Formation of the Holarctic Fauna: Dated molecular phylogenetic and biogeographic insights from the Quedius-lineage of Ground-Dwelling Rove Beetles (Coleoptera, Staphylinidae). Hansen, A. K., Brunke, A. J., Thomsen, P. F., Simonsen, T. J., & Solodovnikov, A. Molecular Phylogenetics and Evolution, 182:107749, May, 2023. ![Formation of the Holarctic Fauna: Dated molecular phylogenetic and biogeographic insights from the Quedius-lineage of Ground-Dwelling Rove Beetles (Coleoptera, Staphylinidae) [link]](https://bibbase.org/img/filetypes/link.svg "link")
Paper doi abstract bibtex Although the Holarctic fauna has been explored for centuries, many questions on its formation are still unanswered. For example, i) what was the impact of the uplift of the Himalaya and Tibetan Plateau?, ii) what were the timings and climate of the faunal bridges connecting the Nearctic and Palearctic regions?, and iii) how did insect lineages respond to the late Paleogene global cooling and regional aridification? To answer these, we developed a phylogenetic dataset of 1229 nuclear loci for a total of 222 species of rove beetles (Staphylinidae) with emphasis in the tribe Quediini, especially Quedius-lineage and its subclade Quedius sensu stricto. Using eight fossils for calibrating molecular clock, we estimated divergence times and then analysed in BioGeoBEARS paleodistributions of the most recent common ancestor for each target lineage. For each species we generated climatic envelopes of the temperature and precipitation and mapped them across the phylogeny to explore evolutionary shifts. Our results suggest that the warm and humid Himalaya and Tibetan Plateau acted as an evolutionary cradle for the Quedius-lineage originating during the Oligocene from where, in the Early Miocene, the ancestor of the Quedius s. str. dispersed into the West Palearctic. With the climate cooling from the Mid Miocene onwards, new lineages within Quedius s. str. emerged and gradually expanded distributions across the Palearctic. In Late Miocene, a member of the group dispersed to the Nearctic region via Beringia before the closure of this land bridge 5.3 Ma. Paleogene global cooling and regional aridification largely shaped the current biogeographic pattern for Quedius s. str. species, many of them originating during the Pliocene and shifting or contracting their ranges during Pleistocene.
@article{hansen_formation_2023,
title = {Formation of the {Holarctic} {Fauna}: {Dated} molecular phylogenetic and biogeographic insights from the {Quedius}-lineage of {Ground}-{Dwelling} {Rove} {Beetles} ({Coleoptera}, {Staphylinidae})},
volume = {182},
issn = {1055-7903},
shorttitle = {Formation of the {Holarctic} {Fauna}},
url = {https://www.sciencedirect.com/science/article/pii/S1055790323000490},
doi = {10.1016/j.ympev.2023.107749},
abstract = {Although the Holarctic fauna has been explored for centuries, many questions on its formation are still unanswered. For example, i) what was the impact of the uplift of the Himalaya and Tibetan Plateau?, ii) what were the timings and climate of the faunal bridges connecting the Nearctic and Palearctic regions?, and iii) how did insect lineages respond to the late Paleogene global cooling and regional aridification? To answer these, we developed a phylogenetic dataset of 1229 nuclear loci for a total of 222 species of rove beetles (Staphylinidae) with emphasis in the tribe Quediini, especially Quedius-lineage and its subclade Quedius sensu stricto. Using eight fossils for calibrating molecular clock, we estimated divergence times and then analysed in BioGeoBEARS paleodistributions of the most recent common ancestor for each target lineage. For each species we generated climatic envelopes of the temperature and precipitation and mapped them across the phylogeny to explore evolutionary shifts. Our results suggest that the warm and humid Himalaya and Tibetan Plateau acted as an evolutionary cradle for the Quedius-lineage originating during the Oligocene from where, in the Early Miocene, the ancestor of the Quedius s. str. dispersed into the West Palearctic. With the climate cooling from the Mid Miocene onwards, new lineages within Quedius s. str. emerged and gradually expanded distributions across the Palearctic. In Late Miocene, a member of the group dispersed to the Nearctic region via Beringia before the closure of this land bridge 5.3 Ma. Paleogene global cooling and regional aridification largely shaped the current biogeographic pattern for Quedius s. str. species, many of them originating during the Pliocene and shifting or contracting their ranges during Pleistocene.},
language = {en},
urldate = {2023-07-04},
journal = {Molecular Phylogenetics and Evolution},
author = {Hansen, Aslak Kappel and Brunke, Adam J. and Thomsen, Philip Francis and Simonsen, Thomas J. and Solodovnikov, Alexey},
month = may,
year = {2023},
keywords = {Terrestrial Ecoregions (CEC 1997)},
pages = {107749},
}
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For example, i) what was the impact of the uplift of the Himalaya and Tibetan Plateau?, ii) what were the timings and climate of the faunal bridges connecting the Nearctic and Palearctic regions?, and iii) how did insect lineages respond to the late Paleogene global cooling and regional aridification? To answer these, we developed a phylogenetic dataset of 1229 nuclear loci for a total of 222 species of rove beetles (Staphylinidae) with emphasis in the tribe Quediini, especially Quedius-lineage and its subclade Quedius sensu stricto. Using eight fossils for calibrating molecular clock, we estimated divergence times and then analysed in BioGeoBEARS paleodistributions of the most recent common ancestor for each target lineage. For each species we generated climatic envelopes of the temperature and precipitation and mapped them across the phylogeny to explore evolutionary shifts. 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Paleogene global cooling and regional aridification largely shaped the current biogeographic pattern for Quedius s. str. species, many of them originating during the Pliocene and shifting or contracting their ranges during Pleistocene.","language":"en","urldate":"2023-07-04","journal":"Molecular Phylogenetics and Evolution","author":[{"propositions":[],"lastnames":["Hansen"],"firstnames":["Aslak","Kappel"],"suffixes":[]},{"propositions":[],"lastnames":["Brunke"],"firstnames":["Adam","J."],"suffixes":[]},{"propositions":[],"lastnames":["Thomsen"],"firstnames":["Philip","Francis"],"suffixes":[]},{"propositions":[],"lastnames":["Simonsen"],"firstnames":["Thomas","J."],"suffixes":[]},{"propositions":[],"lastnames":["Solodovnikov"],"firstnames":["Alexey"],"suffixes":[]}],"month":"May","year":"2023","keywords":"Terrestrial Ecoregions (CEC 1997)","pages":"107749","bibtex":"@article{hansen_formation_2023,\n\ttitle = {Formation of the {Holarctic} {Fauna}: {Dated} molecular phylogenetic and biogeographic insights from the {Quedius}-lineage of {Ground}-{Dwelling} {Rove} {Beetles} ({Coleoptera}, {Staphylinidae})},\n\tvolume = {182},\n\tissn = {1055-7903},\n\tshorttitle = {Formation of the {Holarctic} {Fauna}},\n\turl = {https://www.sciencedirect.com/science/article/pii/S1055790323000490},\n\tdoi = {10.1016/j.ympev.2023.107749},\n\tabstract = {Although the Holarctic fauna has been explored for centuries, many questions on its formation are still unanswered. For example, i) what was the impact of the uplift of the Himalaya and Tibetan Plateau?, ii) what were the timings and climate of the faunal bridges connecting the Nearctic and Palearctic regions?, and iii) how did insect lineages respond to the late Paleogene global cooling and regional aridification? To answer these, we developed a phylogenetic dataset of 1229 nuclear loci for a total of 222 species of rove beetles (Staphylinidae) with emphasis in the tribe Quediini, especially Quedius-lineage and its subclade Quedius sensu stricto. Using eight fossils for calibrating molecular clock, we estimated divergence times and then analysed in BioGeoBEARS paleodistributions of the most recent common ancestor for each target lineage. For each species we generated climatic envelopes of the temperature and precipitation and mapped them across the phylogeny to explore evolutionary shifts. 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