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Significant Developments in Soil Microbiology


Significant Developments in Soil Microbiology

There have been several notable contributions made by several scientists in soil microbiology since the beginning of the present century. Omeliansky in 1902 found out that anaerobic soil bacteria degrade cellulose.

Lipman and Brown in 1903 in the U.S.A., studied ammonification of organic nitrogenous substances by soil microorganisms and developed the 'tumbler or beaker' method for studies on different types of transformations in soil.

The work on rhizosphere started in 1904 by the German scientist Hiltner was later continued in the U.S.A. by Starkey in 1929, in Canada by Lochhead in 1940 and Katznelson in 1946, in Australia by Rovira in 1956, in Czechoslovakia by Matcura and associates in 1961 and in other countries including India by several workers. The importance of

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protozoa in controlling bacterial population and activity in soil was enunciated in 1909 by Russel and Hutchinson at Rothamsted in England.

Side by side with these scientific developments, techniques in the study such as the direct soil examination by Conn in 1918 and the contact slide by Rossi in 1927 and Cholodny in 1930 were innovated. In fact, modifications of some of these techniques are still in vogue today.

The work of Rayner and Melin between 1921 and 1927 in Uppsala marked the beginning of an intensive study of mycorrhiza. Among others who subsequently got interested in mycorrhiza, mention may be made of Harley in the U.K., Gerdemann in Germany, Marx, Trapp and Hacskaylo in the U.S.A. and Bowen in Australia who worked on ectomycorrhizal fungi.


In 1936, Garrett established a school in the U.K. on soil fungi and their ecological classification in relation to the nature of available native substrate. Alexander Fleming in 1929 discovered penicillin which was followed by the discovery of streptomycin by Waksman in 1944.

These findings led to an upsurge in the study of antibiotics in general (as evidenced by large number of antibiotics discovered) and antibiosis in soil in particular.

In recent years, the occurrence and importance of arbuscular endomycorrhizal fungi (Ex. Golmus, Acaulospora) in roots of plants have been repeatedly pointed out. Barbara Mosse at the Rothamsted Experimental Station in England and several other workers in the U.S.A., India and New Zealand have now realized the potential of AM fungi in phosphate mobilization into plants.

The work on microbiological transformations in soil was continued in the forties in Europe at the famous Pasteur Research Institute in Paris by Pochon and his associates.

At the same time, Gerretsen and Mulder were busy in Wageningen on work concerning phosphate mobilization by soil microorganisms and the importance of molybdenum in the nitrogen metabolism of microorganisms.

By about this time, Ruinen in 1956 developed the concept of phyllosphere (the microbiology of leaf surface) from her studies on the leaf surface microflora of Indonesian forest trees.


In the U.S.A., fundamental studies on soil bacteria were carried out by Van Niel in 1931 on chemo-autotrophic bacteria and bacterial photosynthesis, by Umbreit in 1947 on problems of autotrophy, by Barker on anaerobic fermentation by methane bacteria, by Starkey in 1945 on transformations of iron bacteria and by Allen and Allen in 1940 on soil bacteria in general and root nodule bacteria in particular.


The contributions made by Fred and co-workers in 1932 in connection with nodule bacteria deserve special mention. Subsequently, Alexander in 1961 started a school of soil microbiology at the Cornell University, with particular reference to microbiological aspects of pesticide degradation.

The colourful microalgae fascinated many workers all over the world. Fritsch, Fogg and Stewart in the U.K. and Iyengar in India were the foremost investigators in the study of algae in general and microalgae in particular.

 

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