ArticleCurrent zoology2020
Linking evolutionary mode to palaeoclimate change reveals rapid radiations of staphylinoid beetles in low-energy conditions.
Article in Current zoology, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 9 papers.
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9 citing papers in PubMed.
- The timescale of nematode evolution reveals late and convergent radiations of parasitism.Nature ecology & evolution · 2026Article
- Article
- A new fossil species of the extant genusEcology and evolution · 2024Article
- Review
- First record of Jacobsoniidae (Coleoptera) on the African continent in Holocene copal from Tanzania: biogeography since the Cretaceous.Scientific reports · 2023Article
- Mitochondrial phylogenomics provides insights into the phylogeny and evolution of spiders (Arthropoda: Araneae).Zoological research · 2022Article
- The oldest fossil record of Pseudopsinae from the Lower Cretaceous Yixian Formation of northeastern China (Coleoptera: Staphylinidae: Pseudopsinae).Scientific reports · 2022Article
- Integrated phylogenomics and fossil data illuminate the evolution of beetles.Royal Society open science · 2022Article
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6 authors.
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Abstract
Staphylinoidea (Insecta: Coleoptera) is one of the most species-rich groups in animals, but its huge diversity can hardly be explained by the popular hypothesis (co-radiation with angiosperms) that applies to phytophagous beetles. We estimated the evolutionary mode of staphylinoid beetles and investigated the relationship between the evolutionary mode and palaeoclimate change, and thus the factors underlying the current biodiversity pattern of staphylinoid beetles. Our results demonstrate that staphylinoid beetles originated at around the Triassic-Jurassic bound and the current higher level clades underwent rapid evolution (indicated by increased diversification rate and decreased body size disparity) in the Jurassic and in the Cenozoic, both with low-energy climate, and they evolved much slower during the Cretaceous with high-energy climate. Climate factors, especially low O
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