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Educators' Resource Guide
EDUCATORS' RESOURCE GUIDE Produced and published by 3D Entertainment Distribution Written by Dr. Elisabeth Mantello In collaboration with Jean-Michel Cousteau’s Ocean Futures Society TABLE OF CONTENTS TO EDUCATORS .................................................................................................p 3 III. PART 3. ACTIVITIES FOR STUDENTS INTRODUCTION .................................................................................................p 4 ACTIVITY 1. DO YOU Know ME? ................................................................. p 20 PLANKton, SOURCE OF LIFE .....................................................................p 4 ACTIVITY 2. discoVER THE ANIMALS OF "SECRET OCEAN" ......... p 21-24 ACTIVITY 3. A. SECRET OCEAN word FIND ......................................... p 25 PART 1. SCENES FROM "SECRET OCEAN" ACTIVITY 3. B. ADD color to THE octoPUS! .................................... p 25 1. CHristmas TREE WORMS .........................................................................p 5 ACTIVITY 4. A. WHERE IS MY MOUTH? ..................................................... p 26 2. GIANT BasKET Star ..................................................................................p 6 ACTIVITY 4. B. WHat DO I USE to eat? .................................................. p 26 3. SEA ANEMONE AND Clown FISH ......................................................p 6 ACTIVITY 5. A. WHO eats WHat? .............................................................. p 27 4. GIANT CLAM AND ZOOXANTHELLAE ................................................p -
Petition to List the Black Teatfish, Holothuria Nobilis, Under the U.S. Endangered Species Act
Before the Secretary of Commerce Petition to List the Black Teatfish, Holothuria nobilis, under the U.S. Endangered Species Act Photo Credit: © Philippe Bourjon (with permission) Center for Biological Diversity 14 May 2020 Notice of Petition Wilbur Ross, Secretary of Commerce U.S. Department of Commerce 1401 Constitution Ave. NW Washington, D.C. 20230 Email: [email protected], [email protected] Dr. Neil Jacobs, Acting Under Secretary of Commerce for Oceans and Atmosphere U.S. Department of Commerce 1401 Constitution Ave. NW Washington, D.C. 20230 Email: [email protected] Petitioner: Kristin Carden, Oceans Program Scientist Sarah Uhlemann, Senior Att’y & Int’l Program Director Center for Biological Diversity Center for Biological Diversity 1212 Broadway #800 2400 NW 80th Street, #146 Oakland, CA 94612 Seattle,WA98117 Phone: (510) 844‐7100 x327 Phone: (206) 324‐2344 Email: [email protected] Email: [email protected] The Center for Biological Diversity (Center, Petitioner) submits to the Secretary of Commerce and the National Oceanographic and Atmospheric Administration (NOAA) through the National Marine Fisheries Service (NMFS) a petition to list the black teatfish, Holothuria nobilis, as threatened or endangered under the U.S. Endangered Species Act (ESA), 16 U.S.C. § 1531 et seq. Alternatively, the Service should list the black teatfish as threatened or endangered throughout a significant portion of its range. This species is found exclusively in foreign waters, thus 30‐days’ notice to affected U.S. states and/or territories was not required. The Center is a non‐profit, public interest environmental organization dedicated to the protection of native species and their habitats. -
Echinoidea Clypeasteroidea
Biodiversity Journal, 2014, 5 (2): 291–358 Analysis of some astriclypeids (Echinoidea Clypeast- eroida) Paolo Stara1* & Luigi Sanciu2 1Centro Studi di Storia Naturale del Mediterraneo - Museo di Storia Naturale Aquilegia, Via Italia 63, Pirri-Cagliari and Geomuseo Monte Arci, Masullas, Oristano, Sardinia, Italy; e-mail: [email protected] *Corresponding author The systematic position of some astriclypeid species assigned through times to the genera Amphiope L. Agassiz, 1840 and Echinodiscus Leske, 1778 is reviewed based on the plating ABSTRACT pattern characteristics of these two genera universally accepted, and on the results of new studies. A partial re-arrangement of the family Astriclypeidae Stefanini, 1912 is herein pro- posed, with the institution of Sculpsitechinus n. g. and Paraamphiope n. g., both of them char- acterized by a peculiar plating-structure of the interambulacrum 5 and of the ambulacra I and V. Some species previously attributed to Amphiope and Echinodiscus are transferred into these two new genera. Two new species of Astriclypeidae are established: Echinodiscus andamanensis n. sp. and Paraamphiope raimondii n. sp. Neotypes are proposed for Echin- odiscus tenuissimus L. Agassiz, 1840 and E. auritus Leske, 1778, since these species were still poorly defined, due to the loss of the holotypes and, for E. auritus, also to the unclear geographical/stratigraphical information about the type-locality. A number of additional nom- inal fossil and extant species of "Echinodiscus" needs revision based on the same method. KEY WORDS Astriclypeidae; Amphiope; Paraamphiope; Echinodiscus; Sculpsitechinus; Oligo-Miocene. Received 28.02.2014; accepted 14.03.2014; printed 30.06.2014 Paolo Stara (ed.). Studies on some astriclypeids (Echinoidea Clypeasteroida), pp. -
Illinois Fossils Doc 2005
State of Illinois Illinois Department of Natural Resources Illinois Fossils Illinois Department of Natural Resources he Illinois Fossils activity book from the Illinois Department of Natural Resources’ (IDNR) Division of Education is designed to supplement your curriculum in a vari- ety of ways. The information and activities contained in this publication are targeted toT grades four through eight. The Illinois Fossils resources trunk and lessons can help you T teach about fossils, too. You will find these and other supplemental items through the Web page at https://www2.illinois.gov/dnr/education/Pages/default.aspx. Contact the IDNR Division of Education at 217-524-4126 or [email protected] for more information. Collinson, Charles. 2002. Guide for beginning fossil hunters. Illinois State Geological Survey, Champaign, Illinois. Geoscience Education Series 15. 49 pp. Frankie, Wayne. 2004. Guide to rocks and minerals of Illinois. Illinois State Geological Survey, Champaign, Illinois. Geoscience Education Series 16. 71 pp. Killey, Myrna M. 1998. Illinois’ ice age legacy. Illinois State Geological Survey, Champaign, Illinois. Geoscience Education Series 14. 67 pp. Much of the material in this book is adapted from the Illinois State Geological Survey’s (ISGS) Guide for Beginning Fossil Hunters. Special thanks are given to Charles Collinson, former ISGS geologist, for the use of his fossil illustrations. Equal opportunity to participate in programs of the Illinois Department of Natural Resources (IDNR) and those funded by the U.S. Fish and Wildlife Service and other agencies is available to all individuals regardless of race, sex, national origin, disability, age, reli-gion or other non-merit factors. -
Energetics of Larval Swimming and Metamorphosis in Four Species of Bugula (Bryozoa)
Energetics of Larval Swimming and Metamorphosis in Four Species of Bugula (Bryozoa) DEAN E. WENDT* Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, Massachusetts 02138 Abstract. The amount of energy available to larvae dur Introduction ing swimming, location of a suitable recruitment site, and metamorphosis influences the length of time they can spend The larval life of many marine invertebrates is character in the plankton. Energetic parameters such as swimming ized by three distinct phases. The first, a swimming phase, speed, oxygen consumption during swimming and meta is both a means of dispersal and, in planktotrophic larvae, a morphosis, and elemental carbon and nitrogen content were time to sequester the energy needed for larval development measured for larvae of four species of bryozoans, Bugula and metamorphosis. The two subsequent phases—settle neritina, B. simplex, B. stolonifera, and B. turrita. The ment and metamorphosis—can be temporally distinct, as in larvae of these species are aplanktotrophic with a short some echinoderm larvae (e.g., Strathmann, 1974), or tightly free-swimming phase ranging from less than one hour to a coupled, as in bryozoan larvae (e.g., Ryland, 1974). That the maximum of about 36 hours. There is about a fivefold duration of the larval swimming phase can have detrimental difference in larval volume among the four species, which effects on the latter two phases of the life cycle has been scales linearly with elemental carbon content and, presum demonstrated for several species in at least three phyla, ably, with the amount of endogenous reserves available for including bryozoans (Nielson, 1981; Woollacott et al., 1989; Orellana and Cancino, 1991; Hunter and Fusetani, swimming and metamorphosis. -
"Lophophorates" Brachiopoda Echinodermata Asterozoa
Deuterostomes Bryozoa Phoronida "lophophorates" Brachiopoda Echinodermata Asterozoa Stelleroidea Asteroidea Ophiuroidea Echinozoa Holothuroidea Echinoidea Crinozoa Crinoidea Chaetognatha (arrow worms) Hemichordata (acorn worms) Chordata Urochordata (sea squirt) Cephalochordata (amphioxoius) Vertebrata PHYLUM CHAETOGNATHA (70 spp) Arrow worms Fossils from the Cambrium Carnivorous - link between small phytoplankton and larger zooplankton (1-15 cm long) Pharyngeal gill pores No notochord Peculiar origin for mesoderm (not strictly enterocoelous) Uncertain relationship with echinoderms PHYLUM HEMICHORDATA (120 spp) Acorn worms Pharyngeal gill pores No notochord (Stomochord cartilaginous and once thought homologous w/notochord) Tornaria larvae very similar to asteroidea Bipinnaria larvae CLASS ENTEROPNEUSTA (acorn worms) Marine, bottom dwellers CLASS PTEROBRANCHIA Colonial, sessile, filter feeding, tube dwellers Small (1-2 mm), "U" shaped gut, no gill slits PHYLUM CHORDATA Body segmented Axial notochord Dorsal hollow nerve chord Paired gill slits Post anal tail SUBPHYLUM UROCHORDATA Marine, sessile Body covered in a cellulose tunic ("Tunicates") Filter feeder (» 200 L/day) - perforated pharnx adapted for filtering & repiration Pharyngeal basket contractable - squirts water when exposed at low tide Hermaphrodites Tadpole larvae w/chordate characteristics (neoteny) CLASS ASCIDIACEA (sea squirt/tunicate - sessile) No excretory system Open circulatory system (can reverse blood flow) Endostyle - (homologous to thyroid of vertebrates) ciliated groove -
Evidence for Selection on a Chordate Histocompatibility Locus
ORIGINAL ARTICLE doi:10.1111/j.1558-5646.2012.01787.x EVIDENCE FOR SELECTION ON A CHORDATE HISTOCOMPATIBILITY LOCUS Marie L. Nydam,1,2,3 Alyssa A. Taylor,3 and Anthony W. De Tomaso3 1Division of Science and Mathematics, Centre College, Danville, Kentucky 40422 2E-mail: [email protected] 3Department of Molecular, Cellular, and Developmental Biology, University of California Santa Barbara, Santa Barbara, California 93106 Received June 7, 2011 Accepted July 31, 2012 Allorecognition is the ability of an organism to differentiate self or close relatives from unrelated individuals. The best known applications of allorecognition are the prevention of inbreeding in hermaphroditic species (e.g., the self-incompatibility [SI] systems in plants), the vertebrate immune response to foreign antigens mediated by MHC loci, and somatic fusion, where two genetically independent individuals physically join to become a chimera. In the few model systems where the loci governing allorecognition outcomes have been identified, the corresponding proteins have exhibited exceptional polymorphism. But information about the evolution of this polymorphism outside MHC is limited. We address this subject in the ascidian Botryllus schlosseri,where allorecognition outcomes are determined by a single locus, called FuHC (Fusion/HistoCompatibility). Molecular variation in FuHC is distributed almost entirely within populations, with very little evidence for differentiation among different populations. Mutation plays a larger role than recombination in the creation of FuHC polymorphism. A selection statistic, neutrality tests, and distribution of variation within and among different populations all provide evidence for selection acting on FuHC, but are not in agreement as to whether the selection is balancing or directional. -
Late Cretaceous-Early Palaeogene Echinoderms and the K/T Boundary in the Southeast Netherlands and Northeast Belgium — Part 6: Conclusions
pp 507-580 15-01-2007 14:51 Pagina 505 Late Cretaceous-Early Palaeogene echinoderms and the K/T boundary in the southeast Netherlands and northeast Belgium — Part 6: Conclusions John W.M. Jagt Jagt, J.W.M. Late Cretaceous-Early Palaeogene echinoderms and the K/T boundary in the southeast Netherlands and northeast Belgium — Part 6: Conclusions. — Scripta Geol., 121: 505-577, 8 figs., 9 tables, Leiden, December 2000. John W.M. Jagt, Natuurhistorisch Museum Maastricht, Postbus 882, NL-6200 AW Maastricht, The Netherlands, E-mail: [email protected] Key words: Echinodermata, Late Cretaceous, Early Palaeogene, palaeobiology, K/T boundary, extinc- tion. The palaeobiology of echinoderms occurring in the Meerssen and Geulhem members is discussed and changes in diversity across the K/T boundary are documented. Using literature data on the ecology of extant faunas, the various echinoderm groups are considered. Naturally, such data can only be applied with due caution to fossil forms, whose skeletal morphology is often incompletely known. This holds especially true for asteroids, ophiuroids, and crinoids, which, upon death, rapidly disinte- grate into jumbles of dissociated ossicles. Bioturbation, scavenging, and current winnowing all con- tribute to blurring the picture still further. However, data on extant forms do allow a preliminary sub- division of fossil species into various ecological groups, which are discussed herein. Combining recently published data on K/T boundary sections in Jylland and Sjælland (Denmark) with the pic- ture drawn here for the Maastricht area results in the following best constrained scenario. The demise of the highly diverse latest Maastrichtian echinoderm faunas, typical of shallow-water settings with local palaeorelief and associated unconsolidated bottoms, was rapid, suggestive of a catastrophic event (e.g. -
The A/P Axis in Echinoderm Ontogeny and Evolution: Evidence from Fossils and Molecules
EVOLUTION & DEVELOPMENT 2:2, 93–101 (2000) The A/P axis in echinoderm ontogeny and evolution: evidence from fossils and molecules Kevin J. Peterson,a,b César Arenas-Mena,a,c and Eric H. Davidsona,* aDivision of Biology, California Institute of Technology, Pasadena, CA 91125, USA; bDivision of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA; cStowers Institute for Medical Research, Kansas City, MO 64110, USA *Author for correspondence (email: [email protected]) SUMMARY Even though echinoderms are members of the such that there is but a single plane of symmetry dividing the Bilateria, the location of their anterior/posterior axis has re- animal into left and right halves. We tentatively hypothesize mained enigmatic. Here we propose a novel solution to the that this plane of symmetry is positioned along the dorsal/ven- problem employing three lines of evidence: the expression of tral axis. These axis identifications lead to the conclusion that a posterior class Hox gene in the coeloms of the nascent the five ambulacra are not primary body axes, but instead are adult body plan within the larva; the anatomy of certain early outgrowths from the central anterior/posterior axis. These fossil echinoderms; and finally the relation between endo- identifications also shed insight into several other evolutionary skeletal plate morphology and the associated coelomic tis- mysteries of various echinoderm clades such as the indepen- sues. All three lines of evidence converge on the same answer, dent evolution of bilateral symmetry in irregular echinoids, but namely that the location of the adult mouth is anterior, and the do not elucidate the underlying mechanisms of the adult co- anterior/posterior axis runs from the mouth through the adult elomic architecture. -
Classification
Science Classification Pupil Workbook Year 5 Unit 5 Name: 2 3 Existing Knowledge: Why do we put living things into different groups and what are the groups that we can separate them into? You can think about the animals in the picture and all the others that you know. 4 Session 1: How do we classify animals with a backbone? Key Knowledge Key Vocabulary Animals known as vertebrates have a spinal column. Vertebrates Some vertebrates are warm-blooded meaning that they Species maintain a consistent body temperature. Some are cold- Habitat blooded, meaning they need to move around to warm up or cool down. Spinal column Vertebrates are split into five main groups known as Warm-blooded/Cold- mammals, amphibians, reptiles, birds and fish. blooded Task: Look at the picture here and think about the different groups that each animal is part of. How is each different to the others and which other animals share similar characteristics? Write your ideas here: __________________________ __________________________ __________________________ __________________________ __________________________ __________________________ ____________________________________________________ ____________________________________________________ ____________________________________________________ ____________________________________________________ ____________________________________________________ 5 How do we classify animals with a backbone? Vertebrates are the most advanced organisms on Earth. The traits that make all of the animals in this group special are -
Brittle-Star Mass Occurrence on a Late Cretaceous Methane Seep from South Dakota, USA Received: 16 May 2018 Ben Thuy1, Neil H
www.nature.com/scientificreports OPEN Brittle-star mass occurrence on a Late Cretaceous methane seep from South Dakota, USA Received: 16 May 2018 Ben Thuy1, Neil H. Landman2, Neal L. Larson3 & Lea D. Numberger-Thuy1 Accepted: 29 May 2018 Articulated brittle stars are rare fossils because the skeleton rapidly disintegrates after death and only Published: xx xx xxxx fossilises intact under special conditions. Here, we describe an extraordinary mass occurrence of the ophiacanthid ophiuroid Brezinacantha tolis gen. et sp. nov., preserved as articulated skeletons from an upper Campanian (Late Cretaceous) methane seep of South Dakota. It is uniquely the frst fossil case of a seep-associated ophiuroid. The articulated skeletons overlie centimeter-thick accumulations of dissociated skeletal parts, suggesting lifetime densities of approximately 1000 individuals per m2, persisting at that particular location for several generations. The ophiuroid skeletons on top of the occurrence were preserved intact most probably because of increased methane seepage, killing the individuals and inducing rapid cementation, rather than due to storm-induced burial or slumping. The mass occurrence described herein is an unambiguous case of an autochthonous, dense ophiuroid community that persisted at a particular spot for some time. Thus, it represents a true fossil equivalent of a recent ophiuroid dense bed, unlike other cases that were used in the past to substantiate the claim of a mid-Mesozoic predation-induced decline of ophiuroid dense beds. Brittle stars, or ophiuroids, are among the most abundant and widespread components of the marine benthos, occurring at all depths and latitudes of the world oceans1. Most of the time, however, ophiuroids tend to live a cryptic life hidden under rocks, inside sponges, epizoic on corals or buried in the mud (e.g.2) to such a point that their real abundance is rarely appreciated at frst sight. -
Distant Learning for Middle School Science for STUDENTS!
St. Louis Public Schools Continuous Learning for Students Middle School Science Welcome to Distant Learning for Middle School Science for STUDENTS! Students are encouraged to maintain contact with their home school and classroom teacher(s). If you have not already done so, please visit your child’s school website to access individual teacher web pages for specific learning/assignment information. If you cannot reach your teacher and have elected to use these resources, please be mindful that some learning activities may require students to reply online, while others may require students to respond using paper and pencil. In the event online access is not available and the teacher cannot be reached, responses should be recorded on paper and completed work should be dropped off at your child’s school. Please contact your child’s school for the dates and times to drop off your child’s work. If you need additional resources to support virtual learning, please visit: https://www.slps.org/extendedresources Overview of Week 6: Students engage with the performance task Evolution of Andes where they use what they know about the rock cycle and how earth systems interact (weeks 3-5 (April 6-24) of Continuous Learning plans) to create a model of how the growing Andes could have led to the sloths living in the Amazon and write an argument about how the Andes led to the sloths using their model as evidence. Students will present their final model and argument via PowerPoint slides, essay, or poster. To access all instructional fillable pdf files, also available in print, for Week 6 go HERE.