Abstract
Gas vacuoles are found only in aquatic prokaryotes (Cohen-Bazire, Kunisawa, and Pfennig, 1969; Walsby, 1974) where, by virtue of their low density, they are important in providing buoyancy. Among cyanobacteria, gas vacuoles are found most commonly in the truly planktonic forms that grow freely suspended in lakes. Gas vacuoles are found in all of the waterbloom-forming cyanobacteria and are responsible for buoying them to the water surface (Reynolds and Walsby, 1975). However, there are some non-gas-vacuolate cyanobacteria that are found in the plankton. They are either attached to waterbloom-forming colonies or are small-celled or slender filamentous types with low sedimentation speeds. These nonvacuolate forms can be isolated by the methods described by Rippka, Waterbury, and Stanier (this Handbook, Chapter 8).
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Walsby, A.E. (1981). Cyanobacteria: Planktonic Gas-Vacuolate Forms. In: Starr, M.P., Stolp, H., Trüper, H.G., Balows, A., Schlegel, H.G. (eds) The Prokaryotes. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-13187-9_10
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DOI: https://doi.org/10.1007/978-3-662-13187-9_10
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