New anuran material from Deseadan beds of Scarritt Pocket, Chubut Province, and the supposed presence of palearctic bufonids in the Oligocene of Patagonia
In 1949 Schaeffer described several anuran taxa based on remains from Deseadan beds of the western part of the meseta Canquel in central Patagonia. Among those taxa is the extinct neobatrachian Neoprocoela edentata Schaeffer, the evolutionary relationships of which are still controversial. It was su...
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| Lenguaje: | Español |
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1999
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| LEADER | 13505caa a22011057a 4500 | ||
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| 001 | PAPER-19649 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205100.0 | ||
| 008 | 190411s1999 xx ||||fo|||| 00| 0 spa|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-0032748187 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Báez, A.M. | |
| 245 | 1 | 0 | |a New anuran material from Deseadan beds of Scarritt Pocket, Chubut Province, and the supposed presence of palearctic bufonids in the Oligocene of Patagonia |
| 246 | 3 | 1 | |a Nuevo material de anuros en estratos deseadenses de Scarritt Pocket, provincia del Chubut, y la supuesta presencia de bufonidos palearticos en el Oligoceno de Patagonia |
| 260 | |c 1999 | ||
| 270 | 1 | 0 | |m Baez, A.M.; Departamento de Ciencias Geologicas, Fac. de Cienc. Exactas y Naturales, Universidad de Buenos Aires, Pabellon II, Ciudad Universitaria, 1428 Buenos Aires, Argentina |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a In 1949 Schaeffer described several anuran taxa based on remains from Deseadan beds of the western part of the meseta Canquel in central Patagonia. Among those taxa is the extinct neobatrachian Neoprocoela edentata Schaeffer, the evolutionary relationships of which are still controversial. It was suggested that this species is related to the Bufo calamita Laurenti species group, which has a Palearctic distribution at present. Subsequently, it was claimed that additional material collected from the same beds and locality confirmed the presence of the B. calamita group in Patagonia. The specimen on which this latter statement apparently was based was prepared and is described herein. Comparisons of the preserved elements neither support referral to Neoprocoela, nor their bufonid affinities; instead, the squamosals, vertebral column, humeri, and ilia resemble those of telmatobine 'leptodactylids'. |l eng | |
| 593 | |a CONICET, Depto. de Ciencias Geológicas, Universidad de Buenos Aires, 1428 Buenos Aires, Argentina | ||
| 593 | |a División Herpetología, Museo Argentino de Cie. Naturales, Avenida Angel Gallardo 470, 1405 Buenos Aires, Argentina | ||
| 690 | 1 | 0 | |a AMPHIBIA |
| 690 | 1 | 0 | |a ANURA |
| 690 | 1 | 0 | |a BUFO CALAMITA GROUP |
| 690 | 1 | 0 | |a DESEADAN |
| 690 | 1 | 0 | |a NEOPROCOELA |
| 690 | 1 | 0 | |a OLIGOCENE |
| 690 | 1 | 0 | |a PATAGONIA |
| 690 | 1 | 0 | |a TELMATOBINES |
| 690 | 1 | 0 | |a OLIGOCENE |
| 690 | 1 | 0 | |a AMPHIBIA |
| 690 | 1 | 0 | |a NEOPROCOELA |
| 651 | 4 | |a SOUTH AMERICA | |
| 700 | 1 | |a Fernicola, J.C. | |
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