Tooth Microstructure of the Early Permian Aquatic Predator Stereosternum Tumidum
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New Permian Fauna from Tropical Gondwana
ARTICLE Received 18 Jun 2015 | Accepted 18 Sep 2015 | Published 5 Nov 2015 DOI: 10.1038/ncomms9676 OPEN New Permian fauna from tropical Gondwana Juan C. Cisneros1,2, Claudia Marsicano3, Kenneth D. Angielczyk4, Roger M. H. Smith5,6, Martha Richter7, Jo¨rg Fro¨bisch8,9, Christian F. Kammerer8 & Rudyard W. Sadleir4,10 Terrestrial vertebrates are first known to colonize high-latitude regions during the middle Permian (Guadalupian) about 270 million years ago, following the Pennsylvanian Gondwanan continental glaciation. However, despite over 150 years of study in these areas, the bio- geographic origins of these rich communities of land-dwelling vertebrates remain obscure. Here we report on a new early Permian continental tetrapod fauna from South America in tropical Western Gondwana that sheds new light on patterns of tetrapod distribution. Northeastern Brazil hosted an extensive lacustrine system inhabited by a unique community of temnospondyl amphibians and reptiles that considerably expand the known temporal and geographic ranges of key subgroups. Our findings demonstrate that tetrapod groups common in later Permian and Triassic temperate communities were already present in tropical Gondwana by the early Permian (Cisuralian). This new fauna constitutes a new biogeographic province with North American affinities and clearly demonstrates that tetrapod dispersal into Gondwana was already underway at the beginning of the Permian. 1 Centro de Cieˆncias da Natureza, Universidade Federal do Piauı´, 64049-550 Teresina, Brazil. 2 Programa de Po´s-Graduac¸a˜o em Geocieˆncias, Departamento de Geologia, Universidade Federal de Pernambuco, 50740-533 Recife, Brazil. 3 Departamento de Cs. Geologicas, FCEN, Universidad de Buenos Aires, IDEAN- CONICET, C1428EHA Ciudad Auto´noma de Buenos Aires, Argentina. -
Reptile Family Tree
Reptile Family Tree - Peters 2015 Distribution of Scales, Scutes, Hair and Feathers Fish scales 100 Ichthyostega Eldeceeon 1990.7.1 Pederpes 91 Eldeceeon holotype Gephyrostegus watsoni Eryops 67 Solenodonsaurus 87 Proterogyrinus 85 100 Chroniosaurus Eoherpeton 94 72 Chroniosaurus PIN3585/124 98 Seymouria Chroniosuchus Kotlassia 58 94 Westlothiana Casineria Utegenia 84 Brouffia 95 78 Amphibamus 71 93 77 Coelostegus Cacops Paleothyris Adelospondylus 91 78 82 99 Hylonomus 100 Brachydectes Protorothyris MCZ1532 Eocaecilia 95 91 Protorothyris CM 8617 77 95 Doleserpeton 98 Gerobatrachus Protorothyris MCZ 2149 Rana 86 52 Microbrachis 92 Elliotsmithia Pantylus 93 Apsisaurus 83 92 Anthracodromeus 84 85 Aerosaurus 95 85 Utaherpeton 82 Varanodon 95 Tuditanus 91 98 61 90 Eoserpeton Varanops Diplocaulus Varanosaurus FMNH PR 1760 88 100 Sauropleura Varanosaurus BSPHM 1901 XV20 78 Ptyonius 98 89 Archaeothyris Scincosaurus 77 84 Ophiacodon 95 Micraroter 79 98 Batropetes Rhynchonkos Cutleria 59 Nikkasaurus 95 54 Biarmosuchus Silvanerpeton 72 Titanophoneus Gephyrostegeus bohemicus 96 Procynosuchus 68 100 Megazostrodon Mammal 88 Homo sapiens 100 66 Stenocybus hair 91 94 IVPP V18117 69 Galechirus 69 97 62 Suminia Niaftasuchus 65 Microurania 98 Urumqia 91 Bruktererpeton 65 IVPP V 18120 85 Venjukovia 98 100 Thuringothyris MNG 7729 Thuringothyris MNG 10183 100 Eodicynodon Dicynodon 91 Cephalerpeton 54 Reiszorhinus Haptodus 62 Concordia KUVP 8702a 95 59 Ianthasaurus 87 87 Concordia KUVP 96/95 85 Edaphosaurus Romeria primus 87 Glaucosaurus Romeria texana Secodontosaurus -
Unusual Isotopic Composition of Carbonates from the Irati Formation, Brazil
WAGNER FERRARESI DE GIOVANI 1 ENEAS SALATI F <--entro de Energia Nuclear na Agricultura, ESALQ-USP, Piracicaba, Brazil ONILDO J. MARINI Departmento de Geocièncias, Universidade de Brasilia, Brasilia, Brazil IRVING FRIEDMAN U.S. Geological Survey, Denver, Colorado 80225 Unusual Isotopic Composition of Carbonates from the Irati Formation, Brazil ABSTRACT easily identifiable lithology makes it a good were collected at the town of Sao Mateus do marker horizon. The formation was as- Sul. Near this outcrop, 5 more samples (Fig. Samples of dolomite and limestone from signed by MacGregor (in Mendes, 1967, p. 1, loc. II; Table 3, SMS samples) of the the Permian Irati Formation collected in the 139) to the Permian, in his study of the fossil intermediate zone were collected. Paraná Basin, southern Brazil, have been reptile Mesosaurus brasiliensis. Nine samples were collected from the analyzed for 8Cia and SO18. The 8C'3 ranges Carbon and oxygen isotopic composi- state of Santa Catarina: 5 from Papanduva from +18.3°/oo to -17.4°/oo PDB, while the tions have been used to differentiate (Fig. 1, loc. Ill; Table 4, P samples) and 4 SO18 ranges from -2.6°/oo to -12.5°/oo limestones deposited in marine environ- from Correia Pinto (Fig. 1, loc. IV; Table 4, PDB. In some quarries where the exposures ments from those originating from fresh CP samples). are especially good, a large variation in 8C13 water. For example, Clayton and Degens From the state of Rio Grande do Sul, 5 can be found. The lower, dense gray (1959) have shown that in 30 samples of samples were collected in Pantano Grande dolomite has light carbon ( —17to +2.6%o), limestone (mainly Pennsylvanian) the 8C13 (Table 5), in an outcrop of very poor quality, whereas the overlying intermediate zone of differs for samples from the two environ- containing clayey soil formed by decomposi- interbedded organic-rich shale and black ments. -
A Coluna Vertebral De Brazilosaurus Sanpauloensis Shikama
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Biblioteca Digital de Periódicos da UFPR (Universidade Federal do Paraná) Acta Biol. Par., Curitiba, 30 (1, 2, 3, 4): 151-173. 2001. 151 A coluna vertebral de Brazilosaurus sanpauloensis Shikama & Ozaki, 1966 da Formação Irati, Permiano da Bacia do Paraná (Brasil) (Proganosauria, Mesosauridae) The vertebral column of Brazilosaurus sanpauloensis Shikama & Ozaki, 1966 from Irati Formation, Permian of Paraná Basin, (Brazil) (Proganosauria, Mesosauridae) FERNANDO A. SEDOR1 & JORGE FERIGOLO2 Os Mesosauridae incluídos na ordem Proganosauria (BAUR, 1887) constituem dentre os “Reptilia”, um pequeno grupo extinto de formas lacertiformes esguias, de pequeno porte, adaptados à vida aquática ou semi-aquática (cf. ROMER, 1956; 1966). A distribuição temporal e geográfica do grupo restringe-se ao Permiano da América do Sul e da África. No Brasil, os Mesosauridae ocorrem na Formação Irati da Bacia do Paraná, e, no continente africano, ocorrem na Formação Whitehill, do Sistema Karoo (COPE, 1886; MCGREGOR, 1908; SHIKAMA & OZAKI, 1966; MENDES, 1967; ROÖSLER, 1970; ARAÚJO, 1976; BORGOMANERO & LEONARDI, 1979; MOREIRA et al., 1984). Também são referidas ocorrências de Mesosauridae no Paraguai (Beder; e Harrington, apud OELOFSEN & ARAÚJO, 1983) e no Uruguai (Guillemain; e Walther, apud MONES, 1986). 1 Museu de Ciências Naturais (MCN) — SCB, Universidade Federal do Paraná — Caixa Postal 19031 — 81531-990 Curitiba, Paraná, Brasil. Email: [email protected] Pesquisador do Museu de Ciências Naturais — Fundação Zoobotânica do Rio Grande do Sul, Porto Alegre, RS, Brasil. 152 Acta Biol. Par., Curitiba, 30 (1, 2, 3, 4): 151-173. 2001. Os sedimentos sul-americanos portadores de mesossaurídeos situam- se dentro do intervalo temporal do Kazaniano e os africanos entre Permiano Inferior e Permiano Médio (PINTO, 1972a; OELOFSEN & ARAÚJO, 1987), correspondendo à porção mais superior do Sakmariano. -
IV. Northern South America EIA/ARI World Shale Gas and Shale Oil Resource Assessment
IV. Northern South America EIA/ARI World Shale Gas and Shale Oil Resource Assessment IV. NORTHERN SOUTH AMERICA SUMMARY Northern South America has prospective shale gas and shale oil potential within marine- deposited Cretaceous shale formations in three main basins: the Middle Magdalena Valley and Llanos basins of Colombia, and the Maracaibo/Catatumbo basins of Venezuela and Colombia, Figure IV-1. The organic-rich Cretaceous shales (La Luna, Capacho, and Gacheta) sourced much of the conventional gas and oil produced in Colombia and western Venezuela, and are similar in age to the Eagle Ford and Niobrara shale plays in the USA. Ecopetrol, ConocoPhillips, ExxonMobil, Shell, and others have initiated shale exploration in Colombia. Colombia’s petroleum fiscal regime is considered attractive to foreign investment. Figure IV-1: Prospective Shale Basins of Northern South America Source: ARI 2013 May 17, 2013 IV-1 IV. Northern South America EIA/ARI World Shale Gas and Shale Oil Resource Assessment For the current EIA/ARI assessment, the Maracaibo-Catatumbo Basin was re-evaluated while new shale resource assessments were undertaken on the Middle Magdalena Valley and Llanos basins. Technically recoverable resources (TRR) of shale gas and shale oil in northern South America are estimated at approximately 222 Tcf and 20.2 billion bbl, Tables IV-1 and IV- 2. Colombia accounts for 6.8 billion barrels and 55 Tcf of risked TRR, while western Venezuela has 13.4 billion barrels and 167 Tcf. Eastern Venezuela may have additional potential but was not assessed due to lack of data. Colombia’s first publicly disclosed shale well logged 230 ft of over-pressured La Luna shale with average 14% porosity. -
The Permian Tiaraju Bivalve Assemblage
DOI: 10.1590/2317‑4889201720170013 ARTICLE The Permian Tiaraju bivalve assemblage, Passa Dois Group, southern Brazil: biostratigraphic and paleobiogeographic significance Assembleia de bivalves permianos de Tiaraju, Grupo Passa Dois, sul do Brasil: significado bioestratigráfico e paleobiogeográfico Marcello Guimarães Simões1*, Juliana Machado David2, Luiz Eduardo Anelli2, Carla Klein3, Suzana Aparecida Matos1, Vitor Bonatto Guerrini4, Lucas Veríssimo Warren4 ABSTRACT: Permian bivalves of the Paraná Basin evolved in a large RESUMO: Bivalves permianos da Bacia do Paraná evoluíram em inland sea, under conditions of extreme isolation and environmental um imenso mar interior, sob condições de extremo isolamento e estresse stress. Although known since 1918, its evolutionary history is still obs‑ ambiental. Embora conhecidos desde 1918, a história evolutiva desses cure due to the incomplete and biased information on faunal com‑ bivalves é ainda obscurecida pelo conhecimento incompleto e enviesado position and stratigraphic distribution of various assemblages. Hence, sobre a composição faunística e a distribuição estratigráfica de várias the description of the Tiaraju assemblage, the only known bivalve oc‑ assembleias. Portanto, a descrição da assembleia de Tiaraju, a única currence in the Passa Dois Group from the southernmost Brazil, adds conhecida no Grupo Passa Dois do sul do Brasil, contribui com novas new key information on the composition, biocorrelation and age of informações‑chave sobre a composição, biocorrelação e idade dessa this unique molluscan fauna. Terraia falconeri, Cowperesia emerita, Hol‑ fauna de moluscos únicos. Terraia falconeri, Cowperesia emerita, dhausiella elongata, and Terraia altissima were recorded and described. Holdhausiella elongata e Terraia altissima foram registradas e descritas. T. falconeri is the commonest species, followed by C. -
Do Trissico Superior Do Rio Grande Do
Ano 23 - Edição especial VI Simpósio Brasileiro de Paleontologia de Vertebrados Ribeirão Preto - Maio/2008 Paleontologia em Destaque. Edição Especial VI Simpósio Brasileiro de Paleontologia de Vertebrados Editores para esta edição especial: Max C. Langer, Jonathas S. Bittencourt e Mariela C. Castro Tiragem: 200 exemplares. Distribuídos em 27 de maio de 2008. Impressão: Gráfica Martingraf Endereço: Laboratório de Paleontologia, FFCLRP-USP. Av. Bandeirantes 3.900. 14040-901, Ribeirão Preto-SP E-mail: [email protected] Web: http://www.sbpbrasil.org/ Paleontologia em Destaque: boletim informativo da Sociedade Brasileira de Paleontologia. -- Vol. 1, no 1 (1984) - ISSN: 1516-1811 1. Geociências. 2. Paleontologia. 3. Sociedade Brasileira de Paleontologia SOCIEDADE BRASILEIRA DE PALEONTOLOGIA (GESTÃO 2007-2009) Presidente: João Carlos Coimbra (UFRGS) Vice-Presidente: Ana Maria Ribeiro (FZB/RS) 1° Secretário: Marina Bento Soares (UFRGS) 2ª Secretária: Soraia Girardi Bauermann (ULBRA) 1ª Tesoureira: Patrícia Hadler Rodrigues (FZB/RS) 2ª Tesoureira: Karin Elise Bohns Meyer (UFMG) Diretora de Publicações: Carla B. Kotzian (UFSM) 2 VI Simpósio Brasileiro de Paleontologia de Vertebrados Boletim de Resumos Editores Max C. Langer Jonathas S. Bittencourt Mariela C. Castro FFCLRP-USP, Ribeirão Preto-SP 2008 3 Logotipo: A concepção tripartida do logotipo do VI Simpósio Brasileiro de Paleontologia de Vertebrados reflete as três eras do Fanerozóico e suas denominações populares: Paleozóico ou “Era dos Peixes” (representado pelo tubarão Tribodus limae, apesar deste ser do Mesozóico), Mesozóico ou “Era dos Répteis” (representado pelo dinossauro Staurikosaurus pricei) e Cenozóico ou “Era dos Mamíferos” (representado pelo tigre dentes-de-sabre Smilodon populator). Ainda, os três táxons escolhidos são representativos dos, talvez, três mais importantes, ou ao menos mais famosos, depósitos fossilíferos contendo vertebrados no Brasil: a Formação Santana, Cretáceo inferior do sul do Ceará (representada por T. -
Callibrachion and Datheosaurus, Two Historical and Previously Mistaken Basal Caseasaurian Synapsids from Europe
Callibrachion and Datheosaurus, two historical and previously mistaken basal caseasaurian synapsids from Europe FREDERIK SPINDLER, JOCELYN FALCONNET, and JÖRG FRÖBISCH Spindler, F., Falconnet, J., and Fröbisch, J. 2016. Callibrachion and Datheosaurus, two historical and previously mis- taken basal caseasaurian synapsids from Europe. Acta Palaeontologica Polonica 61 (3): 597–616. This study represents a re-investigation of two historical fossil discoveries, Callibrachion gaudryi (Artinskian of France) and Datheosaurus macrourus (Gzhelian of Poland), that were originally classified as haptodontine-grade sphenaco- dontians and have been lately treated as nomina dubia. Both taxa are here identified as basal caseasaurs based on their overall proportions as well as dental and osteological characteristics that differentiate them from any other major syn- apsid subclade. As a result of poor preservation, no distinct autapomorphies can be recognized. However, our detailed investigations of the virtually complete skeletons in the light of recent progress in basal synapsid research allow a novel interpretation of their phylogenetic positions. Datheosaurus might represent an eothyridid or basal caseid. Callibrachion shares some similarities with the more derived North American genus Casea. These new observations on Datheosaurus and Callibrachion provide new insights into the early diversification of caseasaurs, reflecting an evolutionary stage that lacks spatulate teeth and broadened phalanges that are typical for other caseid species. Along with Eocasea, the former ghost lineage to the Late Pennsylvanian origin of Caseasauria is further closed. For the first time, the presence of basal caseasaurs in Europe is documented. Key words: Synapsida, Caseasauria, Carboniferous, Permian, Autun Basin, France, Intra-Sudetic Basin, Poland. Frederik Spindler [[email protected]], Dinosaurier-Park Altmühltal, Dinopark 1, 85095 Denkendorf, Germany. -
Appendix 1: Palaeontology of the Whitehill Formation, Loeriesfontein Area
APPENDIX 1: PALAEONTOLOGY OF THE WHITEHILL FORMATION, LOERIESFONTEIN AREA (Modified from an unpublished technical report by J.E. Almond (2008) for the Council for Geoscience, Pretoria, and to be incorporated into the geological sheet explanation for the 1: 250 000 geological map sheet 3018 Loeriesfontein. NB Full references will appear in this publication, and are not given here) Excellent exposures of carbon-rich mudrocks of the Whitehill Formation in the immediate vicinity of Loeriesfontein ( eg along the tar road to Nieuwoudtville) as well as at Ezelfontein to the northwest of town have yielded some of the most important assemblages of animal fossils known from the Ecca Group of the main Karoo Basin. These include mesosaurid reptiles, palaeoniscoid fish, pygocephalomorphic crustaceans, as well as rarer material of fossil wood, insects, trace fossils and palynomorphs ( eg Jubb & Gardiner 1975, Oelofsen 1981, 1987, Almond 1996, Visser 1992, 1994, Evans & Bender 1994, Evans 2005). The vertical zonation of fish, crustacean and mesosaurid fossils within the Whitehill succession at Loeriesfontein has been outlined by Oelofsen (1981, 1987), Visser (1992, 1994) and Evans (2005). The preservation and stability of fossil material from this area have often been enhanced by thermal metamorphism associated with nearby dolerite intrusions of Jurassic age. The prolific but low diversity Whitehill fossil biota strongly suggests that non-marine, brackish, freshwater or occasionally even hypersaline salinities prevailed in the basin at the time. This is supported by the local abundance in the middle and upper parts of the succession of pygocephalomorph crustaceans, a group that is typically (though not exclusively) associated with non-marine mudrocks (Gray 1988). -
Glossopteris Flora Nova Abordagem Para O Estudo Das Paleofloras Utilizando Sistemas De Informação Geográfica Aplicada a Flora Glossopteris
DOI: 10.5327/Z23174889201400040011 ARTICLE New approach for the study of paleofloras using geographical information systems applied to Glossopteris Flora Nova abordagem para o estudo das paleofloras utilizando sistemas de informação geográfica aplicada a Flora Glossopteris Isabel Cortez Christiano-de-Souza1*, Fresia Ricardi-Branco1, Adalene Moreira Silva2, Linda Gentry El Dash3, Rafael Souza Faria1 ABSTRACT: This paper introduces a methodology which makes RESUMO: O presente artigo introduz a uma metodologia na qual será possible the visualization of the spatial distribution of plant fossils possível a visualização da distribuição espacial de fitofósseis. Tal metod- and applies it to the occurrences of the Gondwana Floristic Province ologia será aplicada a ocorrências da Província Florística do Gondwana present on the eastern border of the Brazilian portion of the Paraná presente na borda leste da porção brasileira da Bacia do Paraná durante Basin during the Neopaleozoic. This province was chosen due to the o Neopaleozóico. Essa província foi escolhida tendo em vista que nela existence of a large number of publications referring to their occur- há grande número de publicações referentes às suas ocorrências. Isso tor- rence, so that a meta-analysis of their distribution could be based on na possível a meta-análise de sua distribuição, uma vez que há ampla ample information. The first step was the construction of a composite gama de informações. O primeiro passo foi a construção de uma base de database including geographical location, geology, and the botanical dados composta, incluindo localização geográfica, geologia e sistemática systematics of each relevant fossil. The geographical locations were botânica de cada fóssil de interesse. -
3D Implicit Modeling Applied to the Evaluation of CO2 Geological Storage in the Shales of the Irati Formation, Paraná Basin, Southeastern Brazil
3D implicit modeling applied to the evaluation of CO2 geological storage in the shales of the Irati Formation, Paraná Basin, Southeastern Brazil Saulo B. de Oliveira ( [email protected] ) Universidade de São Paulo Instituto de Energia e Meio Ambiente https://orcid.org/0000-0002-2149- 1297 Colombo C. G. Tassinari Universidade de Sao Paulo Instituto de Energia e Ambiente Richardson M. A-A. Universidade de Sao Paulo Instituto de Energia e Ambiente Ignacio Torresi Seequent Limited Research Article Keywords: CO2 geological storage, 3D geological modeling, carbon capture and storage, Irati Formation, Paraná Basin Posted Date: April 19th, 2021 DOI: https://doi.org/10.21203/rs.3.rs-420789/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Version of Record: A version of this preprint was published at Greenhouse Gases: Science and Technology on August 11th, 2021. See the published version at https://doi.org/10.1002/ghg.2111. Page 1/35 Abstract The Paris Agreement established global ambitious targets for reducing carbon dioxide (CO2) emissions, requiring the rapid and extensive development of low carbon technologies, and one of the most ecient is CO2 geological storage. Among the deep geological formations used for CO2 storage, the shale layers have been a new emerging topic showing to be ecient because they are abundant and have a high content of organic matter, being favorable for CO2 retention. However, one of the challenges in evaluating a location for possible reservoirs is the adequate geological characterization and storage volume estimates. This research evaluated the Irati Formation of the Paraná Basin, through the information from hydrocarbon exploration wells in Southeastern Brazil, where most stationary sources of carbon emissions are located. -
Permian Woods with Preserved Primary Structures from the Southeast of Brazil (Irati Formation, Paraná Basin)
Palaeobio Palaeoenv (2018) 98:385–401 https://doi.org/10.1007/s12549-018-0320-9 ORIGINAL PAPER Permian woods with preserved primary structures from the southeast of Brazil (Irati Formation, Paraná basin) Rafael Souza Faria1 & Fresia Ricardi-Branco1 & Rosemarie Rohn2 & Marcelo Adorna Fernandes3 & Isabel Christiano-De-Souza1 Received: 11 September 2017 /Revised: 27 November 2017 /Accepted: 6 February 2018 /Published online: 24 March 2018 # Senckenberg Gesellschaft für Naturforschung and Springer-Verlag GmbH Germany, part of Springer Nature 2018 Abstract This research described fossil woods with pre- non-contiguous pits (abietoid vascular rays). Xeromorphic served pith and primary xylem from strata of the Irati features observed in these specimens, such as a pith with Formation (Artinskian) of the Paraná Basin (southeastern groups of sclereids and false growth rings, may be related to Brazil). The three specimens studied are all related to the the depositional environment of the Irati Formation. The Coniferales and include the following taxa: Solenopitys specific factor triggering the xeromorphy has not yet been paulistana Kräusel, Atlanticoxylon ibiratinum n. sp. and determined, but the present study corroborates clearly the Abietopitys sp. Kräusel. Solenopitys paulistana represents sedimentary evidence of dry conditions during the deposi- a species with a solid, heterocellular pith with a peripheral tion of the Irati Formation, as seen in the 30-m-thick car- secretory canal system. Atlanticoxylon ibiratinum n. sp. has bonate layer extending through four South American a lacunose, heterocelular pith with Bnests^ of sclereids, with countries. a central secretory canal and a peripheral system of canals. Abietopitys sp. has a solid, lobed, homocelular pith associ- Keywords Fossil wood .