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Combining phytolith analysis with historical ecology to reveal the long-term, local-scale dynamics within a savannah-forest landscape mosaic

机译:将植物石料分析与历史生态相结合,以揭示热带草原-森林景观马赛克中的长期局部尺度动态

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An understanding of the historical range of variability of an ecosystem can improve management and restoration activities, but this variability depends on the spatial and temporal scale at which it is measured. We examined the extent of local-scale variation in vegetation prior to European settlement across a savannah-forest landscape mosaic on southeastern Vancouver Island, British Columbia, Canada. We used phytoliths extracted from soil surface samples to calibrate an index that differentiates open savannahs from closed canopy Douglas-fir forests and then examined shifts in this index with soil depth at seven local sites. We tested whether changes with depth aligned with known vegetation changes based on land survey records from the mid-1800s, and then inferred vegetation change prior to European settlement. The log ratio of astrosclereids (phytolith specific to Douglas-fir) and rondels (phytolith specific to grasses) in soil surface samples accurately distinguished between current vegetation types, and shifts in this ratio with depth were sensitive to known historical changes in most of the cores. Some sites have supported open savannah vegetation for at least 2,000 years, while others that were formerly open have been filled in by Douglas-fir forest. However, this infilling appears to have begun at different times for different sites. Our findings demonstrate that the degree and timing of historical variation in vegetation can differ between local sites within a broader regional landscape that appears relatively stable.
机译:对生态系统变异性历史范围的理解可以改善管理和恢复活动,但是这种变异性取决于对其进行测量的时空尺度。我们在加拿大不列颠哥伦比亚省温哥华岛东南部的热带草原森林景观马赛克上进行欧洲定居之前,研究了植被局部尺度变化的程度。我们使用从土壤表面样品中提取的植石来校准一个指数,该指数将开阔大草原与封闭的冠层花旗松森林区分开来,然后检查了该指数随土壤深度在七个地方的变化。我们根据1800年代中期的土地调查记录测试了深度变化是否与已知植被变化相吻合,然后推断出欧洲定居之前的植被变化。能够准确地区分当前植被类型的土壤表层样品中星形胶束菌(道格拉斯冷杉特有的植物体)和龙德尔斯(草特有的植物体)的对数比,并且该比值随深度的变化对大多数核心的已知历史变化敏感。 。一些地点支持开放的热带稀树草原植被至少2,000年,而其他以前开放的地点被花旗松森林所填埋。但是,对于不同的站点,这种填充似乎在不同的时间开始了。我们的发现表明,植被历史变化的程度和时机在看起来相对稳定的更广泛的区域景观内的局部地点之间可能有所不同。

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