The decomposition of celluloses is carried on in the soil, and in nature in general, by a large number of different organisms. These belong morphologically to the bacteria, the fungi, and the actinomycetes. The organisms decomposing cellulose, especially the bacteria, vary not only in their morphological, but also in their physiological characteristics. The ability to decompose cellulose seems to be widespread among the fungi and actinomycetes, although some fungi are unable to decompose cellulose at all, while others can readily utilize celluloses as the only source of energy. The growth of actinomycetes, even in the case of those forms which are capable of breaking down celluloses in the absence of other sources of energy, is so limited and the transformation of the cellulose is so small that one might venture the suggestion that they play a rather limited r6le in this process. The bacteria capable of decomposing cellulose fall, however, into a few phy~iologically distinct groups. Physiologically they have been classified as (a) aerobic, (b) anaerobic, (c) thermophilic and (d) denitrifying forms. Morphologically they are (a) sporeforming rods, (b) non-spore forming rods, (c) spirochaetes and vibrios. A few, like the Spirochaeta cytophaga Hutchinson and Clayton, can grow only on cellulose media, while others, like the organisms isolated by Kellerman, McBeth and their associates, seem 1o be able to grow also on other media free from IPaper No. 250 of the Journal Series, New Jersey Agricultural Experiment Stations, Departme nt of Soil Chemistry and Bacteriology.