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首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Emergent geomorphic-vegetation interactions on a subalpine alluvial fan
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Emergent geomorphic-vegetation interactions on a subalpine alluvial fan

机译:亚高山冲积扇上的新兴地貌-植被相互作用

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Following perturbation, an ecosystem (flora, fauna, soil) should evolve as a function of time at a rate conditioned by external variables (relief, climate, geology). More recently, biogeomorphologists have focused upon the notion of co-development of geomorphic processes with ecosystems over very short through to very long (evolutionary) timescales. Alpine environments have been a particular focus of this co-development. However, work in this field has tended to adopt a simplified view of the relationship between perturbation and succession, including: how the landform and ecosystem itself conditions the impact of a perturbation to create a complex spatial response impact; and how perturbations are not simply ecosystem destroyers but can be a significant source of ecosystem resources. What this means is that at the within landform scale, there may well be a complex and dynamic topographic and sedimentological template that co-develops with soil, flora and fauna. Here, we present and test a conceptual model of this template for a subalpine alluvial fan. We combine detailed floristic inventory with soil inventory, determination of edaphic variables and analysis of historical aerial imagery. Spatial variation in the probability of perturbation of sites on the fan surface was associated with down fan variability in the across-fan distribution of fan ages, fan surface channel characteristics and fan surface sedimentology. Floristic survey confirmed that these edaphic factors distinguished site floristic richness and plant communities up until the point that the soil-vegetation system was sufficiently developed to sustain plant communities regardless of edaphic conditions. Thus, the primary explanatory variable was the estimated age of each site, which could be tied back into perturbation history and its spatial expression due to the geometry of the fan: distinct plant communities were emergent both across fan and down fan, a distribution maintained by the way in which the fan dissipates potentially perturbing events. Copyright (c) 2015 John Wiley & Sons, Ltd.
机译:扰动之后,生态系统(植物区系,动物区系,土壤)应随时间变化,其变化速率受外部变量(浮雕,气候,地质)的影响。最近,生物地貌学家将注意力集中在从很短到很长(进化)的时间尺度上与生态系统共同发展地貌过程的概念上。高山环境一直是这一共同发展的重点。但是,该领域的工作倾向于对扰动和演替之间的关系采用简化的观点,包括:地形和生态系统本身如何调节扰动的影响以产生复杂的空间响应影响;以及干扰不仅是生态系统破坏者,而且可以成为生态系统资源的重要来源。这意味着在地形范围内,很可能存在与土壤,动植物共同发展的复杂而动态的地形和沉积学模板。在这里,我们介绍并测试该模板的概念模型用于亚高山冲积扇。我们将详细的植物种类清单与土壤清单,确定的环境变量和历史航空影像分析相结合。风扇表面位置受扰动概率的空间变化与风扇年龄,风扇表面通道特征和风扇表面沉积学的跨风扇分布下降有关。植物学调查证实,这些营养因子可以区分植物区系丰富度和植物群落,直到土壤植被系统充分发育以维持植物群落,而无论其环境如何。因此,主要的解释变量是每个站点的估计年龄,由于风扇的几何形状,可以将其与扰动历史及其空间表达联系起来:在风扇和向下的风扇上都出现了不同的植物群落,由风扇消散潜在干扰事件的方式。版权所有(c)2015 John Wiley&Sons,Ltd.

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