Phylogeny and Biogeography of a Cosmopolitan Frog Radiation: Late Cretaceous Diversification Resulted in Continent-Scale Endemism in the Family Ranidae

Ranidae is a large anuran group with a nearly cosmopolitan distribution. We investigated the phylogenetic relationships and early biogeographic history of ranid frogs, using 104 representatives of all subfamilies and families, sampled from throughout their distribution. Analyses of ∼ 1570 bp of nucl...

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Published inSystematic biology Vol. 55; no. 4; pp. 579 - 594
Main Authors Bossuyt, Franky, Brown, Rafe M., Hillis, David M., Cannatella, David C., Milinkovitch, Michel C., Kjer, Karl
Format Journal Article
LanguageEnglish
Published England Society of Systematic Zoology 01.08.2006
Taylor & Francis
Oxford University Press
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Abstract Ranidae is a large anuran group with a nearly cosmopolitan distribution. We investigated the phylogenetic relationships and early biogeographic history of ranid frogs, using 104 representatives of all subfamilies and families, sampled from throughout their distribution. Analyses of ∼ 1570 bp of nuclear gene fragments (Rag-1, rhod, Tyr) and ∼ 2100 bp of the mitochondrial genome (12S rRNA, tRNAVAL, 16S rRNA) indicate that the monophyly of several taxa can be rejected with high confidence. Our tree is characterized by a clear historical association of each major clade with one Gondwanan plate. This prevalence of continent-scale endemism suggests that plate tectonics has played a major role in the distribution of ranid frogs. We performed dispersal-vicariance analyses, as well as analyses constrained by paleogeographic data, to estimate ancestral distributions during early ranid diversification. Additionally, we used molecular clock analyses to evaluate whether these scenarios fit the temporal framework of continental breakup. Our analyses suggest that a scenario in which the ancestors of several clades (Rhacophorinae, Dicroglossinae, Raninae) reached Eurasia via the Indian subcontinent, and the ancestor of Ceratobatrachinae entered via the Australia–New Guinea plate, best fits the paleogeographic models and requires the fewest number of dispersal/vicariance events. However, several alternatives, in which part of the ranid fauna colonized Laurasia from Africa, are not significantly worse. Most importantly, all hypotheses make clear predictions as to where to expect key fossils and where to sample other living ranids, and thus constitute a strong basis for further research.
AbstractList Ranidae is a large anuran group with a nearly cosmopolitan distribution. We investigated the phylogenetic relationships and early biogeographic history of ranid frogs, using 104 representatives of all subfamilies and families, sampled from throughout their distribution. Analyses of ~1570 bp of nuclear gene fragments (Rag-1, rhod, Tyr) and ~2100 bp of the mitochondrial genome (12S rRNA, tRNA^sup V AL^, 16S rRNA) indicate that the monophyly or several taxa can be rejected with high confidence. Our tree is characterized by a clear historical association of each major clade with one Gondwanan plate. This prevalence of continent-scale endemism suggests that plate tectonics has played a major role in the distribution of ranid frogs. We performed dispersal-vicariance analyses, as well as analyses constrained by paleogeographic data, to estimate ancestral distributions during early ranid diversification. Additionally, we used molecular clock analyses to evaluate whether these scenarios fit the temporal framework of continental breakup. Our analyses suggest that a scenario in which the ancestors of several clades (Rhacophorinae, Dicroglossinae, Raninae) reached Eurasia via the Indian subcontinent, and the ancestor of Ceratobatrachinae entered via the Australia-New Guinea plate, best fits the paleogeographic models and requires the fewest number of dispersal/vicariance events. However, several alternatives, in which part of the ranid fauna colonized Laurasia from Africa, are not significantly worse. Most importantly, all hypotheses make clear predictions as to where to expect key fossils and where to sample other living ranids, and thus constitute a strong basis for further research. [PUBLICATION ABSTRACT]
Abstract Ranidae is a large anuran group with a nearly cosmopolitan distribution. We investigated the phylogenetic relationships and early biogeographic history of ranid frogs, using 104 representatives of all subfamilies and families, sampled from throughout their distribution. Analyses of ∼ 1570 bp of nuclear gene fragments (Rag-1, rhod, Tyr) and ∼ 2100 bp of the mitochondrial genome (12S rRNA, tRNAVAL, 16S rRNA) indicate that the monophyly of several taxa can be rejected with high confidence. Our tree is characterized by a clear historical association of each major clade with one Gondwanan plate. This prevalence of continent-scale endemism suggests that plate tectonics has played a major role in the distribution of ranid frogs. We performed dispersal-vicariance analyses, as well as analyses constrained by paleogeographic data, to estimate ancestral distributions during early ranid diversification. Additionally, we used molecular clock analyses to evaluate whether these scenarios fit the temporal framework of continental breakup. Our analyses suggest that a scenario in which the ancestors of several clades (Rhacophorinae, Dicroglossinae, Raninae) reached Eurasia via the Indian subcontinent, and the ancestor of Ceratobatrachinae entered via the Australia–New Guinea plate, best fits the paleogeographic models and requires the fewest number of dispersal/vicariance events. However, several alternatives, in which part of the ranid fauna colonized Laurasia from Africa, are not significantly worse. Most importantly, all hypotheses make clear predictions as to where to expect key fossils and where to sample other living ranids, and thus constitute a strong basis for further research.
Ranidae is a large anuran group with a nearly cosmopolitan distribution. We investigated the phylogenetic relationships and early biogeographic history of ranid frogs, using 104 representatives of all subfamilies and families, sampled from throughout their distribution. Analyses of approximately 1570 bp of nuclear gene fragments (Rag-1, rhod, Tyr) and approximately 2100 bp of the mitochondrial genome (12S rRNA, tRNAVAL, 16S rRNA) indicate that the monophyly of several taxa can be rejected with high confidence. Our tree is characterized by a clear historical association of each major clade with one Gondwanan plate. This prevalence of continent-scale endemism suggests that plate tectonics has played a major role in the distribution of ranid frogs. We performed dispersal-vicariance analyses, as well as analyses constrained by paleogeographic data, to estimate ancestral distributions during early ranid diversification. Additionally, we used molecular clock analyses to evaluate whether these scenarios fit the temporal framework of continental breakup. Our analyses suggest that a scenario in which the ancestors of several clades (Rhacophorinae, Dicroglossinae, Raninae) reached Eurasia via the Indian subcontinent, and the ancestor of Ceratobatrachinae entered via the Australia-New Guinea plate, best fits the paleogeographic models and requires the fewest number of dispersal/vicariance events. However, several alternatives, in which part of the ranid fauna colonized Laurasia from Africa, are not significantly worse. Most importantly, all hypotheses make clear predictions as to where to expect key fossils and where to sample other living ranids, and thus constitute a strong basis for further research.
Ranidae is a large anuran group with a nearly cosmopolitan distribution. We investigated the phylogenetic relationships and early biogeographic history of ranid frogs, using 104 representatives of all subfamilies and families, sampled from throughout their distribution. Analyses of ∼1570 bp of nuclear gene fragments (Rag-1, rhod, Tyr) and ∼2100 bp of the mitochondrial genome (12S rRNA,$tRNA^{VAL}$, 16S rRNA) indicate that the monophyly of several taxa can be rejected with high confidence. Our tree is characterized by a clear historical association of each major clade with one Gondwanan plate. This prevalence of continent-scale endemism suggests that plate tectonics has played a major role in the distribution of ranid frogs. We performed dispersal-vicariance analyses, as well as analyses constrained by paleogeographic data, to estimate ancestral distributions during early ranid diversification. Additionally, we used molecular clock analyses to evaluate whether these scenarios fit the temporal framework of continental breakup. Our analyses suggest that a scenario in which the ancestors of several clades (Rhacophorinae, Dicroglossinae, Raninae) reached Eurasia via the Indian subcontinent, and the ancestor of Ceratobatrachinae entered via the Australia--New Guinea plate, best fits the paleogeographic models and requires the fewest number of dispersal / vicariance events. However, several alternatives, in which part of the ranid fauna colonized Laurasia from Africa, are not significantly worse. Most importantly, all hypotheses make clear predictions as to where to expect key fossils and where to sample other living ranids, and thus constitute a strong basis for further research.
Ranidae is a large anuran group with a nearly cosmopolitan distribution. We investigated the phylogenetic relationships and early biogeographic history of ranid frogs, using 104 representatives of all subfamilies and families, sampled from throughout their distribution. Analyses of ∼ 1570 bp of nuclear gene fragments (Rag-1, rhod, Tyr) and ∼ 2100 bp of the mitochondrial genome (12S rRNA, tRNAVAL, 16S rRNA) indicate that the monophyly of several taxa can be rejected with high confidence. Our tree is characterized by a clear historical association of each major clade with one Gondwanan plate. This prevalence of continent-scale endemism suggests that plate tectonics has played a major role in the distribution of ranid frogs. We performed dispersal-vicariance analyses, as well as analyses constrained by paleogeographic data, to estimate ancestral distributions during early ranid diversification. Additionally, we used molecular clock analyses to evaluate whether these scenarios fit the temporal framework of continental breakup. Our analyses suggest that a scenario in which the ancestors of several clades (Rhacophorinae, Dicroglossinae, Raninae) reached Eurasia via the Indian subcontinent, and the ancestor of Ceratobatrachinae entered via the Australia–New Guinea plate, best fits the paleogeographic models and requires the fewest number of dispersal/vicariance events. However, several alternatives, in which part of the ranid fauna colonized Laurasia from Africa, are not significantly worse. Most importantly, all hypotheses make clear predictions as to where to expect key fossils and where to sample other living ranids, and thus constitute a strong basis for further research.
Author Bossuyt, Franky
Cannatella, David C.
Brown, Rafe M.
Hillis, David M.
Milinkovitch, Michel C.
Author_xml – sequence: 1
  givenname: Franky
  surname: Bossuyt
  fullname: Bossuyt, Franky
  email: Biology Department, Unit of Ecology & Systematics, Vrije Universiteit Brussel Pleinlaan 2, B-1050, Brussels, Belgium fbossuyt@vub.ac.be, fbossuyt@vub.ac.be
  organization: Biology Department, Unit of Ecology & Systematics, Vrije Universiteit Brussel Pleinlaan 2, B-1050, Brussels, Belgium E-mail: fbossuyt@vub.ac.be
– sequence: 2
  givenname: Rafe M.
  surname: Brown
  fullname: Brown, Rafe M.
  organization: Section of Integrative Biology and Texas Memorial Museum, The University of Texas at Austin Austin, Texas, 78712, USA
– sequence: 3
  givenname: David M.
  surname: Hillis
  fullname: Hillis, David M.
  organization: Section of Integrative Biology and Center for Computational Biology and Bioinformatics, University of Texas Austin, Texas, 78712, USA
– sequence: 4
  givenname: David C.
  surname: Cannatella
  fullname: Cannatella, David C.
  organization: Section of Integrative Biology and Texas Memorial Museum, The University of Texas at Austin Austin, Texas, 78712, USA
– sequence: 5
  givenname: Michel C.
  surname: Milinkovitch
  fullname: Milinkovitch, Michel C.
  organization: Laboratory of Evolutionary Genetics, Université Libre de Bruxelles (ULB), C.P. 300, Institute for Molecular Biology and Medicine Rue Jeener & Brachet 12, B-6041, Gosselies, Belgium
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  givenname: Karl
  surname: Kjer
  fullname: Kjer, Karl
  email: fbossuyt@vub.ac.be
  organization: Biology Department, Unit of Ecology & Systematics, Vrije Universiteit Brussel, Pleinlaan 2, B-1050, Brussels, Belgium, Austin, Texas, 78712, USA, Austin, Texas, 78712, USA, Rue Jeener & Brachet 12, B-6041, Gosselies, Belgium
BackLink https://www.ncbi.nlm.nih.gov/pubmed/16857652$$D View this record in MEDLINE/PubMed
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2006 Society of Systematic Biologists 2006
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Keywords Anura
Ranoidea
Ranidae
biogeography
convergence
radiation
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Snippet Ranidae is a large anuran group with a nearly cosmopolitan distribution. We investigated the phylogenetic relationships and early biogeographic history of...
Abstract Ranidae is a large anuran group with a nearly cosmopolitan distribution. We investigated the phylogenetic relationships and early biogeographic...
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crossref
pubmed
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jstor
istex
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StartPage 579
SubjectTerms Amphibians
Anger
Animals
Anura
Base Sequence
Bayes Theorem
Biogeography
Calibration
convergence
Demography
DNA, Mitochondrial - genetics
Evolution
Evolution, Molecular
Evolutionary biology
Fossils
Frogs
Genetic Speciation
Geography
Geological time
Likelihood Functions
Models, Genetic
Models, Theoretical
Molecular Sequence Data
Paleogeography
Phylogeny
Plate tectonics
radiation
Ranidae
Ranidae - genetics
Ranoidea
Sequence Analysis, DNA
Species Specificity
Title Phylogeny and Biogeography of a Cosmopolitan Frog Radiation: Late Cretaceous Diversification Resulted in Continent-Scale Endemism in the Family Ranidae
URI https://api.istex.fr/ark:/67375/HXZ-BGJ43M5S-L/fulltext.pdf
https://www.jstor.org/stable/20142956
https://www.ncbi.nlm.nih.gov/pubmed/16857652
https://www.proquest.com/docview/194782266
https://search.proquest.com/docview/68655428
Volume 55
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