Benthic Autotrophy in Netarts Bay, Oregon

Total Page:16

File Type:pdf, Size:1020Kb

Benthic Autotrophy in Netarts Bay, Oregon NETARTS BA) OREGON Final TechnicalReport to the Environ mental Protection Agency BENTHIC AUTOTROPHY IN NETARTS BAY, OREGON E ST U AR E In Reference to BIOLOGICAL Jiiiii( / EPA Research P ROCESSES \PRocE Grant No. R806780 (ACRO- OregonState University May I, 1983 7 ZOSTERA ALGAL / ss xposil PRIMARY PRIMARY \ 'ROD PROD1T O(TRITAL) PRETIO BENThIC AUTOTROPHY IN NETARTS BAY, OREGON Final Report Submitted June 1, 1983, to the Environmental Protection Agency 200 S.W. 35th Street Corvallis, OR97331 Prepared by C. David Mclntire, Professor and Michael W. Davis, Mary E. Kentula, and Mark Whiting Research Assistants Department of Botany and Plant Pathology Oregon State University Corvallis, OR 97331 in reference to EPA Research Grant No. R806780 entitled: "Relationships Between Nutrient Fluxes and Benthic Plant Processes in Netarts Bay, Oregon TABLE OF CONTENTS Introduction Background . .. .......... ....... Conceptual Framework for the Research Ecosystem Processes and Process Capacity ATentative Model of Estuarine Processes Netarts Bay . ............ ...... ...... EPARhodanuLneStudiesofl978andl979 ...... Some Relevant Literature ......... ........... ....... Benthic Microflora ...... .......... ...... Zostera and Macroalgae . .. Some Relevant Laboratory Studies ............................... Columbia River Project . ..... .. TheAlgaiPrimaryProductionSubsystetu... ........... Production Dynamics of Sediment-Associated Algae in Netarts Bay, Oregon . ....... Sampling Strategy ............... Methods . , . .. , ........ Primary Production . .......... Biomass . a * . .. ...... a a . Sediment Properties . ......... .......... Physical and Chemical Variables Data Analysis . .. ........ Results . .. ....... Physical Properties . * . .. Organic Matter . .. a a . a . a . a a . a a Chlorophyll a Concentration . ...... a a a . .. Primary Production . ......... a . a . a aa a . a a Relationships Among Variables .. .. ......... ... .. .. Interpretation of AutotrophicPatterns .................. ..... Experimental Studies of Estuarine Benthic Algae Yaquina Bay . a a . ...................... a a a a . a a . ....... Methods ................................. .......... .... ....... Primary Production . a a a .a . ..... a a a Biomass . a a a a . a a a a . a a . a a a . a a a . a . Isolation of DiatomAssemblages Physical Variables * . ......... a . * a a a . a a a a. a a . a a a Results .. ...... ............... ....a.... .aaaa.. .a.a..... I.. Experiments withlntact Sediment Cores Experiments with Isolated Epipelic Diatoms ...... Experiments with Isolated Macroalgae ... .......... Interpretation of Experiments ...... .. a . a ......... a a . ....... Effects of Estuarine Infauna on Sediment-Associated Microalgae Study Site ....... ......... ..... .. ............ Methods ....................................... -3- -Experimental Design . Metabolic Activity .......................................... Chlorophyll a Analysis ...................................... Macrofaunal Abundance ....................................... Statistical Analysis ........................................ Results ....... ................................................. Field Defaunation Experiment ................................ Laboratory Defaunation Experiment ........................... Interpretation of Defaunation Experiments ...................... The Diatom Flora of Netarts Bay ................................... Sampling ..... .................................................. Methods ........ ................................................ Data Analysis .................................................. Results ........................................................ StructureofEnvironmentalflata ............................. The Diatom Flora ............................................ AutecologyofSelectedTaxa ................................. Community Patterns .......................................... The Zostera Primary Production Subsystem ............................ Materials and Methods ............................................. DescriptionoflntensiveStudyArea ............................ SelectionofQuadratandSampleSize. .......................... Measurement of Biomass ......................................... MeasurementofPrimaryProduction .............................. Short Marking Methbd ........................................ RadjoactiveCarbon(14C) Method............................. Data Analysis .................................................. Morphometrics and Autecology of Zostera marina L. in Netarts Bay Sexual Reproduction ............................................. Vegetative Growth .............................................. ProductionDynamicsofZostera .................................... Biomass ...... .................................................. Primary Production ............................................. Relationship Between Zostera and Epiphytic Assemblages ............ Description of EpiphyticAssemblages ........................... Biomass .... .................................................... Production . .................................................... Components of Variance ......................................... Bioenergetics of the Zostera Primary Production Subsystem ......... Discussion ......... ............................................... References .... ...................................................... Appendixl........... INTRODUCTION This final report was prepared primarily for the information of persons having the responsibility of judging the merit of research supported by a grant from the Environmental Protection Agency (EPA No. R806780). The research program was initiated September 1, 1979 and the original project and budget periods extended from this date to August 30, 1981.Extensions of the project and budget periods were requested in May, 1981 and again in January, 1982. These extensions were granted, and the termination date for the project and budget periods was reset to August 30, 1982. Although scientists and other individuals interested in the production dynamics of benthic plants in estuaries may find this report an informative summary of our work during the prOject period, it is not intended to be a definitive publication and should not be evaluated as such. Instead, five manuscripts representing segments of the research presented in this report are in preparation for submission to refereed professional journals. The primary purpose of the final report is to integrate the various aspects of the research and to provide an outlet for the data that can be made available to other scientists. The general objective of research supported by EPA Grant No. R806780 was to determine mechanisms that control the production dynamics of benthic plants and associated epiphytes in Netarts Bay relative to physical processes and changing patterns of nutrient distribution. In particular, we were especially concerned with biological processes that were related to the patterns of nutrient flux determined by the EPA dye studies of August, 1978 and January, 1979. These studies involved the introduction of Rhodamine dye and subsequent -5- comparisons of the dye concentration with concentrations of substances of interest at selected stations in the estuary. Nutrients of interest included dissolved organic carbon (DOC), particulate organic carbon (POC), nitrate- nitrate (NO2-NO3), orthophosphorous (Ortho-P), ammonia nitrogen (NH3), and molybdate reactive silica (Si); in addition, temperature, salinity, turbidity, fluorescence at 460 nm and 660 nm, and Rhodamine concentrations also were monitored, The results of the EPA investigation suggested that nutrient dynamics were strongly related to biological processes associated with large areas of seagrass (Zostera marina) during August; but in January, correspond- ing patterns were more closely related to physical processes. Therefore, our general objective stated above was compatible with the EPA's research program at Netarts Bay and provided the basis for a detailed examination of benthic plant processes in the estuary. For research purposes, it was convenient to partition our work on benthic plant processes in Netarts Bay into two subsystems: Zostera Primary Produc- tion and Algal Primary Production. These subsystems are part of a tentative conceptual model of the entire estuarine ecosystem, the details of which are described in the next section of this report. The research approach involved an intensive field investigation of the two subsystems during a two-year period and some concurrent experimental work on the Algal Primary Production subsystem. The sampling strategy in the field was carefully designed to take advantage of the existing knowledge of nutrient distribution and circulation in the estuary. This report is organized into three major subsections: Background, The Algal Primary Production Subsystem, and The Zostera Primary Production Subsystem. In the Background section, we present a conceptual framework for the research, briefly describe the estuary, review the EPA dye studies of 1978 and 1979, and present a review of relevant literature. The Algal Primary Production Subsystem section is concerned with the production dynamics of benthic micro and macroalgae relative to sediment properties and other physical and biological variables. In this section, we also present the results of laboratory studies designed to establish functional relationships between algal primary production and selected physical and biological factors. The Zostera Primary
Recommended publications
  • Distribution and Sedimentary Characteristics of Tsunami Deposits
    Sedimentary Geology 200 (2007) 372–386 www.elsevier.com/locate/sedgeo Distribution and sedimentary characteristics of tsunami deposits along the Cascadia margin of western North America ⁎ Robert Peters a, , Bruce Jaffe a, Guy Gelfenbaum b a USGS Pacific Science Center, 400 Natural Bridges Drive, Santa Cruz, CA 95060, United States b USGS 345 Middlefield Road, Menlo Park, CA 94025, United States Abstract Tsunami deposits have been found at more than 60 sites along the Cascadia margin of Western North America, and here we review and synthesize their distribution and sedimentary characteristics based on the published record. Cascadia tsunami deposits are best preserved, and most easily identified, in low-energy coastal environments such as tidal marshes, back-barrier marshes and coastal lakes where they occur as anomalous layers of sand within peat and mud. They extend up to a kilometer inland in open coastal settings and several kilometers up river valleys. They are distinguished from other sediments by a combination of sedimentary character and stratigraphic context. Recurrence intervals range from 300–1000 years with an average of 500–600 years. The tsunami deposits have been used to help evaluate and mitigate tsunami hazards in Cascadia. They show that the Cascadia subduction zone is prone to great earthquakes that generate large tsunamis. The inclusion of tsunami deposits on inundation maps, used in conjunction with results from inundation models, allows a more accurate assessment of areas subject to tsunami inundation. The application of sediment transport models can help estimate tsunami flow velocity and wave height, parameters which are necessary to help establish evacuation routes and plan development in tsunami prone areas.
    [Show full text]
  • States Vulnerable to Ocean Acidification
    PACIFIC NORTHWEST IS AT HIGH RISK FOR ECONOMIC HARM DUE TO OCEAN ACIDIFICATION According to a new assessment of the U.S. communities most vul- nerable to ocean acidification, the Date Water Pacific Northwest is at high risk of Unfavorable Economic Sensitivity To Shellfish Score Other Factors economic harm. Communities and 2006 - 2030 High Algae Blooms 2031 - 2050 Medium High River Inputs governments can still take action, 2051 - 2070 Medium Upwelling 2071 - 2099 Medium Low researchers say. 2099 + Low MAP LEFT: The long-term economic impacts of ocean acidification are expected to be most severe in regions where ocean areas are acidifying soonest (black) and where the residents rely most on local shellfish for their livelihood (red). Local factors such as algae blooms from nutrient pollu- tion, local upwelling currents, and poorly buffered rivers (green, purple, blue) can amplify acidification locally. adapted by NRDC from Ekstrom et al., 2015 adapted by NRDC from Ekstrom et al., 2015 WHY IS THE PACIFIC NORTHWEST A HOTSPOT? ECONOMIC DEPENDENCE OCEAN VULNERABILITY A SALTY GOLDMINE. Shelled Some believe Puget Sound is the greatest oyster-growing mollusk fisheries in Washington region on the planet. Cold, clean and Oregon produce slightly water from deep currents off the more than $100 million annu- coast, a winding coastline with ally in direct sales. Though the thousands of inlets with sheltered economic benefits extend well water, and an abundant supply of beyond the value of the harvest. The estimated mountain-fed rivers all contribute to this perception. But this same formula has also total annual economic impact of aquaculture in put the region at risk from ocean acidification.
    [Show full text]
  • EA for Cascadia Spring/Summer Survey 2020
    Draft Environmental Assessment/Analysis of a Marine Geophysical Survey by R/V Marcus G. Langseth of the Cascadia Subduction Zone in the Northeast Pacific Ocean, Late Spring/Summer 2020 Prepared for Lamont-Doherty Earth Observatory 61 Route 9W, P.O. Box 1000 Palisades, NY 10964-8000 and National Science Foundation Division of Ocean Sciences 4201 Wilson Blvd., Suite 725 Arlington, VA 22230 by LGL Ltd., environmental research associates 22 Fisher St., POB 280 King City, Ont. L7B 1A6 21 November 2019 LGL Report FA0186-01A Table of Contents TABLE OF CONTENTS LIST OF FIGURES .......................................................................................................................................... iv LIST OF TABLES ............................................................................................................................................. v ABSTRACT .................................................................................................................................................... vi LIST OF ACRONYMS ..................................................................................................................................... ix I PURPOSE AND NEED ................................................................................................................................... 1 1.1 Mission of NSF ................................................................................................................................ 1 1.2 Purpose of and Need for the Proposed Action ................................................................................
    [Show full text]
  • Oceanography of the Pacific Northwest Coastal Ocean and Estuaries with Application to Coastal Ecosystems
    Oceanography of the Pacific Northwest Coastal Ocean and Estuaries with Application to Coastal Ecosystems Barbara M. Hickey1 and Neil S. Banas School of Oceanography Box 355351 University of Washington, Seattle, WA 98195-7940 Tel.: 206 543 4737 e-mail: [email protected] Submitted to Estuaries May 2002 1Corresponding author. Hickey and Banas 2 Abstract This paper reviews and synthesizes recent results on both the coastal zone of the U.S. Pacific Northwest (PNW) and several of its estuaries, as well as presenting new data from the PNCERS program on links between the inner shelf and the estuaries, and smaller-scale estuarine processes. In general ocean processes are large-scale on this coast: this is true of both seasonal variations and event-scale upwelling-downwelling fluctuations, which are highly energetic. Upwelling supplies most of the nutrients available for production, although the intensity of upwelling increases southward while primary production is higher in the north, off the Washington coast. This discrepancy is attributable to mesoscale features: variations in shelf width and shape, submarine canyons, and the Columbia River plume. These and other mesoscale features (banks, the Juan de Fuca eddy) are important as well in transport and retention of planktonic larvae and harmful algae blooms. The coastal-plain estuaries, with the exception of the Columbia River, are relatively small, with large tidal forcing and highly seasonal direct river inputs that are low-to-negligible during the growing season. As a result primary production in the estuaries is controlled principally not by river-driven stratification but by coastal upwelling and bulk exchange with the ocean.
    [Show full text]
  • Holocene) Diatoms (Bacillariophyta
    U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Taxonomy of recent and fossil (Holocene) diatoms (Bacillariophyta) from northern Willapa Bay, Washington by Eileen Hemphill-Haley1 OPEN-FILE REPORT 93-289 This report is preliminary and has not been reviewed for conformity with Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1. Menlo Park, CA 94025 TABLE OF CONTENTS ABSTRACT........................................................................................................................! INTRODUCTION..............................................................................................................^ Background for the Study .......................................................................................1 Related Studies......................................................................................................2 METHODS........................................................................................................................^ FLORAL LIST.....................................................................................................................4 ACKNOWLEDGMENTS......................................................................................................120 REFERENCES...................................................................................................................121 FIGURES Figure 1. Sample
    [Show full text]
  • Paleoseismicity of the Southern End of the Cascadia Subduction Zone, Northwestern California by David W
    Bulletin of the Seismological Society of America, Vol. 102, No. 3, pp. 1059–1078, June 2012, doi: 10.1785/0120110103 Ⓔ Paleoseismicity of the Southern End of the Cascadia Subduction Zone, Northwestern California by David W. Valentine, Edward A. Keller, Gary Carver, Wen-Hao Li, Christine Manhart, and Alexander R. Simms Abstract The southern end of the Cascadia subduction zone (CSZ) in northwestern California poses a high seismic hazard. This study uses the Quaternary stratigraphy of the bays and estuaries to reconstruct coseismic subsidence caused by strong to great earthquakes. We used lithology, macrofossils, and microfossils to estimate the amount of relative sea-level change at contacts caused by coseismic subsidence. Our paleo- seismic record contains evidence of four to six earthquakes over the past 2000 years. Using the pattern and magnitude of submergence and other paleoseismic information (trenches and other sites), we determine whether the earthquakes were local or regio- nal. We found that the record contained evidence for both smaller strong to major earthquakes on local structures (Mw 6.5–7.2) and larger regional subduction-zone- M >8:2 related great earthquakes ( w ). We compared our record to other records from Oregon and Washington and found three earthquakes likely caused by the rupture of the entire CSZ around approximately 230–270 (the A.D. 1700 event), 1150–1400, and 1750–1900 cal B.P. In addition, two other local earthquakes likely occurred around 500–600, 1000–1250, and possibly 1500–1650 cal B.P. Online Material: Table of radiocarbon ages obtained in the study. Introduction Prior to the works of Heaton and Kanamori (1984) and Our new record of earthquakes is compared to other paleoseis- Atwater (1987), the earthquake and tsunami threat along the mic studies further to the north to provide a better understand- Cascadia subduction zone (CSZ) was classified as minimal ing of the length of rupture along the CSZ.
    [Show full text]
  • The West Coast Ocean Acidification and Hypoxia Science Panel MAJOR FINDINGS, RECOMMENDATIONS, and ACTIONS
    The West Coast Ocean Acidification and Hypoxia Science Panel MAJOR FINDINGS, RECOMMENDATIONS, AND ACTIONS APRIL 2016 Table of Contents I. Introduction ............................................................................................................................................................................................................................. 4 II. Major Findings ......................................................................................................................................................................................................................... 5 III. Panel Recommendations ......................................................................................................................................................................................................... 6 IV. Appendices...............................................................................................................................................................................................................................13 Appendix A: Why West Coast managers should care about ocean acidification .......................................................................................................................................................14 Appendix B: Why the West Coast is vulnerable to ocean acidification – and what we can learn from it .............................................................................................................16 Appendix c: Managing for resilience
    [Show full text]
  • Netarts Water Trail Guidebook
    YOU HAVE ARRIVED! SCROLL DOWN TO FIND YOUR MOST CURRENT DRAFT This page does not print tillamook county water trail OREGON neTARTS WATERSHED Produced by the Tillamook Estuaries Partnership WelcomeWelcome to the Nehalemto Netarts Bay With the publication of the Netarts Bay water trail guidebook, a chapter closes for the local water trail community. It was over ten years ago that the Tillamook County Water Trail (TCWT) vision was brought forth. Since then, the five watersheds of Tillamook County have been celebrated through four guidebooks which reveal the uniqueness and similarities of local waterways and entice paddlers to explore further. Though the guidebooks are now complete, it is not the end of this endeavor. It will be exciting to see what blossoms from this experience and the efforts inspired by water trail enthusiasts. The TCWT has been a huge success, offering information that may not otherwise get into the hands of visitors, residents, and non-motorized paddlers. This project demonstrates that stewardship can happen in a thoughtful way, gently guiding folks in a direction of a healthy environment, while balancing recreation, community, and economy. Netarts Bay invites one to slow down, breathe deeply, and take a closer look. The bay is relatively small at just under four square miles. There are 14 streams and tributaries that encompass the entire 19 square mile watershed. Some wander through wetlands and others flow directly to the bay. The small community of Netarts Don Best, Best Impressions Picture Co. Don Best, lies at the north end of the bay and neighboring Oceanside is close by.
    [Show full text]
  • Aragonite Saturation State Dynamics in a Coastal Upwelling Zone Katherine E
    GEOPHYSICAL RESEARCH LETTERS, VOL. 40, 2720–2725, doi:10.1002/grl.50460, 2013 Aragonite saturation state dynamics in a coastal upwelling zone Katherine E. Harris,1 Michael D. DeGrandpre,1 and Burke Hales2 Received 11 February 2013; revised 8 April 2013; accepted 9 April 2013; published 6 June 2013. [1] Coastal upwelling zones may be at enhanced risk from [3] Coastal upwelling zones, such as the one along the ocean acidification as upwelling brings low aragonite U.S. Pacific coast, naturally experience low ΩAr values as saturation state (ΩAr) waters to the surface that are further Ekman transport pumps subsurface water onto the shelf dur- suppressed by anthropogenic CO2. ΩAr was calculated with ing periods of equatorward winds [Hales et al., 2005a; Feely pH, pCO2, and salinity-derived alkalinity time series data et al., 2008; Cao et al., 2011; Fassbender et al., 2011]. These from autonomous pH and pCO2 instruments moored on upwelling events also bring nutrients into the euphotic zone the Oregon shelf and shelf break during different seasons [Hales et al., 2005b]; and as a result, coastal upwelling zones from 2007 to 2011. Surface ΩAr values ranged between are some of the most biologically productive in the world 0.66 Æ 0.04 and 3.9 Æ 0.04 compared to an estimated [Muller-Karger et al., 2005]. The resultant commercial fish- pre-industrial range of 1.0 Æ 0.1 to 4.7 Æ 0.1. Upwelling eries are economically important [Chavez and Messie, 2009] of high-CO2 water and subsequent removal of CO2 by and therefore ocean acidification could have important implica- phytoplankton imparts a dynamic range to ΩAr from tions for both the marine ecosystem and the fisheries economy ~1.0 to ~4.0 between spring and autumn.
    [Show full text]
  • Changing Ocean Chemistry a High School Curriculum on Ocean Acidification’S Cause, Impacts, and Solutions
    Changing Ocean Chemistry A High School Curriculum on Ocean Acidification’s Cause, Impacts, and Solutions Brian Erickson Marine Resource Management Program, Oregon State University Tracy Crews Oregon Sea Grant, Oregon State University Sm&fut Oregon Changing Ocean Chemistry A High School Curriculum on Ocean Acidification’s Cause, Impacts, and Solutions Brian Erickson Marine Resource Management Program, Oregon State University Tracy Crews Oregon Sea Grant, Oregon State University Written by Brain Erickson and Tracy Crews; designed and laid out by Heidi Lewis; edited by Rick Cooper, Brian Erickson, and Tracy Crews; cover photo by Tiffany Woods; inset photos by iStock.com/heinstirrer (top) and Tiffany Woods (middle and bottom). © 2019 by Oregon State University. This publication may be photocopied or reprinted in its entirety for noncommercial purposes. To order additional copies of this publication, call 541-737-4849. This publication is available in an accessible format on our website at seagrant.oregonstate.edu/publications, where you can also find a complete list of Oregon Sea Grant publications. This report was prepared by Oregon Sea Grant under award number NA18OAR4170072 (project number A/E/C-OED 2018-21) from the National Oceanic and Atmospheric Administration’s National Sea Grant College Program, U.S. Department of Commerce, and by appropriations made by the Oregon State Legislature. The statements, findings, conclusions, and recommendations are those of the authors and do not necessarily reflect the views of these funders. Gifuit OregonState Oregon University• Oregon Sea Grant Corvallis, OR ORESU-E-19-002 Acknowledgments This curriculum would not have been possible without funding from Wendy and Eric Schmidt’s generous gift in support of Oregon State University’s Marine Studies Initiative, in honor of Dr.
    [Show full text]
  • Barton, Alan, Et Al. the Pacific Oyster
    Limnol. Oceanogr., 57(3), 2012, 698–710 E 2012, by the Association for the Sciences of Limnology and Oceanography, Inc. doi:10.4319/lo.2012.57.3.0698 The Pacific oyster, Crassostrea gigas, shows negative correlation to naturally elevated carbon dioxide levels: Implications for near-term ocean acidification effects Alan Barton,a Burke Hales,b,* George G. Waldbusser,b Chris Langdon,c and Richard A. Feelyd a Pacific Coast Shellfish Grower’s Association, Emerald Isle, North Carolina bCollege of Oceanic and Atmospheric Sciences, Oregon State University, Corvallis, Oregon c Department of Fisheries and Wildlife and Coastal Marine Experiment Station, Oregon State University, Newport, Oregon dPacific Marine Environmental Laboratory, National Oceanic and Atmospheric Administration, Seattle, Washington Abstract We report results from an oyster hatchery on the Oregon coast, where intake waters experienced variable carbonate chemistry (aragonite saturation state , 0.8 to . 3.2; pH , 7.6 to . 8.2) in the early summer of 2009. Both larval production and midstage growth (, 120 to , 150 mm) of the oyster Crassostrea gigas were significantly negatively correlated with the aragonite saturation state of waters in which larval oysters were spawned and reared for the first 48 h of life. The effects of the initial spawning conditions did not have a significant effect on early-stage growth (growth from D-hinge stage to , 120 mm), suggesting a delayed effect of water chemistry on larval development. Rising atmospheric carbon dioxide (CO2) driven by on the North American Pacific coast takes on the order of anthropogenic emissions has resulted in the addition of decades to transit from the point of subduction to the over 140 Pg-C (1 Pg 5 1015 g) to the ocean (Sabine et al.
    [Show full text]
  • Netarts Sand Spit
    PRESERVE ANALYSIS : NETARTS SAND SPIT Prepared by Gregg L, Bonacker Robert C. Martin Robert E. Frenkel OREGON NATURAL AREA PRESERVES $1 ADVISORY COMMITTEE to the State Land Board Salem, Oregon August, 1979 NATURAL AREA PRESERVES ADVISORY COMMITTEE to the OREGON STATE LAND BOARD Victor Atiyeh Norma Paulus Clay Myers Governor Secretary of State State Treasurer Members Robert E. Frenkel (Chairman), Corvallis Bruce Nolf (Vice Chairman), Bend Charles Collins, Roseburg Richard Forbes, Portland Jefferson Gonor, Newport Jean L. Siddall, Lake Oswego David Wagner, Eugene Ex- Officio Members Judith Hvam Williams S. Phelps Department of Fish and Wildlife State Forestry Department Peter Bond J. Morris Johnson State Parks and Recreation Division State System of Higher Education PRESERVE ANALYSIS: NETARTS SAND SPIT prepared by Gregg L. Bonacker Robert C. Martin and Robert E. Frenkel Oregon Natural Area Preserves Advisory Committee to the State Land Board Salem, Oregon August, 1979 - -- - ,. PREFACE The purpose of this preserve analysis is to document the significant natural values of Netarts Sand Spit in Cape Lookout State Park to aid in deciding whether to recommend the dedication of a portion of the spit as a natural area preserve within the Oregon System of Natural Areas. Preserve management, agency agreements, and management planning are therefore not a function of this document. Netarts Sand Spit and its adjacent relatively undisturbed estuary have long been recognized together as one of Oregon's finest coastal features. The sand spit, without structures and with little human impact, is the most pristine sand spit in the state. With a diversity of geological and biological types, the sand spit has already attracted considerable amount of scientific research.
    [Show full text]