Department of Biology, Duke University, Durham, North Carolina, USA.
Royal Botanic Gardens Kew, Richmond, TW9 3AE, UK.
Mol Ecol. 2022 Oct;31(19):4901-4918. doi: 10.1111/mec.16632. Epub 2022 Aug 15.
Madagascar's Central Highlands are largely composed of grasslands, interspersed with patches of forest. The historical perspective was that Madagascar's grasslands had anthropogenic origins, but emerging evidence suggests that grasslands were a component of the pre-human Central Highlands vegetation. Consequently, there is now vigorous debate regarding the extent to which these grasslands have expanded due to anthropogenic pressures. Here, we shed light on the temporal dynamics of Madagascar's vegetative composition by conducting a population genomic investigation of Goodman's mouse lemur (Microcebus lehilahytsara; Cheirogaleidae). These small-bodied primates occur both in Madagascar's eastern rainforests and in the Central Highlands, making them a valuable indicator species. Population divergences among forest-dwelling mammals will reflect changes to their habitat, including fragmentation, whereas patterns of post-divergence gene flow can reveal formerly wooded migration corridors. To explore these patterns, we used RADseq data to infer population genetic structure, demographic models of post-divergence gene flow, and population size change through time. The results offer evidence that open habitats are an ancient component of the Central Highlands, and that widespread forest fragmentation occurred naturally during a period of decreased precipitation near the last glacial maximum. Models of gene flow suggest that migration across the Central Highlands has been possible from the Pleistocene through the recent Holocene via riparian corridors. Though our findings support the hypothesis that Central Highland grasslands predate human arrival, we also find evidence for human-mediated population declines. This highlights the extent to which species imminently threatened by human-mediated deforestation may already be vulnerable from paleoclimatic conditions.
马达加斯加中央高原主要由草原组成,间有森林斑块。历史上认为,马达加斯加的草原是人为起源的,但新出现的证据表明,草原是人类出现前中央高原植被的组成部分。因此,现在人们对这些草原在多大程度上由于人为压力而扩张存在激烈的争论。在这里,我们通过对 Goodman 鼠狐猴(Microcebus lehilahytsara;鼠狐猴科)进行群体基因组研究,揭示了马达加斯加植被组成的时间动态。这些体型较小的灵长类动物既存在于马达加斯加东部雨林中,也存在于中央高原,是一种有价值的指示物种。森林栖息哺乳动物的种群分化将反映其栖息地的变化,包括碎片化,而分化后基因流的模式可以揭示以前树木繁茂的迁徙走廊。为了探索这些模式,我们使用 RADseq 数据推断了种群遗传结构、分化后基因流的人口统计模型以及随时间变化的种群规模变化。研究结果表明,开阔的栖息地是中央高原的一个古老组成部分,广泛的森林破碎化是在末次冰期最盛期附近降水减少期间自然发生的。基因流模型表明,从中更新世到全新世,通过河流走廊,穿越中央高原的迁徙一直是可能的。虽然我们的研究结果支持了中央高地草原在人类到来之前就存在的假说,但我们也发现了人类介导的种群减少的证据。这突显了受人类介导的森林砍伐威胁的物种可能已经受到古气候条件影响的程度。