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Decomposition often Central Himalayan forest litter species was studied for two years to examine: (i) the temporal changes in nutrient concentration and weight loss and its spatial patterns; and (ii) to develop a regional model oflitter weight loss based on the dual controls of climate and substrate quality. (2) The experiments involved five forest communities in an altitudinal gradient, each with distinct vegetation and soil. In addition, a standard leaf litter was placed on the forest floor of each of these forests. (3) Litters high in cell wall constituents tend to be lower in nutrient concentrations. Relative patterns of change in K and Ca concentrations tended to differ from those ofN, P and Na. (4) Monthly rainfall could account for 25-89% of monthly weight loss of litter on each site. Analysis of the variation in annual weight loss from site to site indicates that the annual temperature, actual evapotranspiration (AET) and altitude explained, respectively, 48.7%, 53.6% and 49.1% of the variability. (5) Measures of cell wall constituents, e.g. lignin concentration, could account for up to 60% of the variability in weight loss in the first year; however, lignin, as a predictor of " I weight loss rate, contains considerable information about plant nutrients. Linear combinations of lignin, annual temperature and AET/lignin, produced an r2 of >0,78. (6) In warm temperate and subtropical climates the cell wall constituents seem to be good predictors of weight loss in the first year while in cool temperate to arctic climates, the early stages of decay are prolonged, resulting in good prediction by litter nutrients.

Decomposition of branch litter of four angiosperm and one conifer species was studied over a two-year period. Litter species and the corresponding forest type are: (i) Shorea robusta, sal forest at 329 m; (ii) Lyonia ovalifolia, mixed-pine broadleaf forest at 1 350m; (iii) Pinus roxburghii, pine forest at 1 750m; (iv) Quercus leucotrichophora, mixed oak-pine forest at 1 850 m; and (v) Quercus lanuginosa, mixed oak forest at 2 150 m.The weight loss ranged from 4 4 -8 9 % . Litter moisture and air temperature had significant positive effect on decomposition. The decomposition rate decreased with an increase in altitude and was inversely related with lignin content. Linear combinations of lignin content with rainfall and with temperature indicated significant interactive influence on decomposition. Snyder (Singh & Singh, 1984). Mierocerotermes championiiBranches of the above species (4.4 to 5,4cm Vegetatio 64, 49-53, 1985.

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