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随着大气水压力的上升,热带树木的死亡率增加了。

Tropical tree mortality has increased with rising atmospheric water stress.

机构信息

Smithsonian Environmental Research Center, Edgewater, MD, USA.

Environmental Change Institute, School of Geography and the Environment, University of Oxford, Oxford, UK.

出版信息

Nature. 2022 Aug;608(7923):528-533. doi: 10.1038/s41586-022-04737-7. Epub 2022 May 18.

Abstract

Evidence exists that tree mortality is accelerating in some regions of the tropics, with profound consequences for the future of the tropical carbon sink and the global anthropogenic carbon budget left to limit peak global warming below 2 °C. However, the mechanisms that may be driving such mortality changes and whether particular species are especially vulnerable remain unclear. Here we analyse a 49-year record of tree dynamics from 24 old-growth forest plots encompassing a broad climatic gradient across the Australian moist tropics and find that annual tree mortality risk has, on average, doubled across all plots and species over the last 35 years, indicating a potential halving in life expectancy and carbon residence time. Associated losses in biomass were not offset by gains from growth and recruitment. Plots in less moist local climates presented higher average mortality risk, but local mean climate did not predict the pace of temporal increase in mortality risk. Species varied in the trajectories of their mortality risk, with the highest average risk found nearer to the upper end of the atmospheric vapour pressure deficit niches of species. A long-term increase in vapour pressure deficit was evident across the region, suggesting that thresholds involving atmospheric water stress, driven by global warming, may be a primary cause of increasing tree mortality in moist tropical forests.

摘要

有证据表明,热带地区的一些地区的树木死亡率正在加速上升,这对热带碳汇的未来以及限制全球变暖峰值低于 2°C 的全球人为碳预算产生了深远的影响。然而,驱动这种死亡率变化的机制以及哪些特定物种特别脆弱仍不清楚。在这里,我们分析了澳大利亚湿润热带地区 24 个原始森林样地 49 年的树木动态记录,这些样地跨越了广泛的气候梯度,结果发现,所有样地和物种的年树木死亡率风险在过去 35 年中平均增加了一倍,这表明预期寿命和碳滞留时间可能减少一半。与生长和补充带来的收益相比,生物量的损失没有得到弥补。在湿度较低的局部气候下,样地的平均死亡率风险更高,但局部平均气候并不能预测死亡率风险随时间增加的速度。不同物种的死亡率风险轨迹存在差异,在物种的大气蒸气压亏缺生态位的上限附近发现了最高的平均风险。该地区长期存在蒸气压亏缺增加的现象,这表明,由全球变暖驱动的大气水分胁迫阈值可能是湿润热带森林中树木死亡率增加的主要原因。

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