DOCSLIB.ORG

Back Matter (PDF)

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Back Matter (PDF) INDEX TO THE PROCEEDINGS. Brick-earth of Sussex, 62. Copper-mines of Namaqualand, R. N. British and foreign tertiaries, Mr. Prest- Rubidge on the, 233. wich on the, 89. Correlation of the eocene tertiaries of British species of fossil Mastodon, 322. England, France, and Belgium, Mr~ Bruxellian tertiaries, 106. Prestwich on the, 89. Buist, G., on the occurrence of crystal- Crag, Dr. Falconer on the age of the, lization i*n a stucco-casting, 11. 359; mammalia of the, 351 ; the Mas, Bulgaria, Capt. Spratt on the geology todon of the, 322, 347. of parts of, 72. Cretaceous fossils of Aberdeenshire, Mr. Bunbury, C., on peat-deposit, noticed, Salter on the, 83. cxxxiv. Crete, notice of the late earthquake at, Calcaire grossier and Bracklesham 240. saRds, compared, 90. Crimea and Bulgaria, Capt. Spratt on Cambrian rocks, annelide-burrows in the comparison of the geological fea- the, 199. tures of, 79. Campbell, R., on the occurrence of an Crustacean, fossil,from the lias bone-bed, earthquake at Rhodes, 176. 360; from the coal-measures, 363 ; Cephalaspis Murchisoni, 284. from the magnesian limestonez 213. ornatus, 285. Crystallization in a stucco-casting, Dr. Salweyi, 283. Buist on the occurrence of, 11. Chalk, allophane in the, 13. Cuba, description of copper-lodes at San Chalk-flints and greensand of Aberdeen- Fernando in, 240. shire, fossils from the, 83. Cyprina Fergusoni, 87. Changes of level in Hants and the Isle Dardanelles, marine deposits at the, 81. of Wight, 64. Dartmoor, the rock-basins of, 231. Charlton, allophaue in the chalk at, 13. Degous~c and Laurent on the Valen- Chemnilzia Roessleri, 216. ciennes coal-basin, noticed, exix. Chile, the occurrence of bones of Mas- De la Harpe on the English eocene todon in, 291. flora, noticed, cviii. Chiton Howseanus, 216. Dentaliurn cwlatum, 87. Loftusianus, 216. Dentition of Dichodon and allied ani- Clarke, Capt., on the mean density of mals, 194; of Mastodon and Ele- the earth, noticed, cxxx. phant, 312. Clarke, Rev. W. B., additional notice of Deshayes, G., on the Paris tertiary mol- the occurrence of volcanic bombs in luscs, noticed, cv. Australasia, 188. Dichobune, description of the genus, by Cleghorn, J., on the rock-basins of Prof. Owen, 258. Dartmoor, 231 ; noticed, cxxxv. Dichobune woina, 254. Coal in Siam, 188. Dichodon cuspidatus, Prof. Owen on Coal-shales at Medlock Park Bridge, the, 190. description of a new crustacean from Dichodon, description of the genus, by the, 363. Prof. Owen, 190. Coan, Rev. T., on the volcanic eruptions Dinotherium, Dr. Falconer on the, 310. in Hawaii, 170. Donations to the Society, ix, 135, 219, Cocchi, I., on the geology of Tuscany, 294, 371. noticed, cxiii. Dorset and Hants, the gravels of, 40, 45. Cololites, Mr. Salter on, 204. Drift-clay of Sussex, 55. Columnar rocks near Varna, 75. Ducktowu in East Tennessee, U.S., de- Committee, Report of the Library and scription of the copper-lodes of, 244. Museum, iii. Durham, Mr. Kirkby on some Permian Concordia mine, Namaqualand, 234. fossils from, 213. Conglomerates and quartzites of North- Earthquake at Crete, 240; at Rhodes, west Scotland, 17. 176. Copperberg in Namaqualand, 234. Egerton, Sir P., palichthyologic notes, Copper-lodes at San Fernando, near No. 9, on some fish-remains from the Cienfuegos in Cuba, Prof. D. T. An- neighbourhood of Ludlow, 282. steal on the, 240; near Sykesville, in Elephants occurring in the fossil state Maryland, North America, 242 ; of in Great Britain, Dr: Falconer on the Ducktown, in East Tennessee, U.S., species of, 307. description of the, 245 ; map of the Elephas, Dr. Falconer's diagnosis of the Ducktown mineral district, 247. genus, 317. INDEX TO THE PROCEEDINGS. Eocene tertiaries of England, France, tiary deposits of the Sussex coast, 40 ; and Belgium, Mr. Prestwich on the noticed, xcvi. correlation of the, 89. Goniodactylus (recent), 368. Euboea, the coast of Greece, and Salo- Gossan-lodes in the Ducktown mineral nika, Capt. Spratt on the freshwater district, U.S., 248. deposits of, 177. Gould, Charles, description of a new Euelephas, Dr. Falconer on the, 315. fossil crustacean (Tropifer l~evis, C. Falconer, Dr. H., on the species of Mas- Gould) from the lias bone-bed, by, todon and Elephant occurring in the 360. fossil state in Great Britain, Part I. Granite of Namaqualand, 235. Mastodon, 307 ; description of two Gravels of Dorset and ttants, 40 ; Sus- species of the fossil mammalian genus sex, 41, 47. Plagiaulax from Purbeck , 261. Greece, Capt. Spratt on the freshwater Ferguson, W., on the chalk-flints and deposits of the coast of, 177. greensand found in kberdeenshire, 88. Greensand in Aberdeenshire, fossils of Fish-remains from the neighbourhood the, 85. of Ludlow, 282, 290. Gr~s de Bcanchamp, 107. Flustrellaria dentata, 86. Hants, the gravels of, 40. Forbes, E., on the tertiaries of the Isle Harkness, R., on the Dingle Promon- of Wight, noticed, ciii. tory, noticed, lxxxii; on the lowest Fossil crustacean, description of a new, sedimentary rocks of Scotland, no- by Mr. C. Gould, 360; from the coal- ticed, lxxviii; on the Permian rocks measures, description of, by Prof. of the south of Scotland, noticed, Huxley, 363. lxxxi; J. Blyth on the cleavage of Fossiliferous ironstone occurring on the the Devonian rocks in Ireland, no- North Downs, Mr. Prestwich on ticed, lxxxii. some, 212. Haughton, S., on the carboniferous and Fossils found in the chalk-flints and old red beds of Ireland, noticed, cxxi. greensand of Aberdeenshire, 83 ; from Hawaii, the volcanic eruptions in, 164, Bulgaria, 82; from Varna, the Bul. 170, 176. garian coast, and the Dardanelles, 82 ; Helminthites, Mr. Salter on, 204. of the Barton clay, 118 ; of the mud- Hennessy, on the earth's internal struc- deposits of the Sussex levels, 51. ture, noticed, cxxix. Fossil species of Mastodon and Elephas, Highcliff, sections at, 45, 108. 307. Hillier, C. B., and H. J. Moyle, notice vertebrm of a serpent (Laophis of the occurrence of metalliferous crotalo'ides, Ow.) discovered by Capt. ores and coal in Siam, ] 88. Spratt in a tertiary formation at Sa- Hippothoa Foigtiana, 217. lonika, 183, 196. Hopkins, W., on the internal structure French coast, gravels of the, 43. of the earth, noticed, cxxix. Freshwater deposits of Bulgaria, 80; Huxley, T. H., description of a new of Euboea, the coast of Greece, and crustacean (Pygocephalus Cooped, Salonika, Capt. Spratt on the, 177. Huxley) from the coal-measures, by, Geinitz, H. B., on the coal-formation 363. of Saxony, noticed, exxv. Hypsiprymnus Gaimardi (recent), 278. General Meeting, Annual, i. Ice-carried boulder at Borgholm, 189. Geological age of the Mastodons, 343. Ichthyodorulites from near Ludlow, history of the north-westeru di- 288. strict of Scotland, 36. Indian Geological Survey, memoirs of Geology of Namaqualand, Dr. Rubidge the, noticed, cxxiii. on the, 233; some parts of Greece, Ironstone, fossilfferous, of the North Capt. Spratt on the, 177 ; the:Bul- Downs, 212. garian coast, Capt. Spratt on the, 72; Isle of Wight, lower jaw and teeth of the N.W. Highlands, Prof. J. Nicol an anoplotherioid quadruped (Dicho- on the, 17; the Sussex coast, Mr. bune ovina) from the upper eocene Godwin-Austen on the, 40; Varna marl in the, 254 ; Dichodon cuspida- and its vicinity, Capt. Spratt on the, tus from the, 190; sectional lists of 72. the tertiarybeds at the, 109 ; sections Gneiss of Namaqualand,235 ; the north- of cliffs at, 108,109; the gravels of, 46. west of Scotland, 17. Jones, T. Rupert, on Esthcria minuta, Godwin-Austcn, R., on the newer ter- noticed, exxxix. INDEX TO THE PROCEEDINGS. Kelly, J., on the carboniferous rocks and tion of Manna Loa, 176; noticed, old red sandstone of Ireland, noticed, cxxxii. CXX. Mineral-veins of Namaqualand, 233. Kilauca, volcano of, 165. -------, Prof. Anstcd on some re- Kinahan, C. H., on the igneous rocks markable, 240. of the Berehaveu district, noticed, Mineral waters from the Turko-Persian .., CXXlll. frontier, 184. King, W., on the Permian formation of Molecular changes, Dr.Buist on, 11. Ireland, noticed, cxxviii. Moore, J. C., on the Silurian rocks of Kirkby, J. W., on some Permian fossils Wigtonshire, noticed, lxxxiii. from Durham, 213 ; noticed, cxxxviii. Morris, J., on the occurrence of allo- Kollyrite, Mr. Morris on, 16. phane at Charlton,Kent, 13 ; noticed, Kustenjeh, section at, 78. CXXXV. Laekenian tertiaries, 107. Moyle, H. J., and C. B. HHillier, notice Lake Van, analysis of the water from, •of the occurrence of metalliferous 186. ores and coal in Siam, 188. Laophis crotalo~des, 196. Murchison, Sir R., note on the relative Lias bone-bed;crustacean from the,360. position of the strata near Ludlow, Library Committee, Report of the, iii. containing the ichthyolites described Lima elegans, 85. by Sir P. Egerton, 290 ; reply on re- Permiwna, 217. ceiving for M. J. Barrande the Wol- Limestones, fossilfferous, of the North. lastou Medal, xxiv. western Islands, 17. Museum Committee, Report of the, iii. Limopsis texlurata, 86. Mysis (recent), 368. Livonati Hills on the Locrian coast, Namaqualand, Dr. Rubidge on the cop- section of the freshwater deposits per-mines of, 233. at the, 180. Newer tertiary deposits of the Sussex Longmynd, Mr. Salter on annelide- coast, 40. burrows and surface-markings from Nicol, James, on the red sandstone the Cambrian rocks of the, 199; and conglomerate, and the super- section of the, 200. posed quartz-rocks, limestones, and l,oxodon, Dr. Falconer on the, 315. gneiss of the north-west coast of Ludlow, Sir P. Egerton on some fish- Scotland, 17 ; noticed, lxxxiv. remains from the neighbourhood of, North America, description of some 282, 290. copper-lodes in, 242. Lyell, Sir C. (Vice-President), Address North Downs, some fossiliferous iron- on handing to Sir R.
Load more

Recommended publications
  • Front Matter (PDF)
    THE- QUARTERLY JOURNAL OF THE GEOLOGICAL SOCIETY OF LONDON. EDITED BY THE ASSISTANT-SECRETARY OF THE GEOLOGICAL SOCIETY. VOLUME THE THIRTEENTH. 1857. PART THE FIRST. PROCEEDINGS OF THE GEOLOGICAL SOCIETY. LONDON : LONGMAN, BROWN, GREEN, LONGMANS, AND ROBERTS. PARIS :--FRIED. KLINCKSIECK, 11 RUE DE LILLE; BAUDRY, 9 RUE DU COQ, PRES LE LOUVRE; LEIPZIG, T. O. WEIGEL. SOLD ALSO AT THE APARTMENTS OF THE SOCIETY. MDCCCLVI[. OF THE 0 FFI CE RS OF THE GEOLOGICAL SOCIETY OF LONDON. .... ~...,. ........ .~ .... Elected February 20, 1857. ~rt~i~tnt. Col. Portloek, R.E., F.R.S. ~itt~rt~i~tnt~;. R. A. Godwin-Austen, Esq., B.A., F.R.S. William Hopkins, Esq., M.A., F.R.S. Leonard Horner, Esq., F.R.S.L. & E. Sir R. I. Murehison, G.C.St.S., F.R.S. & L.S. c~ttrttarit~. Robert W. Mylne, Esq. Warington W. Smyth, Esq., M.A. :FQrti~n bttretam. William John Hamilton, Esq., F.R.S. ~rta~ur~r. Joseph Prestwieh, Esq., F.R.8. Samuel H. Beekles, Esq. John C. Moore, Esq., M.A., F.R.8. Prof. Charles Daubeny, M.D., F.R.S. & L.S. Sir R. I. Murehison, G.C.St.S., F.RS. & Earl of Ducie, F.R.S. L.S. Hugh Falconer, M.D., F.R.S. Robert W, Mylne, Esq. Thomas F. Gibson, Esq. Prof. B. Owen, M.D., LL.D., F.R.S. & L.S. R. A. Godwin-Austen, Esq., B.A., F.R.S. S. R. Pattison, Esq. William John Hamilton~ Esq., F.R.S. Col. Portloek, R.E., F.R.S.
    [Show full text]
  • Pliocene Stratigraphic Paleobiology in Tuscany and the Fossil Record Of
    FLORE Repository istituzionale dell'Università degli Studi di Firenze Pliocene stratigraphic paleobiology in Tuscany and the fossil record of marine megafauna Questa è la Versione finale referata (Post print/Accepted manuscript) della seguente pubblicazione: Original Citation: Pliocene stratigraphic paleobiology in Tuscany and the fossil record of marine megafauna / Dominici, Stefano; Danise, Silvia; Benvenuti, Marco. - In: EARTH-SCIENCE REVIEWS. - ISSN 0012-8252. - ELETTRONICO. - 176(2018), pp. 277- 310. [10.1016/j.earscirev.2017.09.018] Availability: This version is available at: 2158/1139176 since: 2020-12-18T15:37:43Z Published version: DOI: 10.1016/j.earscirev.2017.09.018 Terms of use: Open Access La pubblicazione è resa disponibile sotto le norme e i termini della licenza di deposito, secondo quanto stabilito dalla Policy per l'accesso aperto dell'Università degli Studi di Firenze (https://www.sba.unifi.it/upload/policy-oa-2016-1.pdf) Publisher copyright claim: (Article begins on next page) 10 October 2021 Earth-Science Reviews 176 (2018) xxx–xxx Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Pliocene stratigraphic paleobiology in Tuscany and the fossil record of MARK marine megafauna ⁎ Stefano Dominicia, , Silvia Daniseb, Marco Benvenutic a Università degli Studi di Firenze, Museo di Storia Naturale, Firenze, Italy b Plymouth University, School of Geography, Earth and Environmental Sciences, Plymouth, United Kingdom c Università degli Studi di Firenze, Dipartimento di Scienze della Terra, Firenze, Italy ABSTRACT Tuscany has a rich Pliocene record of marine megafauna (MM), including mysticetes, odontocetes, sirenians and seals among the mammals, and six orders of sharks among the elasmobranchs.
    [Show full text]
  • Mals, Aided by a Valuable Collection of Small Isolated Teeth and The
    Article XVII. -FOSSIL MAMMAL,S OF THE UPPER CRETACEOUS BEDS. By HENRY FAIRFIELD OSBORN. It is interesting to return to the study of the Cretaceous mam- mals, aided by a valuable collection of small isolated teeth and jaws, which the American Museum owes to the skill of Dr. Wort- man and Mr. 0. A. Peterson of the Expedition of I892. This collection of about 400 specimens was made primarily with the object of completing the series of types of American fossil mam- mals, which has been undertaken for the Museum. It represents the great majority, but not all, of the types already described from the Laramie; it apparently adds a few new forms, and enables the writer to offer a further review of the Upper Creta- ceous mammals thus far made known through the works of Cope, Marsh and Osborn. The object of this paper is to show, as nearly as can be done at present, what these Cretaceous mammals were, by bringing the scattered teeth together and reconstructing the upper and lower dentition; and secondly, to consider how they are related in general structure, and in the stages of evolution which they represent, to the older Jurassic and more recent Puerco mam- mals from the basal Eocene. The main conclusions reached in these studies support and extend the opinions expressed by the writer in earlier papers, namely, that: i. This Laramie fauna is widely separated from the Upper Jurassic, and is more nearly contemporaneous with the basal Eocene forms of the Puerco, and the Cernaysian of France. 2. It is not highly varied, but on the other hand rather limited in the number of distinct types represented, including only two, or possibly three, of the well-known types of Multituberculata (Allotheria) and several types of Trituberculates which can now be distinguished.
    [Show full text]
  • Paleobiology and Taxonomy of Extinct Lamnid and Otodontid Sharks (Chondrichthyes, Elasmobranchii, Lamniformes)
    PALEOBIOLOGY AND TAXONOMY OF EXTINCT LAMNID AND OTODONTID SHARKS (CHONDRICHTHYES, ELASMOBRANCHII, LAMNIFORMES) By DANA JOSEPH EHRET A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 2010 1 © 2010 Dana Joseph Ehret 2 To my family, Bryan, Debra, and Sydney Ehret, Alyssa, Jim, Doyle, and Cowan Fagen for all of their support 3 ACKNOWLEDGMENTS I am grateful for the guidance of my advisor Bruce MacFadden, who has been a source of intellectual and research support. I thank my Ph.D. Committee, including Doug Jones, Karen Bjorndal, Jonathan Bloch, Greg Erickson, Dick Franz, and Gordon Hubbell, for their support with my research. I would especially like to thank Gordon and Kate Hubbell for all of their hospitality, time spent teaching me about fossil sharks, and moral support. Jonathan Bloch has contributed to my development as a researcher and has provided invaluable advice while searching and applying for jobs. Richard Hulbert has helped by teaching me curatorial and field collection techniques, offering editorial advice, and providing access to fossil materials. My dissertation research would not have been possible without access to museum collections including: the Florida Museum of Natural History (FLMNH), Jaws International, Gainesville, Florida (GH), Museo de Historia Natural Javier Prado, Lima, Peru (MUSM), Royal Belgian Institute of Natural Sciences, Brussels, Belgium (IRSNB), Saitama Prefectural Museum, Saitama,
    [Show full text]
  • Skeleton of the Fossil Shark Isurus Denticulatus from the Turonian (Late Cretaceous) of Germany—Ecological Coevolution with Prey of Mackerel Sharks
    Hindawi Publishing Corporation Paleontology Journal Volume 2014, Article ID 934235, 20 pages http://dx.doi.org/10.1155/2014/934235 Research Article Skeleton of the Fossil Shark Isurus denticulatus from the Turonian (Late Cretaceous) of Germany—Ecological Coevolution with Prey of Mackerel Sharks Cajus G. Diedrich Private Research Institute Paleologic, Petra Bezruce 96, CZ-26751 Zdice, Czech Republic Correspondence should be addressed to Cajus G. Diedrich; [email protected] Received 19 May 2013; Accepted 24 July 2013; Published 13 May 2014 Academic Editors: A. Garcia-Alix, A. M. F. Valli, and F. Vega Copyright © 2014 Cajus G. Diedrich. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. An Isurus denticulatus (Glickman, 1957) shark skeleton from the late Turonian (Late Cretaceous) of Germany is described within a diverse upwelling influenced fish fauna of northern Germany, Europe. It was found in the turbiditic marly limestones atthe submarine Northwestphalian Lippe Swell in the southern Proto-North Sea Basin. Compared to modern mackerel shark Isurus oxyrinchus Rafinesque, 1809, including cranial denticles, this allows a revision of the younger synonym “Cretoxyrhina Glickman, 1964”. Within the Cretaceous Isurus, a loss of the lateral tooth cusps and nutritive clefts of the roots (considered as plesiomorphic character of the Lamnidae) took place from the Albian (Early Cretaceous) to the Campanian (Late Cretaceous). The tooth morphology changed during the Albian-Turonian from a tearing (I. denticulatus)toacutting(I. mantelli) type (Coniacian- Campanian). The complete lateral cusplet and symphyseal teeth reduction in Isurus attheendoftheCretaceousseemtobea result of the coevolutionary changing feeding habits of a worldwide expanding shark.
    [Show full text]
  • Fossil Xenarthran Mammals from Venezuela - Taxonomy, Patterns of Evolution and Associated Faunas
    Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2010 Fossil xenarthran mammals from Venezuela - taxonomy, patterns of evolution and associated faunas Carlini, A A Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: https://doi.org/10.5167/uzh-58039 Dissertation Published Version Originally published at: Carlini, A A. Fossil xenarthran mammals from Venezuela - taxonomy, patterns of evolution and associated faunas. 2010, University of Zurich, Faculty of Science. FOSSIL XENARTHRAN MAMMALS FROM VENEZUELA – TAXONOMY, PATTERNS OF EVOLUTION AND ASSOCIATED FAUNAS Dissertation zur Erlangung der naturwissenschaftlichen Doktorwürde (Dr. sc. nat.) vorgelegt der Mathematisch-naturwissenschaftlichen Fakultät der Universität Zürich von Alfredo A. Carlini aus Argentinien Promotionskomitee Prof. Dr. Marcelo Sánchez (Leiter der Dissertation, Vertreter der Universität Zürich) PD Dr. Winand Brinkmann Dr. Richard H. Madden Prof. Dr. Lukas Keller Zürich, 2010 ALFREDO A. CARLINI FOSSIL XENARTHRAN MAMMALS FROM VENEZUELA Zusammenfassung der Dissertation für nichtakademisches Laienpublikum Basierend auf Analysen neuer Fossilfunde werden in der vorliegenden Studie neue Erkenntnisse zur Evolution der Xenarthra des tropischen Südamerikas vorgestellt. Die Vielfalt der Säugetierformen der letzten 10 Millionen Jahre in Venezuela ist ein Schlüssel zum Verständnis der Faunenbewegungen zwischen Süd-, Mittel- und Nordamerika sowie den karibischen Inseln. Es wurden Vertreter zweier Taxa der Xenarthra untersucht: Faultiere, sowie der durch körperbedeckende „Panzer“ charakterisierten Gürteltiere und Glyptodonten. Einige der neu beschriebenen Fossilien repräsentieren neue Stammeslinien und es wurden neuer Gattungen sowie Arten gefunden, welche aus dem südlichen Südamerika unbekannt sind. Der erste Nachweis des Glyptodonten Glyptotherium innerhalb Südamerikas ist ein Indiz für das Vorhandensein von eiszeitlichen „Korridoren“ durch den amerikanischen Kontinent.
    [Show full text]
  • A Phylogenetic Blueprint for a Modern Whale ⇑ John Gatesy A, , Jonathan H
    Molecular Phylogenetics and Evolution xxx (2012) xxx–xxx Contents lists available at SciVerse ScienceDirect Molecular Phylogenetics and Evolution journal homepage: www.elsevier.com/locate/ympev A phylogenetic blueprint for a modern whale ⇑ John Gatesy a, , Jonathan H. Geisler b, Joseph Chang a, Carl Buell c, Annalisa Berta d, Robert W. Meredith a,e, Mark S. Springer a, Michael R. McGowen f a Department of Biology, University of California, Riverside, CA 92521, USA b Department of Anatomy, New York College of Osteopathic Medicine, New York Institute of Technology, Northern Boulevard, Old Westbury, NY 11568, USA c 22 Washington Avenue, Schenectady, NY 12305, USA d Department of Biology, San Diego State University, San Diego, CA 92182, USA e Department of Biology and Molecular Biology, Montclair State University, Montclair, NJ 07043, USA f Center for Molecular Medicine and Genetics, Wayne State University School of Medicine, 540 E. Canfield St., Detroit, USAMI 48201, USA article info abstract Article history: The emergence of Cetacea in the Paleogene represents one of the most profound macroevolutionary Available online xxxx transitions within Mammalia. The move from a terrestrial habitat to a committed aquatic lifestyle engendered wholesale changes in anatomy, physiology, and behavior. The results of this remarkable Keywords: transformation are extant whales that include the largest, biggest brained, fastest swimming, loudest, Cetacea deepest diving mammals, some of which can detect prey with a sophisticated echolocation system Phylogeny (Odontoceti – toothed whales), and others that batch feed using racks of baleen (Mysticeti – baleen Supermatrix whales). A broad-scale reconstruction of the evolutionary remodeling that culminated in extant ceta- Fossil ceans has not yet been based on integration of genomic and paleontological information.
    [Show full text]
  • New Morphological Evidence for the Phylogeny of Artiodactyla, Cetacea, and Mesonychidae
    PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, NY 10024 Number 3344, 53 pp., 11 ®gures August 28, 2001 New Morphological Evidence for the Phylogeny of Artiodactyla, Cetacea, and Mesonychidae JONATHAN H. GEISLER1 ABSTRACT Parsimony-based analyses of a data set including 68 taxa coded for 186 morphological characters corroborate monophyly of Artiodactyla (even-toed ungulates), Suiformes (hippos, pigs, peccaries), Neoselenodontia (camels, deer, cows), and Acreodi (whales, dolphins, por- poises, mesonychids). Additional ®ndings include a sister-group relationship between Cain- otheriidae and Cameloidea (Camelidae 1 Oromerycidae), Elomeryx as the sister group to all other suiform artiodactyls, Protoceratidae as the basal branch of Neoselenodontia, and para- phyly of Mesonychidae. The molecule-based groups Whippomorpha (whales, dolphins, hip- pos), Cetruminantia (whales, deer, cows), and Artiofabula (whales, cows, pigs) are contradicted by these data and occur together in trees that are at least 25 steps longer than the most parsimonious ones. In terms of tree length, the molecule-based topology is contradicted by morphological data with and without extinct taxa, and unlike previous, morphology-based analyses, the exclusion of Cetacea from the clade of living artiodactyls is not dependent on the inclusion of extinct taxa. Artiodactyla is diagnosed in all most parsimonious trees by several characters, including a short mastoid process of the petrosal, absence of an alisphenoid canal, and presence of an entocingulum on P4. Some previously suggested artiodactyl syna- pomorphies, such as an enlarged facial exposure of the lacrimal and absence of contact be- tween the frontal and alisphenoid, are shown to be synapomorphies of more exclusive clades within Artiodactyla.
    [Show full text]