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首页> 外文期刊>Plant Ecology >Effects of topography on tropical lower montane forests under different geological conditions on Mount Kinabalu, Borneo
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Effects of topography on tropical lower montane forests under different geological conditions on Mount Kinabalu, Borneo

机译:地形对婆罗洲京那巴鲁山不同地质条件下热带低山地森林的影响

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Species composition and forest structure change with topography. However, mechanisms for topographical vegetation changes are still not well understood, because a topographical gradient is a complex environmental gradient inclusive of many factors. The foot of Mt. Kinabalu is covered with three types of geological substrates, i.e. Quaternary and Tertiary sedimentary rocks and ultrabasic (serpentine) rock. Quaternary and Tertiary sedimentary rocks are different in site age, but controlled in primary minerals. Tertiary sedimentary and ultrabasic rocks are contrasting in primary minerals, but are comparable in age. This setting provides an opportunity to examine the vegetation differentiation along topographical gradients that are contrasting in major-nutrient supply due to the difference in site age and parent rock. We established a total of nine study plots by choosing three topographical units (ridge, middle- and lower-slope) on each substrate in the tropical lower montane forest. Pool size and supply of soil N and P decreased upslope on each substrate, and the magnitude of the reduction from slope to ridge decreased in the order of Quaternary sedimentary > Tertiary sedimentary > ultrabasic rock. Between-substrate difference in soil nutrient condition was greater on the lower-slopes than the ridges. Maximum tree size decreased and stem density increased upslope on each substrate. Detrended correspondence analysis demonstrated that species composition also changed along topographical gradients on all substrates. However, the magnitude of topographical changes in forest structure and species composition varied with substrate and decreased from Quaternary sedimentary > Tertiary sedimentary > ultrabasic rock. The greatest between-substrate difference in vegetation occurred on the lower-slopes. Accordingly, our results suggest that the magnitude of vegetation changes due to topography becomes smaller with decreasing pool size and supply of nutrients. [References: 45]
机译:物种组成和森林结构随地形变化。但是,由于地形梯度是一个复杂的环境梯度,其中包括许多因素,因此地形植被变化的机制仍未得到很好的理解。山脚京那巴鲁覆盖着三种类型的地质基质,即第四纪和第三纪沉积岩和超碱性(蛇纹石)岩。第四纪和第三纪沉积岩的站点年龄不同,但主要矿物受控制。第三纪沉积和超基性岩石在主要矿物中形成对比,但在年龄上可比。这种设置提供了一个机会来检查沿地形梯度的植被分化,由于场地年龄和母岩的差异,这些地形在主要养分供应方面形成对比。我们通过在热带山地低森林中的每个基底上选择三个地形单位(山脊,中坡和下坡)建立了总共九个研究地块。在每个基底上,库的大小和土壤氮和磷的供应量减少了上坡,并且从斜坡到山脊的减少幅度按第四纪沉积>第三纪沉积>超基性岩的顺序减小。在较低的坡度上,土壤养分状况的基质间差异要比在脊上大。在每个基质上,最大的树木尺寸减小,茎密度增加。去趋势对应分析表明,在所有底物上物种组成也随地形梯度变化。然而,森林结构和物种组成的地形变化幅度随基质而变化,并且从第四纪沉积>第三纪沉积>超基性岩减小。植被之间最大的基底间差异发生在下坡。因此,我们的结果表明,随着水池大小和养分供应的减少,由于地形引起的植被变化幅度变小。 [参考:45]

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