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Uma Perspectiva Macroecológica Sobre O Risco De Extinção Em Mamíferos
Universidade Federal de Goiás Instituto de Ciências Biológicas Programa de Pós-graduação em Ecologia e Evolução Uma Perspectiva Macroecológica sobre o Risco de Extinção em Mamíferos VINÍCIUS SILVA REIS Goiânia 2019 VINÍCIUS SILVA REIS Uma Perspectiva Macroecológica sobre o Risco de Extinção em Mamíferos Tese apresentada ao Programa de Pós-graduação em Ecologia e Evolução do Departamento de Ecologia do Instituto de Ciências Biológicas da Universidade Federal de Goiás como requisito parcial para a obtenção do título de Doutor em Ecologia e Evolução. Orientador: Profº Drº Matheus de Souza Lima- Ribeiro Co-orientadora: Profª Drª Levi Carina Terribile Goiânia 2019 DEDI CATÓRIA Ao meu pai Wilson e à minha mãe Iris por sempre acreditarem em mim. “Esper o que próxima vez que eu te veja, você s eja um novo homem com uma vasta gama de novas experiências e aventuras. Não he site, nem se permita dar desculpas. Apenas vá e faça. Vá e faça. Você ficará muito, muito feliz por ter feito”. Trecho da carta escrita por Christopher McCandless a Ron Franz contida em Into the Wild de Jon Krakauer (Livre tradução) . AGRADECIMENTOS Eis que a aventura do doutoramento esteve bem longe de ser um caminho solitário. Não poderia ter sido um caminho tão feliz se eu não tivesse encontrado pessoas que me ensinaram desde método científico até como se bebe cerveja de verdade. São aos que estiveram comigo desde sempre, aos que permaneceram comigo e às novas amizades que eu construí quando me mudei pra Goiás que quero agradecer por terem me apoiado no nascimento desta tese: À minha família, em especial meu pai Wilson, minha mãe Iris e minha irmã Flora, por me apoiarem e me incentivarem em cada conquista diária. -
ESTUDO DA MORFOLOGIA DENTÁRIA DE Xenorhinotherium Bahiense CARTELLE & LESSA, 1988 (LITOPTERNA, MACRAUCHENIIDAE)
LEONARDO SOUZA LOBO ESTUDO DA MORFOLOGIA DENTÁRIA DE Xenorhinotherium bahiense CARTELLE & LESSA, 1988 (LITOPTERNA, MACRAUCHENIIDAE) UNIVERSIDADE FEDERAL DE VIÇOSA VIÇOSA MINAS GERAIS – BRASIL 2015 FichaCatalografica :: Fichacatalografica https://www3.dti.ufv.br/bbt/ficha/cadastrarficha/visua... Ficha catalográfica preparada pela Biblioteca Central da Universidade Federal de Viçosa - Câmpus Viçosa T Lobo, Leonardo Souza, 1989- L864e Estudo da morfologia dentária de Xenorhinotherium 2015 bahiense Cartelle & Lessa, 1988 (Litopterna, Macraucheniidae) / Leonardo Souza Lobo. - Viçosa, MG, 2015. x, 175f. : il. (algumas color.) ; 29 cm. Inclui anexos. Inclui apêndices. Orientador : Gisele Mendes Lessa Del Giúdice. Dissertação (mestrado) - Universidade Federal de Viçosa. Referências bibliográficas: f.100-119. 1. Morfologia animal. 2. Morfometria. 3. Arcada ósseo dentária. 4. Fóssil. 5. Xenorhinotherium bahiense. I. Universidade Federal de Viçosa. Departamento de Biologia Animal. Programa de Pós-graduação em Biologia Animal. II. Título. CDD 22. ed. 591.35 2 de 3 12-11-2015 14:15 LEONARDO SOUZA LOBO ESTUDO DA MORFOLOGIA DENTÁRIA DE Xenorhinotherium bahiense CARTELLE & LESSA, 1988 (LITOPTERNA, MACRAUCHENIIDAE) Dissertação apresentada à Universidade Federal de Viçosa, como parte das exigências do Programa de Pós- Graduação em Biologia Animal, para obtenção do título de Magister Scientiae. VIÇOSA MINAS GERAIS – BRASIL 2015 LEONARDO SOUZA LOBO ESTUDO DA MORFOLOGIA DENTÁRIA DE Xenorhinotherium bahiense CARTELLE & LESSA, 1988 (LITOPTERNA, MACRAUCHENIIDAE) Dissertação apresentada à Universidade Federal de Viçosa, como parte das exigências do Programa de Pós- Graduação em Biologia Animal, para obtenção do título de Magister Scientiae. APROVADA: 27 de março de 2015 _______________________ _______________________ Ana Maria Ribeiro Pedro Seyferth Ribeiro Romano (Coorientador) _______________________ Gisele Mendes Lessa del Giúdice (Orientadora) 'A tooth! A tooth! my kingdom for a tooth!' Thomas Huxley, 8 de Dezembro de 1858. -
Papers in Press
Papers in Press “Papers in Press” includes peer-reviewed, accepted manuscripts of research articles, reviews, and short notes to be published in Paleontological Research. They have not yet been copy edited and/or formatted in the publication style of Paleontological Research. As soon as they are printed, they will be removed from this website. Please note they can be cited using the year of online publication and the DOI, as follows: Humblet, M. and Iryu, Y. 2014: Pleistocene coral assemblages on Irabu-jima, South Ryukyu Islands, Japan. Paleontological Research, doi: 10.2517/2014PR020. doi:10.2517/2018PR013 Features and paleoecological significance of the shark fauna from the Upper Cretaceous Hinoshima Formation, Himenoura Group, Southwest Japan Accepted Naoshi Kitamura 4-8-7 Motoyama, Chuo-ku Kumamoto, Kumamoto 860-0821, Japan (e-mail: [email protected]) Abstract. The shark fauna of the Upper Cretaceous Hinoshima Formation (Santonian: 86.3–83.6 Ma) of the manuscriptHimenoura Group (Kamiamakusa, Kumamoto Prefecture, Kyushu, Japan) was investigated based on fossil shark teeth found at five localities: Himedo Park, Kugushima, Wadanohana, Higashiura, and Kotorigoe. A detailed geological survey and taxonomic analysis was undertaken, and the habitat, depositional environment, and associated mollusks of each locality were considered in the context of previous studies. Twenty-one species, 15 genera, 11 families, and 6 orders of fossil sharks are recognized from the localities. This assemblage is more diverse than has previously been reported for Japan, and Lamniformes and Hexanchiformes were abundant. Three categories of shark fauna are recognized: a coastal region (Himedo Park; probably a breeding site), the coast to the open sea (Kugushima and Wadanohana), and bottom-dwelling or near-seafloor fauna (Kugushima, Wadanohana, Higashiura, and Kotorigoe). -
Mammals from Upper Pleistocene of Afrânio, Pernambuco, Northeast of Brazil
Quaternary and Environmental Geosciences (2010) 02(2):01-11 Mamíferos do Pleistoceno Superior de Afrânio, Pernambuco, nordeste do Brasil Mammals from Upper Pleistocene of Afrânio, Pernambuco, northeast of Brazil Fabiana Marinho Silvaab, César Felipe Cordeiro Filgueirasac, Alcina Magnólia Franca Barretoad, Édison Vicente Oliveiraae a Universidade Federal de Pernambuco b c d e [email protected], [email protected], [email protected], [email protected] RESUMO Os mamíferos pleistocênicos são encontrados com frequência em toda a região Nordeste do Brasil. Os fósseis em geral ocorrem em tanques, lagoas, terraços fluviais, cavernas e ravinas. No estado de Pernambuco são registradas ocorrências de mamíferos pleistocênicos em 38 municípios. Neste trabalho, foram estudados aspectos taxonômicos e tafonômicos de paleofauna, preservada em lagoas da bacia do riacho Caboclo, tributário do rio São Francisco, em Afrânio, Pernambuco, Brasil. A pesquisa envolveu levantamento bibliográfico, cartográfico, trabalhos de campo e laboratoriais. Mais de 1.250 ossos, dentes e osteodermos foram estudados. A associação fossilífera é monotípica, poliespecífica, com os graus de fragmentação e desgaste variando em quatro classes. Os ossos foram preservados por conservação da composição química original, permineralização e substituição por calcita e por calcita magnesiana. Foi identificada uma diversificada fauna distribuída em cinco ordens (Tardigrada, Cingulata, Notoungulata, Proboscidea e Perissodactyla), sete famílias (Megatheriidae, Mylodontidae, Dasypodidae, Glyptodontidae, Toxodontidae, Gomphotheriidae e Equidae) com os taxa: Eremotherium laurillardi, Mylodonopsis ibseni, Panochthus greslebini, Holmesina paulacoutoi, Hoplophorus euphractus, Stegomastodon waringi, Toxodon platensis, equídeo e gliptodontideo indeterminados. Foram registrados pela primeira vez em Pernambuco os gêneros Hoplophorus e Mylodonopsis. A paleofauna é predominantemente herbívora, de um paleoambiente de savana ou cerrado. -
The Origin and Early Evolution of Dinosaurs
Biol. Rev. (2010), 85, pp. 55–110. 55 doi:10.1111/j.1469-185X.2009.00094.x The origin and early evolution of dinosaurs Max C. Langer1∗,MartinD.Ezcurra2, Jonathas S. Bittencourt1 and Fernando E. Novas2,3 1Departamento de Biologia, FFCLRP, Universidade de S˜ao Paulo; Av. Bandeirantes 3900, Ribeir˜ao Preto-SP, Brazil 2Laboratorio de Anatomia Comparada y Evoluci´on de los Vertebrados, Museo Argentino de Ciencias Naturales ‘‘Bernardino Rivadavia’’, Avda. Angel Gallardo 470, Cdad. de Buenos Aires, Argentina 3CONICET (Consejo Nacional de Investigaciones Cient´ıficas y T´ecnicas); Avda. Rivadavia 1917 - Cdad. de Buenos Aires, Argentina (Received 28 November 2008; revised 09 July 2009; accepted 14 July 2009) ABSTRACT The oldest unequivocal records of Dinosauria were unearthed from Late Triassic rocks (approximately 230 Ma) accumulated over extensional rift basins in southwestern Pangea. The better known of these are Herrerasaurus ischigualastensis, Pisanosaurus mertii, Eoraptor lunensis,andPanphagia protos from the Ischigualasto Formation, Argentina, and Staurikosaurus pricei and Saturnalia tupiniquim from the Santa Maria Formation, Brazil. No uncontroversial dinosaur body fossils are known from older strata, but the Middle Triassic origin of the lineage may be inferred from both the footprint record and its sister-group relation to Ladinian basal dinosauromorphs. These include the typical Marasuchus lilloensis, more basal forms such as Lagerpeton and Dromomeron, as well as silesaurids: a possibly monophyletic group composed of Mid-Late Triassic forms that may represent immediate sister taxa to dinosaurs. The first phylogenetic definition to fit the current understanding of Dinosauria as a node-based taxon solely composed of mutually exclusive Saurischia and Ornithischia was given as ‘‘all descendants of the most recent common ancestor of birds and Triceratops’’. -
2020 GSRS Abstract Book and Schedule.Pdf (12.83
VIRGINIA TECH DEPARTMENT OF GEOSCIENCES 25TH ANNUAL GEOSCIENCES STUDENT RESEARCH SYMPOSIUM FEBRUARY 13-14, 2020 KELLY HALL ROOM 310 HTTPS://GSRSVTGEOS.WIXSITE.COM/HOME GEOSCIENCES STUDENT RESEARCH SYMPOSIUM AT VT GEOS @GSRS_VTGEOS @GSRS_VTGEOS 25th Annual GSRS Welcome to the 2020 Geosciences Student Research Symposium. In 2020, we are celebrating the quadricentennial of GSRS, 25thGSRS. This event is entirely student-led and Fundraising and logistics are organized by a committee of graduate students. GSRS objectives are to help students gain experience in developing communication skills, event preparation, leadership, mentorship, and team-building. GSRS provides students a platform to communicate their research across the far-reaching disciplines of our department which promotes student growth as scientists in a collegial environment. Students also gain practice in communicating their research to a broad audience which offers a unique opportunity for students to prepare for future talks at national conferences. GSRS brings the geoscience family together through scientific talks, poster sessions, and discussions during Breakfasts, lunches, and department’s favorite banquet! GSRS would not be possible without the help of our greater geoscience family and friends. Thank you very much to everyone who donated to GSRS through our Virginia Tech Crowdfunding Campaign last fall. This symposium would not be possible without your generosity. Thank you to Carol Lee Donuts, Blacksburg Bagels, Due South, Moe’s, and Custom Catering for working with us through the catering process. Thank you to the VT Police Department and Rhino security for providing security at our banquet. Thank you very much to everyone in the Department of Geosciences (students, faculty, and staff) for helping to make GSRS possible. -
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. -
A Beaked Herbivorous Archosaur with Dinosaur Affinities from the Early Late Triassic of Poland
Journal of Vertebrate Paleontology 23(3):556±574, September 2003 q 2003 by the Society of Vertebrate Paleontology A BEAKED HERBIVOROUS ARCHOSAUR WITH DINOSAUR AFFINITIES FROM THE EARLY LATE TRIASSIC OF POLAND JERZY DZIK Instytut Paleobiologii PAN, Twarda 51/55, 00-818 Warszawa, Poland, [email protected] ABSTRACTÐAn accumulation of skeletons of the pre-dinosaur Silesaurus opolensis, gen. et sp. nov. is described from the Keuper (Late Triassic) claystone of KrasiejoÂw in southern Poland. The strata are correlated with the late Carnian Lehrberg Beds and contain a diverse assemblage of tetrapods, including the phytosaur Paleorhinus, which in other regions of the world co-occurs with the oldest dinosaurs. A narrow pelvis with long pubes and the extensive development of laminae in the cervical vertebrae place S. opolensis close to the origin of the clade Dinosauria above Pseudolagosuchus, which agrees with its geological age. Among the advanced characters is the beak on the dentaries, and the relatively low tooth count. The teeth have low crowns and wear facets, which are suggestive of herbivory. The elongate, but weak, front limbs are probably a derived feature. INTRODUCTION oped nutrient foramina in its maxilla. It is closely related to Azendohsaurus from the Argana Formation of Morocco (Gauf- As is usual in paleontology, with an increase in knowledge fre, 1993). The Argana Formation also has Paleorhinus, along of the fossil record of early archosaurian reptiles, more and with other phytosaurs more advanced than those from Krasie- more lineages emerge or extend their ranges back in time. It is joÂw (see Dutuit, 1977), and it is likely to be somewhat younger. -
Late Cenozoic Large Mammal and Tortoise Extinction in South America
Cione et al: Late Cenozoic extinction Rev.in South Mus. America Argentino Cienc. Nat., n.s.1 5(1): 000, 2003 Buenos Aires. ISSN 1514-5158 The Broken Zig-Zag: Late Cenozoic large mammal and tortoise extinction in South America Alberto L. CIONE1, Eduardo P. TONNI1, 2 & Leopoldo SOIBELZON1 1Departamento Científico Paleontología de Vertebrados, 'acultad de Ciencias Naturales y Museo, Paseo del Bosque, 1900 La Plata, Argentina. 2Laboratorio de Tritio y Radiocarbono, LATYR. 'acultad de Ciencias Naturales y Museo, Paseo del Bosque, 1900 La Plata, Argentina. E-mail: [email protected], [email protected], [email protected]. Corresponding author: Alberto L. CIONE Abstract: During the latest Pleistocene-earliest Holocene, South American terrestrial vertebrate faunas suffered one of the largest (and probably the youngest) extinction in the world for this lapse. Megamammals, most of the large mammals and a giant terrestrial tortoise became extinct in the continent, and several complete ecological guilds and their predators disappeared. This mammal extinction had been attributed mainly to overkill, climatic change or a combination of both. We agree with the idea that human overhunting was the main cause of the extinction in South America. However, according to our interpretation, the slaughtering of mammals was accom- plished in a particular climatic, ecological and biogeographical frame. During most of the middle and late Pleis- tocene, dry and cold climate and open areas predominated in South America. Nearly all of those megamammals and large mammals that became extinct were adapted to this kind of environments. The periodic, though rela- tively short, interglacial increases in temperature and humidity may have provoked the dramatic shrinking of open areas and extreme reduction of the biomass (albeit not in diversity) of mammals adapted to open habitats. -
To Link and Cite This Article: Doi
Submitted: October 1st, 2019 – Accepted: June 8th, 2020 – Published online: June 11th, 2020 To link and cite this article: doi: https://doi.org/10.5710/AMGH.08.06.2020.3306 1 COTYLAR FOSSA, ITS INTERPRETATION AND FUNCTIONALITY. 2 THE CASE FROM SOUTH AMERICAN NATIVE UNGULATES 3 4 MALENA LORENTE1,2, 3 5 1 División Paleontología de Vertebrados, Museo de La Plata. Paseo del Bosque s/n B1900FWA, La 6 Plata, Buenos Aires, Argentina; [email protected]; 2 CONICET; 3 Facultad de Ciencias 7 Naturales y Museo 8 9 Number of pages: 21, 7 figures 10 Proposed header: LORENTE, COTYLAR FOSSA 1 11 12 Abstract. The cotylar fossa is a complex anatomical character in the astragalar medial malleolar 13 facet. It represents a dynamic relationship between the astragalus and the tibia in the upper tarsal 14 joint. The astragalus must accommodate the medial tibial malleolus when the tibia is in an extreme 15 flexion. It is one of the three morphological synapomorphies considered for Afrotheria, although it 16 is also a recurrent trait among different groups of mammals. Here, fossil South American Native 17 Ungulates and extant mammals were surveyed to reevaluate how much this character is spread and 18 how variable it is. Beyond afrotherians, it is observed that it also appears in primates, macropodid 19 marsupials, laurasiatherian archaic ungulates, perissodactyls, pantodonts, and dinoceratans; it is also 20 in some but not all of the extinct endemic ungulates from South America. No function has been 21 suggested before for the presence of a cotylar fossa. The cotylar fossa could be an adaptation to a 22 passive, rest related posture. -
Electron Spin Resonance Dating of the Late Quaternary Megafauna Fossils from Baixa Grande, Bahia, Brazil
Quaternary International 305 (2013) 91e96 Contents lists available at SciVerse ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Electron Spin Resonance dating of the Late Quaternary megafauna fossils from Baixa Grande, Bahia, Brazil R.C. Ribeiro a, Angela Kinoshita b,c, Ana Maria Graciano Figueiredo d, I.S. Carvalho a, Oswaldo Baffa b,* a Universidade Federal do Rio de Janeiro, Instituto de Geociências e Departamento de Geologia, Rio de Janeiro-RJ, Brazil b Departamento de Física, Faculdade de Filosofia, Ciências e Letras, Universidade de São Paulo, 14040-901 Ribeirão Preto, SP, Brazil c Universidade Sagrado Coração, Bauru-SP, Brazil d Instituto de Pesquisas Energéticas e Nucleares (IPEN), São Paulo-SP, Brazil article info abstract Article history: Electron Spin Resonance (ESR) spectroscopy was applied to date megafauna fossil teeth of Stegomastodon Available online 20 July 2012 À waringi and Toxodontinae (two teeth) found in Baixa Grande, Bahia, Brazil. The CO2 signal with spec- troscopic features gt ¼ 2.0018 and g// ¼ 1.9973 used for ESR dating was detected in all fossil enamel. The additive method was employed to construct the dose response curve and to calculate the Equivalent Dose (De). Neutron Activation Analysis of enamel, dentine and soil where the samples were buried was used to determine the main radioisotopes concentration. These data were used in the conversion of De into age, using the ROSY ESR dating software. The results of age obtained were 50 Æ 10 ka for S. waringi, and 43 Æ 8 ka and 9 Æ 2 ka for Toxodontinae teeth. Although Late Quaternary fossils from the extinct South American megafauna are relatively common in Brazilian’s Northeast region, few geochronological studies were conducted. -
The Paleoenvironments of Azhdarchid Pterosaurs Localities in the Late Cretaceous of Kazakhstan
A peer-reviewed open-access journal ZooKeys 483:The 59–80 paleoenvironments (2015) of azhdarchid pterosaurs localities in the Late Cretaceous... 59 doi: 10.3897/zookeys.483.9058 RESEARCH ARTICLE http://zookeys.pensoft.net Launched to accelerate biodiversity research The paleoenvironments of azhdarchid pterosaurs localities in the Late Cretaceous of Kazakhstan Alexander Averianov1,2, Gareth Dyke3,4, Igor Danilov5, Pavel Skutschas6 1 Zoological Institute of the Russian Academy of Sciences, Universitetskaya nab. 1, 199034 Saint Petersburg, Russia 2 Department of Sedimentary Geology, Geological Faculty, Saint Petersburg State University, 16 liniya VO 29, 199178 Saint Petersburg, Russia 3 Ocean and Earth Science, National Oceanography Centre, Sou- thampton, University of Southampton, Southampton SO14 3ZH, UK 4 MTA-DE Lendület Behavioural Ecology Research Group, Department of Evolutionary Zoology and Human Biology, University of Debrecen, 4032 Debrecen, Egyetem tér 1, Hungary 5 Zoological Institute of the Russian Academy of Sciences, Universi- tetskaya nab. 1, 199034 Saint Petersburg, Russia 6 Department of Vertebrate Zoology, Biological Faculty, Saint Petersburg State University, Universitetskaya nab. 7/9, 199034 Saint Petersburg, Russia Corresponding author: Alexander Averianov ([email protected]) Academic editor: Hans-Dieter Sues | Received 3 December 2014 | Accepted 30 January 2015 | Published 20 February 2015 http://zoobank.org/C4AC8D70-1BC3-4928-8ABA-DD6B51DABA29 Citation: Averianov A, Dyke G, Danilov I, Skutschas P (2015) The paleoenvironments of azhdarchid pterosaurs localities in the Late Cretaceous of Kazakhstan. ZooKeys 483: 59–80. doi: 10.3897/zookeys.483.9058 Abstract Five pterosaur localities are currently known from the Late Cretaceous in the northeastern Aral Sea region of Kazakhstan. Of these, one is Turonian-Coniacian in age, the Zhirkindek Formation (Tyulkili), and four are Santonian in age, all from the early Campanian Bostobe Formation (Baibishe, Akkurgan, Buroinak, and Shakh Shakh).