Reestablishing Olympia Oyster Populations in Puget Sound, Washington
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South Tacoma Way, Circa 1913, Photo Courtesy of the Tacoma Public Library, Amzie D
The west side of the 5200 block of South Tacoma Way, circa 1913, photo courtesy of the Tacoma Public Library, Amzie D. Browning Collection 158 2 011 Historic South Tacoma Way South Tacoma Way Business District In early 2011, Historic Tacoma reached out to the 60+ member South Tacoma Business District Association as part of its new neighborhood initiative. The area is home to one of the city’s most intact historic commercial business districts. A new commuter rail station is due to open in 2012, business owners are interested in S 52nd St taking advantage of City loan and grant programs for façade improvements, and Historic Tacoma sees S Washington St great opportunities in partnering with the district. S Puget Sound Ave The goals of the South Tacoma project are to identify and assess historic structures and then to partner with business owners and the City of Tacoma to conserve and revitalize the historic core of the South Tacoma Business District. The 2011 work plan includes: • conducting a detailed inventory of approximately 50 commercial structures in the historic center of the district • identification of significant and endangered South Way Tacoma properties in the district • development of action plans for endangered properties • production of a “historic preservation resource guide for community leaders” which can be S 54th St used by community groups across the City • ½ day design workshop for commercial property owners • production & distribution of a South Tacoma Business District tour guide and map • nominations to the Tacoma Register of Historic Places as requested by property owners • summer walking tour of the district Acknowledgements Project funding provided by Historic Tacoma, the South Tacoma Business District Association, the South Tacoma Neighborhood Council, the University of Washington-Tacoma, and Jim and Karen Rich. -
Identifying Potential Juvenile Steelhead Predators in the Marine Waters of the Salish Sea
Early Marine Survival Project Washington Department of Fish & Wildlife Identifying Potential Juvenile Steelhead Predators In the Marine Waters of the Salish Sea Scott F. Pearson, Steven J. Jeffries, and Monique M. Lance Wildlife Science Division Washington Department of Fish and Wildlife, Olympia Austen Thomas Zoology Department University of British Columbia Robin Brown Early Marine Survival Project Washington Department of Fish & Wildlife Cover photo: Robin Brown, Oregon Department of Fish and Wildlife. Seals, sea lions, gulls and cormorants on the tip of the South Jetty at the mouth of the Columbia River. We selected this photograph to emphasize that bird and mammal fish predators can be found together in space and time and often forage on the same resources. Suggested citation: Pearson, S.F., S.J. Jeffries, M.M. Lance and A.C. Thomas. 2015. Identifying potential juvenile steelhead predators in the marine waters of the Salish Sea. Washington Department of Fish and Wildlife, Wildlife Science Division, Olympia. Identifying potential steelhead predators 1 INTRODUCTION Puget Sound wild steelhead were listed as threatened under the Endangered Species Act in 2007 and their populations are now less than 10% of their historic size (Federal Register Notice: 72 FR 26722). A significant decline in abundance has occurred since the mid-1980s (Federal Register Notice: 72 FR 26722), and data suggest that juvenile steelhead mortality occurring in the Salish Sea (waters of Puget Sound, the Strait of Juan de Fuca and the San Juan Islands as well as the water surrounding British Columbia’s Gulf Islands and the Strait of Georgia) marine environment constitutes a major, if not the predominant, factor in that decline (Melnychuk et al. -
South Puget Sound Community College Year Three Mid-Cycle Evaluation
South Puget Sound Community College Year Three Mid-Cycle Evaluation Dr. Timothy Stokes President September, 2014 Table of Contents Report on Year One Recommendation ......................................................................................................... 1 Mission .......................................................................................................................................................... 1 Part I .............................................................................................................................................................. 1 Mission Fulfillment .................................................................................................................................... 1 Operational Planning ................................................................................................................................ 2 Core Themes, Objectives and Indicators .................................................................................................. 3 Part II ............................................................................................................................................................. 4 Rationale for Indicators of Achievement .................................................................................................. 5 Increase Student Retention (Objective 1.A) ......................................................................................... 5 Support Student Completion (Objective 1.B) ...................................................................................... -
An Assessment of Potential Heavy Metal Contaminants in Bivalve Shellfish from Aquaculture Zones Along the Coast of New South Wales, Australia
PEER-REVIEWED ARTICLE Hazel Farrell,* Phil Baker, Grant Webster, Food Protection Trends, Vol 38, No. 1, p. 18–26 Copyright© 2018, International Association for Food Protection Edward Jansson, Elizabeth Szabo and 6200 Aurora Ave., Suite 200W, Des Moines, IA 50322-2864 Anthony Zammit NSW Food Authority, 6 Ave. of the Americas, Newington NSW 2127, Australia An Assessment of Potential Heavy Metal Contaminants in Bivalve Shellfish from Aquaculture Zones along the Coast of New South Wales, Australia ABSTRACT INTRODUCTION Evaluation of shellfish aquaculture for potential contam- Certain elements are essential in human physiology; inants is essential for consumer confidence and safety. however, an incorrect balance or excess of certain elements Every three years, between 1999 and 2014, bivalve in the diet can result in negative health effects. Heavy metals shellfish from aquaculture zones in up to 31 estuaries are of particular concern because of their ability to persist across 2,000 km of Australia’s east coast were tested and accumulate in the environment. While heavy metals for cadmium, copper, lead, mercury, selenium and zinc. can occur naturally in the environment, human activities Inorganic arsenic was included in the analyses in 2002, and run-off from urban and agricultural land use may and total arsenic was used as a screen for the inorganic increase their concentrations (6, 29). This is particularly form in subsequent years. Concentrations of inorganic important when considering the growing demands on arsenic, cadmium, lead and mercury were low and did not coastal resources due to increasing populations (3) and the exceed maximum limits mandated in the Australia New ability of filter feeding bivalve shellfish to bio-accumulate Zealand Food Standards Code. -
National Review of Ostrea Angasi Aquaculture: Historical Culture, Current Methods and Future Priorities
National review of Ostrea angasi aquaculture: historical culture, current methods and future priorities Christine Crawford Institute of Marine and Antarctic Studies ! [email protected] " secure.utas.edu.au/profles/staff/imas/Christine-Crawford Executive summary Currently in Australia Ostrea angasi oysters (angasi) are being cultured on a small scale, with several farmers growing relatively small numbers of angasis on their predominately Sydney rock or Pacifc oyster farms. Very few farmers are culturing commercially viable quantities of angasi oysters. There are several reasons for this. Although angasi oysters occur in the intertidal zone, they are naturally most abundant in the subtidal and are less tolerant of fuctuating environmental conditions, especially temperature and salinity, than other oyster species. They also have a much shorter shelf life and start to gape after one to two days. Additionally, angasi oysters are susceptible to Bonamiosis, a parasitic disease which has caused major mortalities in several areas. Stress caused by extremes or a combination of factors such as high stocking densities, rough handling, poor food, high temperatures and low salinities have all been observed to increase the prevalence of Bonamiosis. Growth rates of angasi oysters have also been variable, ranging from two to four years to reach market size. From discussions with oyster famers, managers and researchers and from a review of the literature I suggest that the survival and growth of cultured angasi oysters could be signifcantly improved by altering some farm management practices. Firstly, growout techniques need to be specifcally developed for angasi oysters which maintain a low stress environment (not modifcations from other oysters). -
Tacoma‐Pierce County Board of Health
Tacoma‐Pierce County Board of Health Regular Meeting Agenda 3629 South D Street, Tacoma, WA 98418 January 20, 2021 Board of Health Clerk, (253) 798‐2899 3 ‐ 5 p.m. Board Members Remote Attendance Only Keith Blocker Dial in: 253 215 8782 Marty Campbell Meeting ID: 992 6138 9468 Bruce Dammeier William Hirota, MD Passcode: 575390 Patricia Johnson Dave Morell Catherine Ushka I. CALL TO ORDER Derek Young II. ROLL CALL III. ELECTION OF BOARD OF HEALTH (BOH) OFFICERS Motion for 2021 BOH Chair Motion for 2021 BOH Vice Chair IV. COMMENTS BY THE PUBLIC The Board will consider written and oral public comments. Submit written comments any time prior to when a Board of Health meeting adjourns at [email protected]. Written comments we receive prior to noon on the date of a Board of Health meeting will go to Board members before the meeting. For the duration of the declared public health emergency, make oral comments when you join the meeting by phone with the number, meeting ID, and passcode at the top of the agenda. Press *9 to raise your hand and signal you wish to make a comment. You will be announced by your name or the last four digits of your phone number. Comments unrelated to specific agenda items have a two‐minute limit per person. The Chair has the authority to change the time limits as deemed necessary. All written and oral comments will become part of the meeting record. V. COVID‐19: Update [Anthony L‐T Chen, Director of Health] [Nigel Turner, Incident Commander] [Kayla Scrivner, Public Health Nurse] VI. -
Breeding and Domestication of Eastern Oyster (Crassostrea
W&M ScholarWorks VIMS Articles Virginia Institute of Marine Science 2014 Breeding And Domestication Of Eastern Oyster (Crassostrea Virginica) Lines For Culture In The Mid-Atlantic, Usa: Line Development And Mass Selection For Disease Resistance Anu Frank-Lawale Virginia Institute of Marine Science Standish K. Allen Jr. Virginia Institute of Marine Science Lionel Degremont Virginia Institute of Marine Science Follow this and additional works at: https://scholarworks.wm.edu/vimsarticles Part of the Marine Biology Commons Recommended Citation Frank-Lawale, Anu; Allen, Standish K. Jr.; and Degremont, Lionel, "Breeding And Domestication Of Eastern Oyster (Crassostrea Virginica) Lines For Culture In The Mid-Atlantic, Usa: Line Development And Mass Selection For Disease Resistance" (2014). VIMS Articles. 334. https://scholarworks.wm.edu/vimsarticles/334 This Article is brought to you for free and open access by the Virginia Institute of Marine Science at W&M ScholarWorks. It has been accepted for inclusion in VIMS Articles by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. Journal of Shellfish Research, Vol. 33, No. 1, 153–165, 2014. BREEDING AND DOMESTICATION OF EASTERN OYSTER (CRASSOSTREA VIRGINICA) LINES FOR CULTURE IN THE MID-ATLANTIC, USA: LINE DEVELOPMENT AND MASS SELECTION FOR DISEASE RESISTANCE ANU FRANK-LAWALE,* STANDISH K. ALLEN, JR. AND LIONEL DE´GREMONT† Virginia Institute of Marine Science, Aquaculture Genetics and Breeding Technology Center, College of William and Mary, 1375 Greate Road, Gloucester Point, VA 23062 ABSTRACT A selective breeding program for Crassostrea virginica was established in 1997 as part of an initiative in Virginia to address declining oyster harvests caused by the two oyster pathogens Haplosporidium nelsoni (MSX) and Perkinsus marinus (Dermo). -
Geology of Blaine-Birch Bay Area Whatcom County, WA Wings Over
Geology of Blaine-Birch Bay Area Blaine Middle Whatcom County, WA School / PAC l, ul G ant, G rmor Wings Over Water 2020 C o n Nest s ero Birch Bay Field Trip Eagles! H March 21, 2020 Eagle "Trees" Beach Erosion Dakota Creek Eagle Nest , ics l at w G rr rfo la cial E te Ab a u ant W Eagle Nest n d California Heron Rookery Creek Wave Cut Terraces Kingfisher G Nests Roger's Slough, Log Jam Birch Bay Eagle Nest G Beach Erosion Sea Links Ponds Periglacial G Field Trip Stops G Features Birch Bay Route Birch Bay Berm Ice Thickness, 2,200 M G Surficial Geology Alluvium Beach deposits Owl Nest Glacial outwash, Fraser-age in Barn k Glaciomarine drift, Fraser-age e e Marine glacial outwash, Fraser-age r Heron Center ll C re Peat deposits G Ter Artificial fill Terrell Marsh Water T G err Trailhead ell M a r k sh Terrell Cr ee 0 0.25 0.5 1 1.5 2 ± Miles 2200 M Blaine Middle Glacial outwash, School / PAC Geology of Blaine-Birch Bay Area marine, Everson ll, G Gu Glaciomarine Interstade Whatcom County, WA morant, C or t s drift, Everson ron Nes Wings Over Water 2020 Semiahmoo He Interstade Resort G Blaine Semiahmoo Field Trip March 21, 2020 Eagle "Trees" Semiahmoo Park G Glaciomarine drift, Everson Beach Erosion Interstade Dakota Creek Eagle Nest Glac ial Abun E da rra s, Blaine nt ti c l W ow Eagle Nest a terf California Creek Heron Glacial outwash, Rookery Glaciomarine drift, G Field Trip Stops marine, Everson Everson Interstade Semiahmoo Route Interstade Ice Thickness, 2,200 M Kingfisher Surficial GNeeoslotsgy Wave Cut Alluvium Glacial Terraces Beach deposits outwash, Roger's Glacial outwash, Fraser-age Slough, SuGmlaacsio mSataridnee drift, Fraser-age Log Jam Marine glacial outwash, Fraser-age Peat deposits Beach Eagle Nest Artificial fill deposits Water Beach Erosion 0 0.25 0.5 1 1.5 2 Miles ± Chronology of Puget Sound Glacial Events Sources: Vashon Glaciation Animation; Ralph Haugerud; Milepost Thirty-One, Washington State Dept. -
Development of a Hydrodynamic Model of Puget Sound and Northwest Straits
PNNL-17161 Prepared for the U.S. Department of Energy under Contract DE-AC05-76RL01830 Development of a Hydrodynamic Model of Puget Sound and Northwest Straits Z Yang TP Khangaonkar December 2007 DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor Battelle Memorial Institute, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof, or Battelle Memorial Institute. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. PACIFIC NORTHWEST NATIONAL LABORATORY operated by BATTELLE for the UNITED STATES DEPARTMENT OF ENERGY under Contract DE-AC05-76RL01830 Printed in the United States of America Available to DOE and DOE contractors from the Office of Scientific and Technical Information, P.O. Box 62, Oak Ridge, TN 37831-0062; ph: (865) 576-8401 fax: (865) 576-5728 email: [email protected] Available to the public from the National Technical Information Service, U.S. Department of Commerce, 5285 Port Royal Rd., Springfield, VA 22161 ph: (800) 553-6847 fax: (703) 605-6900 email: [email protected] online ordering: http://www.ntis.gov/ordering.htm This document was printed on recycled paper. -
Olympia Oyster (Ostrea Lurida)
COSEWIC Assessment and Status Report on the Olympia Oyster Ostrea lurida in Canada SPECIAL CONCERN 2011 COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC. 2011. COSEWIC assessment and status report on the Olympia Oyster Ostrea lurida in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. xi + 56 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Previous report(s): COSEWIC. 2000. COSEWIC assessment and status report on the Olympia Oyster Ostrea conchaphila in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vii + 30 pp. (www.sararegistry.gc.ca/status/status_e.cfm) Gillespie, G.E. 2000. COSEWIC status report on the Olympia Oyster Ostrea conchaphila in Canada in COSEWIC assessment and update status report on the Olympia Oyster Ostrea conchaphila in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. 1-30 pp. Production note: COSEWIC acknowledges Graham E. Gillespie for writing the provisional status report on the Olympia Oyster, Ostrea lurida, prepared under contract with Environment Canada and Fisheries and Oceans Canada. The contractor’s involvement with the writing of the status report ended with the acceptance of the provisional report. Any modifications to the status report during the subsequent preparation of the 6-month interim and 2-month interim status reports were overseen by Robert Forsyth and Dr. Gerald Mackie, COSEWIC Molluscs Specialist Subcommittee Co-Chair. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: 819-953-3215 Fax: 819-994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Ếvaluation et Rapport de situation du COSEPAC sur l’huître plate du Pacifique (Ostrea lurida) au Canada. -
Water Quality
Section 7: Water Quality SECTION 7 How is Puget Sound’s Water Quality Changing? Puget Sound is projected to experience a continued increase in sea surface temperatures, and continued declines in pH and dissolved oxygen concentrations. These changes, which could affect marine ecosystems and the shellfish industry, will be affected by variations in coastal upwelling and circulation within Puget Sound. While it is currently not known how climate change will affect circulation and upwelling in the region, these processes will continue to fluctuate in response to natural climate variability. Impacts on marine ecosystems and shellfish farming generally point to increasing stress for fish and shellfish populations. Efforts to address Puget Sound’s water quality are increasing, particularly in the areas of ocean acidification monitoring and implementation of risk reduction practices in the shellfish industry. Climate Drivers of Change DRIVERS Wind patterns, natural climate variability, and projected changes in temperature and precipitation can all affect water quality in Puget Sound.A Observations show a clear warming trend, and all scenarios project continued warming during this century. Most scenarios project that this warming will be outside of the range of historical variations by mid-century (see Section 2).1,2 Warming. The salinity of Puget Sound’s waters is tightly linked to freshwater inflows from streams. Increasing air temperatures will result in more precipitation falling as rain instead of snow, leading to more freshwater inflows into Puget Sound during winter months, and decreased freshwater inflows during summer. In addition, increasing air temperatures are expected to drive a continued increase in water temperatures, increasing the likelihood of harmful algal blooms (see Section 3). -
Ground-Water Flooding in Glacial Terrain of Southern Puget Sound
science fora changing world Ground-Water Flooding in Glacial Terrain of Southern Puget Sound, Washington glacial lakes, and diverting drainage landforms and, in some places, eroded southward to the Chehalis River and then away sediments deposited during the west to the Pacific Ocean to create exten glacial advance. Coarse sediment, known sive outwash plains6' 7' 10. At its maximum as the Steiiacoom Gravel, was also extent, the glacier stretched from the deposited on the upland by water flowing Cascade Range to the Olympic Mountains through the intersecting channels and and extended south as far as Tenino, braided streams that further conveyed the Wash., in Thurston County, occupying all water away from the proglacial lake.2- 13 of the lowland area and lower mountain This gravel deposit is consistently coarse valleys. The glacier reached altitudes up over the central Pierce County upland to 4,000 feet along the mountain front10; area. Stones in the Steiiacoom Gravel are 6,000 feet near the present day United predominantly 1 inch in size and most do States-Canada border; 3,000 feet near not exceed 3 inches. 13 The thickness of Seattle; 2,200 feet near Tacoma; and less the gravel is generally 20 feet or less with than 1.000 feet near Olympia. 1' 4- 10 a maximum that rarely exceeds 60 feet. The resulting landscape is characterized T^\ ue to a global warming trend, the by many shallow, elongated depressions Figure 1. Proglacial Lake Puyattup and J ^Vashon Glacier began retreating and ice-contact depressions (kettles). The successive Lake Spillways (modified from its terminus about 17.000 years ago.7 larger and deeper depressions are occu from Thorson, 1979).