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Philos Trans R Soc Lond B Biol Sci. 2018 Oct 8;373(1760):20170308. doi: 10.1098/rstb.2017.0308.
2
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Climatic and anthropogenic drivers of northern Amazon fires during the 2015-2016 El Niño event.2015-2016 年厄尔尼诺事件期间,影响北亚马孙地区火灾的气候和人为因素。
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Twenty-first century droughts have not increasingly exacerbated fire season severity in the Brazilian Amazon.21 世纪的干旱并未使巴西亚马逊地区的火灾季节严重程度加剧。
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Climatic and local stressor interactions threaten tropical forests and coral reefs.气候和地方胁迫因子的相互作用威胁着热带森林和珊瑚礁。
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New insights into the variability of the tropical land carbon cycle from the El Niño of 2015/2016.从2015/2016年厄尔尼诺现象看热带陆地碳循环的变率新见解
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本文引用的文献

1
Quantifying immediate carbon emissions from El Niño-mediated wildfires in humid tropical forests.量化厄尔尼诺现象引发的潮湿热带森林野火的即时碳排放。
Philos Trans R Soc Lond B Biol Sci. 2018 Oct 8;373(1760):20170312. doi: 10.1098/rstb.2017.0312.
2
The future of hyperdiverse tropical ecosystems.热带超多样性生态系统的未来。
Nature. 2018 Jul;559(7715):517-526. doi: 10.1038/s41586-018-0301-1. Epub 2018 Jul 25.
3
Causes of reduced leaf-level photosynthesis during strong El Niño drought in a Central Amazon forest.强烈厄尔尼诺干旱期间亚马孙中部森林叶片光合作用降低的原因。
Glob Chang Biol. 2018 Sep;24(9):4266-4279. doi: 10.1111/gcb.14293. Epub 2018 May 30.
4
Coordination and trade-offs among hydraulic safety, efficiency and drought avoidance traits in Amazonian rainforest canopy tree species.亚马孙雨林冠层树种在水力安全、效率和耐旱性特征之间的协调和权衡。
New Phytol. 2018 May;218(3):1015-1024. doi: 10.1111/nph.15058. Epub 2018 Feb 19.
5
21st Century drought-related fires counteract the decline of Amazon deforestation carbon emissions.二十一世纪与干旱相关的火灾抵消了亚马孙毁林碳排放的减少。
Nat Commun. 2018 Feb 13;9(1):536. doi: 10.1038/s41467-017-02771-y.
6
A multi-species synthesis of physiological mechanisms in drought-induced tree mortality.干旱诱导树木死亡的生理机制的多物种综合。
Nat Ecol Evol. 2017 Sep;1(9):1285-1291. doi: 10.1038/s41559-017-0248-x. Epub 2017 Aug 7.
7
Mining drives extensive deforestation in the Brazilian Amazon.采矿导致巴西亚马逊地区大面积森林砍伐。
Nat Commun. 2017 Oct 18;8(1):1013. doi: 10.1038/s41467-017-00557-w.
8
Tropical forests are a net carbon source based on aboveground measurements of gain and loss.根据对热带森林地上生物量增加和减少的测量,热带森林是一个碳汇。
Science. 2017 Oct 13;358(6360):230-234. doi: 10.1126/science.aam5962. Epub 2017 Sep 28.
9
Negative emissions from stopping deforestation and forest degradation, globally.全球范围内,通过停止砍伐森林和森林退化实现负排放。
Glob Chang Biol. 2018 Jan;24(1):350-359. doi: 10.1111/gcb.13876. Epub 2017 Sep 22.
10
Unprecedented drought over tropical South America in 2016: significantly under-predicted by tropical SST.2016 年南美洲热带地区发生了史无前例的干旱:热带海表温度的预测明显不足。
Sci Rep. 2017 Jul 19;7(1):5811. doi: 10.1038/s41598-017-05373-2.

干旱和火灾后人类干扰亚马逊森林的树木生长和茎碳积累

Tree growth and stem carbon accumulation in human-modified Amazonian forests following drought and fire.

机构信息

Environmental Change Institute, University of Oxford, Oxford OX1 3QY, UK

Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, UK.

出版信息

Philos Trans R Soc Lond B Biol Sci. 2018 Oct 8;373(1760):20170308. doi: 10.1098/rstb.2017.0308.

DOI:10.1098/rstb.2017.0308
PMID:30297467
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6178429/
Abstract

Human-modified forests are an ever-increasing feature across the Amazon Basin, but little is known about how stem growth is influenced by extreme climatic events and the resulting wildfires. Here we assess for the first time the impacts of human-driven disturbance in combination with El Niño-mediated droughts and fires on tree growth and carbon accumulation. We found that after 2.5 years of continuous measurements, there was no difference in stem carbon accumulation between undisturbed and human-modified forests. Furthermore, the extreme drought caused by the El Niño did not affect carbon accumulation rates in surviving trees. In recently burned forests, trees grew significantly more than in unburned ones, regardless of their history of previous human disturbance. Wood density was the only significant factor that helped explain the difference in growth between trees in burned and unburned forests, with low wood-density trees growing significantly more in burned sites. Our results suggest stem carbon accumulation is resistant to human disturbance and one-off extreme drought events, and it is stimulated immediately after wildfires. However, these results should be seen with caution-without accounting for carbon losses, recruitment and longer-term changes in species composition, we cannot fully understand the impacts of drought and fire in the carbon balance of human-modified forests.This article is part of a discussion meeting issue 'The impact of the 2015/2016 El Nino on the terrestrial tropical carbon cycle: patterns, mechanisms and implications'.

摘要

人为干扰的森林在亚马逊盆地内不断增加,但人们对于极端气候事件及其引发的野火如何影响树干生长知之甚少。在这里,我们首次评估了人为干扰与厄尔尼诺现象引发的干旱和火灾相结合对树木生长和碳积累的影响。我们发现,经过 2.5 年的连续测量,未受干扰和人为干扰的森林之间的树干碳积累没有差异。此外,由厄尔尼诺现象引起的极端干旱并没有影响幸存树木的碳积累率。在最近发生火灾的森林中,树木的生长明显高于未燃烧的森林,而不论其先前是否有人为干扰的历史。木材密度是唯一能够帮助解释燃烧和未燃烧森林中树木生长差异的重要因素,低密度树木在燃烧的地点生长得更为显著。我们的研究结果表明,树干碳积累能够抵抗人为干扰和一次性的极端干旱事件,并且在野火之后立即得到促进。然而,这些结果应该谨慎看待——如果不考虑碳损失、补充和物种组成的长期变化,我们就无法全面了解干旱和火灾对人为干扰森林碳平衡的影响。本文是关于“2015/2016 年厄尔尼诺现象对热带陆地碳循环的影响:模式、机制和意义”讨论专题的一部分。