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Rackham School of Graduate Studies, University of Michigan","doi-asserted-by":"publisher","id":[{"id":"10.13039\/100006801","id-type":"DOI","asserted-by":"publisher"}]},{"DOI":"10.13039\/100006069","name":"Society of Systematic Biologists","doi-asserted-by":"publisher","id":[{"id":"10.13039\/100006069","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":["royalsocietypublishing.org"],"crossmark-restriction":true},"short-container-title":["Proc. R. Soc. B."],"published-print":{"date-parts":[[2024,8]]},"abstract":"<jats:p>The separation of closely related terrestrial or freshwater species by vast marine barriers represents a biogeographical riddle. Such cases can provide evidence for vicariance, a process whereby ancient geological events like continental rifting divided ancestral geographical ranges. With an evolutionary history extending tens of millions of years, freshwater ecology, and distribution encompassing widely separated southern landmasses, osteoglossid bonytongue fishes are a textbook case of vicariance attributed to Mesozoic fragmentation of the Gondwanan supercontinent. Largely overlooked fossils complicate the clean narrative invoked for extant species by recording occurrences on additional continents and in marine settings. Here, we present a new total-evidence phylogenetic hypothesis for bonytongue fishes combined with quantitative models of range evolution and show that the last common ancestor of extant osteoglossids was likely marine, and that the group colonized freshwater settings at least four times when both extant and extinct lineages are considered. The correspondence between extant osteoglossid relationships and patterns of continental fragmentation therefore represents a striking example of biogeographical pseudocongruence. Contrary to arguments against vicariance hypotheses that rely only on temporal or phylogenetic evidence, these results provide direct palaeontological support for enhanced dispersal ability early in the history of a group with widely separated distributions in the modern day.<\/jats:p>","DOI":"10.1098\/rspb.2024.1293","type":"journal-article","created":{"date-parts":[[2024,8,13]],"date-time":"2024-08-13T23:05:30Z","timestamp":1723590330000},"update-policy":"https:\/\/doi.org\/10.1098\/crossmark-policy","source":"Crossref","is-referenced-by-count":13,"title":["Fossils indicate marine dispersal in osteoglossid fishes, a classic example of continental vicariance"],"prefix":"10.1098","volume":"291","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-6096-3875","authenticated-orcid":true,"given":"Alessio","family":"Capobianco","sequence":"first","affiliation":[{"name":"GeoBio-Center LMU, Ludwig-Maximilians-Universit\u00e4t M\u00fcnchen , Munich, Germany"},{"name":"Department of Earth and Environmental Sciences, Palaeontology &amp; Geobiology, Ludwig-Maximilians-Universit\u00e4t M\u00fcnchen , Munich, Germany"},{"name":"Department of Earth and Environmental Sciences, University of Michigan , Ann Arbor, MI, USA"},{"name":"Museum of Paleontology, University of Michigan , Ann Arbor, MI, USA"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-0114-7384","authenticated-orcid":true,"given":"Matt","family":"Friedman","sequence":"additional","affiliation":[{"name":"Department of Earth and Environmental Sciences, University of Michigan , Ann Arbor, MI, USA"},{"name":"Museum of Paleontology, University of Michigan , Ann Arbor, MI, USA"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"175","published-online":{"date-parts":[[2024,8,14]]},"reference":[{"key":"e_1_3_8_2_2","doi-asserted-by":"publisher","DOI":"10.5962\/bhl.title.82303"},{"key":"e_1_3_8_3_2","volume-title":"The geographical distribution of animals; with a study of the relations of living and extinct faunas as elucidating the past changes of the Earth\u2019s surface","author":"Wallace AR","year":"1876","unstructured":"Wallace AR . 1876 The geographical distribution of animals; with a study of the relations of living and extinct faunas as elucidating the past changes of the Earth\u2019s surface. 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