Five species accounted for 95 percent of the stems of at least 10 cm DBH on three plots totaling 0.22 ha in the dwarf cloud forest of the Luquillo Mountains in Puerto Rico. Mean density for stems of at least 10 cm DBH was 3671 ? 516 stems/ha, and mean basal area was 49.1 ? 8.2 m2/ha. The aboveground woody biomass on two small plots of 0.0036 ha, one located on a ridge and the other 100 m to the leeward, was 48 and 110 t/ha, respectively. Leaf area index on the ridge was 1.99 m2/m2, leaf biomass was 288 g/m2, and specific leaf weight was 14.5 mg/cm2. Mean annual litterfall rates averaged only 0.85 g/m2/day (3.10 t/ha/yr), of which 79 percent was leaf litter, 9 percent wood litter, and 12 percent miscellaneous material. The rate at which nutrients returned to the soil (kg/ha/yr) averaged 23.9 for nitrogen, 0.7 for phosphorus, 4.3 for potassium, 16.3 for calcium, and 7.6 for magnesium. The annual increment in tree diameter was low, averaging only 0.03 ? 0.01 cm/yr. For trees at least 2.5 cm in diameter, aboveground biomass accumulated at an average rate of 45 g/m2/yr. Net primary productivity was 3.84 t/ha/yr. ZONATION OF FORESTS WITHIN MONTANE HABITATS on tropical islands is condensed into a narrow altitudinal range, a phenomenon known as the Massenerhebung effect. One example is the Luquillo Mountains of northeastern Puerto Rico, which abruptly rise to 1060 m in only 15 km. As elevation increases, the number of arborescent stems/ha increases, while decreases occur in average height of dominants, average DBH, basal area/ha, and number of species per unit area (White 1963). The dwarf forest, an association in the lower montane rain forest (sensu Holdridge 1967, Ewel & Whitmore 1973) on the upper slopes and summits of the Luquillo Mountains, is short, frequently contorted, and densecovered with epiphytes including bromeliads, liverworts, and mosses-and includes only a few species of trees (Beard 1949, Wadsworth 1951, Howard 1968). The climate is wet, with nearly 5000 mm/yr of rainfall. Mean monthly temperatures range from 18 to 20?C (Weaver et al. 1973). The vegetation is commonly saturated with moisture and frequently enveloped in clouds. Both aerial and superficial roots are common (Lyford 1969). Saturated soils, impeded root respiration, physiological drought, high winds, high soil leaching, low nutrient availability, low temperatures, high fog incidence, reduced solar insolation, high humidity, reduced transpiration rates, and shallow soil have all been suggested as causal agents in stunting, either individually or in combination (Gleason & Cook 1927, Beard 1944, Wadsworth & Bonnet 1951, Holdridge 1967, Odum 1968, Baynton 1969, Grubb 1971, Weaver et al. 1973). Similar forests elsewhere in the Caribbean and Central America have been discussed by La Bastille and Pool (1978). Despite the abundance of hypotheses regarding the cause of dwarf cloud forests, little information is available on their growth rates, net primary productivity (NPP), and nutrient cyding. The purpose of this study is to determine species composition and standing biomass of the dwarf forest, and to estimate the rates of NPP, litterfall, and diameter and biomass growth of arborescent species. Rates of nutrient return to the soil are also in-