Respiration from coarse wood litter in central Amazon forests

被引:0
作者
Jeffrey Q. Chambers
Joshua P. Schimel
Atonio D. Nobre
机构
[1] University of California,Department of Ecology, Evolution and Marine Biology
[2] Instituto Nacional de Pesquisas da Amazônia (INPA),Department of Ecology, Evolution and Marine Biology
[3] Biological Dynamics of Forest Fragments Project INPA,undefined
[4] University of California,undefined
[5] Instituto Nacional de Pesquisas da Amazônia (INPA),undefined
来源
Biogeochemistry | 2001年 / 52卷
关键词
carbon cycling; heterotrophic respiration; net ecosystem exchange; predictive model; tropical forest; wood decomposition;
D O I
暂无
中图分类号
学科分类号
摘要
Respiration from coarse litter (trunks and large branches >10 cm diameter) was studied in central Amazon forests. Respiration ratesvaried over almost two orders of magnitude (1.003–0.014 µg Cg−1 C min−1, n = 61), and weresignificantly correlated with wood density (r2adj= 0.42), and moisture content (r2adj= 0.39). Additional samples taken from a nearby pasture indicatedthat wood moisture content was the most important factor controllingrespiration rates across sites (r2adj =0.65). Based on average coarse litter wood density and moisture content,the mean long-term carbon loss rate due to respiration was estimated tobe 0.13 yr−1 (range of 95% prediction interval(PI) = 0.11–0.15 yr−1). Comparing meanrespiration rate with mean mass loss (decomposition) rate from aprevious study, respiratory emissions to the atmosphere from coarselitter were predicted to be 76% (95% PI =65–88%) of total carbon loss, or about 1.9 (95% PI= 1.6–2.2) Mg C ha−1yr−1. Optimum respiration activity corresponded toabout 2.5 g H2O g−1 dry wood, and severelyrestricted respiration to < 0.5 g H2O g−1dry wood. Respiration from coarse litter in central Amazon forests iscomparable in magnitude to decomposing fine surface litter (e.g. leaves,twigs) and is an important carbon cycling component when characterizingheterotrophic respiration budgets and net ecosystem exchange(NEE).
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页码:115 / 131
页数:16
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共 120 条
[1]  
Boddy L(1983)Effect of temperature and water potential on growth rate of wood-rotting Basidiomycetes Trans. Brit. Mycol. Soc. 80 141-149
[2]  
Boddy L(1983)Microclimate and moisture dynamics of wood decomposing in terrestrial ecosystems Soil Biol. Biochem. 15 149-157
[3]  
Bravard S(1989)Geochemical differences in an Oxisol-Spodosol toposequence of Amazonia, Brazil Geoderma 44 29-42
[4]  
Righi D(1988)Early patterns of heterotrophic activity in conifer logs Proceedings of the Royal Society of Edinburgh 94B 33-43
[5]  
Carptenter SE(1998)Ancient trees in Amazonia Nature 391 135-136
[6]  
Harmon ME(1995)Gas diffusivity and the production of CO2 in deep soils of the eastern Amazon Tellus 47B 550-565
[7]  
Ingham ER(1984)Minimum water potentials for growth of some litter-decomposing agarics and other basidiomycetes Trans. Brit. Mycol. Soc. 83 152-153
[8]  
Kelsey RG(1985)Changes in relationship between water content and water potential after decay and its significance for fungal successions Trans. Brit. Mycol. Soc. 85 649-653
[9]  
Lattin JD(1990)Atmosphere-Biosphere exchange of CO Journal of Geophysical Research 95 16851-16864
[10]  
Schowalter TD(1997) and O Journal of Geophysical Research 102 28, 987-28, 996