Redalyc.New Information on Riograndia Guaibensis Bonaparte
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JVP 26(3) September 2006—ABSTRACTS
Neoceti Symposium, Saturday 8:45 acid-prepared osteolepiforms Medoevia and Gogonasus has offered strong support for BODY SIZE AND CRYPTIC TROPHIC SEPARATION OF GENERALIZED Jarvik’s interpretation, but Eusthenopteron itself has not been reexamined in detail. PIERCE-FEEDING CETACEANS: THE ROLE OF FEEDING DIVERSITY DUR- Uncertainty has persisted about the relationship between the large endoskeletal “fenestra ING THE RISE OF THE NEOCETI endochoanalis” and the apparently much smaller choana, and about the occlusion of upper ADAM, Peter, Univ. of California, Los Angeles, Los Angeles, CA; JETT, Kristin, Univ. of and lower jaw fangs relative to the choana. California, Davis, Davis, CA; OLSON, Joshua, Univ. of California, Los Angeles, Los A CT scan investigation of a large skull of Eusthenopteron, carried out in collaboration Angeles, CA with University of Texas and Parc de Miguasha, offers an opportunity to image and digital- Marine mammals with homodont dentition and relatively little specialization of the feeding ly “dissect” a complete three-dimensional snout region. We find that a choana is indeed apparatus are often categorized as generalist eaters of squid and fish. However, analyses of present, somewhat narrower but otherwise similar to that described by Jarvik. It does not many modern ecosystems reveal the importance of body size in determining trophic parti- receive the anterior coronoid fang, which bites mesial to the edge of the dermopalatine and tioning and diversity among predators. We established relationships between body sizes of is received by a pit in that bone. The fenestra endochoanalis is partly floored by the vomer extant cetaceans and their prey in order to infer prey size and potential trophic separation of and the dermopalatine, restricting the choana to the lateral part of the fenestra. -
Ischigualasto Formation. the Second Is a Sile- Diversity Or Abundance, but This Result Was Based on Only 19 of Saurid, Ignotosaurus Fragilis (Fig
This article was downloaded by: [University of Chicago Library] On: 10 October 2013, At: 10:52 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Journal of Vertebrate Paleontology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/ujvp20 Vertebrate succession in the Ischigualasto Formation Ricardo N. Martínez a , Cecilia Apaldetti a b , Oscar A. Alcober a , Carina E. Colombi a b , Paul C. Sereno c , Eliana Fernandez a b , Paula Santi Malnis a b , Gustavo A. Correa a b & Diego Abelin a a Instituto y Museo de Ciencias Naturales, Universidad Nacional de San Juan , España 400 (norte), San Juan , Argentina , CP5400 b Consejo Nacional de Investigaciones Científicas y Técnicas , Buenos Aires , Argentina c Department of Organismal Biology and Anatomy, and Committee on Evolutionary Biology , University of Chicago , 1027 East 57th Street, Chicago , Illinois , 60637 , U.S.A. Published online: 08 Oct 2013. To cite this article: Ricardo N. Martínez , Cecilia Apaldetti , Oscar A. Alcober , Carina E. Colombi , Paul C. Sereno , Eliana Fernandez , Paula Santi Malnis , Gustavo A. Correa & Diego Abelin (2012) Vertebrate succession in the Ischigualasto Formation, Journal of Vertebrate Paleontology, 32:sup1, 10-30, DOI: 10.1080/02724634.2013.818546 To link to this article: http://dx.doi.org/10.1080/02724634.2013.818546 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. However, Taylor & Francis, our agents, and our licensors make no representations or warranties whatsoever as to the accuracy, completeness, or suitability for any purpose of the Content. -
O Esqueleto Pós-Craniano De Exaeretodon Riograndensis Abdala Et Al
Rev. bras. paleontol. 10(2):79-94, Maio/Agosto 2007 © 2007 by the Sociedade Brasileira de Paleontologia O ESQUELETO PÓS-CRANIANO DE EXAERETODON RIOGRANDENSIS ABDALA ET AL. (CYNODONTIA, TRAVERSODONTIDAE), TRIÁSSICO DO BRASIL TÉO VEIGA DE OLIVEIRA, CESAR LEANDRO SCHULTZ & MARINA BENTO SOARES Instituto de Geociências, UFRGS, Avenida Bento Gonçalves, 9500, 91501-970, Porto Alegre, RS, Brasil. [email protected], [email protected], [email protected] RESUMO – Pela primeira vez, elementos pós-cranianos de Exaeretodon riograndensis, um cinodonte traversodontídeo da Cenozona de Rhynchosauria da Formação Santa Maria, Neotriássico do sul do Brasil, são descritos e comparados com E. frenguellii e outros cinodontes não-mamalianos. O material inclui parte da coluna vertebral, radio, ulna e elementos da cintura pélvica. As diferenças mais significativas em relação a E. frenguellii estão na morfologia e nas dimensões do arco neural do atlas, na presença de intercentros em vértebras cervicais posteriores ao áxis e na ausência da dilatação do ápice do espinho neural das vértebras truncais. A morfologia da região sacral da coluna, do rádio, da ulna e da cintura pélvica são concordantes com o observado em E. frenguellii. A comparação com outros táxons de cinodontes não-mamalianos permite a observação da nítida evolução em mosaico do esqueleto pós-craniano destes animais: E. riograndensis mostra alguns caracteres similares a outros Cynognathia (grupo ao qual pertence), enquanto outros são mais próximos aos observados em alguns Probainognathia (incluindo mamíferos), como a natureza mais avançada do complexo atlas-áxis. Palavras-chave: Triássico, Brasil, Formação Santa Maria, Traversodontidae, Exaeretodon riograndensis, pós-crânio. ABSTRACT – THE POSTCRANIAL SKELETON OF EXAERETODON RIOGRANDENSIS ABDALA ET AL. -
Studies on Continental Late Triassic Tetrapod Biochronology. I. the Type Locality of Saturnalia Tupiniquim and the Faunal Succession in South Brazil
Journal of South American Earth Sciences 19 (2005) 205–218 www.elsevier.com/locate/jsames Studies on continental Late Triassic tetrapod biochronology. I. The type locality of Saturnalia tupiniquim and the faunal succession in south Brazil Max Cardoso Langer* Departamento de Biologia, FFCLRP, Universidade de Sa˜o Paulo (USP), Av. Bandeirantes 3900, 14040-901 Ribeira˜o Preto, SP, Brazil Received 1 November 2003; accepted 1 January 2005 Abstract Late Triassic deposits of the Parana´ Basin, Rio Grande do Sul, Brazil, encompass a single third-order, tetrapod-bearing sedimentary sequence that includes parts of the Alemoa Member (Santa Maria Formation) and the Caturrita Formation. A rich, diverse succession of terrestrial tetrapod communities is recorded in these sediments, which can be divided into at least three faunal associations. The stem- sauropodomorph Saturnalia tupiniquim was collected in the locality known as ‘Waldsanga’ near the city of Santa Maria. In that area, the deposits of the Alemoa Member yield the ‘Alemoa local fauna,’ which typifies the first association; includes the rhynchosaur Hyperodapedon, aetosaurs, and basal dinosaurs; and is coeval with the lower fauna of the Ischigualasto Formation, Bermejo Basin, NW Argentina. The second association is recorded in deposits of both the Alemoa Member and the Caturrita Formation, characterized by the rhynchosaur ‘Scaphonyx’ sulcognathus and the cynodont Exaeretodon, and correlated with the upper fauna of the Ischigualasto Formation. Various isolated outcrops of the Caturrita Formation yield tetrapod fossils that correspond to post-Ischigualastian faunas but might not belong to a single faunal association. The record of the dicynodont Jachaleria suggests correlations with the lower part of the Los Colorados Formation, NW Argentina, whereas remains of derived tritheledontid cynodonts indicate younger ages. -
The Mammary Gland and Its Origin During Synapsid Evolution
P1: GMX Journal of Mammary Gland Biology and Neoplasia (JMGBN) pp749-jmgbn-460568 January 9, 2003 17:51 Style file version Nov. 07, 2000 Journal of Mammary Gland Biology and Neoplasia, Vol. 7, No. 3, July 2002 (C 2002) The Mammary Gland and Its Origin During Synapsid Evolution Olav T. Oftedal1 Lactation appears to be an ancient reproductive trait that predates the origin of mammals. The synapsid branch of the amniote tree that separated from other taxa in the Pennsylva- nian (>310 million years ago) evolved a glandular rather than scaled integument. Repeated radiations of synapsids produced a gradual accrual of mammalian features. The mammary gland apparently derives from an ancestral apocrine-like gland that was associated with hair follicles. This association is retained by monotreme mammary glands and is evident as ves- tigial mammary hair during early ontogenetic development of marsupials. The dense cluster of mammo-pilo-sebaceous units that open onto a nipple-less mammary patch in monotremes may reflect a structure that evolved to provide moisture and other constituents to permeable eggs. Mammary patch secretions were coopted to provide nutrients to hatchlings, but some constituents including lactose may have been secreted by ancestral apocrine-like glands in early synapsids. Advanced Triassic therapsids, such as cynodonts, almost certainly secreted complex, nutrient-rich milk, allowing a progressive decline in egg size and an increasingly altricial state of the young at hatching. This is indicated by the very small body size, presence of epipubic bones, and limited tooth replacement in advanced cynodonts and early mammali- aforms. Nipples that arose from the mammary patch rendered mammary hairs obsolete, while placental structures have allowed lactation to be truncated in living eutherians. -
Um Novo E Peculiar Cinodonte Traversodontídeo Para O Triássico Médio Do Rio Grande Do Sul E Suas Implicações Para a Paleoecologia De
UNIVERSIDADE FEDERAL DO RIO GRANDE DO SUL INSTITUTO DE GEOCIÊNCIAS PROGRAMA DE PÓS-GRADUAÇÃO EM GEOCIÊNCIAS Um Novo e Peculiar Cinodonte Traversodontídeo para o Triássico Médio do Rio Grande do Sul e suas Implicações para a Paleoecologia de Cynodontia Míriam Reichel Orientador: Prof. Dr. Cesar Leandro Schultz Co-Orientadora: Profª. Drª. Marina Bento Soares Comissão Examinadora: Prof. Dr. José Fernando Bonaparte Prof. Dr. Mario Cozzuol Profª. Drª. Cristina Vega Dias Dissertação de Mestrado apresentada como requisito para obtenção do título de Mestre em Ciências Livros Grátis http://www.livrosgratis.com.br Milhares de livros grátis para download. Reichel, Miriam Um novo e peculiar Cinodonte Traversodontídeo para triássico médio do Rio Grande do Sul e suas implicações para a Paleoecologia de Cynodontia. / Miriam Reichel. - Porto Alegre : UFRGS, 2006. [145 f.] il. Dissertação (Mestrado). - Universidade Federal do Rio Grande do Sul. Instituto de Geociências. Programa de Pós-Graduação em Geociências. Porto Alegre, RS - BR, 2006. 1. Paleoecologia. 2. Cynodontia. 3. Traversodontidae. 4. Triássico Médio. 5. Formação Santa Maria. 6. Rio Grande do Sul. I. Título. _____________________________ Catalogação na Publicação Biblioteca Geociências - UFRGS Renata Cristina Grun CRB 10/1113 AGRADECIMENTOS • Ao professor Dr. José Fernando Bonaparte, pelos ensinamentos a respeito dos cinodontes, por estimular este trabalho, contribuindo com importantes comentários, e pela grande dedicação à paleontologia e àqueles que por ela se interessam. • Ao professor Dr. Cesar Leandro Schultz, por orientar este trabalho, por sempre tornar o ambiente de trabalho agradável, pelos conselhos e pela amizade. • À professora Dra. Marina Bento Soares, por me trazer para o mundo dos cinodontes, pela paciência e didática de fundamental importância para este trabalho, pelo carinho e pela amizade. -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
Dinosaur Remains from the 'Botucaraí Hill' (Caturrita Formation), Late
This article was downloaded by: [Jonathas Souza Bittencourt] On: 17 August 2012, At: 06:23 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Historical Biology: An International Journal of Paleobiology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/ghbi20 Dinosaur remains from the ‘Botucaraí Hill’ (Caturrita Formation), Late Triassic of south Brazil, and their stratigraphic context Jonathas Souza Bittencourt a b , Átila Augusto Stock da Rosa c , Cesar Leandro Schultz d & Max Cardoso Langer a a Departamento de Biologia, Universidade de São Paulo, Av. Bandeirantes 3900, 1404-901, Ribeirão Preto (SP), Brazil b Departamento de Geologia, Universidade Federal de Minas Gerais, Av. Antônio Carlos 6670, 31270-901, Belo Horizonte (MG), Brazil c Departamento de Geociências, Universidade Federal de Santa Maria, Av. Roraima 1000, 97105-900, Santa Maria (RS), Brazil d Instituto de Geociências, Universidade Federal do Rio Grande do Sul, Av. Bento Gonçalves 9500, 91501-970, Porto Alegre (RS), Brazil Version of record first published: 17 Aug 2012 To cite this article: Jonathas Souza Bittencourt, Átila Augusto Stock da Rosa, Cesar Leandro Schultz & Max Cardoso Langer (2012): Dinosaur remains from the ‘Botucaraí Hill’ (Caturrita Formation), Late Triassic of south Brazil, and their stratigraphic context, Historical Biology: An International Journal of Paleobiology, DOI:10.1080/08912963.2012.694881 To link to this article: http://dx.doi.org/10.1080/08912963.2012.694881 PLEASE SCROLL DOWN FOR ARTICLE Full terms and conditions of use: http://www.tandfonline.com/page/terms-and-conditions This article may be used for research, teaching, and private study purposes. -
Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships
438 Article 438 by Saswati Bandyopadhyay1* and Sanghamitra Ray2 Gondwana Vertebrate Faunas of India: Their Diversity and Intercontinental Relationships 1Geological Studies Unit, Indian Statistical Institute, 203 B. T. Road, Kolkata 700108, India; email: [email protected] 2Department of Geology and Geophysics, Indian Institute of Technology, Kharagpur 721302, India; email: [email protected] *Corresponding author (Received : 23/12/2018; Revised accepted : 11/09/2019) https://doi.org/10.18814/epiiugs/2020/020028 The twelve Gondwanan stratigraphic horizons of many extant lineages, producing highly diverse terrestrial vertebrates India have yielded varied vertebrate fossils. The oldest in the vacant niches created throughout the world due to the end- Permian extinction event. Diapsids diversified rapidly by the Middle fossil record is the Endothiodon-dominated multitaxic Triassic in to many communities of continental tetrapods, whereas Kundaram fauna, which correlates the Kundaram the non-mammalian synapsids became a minor components for the Formation with several other coeval Late Permian remainder of the Mesozoic Era. The Gondwana basins of peninsular horizons of South Africa, Zambia, Tanzania, India (Fig. 1A) aptly exemplify the diverse vertebrate faunas found Mozambique, Malawi, Madagascar and Brazil. The from the Late Palaeozoic and Mesozoic. During the last few decades much emphasis was given on explorations and excavations of Permian-Triassic transition in India is marked by vertebrate fossils in these basins which have yielded many new fossil distinct taxonomic shift and faunal characteristics and vertebrates, significant both in numbers and diversity of genera, and represented by small-sized holdover fauna of the providing information on their taphonomy, taxonomy, phylogeny, Early Triassic Panchet and Kamthi fauna. -
The Mesozoic Era Alvarez, W.(1997)
Alles Introductory Biology: Illustrated Lecture Presentations Instructor David L. Alles Western Washington University ----------------------- Part Three: The Integration of Biological Knowledge Vertebrate Evolution in the Late Paleozoic and Mesozoic Eras ----------------------- Vertebrate Evolution in the Late Paleozoic and Mesozoic • Amphibians to Reptiles Internal Fertilization, the Amniotic Egg, and a Water-Tight Skin • The Adaptive Radiation of Reptiles from Scales to Hair and Feathers • Therapsids to Mammals • Dinosaurs to Birds Ectothermy to Endothermy The Evolution of Reptiles The Phanerozoic Eon 444 365 251 Paleozoic Era 542 m.y.a. 488 416 360 299 Camb. Ordov. Sil. Devo. Carbon. Perm. Cambrian Pikaia Fish Fish First First Explosion w/o jaws w/ jaws Amphibians Reptiles 210 65 Mesozoic Era 251 200 180 150 145 Triassic Jurassic Cretaceous First First First T. rex Dinosaurs Mammals Birds Cenozoic Era Last Ice Age 65 56 34 23 5 1.8 0.01 Paleo. Eocene Oligo. Miocene Plio. Ple. Present Early Primate First New First First Modern Cantius World Monkeys Apes Hominins Humans A modern Amphibian—the toad A modern day Reptile—a skink, note the finely outlined scales. A Comparison of Amphibian and Reptile Reproduction The oldest known reptile is Hylonomus lyelli dating to ~ 320 m.y.a.. The earliest or stem reptiles radiated into therapsids leading to mammals, and archosaurs leading to all the other reptile groups including the thecodontians, ancestors of the dinosaurs. Dimetrodon, a Mammal-like Reptile of the Early Permian Dicynodonts were a group of therapsids of the late Permian. Web Reference http://www.museums.org.za/sam/resource/palaeo/cluver/index.html Therapsids experienced an adaptive radiation during the Permian, but suffered heavy extinctions during the end Permian mass extinction. -
And Early Jurassic Sediments, and Patterns of the Triassic-Jurassic
and Early Jurassic sediments, and patterns of the Triassic-Jurassic PAUL E. OLSEN AND tetrapod transition HANS-DIETER SUES Introduction parent answer was that the supposed mass extinc- The Late Triassic-Early Jurassic boundary is fre- tions in the tetrapod record were largely an artifact quently cited as one of the thirteen or so episodes of incorrect or questionable biostratigraphic corre- of major extinctions that punctuate Phanerozoic his- lations. On reexamining the problem, we have come tory (Colbert 1958; Newell 1967; Hallam 1981; Raup to realize that the kinds of patterns revealed by look- and Sepkoski 1982, 1984). These times of apparent ing at the change in taxonomic composition through decimation stand out as one class of the great events time also profoundly depend on the taxonomic levels in the history of life. and the sampling intervals examined. We address Renewed interest in the pattern of mass ex- those problems in this chapter. We have now found tinctions through time has stimulated novel and com- that there does indeed appear to be some sort of prehensive attempts to relate these patterns to other extinction event, but it cannot be examined at the terrestrial and extraterrestrial phenomena (see usual coarse levels of resolution. It requires new fine- Chapter 24). The Triassic-Jurassic boundary takes scaled documentation of specific faunal and floral on special significance in this light. First, the faunal transitions. transitions have been cited as even greater in mag- Stratigraphic correlation of geographically dis- nitude than those of the Cretaceous or the Permian junct rocks and assemblages predetermines our per- (Colbert 1958; Hallam 1981; see also Chapter 24). -
Evolution of the Mammalian Fauces Region and the Origin of Suckling
Evolution of the mammalian fauces region and the origin of suckling The Harvard community has made this article openly available. Please share how this access benefits you. Your story matters Citation Crompton, Alfred, Catherine Musinsky, Jose Bonaparte, Bhart- Anjan Bhullar, and Tomasz Owerkowicz. Evolution of the mammalian fauces region and the origin of suckling (2018). Citable link https://nrs.harvard.edu/URN-3:HUL.INSTREPOS:37364482 Terms of Use This article was downloaded from Harvard University’s DASH repository, and is made available under the terms and conditions applicable to Other Posted Material, as set forth at http:// nrs.harvard.edu/urn-3:HUL.InstRepos:dash.current.terms-of- use#LAA 1 Evolution of the mammalian fauces region and the origin of suckling Alfred Crompton1†, Catherine Musinsky1, Jose Bonaparte2, Bhart-Anjan Bhullar3, Tomasz Owerkowicz4 1: Harvard University, Organismic and Evolutionary Biology Department, Museum of Comparative Zoology, 26 Oxford St, Cambridge, MA 02138 USA 2: Museo Municipal de C. Naturales "C. Ameghino", 6600 MERCEDES – BS. AS. Argentina 3: Department of Geology & Geophysics, Yale University, PO Box 208109, New Haven, CT 06520- 8109 USA 4: Department of Biology, California State University in San Bernadino, 5500 University Pkwy, San Bernardino, CA 92407 USA †corresponding author: ORCID 0000-0001-6008-2587, [email protected], 617-495-3202 Acknowledgments Thanks to Dr. Edgar Allin for his comments on an early draft of this paper. Thanks to the Museum of Comparative Zoology, its Director, Professor James Hanken, and to the Center for Nanoscale Systems at Harvard University for providing the facilities and finances for this research.