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Land-use change under a warming climate facilitated upslope expansion of Himalayan silver fir (Abies spectabilis (D. Don) Spach)

机译:变暖气候下的土地利用变化促进了喜马拉雅银杉(abies spectabilis(D。Don)spach)的上坡扩张

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摘要

Global warming is triggering some species to shift towards the poles or higher elevations, but spatial translocation is also influenced by land-use regime or intensity. The Himalayan climate is getting warmer and land use has changed, reducing in intensity in some areas. We estimated the upper species limit (USL) and tree limit of Abies spectabilis (D. Don) Spach and assessed whether these have changed over recent years. We hypothesise an upslope shift in response to enhanced temperature and changes in land-use intensity. Our four transects were located in treeline ecotones of two protected areas in Nepal, namely Manaslu Conservation Area (3 transects) and Gaurishankar Conservation Area (1 transect). Transects (20 m wide) ran from the USL of A. spectabilis down towards the treeline and beyond to the forest line. Length of each transect varied depending on local conditions. Co-ordinates, elevation, height and age of each A. spectabilis individual along the transects were recorded. We noted an upward shift of both the USL and the tree limit. The rate of shift was ca. 20 m per decade for the USL and 12 m per decade for the tree limit in the area of reduced land-use intensity and in the area with no change in land use, 5 m per decade for the USL, but almost nil for tree limit. The seedling density was higher below the treeline than above. Reduced intensity of land use was the dominant factor in upslope shift of A. spectabilis at both the USL and the tree limit.
机译:全球变暖正在触发一些物种向两极或更高海拔转移,但是空间转移也受到土地利用制度或强度的影响。喜马拉雅气候正在变暖,土地使用发生了变化,在某些地区强度有所降低。我们估算了阔叶冷杉(Dieson Spatabilis)(D. Don)Spach的树种上限(USL)和树木上限,并评估了近年来这些树种是否发生了变化。我们假设温度升高和土地利用强度变化会导致坡度上升。我们的四个样带位于尼泊尔两个保护区的树线过渡带,即马纳斯卢峰保护区(3个样带)和高里山卡保护区(1个样带)。横断面(宽20 m)从A. spectabilis的USL向下延伸至林线,然后延伸至林线。每个样条线的长度取决于当地条件。记录沿横断面的每只奇异曲霉的坐标,高度,高度和年龄。我们注意到USL和树限制都向上移动。移位率约为。在土地利用强度降低的地区和土地利用无变化的地区,USL每十年20 m,树木极限每10 m 12m,USL每十年10 m,但树木极限几乎为零。树木下方的幼苗密度高于上方。在USL和树木极限处,土地利用强度的降低是壮观曲霉向上坡转移的主要因素。

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