Ichthyoliths of the Corumbatai Formation: new occurrences and interpretations for Sao Paulo state, Brazil (northeastern Parana basin)

被引:2
作者
Jurigan, Isabela [1 ]
Ricardi-Branco, Fresia [1 ]
Delcourt, Rafael [2 ]
机构
[1] Univ Estadual Campinas, Geosci Inst, Carlos Gomes 250, BR-13083855 Campinas, SP, Brazil
[2] Univ Sao Paulo, Dept Biol, Ave Bandeirantes 3900, BR-14040901 Ribeirao Preto, SP, Brazil
基金
巴西圣保罗研究基金会;
关键词
Fish teeth; Rhomboid scales; Lower actinopterygians; Xenacanthiformes; Permian; RASTO FORMATION; IRATI FORMATION; CHONDRICHTHYES; ELASMOBRANCHII; SHARK; FISH; REEVALUATION; ASSEMBLAGE; RIO;
D O I
10.1016/j.jsames.2022.103958
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Permian ichthyofauna of the Passa Dois Group is well known for the ubiquitous presence of disarticulated elements of a variety of fish taxa that remains largely understudied. Lower actinopterygians (Palaeonisciformes) are the most abundant, together with isolated teeth of Xenacanthiformes chondrichthians. This study brings new information on the external micro-ornamentations of actinopterygian teeth and rhomboid scales of the Corumbatai Formation collected for the first time in Santa Rosa de Viterbo region in the State of Sao Paulo, as well as a new proposition to approach this remains by using cluster analysis. These fossils were found in distal storm deposits (tempestite) and were separated from the rock matrix for analysis. Six distinct actinopterygian tooth morphotypes were identified. Curved forms are dominant in the assemblage, with ornamentations varying from smooth to ribbed shafts and others with grooves and tubercles. The scales are very fragmented showing surface micro-punctuations and longitudinal ridges. The Xenacanthiformes tricuspid teeth were very scarce in the assemblage and no complete specimen was recovered. Nonetheless, it was possible to identify them by their subtriangular shape and drop-shaped basal tubercle. Both ichthyodonts and scales show characteristics similar to at least other 26 occurrences, spread over more than 1000 km, and already described in the literature strati -graphically positioned above and below the Corumbatai Formation, attesting the wide temporal and spatial distribution of these fossils.
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页数:19
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