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Zootaxa,Montealtosuchus Arrudacamposi, a New Peirosaurid
Zootaxa 1607: 35–46 (2007) ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ ZOOTAXA Copyright © 2007 · Magnolia Press ISSN 1175-5334 (online edition) Montealtosuchus arrudacamposi, a new peirosaurid crocodile (Mesoeucrocodylia) from the Late Cretaceous Adamantina Formation of Brazil ISMAR DE SOUZA CARVALHO1, FELIPE MESQUITA DE VASCONCELLOS1 & SANDRA APARE- CIDA SIMIONATO TAVARES2 1Universidade Federal do Rio de Janeiro. Departamento de Geologia, CCMN/IGEO. 21.949-900 Cidade Universitária - Ilha do Fundão. Rio de Janeiro - RJ. Brasil. E-mail: [email protected]; [email protected] 2Museu de Paleontologia de Monte Alto. Praça do Centenário, Centro de Artes s/no. 15.910-000, MonteAlto-Brazil. E-mail: [email protected] Abstract We describe a new species of Peirosauridae (Crocodyliformes, Mesoeucrocodylia), Montealtosuchus arrudacamposi gen. nov. et sp. nov., from the Late Cretaceous (Turonian-Santonian) strata of the Bauru Basin, Brazil. Montealtosuchus was found at the outskirts of Monte Alto County in reddish sandstones of the Adamantina Formation. This specimen is exquisitely preserved with skull, mandible, postcranial and exoskeletal elements in articulation that provides critical information of the anatomy of this group. The occurrence of Peirosauridae in the Adamantina Formation (Turonian-San- tonian) widens the chronostratigraphic range of this Mesoeucrocodylia taxon in Brazil. Recent analysis suggests that the Peirosauridae is restricted to the Late Cretaceous deposits of South America. Key words: Montealtosuchus arrudacamposi gen. nov. et sp. nov.; Peirosauridae; Upper Cretaceous; Adamantina For- mation; Bauru Basin Introduction The Bauru Basin comprises an area between latitudes 18o S and 24o S, and longitudes 47o W and 56o W, and covers an area over 370.000 km2 in the southeast interior of Brazil, with outcrops in São Paulo, Minas Gerais, Mato Grosso do Sul and Goiás states. -
The Baurusuchidae Vs Theropoda Record in the Bauru Group (Upper Cretaceous, Brazil): a Taphonomic Perspective
Journal of Iberian Geology https://doi.org/10.1007/s41513-018-0048-4 RESEARCH PAPER The Baurusuchidae vs Theropoda record in the Bauru Group (Upper Cretaceous, Brazil): a taphonomic perspective Kamila L. N. Bandeira1 · Arthur S. Brum1 · Rodrigo V. Pêgas1 · Giovanne M. Cidade2 · Borja Holgado1 · André Cidade1 · Rafael Gomes de Souza1 Received: 31 July 2017 / Accepted: 23 January 2018 © Springer International Publishing AG, part of Springer Nature 2018 Abstract Purpose The Bauru Group is worldwide known due to its high diversity of archosaurs, especially that of Crocodyliformes. Recently, it has been suggested that the Crocodyliformes, especially the Baurusuchidae, were the top predators of the Bauru Group, based on their anatomical convergence with theropods and the dearth of those last ones in the fossil record of this geological group. Methods Here, we erect the hypothesis that assumption is taphonomically biased. For this purpose, we made a literature survey on all the published specimens of Theropoda, Baurusuchidae and Titanosauria from all geological units from the Bauru Group. Also, we gathered data from the available literature, and we classifed each fossil fnd under a taphonomic class proposed on this work. Results We show that those groups have diferent degrees of bone representativeness and diferent qualities of preservation pattern. Also, we suggest that baurusuchids lived close to or in the abundant food plains, which explains the good preserva- tion of their remains. Theropods and titanosaurs did not live in association with such environments and the quality of their preservation has thus been negatively afected. Conclusions We support the idea that the Baurusuchidae played an important role in the food chain of the ecological niches of the Late Cretaceous Bauru Group, but the possible biases in their fossil record relative to Theropoda do not support the conclusion that baurusuchids outcompeted theropods. -
A New Sebecid Mesoeucrocodylian from the Rio Loro Formation (Palaeocene) of North-Western Argentina
Zoological Journal of the Linnean Society, 2011, 163, S7–S36. With 17 figures A new sebecid mesoeucrocodylian from the Rio Loro Formation (Palaeocene) of north-western Argentina DIEGO POL1* and JAIME E. POWELL2 1CONICET, Museo Paleontológico Egidio Feruglio, Ave. Fontana 140, Trelew CP 9100, Chubut, Argentina 2CONICET, Instituto Miguel Lillo, Miguel Lillio 205, San Miguel de Tucumán CP 4000, Tucumán, Argentina Received 2 March 2010; revised 10 October 2010; accepted for publication 19 October 2010 A new basal mesoeucrocodylian, Lorosuchus nodosus gen. et sp. nov., from the Palaeocene of north-western Argentina is presented here. The new taxon is diagnosed by the presence of external nares facing dorsally, completely septated, and retracted posteriorly, elevated narial rim, sagittal crest on the anteromedial margins of both premaxillae, dorsal crests and protuberances on the anterior half of the rostrum, and anterior-most three maxillary teeth with emarginated alveolar margins. This taxon is most parsimoniously interpreted as a bizarre and highly autapomorphic basal member of Sebecidae, a position supported (amongst other characters) by the elongated bar-like pterygoid flanges, a laterally opened notch and fossa in the pterygoids located posterolaterally to the choanal opening (parachoanal fossa), base of postorbital process of jugal directed dorsally, and palatal parts of the premaxillae meeting posteriorly to the incisive foramen. Lorosuchus nodosus also shares with basal neosuchians a suite of derived characters that are interpreted as convergently acquired and possibly related to their semiaquatic lifestyle. The phylogenetic analysis used for testing the phylogenetic affinities of L. nodosus depicts Sebecidae as the sister group of Baurusuchidae, forming a monophyletic Sebecosuchia that is deeply nested within Notosuchia. -
CROCODYLIFORMES, MESOEUCROCODYLIA) from the EARLY CRETACEOUS of NORTH-EAST BRAZIL by DANIEL C
[Palaeontology, Vol. 52, Part 5, 2009, pp. 991–1007] A NEW NEOSUCHIAN CROCODYLOMORPH (CROCODYLIFORMES, MESOEUCROCODYLIA) FROM THE EARLY CRETACEOUS OF NORTH-EAST BRAZIL by DANIEL C. FORTIER and CESAR L. SCHULTZ Departamento de Paleontologia e Estratigrafia, UFRGS, Avenida Bento Gonc¸alves 9500, 91501-970 Porto Alegre, C.P. 15001 RS, Brazil; e-mails: [email protected]; [email protected] Typescript received 27 March 2008; accepted in revised form 3 November 2008 Abstract: A new neosuchian crocodylomorph, Susisuchus we recovered the family name Susisuchidae, but with a new jaguaribensis sp. nov., is described based on fragmentary but definition, being node-based group including the last com- diagnostic material. It was found in fluvial-braided sedi- mon ancestor of Susisuchus anatoceps and Susisuchus jagua- ments of the Lima Campos Basin, north-eastern Brazil, ribensis and all of its descendents. This new species 115 km from where Susisuchus anatoceps was found, in corroborates the idea that the origin of eusuchians was a rocks of the Crato Formation, Araripe Basin. S. jaguaribensis complex evolutionary event and that the fossil record is still and S. anatoceps share a squamosal–parietal contact in the very incomplete. posterior wall of the supratemporal fenestra. A phylogenetic analysis places the genus Susisuchus as the sister group to Key words: Crocodyliformes, Mesoeucrocodylia, Neosuchia, Eusuchia, confirming earlier studies. Because of its position, Susisuchus, new species, Early Cretaceous, north-east Brazil. B razilian crocodylomorphs form a very expressive Turonian–Maastrichtian of Bauru basin: Adamantinasu- record of Mesozoic vertebrates, with more than twenty chus navae (Nobre and Carvalho, 2006), Baurusuchus species described up to now. -
A New Peirosaurid (Crocodyliformes, Mesoeucrocodylia) from the Upper Cretaceous of Patagonia, Argentina
ARTICLES AMEGHINIANA - 2016 - Volume 53 (1): 14 – 25 ISSN 0002-7014 A NEW PEIROSAURID (CROCODYLIFORMES, MESOEUCROCODYLIA) FROM THE UPPER CRETACEOUS OF PATAGONIA, ARGENTINA FRANCISCO BARRIOS 1, ARIANA PAULINA-CARABAJAL 1,2 AND PAULA BONA 2,3 1Museo Municipal Carmen Funes, Av. Córdoba 55, Q8318EBA Plaza Huincul, Neuquén, Argentina. [email protected] ; [email protected] 2CONICET, Consejo Nacional de Investigaciones Científicas y Técnicas, Av. Rivadavia 1917, C1033AAJ Ciudad Autónoma de Buenos Aires, Argentina. 3División Paleontología Vertebrados, Museo de La Plata, Universidad Nacional de La Plata. Paseo del Bosque s/n, B1900FWA La Plata, Argentina. [email protected] Abstract . Peirosaurids are a group of Cretaceous continental crocodyliforms from Gondwana. Two species are known from the Neuquén Group in Argentina: Lomasuchus palpebrosus (Portezuelo Formation, late Turonian–early Coniacian) and Gasparinisuchus peirosauroides (Bajo de la Carpa and Anacleto formations, Santonian and early Campanian, respectively). Here, we describe the first peirosaurid from the Cerro Lisandro Formation, Bayomesasuchus hernandezi gen. et sp. nov. The material corresponds to a fragmentary skull and mandible. Although frag - mentary, this is the most complete crocodyliform specimen recorded for the Cerro Lisandro Formation. In a phylogenetic analysis Bayome - sasuchus is depicted in a polytomy together with South American peirosaurids and the African form Hamadasuchus rebouli . Key words. Bayomesasuchus . Peirosauridae. Cerro Lisandro Formation. Cretaceous . Resumen. UN NUEVO PEIROSÁURIDO (CROCODYLIFORMES, MESOEUCROCODYLIA) DEL CRETÁCICO SUPERIOR DE PATAGONIA, ARGEN - TINA. Los peirosáuridos constituyen un grupo de crocodiliformes continentales del Cretácico de Gondwana. Para el Grupo Neuquén, Argentina, se conocen dos especies: Lomasuchus palpebrosus (Formación Portezuelo, Turoniano tardío–Coniaciano temprano) y Gasparinisuchus peiro - sau roides (Formaciones Bajo de la Carpa y Anacleto, Santoniano y Campaniano temprano, respectivamente). -
From the Late Cretaceous of Minas Gerais, Brazil: New Insights on Sphagesaurid Anatomy and Taxonomy
The first Caipirasuchus (Mesoeucrocodylia, Notosuchia) from the Late Cretaceous of Minas Gerais, Brazil: new insights on sphagesaurid anatomy and taxonomy Agustín G. Martinelli1,2,3, Thiago S. Marinho2,4, Fabiano V. Iori5 and Luiz Carlos B. Ribeiro2 1 Instituto de Geociencias, Universidade Federal do Rio Grande do Sul, Porto Alegre, Rio Grande do Sul, Brazil 2 Centro de Pesquisas Paleontológicas L. I. Price, Complexo Cultural e Científico Peirópolis, Pró-Reitoria de Extensão Universitária, Universidade Federal do Triangulo Mineiro, Uberaba, Minas Gerais, Brazil 3 CONICET-Sección Paleontologia de Vertebrados, Museo Argentino de Ciencias Naturales “Bernardino Rivadavia”, Buenos Aires, Argentina 4 Departamento de Ciências Biológicas, Universidade Federal do Triângulo Mineiro, Instituto de Ciências Exatas, Naturais e Educação, Uberaba, Minas Gerais, Brazil 5 Museu de Paleontologia “Prof. Antonio Celso de Arruda Campos”, Monte Alto, Sao Paulo, Brazil ABSTRACT Field work conducted by the staff of the Centro de Pesquisas Paleontológicas Llewellyn Ivor Price of the Universidade Federal do Triângulo Mineiro since 2009 at Campina Verde municipality (MG) have resulted in the discovery of a diverse vertebrate fauna from the Adamantina Formation (Bauru Basin). The baurusuchid Campinasuchus dinizi was described in 2011 from Fazenda Três Antas site and after that, preliminary descriptions of a partial crocodyliform egg, abelisaurid teeth, and fish remains have been done. Recently, the fossil sample has been considerably increased including the discovery -
Freshwater Decapoda Trace Fossils in Floodplain Paleosols of Marilia Formation in Minas Gerais State (Se Brazil)
Rev. bras. paleontol. 20(3):287-298, Setembro/Dezembro 2017 © 2017 by the Sociedade Brasileira de Paleontologia doi:10.4072/rbp.2017.3.02 FRESHWATER DECAPODA TRACE FOSSILS IN FLOODPLAIN PALEOSOLS OF MARILIA FORMATION IN MINAS GERAIS STATE (SE BRAZIL) DIEGO LUCIANO DO NASCIMENTO, ALESSANDRO BATEZELLI & FRANCISCO SÉRGIO BERNARDES LADEIRA Source to sink and Paleopedology Research Group (SPRG), Instituto de Geociências, UNICAMP, Campinas, SP, Brazil. [email protected], [email protected], [email protected] ABSTRACT – The Marilia Formation (Bauru Group, Bauru Basin) is an important record of the Upper Cretaceous in Brazil, and hosts an important fossil content. However, works regarding continental ichnology in this unit are still scarce. In order to improve this knowledge, the present work describes the occurrence of Camborygma litonomos in paleosols developed from floodplain deposits of the Marilia Formation in the Minas Gerais State. This trace fossil is associated with the activity of freshwater crayfishes, digging the soil looking for protection and to avoid the carapace dryness. Crayfish body fossils have not yet been described in deposits of the Bauru Group, thus, the trace fossil here recorded is the exclusive evidence of this organism, which is of great importance to the knowledge of the invertebrates paleodiversity of the Marilia Formation during the Late Cretaceous. Key words: ichnology, Camborygma litonomos, crustaceans, Upper Cretaceous, Bauru Group, paleopedology. RESUMO – A Formação Marília (Grupo Bauru, Bacia Bauru) é um importante registro do Cretáceo Superior no Brasil e possui um importante conteúdo fossilífero. No entanto, os trabalhos sobre icnologia continental desta unidade ainda são escassos. A fim de ampliar este conhecimento, o presente trabalho descreve a ocorrência de Camborygma litonomos em paleossolos desenvolvidos em depósitos de planície de inundação no Estado de Minas Gerais. -
Early Cretaceous) of Bahia, Brazil
Anais da Academia Brasileira de Ciências (2018) (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 http://dx.doi.org/10.1590/0001-3765201720170382 www.scielo.br/aabc | www.fb.com/aabcjournal New Crocodyliform specimens from Recôncavo-Tucano Basin (Early Cretaceous) of Bahia, Brazil RAFAEL G. DE SOUZA1 and DIOGENES A. CAMPOS2 1Laboratório de Sistemática e Tafonomia de Vertebrados Fósseis, Setor de Paleovertebrados, Departamento de Geologia e Paleontologia, Museu Nacional, Universidade Federal do Rio de Janeiro, Quinta da Boa Vista, s/n, São Cristóvão, 20940-040 Rio de Janeiro, RJ, Brazil ²Museu de Ciências da Terra - CPRM, Av. Pasteur, 404, 22290-255 Rio de Janeiro, RJ, Brazil Manuscript received on May 19, 2017; accepted for publication on October 23, 2017 ABSTRACT In 1940, L.I. Price and A. Oliveira recovered four crocodyliform specimens from the Early Cretaceous Bahia Supergroup (Recôncavo-Tucano Basin). In the present work, we describe four different fossil specimens: an osteoderm, a fibula, a tibia, and some autopodial bones. No further identification besides Mesoeucrocodylia was made due to their fragmentary nature and the reduced number of recognized synapomorphies for more inclusive clades. With exception of the fibula, all other specimens have at least one particular feature, which with new specimens could represent new species. The new specimens described here increase the known diversity of Early Cretaceous crocodyliforms from Brazil. This work highlights the great fossiliferous -
A New Sebecid from the Paleogene of Brazil and the Crocodyliform Radiation After the K–Pg Boundary
A New Sebecid from the Paleogene of Brazil and the Crocodyliform Radiation after the K–Pg Boundary Alexander W. A. Kellner1*, Andre´ E. P. Pinheiro2, Diogenes A. Campos3 1 Laborato´rio de Sistema´tica e Tafonomia de Vertebrados Fo´sseis - Departamento de Geologia e Paleontologia, Museu Nacional - Universidade Federal do Rio de Janeiro, Rio de Janeiro, Brazil, 2 Laborato´rio de Macrofo´sseis - Departamento de Geologia, Universidade Federal do Rio de Janeiro, Rio de Janeiro, Brazil, 3 Museu de Cieˆncias da Terra, Servic¸o Geolo´gico do Brasil - Companhia de Pesquisa de Recursos Minerais, Rio de Janeiro, Brazil Abstract A new crocodyliform, Sahitisuchus fluminensis gen. et sp. nov., is described based on a complete skull, lower jaw and anterior cervical vertebrae collected in the Sa˜o Jose´ de Itaboraı´ Basin of Rio de Janeiro, Brazil. The specimen is one of the best preserved crocodyliforms from Paleocene deposits recovered so far and represents a sebecosuchian, one of the few clades that survived the Cretaceous-Paleogene biotic crisis. The new taxon is found in the same deposit as an alligatoroid, a group that experienced large diversification in the Paleogene. The sebecosuchian record suggests that after the Cretaceous- Paleogene biotic crisis, the less specialized members of this clade characterized by a higher number of teeth compared to the baurusuchid sebecosuchians survived, some having terrestrial habits while others developed a semi-aquatic life style (e.g., Lorosuchus). Starting in the Eocene, sebecid sebecosuchians became specialized with a more accentuated oreinirostry as observed in Sebecus and in Langstonia, but not showing the typical reduced dentition developed by the Cretaceous baurusuchid sebecosuchians. -
Postcranial Skeletons of Caipirasuchus (Crocodyliformes, Notosuchia, Sphagesauridae) from the Upper Cretaceous (Turonianesantonian) of the Bauru Basin, Brazil
Cretaceous Research 60 (2016) 109e120 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes Postcranial skeletons of Caipirasuchus (Crocodyliformes, Notosuchia, Sphagesauridae) from the Upper Cretaceous (TuronianeSantonian) of the Bauru Basin, Brazil * Fabiano Vidoi Iori a, b, , Ismar de Souza Carvalho c, Thiago da Silva Marinho d a Museu de Paleontologia “Prof. Antonio Celso de Arruda Campos”, Centro de Artes, Praça do Centenario, CEP 15910-000, Monte Alto, SP, Brazil b Instituto Municipal de Ensino Superior de Catanduva (IMES), Rodovia Washington Luis, km 382, CEP 15800-971, Catanduva, SP, Brazil c Universidade Federal do Rio de Janeiro (UFRJ), Instituto de Geoci^encias (IGEO), Departamento de Geologia, Cidade Universitaria, Ilha do Fundao,~ Av. Athos da Silveira Ramos, 274, Bloco G, 21941-916, Rio de Janeiro, RJ, Brazil d Universidade Federal do Triangulo^ Mineiro (UFTM), Pro-Reitoria de Extensao~ Universitaria, Centro de Pesquisas Paleontologicas L. I. Price, Complexo Cultural e Científico de Peiropolis (CCCP), R. Estanislau Collenghi 194, Peiropolis, 38039-755 Uberaba, MG, Brazil article info abstract Article history: Caipirasuchus is a sphagesaurid crocodyliform genus known from Upper Cretaceous rocks (Turonian Received 10 August 2015 eSantonian) of the Bauru Basin, Brazil. Although their earlier descriptions were restricted to skull and Received in revised form mandible morphology, three species have been identified. In the present study, the skeletons of three 30 November 2015 specimens were analyzed from the collection of Prof. Antonio Celso de Arruda Campos Paleontology Accepted in revised form 30 November 2015 Museum: Caipirasuchus montealtensis (MPMA 68-0003/12), Caipirasuchus paulistanus (MPMA 67-0001/ Available online xxx 00) and Caipirasuchus sp. -
New Crocodyliform Specimens from Recôncavo-Tucano Basin (Early Cretaceous) of Bahia, Brazil
Anais da Academia Brasileira de Ciências (2019) 91(Suppl. 2): e20170382 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 http://dx.doi.org/10.1590/0001-3765201720170382 www.scielo.br/aabc | www.fb.com/aabcjournal New Crocodyliform specimens from Recôncavo-Tucano Basin (Early Cretaceous) of Bahia, Brazil RAFAEL G. DE SOUZA1 and DIOGENES A. CAMPOS2 1Laboratório de Sistemática e Tafonomia de Vertebrados Fósseis, Setor de Paleovertebrados, Departamento de Geologia e Paleontologia, Museu Nacional, Universidade Federal do Rio de Janeiro, Quinta da Boa Vista, s/n, São Cristóvão, 20940-040 Rio de Janeiro, RJ, Brazil ²Museu de Ciências da Terra - CPRM, Av. Pasteur, 404, 22290-255 Rio de Janeiro, RJ, Brazil Manuscript received on May 19, 2017; accepted for publication on October 23, 2017 How to cite: SOUZA RG AND CAMPOS DA. 2019. New Crocodyliform specimens from Recôncavo-Tucano Basin (Early Cretaceous) of Bahia, Brazil. An Acad Bras Cienc 91: e20170382. DOI 10.1590/0001-3765201720170382. Abstract: In 1940, L.I. Price and A. Oliveira recovered four crocodyliform specimens from the Early Cretaceous Bahia Supergroup (Recôncavo-Tucano Basin). In the present work, we describe four different fossil specimens: an osteoderm, a fibula, a tibia, and some autopodial bones. No further identification besides Mesoeucrocodylia was made due to their fragmentary nature and the reduced number of recognized synapomorphies for more inclusive clades. With exception of the fibula, all other specimens have at least one particular feature, which with new specimens could represent new species. The new specimens described here increase the known diversity of Early Cretaceous crocodyliforms from Brazil. -
(Crocodyliformes, 1 Mesoeucrocodylia) During
1 DIVERSITY PATTERNS OF NOTOSUCHIA (CROCODYLIFORMES, 2 MESOEUCROCODYLIA) DURING THE CRETACEOUS OF GONDWANA 3 4 5 DIEGO POL1 and JUAN MARTIN LEARDI2 6 7 1CONICET. Museo Paleontológico Egidio Feruglio, Av. Fontana 140, U9100GYO 8 Trelew, Chubut, Argentina. [email protected] 9 2IDEAN, Departamento de Ciencias Geológicas, Universidad de Buenos Aires, Ciudad 10 Universitaria Pab. II, C1428EHA Ciudad Autónoma de Buenos Aires, Argentina. 11 [email protected] 12 13 38pp. (text+references); 5 figs. 14 15 RH: POL AND LEARDI: NOTOSUCHIAN DIVERSITY PATTERNS 16 1 17 Abstract. Notosuchia is a diverse clade of Crocodyliformes that achieved a remarkable 18 diversity during the Cretaceous. This group is particularly abundant in continental 19 deposits of Gondwana throughout the Cretaceous, especially in South America. 20 Notosuchia was first recognized as a distinct group by the early work of Gasparini in the 21 1970’s and in the last decades numerous discoveries and studies have increased the 22 geographical, temporal and taxonomical scope of this clade. Here we analyze the 23 patterns of diversity of Notosuchia during the Cretaceous, considering their taxic and 24 phylogenetic diversity, as well as implementing sampling corrections aiming to account 25 for the uneven fossil record of different stages of the Cretaceous. We identify two 26 subsequent pulses of diversification in the late Early Cretaceous and the middle Late 27 Cretaceous, followed by two separate extinction events that occurred during the latest 28 Cretaceous (Campanian/Maastrichtian). We discuss the contribution of the South 29 American, African, and Malagasy fossil records to the diversity curves, which indicates 30 the African fossil record dominates the first pulse of diversification and the South 31 American fossil record exclusively compose the second pulse of diversification.