Mollusca: Bivalvia) Except Ennucula Iredale, 1931
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Notes on Nucula
[ 629 ] Notes on Nucula. By Kyosuke Hirasaka. Professor of Zoology, Imperial University, Formosa. With 5 Figures in the Text. THESEnotes record the result of work done at the Plymouth Laboratory during the summer of 1926. They deal chiefly with the feeding habits of Nucula, a Proto branch possessing the type of feeding mechanism characteristic of that order, and not found in any other Lamellibranch. During the course of my work I found VIes' interesting paper on the sense organ of Nucula. After studying the organ, I arrived at a different interpretation of its function from that reached by VIes. I owe very much to the kindness of the Director and other members of the staff of the Laboratory, and am also indebted to Professor H. G. Cannon for friendly advice. Three species of Nucula, common in the vicinity of Plymouth, were used, namely, N. nucleus, N. radiata, and N. nitida. Much important work has been done on Nucula nucleus, the most common European species, as well as on N ucula proxima and N ucula delphinodonta, which live on the American side of the Atlantic. Of course, many characters are common to these species, but not all. The material used was dredged in 20 to 30 fathoms off Plymouth by the research steamer" Salpa," N. nucleus"being the most abundant species. The Nucula were kept alive in a small glass dish with a little of the mud that was collected with them. A current of water from the general <tquarium supply was provided, and the animals remained quite healthy during the two and a half months of my stay at the Laboratory. -
Cretaceous Acila (Truncacila) (Bivalvia: Nuculidae) from the Pacific Slope of North America
THE VELIGER ᭧ CMS, Inc., 2006 The Veliger 48(2):83–104 (June 30, 2006) Cretaceous Acila (Truncacila) (Bivalvia: Nuculidae) from the Pacific Slope of North America RICHARD L. SQUIRES Department of Geological Sciences, California State University, Northridge, California 91330-8266, USA AND LOUELLA R. SAUL Invertebrate Paleontology Section, Natural History Museum of Los Angeles County, 900 Exposition Boulevard, Los Angeles, California 90007, USA Abstract. The Cretaceous record of the nuculid bivalve Acila (Truncacila) Grant & Gale, 1931, is established for the first time in the region extending from the Queen Charlotte Islands, British Columbia, southward to Baja California, Mexico. Its record is represented by three previously named species, three new species, and one possible new species. The previously named species are reviewed and refined. The cumulative geologic range of all these species is Early Cretaceous (late Aptian) to Late Cretaceous (early late Maastrichtian), with the highest diversity (four species) occurring in the latest Campanian to early Maastrichtian. Acila (T.) allisoni, sp. nov., known only from upper Aptian strata of northern Baja California, Mexico, is one of the earliest confirmed records of this subgenus. ‘‘Aptian’’ reports of Trun- cacila in Tunisia, Morocco, and possibly eastern Venzeula need confirmation. Specimens of the study area Acila are most abundant in sandy, shallow-marine deposits that accumulated under warm- water conditions. Possible deeper water occurrences need critical evaluation. INTRODUCTION and Indo-Pacific regions and is a shallow-burrowing de- posit feeder. Like other nuculids, it lacks siphons but has This is the first detailed study of the Cretaceous record an anterior-to-posterior water current (Coan et al., 2000). -
DEEP SEA LEBANON RESULTS of the 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project
DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project March 2018 DEEP SEA LEBANON RESULTS OF THE 2016 EXPEDITION EXPLORING SUBMARINE CANYONS Towards Deep-Sea Conservation in Lebanon Project Citation: Aguilar, R., García, S., Perry, A.L., Alvarez, H., Blanco, J., Bitar, G. 2018. 2016 Deep-sea Lebanon Expedition: Exploring Submarine Canyons. Oceana, Madrid. 94 p. DOI: 10.31230/osf.io/34cb9 Based on an official request from Lebanon’s Ministry of Environment back in 2013, Oceana has planned and carried out an expedition to survey Lebanese deep-sea canyons and escarpments. Cover: Cerianthus membranaceus © OCEANA All photos are © OCEANA Index 06 Introduction 11 Methods 16 Results 44 Areas 12 Rov surveys 16 Habitat types 44 Tarablus/Batroun 14 Infaunal surveys 16 Coralligenous habitat 44 Jounieh 14 Oceanographic and rhodolith/maërl 45 St. George beds measurements 46 Beirut 19 Sandy bottoms 15 Data analyses 46 Sayniq 15 Collaborations 20 Sandy-muddy bottoms 20 Rocky bottoms 22 Canyon heads 22 Bathyal muds 24 Species 27 Fishes 29 Crustaceans 30 Echinoderms 31 Cnidarians 36 Sponges 38 Molluscs 40 Bryozoans 40 Brachiopods 42 Tunicates 42 Annelids 42 Foraminifera 42 Algae | Deep sea Lebanon OCEANA 47 Human 50 Discussion and 68 Annex 1 85 Annex 2 impacts conclusions 68 Table A1. List of 85 Methodology for 47 Marine litter 51 Main expedition species identified assesing relative 49 Fisheries findings 84 Table A2. List conservation interest of 49 Other observations 52 Key community of threatened types and their species identified survey areas ecological importanc 84 Figure A1. -
Special Issue3.7 MB
Volume Eleven Conservation Science 2016 Western Australia Review and synthesis of knowledge of insular ecology, with emphasis on the islands of Western Australia IAN ABBOTT and ALLAN WILLS i TABLE OF CONTENTS Page ABSTRACT 1 INTRODUCTION 2 METHODS 17 Data sources 17 Personal knowledge 17 Assumptions 17 Nomenclatural conventions 17 PRELIMINARY 18 Concepts and definitions 18 Island nomenclature 18 Scope 20 INSULAR FEATURES AND THE ISLAND SYNDROME 20 Physical description 20 Biological description 23 Reduced species richness 23 Occurrence of endemic species or subspecies 23 Occurrence of unique ecosystems 27 Species characteristic of WA islands 27 Hyperabundance 30 Habitat changes 31 Behavioural changes 32 Morphological changes 33 Changes in niches 35 Genetic changes 35 CONCEPTUAL FRAMEWORK 36 Degree of exposure to wave action and salt spray 36 Normal exposure 36 Extreme exposure and tidal surge 40 Substrate 41 Topographic variation 42 Maximum elevation 43 Climate 44 Number and extent of vegetation and other types of habitat present 45 Degree of isolation from the nearest source area 49 History: Time since separation (or formation) 52 Planar area 54 Presence of breeding seals, seabirds, and turtles 59 Presence of Indigenous people 60 Activities of Europeans 63 Sampling completeness and comparability 81 Ecological interactions 83 Coups de foudres 94 LINKAGES BETWEEN THE 15 FACTORS 94 ii THE TRANSITION FROM MAINLAND TO ISLAND: KNOWNS; KNOWN UNKNOWNS; AND UNKNOWN UNKNOWNS 96 SPECIES TURNOVER 99 Landbird species 100 Seabird species 108 Waterbird -
A Technical Characterization of Estuarine and Coastal New Hampshire New Hampshire Estuaries Project
AR-293 University of New Hampshire University of New Hampshire Scholars' Repository PREP Publications Piscataqua Region Estuaries Partnership 2000 A Technical Characterization of Estuarine and Coastal New Hampshire New Hampshire Estuaries Project Stephen H. Jones University of New Hampshire Follow this and additional works at: http://scholars.unh.edu/prep Part of the Marine Biology Commons Recommended Citation New Hampshire Estuaries Project and Jones, Stephen H., "A Technical Characterization of Estuarine and Coastal New Hampshire" (2000). PREP Publications. Paper 294. http://scholars.unh.edu/prep/294 This Report is brought to you for free and open access by the Piscataqua Region Estuaries Partnership at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in PREP Publications by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. A Technical Characterization of Estuarine and Coastal New Hampshire Published by the New Hampshire Estuaries Project Edited by Dr. Stephen H. Jones Jackson estuarine Laboratory, university of New Hampshire Durham, NH 2000 TABLE OF CONTENTS ACKNOWLEDGEMENTS TABLE OF CONTENTS ............................................................................................i LIST OF TABLES ....................................................................................................vi LIST OF FIGURES.................................................................................................viii -
Rebuilding Biodiversity of Patagonian Marine Molluscs After the End-Cretaceous Mass Extinction
Rebuilding Biodiversity of Patagonian Marine Molluscs after the End-Cretaceous Mass Extinction Martin Aberhan1*, Wolfgang Kiessling1,2 1 Museum fu¨r Naturkunde, Leibniz Institute for Evolution and Biodiversity Science, Berlin, Germany, 2 GeoZentrum Nordbayern, Pala¨oumwelt, Universita¨t Erlangen2 Nu¨rnberg, Erlangen, Germany Abstract We analysed field-collected quantitative data of benthic marine molluscs across the Cretaceous–Palaeogene boundary in Patagonia to identify patterns and processes of biodiversity reconstruction after the end-Cretaceous mass extinction. We contrast diversity dynamics from nearshore environments with those from offshore environments. In both settings, Early Palaeogene (Danian) assemblages are strongly dominated by surviving lineages, many of which changed their relative abundance from being rare before the extinction event to becoming the new dominant forms. Only a few of the species in the Danian assemblages were newly evolved. In offshore environments, however, two newly evolved Danian bivalve species attained ecological dominance by replacing two ecologically equivalent species that disappeared at the end of the Cretaceous. In both settings, the total number of Danian genera at a locality remained below the total number of late Cretaceous (Maastrichtian) genera at that locality. We suggest that biotic interactions, in particular incumbency effects, suppressed post-extinction diversity and prevented the compensation of diversity loss by originating and invading taxa. Contrary to the total number of genera at localities, diversity at the level of individual fossiliferous horizons before and after the boundary is indistinguishable in offshore environments. This indicates an evolutionary rapid rebound to pre-extinction values within less than ca 0.5 million years. In nearshore environments, by contrast, diversity of fossiliferous horizons was reduced in the Danian, and this lowered diversity lasted for the entire studied post-extinction interval. -
080058-89.02.017.Pdf
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Guide to Estuarine and Inshore Bivalves of Virginia
W&M ScholarWorks Dissertations, Theses, and Masters Projects Theses, Dissertations, & Master Projects 1968 Guide to Estuarine and Inshore Bivalves of Virginia Donna DeMoranville Turgeon College of William and Mary - Virginia Institute of Marine Science Follow this and additional works at: https://scholarworks.wm.edu/etd Part of the Marine Biology Commons, and the Oceanography Commons Recommended Citation Turgeon, Donna DeMoranville, "Guide to Estuarine and Inshore Bivalves of Virginia" (1968). Dissertations, Theses, and Masters Projects. Paper 1539617402. https://dx.doi.org/doi:10.25773/v5-yph4-y570 This Thesis is brought to you for free and open access by the Theses, Dissertations, & Master Projects at W&M ScholarWorks. It has been accepted for inclusion in Dissertations, Theses, and Masters Projects by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. GUIDE TO ESTUARINE AND INSHORE BIVALVES OF VIRGINIA A Thesis Presented to The Faculty of the School of Marine Science The College of William and Mary in Virginia In Partial Fulfillment Of the Requirements for the Degree of Master of Arts LIBRARY o f the VIRGINIA INSTITUTE Of MARINE. SCIENCE. By Donna DeMoranville Turgeon 1968 APPROVAL SHEET This thesis is submitted in partial fulfillment of the requirements for the degree of Master of Arts jfitw-f. /JJ'/ 4/7/A.J Donna DeMoranville Turgeon Approved, August 1968 Marvin L. Wass, Ph.D. P °tj - D . dvnd.AJlLJ*^' Jay D. Andrews, Ph.D. 'VL d. John L. Wood, Ph.D. William J. Hargi Kenneth L. Webb, Ph.D. ACKNOWLEDGEMENTS The author wishes to express sincere gratitude to her major professor, Dr. -
Molluscs: Bivalvia Laura A
I Molluscs: Bivalvia Laura A. Brink The bivalves (also known as lamellibranchs or pelecypods) include such groups as the clams, mussels, scallops, and oysters. The class Bivalvia is one of the largest groups of invertebrates on the Pacific Northwest coast, with well over 150 species encompassing nine orders and 42 families (Table 1).Despite the fact that this class of mollusc is well represented in the Pacific Northwest, the larvae of only a few species have been identified and described in the scientific literature. The larvae of only 15 of the more common bivalves are described in this chapter. Six of these are introductions from the East Coast. There has been quite a bit of work aimed at rearing West Coast bivalve larvae in the lab, but this has lead to few larval descriptions. Reproduction and Development Most marine bivalves, like many marine invertebrates, are broadcast spawners (e.g., Crassostrea gigas, Macoma balthica, and Mya arenaria,); the males expel sperm into the seawater while females expel their eggs (Fig. 1).Fertilization of an egg by a sperm occurs within the water column. In some species, fertilization occurs within the female, with the zygotes then text continues on page 134 Fig. I. Generalized life cycle of marine bivalves (not to scale). 130 Identification Guide to Larval Marine Invertebrates ofthe Pacific Northwest Table 1. Species in the class Bivalvia from the Pacific Northwest (local species list from Kozloff, 1996). Species in bold indicate larvae described in this chapter. Order, Family Species Life References for Larval Descriptions History1 Nuculoida Nuculidae Nucula tenuis Acila castrensis FSP Strathmann, 1987; Zardus and Morse, 1998 Nuculanidae Nuculana harnata Nuculana rninuta Nuculana cellutita Yoldiidae Yoldia arnygdalea Yoldia scissurata Yoldia thraciaeforrnis Hutchings and Haedrich, 1984 Yoldia rnyalis Solemyoida Solemyidae Solemya reidi FSP Gustafson and Reid. -
Conserving Marine Biodiversity in South Australia - Part 1 - Background, Status and Review of Approach to Marine Biodiversity Conservation in South Australia
Conserving Marine Biodiversity in South Australia - Part 1 - Background, Status and Review of Approach to Marine Biodiversity Conservation in South Australia K S Edyvane May 1999 ISBN 0 7308 5237 7 No 38 The recommendations given in this publication are based on the best available information at the time of writing. The South Australian Research and Development Institute (SARDI) makes no warranty of any kind expressed or implied concerning the use of technology mentioned in this publication. © SARDI. This work is copyright. Apart of any use as permitted under the Copyright Act 1968, no part may be reproduced by any process without prior written permission from the publisher. SARDI is a group of the Department of Primary Industries and Resources CONTENTS – PART ONE PAGE CONTENTS NUMBER INTRODUCTION 1. Introduction…………………………………..…………………………………………………………1 1.1 The ‘Unique South’ – Southern Australia’s Temperate Marine Biota…………………………….…….1 1.2 1.2 The Status of Marine Protected Areas in Southern Australia………………………………….4 2 South Australia’s Marine Ecosystems and Biodiversity……………………………………………..9 2.1 Oceans, Gulfs and Estuaries – South Australia’s Oceanographic Environments……………………….9 2.1.1 Productivity…………………………………………………………………………………….9 2.1.2 Estuaries………………………………………………………………………………………..9 2.2 Rocky Cliffs and Gulfs, to Mangrove Shores -South Australia’s Coastal Environments………………………………………………………………13 2.2.1 Offshore Islands………………………………………………………………………………14 2.2.2 Gulf Ecosystems………………………………………………………………………………14 2.2.3 Northern Spencer Gulf………………………………………………………………………...14 -
The Gela Basin Pockmark Field in the Strait of Sicily
EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Natural Hazards Natural Hazards and Earth System and Earth System Sciences Sciences Discussions Open Access Open Access Atmospheric Atmospheric Chemistry Chemistry and Physics and Physics Discussions Open Access Open Access Atmospheric Atmospheric Measurement Measurement Techniques Techniques Discussions Open Access Biogeosciences, 10, 4653–4671, 2013 Open Access www.biogeosciences.net/10/4653/2013/ Biogeosciences doi:10.5194/bg-10-4653-2013 Biogeosciences Discussions © Author(s) 2013. CC Attribution 3.0 License. Open Access Open Access Climate Climate of the Past of the Past Discussions The Gela Basin pockmark field in the strait of Sicily (Mediterranean Open Access Open Access Sea): chemosymbiotic faunal and carbonate signaturesEarth System of postglacial Earth System Dynamics Dynamics to modern cold seepage Discussions M. Taviani1,2, L. Angeletti1, A. Ceregato1, F. Foglini1, C. Froglia3, and F. Trincardi1 Open Access 1ISMAR-CNR Istituto di Scienze Marine, Via Gobetti 101, 40129, Bologna, Italy Geoscientific Geoscientific Open Access 2Woods Hole Oceanographic Institution, 266 Woods Hole Rd, Woods Hole, Ma. 02543, USAInstrumentation Instrumentation 3 ISMAR-CNR Istituto di Scienze Marine, Largo Fiera della Pesca 2, 60125, Ancona, Italy Methods and Methods and Correspondence to: M. Taviani ([email protected]) Data Systems Data Systems Discussions Open Access Received: 10 December 2012 – Published in Biogeosciences Discuss.: 22 January 2013 Open Access Revised: 24 April 2013 – Accepted: 23 May 2013 – Published: 12 July 2013 Geoscientific Geoscientific Model Development Model Development Abstract. The geo-biological exploration of a pockmark brachia sp.), and 9609.5 ± 153.5 yr cal BP (L. -
2020 Interim Receiving Waters Monitoring Report
POINT LOMA OCEAN OUTFALL MONTHLY RECEIVING WATERS INTERIM RECEIVING WATERS MONITORING REPORT FOR THE POINTM ONITORINGLOMA AND SOUTH R EPORTBAY OCEAN OUTFALLS POINT LOMA 2020 WASTEWATER TREATMENT PLANT NPDES Permit No. CA0107409 SDRWQCB Order No. R9-2017-0007 APRIL 2021 Environmental Monitoring and Technical Services 2392 Kincaid Road x Mail Station 45A x San Diego, CA 92101 Tel (619) 758-2300 Fax (619) 758-2309 INTERIM RECEIVING WATERS MONITORING REPORT FOR THE POINT LOMA AND SOUTH BAY OCEAN OUTFALLS 2020 POINT LOMA WASTEWATER TREATMENT PLANT (ORDER NO. R9-2017-0007; NPDES NO. CA0107409) SOUTH BAY WATER RECLAMATION PLANT (ORDER NO. R9-2013-0006 AS AMENDED; NPDES NO. CA0109045) SOUTH BAY INTERNATIONAL WASTEWATER TREATMENT PLANT (ORDER NO. R9-2014-0009 AS AMENDED; NPDES NO. CA0108928) Prepared by: City of San Diego Ocean Monitoring Program Environmental Monitoring & Technical Services Division Ryan Kempster, Editor Ami Latker, Editor June 2021 Table of Contents Production Credits and Acknowledgements ...........................................................................ii Executive Summary ...................................................................................................................1 A. Latker, R. Kempster Chapter 1. General Introduction ............................................................................................3 A. Latker, R. Kempster Chapter 2. Water Quality .......................................................................................................15 S. Jaeger, A. Webb, R. Kempster,