Bayesian Tip-Dated Phylogenetics: Topological Effects, Stratigraphic Fit
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Reptile-Like Physiology in Early Jurassic Stem-Mammals
bioRxiv preprint doi: https://doi.org/10.1101/785360; this version posted October 10, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Title: Reptile-like physiology in Early Jurassic stem-mammals Authors: Elis Newham1*, Pamela G. Gill2,3*, Philippa Brewer3, Michael J. Benton2, Vincent Fernandez4,5, Neil J. Gostling6, David Haberthür7, Jukka Jernvall8, Tuomas Kankanpää9, Aki 5 Kallonen10, Charles Navarro2, Alexandra Pacureanu5, Berit Zeller-Plumhoff11, Kelly Richards12, Kate Robson-Brown13, Philipp Schneider14, Heikki Suhonen10, Paul Tafforeau5, Katherine Williams14, & Ian J. Corfe8*. Affiliations: 10 1School of Physiology, Pharmacology & Neuroscience, University of Bristol, Bristol, UK. 2School of Earth Sciences, University of Bristol, Bristol, UK. 3Earth Science Department, The Natural History Museum, London, UK. 4Core Research Laboratories, The Natural History Museum, London, UK. 5European Synchrotron Radiation Facility, Grenoble, France. 15 6School of Biological Sciences, University of Southampton, Southampton, UK. 7Institute of Anatomy, University of Bern, Bern, Switzerland. 8Institute of Biotechnology, University of Helsinki, Helsinki, Finland. 9Department of Agricultural Sciences, University of Helsinki, Helsinki, Finland. 10Department of Physics, University of Helsinki, Helsinki, Finland. 20 11Helmholtz-Zentrum Geesthacht, Zentrum für Material-und Küstenforschung GmbH Germany. 12Oxford University Museum of Natural History, Oxford, OX1 3PW, UK. 1 bioRxiv preprint doi: https://doi.org/10.1101/785360; this version posted October 10, 2019. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. 13Department of Anthropology and Archaeology, University of Bristol, Bristol, UK. 14Faculty of Engineering and Physical Sciences, University of Southampton, Southampton, UK. -
Dome-Headed, Small-Brained Island Mammal from the Late Cretaceous of Romania
Dome-headed, small-brained island mammal from the Late Cretaceous of Romania Zoltán Csiki-Savaa,1, Mátyás Vremirb, Jin Mengc, Stephen L. Brusatted, and Mark A. Norellc aLaboratory of Paleontology, Faculty of Geology and Geophysics, University of Bucharest, 010041 Bucharest, Romania; bDepartment of Natural Sciences, Transylvanian Museum Society, 400009 Cluj-Napoca, Romania; cDivision of Paleontology, American Museum of Natural History, New York, NY 10024; and dSchool of GeoSciences, Grant Institute, University of Edinburgh, EH9 3FE Edinburgh, United Kingdom Edited by Neil H. Shubin, The University of Chicago, Chicago, IL, and approved March 26, 2018 (received for review January 20, 2018) The island effect is a well-known evolutionary phenomenon, in describe the anatomy of kogaionids in detail, include them in a which island-dwelling species isolated in a resource-limited envi- comprehensive phylogenetic analysis, estimate their body sizes, ronment often modify their size, anatomy, and behaviors compared and present a reconstruction of their brain and sense organs. with mainland relatives. This has been well documented in modern This species exhibits several features that we interpret as re- and Cenozoic mammals, but it remains unclear whether older, more lated to its insular habitat, most notably a brain that is sub- primitive Mesozoic mammals responded in similar ways to island stantially reduced in size compared with close relatives and habitats. We describe a reasonably complete and well-preserved skeleton of a kogaionid, an enigmatic radiation of Cretaceous island- mainland contemporaries, demonstrating that some Mesozoic dwelling multituberculate mammals previously represented by frag- mammals were susceptible to the island effect like in more mentary fossils. -
April Isch Neander
February 2017 Curriculum Vitae April Isch Neander Scientific Illustrator University of Chicago Department of Organismal Biology and Anatomy 1027 E 57th Street Anatomy 306 Chicago, IL 60637 [email protected] 773.702.4715 Education M.S. Biomedical Visualization, University of Illinois at Chicago, 2012 Graduate Research Project: Visualizing the Parasagittal Step Cycle of Kryptobaatar dashzevegi, a Multituberculate with Transitional Shoulder Girdle. B.A. Biology, University of Vermont, 2010 Minor in Studio Art Publications Published Art and Illustrations Luo, Z. X., Schultz, J. A., & Ekdale, E. G. (2016). Evolution of the Middle and Inner Ears of Mammaliaforms: The Approach to Mammals. In Evolution of the Vertebrate Ear (pp. 139-174). Springer International Publishing. Brusatte, S., Luo, Z. X. (2016, June). Ascent of the Mammals. Scientific American, 30-35. Luo, Z. X., Gatesy, S. M., Jenkins, F. A., Amaral, W. W., & Shubin, N. H. (2015). Mandibular and dental characteristics of Late Triassic mammaliaform Haramiyavia and their ramifications for basal mammal evolution. Proceedings of the National Academy of Sciences, 112(51), E7101-E7109. Chang, Kenneth. (2015, November 16). Jawbone in Rock May Clear Up a Mammal Family Mystery. The New York Times. Hopson, James A. (2015). Fossils, Trackways, and Transitions in Locomotion. In Dial, Kenneth P., Neil Shubin, and Elizabeth L. Brainerd, eds. Great transformations in vertebrate evolution (pp. 125-141). University of Chicago Press. Luo, Z. X., Meng, Q. J., Ji, Q., Liu, D., Zhang, Y. G., & Neander, A. I. (2015). Evolutionary development in basal mammaliaforms as revealed by a docodontan. Science, 347(6223), 760-764. Meng, Q. J., Ji, Q., Zhang, Y. -
The Ear in Mammal-Like Reptiles and Early Mammals
Acta Palaeontologica Polonica Vol. 28, No. 1-2 pp, 147-158 Warszawa, 1983 Second Symposium on Mesozoic T erre stial Ecosystems, Jadwisin 1981 KENNETH A. KERMACK and FRANCES MUSSETT THE EAR IN MAMMAL-LIKE REPTILES AND EARLY MAMMALS KERMACK, K . A. a nd MUSS ETT, F.: The ear in mammal-like r eptiles an d early mammals. Acta Palaeont. P olonica , 28, 1-2, 147-158, 1983. Th e early m embers of the Theropsida lacked a tympanic membrane. In the later theropslds, the Therapsid a, a tym p an ic membrane develop ed from thc skin on the lateral side of th e lower jaw. The tympanum is not homologous In the Therapsida and ' t he Sauropslda. The ther apsid ea r w as a poor receiver of airborne sound, both In hi gh frequency r esp onse and In the r ange of frequencies encompassed. With the radiation of the Sauropsida in the Triassic the large therapsids became extinct, the small therap si ds evolv ed In to the mammal s and became nocturnal. High frequency hearin g w as essen tial for the nocturn al mode of life; quadrate and arttcutar became diss ociated from the jaw hinge to become the m ammali an au di tory ossi cles . I n the Theria the cochlea became coil ed. The spiral cochlea could n ot have existed until there w as a middle ear w ith the n ec essary h ig h f re q uency r esp onse. This m ay n ot have been until the Cretace ous. -
A Review of Palaeozoic and Mesozoic Tetrapods from Greenland
A review of Palaeozoic and Mesozoic tetrapods from Greenland MARCO MARZOLA, OCTÁVIO MATEUS, JESPER MILÀN & LARS B. CLEMMENSEN Marzola, M., Mateus, O., Milàn, J. & Clemmensen, L.B. 2018. A review of Palaeozoic and Mesozoic tetrapods from Greenland. © 2018 by Bulletin of the Geological Society of Denmark, Vol. 66, pp. 21–46. ISSN 2245-7070. (www.2dgf.dk/publikationer/bulletin). https://doi.org/10.37570/bgsd-2018-66-02 This article presents a synthesis of Palaeozoic and Mesozoic fossil tetrapods from Greenland, includ- ing an updated review of the holotypes and a new photographic record of the main specimens. All fossil tetrapods found are from East Greenland, with at least 30 different known taxa: five stem tetra- pods (Acanthostega gunnari, Ichthyostega eigili, I. stensioi, I. watsoni, and Ymeria denticulata) from the Late Received 1 December 2016 Devonian of the Aina Dal and Britta Dal Formations; four temnospondyl amphibians (Aquiloniferus Accepted in revised form kochi, Selenocara groenlandica, Stoschiosaurus nielseni, and Tupilakosaurus heilmani) from the Early Triassic 27 October 2017 of the Wordie Creek Group; two temnospondyls (Cyclotosaurus naraserluki and Gerrothorax cf. pulcher- Published online rimus), one testudinatan (cf. Proganochelys), two stagonolepids (Aetosaurus ferratus and Paratypothorax 3 March 2018 andressorum), the eudimorphodontid Arcticodactylus, undetermined archosaurs (phytosaurs and both sauropodomorph and theropod dinosaurs), the cynodont Mitredon cromptoni, and three mammals (Ha- ramiyavia clemmenseni, Kuehneotherium, and cf. ?Brachyzostrodon), from the Late Triassic of the Fleming Fjord Formation; one plesiosaur from the Early Jurassic of the Kap Stewart Formation; one plesiosaur and one ichthyosaur from the Late Jurassic of the Kap Leslie Formation, plus a previously unreported Late Jurassic plesiosaur from Kronprins Christian Land. -
Journal of Vertebrate Paleontology Endocranial and Inner Ear
Supplementary data – Journal of Vertebrate Paleontology Endocranial and inner ear morphology of Vintana sertichi (Mammalia, Gondwanatheria) from the Late Cretaceous of Madagascar SIMONE HOFFMANN,1 PATRICK M. O’CONNOR,2, 3 E. CHRISTOPHER KIRK,4, 5 JOHN R. WIBLE,6 and DAVID W. KRAUSE1 1Department of Anatomical Sciences, Stony Brook University, Stony Brook, New York 11794-8081, U.S.A., [email protected], [email protected]; 2Department of Biomedical Sciences, 228 Irvine Hall, Ohio University, Athens, Ohio 45701, U.S.A., [email protected]; 3Ohio Center for Ecology and Evolutionary Studies, Irvine Hall, Athens, Ohio 45701, U.S.A.; 4Department of Anthropology, University of Texas at Austin, Austin, Texas 78712, U.S.A., [email protected]; 5Vertebrate Paleontology Laboratory, Jackson School of Geosciences, University of Texas at Austin, Texas 78712, U.S.A.; 6Section of Mammals, Carnegie Museum of Natural History, 5800 Baum Boulevard, Pittsburgh, Pennsylvania 15206, U.S.A., [email protected] TABLE S1. Endocranial volume and body masses in 517 extinct (†) and extant cynodonts. Encephalization quotient (EQ) calculated from endocranial volume (EV) including olfactory bulbs, and body mass (BM) using Eisenberg’s (1981) equation = EV/(0.055[BM]0.74). Endocranial volume is given in cm3 (= ml = 1000 mm3 = g). Body mass for Vintana is given as lower, mean, and upper estimates for the uncorrected and corrected endocranial volume. Wilson and Reader (2005) was used as the taxonomic authority. References: 1 = this study; 2 = Kirk et al. (this volume); 3 = Rodrigues et al. (2013); 4 = Macrini (2006); 5 = Rowe et al. (2011); 6 = Jerison (1973); 7 = Krause and Kielan-Jaworowska (1993); 8 = Haug (1987); 9 = Ashwell (2008); 10 = Eisenberg and Wilson (1981); 11 = Kielan-Jaworowska (1984); 12 = Eisenberg (1981); 13 = Stephan et al. -
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. -
A Fresh Approach to Stellar Benchmarking
NEWS & VIEWS RESEARCH a Million years ago b 250 200 150 100 50 Triassic Jurassic Cretaceous Haramiyavia European haramiyidans Haramiyidans Vintana Hahnodon Cifelliodon Cifelliodon Chinese haramiyidans Monotremes Vintana Placentals Mammals Marsupials Figure 2 | Re-evaluating the evolution and biogeography of haramiyidans. India. The authors’ analysis expands the Cretaceous range of haramiyidans to a, Huttenlocker et al.1 analysed relationships between the early branches of Madagascar (Vintana) and North America (Cifelliodon). Combined with the the family tree for mammals and their more primitive relatives. The resulting fact that other fossils of haramiyidans from the Triassic (purple) have been evolutionary tree indicates that haramiyidans are not mammals, contrary to found in Europe and Greenland, and that haramiyidans from the Jurassic (blue) some previous evidence5,6,8,9. The analysis also places the Cretaceous genus have been found in Europe, China and Tanzania, this work implies a much Vintana in Haramiyida for the first time. b, Cretaceous haramiyidans (indicated broader temporal and geographical distribution of haramiyidans than had by green circles) have previously been found in northern Africa and possibly previously been hypothesized. that, although the Chinese haramiyidans are Simone Hoffmann is in the Department of 3. Rowe, T. B., Macrini, T. E. & Luo, Z.-X. Science 332, represented by complete skeletons, the speci- Anatomy, New York Institute of Technology, 955–957 (2011). 4. Koyabu, D., Maier, W. & Sánchez-Villagra, M. R. mens are essentially 2D. Most of the skulls are College of Osteopathic Medicine, Old Proc. Natl Acad. Sci. USA 109, 14075–14080 little more than flattened outlines, which lim- Westbury, New York 11568, USA. -
213 a New Haramiyid Indicating a Complex Pattern of Evolution In
Vol.27 No.4 2013 Science Watch A New Haramiyid Indicating a Complex Pattern of Evolution in Mesozoic Mammals Earth Science major unsolved problem in mammalian evolution is University reported a new haramiyid from the Jurassic period the origin of Allotheria, including Multituberculata of China, Arboroharamiya jenkinsi, a partial skeleton with A and Haramiyida. Multituberculates are the most both mandibles associated with teeth and isolated upper teeth. diverse and best known Mesozoic era mammals and This largest known haramiyid reveals additional mammalian ecologically resemble rodents, but haramiyids are known features of this group, and helps to identify other haramiyids mainly from isolated teeth, hampering our search for their represented by isolated teeth, indicating a complex pattern phylogenetic relationships. Researchers from the Institute of evolution involving many convergences and/or reversals of Vertebrate Paleontology and Paleoanthropology (IVPP), existed in Mesozoic mammals, as reported August 8 in CAS, the Shandong Tianyu Museum of Nature and the Linyi Nature. Reconstruction of Arboroharamiya jenkinsi. (Image by BI Shundong) Bulletin of the Chinese Academy of Sciences 213 BCAS Vol.27 No.4 2013 The new specimen was unearthed from the Middle–Late Jurassic Tiaojishan Formation in the town of Mutoudeng, Qinglong County, Hebei Province, China, dated about 160 million years. Researchers said it is the largest known haramiyid with a body mass estimated at 354 grams. Arboroharamiya, as with other mammals, has body Earth Science hair (preserved as impressions), a single-boned (dentary) mandible that implies a three-boned middle ear. The dentition is differentiated into incisors and multi-rooted premolars and molars, with the canine presumably lost. -
Lower Triassic Postcanine Teeth with Allotherian-Like Crowns
Research Letters South African Journal of Science 103, May/June 2007 245 Lower Triassic postcanine teeth with allotherian-like crowns F. Abdala*‡, H. Mocke*§ and P.J. Hancox* The Allotheria are fossil mammals with upper and lower post- canines usually showing two longitudinal rows of cusps separated by a central valley. The group comprises the poorly known haramiyids, mostly represented by isolated teeth, and the notably diverse and long-lived multituberculates; its monophyly is uncer- tain. The oldest records of this particular group are the Late Triassic (Norian–Rhaetian) haramiyids. We present here postcanines with haramiyid-like crowns that were recovered from the Lower Triassic of South Africa. A distinguishing feature of the new teeth is that they are single-rooted. This is the oldest record of mammal-like teeth with crowns having parallel rows of cusps, representing a temporal extension of some 43 million years from similar crown patterns of haramiyids and tritylodontids. This finding reinforces evidence of the remarkable faunal turnover of therapsids in the Early/Middle Triassic, at which time an explosive origin followed by a rapid early diversification of herbivorous/omnivorous forms with occluding expanded postcanines took place. Introduction The Beaufort Group of the South African Karoo shows an abundance and diversity of non-mammalian synapsids, which have allowed for biostratigraphic subdivisions ranging from Middle Permian to Middle Triassic.1 The youngest of these Fig. 1.Allotherian-like teeth.A, Occlusal and lateral views of BP/1/6515 (Pattern 1); B, occlusal and lateral views of BP/1/6516 (Pattern 2). biozones, the Cynognathus Assemblage Zone (AZ), comprises the full extent of the Burgersdorp Formation of the Tarkastad Sub- found to be most parsimonious from an unconstrained search, group (J. -
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.