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Morfologia Pós-Craniana De Candidodon Itapecuruense (Crocodylomorpha, Mesoeucrocodylia), Do Cretáceo Do Brasil
Revista Brasileira de Paleontologia 7(1):87-92, Janeiro/Junho 2004 © 2004 by the Sociedade Brasileira de Paleontologia MORFOLOGIA PÓS-CRANIANA DE CANDIDODON ITAPECURUENSE (CROCODYLOMORPHA, MESOEUCROCODYLIA), DO CRETÁCEO DO BRASIL PEDRO HENRIQUE NOBRE Depto. de Geologia, UFRJ, Av. Brigadeiro Trompowski, s/nº, Ilha do Fundão, 21.949-900, RJ, Brasil. [email protected] RESUMO – Candidodon itapecuruense Carvalho & Campos é um Mesoeucrocodylia, proveniente da Formação Itapecuru (Cretáceo Inferior), bacia do Parnaíba, Brasil. Esta espécie caracteriza-se por apresentar dentes de morfologia complexa, com uma cúspide principal e uma série de cúspides menores na base da coroa. São apresentados novos elementos referentes ao esqueleto pós-craniano de C. itapecuruense, bem como suas relações com outros Crocodylomorpha. O esqueleto pós-craniano de C. itapecuruense apresenta vértebras anficélicas com o corpo arredondado a levemente quadrangular. O úmero é alongado, cilíndrico e com uma crista deltopeitoral pronunciada. O fêmur é estreito, com a diáfise cilíndrica e reta. Os metatarsais são longos, delgados e com as extremidades pouco expandidas. Apresenta osteodermos muito delgados, de contorno quadrangular a cordiforme não ultrapassando 1mm de espessura, sendo a superfície interna lisa e a externa ornamentada com rugosidades e depressões irregulares. Em todos os osteodermos observa-se, na superfície externa, uma crista localizada no terço posterior da peça. Palavras-chave: Crocodylomorpha, Mesoeucrocodylia, Cretáceo Inferior, bacia do Parnaíba. Abstract – THE POSTCRANIAL MORPHOLOGY OF CANDIDODON ITAPECURUENSE (CROCODYLO- MORPHA, MESOEUCROCODYLIA), CRETACEOUS, OF BRAZIL. Candidodon itapecuruense Carvalho & Campos, 1988 is a Mesoeucrocodylia from the Itapecuru Formation (Lower Cretaceous), Parnaíba Basin, Brazil. This species is characterized by presenting teeth with a main cuspid and a series of smaller cuspids in crown base. -
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). -
The Morphology and Systematics of the Clam Shrimp Platyestheria Gen
Cretaceous Research 91 (2018) 274e286 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes The morphology and systematics of the clam shrimp Platyestheria gen. nov. abaetensis (Cardoso) (Crustacea, Spinicaudata) from the Lower Cretaceous of the Sanfranciscana Basin, southeast Brazil * Jonathas S. Bittencourt a, , Rosemarie Rohn b, Oscar F. Gallego c, Mateo D. Monferran c, Alexandre Uhlein a a Laboratorio de Paleontologia e Macroevoluçao,~ Centro de Pesquisas Professor Manoel Teixeira da Costa, Departamento de Geologia, Instituto de Geoci^encias, Universidade Federal de Minas Gerais, Av. Presidente Antonio^ Carlos 6627, Pampulha, 31270-901, Belo Horizonte, MG, Brazil b Sao~ Paulo State University (UNESP), Institute of Geosciences and Exact Sciences, Department of Applied Geology, Rio Claro Campus, Av. 24A, 1515, 13506- 900, Rio Claro, SP, Brazil c Centro de Ecología Aplicada del Litoral, CONICET-UNNE and Geología Historica-Micropaleontología (Area Ciencias de la Tierra - Departamento de Biología), FaCENA-UNNE, Casilla de Correo 128, 3400 Corrientes, Argentina article info abstract Article history: New specimens of the clam shrimp ‘Pseudestheria’ abaetensis Cardoso, 1971 (Spinicaudata) are described. Received 6 February 2018 The material was collected from the Quirico Formation (Lower Cretaceous of the Sanfranciscana Basin), at Received in revised form the same locality as the type series of the species. The carapaces are very large, oval and elongated, with 4 May 2018 anteriorly located and slightly projected umbo, straight dorsal margin, with flattened growth bands and Accepted in revised form 22 June 2018 15e20 serrated growth lines. Details of the microscopic structure of the carapace were analysed under Available online 26 June 2018 scanning electron microscope for the first time, disclosing a unique reticular pattern of ornamentation. -
The Neostratotype of Itapecuru Formation (Lower-Middle Albian) and Its Impact for Mesozoic Stratigraphy of Parnaíba Basin
Anais da Academia Brasileira de Ciências (2019) 91(Suppl. 2): e20180730 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 http://dx.doi.org/10.1590/0001-3765201920180730 www.scielo.br/aabc | www.fb.com/aabcjournal The Neostratotype of Itapecuru Formation (Lower-Middle Albian) and Its Impact for Mesozoic Stratigraphy of Parnaíba Basin FRANCISCO J. CORRÊA-MARTINS1,2 1Programa de Pós-Graduação em Geologia, Universidade Federal do Rio de Janeiro, Avenida Athos da Silveira Ramos, 274, Ilha do Fundão, 21910-200 Rio de Janeiro, RJ, Brazil 2Departamento de Geociências, Instituto de Agronomia, Universidade Federal Rural do Rio de Janeiro, BR-465, Km 7, 23897-000 Seropédica, RJ, Brazil Manuscript received on July 23, 2018; accepted for publication on December 21, 2018 How to cite: CORRÊA-MARTINS FJ. 2019. The Neostratotype of Itapecuru Formation (Lower-Middle Albian) and Its Impact for Mesozoic Stratigraphy of Parnaíba Basin. An Acad Bras Cienc 91: e20180730. DOI 10.1590/0001- 3765201920180730. Abstract: This study defines the neostratotype of the Lower-Middle Albian Itapecuru Formation in the Parnaíba Basin, Northeast Brazil. In this sedimentary succession along the right bank of the Itapecuru River near the Itapecuru-Mirim City, Maranhão State, three lithofacies associations are recognized. The first is silty claystone with some very fine sand, micaceous, reddish color, thin laminated, showing a tabular aspect, interpreted as floodplain fines in a distal position. The second is clayey siltstone, reddish color, with ripple cross-lamination, very thin cross-laminated wacke lenses, grading to thin parallel lamination, in apparently tabular layers, interpreted as crevasse splay and distributive channels deposits in successive avulsion events. -
The Cretaceous (Cenomanian) Continental Record of the Laje Do Coringa flagstone (Alcântara Formation), Northeastern South America
Journal of South American Earth Sciences 53 (2014) 50e58 Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames The Cretaceous (Cenomanian) continental record of the Laje do Coringa flagstone (Alcântara Formation), northeastern South America Manuel Alfredo Medeiros a,*, Rafael Matos Lindoso b, Ighor Dienes Mendes a, Ismar de Souza Carvalho b a Universidade Federal do Maranhão, Campus do Bacanga, Avenida dos Portugueses, s/n, CEP: 65.085-580 São Luís, MA, Brazil b Universidade Federal do Rio de Janeiro, Departamento de Geologia, CCMN/IGEO, CEP 21.949-900, Cidade Universitária, Ilha do Fundão, Rio de Janeiro, RJ, Brazil article info abstract Article history: The fossil taxa of the Cenomanian continental flora and fauna of São Luís Basin are observed primarily in Received 25 August 2013 the bone bed of the Laje do Coringa, Alcântara Formation. Many of the disarticulated fish and tetrapod Accepted 8 April 2014 skeletal and dental elements are remarkably similar to the chronocorrelate fauna of Northern Africa. In this study, we present a summary of the continental flora and fauna of the Laje do Coringa bone-bed. The Keywords: record emphasizes the existence of a trans-oceanic typical fauna, at least until the early Cenomanian, Alcântara Formation which may be interpreted as minor evolutionary changes after a major vicariant event or as a result of a São Luís Basin land bridge across the equatorial Atlantic Ocean, thereby allowing interchanges between South America Cretaceous Cenomanian and Africa. The paleoenvironmental conditions in the northern Maranhão State coast during that time were inferred as forested humid areas surrounded by an arid to semi-arid landscape. -
A New Genus of Dipnoiformes from the Cretaceous of Brazil
“main” — 2011/10/18 — 12:41 — page 1181 — #1 Anais da Academia Brasileira de Ciências (2011) 83(4): 1181-1192 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 www.scielo.br/aabc A new genus of Dipnoiformes from the Cretaceous of Brazil CARLOS E.V. TOLEDO1, ELIANE P. DE SOUSA2, MANUEL A.A. MEDEIROS3 and REINALDO J. BERTINI4 1USP/IGC/GSA, Rua do Lago, 562, Cidade Universitária, Butantã, 05508-080 São Paulo, SP, Brasil 2UEMA/CECEN, Cidade Universitária Paulo VI, Bairro Tirirical, Caixa Postal 09, 65000-000 São Luís, MA, Brasil 3Departamento de Biologia, Universidade Federal do Maranhão, Campus do Bacanga, Avenida dos Portugueses, s/n, 65085-580 São Luís, MA, Brasil 4UNESP/IGCE/DGA/NEPV, Avenida 24-A, 1515, Campus Rio Claro, Bairro Bela Vista, 13506-900 Rio Claro, SP, Brasil Manuscript received on November 13, 2009; accepted for publication on March 1, 2011 ABSTRACT The Alcântara Formation, an important stratigraphic unit from the early Cenomanian of Brazil, was deposited under transitional (estuarine) conditions, and its fossil record includes fragmentary remains of plants, fishes, crocodylomorphs, pterosaurs and dinosaurs, with a noteworthy diversity of dipnoiformes tooth plates. The dipnoiformes material reported here comprises a new taxon, Equinoxiodus alcantarensis, gen. et sp. nov. Most of the identified morphotypes of continental vertebrates collected in the Alcântara Formation are similar to chronocorrelative faunas from Northern Africa, but this new genus of Dipnoiformes indicates some degree of paleogeographic isolation and endemism. This was probably caused by the widening of the equatorial Atlantic Ocean during the early Cenomanian, which may have selectively affected some species. -
(Sauropoda: Diplodocoidea) from the Middle Cretaceous of Northern Brazil
Cretaceous Research 104 (2019) 104191 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes A new rebbachisaurid (Sauropoda: Diplodocoidea) from the middle Cretaceous of northern Brazil Rafael Matos Lindoso a, c, *, Manuel Alfredo Araújo Medeiros b, Ismar de Souza Carvalho c, Agostinha Araújo Pereira d, Ighor Dienes Mendes e, Fabiano Vidoi Iori f, Eliane Pinheiro Sousa g, Silvia Helena Souza Arcanjo b, Taciane Costa Madeira Silva b a Instituto Federal de Educaçao,~ Ci^encia e Tecnologia do Maranhao,~ Pro-Reitoria de Pesquisa, Pos-Graduaç ao~ e Inovaçao~ e PRPGI, Av. Colares Moreira, 477, Renascença, Sao~ Luís, MA, CEP: 65.075-441, Brazil b Universidade Federal do Maranhao,~ Campus do Bacanga, Avenida dos Portugueses, s/n, CEP: 65.085-580, Sao~ Luís, MA, Brazil c Universidade Federal do Rio de Janeiro, Departamento de Geologia, CCMN/IGEO, Cidade Universitaria, Ilha do Fundao,~ CEP: 21.949-900, Rio de Janeiro, RJ, Brazil d Centro de Pesquisa de Historia Natural e Arqueologia do Maranhao,~ Rua do Giz, 59, Centro, CEP:65.010-680, Sao~ Luís, Maranhao,~ Brazil e Universidade Federal do Rio de Janeiro, Programa de Pos-Graduaç ao~ em Biodiversidade e Biologia Evolutiva, CCS/IB, Cidade Universitaria, Ilha do Fundao,~ CEP: 21.941-902, Rio de Janeiro, RJ, Brazil f Museu de Paleontologia Pedro Candolo, Estaçao~ Cultura, Praça Farmac^eutico Bruno Garisto, CEP: 15.890-000, Uchoa, SP, Brazil g Universidade Estadual do Maranhao,~ Departamento de Biologia, Cidade Universitaria Paulo VI, CEP: 65.055-970, Sao~ Luís, MA, Brazil article info abstract Article history: A new genus and species of Rebbachisauridae sauropod from the Cenomanian of the Sao~ Luís Basin, Received 30 May 2018 Alcantara^ Formation, Itapeuasaurus cajapioensis gen. -
Dipnoi: ?Neoceratodontidae) from the Late Cretaceous of Brazil
Zootaxa 3905 (3): 397–406 ISSN 1175-5326 (print edition) www.mapress.com/zootaxa/ Article ZOOTAXA Copyright © 2015 Magnolia Press ISSN 1175-5334 (online edition) http://dx.doi.org/10.11646/zootaxa.3905.3.5 http://zoobank.org/urn:lsid:zoobank.org:pub:6345CB5A-F4CE-4791-BE92-E77206BDDE0F A new species of Equinoxiodus (Dipnoi: ?Neoceratodontidae) from the Late Cretaceous of Brazil ELIANE PINHEIRO DE SOUSA1, MANUEL ALFREDO MEDEIROS2, CARLOS EDUARDO VIEIRA TOLEDO3, REINALDO J. BERTINI4, AGOSTINHA ARAÚJO PEREIRA5 & RAFAEL MATOS LINDOSO6 1Departamento de Biologia, Universidade Estadual do Maranhão, Cidade Universitária Paulo VI, CEP: 65055-970 São Luís, MA, Brazil. E-mail: [email protected] 2Departamento de Química e Biologia, Universidade Federal do Maranhão, Campus do Bacanga, CEP: 65.085-580, São Luís, Mara- nhão, Brazil. E-mail: [email protected] 3USP/ IGC/ GSA, Rua do Lago / 562, Cidade Universitária, Butantã, CEP: 05.508-080, São Paulo, Brasil. E-mail: [email protected] 4UNESP/ IGCE/ DGA/ NEPV, Av. 24 A, 1515, Campus Rio Claro, Bairro Bela Vista, CP 178, CEP: 13.506-900, Rio Claro, São Paulo, Brazil. E-mail: [email protected] 5Centro de Pesquisa de História Natural e Arqueologia do Maranhão, Rua do Giz, 59, Centro, CEP:65010-680, São Luís, Maranhão, Brazil. E-mail: [email protected] 6Universidade Federal do Rio de Janeiro, Departamento de Geologia, CCMN/IGEO, RJ 21.949-900, Cidade Universitária-Ilha do Fundão, Rio de Janeiro, Brazil. E-mail: [email protected] Correspondence should be sent to E.S. PINHEIRO: Departamento de Química e Biologia, Universidade Estadual do Maranhão, Cidade Universitária Paulo VI, CEP: 65055-970 São Luís, MA, Brazil. -
New Plant Fossils from the Lower Cretaceous of the Parnaíba Basin, Northeastern Brazil
DOI: 10.1590/2317-4889201820170071 ARTICLE New plant fossils from the Lower Cretaceous of the Parnaíba Basin, Northeastern Brazil: Southern Laurasia links Rafael Matos Lindoso1*, Tânia Lindner Dutra2, Ismar de Souza Carvalho3, Manuel Alfredo Medeiros4 ABSTRACT: This study reports on the presence of a diverse set of gymnosperm and angiosperm macrofossils from the Codó Formation, Parnaíba Basin, whose assemblage was previously known only by the occurrence of pollen grains, spores, wood fragments, leaves and roots associated with Nympheaceae. In the Brejo municipality, northeastern Maranhão State, marl levels attest a transitional to marginal lacustrine environment, with occasional marine ingressions, demonstrated by the presence of crustaceans, gastropods and fishes. The plant fossils are preserved exclusively by molds and impressions, and its diversity is represented by few specimens, suggesting taphonomic processes of selection and transportation. The taphoflora is composed of Gnetales (?Drewria), conifers (Cupressinocladus and Brachyphyllum), and basal angiosperms (Nympheales, Magnollids, and/or basal Eudicots), which support an upper Aptian – ?Albian age. It displays affinities with both the well-known flora of the Araripe Basin (Santana Formation) as well as those ones identified in deposits from the south of North America (Potomac Group), suggesting that terrestrial links persisted in the equatorial areas of the Pangea at the end of the Early Cretaceous. KEYWORDS: Lower Cretaceous; Macroflora; Parnaíba Basin; Codó Formation. INTRODUCTION Gnetales, with Bennettitales, Caytoniales, Pteridospermales and early angiosperms as a minor component (Regali et al. In the beginning of the Cretaceous, ferns and gymno- 1974, Lima 1982, Kunzmann et al. 2006, Bernardes-de- sperms dominated the plant communities of a broad equa- Oliveira et al. -
UNIVERSIDADE ESTADUAL PAULISTA Instituto De Geociências E Ciências Exatas Campus Rio Claro
UNIVERSIDADE ESTADUAL PAULISTA Instituto de Geociências e Ciências Exatas Campus Rio Claro REGISTRO DE DINOSSAUROS NA REGIÃO DA CIDADE DE COROATÁ, EO/MESOALBIANO DA BACIA DE SÃO LUÍS-GRAJAÚ, ESTADO DO MARANHÃO Darciléa Ferreira Castro Orientador: Prof.Dr.Reinaldo J. Bertini Dissertação de Mestrado elaborada junto ao Programa de Pós-Graduação em Geociências - Área de Concentração em Geologia Regional para a obtenção do Título de Mestre em Geociências Rio Claro (SP) 2006 SUMÁRIO Índice i Índice de Figuras iii Resumo v Abstract vi 1. Introdução 1 2. Material e Métodos 44 7. Resultados 48 8. Discussão 61 9. Conclusões 68 10. Referências Bibliográficas 69 i ÍNDICE 1. INTRODUÇÃO 1 2. OBJETIVOS PRINCIPAIS 2 3. GEOLOGIA REGIONAL 3 3.1. Bacia de São Luís-Grajaú 3 3.1.1. Formações Codó e Grajaú 8 3.1.2. Grupo Itapecuru 9 3.1.2.1. Unidade Indiferenciada 9 3.1.2.2. Formação Alcântara 10 3.2.2.3. Formação Cujupe 11 3.2.3. Formações Pirabas e Barreiras 12 4. CONTEXTO TAXONÔMICO 13 4.1. Dinossauros 13 4.1.1. Saurópodos 13 4.4.1.1. Elementos pós-cranianos 19 4.4.1.1.1. Esqueleto axial 19 4.4.1.1.2.Característica pneumática em elementos vertebrais (Tecido esponjoso) 22 4.4.1.1.3. Esqueleto apendicular 25 4.4.4.1. Origem e diversidade 28 4.1.1.1. Diplodocoidea 28 4.1.1.1.1. Rebbachisauridae 31 4.1.1.1.1.1. Características – “Rebbachisaurus” 32 4.1.1.2. Titanosauria 33 4.1.1.2.1. Características - Titanosauria 36 4.1.1.2.2. -
Distributional Patterns of †Mawsoniidae (Sarcopterygii: Actinistia)
Anais da Academia Brasileira de Ciências (2014) 86(1): 159-170 (Annals of the Brazilian Academy of Sciences) Printed version ISSN 0001-3765 / Online version ISSN 1678-2690 http://dx.doi.org/10.1590/0001-3765201420130035 www.scielo.br/aabc Distributional patterns of †Mawsoniidae (Sarcopterygii: Actinistia) RAPHAEL MIGUEL1, VALÉRIA GALLO1 and JUAN J. MORRONE2 1Universidade do Estado do Rio de Janeiro, Instituto de Biologia, Departamento de Zoologia, Laboratório de Sistemática e Biogeografia, Rua São Francisco Xavier, 524, Maracanã, 20550-013 Rio de Janeiro, RJ, Brasil 2Universidad Nacional Autónoma de México, Facultad de Ciencias, Departamento de Biología Evolutiva, Museo de Zoología “Alfonso L. Herrera”, Apdo. Postal 70-399, 04510 Mexico, D.F., Mexico Manuscript received on January 31, 2013; accepted for publication on June 12, 2013 ABSTRACT Mawsoniidae are a fossil family of actinistian fish popularly known as coelacanths, which are found in continental and marine paleoenvironments. The taxon is considered monophyletic, including five valid genera (Axelrodichthys, Chinlea, Diplurus, Mawsonia and Parnaibaia) and 11 genera with some taxonomical controversy (Alcoveria, Changxingia, Garnbergia, Heptanema, Indocoelacanthus, Libys, Lualabaea, Megalocoelacanthus, Moenkopia, Rhipis and Trachymetopon). The genera restricted to the Northern Hemisphere (Diplurus and Chinlea) possess the oldest records (Late Triassic), whereas those found in the Southern Hemisphere (Mawsonia, Axelrodichthys, and Parnaibaia) extend from Late Jurassic to Late Cretaceous, especially in Brazil and Africa. We identified distributional patterns of Mawsoniidae, applying the panbiogeographical method of track analysis, and obtained three generalized tracks (GTs): GT1 (Northeastern Newark) in strata of the Newark Group (Upper Triassic); GT2 (Midwestern Gondwana) in the Lualaba Formation (Upper Jurassic); and GT3 (Itapecuru-Alcântara-Santana) in the Itapecuru-Alcântara- Santana formations (Lower Cretaceous). -
Depositions. Faces in Late Cretaceous-?Lower Tertiary Deposits from Northwestern Maranhao State, Brazil
Revista Brasileira de Geociencias 29(2):237-244, junho de 1999 DEPOSITIONS. FACES IN LATE CRETACEOUS-?LOWER TERTIARY DEPOSITS FROM NORTHWESTERN MARANHAO STATE, BRAZIL RODRIGO DIAS LIMA* & DILCE DE FATIMA ROSSETTI* ABSTRACT Late Cretaceous-?Lower Tertiary deposits from northwestern Maranhao State (northern Brazil) were investigated using facies analysis in outcrops in combination with subsurface data provided from gamma-ray profiles. Four facies associations were recognized in this area and attributed to: a) mouth bar (facies association 1); b) braided fluvial/distributary channel (facies association 2); c) distal mouth bar/crevasse lobe (facies association 3); and d) interdistributary bay/prodelta (facies association 4). Mouth bar deposits consist of well-sorted, fine- to very-fine grained sandstone with a variety of sedimentary structures, mostly including: convolute lamination; overturned foresets; sigmoidal, trough, and tabular cross stratifications; and massive bedding. Growth faults and slumpings are common features associated with these deposits. Braided fluvial/distributary channel deposits are characterized by poorly-sorted, coarse-grained cross-stratified sandstone with sharp, locally concave-up, basal surfaces mantled by lags. Distal mouth bar/crevasse lobe deposits consist of a succession of strata formed by coarsening upward cycles represented by massive and cross-laminated sandstones that are interbedded with mudstones containing abundant plant remains. Finally, interdistributary bay/prodelta deposits include mudstones with abundant plant remains and streaks of silt and very-fine grained sandstones. The four facies associations described above characterize depositional environments typical of delta settings, an interpretation consistent with the funnel-shaped gamma-ray patterns observed in well logs. Correlation of these deposits with a wave-dominated estuarine system (i.e., Cujupe Formation) exposed in the eastern of Sao Luis Basin led to attribute them to a bayhead delta complex located in the innermost portion of this estuary.