Tetrapod-Like Pelvic Girdle in a Walking Cavefish Brooke E
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The Wingtips of the Pterosaurs: Anatomy, Aeronautical Function and Palaeogeography, Palaeoclimatology, Palaeoecology Xxx (2015) Xxx Xxx 3 Ecological Implications
Our reference: PALAEO 7445 P-authorquery-v11 AUTHOR QUERY FORM Journal: PALAEO Please e-mail your responses and any corrections to: Article Number: 7445 E-mail: [email protected] Dear Author, Please check your proof carefully and mark all corrections at the appropriate place in the proof (e.g., by using on-screen annotation in the PDF file) or compile them in a separate list. Note: if you opt to annotate the file with software other than Adobe Reader then please also highlight the appropriate place in the PDF file. To ensure fast publication of your paper please return your corrections within 48 hours. For correction or revision of any artwork, please consult http://www.elsevier.com/artworkinstructions. We were unable to process your file(s) fully electronically and have proceeded by Scanning (parts of) your Rekeying (parts of) your article Scanning the article artwork Any queries or remarks that have arisen during the processing of your manuscript are listed below and highlighted by flags in the proof. Click on the ‘Q’ link to go to the location in the proof. Location in article Query / Remark: click on the Q link to go Please insert your reply or correction at the corresponding line in the proof Q1 Your article is registered as a regular item and is being processed for inclusion in a regular issue of the journal. If this is NOT correct and your article belongs to a Special Issue/Collection please contact [email protected] immediately prior to returning your corrections. Q2 Please confirm that given names and surnames have been identified correctly. -
BONY FISHES 602 Bony Fishes
click for previous page BONY FISHES 602 Bony Fishes GENERAL REMARKS by K.E. Carpenter, Old Dominion University, Virginia, USA ony fishes constitute the bulk, by far, of both the diversity and total landings of marine organisms encoun- Btered in fisheries of the Western Central Atlantic.They are found in all macrofaunal marine and estuarine habitats and exhibit a lavish array of adaptations to these environments. This extreme diversity of form and taxa presents an exceptional challenge for identification. There are 30 orders and 269 families of bony fishes presented in this guide, representing all families known from the area. Each order and family presents a unique suite of taxonomic problems and relevant characters. The purpose of this preliminary section on technical terms and guide to orders and families is to serve as an introduction and initial identification guide to this taxonomic diversity. It should also serve as a general reference for those features most commonly used in identification of bony fishes throughout the remaining volumes. However, I cannot begin to introduce the many facets of fish biology relevant to understanding the diversity of fishes in a few pages. For this, the reader is directed to one of the several general texts on fish biology such as the ones by Bond (1996), Moyle and Cech (1996), and Helfman et al.(1997) listed below. A general introduction to the fisheries of bony fishes in this region is given in the introduction to these volumes. Taxonomic details relevant to a specific family are explained under each of the appropriate family sections. The classification of bony fishes continues to transform as our knowledge of their evolutionary relationships improves. -
Your Inner Fish
CHAPTER THREE HANDY GENES While my colleagues and I were digging up the first Tiktaalik in the Arctic in July 2004, Randy Dahn, a researcher in my laboratory, was sweating it out on the South Side of Chicago doing genetic experiments on the embryos of sharks and skates, cousins of stingrays. You’ve probably seen small black egg cases, known as mermaid’s purses, on the beach. Inside the purse once lay an egg with yolk, which developed into an embryonic skate or ray. Over the years, Randy has spent hundreds of hours experimenting with the embryos inside these egg cases, often working well past midnight. During the fateful summer of 2004, Randy was taking these cases and injecting a molecular version of vitamin A into the eggs. After that he would let the eggs develop for several months until they hatched. His experiments may seem to be a bizarre way to spend the better part of a year, let alone for a young scientist to launch a promising scientific career. Why sharks? Why a form of vitamin A? 61 To make sense of these experiments, we need to step back and look at what we hope they might explain. What we are really getting at in this chapter is the recipe, written in our DNA, that builds our bodies from a single egg. When sperm fertilizes an egg, that fertilized egg does not contain a tiny hand, for instance. The hand is built from the information contained in that single cell. This takes us to a very profound problem. -
Fish Locomotion: Recent Advances and New Directions
MA07CH22-Lauder ARI 6 November 2014 13:40 Fish Locomotion: Recent Advances and New Directions George V. Lauder Museum of Comparative Zoology, Harvard University, Cambridge, Massachusetts 02138; email: [email protected] Annu. Rev. Mar. Sci. 2015. 7:521–45 Keywords First published online as a Review in Advance on swimming, kinematics, hydrodynamics, robotics September 19, 2014 The Annual Review of Marine Science is online at Abstract marine.annualreviews.org Access provided by Harvard University on 01/07/15. For personal use only. Research on fish locomotion has expanded greatly in recent years as new This article’s doi: approaches have been brought to bear on a classical field of study. Detailed Annu. Rev. Marine. Sci. 2015.7:521-545. Downloaded from www.annualreviews.org 10.1146/annurev-marine-010814-015614 analyses of patterns of body and fin motion and the effects of these move- Copyright c 2015 by Annual Reviews. ments on water flow patterns have helped scientists understand the causes All rights reserved and effects of hydrodynamic patterns produced by swimming fish. Recent developments include the study of the center-of-mass motion of swimming fish and the use of volumetric imaging systems that allow three-dimensional instantaneous snapshots of wake flow patterns. The large numbers of swim- ming fish in the oceans and the vorticity present in fin and body wakes sup- port the hypothesis that fish contribute significantly to the mixing of ocean waters. New developments in fish robotics have enhanced understanding of the physical principles underlying aquatic propulsion and allowed intriguing biological features, such as the structure of shark skin, to be studied in detail. -
Amblyopsidae, Amblyopsis)
A peer-reviewed open-access journal ZooKeys 412:The 41–57 Hoosier(2014) cavefish, a new and endangered species( Amblyopsidae, Amblyopsis)... 41 doi: 10.3897/zookeys.412.7245 RESEARCH ARTICLE www.zookeys.org Launched to accelerate biodiversity research The Hoosier cavefish, a new and endangered species (Amblyopsidae, Amblyopsis) from the caves of southern Indiana Prosanta Chakrabarty1,†, Jacques A. Prejean1,‡, Matthew L. Niemiller1,2,§ 1 Museum of Natural Science, Ichthyology Section, 119 Foster Hall, Department of Biological Sciences, Loui- siana State University, Baton Rouge, Louisiana 70803, USA 2 University of Kentucky, Department of Biology, 200 Thomas Hunt Morgan Building, Lexington, KY 40506, USA † http://zoobank.org/0983DBAB-2F7E-477E-9138-63CED74455D3 ‡ http://zoobank.org/C71C7313-142D-4A34-AA9F-16F6757F15D1 § http://zoobank.org/8A0C3B1F-7D0A-4801-8299-D03B6C22AD34 Corresponding author: Prosanta Chakrabarty ([email protected]) Academic editor: C. Baldwin | Received 12 February 2014 | Accepted 13 May 2014 | Published 29 May 2014 http://zoobank.org/C618D622-395E-4FB7-B2DE-16C65053762F Citation: Chakrabarty P, Prejean JA, Niemiller ML (2014) The Hoosier cavefish, a new and endangered species (Amblyopsidae, Amblyopsis) from the caves of southern Indiana. ZooKeys 412: 41–57. doi: 10.3897/zookeys.412.7245 Abstract We describe a new species of amblyopsid cavefish (Percopsiformes: Amblyopsidae) in the genus Amblyopsis from subterranean habitats of southern Indiana, USA. The Hoosier Cavefish, Amblyopsis hoosieri sp. n., is distinguished from A. spelaea, its only congener, based on genetic, geographic, and morphological evi- dence. Several morphological features distinguish the new species, including a much plumper, Bibendum- like wrinkled body with rounded fins, and the absence of a premature stop codon in the gene rhodopsin. -
Median Fin Patterning in Bony Fish: Caspase-3 Role in Fin Fold Reabsorption
Eastern Illinois University The Keep Undergraduate Honors Theses Honors College 2017 Median Fin Patterning in Bony Fish: Caspase-3 Role in Fin Fold Reabsorption Kaitlyn Ann Hammock Follow this and additional works at: https://thekeep.eiu.edu/honors_theses Part of the Animal Sciences Commons Median fin patterning in bony fish: caspase-3 role in fin fold reabsorption BY Kaitlyn Ann Hammock UNDERGRADUATE THESIS Submitted in partial fulfillment of the requirement for obtaining UNDERGRADUATE DEPARTMENTAL HONORS Department of Biological Sciences along with the HonorsCollege at EASTERN ILLINOIS UNIVERSITY Charleston, Illinois 2017 I hereby recommend this thesis to be accepted as fulfilling the thesis requirement for obtaining Undergraduate Departmental Honors Date '.fHESIS ADVI 1 Date HONORSCOORDmATOR f C I//' ' / ·12 1' J Date, , DEPARTME TCHAIR Abstract Fish larvae develop a fin fold that will later be replaced by the median fins. I hypothesize that finfold reabsorption is part of the initial patterning of the median fins,and that caspase-3, an apoptosis marker, will be expressed in the fin fold during reabsorption. I analyzed time series of larvae in the first20-days post hatch (dph) to determine timing of median findevelopment in a basal bony fish- sturgeon- and in zebrafish, a derived bony fish. I am expecting the general activation pathway to be conserved in both fishesbut, the timing and location of cell death to differ.The dorsal fin foldis the firstto be reabsorbed in the sturgeon starting at 2 dph and rays formed at 6dph. This was closely followed by the anal finat 3 dph, rays at 9 dph and only later, at 6dph, does the caudal fin start forming and rays at 14 dph. -
Batoid Locomotion: Effects of Speed on Pectoral Fin Deformation in the Little Skate, Leucoraja Erinacea Valentina Di Santo1,*, Erin L
© 2017. Published by The Company of Biologists Ltd | Journal of Experimental Biology (2017) 220, 705-712 doi:10.1242/jeb.148767 RESEARCH ARTICLE Batoid locomotion: effects of speed on pectoral fin deformation in the little skate, Leucoraja erinacea Valentina Di Santo1,*, Erin L. Blevins1,2 and George V. Lauder1 ABSTRACT more efficient at higher speeds and for long-distance translocations Most batoids have a unique swimming mode in which thrust is (Di Santo and Kenaley, 2016). Although many batoid species are generated by either oscillating or undulating expanded pectoral fins accurately described by these two extreme modes, several species that form a disc. Only one previous study of the freshwater stingray has fall into a continuum between 0.5 and 1.0 wave, and are defined as quantified three-dimensional motions of the wing, and no comparable ‘semi-oscillators’ (Schaefer and Summers, 2005). data are available for marine batoid species that may differ The mechanics of propulsion in cartilaginous fishes have been considerably in their mode of locomotion. Here, we investigate three- investigated over the years through studies of morphology, dimensional kinematics of the pectoral wing of the little skate, kinematics, hydrodynamics, muscle activity and energetics Leucoraja erinacea, swimming steadily at two speeds [1 and (Daniel, 1988; Di Santo and Kenaley, 2016; Donley and 2 body lengths (BL) s−1]. We measured the motion of nine points in Shadwick, 2003; Fontanella et al., 2013; Lauder, 2015; Lauder three dimensions during wing oscillation and determined that there are and Di Santo, 2015; Porter et al., 2011; Rosenberger and Westneat, significant differences in movement amplitude among wing locations, 1999; Rosenblum et al., 2011). -
New Heterodontosaurid Remains from the Cañadón Asfalto Formation: Cursoriality and the Functional Importance of the Pes in Small Heterodontosaurids
Journal of Paleontology, 90(3), 2016, p. 555–577 Copyright © 2016, The Paleontological Society 0022-3360/16/0088-0906 doi: 10.1017/jpa.2016.24 New heterodontosaurid remains from the Cañadón Asfalto Formation: cursoriality and the functional importance of the pes in small heterodontosaurids Marcos G. Becerra,1 Diego Pol,1 Oliver W.M. Rauhut,2 and Ignacio A. Cerda3 1CONICET- Museo Palaeontológico Egidio Feruglio, Fontana 140, Trelew, Chubut 9100, Argentina 〈[email protected]〉; 〈[email protected]〉 2SNSB, Bayerische Staatssammlung für Paläontologie und Geologie and Department of Earth and Environmental Sciences, LMU München, Richard-Wagner-Str. 10, Munich 80333, Germany 〈[email protected]〉 3CONICET- Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, Museo Carlos Ameghino, Belgrano 1700, Paraje Pichi Ruca (predio Marabunta), Cipolletti, Río Negro, Argentina 〈[email protected]〉 Abstract.—New ornithischian remains reported here (MPEF-PV 3826) include two complete metatarsi with associated phalanges and caudal vertebrae, from the late Toarcian levels of the Cañadón Asfalto Formation. We conclude that these fossil remains represent a bipedal heterodontosaurid but lack diagnostic characters to identify them at the species level, although they probably represent remains of Manidens condorensis, known from the same locality. Histological features suggest a subadult ontogenetic stage for the individual. A cluster analysis based on pedal measurements identifies similarities of this specimen with heterodontosaurid taxa and the inclusion of the new material in a phylogenetic analysis with expanded character sampling on pedal remains confirms the described specimen as a heterodontosaurid. Finally, uncommon features of the digits (length proportions among nonungual phalanges of digit III, and claw features) are also quantitatively compared to several ornithischians, theropods, and birds, suggesting that this may represent a bipedal cursorial heterodontosaurid with gracile and grasping feet and long digits. -
Dinosauropodes
REPRINT FROM THE ORIGINAL BOOKLET by CHARLES N. STREVELL Deseret News Press, Salt Lake City, 1932 DINOSAUROPODES This article first appeared in the 1932 Christmas edition of the Deseret News. It has been made into a more convenient form for distribution to my friends. It is given with the hope that it may prove as interesting to you as my hobby has been to me. Your friend, DINOSAUROPODES CHARLES N. STREVELL Dinosaurs in Combat NE of the most interesting chapters of the earth’s past history is that of the time when there were laid down the Triassic strata of the famed Connecticut Valley, interesting in the profusion of its indicated life and fascinating in the baffling obscurity which shrouds most of its former denizens, the only records of whose existence are ‘Footprints on the sands of time.’ “It is not surprising therefore, that geologists should have turned to the collecting and deciphering of such records with zeal; nor is it to be marveled at that, after exhaustive researches of the late President Edward Hitchcock, workers should have been attracted to other more productive fields, leaving the foot prints aside as of little moment compared with the wonderful discoveries in the great unknown west.” The remarks quoted above are by Dr. Richard Swann Lull of Yale University in the introduction to his “Triassic Life of the Connecticut Valley” and cannot be improved on for the beginning of an article on footprints, whether found in Connecticut or Utah. The now famous tracks In the brown stone of the Connecticut Valley seem to have first been found by Pliny Moody in 1802 when he ploughed up a specimen on his farm, showing small imprints which later on were popularly called the tracks of Noah’s raven. -
Pterosaurs Flight in the Age of Dinosaurs Now Open 2 News at the Museum 3
Member Magazine Spring 2014 Vol. 39 No. 2 Pterosaurs Flight in the Age of Dinosaurs now open 2 News at the Museum 3 From the After an unseasonably cold, snowy winter, will work to identify items from your collection, More than 540,000 Marine Fossils the Museum is pleased to offer a number of while also displaying intriguing specimens from President springtime opportunities to awaken the inner the Museum’s own world-renowned collections. Added to Paleontology Collection naturalist in us all. This is the time of year when Of course, fieldwork and collecting have Ellen V. Futter Museum scientists prepare for the summer been hallmarks of the Museum’s work since Collections at a Glance field season as they continue to pursue new the institution’s founding. What has changed, discoveries in their fields. It’s also when Museum however, is technology. With a nod to the many Over nearly 150 years of acquisitions and Members and visitors can learn about their ways that technology is amplifying how scientific fieldwork, the Museum has amassed preeminent own discoveries during the annual Identification investigations are done, this year, ID Day visitors collections that form an irreplaceable record Day in Theodore Roosevelt Memorial Hall. can learn how scientists use digital fabrication of life on Earth. Today, 21st-century tools— Held this year on May 10, Identification Day to aid their research and have a chance to sophisticated imaging techniques, genomic invites visitors to bring their own backyard finds have their own objects scanned and printed on analyses, programs to analyze ever-growing and curios for identification by Museum scientists. -
Amphibious Fishes: Terrestrial Locomotion, Performance, Orientation, and Behaviors from an Applied Perspective by Noah R
AMPHIBIOUS FISHES: TERRESTRIAL LOCOMOTION, PERFORMANCE, ORIENTATION, AND BEHAVIORS FROM AN APPLIED PERSPECTIVE BY NOAH R. BRESSMAN A Dissertation Submitted to the Graduate Faculty of WAKE FOREST UNIVESITY GRADUATE SCHOOL OF ARTS AND SCIENCES in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY Biology May 2020 Winston-Salem, North Carolina Approved By: Miriam A. Ashley-Ross, Ph.D., Advisor Alice C. Gibb, Ph.D., Chair T. Michael Anderson, Ph.D. Bill Conner, Ph.D. Glen Mars, Ph.D. ACKNOWLEDGEMENTS I would like to thank my adviser Dr. Miriam Ashley-Ross for mentoring me and providing all of her support throughout my doctoral program. I would also like to thank the rest of my committee – Drs. T. Michael Anderson, Glen Marrs, Alice Gibb, and Bill Conner – for teaching me new skills and supporting me along the way. My dissertation research would not have been possible without the help of my collaborators, Drs. Jeff Hill, Joe Love, and Ben Perlman. Additionally, I am very appreciative of the many undergraduate and high school students who helped me collect and analyze data – Mark Simms, Tyler King, Caroline Horne, John Crumpler, John S. Gallen, Emily Lovern, Samir Lalani, Rob Sheppard, Cal Morrison, Imoh Udoh, Harrison McCamy, Laura Miron, and Amaya Pitts. I would like to thank my fellow graduate student labmates – Francesca Giammona, Dan O’Donnell, MC Regan, and Christine Vega – for their support and helping me flesh out ideas. I am appreciative of Dr. Ryan Earley, Dr. Bruce Turner, Allison Durland Donahou, Mary Groves, Tim Groves, Maryland Department of Natural Resources, UF Tropical Aquaculture Lab for providing fish, animal care, and lab space throughout my doctoral research. -
Tetrapod Biostratigraphy and Biochronology of the Triassic–Jurassic Transition on the Southern Colorado Plateau, USA
Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 242–256 www.elsevier.com/locate/palaeo Tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau, USA Spencer G. Lucas a,⁎, Lawrence H. Tanner b a New Mexico Museum of Natural History, 1801 Mountain Rd. N.W., Albuquerque, NM 87104-1375, USA b Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY 13214, USA Received 15 March 2006; accepted 20 June 2006 Abstract Nonmarine fluvial, eolian and lacustrine strata of the Chinle and Glen Canyon groups on the southern Colorado Plateau preserve tetrapod body fossils and footprints that are one of the world's most extensive tetrapod fossil records across the Triassic– Jurassic boundary. We organize these tetrapod fossils into five, time-successive biostratigraphic assemblages (in ascending order, Owl Rock, Rock Point, Dinosaur Canyon, Whitmore Point and Kayenta) that we assign to the (ascending order) Revueltian, Apachean, Wassonian and Dawan land-vertebrate faunachrons (LVF). In doing so, we redefine the Wassonian and the Dawan LVFs. The Apachean–Wassonian boundary approximates the Triassic–Jurassic boundary. This tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau confirms that crurotarsan extinction closely corresponds to the end of the Triassic, and that a dramatic increase in dinosaur diversity, abundance and body size preceded the end of the Triassic. © 2006 Elsevier B.V. All rights reserved. Keywords: Triassic–Jurassic boundary; Colorado Plateau; Chinle Group; Glen Canyon Group; Tetrapod 1. Introduction 190 Ma. On the southern Colorado Plateau, the Triassic– Jurassic transition was a time of significant changes in the The Four Corners (common boundary of Utah, composition of the terrestrial vertebrate (tetrapod) fauna.