1992
DOI: 10.2307/2260861
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Ecological Studies on a Lowland Evergreen Rain Forest on Maraca Island, Roraima, Brazil. II. Litter and Nutrient Cycling

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Cited by 118 publications
(83 citation statements)
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“…The total litterfall recorded over the course of the year at the four study sites on the middle Xingu River were consistent with the estimates obtained for other Amazonian forests, including terra firme habitats, and igapó and várzea swamps (Klinge, 1977;Adis et al, 1979;Silva and Lobo, 1982;Silva, 1984;Worbes, 1986b;Scott et al, 1992). The leaf fraction accounted for more than 50% of the volume of litter, even at the sites (Arroz Cru) where the lowest values were recorded.…”
Section: Discussionsupporting
confidence: 83%
“…The total litterfall recorded over the course of the year at the four study sites on the middle Xingu River were consistent with the estimates obtained for other Amazonian forests, including terra firme habitats, and igapó and várzea swamps (Klinge, 1977;Adis et al, 1979;Silva and Lobo, 1982;Silva, 1984;Worbes, 1986b;Scott et al, 1992). The leaf fraction accounted for more than 50% of the volume of litter, even at the sites (Arroz Cru) where the lowest values were recorded.…”
Section: Discussionsupporting
confidence: 83%
“…As much as 8 tons of leaf litter per hectare per year can be introduced to the soil surface of a tropical rainforest. Annual inputs per gram of litter can equate to approximately 14 mg N, 0.5 mg P, 2 mg K, 8 mg Ca, and 2 mg Mg (Ewel 1976; Scott et al 1992). These nutrient additions, estimated to have occurred over a period of approximately 110 years, were associated with 81 μg N g −1 soil, 900 μg P g −1 soil, 8 μg K g −1 soil, 2,400 μg Ca g −1 soil and 365 μg Mg g −1 soil (Scott et al 1992).…”
Section: Decomposition Stages and Gravesoil Ecologymentioning
confidence: 99%
“…Annual inputs per gram of litter can equate to approximately 14 mg N, 0.5 mg P, 2 mg K, 8 mg Ca, and 2 mg Mg (Ewel 1976; Scott et al 1992). These nutrient additions, estimated to have occurred over a period of approximately 110 years, were associated with 81 μg N g −1 soil, 900 μg P g −1 soil, 8 μg K g −1 soil, 2,400 μg Ca g −1 soil and 365 μg Mg g −1 soil (Scott et al 1992). While the effect of cadaver decomposition on soil nutrient status can be similar to, or less than, that observed with plant and fecal breakdown, peak nutrient values associated with cadaver decomposition can occur in much less time than required by fecal or plant materials.…”
Section: Decomposition Stages and Gravesoil Ecologymentioning
confidence: 99%
“…Other factors also affecting production are the plant species [4], the age of the forest system [2,32] and species density [3]. [39,40], Scott et al [43], Son and Gower [44]. [27] and Turrión et al [45].…”
mentioning
confidence: 99%