Back to the title page | E-thesis main page

1. Introduction

1.1 Cyanobacteria

Cyanobacterial evolution begun at least 2000 million years ago according to paleontological data (Hofmann, 1976 and Knoll & Golubic, 1991: cited by Golubic et al. , 1995). Cyanobacteria are a morphologically diverse group of oxygenic photosynthetic prokaryotes (Rippka et al. , 1979), which are phylogenetically closely related to each other and to chloroplasts (Giovannoni et al. , 1988). Chloroplasts have originated from cyanobacteria by one or more endosymbiotic events between non-photosynthetic eukaryotic organisms and cyanobacteria (Douglas, 1994).

Cyanobacteria and oxygenic Eukaryotes, algae and plants, have generated oxygen in the earth’s atmosphere. Atmospheric oxygen concentrations were high enough to promote the selection of heterocystous cyanobacteria approximately 2100 million years ago based on chemical analysis of ancient weathering profiles (Holland & Beukes, 1990: cited by Golubic et al. , 1995). The molecular phylogenetic study of Giovannoni et al. (1988) has shown that the last diverging cyanobacterial groups were the heterocystous groups in which the nitrogen (N) fixing enzyme, nitrogenase, was protected from oxygen in heterocysts.

 

1.1.1 Geographic and ecological distribution of cyanobacteria

Due to their early evolutionary history, cyanobacteria occur abundantly in a wide range of habitats (Schopf, 1994). Cyanobacteria are known as freshwater (Hoffmann, 1996) and marine (Hoffmann, 1994) organisms, and in addition, especially the filamentous forms, also occupy a variety of terrestrial habitats (Hoffmann, 1989). Cyanobacteria form symbiotic associations with a wide range of organisms: algae, fungi, pteridophytes, gymnosperms, angiosperms, some animals, bacteria, and non-photosynthetic protists. In these associations, the cyanobacterial symbionts (cyanobionts) are usually heterocystous and filamentous forms. Nostoc is commonly found, but also Anabaena , Calothrix , Fischerella , and Scytonema spp. have been observed in symbiotic associations (Rowell & Kerby, 1991).

The filamentous heterocystous Nodularia , the main object of this thesis, occurs in saline and brackish waters and in soil all over the world (Table 1). Aphanizomenon , which was also studied in this thesis, lives in both fresh (Sivonen et al. , 1990; Paerl, 1996) and brackish waters (Hällfors, 1979; Edler et al. , 1984).

 

Table 1. Geographical and ecological distribution of the cyanobacterium Nodularia .

Location Description of the source
(identification of species)
Reference
Saline aquatic environments    
Africa:    
- Banagher Pan, South-Africa Saline pond ( N. spumigena var. vacuolaria ) Hutchinson et al. , 1932
- South Africa, Namibia, Botswana, Zimbabwe, and Mozambique Saline lakes ( N. spumigena ) Seaman et al ., 1991
Antarctica:    
- South Shetland Islands Unknown source ( N. harveyana ) Komárek et al. , 1999
- Wilkes Saline lakes and ponds ( Nodularia sp.) Wright & Burton, 1981
Australia:    
- Lake Alexandrina, and Lake Albert, South Australia Saline lakes ( N. spumigena ) Francis 1878; Baker & Humpage, 1994
- Lake Ellesmere, New Zealand Saline lake ( N. spumigena ) Carmichael et al. , 1988
- Lake Corangamite and Lake Coraculac, Victoria Saline lakes ( N. spumigena ) Hammer, 1981
- Orielton Lagoon, Tasmania Coastal embayment ( N. spumigena ) Jones et al. , 1994b
- Peel-Harvey Estuary, Western Australia Estuarine ( Nodularia sp.) Lukatelich & McComb, 1986
Central America:    
- Alchichica, Puebla State, Mexico Volcanic saline lake ( N. cf. spumigena ) Tavera & Komárek, 1996
North America:    
- Walker Lake, Nevada, USA Terminal saline lake ( N. spumigena ) Cooper & Koch, 1984
- Pyramid Lake, Nevada, USA Terminal desert lake ( N. spumigena ) Galat et al. , 1981
- British Columbia and Saskatchewan, Canada Saline lakes and ponds ( N. spumigena ) Hammer et al. , 1983
- Basin, Redberry, Deadmoose, Whiteshore, and Manito lakes, Saskatchewan, Canada Saline lakes ( N. spumigena , N. harveyana ) Nordin & Stein, 1980
- Big Quill Lake, Saskatchewan, Canada Saline lake ( N. spumigena ) Nordin & Stein, 1980
- Riefel Wildlife Refuge, British Columbia, Canada Coastal water ( N. harveyana ) Nordin & Stein, 1980
- Sande Fuca and Devis Lake, Washington, USA

Coastal waters ( N. spumigena , N. harveyana )

Nordin & Stein, 1980
- Great Salt Lake, Utah, USA Terminal desert lake ( N. spumigena ) Stephens, 1990
South America:    
- Castillos lagoon, Uruguay Coastal water ( N. baltica-spumigena type) del Carmen Pérez et al. , 1999
Central and Southwest Asia:    
- Balkash Lake and Lake Aral, Kazakhstan/Uzbekistan Saline tectonic lakes ( N. spumigena ) Ergashev, 1979
- the Sea of Azov, Ukraina Brackish water ( N. spumigena f. typica ) Zenkevitch, 1963
- the Caspian Sea

Brackish water ( N. spumigena , N. harveyana )

Zenkevitch, 1963
Europe:    
- Bafra Balik Gölleri (Balik Gölü, Uzun Göl), Turkey

Unknown source ( N. spumigena , N. harveyana )

Gönülol & Comak, 1992
- the Baltic Sea, Europe

Brackish water ( N. spumigena , N. harveyana )

Hällfors, 1979; Edler et al. , 1984
- Banter See, Wilhelmshaven, Germany Brackish lake ( N. spumigena ) Nehring, 1993
- The Gulf of St. Eufemia, the Mediterranean Sea, Italy Brackish water ( N. harveyana ) Pushparaj et al. , 1994
- Kattegat, The North Sea Marine water ( N. spumigena ) Smayda, 1998
- Barrow Ski Club Lake, England Brackish lake ( N. spumigena ) Twist & Codd, 1997
Other locations:    
- Osoyoos, British Columbia, Canada

Alkaline soil near saline ponds ( N. spumigena )

Camm & Stein, 1974;Nordin & Stein, 1980; www.pasteur.fr

- Lucknow, India Alkaline soil ( N. harveyana ) Dixit et al. , 1985
- Debari, India Alkaline soil ( N. spumigena ) Gopal et al. , 1975
- Svätý Jur, Slovakia Littoral of brook ( N. sphaerocarpa Hindàk, 1999
- the Gulf of Bothnia, the Baltic Sea Ice ( N. spumigena ) Laamanen, 1996
- Lindåspollene, Norway Littoral zone of fjord ( Nodularia sp.) Lännergren, 1980
- Simpon’s Gap, Australia Water hole, soil ( N. spumigena ) Nordin & Stein, 1980
- São Paulo, Brazil Littoral zone of river ( N. willei ) Sant΄Anna, 1991
- Guadarrama mountain and Coto de Doñana, Spain Freshwater brook and lagoon ( Nodularia sp.) Sanz-Alférez & del Campo, 1994
- Allahabad, India Soil near lake ( N. harveyana ) Tiwari & Pandey, 1976
- Buerto Princesa, Palawan, Philippines On intertidal rocks ( N. harveyana) Umezaki, 1995
- Gibraltar Point, Lincolnshire, UK Salt marsh ( N. harveyana ) Warr et al. , 1984
- Dax, France

Thermal spring ( N. sphaerocarpa / harveyana )

www.pasteur.fr
(strain PCC7804

 

 

1.1.2 Cyanobacterial blooms in the Baltic Sea

In the Baltic Sea, late-summer blooms of nitrogen fixing filamentous cyanobacteria are an annual phenomenon (Kononen, 1992). The geographical extent and the magnitude of these population explosions of cyanobacteria has been suspected to increase (Kahru et al. , 1994) due to the increased nutrient concentrations (Wulff et al. , 1990) and changed nutrient ratios in the Baltic Sea (Smayda, 1990).

In most open sea areas of the Baltic Sea, the blooms in July-August are dominated by Nodularia and Aphanizomenon . In addition, Anabaena is present in the blooms (Kononen & Niemi, 1984; Sivonen et al. , 1989a,b; Kononen et al. , 1993b). Several other cyanobacterial genera, e.g. Aphanothece , Chroococcus , Snowella, Merismopedia , Microcystis , Lyngbya , and Planktothrix have been recorded especially from coastal areas of the Baltic Sea (Hällfors, 1979; Edler et al. , 1984). In addition, several studies (Jochem, 1988; Kuosa, 1991; Heinänen et al. , 1995) have described the importance of cyanobacterial picoplankton, identified as Synechococcus , in the phytoplankton community of the Baltic Sea.

In the Baltic Sea, Nodularia has been confirmed as the only toxin-producing cyanobacterial genus so far (Sivonen et al. 1989a,b; Kononen et al. , 1993b), and animal poisonings have been associated with blooms of this genus (Nehring, 1993).

 

1.1.3 Toxicosis and exposure routes of cyanobacterial hepatotoxins

Hepatotoxins have most frequently been associated with incidents of animal poisonings. The first scientific report on a cyanobacterial poisoning is that by Francis (1878). The author reported that stock deaths in Australia had occurred as a result of drinking from a lake infested by a bloom of Nodularia spumigena . Since the finding of Francis, there have been numerous reports of animal poisonings that have been associated with Nodularia blooms (Table 2) and with other cyanobacterial genera (Sivonen, 1990a; Ressom et al. , 1994; Kuiper-Goodman et al. , 1999). There have also been several reports of human illness - even deaths - attributed to toxic cyanobacteria (Ressom et al. , 1994; Hunter, 1998; Codd et al. , 1999b; Kuiper-Goodman et al. , 1999). The poisoning episodes and monitoring surveys of toxic blooms (Sivonen, 1998; Codd et al. , 1999b; Sivonen & Jones, 1999) have revealed that cyanobacterial toxins are common and pose serious health hazards for animals and human beings throughout the world.

Cyanobacterial peptide toxins are linked to incidences of different human illnesses, including skin and eye irritation, allergy-like symptoms, gastro-enteritis, and hepatoenteritis caused by acute exposure to toxins (Carmichael & Falconer, 1993; Ressom et al. , 1994; Codd et al. , 1999b; Kuiper-Goodman et al. , 1999). Chronic exposure to microcystins through drinking water may increase incidences of human liver cancer (Codd, 1998; Codd et al., 1999b; Kuiper-Goodman et al. , 1999). A severe hepatoenteritis of the population in Palm Island, Queensland, Australia was also associated with drinking water contaminated with Cylindrospermopsis raciborskii (Byth, 1980; Hawkins et al. , 1985). In Brazil, a major human poisoning episode was attributed to water used for dialysis containing microcystins in 1996 (Jochimsen et al. , 1998; Pouria et al. , 1998). This poisoning caused the death of at least 55 people due to severe liver damage.

These episodes showed that hemodialysis water is an important exposure route for cyanobacterial toxins together with the consumption of drinking water. Furthermore, the recreational use of waters has caused illness in individuals who have been in skin contact with blooms (Carmichael & Falconer, 1993; Hunter, 1998; Codd, 1998; Codd et al. , 1999b). For example, in Australia, people have had skin, eye and respiratory symptoms after contact with a bloom of Nodularia (Soong et al. , 1992). Consumption of contaminated cyanobacterial cell dietary supplements, plant products, shellfish and fish may lead to minor exposure to cyanobacterial toxins (Codd et al. , 1999b). For example, cyanobacterial hepatotoxins have been found from salad lettuce (Codd et al. , 1999a) and from mussels (Chen et al. , 1993; Falconer et al. , 1992). In addition, showering and bathing are possible routes of exposure (Codd, 1998; Codd et al. , 1999b).

Table 2. Toxic Nodularia blooms observed in monitoring surveys and due to poisoning episodes
……………………………………………………………………………………………………………
The descriptions of clinical, pathological, and histological findings due to cyanobacterial hepatotoxins are described in section 1.3.2.
*Intoxication by Nodularia was suspected, but no toxicity tests or pathological surveys were made.

Location and date Affected animal (findings of hepatoxicity) and/or bioassays (animal, administration, findings) Nodularia and/or nodularin (detection method) Reference
Autralia:      
- Lake Alexandrina, 1878 Sheep (pathological findings) Nodularia in water Francis, 1878
- Broomehill dam, 1974 Sheep (pathological findings), bioassays (sheep and pigs, oral, clinical and histological findings) Nodularia in water Main et al. , 1977
- Lake Alexandrina and Lake Albert, 1990-93 Hepatotoxicity of most Nodularia -dominated samples (mouse, i.p., MLD 100 ) Nodularin in several bloom samples (HPLC) Baker & Humbage, 1994
- Orielton Lagoon, Tasmania, 1992-93   5-3500 ΅g nodularin g -1 dw (HPLC) Jones et al ., 1994b; Blackburn & Jones, 1995
- Lake Alexandrina and Lake Albert, 1994-95  

0.02-1.7 ΅g nodularin l -1 (HPLC)

Heresztyn & Nicholson, 1997
Europe / the Baltic Sea      
- Kleiner Jasmunder Bodden, Germany, 1963 Ducks (pathological findings) Nodularia in water Kalbe & Thieß, 1964
- Gotland, Simrishamn, Karlshamn, and Ystad, Sweden, 1982

Dogs (clinical and pathological findings), bioassay (mouse, i.p.,> 40 MU g -1 dw -1 )

Nodularia in water Lind et al. , 1983; Lundberg et al. , 1983; Edler et al. , 1985
- Strelasund, Germany, 1983 Cattle (clinical and pathological findings) Nodularia in water von Gußmann et al. , 1985
- Porvoo, Finland, 1984 Dogs (pathological findings) Nodularia in water Persson et al. , 1984
- Saarenmaa, Estonia, 1984 Bull calves* Nodularia in water Olli, 1996
- Arkona Sea, 1986 Bioassay (mouse, i.p., LD 50 95-455 mg kg -1 ) Nodularin detected in all hepatotoxic Nodularia bloom samples (HPLC) Sivonen et al. , 1989a
- Arkona Basin, Baltic Proper, and Gulf of Finland, 1985-87 Bioassay (mouse, i.p., MLD 100 125-2500 mg kg -1 in most of the samples) 0.1-2.4 mg nodularin g -1 dry weight -1 (dw -1 ) (HPLC) Sivonen et al. , 1989b
- Gulf of Finland, and Gulf of Bothnia, 1990-91 Bioassay (mouse, i.p., MLD 100 ), samples collected from the Bothnian Sea were hepatotoxic 0.3-18.1 mg g -1 nodularin dw -1 of hepatotoxic blooms samples and 0.01-4.9 mg nodularin l -1 in all water samples (HPLC) Kononen et al. , 1993b
Europe / North Sea      
- Århusbugten and Kaløvigområdet, Danemark, 1975 Dogs (clinical and pathological findings) Nodularia in water Lindstrøm, 1976
- Banter See, Wihelmshaven, Germany, 1990 Dogs (clinical and pathological findings) Nodularia in water Nehring, 1993
Africa:      
- Malmesbury, South Africa, 1993-94 Calves (clinical findings), bioassay (mouse, i.p.), cows (pathological findings), and sheep (pathological findings, and blood chemistry) Nodularia spumigena in water van Halderen et al. , 1995
- Lake Zeekoeivlei, Cape Town, South Africa, 1994 Dog (clinical and histological findings), bioassay (mouse, i.p., hepatotoxicity) Nodularia spumigena accounted for about 95% of the bloom containing 3.5 ΅g nodularin mg -1 (HPLC) Harding et al. , 1995

 

1.1.4 Ecological effects of cyanobacterial toxins

The ecological role of cyanobacterial toxins is still not understood despite the numerous studies on physiological and ecological bases for toxin production. Toxin production is most likely related to the physical, chemical, and biotic environment, in which cyanobacteria compete with other organisms to maximise their growth and reproduction (Ressom et al. , 1994; Paerl & Millie, 1996). For example, cyanobacteria are known to have toxic effects on phytoplankton and aquatic macrophytes (reviewed by Ressom et al. , 1994) and Nodularia blooms have been suspected to reduce fish abundance (Potter et al. , 1983; Lenanton et al. , 1985). In addition, field observations have revealed that zooplankton (Watanabe et al. , 1992; Kotak et al. , 1996), macroinvertebrates (Zurawell et al. , 1999), and mussels (Lindholm et al ., 1989 ; Falconer et al. , 1992; Chen et al. , 1993) accumulate microcystins and nodularins. These observations indicated that cyanobacterial toxins can have effects on higher trophic levels, thus they may be transfered in aquatic food chains.

Toxin production can also be a defence mechanism against grazers (see Ressom et al. , 1994; Hanazato, 1996). Toxic Microcystis and Nodularia (Reinikainen et al. , 1994; Hietala et al. , 1995; Walls et al. , 1997; Koski et al. , 1999) and toxins produced by these cyanobacteria (DeMott et al. , 1991) have been demonstrated to have harmful effects on zooplankton grazers in the laboratory. In field studies of the Baltic Sea, cyanobacterial blooms were not consumed by copepods and exposure of copepods to a bloom depressed their egg production (Sellner et al. , 1994, 1996). In some of these studies, also non-toxic cyanobacteria had negative effects on zooplankton, thus, there might be other factors than toxicity which affect food quality. For example, cell size and morphology affect ingestibility and assimilability of food (Koski, 1999).

Cyanobacteria are known to produce a wide range of compounds with dissimilar bioactivities (see section 1.3). For example, in Microcystis , different compounds have been suggested to be toxic to Daphnia and inhibit its filtering (Jungmann et al. , 1991). Recently, two variants of Microcystis PCC7806 strains, a wild-type strain and a mutant not able to produce toxin, were used to study the role of microcystins in the defence of Microcystis strains against Daphnia galeata (Rohrlack et al. , 1999). The wild-type strain was toxic to D. galeata , whereas the mutant was not lethal. Yet, both types of PCC7806 were able to reduce the Daphnia ingestion rate. The study gave strong evidence that microcystins were responsible for the poisoning of Daphnia , but they were not responsible for inhibition of the ingestion process.

 

1.2 Factors leading to cyanobacterial success

Cyanobacterial blooms have been thought to be a consequence of increased nutrient concentrations of fresh and marine waters where they occur seasonally during warm water temperatures. Although nutrients and temperature are regarded as the most important factors for the success of cyanobacteria (Paerl, 1988, 1996) several different factors have been presented to explain cyanobacterial success in aquatic environments (Hyenstrand et al. , 1998).

According to the review of Hyenstrand (1998), cyanobacteria are favoured by a low ratio of total N to total phosphorus (P) and by a high water temperature. Non-nitrogen fixing cyanobacteria require ammonium (NH 4 + ) whereas a scarcity of N benefits the development of population of nitrogen fixing cyanobacteria, which differ from non-nitrogen fixing cyanobacteria for high requirements of trace elements (e.g. iron). Furthermore, cyanobacteria gain competitive advantage by storing P and by regulating their buoyancy. With the help of these properties, they can survive during periods of P-deficiency and regulate their vertical position in the water column. Moreover, cyanobacteria can replace eukaryotic phytoplankton in high pH or low CO 2 situations, and under low light conditions. Cyanobacteria can avoid grazing e.g. by producing toxins.

 

1.2.1 Factors favouring bloom formation and growth of Nodularia and Aphanizomenon

In Australia and the Baltic Sea, low N and high P concentrations have been related to Nodularia blooms (Table 3). In the Baltic Sea, a low N:P-ratio has also been observed to favour the dominance of Aphanizomenon . In addition, P and in some cases N stimulated the growth of heterocystous cyanobacteria in most of the enrichment experiments in situ (Table 3).

Blooms of Nodularia are common in the N-deficient parts of the Baltic Sea, and they only occur exceptionally in the Kattegat which is connected to the Baltic Proper (the Baltic Sea). The absence of Nodularia in Kattegat, which has equally low N:P-ratios, is probably related to its high salinity (Granéli et al. , 1990). High salinities have been observed to depress the growth of Nodularia in Peel-Harvey Estuary, Orielton Lagoon and Great Salt Lake (Table 3). In addition, laboratory studies with cultures have shown that salinities higher than 30 ‰ repressed the growth (Horstmann, 1975; Nordin & Stein, 1980; Warr et al. , 1984; Blackburn et al. , 1996) and promoted the sporulation of Nodularia (Nordin & Stein, 1980; Jones et al. , 1994b).

In addition to the chemical controlling factors, cyanobacterial blooms are also controlled by physical factors such as temperature, light, and water stability (Paerl, 1996; Hyenstrand, 1998). High water temperatures have been reported to support Nodularia blooms in saline and in brackish waters (Table 3). Cold weather depresses initiation of cyanobacterial blooms, and cloudy and windy weather prevents the cyanobacteria from accumulating at the water surface (Table 3). The ecology and the physiology of heterocystous cyanobacterial blooms in the Baltic Sea have thoroughly been reviewed by Kononen (1992), Kononen and Leppänen (1997), and Sellner (1997).

In addition to enrichment tests done with natural communities in situ and in the laboratory (Table 3), unialgal cultures have been used to study the effects of several factors on cyanobacterial growth in the laboratory. The study of Nordin and Stein (1980) demonstrated that maximum growth of Nodularia strains occurred at salinities of 5-10‰ (test range 1-60‰), temperatures of 25-30°C (test range 15-35°C), pHs of 10.0-10.5 (test range 6.0-11.0), and light intensities of 6000 lx (test range 240-6000 lx). No preference was shown for dominant anions (Na + , Mg 2 + ) or cations (Cl - , CO 3 2- , SO 4 2- ). All strains grew well with various levels of nitrate (0.25-1.0 g NO 3 - -N l -1 ) but poor growth resulted when NH 4 + or urea was the N source (Nordin & Stein, 1980). Later, Huber (1986b) found no stimulation of growth of Nodularia by NH 4 + or NO 3 - at concentrations from 0 to 20 mg N l -1 . Horstman’s study (1975) showed that Nodularia strains grew best at salinities of 5-15‰ (test range 0-30‰). Warr et al. (1984) studied the effect of different salinities and N sources on the growth of Nodularia harveyana . They found that growth was highest at 0-35‰ (test range 0-70‰). Moreover, the growth on NH 4 + (20 mg N l -1 ) was higher than on NO 3 - (20 mg N l -1 ) and on gaseous N. The study of Blackburn et al. (1996) showed that growth of Nodularia strains at 0 and 35‰ was lower than at 12 and 24‰. According to Melin and Lindahl (1973), the growth of the Baltic Sea Aphanizomenon culture was stimulated by the addition of PO 4 3- , chelated trace elements or a combination of these. The highest biomass accumulations of N. spumigena and Aphanizomenon sp. occurred at the highest studied light intensity (test range 1-100 ΅mol m -2 s -1 ) (Holswilder, 1999). For both genera, the growth at the two lowest irradiances (1 and 6 ΅mol m -2 s -1 ) differed significantly from the two highest irradiances (60 and 100 ΅mol m -2 s -1 ). Furthermore, the biomass of N. spumigena cultures grown in moderately P-limited conditions (N:P = 32:1, molar ratio) was significantly higher than those of extremely P-limited (N:P = 64:1) and non-P-limited (N:P = 16:1) (Holswilder, 1999).

Gopal et al. (1975) found that an alkaline pH (test range 4-9) was most suitable for growth and that nutrients stimulated growth of N. spumigena strain. Growth increased when phosphate (PO 4 3- ) and NO 3 - were added. This soil strain was found to tolerate high concentrations of copper (1.5 ΅g l -1 ) and zinc (2.0 ΅g l -1 ). Dixit et al. (1985) studied the growth of Nodularia with different N sources. Ammonium chloride (0.5 mM) was highly toxic to this soil strain, while sodium nitrate (2 mM) and nitrite (2 mM) supported optimal growth. Furthermore, his studies indicated maximum growth at 20-25°C, pH 7.5-9.0 and light intensity 1000-5000 lx. Camm and Stein (1974) reported that urea was toxic at high concentrations of 8.8 mM and 4.4 mM to soil strains of N. spumigena whereas concentrations lower than those inhibited growth on N-free medium and on NO 3 - -medium.

 

1.2.2. Factors controlling nitrogen fixation in Nodularia and Aphanizomenon

Many cyanobacteria have been experimentally shown to perform nitrogen fixation under anaerobic conditions, but fewer are able to grow at the expense of atmospheric N 2 under aerobic conditions (see Flores & Herrero, 1994). Certain cyanobacteria, which are able to perform aerobic nitrogen fixation, have developed heterocysts as a protective structure for nitrogen fixation for the oxygen-sensitive enzyme, nitrogenase. Heterocysts are present within order Nostocales in three families: Nostocaceae , Scytonemataceae , and Rivulariaceae (Castenholz, 1989b).

The progress of cyanobacterial nitrogen fixation research until 1988 has been reviewed by Gallon and Chaplin (1988). Most estimates of nitrogen fixation are derived using the acetylene reduction method. This method is based on the property of nitrogenase to reduce compounds with a triplet bond such as dinitrogen (N 2 ) and acetylene. The end product of the acetylene reduction, ethylene, can be measured using gas chromatography. The acetylene reduction method has been widely adopted as a method for quantifying nitrogen fixation, since it was first introduced by Stewart and co-authors (Stewart et al. , 1967). Most of the estimates of nitrogen fixation in field populations in the Baltic Sea are based on this method (see references in Table 3), but the 15 N method (Moisander et al. , 1996) and laser photoacoustic detection of ethylene (Zuckermann et al. , 1997) have been also used. The nitrogen fixation system in cyanobacteria has been intensively studied by molecular techniques. These techniques have made it possible to study the environmental regulation of cyanobacterial nitrogen fixation at a genetic level (see Flores & Herrero, 1994).

Nitrogen fixing cyanobacteria have a selective advantage in N-limited environments such as the open Baltic Sea. In the Baltic Sea, cyanobacterial nitrogen fixation has been estimated to be about 9% of the total N input (Larsson et al. , 1985). The estimated N inputs through nitrogen fixation vary in different areas of the Baltic Sea (Larsson et al. , 1985; Howart et al. , 1988a; Sellner, 1997). Estimations for nitrogen fixation rates and the importance for lakes, estuaries, and oceans have been reviewed by Howarth et al. (1988a). Nitrogen fixation rates are controlled by many chemical and physical factors (Bothe, 1982; Howarth et al. , 1988b). Light, temperature, nutrients and salinity are known to control nitrogen fixation in Nodularia and Aphanizomenon blooms (Table 3).

 

Table 3. Factors promoting and inhibiting growth and nitrogen fixation of the planktonic cyanobacteria Nodularia and Aphanizomenon in brackish and saline waters according to field observations and experimental studies with natural phytoplankton communities ……………………………………………………………………………………………………
Abbreviations: N, nitrogen; NO 3 - , nitrate; DIN, dissolved inorganic nitrogen; P, phosphorus; PO 4 3- , phosphate; SRP, soluble reactive phosphorus.

Type of study Location and date

Results

Reference

Field observations    
Australia:    
- Lake Alexandrina, 1975-78 High turbulence and turbidity ended blooms of nitrogen fixing cyanobacteria. Geddes, 1984
- Peel-Harvey Estuary, 1977-83 Summer Nodularia blooms were related to high P concentration and fresh water loading from river flow during the previous winter. At the time of P loading, Nodularia growth was limited by temperature. In the years with no Nodularia blooms, the salinity exceeded 15‰ by the time water temperatures reached 18ΊC. Hillman et al. , 1990
- Peel-Harvey Estuary, 1977-83 Nitrogen fixation of N. spumigena blooms decreased with depth in response to light, and with increasing bloom age. Furthermore, high N concentrations, salinites, and water temperatures decreased nitrogen fixation. A positive correlation between nitrogen fixation and biomass was found. Huber, 1986a
- Orielton Lagoon, Tasmania, 1992-93 Nodularia blooms were favoured by low salinity (< 24 g kg -1 ) and high water temperature (~ 18-24ΊC).

Jones et al. , 1994b; Blackburn & Jones, 1995

- Peel-Harvey Estuary, 1977-83 Nodularia blooms were related to high P concentration (100-200 ΅g PO 4 3- l -1 ), low N:P-ratio (< 20:1), and low salinity (< 30‰). Lukatelich & McComb, 1986
Canada:    

- 41 saline lakes, Saskatchewan, 1959-82

Growth of Nodularia was observed in ten lakes ranging in salinity from 10-20 to 204 g l -1 . Hammer et al. , 983
USA:    
- Waler Lake, Nevada, 1975-77 Nodularia spumigena blooms were associated with low levels of inorganic N. The maximum numbers of Nodularia occurred at depth of one meter. Cooper & Koch, 1984
- Pyramid Lake, Nevada, 1972-86 Low N:P-ratios, as well as climatic forcing of fluvial discharge and lake mixing patterns were important for seasonal succession of N. spumigena . Galat & Verdin, 1988
- Pyramid Lake, Nevada, 1986 Nodularia blooms were initiated by high SRP and low DIN concentrations and dispersed by strong winds. Galat & Verdin, 1989
- Pyramid Lake, Nevada, 1972-86 Adequate P, but limited N supplies triggered Nodularia blooms, which were restricted to summer and autumn when the lake was thermally stratified. Galat et al. , 1990
- Pyramid Lake, Nevada, 1979 Nitrogen fixation depended on calm periods when Nodularia floated to the surface. Near-surface dependence of Nodularia distinguished it from most nitrogen fixing genera which were damaged in high light conditions. Also, low N concentration and high P concentration were controlling factors for nitrogen fixation. Horne & Galat, 1985
- Pyramid Lake, Nevada, 1989-92 High water temperature and column stability favoured Nodularia blooms. Lebo et al. , 1994
- Great Salt Lake, Utah, 1847-1987 The proportion of N. spumigena increased with the decrease in salinity, which has decreased from ~28 to 16% in the north part and from ~21 to 6% in the south part. Stephens, 1990
Europe/Baltic Sea:    
- Gulf of Bothnia, 1991 Nodulalaria spumigena and Aphanizomenon sp. did not occur in the Bothnian Bay, where phosphorus limited the growth of the phytoplankton. Andersson et al. , 1996
- Gulf of Finland, 1990 A bloom of A. flos-aquae was promoted by a nutrient pulse with a DIN:DIP-ratio of 15. Grönlund et al. , 1996
- Gulf of Riga and Gulf of Finland, 1994 There was a clear difference in biomass and sinking loss of Aphanizomenon between the study areas. In the Gulf of Riga, the deep water rich in N invoked biomass increase and promoted the buoyancy control of Aphanizomenon . Also, light controlled the vertical distribution and sinking loss rates of Aphanizomenon . Heiskanen & Olli, 1996
- Arkona Sea, 1974 The highest nitrogenase activity per heterocyst as well as the highest biomass and the number of heterocysts were observed from the surface water layers with the highest Nodularia bloom densities. Blooms were initiated through P enrichment of warm, stratified surface waters low in N. Hübel & Hübel, 1980
- Baltic Proper, 1982 Phytoplankton growth was increased in fronts resulting from nutrient enrichment by upwelling. Kahru et al. , 1984
- Gulf of Finland, 1972-85 Cyanobacteria were associated with high water temperatures. Kononen, 1988
- Baltic Sea, 1979-88 The monitoring data showed a rather similar distribution of A. flos-aquae and N. spumigena in relation to salinity whereas they have clearly different temperature optima. Kononen, 1992
- Gulf of Finland, 1968-81 High P concentrations and low N:P-ratios favoured heterocystous cyanobacterial species. Kononen & Niemi, 1984
- Gulf of Finland, 1990 A. flos-aquae bloom formation was associated with frontal upwelling bringing up deep waters with a low N:P-ratio. Kononen & Nõmmann, 1992
- Gulf of Finland, 1993 Cyanobacterial growth in the frontal zone was stimulated by PO 4 3- -replenishment zones ( A. flos-aquae ) and warming and shallowing of the surface layer ( N. spumigena ) under calm weather conditions. Kononen & Leppänen, 1997
- Baltic Sea Nodularia spumigena and A. flos-aquae were dissimilar regarding their temperature, salinity, and light optima, as well as in the affinity for PO 4 3- . The initiation of Nodularia blooms was not restricted to the frontal zone, but took place on a basin-wide scale, as a result of warming and shallowing of the surface layers under calm weather conditions. A. flos-aquae benefited from P pulses.

Kononen et al. , 1996

 

- Gulf of Finland, 1994 Nodularia was concentrated in the near-surface layer, while the maximum abundance of Aphanizomenon was observed in the top 7- to 10-m layer throughout the day. Kononen et al. , 1998
- Baltic Sea The upwelling water with a low N:P-ratio and a warm stable water column were the most important variables controlling blooms of heterocystous cyanobacteria. Leppänen et al. , 1988
- Bothnian Sea, 1977-78 Aphanizomenon flos-aquae occurred from mid-June to the end of December. In the Bothnian Bay, the mean values of heterocyst activity (1332-1880 nmol C 2 H 4 x 10 -7 het -1 h -1 ) and heterocyst frequency (0.5-2.3 mm -1 ) were low compared to values in the other parts of the Baltic Sea due to low P concentrations. The heterocyst activity and frequency increased with increasing concentration of P. Lindahl & Wallström, 1985
- Baltic Proper, 1976 The heterocyst frequency of A. flos-aquae decreased during the study, probably due to high N concentrations in water. Upwelling of bottom water caused the disappearance of cyanobacteria and reduced the number of heterocysts. Lindahl et al. , 1978
- Baltic Proper, 1975 At the beginning of August, Nodularia declined and Aphanizomenon became the dominant nitrogen fixing genera. While Aphanizomenon was distributed within the whole euphotic layer, the Nodularia population was mainly floating on the surface. The nitrogen fixation showed principally the same vertical variation as the number of heterocysts, and was to a minor extent determined by the heterocyst activity. Lindahl et al. , 1980
- Gulf of Finland, 1994 The nitrogen fixation activity decreased during the study with the heterocyst frequency of Nodularia and Aphanizomenon. The highest nitrogen fixation rates were found in the samples grown at the highest irradiance, and nitrogen fixation took place also in the dark. Under the highest irradiance, nitrogen fixation activity correlated positively with heterocyst frequency of Nodularia . Moisander et al. , 1996
- Gulf of Finland, 1992 In the early phase of the bloom, a salinity front had a marked effect on the spatial distribution of Nodularia and Aphanizomenon . Their biomass decreased steeply at the low salinity side of the front. During later bloom stages, spatial separations of Nodularia and Aphanizomenon disappeared. Moisander et al. , 1997
- Baltic Sea A low N:P-ratio promoted cyanobacterial blooms, especially in areas characterized by upwelling of P-rich bottom water. In the Bothnian Bay, where P rather than N limits phytoplankton production, no blooms exist. Niemi, 1979
- Baltic Proper and Gulf of Finland 1980, -82,
and –84
Nodularia was found in the uppermost five meters, while Aphanizomenon was distributed throughout the euphotic water layer. The dominance of Nodularia increased whereas the proportion of Aphanizomenon decreased towards the southern Baltic Sea. Nodularia occurs generally in the open sea area, while Aphanizomenon occurs in high abundance also in coastal areas. Cyanobacterial biomass and nitrogen fixation fluctuated strongly in space and time owing to patchiness and movement of the water masses. No clear connection was found between bloom development and nutrient concentrations. Niemistö et al. , 1989
- Gulf of Gdansk, 1992-94 A decrease of the N:P-ratio was favourable for nitrogen fixing cyanobacteria. N. spumigena preferred higher temperatures for growth than A. flos-aquae . Pliński & Jσzwiak, 1996
- Gulf of Finland, 1993 Nodularia spumigena was a common species in all the areas of the Gulf of Finland except the Neva Estuary where the oversupply of N promotes the growth of non-heterocystous species such as Planktothrix agardhii . Rantajärvi et al. , 1998
- Gulf of Finland, 1978 Total P and total N correlated positively with Nodularia biomass in eutrophic waters, while positive correlation between total P and Nodularia biomass was found in oligotrophic waters. Rinne & Tarkiainen, 1978
- Gulf of Bothnia, 1978-79 The nitrogen fixation, the number of heterocysts, and the biomass o f A. flos-aquae and N. spumigena showed the same horizontal distribution. The level of nitrogen fixation was negligible in the Bothnian Bay. In the central and southern Bothnian Sea they were markedly lower (1/10) than in the northern Baltic Proper and the Gulf of Finland. The absence of blooms of heterocystous species and nitrogen fixation from the north of the Gulf of Finland is apparently connected with the high inorganic N:P-ratio in that area. Also, low temperature may prevent development of blooms. The vertical abundance of heterocystous genera differed: the vertical maximum of Aphanizomenon occurred at 10-20 m, while the highest abundance of Nodularia was near the surface. Rinne et al ., 1981
- Southern Baltic Proper, 1993 In surface waters, the increased irradiance experienced by A. flos-aquae supported increased rate of nitrogen fixation. Stal et al. , 1998
- Southern Baltic Sea, 1993, -95 Nitrogenase activity was saturated at about 600 ΅mol photons m -2 s -1 , but considerable activity was found also in the dark. Stal et al. , 1999
- Baltic Sea, 1992-94 Nodularia spumigena and A. flos-aguae were mostly restricted to the water above the thermocline, and in calm conditions their concentration increased towards the top of the water column. The highest concentrations were within the top 10 m of the water column. Walsby et al. , 1995
- Baltic Proper, 1983-85 The biomass of A. flos-aquae varied between the years mainly due to variation in water temperature. Also, the biomass and the number of heterocysts increased with increasing distance from the sewage treatment plant due to a low N:P-ratio. The biomass of Aphanizomenon was highest in 1984 when the P loading from the plant was highest. Wallström, 1988
Experiments performed in situ and in the laboratory    
- Gulf of Bothnia, Baltic Sea, 1991 Phytoplankton was P limited in the Bothnian Bay and the coastal area of the Bothnian Sea, and N limited in the offshore Bothnian Sea. Andersson et al. , 1996
- Arkona Sea, Baltic Sea, 1978-79 Addition of N or N and P increased the biomass and changed the composition of phytoplankton. N. spumigena was one of the phytoplankton species which reacted most strongly to the enrichment. Granéli, 198
- Harvey Estuary, 1981-84 and Peel Inlet 1982-84, Australia The Nodularia biomass was higher in the P treatment than in the iron and N treatments. Hamel & Huber, 1985
- Baltic Proper, Baltic Sea, 1972 Cyanobacterial growth was stimulated by addition of PO 4 3 - , and PO 4 3 - and NO 3 - . When N became deficient, an increase in the frequency of heterocysts was observed, which resulted in higher nitrogen fixing ability. Horstmann, 1975
- Peel-Harvey Estuary, Australia Light controlled nitrogen fixation in Nodularia . Nitrogen fixation was higher in the light than in the dark, where it was related to the length of prior exposure to light. Huber, 1986b
- Peel-Harvey Estuary, Australia, 1981 When P was added in the laboratory to natural Nodularia populations, there was a distinct inverse relationship between phosphatase activity and P taken up. The addition of P had little effect on biomass. Huber & Hamel, 1985
- Gulf of Finland, Baltic Sea, 1990, -92 The nutrient additions benefited the growth of smaller phytoplankton species over the filamentous heterocystous cyanobacteria. Kononen et al. , 1993a
- Pyramid Lake, Nevada, USA, 1989-92 Only time when N addition did not stimulate phytoplankton growth was during periods of winter mixing and N. spumigena bloom. Lebo et al., 1994
- Baltic Proper, Baltic Sea, 1975 Phosphate alone and in combination with chelated metals increased the heterocyst frequency of A. flos-aquae . Combined additions of NO 3 - and PO 4 3 - together stimulated the 14 C-uptake. Lindahl et al. , 1980
- Pyramid Lake, Nevada, USA, 1989-90 Phosphate enrichment, when added singly or in combination with DIN, had no effect on chlorophyll- a production. Nitrogen enrichment had a positive response at all times of the year except during a bloom of N. spumigena and after complete lake mixing. Reuter et al. , 1993
- Gulf of Finland, Baltic Sea, 1974-75 Phosphorus was more important for the growth of Nodularia than N. In the very eutrophic areas, also N had a growth-increasing effect. Rinne & Tarkiainen, 1978
- Arkona Basin, Baltic Sea, 1981 Temperature appeared to be the main factor influencing growth of Nodularia , which was also stimulated by N deficiency. Schiewer et al. , 1986
- Southern Baltic Sea, 1993, -95 Nodularia was limited by iron, which stimulated both growth and nitrogenase activity . Phosphate stimulated nitrogenase activity to the same extent as iron but did not stimulate growth. Nitrogenous compounds and molybdate did not affect nitrogenase activity whereas elimination of sulfate stimulated it strongly. Stal et al. , 1999
- Gulf of Finland, Baltic Sea, 1982 Ammonium was the main limiting nutrient for the phytoplankton community as a whole, but the nitrogen fixing cyanobacteria were P-limited. Tamminen et al. , 1985
- Baltic Proper, Baltic Sea, 1988 Phosphorus had no effect on the biomasses of cyanobacterial species. During a mesocosm experiment, A. flos-aquae almost disappeared when N was present and the population of N. spumigena increased slowly probably due to the low water temperatures. On the basis of growth rates of N. spumigena at different nutrient conditions, N. spumigena may be superior to A. flos-aquae in competition for P. Wallström et al. , 1992

 


In laboratory experiments done with Nodularia cultures, nitrogen fixation was highest at salinities of 0- 35‰ and salinities higher than 35‰ decreased the nitrogen fixation (Warr et al ., 1984). In another study, highest nitrogen fixation was detected at salinity of 5-10‰ and lower salinities than 5‰ decreased the nitrogen fixation (Huber, 1986b). Phosphorus addition stimulated nitrogen fixation in P-starved Nodularia cultures (Huber, 1986b), while NH 4 + addition inhibited nitrogen fixation (Sanz-Alférez & del Campo, 1994). A very high NH 4 + concentration (42 mg l -1 ) inhibited nitrogen fixation by both Aphanizomenon and Nodularia (Moisander et al. , 1996). According to Huber (1986b), NH 4 + completely inhibited nitrogenase activity whereas NO 3 - did not. Light has also been demonstrated to control nitrogen fixation of Nodularia cultures (Huber, 1986b; Sanz-Alférez & del Campo, 1994; Zuckermann et al. , 1997). In outdoor cultures of N. harveyana nitrogenase activity was influenced by the growth rate and not by high light intensity (Pushparaj et al. , 1994).

 

1.2.3. Factors influencing cyanobacterial hepatotoxin production

There is no information available about environmental conditions that influence hepatotoxin production in Nodularia blooms in the field whereas factors affecting toxin concentrations in Microcystis -blooms in eutrophic lakes have been examined, and the results are contradictionary. In the Hartbeespoort Dam (South Africa), microcystin-YR, -LR, -YA and -LA concentrations correlated positively with solar radiation and water temperature, and microcystin-YR, and –YA correlated negatively with PO 4 3- concentration (Wicks & Thiel, 1990). In the Coal, Driedmeat, and Little Beaver lakes (Canada), no correlation between microcystin-LR and water temperature was discovered, whereas the toxin concentration correlated positively with total and dissolved P and negatively with NO 3 - (Kotak et al. , 1995). Earlier, in Coal Lake microcystin-LR was positively correlated with water temperature and P concentration (Kotak et al. , 1993). In Babtiste, Narrow, Skeleton, Steele, the Coal, Little Beaver and Driedmeat lakes (Canada), microcystin-LR correlated positively with total P and total N (Zurawell et al. , 1999). In Lake Grand-Lieu (France), microcystin-LR and one of microcystin–RR variants correlated negatively with solar radiation, and both microcystin-RR variants correlated positively with dissolved P and NO 3 - (Vezie et al. , 1998). In Lake Tuusulanjärvi (Finland), microcystin-LR correlated positively with total N and total P and negatively with dissolved NO 3 - (Lahti et al. , 1997). A corresponding analysis of field data on environmental factors during 78 water blooms from 72 Finnish lakes revealed that hepatotoxic Microcystis blooms correlated with high PO 4 3- concentrations (Rapala & Sivonen, 1998).

Growth and nodularin levels in response to salinity changes have been studied in laboratory experiments (Blackburn et al. , 1996). Nodularin concentrations on both gravimetric and cellular basis decreased at the highest studied salinity (35 ‰). In addition, nodularin production has been demonstrated to be controlled by light and by P (Holswilder, 1999). Nodularin production was reduced under light limitation and increased under P limitation. In addition, N addition was shown to promote growth and to increase the nodularin content of a Nodularia -culture, which was grown on N-containing medium (Carmichael et al. , 1988).

Variation of cellular toxin levels under different growth conditions have been studied in the laboratory mainly with batch-cultures of hepatotoxic Microcystis , Oscillatoria , Anabaena , and neurotoxic Anabaena , Aphanizomenon , and Planktothrix (reviewed by Rapala, 1998 and by Sivonen & Jones, 1999). In these laboratory experiments, temperature, light, and nutrients were most frequently examined. In addition, the effects of pH, carbon dioxide, salinity, and micronutrients were examined. The majority of studies indicated that cellular toxin levels were highest under conditions most favourable for growth. Differences in responses of hepatotoxic and neurotoxic strains have been observed, e.g. P had a pronounced effect on hepatotoxin levels, but not on neurotoxin levels. Nitrogen had no effect on toxin production by nitrogen fixing species, while non-heterocystous species, such as Microcystis and Oscillatoria , produced more toxins under N-rich media. All these laboratory studies have provided evidence of environmental regulation of gravimetric toxin concentration. Orr and Jones (1998) suggested that toxin concentration in Microcystis is controlled by the effects of environmental factors on the rate of cell division, not through any direct effect on the metabolic pathways on toxin production. This suggestion was based on laboratory experiments with Microcystis aeruginosa cultures and on re-evaluation of data made on microcystin-producing Anabaena and Oscillatoria cultures presented by others (Sivonen, 1990b; Rapala et al. , 1997).

Cyanobacterial hepatotoxins are so-called intracellular toxins, and they are released from cells when they are damaged or lysing (see Sivonen & Jones, 1999). Chemical, physical, and biological degradation of cyanobacterial toxins have been demonstrated to occur (Hrudey et al. , 1999; Sivonen & Jones, 1999). Twist and Codd (1997) studied degradation of nodularin under light and dark conditions and found photochemical breakdown of nodularin. In addition, nodularin was degraded when components of Nodularia cells were present. These components most likely contained nodularin degrading and metabolising bacteria. In water of Lake Alexandrina, where N. spumigena blooms have occurred for months, nodularin was degraded by bacterial communities within 48-50 h (half-life 24 h) (Heresztyn & Nicholson, 1997).

Furthermore, three bacterial strains, which have been isolated from sediments of the Lake Tuusulanjärvi (Finland), were able to degrade nodularin (Lahti et al. , 1998). On the contrary, the bacterial strain isolated from water sample treated with Microcystis aeruginosa extract, was not able to degrade nodularin, although it has degradative activity against microcystins (Jones et al ., 1994a).

 

1.3. Bioactive peptides from cyanobacteria

Cyanobacteria contain a large number of secondary metabolites, compounds not essential for growth and reproduction. These include peptides, macrolides, and glycosides (Patterson et al. , 1994; Namikoshi & Rinehart, 1996). These compounds have been reported to possess a number of bioactivities: antiviral (Pattersson et al. , 1993, 1994), antifungal (Patterson et al. , 1994), cytotoxic (Patterson et al., 1991), protein phosphatase inhibitory (Honkanen et al. , 1995) and antineoplastic activities (Moore et al. , 1996). For example, Nodularia harveyana has antifungal, antibacterial, and alleopathic activities (Pushparajat et al. , 1999). Many of these secondary metabolites are toxic to animals and humans (Carmichael & Falconer, 1993; Falconer, 1996; Hunter, 1995, 1998; Codd et al. , 1999b).

 

1.3.1. Structure of nodularin

Cyanobacteria produce two main types of toxins: neurototoxins and hepatotoxins (Carmichael, 1992, 1994; Codd, 1998; Sivonen, 1998). Hepatotoxins are produced by several genera: Anabaena , Aphanizomenon , Cylindrospermopsis , Microcystis, Nodularia , Nostoc , and Oscillatoria (Carmichael, 1994; Sivonen, 1998; Sivonen & Jones, 1999). Hepatotoxins are divided into three groups: alkaloids (cylindrospermopsin), heptapeptides (microcystins) and pentapeptides (nodularins). Cylindrospermopsin is produced by Cylindrospermopsis raciborskii (Hawkins et al. , 1985, 1997), Aphanizomenon ovalisporun (Banker et al. , 1997), and by Umezakia natans (Harada et al. , 1994). Structurally related cyclic peptides, microcystins and nodularins, differ from each other in their number and type of certain amino acids (Carmichael, 1992; Sivonen, 1998). Microcystins, which are named after the genus Microcystis from which they were first identified, are produced by several cyanobacterial genera and consist of seven amino acids. The main differences between the different variants of microcystins are in the two variable L-amino acids, and methylation or non-methylation of certain amino acids (Sivonen & Jones, 1999). Nodularin is produced only by Nodularia and is composed of five amino acids (Rinehart et al. , 1988). Three of those amino acids are the same as in microcystins: D-MeAsp 1 (D- erythro -b -methylaspartic acid), Adda 3 , and D-Glu 4 (D-glutamic acid)(Fig. 1). In addition to these, nodularin consists of L-Arg 2 (L-arginine) and Mdhb 5 [2-(methylamino)-2-dehydrobutyric acid]. Both toxins contain a unique C 20 amino acid, 3-amino-9-methoxy-2,6,8-trimethyl-10-phenyldeca-4,6-dienoic acid, which is abbreviated as Adda. This amino acid is essential for the hepatotoxicity (Harada et al. , 1990; Rinehart et al. , 1994). The same peptide structure, named nodularin by Rinehart et al. (1988), has been found in Nodularia blooms and strains sampled from Australia (Runnegar et al. , 1988), New Zealand (Carmichael et al. , 1988; Rinehart et al. , 1988) and the Baltic Sea (Eriksson et al. , 1988; Sivonen et al. , 1989a; Sandström et al. , 1990).

Nodularin show considerably less structural variation than microcystins (Rinehart et al. , 1994). To date, five different natural analogues of nodularin have been characterised (Table 4). Furthermore, the compound [L- Val 2 ] , named motuporin, has been found from a marine sponge (de Silva et al. , 1992), in which the compound is probably produced by a symbiotic cyanobacterium. This analogue differs from nodularin by substitution of a valine (Val) residue for an Arg residue. In addition, two dihydronodularins have been synthesised chemically (Namikoshi et al. , 1993).

Most nodularins have an intraperitoneal LD 50 of 50-150 ΅g kg -1 in mice (Table 4), which is calculated to be at least 200 times lower than the oral LD 50 (Kiviranta et al. , 1990). In a similar manner as microcystins (Harada et al., 1990), nodularins with an 6 Z -Adda isomer and with modified D-Glu do not display toxicity. Furthermore, the cyclic structure is necessary for the toxicity, since linear peptides are biologically non-toxic (Choi et al. , 1993).

 

 

The linear peptide was first isolated when studying the biosynthesis of nodularin. This non-toxic peptide was thought to be a precursor of nodularin (Choi et al. , 1993; Rinehart et al. , 1994). Later, linear and cyclic peptides, spumigins and nodulapeptins, have been isolated from the toxic Nodularia strain AV1, but these compounds were not found from the non-toxic Nodularia HKVV strain (Fujii et al. , 1997a, b). In addition, glycosidic compounds have been isolated from Nodularia strains (Soriente et al. , 1992; Fujii et al. , 1997b). The function of these compounds is not known.

The immuno-gold labelling of hepatotoxins has revealed that the toxins are primarily localised in the thylakoid area and nucleoid in Microcystis and Nodularia cells, with smaller amounts in the cell wall and sheath. In the same study, nodularin was found both in vegetative cells and heterocysts (Shi et al. , 1995).

Table 4. Nodularin variants and their hepatotoxicity (modified from Rinehart et al. , 1994)
………………………………………………………………………………………………………

ND, not determined; NK, not known

Toxin Origin Intraperitoneal
(mouse) LD50 (΅g kg-1 )
Reference
nodularin

Nodularia strain
Nodularia bloom
Nodularia bloom
Nodularia strain
Nodularia bloom and strain
Nodularia bloom

60
50
50
70
70
50

Carmichael et al. , 1988
Eriksson et al. , 1988
Rinehart et al., 1988
Runnegar et al. , 1988
Sivonen et al ., 1989b
Sandström et al. , 1990

[ D -Asp 1 ]nodularin Nodularia strain 75 Namikoshi et al. , 1994
[DMAdda 3 ]nodularin Nodularia bloom 150 Namikoshi et al. , 1994
[(6 Z )-Adda 3 ]nodularin Nodularia bloom > 2000 Namikoshi et al. , 1994
[ D -Glu-OCH 3 4 ]nodularin NK > 1200 Rinehart et al. , 1994
[L-Val 2 ]nodularin
(= motuporin)
Theonella swinhoei Gray ND de Silva et al. , 1992
dihydronodularins:      
[ D -MeAbu 5 ]nodularin Nodularia strain 150 Namikoshi et al. , 1993
[ L -MeAbu 5 ]nodularin Nodularia strain 150 Namikoshi et al. , 1993

 

 

1.3.2. Mechanism of hepatotoxicity in mammals

After the hepatotoxins are released from the cyanobacterial cells in the digestive system and taken up in the ileum, they pass through the hepatic portal vein into the primary target organ, the liver (Carmichael & Falconer, 1993; Nishiwaki et al. , 1994). The liver specificity of the hepatotoxins is dependent on the active uptake of these compounds by the bile acid transporter mechanism (Carmichael, 1992; Carmichael & Falconer, 1993). In hepatocytes, they cause hyperphosphorylation of various proteins such as cytokeratin peptides 8 and 18 (Ohta et al. , 1992), and this leads to disturbances in the cell’s cytoskeleton and in morphological changes (e.g. Eriksson et al. , 1990, 1992a,b; Ohta et al. , 1992, 1994; Toivola et al. , 1997). Changes in cell shape and losses of the cell’s contacts with other hepatocytes and with sinusoidal capillaries lead to a lethal intrahepatic haemorrhage or hepatic insufficiency within a few hours to a few days (Carmichael, 1992, 1994; Carmichael & Falconer, 1993).

In mammals, signs of poisoning due to hepatotoxins include weakness, reluctance to move, pallor of the extremities and mucous membranes, anorexia, vomiting, cold extremities and hypovolaemic shock (Carmichael, 1992; Carmichael & Falconer, 1993). Before the animals die of intrahepatic haemorrhage and hypovolaemic shock, they frequently suffer muscle tremors and fall into a coma (Carmichael, 1992). The conclusion that death has resulted from intrahepatic haemorrhage can be confirmed by an autopsy that reveals an enlarged liver. In addition, a blood chemistry, which reveals low hepatic haemoglobin and iron concentrations, expose blood loss responsible for shock (Carmichael, 1992). Besides, necrosis and lysis of hepatocytes, accompanied by marked haemorrhages, are discovered in histological examinations (e.g. Runnegar et al. , 1988).

In all eukaryotic cells, intracellular signal transduction is principally linked to extracellular signals via reversible protein phosphorylation by protein kinases and phosphatases. Eukaryotic protein phosphatases (PPs) are structurally and functionally dissimilar enzymes, which belong to the PPP, PPM, and PTP gene families. PPs in the PTP family dephosphorylate phosphotyrosine whereas phosphoserine and phosphothreonine are dephosphorylated by PPMs and PPPs. The PPP family includes PP1, PP2A, and PP2B, which are the most abundant eukaryotic protein Ser/Thr phosphatases (Barford, 1996). PPs play a crucial role in a variety of cellular processes such as cell proliferation and differentiation (Shenolikar, 1994; Wera & Hemmings, 1995).

PPs have been shown to be inhibited by a variety of natural toxins. These include okadaic acid (Holmes & Boland, 1993; Honkanen et al. , 1994), a fatty acid polyether (Yasumoto et al. , 1985). This seafood toxin, which cause diarrhoeic shellfish poisoning (DSP), is produced by marine dinoflagellates and accumulates in filter-feeding organisms (Aune & Yndestad 1993; Steidinger, 1993; Scoging 1998). Okadaic acid was the first toxin reported to inhibit PP1 and PP2A (Takai et al. , 1987; Bialojan & Takai, 1988; Adamson et al. , 1989; Haystead et al. , 1989, and others). Since then, microcystins and nodularin have also been found to inhibit PP1 and PP2A (MacKintosh et. al. , 1990; Matsushima et al. , 1990; Yoshizawa et al. , 1990; Siegl et al. , 1990; Honkanen et al. , 1990, 1991, 1994; Ohta et al. , 1994; Suganuma et al. , 1992; Runnegar et al. , 1993).

The toxins inhibit distinct PPs differentially. For instance, the inhibitory effects of nodularin and microcystin-LR and –LA are higher for PP2A than for PP1 (Honkanen et al. , 1994). The different sensitivity of PP1 and PP2A to the toxins can be due to the presence of a cysteine residue at position 269 in PP2A and a phenylalanine residue at position 276 in PP1 (Lee et al. , 1999) .

Through inhibition of PPs activities these structurally diverse toxins, which are produced by different organisms, prevent dephosphorylation of phosphoserine and phosphothreonine and therefore increase protein phosphorylation (see Quinn et al. , 1993). Protein phosphorylation plays a central role in many adaptive responses to environmental signals also in cyanobacteria (Tandeau de Marsac & Houmard, 1993; Mann 1994). However, cyanobacterial PPs are resistant to their own toxins, such as microcystin-LR (Shi et al. , 1999).

It is known that the different toxins compete for binding to PP1, since prior binding of microcystins (Matshushima et al. , 1990; Yoshizawa et al. , 1990), nodularin (Yoshizawa et al. , 1990), and calyculin to PP1 (Suganuma et al. , 1990) prevent binding of okadaic acid. Furthermore, the prior binding of okadaic acid and inhibitor-1 and inhibitor-2 prevented PP1 from interacting with microcystin (MacKintosh et al. , 1990).

 

1.3.3. Tumour promotion caused by protein phosphatase inhibitors

Masami Suganuma was the first to report that okadaic acid is a tumour promoter (Adamson et al. , 1989). Later, structurally various compounds including microcystins and nodularin that inhibit PP1 and PP2A were found and named as "Tumor Promoters of the Okadaic Acid Activity Class" (Fujiki & Suganuma, 1993). Further studies of these compounds revealed that inhibition of PP1 and PP2A is a general tumour promotion pathway in various organs (Fujiki & Suganuma, 1999). The next step in tumour promotion, after inhibition of PPs, is the expression of the TNTµ gene and early-response genes (Sueoka et al. , 1997; Fujiki & Suganuma, 1999). These expressions are assumed to be associated with mRNA stabilisation.

In rat liver, repeated intraperitoneal injections of microcystin-LR and nodularin induced tumours (Nishiwaki-Matsushima et al. , 1992a; Ohta et al. , 1994). Skin tumour growth was promoted by oral consumption of Microcystis in drinking water (Falconer, 1991, 1996). Furthermore, several epidemiological studies in China have indicated that people taking their drinking water from ponds and ditches contaminated with Microcystis blooms have a much higher incidence of primary liver cancer than those using river or well water (Fujiki et al. , 1996; Hunter, 1998).

Nodularin and microcystin-LR have the same specific activity in inhibition of PP1 and PP2A (Yoshizawa et al. , 1990). Nodularin promotes liver tumour growth with higher activity than microcystin-LR (Ohta et al. , 1994; Fujiki et al. , 1996). In addition, nodularin is a liver carcinogen with both initiating and tumour-promoting activities, whereas microcystin-LR is a liver tumour promoter without an initiating activity (Ohta et al. , 1994; Fujiki et al. , 1996).

 

1.3.4. Structure-activity relationship of peptide toxins

The microcystins and nodularin inhibit PP1 and PP2A and show hepatotoxicity with similar potency. The cyclic stucture of the microcystins and nodularins share many common features. Furthermore, there are variants of microcystins and nodularin that also contain common residues in the variable regions. For instance, microcystin-LR and nodularin have Arg in common. The study of Nishiwaki-Matsushima and co-authors (1992b) with naturally occurring geometrical isomers of microcystin-LR and -LA has shown that the Arg residue did not significantly interact with the enzymes and can be substituted by other amino acids without loss of hepatotoxicity. This was further verified by the isolation of a nodularin variant, motuporin (de Silva et al , 1992). Motuporin is similar in structure to nodularin, but has Arg instead of Val. Despite this structural difference, both of these compounds inhibit PPs with similar potency. Furthermore, there are many naturally occurring toxic microcystins in which a number of residues replace the leucine (Leu) and/or the Arg in the peptide ring (Carmichael, 1992; Rinehart et al. , 1994), indicating that these residues are not critical for the inhibition of PPs. On the contrary, it has been reported that Adda, which is also common for microcystins and nodularins, is essential for the activity and that the peptides with the 6Z-Adda isomer are biologically inactive (Nishiwaki-Matsushima et al. , 1991; Rinehart et al. , 1994). Also, D-Glu has an important role in hepatotoxicity, since esterification of its free carboxyl group leads to a total loss of activity (Rinehart et al. , 1994). These findings suggest that only the Adda and Glu residues play important roles in the hepatotoxicity, thus they have functions in interactions with microcystins and nodularins to PP1 and PP2A.

Three-dimensional (3-D) structures of microcystins (Rudolp-Böhner et al. , 1994; Bagu et al. , 1995, 1997; Trogen et al. , 1996, 1998) and motuporin (Bagu et al. , 1995, 1997) have been determined by nuclear magnetic resonance spectroscopy (NMR). Conformational studies have shown that microcystin-LR (Bagu et al. , 1995; Trogen et al. , 1996), microcystin-RR (Trogen et al. , 1998), and motuporin (Bagu et al. , 1995) possess a saddle-shaped peptide ring. Furthermore, the Adda side-chain in both toxins and Arg in microcystin were shown to be flexible, whereas Val in motuporin was less flexible than Arg. The conformational similarities of microcystin and nodularin imply that these peptide toxins inhibit PPs in a similar way.

The NMR results differ from the results obtained using a molecular modelling analysis of the 3-D structures of microcystin-LR and nodularin, which predicted that these toxins have planar peptide rings (Lanaras et al. , 1991; Taylor et al. , 1992). The comparison of Lanaras and co-workers was later optimised by Taylor et al. (1992), who used molecular modelling to calculate the energetically lowest conformations for microcystin-LR. Later, molecular modelling was expanded to include several naturally occurring toxins: cantharidin, calyculin-A, okadaic acid, tautomycin (Quinn et al. , 1993; Gauss et al. , 1997; Gupta et al. , 1997). The conformational studies of natural toxins have been reviewed by Quinn et al. (1996), who has also developed a pharmacophore model for okadaic acid, calyculin-A, and microcystin-LR (Quinn et al. , 1993). This model contains a conserved acidic group, two potential hydrogen-bonding sites, and a non-polar side-chain.

The 3-D structures of the inhibitors alone do not explain how PPs are inhibited, therefore, the bound conformations of inhibitors to protein phosphatases are needed. Crystal structures have been determined for rabbit PP1 complexed with microcystin-LR (Goldberg et al. , 1995) and for human PP1 complexed with tungsten (Egloff et al. , 1995). These structures clarify how PP1 dephosphorylate substrates and how it is regulated.

The study of Goldberg et al. (1995) showed how PP1 is inhibited by microcystin. Microcystin interacts with the PP1 in a Y-shaped groove on the surface of the enzyme at three sites: the metal-binding site, the hydrophobic groove and the edge of the C-terminal groove near the active site (Goldberg et al. , 1995).

Lee and co-workers (Zhang & Lee, 1997; Lee et al ., 1999) have mutated residues in these grooves to assess the importance of these structures in substrate recognition. Strong effects were only observed for mutation of residues involved in phosphate binding and orientation at the active site (Lee et al ., 1999).

In the interaction between microcystin and PP1, the Glu residue of the microcystin binds indirectly to the metals via two of the metal-liganded water molecules. The long hydrophobic Adda group is inserted into the hydrophobic groove. The Leu residue of microcystin interacts with the side-chain of tyrosine 272 (Tyr 272) within the ß12/ß13-loop of the C-terminal groove (Goldberg et al. , 1995). The role of the ß12/ß13-loop in toxin binding has been confirmed by studies with different mutants (Shima et al., 1994; Zhang et al. , 1994, 1996; Lee et al. , 1999) .

Functional differences exist between the microcystins and nodularins with respect to their interaction with PPs. These enzymes are initially bound non-covalently and inhibited by these toxins. In contrast to the microcystins (Goldberg et al. , 1995; MacKintosh et al. , 1995; Runnegar et al. , 1995), motuporin does not form a secondary covalent bond after inhibition of PP1 (Bagu et al. , 1995, 1997). The explanation why nodularins are incapable of forming a covalent linkage with PP1 is the difference in the position of N-methyldehydrobutyrine (Mdhb) residue in motuporin relative to the counterpart N-methyldehydroalanine (Mdha) in microcystin-LR (Bagu et al. , 1995, 1997). The different position of Mdhb at the surface of the PP1-toxin complex compared to microcystins may facilitate a chemical interaction with further macromolecules, which may explain the carcinogenic properties of nodularins (Ohta et al. , 1994; Bagu et al. , 1997). Furthermore, the higher tumour promoting activity and the carcinogenicity of nodularin are thought to be caused by smaller size of nodularin compared to microcystin. For that reason, nodularin is more easily taken into the hepatocytes than microcystin-LR (see Fujiki et al. , 1996).

 

1.3.5. Biosynthesis of peptide toxins

Microbes synthesise non-ribosomally cyclic and linear peptides by large modular multienzyme complexes, peptide synthetases. The peptide sythetases use the so-called thiotemplate mechanism for the synthesis of peptides (von Döhren et al. , 1997; Konz & Marahiel, 1999).

Peptide synthetase genes have been identified from several Microcystis aeruginosa strains (Meißner et al. , 1996; Dittmann et al. , 1996, 1997). One of these strains (PCC7806) has been transformed to non-toxic form by the mutation of a microcystin synthetase gene, which demonstrates that this gene, called mcyB , encodes a microcystin synthetase (Dittmann et al. , 1997). Recently, mcyB was shown to hybridise, with variable signal intensity, to DNAs from several hepatotoxic strains of Oscillatoria , Microcystis , and Anabaena (Neilan et al. 1999). On the contrary, two peptide synthetase genes encoding anabaenopeptilides (cyclic depsipeptides) in the Anabaena sp. strain 90 (Rouhiainen et al. , 2000) hybridised insignificantly to non-heterocystous microcystin-producing strains. However, this probe gave strong signals with all hepatotoxic Anabaena strains, and it also cross-hybridised to most of the hepatotoxic Nostoc and Nodularia strains (Neilan et al. , 1999). Recently, three open reading frames encoding peptide synthetases involved in microcystin synthesis were identified (Nishizawa et al. , 1999).

The biosynthesis of nodularin has been studied by NMR analysis of nodularin obtained from experiments with several 13 C-labelled precursors (Choi et al. , 1993; Rinehart et al. , 1994). Carbons in Adda are derived from acetate, methionine, phenylalanine, and propionate (Moore et al., 1991; Choi et al. , 1993; Rinehart et al. , 1994). Acetate and pyruvate were also incorporated into Arg and Glu. Furthermore, D-MeAsp and Mdhb were labelled with propionate and methionine, respectively. The complete synthesis of the natural nodularin variant, motuporin, has been published (Valentekovich & Schreiber, 1995; Bauer & Armstrong, 1999). In addition, synthetic analogues of nodularin have been obtained (Mehrotra & Gani, 1996). A general route for the preparation of microcystins and nodularins has been provided by Kim et al. (1996).

 

1.3.6. Analytical methods of cyanobacterial toxins

Falconer (1993) and Harada et al. (1999) have written reviews of biological, biochemical, and chemical methods for assays of cyanobacterial toxins. Cyanobacterial toxins in water and in cells have been detected and identified by a range of methods that differ in selectivity and sensitivity (Harada, 1996; Harada et al. , 1999). Early methods for the assay of cyanobacterial toxins were based on the mouse bioassay. This method was widely used for determination of outright toxicity and toxin concentration. Furthermore, a number of invertebrates have been investigated for use as bioassays for toxins (Harada et al. , 1999). Later, biochemical tests such as the protein phosphatase inhibition assay (An & Carmichael, 1994; Ward et al. , 1998; Harada et al. , 1999) and the enzyme-linked immuno-sorbent assay (ELISA) (Chu et al. , 1989, 1990; Harada, 1996; Harada et al. , 1999) were developed for detection of peptide hepatotoxins, microcystins and nodularins.

Due to functional groups in the molecules cyanobacterial peptide toxins have common physico-chemical properties such as molecular weight and activities. For that reason they can be analysed by the same analytical methods (Harada et al. , 1999). The most commonly-used analytical system for cyanobacterial peptide toxins is high performance liquid chromatography (HPLC) combined with ultraviolet (UV) detection which relies on their retention times and UV spectra for identification (Harada, 1996; Meriluoto, 1997; Harada et al., 1999; Pelander, 2000). HPLC has been the most intensively used method when studying cellular toxin concentrations in cyanobacteria under different growth conditions (Sivonen & Jones, 1999).

 

1.4. Cyanobacterial taxonomy

Cyanobacteria were traditionally classified on the basis of their morphology. Despite the fact that their morphology is complex when compared to most other microbes, the taxonomy based on morphological characteristics does not necessarily result in a phylogenetically reliable taxonomy (Giovannoni et al. , 1988; Wilmotte, 1994). Nowadays, bacterial taxonomy relies on different kinds of information derived from phenotypic and genotypic data (Vandamme et al. , 1996).

The use of phenotypic and genotypic characteristics in cyanobacterial taxonomy was pioneered by Stanier and collaborators (e.g. Kenyon et al. , 1972; Herdman et al. , 1979a,b; Rippka et al. , 1979). The characteristics used include morphology, pigment and fatty acid composition, photoheterotrophic growth, nitrogenase activity, DNA base composition, and genome size. The taxonomic system of Rippka et al. (1979), which was based on identification of 178 cyanobacterial cultures in the Pasteur Culture Collection, recognised 22 genera placed in five taxonomic sections. Section I contains unicellular cyanobacteria that reproduce either by binary fission ( Gloeobacter , Gloeocapsa , Gloeothece , Synechococcus , Synechocystis ) or by budding ( Chamaesiphon ) whereas the unicellular members in section II divide only by multiple fission, which leads to formation of motile ( Dermocarpa ) or inmotile ( Xenococcus ) baeocytes, or by both binary fission and multiple fission ( Dermocarpella , Myxosarcina , Chroococcidiopsis , Pleurocapsa group). Members in sections from III to V are filamentous. The filamentous cyanobacteria in section III ( Spirulina , Oscillatoria , LPP group A, Pseudanabaena , LPP group B) compose only of vegetative cells while the filamentous cyanobacteria of sections IV and V contain additionally heterocysts and sometimes akinetes. In section IV, filamentous cyanobacteria are distinguishable by hormogonium formation ( Nostoc , Scytonema , Calothrix ) or its absence ( Anabaena , Nodularia , Cylindrospermum ). Divisions of cells of the filamentous, heterocystous cyanobacteria belonging to sections III and IV occur in one plane whereas members in section V ( Chlorogloeopsis , Fischerella ) divide on more than one plane.

The bacteriological taxonomic system created for cyanobacteria by Rippka et al . (1979) has been modified by Castenholz (1989a, b, c), Waterbury (1989), and Waterbury and Rippka (1989) in the volume three of "Bergey’s Manual of Systematic Bacteriology". This system also includes descriptions of cyanobacteria which are observed, but which have not been succesfully maintained in cultures. In addition, ecological features of cyanobacteria have been included. In their separate studies, Anagnostidis and Komárek (1988, 1990) and Komárek and Anagnostidis (1986, 1989) have revised the taxonomy of cyanobacteria using both bacteriological and botanical approaches. The authors made an extensive review of the literature and applied phenotypic and genotypic data concerning cyanobacterial taxonomy.

 

 

Molecular phylogenetic analysis have revealed at least ten distinct eubacterial phyla (Woese, 1987). One of these contains oxygenic photosynthetic prokaryotes, cyanobacteria and prochlorophytes, which have different pigment compositions and are genetically related on the basis of 16S rRNA sequences (Woese, 1987).

Cyanobacteria contain chlorophyll- a and phycobiliproteins and prochlorophytes possess chlorophyll- a as well as chlorophyll- b , but lack phycobiliproteins (Castenholz & Rippka, 1989; Lewin, 1989; Matthijs et al. , 1994). The prochlorophytes contain three genera: Prochloron , Prochlorothrix (Lewin, 1989), and Prochlorococcus (Partensky et al. , 1999). 16S rDNA sequence analysis has revealed that prochlorophytes emerged within the cyanobacteria, but on separate branches (Urbach et al. , 1992; Wilmotte, 1994). Prochlorophytes are phylogenetically nearest to Synechococcus (Urbach et al. , 1998).

The evolutionary relationships among cyanobacteria have been published by Giovannoni et al. (1988), Wilmotte (1994), and Turner (1997). The 16S rRNA sequence analysis (Fig. 2) were congruent to the taxonomic sections of II, III and IV defined by Rippka et al. , (1979). On the contrary, sections I and III were scattered in different lineages and sometimes mixed. The heterocystous filamentous strains were all in the same cluster. In this cluster, the Nodularia strain PCC73104 grouped with the Anabaena cylindrica PCC7122 strain. Furthermore, it was closely related to Nostoc (PCC73102 and PCC7120) and to the Cylindrospermum (PCC7417) strains (Wilmotte, 1994).

 

1.4.1. Molecular methods used in cyanobacterial taxonomy

Most bacterial genomes contain genes from multiple sources, even from genetically distant ones (Doolittle, 1999). Nowadays, it is suspected that the even most trusted chronometers, rRNA genes, can be transferred (Doolittle, 1999). These genes, which are functionally constant and are composed of highly conserved as well as more variable domains, have been utilised for phylogenetic analysis in bacteria (Vandamme et al. , 1996). Outlines of bacterial phylogenetic relationships emerged from the work of Woese (1987), who pioneered the comparison of rDNA sequences.

The first complete cyanobacterial 16S rDNA sequence was released by Tomioka and Sugiura (1983). In 1988, Giovannoni and co-authors published the first study of evolutionary relationships among cyanobacteria using partial 16S rDNA sequences (Giovannoni et al. , 1988). The sequencing of the 16S rRNA gene have resulted in a rRNA sequence database. At the end of 1998, 171 16S rRNA genes were sequenced from cyanobacteria.

These 171 cyanobacterial rDNA sequences (81 complete sequences comprising nearly 1500 nucleotides and 90 partial sequences) serve as the backbone for modern cyanobacterial taxonomy (Wilmotte, 1994). One partial (ARB_40A3CBCC, Giovannoni et al. 1988) and one complete (aj22447, Hayes & Barker, 1997) 16S rDNA sequence exist from Nodularia .

The molecular methods for studying genotypic relationships among cyanobacteria have been reviewed by Wilmotte (1994). In the present work, only the DNA- and rRNA sequence-based studies of free-living cultured cyanobacteria have been reviewed (Table 5).

Over the recent years, techniques based on sequences of rRNA genes have become the most widely used methods for identification, classification, and phylogeny of cyanobacteria. In addition to direct comparison of the DNA sequences, other methods based on amplification of rRNA genes have been used. The amplified ribosomal genes can be digested by restriction enzymes and the resulting patterns analysed, this technique has been termed restriction fragment length polymorphism (RFLP). Before the introduction of the polymerase chain reaction (PCR) method (Lane et al. , 1985), ribotyping based on labelled-rRNA probe have revealed the hybridised fragments generated after restriction enzyme digestion.

During the last few years, a battery of DNA-directed typing methods has been used for PCR-based genomic fingerprinting of cyanobacteria. Genomic fingerprints have been produced by PCR with random (RAPD) or by arbitrary primers (AP). In addition, fingerprints have been generated with primers corresponding to the repetitive extragenic palindromic (REP) and enterobacterial repetitive intergenic consensus (ERIC) sequences, and to the long and short tandemly repeated repetitive (LTRR and STRR) sequences. The function of repetitive and random amplified polymorphic DNA elements is not known. In addition, cyanobacterium-specific primers have been developed to identify cultured and natural samples. This method has been named "Specific PCR identification" or "Diagnostic PCR".

DNA base composition has been determined for several cyanobacterial strains in the Pasteur Culture Collection. Generally, large differences in DNA base composition reflect the fact that strains are not closely related, whereas similar guanine and cytosine (G+C) percentages give no information about genotypic relationships, therefore the taxonomic value of this method at the species level is low (Wilmotte, 1994). The species should be delineated according to DNA-DNA hybridisation studies, which established the base composition homology between different DNA strains. For strains of the same species at least 70% hybridisation is needed (Wayne et al ., 1987). Furthermore, protein-coding genes have been sequenced and probed. These genes can be used for identification and for classification of strains, but not for phylogeny, since they are not universally distributed and essential among bacteria (Woese, 1987), thus different molecular methods gave different taxonomic information (Vandamme et al. , 1996).

 

Table 5. DNA- and rRNA sequence-based techniques applied for studying the genetic diversity of free-living cyanobacteria

………………………………………………………………………………………………………………………………………..

List of studied genes (their product and/or function): apcAB, allophycocyanin (phycobiliproteins, constituting the phycobilisome core); cpcABC, phycocyanin (phycobiliproteins, constituting the rod elements of phycobilisome); cpeAB , phycoerythrin (phycobiliproteins, constituting the rod elements of phycobilisome); glnA, glutamine synthetase (NH 4 + assimilation); gvp A, structural gas vesicle protein (buoyancy); nifDH, dinitrogenase and nitrogenase reductase (nitrogenase, nitrogen fixation); petBD, cytochrome b 6 and subunit IV (cytochrome b 6 /f complex, photosynthetic electron transport); psbAD, D1 and D2 proteins (photosystem II, photosynthetic electron transfer); psbBC, antenna polypeptides CP47 and CP43 (photosystem II, oxygen evolution); rbcLS, large and small subunits of RubisCo (CO 2 fixation); rpoCD, core enzyme and sigma factors (RNA polymerase, transcription).

Method Reference
Sequencing:  
- 16S rRNA

Bonen & Doolittle, 1976; Tomioka & Sugiura, 1983; Giovannoni et al. , 1988; Ligon et al. , 1991; Wilmotte et al. , 1992, 1993, 1994; Nelissen et al. , 1992, 1994, 1996; Garchia-Pichel et al. , 1996, 1998; Palinska et al. , 1996; Neilan et al. , 1994a,b, 1997a; Ishida et al. , 1997; Kane et al. , 1997; Turner, 1997; Turner et al. , 1999; Otsuka et al. , 1998; Urbach et al. , 1998; Rudi et al. , 1997, 1998; Barker et al. , 1999; Honda et al. , 1999; Saker et al. , 1999; Shaw et al. , 1999; Lyra et al. , 2000

- rRNA ITS

Williamson & Doolittle, 1983; Tomioka & Sugiura, 1984; Nelissen et al. , 1994; Barker et al. , 1999; Otsuka et al. , 1999; Postius & Ernst, 1999

- tRNA Leu (UAA) Rudi & Jakobsen, 1997, 1999
- rpoC

Palenik & Swift, 1996; Toledo & Palenik, 1997; Wilson et al. , 2000

- PC-IGS Hayes & Barker, 1997; Barker et al. , 1999; Bolch et al. , 1999
- psbB , petBD Urbach et al. , 1998
- nifH

Ben-Borath & Zehr, 1994; Ben-Borath et al. , 1993; Steppe et al. , 1996; Zehr et al. , 1997

- rbcLX Rudi et al. , 1998
- gvpA -IGS Barker et al. , 1999
PCR/DGGE:  
- 16S rRNA Garchia-Pichel et al. , 1996
PCR/RFLP:  
- 16S rRNA Lyra et al. , 1997, 2000; Margheri et al. , 1999
- rRNA ITS

eilan, 1996; Neilan et al. , 1997b; Lu et al. , 1997; West & Adams, 1997; Smith et al. , 1998; Scheldeman et al. , 1999

- PC-IGS

Neilan et al. , 1995; Bolch et al. , 1996; Neilan, 1996; Bolch et al. , 1999

Specific PCR identification:  
- PC-IGS Neilan et al. , 1995; Hayes & Barker, 1997; Barker et al. , 1999
- rRNA ITS Neilan, 1996; Neilan et al. , 1997b; Barker et al. , 1999
- gvpA -IGS Barker et al. , 1999
- rpoC1 Wilson et al. , 2000
PCR:  
- with RAPD and AP primers

Neilan, 1995, 1996; Komárek, 1996; Nishihara et al. , 1997; West & Adams, 1997; Bolch et al. , 1999

- with repetitive DNA sequences
(REP, ERIC, HIP1, STRR, LTRR)

Versalovic et al . , 1991; Robinson et al. , 1995; Rasmussen & Svenning, 1998; Smith et al., 1998; Lyra et al. , 2000; Wilson et al. , 2000

Southern blot RFLP hybricization:  
Probes:  
- REPs Asayma et al. , 1996
- rRNA, cpcABC , psbA , rbcL , cpeAB Douglas & Carr, 1988
- psbAI Ernst et al. , 1995; Postius & Ernst, 1999
- glnA , rbcS , psbA , nifD excision elements Gebhardt & Nierzwicki-Bauer, 1991
- psbA , psbCD Golden et al. , 1989
- STRR Mazel et al. , 1990; Rouhiainen et al. , 1995
- rRNA Golden et al. , 1989; Nelissen et al. , 1996
- 16S and 23S rRNA Nichols et al. , 1982
- tRNA Leu (UAA) Rudi & Jakobsen 1997, 1999
- 16S rRNA Schönhuber et al. , 1999
- psbA1 , cpeA , cpeB Wood & Townsend, 1990
- cpcAB , apcAB , gvpA1 , nifH Zimmermann & Culley, 1991
DNA base composition:

Herdman et al. , 1979a; Stam, 1980; Stulp & Stam, 1984; Wilmotte & Stam, 1984

DNA-DNA hybridization:

Stam, 1980; Lachance, 1981; Stulp & Stam, 1984; Wilmotte & Stam, 1984

 

 

 

1.4.2. Morphological and genetic variation of Nodularia cultures and populations

Komárek and co-authors (1993) have studied the taxonomy of the genus Nodularia . Within this genus, two distinct groups of species, based on the ability to produce gas vesicles, were differentiated. The studies of the ultrastructure of genus Nodularia (Gumpert et al. , 1987; Šmarda et al. , 1988; Albertano et al. , 1996; Šmarda & Šmajs, 1996) have revealed large amounts of densely packed gas vesicles. Their densities in cells separated them into three distinct types (Šmarda & Šmajs, 1996). For example, the Baltic Sea Nodularia had three types of gas vesicles in species of N. baltica , N. spumigena , and N. litorea (Šmarda & Šmajs, 1996).

In addition to the size and the density of gas vesicles, Komárek et al. (1993) have used several other markers in the intrageneric taxonomy of Nodularia : the size of cells of all types, the morphology of akinetes, and the ecological properties of species types. Based on these features, Komárek et al. (1993) suggested distinction of several types of Nodularia species including three benthic species ( N. harveyana , N. sphaerocarpa , N. willei ) and four planktic species ( N. baltica , N. litorea , N. spumigena , N. crassa ). Four of these species (Table 6: N. harveyana , N. baltica , N. litorea , N. spumigena ) have been isolated from the Baltic Sea (Komárek et al. , 1993).

In the study of Hayes and Barker (1997), the genetic diversity of Baltic Sea Nodularia population seemed to be restricted to few genotypes. The diagnostic PCR study (also termed specific PCR identification) of Nodularia population in the Southern Baltic Sea in 1996 showed two PC-IGS (the intergenic spacer region of the phycocyanin operon) genotypes from 156 filaments. Later in 1994, the study of Barker et al. (1999) revealed three groups based on PC-IGS, two groups based on gvp A-IGS (the intergenic spacer region between two copies of gvpA gene), and three groups based on rDNA-ITS (the 16S-23S rRNA internal transcribed region) in thirteen clonal Nodularia strains. The authors could not find any correlation between the genotypic and phenotypic characters examined (trichome width, degree of coiling, and properties of gas vesicles).

The morphological and genetic variation using RFLP and DNA sequencing of the cpcBA -IGS region and RAPD-PCR of Nodularia strains from Australia and from other geographical sites have been studied (Bolch et al. , 1996, 1999). Geographically diverse Nodularia strains had a near cpcBA -IGS (the phycocyanin intergenic spacer region) sequence identity (Bolch et al. , 1999) suggesting that Nodularia is globally distributed as suggested also by Hayes and Barker (1997). However, genetically distinct geographical strains were showed by RAPD-PCR (Bolch et al , 1999) and by RFLP of the cpcBA -IGS (Bolch et al. 1996). Genetic groupings based on the sequence identity were supported by morphological features (size and morphology of vegetative cells, heterocysts and akinetes, and diameter and morphology of trichomes) (Bolch et al., 1999).

It has been suggested that the Baltic Sea Nodularia populations have exchanged genetic material, since the PC-IGS, gvpA -IGS, and rDNA-ITS genotypic groupings of Nodularia strains were not congruent (Barker et al. , 1999). The exchange of genetic material between genetically closely related cyanobacteria has been suggested also by Rudi et al. (1998). The authors proposed that the genetic exchange has led to the observed sequence homogeneity between these organisms and that it may also explain the similarity between the fossil and the recent species found by Schopf and others (1994). However, several studies have revealed that, for example, Synechococcus strains take up the DNA of any source (see Lorenz & Wackernagel, 1994) meaning that exchange may even occur between distant genera.

 

Table 6. Morphological and ecological properties of planktonic and benthic Nodularia
species recorded in the Baltic Sea

………………………………………………………………………………………………………………………………………

Data on morphological and ecological properties were taken from Komárek et al. (1993) and data on gas vesicles were
derived from Šmarda & Šmajs (1996). NA, Not applicable.

Charcters N. baltica N. harveyana N litorea N. spumigena
Trichome:        
Width (΅m)

5-6

4-5 10-15 7-12
Cell length (΅m) 2-5 2-3 2-4 2-4
Heterocysts:        
Length x width (΅m) 2-5 x 5-8 3-5 x 4-6 4-7 x 10-15 4-5 x 9-14
Akinetes:        
Length x width (΅m) 4-8 x 6-9 4-8 x 6-7 6-10 x 14-15 6-12 x 10-12
Observations

Sometimes solitary or in rows

In series of two to sixteen

Solitary or in short series

In series or discontinuous rows, rarely solitary or in twos

Gas vesicles:        
Present? Yes No Yes Variable
Density (΅m -2 ) 140/160-180 NA 215/230-240 139/160-180
Ecology

Metaphyton or phytoplankton; marine, brackishand saline waters.

Benthic or periphyton; saline pools and lakes, thermal springs and marshes with high salinity.

Phytoplankton; marine, brackish and saline waters.

Metaphyton and euplankton; marine, brackish and saline waters.

 

 


Back to the title page | E-thesis main page