DOCSLIB.ORG

Caputo, M, 1984

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Caputo, M, 1984 UNIVERSITY OF CALIFORNIA Stratigraphy, Tectonics, Paleoclimatology and Paleogeography of Northern Basins of Brazil A Dissertation submitted in partial satisfaction of the requirements of the degree of Doctor of Philosophy in Geology by Mario VicenteCaputo Committee in charge: Professor John C. Crowell, Chairman Professor James R. Boles Professor Richard Y. Fisher Professor Knut Bjorlykke, University of Bergen, Bergen, Norway Professor Antonio A. Rocha-Campos, University of São Paulo, Brazil Professor Rodi A. Medeiros, Petroleo Brasileiro S.A.· February 1984 The dissertation of Mario Vicente Caputo Is approved: February 1984 ii February 15, 1984 Copyright by Mario Vicente Caputo 1984 iii ACKNOWLEDGEMENTS I wish to express on, deep appreciation to all those individuals whose suggestions, criticism, encouragement and support have made this study possible. I am most grateful to Petróleo Brasileiro S. A. Petrobras (Brazilian State Oil Company), especially to Carlos Walter· Marinho Campos (member of the Board of Directors of Petrobras) for his constant support to this research project, and for making unpublished data from Petrobras files available for this broad study. Appreciation is also expressed to Raul Mosmann (General Manager·of the Department of Exploration), Raymundo Ruy Bahia (Manager·of Exploration of the Northern Exploration District) and Jeconias Queiroz (General Chief of Geologic Operations) who allowed me to develop this study. I wish to express my sincere gratitude to Dr. John C. Crowell for his guidance and counsel which at times went above and beyond his duty of advising Professor. Formal recognition is given to Drs. James R. Boles, Knut Bjorlykke and Richard V. Fisher for their· friendship and generous allocation of time whenever called upon. I desire to express my appreciation to Frederico Waldemar Lange for his comments and insights which improved the English text. Finally, I wish to express my deepest gratitude to my parents, Pedro and Zelinda and wife Maria da Glor·ia, who have ever been a source of inspiration and renewed strength. To them this study is dedicated. iv VITA March 4, 1938 – Born – Santana do Livramento, R.S.,Brazil 1961 - B.A., Universidade Federal do Rio Grande do Sul, Brazil. 1962-1983 – Oil geologist at Petróleo Brasileiro, S.A. (Petrobras). PUBLICATIONS Caputo,M. V., 1971. Nomenclatura estratigráfica da Bacia do Amazonas – Histórico e atualização. Soc. Bras. Geol., An. XXXVI Congres. Bras. Geol., V. 3, p. 35-46 (with R. Rodrigues and D. N. N. Vasconcelos). Caputo, M, V., and Crowell, J. C., 1984. Migration of glacial centers across Gondwana during Paleozoic era. Geol. Soc. of Am. Bull. (in press). Caputo, M. V., 1984. Late Devonian glaciation in South America. Special issue. Palaeogeography, Palaeoclimatology and Palaeoecology (in press). v ABSTRACT Stratigraphy, Tectonics, Paleoclimatology and Paleogeography of Northern Basins of Brazil by Mário Vicente Caputo Paleozoic basins in northern Brazil contain thick sequences of sedimentary rocks, including diamictites. Because several different geological environments may generate diamictites a study of tec­ tonism, stratigraphy, paleoclimatology and paleogeography was made in order to deduce the processes involved in their origin. A large part of northern Brazil strata is underlain by metavolcanic and metasedimentary sequences steeply folded and metamorphosed during many tectonic events from about 3,600 to 1,000 m.y. ago. Northeast Brazil was also affected by the Brazilian tectonic cycle from about 700 to 450 m.y. ago. The pre-basin weak zones and resulting trends are responsible for the shape and geometry of 3 huge intracratonic basins developed during Paleozoic time: the Solimões, Amazonas and Parnaíba basins. The three basins had a similar geologic development during Paleozoic times; from Ordovician to Early Carboniferous time only clastic rocks were deposited, and from Late Carboniferous to Permian time carbonate and evaporites were also laid down. Tectonism that affected basins is related to uplift and collapse vi that preceded the break up of Pangea and subduction activity along the Solimões Basin, in the western side of the South American continent. Climate· has influenced the characteristics of each formation. Paleolatitudes based on paleoclimatic indicators such as tillites, eolian sands, coal, bauxite, red beds, evaporites, limestone, fauna and flora, changed from polar and circumpolar to equatorial during Phanerozoic times. Glaciation was recorded in Ordovician-Silurian, Late Devonian and Early Carboniferous times. A Late Devonian glaciation left a clear imprint as shown by sedimentary facies. Diamictites with striated, faceted and polished pebbles; rhythmites with dropstones; erratic boulders; striated pave­ ments and deformed sandstones document glacial conditions. Study of the migration of glacial centers based on the available literature and new data from Brazil shows that they closely follow published paleomagnetic wander data and that there is a close rela­ tionship between all Paleozoic glaciations and the Brazilian gla­ ciations. Ice centers moved from northern Africa to southwestern South America from Late Ordovician to Early Silurian time. From Mid-Silurian to early Late Devonian time no record of glaciation is known. In Late Devonian time intermittent glaciation initiated again in central South America and, from Late Devonian to Late Permian time ice centers migrated toward Antarctica across South America and South Africa. The Devonian and Ordovician-Silurian glaciations together vii with the Permo-Carboniferous glaciations may all have primarily resulted from the shifting position of the Gondwana continent with respect to the South Pole. viii TABLE OF CONTENTS Page ACKNOWLEDGEMENTS …………………………………..…………………………………………….iv VITA, PUBLICATIONS…..……………………………………………………….v ABSTRACT………………………………………………………………………….vi LIST OF FIGURES.….……………………..………….………………………….…xiv PHOTO CAPTIONS……….…………………………………………………………………………xix CHAPTER 1. INTRODUCTION ………………………………………………….…………….………1 Scope and Methods of Study ………………………………………………...5 CHAPTER 2. CRITERIA FOR PALEOCLIMATIC STUDIES………..…………….8 Limestone………………………………………………………………………10 Evaporites………………………………………………………………………14 Red Beds……………………………………………………………………….18 Bauxite………………………………………………………………………….19 Coal……………………………………………………………………………..22 Aeolian Sands………………………………………………………………….24 Tilites………………………………………………………….………………...26 CHAPTER 3. CRITERIA FOR THE IDENTIFICATION OF GLACIGENIC DEPOSITS…………………………………………….…………………..30 Direct Evidence for Glaciation………………………………………………....34 Pavement and Boulder Pavement……………………………………...36 Striations and Related Features………………………………....….36 Periglacial Deposits……………………………………………….….......37 Glacio Marine Deposts…………………………………………..............38 Dropstones………………………………………………………..............40 Patterned Ground and Other Features…………………………….…...41 Indirect Evidence for Glaciation……………………………………………….…44 Loess………………………………………………….……………….……44 Regressions and Transgressions………………………………………....46 Massive Biotic Extinction…………………………………………………...46 Paleogeographic Reconstruction……….…………………………………47 Paleomagnetic Data………………………………………………………...48 CHAPTER 4. TECTONIC DEVELOPMENT OF SOUTH AMERICA FROM EARLY PRECAMBRIAN TO ORDOVICIAN TIME…………..……….…49 Amazonian Platform………………………………………………………….......53 Central Amazonian Province…………………………………….………...58 Maroni-Itacaiunas Fold Belt…………………………………….……….…59 ix Central Guyana Fold Belt……………………………………….…………….62 Rio Negro –Juruena Fold Belt………………………………………………..62 Rondonian Fold Belt…………………………………………………………...63 Brazilian Platform……………………………………………………….…………....67 Araguaia Fold Belt…………………………………………………………… ..68 Araioses Fold Belt…..................................................................................72 São Luís Craton.........................................................................................74 Goiás Massif..............................................................................................75 Brasilia Fold Belt........................................................................................76 São Francisco Craton................................................................................77 Ribeira and Própria Fold Belts...................................................................78 Plate Tectonics VS. Ensialic Tectonics……………………………………….......82 CHAPTER 5. ORIGIN AND DEVELOPMENT Of NORTHERN BRAZILIAN BASINS..89 Basic Concepts……………………………………………………………….89 Origin of the basins………………..………………………………..………..91 Basin Amplification……………………………………………………….…..96 CHAPTER 6. GENERAL REMARKS ON STRATIGRAPHY………….……………….99 CHAPTER 7. PIMENTA BUENO BASIN…………..………………..……….………....110 Pimenta Bueno Formation……………………………………………….....112 Unnamed Formation..............................................................................118 Fazenda da Casa Branca Formation......................................................118 Anari Basalt............................................................................................122 Botucatu Formation................................................................................122 Parecis Formation..................................................................................124 CHAPTER 8. SOLIMÕES BASIN………………………………………………………...126 Uatumã Group…………………………........…………………………….…….....128 Prosperança Formation………….......................................................130 Jutaí Formation..................................................................................134 Juruá Formation.................................................................................138
Load more

Recommended publications
  • The Brazilian Cretaceous
    © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zobodat.at in Zitteliana 10 277-283 München, I. Juli I983 ISSN 0373-9627 The Brazilian Cretaceous By IGNACIO MACHADO BRITO & DIÓGENES dc ALMEIDA CAMEOS*) With I text figure and 1 plate ABSTRACT The Cretaceous is one of the best known systems in Brazil, Owing to the impossibility of correlating the three first being very well represented in the basins of the Northeast, on phases with the international stratigraphic column, we here the continental shelf and covering the large palaeozoic basins. propose to them local stages which could also be identified on The system is presented in its most complete form on the the African Atlantic coastal basins: Donjoanian, Bahian and coastal and interior basins of the Northeast, since the Jura- Alagoan. Cretaceous transition until the Maastrichtian-Tertiary. The marine phase can be recognized since the Upper Aptian It can be divided into four phases: continental or prerift, la­ and it is almost perfectly correlated to the standard geological custrine or rift, transitional or saline, and marine. column. KURZFASSUNG Die Kreide ist eines der bestuntersuchten Systeme in Brasi­ „rifting“, Ubergangsphase oder brackisch salinar und voll­ lien; sie ist verbreitet in den Becken Nordost-Brasiliens und marine Phase. Da die ersten 3 Phasen nicht international zu auf dem Schelf. Am vollständigsten ist sie vertreten von der korrelieren sind, werden 3 lokale Einheiten benannt und defi­ Jura/Kreidc-Cirenze bis zur Maastricht/Tertiär-Grenze in niert, die sich auch in den westafrikanischen atlantischen Kü­ den Küstenbecken und den im Landesinnem gelegenen Bck- stenbecken erkennen lassen: Donjoanian, Bahian und Alago­ ken die Nordost-Brasilien repräsentieren.
    [Show full text]
  • Abstracts (Pdf)
    63RD SYMPOSIUM FOR VERTEBRATE PALAEONTOLOGY AND COMPARATIVE ANATOMY & 24TH SYMPOSIUM OF PALAEONTOLOGICAL PREPARATION AND CONSERVATION WITH THE GEOLOGICAL CURATORS’ GROUP 1 CONTENTS Meeting Schedule 4 Abstracts SPPC talks 10 SVPCA talks 14 SVPCA posters 78 Delegate List 112 2 ACKNOWLEDGEMENTS The organisers would like to thank the Palaeontological Association for their support of this meeting, and also for their continued management of the Jones Fenleigh Memorial Fund. A huge amount of the work putting the meeting together was co-ordinated by Mark Young, including editing this Abstract volume, handling abstract submissions and overall organisation. We also thank Stu Pond and Jessica Lawrence Wujek for designing this year's SVPCA logo. Liz Martin-Silverstone and Jessica Lawrence Wujek co-ordinated most of the behind-the- scenes management for this meeting while Stu Pond designed this year’s Conference circulars. Our logo represents a local fossil, Polacanthus from the Isle of Wight (based on a fossil collected by Martin Simpson and Lyn Spearpoint). Finally, we thank Richard Forrest for working on the website and providing general information and support. This year’s meetings are supported by the Hampshire Cultural Trust, Dinosaur Isle, Geological Curators Group, Siri Scientific Press, Palaeocast and Frontiers in Earth Science. HOST COMMITTEE Ocean and Earth Science, University of Southampton, National Oceanography Centre Gareth Dyke John Marshall Darren Naish Mark Young Jessica Lawrence Wujek Liz Martin-Silverstone Stu Pond Aubrey Roberts James Hansford Hampshire Cultural Trust Christine Taylor Dinosaur Isle Gary Blackwell Geological Curator's Group Kathryn Riddington 3 MEETING SCHEDULE Monday 31st August 9:00-9:45 SPPC/GCG registration at NOC Security desk (4th floor) Session — SPPC Chair — Mark Young 10:00-10:20 Mark Graham Fossils, Footprints & Fakes 10:20-10:40 Emma Bernard A brief history of the best collection of fossil fish in the world – probably… 10:40-11:00 Jeff Liston et al.
    [Show full text]
  • 3 86-Itapecuruemys.Pdf
    Journal of South American Earth Sciences xxx (xxxx) xxx Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames A new Cretaceous Pleurodira Pelomedusoides from the Lower Cretaceous of Parnaíba Basin, Brazil Diogo Lins Batista a,b,*, Ismar de Souza Carvalho b, Marcelo S. de la Fuente c a Universidade Federal do Rio de Janeiro, Instituto de Biologia, Programa de Pos-Graduaç´ ao~ em Biodiversidade e Biologia Evolutiva, Interbloco B/C, Av. Carlos Chagas Filho, 373, Cidade Universitaria,´ Ilha do Fundao,~ Rio de Janeiro, RJ, Brazil b Universidade Federal do Rio de Janeiro, Instituto de Geoci^encias, Departamento de Geologia, Laboratorio´ de Estudos Paleontologicos,´ Av. Athos da Silveira Ramos 274, Cidade Universitaria,´ Ilha do Fundao,~ Rio de Janeiro, RJ, Brazil c Instituto de Evolucion,´ Ecología Historica´ y Ambiente (IDEVEA-CONICET-Universidad Tecnologica´ Nacional, Facultad Regional San Rafael, Calle Urquiza 314, 5600, San Rafael, Provincia de Mendoza, Argentina ARTICLE INFO ABSTRACT Keywords: The new Pleurodira turtle Itapecuruemys amazonensis gen. et sp. nov. from the Itapecuru Formation (Parnaíba Pleurodira Basin, Brazil) is described. The new species is represented only by its holotype, which consists of an almost Pelomedusoides complete carapace and plastron, with an oval-shaped outline. The most peculiar characters of Itapecuruemys Lower Cretaceous amazonensis are: neural plates six and seven are separated by costal six, and the seventh neural plate contacts the Parnaíba basin sixth, seventh and eighth costal plates and a suprapygal. The phylogenetic hypothesis proposed in this paper Brazil suggests that Itapecuruemys amazonensis, together with Cearachelys and Galianemys spp., form a monophyletic assemblage and also widen the paleoherpetological diversity of the Itapecuru Formation in the Parnaíba Basin (Brazil).
    [Show full text]
  • Accraian Series, 352-354 Acre Series, 55 Acre Subbasin, 32 A<;:U
    INDEX A Andrelandia Series, 431 Accraian Series, 352-354 AnnobonI~and,530-531 Acre Series, 55 Antarctic Peninsula, 210 Acre subbasin, 32 Anwiafutu Limestone, 361 A<;:u Formation, 122 Apollonian System, 361 A<;:ungui group, 433 Apora high, 92 Adamaoua Belt, 375 Aptian, 12, 14,94,98,104,109,118,191, massif, 385 201,306,307,308,320,329 Adolphskraa1 Shale, 268 Argentine Adrar succession, 466 continental platform, 136-139 Agoula River series, 315 - 316 marginal basins Agua Bonita graben, 37 basement ridge, 143-145 Agulhas basin, 264 Cretaceous units, 152-155 Agwu Shales, 364 general geology, 139-162 Ahlmannrygg Group, 226, 227 geologie development, 162-163 Ajua Shales, 354 post-Upper Jurassie sediments, 145-152 Akawaian episode, 395 pre-Upper Jurassie basement, 140-152 Alagoas graben, 95, 98 structurallineaments, 158-162 Albian, 14,94,98,108,118,119,309,312, tectonics, 160-162 320,329,358-359,373 Tertiary, 155-158 Alian<;:a Formation, 94, 98 Argiles du bas fleuve, 330 Alter do Chäo Formation, 57 Arufu Limestone, 359 Amapa Series, 395 Ascension Island, 539, 540, 542, 543 Amazon basin, 30-31 analyses, 500 Carboniferous,48-54 geology, 497 -499 Devonian sedimentation, 45-49 petrology, geochemistry, 499-501 igneous rocks, 69-74 sedimentation history ,74-79 Assabu sandstone, 465 structural pattern, 32-37 Asu River Group, 359 tectonic activity, 40 Atlantic Ameki Formation, 368 high, 118 Amelang Formation, 232, 233 highland, 253 Amsaga Series, 466, 468 Awaga Series, 320 Anambra embayment, 384 Azile Series, 321 575 576 Index B C Badagba quartzite, 474,
    [Show full text]
  • See in English
    SIGEP Geological and Paleontological Sites of Brazil SIGEP 013 Ichnofossils of the Porto Primavera Power Plant, State of São Paulo Dinosaur and mammal footprints in rocks from the Caiuá neocretaceous desert Luiz Alberto Fernandes 1 Fernando Antonio Sedor 2 Rafael Costa da Silva 3 Luiz Roberto da Silva 4 Adalberto Aurélio Azevedo 5 Alessandra Gonçalves Siqueira 6 1 Universidade Federal do Paraná - Depto. de Geologia/Caixa Postal 19.001/CEP 81531-990, Curitiba, Paraná/e-mail: [email protected] 2 Universidade Federal do Paraná - Museu de Ciências Naturais/e-mail: [email protected] 3 Companhia de Pesquisa de Recursos Minerais/RJ-DEGEO/DIPALE/e-mail: [email protected] 4 Companhia Energética de São Paulo – CESP/e-mail: [email protected] 5 Instituto de Pesquisas Tecnológicas do Estado de São Paulo S/A – IPT/e-mail: [email protected] 6 Instituto de Pesquisas Tecnológicas do Estado de São Paulo S/A – IPT/e.mail: [email protected] © Fernandes,L.A.; Sedor,F.A.; Silva,R.C.; Silva,L.R.; Azevedo,A.A.; Siqueira,A.G. 2008. Ichnofossils of the Porto Primavera Power Plant, State of São Paulo - Dinosaur and mammal footprints in rocks from the Caiuá neocretaceous desert. In: Winge,M.; Schobbenhaus,C.; Souza,C.R.G.; Fernandes,A.C.S.; Berbert-Born,M.; Queiroz,E.T.; (Edit.) Sítios Geológicos e Paleontológicos do Brasil. Available on line since 26/09/2008 at the address: http://www.unb.br/ig/sigep/sitio013/sitio013english.pdf [actually http://www.sigep.cprm.gov.br/sitio013/sitio013english.pdf] (The above bibliographic reference of author copy
    [Show full text]
  • Abstracts Volume
    63RD SYMPOSIUM FOR VERTEBRATE PALAEONTOLOGY AND COMPARATIVE ANATOMY & 24TH SYMPOSIUM OF PALAEONTOLOGICAL PREPARATION AND CONSERVATION WITH THE GEOLOGICAL CURATORS’ GROUP 1 CONTENTS Meeting Schedule 4 Abstracts SPPC talks 10 SVPCA talks 14 SVPCA posters 78 Delegate List 112 2 ACKNOWLEDGEMENTS The organisers would like to thank the Palaeontological Association for their support of this meeting, and also for their continued management of the Jones Fenleigh Memorial Fund. A huge amount of the work putting the meeting together was co-ordinated by Mark Young, including editing this Abstract volume, handling abstract submissions and overall organisation. We also thank Stu Pond and Jessica Lawrence Wujek for designing this year's SVPCA logo. Liz Martin-Silverstone and Jessica Lawrence Wujek co-ordinated most of the behind-the- scenes management for this meeting while Stu Pond designed this year’s Conference circulars. Our logo represents a local fossil, Polacanthus from the Isle of Wight (based on a fossil collected by Martin Simpson and Lyn Spearpoint). Finally, we thank Richard Forrest for working on the website and providing general information and support. This year’s meetings are supported by the Hampshire Cultural Trust, Dinosaur Isle, Geological Curators Group, Siri Scientific Press, Palaeocast and Frontiers in Earth Science. HOST COMMITTEE Ocean and Earth Science, University of Southampton, National Oceanography Centre Gareth Dyke John Marshall Darren Naish Mark Young Jessica Lawrence Wujek Liz Martin-Silverstone Stu Pond Aubrey Roberts James Hansford Hampshire Cultural Trust Christine Taylor Dinosaur Isle Gary Blackwell Geological Curator's Group Kathryn Riddington 3 MEETING SCHEDULE Monday 31st August 9:00-9:45 SPPC/GCG registration at NOC Security desk (4th floor) Session — SPPC Chair — Mark Young 10:00-10:20 Mark Graham Fossils, Footprints & Fakes 10:20-10:40 Emma Bernard A brief history of the best collection of fossil fish in the world – probably… 10:40-11:00 Jeff Liston et al.
    [Show full text]
  • Geoconservation of the Paleontological
    Environmental Earth Sciences (2019) 78:707 https://doi.org/10.1007/s12665-019-8722-1 ORIGINAL ARTICLE Geoconservation of the paleontological heritage of the geosite of dinosaur footprints (sauropods) in the locality of São Domingos, municipality of Itaguatins, state of Tocantins, Brazil R. F. Lopes1 · C. R. A. Candeiro2 · S. de Valais3 Received: 7 June 2019 / Accepted: 25 November 2019 © Springer-Verlag GmbH Germany, part of Springer Nature 2019 Abstract The present study aimed at performing a quantitative evaluation to propose a geoconservation plan to the São Domingos geosite, and, therefore, to contribute with feasible actions, to the preservation of this paleontological heritage. The study area is located in the district in the Itaguatins municipality, northern Tocantins state, Brazil. The studied geosite is characterized by the presence of track fossils. The tracks have been assigned to herbivorous dinosaurs, basal sauropods, which were living in the area during the frst periods of the Cretaceous. The following aspects were quantitatively evaluated: risk of degrada- tion and potential for the educational and touristic use of the area. All these aspects were quantitatively evaluated with the methodology described in the app web GEOSSIT, administered by the Companhia de Pesquisa de Recursos Minerais. The São Domingos geosite has a high scientifc value, with a national relevance, a moderate potential of educational use, a low potential of tourist use, and a high risk of degradation. The site, with interest and paleontological value, has the potential to be used in all level educational activities at, and it is important it should be used for such activities. The elements of the geosite are currently in an advanced degree of degradation, and urgent measures are required to mitigate the erosive activi- ties that afect the footprint-bearing surfaces and that gradually increase their erosion.
    [Show full text]
  • The Paleontological Heritage of Northern Tocantins State and Southwest Maranhão State, Brazil: a Preliminary Synthesis
    DOI: 10.5212/TerraPlural.v.15.2117157.019 The Paleontological Heritage of Northern Tocantins State and Southwest Maranhão State, Brazil: a Preliminary Synthesis O patrimônio paleontológico do norte do estado do Tocantins e sudoeste do Maranhão, Brasil: uma síntese preliminar El patrimonio paleontológico del norte del estado de Tocantins y suroeste de Maranhão, Brasil: una síntesis preliminar Raylon da Frota Lopes https://orcid.org/0000-0002-1715-0975 [email protected] Universidade Federal de Goiás, UFG, Goiânia, GO Claudia Valéria de Lima https://orcid.org/0000-0001-9991-2541 [email protected] Universidade Federal de Goiás, UFG, Goiânia, GO Carlos Roberto A. Candeiro https://orcid.org/0000-0002-8128-4660 [email protected] Universidade Federal de Goiás, UFG, Aparecida de Goiânia, GO Abstract: This paper aims to present a preliminary synthesis of the Paleontological Heritage of northern Tocantins State and southwest Maranhão State. It is a compound mainly from Paleozoic and Mesozoic rocks of the intracratonic Parnaíba Basin. Fossils from these regions include body fossils of sharks, gymnosperm trunks, mineralized ferns, ichnofossils of sauropods and theropods, and indeterminate leaf molds. Keywords: Geodiversity, Parnaíba Basin, fossiliferous survey. Resumo: Este artigo visa apresentar uma síntese preliminar do patrimônio paleontológico da região norte do estado do Tocantins e sudoeste do Maranhão, proveniente, em sua maioria de rochas com gênese no Paleozoico e Mesozoico da Bacia Intracratônica do Parnaíba. Os fósseis consistem em somatofósseis de tubarões, troncos de gimnospermas, e samambaias mineralizados, icnofósseis de saurópodes e terópodes, e moldes de folhas indeterminados. Palavras-chave: Geodiversidade, Bacia do Parnaíba, levantamento fossílífero. Resumen: Este trabajo tiene como objetivo presentar una síntesis preliminar del patrimonio paleontológico de la región norte del estado de Tocantins y suroeste Terr@Plural, Ponta Grossa, v.15, p.
    [Show full text]
  • Report on the Upper Permian and Lower Cretaceous Fossiliferous Localities Vertebrates-Bearing in the Central- North of Tocantins State, Brazil
    Brazilian Geographical Journal: Geosciences and Humanities research medium, Uberlândia, v. 1, n. 2, p. 372-386, jul./dec. 2010 Brazilian Geographical Journal: Geosciences and Humanities research medium UFU ARTICLES /A RTIGOS /A RTÍCULOS /A RTICLES Report on the Upper Permian and Lower Cretaceous fossiliferous localities vertebrates-bearing in the central- north of Tocantins State, Brazil Master Student Yuri Modesto Alves Programa de Pós-Graduação em Geologia, Departamento de Geologia, Universidade Federal do Rio de Janeiro E-mail: [email protected] ABSTRACT ARTICLE HISTORY Since the second half of the last century, fossils of vertebrates have been encountered in the Balsas and Mearim group in the center north area of the State of KEY WORDS : Tocantins Tocantins, Parnaiba Basin. The Pedra de Fogo and Pedra de Fogo Formation Corda formations compose these unities respectively Corda Formation and their respective ages are dated as Upper Permian Fossil Vertebrates and Lower Cretaceous in age. Upper Permian and Lower Cretaceous vertebrates were recovered in the municipalities of Filadélfia (1), Barra do Ouro, Received: 09 December 2010 Filadélfia (2), Guaraí and Itaguatins. This fauna Accepeted: 24 December 2010 consists essentially of fragments (scales, spines, teeth, etc.) of paleonisciforms, elasmobranches, coelacantids and one sauropod dinosaur ichnofossil. All, with the exception of the sauropod and the municipality of Itaguatins, are outercroppings of the Trisidela Member (Pedra de Fogo Formation). RESUMO – NOTA SOBRE AS LOCALIDADES PALAVRAS CHAVE : FOSSILÍFERAS PORTADORAS DE VERTEBRADOS DO Tocantins PERMIANO SUPERIOR E CRETÁCEO INFERIOR DA REGIÃO Formação Pedra de Fogo CENTRO -NORTE DO ESTADO DO TOCANTINS , BRASIL . Formação Corda Desde a segunda metade do século passado, fósseis de Vertebrados fósseis vertebrados têm sido encontradas em rochas dos grupos Balsas e Mearim, porção centro norte do estado do Tocantins, Bacia do Parnaíba.
    [Show full text]
  • The Petroleum Resource Potential of Brazil
    The Petroleum Resource Potential of Brazil Table of Contents Page EXECUTIVE SUMMARY ................................................................... 1-1 TABLE OF CONTENTS .................................................................... 2-1 INTRODUCTION ........................................................................... 3-1 OBJECTIVES AND BACKGROUND OF STUDY .................................... 3-1 SOURCE OF DATA AND LIMITATIONS ............................................ 3-2 METHODOLOGY .................................................................... 3-3 MANNER OF PRESENTATION ..................................................... 3-4 ACKNOWLEDGMENTS ............................................................. 3-6 REGIONAL OVERVIEW .................................................................... 4-1 PHYSIOGRAPHY OF BRAZIL’S CONTINENTAL MARGIN ........................ 4-1 TECTONIC AND STRATIGRAPHIC EVOLUTION OF BRAZIL’S CONTINENTAL MARGIN ........................................................... 4-1 Pre-Rift History ........................................................... 4-6 Rift Stage (Non-Marine) .................................................. 4-6 Transitional Stage ........................................................ 4-8 Drift Stage (Marine) ...................................................... 4-8 STRUCTURAL FRAMEWORK OF BRAZIL’S MARGINAL BASINS ................. 4-10 AFRICAN ANALOGS TO BRAZILIAN MARGINAL BASINS ........................ 4-13 IVORY COAST ANALOGS .........................................................
    [Show full text]
  • Ichthyofauna from the Codó Formation, Lower Cretaceous (Aptian, Parnaíba Basin), Northeastern Brazil and Their Paleobiogeographical and Paleoecological Significance
    Palaeogeography, Palaeoclimatology, Palaeoecology 447 (2016) 53–64 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Ichthyofauna from the Codó Formation, Lower Cretaceous (Aptian, Parnaíba Basin), Northeastern Brazil and their paleobiogeographical and paleoecological significance Rafael Matos Lindoso a,⁎, John Graham Maisey b, Ismar de Souza Carvalho a a Universidade Federal do Rio de Janeiro, Departamento de Geologia, CCMN/IGEO, RJ 21, 949-900 Cidade Universitária-Ilha do Fundão, Rio de Janeiro, Brazil b Department of Vertebrate Paleontology, American Museum of Natural History, 79St. & Central Park West, New York, NY 10024, USA article info abstract Article history: Although fossils from the Codó Formation have been known for over seventy years, their abundance and biotic Received 13 October 2015 diversity have only recently become better understood. Numerous specimens of fossil fishes have been collected Received in revised form 28 January 2016 at new localities in Brejo municipality, Northeastern Brazil, and are interpreted here in the light of evidence for an Accepted 29 January 2016 epicontinental seaway extending from the Equatorial Atlantic (Tethys Ocean). Similarities are noted among fossil Available online 6 February 2016 fish assemblages from the Codó, Santana and Riachuelo formations, which suggests connections (perhaps inter- – Keywords: mittent) between the Parnaíba, Araripe and Sergipe-Alagoas basins during the Early Cretaceous (Aptian
    [Show full text]
  • Early- and Mid-Cretaceous Archosaur Localities of North-Central Texas
    Early- and Mid-Cretaceous Archosaur Localities of North-Central Texas Guidebook for the field trip held October 13, 2015 in conjunction with the 75th Annual Meeting of the Society of Vertebrate Paleontology in Dallas, Texas Field Trip Leaders: Thomas Adams, Witte Museum James Farlow, Indiana University–Purdue University Fort Wayne Christopher Noto, University of Wisconsin–Parkside Christopher Strganac, Perot Museum of Nature and Science Christopher Noto, Editor 2015 © 2015 by the authors using a Creative Commons Attribution-Non Commercial-No Derivatives 4.0 International License Early- and Mid-Cretaceous Archosaur Localities of North-Central Texas, SVP 2015 Meeting Field Trip Guidebook TABLE OF CONTENTS FIELD TRIP OVERVIEW 2 Christopher Strganac STOP 1 ARCHOSAURS OF THE LOWER CRETACEOUS TRINITY GROUP OF CENTRAL AND NORTH CENTRAL TEXAS WITH A STOP AT THE JONES 5 RANCH QUARRY Thomas L. Adams STOP 2 DINOSAUR FOOTPRINTS FROM THE GLEN ROSE FORMATION (PALUXY RIVER, DINOSAUR VALLEY STATE PARK, SOMERVELL COUNTY, 14 TEXAS) James O. Farlow, Karl T. Bates, Rena M. Bonem, Benjamin F. Dattilo, Peter L. Falkingham, Raymond Gildner, Jerry Jacene, Glen J. Kuban, Anthony J. Martin, Mike O’Brien, James Whitcraft STOPS 3 and 4 38 ARCHOSAUR FOSSIL LOCALITIES IN THE WOODBINE FORMATION (CENOMANIAN) OF NORTH CENTRAL TEXAS Christopher R. Noto Cover Image: Reconstruction of possible Paluxy River trackmakers from Dinosaur Valley State Park, based on Paluxysaurus and Acrocanthosaurus. Artwork by Mike O’Brien. Early- and Mid-Cretaceous Archosaur Localities of North-Central Texas, SVP 2015 Meeting Field Trip Guidebook ACKNOWLEDGMENTS We are grateful to William R. (Bill) and Dacie Jones for their gracious hospitality and allowing access to their ranch.
    [Show full text]