Journal
GLOBAL CHANGE BIOLOGY
Volume 12, Issue 2, Pages 284-293Publisher
WILEY
DOI: 10.1111/j.1365-2486.2005.01096.x
Keywords
decomposition; forest floor mass; litterfall; long-term carbon; microbial biomass; soil carbon
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Wet tropical forests play a critical role in global ecosystem carbon (C) cycle, but C allocation and the response of different C pools to nutrient addition in these forests remain poorly understood. We measured soil organic carbon (SOC), litterfall, root biomass, microbial biomass and soil physical and chemical properties in a wet tropical forest from May 1996 to July 1997 following a 7-year continuous fertilization. We found that although there was no significant difference in total SOC in the top 0-10 cm of the soils between the fertilization plots (5.42 +/- 0.18 kg m(-2)) and the control plots (5.27 +/- 0.22 kg m(-2)), the proportion of the heavy-fraction organic C in the total SOC was significantly higher in the fertilized plots (59%) than in the control plots (46%) (P < 0.05). The annual decomposition rate of fertilized leaf litter was 13% higher than that of the control leaf litter. We also found that fertilization significantly increased microbial biomass (fungi+bacteria) with 952 +/- 48 mg kg(-1)soil in the fertilized plots and 755 +/- 37 mg kg(-1)soil in the control plots. Our results suggest that fertilization in tropical forests may enhance long-term C sequestration in the soils of tropical wet forests.
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