Relationships between phytoplankton dynamics and the availability of light and nutrients in a shallow sub-tropical lake

The role of light and nutrient availability in controlling theabundance and structure of phytoplankton populations was studiedin Lake Okeechobee, a large eutrophic lake in south florida,USA. Measurement of selected environmental parameters at samplingsites within four ecologically distinct regions of the lakewere combined with direct experimental determinations of limitinglevels of light and nutrients for phytoplankton growth to determinespatial and temporal variations in the relative roles of theselimiting factors. Estimated mean light availability in the mixedlayer, I_m, was significantly lower in the turbid central regionof the lake than in other regions. Correlations between I_m andphytoplankton standing crops led to the conclusion that lowlight availability in the central region of the lake, and toa lesser extent in other areas, restricts phytoplankton standingcrops to levels below the potential provided by the nutrientsavailable. The results of the irradiance-growth experimentsconfirmed the conclusions of the correlation analyses that phytoplanktongrowth is restricted by the levels of light availability experiencedduring the winter and spring in the central region of the lake.Bioassays indicated that nitrogen was the most frequently limitingnutrient for phytoplankton growth. High rates of nitrogen fixationwere frequently observed in the lake, along with correspondinglyhigh abundances of nitrogen-fixing cyanobacteria and nitrogenfixation activity. Elevated concentrations of soluble inorganicnitrogen appeared to suppress both nitrogen fixation and therelative abundance of nitrogen-fixing cyanobacteria.     

固氮蓝细菌束毛藻生物固氮策略研究进展

固氮蓝细菌束毛藻(Tricodesmium)是海洋中丰度最高的固氮微生物,贡献了约42%的海洋生物固氮,为海洋生态系统提供了新的氮源,驱动海洋初级生产力和食物网,在海洋生物地球化学循环中发挥重要作用。作为海洋中“新氮”主要贡献者,束毛藻是一种不产生异形胞的丝状固氮蓝细菌。因为生物固氮的关键酶固氮酶对氧气十分敏感,一般固氮蓝细菌通常产生异形胞或采用夜间固氮的方式进行生物固氮,避免氧气对固氮酶的抑制作用。近年来研究发现,束毛藻具有一套独特的生物固氮体系,能够使同一藻丝在白天同时完成光合作用和生物固氮,并具有复杂的调控机制。本文综述了近年来束毛藻生物固氮策略的最新研究进展,介绍了其生物固氮和光合作用之间的精密调控机制,对拓展固氮微生物尤其是海洋蓝细菌固氮机制的认识具有借鉴意义。     

Arrangement of nitrogenase structural genes in an aerobic filamentous nonheterocystous cyanobacterium.

Members of the marine filamentous, nonheterocystous cyanobacterial genus Trichodesmium not only are capable of fixing nitrogen aerobically in the light but when grown under a light-dark cycle will fix nitrogen only during the light phase. In this study, we constructed a restriction map of the structural nitrogen fixation genes (nifHDK) in Trichodesmium sp. strain NIBB 1067. We found that the organization of the nif genes in Trichodesmium sp. strain NIBB 1067 is contiguous, as found in other nonheterocystous cyanobacteria and in heterocysts. Furthermore, the nif gene arrangement was identical when the cultures were grown with combined nitrogen or under nitrogen-fixing conditions. Therefore, no gene rearrangements occur, such as those that occur during the development of heterocysts in heterocystous species.     

Unicellular, aerobic nitrogen-fixing cyanobacteria of the genus Cyanothece.

Two marine, unicellular aerobic nitrogen-fixing cyanobacteria, Cyanothece strain BH63 and Cyanothece strain BH68, were isolated from the intertidal sands of the Texas Gulf coast in enrichment conditions designed to favor rapid growth. By cell morphology, ultrastructure, a GC content of 40%, and aerobic nitrogen fixation ability, these strains were assigned to the genus Cyanothece. These strains can use molecular nitrogen as the sole nitrogen source and are capable of photoheterotrophic growth in the presence of 3-(3,4-dichlorophenyl)-1,1-dimethylurea and glycerol. The strains demonstrated a doubling time of 10 to 14 h in the presence of nitrate and 16 to 20 h under nitrogen-fixing conditions. Rapid growth of nitrogen-fixing cultures can be obtained in continuous light even when the cultures are continuously shaken or bubbled with air. Under 12-h alternating light and dark cycles, the aerobic nitrogenase activity was confined to the dark phase. The typical rates of aerobic nitrogenase activity in Cyanothece strains BH63 and BH68 were 1,140 and 1,097 nmol of C2H2 reduced per mg (dry weight) per h, respectively, and nitrogenase activity was stimulated twofold by light. Ultrastructural observations revealed that numerous inclusion granules formed between the photosynthetic membranes in cells grown under nitrogen-fixing conditions. These Cyanothece strains posses many characteristics that make them particularly attractive for a detailed analysis of the interaction of nitrogen fixation and photosynthesis in an aerobic diazotroph.     

城市景观水体中固氮微生物多样性及固氮活性检测

为探究城市景观水体中固氮微生物群落结构、多样性及固氮活性, 揭示水体中固氮蓝藻的固氮贡献, 研究选取新乡市牧野湖和人民公园水体两个小型水体进行研究。通过理化指标测定, 发现两个水体均处于富营养化状态, 借助高通量测序, 对两水体中微生物的16S rDNA和固氮酶nifH基因进行测序, 并利用乙炔还原法测定水体中固氮微生物的固氮速率。结果表明: 牧野湖水体中的原核生物类群共检测出32个门, 275个属; 固氮微生物共检测出9个门, 66个属。人民公园水体中的原核生物类群共检测出31个门, 238个属; 固氮微生物共检测出4个门, 13个属。固氮蓝藻在两个水体固氮微生物类群中分别占有3%和9.3%, 牧野湖固氮微生物丰富度相对较高, 与人民公园水体固氮微生物多样性差异较大。乙炔还原法测固氮速率结果显示, 两水体均未检测到固氮活性, 推测在富营养化的水体中固氮活性可能被抑制。     

Occurrence of sym-homospermidine as the major polyamine in nitrogen-fixing cyanobacteria

We analyzed the amount of polyamines in a variety of cyanobacteria including nitrogen-fixing and nonfixing species. All the cyanobacteria capable of fixing nitrogen, contained sym-homospermidine as the major polyamine. The concentration of putrescine, spermidine and spermine was extremely low in these cyanobacteria. The cyanobacteria which normally fail to fix nitrogen contained spermidine as the major polyamine, while the sym-homospermidine content was very low or under the limits of detection. Apparently there is a close relationship between the sym-homospermidine content and the ability to fix nitrogen in cyanobacteria.     

Do top-down and bottom-up controls interact to exclude nitrogen-fixing cyanobacteria from the plankton of estuaries? An exploration with a simulation model

Explaining the nearly ubiquitous absence of nitrogen fixation by planktonic organisms in strongly nitrogen-limited estuaries presents a major challenge to aquatic ecologists. In freshwater lakes of moderate productivity, nitrogen limitation is seldom maintained for long since heterocystic, nitrogen-fixing cyanobacteria bloom, fix nitrogen, and alleviate the nitrogen limitation. In marked contrast to lakes, this behavior occurs in only a few estuaries worldwide. Primary production is limited by nitrogen in most temperate estuaries, yet no measurable planktonic nitrogen fixation occurs. In this paper, we present the hypothesis that the absence of planktonic nitrogen fixers from most estuaries is due to an interaction of bottom-up and top-down controls. The availability of Mo, a trace metal required for nitrogen fixation, is lower in estuaries than in freshwater lakes. This is not an absolute physiological constraint against the occurrence of nitrogen-fixing organisms, but the lower Mo availability may slow the growth rate of these organisms. The slower growth rate makes nitrogen-fixing cyanobacteria in estuaries more sensitive to mortality from grazing by zooplankton and benthic organisms.We use a simple, mechanistically based simulation model to explore this hypothesis. The model correctly predicts the timing of the formation of heterocystic, cyanobacterial blooms in freshwater lakes and the magnitude of the rate of nitrogen fixation. The model also correctly predicts that high zooplankton biomasses in freshwaters can partially suppress blooms of nitrogen-fixing cyanobacteria, even in strongly nitrogen-limited lakes. Further, the model indicates that a relatively small and environmentally realistic decrease in Mo availability, such as that which may occur in seawater compared to freshwaters due to sulfate inhibition of Mo assimilation, can suppress blooms of heterocystic cyanobacteria and prevent planktonic nitrogen fixation. For example, the model predicts that at a zooplankton biomass of 0.2 mg l^–1, cyanobacteria will bloom and fix nitrogen in lakes but not in estuaries of full-strength seawater salinity because of the lower Mo availability. Thus, the model provides strong support for our hypothesis that bottom-up and top-down controls may interact to cause the absence of planktonic nitrogen fixation in most estuaries. The model also provides a basis for further exploration of this hypothesis in individual estuarine systems and correctly predicts that planktonic nitrogen fixation can occur in low salinity estuaries, such as the Baltic Sea, where Mo availability is greater than in higher salinity estuaries.     

Sucrose synthase is involved in the conversion of sucrose to polysaccharides in filamentous nitrogen-fixing cyanobacteria

Higher plants and cyanobacteria metabolize sucrose (Suc) by a similar set of enzymes. Suc synthase (SuS, UDP-glucose: D: -fructose 2-alpha-D: -glucosyl transferase, EC 2.4.1.13) catalyses the synthesis and cleavage of Suc, and in higher plants, it plays an important role in polysaccharides biosynthesis and carbon allocation. In this work, we have studied the functional relationship between SuS and the metabolism of polysaccharides in filamentous nitrogen-fixing cyanobacteria. We show that the nitrogen and carbon sources and light regulate the expression of the SuS encoding gene (susA), in a similar way that they regulate the accumulation of polysaccharides. Furthermore, glycogen content in an Anabaena sp. mutant strain with an insertion inactivation of susA was lower than in the wild type strain under diazotrophic conditions, while both glycogen and polysaccharides levels were higher in a mutant strain constitutively overexpressing susA. We also show that there are soluble and membrane-bound forms of SuS in Anabaena. Taken together, these results strongly suggest that SuS is involved in the Suc to polysaccharides conversion according to nutritional and environmental signals in filamentous nitrogen-fixing cyanobacteria.     

Distribution of nitrogen-fixing cyanobacteria (Nostocaceae) during rice cultivation in fertilized and unfertilized paddy fields

This study describes the development of nitrogen-fixing cyanobacteria (Nostocaceae) during different stages of rice seedlings plantation in fertilized and unfertilized paddy fields in north Bihar, India. A heterogeneous population of cyanobacteria was randomly harvested around day 20, 40 and 60 of rice seedlings plantation, and the diversity was analyzed. Thirtytwo species (7 genera) were identified from unfertilized fields, of which Anabaena was represented by 12 species, Anabaenopsis and Aulosira by 3 each, Cylindrospermum by 4, Nostoc by 8 and Aphanizomenon and Nodularia by 1 species each. However, fertilized fields contained only 25 species (7 genera), of which 8 each belonged to Nostoc and Anabaena , 3 to Cylindrospermum , 2 to each Anabaenopsis and Aulosira and 1 to each Aphanizomenon and Nodularia . Although Nostoc and Anabaena were dominant in both fertilized and unfertilized paddy fields, a marked decrease in nitrogen-fixing cyanobacteria was recorded from fertilized fields. In both treatments, the diversity of nitrogen-fixing cyanobacteria was at a maximum around day 60 after seedling plantation. The current study concludes that there is a negative effect of nitrogenous fertilizers on the development of heterocystous cyanobacteria in rice fields. It is proposed that early appearing efficient nitrogen-fixers should be used as nitrogen fertilizers in the management for better establishment and exploitation of heterocystous cyanobacteria for sustainable agricultural practices.     

Study of nitrogen fixation in microbial communities of oil-contaminated marine sediment microcosms

Aerobic microbial degradation of pollutant oil (petroleum) in aquatic environments is often severely limited by the availability of combined nitrogen. We therefore studied whether the microbial community enriched in marine sediment microcosms with an added oil layer and exposure to light harboured nitrogenase activity. The acetylene reduction (AR) assay indeed indicated active nitrogenase; however, similar activity was observed in oil-free control microcosms. In both microcosms, the AR rate was significantly reduced upon a dark shift, indicating that enriched cyanobacteria were the dominant diazotrophs. Analysis of structural dinitrogenase reductase genes (nifH) amplified from both microcosms indeed revealed NifH sequences related mostly to those of heterocystous cyanobacteria. NifH sequences typically affiliating with those of heterotrophic bacteria were more frequently retrieved from the oil-containing sediment. Expression analyses showed that mainly nifH genes similar to those of heterocystous cyanobacteria were expressed in the light. Upon a dark shift, nifH genes related to those of non-heterocystous cyanobacteria were expressed. Expression of nifH assignable to heterotrophs was apparently not significant. It is concluded that cyanobacteria are the main contributors of fixed nitrogen to oil-contaminated and pristine sediments if nitrogen is a limiting factor and if light is available. Hence, also the oil-degrading heterotrophic community may thus receive a significant part of combined nitrogen from cyanobacteria, even though oil vice versa apparently does not stimulate an additional nitrogen fixation in the enriched community.     

Isolation and purification of an axenic diazotrophic drought-tolerant cyanobacterium, Nostoc commune, from natural cyanobacterial crusts and its utilization for field research on soils polluted with radioisotopes

Nitrogen fixation and drought tolerance confer the ability to grow on dry land, and some terrestrial cyanobacteria exhibit these properties. These cyanobacteria were isolated in an axenic form from Nostoc commune clusters and other sources by modifying the method used to isolate the nitrogen-fixing and drought-tolerant cyanobacterium Nostoc sp. HK-01. Of these cyanobacteria, N. commune, which is difficult to isolate and purify, uses polysaccharides to maintain water, nitrogen fertilizers for nitrogen fixation, and can live in extreme environments because of desiccation tolerance. In this study, we examined the use of N. commune as biosoil for space agriculture and possible absorption of radioisotopes ((134)Cs, (137)Cs). This article is part of a Special Issue entitled: Photosynthesis Research for Sustainability: from Natural to Artificial.     

Nitrogen fixation in Arctic vegetation and soils from Svalbard,Norway

Nitrogen fixation was measured by the acetylene reduction method in a high Arctic ecosystem at Kongsfjorden, Spitsbergen (79°N, 12°E). The most important source of biologically fixed nitrogen was found in cyanobacteria either as free living colonies ofNostoc sp. in wet unvegetated or sparsely vegetated grounds or growing as epiphytes on bryophytes. Fixation associated with plant roots or in soil and peat samples had little or no significance for nitrogen input to the ecosystem. The ability to support an epiphytic flora of nitrogen-fixing cyanobacteria varied greatly between bryophyte species.Calliergon richardsonii andSanionia uncinata seemed especially well adapted for harbouring epiphytic cyanobacteria, but the extent of nitrogen fixation varied with the growing location. The rate of nitrogen fixation was greatly influenced by grazing by geese. In a geese-grazing area values were found with a maximum of 693.6±1.5 nmol C₂H₄ h⁻¹ g (dry weight)⁻¹ while the maximum value for ungrazed areas was 65.3±16.6 nmol C₂H₄ h⁻¹ g (dry weight)⁻¹. In the grazed area cyanobacteria were also found fixing nitrogen epiphytically on grass. The high plant productivity, supporting heavy grazing, clearly indicates an effective transfer of fixed nitrogen to the plant community. Under cliffs harbouring colonies of birds, the biological nitrogen fixation was inhibited by bird droppings.     

Low temperature delays timing and enhances the cost of nitrogen fixation in the unicellular cyanobacterium Cyanothece

Marine nitrogen-fixing cyanobacteria are largely confined to the tropical and subtropical ocean. It has been argued that their global biogeographical distribution reflects the physiologically feasible temperature range at which they can perform nitrogen fixation. In this study we refine this line of argumentation for the globally important group of unicellular diazotrophic cyanobacteria, and pose the following two hypotheses: (i) nitrogen fixation is limited by nitrogenase activity at low temperature and by oxygen diffusion at high temperature, which is manifested by a shift from strong to weak temperature dependence of nitrogenase activity, and (ii) high respiration rates are required to maintain very low levels of oxygen for nitrogenase, which results in enhanced respiratory cost per molecule of fixed nitrogen at low temperature. We tested these hypotheses in laboratory experiments with the unicellular cyanobacterium Cyanothece sp. {"type":"entrez-nucleotide","attrs":{"text":"BG043511","term_id":"12489990","term_text":"BG043511"}}BG043511. In line with the first hypothesis, the specific growth rate increased strongly with temperature from 18 to 30 °C, but leveled off at higher temperature under nitrogen-fixing conditions. As predicted by the second hypothesis, the respiratory cost of nitrogen fixation and also the cellular C:N ratio rose sharply at temperatures below 21 °C. In addition, we found that low temperature caused a strong delay in the onset of the nocturnal nitrogenase activity, which shortened the remaining nighttime available for nitrogen fixation. Together, these results point at a lower temperature limit for unicellular nitrogen-fixing cyanobacteria, which offers an explanation for their (sub)tropical distribution and suggests expansion of their biogeographical range by global warming.     

Is the distribution of nitrogen‐fixing cyanobacteria in the oceans related to temperature?

Approximately 50% of the global natural fixation of nitrogen occurs in the oceans supporting a considerable part of the new primary production. Virtually all nitrogen fixation in the ocean occurs in the tropics and subtropics where the surface water temperature is 25°C or higher. It is attributed almost exclusively to cyanobacteria. This is remarkable firstly because diazotrophic cyanobacteria are found in other environments irrespective of temperature and secondly because primary production in temperate and cold oceans is generally limited by nitrogen. Cyanobacteria are oxygenic phototrophic organisms that evolved a variety of strategies protecting nitrogenase from oxygen inactivation. Free-living diazotrophic cyanobacteria in the ocean are of the non-heterocystous type, namely the filamentous Trichodesmium and the unicellular groups A–C. I will argue that warm water is a prerequisite for these diazotrophic organisms because of the low-oxygen solubility and high rates of respiration allowing the organism to maintain anoxic conditions in the nitrogen-fixing cell. Heterocystous cyanobacteria are abundant in freshwater and brackish environments in all climatic zones. The heterocyst cell envelope is a tuneable gas diffusion barrier that optimizes the influx of both oxygen and nitrogen, while maintaining anoxic conditions inside the cell. It is not known why heterocystous cyanobacteria are absent from the temperate and cold oceans and seas.     

Nitrogen Turnover in Marine and Brackish Habitats: I. Nitrogen Fixation

Potential nitrogen-fixing genera were found to be abundant intwo natural populations of blue-green algae, one from a rockycoast and the other from a sand-dune slack. ¹⁵N studies confirmedthat these populations fixed nitrogen in the laboratory andin the field. Preliminary quantitative data on Fixation in thefield suggest that the algae contribute appreciable quantitiesof fixed nitrogen to the environments in which they occur.     

Epilithic cyanobacterial communities of a marine tropical beach rock (Heron Island, Great Barrier Reef): diversity and diazotrophy

The diversity and nitrogenase activity of epilithic marine microbes in a Holocene beach rock (Heron Island, Great Barrier Reef, Australia) with a proposed biological calcification "microbialite" origin were examined. Partial 16S rRNA gene sequences from the dominant mat (a coherent and layered pink-pigmented community spread over the beach rock) and biofilms (nonstratified, differently pigmented microbial communities of small shallow depressions) were retrieved using denaturing gradient gel electrophoresis (DGGE), and a clone library was retrieved from the dominant mat. The 16S rRNA gene sequences and morphological analyses revealed heterogeneity in the cyanobacterial distribution patterns. The nonheterocystous filamentous genus Blennothrix sp., phylogenetically related to Lyngbya, dominated the mat together with unidentified nonheterocystous filaments of members of the Pseudanabaenaceae and the unicellular genus Chroococcidiopsis. The dominance and three-dimensional intertwined distribution of these organisms were confirmed by nonintrusive scanning microscopy. In contrast, the less pronounced biofilms were dominated by the heterocystous cyanobacterial genus Calothrix, two unicellular Entophysalis morphotypes, Lyngbya spp., and members of the Pseudanabaenaceae family. Cytophaga-Flavobacterium-Bacteroides and Alphaproteobacteria phylotypes were also retrieved from the beach rock. The microbial diversity of the dominant mat was accompanied by high nocturnal nitrogenase activities (as determined by in situ acetylene reduction assays). A new DGGE nifH gene optimization approach for cyanobacterial nitrogen fixers showed that the sequences retrieved from the dominant mat were related to nonheterocystous uncultured cyanobacterial phylotypes, only distantly related to sequences of nitrogen-fixing cultured cyanobacteria. These data stress the occurrence and importance of nonheterocystous epilithic cyanobacteria, and it is hypothesized that such epilithic cyanobacteria are the principal nitrogen fixers of the Heron Island beach rock.     

Pattern of cyanophycin accumulation in nitrogen-fixing and non-nitrogen-fixing cyanobacteria

The temporal and spatial accumulation of cyanophycin was studied in two unicellular strains of cyanobacteria, the diazotrophic Cyanothece sp. strain ATCC 51142 and the non-diazotrophic Synechocystis sp. strain PCC 6803. Biochemistry and electron microscopy were used to monitor the dynamics of cyanophycin accumulation under nitrogen-sufficient and nitrogen-deficient conditions. In Cyanothece sp. ATCC 51142 grown under 12 h light/12 h dark nitrogen-fixing conditions, cyanophycin was temporally regulated relative to nitrogenase activity and accumulated in granules after nitrogenase activity commenced. Cyanophycin granules reached a maximum after the peak of nitrogenase activity and eventually were utilized completely. Knock-out mutants were constructed in Synechocystis sp. PCC 6803 cphA and cphB genes to analyze the function of these genes and cyanophycin accumulation under nitrogen-deficient growth conditions. The mutants grew under such conditions, but needed to degrade phycobilisomes as a nitrogen reserve. Granules could be seen in some wild-type cells after treatment with chloramphenicol, but were never found in Delta cphA and Delta cphB mutants. These results led to the conclusion that cyanophycin is temporally and spatially regulated in nitrogen-fixing strains such as Cyanothece sp. ATCC 51142 and represents a key nitrogen reserve in these organisms. However, cyanophycin appeared to play a less important role in the non-diazotrophic unicellular strains and phycobilisomes appeared to be the main nitrogen reserve.     

Modeling culture profiles of the heterocystous N2-fixing cyanobacterium Anabaena flos-aquae

Heterocyst differentiation is a unique feature of nitrogen-fixing cyanobacteria, potentially important for photobiological hydrogen production. Despite the significant advances in genetic investigation on heterocyst differentiation, there were no quantitative culture-level models that describe the effects of cellular activities and cultivation conditions on the heterocyst differentiation. Such a model was developed in this study, incorporating photosynthetic growth of vegetative cells, heterocyst differentiation, self-shading effect on light penetration, and nitrogen fixation. The model parameters were determined by fitting experimental results from the growth of the heterocystous cyanobacterium Anabaena flos-aquae CCAP 1403/13f in media without and with different nitrate concentrations and under continuous illumination of white light at different light intensities (2, 5, 10, 17, 20 and 50 microE m-2 s-1). The model describes the experimental profiles well and gives reasonable predictions even for the transition of growth from that on external N source to that via nitrogen fixation, responding to the change in external N concentrations. The significance and implications of the best-fit values of the model parameters are discussed.     

Bacteroids in the Rhizobium-Legume Symbiosis Inhabit a Plant Internal Lytic Compartment: Implications for other Microbial Endosymbioses

All nitrogen-fixing bacteroids within legume root nodule cellsare surrounded by a host-derived peribacteroid membrane. Componentsof this membrane are supplied directly by the ER and Golgi ofthe host cell. The peribacteroid space lies between the peribacteroidand bacteroid membranes and contains several activities typicallyfound in vacuoles, namely; protease, acid trehalase, alpha-mannosidaseisoenzyme II and protein protease inhibitor. Thus bacteroidsinhabit an environment which fulfils the definition of a lysosome.Since the endosymbiotic organelles are morphologically differentfrom the lytic compartment normally present in a root cortexcell (the central vacuole), it is proposed that they representorgan-specific modifications of lysosomes, analogous to theprotein bodies of seeds. Perisymbiontic membranes are features common to all known plantendosymbioses (involving rhizobia, cyanobacteria, actinomycetes,vesicular-arbuscular mycorrhiza etc.) and the implications ofthis lead to the hypothesis that in all these cases the endosymbiontis compartmentalized within a specialized host lysosome. Key words: Actinomycetes, cyanobacteria, fixed nitrogen, peri-bacteroid/symbiont membrane/space, protein bodies, vesiculararbuscular mycorrhiza     

A cyanobacterial recombination study, involving an efficient N2-fixing non-heterocystous partner

Many filamentous cyanobacteria fix atmospheric nitrogen under natural conditions in specialized anaerobic compartments, heterocysts, interspersed between vegetative cells, which provide protection to the O2-sensitive nitrogenase. A few unicellular cyanobacterial strains are also known to fix nitrogen aerobically at a slower rate. Filamentous cyanobacteria lacking heterocysts are not known so far to fix nitrogen. We describe the isolation and purification of a non-heterocystous filamentous cyanobacterium from the fronds of the water-fern Azolla, fixing nitrogen at 18.7+/-0.2 n moles ethylene microg Chl. a(-1) h(-1) when grown in nitrogen-free medium at a low level of oxygen between two layers of agar. This strain of Anabaena azollae has been designated as het- nif+ (non-heterocystous and nitrogen-fixing), and is found to be easily and effectively preserved in nitrogen-free medium in standard synthetic cyanobacterial nutrient medium (pH 8.5) at a continuous light intensity of 2800 lx at 25+/-1 degrees C. This het- nif+ strain is an effective donor of the nif+ marker to a het+ nif- strain of another cyanobacterium, Nostoc muscorum, when both are grown together in a recombination study.