Taphonomy and paleohistology of a dinosaur rib from Marília Formation, Bauru Group, in the state of Minas Gerais, Brazil

被引:2
作者
Paio, Vinicius Jose Marostica [1 ]
Jurigan, Isabela [1 ]
Delcourt, Rafael [2 ,4 ]
de Faria, Rafael Souza [3 ]
Batezelli, Alessandro [1 ]
Ricardi-Branco, Fresia [1 ]
机构
[1] Univ Estadual Campinas UNICAMP, Dept Geol & Recursos Nat, Inst Geociencias, Rua Carlos Gomes,250 Cidade Univ, BR-13083855 Campinas, SP, Brazil
[2] Univ Sao Paulo, Fac Filosofia Ciencias & Letras Ribeirao Preto, Dept Biol, Lab Paleontol, Ave Bandeirantes 3900, BR-14040901 Ribeirao Preto, SP, Brazil
[3] Pontificia Univ Catolica Campinas PUC Campinas, Fac Ciencias Biol, Ctr Ciencias Vida, Ave John Boyd Dunlop S-N, BR-13060904 Campinas, SP, Brazil
[4] Bayer Staatssammlung Palaontol & Geol, Richard Wagner Str 10, D-80333 Munich, Germany
基金
巴西圣保罗研究基金会;
关键词
Osteohistology; Bone weathering; Fossil diagenesis; Bauru basin; ADAMANTINA FORMATION; SAUROPOD DINOSAUR; UBERABATITAN-RIBEIROI; SAO-PAULO; BONE; RECORD; THEROPODA; TITANOSAURIA; HISTORY; BASIN;
D O I
10.1016/j.cretres.2024.105899
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The Bauru Group (CampanianeMaastrichtian) has one of the richest fossil records of Cretaceous in South America. All dinosaur fossils from this unit were assigned to Saurischia, most of them poorly preserved. We present the histological and taphonomic analysis of a dinosaur dorsal rib fragment from the Mar & iacute;lia Formation in the western state of Minas Gerais. Thin sections were prepared to describe the microstructures of the bone tissue and the fossilization processes involved in preserving the specimen. An elemental analysis was also performed to verify the chemical composition of the fossil and rock matrix. Haversian bone was identified in the rib cortex, and no growth marks or an external fundamental system were found. The rib probably belonged to a saurischian dinosaur because of its plank shape and elliptical cross-section. Hypotheses regarding taphonomic processes were inferred. An extended period of subaerial exposure, followed by high-energy transport, was interpreted due to extensive fractures and signs of abrasion on the outer surface of the bone. Pyrite pseudomorphs (framboids) indicate that the bone was deposited in a reductive environment. After burial, the rapid precipitation of calcite and alkaline stability allowed the preservation of apatite during the recrystallization phase. The manganese hydroxides were deposited on apatite crystals during early diagenesis. We concluded that the fossil rib presented a common taphonomic bias identified among vertebrate fossils of the Bauru Group, which is associated with the exposure of the bones to arid and semiarid climates, their transport into the depositional environments and pedogenetic influence during fossil diagenesis. (c) 2024 Elsevier Ltd. All rights reserved.
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页数:12
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