Similar pattern, different paths: tracing the biogeographical history of Megaloptera (Insecta: Neuropterida) using mitochondrial phylogenomics

变异 生物扩散 生物 间断 生态学 生物地理学 间断分布 泛大陆 古生物学 系统发育学 系统地理学 系统发育树 人口 人口学 社会学 构造盆地 基因 二叠纪 生物化学
作者
Yunlan Jiang,Yue Lu,Fan Yang,Jéssica P. Gillung,Shaun L. Winterton,Benjamin Price,Atilano Contreras‐Ramos,Fumio Hayashi,Ulrike Aspöck,Horst Aspöck,David K. Yeates,Ding Yang,Xingyue Liu
出处
期刊:Cladistics [Wiley]
卷期号:38 (3): 374-391 被引量:13
标识
DOI:10.1111/cla.12494
摘要

The sequential breakup of the supercontinent Pangaea since the Middle Jurassic is one of the crucial factors that has driven the biogeographical patterns of terrestrial biotas. Despite decades of effort searching for concordant patterns between diversification and continental fragmentation among taxonomic groups, increasing evidence has revealed more complex and idiosyncratic scenarios resulting from a mixture of vicariance, dispersal and extinction. Aquatic insects with discreet ecological requirements, low vagility and disjunct distributions represent a valuable model for testing biogeographical hypotheses by reconstructing their distribution patterns and temporal divergences. Insects of the order Megaloptera have exclusively aquatic larvae, their adults have low vagility, and the group has a highly disjunct geographical distribution. Here we present a comprehensive phylogeny of Megaloptera based on a large-scale mitochondrial genome sequencing of 99 species representing >90% of the world genera from all major biogeographical regions. Molecular dating suggests that the deep divergence within Megaloptera pre-dates the breakup of Pangaea. Subsequently, the intergeneric divergences within Corydalinae (dobsonflies), Chauliodinae (fishflies) and Sialidae (alderflies) might have been driven by both vicariance and dispersal correlated with the shifting continent during the Cretaceous, but with strikingly different and incongruent biogeographical signals. The austral distribution of many corydalids appears to be a result of colonization from Eurasia through southward dispersal across Europe and Africa during the Cretaceous, whereas a nearly contemporaneous dispersal via northward rafting of Gondwanan landmasses may account for the colonization of extant Eurasian alderflies from the south.
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