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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. -
Fossil Collecting Areas in Iowa
FOSSIL COLLECTING AREAS IN IOWA The following list, although far from compete, includes a few of the better fossil collecting areas in Iowa. 1. Rockford, Floyd County (¼ mile south and ¼ mile west of the Rockford Brick and Tile Company pit, on county road “D”). Well preserved brachiopods, gastropods, and corals are most abundant in the yellowish shales that overlie the blue-gray beds. The fossils occurring here are known as the Hackberry fauna and have been described by C.L. and M.A. Fenton in a book entitled, “The Hackberry State of the Upper Devonian,” published by the MacMillan Company in 1924. 2. Bird Hill, Cerro Gordo County This is near the center of the north line of section 24, T 95N, R.19W, about 3½ miles west and ¼ mile south of the Rockford Brick and Tile Company Plant. The Hackberry fauna can be collected here also. 3. Elgin-Clermont area, Fayette County In the Elgin Member of the Maquoketa Formation large trilobites and both straight and coiled cephalopods are found. Fragments of trilobites are common, but whole specimens are rare. Road cuts along the new highway between Clermont and Elgin, the dry stream bed along county road “Y” east of Clermont, and the high-road cuts along the Turkey River southeast of Elgin are all good collecting sites. References for this area are: (1) Slocum, A.W., “Trilobites from the Maquoketa Beds of Fayette County, Iowa,” Iowa Geological Survey Annual Report, Volume 25; (2) Walter, O.T., “Trilobites of Iowa and some Related Paleozoic Forms,” Iowa Geological Survey Annual Report, Volume 31; (3) Ladd, H.S., “Stratigraphy and Paleontology of the Maquoketa Shale of Iowa,” Iowa Geological Survey Annual Report, Volume 34. -
BIOLOGY and METHODS of CONTROLLING the STARFISH, Asterias Forbesi {DESOR}
BIOLOGY AND METHODS OF CONTROLLING THE STARFISH, Asterias forbesi {DESOR} By Victor L. Loosanoff Biological Laboratory Bureau of Commercial Fisheries U. S. Fish and Wildlife Service Milford, Connecticut CONTENTS Page Introduction. .. .. ... .. .. .. .. ... .. .. .. ... 1 Distribution and occurrence....................................................... 2 Food and feeding ...................................................................... 3 Methods of controL........................................ ........................... 5 Mechanical methods : Starfish mop...................................................... .................. 5 Oyster dredge... ........................ ............. ..... ... ...................... 5 Suction dredge..................................................................... 5 Underwater plow ..... ............................................................. 6 Chemical methods .................................................................. 6 Quicklime............................. ........................... ................... 7 Salt solution......... ........................................ ......... ............. 8 Organic chemicals....... ..... ... .... .................. ........ ............. ...... 9 Utilization of starfish................................................................ 11 References..... ............................................................... ........ 11 INTRODUCTION Even in the old days, when the purchas ing power of the dollar was much higher, The starfish has long -
Marine Invertebrate Field Guide
Marine Invertebrate Field Guide Contents ANEMONES ....................................................................................................................................................................................... 2 AGGREGATING ANEMONE (ANTHOPLEURA ELEGANTISSIMA) ............................................................................................................................... 2 BROODING ANEMONE (EPIACTIS PROLIFERA) ................................................................................................................................................... 2 CHRISTMAS ANEMONE (URTICINA CRASSICORNIS) ............................................................................................................................................ 3 PLUMOSE ANEMONE (METRIDIUM SENILE) ..................................................................................................................................................... 3 BARNACLES ....................................................................................................................................................................................... 4 ACORN BARNACLE (BALANUS GLANDULA) ....................................................................................................................................................... 4 HAYSTACK BARNACLE (SEMIBALANUS CARIOSUS) .............................................................................................................................................. 4 CHITONS ........................................................................................................................................................................................... -
The Sea Stars (Echinodermata: Asteroidea): Their Biology, Ecology, Evolution and Utilization OPEN ACCESS
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/328063815 The Sea Stars (Echinodermata: Asteroidea): Their Biology, Ecology, Evolution and Utilization OPEN ACCESS Article · January 2018 CITATIONS READS 0 6 5 authors, including: Ferdinard Olisa Megwalu World Fisheries University @Pukyong National University (wfu.pknu.ackr) 3 PUBLICATIONS 0 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Population Dynamics. View project All content following this page was uploaded by Ferdinard Olisa Megwalu on 04 October 2018. The user has requested enhancement of the downloaded file. Review Article Published: 17 Sep, 2018 SF Journal of Biotechnology and Biomedical Engineering The Sea Stars (Echinodermata: Asteroidea): Their Biology, Ecology, Evolution and Utilization Rahman MA1*, Molla MHR1, Megwalu FO1, Asare OE1, Tchoundi A1, Shaikh MM1 and Jahan B2 1World Fisheries University Pilot Programme, Pukyong National University (PKNU), Nam-gu, Busan, Korea 2Biotechnology and Genetic Engineering Discipline, Khulna University, Khulna, Bangladesh Abstract The Sea stars (Asteroidea: Echinodermata) are comprising of a large and diverse groups of sessile marine invertebrates having seven extant orders such as Brisingida, Forcipulatida, Notomyotida, Paxillosida, Spinulosida, Valvatida and Velatida and two extinct one such as Calliasterellidae and Trichasteropsida. Around 1,500 living species of starfish occur on the seabed in all the world's oceans, from the tropics to subzero polar waters. They are found from the intertidal zone down to abyssal depths, 6,000m below the surface. Starfish typically have a central disc and five arms, though some species have a larger number of arms. The aboral or upper surface may be smooth, granular or spiny, and is covered with overlapping plates. -
Mary Anning of Lyme Regis: 19Th Century Pioneer in British Palaeontology
Headwaters Volume 26 Article 14 2009 Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology Larry E. Davis College of St. Benedict / St. John's University, [email protected] Follow this and additional works at: https://digitalcommons.csbsju.edu/headwaters Part of the Geology Commons, and the Paleontology Commons Recommended Citation Davis, Larry E. (2009) "Mary Anning of Lyme Regis: 19th Century Pioneer in British Palaeontology," Headwaters: Vol. 26, 96-126. Available at: https://digitalcommons.csbsju.edu/headwaters/vol26/iss1/14 This Article is brought to you for free and open access by DigitalCommons@CSB/SJU. It has been accepted for inclusion in Headwaters by an authorized editor of DigitalCommons@CSB/SJU. For more information, please contact [email protected]. LARRY E. DAVIS Mary Anning of Lyme Regis 19th Century Pioneer in British Palaeontology Ludwig Leichhardt, a 19th century German explorer noted in a letter, “… we had the pleasure of making the acquaintance of the Princess of Palaeontology, Miss Anning. She is a strong, energetic spinster of about 28 years of age, tanned and masculine in expression …” (Aurousseau, 1968). Gideon Mantell, a 19th century British palaeontologist, made a less flattering remark when he wrote in his journal, “… sallied out in quest of Mary An- ning, the geological lioness … we found her in a little dirt shop with hundreds of specimens piled around her in the greatest disorder. She, the presiding Deity, a prim, pedantic vinegar looking female; shred, and rather satirical in her conversation” (Curwin, 1940). Who was Mary Anning, this Princess of Palaeontology and Geological Lioness (Fig. -
The Paleontology Synthesis Project and Establishing a Framework for Managing National Park Service Paleontological Resource Archives and Data
Lucas, S.G. and Sullivan, R.M., eds., 2018, Fossil Record 6. New Mexico Museum of Natural History and Science Bulletin 79. 589 THE PALEONTOLOGY SYNTHESIS PROJECT AND ESTABLISHING A FRAMEWORK FOR MANAGING NATIONAL PARK SERVICE PALEONTOLOGICAL RESOURCE ARCHIVES AND DATA VINCENT L. SANTUCCI1, JUSTIN S. TWEET2 and TIMOTHY B. CONNORS3 1National Park Service, Geologic Resources Division, 1849 “C” Street, NW, Washington, D.C. 20240, [email protected]; 2National Park Service, 9149 79th Street S., Cottage Grove, MN 55016, [email protected]; 3National Park Service, Geologic Resources Division, 12795 W. Alameda Parkway, Lakewood, CO 80225, [email protected] Abstract—The National Park Service Paleontology Program maintains an extensive collection of digital and hard copy documents, publications, photographs and other archives associated with the paleontological resources documented in 268 parks. The organization and preservation of the NPS paleontology archives has been the focus of intensive data management activities by a small and dedicated team of NPS staff. The data preservation strategy complemented the NPS servicewide inventories for paleontological resources. The first phase of the data management, referred to as the NPS Paleontology Synthesis Project, compiled servicewide paleontological resource data pertaining to geologic time, taxonomy, museum repositories, holotype fossil specimens, and numerous other topics. In 2015, the second phase of data management was implemented with the creation and organization of a multi-faceted digital data system known as the NPS Paleontology Archives and NPS Paleontology Library. Two components of the NPS Paleontology Archives were designed for the preservation of both park specific and servicewide paleontological resource archives and data. A third component, the NPS Paleontology Library, is a repository for electronic copies of geology and paleontology publications, reports, and other media. -
Biology of Echinoderms
Echinoderms Branches on the Tree of Life Programs ECHINODERMS Written and photographed by David Denning and Bruce Russell Produced by BioMEDIA ASSOCIATES ©2005 - Running time 16 minutes. Order Toll Free (877) 661-5355 Order by FAX (843) 470-0237 The Phylum Echinodermata consists of about 6,000 living species, all of which are marine. This video program compares the five major classes of living echinoderms in terms of basic functional biology, evolution and ecology using living examples, animations and a few fossil species. Detailed micro- and macro- photography reveal special adaptations of echinoderms and their larval biology. (THUMBNAIL IMAGES IN THIS GUIDE ARE FROM THE VIDEO PROGRAM) Summary of the Program: Introduction - Characteristics of the Class Echinoidea phylum. spine adaptations, pedicellaria, Aristotle‘s lantern, sand dollars, urchin development, Class Asteroidea gastrulation, settlement skeleton, water vascular system, tube feet function, feeding, digestion, Class Holuthuroidea spawning, larval development, diversity symmetry, water vascular system, ossicles, defensive mechanisms, diversity, ecology Class Ophiuroidea regeneration, feeding, diversity Class Crinoidea – Topics ecology, diversity, fossil echinoderms © BioMEDIA ASSOCIATES (1 of 7) Echinoderms ... ... The characteristics that distinguish Phylum Echinodermata are: radial symmetry, internal skeleton, and water-vascular system. Echinoderms appear to be quite different than other ‘advanced’ animal phyla, having radial (spokes of a wheel) symmetry as adults, rather than bilateral (worm-like) symmetry as in other triploblastic (three cell-layer) animals. Viewers of this program will observe that echinoderm radial symmetry is secondary; echinoderms begin as bilateral free-swimming larvae and become radial at the time of metamorphosis. Also, in one echinoderm group, the sea cucumbers, partial bilateral symmetry is retained in the adult stages -- sea cucumbers are somewhat worm–like. -
Fossil Collecting in Ohio
No. 17 OHIOGeoFacts DEPARTMENT OF NATURAL RESOURCES • DIVISION OF GEOLOGICAL SURVEY FOSSIL COLLECTING IN OHIO Hobbyists have long known about Ohio’s great abundance and WHERE FOSSILS ARE FOUND IN OHIO diversity of fossils. Many world-famous paleontologists—geologists who study fossils—began their careers as youngsters collecting fossils Ordovician rocks in Ohio are world famous for in their native Ohio. Fossils from Ohio are important constituents the abundance, variety, and excellent preserva- of museum collections throughout the United States and Europe. tion of the fossils they contain. The limestones and shales exposed in almost every road cut or WHY OHIO HAS FOSSILS stream bed in southwestern Ohio, southeastern Indiana, and north-central Kentucky provide The area that is now Ohio was not always dry land as it is today. the opportunity to collect a bonanza of fossils. Approximately 510 million years ago (m.y.a.), Ohio was south of the Among the more abundant types of fossils col- Equator. As the North American Plate moved to its current position ORDOVICIAN lected from Ordovician rocks are brachiopods, 508–438 m.y.a. through the process of plate tectonics, tropical to subtropical seas bryozoans, gastropods, and trilobites. repeatedly transgressed over the plate. It is because of those warm Silurian rocks of western Ohio are not known seas that Ohio has the abundant fossils that people collect today. for their fossils. When the limestones and shales The seas that covered Ohio during the Ordovician, Silurian, and were fi rst deposited they were quite fossilifer- most of the Devonian Periods of the Paleozoic Era were the site of ous. -
Primitive Soft-Bodied Cephalopods from the Cambrian
ACCEPTED DRAFT Please note that this is not the final manuscript version. Links to the published manuscript, figures, and supplementary information can be found at http://individual.utoronto.ca/martinsmith/nectocaris.html doi: 10.1038/nature09068 Smith & Caron 2010, Page 1 Primitive soft-bodied cephalopods from the Cambrian Martin R. Smith 1, 2* & Jean-Bernard Caron 2, 1 1Departent of Ecology and Evolutionary Biology, University of Toronto, 25 Harbord Street, Ontario, M5S 3G5, Canada 2Department of Palaeobiology, Royal Ontario Museum, 100 Queen ’s Park, Toronto, Ontario M5S 2C6, Canada *Author for correspondence The exquisite preservation of soft-bodied animals in Burgess Shale-type deposits provides important clues into the early evolution of body plans that emerged during the Cambrian explosion 1. Until now, such deposits have remained silent regarding the early evolution of extant molluscan lineages – in particular the cephalopods. Nautiloids, traditionally considered basal within the cephalopods, are generally depicted as evolving from a creeping Cambrian ancestor whose dorsal shell afforded protection and buoyancy 2. Whilst nautiloid-like shells occur from the Late Cambrian onwards, the fossil record provides little constraint on this model, or indeed on the early evolution of cephalopods. Here, we reinterpret the problematic Middle Cambrian animal Nectocaris pteryx 3, 4 as a primitive (i.e. stem-group), non-mineralized cephalopod, based on new material from the Burgess Shale. Together with Nectocaris, the problematic Lower Cambrian taxa Petalilium 5 and (probably) Vetustovermis 6, 7 form a distinctive clade, Nectocarididae, characterized by an open axial cavity with paired gills, wide lateral fins, a single pair of long, prehensile tentacles, a pair of non-faceted eyes on short stalks, and a large, flexible anterior funnel. -
The Greatest Challenge to 21St Century Paleontology: When Commercialization of Fossils Threatens the Science
Palaeontologia Electronica http://palaeo-electronica.org The greatest challenge to 21st century paleontology: When commercialization of fossils threatens the science Kenshu Shimada, Philip J. Currie, Eric Scott, and Stuart S. Sumida As we proceed into the 21st century, the sci- responses to geological and climatic factors. Pale- ence of paleontology has achieved a remarkable ontology presently enjoys a new “Golden Age,” prominence and popularity, providing increasingly progressing by leaps while also serving, as always, detailed perspective on critical biological and geo- to inspire young minds to explore science and the logical processes. Spectacular new discoveries natural world. excite the imagination and spur new investigations, Yet at the outset of the millennium, three inter- while more abundant fossils studied using new connected, troubling challenges confront paleontol- techniques enable more precise interpretations of ogists: 1) a shrinking job market, 2) diminishing diversity, variation, changes through time, and funding sources, and 3) heightened commercial- Editor’s note: The commercial collection and sale of fossils, as well as the still developing regulations involving collection of fossils on public lands, have emerged as one of the most contentious issues in pale- ontology. These issues pit not only professional paleontologists and commercial collectors against each other, but have produced rifts within the paleontological community. Here Shimada and his co-authors vig- orously present a position supported by many vertebrate paleontologists. I repeat a call in an earlier com- mentary (Plotnick, 2011; palaeo-electronica.org/2011_1/commentary/mainstream.htm) for additional contributions that would discuss these issues that are so crucial to our field. Please send directly to Roy E. -
Raymond M. Alf Museum of Paleontology EDUCATOR's GUIDE
Raymond M. Alf Museum of Paleontology EDUCATOR’S GUIDE Dear Educator: This guide is recommended for educators of grades K-4 and is designed to help you prepare students for their Alf Museum visit, as well as to provide resources to enhance your classroom curriculum. This packet includes background information about the Alf Museum and the science of paleontology, a summary of our museum guidelines and what to expect, a pre-visit checklist, a series of content standard-aligned activities/exercises for classroom use before and/or after your visit, and a list of relevant terms and additional resources. Please complete and return the enclosed evaluation form to help us improve this guide to better serve your needs. Thank you! Paleontology: The Study of Ancient Life Paleontology is the study of ancient life. The history of past life on Earth is interpreted by scientists through the examination of fossils, the preserved remains of organisms which lived in the geologic past (more than 10,000 years ago). There are two main types of fossils: body fossils, the preserved remains of actual organisms (e.g. shells/hard parts, teeth, bones, leaves, etc.) and trace fossils, the preserved evidence of activity by organisms (e.g. footprints, burrows, fossil dung). Chances for fossil preservation are enhanced by (1) the presence of hard parts (since soft parts generally rot or are eaten, preventing preservation) and (2) rapid burial (preventing disturbance by bio- logical or physical actions). Many body fossils are skeletal remains (e.g. bones, teeth, shells, exoskel- etons). Most form when an animal or plant dies and then is buried by sediment (e.g.