Managing and Classifying Wetlands in the Mekong River Delta
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Information Sheet on Ramsar Wetlands (RIS)– 2009-2012 Version
Information Sheet on Ramsar Wetlands (RIS)– 2009-2012 version Available for download from http://www.ramsar.org/ris/key_ris_index.htm. Categories approved by Recommendation 4.7 (1990), as amended by Resolution VIII.13 of the 8th Conference of the Contracting Parties (2002) and Resolutions IX.1 Annex B, IX.6, IX.21 and IX. 22 of the 9th Conference of the Contracting Parties (2005). Notes for compilers: 1. The RIS should be completed in accordance with the attached Explanatory Notes and Guidelines for completing the Information Sheet on Ramsar Wetlands. Compilers are strongly advised to read this guidance before filling in the RIS. 2. Further information and guidance in support of Ramsar Site designations are provided in the Strategic Framework and guidelines for the future development of the List of Wetlands of International Importance (Ramsar Wise Use Handbook 14, 3nd edition). 3. Once completed, the RIS (and accompanying map(s)) should be submitted to the Ramsar Secretariat. Compilers should provide an electronic (MS Word) copy of the RIS and, where possible, digital copies of all maps. 1. Name and address of the compiler of this form: Dr. Srey Sunleang, FOR OFFICE USE ONLY. Director, DD MM YY Department of Wetlands and Coastal Zones, Ministry of Environment, #48 Preah Sihanouk Blvd., Tonle Bassac, Chamkar Morn, Phnom Penh, Cambodia Designation date Site Reference Number Tel: (855) 77-333-456 Fax (855)-23-721-073 E-mail: [email protected] 2. Date this sheet was completed: 9 September, 2011 3. Country: Cambodia 4. Name of the Ramsar Site: The precise name of the designated Site in one of the three official languages (English, French or Spanish) of the Convention. -
Missouri River Floodplain from River Mile (RM) 670 South of Decatur, Nebraska to RM 0 at St
Hydrogeomorphic Evaluation of Ecosystem Restoration Options For The Missouri River Floodplain From River Mile (RM) 670 South of Decatur, Nebraska to RM 0 at St. Louis, Missouri Prepared For: U. S. Fish and Wildlife Service Region 3 Minneapolis, Minnesota Greenbrier Wetland Services Report 15-02 Mickey E. Heitmeyer Joseph L. Bartletti Josh D. Eash December 2015 HYDROGEOMORPHIC EVALUATION OF ECOSYSTEM RESTORATION OPTIONS FOR THE MISSOURI RIVER FLOODPLAIN FROM RIVER MILE (RM) 670 SOUTH OF DECATUR, NEBRASKA TO RM 0 AT ST. LOUIS, MISSOURI Prepared For: U. S. Fish and Wildlife Service Region 3 Refuges and Wildlife Minneapolis, Minnesota By: Mickey E. Heitmeyer Greenbrier Wetland Services Advance, MO 63730 Joseph L. Bartletti Prairie Engineers of Illinois, P.C. Springfield, IL 62703 And Josh D. Eash U.S. Fish and Wildlife Service, Region 3 Water Resources Branch Bloomington, MN 55437 Greenbrier Wetland Services Report No. 15-02 December 2015 Mickey E. Heitmeyer, PhD Greenbrier Wetland Services Route 2, Box 2735 Advance, MO 63730 www.GreenbrierWetland.com Publication No. 15-02 Suggested citation: Heitmeyer, M. E., J. L. Bartletti, and J. D. Eash. 2015. Hydrogeomorphic evaluation of ecosystem restoration options for the Missouri River Flood- plain from River Mile (RM) 670 south of Decatur, Nebraska to RM 0 at St. Louis, Missouri. Prepared for U. S. Fish and Wildlife Service Region 3, Min- neapolis, MN. Greenbrier Wetland Services Report 15-02, Blue Heron Conservation Design and Print- ing LLC, Bloomfield, MO. Photo credits: USACE; http://statehistoricalsocietyofmissouri.org/; Karen Kyle; USFWS http://digitalmedia.fws.gov/cdm/; Cary Aloia This publication printed on recycled paper by ii Contents EXECUTIVE SUMMARY .................................................................................... -
Chapter 5 Groundwater Quality and Hydrodynamics of an Acid Sulfate Soil Backswamp
Chapter 5 Groundwater Quality and Hydrodynamics of an Acid Sulfate Soil Backswamp 5.1 Introduction Intensive drainage of coastal floodplains has been the main factor contributing to the oxidation of acid sulfate soils (ASS) (Indraratna, Blunden & Nethery 1999; Sammut, White & Melville 1996). Drainage of backswamps removes surface water, thereby increasing the effect of evapotranspiration on watertable drawdown (Blunden & Indraratna 2000) and transportation of acidic salts to the soil surface through capillary action (Lin, Melville & Hafer 1995; Rosicky et al. 2006). During high rainfall events the oxidation products (i.e. metals and acid) are mobilised into the groundwater, and acid salts at the sediment surface are dissolved directly into the surface water (Green et al. 2006). The high efficiency of drains readily transports the acidic groundwater and surface water into the estuary and can have a detrimental impact on downstream habitats (Cook et al. 2000). The quality of water discharged from a degraded ASS wetland is controlled by the water balance, which over a given time period is: P + I + Li = E + Lo + D + S (Equation 5.1) where P is precipitation, I is irrigation, Li is the lateral inflow of water, E is evapotranspiration, Lo is surface and subsurface lateral outflow of water, D is the drainage to the watertable and S is the change in soil moisture storage above the watertable (Indraratna, Tularam & Blunden 2001; Sammut, White & Melville 1996; White et al. 1997). While this equation may give a general overview of sulfidic floodplain hydrology, an understanding of site-specific details is required for effective remediation and management of degraded ASS wetlands. -
PESHTIGO RIVER DELTA Property Owner
NORTHEAST - 10 PESHTIGO RIVER DELTA WETLAND TYPES Drew Feldkirchner Floodplain forest, lowland hardwood, swamp, sedge meadow, marsh, shrub carr ECOLOGY & SIGNIFICANCE supports cordgrass, marsh fern, sensitive fern, northern tickseed sunflower, spotted joe-pye weed, orange This Wetland Gem site comprises a very large coastal • jewelweed, turtlehead, marsh cinquefoil, blue skullcap wetland complex along the northwest shore of Green Bay and marsh bellflower. Shrub carr habitat is dominated three miles southeast of the city of Peshtigo. The wetland by slender willow; other shrub species include alder, complex extends upstream along the Peshtigo River for MARINETTE COUNTY red osier dogwood and white meadowsweet. Floodplain two miles from its mouth. This site is significant because forest habitats are dominated by silver maple and green of its size, the diversity of wetland community types ash. Wetlands of the Peshtigo River Delta support several present, and the overall good condition of the vegetation. - rare plant species including few-flowered spikerush, The complexity of the site – including abandoned oxbow variegated horsetail and northern wild raisin. lakes and a series of sloughs and lagoons within the river delta – offers excellent habitat for waterfowl. A number This Wetland Gem provides extensive, diverse and high of rare animals and plants have been documented using quality wetland habitat for many species of waterfowl, these wetlands. The area supports a variety of recreational herons, gulls, terns and shorebirds and is an important uses, such as hunting, fishing, trapping and boating. The staging, nesting and stopover site for many migratory Peshtigo River Delta has been described as the most birds. Rare and interesting bird species documented at diverse and least disturbed wetland complex on the west the site include red-shouldered hawk, black tern, yellow shore of Green Bay. -
A Synthesis of Information I
Outer Continental Shelf Environmental Assessment Program * A Synthesis of Information I U.S. DEPARTMENT OF COMMERCE U.S. DEPARTMENT OF THE INTEXIOR National Oceanic and Atmospheric Administration Minerals Management Service National Ocean Service Alaska OCS Region Office of Oceanography and Marine Assessment . .:.% y! Ocean Assessments Division ' t. CU ' k Alaska Office OCS Study, MMS 89-0081 . '.'Y. 4 3 --- NOTICES This report has been prepared as part of the U.S. Department bf Commerce, National Oceanic and Atmospheric Administration's Outer Continental Shelf Environmental Assessment Program, and approved for publication. The inter- pretation of data and opinions expressed in this document are those of the authors. Approval does not necessarily signify that the contents reflect the views and policies of the Department of Commerce or those of the Department of the Interior. The National Oceanic and Atmospheric Administration (NOAA) does not approve, recommend, or endorse any proprietary material mentioned in this publication. No reference shall be made to NOAA or to this publication in any advertising or sales promotion which would indicate or imply that NOAA approves, recommends, or endorses any proprietary product or proprietary material mentioned herein, or which has as its purpose or intent to cause directly or indirectly the advertised product to be used or purchased because of this publication. Cover: LandsatTMimage of the Yukon Delta taken on Julg 22, 1975, showing the thamal gradients resulting from Yukon River discharge. In this image land is dqicted in sesof red indicating warmer temperatures versus the dark blues (colder temperatures) of Bering Sea waters. Yukon River water, cooh than the surround- ing land but wanner than marine waters, is represented bg a light aqua blue. -
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. -
Cypress Creek National Wildlife Refuge, Illinois
Hydrogeomorphic Evaluation of Ecosystem Restoration Options for Cypress Creek National Wildlife Refuge, Illinois Prepared For: U. S. Fish and Wildlife Service Division of Refuges, Region 3 Minneapolis, Minnesota Greenbrier Wetland Services Report 12-05 Mickey E. Heitmeyer Karen E. Mangan July 2012 HYDROGEOMORPHIC EVALUATION OF ECOSYSTEM RESTORATION OPTIONS FOR CYPRESS CREEK NATIONAL WILDLIFE REFUGE, ILLINOIS Prepared For: U.S. Fish and Wildlife Service National Wildlife Refuge System, Region 3 Minneapolis, MN and Cypress Creek National Wildlife Refuge Ullin, IL By: Mickey E. Heitmeyer, PhD Greenbrier Wetland Services Rt. 2, Box 2735 Advance, MO 63730 and Karen E. Mangan U.S. Fish and Wildlife Service Cypress Creek National Wildlife Refuge 0137 Rustic Campus Drive Ullin, IL 62992 Greenbrier Wetland Services Report 12-05 July 2012 Mickey E Heitmeyer, PhD Greenbrier Wetland Services Route 2, box 2735 Advance, MO. 63730 Publication No. 12-05 Suggested citation: Heitmeyer, M. E., K. E. Mangan. 2012. Hy- drogeomorphic evaluation of ecosystem restora- tion and management options for Cypress Creek National Wildlife Refuge,Ullin Il.. Prepared for U. S. Fish and Wildlife Service, Region 3, Minne- apolis, MN and Cypress Creek National Wildlife Refuge,Ullin,Il. Greenbrier Wetland Services Report 12-05, Blue Heron Conservation Design and Printing LLC, Bloomfield, MO. Photo credits: COVER: Limekiln Slough by Michael Jeffords Michael Jeffords, Jan Sundberg, Cary Aloia (Gardners- Gallery.com), Karen Kyle This publication printed on recycled paper by ii -
Floodplain Geomorphic Processes and Environmental Impacts of Human Alteration Along Coastal Plain Rivers, Usa
WETLANDS, Vol. 29, No. 2, June 2009, pp. 413–429 ’ 2009, The Society of Wetland Scientists FLOODPLAIN GEOMORPHIC PROCESSES AND ENVIRONMENTAL IMPACTS OF HUMAN ALTERATION ALONG COASTAL PLAIN RIVERS, USA Cliff R. Hupp1, Aaron R. Pierce2, and Gregory B. Noe1 1U.S. Geological Survey 430 National Center, Reston, Virginia, USA 20192 E-mail: [email protected] 2Department of Biological Sciences, Nicholls State University Thibodaux, Louisiana, USA 70310 Abstract: Human alterations along stream channels and within catchments have affected fluvial geomorphic processes worldwide. Typically these alterations reduce the ecosystem services that functioning floodplains provide; in this paper we are concerned with the sediment and associated material trapping service. Similarly, these alterations may negatively impact the natural ecology of floodplains through reductions in suitable habitats, biodiversity, and nutrient cycling. Dams, stream channelization, and levee/canal construction are common human alterations along Coastal Plain fluvial systems. We use three case studies to illustrate these alterations and their impacts on floodplain geomorphic and ecological processes. They include: 1) dams along the lower Roanoke River, North Carolina, 2) stream channelization in west Tennessee, and 3) multiple impacts including canal and artificial levee construction in the central Atchafalaya Basin, Louisiana. Human alterations typically shift affected streams away from natural dynamic equilibrium where net sediment deposition is, approximately, in balance with net -
National Reports on Wetlands in South China Sea
United Nations UNEP/GEF South China Sea Global Environment Environment Programme Project Facility “Reversing Environmental Degradation Trends in the South China Sea and Gulf of Thailand” National Reports on Wetlands in South China Sea First published in Thailand in 2008 by the United Nations Environment Programme. Copyright © 2008, United Nations Environment Programme This publication may be reproduced in whole or in part and in any form for educational or non-profit purposes without special permission from the copyright holder provided acknowledgement of the source is made. UNEP would appreciate receiving a copy of any publication that uses this publicationas a source. No use of this publication may be made for resale or for any other commercial purpose without prior permission in writing from the United Nations Environment Programme. UNEP/GEF Project Co-ordinating Unit, United Nations Environment Programme, UN Building, 2nd Floor Block B, Rajdamnern Avenue, Bangkok 10200, Thailand. Tel. +66 2 288 1886 Fax. +66 2 288 1094 http://www.unepscs.org DISCLAIMER: The contents of this report do not necessarily reflect the views and policies of UNEP or the GEF. The designations employed and the presentations do not imply the expression of any opinion whatsoever on the part of UNEP, of the GEF, or of any cooperating organisation concerning the legal status of any country, territory, city or area, of its authorities, or of the delineation of its territories or boundaries. Cover Photo: A vast coastal estuary in Koh Kong Province of Cambodia. Photo by Mr. Koch Savath. For citation purposes this document may be cited as: UNEP, 2008. -
Analyzing Trends of Dike-Ponds Between 1978 and 2016 Using Multi-Source Remote Sensing Images in Shunde District of South China
sustainability Article Analyzing Trends of Dike-Ponds between 1978 and 2016 Using Multi-Source Remote Sensing Images in Shunde District of South China Fengshou Li 1, Kai Liu 1,* , Huanli Tang 2, Lin Liu 3,4,* and Hongxing Liu 4,5 1 Guangdong Key Laboratory for Urbanization and Geo-simulation, Guangdong Provincial Engineering Research Center for Public Security and Disaster, School of Geography and Planning, Sun Yat-Sen University, Guangzhou 510275, China; [email protected] 2 Guangzhou Zengcheng District Urban and Rural Planning and Surveying and Mapping Geographic Information Institute, Guangzhou 511300, China; [email protected] 3 Center of Geo-Informatics for Public Security, School of Geographic Sciences, Guangzhou University, Guangzhou 510006, China 4 Department of Geography and Geographic Information Science, University of Cincinnati, Cincinnati, OH 45221, USA; [email protected] 5 Department of Geography, the University of Alabama, Tuscaloosa, AL 35487, USA * Correspondence: [email protected] (K.L.); [email protected] (L.L.); Tel.: +86-020-8411-3044 (K.L.); +1-513-556-3429 (L.L.); Fax: +86-020-8411-3057 (K.L. & L.L.) Received: 27 August 2018; Accepted: 26 September 2018; Published: 30 September 2018 Abstract: Dike-ponds have experienced significant changes in the Pearl River Delta region over the past several decades, especially since China’s economic reform, which has seriously affected the construction of ecological environments. In order to monitor the evolution of dike-ponds, in this study we use multi-source remote sensing images from 1978 to 2016 to extract dike-ponds in several periods using the nearest neighbor classification method. -
Dispersal of Larval Suckers at the Williamson River Delta, Upper Klamath Lake, Oregon, 2006–09
Prepared in cooperation with the Bureau of Reclamation Dispersal of Larval Suckers at the Williamson River Delta, Upper Klamath Lake, Oregon, 2006–09 Scientific Investigations Report 2012–5016 U.S. Department of the Interior U.S. Geological Survey Cover: Inset: Larval sucker from Upper Klamath Lake, Oregon. (Photograph taken by Allison Estergard, Student, Oregon State University, Corvallis, Oregon, 2011.) Top: Photograph taken from the air of the flooded Williamson River Delta, Upper Klamath Lake, Oregon. (Photograph taken by Charles Erdman, Fisheries Technician, Williamson River Delta Preserve, Klamath Falls, Oregon, 2008.) Bottom left: Photograph of a pop net used by The Nature Conservancy to collect larval suckers in Upper Klamath Lake and the Williamson River Delta, Oregon. (Photograph taken by Heather Hendrixson, Director, Williamson River Delta Preserve, Klamath Falls, Oregon, 2006.) Bottom middle: Photograph of a larval trawl used by Oregon State University to collect larval suckers in Upper Klamath Lake and the Williamson River Delta, Oregon. (Photograph taken by David Simon, Senior Faculty Research Assistant, Oregon State University, Corvallis, Oregon, 2010.) Bottom right: Photograph of a plankton net used by the U.S. Geological Survey to collect larval suckers in Upper Klamath Lake and the Williamson River Delta, Oregon. (Photographer unknown, Klamath Falls, Oregon, 2009.) Dispersal of Larval Suckers at the Williamson River Delta, Upper Klamath Lake, Oregon, 2006–09 By Tamara M. Wood, U.S. Geological Survey, Heather A. Hendrixson, The Nature Conservancy, Douglas F. Markle, Oregon State University, Charles S. Erdman, The Nature Conservancy, Summer M. Burdick, U.S. Geological Survey, Craig M. Ellsworth, U.S. Geological Survey, and Norman L. -
Losses of Salt Marsh in China: Trends, Threats and Management
Losses of salt marsh in China: Trends, threats and management Item Type Article Authors Gu, Jiali; Luo, Min; Zhang, Xiujuan; Christakos, George; Agusti, Susana; Duarte, Carlos M.; Wu, Jiaping Citation Gu J, Luo M, Zhang X, Christakos G, Agusti S, et al. (2018) Losses of salt marsh in China: Trends, threats and management. Estuarine, Coastal and Shelf Science 214: 98–109. Available: http://dx.doi.org/10.1016/j.ecss.2018.09.015. Eprint version Post-print DOI 10.1016/j.ecss.2018.09.015 Publisher Elsevier BV Journal Estuarine, Coastal and Shelf Science Rights NOTICE: this is the author’s version of a work that was accepted for publication in Estuarine, Coastal and Shelf Science. Changes resulting from the publishing process, such as peer review, editing, corrections, structural formatting, and other quality control mechanisms may not be reflected in this document. Changes may have been made to this work since it was submitted for publication. A definitive version was subsequently published in Estuarine, Coastal and Shelf Science, [, , (2018-09-18)] DOI: 10.1016/j.ecss.2018.09.015 . © 2018. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http:// creativecommons.org/licenses/by-nc-nd/4.0/ Download date 09/10/2021 17:12:34 Link to Item http://hdl.handle.net/10754/628759 Accepted Manuscript Losses of salt marsh in China: Trends, threats and management Jiali Gu, Min Luo, Xiujuan Zhang, George Christakos, Susana Agusti, Carlos M. Duarte, Jiaping Wu PII: S0272-7714(18)30220-8 DOI: 10.1016/j.ecss.2018.09.015 Reference: YECSS 5973 To appear in: Estuarine, Coastal and Shelf Science Received Date: 15 March 2018 Revised Date: 21 August 2018 Accepted Date: 14 September 2018 Please cite this article as: Gu, J., Luo, M., Zhang, X., Christakos, G., Agusti, S., Duarte, C.M., Wu, J., Losses of salt marsh in China: Trends, threats and management, Estuarine, Coastal and Shelf Science (2018), doi: https://doi.org/10.1016/j.ecss.2018.09.015.