Simple three‐pool model accurately describes patterns of long‐term litter decomposition in diverse climates

分解 木质素 环境科学 生态系统 垃圾箱 初级生产 纤维素 植物凋落物 固碳 气候变化 大气科学 生态学 化学 土壤科学 生物 二氧化碳 地质学 有机化学
作者
E. Carol Adair,William J. Parton,STEVEN J. DEL GROSSO,Whendee L. Silver,Mark E. Harmon,Sonia A. Hall,Ingrid C. Burke,Stephen C. Hart
出处
期刊:Global Change Biology [Wiley]
卷期号:14 (11): 2636-2660 被引量:535
标识
DOI:10.1111/j.1365-2486.2008.01674.x
摘要

Abstract As atmospheric CO 2 increases, ecosystem carbon sequestration will largely depend on how global changes in climate will alter the balance between net primary production and decomposition. The response of primary production to climatic change has been examined using well‐validated mechanistic models, but the same is not true for decomposition, a primary source of atmospheric CO 2 . We used the Long‐term Intersite Decomposition Experiment Team (LIDET) dataset and model‐selection techniques to choose and parameterize a model that describes global patterns of litter decomposition. Mass loss was best represented by a three‐pool negative exponential model, with a rapidly decomposing labile pool, an intermediate pool representing cellulose, and a recalcitrant pool. The initial litter lignin/nitrogen ratio defined the size of labile and intermediate pools. Lignin content determined the size of the recalcitrant pool. The decomposition rate of all pools was modified by climate, but the intermediate pool's decomposition rate was also controlled by relative amounts of litter cellulose and lignin (indicative of lignin‐encrusted cellulose). The effect of climate on decomposition was best represented by a composite variable that multiplied a water‐stress function by the Lloyd and Taylor variable Q 10 temperature function. Although our model explained nearly 70% of the variation in LIDET data, we observed systematic deviations from model predictions. Below‐ and aboveground material decomposed at notably different rates, depending on the decomposition stage. Decomposition in certain ecosystem‐specific environmental conditions was not well represented by our model; this included roots in very wet and cold soils, and aboveground litter in N‐rich and arid sites. Despite these limitations, our model may still be extremely useful for global modeling efforts, because it accurately ( R 2 =0.6804) described general patterns of long‐term global decomposition for a wide array of litter types, using relatively minimal climatic and litter quality data.
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