Short Note: An intriguing penguin bone from the Late Eocene of Seymour Island, Antarctic Peninsula

Penguins (Aves: Sphenisciformes) are interesting to both neontologists and palaeontologists (e.g. Davis & Renner 2003). The fossil record of these extremely specialized inhabitants of the Southern Hemisphere extends back to the Palaeocene epoch (Slack et al. 2006). Extinct penguins are known fro...

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Published in:Antarctic Science
Main Author: Jadwiszczak, Piotr
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2008
Subjects:
Online Access:http://dx.doi.org/10.1017/s0954102008001405
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102008001405
id crcambridgeupr:10.1017/s0954102008001405
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spelling crcambridgeupr:10.1017/s0954102008001405 2024-09-09T19:08:25+00:00 Short Note: An intriguing penguin bone from the Late Eocene of Seymour Island, Antarctic Peninsula Jadwiszczak, Piotr 2008 http://dx.doi.org/10.1017/s0954102008001405 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102008001405 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Antarctic Science volume 20, issue 6, page 589-590 ISSN 0954-1020 1365-2079 journal-article 2008 crcambridgeupr https://doi.org/10.1017/s0954102008001405 2024-06-19T04:04:46Z Penguins (Aves: Sphenisciformes) are interesting to both neontologists and palaeontologists (e.g. Davis & Renner 2003). The fossil record of these extremely specialized inhabitants of the Southern Hemisphere extends back to the Palaeocene epoch (Slack et al. 2006). Extinct penguins are known from localities within the range of their modern-day relatives (Fordyce & Jones 1990), and the oldest diverse assemblage comes from the Eocene La Meseta Formation of Seymour Island, Antarctic Peninsula, the only such locality south of the Antarctic Convergence (Myrcha et al. 2002, Jadwiszczak 2006a). Several collections amounting to over three thousand bones (mainly isolated skeletal elements) have been acquired since 1901 from that formation, and 15 penguin species have been erected so far (Jadwiszczak 2006a, table 1, Tambussi et al. 2006). Only ten of them (grouped into six genera) appear to be taxonomically distinct, and their type specimens are tarsometatarsi (Simpson 1971, Myrcha et al. 2002, Jadwiszczak 2006a, 2006b, p. 296). Individuals from six species belonging to four genera most probably were not larger than those of Aptenodytes forsteri G.R. Gray, 1844, the heaviest and tallest extant penguin (Jadwiszczak 2001, table 3). Interestingly, representatives of all ten species may have co-existed in the West Antarctic during the Late Eocene epoch, just prior to the final break-up of Gondwana (Jadwiszczak 2006a). Presented here is an intriguing partial tarsometatarsus of a small-sized penguin from the Late Eocene of Antarctic Peninsula, probably representing a new genus and species. Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctic Science Aptenodytes forsteri Seymour Island Cambridge University Press 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 Antarctic Science 20 6 589 590
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Penguins (Aves: Sphenisciformes) are interesting to both neontologists and palaeontologists (e.g. Davis & Renner 2003). The fossil record of these extremely specialized inhabitants of the Southern Hemisphere extends back to the Palaeocene epoch (Slack et al. 2006). Extinct penguins are known from localities within the range of their modern-day relatives (Fordyce & Jones 1990), and the oldest diverse assemblage comes from the Eocene La Meseta Formation of Seymour Island, Antarctic Peninsula, the only such locality south of the Antarctic Convergence (Myrcha et al. 2002, Jadwiszczak 2006a). Several collections amounting to over three thousand bones (mainly isolated skeletal elements) have been acquired since 1901 from that formation, and 15 penguin species have been erected so far (Jadwiszczak 2006a, table 1, Tambussi et al. 2006). Only ten of them (grouped into six genera) appear to be taxonomically distinct, and their type specimens are tarsometatarsi (Simpson 1971, Myrcha et al. 2002, Jadwiszczak 2006a, 2006b, p. 296). Individuals from six species belonging to four genera most probably were not larger than those of Aptenodytes forsteri G.R. Gray, 1844, the heaviest and tallest extant penguin (Jadwiszczak 2001, table 3). Interestingly, representatives of all ten species may have co-existed in the West Antarctic during the Late Eocene epoch, just prior to the final break-up of Gondwana (Jadwiszczak 2006a). Presented here is an intriguing partial tarsometatarsus of a small-sized penguin from the Late Eocene of Antarctic Peninsula, probably representing a new genus and species.
format Article in Journal/Newspaper
author Jadwiszczak, Piotr
spellingShingle Jadwiszczak, Piotr
Short Note: An intriguing penguin bone from the Late Eocene of Seymour Island, Antarctic Peninsula
author_facet Jadwiszczak, Piotr
author_sort Jadwiszczak, Piotr
title Short Note: An intriguing penguin bone from the Late Eocene of Seymour Island, Antarctic Peninsula
title_short Short Note: An intriguing penguin bone from the Late Eocene of Seymour Island, Antarctic Peninsula
title_full Short Note: An intriguing penguin bone from the Late Eocene of Seymour Island, Antarctic Peninsula
title_fullStr Short Note: An intriguing penguin bone from the Late Eocene of Seymour Island, Antarctic Peninsula
title_full_unstemmed Short Note: An intriguing penguin bone from the Late Eocene of Seymour Island, Antarctic Peninsula
title_sort short note: an intriguing penguin bone from the late eocene of seymour island, antarctic peninsula
publisher Cambridge University Press (CUP)
publishDate 2008
url http://dx.doi.org/10.1017/s0954102008001405
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102008001405
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
Antarctic Science
Aptenodytes forsteri
Seymour Island
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctic Science
Aptenodytes forsteri
Seymour Island
op_source Antarctic Science
volume 20, issue 6, page 589-590
ISSN 0954-1020 1365-2079
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0954102008001405
container_title Antarctic Science
container_volume 20
container_issue 6
container_start_page 589
op_container_end_page 590
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