Fig. 21 in The Basal Penguin (Aves: Sphenisciformes) Perudyptes Devriesi And A Phylogenetic Evaluation Of The Penguin Fossil Record

Fig. 21. Phylogeny of Sphenisciformes calibrated to the stratigraphic record. Ghost lineages (Norell, 1992) are minimized. Dotted lines extending the range of clade 7 are based on identification of fragmentary fossils of late Eocene age to this clade. We utilize age ranges for Spheniscus urbinai and...

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Main Authors: Ksepka, Daniel T., Clarke, Julia A.
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2010
Subjects:
Online Access:https://doi.org/10.5281/zenodo.10112125
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spelling ftzenodo:oai:zenodo.org:10112125 2024-09-15T17:43:45+00:00 Fig. 21 in The Basal Penguin (Aves: Sphenisciformes) Perudyptes Devriesi And A Phylogenetic Evaluation Of The Penguin Fossil Record Ksepka, Daniel T. Clarke, Julia A. 2010-06-03 https://doi.org/10.5281/zenodo.10112125 unknown Zenodo https://doi.org/10.1206/653.1 lsid:urn:lsid:plazi.org:pub:F20CFF92FF97FFB67C01FFFDFF9E4C31 https://zenodo.org/record/10112083 https://zenodo.org/communities/biosyslit https://doi.org/10.5281/zenodo.10112124 https://doi.org/10.5281/zenodo.10112125 oai:zenodo.org:10112125 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Bulletin of the American Museum of Natural History, 2010(337), 1-77, (2010-06-03) Biodiversity Taxonomy info:eu-repo/semantics/other 2010 ftzenodo https://doi.org/10.5281/zenodo.1011212510.1206/653.110.5281/zenodo.10112124 2024-07-27T06:28:49Z Fig. 21. Phylogeny of Sphenisciformes calibrated to the stratigraphic record. Ghost lineages (Norell, 1992) are minimized. Dotted lines extending the range of clade 7 are based on identification of fragmentary fossils of late Eocene age to this clade. We utilize age ranges for Spheniscus urbinai and Spheniscus megaramphus provided by Stucchi (2007). Most penguins from the La Meseta Formation occur in Telm 7 (34.2–36.1 Ma), but a few species have been reported from lower units (see Myrcha et al., 2002; Jadwiszczak, 2006a), accounting for the extended ranges of Delphinornis larseni, Anthropornis grandis, and Palaeeudyptes gunnari. A specimen from the Chilcatay Formation (see fig. 1) referred to Palaeospheniscus sp. by Acosta Hospitaleche and Stucchi (2005) is provisionally referred to Palaeospheniscus patagonicus (Ksepka, 2007), accounting for the longer range of this taxon. For taxa that are poorly constrained in age, the midpoint of possible ages is used (e.g., Marplesornis is placed at the late Miocene). Geographical locality for fossil taxa and breeding range of extant taxa are provided in parentheses following taxa names. Asterisks indicate taxa with extensive breeding ranges including oceanic islands (see Bertelli and Giannini [2005] for more data on these species). Abbreviations: AF, Africa; AN, Antarctica; AU, Australia; NZ, New Zealand and surrounding islands; SA, South America. Published as part of Ksepka, Daniel T. & Clarke, Julia A., 2010, The Basal Penguin (Aves: Sphenisciformes) Perudyptes Devriesi And A Phylogenetic Evaluation Of The Penguin Fossil Record, pp. 1-77 in Bulletin of the American Museum of Natural History 2010 (337) on page 40, DOI:10.1206/653.1, http://zenodo.org/record/10112083 Other/Unknown Material Antarc* Antarctica Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic Biodiversity
Taxonomy
spellingShingle Biodiversity
Taxonomy
Ksepka, Daniel T.
Clarke, Julia A.
Fig. 21 in The Basal Penguin (Aves: Sphenisciformes) Perudyptes Devriesi And A Phylogenetic Evaluation Of The Penguin Fossil Record
topic_facet Biodiversity
Taxonomy
description Fig. 21. Phylogeny of Sphenisciformes calibrated to the stratigraphic record. Ghost lineages (Norell, 1992) are minimized. Dotted lines extending the range of clade 7 are based on identification of fragmentary fossils of late Eocene age to this clade. We utilize age ranges for Spheniscus urbinai and Spheniscus megaramphus provided by Stucchi (2007). Most penguins from the La Meseta Formation occur in Telm 7 (34.2–36.1 Ma), but a few species have been reported from lower units (see Myrcha et al., 2002; Jadwiszczak, 2006a), accounting for the extended ranges of Delphinornis larseni, Anthropornis grandis, and Palaeeudyptes gunnari. A specimen from the Chilcatay Formation (see fig. 1) referred to Palaeospheniscus sp. by Acosta Hospitaleche and Stucchi (2005) is provisionally referred to Palaeospheniscus patagonicus (Ksepka, 2007), accounting for the longer range of this taxon. For taxa that are poorly constrained in age, the midpoint of possible ages is used (e.g., Marplesornis is placed at the late Miocene). Geographical locality for fossil taxa and breeding range of extant taxa are provided in parentheses following taxa names. Asterisks indicate taxa with extensive breeding ranges including oceanic islands (see Bertelli and Giannini [2005] for more data on these species). Abbreviations: AF, Africa; AN, Antarctica; AU, Australia; NZ, New Zealand and surrounding islands; SA, South America. Published as part of Ksepka, Daniel T. & Clarke, Julia A., 2010, The Basal Penguin (Aves: Sphenisciformes) Perudyptes Devriesi And A Phylogenetic Evaluation Of The Penguin Fossil Record, pp. 1-77 in Bulletin of the American Museum of Natural History 2010 (337) on page 40, DOI:10.1206/653.1, http://zenodo.org/record/10112083
format Other/Unknown Material
author Ksepka, Daniel T.
Clarke, Julia A.
author_facet Ksepka, Daniel T.
Clarke, Julia A.
author_sort Ksepka, Daniel T.
title Fig. 21 in The Basal Penguin (Aves: Sphenisciformes) Perudyptes Devriesi And A Phylogenetic Evaluation Of The Penguin Fossil Record
title_short Fig. 21 in The Basal Penguin (Aves: Sphenisciformes) Perudyptes Devriesi And A Phylogenetic Evaluation Of The Penguin Fossil Record
title_full Fig. 21 in The Basal Penguin (Aves: Sphenisciformes) Perudyptes Devriesi And A Phylogenetic Evaluation Of The Penguin Fossil Record
title_fullStr Fig. 21 in The Basal Penguin (Aves: Sphenisciformes) Perudyptes Devriesi And A Phylogenetic Evaluation Of The Penguin Fossil Record
title_full_unstemmed Fig. 21 in The Basal Penguin (Aves: Sphenisciformes) Perudyptes Devriesi And A Phylogenetic Evaluation Of The Penguin Fossil Record
title_sort fig. 21 in the basal penguin (aves: sphenisciformes) perudyptes devriesi and a phylogenetic evaluation of the penguin fossil record
publisher Zenodo
publishDate 2010
url https://doi.org/10.5281/zenodo.10112125
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Bulletin of the American Museum of Natural History, 2010(337), 1-77, (2010-06-03)
op_relation https://doi.org/10.1206/653.1
lsid:urn:lsid:plazi.org:pub:F20CFF92FF97FFB67C01FFFDFF9E4C31
https://zenodo.org/record/10112083
https://zenodo.org/communities/biosyslit
https://doi.org/10.5281/zenodo.10112124
https://doi.org/10.5281/zenodo.10112125
oai:zenodo.org:10112125
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.1011212510.1206/653.110.5281/zenodo.10112124
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