Low-severity wildfire prevents catastrophic impacts on fungal communities and soil carbon stability in a fire-affected Douglas-fir ecosystem

IF 5.6 1区 农林科学 Q1 SOIL SCIENCE
Timothy J. Philpott, Gabriel Danyagri, Brian Wallace, Mae Frank
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Abstract

The growing frequency, extent and severity of wildfire is destabilizing carbon sinks in western North America, underscoring an urgent need to better understand fire impacts on soil carbon stocks, carbon stability, and fungi that regulate soil carbon cycling. Here, we examined the effects of wildfire two years post-burn on soil carbon and fungal communities across a fire severity gradient in Douglas-fir forests in central British Columbia, Canada. We observed no significant differences in soil carbon or fungal community composition between low-severity and unburned stands. In contrast, high-severity wildfire resulted in a 49 % reduction in belowground carbon stocks (20.7 Mg C·ha−1), a 91 % decline in ectomycorrhizal fungi, 5- to 27-fold increases in pathogenic fungi, and a proliferation of pyrophilous taxa compared to unburned stands. Carbon was lost primarily as light particulate organic matter, whereas impacts to mineral-associated carbon were muted. Pyrogenic carbon preferentially associated with the mineral fraction, modestly increasing (∼0.15 Mg C·ha−1) the proportion of carbon resistant to decay in this stable fraction. Select helotialean (e.g. Phialocephala fortinii) and other pyrophilous taxa were well-correlated with pyrogenic carbon, suggesting this consortium is well-adapted to decompose persistent carbon and will likely continue to mineralize soil carbon even after high severity wildfire. The markedly higher abundance of pathogenic fungi and reduced ectomycorrhizal abundance in stands affected by high-severity fires pose risks to post-fire recovery, particularly if pathogen proliferation reduces conifer fitness. These results highlight that low-severity wildfires have comparatively muted impacts on soil carbon and fungal communities relative to high-severity wildfires, underscoring the importance of management strategies such as thinning and prescribed burns to mitigate the catastrophic effects of high-severity wildfires.
野火发生的频率、范围和严重程度不断增加,破坏了北美西部碳汇的稳定,因此迫切需要更好地了解火灾对土壤碳储量、碳稳定性以及调节土壤碳循环的真菌的影响。在这里,我们研究了加拿大不列颠哥伦比亚省中部花旗松林火灾严重程度梯度中,野火燃烧两年后对土壤碳和真菌群落的影响。我们观察到,低严重性森林和未燃烧森林的土壤碳和真菌群落组成没有明显差异。相反,与未燃烧林分相比,严重野火导致地下碳储量(20.7 Mg C-ha-1)减少了 49%,外生菌根真菌减少了 91%,病原真菌增加了 5 到 27 倍,亲火类群大量增加。碳主要以轻颗粒有机物的形式流失,而对矿质碳的影响不大。火成碳优先与矿物部分结合,适度增加了(0.15 兆克碳-公顷-1)这一稳定部分中抗腐碳的比例。部分 helotialean(如 Phialocephala fortinii)和其他亲火类群与热源碳密切相关,表明该类群非常适合分解持久性碳,即使在高强度野火后仍可能继续矿化土壤碳。在受高严重性火灾影响的林分中,病原真菌的丰度明显较高,而外生菌根的丰度则有所降低,这给火灾后的恢复带来了风险,特别是如果病原菌的扩散降低了针叶林的适应性。这些结果突出表明,与高火险野火相比,低火险野火对土壤碳和真菌群落的影响相对较小,这也强调了稀植和规定燃烧等管理策略对减轻高火险野火灾难性影响的重要性。
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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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