2015
DOI: 10.1111/1365-2745.12467
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Decay rates of leaf litters from arbuscular mycorrhizal trees are more sensitive to soil effects than litters from ectomycorrhizal trees

Abstract: 1.While it is well established that leaf litter decomposition is controlled by climate and substrate quality at broad spatial scales, conceptual frameworks that consider how local-scale factors affect litter decay in heterogeneous landscapes are generally lacking. 2. A critical challenge in disentangling the relative impacts of and interactions among local-scale factors is that these factors frequently covary due to feedbacks between plant and soil communities. For example, forest plots dominated by trees that… Show more

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Cited by 98 publications
(93 citation statements)
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“…Variation in fine-scale soil conditions has been proposed to explain differences in local decomposition rates [7, 42], but we found mixed evidence to extend this hypothesis into fire-dominated systems. We found significant differences in decomposition rates across landscape positions (i.e.…”
Section: Discussionmentioning
confidence: 44%
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“…Variation in fine-scale soil conditions has been proposed to explain differences in local decomposition rates [7, 42], but we found mixed evidence to extend this hypothesis into fire-dominated systems. We found significant differences in decomposition rates across landscape positions (i.e.…”
Section: Discussionmentioning
confidence: 44%
“…Historically, climactic variables like precipitation and temperature have been thought to exert the strongest control over decomposition rates at the global scale [3, 4], but there has recently been a push to move away from this climate-centric paradigm and incorporate local, biotic regulatory factors into decomposition frameworks [5, 6]. Within ecosystems, the effect of litter quality on decomposition is modulated by local soil environmental conditions and microclimate [7, 8]. Across biomes, litter decomposition may be predominantly explained by litter quality, itself which may be related to the life history strategies of individual species [6].…”
Section: Introductionmentioning
confidence: 99%
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“…N的输入、 稳定及输出等过程, 从而造成不同菌根类 型森林土壤C、N循环的差异 (Austin & Zanne, 2015;Brzostek et al, 2015;Midgley et al, 2015;Moore et al, 2015;Soudzilovskaia et al, 2015)。然而, 由于试 验方法、研究尺度等限制, 不同菌根类型树种对森 林土壤C、 N循环过程的影响机制仍存在较大的不确 定性 (Moore et al, 2015) (Vesterdal et al, 2013;Lin et al, 2016)。对AM和EM森林凋落物层C 储量差异的研究结果较为一致, 均表现为AM小于 EM (图1, Vesterdal et al, 2013;Lin et al, 2016)。两 个菌根类型树种凋落物C输入量基本相同; 而由于 AM树种凋落物质量较高(主要因其C或木质素浓度 与N浓度的比值均显著小于EM树种), 质量损失较 快, 从而使AM森林凋落物层C输出量高于EM森林 (Cornelissen et al, 2001;Lin et al, 2016;Taylor et al, …”
Section: )。 不同菌根树种可通过地上(凋落物)及地下(根 系及菌根真菌)特性直接或间接地影响森林土壤C、unclassified
“…。菌根真菌不仅对植物的 存活和生长具有重要作用, 而且其与土壤自由微生 物的相互作用在森林生态系统的生态过程(尤其是 土壤碳(C)、氮(N)循环)中也扮演着重要角色 (Orwin et al, 2011;Veresoglou et al, 2012;Phillips et al, 2013;Bardgett et al, 2014;McCormack et al, 2015;Laliberté, 2016)。由于森林土壤固定的C、N库容巨 大 (Lal et al, 2015), 森林生态系统AM、EM树种相 对丰度随全球变化而发生的改变很可能会导致陆地 生 态 系 统 生 物 地 球 化 学 循 环 过 程 的 显 著 变 化 (Phillips et al, 2012;石兆勇等, 2012b;Terrer et al, 2016Terrer et al, , 2017)。阐明不同菌根类型森林土壤C、N循环 的差异及其影响机制, 对于提高森林生产力、预测 森林生态系统对全球变化的响应等具有重要意义 (Averill et al, 2014;Midgley et al, 2015;Soudzilovskaia et al, 2015)。 与树种的叶习性和谱系分类(例如针叶裸子植 物与阔叶被子植物)相比, 按菌根类型进行树种分 类能更好地解释森林生态系统土壤C、 N循环的变异 性乃至森林生产力对全球变化的响应 (Phillips et al, 2013;Midgley & Phillips, 2014;Terrer et al, 2016, …”
unclassified