Hawkesbury Institute for the Environment, Western Sydney University, Penrith, New South Wales, Australia.
Department of Sustainable Resources Management, College of Environmental Science and Forestry, State University of New York, Syracuse, NY, USA.
Nature. 2020 Apr;580(7802):227-231. doi: 10.1038/s41586-020-2128-9. Epub 2020 Apr 8.
Atmospheric carbon dioxide enrichment (eCO) can enhance plant carbon uptake and growth, thereby providing an important negative feedback to climate change by slowing the rate of increase of the atmospheric CO concentration. Although evidence gathered from young aggrading forests has generally indicated a strong CO fertilization effect on biomass growth, it is unclear whether mature forests respond to eCO in a similar way. In mature trees and forest stands, photosynthetic uptake has been found to increase under eCO without any apparent accompanying growth response, leaving the fate of additional carbon fixed under eCO unclear. Here using data from the first ecosystem-scale Free-Air CO Enrichment (FACE) experiment in a mature forest, we constructed a comprehensive ecosystem carbon budget to track the fate of carbon as the forest responded to four years of eCO exposure. We show that, although the eCO treatment of +150 parts per million (+38 per cent) above ambient levels induced a 12 per cent (+247 grams of carbon per square metre per year) increase in carbon uptake through gross primary production, this additional carbon uptake did not lead to increased carbon sequestration at the ecosystem level. Instead, the majority of the extra carbon was emitted back into the atmosphere via several respiratory fluxes, with increased soil respiration alone accounting for half of the total uptake surplus. Our results call into question the predominant thinking that the capacity of forests to act as carbon sinks will be generally enhanced under eCO, and challenge the efficacy of climate mitigation strategies that rely on ubiquitous CO fertilization as a driver of increased carbon sinks in global forests.
大气二氧化碳富集(eCO)可以增强植物的碳吸收和生长,从而通过减缓大气 CO 浓度的增加速度,为气候变化提供重要的负反馈。尽管从年轻的成长期森林中收集到的证据普遍表明,生物量生长对 CO 施肥有很强的影响,但尚不清楚成熟森林是否以类似的方式对 eCO 做出反应。在成熟的树木和森林中,光合吸收在 eCO 下被发现增加,而没有任何明显的伴随生长反应,这使得 eCO 下固定的额外碳的命运不清楚。在这里,我们利用成熟森林中第一个生态系统规模的自由空气 CO 富集(FACE)实验中的数据,构建了一个综合生态系统碳预算,以追踪森林对四年 eCO 暴露的反应过程中碳的命运。我们表明,尽管 eCO 处理(比环境水平高 150 个部分每百万(+38%))通过总初级生产力诱导了 12%(+247 克碳/平方米/年)的碳吸收增加,但这种额外的碳吸收并没有导致生态系统水平的碳封存增加。相反,大部分额外的碳通过几种呼吸通量释放回大气中,仅增加的土壤呼吸就占总吸收盈余的一半。我们的结果对森林在 eCO 下将普遍增强作为碳汇的能力的主流观点提出了质疑,并对依赖普遍的 CO 施肥作为全球森林增加碳汇的驱动因素的气候缓解策略的有效性提出了挑战。