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Changes in Soil Fungal Communities, Extracellular Enzyme Activities, and Litter Decomposition Across a Fire Chronosequence in Alaskan Boreal Forests

机译:阿拉斯加北方森林火灾时序中土壤真菌群落,细胞外酶活性和凋落物分解的变化

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Wildfires are a pervasive disturbance in boreal forests, and the frequency and intensity of boreal wildfires is expected to increase with climate warming. Boreal forests store a large fraction of global soil organic carbon (C), but relatively few studies have documented how wildfires affect soil microbial communities and soil C dynamics. We used a fire chronosequence in upland boreal forests of interior Alaska with sites that were 1, 7, 12, 24, 55, 90, and 100 years post-fire to examine the short- and long-term responses of fungal community composition, fungal abundance, extracellular enzyme activity, and litter decomposition to wildfires. We hypothesized that post-fire changes in fungal abundance and community composition would constrain decomposition following fires. We found that wildfires altered the composition of soil fungal communities. The relative abundance of ascomycetes significantly increased following fire whereas basidiomycetes decreased. Post-fire decreases in basidiomycete fungi were likely attributable to declines in ectomycorrhizal fungi. Fungal hyphal lengths in the organic horizon significantly declined in response to wildfire, and they required at least 24 years to return to pre-fire levels. Post-fire reductions in fungal hyphal length were associated with decreased activities of hydrolytic extracellular enzymes. In support of our hypothesis, the decomposition rate of aspen and black spruce litter significantly increased as forests recovered from fire. Our results indicate that post-fire reductions in soil fungal abundance and activity likely inhibit litter decomposition following boreal wildfires. Slower rates of litter decay may lead to decreased heterotrophic respiration from soil following fires and contribute to a negative feedback to climate warming.
机译:野火是北方森林的普遍干扰,随着气候变暖,北方野火的频率和强度预计会增加。北方森林存储了全球土壤有机碳(C)的很大一部分,但是很少有研究记录野火如何影响土壤微生物群落和土壤C动态。我们在阿拉斯加内陆的北方寒带森林中使用火灾的时序,以火灾发生后1、7、12、24、55、90和100年的地点为研究对象,研究真菌群落组成的短期和长期响应,即真菌丰度,细胞外酶活性和凋落物分解为野火。我们假设火灾后真菌丰富度和群落组成的变化会限制火灾后的分解。我们发现野火改变了土壤真菌群落的组成。火灾后,子囊菌的相对丰度显着增加,而担子菌的相对丰度下降。火后担子菌真菌的减少可能归因于外生菌根真菌的减少。响应野火,有机层中的真菌菌丝长度显着减少,并且它们至少需要24年才能恢复到火灾前的水平。火灾后真菌菌丝长度的减少与水解细胞外酶的活性降低有关。为支持我们的假设,随着森林从大火中恢复,白杨和黑云杉凋落物的分解率显着提高。我们的结果表明,火灾后土壤真菌丰度和活性的降低可能会抑制北方野火后凋落物的分解。凋落物腐烂率降低可能导致火灾后土壤的异养呼吸减少,并导致气候变暖的负面反馈。

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