consequently does not directly influence the nucleation process of CaCO₃ at the surface of S. leopoliensis. Furthermore, ion exchange processes did not affect the kinetics, indicating a passive nucleation process wherein the cell surface or extracellular polymers provided preferential sites for mineral nucleation. The catalyzing effect of the cyanobacteria on calcite nucleation was equivalent to a ∼18% reduction in the specific interfacial free energy of the calcite nuclei. This result and the ubiquitous abundance of cyanobacteria suggest that this process may have an impact on local and global carbon cycling.     

Bacterially mediated precipitation in marine stromatolites

Stromatolites are laminated, lithified (CaCO₃) sedimentary deposits formed by precipitation and/or sediment accretion by cyanobacterial–bacterial mat communities. Stromatolites have been associated with these communities as far back as the Precambrian era some 2+ billion years ago. The means by which microbial communities mediate the precipitation processes have remained unclear, and are the subject of considerable debate and speculation. Two alternative explanations for microbially mediated precipitation include: (i) cyanobacterial photosynthesis increases pH in a system supersaturated in respect of CaCO₃, resulting in CaCO₃ precipitation and then laminated lithification, and (ii) decomposition of cyanobacterial extracellular organic matter (e.g. sheaths, mucilage and organic acids) by microheterotrophs leads to release of organic-bound Ca²⁺ ions and CaCO₃ precipitation. We evaluated these explanations by examining metabolically active, lithifying stromatolitic mat communities from Highborne Cay, Bahamas, using microautoradiography. Microautoradiographic detection of ¹⁴CO₂ fixation and ³H organic matter ( d -glucose and an amino acid mixture) utilization by photosynthetically active cyanobacteria and microheterotrophs, combined with community-level uptake experiments, indicate that bacteria, rather than cyanobacteria are the dominant sites of CaCO₃ deposition. In the oligotrophic waters in which stromatolites exist, microheterotrophs are reliant on the photosynthetic community as a main source of organic matter. Therefore, autotrophic production indirectly controls microbially mediated precipitation and stromatolite formation in these shallow marine environments.     

Modification of the pII protein in response to carbon and nitrogen availability in filamentous heterocystous cyanobacteria

Abstract In the filamentous cyanobacterium Calothrix PCC 7504, which fixes N₂ aerobically, the modification state of the regulatory P_II protein (GlnB) was shown to depend on nitrogen and carbon availability, as observed in the unicellular non-fixing strain Synechococcus PCC 7942. However, the conditions for modifications, the time dependence of the process and the electrophoretic behavior of the native P_II isoforms differed somewhat between the two strains. In another strain, Calothrix PCC 7601, which has lost the capability to fix N₂, P_II was modified only if ammonia plus an inhibitor of glutamine synthetase were present. It is proposed that: (i) the behavior of the P_II proteins depends upon the physiological properties of the strains; and (ii) the modification system of P_II per se may differ between the two cyanobacterial genera.     

ISOLATION OF ccmKLMN GENES FROM THE MARINE CYANOBACTERIUM, SYNECHOCOCCUS SP. PCC7002 (CYANOPHYCEAE), AND EVIDENCE THAT CcmM IS ESSENTIAL FOR CARBOXYSOME ASSEMBLY

A high CO₂ requiring mutant of the marine cyanobacterium Synechococcus PCC7002 was generated using a random gene-tagging procedure. This mutant demonstrated a reduced photosynthetic affinity for inorganic carbon (C_i) and accumulated high internal levels of C_i that could not be used for photosynthesis. Analysis of the mutant genomic DNA showed that the mutagenesis had disrupted a cluster of genes involved in the cyanobacterial CO₂ concentrating mechanism (CCM), the so-called ccm genes. These characteristics are consistent with a cyanobacterial mutant with defects in carboxysome assembly and/or functioning. Further genomic analyses indicated that the genes of the Synechococcus PCC7002 operon, ccmKLMN , are structurally similar to those of two closely related cyanobacteria, Synechococcus PCC7942 and Synechocystis PCC6803. The Synechococcus PCC7002 ccmM gene, which encodes a polypeptide with a predicted size of 70 kDa, was the direct target of the mutagenesis event. The CcmM protein has two distinct regions: an N-terminal region that shows similarity to an archaeon gamma carbonic anhydrase and a C-terminal region that contains repeated domains demonstrating sequence similarity to the small subunit of Rubisco. Physiological analysis of a ccmM -defined mutant showed that these cells were essentially identical to the original mutant; they required high CO₂ concentrations for growth, they had a low photosynthetic affinity for C_i, and they internalized C_i to high levels. Moreover, ultrastructural examination showed that both the original and the defined mutants lack carboxysomes. Thus, our results demonstrate that the ccmM gene of Synechococcus PCC7002 encodes a polypeptide that is essential for carboxysome assembly and therefore for proper functioning of the cyanobacterial CCM.     

Characteristics and turnover of exopolymeric substances in a hypersaline microbial mat

The properties and microbial turnover of exopolymeric substances (EPS) were measured in a hypersaline nonlithifying microbial mat (Eleuthera, Bahamas) to investigate their potential role in calcium carbonate (CaCO₃) precipitation. Depth profiles of EPS abundance and enzyme activities indicated that c . 80% of the EPS were turned over in the upper 15–20 mm. Oxic and anoxic mat homogenates amended with low-molecular-weight (LMW) organic carbon, sugar monomers, and different types of EPS revealed rapid consumption of all substrates. When comparing the consumption of EPS with that of other substrates, only marginally longer lag times and lower rates were observed. EPS (5–8%) were readily consumed during the conversion of labile to refractory EPS. This coincided with a decrease in glucosidase activity and a decrease in the number of acidic functional groups on the EPS. Approximately half of the calcium bound to the EPS remained after 10 dialyses steps. This tightly bound calcium was readily available to precipitate as CaCO₃. We present a conceptual model in which LMW organic carbon complexed with the tightly bound calcium is released upon enzyme activity. This increases alkalinity and creates binding sites for carbonate and allows CaCO₃ to precipitate. Therefore, this model explains interactions between EPS and CaCO₃ precipitation, and underscores the critical role of aerobic and anaerobic microorganisms in early diagenesis and lithification processes.     

Immunolocalization of the uptake hydrogenase in the marine cyanobacterium Lyngbya majuscula CCAP 1446/4 and two Nostoc strains

In N₂-fixing cyanobacteria, the reduction of N₂ to NH₃ is coupled with the production of molecular hydrogen, which is rapidly consumed by an uptake hydrogenase, an enzyme that is present in almost all diazotrophic cyanobacteria. The cellular and subcellular localization of the cyanobacterial uptake hydrogenase remains uncertain, and it is definitely strain dependent. Previous studies focused mainly on heterocystous cyanobacteria and used heterologous antisera. The present work represents the first effort to establish the subcellular localization of the uptake hydrogenase in a N₂-fixing filamentous nonheterocystous cyanobacterium, Lyngbya majuscula CCAP 1446/4, using the first antiserum produced against a cyanobacterial uptake hydrogenase. The data obtained revealed higher specific labelling associated with the thylakoid membranes of L. majuscula , reinforcing the idea that the cyanobacterial uptake hydrogenase is indeed a membrane-bound protein. For comparative purposes, the localization of the uptake hydrogenase was also investigated in two distinct heterocystous cyanobacterial strains, and while in Nostoc sp. PCC 7120 the labelling was only observed in the heterocysts, in Nostoc punctiforme , the presence of uptake hydrogenase antigens was detected in both the vegetative cells and heterocysts, corresponding most probably to an inactive and an active form of the enzyme.     

Monitoring of phosphorus bioavailability in water by an immobilized luminescent cyanobacterial reporter strain

Massive growth of cyanobacteria, known as ‘algal blooms’, has become a major concern for water monitoring. It has been observed that environmental factors like temperature, light, and certain patterns of availability of nutrients such as P, N, Fe influence cyanobacterial proliferation and toxin production. In order to monitor nutrients in aquatic ecosystems, an assay for monitoring phosphorus bioavailability to cyanobacteria was developed. The test consists of an immobilized luminescent reporter strain of Synechococcus PCC 7942, designated APL. The reporter strain harbours the gene coding the reporter protein luciferase from Vibrio harveyi under control of the inducible alkaline phosphatase promoter from Synechococcus PCC 7942, and can be induced under phosphorus limitation. The resultant CyanoSensor detects PO₄³⁻−P in a concentration range of 0.3–8 μM after a sample incubation time of 8 h under continuous illumination (50 μE m⁻² s⁻¹). The sensor also responded to a variety of organic phosphorus sources and was storable for 3 weeks at 4 °C. It could be demonstrated that the CyanoSensor for bioavailability monitoring is an improvement to conventional phosphorus detection methods.     

Calcification in aquatic plants

Abstract. The CaCO₃ deposits of aquatic plants may be intra-, inter- and extracellular. Calcification is mainly the result of photosynthetic CO₂ or HCO⁻₃ assimilation. This raises the local pH and CO²⁻₃ concentration resulting from shifts in the dissolved inorganic carbon equilibrium, due to either net CO₂ depletion as in Halimeda or localized OH⁻ efflux (or H⁺ influx) as in Chara. The plant cell wall may be important in CaCO₃ nucleation by acting as an epitaxial substratum or template, or by creating a microenvironment enriched in Ca²⁺ compared to Mg²⁺. Hypotheses on the reason for the lack of calcification in many aquatic plants are presented.     

A method to probe the cytoplasmic osmolality and osmotic water and solute fluxes across the cell membrane of cyanobacteria with chlorophyll a fluorescence: Experiments with Synechococcus sp. PCC7942

We present a method with which osmotic properties of the cytoplasm of cyanobacterial cells and the osmotic permeability of plasma membranes to water and solutes can be assessed from measurements of chlorophyll a fluorescence. When the electron transport of photosystem II is inhibited, the quantum yield of chlorophyll a fluorescence in cyanobacterial cells varied between a low yield limit that was attained after acclimation to darkness (state 2) and a high yield limit that was attained after acclimation to light (state 1). It was shown recently that the difference between chlorophyll a fluorescence of light‐acclimated and of dark‐acclimated cells relates quantitatively to the internal osmolality of cyanobacteria (G. C. Papageorgiou and A. Alygizaki‐Zorba. 1997. Biochim. Biophys. Acta 1335: 1‐4). In the present work we employed rapid mixing of Synechococcus sp. PCC7942 (strain PAMCOD) suspensions with solutions of defined osmolality in order to measure cell osmolality and turgor threshold, as well as water and solute fluxes across cell membranes. Concentration upshocks with sorbitol, glycine betaine, Na⁺ and K⁺ salts caused rapid (t_1/2 < 10 ms) depression of fluorescence that was correlated to osmotic water outflow from the cells. The fluorescence remained depressed in all cases except for NaCl. With NaCl, the depression was transient and fluorescence recovered with an apparent time constant of 200 ms. The fluorescence rise correlates to inflows of NaCl and water.     

Overproduction and easy recovery of target gene products from cyanobacteria, photosynthesizing microorganisms

New cyanobacterial expression vectors, possessing an origin of replication that functions in a broad range of Gram-negative bacteria, were constructed. To inspect the shuttle vectors, the gene gfp was cloned downstream from the expression control element (ECE) originating from the regulatory region of the Microcystis aeruginosa gene psbA2 (for photosystem II D1 protein), and the vectors were introduced into three kinds of cyanobacteria (Synechocystis sp. PCC 6803, Synechococcus elongatus PCC 7942, and Limnothrix/Pseudanabaena sp. ABRG5-3) by conjugation. Multiple copy numbers of the expression vectors (in the range of 14-25 copies per cell) and a high expression of green fluorescent protein (GFP) at the RNA/protein level were observed in the cyanobacterial transconjugants. Importantly, GFP was observed in a supernatant from the autolysed transconjugants of ABRG5-3 and easily collected from the supernatant without centrifugation and/or further cell lysis. These results indicate the vectors together with the recombinant cells to be useful for overproducing and recovering target gene products from cyanobacteria.     

Biodegradation of organophosphate pesticide using recombinant Cyanobacteria with surface- and intracellular-expressed organophosphorus hydrolase

The opd gene, encoding organophosphorus hydrolase (OPH) from Flavobacterium sp. capable of degrading a wide range of organophosphate pesticides, was surface- and intracellular-expressed in Synechococcus PCC7942, a prime example of photoautotrophic cyanobacteria. OPH was displayed on the cyanobacterial cell surface using the truncated ice nucleation protein as an anchoring motif. A minor fraction of OPH was displayed onto the outermost surface of cyanobacterial cells, as verified by immunostaining visualized under confocal laser scanning microscopy and OPH activity analysis; however, a substantial fraction of OPH was buried in the cell wall, as demonstrated by proteinase K and lysozyme treatments. The cyanobacterial outer membrane acts as a substrate (paraoxon) diffusion barrier affecting whole-cell biodegradation efficiency. After freeze-thaw treatment, permeabilized whole cells with intracellular-expressed OPH exhibited 14-fold higher bioconversion efficiency (Vmax/Km) than that of cells with surface-expressed OPH. As cyanobacteria have simple growth requirements and are inexpensive to maintain, expression of OPH in cyanobacteria may lead to the development of a lowcost and low-maintenance biocatalyst that is useful for detoxification of organophosphate pesticides.     

A comparison of gene organization in the zwf region of the genomes of the cyanobacteria Synechococcus sp. PCC 7942 and Anabaena sp. PCC 7120

Abstract The region of the genome encoding the glucose-6-phosphate dehydrogenase gene zwf was analysed in a unicellular cyanobacterium, Synechococcus sp. PCC 7942, and a filamentous, heterocystous cyanobacterium, Anabaena sp. PCC 7120. Comparison of cyanobacterial zwf sequences revealed the presence of two absolutely conserved cysteine residues which may be implicated in the light/dark control of enzyme activity. The presence in both strains of a gene fbp , encoding fructose-1,6-bisphosphatase, upstream from zwf strongly suggests that the oxidative pentose phosphate pathway in these organisms may function to completely oxidize glucose 6-phosphate to CO₂. The amino acid sequence of fructose-1,6-bisphosphatase does not support the idea of its light activation by a thiol/disulfide exchange mechanism. In the case of Anabaena sp. PCC 7120, the tal gene, encoding transaldolase, lies between zwf and fbp .     

Inhibitory Effect of Omeprazole, a Specific Inhibitor of H+, K+-ATPase, on Spicule Formation in Sea Urchin Embryos and in Cultured Micromere-Derived Cells.

Embryos kept with omeprazole, a specific H⁺, K⁺-ATPase inhibitor, in a period of development between the mesenchyme blastula and the pluteus corresponding stage became abnormal plutei having quite small spicules, somewhat poor pluteus arms and apparently normal archenterons. In micro-mere-derived cells, kept with omeprazole at pH 8.2 in a period between 15 and 40 hr of culture at 20°C, omeprazole strongly inhibited spicule formation but did not block the outgrowth of pseudopodial cables, in which spicule rods were to be formed. These indicate that omeprazole probably exerts no obvious inhibitory effects other than spicule rods formation. Omeprazole-sensitive H⁺, K⁺-ATPase, an H⁺pump, seems to be indispensable for CaCO₃ deposition (formation of spicule rod) in these spicule forming cells. H⁺, produced in overall reaction for CaCO₃ formation: Ca²⁺+ CO₂+H₂O°CaCO₃+2H⁺, is probably released from the cells by this H⁺pump and hence, this reaction tends to go to CaCO₃ production to form spicule rods. Omeprazole, known to become effective following its conversion to a specific inhibitor of H⁺, K⁺-ATPase at acidic pH, is able to inhibit formation of spicule rod at alkaline pH in sea water. This is probably due to an acidification of sea water near the cell surface by H⁺ejection in H⁺, K⁺-ATPase reaction.     

Soft X-ray spectromicroscopy of nickel sorption in a natural river biofilm

Scanning transmission X-ray microscopy (STXM) at the C 1s, O 1s, Ni 2p, Ca 2p, Mn 2p, Fe 2p, Mg 1s, Al 1s and Si 1s edges was used to study Ni sorption in a complex natural river biofilm. The 10-week grown river biofilm was exposed to 10 mg L⁻¹ Ni²⁺ (as NiCl₂) for 24 h. The region of the biofilm examined was dominated by filamentous structures, which were interpreted as the discarded sheaths of filamentous bacteria, as well as a sparse distribution of rod-shaped bacteria. The region also contained discrete particles with spectra similar to those of muscovite, SiO₂ and CaCO₃. The Ni(II) ions were selectively adsorbed by the sheaths of the filamentous bacteria. The sheaths were observed to be metal rich with significant amounts of Ca, Fe and Mn, along with the Ni. In addition, the sheaths had a large silicate content but little organic material. The metal content of the rod-shaped bacterial cells was much lower. The Fe on the sheath was mainly in the Fe(III) oxidation state. Mn was found in II, III and IV oxidation states. The Ni was likely sorbed to Mn–Fe minerals on the sheath. These STXM results have probed nano-scale biogeochemistry associated with bacterial species in a complex, natural biofilm community. They have implications for selective Ni contamination of the food chain and for developing bioremediation strategies.     

Amino acid transport in taxonomically diverse cyanobacteria and identification of two genes encoding elements of a neutral amino acid permease putatively involved in recapture of leaked hydrophobic amino acids.

The activities of uptake of thirteen 14C-labeled amino acids were determined in nine cyanobacteria, including the unicellular strains Synechococcus sp. strain PCC 7942 and Synechocystis sp. strain PCC 6803; the filamentous strain Pseudanabaena sp. strain PCC 6903, and the filamentous, heterocyst-forming strains Anabaena sp. strains PCC 7120 and PCC 7937; Nostoc sp. strains PCC 7413 and PCC 7107; Calothrix sp. strain PCC 7601 (which is a mutant unable to develop heterocysts); and Fischerella muscicola UTEX 1829. Amino acid transport mutants, selected as mutants resistant to some amino acid analogs, were isolated from the Anabaena, Nostoc, Calothrix, and Pseudanabaena strains. All of the tested cyanobacteria bear at least a neutral amino acid transport system, and some strains also bear transport systems specific for basic or acidic amino acids. Two genes, natA and natB, encoding elements (conserved component, NatA, and periplasmic binding protein, NatB) of an ABC-type permease for neutral amino acids were identified by insertional mutagenesis of strain PCC 6803 open reading frames from the recently published genomic DNA sequence of this cyanobacterium. DNA sequences homologous to natA and natB from strain PCC 6803 were detected by hybridization in eight cyanobacterial strains tested. Mutants unable to transport neutral amino acids, including natA and natB insertional mutants, accumulated in the extracellular medium a set of amino acids that always included Ala, Val, Phe, Ile, and Leu. A general role for a cyanobacterial neutral amino acid permease in recapture of hydrophobic amino acids leaked from the cells is suggested.     

Engineering Synechococcus elongatus PCC 7942 for Continuous Growth under Diurnal Conditions

Synechococcus elongatus strain PCC 7942 strictly depends upon the generation of photosynthetically derived energy for growth and is incapable of biomass increase in the absence of light energy. Obligate phototrophs'' core metabolism is very similar to that of heterotrophic counterparts exhibiting diverse trophic behavior. Most characterized cyanobacterial species are obligate photoautotrophs under examined conditions. Here we determine that sugar transporter systems are the necessary genetic factors in order for a model cyanobacterium, Synechococcus elongatus PCC 7942, to grow continuously under diurnal (light/dark) conditions using saccharides such as glucose, xylose, and sucrose. While the universal causes of obligate photoautotrophy may be diverse, installing sugar transporters provides new insight into the mode of obligate photoautotrophy for cyanobacteria. Moreover, cyanobacterial chemical production has gained increased attention. However, this obligate phototroph is incapable of product formation in the absence of light. Thus, converting an obligate photoautotroph to a heterotroph is desirable for more efficient, economical, and controllable production systems.     

Cyanobacterial NDH-1 complexes: multiplicity in function and subunit composition

In cyanobacteria, the NAD(P)H:quinone oxidoreductase (NDH-1) is involved in a variety of functions like respiration, cyclic electron flow around PSI and CO₂ uptake. Several types of NDH-1 complexes, which differ in structure and are responsible for these functions, exist in cyanobacterial membranes. This minireview is based on data obtained by reverse genetics and proteomics studies and focuses on the structural and functional differences of the two types of cyanobacterial NDH-1 complexes: NDH-1L, important for respiration and PSI cyclic electron flow, and NDH-1MS, the low-CO₂ inducible complex participating in CO₂ uptake. The NDH-1 complexes in cyanobacteria share a common NDH-1M 'core' complex and differ in the composition of the distal membrane domain composed of specific NdhD and NdhF proteins, which in complexes involved in CO₂ uptake is further associated with the hydrophilic carbon uptake (CUP) domain. At present, however, very important questions concerning the nature of catalytically active subunits that constitute the electron input device (like NADH dehydrogenase module of the eubacterial 'model' NDH-1 analogs), the substrate specificity and reaction mechanisms of cyanobacterial complexes remain unanswered and are shortly discussed here.     

Interaction of boron and calcium in the cyanobacteria Anabaena and Synechococcus

Although some studies have reported an interaction between boron (B) and calcium (Ca²⁺) in higher plants, there is little evidence for a similar relationship in cyanobacteria. The present study was designed to determine the effect of a supplement of boron to Ca²⁺-deficient cultures of Anabaena PCC 7119 and Synechococcus PCC 7942. Grown under Ca²⁺ deprivation, Anabaena had a slow growth rate and a low photosynthetic pigment content that was related to an inhibition of photosynthesis. Ca²⁺-deficient cells showed a lack of cohesiveness of the heterocyst envelope layers, which was consistent with a rapid decline in nitrogenase activity. A supplement of B led to partial recovery from the effects caused by lack of Ca²⁺. Similarly, low Ca²⁺ had inhibitory effects on growth and metabolism of Synechococcus cultures. In this case, the effect of a B supplement depended on the concentration of Ca²⁺ in the growth medium. When Ca²⁺ was present at normal concentration. B was not required, at least no more than trace amounts. However, when the Ca²⁺ concentration decreased, B was required at increasing levels. An effect of boron on uptake and/or on the binding of Ca²⁺ in cyanobacteria is proposed.