Does the Jurassic Agilodocodon (Mammaliaformes, Docodonta) Have Any Exudativorous Dental Features?
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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. -
The Genome of the Pyrenean Desman and the Effects of Bottlenecks and Inbreeding on the Genomic Landscape of an Endangered Species
Received: 18 August 2020 | Revised: 19 March 2021 | Accepted: 27 April 2021 DOI: 10.1111/eva.13249 ORIGINAL ARTICLE The genome of the Pyrenean desman and the effects of bottlenecks and inbreeding on the genomic landscape of an endangered species Lídia Escoda | Jose Castresana Institute of Evolutionary Biology (CSIC- Universitat Pompeu Fabra), Barcelona, Spain Abstract The Pyrenean desman (Galemys pyrenaicus) is a small semiaquatic mammal endemic Correspondence Jose Castresana, Institute of Evolutionary to the Iberian Peninsula. Despite its limited range, this species presents a strong ge- Biology (CSIC- Universitat Pompeu Fabra), netic structure due to past isolation in glacial refugia and subsequent bottlenecks. Passeig Marítim de la Barceloneta 37, 08003 Barcelona, Spain. Additionally, some populations are highly fragmented today as a consequence of river Email: [email protected] barriers, causing substantial levels of inbreeding. These features make the Pyrenean Funding information desman a unique model in which to study the genomic footprints of differentiation, Plan Nacional I+D+i del Ministerio de bottlenecks and extreme isolation in an endangered species. To understand these Ciencia e Innovación, Grant/Award Number: CGL2017- 84799- P (MINECO/AEI/FEDER, UE) processes, the complete genome of the Pyrenean desman was sequenced and as- sembled using a Bloom filter- based approach. An analysis of the 1.83 Gb reference genome and the sequencing of five additional individuals from different evolutionary units allowed us to detect its main genomic characteristics. The population differen- tiation of the species was reflected in highly distinctive demographic trajectories. In addition, a severe population bottleneck during the postglacial recolonization of the eastern Pyrenees created one of the lowest genomic heterozygosity values recorded in a mammal. -
Checklist of Rodents and Insectivores of the Mordovia, Russia
ZooKeys 1004: 129–139 (2020) A peer-reviewed open-access journal doi: 10.3897/zookeys.1004.57359 RESEARCH ARTICLE https://zookeys.pensoft.net Launched to accelerate biodiversity research Checklist of rodents and insectivores of the Mordovia, Russia Alexey V. Andreychev1, Vyacheslav A. Kuznetsov1 1 Department of Zoology, National Research Mordovia State University, Bolshevistskaya Street, 68. 430005, Saransk, Russia Corresponding author: Alexey V. Andreychev ([email protected]) Academic editor: R. López-Antoñanzas | Received 7 August 2020 | Accepted 18 November 2020 | Published 16 December 2020 http://zoobank.org/C127F895-B27D-482E-AD2E-D8E4BDB9F332 Citation: Andreychev AV, Kuznetsov VA (2020) Checklist of rodents and insectivores of the Mordovia, Russia. ZooKeys 1004: 129–139. https://doi.org/10.3897/zookeys.1004.57359 Abstract A list of 40 species is presented of the rodents and insectivores collected during a 15-year period from the Republic of Mordovia. The dataset contains more than 24,000 records of rodent and insectivore species from 23 districts, including Saransk. A major part of the data set was obtained during expedition research and at the biological station. The work is based on the materials of our surveys of rodents and insectivo- rous mammals conducted in Mordovia using both trap lines and pitfall arrays using traditional methods. Keywords Insectivores, Mordovia, rodents, spatial distribution Introduction There is a need to review the species composition of rodents and insectivores in all regions of Russia, and the work by Tovpinets et al. (2020) on the Crimean Peninsula serves as an example of such research. Studies of rodent and insectivore diversity and distribution have a long history, but there are no lists for many regions of Russia of Copyright A.V. -
Functional Morphology of the Vertebral Column in Remingtonocetus (Mammalia, Cetacea) and the Evolution of Aquatic Locomotion in Early Archaeocetes
Functional Morphology of the Vertebral Column in Remingtonocetus (Mammalia, Cetacea) and the Evolution of Aquatic Locomotion in Early Archaeocetes by Ryan Matthew Bebej A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Ecology and Evolutionary Biology) in The University of Michigan 2011 Doctoral Committee: Professor Philip D. Gingerich, Co-Chair Professor Philip Myers, Co-Chair Professor Daniel C. Fisher Professor Paul W. Webb © Ryan Matthew Bebej 2011 To my wonderful wife Melissa, for her infinite love and support ii Acknowledgments First, I would like to thank each of my committee members. I will be forever grateful to my primary mentor, Philip D. Gingerich, for providing me the opportunity of a lifetime, studying the very organisms that sparked my interest in evolution and paleontology in the first place. His encouragement, patience, instruction, and advice have been instrumental in my development as a scholar, and his dedication to his craft has instilled in me the importance of doing careful and solid research. I am extremely grateful to Philip Myers, who graciously consented to be my co-advisor and co-chair early in my career and guided me through some of the most stressful aspects of life as a Ph.D. student (e.g., preliminary examinations). I also thank Paul W. Webb, for his novel thoughts about living in and moving through water, and Daniel C. Fisher, for his insights into functional morphology, 3D modeling, and mammalian paleobiology. My research was almost entirely predicated on cetacean fossils collected through a collaboration of the University of Michigan and the Geological Survey of Pakistan before my arrival in Ann Arbor. -
Communications from the Mammal Society ± No. 77
J. Zool., Lond. (1998) 246, 443±486 # 1998 The Zoological Society of London Printed in the United Kingdom Communications from the Mammal Society ± No. 77 Edited by M. L. Gorman J. Zool., Lond. (1998) 246, 443±445 # 1998 The Zoological Society of London DNA ®ngerprinting reveals high levels of genetic diversity within British populations of the introduced non-native grey squirrel (Sciurus carolinensis) Z. K. David-Gray 1*, J. Gurnell2 and D. M. Hunt3 1 Department of Biology, Imperial College, University of London, Prince Consort Road, London SW7 2BB, U.K. 2 School of Biological Sciences, Queen Mary and West®eld College, University of London, Mile End Road, London E1 4NS, U.K. 3 Department of Molecular Genetics, Institute of Ophthalmology, University College London, Bath Street, London EC1V 9EL, U.K. INTRODUCTION genetic diversity as a result of recent population bottle- necks. We have used DNA ®ngerprinting (Jeffreys, In general, if populations are founded by very small Wilson & Thein, 1985a), a technique which provides a numbers of individuals, low levels of genetic diversity good indication of genome variability (Jeffreys et al., amongst subsequent generations known as founder 1985b; Kuhnlein et al., 1990; Kunieda et al., 1993) to effects, can be predicted to occur as a result of genetic assess overall levels of genetic diversity in two British drift (Franklin, 1980; Lacy, 1997). A loss of genetic grey squirrel populations; Alice Holt Forest on the variation has been reported in several species that have borders of Hampshire and Surrey in southern England experienced genetic bottlenecks because of habitat and Thetford Forest in East Anglia. -
Femur of a Morganucodontid Mammal from the Middle Jurassic of Central Russia
Femur of a morganucodontid mammal from the Middle Jurassic of Central Russia PETR P. GAMBARYAN and ALEXANDER 0.AVERIANOV Gambaryan, P.P. & Averianov, A.O. 2001. Femur of a morganucodontid mammal from the Middle Jurassic of Central Russia. -Acta Palaeontologica Polonica 46,1,99-112. We describe a nearly complete mammalian femur from the Middle Jurassic (upper Bathonian) from Peski quarry, situated some 100 km south east of Moscow, central Rus- sia. It is similar to the femora of Morganucodontidae in having a globular femoral head, separated from the greater trochanter and reflected dorsally, fovea capitis present, both trochanters triangular and located on the same plane, distal end flat, mediolaterally expanded, and somewhat bent ventrally, and in the shape and proportions of distal condyles. It is referred to as Morganucodontidae gen. et sp. indet. It is the first representa- tive of this group of mammals in Eastern Europe from the third Mesozoic mammal local- ity discovered in Russia. Exquisite preservation of the bone surface allowed us to recon- struct partial hind limb musculature. We reconstruct m. iliopsoas as inserting on the ridge, which starts at the lesser trochanter and extends along the medial femoral margin for more than half of the femur length. On this basis we conclude that the mode of loco- motion of the Peski morganucodontid was similar to that of modern echidnas. During the propulsive phase the femur did not retract and the step elongation was provided by pronation of the femur. Key words : Mammalia, Morganucodontidae, femur, anatomy, locomotion, Jurassic, Russia. Petr P. Gambaryan [[email protected]] and Alexander 0. -
Hair Types in the Fur of the Pyrenean Desman (Insectivora: Talpidae
Hair Types©Akademie in d. Wissenschaften the Fur Wien; downloadof the unter www.biologiezentrum.atPyrenean Desman (Galemys pyrenaicus) GEOFFROY, 1811 (Insectivora: Talpidae: Desmaninae)* B y W a l t e r P o d u s c h k a & Be r n a r d R ic h a r d Mit 7 Figuren (Vorgelegt in der Sitzung der mathem.-naturw. Klasse am 14. März 1985 durch das k. M. Fried rich Sc h a l l e r ) Introduction For more than 25 years, American Mink (Mustela vison SCHREBER, 1877) escaped from a fur farm near El Espinar (Sierra Guadarrama, in northern Central Spain). They quickly spread and are suspected of being the main culprits in the extermination of the local Desman population. However, since this sad fact may also be due to water pollution, to "scientists” and unscrupulous lifetrapping or to the destruction of decidous forests along the riverbanks and their replacement with conifers, the M ink’s alleged guilt has to be substantiated through the finding of Desman bones and/or hair in their faeces. Unfortunately no such proof has yet been undertaken, due mostly to the lack of knowledge about the characteristics of the Desman’s fur. This paper is intended to amend this insufficiency. DAY (1966) published details of a method for the identification of mammalian hair in the faeces of predators, but he distinguished only two hair types: woolly hairs and sharply bent guard hairs. Unfortunately, his general remarks about the lack of a clear distinction between these two types of guard hair and “fine” (= woolly) hairs in the insectivores are incorrect. -
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. -
The History of the World in Comics
TABLE OF CONTENTS Earth Is Born 6 THE CENOZOIC 43 On the Prairies 44 THE PRECAMBRIAN 7 In the Trees 45 The Cradle of Life 8 Little Horses 46 The First Cells 9 The New Giants 47 A World of Microbes 10 Walking Whales 48 Upheavals 1 1 Swimming Whales 49 The First Faunas 12 Trumpeters 50 Island America 5 1 THE PALEOZOIC 13 The Rise of the Ruminants 52 The Explosion of Life 14 The Giraffe’s Neck 53 Pincers of the Sea 15 Teeth in the Sea 54 Conquering the Continents 16 Teeth on Land 55 Jaws of the Sea 17 The Hominids 56 The March of the Fish 18 On Four Feet 19 THE QUATERNARY 57 The Great Forest 20 The Ice Ages 58 Born on Land 2 1 Megafauna of the Tundra 59 The First Giants 22 The Reunion of the Americas 60 Reptiles Unlike the Others 23 An Island Continent 6 1 The Great Extinction 24 The First Humans 62 Conquering the World 63 THE MESOZOIC 25 Mini-Elephants of the Islands 64 The Time of the Crocs 26 Cro-Magnon 65 The First Dinosaurs 27 The Great Warming 66 The First Mammals 28 The Pterosaurs 29 THE TIME OF THE HUMANS 67 The Jurassic Sea 30 The Agricultural Revolution 68 Sea Monsters 3 1 Cows, Pigs, Poultry 69 The Ornithischians 32 The Industrial Revolution 70 The Epic of the Stegosaurs 33 The Sixth Extinction 7 1 The Sauropods 34 Living Planet 72 The Theropods 35 Life in the Universe 73 Dinosaurs with Feathers 36 Wings and Teeth 37 Geologic Time Scale 74 Rivals of the Dinosaurs 38 Fur Balls 39 Glossary 76 Flowers for the Dinosaurs 40 The End of a World 4 1 Index 78 Night of the Cretaceous 42 by Jean-Baptiste de Panafieu • illustrated by Adrienne Barman NEW YORK Triassic: 252 to 201 million years ago THE FIRST DINOSAURS Marasuchus feeds on Some of the archosaurs insects and small animals. -
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. -
Early Cretaceous Amphilestid ('Triconodont') Mammals from Mongolia
Early Cretaceous amphilestid ('triconodont') mammals from Mongolia ZOFIAKIELAN-JAWOROWSKA and DEMBERLYIN DASHZEVEG Kielan-Jaworowską Z. &Daslueveg, D. 1998. Early Cretaceous amphilestid (.tricono- dont') mammals from Mongotia. - Acta Pal.aeontol.ogicaPolonica,43,3, 413438. Asmall collection of ?Aptianor ?Albian amphilestid('triconodont') mammals consisting of incomplete dentaries and maxillae with teeth, from the Khoboor localiĘ Guchin Us counĘ in Mongolia, is described. Grchinodon Troftmov' 1978 is regarded a junior subjective synonym of GobiconodonTroftmov, 1978. Heavier wear of the molariforms M3 andM4than of themore anteriorone-M2 in Gobiconodonborissiaki gives indirect evidence formolariformreplacement in this taxon. The interlocking mechanismbetween lower molariforms n Gobiconodon is of the pattern seen in Kuchneotherium and Ttnodon. The ińterlocking mechanism and the type of occlusion ally Amphilestidae with Kuehneotheriidae, from which they differ in having lower molariforms with main cusps aligned and the dentary-squamosal jaw joint (double jaw joint in Kuehneotheńdae). The main cusps in upper molariforms M3-M5 of Gobiconodon, however, show incipient tńangular arrangement. The paper gives some support to Mills' idea on the therian affinities of the Amphilestidae, although it cannot be excluded that the characters that unite the two groups developed in parallel. Because of scanty material and arnbiguĘ we assign the Amphilestidae to order incertae sedis. Key words : Mammali4 .triconodonts', Amphilestidae, Kuehneotheriidae, Early Cretaceous, Mongolia. Zofia Kiel,an-Jaworowska [zkielnn@twarda,pan.pl], InsĘtut Paleobiologii PAN, ul. Twarda 5 I /5 5, PL-00-8 I 8 Warszawa, Poland. DemberĘin Dash7eveg, Geological Institute, Mongolian Academy of Sciences, Ulan Bator, Mongolia. Introduction Beliajeva et al. (1974) reportedthe discovery of Early Cretaceous mammals at the Khoboor locality (referred to also sometimes as Khovboor), in the Guchin Us Soinon (County), Gobi Desert, Mongolia. -
A New Mammaliaform from the Early Jurassic and Evolution Of
R EPORTS tary trough with a shelflike dorsal medial ridge, and all other nonmammalian mamma- A New Mammaliaform from the liaforms have a medial concavity on the man- dibular angle (8–14, 23), as in nonmamma- Early Jurassic and Evolution of liaform cynodonts (9, 14, 24–27). The post- dentary trough and the medial concavity on Mammalian Characteristics the mandibular angle respectively accommo- dated the prearticular/surangular and the re- Zhe-Xi Luo,1* Alfred W. Crompton,2 Ai-Lin Sun3 flected lamina of the angular (9, 25–27) that are the homologs to the mammalian middle A fossil from the Early Jurassic (Sinemurian, ϳ195 million years ago) represents ear bones (9, 14, 16–21, 23, 26). The absence a new lineage of mammaliaforms, the extinct groups more closely related to of these structures indicates that the postden- the living mammals than to nonmammaliaform cynodonts. It has an enlarged tary bones (“middle ear ossicles”) must have cranial cavity, but no postdentary trough on the mandible, indicating separation been separated from the mandible (Fig. 3). of the middle ear bones from the mandible. This extends the earliest record of Hadrocodium lacks the primitive meckelian these crucial mammalian features by some 45 million years and suggests that sulcus of the mandible typical of all nonmam- separation of the middle ear bones from the mandible and the expanded brain maliaform cynodonts (24–27), stem groups vault could be correlated. It shows that several key mammalian evolutionary of mammaliaforms (8, 9, 14, 23, 26, 27), innovations in the ear region, the temporomandibular joint, and the brain vault triconodontids (28, 29), and nontribosphenic evolved incrementally through mammaliaform evolution and long before the therian mammals (30).