The evolutionary history of the extinct ratite moa and New Zealand Neogene paleogeography

The ratite moa (Aves: Dinornithiformes) were a speciose group of massive graviportal avian herbivores that dominated the New Zealand (NZ) ecosystem until their extinction !600 years ago. Thephylogeny and evolutionary history of this morphologically diverse order has remained controversial since thei...

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Main Authors: Bunce, Michael, Worthy, T., Phillips, M., Holdaway, R., Willerslev, E., Haile, James, Shapiro, B., Scofield, R., Drummond, A., Kamp, P., Cooper, A.
Format: Journal Article
Published: National Academy of Sciences 2009
Subjects:
Online Access:http://www.pnas.org/content/106/49/20646
http://hdl.handle.net/20.500.11937/6212
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author Bunce, Michael
Worthy, T.
Phillips, M.
Holdaway, R.
Willerslev, E.
Haile, James
Shapiro, B.
Scofield, R.
Drummond, A.
Kamp, P.
Cooper, A.
author_facet Bunce, Michael
Worthy, T.
Phillips, M.
Holdaway, R.
Willerslev, E.
Haile, James
Shapiro, B.
Scofield, R.
Drummond, A.
Kamp, P.
Cooper, A.
author_sort Bunce, Michael
building Curtin Institutional Repository
collection Online Access
description The ratite moa (Aves: Dinornithiformes) were a speciose group of massive graviportal avian herbivores that dominated the New Zealand (NZ) ecosystem until their extinction !600 years ago. Thephylogeny and evolutionary history of this morphologically diverse order has remained controversial since their initial description in 1839. We synthesize mitochondrial phylogenetic information from 263subfossil moa specimens from across NZ with morphological, ecological, and new geological data to create the first comprehensive phylogeny, taxonomy, and evolutionary timeframe for all of thespecies of an extinct order. We also present an important new geological/paleogeographical model of late Cenozoic NZ, which suggests that terrestrial biota on the North and South Island landmasseswere isolated for most of the past 20–30 Ma. The data reveal that the patterns of genetic diversity within and between differentmoaclades reflect a complex history following a major marine transgression inthe Oligocene, affected by marine barriers, tectonic activity, and glacial cycles. Surprisingly, the remarkable morphological radiation of moa appears to have occurred much more recently than previousearly Miocene (ca. 15 Ma) estimates, and was coincident with the accelerated uplift of the Southern Alps just ca. 5–8.5 Ma. Together with recent fossil evidence, these data suggest that the recentevolutionary history of nearly all of the iconic NZ terrestrial biota occurred principally on just the South Island.
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spelling curtin-20.500.11937-62122017-02-28T01:30:06Z The evolutionary history of the extinct ratite moa and New Zealand Neogene paleogeography Bunce, Michael Worthy, T. Phillips, M. Holdaway, R. Willerslev, E. Haile, James Shapiro, B. Scofield, R. Drummond, A. Kamp, P. Cooper, A. Oligocene Drowning phylogeny taxonomy ancient DNA Dinornithiformes The ratite moa (Aves: Dinornithiformes) were a speciose group of massive graviportal avian herbivores that dominated the New Zealand (NZ) ecosystem until their extinction !600 years ago. Thephylogeny and evolutionary history of this morphologically diverse order has remained controversial since their initial description in 1839. We synthesize mitochondrial phylogenetic information from 263subfossil moa specimens from across NZ with morphological, ecological, and new geological data to create the first comprehensive phylogeny, taxonomy, and evolutionary timeframe for all of thespecies of an extinct order. We also present an important new geological/paleogeographical model of late Cenozoic NZ, which suggests that terrestrial biota on the North and South Island landmasseswere isolated for most of the past 20–30 Ma. The data reveal that the patterns of genetic diversity within and between differentmoaclades reflect a complex history following a major marine transgression inthe Oligocene, affected by marine barriers, tectonic activity, and glacial cycles. Surprisingly, the remarkable morphological radiation of moa appears to have occurred much more recently than previousearly Miocene (ca. 15 Ma) estimates, and was coincident with the accelerated uplift of the Southern Alps just ca. 5–8.5 Ma. Together with recent fossil evidence, these data suggest that the recentevolutionary history of nearly all of the iconic NZ terrestrial biota occurred principally on just the South Island. 2009 Journal Article http://hdl.handle.net/20.500.11937/6212 http://www.pnas.org/content/106/49/20646 National Academy of Sciences restricted
spellingShingle Oligocene Drowning
phylogeny
taxonomy
ancient DNA
Dinornithiformes
Bunce, Michael
Worthy, T.
Phillips, M.
Holdaway, R.
Willerslev, E.
Haile, James
Shapiro, B.
Scofield, R.
Drummond, A.
Kamp, P.
Cooper, A.
The evolutionary history of the extinct ratite moa and New Zealand Neogene paleogeography
title The evolutionary history of the extinct ratite moa and New Zealand Neogene paleogeography
title_full The evolutionary history of the extinct ratite moa and New Zealand Neogene paleogeography
title_fullStr The evolutionary history of the extinct ratite moa and New Zealand Neogene paleogeography
title_full_unstemmed The evolutionary history of the extinct ratite moa and New Zealand Neogene paleogeography
title_short The evolutionary history of the extinct ratite moa and New Zealand Neogene paleogeography
title_sort evolutionary history of the extinct ratite moa and new zealand neogene paleogeography
topic Oligocene Drowning
phylogeny
taxonomy
ancient DNA
Dinornithiformes
url http://www.pnas.org/content/106/49/20646
http://hdl.handle.net/20.500.11937/6212