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模拟氮沉降影响结壳真菌的木材分解。

Simulated nitrogen deposition affects wood decomposition by cord-forming fungi.

机构信息

Earthwatch Institute, Oxford, UK.

出版信息

Oecologia. 2011 Dec;167(4):1177-84. doi: 10.1007/s00442-011-2057-2. Epub 2011 Jul 7.

DOI:10.1007/s00442-011-2057-2
PMID:21735202
Abstract

Anthropogenic nitrogen (N) deposition affects many natural processes, including forest litter decomposition. Saprotrophic fungi are the only organisms capable of completely decomposing lignocellulosic (woody) litter in temperate ecosystems, and therefore the responses of fungi to N deposition are critical in understanding the effects of global change on the forest carbon cycle. Plant litter decomposition under elevated N has been intensively studied, with varying results. The complexity of forest floor biota and variability in litter quality have obscured N-elevation effects on decomposers. Field experiments often utilize standardized substrates and N-levels, but few studies have controlled the decay organisms. Decomposition of beech (Fagus sylvatica) blocks inoculated with two cord-forming basidiomycete fungi, Hypholoma fasciculare and Phanerochaete velutina, was compared experimentally under realistic levels of simulated N deposition at Wytham Wood, Oxfordshire, UK. Mass loss was greater with P. velutina than with H. fasciculare, and with N treatment than in the control. Decomposition was accompanied by growth of the fungal mycelium and increasing N concentration in the remaining wood. We attribute the N effect on wood decay to the response of cord-forming wood decay fungi to N availability. Previous studies demonstrated the capacity of these fungi to scavenge and import N to decaying wood via a translocating network of mycelium. This study shows that small increases in N availability can increase wood decomposition by these organisms. Dead wood is an important carbon store and habitat. The responses of wood decomposers to anthropogenic N deposition should be considered in models of forest carbon dynamics.

摘要

人为氮(N)沉积会影响许多自然过程,包括森林凋落物分解。腐生真菌是唯一能够完全分解温带生态系统木质纤维素(木质)凋落物的生物,因此真菌对 N 沉积的反应对于理解全球变化对森林碳循环的影响至关重要。在高氮条件下的植物凋落物分解已被深入研究,但结果各异。森林地被层生物的复杂性和凋落物质量的可变性掩盖了 N 对分解者的升高效应。野外实验通常利用标准化的基质和 N 水平,但很少有研究控制分解生物体。在英国牛津郡威瑟姆伍德(Wytham Wood),用两种形成菌索的担子菌真菌,Hypoloma fasciculare 和 Phanerochaete velutina 接种的山毛榉块进行了实验性比较,在现实水平的模拟 N 沉积下进行了实验。与 H. fasciculare 相比,P. velutina 引起的质量损失更大,与 N 处理相比,控制组的质量损失更大。分解伴随着真菌菌丝的生长和剩余木材中 N 浓度的增加。我们将 N 对木材分解的影响归因于菌索形成木材分解真菌对 N 可利用性的反应。先前的研究表明,这些真菌有能力通过菌丝的迁移网络从凋落物中吸收和输入 N。本研究表明,N 可用性的微小增加可以增加这些生物体对木材的分解。枯木是一种重要的碳储存和栖息地。在森林碳动态模型中,应考虑木质分解者对人为 N 沉积的响应。

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本文引用的文献

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Immobilization of a N-labeled nitrate addition by decomposing forest litter.通过分解森林凋落物固定添加的氮标记硝酸盐。
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Global meta-analysis of wood decomposition rates: a role for trait variation among tree species?全球木材分解速率的荟萃分析:树种间性状变异的作用?
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