Palaeospheniscus patagonicus (Aves, Sphenisciformes): New discoveries from the early miocene of Argentina
The penguin skeleton studied here constitutes the fourth partial skeleton found in Patagonia, and the third one with an associated humerus and tarsometatarsus. The finding of this partial skeleton identified with certainty as Palaeospheniscus patagonicus Moreno and Mercerat, 1891 (Aves, Spheniscifor...
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2008
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| LEADER | 15130caa a22011417a 4500 | ||
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| 100 | 1 | |a Hospitaleche, C.A. | |
| 245 | 1 | 0 | |a Palaeospheniscus patagonicus (Aves, Sphenisciformes): New discoveries from the early miocene of Argentina |
| 260 | |c 2008 | ||
| 270 | 1 | 0 | |m Hospitaleche, C. A.; División Paleontología Vertebrados, Museo de La Plata, Paseo del Bosque s/nro, 1900 La Plata, Argentina; email: acostacaro@museo.fcnym.ulp.edu.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a ACOSTA HOSPITALECHE, C., Revisión sistemática de Palaeospheniscus biloculata (Simpson) nov. comb. (Aves, Spheniscidae) de la Formación Gaiman (Mioceno Temprano), Chubut, Argentina. (2007) Ameghiniana, 44, pp. 417-426 | ||
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| 504 | |a ACOSTA HOSPITALECHE, C., CANTO, J., TAMBUSSI, C., Pingüinos (Aves, Spheniscidae) en Coquimbo (Mioceno Medio-Plioceno Tardío), Chile y su vinculación con las corrientes oceánicas. (2006) Revista Española de Paleontología, 21, pp. 115-121 | ||
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| 504 | |a ACOSTA HOSPITALECHE, C., TAMBUSSI, C., DONATO, M., COZZUOL, M., A new miocene penguin from Patagonia and a phylogenetic analysis of living and fossil species (2007) Acta Paleontologica Polonica, 52, pp. 299-314 | ||
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| 504 | |a CAMPBELL, E., JR. AND L. MARCUS. 1988. The relationship of hindlimb bone dimensions to body weight in birds, p. 395-412. In K. Campbell Jr. (ed.), Papers in Avian Paleontology, honoring Pierce Bordkorb. Natural History Museum of Los Angeles County Science Series No. 36, Los Angeles; FLYNN, J. J. AND C. C. SWISHER. 1995. Cenozoic South American Land Mammal Ages: Correlation to global geochronologies, p. 317-333. In W. A. Berggren, D. V Kent, and M. P. Aubry (eds.), Geochronology, Time Scales and Global Stratigraphic Correlation. Society of Economic Mineralogists and Geologists Special Publication, 54; GOLOBOFF, P.A., FARRIS, J.S., KÄ LLERSJÖ, M., OXELMAN, B., RAMÍREZ, M., SZUMIK, C.A., Improvements to resampling measures of group support (2003) Cladistics, 19, pp. 324-332 | ||
| 504 | |a JADWISZCZAK, P., Body size of Eocene Antarctic penguins (2001) Polish Polar Research, 22, pp. 147-158 | ||
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| 504 | |a KSEPKA, T., BERTELLI, S., GIANNINI, N.P., The phylogeny of the living and fossil Sphenisciformes (penguins) (2006) Cladistics, 22, pp. 412-441 | ||
| 504 | |a LEGARRETA, L., ULIANA, M.A., Asociaciones de fósiles y hiatos en el supracretácico- neógeno de Patagonia: Una perspectiva estratigráficosecuencial. (1994) Ameghiniana, 31, pp. 257-281 | ||
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| 504 | |a MALUMIAN, N. 1999. La sedimentación y el volcanismo terciario en la Patagonia extraandina. 1. La sedimentación en la Patagonia extraandina, p. 557-578. In R. Caminos (ed.), Geologia Argentina. Instituto de Geologia y Recursos Minerales, Buenos Aires; MARPLES, B.J., Early Tertiary penguins of New Zealand. Geological Survey (1952) Paleontological Bulletin, 20, pp. 1-66 | ||
| 504 | |a MARPLES, B.J., A fossil penguin from the Late Tertiary of North Canterbury (1960) Records of the Canterbury Museum, 7, pp. 185-195 | ||
| 504 | |a MARTILL, D.M., The preservation of marine vertebrates in the Lower Oxford Clay (Jurassic) of central England (1985) Extraordinary Fossil Biotas; Their Ecological and Evolutionary Significance. Philosophical Transactions of the Royal Society of London B, 311, pp. 155-165. , H. B. Whittington and S. Conway Morris eds | ||
| 504 | |a MAYR, G., Tertiary plotopterids (Aves, Plotopteridae) and a novel hypothesis on the phylogenetic relationships of penguins (Spheniscidae) (2004) Journal of Zoological Systematics and Evolutionary Research, 43, pp. 61-71 | ||
| 504 | |a MAYR, G., CLARKE, J.A., The deep divergences of neornithine birds: A phylogenetic analysis of morphological characters (2003) Cladistics, 19, pp. 527-553 | ||
| 504 | |a MENDÍA, J.E., BAYARSKY, A., Estratigrafía del Terciario en el Valle inferior del Río Chubut (1981) Abstracts VIII Congreso Geotogico, 3, pp. 593-606. , Argentino, San Luis | ||
| 504 | |a NIXON, K. C. 1999-2002. WinClada version 1.0000 Published by the author, Ithaca, New York, USA; O'HARA, R., (1989) Systematics and the study of natural history, with an estimate of the phylogeny of the living penguins (Aves: Spheniscidae), , Unpublished Ph.D. dissertation. Harvard University, 171 pp | ||
| 504 | |a PALAZZESI, L., BARREDA, V., Comunidades florísticas miocenas de Peninsula Valdés: Evidencias palinológicas. Abstracts Reunión anual de comunicaciones y Simposio del 50° aniversario de la Asociación Paleontologica Argentina; (2005) 1° Simposio de Paleontología y Geología de Península Valdés, 1, p. 21 | ||
| 504 | |a PALAZZESI, L., BARREDA, V., SCASSO, R.A., Early Miocene spore and pollen record of the Gaiman Formation (Northeastern Patagonia, Argentina): Correlations and paleoenvironment implications (2006) Abstracts 4° Congreso Latinoamericano de Sedimentología and 11° Reunión Argentina de Sedimentología, 1, p. 161. , San Carlos de Bariloche, Argentina | ||
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| 520 | 3 | |a The penguin skeleton studied here constitutes the fourth partial skeleton found in Patagonia, and the third one with an associated humerus and tarsometatarsus. The finding of this partial skeleton identified with certainty as Palaeospheniscus patagonicus Moreno and Mercerat, 1891 (Aves, Sphenisciformes) allows the first description of elements other than the tarsometatarsus. The material comes from the basal sector of the Gaiman Formation (Early Miocene), located along the Atlantic coast of Chubut Province, south of Rawson city. This unit comprises a succession of shales, fine tuffs, sandstones, tuffaceous sandstones, and coquinas deposited in a shallow marine environment. These beds contain abundant marine vertebrates (sharks, dolphins, rays, birds), mollusk casts, and oyster beds. The skeleton includes: rostrum, two thoracic vertebrae, right coracoid without the distal end, left humerus, right femur, right tarsometatarsus, left fragmentary scapula, left coracoid, left radius without the distal end, proximal portion of left ulna, proximal end of left femur, and preacetabular part of the synsacrum. P. patagonicus would have been a medium-sized penguin weighing about 5 kg that inhabited the breeding colonies established in the nearby Bryn Gwyn area during the early Miocene. Despite the abundance of penguin remains known for Argentina, and the fact that they are among the birds with a better fossil record, this skeleton is an exceptional case. This finding allows a readjustment of the taxonomic criteria applicable to fossil and living species. Copyright © 2008, The Paleontological Society. |l eng | |
| 593 | |a División Paleontología Vertebrados, Museo de La Plata, Paseo del Bosque s/nro, 1900 La Plata, Argentina | ||
| 593 | |a CONICET, Facultad de Ciencias Exactas Y Naturales de la Universidad de Buenos Aires, Ciudad Universitaria, 1428 Buenos Aires, Argentina | ||
| 593 | |a Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas Y Naturales de la Universidad de Buenos Aires, Ciudad Universitaria, Pab. 2, 1428 Buenos Aires, Argentina | ||
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| 700 | 1 | |a Scasso, R.A. | |
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