Data from: Ultraconserved elements improve resolution of marmot phylogeny and offer insights into biogeographic history

Marmots ( Marmota spp.) comprise a lineage of large-bodied ground squirrels that diversified rapidly in the Pleistocene, when the planet quickly transitioned to a drier, colder, and highly seasonal climate—particularly at high latitudes. Fossil evidence indicates the genus spread from North America,...

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Main Author: Mills, Kendall
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2023
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Online Access:https://doi.org/10.5061/dryad.6hdr7sr56
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spelling ftzenodo:oai:zenodo.org:7759923 2024-09-15T17:59:20+00:00 Data from: Ultraconserved elements improve resolution of marmot phylogeny and offer insights into biogeographic history Mills, Kendall 2023-03-22 https://doi.org/10.5061/dryad.6hdr7sr56 unknown Zenodo https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.6hdr7sr56 oai:zenodo.org:7759923 info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode Marmota ultraconserved elements info:eu-repo/semantics/other 2023 ftzenodo https://doi.org/10.5061/dryad.6hdr7sr56 2024-07-26T20:34:45Z Marmots ( Marmota spp.) comprise a lineage of large-bodied ground squirrels that diversified rapidly in the Pleistocene, when the planet quickly transitioned to a drier, colder, and highly seasonal climate—particularly at high latitudes. Fossil evidence indicates the genus spread from North America, across Beringia, and into the European Alps over the course of only a few million years, beginning in the late Pliocene. Marmots are highly adapted to survive long and severely cold winters, and this likely favored their expansion and diversification over this time period. Previous phylogenetic studies have identified two major subgenera of marmots, but the timing of important speciation events and some species relationships have been difficult to resolve. Here we use ultraconserved elements and mitogenomes, with samples from all 15 extant species, to more precisely retrace how and when marmots came to inhabit a vast Holarctic range. Our results indicate marmots arose in North America in the mid Miocene (~16.3 Mya) and dispersed across the Bering Land Bridge in the late Pliocene (~3-4 Mya); in addition, our fossil-calibrated timeline is suggestive of the rise and spread of open grasslands as being particularly important to marmot diversification. The woodchuck ( M. monax ) and the Alaska marmot ( M. broweri ) are found to be more closely related to the Eurasian species than to the other North American species. Paraphyly is evident in the bobak marmot ( M. bobak ) and the hoary marmot ( M. caligata ), and in the case of the latter the data are highly suggestive of a second, cryptic species in the Cascade Mountains of Washington. Funding provided by: Alaska Department of Fish and Game Crossref Funder Registry ID: http://dx.doi.org/10.13039/100008144 Award Number: Funding provided by: University of Alaska Fairbanks Crossref Funder Registry ID: http://dx.doi.org/10.13039/100012574 Award Number: Funding provided by: Society of Systematic Biologists Crossref Funder Registry ID: http://dx.doi.org/10.13039/100006069 Award ... Other/Unknown Material Bering Land Bridge Alaska Beringia Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic Marmota
ultraconserved elements
spellingShingle Marmota
ultraconserved elements
Mills, Kendall
Data from: Ultraconserved elements improve resolution of marmot phylogeny and offer insights into biogeographic history
topic_facet Marmota
ultraconserved elements
description Marmots ( Marmota spp.) comprise a lineage of large-bodied ground squirrels that diversified rapidly in the Pleistocene, when the planet quickly transitioned to a drier, colder, and highly seasonal climate—particularly at high latitudes. Fossil evidence indicates the genus spread from North America, across Beringia, and into the European Alps over the course of only a few million years, beginning in the late Pliocene. Marmots are highly adapted to survive long and severely cold winters, and this likely favored their expansion and diversification over this time period. Previous phylogenetic studies have identified two major subgenera of marmots, but the timing of important speciation events and some species relationships have been difficult to resolve. Here we use ultraconserved elements and mitogenomes, with samples from all 15 extant species, to more precisely retrace how and when marmots came to inhabit a vast Holarctic range. Our results indicate marmots arose in North America in the mid Miocene (~16.3 Mya) and dispersed across the Bering Land Bridge in the late Pliocene (~3-4 Mya); in addition, our fossil-calibrated timeline is suggestive of the rise and spread of open grasslands as being particularly important to marmot diversification. The woodchuck ( M. monax ) and the Alaska marmot ( M. broweri ) are found to be more closely related to the Eurasian species than to the other North American species. Paraphyly is evident in the bobak marmot ( M. bobak ) and the hoary marmot ( M. caligata ), and in the case of the latter the data are highly suggestive of a second, cryptic species in the Cascade Mountains of Washington. Funding provided by: Alaska Department of Fish and Game Crossref Funder Registry ID: http://dx.doi.org/10.13039/100008144 Award Number: Funding provided by: University of Alaska Fairbanks Crossref Funder Registry ID: http://dx.doi.org/10.13039/100012574 Award Number: Funding provided by: Society of Systematic Biologists Crossref Funder Registry ID: http://dx.doi.org/10.13039/100006069 Award ...
format Other/Unknown Material
author Mills, Kendall
author_facet Mills, Kendall
author_sort Mills, Kendall
title Data from: Ultraconserved elements improve resolution of marmot phylogeny and offer insights into biogeographic history
title_short Data from: Ultraconserved elements improve resolution of marmot phylogeny and offer insights into biogeographic history
title_full Data from: Ultraconserved elements improve resolution of marmot phylogeny and offer insights into biogeographic history
title_fullStr Data from: Ultraconserved elements improve resolution of marmot phylogeny and offer insights into biogeographic history
title_full_unstemmed Data from: Ultraconserved elements improve resolution of marmot phylogeny and offer insights into biogeographic history
title_sort data from: ultraconserved elements improve resolution of marmot phylogeny and offer insights into biogeographic history
publisher Zenodo
publishDate 2023
url https://doi.org/10.5061/dryad.6hdr7sr56
genre Bering Land Bridge
Alaska
Beringia
genre_facet Bering Land Bridge
Alaska
Beringia
op_relation https://zenodo.org/communities/dryad
https://doi.org/10.5061/dryad.6hdr7sr56
oai:zenodo.org:7759923
op_rights info:eu-repo/semantics/openAccess
Creative Commons Zero v1.0 Universal
https://creativecommons.org/publicdomain/zero/1.0/legalcode
op_doi https://doi.org/10.5061/dryad.6hdr7sr56
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