Data from: Dispersal largely explains the Gondwanan distribution of the ancient tropical clusioid plant clade
PREMISE OF THE STUDY: The clusioid clade (Malpighiales) has an ancient fossil record (∼90 Ma) and extant representatives exhibit a pantropical distribution represented on all former Gondwanan landmasses (Africa, Australia, India, Madagascar, and South America) except Antarctica. Several biogeographe...
Main Authors: | , , , |
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Format: | Other/Unknown Material |
Language: | unknown |
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Zenodo
2017
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Online Access: | https://doi.org/10.5061/dryad.q4h2r |
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author | Ruhfel, Brad R. Bove, Claudia P. Philbrick, C. Thomas Davis, Charles C. |
author_facet | Ruhfel, Brad R. Bove, Claudia P. Philbrick, C. Thomas Davis, Charles C. |
author_sort | Ruhfel, Brad R. |
collection | Zenodo |
description | PREMISE OF THE STUDY: The clusioid clade (Malpighiales) has an ancient fossil record (∼90 Ma) and extant representatives exhibit a pantropical distribution represented on all former Gondwanan landmasses (Africa, Australia, India, Madagascar, and South America) except Antarctica. Several biogeographers have hypothesized that the clusioid distribution is an example of Gondwanan vicariance. Our aim is to test the hypothesis that the modern distribution of the clusioid clade is largely explained by Gondwanan fragmentation. METHODS: Using a four gene, 207-taxon data set we simultaneously estimated the phylogeny and divergence times of the clusioid clade using a Bayesian Markov chain Monte Carlo approach. Ancestral Area Reconstructions (AARs) were then conducted on a distribution of 1000 trees and summarized on a reduced phylogeny. KEY RESULTS: Divergence time estimates and AARs revealed only two or four cladogenic events that are potentially consistent with Gondwanan vicariance, depending on the placement of the ancient fossil Paleoclusia. In contrast, dispersal occurred on > 25% of the branches, indicating the current distribution of the clade likely reflects extensive recent dispersal during the Cenozoic (< 65 Ma), most of which occurred after the beginning of the Eocene (∼56 Ma). CONCLUSIONS: These results support growing evidence that suggests many traditionally recognized angiosperm clades (families and genera) are too young for their distributions to have been influenced strictly by Gondwanan fragmentation. Instead, it appears that corridors of dispersal may be the best explanation for numerous angiosperm clades with Gondwanan distributions. 4 gene cludioid Alignment nexus alignment file with partition information clusioid4gene_Ruhfel.nex BC_MCCFull_Ruhfel_clusioids Full maximum clade credibility chronogram of the clusioid clade based on the analysis of a combined four-gene data set (BC placement of Paleoclusia; see text for details). Created by BEAST. CC_MCCFull_Ruhfel_clusioids Full maximum clade ... |
format | Other/Unknown Material |
genre | Antarc* Antarctica |
genre_facet | Antarc* Antarctica |
id | ftzenodo:oai:zenodo.org:4952206 |
institution | Open Polar |
language | unknown |
op_collection_id | ftzenodo |
op_doi | https://doi.org/10.5061/dryad.q4h2r10.3732/ajb.1500537 |
op_relation | https://doi.org/10.3732/ajb.1500537 https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.q4h2r oai:zenodo.org:4952206 |
op_rights | info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode |
publishDate | 2017 |
publisher | Zenodo |
record_format | openpolar |
spelling | ftzenodo:oai:zenodo.org:4952206 2025-01-16T19:41:30+00:00 Data from: Dispersal largely explains the Gondwanan distribution of the ancient tropical clusioid plant clade Ruhfel, Brad R. Bove, Claudia P. Philbrick, C. Thomas Davis, Charles C. 2017-05-19 https://doi.org/10.5061/dryad.q4h2r unknown Zenodo https://doi.org/10.3732/ajb.1500537 https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.q4h2r oai:zenodo.org:4952206 info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode Bonnetiaceae Podostemaceae vicariance Hypericaceae Clusiaceae Cenozic Calophyllaceae Malpighiales Gondwana info:eu-repo/semantics/other 2017 ftzenodo https://doi.org/10.5061/dryad.q4h2r10.3732/ajb.1500537 2024-12-05T08:59:52Z PREMISE OF THE STUDY: The clusioid clade (Malpighiales) has an ancient fossil record (∼90 Ma) and extant representatives exhibit a pantropical distribution represented on all former Gondwanan landmasses (Africa, Australia, India, Madagascar, and South America) except Antarctica. Several biogeographers have hypothesized that the clusioid distribution is an example of Gondwanan vicariance. Our aim is to test the hypothesis that the modern distribution of the clusioid clade is largely explained by Gondwanan fragmentation. METHODS: Using a four gene, 207-taxon data set we simultaneously estimated the phylogeny and divergence times of the clusioid clade using a Bayesian Markov chain Monte Carlo approach. Ancestral Area Reconstructions (AARs) were then conducted on a distribution of 1000 trees and summarized on a reduced phylogeny. KEY RESULTS: Divergence time estimates and AARs revealed only two or four cladogenic events that are potentially consistent with Gondwanan vicariance, depending on the placement of the ancient fossil Paleoclusia. In contrast, dispersal occurred on > 25% of the branches, indicating the current distribution of the clade likely reflects extensive recent dispersal during the Cenozoic (< 65 Ma), most of which occurred after the beginning of the Eocene (∼56 Ma). CONCLUSIONS: These results support growing evidence that suggests many traditionally recognized angiosperm clades (families and genera) are too young for their distributions to have been influenced strictly by Gondwanan fragmentation. Instead, it appears that corridors of dispersal may be the best explanation for numerous angiosperm clades with Gondwanan distributions. 4 gene cludioid Alignment nexus alignment file with partition information clusioid4gene_Ruhfel.nex BC_MCCFull_Ruhfel_clusioids Full maximum clade credibility chronogram of the clusioid clade based on the analysis of a combined four-gene data set (BC placement of Paleoclusia; see text for details). Created by BEAST. CC_MCCFull_Ruhfel_clusioids Full maximum clade ... Other/Unknown Material Antarc* Antarctica Zenodo |
spellingShingle | Bonnetiaceae Podostemaceae vicariance Hypericaceae Clusiaceae Cenozic Calophyllaceae Malpighiales Gondwana Ruhfel, Brad R. Bove, Claudia P. Philbrick, C. Thomas Davis, Charles C. Data from: Dispersal largely explains the Gondwanan distribution of the ancient tropical clusioid plant clade |
title | Data from: Dispersal largely explains the Gondwanan distribution of the ancient tropical clusioid plant clade |
title_full | Data from: Dispersal largely explains the Gondwanan distribution of the ancient tropical clusioid plant clade |
title_fullStr | Data from: Dispersal largely explains the Gondwanan distribution of the ancient tropical clusioid plant clade |
title_full_unstemmed | Data from: Dispersal largely explains the Gondwanan distribution of the ancient tropical clusioid plant clade |
title_short | Data from: Dispersal largely explains the Gondwanan distribution of the ancient tropical clusioid plant clade |
title_sort | data from: dispersal largely explains the gondwanan distribution of the ancient tropical clusioid plant clade |
topic | Bonnetiaceae Podostemaceae vicariance Hypericaceae Clusiaceae Cenozic Calophyllaceae Malpighiales Gondwana |
topic_facet | Bonnetiaceae Podostemaceae vicariance Hypericaceae Clusiaceae Cenozic Calophyllaceae Malpighiales Gondwana |
url | https://doi.org/10.5061/dryad.q4h2r |