NEW REMAINS OF MACRANHINGA PARANENSIS NORIEGA (AVES, PELECANIFORMES, ANHINGIDAE) FROM THE MIOCENE OF ENTRE RIOS PROVINCE, ARGENTINA

被引:9
|
作者
Marcelo Diederle, Juan [1 ]
Ignacio Noriega, Jorge [1 ]
Acosta Hospitaleche, Carolina [2 ]
机构
[1] Consejo Nacl Invest Cient & Tecn, CICYTTP, Lab Paleontol Vertebrados, RA-3105 Diamante, Entre Rios, Argentina
[2] Museo La Plata, Div Paleontol Vertebrados, RA-1900 La Plata, Buenos Aires, Argentina
来源
REVISTA BRASILEIRA DE PALEONTOLOGIA | 2012年 / 15卷 / 02期
关键词
Aves; Macranhinga paranensis; vertebrae; Miocene; Argentinian Mesopotamia; ITUZAINGO FORMATION; PLIOCENE-PLEISTOCENE; MIDDLE MIOCENE; FOSSIL WOODS; TOMA VIEJA; PARANA; BASIN; GEN;
D O I
10.4072/rbp.2012.2.08
中图分类号
Q91 [古生物学];
学科分类号
0709 ; 070903 ;
摘要
NEW REMAINS OF MACRANHINGA PARANENSIS NORIEGA (AVES, PELECANIFORMES, ANHINGIDAE) FROM THE MIOCENE OF ENTRE RIOS PROVINCE, ARGENTINA. Macranhinga paranensis Noriega, taxon described on the basis of tarsometatarsi, is known by dissociated remains of both girdles and limb bones coming from the "Conglomerado osifero" or "Mesopotamian" at Entre Rios Province, Argentina (= base of the Ituzaingo Formation; late Miocene). In this contribution we report the first record of four isolated cervical vertebrae which are assigned to M. paranensis, coming from the Parana Formation (middle-late Miocene) at La Ensenada stream (Diamante city, Entre Rios Province) and from the "Conglomerado osifero" at La Toma Vieja fossiliferous locality (Parana city, Entre Rios Province). The systematic assignment of the new material is supported by different ratios calculated among the dimensions of vertebrae, pelvic girdles, and tarsometatarsi referred to M. paranensis, which were compared with the same proportions obtained in closed related taxa. The seventh vertebra presents several differences with that of Anhinga anhinga (Linnaeus) in the morphology of the foramen vertebrale and the facies articularis cranialis; the fifthteenth vertebra is very similar to that of M. runzii Alvarenga & Guilherme and has the zygapophysis cranialis proportionally broader and projected more posteriorly than in A. anhinga. Finally, the eighteenth vertebra has the foramen transversarium more rounded, the base of the zygapophysis caudalis with less ridged borders, and the torus dorsalis more prominent caudally than in A. anhinga. Thus, morphology, size, and metric proportions support the reference of the new materials to M. paranensis. The record of M paranensis in the Parana Formation (middle-late Miocene) extends the temporal range of this taxon.
引用
收藏
页码:203 / 210
页数:8
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