A Phylogenomic Supertree of Birds
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Ecological Correlates of Ghost Lineages in Ruminants
Paleobiology, 38(1), 2012, pp. 101–111 Ecological correlates of ghost lineages in ruminants Juan L. Cantalapiedra, Manuel Herna´ndez Ferna´ndez, Gema M. Alcalde, Beatriz Azanza, Daniel DeMiguel, and Jorge Morales Abstract.—Integration between phylogenetic systematics and paleontological data has proved to be an effective method for identifying periods that lack fossil evidence in the evolutionary history of clades. In this study we aim to analyze whether there is any correlation between various ecomorphological variables and the duration of these underrepresented portions of lineages, which we call ghost lineages for simplicity, in ruminants. Analyses within phylogenetic (Generalized Estimating Equations) and non-phylogenetic (ANOVAs and Pearson correlations) frameworks were performed on the whole phylogeny of this suborder of Cetartiodactyla (Mammalia). This is the first time ghost lineages are focused in this way. To test the robustness of our data, we compared the magnitude of ghost lineages among different continents and among phylogenies pruned at different ages (4, 8, 12, 16, and 20 Ma). Differences in mean ghost lineage were not significantly related to either geographic or temporal factors. Our results indicate that the proportion of the known fossil record in ruminants appears to be influenced by the preservation potential of the bone remains in different environments. Furthermore, large geographical ranges of species increase the likelihood of preservation. Juan L. Cantalapiedra, Gema Alcalde, and Jorge Morales. Departamento de Paleobiologı´a, Museo Nacional de Ciencias Naturales, UCM-CSIC, Pinar 25, 28006 Madrid, Spain. E-mail: [email protected] Manuel Herna´ndez Ferna´ndez. Departamento de Paleontologı´a, Facultad de Ciencias Geolo´gicas, Universidad Complutense de Madrid y Departamento de Cambio Medioambiental, Instituto de Geociencias, Consejo Superior de Investigaciones Cientı´ficas, Jose´ Antonio Novais 2, 28040 Madrid, Spain Daniel DeMiguel. -
PTAČÍ FYLOGENEZE Dovnitř Patří Šplhavci
E Afroaves – řada linií této skupiny je velmi rozrůzněna v Africe a pro Afriku stepokur kropenatý typická (vlhy, zoborožci, mandelíci), ale fosilie africký původ nepodporují. Mnoho (Pterocles burchelli) linií bylo řazeno do řádu srostloprstých, ale ten není monofyletický, poněvadž PTAČÍ FYLOGENEZE dovnitř patří šplhavci. Patří sem i myšáci (Coliiformes) a trogoni. F Australaves – obdobně jako u Afroaves dnes sice řada linií žije jen FYLOGENEZE NA HRUBÉ ÚROVNI A PTAČÍ ŘÁDY v australasijské oblasti, ale fosilní zástupci byli nalezeni všude možně, takže o původu skupiny těžko něco soudit. Zobrazený fylogenetický stromeček zahrnuje jen velké skupiny, přičemž co je „velká“ skupina, je docela arbitrární. Aby vůbec bylo možné dělat O Passerimorphae (nebo Psittacopasserae) – papoušci korektní fylogenetické analýzy, nesmí být těch skupin moc a zároveň je potřeba, aby to byly skupiny, o nichž se předpokládá, že jsou a pěvci sdílejí řadu znaků, například schopnost učit se zpěvu, která byla monofyletické. Reálně se totiž sekvenují samozřejmě jednotliví zástupci (tedy jeden druh, respektive přímo jeden jedinec z dané skupiny), považovaná za klíčovou pro jejich sloučení (pokládala se za znak vzniklý jen a potřebujeme tedy, aby skutečně skupinu reprezentovali. Proto by nestačilo brát zástupce tradičních ptačích řádů, které známe z učebnic, jednou u jejich společného předka, tedy synapomorfii). Ovšem vzhledem k tomu, jelikož se ukázalo, že řada z nich monofyletických není. Tradiční „dravci“ byli například polyfyletičtí, poněvadž zahrnovali monofyletickou že u pěvců je s jistotou známa jen ve skupině Oscines (zpěvní) a navíc se vyskytuje skupinu složenou z orlů, jestřábů, káňat apod. (včetně kondorů), ale taky sokolovité (poštolky, sokoly apod.), kteří jsou ve skutečnosti blízce také u zcela nezávislých kolibříků, musela vzniknout víckrát konvergentně, a to příbuzní pěvcům a papouškům. -
Population Genomic Analysis Reveals That Homoploid Hybrid Speciation Can Speciation Hybrid Homoploid Reveals That Analysis Genomic Population E Origin
PROF. YONGSHUAI SUN (Orcid ID : 0000-0002-6926-8406) PROF. JIANQUAN LIU (Orcid ID : 0000-0002-4237-7418) Population genomic analysis reveals that homoploid hybrid speciation can be a lengthy process Dafu Ru1 *, Yongshuai Sun1,2*, Donglei Wang1*, Yang Chen1, Tianjing Wang1, Quanjun Hu1, Richard J. Abbott3, Jianquan Liu1# 1Key Laboratory for Bio-resource and Eco-environment of Ministry of Education, College of Life Sciences, Sichuan University, Chengdu 610065, P. R. China 2CAS Key Laboratory of Tropical Forest Ecology, Xishuangbanna Tropical Botanical Garden, Chinese Academy of Sciences, Mengla 666303, P. R. China 3School of Biology, Mitchell Building, University of St Andrews, St Andrews, Fife KY16 9TH, UK Article *equal contributions to this work; #corresponding author ([email protected]) Abstract An increasing number of species are thought to have originated by homoploid hybrid speciation (HHS), but in only a handful of cases are details of the process known. A previous study indicated that Picea purpurea, a conifer in the Qinghai-Tibet Plateau (QTP), originated through HHS from P. likiangensis and P. wilsonii. To investigate this origin in more detail we analyzed transcriptome data for 114 individuals collected from 34 populations of the three Picea species from their core distributions in the QTP. Phylogenetic, principal component and admixture analyses of nuclear SNPs showed the species to be delimited genetically and that P. purpurea was admixed with approximately 60% of its ancestry derived from P. wilsonii and 40% from P. likiangensis. Coalescent simulations revealed the best-fitting model of origin involved formation of an intermediate hybrid lineage between P. likiangensis and P. -
The Tarsometatarsus of the Middle Eocene Loon Colymbiculus Udovichenkoi
– 17 – Paleornithological Research 2013 Proceed. 8th Inter nat. Meeting Society of Avian Paleontology and Evolution Ursula B. Göhlich & Andreas Kroh (Eds) The tarsometatarsus of the Middle Eocene loon Colymbiculus udovichenkoi GERALD MAYR1, LEONID GOROBETS2 & EVGENIJ ZVONOK3 1 Senckenberg Research Institute and Natural History Museum Frankfurt, Frankfurt am Main, Germany; E-mail: [email protected] 2 Taras Shevchenko National University of Kiev, Dept. of Ecology and Environmental Protection, Kiev, Ukraine 3 Institute of Geological Sciences of NAS of Ukraine, Branch of Paleontology and Stratigraphy, Kiev, Ukraine Abstract — We describe the previously unknown tarsometatarsus of the earliest unambiguously identified loon, Colymbiculus udovichenkoi, from the Middle Eocene of the Ukraine. Except for being more elongate and apart from details of the hypotarsus morphology, the bone resembles the tarsometatarsus of the Early Miocene Colym- boides minutus. We consider the hypotarsus morphology of Colymbiculus to be plesiomorphic for Gaviiformes. Colymboides and crown group Gaviiformes are each characterized by an autapomorphic hypotarsus morphology, which precludes the former from being directly ancestral to the latter. The similarities shared by C. udovichenkoi and C. minutus, including their small size, are likely to be plesiomorphic for Gaviiformes. Although the disap- pearance of small stem group Gaviiformes may be related to the retreat of loons to cold Northern latitudes, more data are needed to firmly establish this hypothesis. We finally note that early Paleogene stem group Gaviiformes markedly differ from putative Late Cretaceous loons, whose identification needs to be verified by further fossil specimens. Key words: Colymbiculus, Colymboides, fossil birds, Gaviiformes, Eocene, Lutetian, Ukraine Introduction 1982 from the Early Miocene of the Czech Republic (ŠVEC 1982), the earliest stem line- Loons (Gaviiformes) have a fairly comprehen- age representative, being distinctly smaller than sive Neogene fossil record (OLSON 1985; MAYR its modern congeners. -
Flamingo ABOUT the GROUP
Flamingo ABOUT THE GROUP Bulletin of the IUCN-SSC/Wetlands International The Flamingo Specialist Group (FSG) was established in 1978 at Tour du Valat in France, under the leadership of Dr. Alan Johnson, who coordinated the group until 2004 (see profile at www.wetlands.org/networks/Profiles/January.htm). Currently, the group is FLAMINGO SPECIALIST GROUP coordinated from the Wildfowl & Wetlands Trust at Slimbridge, UK, as part of the IUCN- SSC/Wetlands International Waterbird Network. The FSG is a global network of flamingo specialists (both scientists and non- scientists) concerned with the study, monitoring, management and conservation of the world’s six flamingo species populations. Its role is to actively promote flamingo research and conservation worldwide by encouraging information exchange and cooperation amongst these specialists, and with other relevant organisations, particularly IUCN - SSC, Ramsar, WWF International and BirdLife International. FSG members include experts in both in-situ (wild) and ex-situ (captive) flamingo conservation, as well as in fields ranging from field surveys to breeding biology, diseases, tracking movements and data management. There are currently 165 members around the world, from India to Chile, and from France to South Africa. Further information about the FSG, its membership, the membership list serve, or this bulletin can be obtained from Brooks Childress at the address below. Chair Assistant Chair Dr. Brooks Childress Mr. Nigel Jarrett Wildfowl & Wetlands Trust Wildfowl & Wetlands Trust Slimbridge Slimbridge Glos. GL2 7BT, UK Glos. GL2 7BT, UK Tel: +44 (0)1453 860437 Tel: +44 (0)1453 891177 Fax: +44 (0)1453 860437 Fax: +44 (0)1453 890827 [email protected] [email protected] Eastern Hemisphere Chair Western Hemisphere Chair Dr. -
Recommended Band Size List Page 1
Jun 00 Australian Bird and Bat Banding Scheme - Recommended Band Size List Page 1 Australian Bird and Bat Banding Scheme Recommended Band Size List - Birds of Australia and its Territories Number 24 - May 2000 This list contains all extant bird species which have been recorded for Australia and its Territories, including Antarctica, Norfolk Island, Christmas Island and Cocos and Keeling Islands, with their respective RAOU numbers and band sizes as recommended by the Australian Bird and Bat Banding Scheme. The list is in two parts: Part 1 is in taxonomic order, based on information in "The Taxonomy and Species of Birds of Australia and its Territories" (1994) by Leslie Christidis and Walter E. Boles, RAOU Monograph 2, RAOU, Melbourne, for non-passerines; and “The Directory of Australian Birds: Passerines” (1999) by R. Schodde and I.J. Mason, CSIRO Publishing, Collingwood, for passerines. Part 2 is in alphabetic order of common names. The lists include sub-species where these are listed on the Census of Australian Vertebrate Species (CAVS version 8.1, 1994). CHOOSING THE CORRECT BAND Selecting the appropriate band to use combines several factors, including the species to be banded, variability within the species, growth characteristics of the species, and band design. The following list recommends band sizes and metals based on reports from banders, compiled over the life of the ABBBS. For most species, the recommended sizes have been used on substantial numbers of birds. For some species, relatively few individuals have been banded and the size is listed with a question mark. In still other species, too few birds have been banded to justify a size recommendation and none is made. -
Miocene Mammal Reveals a Mesozoic Ghost Lineage on Insular New Zealand, Southwest Pacific
Miocene mammal reveals a Mesozoic ghost lineage on insular New Zealand, southwest Pacific Trevor H. Worthy*†, Alan J. D. Tennyson‡, Michael Archer§, Anne M. Musser¶, Suzanne J. Hand§, Craig Jonesʈ, Barry J. Douglas**, James A. McNamara††, and Robin M. D. Beck§ *School of Earth and Environmental Sciences, Darling Building DP 418, Adelaide University, North Terrace, Adelaide 5005, South Australia, Australia; ‡Museum of New Zealand Te Papa Tongarewa, P.O. Box 467, Wellington 6015, New Zealand; §School of Biological, Earth and Environmental Sciences, University of New South Wales, New South Wales 2052, Australia; ¶Australian Museum, 6-8 College Street, Sydney, New South Wales 2010, Australia; ʈInstitute of Geological and Nuclear Sciences, P.O. Box 30368, Lower Hutt 5040, New Zealand; **Douglas Geological Consultants, 14 Jubilee Street, Dunedin 9011, New Zealand; and ††South Australian Museum, Adelaide, South Australia 5000, Australia Edited by James P. Kennett, University of California, Santa Barbara, CA, and approved October 11, 2006 (sent for review July 8, 2006) New Zealand (NZ) has long been upheld as the archetypical Ma) dinosaur material (13) and isolated moa bones from marine example of a land where the biota evolved without nonvolant sediments up to 2.5 Ma (1, 14), the terrestrial record older than terrestrial mammals. Their absence before human arrival is mys- 1 Ma is extremely limited. Until now, there has been no direct terious, because NZ was still attached to East Antarctica in the Early evidence for the pre-Pleistocene presence in NZ of any of its Cretaceous when a variety of terrestrial mammals occupied the endemic vertebrate lineages, particularly any group of terrestrial adjacent Australian portion of Gondwana. -
Download Vol. 11, No. 3
BULLETIN OF THE FLORIDA STATE MUSEUM BIOLOGICAL SCIENCES Volume 11 Number 3 CATALOGUE OF FOSSIL BIRDS: Part 3 (Ralliformes, Ichthyornithiformes, Charadriiformes) Pierce Brodkorb M,4 * . /853 0 UNIVERSITY OF FLORIDA Gainesville 1967 Numbers of the BULLETIN OF THE FLORIDA STATE MUSEUM are pub- lished at irregular intervals. Volumes contain about 800 pages and are not nec- essarily completed in any one calendar year. WALTER AuFFENBERC, Managing Editor OLIVER L. AUSTIN, JA, Editor Consultants for this issue. ~ HILDEGARDE HOWARD ALExANDER WErMORE Communications concerning purchase or exchange of the publication and all manuscripts should be addressed to the Managing Editor of the Bulletin, Florida State Museum, Seagle Building, Gainesville, Florida. 82601 Published June 12, 1967 Price for this issue $2.20 CATALOGUE OF FOSSIL BIRDS: Part 3 ( Ralliformes, Ichthyornithiformes, Charadriiformes) PIERCE BRODKORBl SYNOPSIS: The third installment of the Catalogue of Fossil Birds treats 84 families comprising the orders Ralliformes, Ichthyornithiformes, and Charadriiformes. The species included in this section number 866, of which 215 are paleospecies and 151 are neospecies. With the addenda of 14 paleospecies, the three parts now published treat 1,236 spDcies, of which 771 are paleospecies and 465 are living or recently extinct. The nominal order- Diatrymiformes is reduced in rank to a suborder of the Ralliformes, and several generally recognized families are reduced to subfamily status. These include Geranoididae and Eogruidae (to Gruidae); Bfontornithidae -
Dieter Thomas Tietze Editor How They Arise, Modify and Vanish
Fascinating Life Sciences Dieter Thomas Tietze Editor Bird Species How They Arise, Modify and Vanish Fascinating Life Sciences This interdisciplinary series brings together the most essential and captivating topics in the life sciences. They range from the plant sciences to zoology, from the microbiome to macrobiome, and from basic biology to biotechnology. The series not only highlights fascinating research; it also discusses major challenges associated with the life sciences and related disciplines and outlines future research directions. Individual volumes provide in-depth information, are richly illustrated with photographs, illustrations, and maps, and feature suggestions for further reading or glossaries where appropriate. Interested researchers in all areas of the life sciences, as well as biology enthusiasts, will find the series’ interdisciplinary focus and highly readable volumes especially appealing. More information about this series at http://www.springer.com/series/15408 Dieter Thomas Tietze Editor Bird Species How They Arise, Modify and Vanish Editor Dieter Thomas Tietze Natural History Museum Basel Basel, Switzerland ISSN 2509-6745 ISSN 2509-6753 (electronic) Fascinating Life Sciences ISBN 978-3-319-91688-0 ISBN 978-3-319-91689-7 (eBook) https://doi.org/10.1007/978-3-319-91689-7 Library of Congress Control Number: 2018948152 © The Editor(s) (if applicable) and The Author(s) 2018. This book is an open access publication. Open Access This book is licensed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license and indicate if changes were made. -
Baker2009chap58.Pdf
Ratites and tinamous (Paleognathae) Allan J. Baker a,b,* and Sérgio L. Pereiraa the ratites (5). Here, we review the phylogenetic relation- aDepartment of Natural Histor y, Royal Ontario Museum, 100 Queen’s ships and divergence times of the extant clades of ratites, Park Crescent, Toronto, ON, Canada; bDepartment of Ecology and the extinct moas and the tinamous. Evolutionary Biology, University of Toronto, Toronto, ON, Canada Longstanding debates about whether the paleognaths *To whom correspondence should be addressed (allanb@rom. are monophyletic or polyphyletic were not settled until on.ca) phylogenetic analyses were conducted on morphological characters (6–9), transferrins (10), chromosomes (11, 12), Abstract α-crystallin A sequences (13, 14), DNA–DNA hybrid- ization data (15, 16), and DNA sequences (e.g., 17–21). The Paleognathae is a monophyletic clade containing ~32 However, relationships among paleognaths are still not species and 12 genera of ratites and 46 species and nine resolved, with a recent morphological tree based on 2954 genera of tinamous. With the exception of nuclear genes, characters placing kiwis (Apterygidae) as the closest rela- there is strong molecular and morphological support for tives of the rest of the ratites (9), in agreement with other the close relationship of ratites and tinamous. Molecular morphological studies using smaller data sets ( 6–8, 22). time estimates with multiple fossil calibrations indicate that DNA sequence trees place kiwis in a derived clade with all six families originated in the Cretaceous (146–66 million the Emus and Cassowaries (Casuariiformes) (19–21, 23, years ago, Ma). The radiation of modern genera and species 24). -
Onetouch 4.0 Scanned Documents
/ Chapter 2 THE FOSSIL RECORD OF BIRDS Storrs L. Olson Department of Vertebrate Zoology National Museum of Natural History Smithsonian Institution Washington, DC. I. Introduction 80 II. Archaeopteryx 85 III. Early Cretaceous Birds 87 IV. Hesperornithiformes 89 V. Ichthyornithiformes 91 VI. Other Mesozojc Birds 92 VII. Paleognathous Birds 96 A. The Problem of the Origins of Paleognathous Birds 96 B. The Fossil Record of Paleognathous Birds 104 VIII. The "Basal" Land Bird Assemblage 107 A. Opisthocomidae 109 B. Musophagidae 109 C. Cuculidae HO D. Falconidae HI E. Sagittariidae 112 F. Accipitridae 112 G. Pandionidae 114 H. Galliformes 114 1. Family Incertae Sedis Turnicidae 119 J. Columbiformes 119 K. Psittaciforines 120 L. Family Incertae Sedis Zygodactylidae 121 IX. The "Higher" Land Bird Assemblage 122 A. Coliiformes 124 B. Coraciiformes (Including Trogonidae and Galbulae) 124 C. Strigiformes 129 D. Caprimulgiformes 132 E. Apodiformes 134 F. Family Incertae Sedis Trochilidae 135 G. Order Incertae Sedis Bucerotiformes (Including Upupae) 136 H. Piciformes 138 I. Passeriformes 139 X. The Water Bird Assemblage 141 A. Gruiformes 142 B. Family Incertae Sedis Ardeidae 165 79 Avian Biology, Vol. Vlll ISBN 0-12-249408-3 80 STORES L. OLSON C. Family Incertae Sedis Podicipedidae 168 D. Charadriiformes 169 E. Anseriformes 186 F. Ciconiiformes 188 G. Pelecaniformes 192 H. Procellariiformes 208 I. Gaviiformes 212 J. Sphenisciformes 217 XI. Conclusion 217 References 218 I. Introduction Avian paleontology has long been a poor stepsister to its mammalian counterpart, a fact that may be attributed in some measure to an insufRcien- cy of qualified workers and to the absence in birds of heterodont teeth, on which the greater proportion of the fossil record of mammals is founded. -
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.