A Trophic Cascade Regulates Salt Marsh Primary Production
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The Systematics and Ecology of the Mangrove-Dwelling Littoraria Species (Gastropoda: Littorinidae) in the Indo-Pacific
ResearchOnline@JCU This file is part of the following reference: Reid, David Gordon (1984) The systematics and ecology of the mangrove-dwelling Littoraria species (Gastropoda: Littorinidae) in the Indo-Pacific. PhD thesis, James Cook University. Access to this file is available from: http://eprints.jcu.edu.au/24120/ The author has certified to JCU that they have made a reasonable effort to gain permission and acknowledge the owner of any third party copyright material included in this document. If you believe that this is not the case, please contact [email protected] and quote http://eprints.jcu.edu.au/24120/ THE SYSTEMATICS AND ECOLOGY OF THE MANGROVE-DWELLING LITTORARIA SPECIES (GASTROPODA: LITTORINIDAE) IN THE INDO-PACIFIC VOLUME I Thesis submitted by David Gordon REID MA (Cantab.) in May 1984 . for the Degree of Doctor of Philosophy in the Department of Zoology at James Cook University of North Queensland STATEMENT ON ACCESS I, the undersigned, the author of this thesis, understand that the following restriction placed by me on access to this thesis will not extend beyond three years from the date on which the thesis is submitted to the University. I wish to place restriction on access to this thesis as follows: Access not to be permitted for a period of 3 years. After this period has elapsed I understand that James Cook. University of North Queensland will make it available for use within the University Library and, by microfilm or other photographic means, allow access to users in other approved libraries. All uses consulting this thesis will have to sign the following statement: 'In consulting this thesis I agree not to copy or closely paraphrase it in whole or in part without the written consent of the author; and to make proper written acknowledgement for any assistance which I have obtained from it.' David G. -
Maritime Swamp Forest (Typic Subtype)
MARITIME SWAMP FOREST (TYPIC SUBTYPE) Concept: Maritime Swamp Forests are wetland forests of barrier islands and comparable coastal spits and back-barrier islands, dominated by tall trees of various species. The Typic Subtype includes most examples, which are not dominated by Acer, Nyssa, or Fraxinus, not by Taxodium distichum. Canopy dominants are quite variable among the few examples. Distinguishing Features: Maritime Shrub Swamps are distinguished from other barrier island wetlands by dominance by tree species of (at least potentially) large stature. The Typic Subtype is dominated by combinations of Nyssa, Fraxinus, Liquidambar, Acer, or Quercus nigra, rather than by Taxodium or Salix. Maritime Shrub Swamps are dominated by tall shrubs or small trees, particularly Salix, Persea, or wetland Cornus. Some portions of Maritime Evergreen Forest are marginally wet, but such areas are distinguished by the characteristic canopy dominants of that type, such as Quercus virginiana, Quercus hemisphaerica, or Pinus taeda. The lower strata also are distinctive, with wetland species occurring in Maritime Swamp Forest; however, some species, such as Morella cerifera, may occur in both. Synonyms: Acer rubrum - Nyssa biflora - (Liquidambar styraciflua, Fraxinus sp.) Maritime Swamp Forest (CEGL004082). Ecological Systems: Central Atlantic Coastal Plain Maritime Forest (CES203.261). Sites: Maritime Swamp Forests occur on barrier islands and comparable spits, in well-protected dune swales, edges of dune ridges, and on flats adjacent to freshwater sounds. Soils: Soils are wet sands or mucky sands, most often mapped as Duckston (Typic Psammaquent) or Conaby (Histic Humaquept). Hydrology: Most Maritime Swamp Forests have shallow seasonal standing water and nearly permanently saturated soils. Some may rarely be flooded by salt water during severe storms, but areas that are severely or repeatedly flooded do not recover to swamp forest. -
WMSDB - Worldwide Mollusc Species Data Base
WMSDB - Worldwide Mollusc Species Data Base Family: TURBINIDAE Author: Claudio Galli - [email protected] (updated 07/set/2015) Class: GASTROPODA --- Clade: VETIGASTROPODA-TROCHOIDEA ------ Family: TURBINIDAE Rafinesque, 1815 (Sea) - Alphabetic order - when first name is in bold the species has images Taxa=681, Genus=26, Subgenus=17, Species=203, Subspecies=23, Synonyms=411, Images=168 abyssorum , Bolma henica abyssorum M.M. Schepman, 1908 aculeata , Guildfordia aculeata S. Kosuge, 1979 aculeatus , Turbo aculeatus T. Allan, 1818 - syn of: Epitonium muricatum (A. Risso, 1826) acutangulus, Turbo acutangulus C. Linnaeus, 1758 acutus , Turbo acutus E. Donovan, 1804 - syn of: Turbonilla acuta (E. Donovan, 1804) aegyptius , Turbo aegyptius J.F. Gmelin, 1791 - syn of: Rubritrochus declivis (P. Forsskål in C. Niebuhr, 1775) aereus , Turbo aereus J. Adams, 1797 - syn of: Rissoa parva (E.M. Da Costa, 1778) aethiops , Turbo aethiops J.F. Gmelin, 1791 - syn of: Diloma aethiops (J.F. Gmelin, 1791) agonistes , Turbo agonistes W.H. Dall & W.H. Ochsner, 1928 - syn of: Turbo scitulus (W.H. Dall, 1919) albidus , Turbo albidus F. Kanmacher, 1798 - syn of: Graphis albida (F. Kanmacher, 1798) albocinctus , Turbo albocinctus J.H.F. Link, 1807 - syn of: Littorina saxatilis (A.G. Olivi, 1792) albofasciatus , Turbo albofasciatus L. Bozzetti, 1994 albofasciatus , Marmarostoma albofasciatus L. Bozzetti, 1994 - syn of: Turbo albofasciatus L. Bozzetti, 1994 albulus , Turbo albulus O. Fabricius, 1780 - syn of: Menestho albula (O. Fabricius, 1780) albus , Turbo albus J. Adams, 1797 - syn of: Rissoa parva (E.M. Da Costa, 1778) albus, Turbo albus T. Pennant, 1777 amabilis , Turbo amabilis H. Ozaki, 1954 - syn of: Bolma guttata (A. Adams, 1863) americanum , Lithopoma americanum (J.F. -
Delaware Bay Estuary Project Supporting the Conservation and Restoration Of
U.S. Fish & Wildlife Service – Coastal Program Delaware Bay Estuary Project Supporting the conservation and restoration of the salt marshes of Delaware Bay People have altered the expansive salt marshes of Delaware Bay for centuries to farm salt hay, try to control mosquitoes, create channels for boats, to increase developable land, and other reasons all resulting in restricted tidal flow, disrupted sediment balances, or increasing erosion. Sea level rise and coastal storms threaten to further negatively impact the integrity of these salt marshes. As we alter or lose the marshes we lose the valuable habitats and ecological services they provide. tidal creek - Katherine Whittemore Addressing the all-important sediment balance of salt marshes is critical for preserving their resilience. A healthy resilient marsh may be able to keep pace with erosion and sea level rise through sediment accretion and growth Downe Twsp, NJ - Brian Marsh of vegetation. However, the delicate sediment balance of salt marshes is DBEP works to support efforts to learn more about the techniques often disrupted by barriers to tidal influence and altered drainage onto and to conserve and restore salt marshes and support the populations of fish and wildlife that rely on them. We support new and off the marsh resulting in sediment ongoing coastal resiliency initiatives and coastal planning as they starved systems, excessive mudflats, or pertain to habitat restoration and conservation. We are interested increased erosion. in finding effective tools and mechanisms for conserving and restoring salt marsh integrity on a meaningful scale and support efforts that bring partners together to approach this challenge. -
Exploring Our Wonderful Wetlands Publication
Exploring Our Wonderful Wetlands Student Publication Grades 4–7 Dear Wetland Students: Are you ready to explore our wonderful wetlands? We hope so! To help you learn about several types of wetlands in our area, we are taking you on a series of explorations. As you move through the publication, be sure to test your wetland wit and write about wetlands before moving on to the next exploration. By exploring our wonderful wetlands, we hope that you will appreciate where you live and encourage others to help protect our precious natural resources. Let’s begin our exploration now! Southwest Florida Water Management District Exploring Our Wonderful Wetlands Exploration 1 Wading Into Our Wetlands ................................................Page 3 Exploration 2 Searching Our Saltwater Wetlands .................................Page 5 Exploration 3 Finding Out About Our Freshwater Wetlands .............Page 7 Exploration 4 Discovering What Wetlands Do .................................... Page 10 Exploration 5 Becoming Protectors of Our Wetlands ........................Page 14 Wetlands Activities .............................................................Page 17 Websites ................................................................................Page 20 Visit the Southwest Florida Water Management District’s website at WaterMatters.org. Exploration 1 Wading Into Our Wetlands What exactly is a wetland? The scientific and legal definitions of wetlands differ. In 1984, when the Florida Legislature passed a Wetlands Protection Act, they decided to use a plant list containing plants usually found in wetlands. We are very fortunate to have a lot of wetlands in Florida. In fact, Florida has the third largest wetland acreage in the United States. The term wetlands includes a wide variety of aquatic habitats. Wetland ecosystems include swamps, marshes, wet meadows, bogs and fens. Essentially, wetlands are transitional areas between dry uplands and aquatic systems such as lakes, rivers or oceans. -
Diamondback Terrapin Malaclemys Terrapin Contributors: Dubose Griffin, David Owens and J
Diamondback Terrapin Malaclemys terrapin Contributors: DuBose Griffin, David Owens and J. Whitfield Gibbons DESCRIPTION Taxonomy and Basic Description The diamondback terrapin is a small, long-lived estuarine turtle endemic to coastal marshes, estuarine bays, lagoons and creeks ranging from Cape Cod, Massachusetts to the Gulf Coast of Texas. Currently, there are five (Hartsell 2001) or seven (Ernst et al. 1994) subspecies. More recently, Hart (2004) identified six management units. The subspecies found in South Carolina is Malaclemys terrapin centrata. Terrapins have varied coloration from black to spotted patterns on the soft tissue and dark or light-colored scutes with strong concentric layers on the carapace. The hind margin of the carapace curls up instead of flaring. Hind legs are large and toes have extensive webs. These turtles are strong, fast swimmers that feed on a variety of mollusks, crustaceans and other invertebrates. In South Carolina, salt marsh periwinkles (Littoraria irrorata) and blue crabs (Callinectes sapidus) are among the terrapin’s primary food sources (Tucker et al. 1995; Levesque 2000). Terrapins are sexually dimorphic. Females are much larger than males and reach 15 to 18 cm (6 to7 inches) in length; males reach 10 to 13 cm (4 to 5 inches) in length. Adult females also have enlarged heads. Terrapins hibernate in the mud during winter and mate in the spring. Eggs are laid May through early August and clutches have 5 to 12 eggs (Pritchard 1979). The number of clutches laid per female in South Carolina is undocumented; however two clutches may be common (David Owens, College of Charleston, pers. -
The Annual Net Primary Production and Decomposition of the Salt Marsh Grass, Spartina Alterniflora, Loisel. in the Barataria Bay Estuary of Louisiana
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1971 The Annual Net Primary Production and Decomposition of the Salt Marsh Grass, Spartina Alterniflora, Loisel. In the Barataria Bay Estuary of Louisiana. Conrad Joseph Kirby Jr Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Kirby, Conrad Joseph Jr, "The Annual Net Primary Production and Decomposition of the Salt Marsh Grass, Spartina Alterniflora, Loisel. In the Barataria Bay Estuary of Louisiana." (1971). LSU Historical Dissertations and Theses. 2139. https://digitalcommons.lsu.edu/gradschool_disstheses/2139 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. INFORMATION TO USERS This dissertation was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1. The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. -
Life Cycle of Oil and Gas Fields in the Mississippi River Delta: a Review
water Review Life Cycle of Oil and Gas Fields in the Mississippi River Delta: A Review John W. Day 1,*, H. C. Clark 2, Chandong Chang 3 , Rachael Hunter 4,* and Charles R. Norman 5 1 Department of Oceanography and Coastal Sciences, Louisiana State University, Baton Rouge, LA 70803, USA 2 Department of Earth, Environmental and Planetary Science, Rice University, Houston, TX 77005, USA; [email protected] 3 Department of Geological Sciences, Chungnam National University, Daejeon 34134, Korea; [email protected] 4 Comite Resources, Inc., P.O. Box 66596, Baton Rouge, LA 70896, USA 5 Charles Norman & Associates, P.O. Box 5715, Lake Charles LA 70606, USA; [email protected] * Correspondence: [email protected] (J.W.D.); [email protected] (R.H.) Received: 20 April 2020; Accepted: 20 May 2020; Published: 23 May 2020 Abstract: Oil and gas (O&G) activity has been pervasive in the Mississippi River Delta (MRD). Here we review the life cycle of O&G fields in the MRD focusing on the production history and resulting environmental impacts and show how cumulative impacts affect coastal ecosystems. Individual fields can last 40–60 years and most wells are in the final stages of production. Production increased rapidly reaching a peak around 1970 and then declined. Produced water lagged O&G and was generally higher during declining O&G production, making up about 70% of total liquids. Much of the wetland loss in the delta is associated with O&G activities. These have contributed in three major ways to wetland loss including alteration of surface hydrology, induced subsidence due to fluids removal and fault activation, and toxic stress due to spilled oil and produced water. -
MUD CREATURE STUDY Overview: the Mudflats Support a Tremendous Amount of Life
MUD CREATURE STUDY Overview: The mudflats support a tremendous amount of life. In this activity, students will search for and study the creatures that live in bay mud. Content Standards Correlations: Science p. 307 Grades: K-6 TIME FRAME fOR TEACHING THIS ACTIVITY Key Concepts: Mud creatures live in high abundance in the Recommended Time: 30 minutes mudflats, providing food for Mud Creature Banner (7 minutes) migratory ducks and shorebirds • use the Mud Creature Banner to introduce students to mudflat and the endangered California habitat clapper rail. When the tide is out, Mudflat Food Pyramid (3 minutes) the mudflats are revealed and birds land on the mudflats to feed. • discuss the mudflat food pyramid, using poster Mud Creature Study (20 minutes) Objectives: • sieve mud in sieve set, using slough water Students will be able to: • distribute small samples of mud to petri dishes • name and describe two to three • look for mud creatures using hand lenses mud creatures • describe the mudflat food • use the microscopes for a closer view of mud creatures pyramid • if data sheets and pencils are provided, students can draw what • explain the importance of the they find mudflat habitat for migratory birds and endangered species Materials: How THIS ACTIVITY RELATES TO THE REFUGE'S RESOURCES Provided by the Refuge: What are the Refuge's resources? • 1 set mud creature ID cards • significant wildlife habitat • 1 mud creature flannel banner • endangered species • 1 mudflat food pyramid poster • 1 mud creature ID book • rhigratory birds • 1 four-layered sieve set What makes it necessary to manage the resources? • 1 dish of mud and trowel • Pollution, such as oil, paint, and household cleaners, when • 1 bucket of slough water dumped down storm drains enters the slough and mudflats and • 1 pitcher of slough water travels through the food chain, harming animals. -
Salt Marsh Monitoring by The
SaltSalt MarshMarsh MonitoringMonitoring byby thethe U.S.U.S. FishFish && WildlifeWildlife ServiceService’’ss NortheastNortheast RegionRegion Ralph Tiner Regional Wetland Coordinator U.S. Fish and Wildlife Service-Northeast Region February 2010 TypesTypes ofof MonitoringMonitoring RemotelyRemotely sensedsensed MonitoringMonitoring Area and type changes (e.g., trends analysis) Can cover large or small areas OnOn--thethe--groundground MonitoringMonitoring Addressing processes (accretion, erosion, subsidence, salt balance, etc.) Analyzing vegetation and soil changes Plot analysis Reference wetlands Evaluating wildlife habitat RemotelyRemotely SensedSensed MonitoringMonitoring NWINWI usesuses aerialaerial imageryimagery toto tracktrack wetlandwetland changeschanges inin wetlandwetland typetype WetlandWetland StatusStatus && TrendsTrends StudiesStudies == aa typetype ofof monitoringmonitoring For large geographic areas Statistical Sampling – analyze changes in 4-square mile plots; generate estimates For small areas Area-based Analysis –analyze complete area for changes over time RegionRegion vsvs LocalLocal ReportsReports CanfieldCanfield Cove,Cove, CTCT 19741974 20042004 Canfield Island Cove 60 50 40 s e 30 Acr 20 10 0 1974 1981 1986 1990 1995 2000 2004 Low Marsh High Marsh Flat ConsiderationsConsiderations forfor SiteSite--specificspecific MonitoringMonitoring SpecialSpecial aerialaerial imageryimagery LowLow tidetide PeakPeak ofof growinggrowing seasonseason NormalNormal issuesissues re:re: qualityquality (e.g.,(e.g., -
Ecology of Freshwater and Estuarine Wetlands: an Introduction
ONE Ecology of Freshwater and Estuarine Wetlands: An Introduction RebeCCA R. SHARITZ, DAROLD P. BATZER, and STeveN C. PENNINGS WHAT IS A WETLAND? WHY ARE WETLANDS IMPORTANT? CHARACTERISTicS OF SeLecTED WETLANDS Wetlands with Predominantly Precipitation Inputs Wetlands with Predominately Groundwater Inputs Wetlands with Predominately Surface Water Inputs WETLAND LOSS AND DeGRADATION WHAT THIS BOOK COVERS What Is a Wetland? The study of wetland ecology can entail an issue that rarely Wetlands are lands transitional between terrestrial and needs consideration by terrestrial or aquatic ecologists: the aquatic systems where the water table is usually at or need to define the habitat. What exactly constitutes a wet- near the surface or the land is covered by shallow water. land may not always be clear. Thus, it seems appropriate Wetlands must have one or more of the following three to begin by defining the wordwetland . The Oxford English attributes: (1) at least periodically, the land supports predominately hydrophytes; (2) the substrate is pre- Dictionary says, “Wetland (F. wet a. + land sb.)— an area of dominantly undrained hydric soil; and (3) the substrate is land that is usually saturated with water, often a marsh or nonsoil and is saturated with water or covered by shallow swamp.” While covering the basic pairing of the words wet water at some time during the growing season of each year. and land, this definition is rather ambiguous. Does “usu- ally saturated” mean at least half of the time? That would This USFWS definition emphasizes the importance of omit many seasonally flooded habitats that most ecolo- hydrology, soils, and vegetation, which you will see is a gists would consider wetlands. -
Noaa 28815 DS1.Pdf
Science of the Total Environment 718 (2020) 137181 Contents lists available at ScienceDirect Science of the Total Environment journal homepage: www.elsevier.com/locate/scitotenv Sea-level rise thresholds for stability of salt marshes in a riverine versus a marine dominated estuary Wei Wu a,⁎, Patrick Biber a, Deepak R. Mishra b, Shuvankar Ghosh c a Division of Coastal Sciences, School of Ocean Science and Engineering, The University of Southern Mississippi, 703 East Beach Dr., Ocean Springs, MS 39564, USA b Center for Geospatial Research, Department of Geography, University of Georgia, Athens, GA 30602, USA c Department of Geospatial Monitoring and Information Technology, French Institute of Pondicherry (IFP), 11, St Louis St, White Town, Puducherry 605001, India HIGHLIGHTS GRAPHICAL ABSTRACT • Salt marshes are more resilient to sea- level rise in estuary with larger river input. • The higher resilience is mainly due to more riverine-borne mineral sediments. • Sea-level rise thresholds are more sensi- tive to biomass in a marine dominated estuary. • Biomass & sediment affect sea-level rise thresholds alike in river-dominated es- tuary. • Belowground biomass contributes more to accretion in estuary with limited river input. article info abstract Article history: We studied the ecological resilience of salt marshes by deriving sea level rise (SLR) thresholds in two estuaries Received 16 September 2019 with contrasting upland hydrological inputs in the north-central Gulf of Mexico: Grand Bay National Estuarine Received in revised form 5 February 2020 Research Reserve (NERR) with limited upland input, and the Pascagoula River delta drained by the Pascagoula Accepted 6 February 2020 River, the largest undammed river in the continental United States.