蓝藻胞外多糖:它们的性质和潜在的生物技术应用

Pengfu Li, S. Harding, Zhi-li Liu
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引用次数: 99

摘要

蓝藻(蓝绿藻)是单细胞或细丝的光合原核生物。具有重要生物学意义的是,某些蓝藻可以固定元素氮(Carr和Whitton, 1982)。一些蓝藻在与底物接触时能够通过滑动运动(Bold and Wynne, 1985)。一些蓝藻具有在干燥和极端温度下生存的能力,并且可以在高pH和高盐度下生长(Flaibani et al., 1989)。蓝藻存在于地球上的大多数环境中。它们在淡水和海洋环境中的分布是世界性的。蓝藻也普遍存在于从热带到极地的土壤和岩石中,从温带气候到极端干旱的沙漠,在那里它们有时参与微生物结壳或垫的形成(Bold和Wynne, 1985;Mazor et al., 1996)。许多重氮营养蓝藻很容易与某些绿藻、苔类、水蕨类和被子植物结合或共生生长(Bold and Wynne, 1985)。长期以来,人们都知道蓝藻可以产生大量的胞外多糖(Drews和Weckesser, 1982)。最近,由于这些物质作为工业胶、生物絮凝剂、土壤调节剂和生物吸附剂的潜在应用,以及它们参与植物的共生过程、滑动运动和微生物与其栖息地之间的一般相互作用,这种大规模生产受到了越来越多的关注(Bertocchi等,1990;画家。1993;Morvan等人,1997;De Philippis和Vincenzini, 1998)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Cyanobacterial Exopolysaccharides: Their Nature and Potential Biotechnological Applications
Cyanobacteria (blue-green algae) are photosynthetic prokaryotic organisms which are unicells or filaments. Of great significance biologically is the fact that certain cyanobacteria can fix elemental nitrogen (Carr and Whitton, 1982). Some cyanobacteri a are capable of movement by gliding when in contact with the substrate (Bold and Wynne, 1985). Some cyanobacteria have the ability to survive desiccation and extremes of temperature, and can grow at high pH and salinity (Flaibani et al., 1989). Cyanobacteria occur in most environments on earth. Their distribution in freshwater and marine environment is cosmopolitan. Cyanobacteria are also commonly found in the soil and in rocks from the tropics to polar regions, and from temperate climates to extreme arid deserts, where they sometimes participate in the formation of microbial crusts or mats (Bold and Wynne, 1985; Mazor et al., 1996). A number of diazotrophic cyanobacteria grow easily in association or symbiosis with certain green algae, liverworts, water ferns, and angiosperms (Bold and Wynne, 1985). Cyanobacteria have been known, for a long time, to produce large amounts of exopolysaccharide (Drews and Weckesser, 1982). Recently, this massive production has received increasing attention due to the potential applications of these substances as industrial gums, bioflocculants, soil conditioners and biosorbants, and to their participation in symbiotic processes in plants, in the gliding movement, and in the general interactions between microorganisms and their habitats (Bertocchi et al., 1990; Painter. 1993; Morvan et al, 1997; De Philippis and Vincenzini, 1998).
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