Chapter 34 Vertebrates
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Timeline of Natural History
Timeline of natural history This timeline of natural history summarizes significant geological and Life timeline Ice Ages biological events from the formation of the 0 — Primates Quater nary Flowers ←Earliest apes Earth to the arrival of modern humans. P Birds h Mammals – Plants Dinosaurs Times are listed in millions of years, or Karo o a n ← Andean Tetrapoda megaanni (Ma). -50 0 — e Arthropods Molluscs r ←Cambrian explosion o ← Cryoge nian Ediacara biota – z ←Earliest animals o ←Earliest plants i Multicellular -1000 — c Contents life ←Sexual reproduction Dating of the Geologic record – P r The earliest Solar System -1500 — o t Precambrian Supereon – e r Eukaryotes Hadean Eon o -2000 — z o Archean Eon i Huron ian – c Eoarchean Era ←Oxygen crisis Paleoarchean Era -2500 — ←Atmospheric oxygen Mesoarchean Era – Photosynthesis Neoarchean Era Pong ola Proterozoic Eon -3000 — A r Paleoproterozoic Era c – h Siderian Period e a Rhyacian Period -3500 — n ←Earliest oxygen Orosirian Period Single-celled – life Statherian Period -4000 — ←Earliest life Mesoproterozoic Era H Calymmian Period a water – d e Ectasian Period a ←Earliest water Stenian Period -4500 — n ←Earth (−4540) (million years ago) Clickable Neoproterozoic Era ( Tonian Period Cryogenian Period Ediacaran Period Phanerozoic Eon Paleozoic Era Cambrian Period Ordovician Period Silurian Period Devonian Period Carboniferous Period Permian Period Mesozoic Era Triassic Period Jurassic Period Cretaceous Period Cenozoic Era Paleogene Period Neogene Period Quaternary Period Etymology of period names References See also External links Dating of the Geologic record The Geologic record is the strata (layers) of rock in the planet's crust and the science of geology is much concerned with the age and origin of all rocks to determine the history and formation of Earth and to understand the forces that have acted upon it. -
Brains of Primitive Chordates 439
Brains of Primitive Chordates 439 Brains of Primitive Chordates J C Glover, University of Oslo, Oslo, Norway although providing a more direct link to the evolu- B Fritzsch, Creighton University, Omaha, NE, USA tionary clock, is nevertheless hampered by differing ã 2009 Elsevier Ltd. All rights reserved. rates of evolution, both among species and among genes, and a still largely deficient fossil record. Until recently, it was widely accepted, both on morpholog- ical and molecular grounds, that cephalochordates Introduction and craniates were sister taxons, with urochordates Craniates (which include the sister taxa vertebrata being more distant craniate relatives and with hemi- and hyperotreti, or hagfishes) represent the most chordates being more closely related to echinoderms complex organisms in the chordate phylum, particu- (Figure 1(a)). The molecular data only weakly sup- larly with respect to the organization and function of ported a coherent chordate taxon, however, indicat- the central nervous system. How brain complexity ing that apparent morphological similarities among has arisen during evolution is one of the most chordates are imposed on deep divisions among the fascinating questions facing modern science, and it extant deuterostome taxa. Recent analysis of a sub- speaks directly to the more philosophical question stantially larger number of genes has reversed the of what makes us human. Considerable interest has positions of cephalochordates and urochordates, pro- therefore been directed toward understanding the moting the latter to the most closely related craniate genetic and developmental underpinnings of nervous relatives (Figure 1(b)). system organization in our more ‘primitive’ chordate relatives, in the search for the origins of the vertebrate Comparative Appearance of Brains, brain in a common chordate ancestor. -
(= Amphioxus) Branchiostoma Floridae
MARINE ECOLOGY PROGRESS SERIES Vol. 130: 71-84,1996 Published January 11 Mar Ecol Prog Ser Larval settlement, post-settlement growth and secondary production of the Florida lancelet (= amphioxus) Branchiostoma floridae M. D. Stokes* Marine Biology Research Division, Scripps Institution of Oceanography, La Jolla, California 92093-0202, USA ABSTRACT A population of Branch~ostomaflondae in Tampa Bay, Flonda, USA was sieved from the substratum frequently (often daily) from June 1992 through September 1994 Body lengths were mea- sured for 54264 luvenlle and adult lancelets The breedlng season lasted each year from early May through early September and newly metamorphosed lancelets settled as luveniles from late May through mid October, dunng this period of the year dlstinct settlements occurred approxmately every 1 to 3 wk Post-settlement growth was followed as changes in modal length on size-frequency histo- grams Changes in cohort growth over this peliod were compared to several different simple and seasonally oscillating growth models The von Bertalanffy functlon in smple and oscillating forms provided the best estmates of lancelet growth The lancelets grew in summer (almost 0 5 mm d-' in recently settled luveniles), but growth slowed and almost ceased durlng wlnter B flondae can llve at least 2 yr and can reach a maxlmum length of 58 mm The maximal secondary productlon was 61 53 g m-' yrrl (ash-free dry welght) and the productlon to biomass ratio was 11 64 Population den- sities at the study site ranged from about 100 to 1200 lancelets m ' KEY WORDS: Lancelet . Amphioxus . Branchiostorna flondae . Growth . Production . Breeding season . -
Phylum Chordata
Phylum Chordata 48,000 species very diverse phylum but still more unity in major characteristics than in most other phyla most advanced phylum of animal kingdom one to which we belong along with fish, amphibians reptiles, birds and other mammals some of the largest or most massive animals true coelom 4 major identifying characteristics: 1. Notochord flexible rodlike structure enclosed by a fibrous sheath extends the length of the body in larva and/or adult provides basic support and serves as main axis for muscle attachments to permit “fishlike” undulatory movements first part of skeleton to form in embryo in primitive chordates the notochord persists through life Animals: Chordates & Introduction to Vertebrates; Ziser Lecture Notes, 2006 1 in most chordates the notochord is replaced by a vertebral column of bone remnants of the notochord remain as “intervertebral discs” 2. Dorsal tubular nerve cord in most invert groups; nerve cord is ventral & paired in chordates the nerve cord is a single dorsal hollow nerve cord front end usually enlarged to form brain 3. Pharyngeal (gill) slits slit-like opening sleading from throat to outside first evolved as a filter feeding apparatus still used by some to filter water for food in others as gills in some groups they are only found in embryo and lost as adults 4. endostyle or thyroid gland specific kind of tissue found only in chordates was originally part of the feeding apparatus endostyle secretes mucus and traps food inside the pharyngeal cavity eg. lamprey larva in most chordates the same tissue has become an endocrine Animals: Chordates & Introduction to Vertebrates; Ziser Lecture Notes, 2006 2 gland in the neck region that helps control metabolism 5. -
Abstract Introduction
Marine and Freshwater Miscellanea III KEY TRAITS OF AMPHIOXUS SPECIES (CEPHALOCHORDATA) AND THE GOLT1 Daniel Pauly and Elaine Chu Sea Around Us, Institute for the Oceans and Fisheries University of British Columbia, Vancouver, B.C, Canada Email: [email protected] Abstract Major biological traits of amphioxus species (Cephalochordata) are presented with emphasis on the size reached by their 32 valid species in the genera Asymmetron (2 spp.), Branchiostoma (25 spp.), and Epigonichthys (5 spp.) and on related features, i.e., growth parameters and size at first maturity. Overall, these traits combined with features of their respiration, suggest that the cephalochordates conform to the Gill Oxygen Limitation Theory (GOLT), which relates the growth performance of water-breathing ectotherms to the surface area of their respiratory organ(s). Introduction The small fish-like animals know as ‘lancelet‘ or ‘amphioxius’ belong the subphylum Cephalochordata, which is either a sister group, or related to the ancestor of the vertebrate animals (see Garcia-Fernàndez and Benito-Gutierrez 2008). The cephalochordates consist of 3 families (the Asymmetronidae, Epigonichthyidae and Branchiostomidae), with one genus each, Asymmetron (2 spp.), Branchiostoma (24 spp.) and Epigonichthys (6 spp.), as detailed in Table 1 and SeaLifeBase (www.sealifebase.org). This contribution is to assemble some of the basic biological traits of lancelets (Figure 1), notably the maximum size each of their 34 species can reach, which is easily their most important attribute, though it is often ignored (Haldane 1926). Finally, reported lengths at first maturity of cephalochordates were related to the corresponding, population-specific maximum length, to test whether these animals mature as predicted by the Gill- Oxygen Limitation Theory (GOLT; see Pauly 2021a, 2021b). -
Chordates (Phylum Chordata)
A short story Leathem Mehaffey, III, Fall 201993 The First Chordates (Phylum Chordata) • Chordates (our phylum) first appeared in the Cambrian, 525MYA. 94 Invertebrates, Chordates and Vertebrates • Invertebrates are all animals not chordates • Generally invertebrates, if they have hearts, have dorsal hearts; if they have a nervous system it is usually ventral. • All vertebrates are chordates, but not all chordates are vertebrates. • Chordates: • Dorsal notochord • Dorsal nerve chord • Ventral heart • Post-anal tail • Vertebrates: Amphioxus: archetypal chordate • Dorsal spinal column (articulated) and skeleton 95 Origin of the Chordates 96 Haikouichthys Myllokunmingia Note the rounded extension to Possibly the oldest the head bearing sensory vertebrate: showed gill organs bars and primitive vertebral elements Early and primitive agnathan vertebrates of the Early Cambrian (530MYA) Pikaia Note: these organisms were less Primitive chordate, than an inch long. similar to Amphioxus 97 The Cambrian/Ordovician Extinction • Somewhere around 488 million years ago something happened to cause a change in the fauna of the earth, heralding the beginning of the Ordovician Period. • Rather than one catastrophe, the late-Cambrian extinction seems to be a series of smaller extinction events. • Historically the change in fauna (mostly trilobites as the index species) was thought to be due to excessive warmth and low oxygen. • But some current findings point to an oxygen spike due perhaps to continental drift into the tropics, driving rapid speciation and consequent replacement of old with new organisms. 98 Welcome to the Ordovician YOU ARE HERE 99 The Ordovician Sea, 488 million years 100 ago The Ordovician Period lasted almost 45 million years, from 489 to 444 MYA. -
Sponges Cnidarians Chordates Brachiopods Annelids Molluscs Ediacaran Arthropods 635 Cambrian PALEOZOIC PROTEROZOIC 605 Time (Mil
© 2014 Pearson Education, Inc. 1 Sponges Cnidarians Echinoderms Chordates Brachiopods Annelids Molluscs Arthropods PROTEROZOIC PALEOZOIC Ediacaran Cambrian 635 605 575 545 515 485 0 Time (millions of years age) © 2014 Pearson Education, Inc. 2 Food particles in mucus Choanocyte Collar Flagellum Choanocyte Phagocytosis of Amoebocyte food particles Pores Spicules Water flow Amoebocytes Azure vase sponge (Callyspongia plicifera) © 2014 Pearson Education, Inc. 3 (a) Hydrozoa (b) Scyphozoa (c) Anthozoa © 2014 Pearson Education, Inc. 4 15 µm 75 µm (a) Valeria (800 mya): (b) Spiny acritarch roughly spherical, no (575 mya): about five structural defenses, times larger than soft-bodied Valeria and covered in hard spines © 2014 Pearson Education, Inc. 5 (a) Radial symmetry (b) Bilateral symmetry © 2014 Pearson Education, Inc. 6 Body cavity Body covering (from ectoderm) Tissue layer lining body cavity and suspending Digestive tract internal organs (from endoderm) (from mesoderm) © 2014 Pearson Education, Inc. 7 Porifera Metazoa Ctenophora ANCESTRAL Eumetazoa PROTIST Cnidaria Deuterostomia Hemichordata 770 million Echinodermata years ago 680 million Chordata years ago Lophotrochozoa Lophotrochozoa Platyhelminthes Bilateria Rotifera Ectoprocta Brachiopoda 670 million years ago Mollusca Ecdysozoa Annelida Nematoda Arthropoda © 2014 Pearson Education, Inc. 8 © 2014 Pearson Education, Inc. 9 Notochord Dorsal, hollow nerve cord Muscle segments Mouth Anus Post-anal tail Pharyngeal slits or clefts © 2014 Pearson Education, Inc. 10 (a) Lancelet (b) Tunicate -
New Records of the Lancelet Branchiostoma Lanceolatum in Scottish Waters
The Glasgow Naturalist (online 2019) Volume 27, Part 1 New records of the lancelet Branchiostoma lanceolatum in Scottish waters M. O’Reilly1, S. Nowacki1, M. Baptie1, E. Gerrie1 & M. MacKenzie2 1Scottish Environment Protection Agency, Angus Smith Building, 6 Parklands Avenue, Eurocentral, Holytown, North Lanarkshire ML1 4WQ 2Scottish Environment Protection Agency, Graesser House, Fodderty Way, Dingwall IV15 9XB 1E-mail: [email protected] ABSTRACT New records of the lancelet Branchiostoma lanceolatum from Scottish waters are presented. Most of the records originate from sublittoral monitoring around fish farms from Orkney, Shetland, the Western Isles, the Isles of Skye and Mull, but also from a distillery discharge in the Firth of Clyde and a plankton survey in the Sea of the Hebrides. Lancelets were recovered in sediment grab samples from 6 - 60 m depth. Some recent accounts of intertidal lancelets are also cited. The lancelets appear to prefer coarser sediments and in the fish farm surveys were found predominantly at reference sites, away from the immediate influence of farm deposition. INTRODUCTION The lancelet Branchiostoma lanceolatum (Pallas, 1774) is an obscure, vaguely fish-like creature, up to 8 cm long, which lives buried in sand or coarse sediments in British seas. Its body is laterally compressed, pinkish white in colour, and pointed at both ends with a lance- like tail fin (Fig. 1). There are no paired fins, nor eyes, nor even a well-defined head, and it has only a small mouth surrounded by cirri, used to filter organic matter from the surrounding water. It has a dorsal notochord and segmented muscle blocks allowing it to swim in a sinusoidal fish-like manner, but no backbone, and it is therefore classified as an invertebrate (Barnes, 2015). -
Biology of Chordates Video Guide
Branches on the Tree of Life DVD – CHORDATES Written and photographed by David Denning and Bruce Russell ©2005, BioMEDIA ASSOCIATES (THUMBNAIL IMAGES IN THIS GUIDE ARE FROM THE DVD PROGRAM) .. .. To many students, the phylum Chordata doesn’t seem to make much sense. It contains such apparently disparate animals as tunicates (sea squirts), lancelets, fish and humans. This program explores the evolution, structure and classification of chordates with the main goal to clarify the unity of Phylum Chordata. All chordates possess four characteristics that define the phylum, although in most species, these characteristics can only be seen during a relatively small portion of the life cycle (and this is often an embryonic or larval stage, when the animal is difficult to observe). These defining characteristics are: the notochord (dorsal stiffening rod), a hollow dorsal nerve cord; pharyngeal gills; and a post anal tail that includes the notochord and nerve cord. Subphylum Urochordata The most primitive chordates are the tunicates or sea squirts, and closely related groups such as the larvaceans (Appendicularians). In tunicates, the chordate characteristics can be observed only by examining the entire life cycle. The adult feeds using a ‘pharyngeal basket’, a type of pharyngeal gill formed into a mesh-like basket. Cilia on the gill draw water into the mouth, through the basket mesh and out the excurrent siphon. Tunicates have an unusual heart which pumps by ‘wringing out’. It also reverses direction periodically. Tunicates are usually hermaphroditic, often casting eggs and sperm directly into the sea. After fertilization, the zygote develops into a ‘tadpole larva’. This swimming larva shows the remaining three chordate characters - notochord, dorsal nerve cord and post-anal tail. -
Northern Bog Lemming (Synaptomys Borealis) UNDER the U.S
PETITION TO LIST THE Northern Bog Lemming (Synaptomys borealis) UNDER THE U.S. ENDANGERED SPECIES ACT Northern bog lemming. Photo © Dean Pearson (used with permission). Petition Submitted to the U.S. Secretary of Interior Acting through the U.S. Fish and Wildlife Service Petitioner: WildEarth Guardians 1536 Wynkoop Street, Suite 310 Denver, Colorado 80202 303.573.4898 Address correspondence to: Taylor Jones [email protected] Petition prepared by: Taylor Jones WildEarth Guardians and Laura L. Melton University of New Mexico, School of Law September 29, 2014 INTRODUCTION WildEarth Guardians (Guardians) respectfully requests that the Secretary of the Interior, acting through the U.S. Fish and Wildlife Service (Service) list the northern bog lemming (Synaptomys borealis) as “threatened” or “endangered” under the U.S. Endangered Species Act (ESA) (16 U.S.C. §§ 1531-1544). WildEarth Guardians also requests that the Service designate critical habitat for this species. The northern bog lemming is found only in the northern hemisphere in subarctic climates along the northern tree line south into Washington, Idaho, Montana, Minnesota, and New England. Though they typically inhabit sphagnum bogs, they can occasionally be found in other habitats including alpine tundra, wet subalpine meadows, and mossy forests. The glacial relict habitats of northern bog lemmings are isolated and patchy in nature, as are lemming populations, making the risk of extinction very high. No populations of northern bog lemmings are known to exist in captivity and the small mammals are difficult to trap and rarely seen in the wild. Population density surveys have not been successful due to the inability of surveyors to find and trap the lemmings for counting. -
A Paleontological Perspective of Vertebrate Origin
http://www.paper.edu.cn Chinese Science Bulletin 2003 Vol. 48 No. 8 725-735 Cover: The earliest-known and most primitive vertebrates on the A paleontological perspective Earth---Myllokunmingia fengjiaoa , (upper) Zhongjianichthys rostratus of vertebrate origin ( middle ), Haikouichthys ercaicunensis (lower left and lower right). They were SHU Degan Early Life Institute & Department of Geology, Northwest products of the early Cambrian Explosion, University, Xi’an, 710069, China; School of Earth excavated from the famous Chengjiang Sciences and Resources, China University of Geosciences, Beijing, 100083, China Lagersttat, which was formed in the (e-mail:[email protected]) eastern Yunnan about 530 millions of years ago. These ancestral vertebrates not only Abstract The Early Cambrian Haikouichthys and Haikouella have been claimed to be related to contribute in an important developed primitive separate vertebral way to our understanding of vertebrate origin, but there have elements, but also possessed principal been heated debates about how exactly they are to be interpreted. New discoveries of numerous specimens of sensory organs, including a pair of large Haikouichthys not only confirm the identity of previously lateral eyes, nostril with nasal sacs, then described structures such as the dorsal and the ventral fins, and chevron-shaped myomeres, but also reveal many new had led to the transition from acraniates to important characteristics, including sensory organs of the head craniates (true vertebrates). The (e.g. large eyes), and a prominent notochord with differentiated vertebral elements. This “first fish” appears, discoveries of these “naked” agnathans however, to retain primitive reproductive features of have pushed the earliest record of acraniates, suggesting that it is a stem-group craniates. -
The Herpetofauna of the Cubango, Cuito, and Lower Cuando River Catchments of South-Eastern Angola
Official journal website: Amphibian & Reptile Conservation amphibian-reptile-conservation.org 10(2) [Special Section]: 6–36 (e126). The herpetofauna of the Cubango, Cuito, and lower Cuando river catchments of south-eastern Angola 1,2,*Werner Conradie, 2Roger Bills, and 1,3William R. Branch 1Port Elizabeth Museum (Bayworld), P.O. Box 13147, Humewood 6013, SOUTH AFRICA 2South African Institute for Aquatic Bio- diversity, P/Bag 1015, Grahamstown 6140, SOUTH AFRICA 3Research Associate, Department of Zoology, P O Box 77000, Nelson Mandela Metropolitan University, Port Elizabeth 6031, SOUTH AFRICA Abstract.—Angola’s herpetofauna has been neglected for many years, but recent surveys have revealed unknown diversity and a consequent increase in the number of species recorded for the country. Most historical Angola surveys focused on the north-eastern and south-western parts of the country, with the south-east, now comprising the Kuando-Kubango Province, neglected. To address this gap a series of rapid biodiversity surveys of the upper Cubango-Okavango basin were conducted from 2012‒2015. This report presents the results of these surveys, together with a herpetological checklist of current and historical records for the Angolan drainage of the Cubango, Cuito, and Cuando Rivers. In summary 111 species are known from the region, comprising 38 snakes, 32 lizards, five chelonians, a single crocodile and 34 amphibians. The Cubango is the most western catchment and has the greatest herpetofaunal diversity (54 species). This is a reflection of both its easier access, and thus greatest number of historical records, and also the greater habitat and topographical diversity associated with the rocky headwaters.