Whale Evolution: a Whale of a Tale

Total Page:16

File Type:pdf, Size:1020Kb

Whale Evolution: a Whale of a Tale Creation Research Society Quarterly 2012. 49:122–134. 122 Creation Research Society Quarterly Whale Evolution: A Whale of a Tale Jerry Bergman* Abstract review of the evolution of whales from terrestrial land animals finds A that the evidence used to support the current theory is either wrong or very questionable. A focus is on the hip bone and fetal teeth evidence because they are commonly used as proof for the land mammal-to-whale evolution theory. The putative fossil evidence for whale evolution from terrestrial animals is also evaluated, concluding that the examples used are likely all extinct mammals and not transitional forms. Introduction be only about 20 feet long, but baleen A major problem has been deter- The term “whale” is a common noun and blue whales can grow up to 100 feet mining which terrestrial animal whales that can refer to all marine mammals long. Toothed whales are, on average, evolved from. Charles Darwin proposed called cetaceans (members of order smaller then baleen whales, ranging one of the first theories of whale evolu- cetacea), including dolphins and por- from 3 to 32 feet long, although most tion, suggesting they evolved from bears. poises. In this paper the term “whales” are from 10 to 30 feet long. Blue whales He wrote, “I can see no difficulty in a excludes both dolphins and porpoises. can weigh up to 150 tons. race of bears being rendered, by natural Classification of whales divides them selection, more and more aquatic in into two groups; toothed whales and their structure and habits, with larger baleen whales, the latter of which use The Origin of Whales and larger mouths, till a creature was large brush-like structures to filter food The evolution of whales is one of the produced as monstrous as a whale” from the ocean. most difficult evolutionary enigmas, and (Darwin, 1859, p. 184). Other theories Toothed (odontoceti) whales are di- numerous theories have been proposed. include proposals that whales evolved vided into six main families: pilot whales, Historically, whales were classified as from a cow-like animal, a hippopotamus- fin whales, minke whales, blue whales, fish. It was only when Linnaeus changed like animal, a hyena-like animal called humpback whales, narwhal whales, and his original classification and reclassi- a pachyaena, a wolf-like animal called delphinidae, such as dolphins and killer fied them as mammals that their origin pakicetid, a primitive group of hoofed whales (orca). Baleen whales (suborder became an issue (Slijper, 1962). One animals called mesonychids, or even a Mysticeti) are divided into three main current theory is that marine animals catlike animal called a sinonyx. families, right whales, rorqual whales, evolved into terrestrial animals; then The hippo theory, long the leading and gray whales. Of the 76 known whale whales evolved from a terrestrial ungu- candidate because of its DNA similari- species, 66 are toothed whales, and 10 late ancestor (or from some extinct wolf- ties with whales, has recently lost favor are baleen whales. Some species grow to like animal) back into a marine animal. because the proposed hippo precursor lived too recently and in the wrong part of the world to be a whale ances- tor. Since the 1960s, another popular proposal (based on dental similarities * Jerry Bergman PhD, Biology Department, Northwest State College, Archbold, OH and molecular data) has been that Accepted for publication March 3, 2012 whales evolved from hoofed, carnivo- Volume 49, Fall 2012 123 rous mammals called mesonychians, specifically an extinct archaic ungulate (e.g., Thewissen et al., 1998; Harder, 2001). New findings, though, have placed mesonychians in the artiodacty family (even-toed ungulates including camels, hippos, pigs, and ruminants) based on Artiocetus clavis and Rodhoce­ tus balochistanems fossils (Milinkovich and Thewissen, 1997). Others argue that mesonychians cannot be ancestor to whales for several reasons, including all “phylogenetic studies indicate that pakicetids are more closely related to living cetaceans than to artiodactyls and mesonychians” (Thewissen et al., 2001). The latest theory, proposed in 2007 (see Figure 1), is that whales evolved from an Indohyus, a putative 48 million-year- old terrestrial animal the size of a small raccoon that looked like an antler-less Af- rican mouse long-tailed deer (Thewissen, et al., 2007). Some have even described this animal as an overgrown, long-legged rat, looking nothing like a whale. The main evidence it was a whale ancestor is Indohyus’s thickened ear bone, a feature that so far has been seen only in Indohyus and cetaceans (Thewissen, et al., 2007). All of these proposed theories have some support but also problems. For example, whale evolution from artio- dactyls is supported mainly by DNA se- quences yet this is problematic because all artiodactyl teeth have three lobes, a trait lacking in both cetaceans and me- Figure 1. Drawings of the skeletons of one proposal of whale evolution from the sonychians. Thus, this lineage would re- first putative whale to the modern whale. The skeletons are shown on the right. quire a complicated tooth evolution that On the left is the approximate proportions of the animals themselves. The modern “includes reversals, convergences or both” Baleen whale superimposes the skeleton on the size illustration to save space. Note (Milinkovich and Thewissen, 1997, p. the first putative animals in the evolution of whales are extremely small compared 623). Ellis (1987, p. 8) concluded that to modern-day whales, a fact obscured when the fossils are shown as a set. This “all known fossil whales seem to be fully is also a major problem for the theory of whale evolution. The animals, starting developed aquatic mammals; we do not from the bottom, are Indohyus, Pakicetus, Ambulocetus, Rodhocetus, Dorudon, know the steps that led to their return to and at the top, the modern whale Balaena. (Illustration courtesy of Richard Geer) the sea.” This conclusion still holds true. Evolution from Terrestrial Mammals evolutionists typically hypothesize that that transformation of a land tetrapod Evolutionists have always faced the prob- they evolved from some type of terrestrial into a sea mammal requires virtually lem that whales are mammals. Thus, mammal. A problem with this view is all of the tetrapod’s hundreds of major 124 Creation Research Society Quarterly land-adapted traits to be converted 2. Weight-bearing: Land-dwelling ence thirst, a sensory system not needed into sea-adapted designs. Nonetheless, animals consume about 40 percent of by sea-dwelling creatures. In contrast, whale evolution directly from a fish ap- their energy just to move their bodies, marine animals also need to regulate pears even less probable because of the but sea-dwelling creatures use water for body water, but they must do so in very enormous differences between fish and support (Zahn, 1988, p. 28). For this different ways than terrestrial animals. whale anatomy and physiology. As ex- reason the transition from land to water 5. Kidneys: Because water has to be ample, fish use gills for breathing while requires major muscular and skeletal used economically by terrestrial animals, whales use lungs; fish typically lay eggs, system design changes. Whales must they require an efficient kidney system. and whales breastfeed and give birth to not only lose their legs but also evolve The body’s protein metabolism system live young. flippers, pectoral fins, a fluke, and an either excretes or converts wastes. The Other problems with current pro- aerodynamic design, plus a brain and metabolic breakdown of protein pro- posal of whale evolution include the an appropriate nervous system to meet duces ammonia, which is toxic and is radical changes required in the integu- the needs of these many new structures therefore converted into urea, in the end ment system, lactation, breathing, div- and their requirements. reducing the amount of water excreted. ing, feeding methods, nervous system, 3. Heat Retention: Land tempera- In addition, a system of ducts and other eyes (they must be protected in water) tures often change rapidly and can fluc- structures are required for the kidney’s and hearing, and transformation from tuate over a wide range. For this reason, functioning. Sea-dwelling organisms, a walking to a swimming mode of life. land-dwelling organisms must possess a in contrast, discharge waste materials, Some additional examples include loss physical mechanism that can withstand including ammonia, directly into their of body hair, body streamlining, trans- enormous temperature fluctuations. aquatic environment. In short, in order formation of forelimbs into flippers, loss Not only do the temperature changes to evolve from water to land, living of hind limbs, evolution of flukes for in the sea occur very slowly and within things would have had to develop whole swimming, and backward movement a much narrower range, but the water new organ systems to deal with water of nostrils. Thousands of changes are is also much colder, and water has high regulation. Then, to evolve back into required to convert a land tetrapod to thermal conductivity, a major problem aquatic animals, another entirely new a fishlike mammal. All of these systems for warm-blooded mammals (Heyning system must be evolved especially to deal are interrelated and function as a unit, and Mead, 1997, p. 1138). Organisms with salt removal, since whales live in a requiring altering the interrelationships with a body system regulated according toxic saltwater world. of the whole system. Yet other changes to land temperature demands would 6. Breathing Opening: Terrestrial required for a large dog-sized tetrapod need to evolve a whole new protective animals breathe through their nose and animal to evolve into a whale include system to deal with very cold ocean water mouth. In contrast, whales have a the following: temperatures.
Recommended publications
  • The Shark-Toothed Dolphin Squalodon Cetacea
    Carnets Geol. 20 (2) E-ISSN 1634-0744 DOI 10.4267/2042/70716 The shark-toothed dolphin Squalodon (Cetacea: Odontoceti) from the remarkable Montagna della Majella marine vertebrate assemblage (Bolognano Formation, central Italy) Alberto COLLARETA 1 Andrea DI CENCIO 2 Renato RICCI 3 Giovanni BIANUCCI 4 Abstract: The extinct family Squalodontidae consists of heterodont, medium-sized odontocetes, featu- ring a long rostrum that houses large, procumbent incisors and heavily ornamented postcanine teeth carrying accessory denticles, hence their vernacular name, "shark-toothed dolphins". These longirostri- ne toothed whales are often seen as bridging the anatomical gap between archaic Oligocene odontoce- tes and their late Miocene to Holocene relatives. Possibly among the major marine predators of their ti- me, the shark-toothed dolphins are important components of several lower Miocene marine-mammal assemblages from the North Atlantic and Mediterranean/Paratethysian realms. In the present work, a partial skull of Squalodontidae is described from the strata of the Bolognano Formation cropping out in the northeastern sector of the Montagna della Majella massif (Abruzzo, central Italy), which has pre- viously yielded a rich lower Miocene marine-vertebrate assemblage, including eleven taxa of elasmo- branchs as well as subordinate teleosts and very fragmentary remains of marine reptiles and mam- mals. The specimen consists of the anterodorsal portion of a rostrum, preserving parts of both pre- maxillae and left maxilla, and the anteriormost seven upper left teeth. This partial skull is here identi- fied as belonging to the genus Squalodon, whose presence in the Montagna della Majella vertebrate assemblage had already been tentatively proposed on the basis of two fragmentary teeth.
    [Show full text]
  • A New Middle Eocene Protocetid Whale (Mammalia: Cetacea: Archaeoceti) and Associated Biota from Georgia Author(S): Richard C
    A New Middle Eocene Protocetid Whale (Mammalia: Cetacea: Archaeoceti) and Associated Biota from Georgia Author(s): Richard C. Hulbert, Jr., Richard M. Petkewich, Gale A. Bishop, David Bukry and David P. Aleshire Source: Journal of Paleontology , Sep., 1998, Vol. 72, No. 5 (Sep., 1998), pp. 907-927 Published by: Paleontological Society Stable URL: https://www.jstor.org/stable/1306667 REFERENCES Linked references are available on JSTOR for this article: https://www.jstor.org/stable/1306667?seq=1&cid=pdf- reference#references_tab_contents You may need to log in to JSTOR to access the linked references. JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at https://about.jstor.org/terms SEPM Society for Sedimentary Geology and are collaborating with JSTOR to digitize, preserve and extend access to Journal of Paleontology This content downloaded from 131.204.154.192 on Thu, 08 Apr 2021 18:43:05 UTC All use subject to https://about.jstor.org/terms J. Paleont., 72(5), 1998, pp. 907-927 Copyright ? 1998, The Paleontological Society 0022-3360/98/0072-0907$03.00 A NEW MIDDLE EOCENE PROTOCETID WHALE (MAMMALIA: CETACEA: ARCHAEOCETI) AND ASSOCIATED BIOTA FROM GEORGIA RICHARD C. HULBERT, JR.,1 RICHARD M. PETKEWICH,"4 GALE A.
    [Show full text]
  • 4. Palaeontology
    Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2015 Palaeontology Klug, Christian ; Scheyer, Torsten M ; Cavin, Lionel Posted at the Zurich Open Repository and Archive, University of Zurich ZORA URL: https://doi.org/10.5167/uzh-113739 Conference or Workshop Item Presentation Originally published at: Klug, Christian; Scheyer, Torsten M; Cavin, Lionel (2015). Palaeontology. In: Swiss Geoscience Meeting, Basel, 20 November 2015 - 21 November 2015. 136 4. Palaeontology Christian Klug, Torsten Scheyer, Lionel Cavin Schweizerische Paläontologische Gesellschaft, Kommission des Schweizerischen Paläontologischen Abhandlungen (KSPA) Symposium 4: Palaeontology TALKS: 4.1 Aguirre-Fernández G., Jost J.: Re-evaluation of the fossil cetaceans from Switzerland 4.2 Costeur L., Mennecart B., Schmutz S., Métais G.: Palaeomeryx (Mammalia, Artiodactyla) and the giraffes, data from the ear region 4.3 Foth C., Hedrick B.P., Ezcurra M.D.: Ontogenetic variation and heterochronic processes in the cranial evolution of early saurischians 4.4 Frey L., Rücklin M., Kindlimann R., Klug C.: Alpha diversity and palaeoecology of a Late Devonian Fossillagerstätte from Morocco and its exceptionally preserved fish fauna 4.5 Joyce W.G., Rabi M.: A Revised Global Biogeography of Turtles 4.6 Klug C., Frey L., Rücklin M.: A Famennian Fossillagerstätte in the eastern Anti-Atlas of Morocco: its fauna and taphonomy 4.7 Leder R.M.: Morphometric analysis of teeth of fossil and recent carcharhinid selachiens
    [Show full text]
  • Functional Morphology of the Vertebral Column in Remingtonocetus (Mammalia, Cetacea) and the Evolution of Aquatic Locomotion in Early Archaeocetes
    Functional Morphology of the Vertebral Column in Remingtonocetus (Mammalia, Cetacea) and the Evolution of Aquatic Locomotion in Early Archaeocetes by Ryan Matthew Bebej A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Ecology and Evolutionary Biology) in The University of Michigan 2011 Doctoral Committee: Professor Philip D. Gingerich, Co-Chair Professor Philip Myers, Co-Chair Professor Daniel C. Fisher Professor Paul W. Webb © Ryan Matthew Bebej 2011 To my wonderful wife Melissa, for her infinite love and support ii Acknowledgments First, I would like to thank each of my committee members. I will be forever grateful to my primary mentor, Philip D. Gingerich, for providing me the opportunity of a lifetime, studying the very organisms that sparked my interest in evolution and paleontology in the first place. His encouragement, patience, instruction, and advice have been instrumental in my development as a scholar, and his dedication to his craft has instilled in me the importance of doing careful and solid research. I am extremely grateful to Philip Myers, who graciously consented to be my co-advisor and co-chair early in my career and guided me through some of the most stressful aspects of life as a Ph.D. student (e.g., preliminary examinations). I also thank Paul W. Webb, for his novel thoughts about living in and moving through water, and Daniel C. Fisher, for his insights into functional morphology, 3D modeling, and mammalian paleobiology. My research was almost entirely predicated on cetacean fossils collected through a collaboration of the University of Michigan and the Geological Survey of Pakistan before my arrival in Ann Arbor.
    [Show full text]
  • Thewissen Et Al. Reply Replying To: J
    NATURE | Vol 458 | 19 March 2009 BRIEF COMMUNICATIONS ARISING Hippopotamus and whale phylogeny Arising from: J. G. M. Thewissen, L. N. Cooper, M. T. Clementz, S. Bajpai & B. N. Tiwari Nature 450, 1190–1194 (2007) Thewissen etal.1 describe new fossils from India that apparentlysupport fossils, Raoellidae or the raoellid Indohyus is more closely related to a phylogeny that places Cetacea (that is, whales, dolphins, porpoises) as Cetacea than is Hippopotamidae (Fig. 1). Hippopotamidae is the the sister group to the extinct family Raoellidae, and Hippopotamidae exclusive sister group to Cetacea plus Raoellidae in the analysis that as more closely related to pigs and peccaries (that is, Suina) than to down-weights homoplastic characters, althoughin the equallyweighted cetaceans. However, our reanalysis of a modified version of the data set analysis, another topology was equally parsimonious. In that topology, they used2 differs in retaining molecular characters and demonstrates Hippopotamidae moved one node out, being the sister group to an that Hippopotamidae is the closest extant family to Cetacea and that Andrewsarchus, Raoellidae and Cetacea clade. In neither analysis is raoellids are the closest extinct group, consistent with previous phylo- Hippopotamidae closer to the pigs and peccaries than to Cetacea, the genetic studies2,3. This topology supports the view that the aquatic result obtained by Thewissen et al.1. In all our analyses, pachyostosis adaptations in hippopotamids and cetaceans are inherited from their (thickening) of limb bones and bottom walking, which occur in hippo- common ancestor4. potamids9,10, are interpreted to have evolved before the pachyostosis of To conduct our analyses, we started with the same published matrix the auditory bulla, as seen in raoellids and cetaceans1.
    [Show full text]
  • Proceedings of the United States National Museum
    DESCRIPTION OF TWO SQUALODONTS RECENTLY DIS- COVERED IN THE CALVERT CLIFFS, ^LVRYLAND; AND NOTES ON THE SHARK-TOOTHED CETACEANS. By Remington Kellogg, Of the Bureau of Biological Survey, United States Departynent of Agriculture. INTRODUCTION. When the study of paleontology was less advanced than it is at present, any announcement of the discovery of prehistoric animals unlike the living indigenous fauna was usually received with some suspicion. In spite of this distrust, many attempts were made by the early writers to explain the presence of fossil remains of marine mammals in strata above the sea level or at some distance from the seashore. In one of these treatises ' is found what is, apparently, the first notice of the occurrence of fossil remains referable to shark- toothed cetaceans. The author of this work figures a fragment of a mandible, obtained from the tufa of Malta, which possesses three serrate double-rooted molar teeth. Squalodonts as such were first brought to the attention of ]mleon- tologists in 1840, by J. P. S. Grateloup, ' a French naturalist primarily interested in marine invertebrates. In the original description of Squalodon, Grateloup held the view that this rostral fragment from Leognan, France, belonged to some large saurian related to Iguanodon. Following the anouncement of this discovery. Von Meyer ^ called at- tention to the teeth of this fossil, and concluded that the specimen was referable to some flesh-eating cetacean. A year later, Grateloup* concurred in this opinion. One other specimen should be mentioned in this connection, but, unfortunately, its relationships are quite uncer- tain. This specimen consists of a single tooth which was thought to bear resemblance to some pinniped by Von Meyer ^ and named Pachy- odon mirahilis.
    [Show full text]
  • Vestibular Evidence for the Evolution of Aquatic Behaviour in Early
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Publications of the IAS Fellows letters to nature .............................................................. cetacean evolution, leading to full independence from life on land. Vestibular evidence for the Early cetacean evolution, marked by the emergence of obligate evolution of aquatic behaviour aquatic behaviour, represents one of the major morphological shifts in the radiation of mammals. Modifications to the postcranial in early cetaceans skeleton during this process are increasingly well-documented3–9. Pakicetids, early Eocene basal cetaceans, were terrestrial quadrupeds 9 F. Spoor*, S. Bajpai†, S. T. Hussain‡, K. Kumar§ & J. G. M. Thewissenk with a long neck and cursorial limb morphology . By the late middle Eocene, obligate aquatic dorudontids approached modern ceta- * Department of Anatomy & Developmental Biology, University College London, ceans in body form, having a tail fluke, a strongly shortened neck, Rockefeller Building, University Street, London WC1E 6JJ, UK and near-absent hindlimbs10. Taxa which represent bridging nodes † Department of Earth Sciences, Indian Institute of Technology, Roorkee 247 667, on the cladogram show intermediate morphologies, which have India been inferred to correspond with otter-like swimming combined ‡ Department of Anatomy, College of Medicine, Howard University, with varying degrees of terrestrial capability4–8,11. Our knowledge of Washington DC 20059, USA § Wadia Institute of Himalayan Geology, Dehradun 248 001, India the behavioural changes that crucially must have driven the post- k Department of Anatomy, Northeastern Ohio Universities College of Medicine, cranial adaptations is based on functional analysis of the affected Rootstown, Ohio 44272, USA morphology itself. This approach is marred by the difficulty of ............................................................................................................................................................................
    [Show full text]
  • The Walking Whales
    The Walking Whales From Land to Water in Eight Million Years J. G. M. “Hans” Thewissen with illustrations by Jacqueline Dillard university of california press The Walking Whales The Walking Whales From Land to Water in Eight Million Years J. G. M. “Hans” Thewissen with illustrations by Jacqueline Dillard university of california press University of California Press, one of the most distinguished university presses in the United States, enriches lives around the world by advancing scholarship in the humanities, social sciences, and natural sciences. Its activities are supported by the UC Press Foundation and by philanthropic contributions from individuals and institutions. For more information, visit www.ucpress.edu. University of California Press Oakland, California © 2014 by The Regents of the University of California Library of Congress Cataloging-in-Publication Data Thewissen, J. G. M., author. The walking whales : from land to water in eight million years / J.G.M. Thewissen ; with illustrations by Jacqueline Dillard. pages cm Includes bibliographical references and index. isbn 978-0-520-27706-9 (cloth : alk. paper)— isbn 978-0-520-95941-5 (e-book) 1. Whales, Fossil—Pakistan. 2. Whales, Fossil—India. 3. Whales—Evolution. 4. Paleontology—Pakistan. 5. Paleontology—India. I. Title. QE882.C5T484 2015 569′.5—dc23 2014003531 Printed in China 23 22 21 20 19 18 17 16 15 14 10 9 8 7 6 5 4 3 2 1 The paper used in this publication meets the minimum requirements of ansi/niso z39.48–1992 (r 2002) (Permanence of Paper). Cover illustration (clockwise from top right): Basilosaurus, Ambulocetus, Indohyus, Pakicetus, and Kutchicetus.
    [Show full text]
  • The Biology of Marine Mammals
    Romero, A. 2009. The Biology of Marine Mammals. The Biology of Marine Mammals Aldemaro Romero, Ph.D. Arkansas State University Jonesboro, AR 2009 2 INTRODUCTION Dear students, 3 Chapter 1 Introduction to Marine Mammals 1.1. Overture Humans have always been fascinated with marine mammals. These creatures have been the basis of mythical tales since Antiquity. For centuries naturalists classified them as fish. Today they are symbols of the environmental movement as well as the source of heated controversies: whether we are dealing with the clubbing pub seals in the Arctic or whaling by industrialized nations, marine mammals continue to be a hot issue in science, politics, economics, and ethics. But if we want to better understand these issues, we need to learn more about marine mammal biology. The problem is that, despite increased research efforts, only in the last two decades we have made significant progress in learning about these creatures. And yet, that knowledge is largely limited to a handful of species because they are either relatively easy to observe in nature or because they can be studied in captivity. Still, because of television documentaries, ‘coffee-table’ books, displays in many aquaria around the world, and a growing whale and dolphin watching industry, people believe that they have a certain familiarity with many species of marine mammals (for more on the relationship between humans and marine mammals such as whales, see Ellis 1991, Forestell 2002). As late as 2002, a new species of beaked whale was being reported (Delbout et al. 2002), in 2003 a new species of baleen whale was described (Wada et al.
    [Show full text]
  • Evolution of Cerebral and Cerebellar Expansion in Cetaceans
    Muller, A. S. , & Montgomery, S. H. (2019). Co‐evolution of cerebral and cerebellar expansion in cetaceans. Journal of Evolutionary Biology, 32(12), 1418-1431. https://doi.org/10.1111/jeb.13539 Publisher's PDF, also known as Version of record License (if available): CC BY Link to published version (if available): 10.1111/jeb.13539 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via Wiley at https://onlinelibrary.wiley.com/doi/full/10.1111/jeb.13539 . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Received: 8 May 2019 | Accepted: 27 August 2019 DOI: 10.1111/jeb.13539 RESEARCH PAPER Co‐evolution of cerebral and cerebellar expansion in cetaceans Amandine Sophie Muller1 | Stephen Hugh Montgomery1,2 1Department of Zoology, University of Cambridge, Cambridge, UK Abstract 2School of Biological Sciences, University of Cetaceans possess brains that rank among the largest to have ever evolved, either Bristol, Bristol, UK in terms of absolute mass or relative to body size. Cetaceans have evolved these Correspondence huge brains under relatively unique environmental conditions, making them a fasci‐ Stephen Hugh Montgomery, School of nating case study to investigate the constraints and selection pressures that shape Biological Sciences, University of Bristol, 24 Tyndall Avenue, Bristol, BS8 1TQ how brains evolve.
    [Show full text]
  • Genus/Species Skull Ht Lt Wt Stage Range Abacinonyx See Acinonyx Abathomodon See Speothos A
    Genus/Species Skull Ht Lt Wt Stage Range Abacinonyx see Acinonyx Abathomodon see Speothos A. fossilis see Icticyon pacivorus? Pleistocene Brazil Abelia U.Miocene Europe Absonodaphoenus see Pseudarctos L.Miocene USA A. bathygenus see Cynelos caroniavorus Acarictis L.Eocene W USA cf. A. ryani Wasatchian Colorado(US) A. ryani Wasatchian Wyoming, Colorado(US) Acinomyx see Acinonyx Acinonyx M.Pliocene-Recent Europe,Asia,Africa,N America A. aicha 2.3 m U.Pliocene Morocco A. brachygnathus Pliocene India A. expectata see Miracinonyx expectatus? Or Felis expectata? A. intermedius M.Pleistocene A. jubatus living Cheetah M.Pliocene-Recent Algeria,Europe,India,China A. pardinensis 91 cm 3 m 60 kg Astian-Biharian Italy,India,China,Germany,France A. sp. L.Pleistocene Tanzania,Ethiopia A. sp. Cf. Inexpectatus Blancan-Irvingtonian California(US) A. studeri see Miracinonyx studeri Blancan Texas(US) A. trumani see Miracinonyx trumani Rancholabrean Wyoming,Nevada(US) Acionyx possibly Acinonyx? A. cf. Crassidens Hadar(Ethiopia) Acrophoca 1.5 m U.Miocene-L.Pliocene Peru,Chile A. longirostris U.Miocene-L.Pliocene Peru A. sp. U.Miocene-L.Pliocene Chile Actiocyon M-U.Miocene W USA A. leardi Clarendonian California(US) A. sp. M.Miocene Oregon(US) Adcrocuta 82 cm 1.5 m U.Miocene Europe,Asia A. advena A. eximia 80 cm 1.5 m Vallesian-Turolian Europe(widespread),Asia(widespread) Adelphailurus U.Miocene-L.Pliocene W USA, Mexico,Europe A. kansensis Hemphillian Arizona,Kansas(US),Chihuahua(Mexico) Adelpharctos M.Oligocene Europe Adilophontes L.Miocene W USA A. brachykolos Arikareean Wyoming(US) Adracodon probably Adracon Eocene France A. quercyi probably Adracon quercyi Eocene France Adracon U.Eocene-L.Oligocene France A.
    [Show full text]
  • Proquest Dissertations
    Advances in the isotopic analysis of biogenic phosphates and their utility in ecophysiological studies of aquatic vertebrates Item Type text; Dissertation-Reproduction (electronic) Authors Roe, Lois Jane, 1963- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 02/10/2021 18:00:21 Link to Item http://hdl.handle.net/10150/282639 INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter fece, while others may be from any type of computer printer. The quality of this reproductioii is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely afreet reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper lefr-hand comer and continuing from left to right in equal sections with small overlaps. Each original is also photographed in one exposure and is included in reduced form at the back of the book.
    [Show full text]