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Current Perspectives on the Evolution of Birds
Contributions to Zoology, 77 (2) 109-116 (2008) Current perspectives on the evolution of birds Per G.P. Ericson Department of Vertebrate Zoology, Swedish Museum of Natural History, P.O. Box 50007, SE-10405 Stockholm, Sweden, [email protected] Key words: Aves, phylogeny, systematics, fossils, DNA, genetics, biogeography Contents (cf. Göhlich and Chiappe, 2006), making feathers a plesiomorphy in birds. Indeed, only three synapo- Systematic relationships ........................................................ 109 morphies have been proposed for Aves (Chiappe, Genome characteristics ......................................................... 111 2002), although monophyly is never seriously ques- A comparison with previous classifications ...................... 112 Character evolution ............................................................... 113 tioned: 1) the caudal margin of naris nearly reaching Evolutionary trends ............................................................... 113 or overlapping the rostral border of the antorbital Biogeography and biodiversity ............................................ 113 fossa (in the primitive condition the caudal margin Differentiation and speciation ............................................. 114 of naris is farther rostral than the rostral border of Acknowledgements ................................................................ 115 the antorbital fossa), 2) scapula with a prominent References ................................................................................ 115 acromion, -
Disaggregation of Bird Families Listed on Cms Appendix Ii
Convention on the Conservation of Migratory Species of Wild Animals 2nd Meeting of the Sessional Committee of the CMS Scientific Council (ScC-SC2) Bonn, Germany, 10 – 14 July 2017 UNEP/CMS/ScC-SC2/Inf.3 DISAGGREGATION OF BIRD FAMILIES LISTED ON CMS APPENDIX II (Prepared by the Appointed Councillors for Birds) Summary: The first meeting of the Sessional Committee of the Scientific Council identified the adoption of a new standard reference for avian taxonomy as an opportunity to disaggregate the higher-level taxa listed on Appendix II and to identify those that are considered to be migratory species and that have an unfavourable conservation status. The current paper presents an initial analysis of the higher-level disaggregation using the Handbook of the Birds of the World/BirdLife International Illustrated Checklist of the Birds of the World Volumes 1 and 2 taxonomy, and identifies the challenges in completing the analysis to identify all of the migratory species and the corresponding Range States. The document has been prepared by the COP Appointed Scientific Councilors for Birds. This is a supplementary paper to COP document UNEP/CMS/COP12/Doc.25.3 on Taxonomy and Nomenclature UNEP/CMS/ScC-Sc2/Inf.3 DISAGGREGATION OF BIRD FAMILIES LISTED ON CMS APPENDIX II 1. Through Resolution 11.19, the Conference of Parties adopted as the standard reference for bird taxonomy and nomenclature for Non-Passerine species the Handbook of the Birds of the World/BirdLife International Illustrated Checklist of the Birds of the World, Volume 1: Non-Passerines, by Josep del Hoyo and Nigel J. Collar (2014); 2. -
Insular Vertebrate Evolution: the Palaeontological Approach': Monografies De La Societat D'història Natural De Les Balears, Lz: Z05-118
19 DESCRIPTION OF THE SKULL OF THE GENUS SYLVIORNIS POPLIN, 1980 (AVES, GALLIFORMES, SYLVIORNITHIDAE NEW FAMILY), A GIANT EXTINCT BIRD FROM THE HOLOCENE OF NEW CALEDONIA Cécile MOURER-CHAUVIRÉ & Jean Christophe BALOUET MOUREH-CHAUVIRÉ, C. & BALOUET, l.C, zoos. Description of the skull of the genus Syluiornis Poplin, 1980 (Aves, Galliformes, Sylviornithidae new family), a giant extinct bird from the Holocene of New Caledonia. In ALCOVER, J.A. & BaVER, P. (eds.): Proceedings of the International Symposium "Insular Vertebrate Evolution: the Palaeontological Approach': Monografies de la Societat d'Història Natural de les Balears, lZ: Z05-118. Resum El crani de Sylviornismostra una articulació craniarostral completament mòbil, amb dos còndils articulars situats sobre el rostrum, el qual s'insereix al crani en dues superfícies articulars allargades. La presència de dos procesos rostropterigoideus sobre el basisfenoide del rostrum i la forma dels palatins permet confirmar que aquest gènere pertany als Galliformes, però les característiques altament derivades del crani justifiquen el seu emplaçament a una nova família, extingida, Sylviornithidae. El crani de Syluiornis està extremadament eixamplat i dorsoventralment aplanat, mentre que el rostrum és massís, lateralment comprimit, dorsoventralment aixecat i mostra unes cristae tomiales molt fondes. El rostrum exhibeix un ornament ossi gran. La mandíbula mostra una símfisi molt allargada, les branques laterals també presenten unes cristae tomiales fondes, i la part posterior de la mandíbula és molt gruixada. Es discuteix el possible origen i l'alimentació de Syluiornis. Paraules clau: Aves, Galliformes, Extinció, Holocè, Nova Caledònia. Abstract The skull of Syluiornis shows a completely mobile craniorostral articulation, with two articular condyles situated on the rostrum, which insert into two elongated articular surfaces on the cranium. -
Lowest Paleogene Strata on Vega Island, Antarctica
Palaeogeography, Palaeoclimatology, Palaeoecology 402 (2014) 55–72 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Stratigraphy and vertebrate paleoecology of Upper Cretaceous–?lowest Paleogene strata on Vega Island, Antarctica Eric M. Roberts a,⁎, Matthew C. Lamanna b, Julia A. Clarke c, Jin Meng d, Eric Gorscak e, Joseph J.W. Sertich f, Patrick M. O'Connor e, Kerin M. Claeson g,RossD.E.MacPheeh a School of Earth and Environmental Sciences, James Cook University, Townsville, QLD 4811, Australia b Section of Vertebrate Paleontology, Carnegie Museum of Natural History, 4400 Forbes Ave., Pittsburgh, PA 15213, USA c Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, 1 University Station C1100, Austin, TX 78712, USA d Department of Paleontology, American Museum of Natural History, Central Park West at 79th St., New York, NY 10024, USA e Department of Biomedical Sciences, Heritage College of Osteopathic Medicine, Ohio University, Athens, OH 45701, USA f Department of Earth Sciences, Denver Museum of Nature and Science, 2001 Colorado Blvd., Denver, CO 80205, USA g Department of Biomedical Sciences, Philadelphia College of Osteopathic Medicine, Philadelphia, PA 19131, USA h Department of Mammalogy, American Museum of Natural History, Central Park West at 79th St., New York, NY 10024, USA article info abstract Article history: The Upper Cretaceous (Maastrichtian) Sandwich Bluff Member of the López de Bertodano Formation is well Received 24 October 2013 exposed on Vega Island in the James Ross Basin off the northeastern coast of the Antarctic Peninsula. Although Received in revised form 18 February 2014 this unit is one of the richest sources of end-Cretaceous vertebrate fossils in Antarctica, it is also one of the Accepted 3 March 2014 least sedimentologically and stratigraphically characterized units in the basin. -
A Baraminological Analysis of the Land Fowl (Class Aves, Order Galliformes)
Galliform Baraminology 1 Running Head: GALLIFORM BARAMINOLOGY A Baraminological Analysis of the Land Fowl (Class Aves, Order Galliformes) Michelle McConnachie A Senior Thesis submitted in partial fulfillment of the requirements for graduation in the Honors Program Liberty University Spring 2007 Galliform Baraminology 2 Acceptance of Senior Honors Thesis This Senior Honors Thesis is accepted in partial fulfillment of the requirements for graduation from the Honors Program of Liberty University. ______________________________ Timothy R. Brophy, Ph.D. Chairman of Thesis ______________________________ Marcus R. Ross, Ph.D. Committee Member ______________________________ Harvey D. Hartman, Th.D. Committee Member ______________________________ Judy R. Sandlin, Ph.D. Assistant Honors Program Director ______________________________ Date Galliform Baraminology 3 Acknowledgements I would like to thank my Lord and Savior, Jesus Christ, without Whom I would not have had the opportunity of being at this institution or producing this thesis. I would also like to thank my entire committee including Dr. Timothy Brophy, Dr. Marcus Ross, Dr. Harvey Hartman, and Dr. Judy Sandlin. I would especially like to thank Dr. Brophy who patiently guided me through the entire research and writing process and put in many hours working with me on this thesis. Finally, I would like to thank my family for their interest in this project and Robby Mullis for his constant encouragement. Galliform Baraminology 4 Abstract This study investigates the number of galliform bird holobaramins. Criteria used to determine the members of any given holobaramin included a biblical word analysis, statistical baraminology, and hybridization. The biblical search yielded limited biosystematic information; however, since it is a necessary and useful part of baraminology research it is both included and discussed. -
An Avian Femur from the Late Cretaceous of Vega Island, Antarctic Peninsula: Removing the Record of Cursorial Landbirds from the Mesozoic of Antarctica
An avian femur from the Late Cretaceous of Vega Island, Antarctic Peninsula: removing the record of cursorial landbirds from the Mesozoic of Antarctica Abagael R. West1,2,3, Christopher R. Torres4, Judd A. Case5, Julia A. Clarke4,6, Patrick M. O’Connor7,8 and Matthew C. Lamanna1 1 Section of Vertebrate Paleontology, Carnegie Museum of Natural History, Pittsburgh, PA, USA 2 Section of Mammals, Carnegie Museum of Natural History, Pittsburgh, PA, USA 3 Department of Biological Sciences, University of Pittsburgh, Pittsburgh, PA, USA 4 Department of Integrative Biology, University of Texas at Austin, Austin, TX, USA 5 Department of Biology, Eastern Washington University, Cheney, WA, USA 6 Jackson School of Geosciences, University of Texas at Austin, Austin, TX, USA 7 Department of Biomedical Sciences, Ohio University Heritage College of Osteopathic Medicine, Athens, OH, USA 8 Ohio Center for Ecology and Evolutionary Studies, Ohio University, Athens, OH, USA ABSTRACT In 2006, a partial avian femur (South Dakota School of Mines and Technology (SDSM) 78247) from the Upper Cretaceous (Maastrichtian) Sandwich Bluff Member of the López de Bertodano Formation of Sandwich Bluff on Vega Island of the northern Antarctic Peninsula was briefly reported as that of a cariamiform—a clade that includes extant and volant South American species and many extinct flightless and cursorial species. Although other authors have since rejected this taxonomic assignment, SDSM 78247 had never been the subject of a detailed description, hindering a definitive assessment -
Appendix A. Supplementary Material
Appendix A. Supplementary material Comprehensive taxon sampling and vetted fossils help clarify the time tree of shorebirds (Aves, Charadriiformes) David Cernˇ y´ 1,* & Rossy Natale2 1Department of the Geophysical Sciences, University of Chicago, Chicago 60637, USA 2Department of Organismal Biology & Anatomy, University of Chicago, Chicago 60637, USA *Corresponding Author. Email: [email protected] Contents 1 Fossil Calibrations 2 1.1 Calibrations used . .2 1.2 Rejected calibrations . 22 2 Outgroup sequences 30 2.1 Neornithine outgroups . 33 2.2 Non-neornithine outgroups . 39 3 Supplementary Methods 72 4 Supplementary Figures and Tables 74 5 Image Credits 91 References 99 1 1 Fossil Calibrations 1.1 Calibrations used Calibration 1 Node calibrated. MRCA of Uria aalge and Uria lomvia. Fossil taxon. Uria lomvia (Linnaeus, 1758). Specimen. CASG 71892 (referred specimen; Olson, 2013), California Academy of Sciences, San Francisco, CA, USA. Lower bound. 2.58 Ma. Phylogenetic justification. As in Smith (2015). Age justification. The status of CASG 71892 as the oldest known record of either of the two spp. of Uria was recently confirmed by the review of Watanabe et al. (2016). The younger of the two marine transgressions at the Tolstoi Point corresponds to the Bigbendian transgression (Olson, 2013), which contains the Gauss-Matuyama magnetostratigraphic boundary (Kaufman and Brigham-Grette, 1993). Attempts to date this reversal have been recently reviewed by Ohno et al. (2012); Singer (2014), and Head (2019). In particular, Deino et al. (2006) were able to tightly bracket the age of the reversal using high-precision 40Ar/39Ar dating of two tuffs in normally and reversely magnetized lacustrine sediments from Kenya, obtaining a value of 2.589 ± 0.003 Ma. -
2.9 Waterbirds: Identification, Rehabilitation and Management
Chapter 2.9 — Freshwater birds: identification, rehabilitation and management• 193 2.9 Waterbirds: identification, rehabilitation and management Phil Straw Avifauna Research & Services Australia Abstract All waterbirds and other bird species associated with wetlands, are described including how habitats are used at ephemeral and permanent wetlands in the south east of Australia. Wetland habitat has declined substantially since European settlement. Although no waterbird species have gone extinct as a result some are now listed as endangered. Reedbeds are taken as an example of how wetlands can be managed. Chapter 2.9 — Freshwater birds: identification, rehabilitation and management• 194 Introduction such as farm dams and ponds. In contrast, the Great-crested Grebe is usually associated with large Australia has a unique suite of waterbirds, lakes and deep reservoirs. many of which are endemic to this, the driest inhabited continent on earth, or to the Australasian The legs of grebes are set far back on the body region with Australia being the main stronghold making them very efficient swimmers. They forage for the species. Despite extensive losses of almost completely underwater pursuing fish and wetlands across the continent since European aquatic arthropods such as insects and crustaceans. settlement no extinctions of waterbirds have They are strong fliers but are poor at manoeuvering been recorded from the Australian mainland as in flight and generally prefer to dive underwater a consequence. However, there have been some to escape avian predators or when disturbed by dramatic declines in many populations and several humans. Flights between wetlands, some times species are now listed as threatened including over great distances, are carried out under the cover the Australasian Bittern, Botaurus poiciloptilus of darkness when it is safe from attack by most (nationally endangered). -
The Function and Evolution of the Supraorbital Process in Ducks
THE FUNCTION AND EVOLUTION OF THE SUPRAORBITAL PROCESS IN DUCKS ROBERTJ. RAIKOW THE anteriormargin of the orbit in ducksis formedby the lacrimalbone, which articulateswith the anterolateralmargin of the frontal boneand the posterodorsalcorner of the maxillary processof the nasal bone. The evolu- tion of this bone in birds generally has been dealt with recently by Cracraft (Amer. Midl. Naturalist, 80: 316, 1968), whoseterminology for the parts of the lacrimal bone is followedhere. In many ducksthe postero- dorsalcorner of the lacrimal is marked by a small tubercle,which serves as the site of attachment of the anterior end of the orbital membrane,a sheetof connectivetissue that coversand protectsthe dorsalaspect of the eyeball. In some forms this tubercle has become elongated to form a stout, finger-like projection, the supraorbitalprocess. This appears to provide mechanicalprotection to the eyeball and salt gland (Figure 1). Table 1 lists the occurrenceand degree of developmentof this process in the skulls of all living generaof ducks. CORRELATION WITH FEEDING AND LOCOMOTOR HABITS In the following discussion,data on feeding habits are from Delacour (The waterfowlof the world,vols. 1-3, London,Country Life Ltd., 1954, 1956, 1959). Table 1 showsthat the supraorbital processis developed significantlyonly in certain groupsof ducks that feed underwater. It is absentor rudimentaryin the Tadornini, Cairinini, and Anatini, which are primarily surfacefeeders, but also in Merganetta arma.ta,the Torrent Duck, which feedsunderwater. In the Aythyini it is fairly well-developed in severalspecies of Aythya, which are excellentdivers, but is rudimentary in Netta peposaca,which is moreof a surfacefeeder. It is alsorudimentary in the Canvasback,Aythya valisineria,which dives for vegetation.Among the Mergini the supraorbitalprocess is highly developedin eiders (Poly- sticta, Somateria) , scoters( M elanitta) , and Long-tailed Duck ( Clangula byemalls), all of which feed mainly on invertebratestaken from the bottom. -
The Oldest Record of Ornithuromorpha from the Early Cretaceous of China
ARTICLE Received 6 Jan 2015 | Accepted 20 Mar 2015 | Published 5 May 2015 DOI: 10.1038/ncomms7987 OPEN The oldest record of ornithuromorpha from the early cretaceous of China Min Wang1, Xiaoting Zheng2,3, Jingmai K. O’Connor1, Graeme T. Lloyd4, Xiaoli Wang2,3, Yan Wang2,3, Xiaomei Zhang2,3 & Zhonghe Zhou1 Ornithuromorpha is the most inclusive clade containing extant birds but not the Mesozoic Enantiornithes. The early evolutionary history of this avian clade has been advanced with recent discoveries from Cretaceous deposits, indicating that Ornithuromorpha and Enantiornithes are the two major avian groups in Mesozoic. Here we report on a new ornithuromorph bird, Archaeornithura meemannae gen. et sp. nov., from the second oldest avian-bearing deposits (130.7 Ma) in the world. The new taxon is referable to the Hongshanornithidae and constitutes the oldest record of the Ornithuromorpha. However, A. meemannae shows few primitive features relative to younger hongshanornithids and is deeply nested within the Hongshanornithidae, suggesting that this clade is already well established. The new discovery extends the record of Ornithuromorpha by five to six million years, which in turn pushes back the divergence times of early avian lingeages into the Early Cretaceous. 1 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China. 2 Institue of Geology and Paleontology, Linyi University, Linyi, Shandong 276000, China. 3 Tianyu Natural History Museum of Shandong, Pingyi, Shandong 273300, China. 4 Department of Biological Sciences, Faculty of Science, Macquarie University, Sydney, New South Wales 2019, Australia. -
Fossil Evidence of the Avian Vocal Organ from the Mesozoic (PDF)
LETTER doi:10.1038/nature19852 Fossil evidence of the avian vocal organ from the Mesozoic Julia A. Clarke1, Sankar Chatterjee2, Zhiheng Li1,3, Tobias Riede4, Federico Agnolin5,6, Franz Goller7, Marcelo P. Isasi5, Daniel R. Martinioni8, Francisco J. Mussel9 & Fernando E. Novas5 From complex songs to simple honks, birds produce sounds using a laryngeal sound source in frogs, reptiles or mammals, data from the unique vocal organ called the syrinx1,2. Located close to the heart at hyoid skeleton, skull and vertebral column have been proposed to the tracheobronchial junction, vocal folds or membranes attached to inform evolutionary changes in its position in hominoids16 and in modified mineralized rings vibrate to produce sound1–7. Syringeal bats17. However, neither direct fossil evidence nor indirect inferential components were not thought to commonly enter the fossil record6, approaches have so far been used to inform our understanding of the and the few reported fossilized parts of the syrinx are geologically origin of the syrinx. young8–11 (from the Pleistocene and Holocene (approximately 2.5 A three-dimensionally preserved syrinx in a partial skeleton of a million years ago to the present)). The only known older syrinx is Late Cretaceous fossil bird from Vega Island, Antarctic Peninsula an Eocene specimen that was not described or illustrated12. Data (MACN-PV 19.748 (MACN-Museo Argentino de Ciencias Naturales), on the relationship between soft tissue structures and syringeal Figs 1 and 2, Extended Data Figs 1, 2, 4–8, Supplementary Information, three-dimensional geometry are also exceptionally limited5. Here Supplementary Table 1 and Supplementary Fig. 1), is here referred to we describe the first remains, to our knowledge, of a fossil syrinx the species Vegavis iaai18 (Supplementary Information, Extended Data from the Mesozoic Era, which are preserved in three dimensions Figs 4 and 6). -
A North American Stem Turaco, and the Complex Biogeographic History of Modern Birds Daniel J
Field and Hsiang BMC Evolutionary Biology (2018) 18:102 https://doi.org/10.1186/s12862-018-1212-3 RESEARCHARTICLE Open Access A North American stem turaco, and the complex biogeographic history of modern birds Daniel J. Field1,2* and Allison Y. Hsiang2,3 Abstract Background: Earth’s lower latitudes boast the majority of extant avian species-level and higher-order diversity, with many deeply diverging clades restricted to vestiges of Gondwana. However, palaeontological analyses reveal that many avian crown clades with restricted extant distributions had stem group relatives in very different parts of the world. Results: Our phylogenetic analyses support the enigmatic fossil bird Foro panarium Olson 1992 from the early Eocene (Wasatchian) of Wyoming as a stem turaco (Neornithes: Pan-Musophagidae), a clade that is presently endemic to sub-Saharan Africa. Our analyses offer the first well-supported evidence for a stem musophagid (and therefore a useful fossil calibration for avian molecular divergence analyses), and reveal surprising new information on the early morphology and biogeography of this clade. Total-clade Musophagidae is identified as a potential participant in dispersal via the recently proposed ‘North American Gateway’ during the Palaeogene, and new biogeographic analyses illustrate the importance of the fossil record in revealing the complex historical biogeography of crown birds across geological timescales. Conclusions: In the Palaeogene, total-clade Musophagidae was distributed well outside the range of crown Musophagidae in the present day. This observation is consistent with similar biogeographic observations for numerous other modern bird clades, illustrating shortcomings of historical biogeographic analyses that do not incorporate information from the avian fossil record.