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Microbiology

, Volume 78, Issue 4, pp 468–473 | Cite as

A puddle: an ombrophilic cyano-bacterial community

  • G. A. Zavarzin
  • T. V. Alekseeva
Experimental Articles

Abstract

Sequential stages of formation of an ombrophilic cyano-bacterial community on clay were determined in a laboratory model of a puddle community. In a suspension of washed clay obtained from loamy soil, with montmorillonite as the predominant phase, a bacterial neustonic film is initially formed; it acts as a support for cyanobacterial hormogonia. At the next stage, the upper layer of precipitated clay (about 1 mm) is reinforced by a cyano-bacterial structure of Phormidium sp. trichomes and develops a tissue-like structure. The hormogonia and sheathless cyanobacteria remain free from mineral particles. Subsequently, gas formation results in a separation of a dense cyano-bacterial film from the underlying loose suspension and in formation of gas swellings. The mineral component of the film is differentiated: mineral particles of quartz and feldspar grains are attached to Phormidium sp. trichomes, which act as a factor of mineral selection.

Key words

ombrophilic cyano-bacterial community clays stages of community formation mineralogical composition of a cyano-bacterial film 

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References

  1. 1.
    Zavarzin, G.A., Planet of Bacteria, Vestnik Ross. Akad. Nauk, 2008, vol. 78, pp. 317–323.Google Scholar
  2. 2.
    Sokolova, T.A., Dronova, T.Ya., and Tolpeshta, I.I., Glinistye mineraly v pochvakh: Uchebnoe posobie (Clay Mineral in Soils: A Handbook), Tula: Grif i K, 2005.Google Scholar

Copyright information

© Pleiades Publishing, Ltd. 2009

Authors and Affiliations

  1. 1.Winogradsky Institute of MicrobiologyRussian Academy of SciencesMoscowRussia
  2. 2.Institute for Physicochemical and Biological Problems in Soil SciencePushchinoRussia

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