Glossary of Terms Extreme Mammals
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Dinosaur Wars Program Transcript
Page 1 Dinosaur Wars Program Transcript Narrator: For more than a century, Americans have had a love affair with dinosaurs. Extinct for millions of years, they were barely known until giant, fossil bones were discovered in the mid-nineteenth century. Two American scientists, Edward Drinker Cope and Othniel Charles Marsh, led the way to many of these discoveries, at the forefront of the young field of paleontology. Jacques Gauthier, Paleontologist: Every iconic dinosaur every kid grows up with, apatosaurus, triceratops, stegosaurus, allosaurus, these guys went out into the American West and they found that stuff. Narrator: Cope and Marsh shed light on the deep past in a way no one had ever been able to do before. They unearthed more than 130 dinosaur species and some of the first fossil evidence supporting Darwin’s new theory of evolution. Mark Jaffe, Writer: Unfortunately there was a more sordid element, too, which was their insatiable hatred for each other, which often just baffled and exasperated everyone around them. Peter Dodson, Paleontologist: They began life as friends. Then things unraveled… and unraveled in quite a spectacular way. Narrator: Cope and Marsh locked horns for decades, in one of the most bitter scientific rivalries in American history. Constantly vying for leadership in their young field, they competed ruthlessly to secure gigantic bones in the American West. They put American science on the world stage and nearly destroyed one another in the process. Page 2 In the summer of 1868, a small group of scientists boarded a Union Pacific train for a sightseeing excursion through the heart of the newly-opened American West. -
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. -
First Palaeohistological Inference of Resting
First palaeohistological inference of resting metabolic rate in an extinct synapsid, Moghreberia nmachouensis (Therapsida: Anomodontia) Chloe Olivier, Alexandra Houssaye, Nour-Eddine Jalil, Jorge Cubo To cite this version: Chloe Olivier, Alexandra Houssaye, Nour-Eddine Jalil, Jorge Cubo. First palaeohistological inference of resting metabolic rate in an extinct synapsid, Moghreberia nmachouensis (Therapsida: Anomodon- tia). Biological Journal of the Linnean Society, Linnean Society of London, 2017, 121 (2), pp.409-419. 10.1093/biolinnean/blw044. hal-01625105 HAL Id: hal-01625105 https://hal.sorbonne-universite.fr/hal-01625105 Submitted on 27 Oct 2017 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. First palaeohistological inference of resting metabolic rate in extinct synapsid, Moghreberia nmachouensis (Therapsida: Anomodontia) CHLOE OLIVIER1,2, ALEXANDRA HOUSSAYE3, NOUR-EDDINE JALIL2 and JORGE CUBO1* 1 Sorbonne Universités, UPMC Univ Paris 06, CNRS, UMR 7193, Institut des Sciences de la Terre Paris (iSTeP), 4 place Jussieu, BC 19, 75005, Paris, France 2 Sorbonne Universités -CR2P -MNHN, CNRS, UPMC-Paris6. Muséum national d’Histoire naturelle. 57 rue Cuvier, CP38. F-75005, Paris, France 3Département Écologie et Gestion de la Biodiversité, UMR 7179, CNRS/Muséum national d’Histoire naturelle, 57 rue Cuvier, CP 55, Paris, 75005, France *Corresponding author. -
Recent Advances in Studies on Mesozoic and Paleogene Mammals in China
Vol.24 No.2 2010 Paleomammalogy Recent Advances in Studies on Mesozoic and Paleogene Mammals in China WANG Yuanqing* and NI Xijun Institute of Vertebrate Paleontology and Paleoanthropology, CAS, Beijing 10004, China ike in other fields of paleontology, research in from the articular of the lower jaw and the quadrate of the paleomammalogy mainly falls into two aspects. cranium following the process of reduction and detachment LOne is related to the biological nature of fossil from the reptilian mandible, are new elements of the bony mammals, such as their systematics, origin, evolution, chain in the mammalian middle ear. The appearance of phylogenetic relationships, transformation of key features mammalian middle ear allows mammals to hear the sound and paleobiogeography, and the other is related to the of higher frequencies than reptiles do. Generally speaking, geological context, involving biostratigraphy, biochronology, a widely accepted hypothesis is that mammals originated faunal turnover and its relations to the global and regional from a certain extinct reptilian group. The formation and environmental changes. In the last decade, a number of development of the definitive mammalian middle ear well-preserved mammalian specimens were collected from (DMME) has thus become one of the key issues in the study different localities around the country. Such discoveries have of mammalian evolution and has drawn the attention from provided significant information for understanding the early many researchers for many years. evolution of mammals and reconstructing the phylogeny of Developmental biological studies have proven the early mammals. function of the Meckel’s cartilage and its relationship to Studies of Chinese Mesozoic mammals achieved the ear ossicles during the development of mammalian remarkable progress in the past several years. -
Mammalian Origins Major Groups of Synapsida
Mammalogy 4764 9/16/2009 Chapter 4 “Reptile” Mammalian Origins Early mammal Carnivore Amniota Herbivore Feldhamer Table 4.1 Savage and Long 1986 Major Fig. 3.2, Vaughn, Fig. 4.1, Feldhamer groups Mammalian Origins of Dimetrodon Overview Synapsida Synapsids Pelycosaurs and Therapsids First Mammals Mesozoic Era appear Feldhamer Fig. 4.2 Cenozoic Era radiate Savage and Long 1986 Pelycosaur Skull, jaw musculature, and teeth Cynodontia -- Advanced, predaceous therapsids Pelycosaur Scymnognathus Cynognathus Therapsid Early Cynodont Derived Therapsid/Mammal Primitive Late Cynodont Fig. 3.2, Vaughn Thrinaxodon Fig 4.3 & 4, Feldhamer 1 Mammalogy 4764 9/16/2009 Skeletal transition Extinction of Cynodonts Possibly competition from dinosaurs Pelycosaur Early Cynodonts were dog-size, last surviving were squirrel sized Fig. 4.15 Mammals that survived while Cynodonts went extinct (contemporary) were mouse-sized. Cynodont Thrinaxodon Modern Mammal Fig. 3.5, Vaughn Fig. 4.16c, Early Cynodont Early mammals Changes in land masses Feldhamer 4.11 200 - 250 million years ago Derived characters: Dentary/squamosal jaw articulation Diphyodont dentition 200 MYA 180 MYA Mammary glands Secondary palate Early Mid- Viviparity (loss of eggshell) When? Jurassic Jurassic 65 MYA 135 MYA Early Early Cretaceous Cenozoic Feldhamer 4.5, 4.9 Skull and teeth of mammals 2 Mammalogy 4764 9/16/2009 Teeth and Dentition of Mammals Teeth Heterodont teeth with different functions Differentiated on the basis of function, resulting in increased One of the major keys efficiency acquiring and digesting food. to success of mammals Teeth occur in 3 bones of skull: Teeth of mammals are premaxilla, maxilla, dentary extremely variable with different diets -- more than other taxa Feldhamer et al. -
Attachment J Assessment of Existing Paleontologic Data Along with Field Survey Results for the Jonah Field
Attachment J Assessment of Existing Paleontologic Data Along with Field Survey Results for the Jonah Field June 12, 2007 ABSTRACT This is compilation of a technical analysis of existing paleontological data and a limited, selective paleontological field survey of the geologic bedrock formations that will be impacted on Federal lands by construction associated with energy development in the Jonah Field, Sublette County, Wyoming. The field survey was done on approximately 20% of the field, primarily where good bedrock was exposed or where there were existing, debris piles from recent construction. Some potentially rich areas were inaccessible due to biological restrictions. Heavily vegetated areas were not examined. All locality data are compiled in the separate confidential appendix D. Uinta Paleontological Associates Inc. was contracted to do this work through EnCana Oil & Gas Inc. In addition BP and Ultra Resources are partners in this project as they also have holdings in the Jonah Field. For this project, we reviewed a variety of geologic maps for the area (approximately 47 sections); none of maps have a scale better than 1:100,000. The Wyoming 1:500,000 geology map (Love and Christiansen, 1985) reveals two Eocene geologic formations with four members mapped within or near the Jonah Field (Wasatch – Alkali Creek and Main Body; Green River – Laney and Wilkins Peak members). In addition, Winterfeld’s 1997 paleontology report for the proposed Jonah Field II Project was reviewed carefully. After considerable review of the literature and museum data, it became obvious that the portion of the mapped Alkali Creek Member in the Jonah Field is probably misinterpreted. -
EXTREME MAMMALS Amnh.Org/Extrememammals GRADES 3-5 ACTIVITIES
EXTREME MAMMALS amnh.org/extrememammals GRADES 3-5 ACTIVITIES Welcome to Extreme Mammals: The Biggest, Smallest, and Most Amazing Mammals of All Time. Use this sheet to help your class explore what makes a mammal a mammal, and discover what’s normal or extreme when it comes to this incredibly diverse group of animals. The activities below and on the Student Worksheet can be adapted to meet your students’ interests and abilities. BEFORE YOUR VISIT New York State Science Class Discussion: Mammals live everywhere from the sea to the treetops, Core Curriculum and have evolved to swim, glide, burrow, run, hop, climb trees, and even Major Understanding LE 3.1c fl y. Start a discussion by asking students what they think is “normal” for In order to survive in their a mammal when it comes to size, shape, or behavior. What’s “extreme” environment, plants and animals or unusual, and why? For information to support the discussion, refer to must adapt to that environment. the Essential Questions section of the Guide. Research Activity: After your discussion, have students go on a Web Hunt: Dioramas Coming to Life (www2.scholastic.com/ browse/article.jsp?id=11422). Ask students to fi nd examples of mammals on their hunt that will help them fi nd answers to these questions: What is a mammal? What’s “normal” for mammals? and How and why are some mammals “extreme”? DURING YOUR VISIT IN THE EXTREME MAMMALS EXHIBITION Students can use the reproducible on the Use the activities and guiding questions in Sections 1 and 2 reverse side of this sheet to further explore these of Teaching in the Exhibition in this Guide to help students concepts. -
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. -
The Origin of Mammals: a Study of Some Important Fossils
CEN Tech. J., vol. 7(2), 1993, pp. 122–139 The Origin of Mammals: A Study of Some Important Fossils A. W. MEHLERT ABSTRACT For many years evolutionists have pointed to the alleged transition of reptiles to mammals as being the best example of the natural origin of a major taxon. At first sight such claims appear to have considerable justification, but when the fossil evidence is closely examined it can be shown that there are some grave deficiencies, and the claim is not only factually unproved but also contains a number of dubious assumptions. It is therefore proposed to subject certain of the key fossils to more scrutiny. INTRODUCTION AND BRIEF OVERVIEW therapsids of later Permian and Triassic ‘times’. It is supposedly within the order Therapsida (suborder In 1966 Olson wrote, Theriodontia), that we find the subgroups to which the ‘The reptilian-mammalian transition has by far the immediate ancestors of mammals are assigned (see Table finest record of showing the origin of a new 24). class.’ (Emphasis added.)1 Almost all authorities are convinced that the immediate Kemp in 1982 had the same view.2 If it can be shown that reptilian ancestors of the early mammals are to be found in such a claim is not as strong as Olson and Kemp believe, the infraorders Cynodontia, Tritylodontia and Ictidosauria, then by implication, the evolutionary origin of all other although all six theriodont subgroups contain fossils which classes in the animal and plant kingdoms must be even more appear to bear at least some mammalian-like features. doubtful. -
SUPPLEMENTARY INFORMATION: Tables, Figures and References
Samuels, Regnault & Hutchinson, PeerJ Evolution of the patellar sesamoid bone in mammals SUPPLEMENTARY INFORMATION: Tables, Figures and References Supplementary Table S1: Mammaliaform patellar status$ Inclusive clades Genus and Stratigraphic age of Patellar Comments# (partial) species (and taxon, and location(s) state reference(s) used for 0/1/2 patellar status) (absent/ ‘patelloid’/ present) Sinoconodonta Sinoconodon Jurassic, China 0 Patellar groove absent, suggests no rigneyi (Kielan- patella Jaworowska et al., 2004) Sinoconodon is included on our phylogeny within tritylodontids. Morganucodonta Megazostrodon Late Triassic, southern 0 rudnerae (Jenkins Africa & Parrington, 1976) Morganucodonta Eozostrodon sp. Late Triassic, Wales 0 Asymmetric patellar groove, (Jenkins et al., specimens disarticulated so it is hard 1976) to assess the patella but appears absent Docodonta Castorocauda 164 Mya, mid-Jurassic, 0 Semi-aquatic adaptations lutrasimilis (Ji et China al., 2006) Docodonta Agilodocodon 164 Mya, mid-Jurassic, 0 scansorius (Meng China et al., 2015) Docodonta Docofossor 160 Mya, China 0 brachydactylus (Luo et al., 2015b) Docodonta Haldanodon 150-155 Mya, Late 0 Shallow patellar groove exspectatus Jurassic, Portugal (Martin, 2005b) Australosphenida Asfaltomylos Mid-Jurassic, South ? Postcranial material absent patagonicus America (Martin, 2005a) Australosphenida Ornithorhynchus Extant 2 Platypus, genome sequenced Monotremata anatinus (Warren, Hillier, Marshall Graves et (Herzmark, 1938; al., 2008) Rowe, 1988) Australosphenida Tachyglossus -
FROM the EARLY CRETACEOUS (BARREMIAN) WESSEX FORMATION OFTHEISLEOFWIGHT,SOUTHERNBRITAIN by STEVEN C
[Palaeontology, Vol. 49, Part 4, 2006, pp. 889–897] A GOBICONODONTID (MAMMALIA, EUTRICONODONTA) FROM THE EARLY CRETACEOUS (BARREMIAN) WESSEX FORMATION OFTHEISLEOFWIGHT,SOUTHERNBRITAIN by STEVEN C. SWEETMAN School of Earth and Environmental Sciences, University of Portsmouth, Burnaby Building, Burnaby Road, Portsmouth PO1 3QL, UK; e-mail: [email protected] Typescript received 16 June 2004; accepted in revised form 20 June 2005 Abstract: Bulk screening of Early Cretaceous (Barremian) gobiconodontid mammal in Early Cretaceous deposits of strata of the Wessex Formation, exposed in sections on Britain sheds further light on the palaeogeographical distri- the south-west and south-east coasts of the Isle of Wight, bution of an apparently successful clade of Early Creta- southern England, has resulted in the recovery of mammal ceous mammals and together with the occurrence of a remains, the first to be obtained from Wealden Group gobiconodontid in the earliest Cretaceous of North Africa strata since the early 1970s. The fauna comprises at least calls into question recent hypotheses concerning the area six taxa represented by isolated teeth and in addition, in of origin of the Gobiconodontidae and mechanisms of dis- the case of an as yet undescribed spalacotheriid, a partial persal therefrom. dentary. One of the teeth, a distal premolar, is of unique tricuspid, single-rooted morphology and represents the first Key words: Britain, Cretaceous, Gobiconodontidae, Mam- British record of the Gobiconodontidae. Discovery of a malia, palaeogeography, premolar. The Early Cretaceous (Barremian, Wealden Group) which may or may not be of mammalian origin (pers. Wessex Formation of the Isle of Wight, southern England obs.