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From the Middle Eocene of Belgium
[Palaeontology, Vol. 53, Part 2, 2010, pp. 365–376] BONY-TOOTHED BIRDS (AVES: PELAGORNITHIDAE) FROM THE MIDDLE EOCENE OF BELGIUM by GERALD MAYR* and THIERRY SMITH *Forschungsinstitut Senckenberg, Sektion Ornithologie, Senckenberganlage 25, D-60325 Frankfurt am Main, Germany; e-mail [email protected] Royal Belgian Institute of Natural Sciences, Department of Paleontology, Rue Vautier 29, B-1000 Brussels, Belgium; e-mail [email protected] Typescript received 7 April 2009; accepted in revised form 19 July 2009 Abstract: We describe well-preserved remains of the Pelag- deidae (albatrosses) in overall morphology, but because ornithidae (bony-toothed birds) from the middle Eocene of bony-toothed birds lack apomorphies of the Procellariifor- Belgium, including a sternum, pectoral girdle bones and mes, the similarities are almost certainly owing to conver- humeri of a single individual. The specimens are tentatively gence. Bony-toothed birds were often compared with the assigned to Macrodontopteryx oweni Harrison and Walker, ‘Pelecaniformes’ by previous authors, who especially made 1976, which has so far only been known from the holotype comparisons with the Sulidae (gannets and boobies). How- skull and a referred proximal ulna. Another species, about ever, the coracoid distinctly differs from that of extant ‘pelec- two times larger, is represented by an incomplete humerus aniform’ birds, and the plesiomorphic presence of a foramen and tentatively identified as Dasornis emuinus (Bowerbank, nervi supracoracoidei as well as the absence of a well- 1854). The fossils provide critical new data on the osteology delimited articulation facet for the furcula supports a of the pectoral girdle of bony-toothed birds. For the first position outside the Suloidea, the clade to which the Sulidae time, the sternum of one of the smaller species is preserved, belong. -
Set in Stone the NHM Palaeontology Dept
Autumn 2006. Vol. 4, No. 3 Set in Stone The NHM Palaeontology Dept. Newsletter Rocks and Rioja Angela Milner visits Baryonyx in Spain Also in this issue Lorna Steel brings the Dodo back to life Norm MacLeod on science and religion Jon Todd on fieldwork in East Africa Keeper Country Contents Science and Religion: What Scientists Believe Keeper Country: Science and Religion: What Scientists Believe...........................................2 Relations between science and religion are much in that hypothesis; contra ‘common’ sense. The point the news these days. As any such discussion usu- is no matter how many ravens you observe, you Research Roundup........................................4 ally touches on the subject of fossils, that puts won’t be sure ravens are black until and unless you palaeontologists directly in the firing line. At the observe all things, which is impossible. In order to Collections News ..........................................5 recent International Foraminiferan Congress accept the hypothesis ‘all ravens are black’ some- (FORAMS 2006) I found myself having lunch with thing beyond simple deduction is needed, which Bringing the Dodo back to Life.......................5 Jere Lipps, Steve Culver, and Mark Lekkie when brings us back to the issue of belief. Is belief—in the conversation turned from political politics (e.g., black ravens, evolution, or anything else—possible Rocks and Rioja.............................................6 what an embarrassment the current Bush adminis- for those who subscribe to a scientific view of the tration has proven to be) to cultural politics in the world? Lake Rukwa: Palaeontological Fieldwork in form of the science-religion dichotomy. My three US the Basin of a ‘Forgotten’ East African Field colleagues all agreed they were having to be much Naturally, different people answer this question in Lake...............................................................7 more careful in their comments during lectures and different ways. -
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. -
Note on the Sauropod and Theropod Dinosaurs from the Upper Cretaceous of Madagascar*
EXTRACT FROM THE BULLETIN DE LA SOCIÉTÉ GÉOLOGIQUE DE FRANCE 3rd series, volume XXIV, page 176, 1896. NOTE ON THE SAUROPOD AND THEROPOD DINOSAURS FROM THE UPPER CRETACEOUS OF MADAGASCAR* by Charles DEPÉRET. (PLATE VI). Translated by Matthew Carrano Department of Anatomical Sciences SUNY at Stony Brook, September 1999 The bones of large dinosaurian reptiles described in this work were brought to me by my good friend, Mr. Dr. Félix Salètes, primary physician for the Madagascar expedition, from the environs of Maevarana, where he was charged with installing a provisional hospital. This locality is situated on the right bank of the eastern arm of the Betsiboka, 46 kilometers south of Majunga, on the northwest coast of the island of Madagascar. Not having the time to occupy himself with paleontological studies, Dr. Salètes charged one of his auxiliary agents, Mr. Landillon, company sergeant-major of the marines, with researching the fossils in the environs of the Maevarana post. Thanks to the zeal and activity of Mr. Landillon, who was not afraid to gravely expose his health in these researches, I have been able to receive the precious bones of terrestrial reptiles that are the object of this note, along with an important series of fossil marine shells. I eagerly seize the opportunity here to thank Mr. Landillon for his important shipment and for the very precise geological data which he communicated to me concerning the environs of Maevarana, and of which I will now give a short sketch. 1st. Geology of Maevarana and placement of the localities. * Original reference: Depéret, C. -
Dinosaur Species List E to M
Dinosaur Species List E to M E F G • Echinodon becklesii • Fabrosaurus australis • Gallimimus bullatus • Edmarka rex • Frenguellisaurus • Garudimimus brevipes • Edmontonia longiceps ischigualastensis • Gasosaurus constructus • Edmontonia rugosidens • Fulengia youngi • Gasparinisaura • Edmontosaurus annectens • Fulgurotherium australe cincosaltensis • Edmontosaurus regalis • Genusaurus sisteronis • Edmontosaurus • Genyodectes serus saskatchewanensis • Geranosaurus atavus • Einiosaurus procurvicornis • Gigantosaurus africanus • Elaphrosaurus bambergi • Giganotosaurus carolinii • Elaphrosaurus gautieri • Gigantosaurus dixeyi • Elaphrosaurus iguidiensis • Gigantosaurus megalonyx • Elmisaurus elegans • Gigantosaurus robustus • Elmisaurus rarus • Gigantoscelus • Elopteryx nopcsai molengraaffi • Elosaurus parvus • Gilmoreosaurus • Emausaurus ernsti mongoliensis • Embasaurus minax • Giraffotitan altithorax • Enigmosaurus • Gongbusaurus shiyii mongoliensis • Gongbusaurus • Eoceratops canadensis wucaiwanensis • Eoraptor lunensis • Gorgosaurus lancensis • Epachthosaurus sciuttoi • Gorgosaurus lancinator • Epanterias amplexus • Gorgosaurus libratus • Erectopus sauvagei • "Gorgosaurus" novojilovi • Erectopus superbus • Gorgosaurus sternbergi • Erlikosaurus andrewsi • Goyocephale lattimorei • Eucamerotus foxi • Gravitholus albertae • Eucercosaurus • Gresslyosaurus ingens tanyspondylus • Gresslyosaurus robustus • Eucnemesaurus fortis • Gresslyosaurus torgeri • Euhelopus zdanskyi • Gryponyx africanus • Euoplocephalus tutus • Gryponyx taylori • Euronychodon -
Short Review of the Present Knowledge of the Sauropoda
PRESENT KNOWLEDGE OF THE SAUROl'ODA.-HUENE. 121 SHORT REVIEW OF THE PRESENT KNOWLEDGE OF THE SAUROPODA. BY DR. FRIEDRICH BARON HUENE, PROFESSOR AT THE UNIVERSITY OF TUBINGEN, GERMANY. THE Sauropoda are the hugest continental animals the earth has ever seen. They lived from the middle Jurassic to the Danian period of the upper most Cretaceous. Much has been written about them, but nevertheless their natura! classification and development do not yet appear in a desirable clearness. In this respect the immense size of the Sauropoda has been an obstacle. The satisfactory excavation of such gigant.ic skeletons is difficult, and the preparation, which is still more important, needs trained, skilful men working for years. The scientific value of a skeleton is determined in advance by the degree of care by which, during the excavation, the original articulation or the original positions of the bones to each other in the rock is dealt "\vith by sketch-plans in scale as to make sure specially the sequence of the vertebræ. Because of the failure of this in many cases, we still know so astonishingly little about the natura! classification of the Sauropoda as a whole. Most has been written and spoken on the North American Sauropoda. Too little has been done with the earlier Sauropoda. The knowledge of the Upper Cretaceous Sauropoda until now is quite insufficient. The large amount of Tendaguru Sauropoda at Berlin and the recent excavations of the Carnegie Museum at Pittsburgh have not yet been described ; they will probably complete and alter our ideas of the development and classification of the Sauropoda. -
THE GENERA of REPTILES. By
T he Genera of Re pt il e s. By BARON FRANCIS NOPCSA (Budapest). (Eingelangt am 11. Mai 1927.) Among all the Paleontologists living none has dealt with the recent and fossil reptiles with a wider grasp than Prof. L. D o l l o and at his anniversary it seems quite appropriate to review their whole array. The classification used in the following enumeration of all genera of reptiles is much the same as in my hook „Die Familien der Reptilien“; at this instance however an effort has been made to give a precise definition of every systematic unit. Alteration of the classification became necessary among the Dino- cephalians, the Nothosaurians, the Lacertilians (called here Sauroidea), the Coelurosauroidea and the Crocodilia. The new classification of the Sauroidea is intermediate between the classifications proposed by B o u l e n g e r and C a m p . Naturally as a rule only those fossil genera are referred to, that are more than simple catalogue numbers that facilitate the finding of the respective piece in a collection; indeterminable problematic genera of small interest have mostly been omitted. Extinct units and genera are marked in the lists with a cross ("j*). Difficulties of classification have been encountered in the Lacertilia and Ophidia, for in the new system the conventional families of recent Lizards and Serpents has been given subfamily rank and conse quently the different recent subfamilies had to be dropped. Instead of these subfamilies the minor units were separated by greek letters. — The tedious and complicated revision of the genera of recent Lizards and Snakes was done by Prof. -
A Detailed Description of Caspiodontornis Kobystanicus From
Acta zool, cracov. 42(3): 423-433, Kraków, 17 Dec., 1999 A detailed descriptionCaspiodontornis of kobystanicus from the Oligocene of the Caspian seashore Sevil M. ASLANOVA andN. I. BURCHAK-ABRAMOVICH Received: 15 Dec., 1996 Acccpted for publication: 19 June, 1998 ASLANOVA S. M., BURCHAK-ABRAMOVICH N. I. 1999. A detailed description Cas-of piodontornis kobystanicus from the Oligocene of the Caspian seashore. Acta zool, cracov. 42(3): 423-433. ' Abstract. The paper presents a detailed description of a skull and mandibleCaspiodon of tornis kobystanicus, which is a middle-sized member of the bony-toothed birds, differing distinctly from those so far described. It had an alongated pelecaniform bill, flattened dorso-ventrally.The upper bony-teeth were comparatively small, those in the lower jaw be ing larger. Holorhinal nares narrow, pterygoid comparatively short, wide, pelecaniform. Key words: Odontopterygiformes,Caspiodontornis kobystanicus, Oligocene, Apsheron Peninsula, Perekishkyul locality. Sevil M. ASLANOVA, Institute of Palaeobiology, Georgian AS, Potochnaya 4, Tbilisi, Georgia. I. INTRODUCTION The first bony-toothed Odontopteryxbird, toliapica O w en , 1873, was reported from the Early Eocene of England. Next a number of other species were described(S p u lsk i1910, HOWARD 1957, H o p so n1964, etc.).B r o d k o r(1963), b just asO ls o n(1985) later, treated the bony-toothed birds as a suborder in the order Pelecaniformes. In addition to the descriptions of some new species the monographHARRISON by & W a lk e r ( 1976) presents a revision of this group of birds raised to the rank of a separate order, Odontopterygiformes, which, besides, had already been proposed by H o w a r d(1957) before.HARRISON & W a l k e r (1976) have devided the order Odontopterygi- fonnes into four families: Odontopterygidae, Pseudodontopterygidae, Dasomithidae and Pelargonithidae. -
Middle Eocene Vertebrate Fauna from the Aridal Formation, Sabkha of Gueran, Southwestern Morocco
geodiversitas 2021 43 5 e of lif pal A eo – - e h g e r a p R e t e o d l o u g a l i s C - t – n a M e J e l m a i r o DIRECTEUR DE LA PUBLICATION / PUBLICATION DIRECTOR : Bruno David, Président du Muséum national d’Histoire naturelle RÉDACTEUR EN CHEF / EDITOR-IN-CHIEF : Didier Merle ASSISTANT DE RÉDACTION / ASSISTANT EDITOR : Emmanuel Côtez ([email protected]) MISE EN PAGE / PAGE LAYOUT : Emmanuel Côtez COMITÉ SCIENTIFIQUE / SCIENTIFIC BOARD : Christine Argot (Muséum national d’Histoire naturelle, Paris) Beatrix Azanza (Museo Nacional de Ciencias Naturales, Madrid) Raymond L. Bernor (Howard University, Washington DC) Alain Blieck (chercheur CNRS retraité, Haubourdin) Henning Blom (Uppsala University) Jean Broutin (Sorbonne Université, Paris, retraité) Gaël Clément (Muséum national d’Histoire naturelle, Paris) Ted Daeschler (Academy of Natural Sciences, Philadelphie) Bruno David (Muséum national d’Histoire naturelle, Paris) Gregory D. Edgecombe (The Natural History Museum, Londres) Ursula Göhlich (Natural History Museum Vienna) Jin Meng (American Museum of Natural History, New York) Brigitte Meyer-Berthaud (CIRAD, Montpellier) Zhu Min (Chinese Academy of Sciences, Pékin) Isabelle Rouget (Muséum national d’Histoire naturelle, Paris) Sevket Sen (Muséum national d’Histoire naturelle, Paris, retraité) Stanislav Štamberg (Museum of Eastern Bohemia, Hradec Králové) Paul Taylor (The Natural History Museum, Londres, retraité) COUVERTURE / COVER : Réalisée à partir des Figures de l’article/Made from the Figures of the article. Geodiversitas est -
Phylogeny of the Tachinidae (Diptera) As Inferred from Morphological Evidence
Systematic Entomology (2014), 39, 335–353 Signal through the noise? Phylogeny of the Tachinidae (Diptera) as inferred from morphological evidence PIERFILIPPO CERRETTI1,2, JAMES E. O’HARA3, D. MONTGOMERY WOOD3, HIROSHI SHIMA4,DIEGOJ. INCLAN5 andJOHN O. STIREMAN III6 1Department of Biology and Biotechnology ‘Charles Darwin’, University of Rome ‘Sapienza’, Rome, Italy, 2Centro Nazionale Biodiversita` Forestale – Corpo Forestale dello Stato, Verona, Italy, 3Canadian National Collection of Insects, Agriculture and Agri-Food Canada, Ottawa, Canada, 4Kyushu University Museum, Kyushu University, Fukuoka, Japan, 5DAFNAE-Entomology, University of Padova, Padova, Italy and 6Department of Biological Sciences, Wright State University, Dayton, OH, U.S.A. Abstract. The oestroid family Tachinidae represents one of the most diverse lineages of insect parasitoids. Despite their broad distribution, diversity and important role as biological control agents, the phylogeny of this family remains poorly known. Here, we review the history of tachinid systematics and present the first quantitative phylogenetic analysis of the family based on morphological data. Cladistic analyses were conducted using 135 morphological characters from 492 species belonging to 180 tachinid genera, including the four currently recognized subfamilies (Dexiinae, Exoristinae, Phasiinae, Tachininae) and all major tribes. We used characters of eggs, first-instar larvae and adults of both sexes. We examined the effects of implied weighting by reanalysing the data with varying concavity factors. Our analysis generally supports the subfamily groupings Dexiinae + Phasiinae and Tachininae + Exoristinae, with only the Exoristinae and the Phasiinae reconstructed as monophyletic assemblages under a wide range of weighting schemes. Under these conditions, the Dexiinae, which were previously considered a well-established monophyletic assemblage, are reconstructed as being paraphyletic with respect to the Phasiinae. -
The Tachinid Times
The Tachinid Times ISSUE 24 February 2011 Jim O’Hara, editor Invertebrate Biodiversity Agriculture & Agri-Food Canada ISSN 1925-3435 (Print) C.E.F., Ottawa, Ontario, Canada, K1A 0C6 ISSN 1925-3443 (Online) Correspondence: [email protected] or [email protected] My thanks to all who have contributed to this year’s announcement before the end of January 2012. This news- issue of The Tachinid Times. This is the largest issue of the letter accepts submissions on all aspects of tachinid biology newsletter since it began in 1988, so there still seems to be and systematics, but please keep in mind that this is not a a place between peer-reviewed journals and Internet blogs peer-reviewed journal and is mainly intended for shorter for a medium of this sort. This year’s issue has a diverse news items that are of special interest to persons involved assortment of articles, a few announcements, a listing of in tachinid research. Student submissions are particularly recent literature, and a mailing list of subscribers. The welcome, especially abstracts of theses and accounts of Announcements section is more sizable this year than usual studies in progress or about to begin. I encourage authors and I would like to encourage readers to contribute to this to illustrate their articles with colour images, since these section in the future. This year it reproduces the abstracts add to the visual appeal of the newsletter and are easily of two recent theses (one a Ph.D. and the other a M.Sc.), incorporated into the final PDF document. -
1. W. Dawson on the Flora of the Devonian Period
1. W. Dawson on the Flora of the Devonian Period. 311 ART. XXXI.-On the Flora of the Devonian Period in Northeastern America; by J. W. DAWSON, LL.D., F.R.S., Principal of McGill University, Montreal.' [This paper by Prof. Dawson is the one alluded to in his pre vious communication. The 2d part containing descriptions of species is omitted.] The existence of several species of land-plants in the Devo nian rocks of New York and Pennsylvania was ascertained many years ago by the Geological Surveys of those States, and several of these plants have been described and figured in their Reports.' In Canada, Sir W. E. Logan had ascertained, as early as 1843, the presence of an abundant, though apparently mo· notonous and simple, flora in the Devonian strata of Gaspe j but it was not until 1859 that these plants were described by the author in the 'Proceedings' of this Society: More recently Messrs. Matthew and Hartt, two young geologists of St. John, New Brunswick, have found a rich and interesting flora in the semi-metamorphic beds in the vicinity of that city, in which a few fossil plants had previously been observed by Dr. Gesner, Dr. 1 Copied from the Quarterly Journal of the Geological Society, Nov., 1861. • Hall and Vanuxem. Reports on the Geology of New York; Rogers, Report aD Pl'nnsylvania. • Quart. Jour. Geol. Soc. Lond., D.4'1'1. 312 J. W. Dawson on tke Flora of tke Devonian Robb, and Mr. Bennett of St. John; but they had not been fig.