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解释温带泥炭地植被格局的环境因素。

Environmental factors explaining the vegetation patterns in a temperate peatland.

作者信息

Pellerin Stéphanie, Lagneau Louis-Adrien, Lavoie Martin, Larocque Marie

机构信息

Institut de recherche en biologie végétale, Université de Montréal, Québec, Canada.

出版信息

C R Biol. 2009 Aug;332(8):720-31. doi: 10.1016/j.crvi.2009.04.003. Epub 2009 May 6.

Abstract

Although ombrotrophic temperate peatlands are important ecosystems for maintaining biodiversity in eastern North America, the environmental factors influencing their flora are only partly understood. The relationships between plant species distribution and environmental factors were thus studied within the oldest temperate peatland of Québec. Plant assemblages were identified by cluster analysis while CCA was used to related vegetation gradients to environmental factors. Five assemblages were identified; three typical of open bog and two characterized by more minerotrophic vegetation. Thicker peat deposit was encounter underlying the bog assemblages while higher water table level and percentage of free surface water distinguished the minerotrophic assemblages. Overall, the floristic patterns observed were spatially structured along the margins and the expanse. The most important environmental factors explaining this spatial gradient were the percentage of free surface water and the highest water-table level.

摘要

尽管雨养型温带泥炭地是北美东部维持生物多样性的重要生态系统,但影响其植物群的环境因素仅得到部分了解。因此,在魁北克最古老的温带泥炭地内研究了植物物种分布与环境因素之间的关系。通过聚类分析确定植物组合,同时使用典范对应分析(CCA)将植被梯度与环境因素联系起来。确定了五种组合;三种典型的开阔沼泽组合和两种以更多矿质营养植被为特征的组合。在沼泽组合下面遇到了更厚的泥炭沉积,而较高的地下水位和自由地表水百分比区分了矿质营养组合。总体而言,观察到的植物区系格局在边缘和广阔区域呈空间结构。解释这种空间梯度的最重要环境因素是自由地表水百分比和最高地下水位。

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