Mayer Mathias, Baltensweiler Andri, James Jason, Rigling Andreas, Hagedorn Frank
Forest Soils and Biogeochemistry Swiss Federal Institute for Forest, Snow and Landscape Research (WSL) Birmensdorf Switzerland.
Forest Ecology, Institute of Terrestrial Ecosystems (ITES) ETH Zurich Zurich Switzerland.
Glob Ecol Biogeogr. 2024 Jan;33(1):141-150. doi: 10.1111/geb.13779. Epub 2023 Oct 24.
Forest disturbances are increasing around the globe due to changes in climate and management, deteriorating forests' carbon sink strength. Estimates of global forest carbon budgets account for losses of plant biomass but often neglect the effects of disturbances on soil organic carbon (SOC). Here, we aimed to quantify and conceptualize SOC losses in response to different disturbance agents on a global scale.
Global.
1983-2022.
Forest soils.
We conducted a comprehensive global analysis of the effects of harvesting, wildfires, windstorms and insect infestations on forest SOC stocks in the surface organic layer and top mineral soil, synthesizing 927 paired observations from 151 existing field studies worldwide. We further used global mapping to assess potential SOC losses upon disturbance.
We found that both natural and anthropogenic forest disturbances can cause large SOC losses up to 60 Mg ha. On average, the largest SOC losses were found after wildfires, followed by disturbances from windstorms, harvests and insects. However, initial carbon stock size, rather than disturbance agent, had the strongest influence on the magnitude of SOC losses. SOC losses were greatest in cold-climate forests (boreal and mountainous regions) with large accumulations of organic matter on or near the soil surface. Negative effects are present for at least four decades post-disturbance. In contrast, forests with small initial SOC stocks experienced quantitatively lower carbon losses, and their stocks returned to pre-disturbance levels more quickly.
Our results indicate that the more carbon is stored in the forest's organic layers and top mineral soils, the more carbon will be lost after disturbance. Robust estimates of forest carbon budgets must therefore consider disturbance-induced SOC losses, which strongly depend on site-specific stocks. Particularly in cold-climate forests, these disturbance-related losses may challenge forest management efforts to sequester CO.
由于气候和管理方式的变化,全球范围内森林干扰日益增加,森林的碳汇强度不断恶化。全球森林碳预算的估计考虑了植物生物量的损失,但往往忽视了干扰对土壤有机碳(SOC)的影响。在此,我们旨在在全球范围内量化并概念化因不同干扰因素导致的土壤有机碳损失。
全球。
1983 - 2022年。
森林土壤。
我们对采伐、野火、风暴和虫害对表层有机层和上部矿质土壤中森林土壤有机碳储量的影响进行了全面的全球分析,综合了全球151项现有实地研究中的927对观测数据。我们还利用全球地图评估干扰后潜在的土壤有机碳损失。
我们发现,自然和人为的森林干扰都可能导致高达60 Mg/ha的大量土壤有机碳损失。平均而言,野火后土壤有机碳损失最大,其次是风暴、采伐和虫害造成的干扰。然而,初始碳储量大小而非干扰因素对土壤有机碳损失量的影响最大。在土壤表面或附近有机质大量积累的寒冷气候森林(北方和山区)中,土壤有机碳损失最大。干扰后至少四十年都会存在负面影响。相比之下,初始土壤有机碳储量较小的森林碳损失量在数量上较低,且其储量更快恢复到干扰前水平。
我们的结果表明,森林有机层和上部矿质土壤中储存碳越多,干扰后损失的碳就越多。因此,森林碳预算的可靠估计必须考虑干扰引起的土壤有机碳损失,这在很大程度上取决于特定地点的储量。特别是在寒冷气候森林中,这些与干扰相关的损失可能对森林管理中固存二氧化碳的努力构成挑战。