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亚马逊森林对气候变化的组成响应。

Compositional response of Amazon forests to climate change.

机构信息

School of Geography, University of Leeds, Leeds, UK.

Royal Botanic Garden of Edinburgh, Edinburgh, UK.

出版信息

Glob Chang Biol. 2019 Jan;25(1):39-56. doi: 10.1111/gcb.14413. Epub 2018 Nov 8.

DOI:10.1111/gcb.14413
PMID:30406962
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6334637/
Abstract

Most of the planet's diversity is concentrated in the tropics, which includes many regions undergoing rapid climate change. Yet, while climate-induced biodiversity changes are widely documented elsewhere, few studies have addressed this issue for lowland tropical ecosystems. Here we investigate whether the floristic and functional composition of intact lowland Amazonian forests have been changing by evaluating records from 106 long-term inventory plots spanning 30 years. We analyse three traits that have been hypothesized to respond to different environmental drivers (increase in moisture stress and atmospheric CO concentrations): maximum tree size, biogeographic water-deficit affiliation and wood density. Tree communities have become increasingly dominated by large-statured taxa, but to date there has been no detectable change in mean wood density or water deficit affiliation at the community level, despite most forest plots having experienced an intensification of the dry season. However, among newly recruited trees, dry-affiliated genera have become more abundant, while the mortality of wet-affiliated genera has increased in those plots where the dry season has intensified most. Thus, a slow shift to a more dry-affiliated Amazonia is underway, with changes in compositional dynamics (recruits and mortality) consistent with climate-change drivers, but yet to significantly impact whole-community composition. The Amazon observational record suggests that the increase in atmospheric CO is driving a shift within tree communities to large-statured species and that climate changes to date will impact forest composition, but long generation times of tropical trees mean that biodiversity change is lagging behind climate change.

摘要

地球上的大部分生物多样性都集中在热带地区,而这些地区正经历着快速的气候变化。然而,尽管其他地方广泛记录了气候引起的生物多样性变化,但很少有研究关注低地热带生态系统的这个问题。在这里,我们通过评估跨越 30 年的 106 个长期清查样地的记录,来研究完整的低地亚马孙森林的植物区系和功能组成是否发生了变化。我们分析了三个被假设对不同环境驱动因素(水分胁迫和大气 CO 浓度增加)有反应的特征:最大树木大小、生物地理水分缺陷归属和木材密度。树木群落越来越由大型分类群主导,但迄今为止,在社区层面上,还没有检测到平均木材密度或水分缺陷归属的变化,尽管大多数森林样地的旱季都有所加剧。然而,在新招募的树木中,干旱相关的属变得更加丰富,而在旱季加剧最严重的那些样地中,潮湿相关的属的死亡率增加了。因此,一个向更干旱的亚马孙地区的缓慢转变正在进行,组成动态(新树和死亡)的变化与气候变化驱动因素一致,但尚未对整个社区的组成产生重大影响。亚马孙的观测记录表明,大气 CO 的增加正在驱动树木群落向大型物种的转变,而且到目前为止的气候变化将影响森林组成,但热带树木较长的世代时间意味着生物多样性变化滞后于气候变化。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/abc4/6334637/b04435a6536f/GCB-25-39-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/abc4/6334637/228cc684718a/GCB-25-39-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/abc4/6334637/d662af93f9da/GCB-25-39-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/abc4/6334637/d52590c8ec24/GCB-25-39-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/abc4/6334637/864b1a2eccd7/GCB-25-39-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/abc4/6334637/b04435a6536f/GCB-25-39-g005.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/abc4/6334637/228cc684718a/GCB-25-39-g001.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/abc4/6334637/d662af93f9da/GCB-25-39-g002.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/abc4/6334637/d52590c8ec24/GCB-25-39-g003.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/abc4/6334637/864b1a2eccd7/GCB-25-39-g004.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/abc4/6334637/b04435a6536f/GCB-25-39-g005.jpg

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