Coral Sea Atoll Lagoons: Closed Nurseries for the Larvae of a Few Coral Reef Fishes

Total Page:16

File Type:pdf, Size:1020Kb

Coral Sea Atoll Lagoons: Closed Nurseries for the Larvae of a Few Coral Reef Fishes BULLETIN OF MARINE SCIENCE, 54(1): 206-227, 1994 CORAL SEA ATOLL LAGOONS: CLOSED NURSERIES FOR THE LARVAE OF A FEW CORAL REEF FISHES Jeffrey M. Leis ABSTRACT Lagoons of two western Coral Sea atolls (Osprey and Holmes Reefs) were sampled with oblique bongo-net tows and neuston tows a total of three times over 3 years. Equivalent samples were taken in the ocean nearby. Concentrations of oceanic larvae in the lagoons were 13-14% of concentrations in the ocean, but oceanic taxa constituted less than 1% of the larvae captured in the lagoons, Concentrations (number' m -') and abundances (number' m -2) of shorefish larvae were 4-10 times higher in the lagoon than in the ocean, but larvae of more shorefish taxa were found in the ocean, In the lagoons catches were heavily dominated by larvae of apogonids, clupeids, gobiids, pomacentrids and schindleriids, Taxonomic com- position in the lagoons varied little, Based on presence/absence, and sizes of the larvae captured, only 33 taxa (of 15 families) complete or probably complete their pelagic larval period within these atoll lagoons. These include (number of species where larvae were iden- tified below family level): Apogonidae (9), Atherinidae (2), Belonidae (I), Blenniidae (4), Bythitidae (I), Clupeidae (I), Gobiidae, Hemiramphidae, Lutjanidae (I), Microdesmidae (I), Nemipteridae (I), Pempherididae (I), Pomacentridae (3), Pseudochromidae (4), Schindleri- idae (I), Tripterygiidae. In contrast, many reef fishes (from 31 families) were found not to complete their pelagic phase in the lagoons. Thus, only a few fish taxa are capable of completing their life cycles in atoll lagoons, but larvae of most of those that do are abundant, These taxa have predominately closed populations, demonstrating that, contrary to the current paradigm, not all coral reef fishes live in predominately open populations. Although these taxa have closed lagoonal populations over ecological time scales, the wide distribution of the taxa and the ephemeral nature of atoll lagoons make it unlikely they have closed populations over evolutionary time scales, During the pelagic larval phase which characterizes nearly all bony fishes of coral reefs (Leis, 1991a), wide dispersal from the natal reef is possible. This possibility has led most reef-fish ecologists to conclude that reef fishes live in predominately open populations (Sale, 1980; Doherty, 1991)-i.e., that the propa- gules originating from a population of fishes on a given coral reef do not settle back into that population at the end of the pelagic phase, but rather that successful settlers on that reef originate from another reef. However, considerable debate has taken place in the last few years over the degree to which pelagic larvae may indeed return to their natal reef either actively or passively (summarized by Leis, 1991a; Victor, 1991). Some workers have speculated that atoll lagoons may be important, retentive "nursery grounds" for larvae of reef fishes (Johannes, 1978; Leis, 1986b; Colin and Bell, 1991), but the role of atoll lagoons in the pelagic phase of reef fishes has not been adequately investigated (Leis, 1986b, 1991a). If these semi- to fully- enclosed bodies of water serve as nurseries for larvae, then some of the populations of fishes on atolls are not predominately open, and the pelagic larvae will indeed settle back into the populations from which they originated. In this sense, an atoll lagoon would be analogous to a freshwater lake-dispersal can take place outside the system (via open ocean or stream, respectively), but the vast majority of settlement and recruitment would be back to the natal population with little or no recruitment originating from elsewhere. It would be useful to have both a list of species known to have such closed, lagoonal populations, and a list of species known to require non-lagoon conditions during their pelagic phase, and presum- ably less likely to have closed populations. 206 LEIS: LAGOON LARVAE 207 The term lagoon is used in a number of widely different senses, so definition and characterization are necessary. An atoll lagoon is a body of marine water enclosed to a greater or lesser extent by the coral reefs which make up the atoll. Usually, the atoll rises atop a volcanic base from oceanic depths and is separated from other atolls and reefs by very deep water. The atoll coral reefs mayor may not have emergent land upon them. Atoll lagoons vary from less than I km2 to more than 200 km2 in surface area and from a few meters to more than 60 m in depth. Some atoll lagoons are entirely surrounded by reef or emergent land, but most maintain some contact with the surrounding ocean either over the reef flat, or through channels or gaps in the reef of varying depth and width. Atoll lagoons are common in the Indo- Pacific, but uncommon in the Atlantic and eastern Pacific. However, non-atoll coral reefs in all oceans enclose numerous lagoons of varying morphologies, and it is likely their larval fish nursery function will be similar to that of atoll lagoons. The invertebrate zooplankton of atoll lagoons has been studied frequently, but fish larvae have seldom been considered, and when they were, with very few exceptions (Leis, 1991a) the fish larvae were not identified beyond Class level. It was the purpose of this study to identify the types of reef fishes that complete the pelagic portion of their life history within the lagoons of two atolls (Osprey Reef and Holmes Reefs, Fig. 1) in the western Coral Sea off the Great Barrier Reef of Australia, and thus have predominately closed populations in these lagoons. I also wished to assess which species do not complete their pelagic phase within these lagoons. This was done by plankton sampling in the lagoons of these atolls, and in the ocean surrounding them. To conclude that the pelagic phase is completed in the lagoon, it is necessary to capture within the lagoon the full range of sizes of the pelagic phase, of course within the capabilities of the sampling gear. If the size range of a species in the lagoon does not cover the full size range, but is greater than that taken outside the lagoon, a conclusion that the species may be completing its pelagic phase in the lagoon is justified. If sampling outside the lagoon (using identical methods) establishes that larvae outside the size range taken in the lagoon are present, then a conclusion of probable non-completion in the lagoon isjustified. Obviously, no conclusion can be reached about taxa not sampled. Therefore, the resulting lists of species which are or are not completing their pelagic phase in atoll lagoons are minimum and incomplete, but will identify some species which have predominately closed populations, and some species which are perhaps more likely to have open populations because they spend their pelagic phase in open waters. This method of partial assessment is necessary because it was not possible to remain at these remote atolls (which lack emergent land) and sample throughout the year. At best, only a few days sampling at a lagoon was possible on each cruise, and the number of cruises was necessarily limited by logistic considerations. However, two atolls of very different form, size and extent of contact with the surrounding ocean were sampled, and one was visited twice. Therefore, while a fully-balanced sampling design covering a variety of atoll lagoon types was not achieved, to the extent that similar results were attained in each lagoon, there is reason to expect that the results have some generality. MATERIALS AND METHODS Study Area. - Osprey Reef and Holmes Reefs, two atolls in the western Coral Sea (Fig. I, Table I), were sampled on three cruises. The reefs, on the submerged Queensland Plateau, are surrounded by 208 BULLETIN OF MARINE SCIENCE, VOL. 54, NO.1, 1994 Osprey Reef -+N 640 10 km Holmes Reefs 665 I o 10 km Figure 1. Chart of Osprey Reef(top) and Holmes Reefs (bottom). Inset shows location in the western Coral Sea, Numbers are published depths in m. At Holmes Reefs, the lagoon of the eastern reef was sampled: along the western edge of the eastern reefis a submerged ridge (ca. 20 m depth) with a series LEIS: LAGOON LARVAE 209 Table I. Physical characteristics of the two atoll lagoons studied Osprey Reef Holmes Reefs 13'53'S 16'28'S Position 146'35'E 147'53'E Distance off Great Barrier Reef (km) 150 180 Approximate lagoon area (km2) 170 50 Maximum lagoon depth (m) 43 45 Lagoon Enclosed* Opent t Nearly continuous reef; at least one, deep (10-15 m) channel, possibly others . • Western edge a submerged ridge ca. 20 m deep with some patch reefs extending to surface. depths in excess of 2,000 m and lie more than 150 km off the Great Barrier Reef which is situated on the Australian continental shelf. Aside from two small, unvegetated sand cays on the western of the two Holmes Reefs, neither of the reef systems have any emergent land. The studied, eastern portion of Holmes Reefs is separated from the western portion by depths in excess of 600 m. Neither of the reef systems is well charted, and the text descriptions, Table I and Figure I are based on the meager charts available and observations made during the three cruises. The studied lagoons are of similar depth, but vary considerably in size and morphology. The large lagoon at Osprey Reef is enclosed by nearly continuous near-surface reefs, and is connected to the ocean by at least one channel of 10-15 m depth. The smaller lagoon of east Holmes Reef is enclosed on three sides by near-surface reefs, but its western border is a ridge of approximately 20 m depth crowned with a line of near-surface patch reefs.
Recommended publications
  • This Keyword List Contains Indian Ocean Place Names of Coral Reefs, Islands, Bays and Other Geographic Features in a Hierarchical Structure
    CoRIS Place Keyword Thesaurus by Ocean - 8/9/2016 Indian Ocean This keyword list contains Indian Ocean place names of coral reefs, islands, bays and other geographic features in a hierarchical structure. For example, the first name on the list - Bird Islet - is part of the Addu Atoll, which is in the Indian Ocean. The leading label - OCEAN BASIN - indicates this list is organized according to ocean, sea, and geographic names rather than country place names. The list is sorted alphabetically. The same names are available from “Place Keywords by Country/Territory - Indian Ocean” but sorted by country and territory name. Each place name is followed by a unique identifier enclosed in parentheses. The identifier is made up of the latitude and longitude in whole degrees of the place location, followed by a four digit number. The number is used to uniquely identify multiple places that are located at the same latitude and longitude. For example, the first place name “Bird Islet” has a unique identifier of “00S073E0013”. From that we see that Bird Islet is located at 00 degrees south (S) and 073 degrees east (E). It is place number 0013 at that latitude and longitude. (Note: some long lines wrapped, placing the unique identifier on the following line.) This is a reformatted version of a list that was obtained from ReefBase. OCEAN BASIN > Indian Ocean OCEAN BASIN > Indian Ocean > Addu Atoll > Bird Islet (00S073E0013) OCEAN BASIN > Indian Ocean > Addu Atoll > Bushy Islet (00S073E0014) OCEAN BASIN > Indian Ocean > Addu Atoll > Fedu Island (00S073E0008)
    [Show full text]
  • Lagoons and Coastal Wetlands in the Global Change Context: Impacts and Management Issues
    LAGOONS AND COASTAL WETLANDS IN THE GLOBAL CHANGE CONTEXT: IMPACTS AND MANAGEMENT ISSUES International Conference 1. Title of the Project International Conference: “Lagoons and coastal wetlands in the global change context: Impacts and management issues” Venice, July 2003 Starting date: January 2003 2. Objectives of the Project The objective of the present project is to organise and hold an international conference to respond to the challenge of integrating global change issues in wetland management. The conference will have a multidisciplinary view and will be based on high level scientific expertise. The aim is to identify gaps, problems and success in wetland knowledge and management. CORILA is an association between the University of Padua, the University of Venice, the University Institute of Architecture in Venice and the National Research Council, for coordinating and managing the research on the Venice Lagoon system. CORILA is presently managing a large multidisciplinary scientific project on the lagoon of Venice which embraces biology, chemistry, morphology, modelling, architecture and economics and is networking 70 research bodies and institutions. CORILA is in constant dialogue with the Public Administrations and promotes the dissemination of the results of the research to the policy makers. CORILA stipulated an agreement with the UNESCO, Regional Office for Science and Technology, Venice, Italy for the promotion and coordination of scientific research on Venice lagoon system and coastal wetlands. UNESCO, Regional Office for Science and Technology, Venice, Italy has large competencies in wetlands and lagoons conservation, and particularly in the safeguarding of the Venice Lagoon. It is member of MARS (European marine research stations network) and promoter of MAB (Man and the biosphere world network) which promotes and demonstrates a balanced relationship between people and nature.
    [Show full text]
  • Assessing Long-Term Changes in the Beach Width of Reef Islands Based on Temporally Fragmented Remote Sensing Data
    Remote Sens. 2014, 6, 6961-6987; doi:10.3390/rs6086961 OPEN ACCESS remote sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Assessing Long-Term Changes in the Beach Width of Reef Islands Based on Temporally Fragmented Remote Sensing Data Thomas Mann 1,* and Hildegard Westphal 1,2 1 Leibniz Center for Tropical Marine Ecology, Fahrenheitstrasse 6, D-28359 Bremen, Germany; E-Mail: [email protected] 2 Department of Geosciences, University of Bremen, D-28359 Bremen, Germany * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +49-421-2380-0132; Fax: +49-421-2380-030. Received: 30 May 2014; in revised form: 7 July 2014 / Accepted: 18 July 2014 / Published: 25 July 2014 Abstract: Atoll islands are subject to a variety of processes that influence their geomorphological development. Analysis of historical shoreline changes using remotely sensed images has become an efficient approach to both quantify past changes and estimate future island response. However, the detection of long-term changes in beach width is challenging mainly for two reasons: first, data availability is limited for many remote Pacific islands. Second, beach environments are highly dynamic and strongly influenced by seasonal or episodic shoreline oscillations. Consequently, remote-sensing studies on beach morphodynamics of atoll islands deal with dynamic features covered by a low sampling frequency. Here we present a study of beach dynamics for nine islands on Takú Atoll, Papua New Guinea, over a seven-decade period. A considerable chronological gap between aerial photographs and satellite images was addressed by applying a new method that reweighted positions of the beach limit by identifying “outlier” shoreline positions.
    [Show full text]
  • Ecological Characterization of Bioluminescence in Mangrove Lagoon, Salt River Bay, St. Croix, USVI
    Ecological Characterization of Bioluminescence in Mangrove Lagoon, Salt River Bay, St. Croix, USVI James L. Pinckney (PI)* Dianne I. Greenfield Claudia Benitez-Nelson Richard Long Michelle Zimberlin University of South Carolina Chad S. Lane Paula Reidhaar Carmelo Tomas University of North Carolina - Wilmington Bernard Castillo Kynoch Reale-Munroe Marcia Taylor University of the Virgin Islands David Goldstein Zandy Hillis-Starr National Park Service, Salt River Bay NHP & EP 01 January 2013 – 31 December 2013 Duration: 1 year * Contact Information Marine Science Program and Department of Biological Sciences University of South Carolina Columbia, SC 29208 (803) 777-7133 phone (803) 777-4002 fax [email protected] email 1 TABLE OF CONTENTS INTRODUCTION ............................................................................................................................................... 4 BACKGROUND: BIOLUMINESCENT DINOFLAGELLATES IN CARIBBEAN WATERS ............................................... 9 PROJECT OBJECTIVES ..................................................................................................................................... 19 OBJECTIVE I. CONFIRM THE IDENTIY OF THE BIOLUMINESCENT DINOFLAGELLATE(S) AND DOMINANT PHYTOPLANKTON SPECIES IN MANGROVE LAGOON ........................................................................ 22 OBJECTIVE II. COLLECT MEASUREMENTS OF BASIC WATER QUALITY PARAMETERS (E.G., TEMPERATURE, SALINITY, DISSOLVED O2, TURBIDITY, PH, IRRADIANCE, DISSOLVED NUTRIENTS) FOR CORRELATION WITH PHYTOPLANKTON
    [Show full text]
  • The State of Lagoon Treatment in Missouri
    FEATURE Review by Phil Walsack The State Of Lagoon Treatment In Missouri Missouri has more than 900 Facts And Figures Left: Pacific’s new lagoon aeration system municipal governments, and many own was designed by Burns & McDonnell in 2019. The design flow of these 334 systems Right: Clarence’s lagoon in winter. Achieving and operate their wastewater systems. combined is 53.8 million gallons per ammonia compliance can be difficult when In addition to municipal ownership day (MGD) with actual flows of 37.3 the winter arrives. (cities, towns, and villages), public MGD. While most consider lagoon sewer districts and county governments technology a “smaller city” wastewater own an additional 124 systems. It is not solution, six cities discharge more than balance of discharging lagoons. While common knowledge, but there are more 1.0 MGD. Five of the six cities serve the number of communities is large, wastewater permits (called National more than 7,000 people. The six cities the population served is only 184,000. Pollutant Discharge Elimination System (with seven discharge permits) have a These smaller entities have a combined Permits or State Operating Permits) than combined design flow of 12.4 MGD, and design flow of 34.1 MGD and an there are communities; some entities an actual flow of 9.1 MGD. Overall, the actual flow of 23.2 MGD. Interestingly, may have more than one wastewater larger lagoon discharging communities actual flows are decreasing as the facility. represent 59,300 people. rural populations continue to move to Generally, wastewater treatment urban living environments. Permitted There are only 12 additional technologies can be divided into four actual flows are decreasing even though cities greater than 3,000 population major categories, including: mechanical; smaller systems have difficult inflow and discharging effluent from a lagoon lagoon; community septics; and non- infiltration (I&I) issues to solve.
    [Show full text]
  • Section 3.5 Marine Biology
    3.5 MARINE BIOLOGY 3.5.1 Introduction 3.5.1.1 Definition of Resource For purposes of this EIS/OEIS, marine biological resources are defined as marine flora and fauna and habitats that they occupy, occurring within the Point Mugu Sea Range, Mugu Lagoon, and the intertidal and nearshore environment of San Nicolas Island and Point Mugu. This section specifically addresses marine invertebrates and flora. Fish and sea turtles are addressed in Section 3.6, marine mammals are addressed in Section 3.7, and seabirds are addressed in Section 3.8. Threatened and endangered species, as defined by the U.S. Fish and Wildlife Service (USFWS), are also addressed. Species that are federally listed are afforded a degree of regulatory protection, which entails a permitting process including specific mitigation measures for any allowable (incidental) impacts on the species. Species that are proposed to be listed by the USFWS are treated similarly to listed species by that agency; recommendations of the USFWS, however, are advisory rather than mandatory in the case of proposed species. A federally listed endangered species is defined as any species, including subspecies, that is “in danger of extinction throughout all or a significant portion of its range.” A federally listed threatened species is defined as any species “likely to become an endangered species within the foreseeable future throughout all or a significant portion of its range.” “Proposed” endangered or threatened species are those species for which a proposed regulation has been published in the Federal Register, but a final rule has not yet been issued. 3.5.1.2 Regional Setting The Sea Range straddles the ocean off Point Conception which is considered a major geographic feature that affects marine biological diversity.
    [Show full text]
  • Habs in UPWELLING SYSTEMS
    GEOHAB CORE RESEARCH PROJECT: HABs IN UPWELLING SYSTEMS 1 GEOHAB GLOBAL ECOLOGY AND OCEANOGRAPHY OF HARMFUL ALGAL BLOOMS GEOHAB CORE RESEARCH PROJECT: HABS IN UPWELLING SYSTEMS AN INTERNATIONAL PROGRAMME SPONSORED BY THE SCIENTIFIC COMMITTEE ON OCEANIC RESEARCH (SCOR) AND THE INTERGOVERNMENTAL OCEANOGRAPHIC COMMISSION (IOC) OF UNESCO EDITED BY: G. PITCHER, T. MOITA, V. TRAINER, R. KUDELA, P. FIGUEIRAS, T. PROBYN BASED ON CONTRIBUTIONS BY PARTICIPANTS OF THE GEOHAB OPEN SCIENCE MEETING ON HABS IN UPWELLING SYSTEMS AND THE GEOHAB SCIENTIFIC STEERING COMMITTEE February 2005 3 This report may be cited as: GEOHAB 2005. Global Ecology and Oceanography of Harmful Algal Blooms, GEOHAB Core Research Project: HABs in Upwelling Systems. G. Pitcher, T. Moita, V. Trainer, R. Kudela, P. Figueiras, T. Probyn (Eds.) IOC and SCOR, Paris and Baltimore. 82 pp. This document is GEOHAB Report #3. Copies may be obtained from: Edward R. Urban, Jr. Henrik Enevoldsen Executive Director, SCOR Programme Co-ordinator Department of Earth and Planetary Sciences IOC Science and Communication Centre on The Johns Hopkins University Harmful Algae Baltimore, MD 21218 U.S.A. Botanical Institute, University of Copenhagen Tel: +1-410-516-4070 Øster Farimagsgade 2D Fax: +1-410-516-4019 DK-1353 Copenhagen K, Denmark E-mail: [email protected] Tel: +45 33 13 44 46 Fax: +45 33 13 44 47 E-mail: [email protected] This report is also available on the web at: http://www.jhu.edu/scor/ http://ioc.unesco.org/hab ISSN 1538-182X Cover photos courtesy of: Vera Trainer Teresa Moita Grant Pitcher Copyright © 2005 IOC and SCOR.
    [Show full text]
  • The Contribution of Wind-Generated Waves to Coastal Sea-Level Changes
    1 Surveys in Geophysics Archimer November 2011, Volume 40, Issue 6, Pages 1563-1601 https://doi.org/10.1007/s10712-019-09557-5 https://archimer.ifremer.fr https://archimer.ifremer.fr/doc/00509/62046/ The Contribution of Wind-Generated Waves to Coastal Sea-Level Changes Dodet Guillaume 1, *, Melet Angélique 2, Ardhuin Fabrice 6, Bertin Xavier 3, Idier Déborah 4, Almar Rafael 5 1 UMR 6253 LOPSCNRS-Ifremer-IRD-Univiversity of Brest BrestPlouzané, France 2 Mercator OceanRamonville Saint Agne, France 3 UMR 7266 LIENSs, CNRS - La Rochelle UniversityLa Rochelle, France 4 BRGMOrléans Cédex, France 5 UMR 5566 LEGOSToulouse Cédex 9, France *Corresponding author : Guillaume Dodet, email address : [email protected] Abstract : Surface gravity waves generated by winds are ubiquitous on our oceans and play a primordial role in the dynamics of the ocean–land–atmosphere interfaces. In particular, wind-generated waves cause fluctuations of the sea level at the coast over timescales from a few seconds (individual wave runup) to a few hours (wave-induced setup). These wave-induced processes are of major importance for coastal management as they add up to tides and atmospheric surges during storm events and enhance coastal flooding and erosion. Changes in the atmospheric circulation associated with natural climate cycles or caused by increasing greenhouse gas emissions affect the wave conditions worldwide, which may drive significant changes in the wave-induced coastal hydrodynamics. Since sea-level rise represents a major challenge for sustainable coastal management, particularly in low-lying coastal areas and/or along densely urbanized coastlines, understanding the contribution of wind-generated waves to the long-term budget of coastal sea-level changes is therefore of major importance.
    [Show full text]
  • Upwelling As a Source of Nutrients for the Great Barrier Reef Ecosystems: a Solution to Darwin's Question?
    Vol. 8: 257-269, 1982 MARINE ECOLOGY - PROGRESS SERIES Published May 28 Mar. Ecol. Prog. Ser. / I Upwelling as a Source of Nutrients for the Great Barrier Reef Ecosystems: A Solution to Darwin's Question? John C. Andrews and Patrick Gentien Australian Institute of Marine Science, Townsville 4810, Queensland, Australia ABSTRACT: The Great Barrier Reef shelf ecosystem is examined for nutrient enrichment from within the seasonal thermocline of the adjacent Coral Sea using moored current and temperature recorders and chemical data from a year of hydrology cruises at 3 to 5 wk intervals. The East Australian Current is found to pulsate in strength over the continental slope with a period near 90 d and to pump cold, saline, nutrient rich water up the slope to the shelf break. The nutrients are then pumped inshore in a bottom Ekman layer forced by periodic reversals in the longshore wind component. The period of this cycle is 12 to 25 d in summer (30 d year round average) and the bottom surges have an alternating onshore- offshore speed up to 10 cm S-'. Upwelling intrusions tend to be confined near the bottom and phytoplankton development quickly takes place inshore of the shelf break. There are return surface flows which preserve the mass budget and carry silicate rich Lagoon water offshore while nitrogen rich shelf break water is carried onshore. Upwelling intrusions penetrate across the entire zone of reefs, but rarely into the Lagoon. Nutrition is del~veredout of the shelf thermocline to the living coral of reefs by localised upwelling induced by the reefs.
    [Show full text]
  • Pacific Remote Islands Marine National Monument
    U.S. Fish & Wildlife Service Pacific Remote Islands Marine National Monument The Pacific Remote Islands Marine National Monument falls within the Central Pacific Ocean, ranging from Wake Atoll in the northwest to Jarvis Island in the southeast. The seven atolls and islands included within the monument are farther from human population centers than any other U.S. area. They represent one of the last frontiers and havens for wildlife in the world, and comprise the most widespread collection of coral reef, seabird, and shorebird protected areas on the planet under a single nation’s jurisdiction. At Howland Island, Baker Island, Jarvis Island, Palmyra Atoll, and Kingman Reef, the terrestrial areas, reefs, and waters out to 12 nautical miles (nmi) are part of the National Wildlife Refuge System. The land areas at Wake Atoll and Johnston Atoll remain under the jurisdiction of The giant clam, Tridacna gigas, is a clam that is the largest living bivalve mollusk. the U.S. Air Force, but the waters from Photo: © Kydd Pollock 0 to 12 nmi are protected as units of the National Wildlife Refuge System. For all of the areas, fishery-related Marine National Monument, and orders long time periods throughout their entire activities seaward from the 12-nmi refuge of magnitude greater than the reefs near cultural and geological history. These boundaries out to the 50-nmi monument heavily populated islands. Expansive refuges are unique in that they were and boundary are managed by the National shallow coral reefs and deep coral forests, are still largely pristine, though many Oceanic and Atmospheric Administration.
    [Show full text]
  • Bolinas Lagoon Ecosystem Restoration Feasibility Project
    Bolinas Lagoon Ecosystem Restoration Feasibility Project Marin County Open Space District With Funding from the California State Coastal Conservancy & the U.S. Army Corps of Engineers July 2006 Bolinas Lagoon Ecosystem Restoration Feasibility Project Final Public Reports Table of Contents Volume I I Executive Summary II Projecting the Future of Bolinas Lagoon ¢¡¤£ ¥ £ ¦¨§©£ ¥ ¥ £ ¤£ ¢ Volume II III Recent (1850-2005) and late Holocene (400-1850) Sedimentation Rates at Bolinas Lagoon ¤!#"%$&" '(!)*+#, - ./1032#4 5(276 2#8 IV Conceptual Littoral Sediment Budget 9¢:¤; < ; =¨>©; < < ; ? @ABCAA D¤E; ? F GA V Project Reformulation Advisory Committee Summary of Draft Public Report S S TT H¢I¢J%KMLN7OPORQ VI Peer Review and Public Comments on Previous Drafts Reports with Responses U¢V¤W X W Y¨Z©W X X W [ \]^_]] `¤aW [ b c] de¢f a. Peer Reviews of Administrative Draft Report and Responses b. Public Comment Letters on Public Draft Report c. Response to Public Comment Letters Report Availability The report is available in multiple formats: • The report may be read and downloaded from www.marinopenspace.org • CDs are available on request by writing to William Carmen, Project Manager Bolinas Lagoon Ecosystem Restoration Feasibility Study MCOSD 3501 Civic Center Drive Suite 415 San Rafael, CA 94903 Or email: [email protected] • Hard copies of the report are on loan at the following locations: Marin County Library Branches: Bolinas, Stinson Beach, Civic Center, Fairfax, Inverness, Marin City, Novato, Pt. Reyes Station & San Geronimo Valley.
    [Show full text]
  • Assessment of the Aquatic Macrophytes and Algae of the Fosu Lagoon, Cape Coast
    Academic Research Publishing Group Academic Journal of Life Sciences ISSN: 2415-2137 Vol. 1 No. 1, pp: 14-19, 2015 URL: http://arpgweb.com/?ic=journal&journal=18&info=aims Assessment of the Aquatic Macrophytes and Algae of the Fosu Lagoon, Cape Coast. Ghana Felix Jerry Akpabey* Council for Scientific and Industrial Research -Water Research Institute. Environmental Biology and Health Division, P.O. Box AH 38, Achimota, Accra. Ghana Ruth Amole Council for Scientific and Industrial Research Water Research Institute. Environmental Biology and Health Division, P.O. Box AH 38, Achimota, Accra. Ghana Abstract: The Fosu Lagoon serves as a major ecological, economic and cultural (religious) significance to the inhabitants of the community. It provides livelihoods for local fishermen, as well as habitat for rare flora and fauna, is of key importance to the local climate and provided recreational opportunities for the inhabitants of Cape Coast. In recent years, increased human activities have led to deterioration of both fresh and coastal waters in many regions of the world. The Environmental Protection Agency of Ghana have rated the Fosu Lagoon as one such lagoon and is considered the third most polluted lagoon in Ghana after the Korle and Chemu lagoons. Climate change variability has been associated with declining water resources among other factors. Climate change studies in Ghana have shown that major basins in the country are already experiencing water stress and with increasing environmental deterioration, limited water availability and pollution would have tremendous negative impact on aquatic ecosystems including coastal waters such as lagoons. The study revealed that the Fosu Lagoon is covered with mats of mixed vegetation (with Paspalum vaginatum and Typha domingensis dominating) which grow around the banks and over shallow sections of the Lagoon and parts of the landing sites.
    [Show full text]