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有鳞目爬行动物气候生态位的演化

The evolution of climatic niches in squamate reptiles.

作者信息

Pie Marcio R, Campos Leonardo L F, Meyer Andreas L S, Duran Andressa

机构信息

Departamento de Zoologia, Universidade Federal do Paraná, Curitiba, Paraná, Brazil

Programa de Pós-Graduação em Zoologia, Universidade Federal do Paraná, CEP 81531-990 Curitiba, Paraná, Brazil.

出版信息

Proc Biol Sci. 2017 Jul 12;284(1858). doi: 10.1098/rspb.2017.0268.

Abstract

Despite the remarkable diversity found in squamate reptiles, most of their species tend to be found in warm/dry environments, suggesting that climatic requirements played a crucial role in their diversification, yet little is known about the evolution of their climatic niches. In this study, we integrate climatic information associated with the geographical distribution of 1882 squamate species and their phylogenetic relationships to investigate the tempo and mode of climatic niche evolution in squamates, both over time and among lineages. We found that changes in climatic niche dynamics were pronounced over their recent squamate evolutionary history, and we identified extensive evidence for rate heterogeneity in squamate climatic niche evolution. Most rate shifts involved accelerations, particularly over the past 50 Myr. Most squamates occupy similar regions of the climatic niche space, with only a few lineages diversifying into colder and humid climatic conditions. The changes from arid to mesic conditions in some regions of the globe may have provided opportunities for climatic niche evolution, although most lineages tended to remain near their ancestral niche. Variation in rates of climatic niche evolution seems common, particularly in response to the availability of new climatic conditions over evolutionary time.

摘要

尽管有鳞目爬行动物具有显著的多样性,但它们的大多数物种往往分布在温暖/干燥的环境中,这表明气候需求在它们的物种分化中起到了关键作用,然而对于它们气候生态位的演化却知之甚少。在本研究中,我们整合了与1882种有鳞目物种地理分布相关的气候信息及其系统发育关系,以研究有鳞目动物气候生态位随时间和谱系演化的节奏和模式。我们发现,在有鳞目动物最近的进化历史中,气候生态位动态变化显著,并且我们发现了有鳞目动物气候生态位演化中速率异质性的广泛证据。大多数速率变化涉及加速,尤其是在过去5000万年中。大多数有鳞目动物占据气候生态位空间的相似区域,只有少数谱系分化到更寒冷和潮湿的气候条件中。全球某些地区从干旱到湿润条件的变化可能为气候生态位演化提供了机会,尽管大多数谱系倾向于保持在其祖先生态位附近。气候生态位演化速率的变化似乎很常见,特别是在进化过程中对新气候条件可用性的响应方面。

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