4.5 Article

Middle Jurassic origin in India: a new look at evolution of Vermileonidae and time-scaled relationships of lower brachyceran flies

Journal

ZOOLOGICAL JOURNAL OF THE LINNEAN SOCIETY
Volume 194, Issue 3, Pages 938-959

Publisher

OXFORD UNIV PRESS
DOI: 10.1093/zoolinnean/zlab042

Keywords

biogeography; Insecta; mitochondrial DNA; phylogeny

Categories

Funding

  1. National Natural Science Foundation of China [31772497, 31970444, 31970435]

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Vermileonidae is an odd and rarely collected dipteran family, with larvae famous for their unique prey behavior and adults rarely seen. Researchers have sequenced the complete mitochondrial genome of Vermileonidae for the first time, providing insights into its phylogenetic relationships with other flies. By combining mitochondrial genome data with morphology, geographical distribution, and geological history, researchers propose that Vermileonidae originated in India and spread to Africa, the Palaearctic, and the Nearctic through land bridges.
Vermileonidae (wormlions) comprises 61 described species in 12 genera and is one of the oddest and most rarely collected dipteran families. Larvae of Vermileonidae are famous for their pitfall prey behaviour, whereas the adults are rarely seen. Here we report, for the first time, the complete mitochondrial genome from members of Vermileonidae. Phylogenetic reconstruction based on a representative sampling of the order reveals new insights into relationships between the Vermileonidae and other members of lower brachyceran flies. A sister-group relationship between Vermileonidae and Xylophagidae is supported, and the higher-level clade relationships are Tabanomorpha + (Muscomorpha + (Xylophagomorpha + Stratiomyomorpha)). Combining mitochondrial genome data with a morphological phylogeny, geographical distribution and geological history, we propose that the Vermileonidae originated in India during the Middle Jurassic, spreading to Africa via land bridges during the Late Jurassic, to the Palaearctic after the collision of India with Laurasia in the Late Oligocene, and to the Nearctic in the Early Miocene, via either North Atlantic or Beringian land bridges. Wet forested regions have proved to be barriers to their dispersal, explaining their absence from Central Africa, South America and eastern North America.

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