寒带森林昆虫和风暴干扰——易感场地因子及其对生态系统碳的影响

M. Kosunen
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引用次数: 0

摘要

随着气候变化,森林和土壤在碳(C)固存中的重要性不断增强。风暴和虫害爆发等干扰是森林功能、组成和结构的驱动因素,预计其中许多因素在未来会变得更加普遍。然而,使森林易受干扰的环境因素以及干扰对森林C循环的各种影响尚不完全清楚。本文研究了两种常见昆虫——普通松锯蝇(Diprion pini L.)和欧洲云杉树皮甲虫(Ips typographus L.)——易发林分的林分、立地和土壤特征,以及风暴和I. typographus干扰对土壤呼吸、树木和土壤碳含量的影响。研究了芬兰东部和南部森林微生物群落组成和相关碳含量。人工管理下的苏格兰松(Pinus sylvestris L.)和挪威城市云杉(Picea abies (L.))的松木蠹和印图螟对树木的危害程度喀斯特森林分别与不同的立地和土壤特征有关。在肥力较强(土壤碳氮比较低、质地较细)的土壤中,松木的落叶作用更为严重。当树木生长在朝东的立地和最肥沃的立地类型,并结合中等陡坡、浅耕土壤或高土壤C/N比时,冷杉严重型印型蚜虫侵染的累积概率最高。以冷杉为主的冷杉林为研究对象,研究了风暴干扰对林分C的影响,研究了冷杉林分C在树木死亡后5 ~ 7年和1 ~ 4年左右对林分C的影响。土壤表层总CO2通量和异养CO2通量以及表土碳储量差异不大,尽管在干扰和更多的凋落物碎屑碳储量之后,在排版草干扰地,树木碳储量从活碳向死碳转变。受干扰样地土壤表层自养型CO2通量大多低于未受干扰样地。在腐殖质层微生物学上,最明显的差异是树木共生的外生菌根真菌丰度较低,因此,与未受干扰的样地相比,风暴和印刷草干扰样地的微生物和真菌生物量略低。受干扰地点上或附近的剩余活树可能会在一定程度上减轻地下对干扰的反应。本文表明,特定的立地和土壤特征使树木和林分容易受到pini和I. typographus的侵害,这有助于确定易受昆虫干扰的立地。此外,它还提供了自然干扰对北方森林碳循环和土壤微生物学的短期影响的新信息,这对于提高对气候变化对森林碳封存可能影响的复杂性的认识具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Insect and storm disturbance in boreal forests — predisposing site factors and impacts on ecosystem carbon
The importance of forests and soil in carbon (C) sequestration and storage is continually increasing with climate change. Disturbances, such as storms and insect outbreaks, are the drivers of forest functioning, composition and structure, and many of them are predicted to become more common in the future. However, environmental factors that predispose forests to disturbance as well as the diverse effects of disturbances on forest C cycling are not fully known. In this dissertation, stand, site and soil characteristics predisposing forest stands to outbreaks of two common insect species that can cause tree damage and mortality—the common pine sawfly (Diprion pini L.) and the European spruce bark beetle (Ips typographus L.)—were examined, and the impacts of storm and I. typographus disturbance on soil respiration, tree and soil C stocks, and microbial community composition and associated C contents were investigated in forests located in eastern and southern Finland. The level of tree damage by D. pini and I. typographus in managed Scots pine (Pinus sylvestris L.) and urban Norway spruce (Picea abies (L.) Karst.) forests, respectively, were associated with various site and soil characteristics. Defoliation of P. sylvestris by D. pini was more severe on sites with soil properties indicating greater fertility (e.g. lower soil C/N ratio and finer textured). Highest cumulative probabilities for severe I. typographus infestation of P. abies were associated with trees growing on sites having an east-facing aspect and the most fertile site types combined with either moderately steep slopes, shallow till soil or high soil C/N ratio. The effects of storm and I. typographus (5–7 years and circa 1–4 years after tree mortality, respectively) disturbance on forest C were studied in P. abies dominated forests that had been left unmanaged after disturbance. Soil surface total and heterotrophic CO2 effluxes, and topsoil C stocks of storm and I. typographus disturbed and undisturbed sites differed little, despite the shift in tree C stocks from living to dead after both disturbances and greater litter detritus C stocks on the I. typographus disturbed sites. Soil surface autotrophic CO2 effluxes were mostly lower at the disturbed sites than at undisturbed ones. The most distinct differences in the humus layer microbiology were the lower abundances of tree-symbiotic ectomycorrhizal fungi, and consequently slightly lower microbial and fungal biomasses in the storm and I. typographus disturbed sites in comparison to the undisturbed sites. The remaining living trees on or in close proximity to the disturbed sites probably mitigated the belowground response to disturbance to some extent. This dissertation shows that certain site and soil characteristics predispose trees and forest stands to D. pini and I. typographus infestations, which could help in identifying sites that are susceptible to insect disturbance. Furthermore, it provides new information about the short-term effects of natural disturbance on boreal forest C cycling and soil microbiology, which is important for improving understanding of the complexity of the possible impacts of climate change on forest C sequestration.
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