Pre-Gondwanan-breakup origin of Beauprea (Proteaceae) explains its historical presence in New Caledonia and New Zealand

New Caledonia and New Zealand belong to the now largely submerged continent Zealandia. Their high levels of endemism and species richness are usually considered the result of transoceanic dispersal events followed by diversification after they re-emerged from the Pacific Ocean in the mid-Cenozoic. W...

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Published in:Science Advances
Main Authors: He, Tianhua, Lamont, Byron, Fogliani, B.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2016
Subjects:
Online Access:https://hdl.handle.net/20.500.11937/8690
https://doi.org/10.1126/sciadv.1501648
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spelling ftcurtin:oai:espace.curtin.edu.au:20.500.11937/8690 2023-06-11T04:06:46+02:00 Pre-Gondwanan-breakup origin of Beauprea (Proteaceae) explains its historical presence in New Caledonia and New Zealand He, Tianhua Lamont, Byron Fogliani, B. 2016 fulltext https://hdl.handle.net/20.500.11937/8690 https://doi.org/10.1126/sciadv.1501648 unknown http://hdl.handle.net/20.500.11937/8690 doi:10.1126/sciadv.1501648 Journal Article 2016 ftcurtin https://doi.org/20.500.11937/869010.1126/sciadv.1501648 2023-05-30T19:24:24Z New Caledonia and New Zealand belong to the now largely submerged continent Zealandia. Their high levels of endemism and species richness are usually considered the result of transoceanic dispersal events followed by diversification after they re-emerged from the Pacific Ocean in the mid-Cenozoic. We explore the origin and evolutionary history of Beauprea (Proteaceae), which is now endemic to New Caledonia but was once spread throughout eastern Gondwana, including New Zealand. We review the extensive Beauprea-type pollen data in the fossil records and analyze the relationship of these fossil taxa to extant genera within Proteaceae. We further reconstruct the phylogenetic relations among nine extant species of Beauprea and estimate the age of the Beauprea clade. By incorporating extinct taxa into the Beauprea phylogenetic tree, we reconstruct the ancient distribution of this genus. Our analysis shows that Beauprea originated c. 88 Ma (million years ago) in Antarctica-Southeastern Australia and spread throughout Gondwana before its complete breakup. We propose that Beauprea, already existing as two lineages, was carried with Zealandia when it separated from the rest of Gondwana c. 82 Ma, thus supporting an autochthonous origin for Beauprea species now in New Caledonia and historically in New Zealand up to 1 Ma. We show that the presence of Beauprea through transoceanic dispersal is implausible. This means that neither New Caledonia nor New Zealand has been entirely submerged since the Upper Cretaceous; thus, possible vicariance and allopatry must be taken into account when considering the high levels of endemism and species richness of these island groups. Article in Journal/Newspaper Antarc* Antarctica Curtin University: espace New Zealand Pacific Science Advances 2 4 e1501648
institution Open Polar
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language unknown
description New Caledonia and New Zealand belong to the now largely submerged continent Zealandia. Their high levels of endemism and species richness are usually considered the result of transoceanic dispersal events followed by diversification after they re-emerged from the Pacific Ocean in the mid-Cenozoic. We explore the origin and evolutionary history of Beauprea (Proteaceae), which is now endemic to New Caledonia but was once spread throughout eastern Gondwana, including New Zealand. We review the extensive Beauprea-type pollen data in the fossil records and analyze the relationship of these fossil taxa to extant genera within Proteaceae. We further reconstruct the phylogenetic relations among nine extant species of Beauprea and estimate the age of the Beauprea clade. By incorporating extinct taxa into the Beauprea phylogenetic tree, we reconstruct the ancient distribution of this genus. Our analysis shows that Beauprea originated c. 88 Ma (million years ago) in Antarctica-Southeastern Australia and spread throughout Gondwana before its complete breakup. We propose that Beauprea, already existing as two lineages, was carried with Zealandia when it separated from the rest of Gondwana c. 82 Ma, thus supporting an autochthonous origin for Beauprea species now in New Caledonia and historically in New Zealand up to 1 Ma. We show that the presence of Beauprea through transoceanic dispersal is implausible. This means that neither New Caledonia nor New Zealand has been entirely submerged since the Upper Cretaceous; thus, possible vicariance and allopatry must be taken into account when considering the high levels of endemism and species richness of these island groups.
format Article in Journal/Newspaper
author He, Tianhua
Lamont, Byron
Fogliani, B.
spellingShingle He, Tianhua
Lamont, Byron
Fogliani, B.
Pre-Gondwanan-breakup origin of Beauprea (Proteaceae) explains its historical presence in New Caledonia and New Zealand
author_facet He, Tianhua
Lamont, Byron
Fogliani, B.
author_sort He, Tianhua
title Pre-Gondwanan-breakup origin of Beauprea (Proteaceae) explains its historical presence in New Caledonia and New Zealand
title_short Pre-Gondwanan-breakup origin of Beauprea (Proteaceae) explains its historical presence in New Caledonia and New Zealand
title_full Pre-Gondwanan-breakup origin of Beauprea (Proteaceae) explains its historical presence in New Caledonia and New Zealand
title_fullStr Pre-Gondwanan-breakup origin of Beauprea (Proteaceae) explains its historical presence in New Caledonia and New Zealand
title_full_unstemmed Pre-Gondwanan-breakup origin of Beauprea (Proteaceae) explains its historical presence in New Caledonia and New Zealand
title_sort pre-gondwanan-breakup origin of beauprea (proteaceae) explains its historical presence in new caledonia and new zealand
publishDate 2016
url https://hdl.handle.net/20.500.11937/8690
https://doi.org/10.1126/sciadv.1501648
geographic New Zealand
Pacific
geographic_facet New Zealand
Pacific
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation http://hdl.handle.net/20.500.11937/8690
doi:10.1126/sciadv.1501648
op_doi https://doi.org/20.500.11937/869010.1126/sciadv.1501648
container_title Science Advances
container_volume 2
container_issue 4
container_start_page e1501648
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