Environmental Change Institute, School of Geography and the Environment, University of Oxford, Oxford, UK.
Laboratory of Geo-Information and Remote Sensing, Wageningen University and Research, Wageningen, The Netherlands.
Glob Chang Biol. 2018 Feb;24(2):758-772. doi: 10.1111/gcb.13951. Epub 2017 Nov 24.
Tropical montane cloud forests (TMCFs) harbour high levels of biodiversity and large carbon stocks. Their location at high elevations make them especially sensitive to climate change, because a warming climate is enhancing upslope species migration, but human disturbance (especially fire) may in many cases be pushing the treeline downslope. TMCFs are increasingly being affected by fire, and the long-term effects of fire are still unknown. Here, we present a 28-year chronosequence to assess the effects of fire and recovery pathways of burned TMCFs, with a detailed analysis of carbon stocks, forest structure and diversity. We assessed rates of change of carbon (C) stock pools, forest structure and tree-size distribution pathways and tested several hypotheses regarding metabolic scaling theory (MST), C recovery and biodiversity. We found four different C stock recovery pathways depending on the selected C pool and time since last fire, with a recovery of total C stocks but not of aboveground C stocks. In terms of forest structure, there was an increase in the number of small stems in the burned forests up to 5-9 years after fire because of regeneration patterns, but no differences on larger trees between burned and unburned plots in the long term. In support of MST, after fire, forest structure appears to approximate steady-state size distribution in less than 30 years. However, our results also provide new evidence that the species recovery of TMCF after fire is idiosyncratic and follows multiple pathways. While fire increased species richness, it also enhanced species dissimilarity with geographical distance. This is the first study to report a long-term chronosequence of recovery pathways to fire suggesting faster recovery rates than previously reported, but at the expense of biodiversity and aboveground C stocks.
热带山地云雾林(TMCFs)拥有丰富的生物多样性和大量的碳储量。由于其所处的高海拔位置,它们对气候变化特别敏感,因为气候变暖正在促进上坡物种的迁移,但在许多情况下,人类干扰(尤其是火灾)可能会将林线向下推。TMCFs 越来越容易受到火灾的影响,而且火灾的长期影响仍不清楚。在这里,我们提出了一个 28 年的时间序列,以评估火灾的影响和烧毁的 TMCFs 的恢复途径,对碳储量、森林结构和多样性进行了详细分析。我们评估了碳(C)储量池的变化率、森林结构和树木大小分布途径,并测试了关于代谢缩放理论(MST)、C 恢复和生物多样性的几个假设。我们发现了四种不同的 C 储量恢复途径,具体取决于所选 C 池和上次火灾后的时间,其中包括总 C 储量的恢复,但不包括地上 C 储量的恢复。就森林结构而言,由于再生模式,烧毁森林中小茎的数量在火灾后 5-9 年内增加,但长期来看,烧毁和未烧毁的森林之间的大树数量没有差异。支持 MST 的是,火灾后,森林结构似乎在不到 30 年内接近稳定状态的大小分布。然而,我们的结果也提供了新的证据,表明 TMCF 火灾后物种的恢复是特殊的,并遵循多种途径。虽然火灾增加了物种丰富度,但它也增加了物种与地理距离的不相似性。这是第一项报告火灾后恢复途径的长期时间序列的研究,表明恢复速度比以前报告的更快,但以生物多样性和地上 C 储量为代价。