HISTORIA NATURAL Tercera Serie Volumen 2 (2) 2012/5-30
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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. -
Micheli Stefanello
UNIVERSIDADE FEDERAL DE SANTA MARIA CENTRO DE CIÊNCIAS NATURAIS E EXATAS PROGRAMA DE PÓS-GRADUAÇÃO EM BIODIVERSIDADE ANIMAL Micheli Stefanello DESCRIÇÃO E FILOGENIA DE UM NOVO ESPÉCIME DE CINODONTE PROBAINOGNÁTIO DO TRIÁSSICO SUL-BRASILEIRO Santa Maria, RS 2018 Micheli Stefanello DESCRIÇÃO E FILOGENIA DE UM NOVO ESPÉCIME DE CINODONTE PROBAINOGNÁTIO DO TRIÁSSICO SUL-BRASILEIRO Dissertação apresentada ao Curso de Mestrado do Programa de Pós-Graduação em Biodiversidade Animal, Área de Concentração em Sistemática e Biologia Evolutiva, da Universidade Federal de Santa Maria (UFSM, RS), como requisito parcial para obtenção do grau de Mestre em Ciências Biológicas – Área Biodiversidade Animal. Orientador: Prof. Dr. Sérgio Dias da Silva Santa Maria, RS 2018 Micheli Stefanello DESCRIÇÃO E FILOGENIA DE UM NOVO ESPÉCIME DE CINODONTE PROBAINOGNÁTIO DO TRIÁSSICO SUL-BRASILEIRO Dissertação apresentada ao Curso de Mestrado do Programa de Pós-Graduação em Biodiversidade Animal, Área de Concentração em Sistemática e Biologia Evolutiva, da Universidade Federal de Santa Maria (UFSM, RS), como requisito parcial para obtenção do grau de Mestre em Ciências Biológicas – Área Biodiversidade Animal. Aprovada em 28 de fevereiro de 2018: Santa Maria, RS 2018 AGRADECIMENTOS Ao meu orientador, Dr. Sérgio Dias da Silva, pela orientação, por todo o tempo despendido ao longo desse mestrado e por possibilitar meu aprimoramento na área a qual tenho apreço. Aos colegas do Centro de Apoio à Pesquisa Paleontológica da Quarta Colônia da Universidade Federal de Santa Maria (CAPPA/UFSM) e do Laboratório de Paleobiodiversidade Triássica, dessa mesma instituição, pela convivência e por terem ajudado-me de diferentes formas ao longo do mestrado. Em especial, ao colega Rodrigo Temp Müller, pela coleta do espécime (objeto de estudo dessa dissertação), por toda a ajuda com o TNT e com as figuras, e por auxiliar-me de inúmeras formas. -
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. -
Width Measured at the Level of Anterior Squamosal/Parietal Suture
Fig. 5. (A) Scaling of brain vault size (width measured at the level of anterior squamosal/parietal suture) relative to skull size (measured at the distance between the left versus right temporomandibular joints). This shows that allometry of small size of Hadrocodium, by itself, is not sufficient to account for its very large braincase. Had-rocodium's brain vault is larger (wider) than expected for the crown-group mammals with similar skull width from the allometrical regression. By contrast, all contemporaneous mammaliaforms (triangles: Sinoconodon, Morganucodon, and Haldanodon) with the postdentary trough and meckelian groove have smaller (narrower) brain vaults than those living mammal taxa (and Hadrocodium) of comparable skull size. The brain vault is narrower in nonmammaliaform cynodonts (squares: Chaliminia, Massetoganthus, Probelesodon, Probainognathus, and Yunnanodon) than in mammaliaform stem taxa and much narrower than expected for crown group mammals of similar size. The allometric equation (natural logarithmic scale) for the brain vault width (Y) to the skull width at the level of TMJ (X) for species in the mammalian crown groups (circles: 37 living and 8 fossil species): Y =0.98X -0.31 (R2 – 0.715). Data from cynodonts, mammaliaforms, and Hadrocodium are added second arily for comparison with the regression of extant and fossil species of mammalian crown group. (B) Estimated body-size distributions of mammaliaform insectivores in the Early Jurassic Lufeng fauna [following method of Gingerich (50)]. The estimated 2-g body mass of Hadrocodium is in strong contrast to its contemporary mammaliaforms of the Late Triassic and Early Jurassic, such as Sinconodon (from ~13 to ~517 g, based on skull length from 22 to 62 mm) and Morganucodon (from 27 to 89 g, based on skull length from 27 to 38 mm). -
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. -
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. -
A Non-Mammaliaform Cynodont from the Upper Triassic of South Africa: a Therapsid Lazarus Taxon?
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Wits Institutional Repository on DSPACE A non-mammaliaform cynodont from the Upper Triassic of South Africa: a therapsid Lazarus taxon? Fernando Abdala1*, Ross Damiani2, Adam Yates1 & Johann Neveling3 1Bernard Price Institute for Palaeontological Research, School of Geosciences, University of the Witwatersrand, Private Bag 3, WITS, 2050 South Africa 2Staatliches Museum für Naturkunde Stuttgart, Rosenstein 1, D-70191, Stuttgart, Germany 3Council for Geoscience, Private Bag X112, Pretoria, 0001 South Africa Received 20 January 2006. Accepted 10 January 2007 The tetrapod record of the ‘Stormberg Group’, including the Lower Elliot Formation, in the South African Karoo is widely dominated by archosaurian reptiles, contrasting with the therapsid dominion of the subjacent Beaufort Group. The only therapsids represented by skeletal remains in the Upper Triassic Lower Elliot Formation are the large traversodontid cynodont Scalenodontoides macrodontes and the recently described tritheledontid cynodont Elliotherium kersteni. Here we present a fragmentary lower jaw that provides evidence of a third type of cynodont for the Upper Triassic of South Africa. The fossil is tentatively assigned to the Diademodontidae. The latter representative of this family is known from the Late Anisian, and its tentative record in the Norian Lower Elliot Formation, if confirmed, will represent a case of Lazarus taxon. Thus, Diademodontidae apparently disappeared from the fossil record by the end of the Anisian and then reappeared in the Norian of South Africa, a stratigraphic interval of some 21 million years. This new cynodont record, together with the recently described Tritheledontidae, show that cynodonts are now the second most diverse tetrapod group in the Lower Elliot fauna. -
Mammal Evolution
Mammal Evolution Geology 331 Paleontology Triassic synapsid reptiles: Therapsids or mammal-like reptiles. Note the sprawling posture. Mammal with Upright Posture From Synapsids to Mammals, a well documented transition series Carl Buell Prothero, 2007 Synapsid Teeth, less specialized Mammal Teeth, more specialized Prothero, 2007 Yanoconodon, Lower Cretaceous of China Yanoconodon, Lower Cretaceous of China, retains ear bones attached to the inside lower jaw Morganucodon Yanoconodon = articular of = quadrate of Human Ear Bones, or lower reptile upper reptile Auditory Ossicles jaw jaw Cochlea Mammals have a bony secondary palate Primary Palate Reptiles have a soft Secondary Palate secondary palate Reduction of digit bones from Hand and Foot of Permian Synapsid 2-3-4-5-3 in synapsid Seymouria ancestors to 2-3-3-3-3 in mammals Human Hand and Foot Class Mammalia - Late Triassic to Recent Superorder Tricodonta - Late Triassic to Late Cretaceous Superorder Multituberculata - Late Jurassic to Early Oligocene Superorder Monotremata - Early Cretaceous to Recent Superorder Metatheria (Marsupials) - Late Cretaceous to Recent Superorder Eutheria (Placentals) - Late Cretaceous to Recent Evolution of Mammalian Superorders Multituberculates Metatheria Eutheria (Marsupials) (Placentals) Tricodonts Monotremes . Live Birth Extinct: . .. Mammary Glands? Mammals in the Age of Dinosaurs – a nocturnal life style Hadrocodium, a lower Jurassic mammal with a “large” brain (6 mm brain case in an 8 mm skull) Were larger brains adaptive for a greater sense of smell? Big Brains and Early Mammals July 14, 2011 The Academic Minute http://www.insidehighered.com/audio/academic_pulse/big_brains_and_early_mammals Lower Cretaceous mammal from China Jawbones of a Cretaceous marsupial from Mongolia Mammal fossil from the Cretaceous of Mongolia Reconstructed Cretaceous Mammal Early Cretaceous mammal ate small dinosaurs Repenomamus robustus fed on psittacosaurs. -
Osteohistology of Late Triassic Prozostrodontian Cynodonts from Brazil
Osteohistology of Late Triassic prozostrodontian cynodonts from Brazil Jennifer Botha-Brink1,2, Marina Bento Soares3 and Agustín G. Martinelli3 1 Department of Karoo Palaeontology, National Museum, Bloemfontein, South Africa 2 Department of Zoology and Entomology, University of the Free State, Bloemfontein, South Africa 3 Departamento de Paleontologia e Estratigrafia, Instituto de Geociências, Universidade Federal do Rio Grande do Sul, Porto Alegre, Brazil ABSTRACT The Prozostrodontia includes a group of Late Triassic-Early Cretaceous eucynodonts plus the clade Mammaliaformes, in which Mammalia is nested. Analysing their growth patterns is thus important for understanding the evolution of mammalian life histories. Obtaining material for osteohistological analysis is difficult due to the rare and delicate nature of most of the prozostrodontian taxa, much of which comprises mostly of crania or sometimes even only teeth. Here we present a rare opportunity to observe the osteohistology of several postcranial elements of the basal prozostrodontid Prozostrodon brasiliensis, the tritheledontid Irajatherium hernandezi, and the brasilodontids Brasilodon quadrangularis and Brasilitherium riograndensis from the Late Triassic of Brazil (Santa Maria Supersequence). Prozostrodon and Irajatherium reveal similar growth patterns of rapid early growth with annual interruptions later in ontogeny. These interruptions are associated with wide zones of slow growing bone tissue. Brasilodon and Brasilitherium exhibit a mixture of woven-fibered bone tissue and slower growing parallel-fibered and lamellar bone. The slower growing bone tissues are present even during early ontogeny. The relatively slower growth in Brasilodon and Brasilitherium may be related to their small body size compared to Prozostrodon and Irajatherium. These brasilodontids also exhibit osteohistological similarities with the Late Triassic/Early Jurassic mammaliaform Morganucodon and the Late Cretaceous multituberculate mammals Kryptobaatar and Nemegtbaatar.