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火频度驱动土壤碳氮和生态系统生产力的十年际变化。

Fire frequency drives decadal changes in soil carbon and nitrogen and ecosystem productivity.

机构信息

Department of Earth System Science, Stanford University, Stanford, California 94305, USA.

Department of Physical Geography and Ecosystem Science, Lund University, Lund, Sweden.

出版信息

Nature. 2018 Jan 11;553(7687):194-198. doi: 10.1038/nature24668. Epub 2017 Dec 11.

Abstract

Fire frequency is changing globally and is projected to affect the global carbon cycle and climate. However, uncertainty about how ecosystems respond to decadal changes in fire frequency makes it difficult to predict the effects of altered fire regimes on the carbon cycle; for instance, we do not fully understand the long-term effects of fire on soil carbon and nutrient storage, or whether fire-driven nutrient losses limit plant productivity. Here we analyse data from 48 sites in savanna grasslands, broadleaf forests and needleleaf forests spanning up to 65 years, during which time the frequency of fires was altered at each site. We find that frequently burned plots experienced a decline in surface soil carbon and nitrogen that was non-saturating through time, having 36 per cent (±13 per cent) less carbon and 38 per cent (±16 per cent) less nitrogen after 64 years than plots that were protected from fire. Fire-driven carbon and nitrogen losses were substantial in savanna grasslands and broadleaf forests, but not in temperate and boreal needleleaf forests. We also observe comparable soil carbon and nitrogen losses in an independent field dataset and in dynamic model simulations of global vegetation. The model study predicts that the long-term losses of soil nitrogen that result from more frequent burning may in turn decrease the carbon that is sequestered by net primary productivity by about 20 per cent of the total carbon that is emitted from burning biomass over the same period. Furthermore, we estimate that the effects of changes in fire frequency on ecosystem carbon storage may be 30 per cent too low if they do not include multidecadal changes in soil carbon, especially in drier savanna grasslands. Future changes in fire frequency may shift ecosystem carbon storage by changing soil carbon pools and nitrogen limitations on plant growth, altering the carbon sink capacity of frequently burning savanna grasslands and broadleaf forests.

摘要

火灾频率正在全球范围内发生变化,并预计将影响全球碳循环和气候。然而,由于生态系统对火灾频率的数十年变化的反应存在不确定性,因此很难预测改变火灾制度对碳循环的影响;例如,我们并不完全了解火灾对土壤碳和养分储存的长期影响,或者火灾驱动的养分损失是否会限制植物生产力。在这里,我们分析了跨越 65 年的草原、阔叶林和针叶林 48 个地点的数据,在此期间,每个地点的火灾频率都发生了变化。我们发现,频繁燃烧的斑块经历了表层土壤碳和氮的下降,随着时间的推移,这种下降是非饱和的,与未受火灾保护的斑块相比,在 64 年后,碳减少了 36%(±13%),氮减少了 38%(±16%)。在草原和阔叶林火灾中,碳和氮的损失是巨大的,但在温带和北方针叶林则不然。我们还在独立的田间数据集和全球植被动态模型模拟中观察到了可比的土壤碳和氮损失。模型研究预测,由于更频繁的燃烧导致的长期土壤氮损失可能反过来又会使通过净初级生产力固存的碳减少约 20%,而这部分碳是在同一时期燃烧生物质所排放的总碳的 20%。此外,如果不包括土壤碳的多十年变化,那么气候变化对生态系统碳储存的影响可能低估了 30%,尤其是在较干燥的草原。未来火灾频率的变化可能会通过改变土壤碳库和植物生长的氮限制来改变生态系统碳储存,从而改变频繁燃烧的草原和阔叶林的碳汇能力。

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