A New Pleistocene bird assemblage from the Southern Pampas (Buenos Aires, Argentina)
In the present paper we report the most complete fossil avifauna from the southern cone of South America. The specimens here described were collected in the Paso Otero locality, at the middle stream of the Quequén Grande River, Pampean Region (Buenos Aires Province, Argentina). The fossiliferous lev...
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2015
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| LEADER | 24442caa a22018977a 4500 | ||
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| 001 | PAPER-13548 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518204355.0 | ||
| 008 | 170725s2015 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84919935352 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 030 | |a PPPYA | ||
| 100 | 1 | |a Cenizo, M.M. | |
| 245 | 1 | 2 | |a A New Pleistocene bird assemblage from the Southern Pampas (Buenos Aires, Argentina) |
| 260 | |b Elsevier |c 2015 | ||
| 270 | 1 | 0 | |m Cenizo, M.M.; Facultad de Ciencias Exactas y Naturales, Universidad Nacional de La Pampa, Uruguay 151, Argentina |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a In the present paper we report the most complete fossil avifauna from the southern cone of South America. The specimens here described were collected in the Paso Otero locality, at the middle stream of the Quequén Grande River, Pampean Region (Buenos Aires Province, Argentina). The fossiliferous levels belong to the La Chumbiada Member of Luján Formation (37,800 ± 2300. yr BP, late Pleistocene). The assemblage is represented by 60 specimens belonging to at least 22 taxa. The radiocarbon age indicates that Paso Otero birds represent the oldest late Pleistocene avifauna known from the South American continent and the first coming from a clear interstadial event (MIS3). Available evidence indicates similar environmental conditions during the MIS3 interstadial in the Pampean Region of Argentina and the post-Last Glacial Maximum stadials in southeastern Brazil. The absence of significant extinction events in the latest Pleistocene-early Holocene avifaunas of Brazil and Argentina suggests that the main avifaunal composition along southeastern continental lowlands may not be affected by the cyclic retraction and extension of open environments. On the contrary, the fossil record of Peru and Ecuador demonstrates that a large number of taxa, including aquatic and predatory-scavenger birds, have gone extinct along Andean environments at the Pacific coast, and late Pleistocene climatic oscillations may have played a more dramatic impact in these avian communities. © 2014 Elsevier B.V. |l eng | |
| 593 | |a Facultad de Ciencias Exactas y Naturales, Universidad Nacional de La Pampa, Uruguay 151, Santa Rosa, La Pampa, Argentina | ||
| 593 | |a Fundación de Historia Natural Félix de Azara, Departamento de Ciencias Naturales y Antropología, CEBBAD, Universidad Maimónides, Hidalgo 775, Ciudad Autónoma de Buenos Aires, Argentina | ||
| 593 | |a Laboratorio de Anatomía Comparada y Evolución de los Vertebrados, Museo Argentino de Ciencias Naturales Bernardino Rivadavia, Av. Angel Gallardo, 470, Buenos Aires, Argentina | ||
| 593 | |a Facultad de Ciencias Naturales y Museo, Universidad Nacional de La Plata, Calle 122 y 60, La Plata, Argentina | ||
| 690 | 1 | 0 | |a AVIFAUNAS |
| 690 | 1 | 0 | |a INTERSTADIAL |
| 690 | 1 | 0 | |a LUJAN FORMATION |
| 690 | 1 | 0 | |a MARINE ISOTOPE STAGE 3 |
| 690 | 1 | 0 | |a PALEOENVIRONMENTS |
| 690 | 1 | 0 | |a PAMPEAN REGION |
| 690 | 1 | 0 | |a CLIMATE OSCILLATION |
| 690 | 1 | 0 | |a COMMUNITY STRUCTURE |
| 690 | 1 | 0 | |a ENVIRONMENTAL CONDITIONS |
| 690 | 1 | 0 | |a EXTINCTION |
| 690 | 1 | 0 | |a FOSSIL RECORD |
| 690 | 1 | 0 | |a HOLOCENE |
| 690 | 1 | 0 | |a LAST GLACIAL MAXIMUM |
| 690 | 1 | 0 | |a PALEOENVIRONMENT |
| 690 | 1 | 0 | |a PLEISTOCENE |
| 690 | 1 | 0 | |a POSTGLACIAL |
| 690 | 1 | 0 | |a RADIOCARBON DATING |
| 690 | 1 | 0 | |a PAMPAS |
| 690 | 1 | 0 | |a QUEQUEN GRANDE BASIN |
| 650 | 1 | 7 | |2 spines |a BIRD |
| 650 | 1 | 7 | |2 spines |a AVES |
| 651 | 4 | |a ARGENTINA | |
| 651 | 4 | |a BUENOS AIRES [ARGENTINA] | |
| 700 | 1 | |a Agnolin, F.L. | |
| 700 | 1 | |a Pomi, L.H. | |
| 773 | 0 | |d Elsevier, 2015 |g v. 420 |h pp. 65-81 |x 00310182 |w (AR-BaUEN)CENRE-1607 |t Palaeogeogr. Palaeoclimatol. Palaeoecol. | |
| 856 | 4 | 1 | |u https://www.scopus.com/inward/record.uri?eid=2-s2.0-84919935352&doi=10.1016%2fj.palaeo.2014.12.009&partnerID=40&md5=a33fcffb4ed1a4bc25d79e6acb54af7b |y Registro en Scopus |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.palaeo.2014.12.009 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_00310182_v420_n_p65_Cenizo |y Handle |
| 856 | 4 | 0 | |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00310182_v420_n_p65_Cenizo |y Registro en la Biblioteca Digital |
| 961 | |a paper_00310182_v420_n_p65_Cenizo |b paper |c PE | ||
| 962 | |a info:eu-repo/semantics/article |a info:ar-repo/semantics/artículo |b info:eu-repo/semantics/publishedVersion | ||
| 963 | |a VARI | ||
| 999 | |c 74501 | ||