New occurrences of microvertebrate fossil accumulations in Bauru Group, Late Cretaceous of western São Paulo state, Brazil

2016 ◽  
Vol 69 ◽  
pp. 80-90 ◽  
Author(s):  
Y.M. Alveş ◽  
L.P. Bergqvist ◽  
P.M. Brito
Zootaxa ◽  
2005 ◽  
Vol 1083 (1) ◽  
pp. 1 ◽  
Author(s):  
ALMIR R. PEPATO ◽  
CLÁUDIO G. TIAGO

Seven species from the northern littoral zone of São Paulo State (Brazil) are here reported. Copidognathus tupinamborum sp. nov., C. sophiae sp. nov., C. tamoiorum sp. nov. and C. ditadii sp. nov. are described. C. modestus Bartsch, 1984, C. longispinus Bartsch & Iliffe, 1985 and C. floridensis (Newell, 1947) are obtained from the Brazilian littoral for the first time and their descriptions are extended with descriptions of their protonymphs.


Zootaxa ◽  
2013 ◽  
Vol 3686 (2) ◽  
pp. 183 ◽  
Author(s):  
Fabiano Vidoi Iori ◽  
Thiago Da Silva Marinho ◽  
Ismar De Souza Carvalho ◽  
Antonio Celso de Arruda Campos

Zootaxa ◽  
2011 ◽  
Vol 3085 (1) ◽  
pp. 1 ◽  
Author(s):  
RODRIGO M. SANTUCCI ◽  
ANTONIO C. DE ARRUDA-CAMPOS

Remains of a new titanosaur, Aeolosaurus maximus sp. nov., from the Adamantina Formation (Upper Cretaceous), Bauru Group, São Paulo State of Brazil are described. The new species is represented by a single partially articulated skeleton and is characterized by having a well-developed posterior protuberance below the articular area on the anterior and middle haemal arches and a lateral bulge on the distal portion of the articular process of the mid-posterior haemal arches. It shares with other Aeolosaurus species the presence of prezygapophyses curved downward on anterior caudal vertebrae and haemal arches with double articular facets set in a concave posterodorsal surface. These two characteristics are interpreted here as synapomorphies for the genus Aeolosaurus. The new diagnosis for the genus Aeolosaurus does not support the inclusion of Gondwanatitan within Aeolosaurus as previously proposed by some authors. The phylogenetic analysis recovered the two Aeolosaurus from Argentina as sister groups with A. maximus and Gondwanatitan as progressively more basal taxa (Gondwanatitan (A. maximus (A. rionegrinus, A. colhuehuapensis))). Additionally, according to the results of the phylogenetic analysis performed in this work, the taxa Panamericansaurus, Rinconsaurus, and Maxakalisaurus are also nested within Aeolosaurini, being more basal than Aeolosaurus and Gondwanatitan. On the basis of the stratigraph-ical range of the Aeolosaurus occurrences in Argentina and the age proposals based on microfossils for the Bauru Group, it is assumed a Campanian–Maastrichtian age for the top of the Adamantina Formation for the Monte Alto region in São Paulo State and the bottom of the Marília Formation in Peirópolis, Minas Gerais State—the places where Aeolosaurus remains have been reported in Brazil.


2011 ◽  
Vol 83 (1) ◽  
pp. 291-299 ◽  
Author(s):  
William R. Nava ◽  
Agustín G. Martinelli

The record of non-mosasaur squamates (Reptilia, Squamata) is sparse in the Cretaceus fossil record of Brazil and include six putative reports, three from the Aptian-Albian of the Araripe Basin (Tijubina pontei Bonfim-Júnior and Marques, Olindalacerta brasiliensis Evans and Yabumoto, and a lizard indet.) and three from the Upper Cretaceous of the Bauru Group (Pristiguana brasiliensis Estes and Price, Anilioidae gen. et sp. indet., and Squamata gen. et sp. indet.). In this contribution, a new genus and species of lizard, Brasiliguana prudentis gen. et sp. nov., is described based on an isolated left maxilla with teeth. The material was discovered in an outcrop of the Upper Cretaceous Adamantina Formation (Bauru Group) located in the proximity of Presidente Prudente Municipality, São Paulo State, Brazil. The new taxon is considered a basal non-Priscagamidae+Acrodonta iguanian based on the presence of a weakly inclined anterior margin of the maxillary nasal process and maxillary tooth shape and tooth implantation similar to that of iguanians rather than of other lizard groups (e.g. teiids). This finding significantly increases the squamate lizard diversity of South America, which is still poorly understood and sparsely represented in the fossil record.


2004 ◽  
Vol 27 ◽  
pp. 64-74
Author(s):  
João Tadeu Arruda ◽  
Ismar De Souza Carvalho ◽  
Felipe Mesquita de Vasconcellos

The baurusuchids are medium-sized crocodylomorphs with terrestrial habits, found in the Gondwana Cretaceous basins of South America and Paleogene basins of Europe and Africa. Since 1945 many skeletal remains have been found on Western of São Paulo State, in rocks of Adamantina Formation, Bauru Basin (Late Cretaceous). The vicinities of General Salgado County, São Paulo State, had revealed well-preserved and articulated fossils of baurusuchids, allowing studies on the their paleoecology and paleobiology.


2008 ◽  
Vol 61 (3) ◽  
pp. 343-356 ◽  
Author(s):  
Alethéa Ernandes Martins Sallun ◽  
Kenitiro Suguio

Sedimentologic characterization and provenance studies of quaternary colluvial deposits (9±1 to 980±100 ky B.P. - dated by luminescence) were based on textural and mineralogical analyses. These deposits occur extensively between Marília and Presidente Prudente (São Paulo State, Brazil), superimposed on the Bauru Group sedimentary rocks or the Serra Geral Formation basaltic rocks, both of Cretaceous age. They are distributed irregularly throughout the study area and are studied by sedimentologic and morphologic methods. These deposits are composed of very fine to coarse-grained unconsolidated sands, mostly constituted by quartzose monocrystalline grains reddened by iron oxide and hydroxide impregnation. Analyses of grain sizes indicated that total granulometric distributions are richer in the clay fraction than in the sedimentary rocks located. Non-micaceous transparent heavy minerals studied microscopically in fine-grained as well as in very fine-grained sands showed that zircon, tourmaline, staurolite and rutile are present in all the samples. Differences in grain sizes among the colluvial deposits and the Bauru Group sedimentary rocks are attributable to pedogenetic processes.


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