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首页> 外文期刊>Forest Ecology and Management >Fire regimes and structural changes in oak-pine forests of the Mogollon Highlands ecoregion: Implications for ecological restoration
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Fire regimes and structural changes in oak-pine forests of the Mogollon Highlands ecoregion: Implications for ecological restoration

机译:Mogollon Highlands Ecoregion橡树林林中的消防制度和结构变化:生态恢复的影响

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摘要

Ponderosa pine (Pines ponderosa) forests occur at their warmer, drier environmental limits in the Mogollon Highlands ecoregion (MHE) of the Southwestern United States, and are commonly found in stringers or discrete stands that form ecotones with interior chaparral. These "rear edge" forests are likely to be highly vulnerable to rapid changes in structure and composition with climate warming, drought, and wildfire. There is increasing interest in understanding historical conditions, ecosystem changes, and restoration needs for MHE forests. However, comprehensive reconstruction analysis of fire regimes and stand structure has not been done for these systems, which differ from many montane ponderosa pine forests by having an abundance of understory shrubs. In this study we used demographic data from field plots, fire scar samples, and dendroecology to reconstruct historical fire regimes and landscape structure at ponderosa pine-dominated sites that spanned a range of environmental conditions on the Prescott and Tonto National Forests. We found strong evidence of historical surface fire regimes with mean fire intervals ranging 1.3-15.6 years across the five MHE sites during the period 1700-1879. We found very little evidence of historical high-severity fire at any study site. Historical forest structure was open with tree densities ranging 84.7-136.4 trees ha(-1) and stand basal area (BA) ranging 4.5-8.4 m(2) ha(-1). Historical composition showed codominance of ponderosa pine, Arizona white oak (Quercus arizonica), Emory oak (Q. emoryi), and Gambel oak (Q. gambelii). Thus, oak species and likely other hardwoods were important historical components of these ecosystems. Contemporary forests are greater in stand density and BA by 359-703% and 285-502%, respectively, compared to historical estimates. In addition, we observed contemporary shifts in species composition. Changes related to disruption of historical fire regimes have increased susceptibility of ponderosa pine forests in the MHE to rapid shifts in structure and composition that may come about with climate change and high-intensity wildfire. Meeting fuels reduction and ecological restoration goals will be challenging for land managers due to vigorous regeneration responses of shrubs to tree thinning, prescribed burning, or other management activities. Managers will be required to balance attention to historical reference conditions, conservation of biological diversity, and needs for fuels management.
机译:黄松(黄松松树)的森林出现在他们的温暖,在美国西南部的莫戈隆高原生态区(MHE)干燥环境的限制,并在纵梁或离散看台这种形式的过渡带与室内小榭树中很常见。这些“后缘”森林都可能是非常容易受到气候变暖,干旱和野火在结构和组成的快速变化。有理解的历史条件下,生态系统的变化,并为MHE森林恢复的需求越来越大的兴趣。然而,消防制度和林分结构的综合改造分析中没有这些系统,它由许多山地黄松林具有林下灌木的大量不同的实现。在这项研究中,我们使用从田间地块,火疤样本人口数据,以及dendroecology在黄松有占主导地位的网站,横跨了一系列对普雷斯科特和通托国家森林环境条件下重建历史上火和景观结构。我们发现,平均火间隔期间的1800至79年不等跨五个高等教育部网站1.3-15.6年历史地表火政权的有力证据。我们发现历史的高危险火的证据很少在任何研究点。历史森林结构与树的密度范围84.7-136.4树木公顷(-1)开放,站在为4.5-8.4米(2)公顷(-1)的断面积(BA)。历史组合物显示西黄松,亚利桑那州白橡木(栎arizonica),埃默里栎(Q. emoryi),和Gambel栎(Q. gambelii)的共显性。因此,橡木种类和可能其他硬木为这些生态系统的重要组成部分的历史。现代森林中林分密度和更大的BA分别359-703%和285-502%,与历史估计。此外,我们观察到在物种组成当代移位。与历史上火的破坏变化已经在高等教育部增加黄松的松树林的易感性结构和成分变化迅速,其能对气候变化和高强度的野火。会议燃料减少和生态恢复目标将是具有挑战性的土地管理者由于灌木树变薄,火烧,或其他管理活动蓬勃再生响应。管理人员将被要求平衡重视历史的参考条件,保护生物多样性,并为燃料的管理需求。

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