Nearshore Movement Ecology of a Medium-Bodied Shark, the Creek Whaler Carcharhinus Fitzroyensis
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Ovarian Development of the Mud Crab Scylla Paramamosain in a Tropical Mangrove Swamps, Thailand
Available Online JOURNAL OF SCIENTIFIC RESEARCH Publications J. Sci. Res. 2 (2), 380-389 (2010) www.banglajol.info/index.php/JSR Ovarian Development of the Mud Crab Scylla paramamosain in a Tropical Mangrove Swamps, Thailand M. S. Islam1, K. Kodama2, and H. Kurokura3 1Department of Aquaculture and Fisheries, Jessore Science and Technology University, Jessore- 7407, Bangladesh 2Marine Science Institute, The University of Texas at Austin, Channel View Drive, Port Aransas, Texas 78373, USA 3Laboratory of Global Fisheries Science, Department of Global Agricultural Sciences, The University of Tokyo, Bunkyo, Tokyo 113-8657, Japan Received 15 October 2009, accepted in revised form 21 March 2010 Abstract The present study describes the ovarian development stages of the mud crab, Scylla paramamosain from Pak Phanang mangrove swamps, Thailand. Samples were taken from local fishermen between June 2006 and December 2007. Ovarian development was determined based on both morphological appearance and histological observation. Ovarian development was classified into five stages: proliferation (stage I), previtellogenesis (II), primary vitellogenesis (III), secondary vitellogenesis (IV) and tertiary vitellogenesis (V). The formation of vacuolated globules is the initiation of primary vitellogenesis and primary growth. The follicle cells were found around the periphery of the lobes, among the groups of oogonia and oocytes. The follicle cells were hardly visible at the secondary and tertiary vitellogenesis stages. Yolk granules occurred in the primary vitellogenesis stage and are first initiated in the inner part of the oocytes, then gradually concentrated to the periphery of the cytoplasm. The study revealed that the initiation of vitellogenesis could be identified by external observation of the ovary but could not indicate precisely. -
Alternative Stable States of Tidal Marsh Vegetation Patterns and Channel Complexity
ECOHYDROLOGY Ecohydrol. (2016) Published online in Wiley Online Library (wileyonlinelibrary.com) DOI: 10.1002/eco.1755 Alternative stable states of tidal marsh vegetation patterns and channel complexity K. B. Moffett1* and S. M. Gorelick2 1 School of the Environment, Washington State University Vancouver, Vancouver, WA, USA 2 Department of Earth System Science, Stanford University, Stanford, CA, USA ABSTRACT Intertidal marshes develop between uplands and mudflats, and develop vegetation zonation, via biogeomorphic feedbacks. Is the spatial configuration of vegetation and channels also biogeomorphically organized at the intermediate, marsh-scale? We used high-resolution aerial photographs and a decision-tree procedure to categorize marsh vegetation patterns and channel geometries for 113 tidal marshes in San Francisco Bay estuary and assessed these patterns’ relations to site characteristics. Interpretation was further informed by generalized linear mixed models using pattern-quantifying metrics from object-based image analysis to predict vegetation and channel pattern complexity. Vegetation pattern complexity was significantly related to marsh salinity but independent of marsh age and elevation. Channel complexity was significantly related to marsh age but independent of salinity and elevation. Vegetation pattern complexity and channel complexity were significantly related, forming two prevalent biogeomorphic states: complex versus simple vegetation-and-channel configurations. That this correspondence held across marsh ages (decades to millennia) -
The Evolution of the Artificial Wildbird Tidal Mudflat in Fukuoka, Japan
1 The Evolution of the MIA DOCTO + SCOTT WALLS Jacob Bintliff, Mariana Chavez, Daniela Peña Corvillon, Artificial Wildbird Tidal Johanna Hoffman, Katelyn Walker, UC Berkeley, LA 205 Studio Mudflat in Fukuoka, Japan Spring 2012 2 PRESENTATION CONTENT INTRODUCTION // SCIENTIFIC ANALYSIS // WETLAND DESIGN // HUMAN INTERFACE // CONCLUSIONS 3 CONTEXT 4 5 6 CONTEXT BEFORE PRESENT 7 ISLAND CITY 8 9 ITERATIONS ORIGINAL WETLAND PLAN 10 ITERATIONS JAPAN STUDENT WORKSHOP 11 ITERATIONS 2008 Land Use Plan ~8.5 - 9 ha ~12 ha ~10 ha ~10 ~7 ha Setup of the central area ~8.75 ha ~38.25 ha We will establish a lively ~7 ha interactive space by inviting urban functions such as commercial and ~ 6.75 ha corporate functions, and dissemination of information on education, ~2.25 ha Wild Bird Park 3.9 ha 3.1 ha School and Amenities culture, and art. Further, public transportation Green Space facilities and facilities for 4.1 ha convenience are invited Assigned Facilities Teriha Town to improve the business Hospital ~18 ha environment in the area. Apartments 4.1+ ha Joint Independent Houses Spcialist Clinic 1.8 ha ~1.5 ha Commercial Elderly Elderly Center? Center Planned Subdivision 1.6 ha 1.2 ha Coporate (Sold) 0.9 ha Planned Use/Mixed Use Idustrial and hatches based on legend color code and denote use type Research & Development Currently Built Port Warf 1000 m UC BERKELEY LAND USE PLAN 12 ITERATIONS UC BERKELEY LAND USE PLAN 13 ITERATIONS 16 Hectare Wild Bird Park UC BERKELEY - JAPAN WETLAND DESIGN 14 DESIGN GOALS Provide natural habitat for migrating bird species -
Sediment Transport in the San Francisco Bay Coastal System: an Overview
Marine Geology 345 (2013) 3–17 Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margeo Sediment transport in the San Francisco Bay Coastal System: An overview Patrick L. Barnard a,⁎, David H. Schoellhamer b,c, Bruce E. Jaffe a, Lester J. McKee d a U.S. Geological Survey, Pacific Coastal and Marine Science Center, Santa Cruz, CA, USA b U.S. Geological Survey, California Water Science Center, Sacramento, CA, USA c University of California, Davis, USA d San Francisco Estuary Institute, Richmond, CA, USA article info abstract Article history: The papers in this special issue feature state-of-the-art approaches to understanding the physical processes Received 29 March 2012 related to sediment transport and geomorphology of complex coastal–estuarine systems. Here we focus on Received in revised form 9 April 2013 the San Francisco Bay Coastal System, extending from the lower San Joaquin–Sacramento Delta, through the Accepted 13 April 2013 Bay, and along the adjacent outer Pacific Coast. San Francisco Bay is an urbanized estuary that is impacted by Available online 20 April 2013 numerous anthropogenic activities common to many large estuaries, including a mining legacy, channel dredging, aggregate mining, reservoirs, freshwater diversion, watershed modifications, urban run-off, ship traffic, exotic Keywords: sediment transport species introductions, land reclamation, and wetland restoration. The Golden Gate strait is the sole inlet 9 3 estuaries connecting the Bay to the Pacific Ocean, and serves as the conduit for a tidal flow of ~8 × 10 m /day, in addition circulation to the transport of mud, sand, biogenic material, nutrients, and pollutants. -
Journal of the Oklahoma Native Plant Society, Volume 2, Number 1
54 Oklahoma Native Plant Record Volume 2, Number 1, December 2002 Schoenoplectus hallii and S. saximontanus 2000 Wichita Mountain Wildlife Refuge Survey Dr. Lawrence K. Magrath Curator-USAO (OCLA) Herbarium Chickasha, OK 73018-5358 A survey to determine locations of populations of Schoenoplectus hallii and S. saximontanus was conducted at Wichita Mountains Wildlife Refuge in August and September 2000. One or both species were found at 20 of the 134 locations surveyed. A distinctive terminal achene character was found specifically that the transverse ridges of S. hallii appeared to be rounded and S. saximontanus appeared to be rounded with a projecting narrow wing. Basal macroachenes have not yet been properly described but are borne singly at the base of each culm and are about 3-4 times larger than the terminal achenes. It is speculated that amphicarpy may be related to grazing pressure, the basal macroachene being produced even if the upper portion is consumed, as a response to grazing. Both species are grazed/disturbed by bison, elk, and longhorns on the Refuge. Introduction the drawdown mud, sand, or gravel flats. A survey to determine locations of However in some places they occur in shallow populations of Schoenoplectus hallii (A. Gray) water up to a depth of about a foot [30.5cm]. S.G. Smith (Hall’s bulrush) and S. saximontanus They seem to compete with perennial emergent (Fernald) J. Raynal (Rocky Mountain bulrush) plants and with most emergent annuals. was conducted on the Wichita Mountains In addition to the 36 sites that I Wildlife Refuge during late August through personally examined, WMWR staff examined September 2000. -
Bothin Marsh 46
EMERGENT ECOLOGIES OF THE BAY EDGE ADAPTATION TO CLIMATE CHANGE AND SEA LEVEL RISE CMG Summer Internship 2019 TABLE OF CONTENTS Preface Research Introduction 2 Approach 2 What’s Out There Regional Map 6 Site Visits ` 9 Salt Marsh Section 11 Plant Community Profiles 13 What’s Changing AUTHORS Impacts of Sea Level Rise 24 Sarah Fitzgerald Marsh Migration Process 26 Jeff Milla Yutong Wu PROJECT TEAM What We Can Do Lauren Bergenholtz Ilia Savin Tactical Matrix 29 Julia Price Site Scale Analysis: Treasure Island 34 Nico Wright Site Scale Analysis: Bothin Marsh 46 This publication financed initiated, guided, and published under the direction of CMG Landscape Architecture. Conclusion Closing Statements 58 Unless specifically referenced all photographs and Acknowledgments 60 graphic work by authors. Bibliography 62 San Francisco, 2019. Cover photo: Pump station fronting Shorebird Marsh. Corte Madera, CA RESEARCH INTRODUCTION BREADTH As human-induced climate change accelerates and impacts regional map coastal ecologies, designers must anticipate fast-changing conditions, while design must adapt to and mitigate the effects of climate change. With this task in mind, this research project investigates the needs of existing plant communities in the San plant communities Francisco Bay, explores how ecological dynamics are changing, of the Bay Edge and ultimately proposes a toolkit of tactics that designers can use to inform site designs. DEPTH landscape tactics matrix two case studies: Treasure Island Bothin Marsh APPROACH Working across scales, we began our research with a broad suggesting design adaptations for Treasure Island and Bothin survey of the Bay’s ecological history and current habitat Marsh. -
Wetlands, Biodiversity and the Ramsar Convention
Wetlands, Biodiversity and the Ramsar Convention Wetlands, Biodiversity and the Ramsar Convention: the role of the Convention on Wetlands in the Conservation and Wise Use of Biodiversity edited by A. J. Hails Ramsar Convention Bureau Ministry of Environment and Forest, India 1996 [1997] Published by the Ramsar Convention Bureau, Gland, Switzerland, with the support of: • the General Directorate of Natural Resources and Environment, Ministry of the Walloon Region, Belgium • the Royal Danish Ministry of Foreign Affairs, Denmark • the National Forest and Nature Agency, Ministry of the Environment and Energy, Denmark • the Ministry of Environment and Forests, India • the Swedish Environmental Protection Agency, Sweden Copyright © Ramsar Convention Bureau, 1997. Reproduction of this publication for educational and other non-commercial purposes is authorised without prior perinission from the copyright holder, providing that full acknowledgement is given. Reproduction for resale or other commercial purposes is prohibited without the prior written permission of the copyright holder. The views of the authors expressed in this work do not necessarily reflect those of the Ramsar Convention Bureau or of the Ministry of the Environment of India. Note: the designation of geographical entities in this book, and the presentation of material, do not imply the expression of any opinion whatsoever on the part of the Ranasar Convention Bureau concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. Citation: Halls, A.J. (ed.), 1997. Wetlands, Biodiversity and the Ramsar Convention: The Role of the Convention on Wetlands in the Conservation and Wise Use of Biodiversity. -
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. -
6. Geotechnical, Sea Level Rise and Shoreline Improvements
6. GEOTECHNICAL, SEA LEVEL RISE AND SHORELINE IMPROVEMENTS 6.1 GEOTECHNICAL DOCUMENTS 233 6.2 TREASURE ISLAND AND CAUSEWAY GEOTECHNICAL IMPROVEMENTS 234 6.3 YERBA BUENA ISLAND GEOTECHNICAL IMPROVEMENTS 238 6.4 SEA LEVEL RISE STRATEGY AND SHORELINE IMPROVEMENTS 240 TREASURE ISLAND & YERBA BUENA ISLAND MAJOR PHASE 1 APPLICATION 6 - GEOTECHNICAL AND SHORELINE IMPROVEMENTS 231 6.1 GEOTECHNICAL DOCUMENTS The documents noted below were separately distributed to agency representatives from the Department of Public Works (DPW) and the Department of Building Inspection (DBI) on February, 3, 2015, and they are also included herein as Appendix E. 1. Treasure Island Geotechnical Conceptual Design Report, February 2, 2009 2. Treasure Island Geotechnical Conceptual Design Report Appendix 4, February 2, 2009 3. Treasure Island Sub-phase 1A Geotechnical Data Report; Draft, December 31, 2014 4. Technical Memorandum 1, Preliminary Foundation Design Parameters Treasure Island Ferry Terminal Improvements, January 2, 2015 5. Technical Memorandum 2, Preliminary Geotechnical Design for Sub-Phase 1A Shoreline Stabilization, January 2, 2015 6. Treasure Island Sub-phase 1A Interim Geotechnical Characterization Report; Draft, January 5, 2015 TREASURE ISLAND & YERBA BUENA ISLAND MAJOR PHASE 1 APPLICATION 6 - GEOTECHNICAL AND SHORELINE IMPROVEMENTS 233 6.2 TREASURE ISLAND AND CAUSEWAY GEOTECHNICAL IMPROVEMENTS GEOLOGIC SETTING AND DEPOSITIONAL HISTORY into the Bay. The grain-size distribution of windblown sands on Yerba Buena Island is essentially the same as fine silty sands The San Francisco Bay around Treasure Island is underlain interbedded with Young Bay Mud below Treasure Island. The by rocks of the Franciscan Complex of the Alcatraz Terrain, erosion of the windblown sand from Yerba Buena Island and consisting mainly of interbedded greywacke sandstone and surrounding areas is likely the source for both the historic sandy shale. -
Erosion and Accretion on a Mudflat: the Importance of Very 10.1002/2016JC012316 Shallow-Water Effects
PUBLICATIONS Journal of Geophysical Research: Oceans RESEARCH ARTICLE Erosion and Accretion on a Mudflat: The Importance of Very 10.1002/2016JC012316 Shallow-Water Effects Key Points: Benwei Shi1,2 , James R. Cooper3 , Paula D. Pratolongo4 , Shu Gao5 , T. J. Bouma6 , Very shallow water accounted for Gaocong Li1 , Chunyan Li2 , S.L. Yang5 , and YaPing Wang1,5 only 11% of the duration of the entire tidal cycle, but accounted for 1Ministry of Education Key Laboratory for Coast and Island Development, Nanjing University, Nanjing, China, 2Department 35% of bed-level changes 3 Erosion and accretion during very of Oceanography and Coastal Sciences, Louisiana State University, Baton Rouge, LA, USA, Department of Geography and 4 shallow water stages cannot be Planning, School of Environmental Sciences, University of Liverpool, Liverpool, UK, CONICET – Instituto Argentino de neglected when modeling Oceanografıa, CC 804, Bahıa Blanca, Argentina, 5State Key Laboratory of Estuarine and Coastal Research, East China morphodynamic processes Normal University, Shanghai, China, 6NIOZ Royal Netherlands Institute for Sea Research, Department of Estuarine and This study can improve our understanding of morphological Delta Systems, and Utrecht University, Yerseke, The Netherlands changes of intertidal mudflats within an entire tidal cycle Abstract Understanding erosion and accretion dynamics during an entire tidal cycle is important for Correspondence to: assessing their impacts on the habitats of biological communities and the long-term morphological Y. P. Wang, evolution of intertidal mudflats. However, previous studies often omitted erosion and accretion during very [email protected] shallow-water stages (VSWS, water depths < 0.20 m). It is during these VSWS that bottom friction becomes relatively strong and thus erosion and accretion dynamics are likely to differ from those during deeper Citation: flows. -
Alternative Monitoring Approaches for Large Bay-Delta Estuarine Wetland Restoration Projects Adapting to Uncertainty Or Novelty During Accelerated Climate Change
Alternative Monitoring Approaches for Large Bay-Delta Estuarine Wetland Restoration Projects Adapting to Uncertainty or Novelty during Accelerated Climate Change Montezuma Wetlands 2015 Sears Point Wetlands 2015 Peter R. Baye Coastal Ecologist [email protected] Delta Science Program Brown Bag Lunch – February 17, 2016 Estuarine Wetland Restoration San Francisco Bay Area historical context ERA CONTEXT “First-generation” SFE marsh restoration • Regulatory permit & policy (CWA, (1970s-1980s) McAteer-Petris Act, Endangered Species Act • compensatory mitigation • USACE dredge material marsh creation national program; estuarine sediment surplus “Second-generation” SFE marsh restoration • Goals Project era transition to regional planning and larger scale restoration • Wetland policy conflict resolution • Geomorphic pattern & process emphasis 21st century SFE marsh restoration • BEHGU (Goals Project update) era: • Accelerated sea level rise • Estuarine sediment deficit • Climate event extremes, species invasions as “new normal” • advances in wetland sciences Estuarine Wetland Restoration San Francisco Bay Area examples ERA EXAMPLES First-generation SFE marsh restoration • Muzzi Marsh (MRN) (1970s-1980s) • Pond 3 Alameda (ALA) Second-generation SFE marsh restoration • Sonoma Baylands (SON) (1990s) • Hamilton Wetland Restoration (MRN) • Montezuma Wetlands (SOL) 21st century SFE marsh restoration • Sears Point (SON) (climate change) • Aramburu Island (MRN) • Cullinan Ranch (SOL) • Oro Loma Ecotone (“horizontal levee”) (ALA) • South Bay and Napa-Sonoma -
Trophic State and Metabolism in a Southeastern Piedmont Reservoir
TROPHIC STATE AND METABOLISM IN A SOUTHEASTERN PIEDMONT RESERVOIR by Mary Callie Mayhew (Under the direction of Todd C. Rasmussen) Abstract Lake Sidney Lanier is a valuable water resource in the rapidly developing region north of Atlanta, Georgia, USA. The reservoir has been managed by the U.S Army Corps of Engineers for multiple purposes since its completion in 1958. Since approximately 1990, Lake Lanier has been central to series of lawsuits in the “Eastern Water Wars” between Georgia, Alabama and Florida due to its importance as a water-storage facility within the Apalachicola-Chattahoochee-Flint River Basin. Of specific importance is the need to protect lake water quality to satisfy regional water supply demands, as well as for recreational and environmental purposes. Recently, chlorophyll a levels have exceeded state water-quality standards. These excee- dences have prompted the Georgia Environmental Protection Division to develop Total Max- imum Daily Loads for phosphorus in Lake Lanier. While eutrophication in Southeastern Piedmont impoundments is a regional problem, nutrient cycling in these lakes does not appear to behave in a manner consistent with lakes in higher latitudes, and, hence, may not respond to nutrient-abatement strategies developed elsewhere. Although phosphorus loading to Southeastern Piedmont waterbodies is high, soluble reac- tive phosphorus concentrations are generally low and phosphorus exports from the reservoir are only a small fraction of input loads. The prevailing hypothesis is that ferric oxides in the iron-rich, clay soils of the Southeastern Piedmont effectively sequester phosphorus, which then settle into the lake benthos. Yet, seasonal algal blooms suggest the presence of internal cycling driven by uncertain mechanisms.