Diversity of pseudo-toothed birds (Pelagornithidae) from the Eocene of Antarctica

The Antarctic pelagornithid record is restricted to few isolated remains from the Eocene of Seymour Island in the Antarctic Peninsula. Here we report the oldest Antarctic pseudo-toothed bird. It is represented by an incomplete humerus lacking its proximal end, which comes from the lower Eocene level...

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Published in:Journal of Paleontology
Main Authors: Marcos Cenizo, Carolina Acosta Hospitaleche, Marcelo Reguero
Format: Text
Language:English
Published: The Paleontological Society 2015
Subjects:
Online Access:https://doi.org/10.1017/jpa.2015.48
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spelling ftbioone:10.1017/jpa.2015.48 2024-06-02T07:58:03+00:00 Diversity of pseudo-toothed birds (Pelagornithidae) from the Eocene of Antarctica Marcos Cenizo Carolina Acosta Hospitaleche Marcelo Reguero Marcos Cenizo Carolina Acosta Hospitaleche Marcelo Reguero world 2015-09-01 text/HTML https://doi.org/10.1017/jpa.2015.48 en eng The Paleontological Society doi:10.1017/jpa.2015.48 All rights reserved. https://doi.org/10.1017/jpa.2015.48 Text 2015 ftbioone https://doi.org/10.1017/jpa.2015.48 2024-05-07T00:47:45Z The Antarctic pelagornithid record is restricted to few isolated remains from the Eocene of Seymour Island in the Antarctic Peninsula. Here we report the oldest Antarctic pseudo-toothed bird. It is represented by an incomplete humerus lacking its proximal end, which comes from the lower Eocene levels of the La Meseta Formation (Seymour Island). This new specimen facilitates a review of all known pelagornithids from this continent. Antarctic pelagornithids were classified into two morphotypes that exhibit a mix of putative plesiomorphic and derived characters. Considering the worldwide pelagornithid record and according to estimated wingspans, four approximate size-types were identified. The oldest Antarctic specimens (two fragmentary humeri, middle Ypresian) were assigned to morphotype 1 and correspond to the large size-type. The younger materials (Bartonian/?Priabonian) here assigned to morphotype 2 (some cranial remains, fragmentary tarsometatarsus and humerus) correspond to the giant size-type and represent one of the largest known pseudo-toothed birds. Even though species level phylogenetic affinities of Pelagornithidae remain poorly resolved, three key evolutionary events can be recognized: (1) the disappearance of Dasornis in the Early Eocene and the appearance of more advanced forms with a trend to the specialization of large soaring capacity, (2) the origin of Pelagornis sensu lato species in the early Oligocene, and (3) the appearance and dominance of a highly specialized terminal group at Mio/Pliocene time span. Text Antarc* Antarctic Antarctic Peninsula Antarctica Seymour Island BioOne Online Journals Antarctic Antarctic Peninsula Seymour ENVELOPE(-56.767,-56.767,-64.283,-64.283) Seymour Island ENVELOPE(-56.750,-56.750,-64.283,-64.283) The Antarctic Journal of Paleontology 89 5 870 881
institution Open Polar
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language English
description The Antarctic pelagornithid record is restricted to few isolated remains from the Eocene of Seymour Island in the Antarctic Peninsula. Here we report the oldest Antarctic pseudo-toothed bird. It is represented by an incomplete humerus lacking its proximal end, which comes from the lower Eocene levels of the La Meseta Formation (Seymour Island). This new specimen facilitates a review of all known pelagornithids from this continent. Antarctic pelagornithids were classified into two morphotypes that exhibit a mix of putative plesiomorphic and derived characters. Considering the worldwide pelagornithid record and according to estimated wingspans, four approximate size-types were identified. The oldest Antarctic specimens (two fragmentary humeri, middle Ypresian) were assigned to morphotype 1 and correspond to the large size-type. The younger materials (Bartonian/?Priabonian) here assigned to morphotype 2 (some cranial remains, fragmentary tarsometatarsus and humerus) correspond to the giant size-type and represent one of the largest known pseudo-toothed birds. Even though species level phylogenetic affinities of Pelagornithidae remain poorly resolved, three key evolutionary events can be recognized: (1) the disappearance of Dasornis in the Early Eocene and the appearance of more advanced forms with a trend to the specialization of large soaring capacity, (2) the origin of Pelagornis sensu lato species in the early Oligocene, and (3) the appearance and dominance of a highly specialized terminal group at Mio/Pliocene time span.
author2 Marcos Cenizo
Carolina Acosta Hospitaleche
Marcelo Reguero
format Text
author Marcos Cenizo
Carolina Acosta Hospitaleche
Marcelo Reguero
spellingShingle Marcos Cenizo
Carolina Acosta Hospitaleche
Marcelo Reguero
Diversity of pseudo-toothed birds (Pelagornithidae) from the Eocene of Antarctica
author_facet Marcos Cenizo
Carolina Acosta Hospitaleche
Marcelo Reguero
author_sort Marcos Cenizo
title Diversity of pseudo-toothed birds (Pelagornithidae) from the Eocene of Antarctica
title_short Diversity of pseudo-toothed birds (Pelagornithidae) from the Eocene of Antarctica
title_full Diversity of pseudo-toothed birds (Pelagornithidae) from the Eocene of Antarctica
title_fullStr Diversity of pseudo-toothed birds (Pelagornithidae) from the Eocene of Antarctica
title_full_unstemmed Diversity of pseudo-toothed birds (Pelagornithidae) from the Eocene of Antarctica
title_sort diversity of pseudo-toothed birds (pelagornithidae) from the eocene of antarctica
publisher The Paleontological Society
publishDate 2015
url https://doi.org/10.1017/jpa.2015.48
op_coverage world
long_lat ENVELOPE(-56.767,-56.767,-64.283,-64.283)
ENVELOPE(-56.750,-56.750,-64.283,-64.283)
geographic Antarctic
Antarctic Peninsula
Seymour
Seymour Island
The Antarctic
geographic_facet Antarctic
Antarctic Peninsula
Seymour
Seymour Island
The Antarctic
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Seymour Island
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Seymour Island
op_source https://doi.org/10.1017/jpa.2015.48
op_relation doi:10.1017/jpa.2015.48
op_rights All rights reserved.
op_doi https://doi.org/10.1017/jpa.2015.48
container_title Journal of Paleontology
container_volume 89
container_issue 5
container_start_page 870
op_container_end_page 881
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