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Historical colonization and dispersal limitation supplement climate and topography in shaping species richness of African lizards (Reptilia: Agaminae)

机译:历史殖民化和扩散限制补充了气候和地形从而塑造了非洲蜥蜴的物种丰富度(Reptilia:Agaminae)

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摘要

To what extent deep-time dispersal limitation shapes present-day biodiversity at broad spatial scales remains elusive. Here, we compiled a continental dataset on the distributions of African lizard species in the reptile subfamily Agaminae (a relatively young, Neogene radiation of agamid lizards which ancestors colonized Africa from the Arabian peninsula) and tested to what extent historical colonization and dispersal limitation (i.e. accessibility from areas of geographic origin) can explain present-day species richness relative to current climate, topography, and climate change since the late Miocene (~10 mya), the Pliocene (~3 mya), and the Last Glacial Maximum (LGM, 0.021 mya). Spatial and non-spatial multi-predictor regression models revealed that time-limited dispersal via arid corridors is a key predictor to explain macro-scale patterns of species richness. In addition, current precipitation seasonality, current temperature of the warmest month, paleo-temperature changes since the LGM and late Miocene, and topographic relief emerged as important drivers. These results suggest that deep-time dispersal constraints — in addition to climate and mountain building — strongly shape current species richness of Africa’s arid-adapted taxa. Such historical dispersal limitation might indicate that natural movement rates of species are too slow to respond to rates of ongoing and projected future climate and land use change.
机译:深度分散限制在多大程度上影响了当今生物多样性的范围。在这里,我们针对爬行动物亚科Agaminae(一种相对较年轻的agamid蜥蜴的新近辐射,其祖先从阿拉伯半岛殖民了非洲)收集了非洲蜥蜴物种分布的大陆数据集,并测试了历史殖民化和传播限制(即从地理起源地区的可及性)可以解释自中新世晚期(〜10 mya),上新世(〜3 mya)和最后一次冰河期(LGM)以来相对于当前气候,地形和气候变化的当今物种丰富度0.021 mya)。空间和非空间的多指标回归模型显示,通过干旱走廊的限时扩散是解释物种丰富度宏观格局的关键指标。此外,目前的降水季节,最温暖月份的当前温度,自LGM和中新世晚期以来的古温度变化以及地形起伏都成为重要的驱动力。这些结果表明,除了气候和山区建设以外,深层的扩散限制还强烈地影响着非洲干旱适应的分类单元当前的物种丰富度。这种历史上的扩散局限性可能表明,物种的自然移动速度太慢,无法应对当前和预计的未来气候和土地利用变化的速度。

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