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By C. H. Dickinson
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Extra resources for Biology of Plant Litter Decomposition. Volume 1
Harpenden. ATHERTON, N. , CRANWELL, P. , FLOYD, A. J. and HOWARTH, R. D. (1967). Tetrahedron 23, 1653-1667. BARLEY, K. P. and JENNINGS, A. C. (1959). J. agric. Res. 10, 364-370. BARTHOLOMEW, W. V. and KIRKHAM, D. (i960). Trans, jth Int. Congr. Soil Sei. 2, 471-477· BLACK, C. A. (1968). " 2nd edition. John Wiley, New York. BLOOMFIELD, C. /. Set. Fd. Agric. 8, 389-392. BREMNER, J. M. (1967). In "Soil Biochemistry" (A. D. McLaren and G. H. Peterson, eds), pp. 19-62. Marcel Dekker, New York. BUNNELL, F.
Terrestrial Plants Apart from loss of dry matter, quantitative information on the course of decomposition in lower terrestrial plants under natural conditions is limited to a very small number of species. Among the mosses, Sphagnum has received most attention. Kox (1954), for example, by careful microscopic examination of decomposing Sphagnum, was able to relate the sequence of decay to the distribution of cellulose and pectin in stem tissues, before she experimented with associated micro-organisms.
At present it employs no data on microbial biomass or soil invertebrates and excludes feedback effects of mineralization and humus formation on plant growth, but these are not limitations of the method. The model structure was designed to accommodate more detailed process modelling of the activity of decomposer organisms as further data become available and was not designed to model mineral recycling. The well-known *'World Dynamics" model of Forrester (1971) was programmed in DYNAMO and run on an IBM 709-90 computer.