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中至高海拔热带山地常绿树复合群的热生态位和系统发育组装。

The thermal niche and phylogenetic assembly of evergreen tree metacommunities in a mid-to-upper tropical montane zone.

机构信息

Wildlife Biology and Conservation Program, National Centre for Biological Sciences, Tata Institute of Fundamental Research, Bellary Road, Bangalore, Karnataka 560065, India.

出版信息

Proc Biol Sci. 2022 Jun 29;289(1977):20220038. doi: 10.1098/rspb.2022.0038.

Abstract

Frost and freezing temperatures have posed an obstacle to tropical woody evergreen plants over evolutionary time scales. Thus, along tropical elevation gradients, frost may influence woody plant community structure by filtering out lowland tropical clades and allowing extra-tropical lineages to establish at higher elevations. Here we assess the extent to which frost and freezing temperatures influence the taxonomic and phylogenetic structure of naturally patchy evergreen forests (locally known as ) along a mid-upper montane elevation gradient in the Western Ghats, India. Specifically, we examine the role of large-scale macroclimate and factors affecting local microclimates, including patch size and distance from edge, in driving metacommunity structure. We find that the metacommunity shows phylogenetic overdispersion with elevation, with greater representation of extra-tropical lineages above 2000 m, and marked turnover in taxonomic composition of woody communities near the frost-affected forest edge above 2000 m, from those below 2000 m. Both minimum winter temperature and patch size were equally important in determining metacommunity structure, with plots inside very large dominated by older tropical lineages, with many endemics. Phylogenetic overdispersion in the upper montane metacommunity thus resulted from tropical lineages persisting in the interiors of large closed frost-free where their regeneration niche has been preserved over time.

摘要

在进化时间尺度上,霜和冰冻温度对热带木本常绿植物构成了障碍。因此,在热带海拔梯度上,霜可能通过滤除低地热带分支,允许亚热带谱系在较高海拔建立,从而影响木本植物群落结构。在这里,我们评估了霜和冰冻温度在多大程度上影响印度西高止山脉中海拔梯度上自然块状常绿森林(当地称为 )的分类和系统发育结构。具体来说,我们研究了大尺度宏气候以及影响局部小气候的因素(包括斑块大小和与 边缘的距离)在驱动 集合群落结构中的作用。我们发现,随着海拔的升高, 集合群落表现出系统发育上的过度离散,2000 米以上的亚热带谱系代表率更高,而在 2000 米以上受霜影响的森林边缘附近, 木本群落的分类组成发生了明显的变化,与 2000 米以下的群落不同。冬季最低温度和斑块大小对确定集合群落结构同样重要,在非常大的 内部的斑块主要由较老的热带谱系组成,其中有许多特有种。因此,高山 集合群落的系统发育过度离散是由于热带谱系在免受霜害的大型封闭 内部得以存活,其再生生态位随时间得以保存。

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