Characteristics of Three Western Pearlshell (Margaritifera Falcata) Populations in the Chehalis River Basin, Washington State

Item

Title
Eng Characteristics of Three Western Pearlshell (Margaritifera Falcata) Populations in the Chehalis River Basin, Washington State
Date
2013
Creator
Eng Waterstrat, Frithiof Teal
Subject
Eng Environmental Studies
extracted text
CHARACTERISTICS OF THREE WESTERN PEARLSHELL (MARGARITIFERA FALCATA)
POPULATIONS IN THE CHEHALIS RIVER BASIN, WASHINGTON STATE

by
Frithiof Teal Waterstrat

A Thesis
Submitted in partial fulfillment
of the requirements for the degree
Master of Environmental Studies
The Evergreen State College
August 2013

© 2013 by Frithiof T. Waterstrat. All rights reserved.

This Thesis for the Master of Environmental Studies Degree
by
Frithiof Teal Waterstrat
has been approved for
The Evergreen State College

by

________________________
Dr. Carri J. LeRoy
Member of the Faculty

________________________
Date

ABSTRACT
CHARACTERISTICS OF THREE WESTERN PEARLSHELL (MARGARITIFERA FALCATA)
POPULATIONS IN THE CHEHALIS RIVER BASIN, WASHINGTON STATE

Freshwater unionoid mussels are the most imperiled family of freshwater organisms in North
America. In Washington State, documentation of mussel populations, abundances, and
investigations of environmental conditions influencing their morphology are limited to a few
studies. Here, I describe three populations of the western pearlshell (Margaritifera falcata) in
the lower Chehalis River basin occurring along an ecological and physical gradient from a
headwater stream to a major regional river. Quantitative analysis revealed a trend of increasing
shell size as well as shell weight to length ratio along this gradient, but I found no difference in
external shell measurement ratios as watershed area increased. Environmental conditions that
coincide with an increase in western shell size and proportional shell weight are discussed
within. Additionally, information regarding mussel distributions was gleaned from opportunistic
interviews with individuals encountered during this research as well as from field notes during
surveys for native fish populations. These were then compared to existing records of mussel
distributions in Washington. This information led to the reporting of 15 specific mussel
localities in this thesis not yet documented in existing databases. The number of previously
undocumented populations and the existence of local ecological knowledge about mussel
populations make the recognized need for a regionally specific central database for mussel
records more important. Information found in this document will increase our understanding of
the variation among populations of western pearlshell in Washington and provide support for
documenting existing and perhaps historic populations while the mussels, and knowledge of
them, is extant.

TABLE OF CONTENTS

Page

List of Figures:

vi

List of Tables

vii

Acknowledgements

viii

Chapter 1: Introduction

1

Chapter 2: Literature Review

6

Freshwater mussels

6

Declines of freshwater mussels

9

Mussels in Washington State

15

The western pearlshell in Washington State

18

Chapter 3: Methods

24

Site descriptions

24

Sampling design

28

Statistical analysis

35

Chapter 4: Results

38

Western pearlshell abundance estimates

38

Shell Morphology

39

Age and population structure

45

Habitat preferences

47

Informational interviews and opportunistic
sampling

55

Chapter 5: Discussion

56

Demographics and mussel abundance

56

Morphological patterns in mussels along
a river spectrum

58

TABLE OF CONTENTS

Page

Comparisons of environmental conditions

61

Limitations of this study

65

Conclusions

67

Chapter 6: The future of mussels in Washington State

69

Western pearlshell of Washington: Past, present
and future

69

Documentation of mussels in Washington State

71

Conclusions

73

Appendix I: Noted flora and fauna at sites

74

Appendix II: Field protocols and datasheets

77

Appendix 3: Details of informal communications and
opportunistic sampling

85

Works cited

86

LIST OF FIGURES

Page

Figure 1: Conceptualization of pearlshell mussels,
the River Continuum Concept, and Ortmann’s Law

4

Figure 2: Priority Species Habitat Database localities
for native freshwater mussels in Washington State

19

Figure 3: Map of study sites

25

Figure 4: Random sampling grid for mussel plots

29

Figure 5: Directions and dimensions of freshwater mussels 33
Figure 6: Mussel length distributions

39

Figure 7: Mussel valve metric

41

Figure 8: Ortmann’s Law

42

Figure 9: Weight to length ratios for Stillwater Creek
and South Elma study sites

44

Figure 10: Western pearlshell growth rates in Stillwater Creek
and South Elma study sites
45
Figure 11: Mean age of western pearlshell in Stillwater Creek
and South Elma study sites
46
Figure 12: Western pearlshell age composition Stillwater Creek
and South Elma study sites
47
Figure 13: Western pearlshell substrate preference

48

Figure 14: Annual water temperature profiles

50

Figure 15: Mean water temperatures for July –
September, 2012

51

Figure 16: Hydrograph of study sites

52

Figure 17: Mean water velocity at substrates

53

Figure 18: Oral map of native mussels in Washington State 54

vi

LIST OF TABLES

Page

Table 1: Native freshwater mussel species of
Washington State

16

Table 2: Summary table of mussel abundance
and density

38

Table 3: Water quality test results

49

Table 4: Water temperature summary for July –
September, 2012

51

vii

ACKNOWLEDGEMENTS
I would like to thank: Megan Cook1, Michael Elam2, Howard Gearns2, Tim Grun2, Nate
Gilman3, Kira Mazzi2, Zach Moore2, 3, Clay Showalter2, 3, Keith Sweeny2, and Sheila and
Hudson Waterstrat for their assistance in collecting field data. Additionally I thank Molly
Hallock4 (WDFW retired) and Roger Tabor2 for their assistance in data collection and technical
assistance with study design. I am grateful to Dr. Carri LeRoy3 and members of PNW Native
Freshwater Mussel Working Group4, especially Kevin Aitkin2,4 and Al Smith, and Isabella
Sarikhan4 for their advice and expertise during this study. Additionally, I appreciate Phillip
Peterson (Forest and Channel Metrics, Inc.) for leading me to Stillwater Creek and Eric Beach
(Green Diamond Resource Company) for granting me access to private lands.
Lastly, and most dearly, I would like to thank my wonderful wife Sheila, who allowed me to
spend many a night in class and forced me into my studies, as well as my sons: Hudson, for
tolerating my absence at story time, and Leif, for catalyzing the final push.
1. Washington Department of Natural Resources, Geology Division: 600 Capitol Way N, Olympia, WA
98501
2. USFWS Washington Field Office: 510 Desmond Dr. NE, Lacey, WA 98503
3. The Evergreen State College Faculty and Students: 2700 Evergreen Parkway, Olympia, WA 98
4. Pacific Northwest Native Freshwater Mussel Work Group

viii

Chapter 1: Introduction
Freshwater ecosystems are some of the most critically imperiled systems in the world
(Richter et al. 1997, Dudgeon et al. 2006, Strayer and Dudgeon 2010). The obvious and obligate
human, biological, cultural, and public health needs for fresh water, along with declines in water
quality and species richness, have led to contemporary protection, conservation, and restoration
actions in North America. Recently, these efforts have included the management and restoration
of freshwater mussel populations throughout North America. However, the status of freshwater
mussels in the northwestern United States including Washington State is not well known.
Freshwater mussels are recognized as the most imperiled group of organisms in North
America (Williams et al. 1993, Stokstad 2012). Despite this knowledge, only recently have
natural resource managers focused their attention on this diverse and abundant group and its
ecological role. In North America, 35 species are already extinct and 70 more are considered
threatened with extinction (Stokstad 2012). In Washington State there are a number of reports of
declining and disappearing populations of freshwater mussels (Hovingh 2004, Krueger et al.
2007, Hastie and Toy 2008, Helmstetler and Cowles 2008, Cowles 2012, Jespen 2012).
Washington State is home to three genera of freshwater mussels, yet in many of these rivers,
little is known about them and their presence is often overlooked. Washington State’s effort to
document distributions of freshwater mussels, describe the variation among populations in their
habitats, or monitor their populations has been left to a small number of impassioned individuals
and workgroups.
In this study, I focus on the lower Chehalis River basin in southwestern Washington
because of prior documentation of mussel populations in the area, as well as its proximity to

1

active agricultural, industrial, and forest land use practices. In this thesis, I describe the
abundance, demographics, and physical habitats of three populations of western pearlshell
(Margaritifera falcata) within this watershed, and investigate anecdotal knowledge about
freshwater mussels using information from informal interviews.
Western pearlshells are one of the more common and widespread mussel species in
running waters in Washington State and inhabit a wide variety of habitats from the Columbia
River (one of the North America’s largest rivers), to small, roadside ditches with permanent
water. It stands to reason that the physiology and life history of a sessile organism living in such
a large spectrum of environments would also have many variations. This study will provide a
general synopsis of western pearlshell populations in the East Fork Satsop River and the
Chehalis River, as well as specific information that can be used for more expansive detection and
monitoring of the western pearlshell of the Lower Chehalis watershed. I compared western
pearlshell size and growth at three distinct sites to determine if a difference in western pearlshell
morphology exists and if so, what environmental conditions are driving those morphological
variations.
The importance of understanding how mussels grow and respond to different
environmental conditions within their known habitat is of importance for future monitoring,
restoration of habitat, and reintroduction should western pearlshell abundance decline further
within this, or other, watersheds. Monitoring is especially important for mussels because a
population of long-lived individuals can appear stable for decades but actually be composed
mainly of older mussels, lacking the younger cohorts that are vital in replenishing the population
(Jespen et al. 2010b). Studies in Northern Europe have found that physical and chemical
differences in instream conditions can cause measurable differences in shell morphology
2

(Preston et al. 2010). The differences between populations of pearlshell can even cause
reductions in survivorship when individuals are translocated between streams, perhaps
influencing the success of restoring or supplementing populations (Valovirta 1990, Preston et al.
2010).
I completed a pilot study evaluating the cost-effectiveness of different visual survey
methods for freshwater mussels and verifying historic and new populations of native freshwater
mussel fauna in 2011. Many of the surveys were carried out in the East Fork of the Satsop River
from Satsop Springs Hatchery (47° 6.726’ N, 123° 26.393’ W) to the confluence of the mainstem
Satsop River and the Chehalis River (46° 58.609’ N, 123° 29.145’ W). This effort covered
approximately 31.2 km and roughly 100 person hours (F. Waterstrat, unpublished data). These
surveys resulted in locating two previously undocumented populations of freshwater mussels in
the lower reaches of the Satsop River, one of western pearlshell, another of Anodonta Clade II
(historically A. oregenensis), and a failure to relocate a historic western pearlshell locality near
Schafer State Park (47° 5.916’N, 123°27.951’W) on the East Fork of the Satsop River.
Additional surveys were conducted in January 2012 in Stillwater and Phillips creeks which are
both in the headwaters of the East Fork Satsop River after a review of Green Diamond survey
databases and communication with former biologists indicated the presence of freshwater
mussels in that system. One population of western pearlshell was identified in Stillwater Creek
upstream of its confluence with Phillips Creek and an additional population was found in early
August 2012 at roughly 4 river km upstream of the convergence of Stillwater and Bingham
Creeks. Other water bodies in southwest Washington were systematically or opportunistically
surveyed during 2011 – 2013 for native and non-native freshwater mussels and all confirmed

3

observations were reported to Washington Department of Fish & Wildlife. These surveys
provided the initial observations that led to the completion of this thesis.

Figure1: Conceptual diagram relating Ortmann’s "Law" (1920) and the River Continuum (1980) for predictions of
western pearlshell morphology in the lower Chehalis watershed.

Selected survey sites, which ranged from the headwaters to the mainstem of a major
regional river, framed this investigation with the theories outlined in the River Continuum
Concept (Vannote et al 1980) and Ortmann’s Law of Stream Position (Ortmann 1920). Visual
inspection of western pearlshell at each site led to the hypothesis that size would increase and
shell morphology would change in a predictable manner as watershed area and water discharge
increased (Fig 1).
4

Ortmann’s Law describes a broad trend of increasing shell width to length ratio (valve
inflation) for lotic (riverine) mussels increasing in a downstream fashion in the Mississippi River
drainage (Ortmann 1920). This relationship was not found to hold true for eastern species of
Margaritiferidae and to my best knowledge, remains untested in western populations. It has been
hypothesized that the variation in shell morphology, as described in Ortmann’s Law, is a strategy
to either stay anchored in place or allow for quick reburial during a disturbance event such as
swift flows (Stanley 1981, Watters 1994). Shells with increased sculpture or ornamentation have
been proven to help retain sediment and substrate in high flows and shells where ornamentation
is lacking are able to rebury themselves more quickly after or during disturbances (Stanley
1981). In this study I hypothesized that although mussels in the Pacific Northwest lack
ornamentation and that eastern North American Margaritiferidae do not follow Ortmann’s law,
there may be other undescribed phenotypic variation in freshwater mussels related to
environmental conditions (Preston et. al 2010). As previously mentioned, mussel populations in
the Pacific Northwest and Washington State (Jepsen 2010) are declining and many eastern
freshwater mussel species are listed as threatened or endangered according to the US Endangered
Species Act (Stokstad 2012). These designations mandate population recovery and may lead to
the reintroduction of mussels to areas in which they have been extirpated. There is sparse
documentation about the variation among populations of mussels in Washington and there is a
body of evidence that not all populations of mussels are equally successful under various
conditions. A study in Great Britain found differences in shell morphologies and lower mortality
rates of pearlshell within similar environmental conditions than those from outside watersheds
(Preston et. al 2010). This suggests that there is some degree of specialization within species to
differing environmental conditions.

5

Chapter 2: Literature Review:
An alarming decline in freshwater mussel populations and a continuing number of mussel
species extinctions is currently underway in North America. The disappearance of mussels will
be summarized along with an explanation of a number of the possible causes and why immediate
conservation efforts are needed. As freshwater mussels are not commonly to the public, a general
understanding of their biological classification and basic life histories is needed in order to frame
this thesis. A summary of freshwater mussels in the Pacific Northwest, with an emphasis on
ecological trends and environmental conditions affecting western pearlshell, will describe the
research and general knowledge about mussels in Washington State that provide the foundation
for this study.

Freshwater Mussels

Freshwater mussels, hereafter mussels, are molluscs (Linnaeus, 1758) of the class
Bivalvia (Linnaeus, 1758) and the order Unionoida (Fleming, 1828). Literature prior to the
1970’s may refer to mussels as naiads, but most contemporary literature uses the term “mussel”
and they should be considered the same organisms. Globally there are approximately 840 species
of freshwater mussels (Graf and Cummings 2007). North America contains the greatest diversity
of species with between 297 and 302 species represented by the: 1) Margaritiferidae (5 species)
and 2) Unionidae (~295 species) families (Williams et. al. 1993, Graf and Cummings 2007). The
exact number of species is currently in question as genetic tools are being employed to
reevaluate species designations and taxonomic investigations are ongoing (see Mock et al. 2004,
Campbell and Lydeard 2012).

6

Mussels are primarily aquatic infaunal filter-feeding organisms found in perennial
freshwater systems. Although mussels are capable of short vertical migrations in benthic
substrates and short horizontal movements across the substrate, they are typically regarded as
mostly sessile organisms once larvae have settled in the substrate.
Mussels have a unique and complex reproductive life history that includes an obligate
parasitic stage. Mussels use a sperm-cast mating pathway for fertilization, in which sperm
released by males is captured by females during filter-feeding and fertilizes eggs in
suprabranchial gills, outside the reproductive organs of the female, in contrast to true internal
fertilization (Bishop and Pemberton 2006). Once fertilized, embryonic mussels develop into
glochidia, or larval mussels, and hosts (often fish) are attracted to the gravid female in what can
be a stunning variety of behavioral and morphological adaptations. Glochidia are released
singularly or in a discrete mass called a conglutinate and infect an intermediate host organism by
attaching to the gills, scales, fins, and other tissues. Host organisms are almost exclusively bony
fish (Osteichthyes Huxley, 1880) or very infrequently salamanders (Caudata Scopoli, 1777)
(Thomas Watters and O’Dee 1998). The glochidia clamp to the host’s tissue and become
encysted for days to months, sometimes absorbing nutrients from the host, before
metamorphosing into juveniles, releasing from the host organism, and settling in the aquatic
substrate. After settlement, mussels grow into maturity, filter-feed, and for the most part stay in
situ for the remainder of their lives.
Much progress has been made in the past twenty-five years to understand the role of
mussels in freshwater systems. As long-lived and stationary organisms, they are long-term
indicators of ecosystem health within aquatic systems composed primarily of organisms with
relatively short lives and motile life histories. They provide records of environmental conditions
7

and sequester the chemical composition of water in their tissue and deposit visible annual rings
in their shells (Cope et al. 2008, Black et al. 2010, Farris and Hassel 2010). Mussels remove
particulate matter from the water column, which improves water quality, cycling nutrients, and
concentrating dilute nutrients to the benthos subsequently providing food for other organisms.
One of the many ecological processes performed by native freshwater mussels is
suspension-feeding which removes particulate matter from the water column, therefore
improving water quality and concentrating nutrients otherwise unavailable to benthic organisms
(Vaughn et al. 2009). Mussels create a vacuum through the movements of cilia on the gill
mantle, which suctions water, and with it particulate matter, through the incurrent aperture
located posteriorly and ventral to the excurrent aperture. Particulate matter is sorted coarsely by
papillae and then further sorted into food and non-food items by internal labial palps. Non-food
items are encased in a mucus coating and expelled as pseudofeces. Accepted food is digested and
fecal waste is expelled through the excurrent valve. Suspension feeding rates can be more than 1
Liter per hour per mussel and in dense populations mussels are capable of filtering water
volumes in excess of a river’s daily discharge (Vaughn et al. 2008, Haag 2012). Without the
presence of healthy freshwater mussel populations, stream conditions for native organisms can
deteriorate.
As epi-benthic organisms, partially in the substrate and partially in the water column,
mussels transfer energy from the water to the substrate and are described as couplers between
benthic and water column nutrient sources (Vaughn et al. 2008). Mussels also create important
micro- and meso-habitats within and around their aggregations, or beds. Within the bed they
provide stable micro-habitats for macroinvertebrates and microorganisms during high flow
events (Vaughn et al. 2008). They also provide a reliable source of nutrients which can lead to
8

higher densities of macroinvertebrates found within mussel beds than outside of them (Spooner
and Vaughn 2006). For example, the growth and health of Pacific lamprey (Lampetra
tridentate)are greater for those raised within a mussel bed than those excluded from mussels
(Limm and Power 2011). The shells of living or dead mussels provide structures for periphyton

and macroflora to establish and grow upon (Vaughn et al. 2008).
In addition to their unique life histories and important role in water quality and nutrient
cycling, mussels are consumed as food by many organisms such as: muskrats, raccoons, birds,
turtles, sunfish, white sturgeon, and invertebrates (Bauer and Wächtler 2001, Wydoski and
Whitney 2003, Nedeau et al. 2009, Haag 2012). Mussels often occur in large stationary
aggregations, making them both a reliable and abundant food source year round. In North
America muskrats (Ondatra zibethicus) are a primary predator and their consumption of mussels
can influence mussel abundance and species distribution (Neves and Odom 1989).
To humans, mussels have historically and contemporarily provided food sources, material
resources, decorative and functional ornamentation, and sources of income. In the Pacific
Northwest, Native Americans used mussels as a source of food from at least the central Puget
Sound to the Tri-cities vicinity (Wong 1993, O’Brien et al. 2013), and also for tools and
ornamentation (O’Brien et al. 2013). Contemporarily freshwater mussels were of major
economic importance in eastern North America as the raw material for button manufacturing
until post World War II, for the pearl harvest into the 1950’s, and as material to seed the foreign
pearl production industry into the 1990’s (Haag 2012).

Declines of Freshwater Mussels

9

Freshwater mussels are in steep decline globally (Strayer 2008), with sources stating global
declines of 72%, 69%, and 72% (Williams et al 1993, Stein et al. 2000, Turvey 2009
respectively) for the families imperiled in North America. Although estimates of decline within
the Unionid family vary slightly, it is consistently considered the most imperiled family of
organisms in North America. North America had lost 21 species of mussels by the early 1990’s
(Williams et al. 1993) and twenty years later that number increased to 35 extinct species
(Stokstad 2012).
From the 1800’s to post World War II mussel declines in North America were primarily a
result of over harvesting of mussels for the pearl and button trade in the eastern and southeastern
regions. The creation of buttons from shells of freshwater mussels ended after the advent of
modern plastics created a cheap and reliable substitute. This historic commercial use of mussels
created dramatic local declines in mussel populations, but remarkably did not push any species
into extinction (Haag 2012). The harvest of mussels for seeding pearl growth in the Asian pearl
production market continued into the late 1990’s in the southeastern US until the simultaneous
collapse of pearl oyster stocks, the declining Japanese economy, and new pearl seeding methods
by the Chinese and Japanese pearl producers reduced the demand for American mussel shells
(Haag 2012).

Modern extinctions and declines in freshwater fauna including mussels are attributed to four
anthropogenic disturbances: habitat alteration (often because of hydraulic impoundments; Bogan
1993), declining water quality (Williams et al. 1993, Richter et al. 1997, Dudgeon et al. 2006),
invasive species (Williams et. al. 1993), and global climate change (Hastie et al. 2003, Pandolfo
et al. 2010).

10

Impoundments

The alteration of many of North America’s waterways by impoundment, diversions,
channelization, and other means has changed the hydrology and instream water conditions from
their historic natural states. These shifts from lotic to lentic (lake-like) systems have contributed
to lowered numbers and species of freshwater mussels, alteration of temperature regimes and
sediment transport, elimination of host fish to upstream reaches, and deviation from the historic
high and low water discharge periods (Williams et al. 1993, Bogan 1993, 2008, Vaughn and
Taylor 1999, Stokstad 2012). Water pooling behind dams and impoundments increases
sedimentation, smothering riverine species adapted to coarser substrates, increases temperatures
to levels detrimental or fatal to species adapted to cooler temperatures, eliminates the habitat
used by host fish, and isolates mussel populations from each other (Bogan 1993, Vaughn and
Taylor 1999). Riverine mussels, typically thicker shelled than still water mussels, evolved to
withstand the erosional force of moving water and sediments. However, heavy shelled riverine
species are unable to dig out of fine sediments which accumulate behind impoundments and
sink into or are buried by the substrates where they suffocate (Vannote and Minshall 1982).
Dramatic changes in water depth due to draw downs for spring melts or to electric power
demands can lead to mussels becoming stranded out of the water and perishing. Native host fish
required for reproduction of freshwater mussels often share habitat preferences with their
freshwater mussel parasites at some point in their life history. Impoundments can, in some
situations, physically block fish access to upstream habitats eliminating the possibility for
reproduction or altering the habitat to a degree that the lack of fish hosts becomes an ecological
barrier to reproduction (Bogan 1993). Interestingly, impacts of dams and impoundments in many
cases also create habitats that are beneficial to non-native species or to native mussel species not
11

typically found in lotic habitats. Indeed often native lentic-adapted mussel species may replace
their lotic counterparts behind impoundments and a shift from lotic-loving to still water species
may occur (Watters 1999). Mussels require a specific set of physical and biological attributes for
growth and reproduction and the construction of impoundments can alter water bodies and create
unsuitable conditions for historic native populations to exist.

Water Quality and Pollution
Declining water quality from pollution, land use practices, and watershed alterations have
been identified in the decline of freshwater life worldwide. In North America, pollution was
implicated in the destruction of freshwater mussel populations as early as 1909 (Ortmann 1909).
As stationary creatures, mussels have little ability beyond “clamming up” and burrowing into the
substrate to avoid unfavorable water conditions. While this strategy may be useful for short term
avoidance it is of little benefit when encountering chronic conditions of poor water quality.
Pacific drainage mussels in the genera Margaritifera and Anodonta can be found living in
highly urbanized creeks and ponds as well as more pristine environments (Nedaeu et al 2010).
Reports of mussels in urban areas document declining populations and evidence of decreasing
recruitment possibly from the effects of urbanization on habitat (Hastie and Toy 2008). In
general, mussels need waters rich in calcium carbonate to grow and maintain their shells and are
absent in highly acidic conditions which can lead to shell deterioration. The exception to this
common theme is M. margaritifera, a congener of western pearlshell, which is often the only
mussel found in soft, calcium-poor waters. Water quality thresholds for Margaritifera reported in
Great Britain state that levels greater than 1.0 mg/L-1 for nitrate and 0.03 mg/L-1 for phosphate
are detrimental especially to the larval forms (Young et al. 2003). Margaritifera prefer

12

oligotrophic (nutrient-poor) conditions with a neutral to basic pH and conductivity less than 100
µS-1 (Young et al 2003).
As previously stated, mussels have complex life cycles and various life stages. Each life
stage is exposed to the contaminants in the water through a different vector, of varying durations,
at different locations in the watershed, and with differing levels of tolerance to pollutants (Cope
et al. 2008). It is likely that the behavioral and physiological responses of mussels vary with life
stage and species. Once the mussel has settled in the sediment and begun its life as a filter feeder
it is exposed to every particle in the water for the duration of its life and readily accumulates
metals and other pollutants (Naimo 1995). Currently, mussels are being extensively tested for a
host of chemical compounds to understand their effect on mussel physiology. Due to the high
number of species in North America, and the cocktail of pollutants and their unknown
interactions, the full suite of pollutants and their effects on mussels will likely never be fully
documented.

Aquatic Invasive Species
Aquatic invasive species (AIS) are one of the great challenges for native organisms
worldwide including North America’s native freshwater mussel assemblages. Invasive species
can impact mussel populations in several ways. Invasive Dreissena mussels directly compete
with native freshwater mussels for food resources In addition, these invasive mussels attach to
native mussel shells as substrate which impairs their ability to function physiologically, restricts
their ability to move, and exhausts them to death (Haag et al. 1993). The Asian clams in the
Corbicula genus have been in North America since the early 1900’s and also compete with
native mussels for food and habitat (Counts III 1986). However, the impacts of Asian clams on

13

native mussels varies in the literature from detrimental to neutral (Leff et al. 1990). Some
invasive fish may consume native mussels (Poos et al. 2010) and non-native plants can alter the
substrate, planktonic abundance and velocity of streams, limiting habitat and food resources
throughout aquatic ecosystems (Strayer 2010). On the other side of the coin, freshwater mussels
are also among the most successful AIS themselves, including the zebra (Dreissena polymorpha)
and quagga (Dreissena bugensis) mussels, Asian clams (Corbicula spp) (non-unionid mussels),
and the Chinese mussel (Anodonta woodiana) (Douda et al. 2012).

Climate Change
Climate change is a global phenomenon that will affect most organisms on this planet to
some degree. Freshwater mussels are particularly susceptible to shifts in climate because of their
complex and host-obligate life histories and the inability of individuals to migrate in adverse
conditions (Hastie et al. 2003). Mussels have thermal tolerances that may be exceeded as the
seasonal maximum and minimum temperatures expand in range and shift in timing. In fact, some
species may already exist at the edge of their thermal tolerances (Pandolfo et al. 2010). Climate
change has brought measurable changes in the magnitude and timing of precipitation and
snowmelt events that control in-stream water volume. These changes can negatively affect
mussels in a number of ways. An increase in major flood events from increased precipitation
could cause mussels to be scoured from the substrate, and alter host fish assemblages and
movement patterns, in turn decoupling the mussel’s reproductive life history. Rising sea levels
could impact low-lying coastal populations exposed to tidal fluctuations and incursions of salt
water into freshwater mussel habitats (Hastie et al 2003). In the Pacific Northwest climate
change models have predicted wetter, warmer winters and drier, hotter summers (Mote and

14

Salathe 2010). Predicted hotter and drier summers may reduce water volume and discharge. This
can potentially expose shallow mussel beds, cause rivers to deposit sediments and organic
materials, and increase algal growth on the stream bed making it less suitable for mussels (Hastie
et al. 2003).

Mussels in Washington State

Currently, North American freshwater mussels are divided into four broad geographic
regions and 17 faunal provinces (Haag, 2010). The Pacific Region, which includes Washington
State, contains a singular Pacific province which encompasses all waters flowing into the Pacific
Ocean from North America, including the Gulf of California and the Bering Sea. Within this
region, there are at least five species of Pacific freshwater mussels represented by 3 genera:
Margaritifera (1 sp.), Gonidea (1 sp.) and Anodonta (unknown number of spp.) (Nedeau et. al.
2009, Haag 2010), which is the lowest species diversity for any region (Table 1). Nevertheless,
the Pacific Region is unique in that all species are endemic to the region. Washington State is
inhabited by all but one of the five species with western pearlshell being the most widespread
and common (Jepsen et. al. 2010) and all species but the Yukon floater (A.bergingiana) present
(Nedeau et. al. 2009). Three of the five species of freshwater mussels have been recorded in the
Chehalis watershed with the Anodonta Clade I complex not represented (Washington
Department of Fish and Wildlife 2012).

15

Table 1: Taxonomy of freshwater mussels in Washington State is represented by 3 genera of mussels in the
Pacific region as defined by Haag 2012. * Clade I was formerly two species the California floater (A. californiensis)
and the winged floater (A. nuttalliana.). ** Formerly two species the western floater (Anodonta k.) and the Oregon
floater (A. oregonensis)

Native Freshwater Mussel Species of Washington State
Common name
Scientific name
Family
Tribe
“winged” floaters
Anodonta Clade I*
Unionidae
Anodontini
“western” floater
Anodonta Clade II**
Unionidae
Anodontini
western ridged mussel Gonidea angulata
Unionidae
western pearlshell
Margaritifera falcata Margaritiferidae
-

No formal survey of the distribution of freshwater mussels in Washington State has been
undertaken, but regional efforts have been made to document the presence of native mussels. The
state of Montana recently completed a state-wide inventory and outreach program to assess the
status of their freshwater mussel populations. Montana’s inventory could act as both a precedent
and guide for other states in the region as concern and documentation about freshwater mussel
declines in the western states becomes a management concern for wildlife and conservation
entities (Stagliano 2010). Historic and contemporary mussel locality records have been
exhaustively researched and compiled by the Xerces Society at a Pacific Northwest regional
scale. The Washington Department of Fish and Wildlife maintains verified state locality
observation data within the Priority Habitat-Species Database (Washington Department of Fish
and Wildlife 2012) (Fig 2) (http://wdfw.wa.gov/conservation/phs/ 2012). However, these
databases are not the result of a concentrated survey effort for mussels and access and additions
to these databases is limited.

The main body of freshwater mussel research in Washington State investigates
population abundance and habitat associations of the western pearlshell , though several
researchers have also investigated its reproductive traits at different sites (Toy 1998, Adair et al.

16

2009, Allard et al. 2012) and the effects of anthropogenic change on population structure (Hastie
and Toy 2008, Helmstetler and Cowles 2008, Krueger et. al. 2007, Cowles et. al 2012). The
theme for many of these studies is the need for long-term monitoring of population trends and
the quality of their habitats as summarized in a USFWS report (Lohr and Glasgow 2005), yet this
review found only two studies revisiting populations for monitoring in Washington State. Toy
revisited her 1998 thesis study in 2006 and found significant population declines at both sites
(Hastie and Toy 2008). An additional survey found total extirpation of western pearlshell from
the mid-Columbia River (Helmstetler and Cowles 2008).

In addition to the locality information collected and housed by management and
conservation entities there may be information about the distribution of freshwater mussels
known by fishermen, property owners, and other river users in the local communities. The
knowledge of individuals and communities that live in or frequent areas is referred to as local
ecological knowledge (LEK). The declines, disappearances, or new occurrences of mussel
populations can be documented through incorporation of local ecological knowledge (Azzurro et
al. 2011). LEK is often overlooked during scientific studies and can provide a rich spatially and
temporally long-term record of information if it is both accurate and reliable (Brook and
McLachlan 2008).

While LEK can be a valuable resource for documentation and therefore conservation of a
species, it is also the responsibility of the conversation community to educate and excite the local
populous about the organisms that surround them. Outreach to the community about freshwater
mussels is not only an effective method in engaging individuals in their environments, it also

17

aids conservation efforts by creating invested and concerned stewards of the biological
community (Mazzacano 2012)

Western pearlshell in Washington State

This review will focus primarily on the pearlshells, but information from other studies
and mussel species will be used to inform and contrast findings and will be included if
applicable.

By far the most abundant and widespread mussel in the Pacific Northwest is the western
pearlshell (Toy 1998, Jespen et al. 2010b), and for that reason this and the majority of studies
within Washington State have focused on this species. The western pearlshell typically inhabits
cool, clean fast-flowing streams. It possesses a thick shell with a brown to black outer coloration
often with erosion on the umbo region and a white, purple, or salmon colored nacre on the shell
interior (Toy 1998, Nedeau et al. 2009). In western North America, the western pearlshell often
inhabit low gradient lotic systems with stable substrates and low shear stress (Stock 1996,
Howard and Cuffey 2003, Nedeau et al. 2009, Jespen et al. 2010b), where they can occur in great
numbers and densities (Murphy 1942, Nedeau et al. 2009). Western pearlshell become sexually
mature between 9 – 12 years and differentiation of sex has been observed in western Washington
(Toy 1998). Fishes in the family Salmonidae, especially those within the genera Oncorhynchus,
Salmo, and Salvelinus, have been identified as key hosts for the western pearlshell glochidia in
our region. Their interactions are summarized in Jepsen et al. (2010).

18

Figure 2: Freshwater mussel distribution in Washington State created with WDFW Priority Habitat Species data (2011). Note that all species
reported to exist in Washington are represented on this map.

19

As a testament to a sedentary organism’s plasticity and to the difficulty in defining exact
pearlshell habitat associations, western pearlshell exist and reproduce in highly variable areas
wherever suitable habitat and host fish co-occur. Western pearlshells can occur in low gradient
sections of headwater streams at elevations exceeding 1,500 m (Jespen et al. 2010). They have
been observed living in roadside ditches, and have even crossed the Rocky Mountains into
western Montana on their trout hosts. Mussels in the genus Margaritifera can live upwards of a
century (Ziuganov et al. 2000), making them among the longest lived animals on the planet and
the focus of several studies reconstructing the environmental history of lotic habitats (Howard
and Cuffey 2005, Black et al. 2010). However, more typical life spans of mussels in Washington
State reach 60 to 80 years old (Bauer 1992, Ziuganov et al. 2000, Black et al. 2010).

Ecology: Biotic and abiotic controls of western pearlshell

The physical environment, including temperature, water discharge, shear stress, water
chemistry, and nutrient levels, has been documented to have effects on the longevity and growth
rates of freshwater mussels (Bauer 1992). These environmental parameters have been
investigated in Great Britain extensively and throughout the range of the critically endangered
pearlshell (Margaritifera margaritifera) (Bauer 1992, Skinner et al. 2003, Young et al. 2003).
These studies found that human alteration of hydrology and subsequent substrate composition
change as well as the decline of native host fish has led to the near elimination of pearlshells in
Great Britain.

Temperature
Temperature is a major driver of mussel growth, size, and age. Cold conditions in higher
latitudes create slower growth, larger sizes, and longer lifespans in the pearlshell than in
20

populations at lower latitudes and warmer waters in Europe (Bauer 1992). Bauer (1992)
hypothesized that metabolic rates are influenced by water temperature. Colder waters reduce
annual growth rates and slow metabolic processes, but cooler habitats allow for longer lifespans
and ultimately larger mussels. Toy (1998) found that pearlshell mussels in east-central Puget
Sound rapidly increased their seasonal growth rates during the summer months of the year and
that winter conditions showed reduced growth rates. She states that this increase in growth
occurs after the reproductive cycle is complete, indicating that energy may be shifted from
reproduction to growth. Warmer temperatures also tend to increase productivity in aquatic
systems unless dissolved oxygen level or reach a critical low threshold for the organism.
Discharge and velocity:
Discussion of water discharge and velocity excludes lentic habitats, which by definition
are still waters where velocity remains very slow or is nonexistent. Water velocity is determined
by the steepness, or gradient, of the river channel and the roughness of the channel bed which is
determined largely by instream substrate and large woody debris, as well as the sinuosity of the
channel itself. Pearlshell mussels are typically found in streams and rivers that have suitable
habitat for their host fish species, allow for the successful settlement of larval mussels, and have
suitable flow rates, low shear stress, or refugia within the channel (Vannote & Minshall 1982,
Strayer 1999, Howard and Cuffey 2003, 2005, Stone et al. 2004). In most rivers, mussels exist
in areas where velocity maintains a stable non-aggrading substrate or where there are sufficient
refugia, such as boulders or large woody debris, for mussels to remain in place during high flows
(Vannote & Minshall 1982).

21

Pearlshell mussel habitat preferences can be identified at different resolutions within
aquatic systems. Most studies have examined abundance and habitat associations within a single
stream reach or described a single population, but have not examined their distribution from the
headwaters to the mainstem of a watershed (Hastie & Toy, 2008; Lohr & Glasgow, 2005; Stock,
1996; Toy, 1998). Only one investigation in western Washington by Jennifer Stone (2004)
examined freshwater mussels over a significant distance. While it is possible to accurately
predict mussel presence in a lotic system based on physical characteristics defining a stream
reach, their distribution within the reach tends to be highly patchy (Stone et al. 2004).

Theses on western pearlshell in Washington

Two of the earliest studies to address freshwater mussels in Washington State are theses,
one from The Evergreen State College in 1996 by Amy Stock followed by one by Kelly Toy in
1998 at the University of Washington. Stock (1996) focused her research on habitat associations
in a tributary of the Wenatchee River and found that mussel populations existing in poor
salmonid habitat had no juvenile recruitment in over 45 years. Toy contrasted 2 populations of
western pearlshells in eastern Puget Sound drainages to determine age, growth, reproductive
timing, habitat size, and included detailed histology of the reproductive organs. Both studies
found similar substrate and habitat conditions typical of the western pearlshell throughout its
range. They both assessed age and growth by measuring and counting bands on the hinge
ligament. Stock (1996) censused populations based on visual counts and Toy (1998) estimated
populations from transect subsampling within sites.

Toy (1998) investigated mussel abundance at Battle and Bear Creeks and found
average densities of 80 mussels/m2 and 55 mussel/ m2 respectively. She found that these mussels
22

became sexually differentiated, and later sexually mature, at the same size. Individuals in Battle
Creek mature 2 years later than mussels in Bear Creek. She attributed this difference in age at
maturation to the difference in temperatures between the two creeks and proposed that warmer
waters can cause the mussel to mature and grow more quickly. Toy also recognized the
impending peril mussels in urbanizing Seattle might face. Earlier investigations targeting
freshwater mussels in Washington State have set the stage for the synthesis and expansion of
information to create a comprehensive assessment of mussels within Washington State. Interest
and knowledge about freshwater mussels in Washington State is increasing, yet much work
remains to identify mussel localities and explain variation observed among populations.
Documentation of extant mussel population abundance and demographics is crucial to the
monitoring of population stability, and can provide evidence for species protection before
populations are lost (Nedeau et al. 2009, Jespen et al. 2010a, 2010b, 2010c). Understanding the
range of environmental and biological parameters in which mussels exist explains the plasticity
within a species and the limitations of their distribution. More efforts to document mussel
localities, and investigations to scope ecological variation within species and populations, are
needed before a complete assessment of freshwater mussels in Washington State is possible.

23

Chapter 3: Methods
Site Descriptions
This study was conducted within the Lower Chehalis watershed as defined by Water
Resource Inventory Area (WRIA) 22 (Washington Administrative Code 173-500-040), located
in southwestern Washington State (Figure 3- inset). This is the first investigation of mussels in
the Chehalis River beyond opportunistic locality reporting. The Chehalis River runs 125 miles
from its headwaters to Grays Harbor and its watershed is the second largest watershed in
Washington State draining ~7000 km² (USGS Washington Water Science Center, 2013). It was
never glaciated and its mainstem is free of dams. The Chehalis watershed can also be considered
biologically rich as its waters are home to nearly half of all species of freshwater fish in
Washington, including: Chinook salmon (Oncorhynchus tshawytscha), chum salmon (O. keta),
coho salmon (O. kisutch), steelhead (O. mykiss), and Olympic mudminnow (Novumbra hubbsi)
(Wydoski and Whitney 2003) and is home to all three mussel genera occurring within the state
(http://wdfw.wa.gov/conservation/phs/, 2012).
Following initial mussel surveys conducted in WRIA 22, three sites were selected with
easily accessible populations of pearlshell mussels, in close spatial proximity to each other, and
in increasing watershed area. The sites are referred to as Stillwater Creek (headwaters), Lower
Satsop (tributary), and South Elma (mainstem; Fig 3). Two sites, South Elma and Lower Satsop,
are located in Grays Harbor County and Stillwater Creek is located in Mason County. The
Stillwater and Lower Satsop sites are within the Satsop River drainage and South Elma is located
on the Chehalis River 6.5 river km upstream of the Satsop River’s confluence with the Chehalis
River.

24

Figure 3: The location of the three study sites in the Lower Chehalis Watershed (WRIA 22)

25

The Stillwater Creek site is located on a first-order segment of Stillwater Creek, 3.7 km
below its initiation point at an unnamed, spring-fed permanent wetland (~ 47° 13.225’N, 123°
15.729” W) south of the Shelton-Matlock Road and immediately upstream of the convergence of
Stillwater and Phillips Creeks (47° 12.257’N, 123° 12.764’W) (Fig 3). The area is a low gradient
anastomosed reach with pool-riffle stream habitats and enough flow to maintain clean substrate.
Pearlshell mussels appear in patchy but continuous numbers for nearly 0.5 km upstream of the
convergence of Stillwater and Phillips Creeks. The site is surrounded by managed forest land
owned and operated by Green Diamond Resource Company with an extensive graded gravel
road system and riparian buffer.
The surrounding forest is primarily a Douglas-fir (Psuedotsuga menziesii Franco)
plantation, but the immediate riparian forest (33 m buffered area) is a much older heterogeneous
evergreen forest with species typical to this region. Between multiple channels within the overall
stream channel are vegetated areas composed of a mixture of sedges (Cyperaceae spp.), alder
(Alnus rubra Bong), willows (Salix spp.), Pacific nine bark (Physocarpus capitatus Kuntze),
devil’s club (Oplopanax horridus Miquel), and other wetland-associated plant species. This
reach is used by coho and trout as a spawning area and it is likely other salmonids use this reach
for reproduction as well. Reaches up- and downstream had extensive hydrologic alteration by
beaver (i.e. dams) leading to the slowing and widening of channels with extensive beds of
hornworts (Ceratophyllaceae sp) and the buildup of greater than 1 m depth of fine silts and
sediments that may exclude pearlshell mussels.

The Lower Satsop site (46°59.261’ N, 123°29.454’W) is located 2.5 km upstream of the
mouth of the Satsop River where it converges with the Chehalis River and 2 km downstream of
26

the Highway 12 Bridge crossing the Satsop River. The site is immediately upstream of a deep
side channel pool armored by extensive rip-rap in a long riffle-dominated reach. The Satsop
watershed drains 593.1 km2 at the site and the twenty year average discharge for the Lower
Satsop River is 60.77 m3/s at the Highway 12 Bridge and was recorded at USGS gaging station
12035000. The entire site consists of several hundred individual pearlshell mussels and is
centered around a large fallen tree on the west bank of the river. The Lower Satsop site is
surrounded by agricultural land, primarily producing dairy and vegetable crops, with Keyes Road
to the east. The immediate east bank of the river is owned by an unmaintained Washington State
Department of Fish and Wildlife parcel that is used mainly by fishermen to access salmon and
steelhead fishing sites and is primarily composed of a mixed black cottonwood (Poplus
trichocarpa Brayshaw) and willow riparian floodplain forest. The WDFW parcel was formerly
the location of a gravel extraction site presumably for the construction of the Satsop Nuclear
Power Plant, now the Satsop Industrial Park, and extraction of the gravel has left three deep
ponds in the floodplain.

The South Elma site is located 2.5 km south of Elma on Wakefield Road immediately
downstream of the Wakefield Bridge at the head of the southern of two channels in the mainstem
Chehalis River. The two channels are divided by an established mid-channel island (46°
58.915'N, 123° 24.845'W) covered in woody vegetation and roughly 300 m in length. Upstream
of the study site, the river makes an abrupt 90° turn and changes direction from SW to NW. At
this bend there is a deep pool that extends from the corner to the edge of the site where the river
then enters a shallow, swift riffle that continues downstream for at least 200 m. The watershed
drains 3768.4 km2 and the twenty year average discharge for the Chehalis River is 117 m3/s at the

27

Porter Bridge and was recorded at USGS gaging station 12031000. Delzene, Mox Chehalis, and
Eaton Creeks enter the Chehalis River between this USGS gage and the South Elma study site.
The pearlshell population extends in either direction upstream of the bridge with the density
decreasing to an individual or small pockets of mussels found occasionally. The surrounding area
is agricultural to the north, east, and west, but immediately to the south of the site the landscape
rises into the northern edge of the Willapa Hills. Both sides of the river have high bluffs
composed of loose fine sediments. Above the bluffs is a mixed stand of black cottonwood,
willow, and mixed shrubs. See Appendix A for a list of observed flora and fauna at all three
sites.
Sampling design
A simple random sampling design was selected for this study after a review of methods
outlined in Strayer and Smith (2003). Initially a systematic sampling design was developed, but
due to the high level of channel heterogeneity at the Stillwater Creek site, the systematic design
was abandoned for logistical simplicity and a random design was adapted.
The methods used to calculate sample reach area included measuring reach length by
average width and dividing the resulting area into a 1-m2 grid of the reach. This created a
standard x, y map of the site (x: channel width from river right to river left, y: stream
longitudinal distance from upstream to downstream) that was used to divide the reach into
regular sampling plots (Fig 4).

28

Lower Satsop River Random Sampling locations
X, stream width

meter dist.
Y, Stream
Length

0

1

2

0
1

3

4

5

6

7

1
1

1

9

10

11

1

12

13

1

1

14

4

1

3

2

1

1

3

1

1

5

8

total at
x
15 meters

1
1

1
1

1

1

1

5

1

6

2

1

7

1

8

1

1

9

1

1

10

1

1

5

1

1

1

1

1

3
1

1
1

5
3
3

Figure 4: Depiction of random sampling map used to identify sample plot locations in the field. Cells marked “1” in
this example were sampled for mussels and blank cells were not sampled.

The number of plots sampled was determined by multiplying the average segment width
by the segment length. During surveys, I attempted to randomly sample twenty percent of the
plots by calculating sample area and dividing by five (# plots = {L x Waverage)/5}. Sample plot
locations were determined using a random number table composed of the longitudinal and
latitudinal axis positions of each segment.
Establishment of a survey segment at each site required that it meet three criteria: 1) it
included a population of pearlshell mussels, 2) its depth and flow velocity during the summer
low flow period was such that an individual snorkel sampler could both stay in place and sample
the benthic environment, and 3) channel structure was simple enough to allow for reach division
into a grid of sampling plots. Once a segment from each site met the criteria, a continuous 100 m
29

longitudinal distance was measured with an LTI® Impulse hypsometer along an average channel
azimuth as determined by compass on-site. Upstream and downstream extents of the sampling
reach were delineated by flagging and GPS waypoints were taken on a Garmin® Etrex HCx for
reference. The segments spanned the wetted stream width of the channel and were measured to
the nearest tenth of a meter. At South Elma only the left channel was used as a segment, at
Lower Satsop the channel was restricted to the specific habitats where mussels existed and at the
Stillwater site the sum of the braided channel widths was used.
All sampling at plots occurred within a 0.25 m2 (0.5 x 0.5 m) sampling quadrant placed
in the upstream right hand corner of selected plots. The quadrants were made of 0.75 inch
diameter PVC piping and 90° PVC joints. The quadrants were drilled with regular holes to allow
water to enter causing them to sink. In plots with water flow strong enough to move quadrant
squares they were anchored by rebar pounded into the substrate inside the upstream corner.
Mussel data collection
All freshwater mussel handling and collections were performed under the terms of
Washington Department of Fish and Wildlife Scientific Collection Permit #11-400. No mussels
were sacrificed for this study. Enumeration and measurement of mussels, with the exception of
collecting discarded shells (see Aging mussel shells) occurred within the delineated survey
reach. After the sampling quadrant was placed in the selected plot, a snorkeler sampled the
quadrant for live mussels with a visual and tactile search of the quadrant. The sampler removed
all mussels encountered into a mesh bag for identification, census, and valve measurement. The
top layer of substrates, cobble and smaller, was also removed, but the quadrant was not
excavated. If any portion of a mussel shell was inside the border of the quadrant it was included

30

in the total quadrant. All mussels in the quadrant were identified, counted, and measured for
valve length, width, and height to the nearest tenth of a millimeter using a caliper (Pittsburgh®
venier scale 6” utility caliper #7914, CA, USA) (Fig 5). If more than 30 mussels were
encountered in a single plot, measurements were taken from every fourth mussel picked
randomly from the sample bag.
Complete valves in good condition were opportunistically collected from all sites.
However, because only one valve was found at the Lower Satsop (tributary) site, assessment of
age, growth, and length to mass ratios were completed only for the Stillwater (headwaters) and
South Elma (mainstem) sites.
Complete right valves were collected from the Stillwater and South Elma sites and were
retained to calculate length to mass ratios. The valve was weighed to the nearest hundredth of a
gram using a balance (Denver Instruments Model 220 Balance, Bohemia, NY, USA) and its
length measured with a caliper (Pittsburgh® 6” digital caliper #68304, CA, USA).
Aging mussel shells
The left valves of complete mussel shells collected at the Stillwater and South Elma sites
were retained for aging and growth analysis. Only complete valves, without cracks or excessive
erosion were considered for this analysis. At the South Elma sites all valves had a large degree of
erosion in the umbo (or dorsal area) and the ones in the best condition were selected for analysis.
Following methods described for aging bivalves (Schöne 2005) and specifically Margaritifera
falcata (Howard and Cuffey 2006, Black et al. 2010), acceptable valves were measured for
length, height, and width and then incased in epoxy (JB Kwik Weld® Sulphur Springs, TX,
USA). A dime sized area of the valve was covered in white fingernail polish and the sample

31

number was written on the polish. At the Washington Department of Natural Resources (DNR)
Geology Division Laboratory the valves were cut transversely from the umbo to the edge of the
shell perpendicular to external growth lines with a heavy liquid rock-saw and mounted to a 46
mm x 26.75 mm (1.05” -1.81”) glass slide with epoxy (Loctite® translucent yellow Westlake
OH, USA).The mounted section of the mussel was then cut to roughly 0.5 mm with an Ingram
thin-section cut-off saw (Ingram model 135) and ground to ~0.25 mm with a thin section grinder
(Ingram model 400). The mounted thin sections were then polished with very fine grit sand paper
and aluminum powder until imperfections from cutting and grinding were removed. The finished
thin section mounts were stained with a modified Mutvei’s staining solution for four hours at
37°C (Schöne et. al 2005). In this stain Alcian blue was replaced by Coomassie Blue® (Brilliant
Blue) for cost and safety reasons. Finally the mounted specimen had a small amount of mineral
oil applied to clarify annuli by coating small scratches and imperfections not removed by
polishing (MacLellan 1976).
Once prepared and stained, the sections were observed under a compound microscope
(Nikon SMZ-2T) at 50x magnification and each annuli was counted from beak to edge. Average
growth was calculated by dividing the length of the shell by the number of years observed. For
individual valves with erosion at or around the area of the umbo which obscured early annuli, a
minimum age was established from readable annuli.

32

Figure 5: Basic mussel valve orientation and measurements. Image created by Ethan Nedeau, 2009: Freshwater
Mussels of the Pacific Northwest. 2nd edition p.16

Stream habitat assessment
To examine the differences in mussel habitat preferences among sites, physical
characteristics of each site were recorded. Stream habitat assessment followed the Timber-FishWildlife Monitoring Program’s Method Manual for the Habitat Unit Survey (AM9-99-003)
which was designed to quantify major physical characteristics of wadeable streams commonly
encountered in Washington State (Pleus et al. 1999). This survey was designed to provide
guidance in quantifying standardized data about habitat units, stream morphology, and habitat
characteristics. The inorganic dominant and sub-dominant surface substrates were assessed at the
habitat unit level as well as within the sampling quadrant. Substrate categories included:
mud/silt, sand, gravel, cobble, boulder, bedrock, and compacted clay (Appendix II). Gradient
was measured at the segment start to end points while standing on the bed of the river or creek.
Measurements were taken to the nearest tenth of a degree (0.0°) with a range finder (Impluse
200, Laser Technology Inc., Centennial, CO, USA). See Appendix II to reference the field
sampling protocol.

Water temperature, quality, and discharge field measurements

33

Water temperature at each study site was recorded at hourly intervals by temperature data
loggers (Onset® HOBO® Tidbit v2 Temperature Data Logger, Bourne, MA, USA) which were
fully submerged and placed on the river substrate within the mussel bed at each site.
Temperature was also recorded opportunistically at site visits with a hand held thermometer or
with a multimeter probe (YSI® Model 85 Multiparameter Meter, Carlsbad CA, USA).
Dissolved oxygen levels, conductivity, and salinity were measured at each site with the
same YSI multimeter probe. The YSI multimeter was calibrated between site visits. In late
summer 2012 and early spring 2013, water samples were collected for analysis of nitrate, total
phosphorus, pH, alkalinity, and hardness levels. The water samples were analyzed by Dragon
Analytical Laboratories (530 Ronlee Lane NW, Olympia, WA 98502).
Discharge and velocity were measured at each site on September 6, 2012 using a velocity
meter (Marsh-McBirney Flo-Mate Model 2000, Loveland, Colorado, USA). Measurements were
taken following USGS standard methods and additional measurements were taken at the
substrate level to evaluate flows as experienced by mussels. On two occasions velocity and
discharge were measured at the Stillwater site using a neutrally buoyant object and a stopwatch.
The Lower Satsop and South Elma sites both have USGS gaging stations upstream of the study
sites which were used to determine estimates of discharge year-round. High and fast waters made
discharge measurements using the tools available logistically difficult and unsafe at times other
than the low-flow period. At the Stillwater site the velocity and discharge were measured
multiple times throughout the year to create a partial hydrograph.

34

Informal Interviews
Serendipitous interviews were conducted with individuals encountered when surveying
for mussels at or near the study sites to gather information about potentially unknown mussel
localities and to deduce the local level of knowledge about freshwater mussels. The discussions
were commonly initiated by an individual or individuals curious about study activities or by
myself to ease tensions about having an individual working in the area. All information
pertaining to freshwater mussels was recorded in a field notebook without names or other
identifying details and later transcribed.

Statistical Analysis
Mussel measurements
Data collected from living mussels were used to calculate a population estimate of
mussels at each site by multiplying the average number of mussels found in all plots sampled at
each site by the wetted area at each site. At the Lower Satsop site the area of mussel occupation
was small enough that a complete visual census was conducted. The population census at the
Satsop site was contrasted with estimated population size from subsampling to determine an
estimate of sampling accuracy at this site
Site level differences in the mean size of measured mussel valves metrics (length, width,
and height) were determined among sites using an ANVOA. Additionally, Ortmann’s Law
(Ortmann 1920) for increasing valve inflation as river volume increases was tested among the
three study sites as defined by a ratio of length to width. The ratios were calculated by dividing
the mussel width by length (w/l) for each individual measured. Raw and log-transformed data of
shell metrics and Ortmann’s ratio failed to meet the assumptions of normality for parametric tests
35

so resampling ANOVA and regression statistics (Resampling Add-in for Excel 2007) were used
to assure the validity of each test.
Distribution of age and age at size as determined from measurements taken from
complete left valves at study sites in Stillwater Creek and South Elma were compared using a ttest to verify if differences in average population age between these two sites. Regressions for
size at age and growth rate were created and contrasted in ANCOVA analysis at each site.
The resulting length to mass slopes for the two sites were analyzed in an ANCOVA to
describe the different rates of mass at size as a surrogate for valve density.

Habitat measurements
Potential preferential use of substrate habitats by mussels at each site and collectively
among sites were evaluated by analyzing the presence or non-detection of pearlshell mussels in
dominant substrates recorded within each sampled plot. A Chi-squared analysis compared the
expected distribution of mussels, based on the available types of habitat, against where they were
observed. Average and maximum discharge in 2012 for the Satsop and South Elma sites, as
recorded by the Satsop and Porter USGS gage flow stations, respectively were used for analysis.
An average stream discharge rate from Stillwater Creek was calculated from readings taken in
the field using the above described methods. The highest recorded flow was used as a surrogate
for maximum flow at the Stillwater site. Discharge rates from single occurrence where discharge
was measured at all sites in September of 2012 were contrasted. Flow velocities taken at the
substrate level at each site in September 2012 were compared using an ANOVA.
Temperatures recorded in-stream were graphed to depict seasonal variation within and
among sites. Temperatures recorded during the July to September period were compared using

36

ANOVA to contrast temperatures at the warmest and perhaps most productive time of year.
Mean, maximum, and minimum temperatures during the low flow period were also compared.
Water quality measured in field and analyzed in the laboratory was contrasted to existing
literature about Pearlshell tolerances to determine is any locations exceeded critical levels.
Local Ecological Knowledge
Information garnered from informal interviews was compiled and location notes were
taken. These localities were added to known mussel localities as compiled by the WDNR in the
database. Additional useful information was annotated on the map created showing existing
mussel populations in 2013.

37

Chapter 4: Results
Western pearlshell abundance estimates
Nine hundred forty-six total western pearlshells were counted within the quadrant
squares at all sites (Table 2). Western pearlshell abundance estimates were extrapolated from the
average of all quadrant densities at each site and showed an order of magnitude difference
between each population (Table 2). Satsop had the lowest density with an estimated 2.3
pearlshells/m, with Stillwater at 14.2 pearlshells/m and South Elma at 89.6 pearlshells/m. The
highest recorded density at any site was 99 western pearlshells in one 0.25 m2 plot at the South
Elma site.

Table 2: Summary table displaying sampling effort and abundance of western pearlshell at each site. There was a
large variation in western pearlshell density in the areas sampled with an extremely high mean density found at the
South Elma site within the area sampled despite not detecting mussels in 15 of the 33 plots sampled.

Mean
# Plots
Site
Total
Site
Density
sampled Mussels Area
Site
Abundance
mussels/
2)
2
Found (m )
Estimate
(0.25 m
m2
Stillwater Crk
50
178
616.9
14.2
8784
Satsop
50
29
210
2.3
487
South Elma
33
739
715.6
89.6
64104

38

Shell Morphology

Site
Stillwater Crk
Satsop
South Elma

N
178
29
739

Min
14.4
36.2
25.3

Length (mm)
Mean
Max
53.4
77.2
74.5
96.7
98.8
148.1

South Elma
Satsop
Stillwater Crk

Figure 6: Length distribution of western pearlshell valve length at three study sites in the lower Chehalis Basin
showing shorter individuals at Stillwater, an intermediate size at Satsop, and both the largest range and overall
longest mussels at South Elma.

Overall, western pearlshell showed a wide range of size from 8 to 142 mm. The
difference between the shortest and longest western pearlshell was 60.5 mm at Satsop, 62.8 mm
at Stillwater, and 127.8 mm at South Elma. The restricted range of mussel sizes at the Satsop and
Stillwater sites may be related to the relatively smaller populations indicating that recruitment is
infrequent and may have occurred when environmental conditions were suitable for larval
recruitment. Stillwater had a similarly small size range of valve sizes, but the smallest measured
mussel was observed at this site (Figure 6) and gravid individuals with viable glochidia were
observed in early spring 2012. The large number of individuals at this site, the anecdotal reports
39

that indicate long term presence of mussels in the area, and evidence suggest contemporary
spawning events point toward restrictions of maximum size of mussels. South Elma had the
largest range of sizes with more individuals above the mean number than below, typical of
species with a high fecundity – low survivorship strategy.

Western pearlshell were found to significantly increase in length (ANOVA, P = 0.38),
width (ANOVA, P = 0.38), and height (ANOVA, P = 0.04) from the first order headwater
stream site (Stillwater) to the Chehalis River. This confirms our observations that within this
study, western pearlshell tends to increase in size and volume as the distance from stream
initiation point increases. The abundance of western pearlshell is not a good indicator of the
maximum length of mussel (i.e., it is not true that more mussels mean bigger mussels) and likely
there is an overlying biological control restricting the growth of western pearlshell at the
Stillwater site.

40

Figure 7: Mean (+/- 1 SE) length, width, and height of western pearlshell in three sites of
the lower Chehalis Watershed in 2012. Significant differences (ANOVA test) are
indicated by unique letter characters next to each bar.

41

In contrast to increasing mussel sizes, the ratio of increasing length to width
remained consistent at all three study sites (Fig 8). This supports previous reports stating
Margaritiferidae do not conform to Ortmann’s Law which predicts increasing mussel
valve inflation, or width to height rations, in a downstream direction. These results
further support findings that mussels are volumetrically larger as river size increases and
are not changing the proportional shapes of their shells for differing environmental
conditions.

Figure 8: Mean (+/- 1SE) width to length ratio (Ortmann’s ratio) of western pearlshell in three sites of the
Lower Chehalis River basin, 2012. Significant differences (ANOVA test) are indicated by unique letter
characters above each bar.

An interesting differentiation of weight per unit valve length was apparent when
the right valves of mussels were compared between South Elma and Stillwater Creek

42

sites (Fig. 9). The weight: length ratio at the South Elma site (y = -57.13 + 0.793*x) was
found to be significantly greater than that of Stillwater Creek (y = -7.128 + 0.188*x),
indicating either a more dense shell or a thicker shell at South Elma. The lack of
overlapping valve lengths at the sites leaves the possibility that a transition from
proportionally lighter valves to heavier ones occurs at a length of 70 – 80 mm, but no
mussels >77 mm were found at Stillwater Creek to extend the dataset and intact smaller
valves were not found at South Elma.

43

Figure 9: Variation in the dry weight to length ratios of right valves of western pearlshell in Stillwater
Creek (headwater stream) and South Elma site (Chehalis River), 2012. ANCOVA analysis was used to
compare the difference in slope (ratio) at each site. Linear regression results are also given for each site.

44

Age and population structure

Figure 10: Two growth trajectories calculated from left mussel valves at the Stillwater Creek and South
Elma study sites. Valves sizes <40 mm were absent from this analysis as only live mussels of this size were
encountered in 2012. ANCOVA analysis was used to determine if site affect the slope of the growth rate
equation.

Counts of internal annuli from collected shells at the Stillwater and South Elma
sites were plotted separately and resulting slopes were contrasted in an ANCOVA
analysis. The analysis revealed that mussel growth rates were similar at both sites (p =
0.0964) (Fig 10). Only one shell was found at the Satsop site. Because of the small
population at Satsop, the possibility of declining populations, and a non-lethal sampling
permit, no mussels were retained for aging and that site is excluded from these results.

45

Figure 11: Mean age (+/- 1 SE) of western pearlshell sampled in 2012 at the Stillwater Creek and South
Elma sites were compared using an ANOVA. Mussel age of the sample population was derived from age at
length estimates for these sites as shown in Figure 9.

Although the overall growth rate in mussels appears similar between the sites, the
South Elma site was found to have a significantly (p < 0.0001) older population than that
of Stillwater Creek (Fig. 11). A rough estimation of population age structure was
generated from the slopes found in the aging process (Fig. 12). At the Stillwater Creek
the site age was calculated using the equation for the growth line, y = 0.82x – 27.5, and at
South Elma site the line equation was y = 0.35x + 1.58 where y is length and x is age.
Because these lines cross the age axis before the length is zero, an age category of less
than 10 years old was created for those individuals and is displayed.

46

Figure 12: Percent of western pearlshell from South Elma and Stillwater sites in seven age categories,
2012. Ages were determined from counting annuli in mussel shells at various sizes and lengths to create an
age at length calculator for each site.

Habitat Preferences
Habitat conditions and preferences were investigated at each site to examine
differences in habitat selection within the sites by mussels and describe the physical
conditions at each site. Habitat units were identified at each study site, but were fairly
homogenous at every site except the Stillwater site which had a large number of riffle
(33) and pool (16) habitat units and four main braided channels. Habitat at the Satsop site
consisted of a glide with a mean sampled depth of 88.5 cm (max 164 cm) that terminated
in a deep pool, and the South Elma site consisted of parallel continuous riffle (mean
depth 19.2 cm) and glide (mean depth 54 cm) habitats. Among the plots sampled, a Chisquared test found mussels were not found to preferentially occupy one substrate type
47

over another at Stillwater (p= 0.756), Satsop (p= 0.054), South Elma (p= 0.142), or
overall (p= 0.0627). Although there was no statistically preferred selection of one habitat
substrate, gravel substrates represented the most common substrate occupied by mussels
at each site and overall suggest that gravel substrate is important to pearlshell mussels for
occupancy.

Figure 13: Habitat substrate preference does not vary within study sites selected for the presence of mussel.
Gravel and cobble substrate always contained mussels and composed a substantial proportion of the
substrate matrix.

48

Table 3: Water quality thresholds found by Stock and Toy for western pearlshell and by Bauer and Oliver for
M. Margaritifera fall within most measured parameters at the study site. * Margaritifera margaritifera

Water Quality
Stillwater
Satsop
South Elma
Stock 1996
Toy 1998
Bauer*
Oliver*

Fall
Spring
Fall
Spring
Fall
Spring
1996
1998
1988
2000

Alkalinity Hardness
mg/L
mg/L
no result 39.00
33.00
34.00
28.00
27.40
22.20
28.40
35.60
39.50
20.60
19.10
NA
NA
NA
NA
Ca CO3 2 mg/l
<10 mg/l Ca CO3

Nitrate
mg/L

pH

Total Phos
mg/l

D.O.
mg/L-1

Conductivity
μs/cm

nd
0.12
0.12
0.49
0.39
0.24
NA
NA
1
0.5

7.36
7.29
7.32
7.29
7.29
7.21
6.96 - 7.36
6.5 -7.4
NA
6.5-7.2

nd
nd
0.14
0.13
nd
nd
NA
NA
<0.03
<0.03

10.10
10.56
10.23
10.86
9.92
11.07
9.21- 10.14

75.6
73.3
70.6
50.8
74.3
76.2
NA
57 - 106
<70
<100

NA

Water quality measurements taken during the fall of 2012 and spring of 2013 are
within the acceptable limits found in other theses in Washington and slightly higher
compared to conditions reported for its congener Margaritifera margaritifera in Great
Britain (Table 3). The reported alkalinity levels which greatly exceeded most commonly
reported levels in Great Britain (Bauer 1988, Oliver 2000, Sime 2005) may be explained
results from previous studies by the loss of mussels from much of their former range with
more variable alkalinity levels (Morreken 1992, Lucey 2006). There was little variation
in water quality variables tested at the sites at the time of the sampling, suggesting that
these variables are not likely to negatively affect mussel populations.
Water temperatures collected from in-stream temperature sensors show a trend of
increasing temperature as watershed size increased with the warmest temperatures in July
– August and coldest temperatures in January (Fig. 14). During the warmest period of the
year, Stillwater Creek had the coolest mean and recorded temperature, South Elma the
warmest mean and recorded temperature, and Satsop the greatest range of temperatures
(Table 4). Annual water temperature recorded at the USGS station immediately upstream

49

of the South Elma site in 1975 is used here for a reference of mean annual water
temperature. The complete dataset at the South Elma site could not be recovered but
likely followed a similar seasonal pattern as Satsop and Stillwater.

July – Sept:
Period of
warmest water
temperatures

Figure 14: Temperature measurements taken in the Lower Chehalis watershed in 2012 and 2013 using
Onset Tidbit monitors recording each hour. Historic temperature data records are from Washington
Department of Ecology. Note that the larger the body of water the larger range of temperature fluctuation.

During the warm summer period when concurrent temperatures were being
recorded, the South Elma site averaged 17.5 °C, 3.4 degrees warmer than the Stillwater
site and was never cooler than Stillwater Creek. Summer water temperatures were found
to be significantly warmer at South Elma than Stillwater Creek (p < 0.0001) (Fig. 15).
However this difference may not be biologically significant to the mussels. The Stillwater
site had the smallest range of temperature. This may be attributed to the close proximity

50

of Stillwater Creek to a cold groundwater spring and its narrow channel and dense
riparian forest creating a high degree of shading.
Table 4: Summary statistics for water temperatures taken at the substrate level during the warmest part of
the year. Bold font indicates the highest value within each category.

Temperature °C (July - Sept 2012)
Site
Average
Max
Min
Range
S Elma
17.5
20.8
14.6
6.3
Satsop
15.9
19.6
11.9
7.6
Stillwater
14.1
16.7
11.6
5.0

Figure 15: Mean daily water temperature (+/- range) during July-September 2012 at each study site. The
two larger sites have larger ranges of temperature values and there is more stable temperature at the smaller
spring-fed site.

51

Water Discharge and Velocity
Annual discharge was measured once at each site on September 6th, 2012.
Although discharge is only roughly ten times greater at the Satsop and South Elma sites
during low flow periods Stillwater Creek does not display the same magnitude of
discharge from <300 cfs to 30,000 cfs (Fig. 16). The less variable discharge rates and
lack of channel disturbance or flooding observed at Stillwater Creek were markedly
different than the large increases in water discharge and velocity observed at the Chehalis
and Satsop River sites in 2012 and 2013 which resulted in flood and near flood
conditions.

Figure 16: Discharge measurements at Stillwater Creek were made on Sept 6th and Dec 6th, 2012 with a
final measurement on Feb 27th 2013. Scale of the graph is large to replicate USGS generated graphs for
comparison across sites. Discharge measurements made at Satsop and South Elma sites on September 6th
2012 are noted for comparison.* indicates measurements by USGS river discharge stations in 2013-2013.
Both stations are upstream of the sample sites

52

All substrate velocity measurements were taken on the same date, September 6th
2012, as concurrent discharge measurements in riffle or riffle/glide habitats that spanned
the channel. Water velocity at the substrate was much faster at South Elma than the other
two sites during the low flow period. Although not significant, the average substrate
velocity follows a trend of increasing speed within mussel beds as stream size increases.
It is interesting to note that although the annual discharge at Satsop and the Chehalis
River at Porter are very similar, the water velocity at substrate varies greatly (Fig. 17).

A

B
B

Figure 17: Mean velocities (+/- 1SE) at the substrate level compared in an ANOVA for sites containing
pearlshell mussels in the Lower Chehalis watershed in 2012.

53

Figure 18: This map depicts locations were freshwater mussels where reported to exist during conversations with
professional biologists and individuals encountered during surveys or over the course of everyday life in 2012 and 2013.

54

Informal Interviews and opportunistic sampling
As a result of informal conversations with both professional biologists and
individuals encountered on mussel surveys, 15 confirmed mussel localities were
identified that were not located in the WDFW Priority Habitat Species (PHS) database
(Fig. 18). Six conversations identified the South Elma site, used in this study and
recorded in the WDFW PHS database, as having an abundance of mussels. Four of those
conversations were with sport fishermen and two were with highschool students
participating in educational outreach events. Two locations, Lower Nisqually and
Spanaway Creek, are unconfirmed, but probable, based on descriptions of the site and
the mussels referenced during the conversation. Two sites were identified by myself
while conducting routine fish surveys in the Upper Chehalis Watershed (WRIA 23) for
USFWS. One instance of contempary human consumption of mussels was recorded. The
individual stated that “he ate them raw all the time” and had very detailed and accurate
information about locations and abundances of mussels in the Chehalis River betweeen
Porter and Satsop, Washington. In this case the consumption of raw mussels is specuated
to be a partial subsistance measure. Other instances involved fishermen that recounted
their knowledge of the river and its faunal assemblages happily and Washington residents
recalling observations of mussels earlier in their lives. These converstaions allude to
interest and information about freshwater mussels within the general public, recreational,
and scientific communities, and suggest that knowledge of mussel species and their
abundance may be widespread, but remains undocumented. Appendix III detailslocations
and information used to generate the map and will reference the site numbers in Figure
18.

55

Chapter 5: Discussion
There is evidence that freshwater mussels in Washington State and throughout the
Pacific Region are decreasing in abundance and diversity. The work here has been an
attempt to increase our knowledge of freshwater mussel populations in western
Washington State and to better understand what conditions influence their morphology
and growth rates. Earlier studies in Washington have revealed findings that furthered our
understanding of the distribution and life history of pearlshell mussels (Stock 1996, Toy
1998, Stone et al. 2004, Krueger et al. 2007, Hastie and Toy 2008, Helmstetler and
Cowles 2008), but this is the first to examine mussels in the Chehalis Watershed.
Demographics of Mussel populations
Mussels showed variation in densities where they were sampled. On average
Stillwater Creek contained 14 mussels/m2, Satsop 2 mussels/m2, and South Elma over 90
mussels/m2.The average densities found at South Elma are comparable to that of Battle
Creek (80 mussels/m2; Toy 1998) and much higher than those found in Nason Creek
during the late 1990’s (Stock 1996). The recorded abundance of mussels estimated at
these sites is the result of targeting populations and should not be used to estimate
populations outside the study areas.
At the Stillwater Creek and South Elma sites a subset of the entire area visually
confirmed to have mussels was sampled, but at the Satsop site the population was found
to be restricted to an area smaller than the initial survey area assumed. After the Satsop
site was randomly surveyed, a complete visual census of the same sample area was
undertaken. Two snorkelers completed individual visual surveys of the area and
56

determined that the visual surface population of pearlshell mussels was 252 -254 mussels,
roughly half of the estimated population of 487 individuals. Even with the gross
mismatch, relative abundance ratios may remain similar and populations Satsop:
Stillwater Creek: South Elma may remain roughly 1:15:120. Juveniles were not targeted
when sampling and are likely un- or under- represented in all populations. Methods for
sampling for juveniles include sifting through the sediments as outlined in Stayer and
Smith (2003). These would be important future surveys because inclusion of juvenile
mussels would provide evidence of reproduction and provide shells that could help
expand the growth and aging estimates that were limited in the dataset for this study.
The South Elma site is the most populous and diverse site in this study and has the
greatest range of sizes, ages, growth rates, and overall numbers in a continuous spatially
restricted large bed. Small individuals (25 mm) indicate recent recruitment and the large
range of ages and sizes are indicative of reoccurring reproductive events. Sampling at
South Elma reveled 10 western ridged mussels (Gonidea angulata) of small size (38 -72
mm length), interspersed with the western pearlshells.
The Satsop population was the least numerous with 254 individuals and no small
or visually identifiable juvenile mussels found. Satsop also had the most restricted area of
mussel occupancy. This population may represent a population sink in WRIA 22 that
became established during favorable conditions but has not expanded due to either lack
of reproduction within the bed or from transport of glochidia on host fish beyond the bed
(Toy 1998).

57

Stillwater Creek has a large estimated population of over 8000 individuals. Direct
observation of glochidial release from mussels at this site, along with very small
individuals (14.4 cm measured and smaller observed) likely indicate a successfully
reproducing population.
Stillwater Creek has the overall smallest individual mussels of any site. Mussels at this
site are arranged in patchy aggregations throughout the reach, indicating strong microhabitat preferences within the study reach.
Concerns and discussions about how to best estimate mussel populations are
common in the literature (Strayer and Smith 2003, Strayer 2008). Because of the very
great range of densities encountered in sampling plots even one meter apart (0 to 99
mussels/0.25m2) it is difficult to use a small randomly selected sample area to extrapolate
to a larger areas. Earlier accounts of mussel abundance and increasing the number of
plots would help improve abundance estimates. A systematic sampling strategy would
have improved the accuracy of the abundance estimates, but was not applied to this study
due to the heterogeneity of the Stillwater Creek system. A better approach to long-term
monitoring for population trends may be to resample fewer larger plots in exact locations
over many years.
Morphological patterns in mussels along a river spectrum
Valve characteristics
The mussels found at the study sites are situated along a spectrum of increasing
watershed area, stream length, stream order, and were observed to increase in size as
watershed size increased. This observation concurs with the hypothesis set forth in the
58

River continuum Concept that: “In developing a theory of biological strategies along a
river continuum, it should also be possible to observe a number of patterns that describe
various processing rates, growth rates, growth strategies, metabolic strategies, and
community structures and functions” (Vannote et al. 1980). Is the observed increase in
mussel size a response to some function of increasing stream length and or width? Some
ecological gradients have been tested for Margaritifera margaritifera patterns along
changing latitudes and temperatures (Bauer 1992) and for broad patterns in mussel shell
morphology (Ortmann 1920).
Pearlshell mussels in this study were found to follow a gradient of increasing size
in all three dimensions (length, width, and height) as watershed area increased. The ratio
of measurements of shell dimensions did not change from the headwater population to
the downstream population. This concurs with other findings that the pearlshell mussel
(Margaritifera margaritifera) does not follow Ortmann’s Law and provides evidence that
this trend is absent from the five species in the family Margaritiferidae as was previously
found for other species in the family Margaritiferidae (Ortmann 1920, Hornbach et al.
2010, Haag 2012). The western pearlshell may use other morphological or behavioral
adaptations, such as shell thickness, to improve their ability to remain in place, resist
erosional forces in the stream, or for other undescribed needs.
A significant difference in length to weight ratio was measured between the
Stillwater and South Elma sites. Width and height of the shell were not considered in this
analysis because they were already found to be proportionally the same among
populations. This finding is attributed to denser or thicker average mussel shells at the
South Elma site, but neither a standard thickness nor shell density were measured during
59

this study. Heavier shells may indicate a response to one or several environmental
conditions. The much larger volume and speed of water moving through the Chehalis
River may require a more “armored” mussel shell to withstand the erosive scouring by
suspended sand, gravel, and perhaps cobbles that occur to a much lesser degree in the
more stable and smaller Stillwater Creek discharge and velocity rates. Additionally a
denser per unit length (heavier) mussel may stay in place better during high flows that
could scour out a less heavy mussel of equal size. Alternatively this increase in weight at
size could be the result of mussels at South Elma living in a more productive site than the
narrow, shaded, and cooler Stillwater Creek allowing South Elma mussels to dedicate
energy to growing shells.
Age and growth patterns
The comparisons of mussel age and growth rates were limited to the Stillwater
Creek and South Elma populations because of sampling that allowed only for collections
empty and intact shells. Mussels were found to be growing at similar rates, and on
average, mussels are older at South Elma than Stillwater Creek. The mussels range in
ages from <10 to 40 y.o. at Stillwater and <10 to 60 y.o. at South Elma. This indicates
that the initial hypothesis that the observed mussels are smaller because they are slower
growing was erroneous and agrees with the supposition that the small size is an indication
of a younger population.
Toy (1998) found that western pearlshell mussels become sexually mature at a
given size and not at a given age. Based on those findings we should see evidence of
reproduction at the same minimum size at the South Elma and Stillwater Creek sites.

60

Gravid females were seen at the Stillwater Creek site confirming that the minimum
reproductive size has been obtained. To further validate Toy’s finding minimum
reproductive size could be investigated at each site and should be roughly the same.
Three hypothetical reasons for the absence of larger, older mussels at Stillwater
Creek would be highly interesting to investigate. First, and with little evidence to support
it, is that a fish barrier existed until roughly 40 years ago excluding host fish from
Stillwater Creek. Second, evidence of predation on mussels was observed at Stillwater
and South Elma, but because of the high flows mussels are likely not accessible to
predators year round at South Elma as they are at Stillwater Creek. Mammalian predators
likely target the largest mussels because the caloric rewards are greater with larger
individuals. There could be selective removal of large mussels at the Stillwater site year
round eliminating them from population. And third, early logging practices were not
historically protective of water quality and high loads of sediment could have smothered
and killed previous mussel populations at Stillwater creek. Higher flows at the Satsop and
South Elma sites may have removed fine sediments and allowed for the retention of the
older mussel populations there (Vannote and Mishall 1982, Howard and Cuffey 2006).
As logging practices improved or the regeneration of the forest improved in-stream
conditions, the mussels may have populated Stillwater Creek.
Comparison of environmental conditions
In this study the South Elma mussels were studied within parallel riffle and glide
habitats and the Satsop population was found within a single glide. The Stillwater site
was complex and contained a large number of habitat units, but there was little annual

61

variation (with the exception of canopy cover not reported here) in physical variables in
the stream. Vannote and Minshall (1982) stated that pearlshells may benefit from habitats
that do not aggrade, scour, or become turbulent annually, but maintain a constant laminar
flow bringing seston particulates to the mussels. Alternatively, Howard and Cuffey
(2006) hypothesized that segments of rivers that underwent periods of scour provided a
benefit to larger mussels by flushing the fine sediments that inhibit respiration, feeding,
survivorship and otherwise maintaining suitable mussel substrate conditions. The
Chehalis has the largest and oldest mussels and greatest stream discharge agreeing with
Howard and Cuffy’s (2006) hypothesis that high discharge events may remove fine
sediments and clean out the mussel bed favoring older, larger individuals as was found. It
also appeared to have the non-turbulent flow described by Vannote and Mishall (1982)
that favors long term and dense occupation by Margaritifera in larger rivers. Stillwater
Creek has little annual environmental variation. Relatively constant discharge throughout
the year may provide a stable long-term habitat if the bed does not aggrade and beavers
activity does not alter the reach (Hastie and Toy 2008). The Satsop population was
protected by a large fallen tree that shielded the mussels from the destabilizing and
erosive effects of faster water velocity, increased turbulence, and greater sediment
movement in areas of the river adjacent to the bed.
Substrate preference
Substrate preference by mussels was not different between sites nor was there a
preference for one substrate at any site. While no substrate preference among measured
variables was found within or among the sites sampled in this study it is important to
reiterate that this study targeted segments of the watershed that were already known to
62

contain western pearlshell and these findings should not be interpreted as evidence of
nonselective distributions of mussels within streams. Rather, it was hypothesized that if
mussels have a morphological response to differing habitat conditions it might be
reflected in the substrates in which mussels were found. It is interesting to note the
limited presence and use of boulders found at all three sites. Many publications found
that refugia from fast turbulent water behind boulders are important to mussel habitat
(Vannote and Minshall 1982, Stone et al 2006, Howard and Cuffy 2006). The slow
velocities and low discharge rates and Stillwater Creek explain both the absence of
boulders in the system as they cannot be moved or exposed, and the presence of mussels
without them as they are able to maintain their place in the substrate even at high water.
The Satsop site was situated behind a large fallen tree that may act in the same manner as
a boulder. South Elma has the highest discharge and fastest water yet little in the way of
cover substrate to protect the mussels. The large deep pool upstream of the site may settle
out larger substrates before they reach the mussel bed, but that has not been tested.
Temperature
Warmer water temperatures are known to be a factor controlling both mussel size
and growth rates (Bauer 1992). Of special interest in this study is that the Chehalis River
is not fed by glacial melt and the resulting water temperatures and flow reflect seasonal
temperature and precipitation influences and not the later peak discharge events and
prolonged cool water periods found in many of Washington’s large glacial rivers.
Unfortunately, a complete temperature profile was not collected year round at the
South Elma site due to the loss of a temperature sensor during high flow events in 2012

63

and redeployment of an additional logger was not conducted until later in the summer.
However, data were collected at all three sites July through October 2012 capturing the
period of the most dramatic growth in pearlshell mussels in our region (Toy
1998).Temperature was more variable at the South Elma and Satsop sites with South
Elma having both the highest and likely lowest temperatures based on historic patterns.
Stillwater Creek did not approach the high temperatures found at South Elma which had
temperatures reaching as high as 30°C in the 1970’s and likely into the present day
(United States Geological Survey 2013). Temperature is likely to play a role in
influencing the size differences found in pearlshell mussels here as it was in
Margaritifera margaritifera populations in Europe (Ziuganov et al. 2000; Bauer 1992).
Lower annual average temperatures at Stillwater may restrict their annual growth rate,
but overall their maximum size and life span could be longer (Bauer 1992). However
findings in this study found similar growth rates between populations making it unlikely
that the variation in temperatures between sites was influencing growth rates.
Stream discharge
Like temperature, discharge was found to be much more variable at South Elma
and Satsop with flows ranging from roughly 200- 300 cfs at low flow periods to over
30,000 during the rainy November – April periods of high precipitation. By contrast the
Stillwater site had only a 10 cfs difference throughout the year. South Elma was found to
have a much faster water speed at substrate than other sites. The less variable physical
conditions found at Stillwater Creek likely make a more stable environment for mussels
to exist and grow but warmer water could increase primary productivity and growth for
pearlshell mussels (Bauer 1992) and the swifter flows may bring more food sources past
64

the mussels and keep fine sediments from precipitating out of the water column and
burying the mussels (Howard and Cuffey 2006).
Water Quality
Water quality parameters measured in this study were within or close to reported
levels for most variables, the exception being alkalinity. The data found in the British
reports is regarding a separate species of Margaritifera so caution must be used when
relating them to western pearlshell in the Pacific Northwest. The reports are also from a
limited number of rivers with short time periods and may not represent the true range of
conditions in which M. margaritifera are found (Sime 2005).
All three sites border managed lands and there is a possibility that water could be
susceptible to spikes in nitrate levels from fertilization events and animal waste run-off
during large precipitation events, but this hypothesis was not tested because of the
resolution of sampling and the inability to pinpoint sources of nitrogen.
It is interesting that some M. margaritifera populations in Ireland have been
found in much harder rivers than summarized in most reports and the range of alkalinity
tolerances may be much broader than is commonly reported for Margaritifera species
(Moorkens et al 1992, Lucey 2006). The mussels in this study are in much harder water
than reported for most European populations (20.6 – 35.6 mg/L CaCO3, Table 2), but
appear to be establishing large and reproducing populations that have existed for greater
than half a century.
The pH of all three streams was within the range found in other theses and studies
in the state, but never fell below a neutral level as was found in their investigations
65

(Stock 1996, Toy 1998). Conductivity fell within the range that Toy (1998) found, but
was slightly lower on average.
Finally, when interpreting water quality parameters and tolerances it is critical to
address the duration of exposure to different conditions. Water quality ranges that are
beneficial or deleterious to mussels at one stage of their life (glochidia, larval, and
adult)may change as the mussel matures, and typical conditions of their natal water
bodies can influence individual populations (Sime 2005, Preston et al. 2010).
Limitations of this Study
This study was limited to an assessment of mussels found through visual and
tactile searches and likely over looked small juveniles and newly settled larvae. The
smallest individual encountered was 14.4 mm at Stillwater Creek. Their absence from
this study should not be taken as evidence of a lack of recruitment and likely
underestimates the true population age range. The methods used to age mussels in this
study were primitive at best and the sample size of aged mussels was small. Collection of
additional shells from study sites that encompasses a greater range of sizes should be sent
to a lab where proper equipment and experienced personnel can better evaluate the age
and growth of mussels in the lower Chehalis watershed.
It is likely that mussels in these sites responded to variables not investigated in
this study. The levels of primary production, respiration, and nutrient flow at each site
were not measured, but are known to influence the growth of freshwater mussels.
Quantification of additional variables is highly encouraged in the future. Other sites in the

66

lower Chehalis watershed should also be evaluated to increase the scope of the study and
confidence in its findings.
Conclusions
Western pearlshell mussels in this study show an increasing overall shell size in
the three metrics measured (length, width, and height) with increasing watershed size.
The proportions of the mussel’s size do not change concurring with reports that other
Margaritiferidae do not follow patterns observed in Ortmann’s Law (1920).
There is a pattern of increasing shell weight to length ratio between the
headwaters and main-stem habitats in the lower Chehalis Watershed, perhaps to protect
mussels in large rivers from damaging substrate movements in high discharge events.
The growth rate of mussels does not appear to be different between sites despite physical
differences between headwater and river habitats. One explanation for similar growth
rates could be the equalization of growth rates because of the seasonal variation between
sites in discharge, productivity, or temperature. For instance high summer productivity at
the South Elma sites may increase summer growth rates, but turbid water and high
discharge rates may restrict the mussels’ availability to feed and grow in during the rainy
winter and spring seasons. The Stillwater site which is cooler and likely less productive
in the summer months may have the advantage of having low discharge and warmer
waters allowing for feeding and growth in the same period that is restricted at South
Elma.
The large populations at both the South Elma and Stillwater Creek sites appear to
be stable and have evidence of recent reproduction. Both the South Elma and Stillwater
67

Creek sites are located in areas of commercial use. The South Elma site is surrounded by
plant and animal agricultural practices and the Stillwater Creek site is within an actively
managed forest. There has been no long term monitoring of these two sites which were
reported to have “lots of mussels” and be a “stronghold of mussels” respectively by
individuals visiting the sites before me. It is possible that because of a combination of
low levels of land conversion to urban and suburban areas, as well as the Clean Water
Act of 1972 and improving forest practices in Washington State both sites are not in
current peril. The Satsop population is much smaller and no signs of recruitment were
observed. Satsop may represent a sink population that could remain for some time or
perhaps disappear completely in a disturbance event such as the removal of the large
fallen dead tree that was observed to shelter the population. Long term monitoring of
these and other mussel population in the Chehalis River is needed to confirm the stability
and longevity of these populations.
Recent findings have shown that Margaritifera within the same region are not as
successful when translocated to other populated streams that have different characteristics
than within their natal streams (Valovirta 1998, Preston et al. 2010). Future investigations
of Margaritifera in the lower Chehalis River should involve experiments translocating
individuals from populations to measure rates of mortality and growth in different
positions within the watershed.

68

Chapter 6: The future of Freshwater Mussels in Washington
Freshwater mussels, as often stated in the first lines of nearly every publication I
have read during this thesis, are an imperiled group of organisms, and critically so. But
are these statements making the impact and creating the reaction that they desperately
need if their populations are to stabilize or increase? Documentation of mussel
populations in North America have provided protection to 35 species, and at least 10
were given protection under the US Endangered Species Act in 2012 alone (IUCN 2012),
but knowledge of mussel distributions and abundances is still lacking for many species
and in many watersheds. The challenge is to document populations and their abundances
before they decline or disappear from our streams. As there is no known effort to
systematically document freshwater mussels in Washington State the conservation of
mussels may depend on the ability of an informed public to identify and report mussels.
To that end efforts have been made by several organizations to educate and interest the
public about native freshwater mussels.
Pearlshell Mussels of Washington: Past, Present, and Future
As I finish this thesis I was greatly aided by Wendall Haag’s 2012 publication
Freshwater Mussels of North America. The author works in Oxford, Mississippi, not too
far from my childhood home in Mississippi. In my youth I spent time collecting and
observing numerous reptiles, amphibians, fish, and arthropods, ignorant that I was
overlooking an even more mysterious group of organisms at the bottom of those muddy
waterways, and in the case of the flat pigtoe mussel (Pleurobema marshalli) in the
Tombigbee River, their demise (Haag 2012). It was troubling to me that if I could grow

69

up, wandering the streams and lakes, in an area rich in freshwater mussels and never hear
of them, many other curious individuals may also not even know of their existence.
The two theses on pearlshell mussels in this state were written shortly before my
arrival. Amy Stock’s 1996 thesis at the Evergreen State College was written as I was
turning my thoughts to my future and Kelly Toy’s thesis completion at the University of
Washington in 1998 coincided with my high school graduation and arrival at the
University of Washington just a few short months later. Just several weeks prior to the
completion of this thesis I assisted in fish surveys at Bear Creek for monitoring the longterm health of urban streams in King County. I saw, as Toy predicted in 1998 and later
verified (Hastie and Toy 2008), piles of empty mussel shells scattered along the banks of
Bear Creek. In 2008, Toy called for “effective remedial action with the next 5–10 and 50
years”. That five years is up and to the best of my knowledge those populations have
continued to decline, despite the activism of impassioned individuals.
In 2012 and 2013 I led a joint US Fish and Wildlife and Educational Service
District 113 (www.ESD113.org) project dubbed the “Freshwater Mussel Academy.” This
program was inspired in part by Celeste Mazzacano’s citizen science program to monitor
mussels in urban creeks in Portland, Oregon (Dunkle 2012) and my own survey efforts.
The academy was composed of a group of middle and high school students from Grays
Harbor, Lewis, and Thurston counties and designed to both engage and excite students
about uncommon and exciting organisms in their “backyard,” as well as cover topics in
science and conservation biology. During the first half of this event, students were
introduced to the life history and disappearance and decline of mussels. For most of the
students, freshwater mussels were an entirely new organism with strange adaptations and
70

transformative cycles and with a clear association to Washington State’s iconic salmon.
In the second part of the event students went to the South Elma site for a hands-on look at
freshwater mussels and to learn about what it means to be a field technician. During the
field event students collected data that was included in parts of this thesis.
The Freshwater Mussel Academy served not only as a way to educate youth about
the diversity, wonder, decline of freshwater organisms, and their roles in the ecosystem,
but also served as evidence of local ecological knowledge within this generation of
students and perhaps will cause other students to note mussels in the future. Two of the
localities that were identified as undocumented localities of pearlshell mussels were from
conversations with this initial group of students. Several of the students who attended
high school in Elma were already aware of the presence of mussels at the South Elma
site. Since the initial Freshwater Mussel Academy, five other events have been similarly
conducted.
I hope that this effort allows some members in the next generation of scientists
and conservationists to appreciate both organisms that I was unaware of at that age and to
have a more holistic view of Pacific Northwest freshwater ecosystems.
Documentation of Freshwater Mussels in Washington State
Even prior to the 1993 publication by Williams and others documentations of the
impending loss of mussel fauna we have been aware of this decline. What life we see in
the rivers and lakes around us is not as rich as it once was. The Columbia River has been
depleted of its once abundant salmon, sturgeon, brown bears, wolves, grand ponderosa
pine and cotton wood-forests, but perhaps only a few note the loss of its once abundant
71

western pearlshell (Helmstetler and Cowles 2008). The overlooking of a species that once
fed the people and filtered the waters of our region’s largest and arguably most important
waterway highlights the great need for a central permanent entity to document and
monitor the status of these mussels in the Washington and the Pacific Northwest.
The Pacific Northwest Native Freshwater Mussel Work Group, Xerces Society,
and individuals, often self-funded, have dedicated themselves to the conservation of
mussels and the education of public about the plight of freshwater mussels. The Xerces
Society published a species profile for three Pacific Northwest native mussel species:
western pearlshell, western ridged, and California floater mussels which included
compiling extensive records of mussel localities throughout the Pacific Northwest Region
(Jespen et al. 2010a, 2010b, 2010c) including the records housed in the Washington
Department of Fish and Wildlife’s Priority Habitat Species database. This excellent
database, while exhaustive and detailed, was designed to be static. Much about the
locations and abundance of mussels remains undocumented. Field notes are stapled to
ziploc bags containing shells and neighbors of rivers and lakes recount stories of mussels
they once saw, but much of this knowledge goes undocumented as mussels in the Pacific
Northwest continue to disappear. It is acknowledged that a central, maintained, and easily
accessible location to document the presence of native freshwater mussels is needed for
the preservation conservation, and restoration of native freshwater mussels in
Washington and the Pacific Northwest.

72

Conclusion
Documentation and conservation of freshwater mussels in Washington State
should not be left solely to governmental and non-governmental organizations alone but
incorporate the knowledge of the public about localities and relative abundances of native
freshwater mussel species. The relatively few conversations with individuals not typically
considered biologists or conservationists included in this study led to a surprising number
of verifications of previously documented mussel populations and of populations that I
had not found specifically reported. Providing a central location to easily submit
information about mussel localities is acknowledged as a need by many interested in the
conservation of native freshwater mussels. In cases where local knowledge of mussel
populations may not exist, providing volunteer and curricular opportunities to learn and
work with freshwater mussels has been positively received by middle and high school
students in the Chehalis and South Puget Sound region. The educational outreach and
volunteer events produced informed citizens able to report on the localities of new and
future mussel populations and perhaps even sparked the interest of a future malacologist
or two.

73

Appendix I
Noted flora and fauna: This appendix is not a comprehensive list of species found at the
study sites, but rather a record extracted from field notes taken to document the presence
of organisms encountered while sampling.
*evidence of reproduction

Stillwater Creek:
Fauna
Common
Mollusca
Western Pearlshell Mussel*
Aquatic snails
Asian Clam
Arthropoda
Stone Flies
Mayflies
Signal Crayfish*

Flora
Latin
Margaritifera falcata
Juga spp.
Corbicula sp.
Plecoptera
Emphemeroptera
Pacifasticus lenticulus

Petromyzontiformes
Brook Lamprey*
Actinopterygii
Coho Salmon*
Steelhead
Coastal Cutthroat Trout*

Lampetra richardsonii

Three-spined Stickleback
Riffle Sculpin
Aves
Song Sparrow
Common Merganser
Stellars Jay
Amphibia
Northern Red-legged Frog
Pacific Chorus Frog
Reptilia
Common Garter Snake
Mammalia
Beaver
River Otter
Douglas Squirrel
Humans

Gasterosteus aculeatus
Cottus gulosus

Oncorhynchus kisutch
Oncorhynchus mykiss
Salmo clarkii

Melospiza melodia
Mergus merganser
Cyanocitta stelleri

Common
Trees
Red Alder
Western Hemlock
Douglas Fir
Western Red Cedar
Willow
Black Cottonwood
Shrubs
Devils Club

Latin

Stink Currant
Goose Berry
Pacific Nine Bark
Salmon Berry
Herbaceous vegetation
Horse Tails
Coontail
Pacific Bleeding Heart

Ribes bracteosum
Ribes lacustre
Physocarpus capitatus
Rubus spectabilis

Water-crowfoot

Ranunculus aquatilis

Alnus rubra
Tsuga heterophylla
Psuedotsuga menziesii
Thuja plicata
Salix spp
Poplus balsamifera
Oplo-panax horridus

Equistem
Ceratophyllum demersum
Dicentra formosa

Rana aurora
Psuedacris regilla
Thamnophis sirtalis
Castor canadensis
Lontra canadensis
Tamiasciurus douglasii
Homo sapiens

74

Lower Satsop:
Fauna
Common
Bivalvia
Western Pearlshell Mussel*
Asian Clam
Arthropoda
Stone Flies
Mayflies
Actinopterygii
Coho salmon
Steelhead
Coastal Cutthroat Trout
Redside Shiner
Largescale Sucker
Speckled Dace
Aves
Cedar Waxwing
Common Merganser
Chestnut-backed Chickadee
Turkey Vulture
Raven
Crow
Green Heron
Varied Thrush
Osprey
Great Blue Heron
Ruby Crowned Kinglet
Mammalia
Humans

Latin
Margaritifera falcata
Corbicula
Plecoptera
Emphemeroptera

Flora
Common
Trees
Willow
Black Cottonwood
Herbaceous vegetation
Japanese knotweed

Latin
Salix spp
Poplus balsamifera
Fallopia japonica

Oncorhynchus kisutch
Oncorhynchus mykiss
Salmo clarkii
Richardsonius balteatus
Catostomus macrocheilus
Rhinichthys osculus
Bombycilla cedrorum
Mergus merganser
Poecile rufescens
Cathartes aura
Corvus corax
Corvus brachyrhynchos
Butorides virescens
Ixoreus naevius
Pandion haliaetus
Ardea herodias
Regulus calendula
Homo sapiens

75

South Elma:
Fauna
Common
Bivalvia
Asian Clam
Western Ridged Mussel
Western Pearlshell Mussel*
Actinopterygii
Redside Shiner
Largescale Sucker
Aves
Barn owl
Amphibia
Northern Red-legged Frog
Mammalia
Humans

Latin
Corbicula spp
Gonidea angulata
Margaritifera falcata

Flora
Common
Trees
Red Alder
Willow
Black Cottonwood

Latin
Alnus rubra
Salix spp
Poplus balsamifera

Richardsonius balteatus
Catostomus macrocheilus
Tyto alba
Rana aurora
Homo sapiens

76

Appendix II: Field Sampling protocols and datasheets
Western Pearlshell Population Monitoring Protocol
This study will measure the abundance, density, size, and environmental
conditions targeting populations of the western pearlshell (Margaritifera falcata) for the
purpose of understanding demographics within and between 3 populations in the
Chehalis/Satsop watershed. Three study sites have been identified for sampling: 1) a
headwater stream population in Stillwater Creek, 2) the Satsop River, a major tributary,
and 3) the main=stem of the Chehalis River.
Data collection order:
1. Data sheet header information
2. Segment delineation and habitat assessment
3. Quadrant data (depth, temp, vegetation, wood, substrate, stream type)
4. Population counts/mussel measurement
5. Shell collection
6. Water quality (D.O., Temp, velocity, conductivity)
7. Site level
Header information: Fill out header information on all data sheets prior to starting
surveys
Site: three sites will be visited, Stillwater Creek, Lower Satsop River, and South
Elma.
Samplers: Record all sampler initials. Please record your initials first.
Date: Record sampling date: dd-mm-yyyy
Begin and end survey times: use the 24 hr. clock to record your begin and end times
(00:00)
Temp: record air temp at 1m above stream and water temp at the stream bed at the
beginning of the survey
Weather: coarsely describe weather conditions
Study segment and Habitat assessment:
Segment delineation
100 meters of stream length will be assessed at each stream site location. This 100 m
segment will span wetted stream width at some sites (Stillwater Creek and the Chehalis
River) and be restricted to the specific habitats where they exist in others (Satsop). All
segments will encompass areas in which mussels are known to occur and areas that can
be sampled without the need of scuba gear at low flow periods. An average stream
azimuth will be taken at the site and used to define the segment end point and divide the
segment into regular sampling quadrants.
Stream habitat assessment
77

Stream habitat assessment will follow the TFW Monitoring program Method Manual for
the Habitat Unit Survey (Pleus et. al, 1999), and the survey will segment the stream into
pool and riffle habitats. Habitats will be designated with RF for riffle and PL for pool and
be numbered sequentially from the downstream start point to upstream. Riffles are
characterized as shallower faster units with larger substrates in low-gradient areas. This
definition of a riffle includes habitat types such as glides, runs, cascades, and rapids.
Pools are areas of impounded water within a defined depression in the stream bed. Pools
can be formed by features such as changes in water velocity, boulders, LWD, beaver
dams and other blockages. Habitat lengths and widths will be measured as per TFW
guidelines (see below tables and reference TFW AM9-99-003) and recorded on the
habitat data sheet.

Unit
Length (m)
<2.5 to 5
≥5 to 10
≥10 to 20
≥20+

Minimum number
of paces per width
measurement
1
2
3
4+

Table 1: [TFW AM9-99-003 - table 5 (p19)] take the given number of paces between each wetted stream
width in each identified habitat unit.

Mean
segment
bankfull
width (m)
0 to <2.5
≥2.5 to <50
≥ 5 to <10.0
≥ 10 to <
15.0
≥ 15.0 to
<20.0
≥20

Minimum
unit size
(m2)
0.5
1
2

Minimum
residual
pool
depth (m)
0.1
0.2
0.25

3

0.3

4
5

0.35
0.4

Table 2: [TFW AM9-99-003 - table 2 (p10)] Guidelines on determining the minimum parameters that must
be met to be classified as a pool habitat. Residual pool depth = max pool depth – depth of water at pool
crest

Gradient: will be taken between habitat start and end points while standing on the bed of
the river or creek if possible and averaged over the length of the study site.
Measurements will be taken to the nearest tenth of a degree (0.0°).

78

Dominant and subdominant substrates: indicate the inorganic dominant and
subdominant substrates as averaged across the habitat unit. See tables in quadrant habitat
measurements below for substrate classes and definitions.
% Canopy cover: Using ocular estimates, record all vegetative cover above the water
surface to the nearest 10%. Cross verify and calibrate with sampling partner.
% Aquatic Vegetative Cover: Using ocular estimates, record all living vegetative cover
below the water surface to the nearest 10%. Cross verify and calibrate with sampling
partner. This can include filamentous algae, but not diatoms.
Mussels: Record the presence of mussels observed within the habitat unit. This is a quick
presence/absence survey as seen at any time while sampling habitat unit. Record Y (yes)
or N (not noted). It is not necessary to return to this sheet if mussels are discovered while
sampling quadrants.
Quadrant Placement
For every given habitat unit (RF or PL) in the study segment roughly 20 percent of the
area will be sampled for freshwater mussels. The number of quadrants will be determined
by multiplying the average width of the habitat unit times the length and dividing by five
(# quadrants = {L x Waverage)/5}. Quadrant locations will be determined using a random
number table for the longitudinal and latitudinal axis position of the stream (see end of
protocol for random number tables). Select a number by blindly placing a finger, pencil,
stick, or other object on the number table. Repeat the random coordinate selection
process for the number of calculated quadrants for each habitat unit. Check to ensure that
all coordinates are unique and fit within the habitat area parameter; if not repeat random
number selection until useable numbers are generated.
Quadrant Name: Record quadrant as “Site – habitat – x-y” (example: Stillwater-PL3-32).
Quadrant habitat measurements datasheet
Depth: Record water depth at the center of quadrant square to the nearest centimeter.
Woody Debris: Measure diameter and length of each piece of woody debris greater than
15 cm in diameter (>15 cm diameter) in the plot. The diameter and length of larger pieces
can be estimated if reasonable. Record the function that each piece of wood is providing.
Wood Function
Bank Stability
Depositional area
Scour
Loose

Pool
Step
Turbulence
Other

79

Habitat: Record the code that describes the specific stream habitat unit in which the
quadrant was located.
Habitat Code

Habitat Code

Glide

GL

Riffle

RF

Pool

PL

Other

OTHER

Glide: Deep, swift, and smooth surfaced reach of stream always low gradient.
Pool: A deep, slow to still moving habitat unit often associated with a pool wedge
or tailing, and scour area. This includes pools downstream of root balls and debris
jams.
Riffle: A rapid moving, shallow, and turbulent reach of stream typically not steep
(i.e. <6°).
Other: Any habitat unit that does not fit the above descriptions. Take detailed
notes and included sketches as needed.
Substrate: Record the code of the inorganic substrate that mussel was found in/on. If
needed indicate dominant and then subdominant substrates (i.e. GR/MUD). If there is no
subdominant substrate indicate its absence with NA.
Substrate Code

Substrate

Code

Mud/Silt

MUD Boulder

BO

Sand

SA

Bedrock

BED

Gravel

GR

Compacted Clay/ Marine Sediment CLY

Cobble

CO

Other

Other

Mud/Silt: Dense fine particles of sediment <0.06 mm in diameter often
associated with areas of little to no flow.
Sand: Fine granular particle of sediment 0.06 – 2 mm in diameter often
associated with stream banks and settle areas in pools
Gravel: Small rocks and pebbles 2 – 64 mm in diameter
Cobble: Larger rocks 64 – 256 mm in diameter
Boulder: Any rock larger than 256 mm in diameter.
Bedrock: continuous patches of underlying rock geology
Compacted Clay/ Marine Sediment: Marine sediment or compacted clay that
has not turned to sedimentary rock but provides a substrate visually similar to bed
rock. You can walk on this substrate without sinking into it, but may leave
impressions or footprints.
Other: Substrates other than as defined above, please specify in notes
80

Mussel measurements
Count: Record each mussel in a quadrant sequentially on the datasheet and measure each
individual encountered in the quadrant square. If any portion of the shell is within the
inside border of the quadrant, it is included in the total count. Count only live organisms
(not empty shells).
Mussel Name
Common
Scientific
W Pearlshell Margaritifera falcata
W Ridged
Gonidea angulata
Floaters
Anodonta sp

Code
MAFA
GOAN
ANSP

Mussel measurements: Record species code and measurements of each individual
counted to the nearest tenth of a millimeter (0.0mm) for the length, width, and height (Fig
1) in the population estimate.

Figure 1: Mussel measurement guidelines: take measurements at widest point in range to tenth of a
millimeter.
Image created by Ethan Nedeau, 2009: Freshwater Mussels of the Pacific Northwest. 2nd edition p.16

Aging and growth:
At each population site (Stillwater, Satsop, Chehalis) collect up to 20 complete and intact
shells for roughly every 10 cm increment of shell length. (0 – 10, 10 – 20 … 50 – 60 …)
Label mussel shells with species and site name.
Water quality
Dissolved Oxygen, conductivity, pH, and velocity:
These measurements will be taken just upstream, just downstream, and near the midpoint
of the defined study site at every site visit. Dissolved oxygen, conductivity, and
81

temperature measurements will be taken by calibrated YSI 60 or 85 multimeter. Velocity
will be measured with a Flo-Mate 2000 flow meter at the substrate level where mussels
would be present.
Site level variables
Mapping and stream typing: Record stream channel type (braided, channelized,
sinuous, etc.), underlying geology, stream order, and gradient at each site. Note any
roads, the general land-use, stream armoring, and alterations to the riparian area at each
site. Please include rough estimates of area affected.
Additional Data: Take notes and create species lists of all flora and fauna in associated
lentic, lotic, and riparian habitats with as much detail as possible. Of special interest is a
record of fish species seen at sites.

82

Quadrant microhabitat data
Site:
Samplers:
Quadrant
ID
Habitat

Date:

Weather:
page:

Depth Dom
Subdom
Wood Wood
(cm)
Substrate Substrate dia
Funct

of

Notes

83

1. Mussel datasheet
Site:

Date:

Samplers:

Start plot

Quadrant
ID

Count Species

Length

Weather:
End plot
Width

Height

page:
Gravid

of

Juv (Y/N)

Notes

84

Appendix III: Detailed information from informal communications and opportunistic
sampling

MAFA

MAFA

MAFA

AN sp

22

22

22

22

19

19

Biologist

Biologist

Biologist

Clallam Biologist

Clallam Biologist
Biologist/
Clallam educator

Found on survey for mussels.

Beautiful site

located during salmonid survey
conversation and interpretive sign
revealed these populations
interpretive signs and conversation with
park biologist
Called "stronghold of the Mussels" by
biologist

Comments

Y

N

Y

Y

N

N

N

Y

Y

Y

Y

Y

Y

N

Y

Y

Y

Y

Y

N

N

S

S

S

L

L

L

L

L

Live
Ora Field
or
l
Verified Shell

7 Satsop Slough
South Elma on
8 Chehalis River
Taylors Ferry,
9 Chehalis River
Meskill Road
10 Slough Chehalis
11 Discovery Site
South Hanaford
12 Creek
14 Spanaway Creek

Species WRIA County Source

MAFA

22

Mason
Grays
Harbor
Grays
Harbor
Grays
Harbor
Grays
Harbor
Grays
Harbor

Biologist
Anodonta Clade 2
four fishermen, and two students
Sportsman identified this site. Very well known.
Homeless man "eats them Raw" at this
Subsistance site.
Complete shells, likely mammal predation.
Biologist
Side channel Slough off Chehalis River
brought to attention of educator by land
owner on field trip

N

N

Key Locality

AN sp

22

Lewis

Educator

Shell Anodonta Clade II

Y

Y

N

2 Crescent Lake

MAFA

23

Lewis

Biologist

Y

15 Clear Lake

AN sp
UNKW
N

Y

3 Lyre River

MAFA

23

Lewis

Sportsman

Seen Racoons eating them
Anodonta in small pond south of Clear
Lake

N

15 Lower Nisqually

19

4 Stillwater Creek

AN sp

23

Pierce

Educator

Y

N

49

MAFA

5 Lower Stillwater

MAFA

10

Pierce

On Lower Nisqually

Y

1 Sooes River

6 Satsop WDFW

AN sp
UNKW
N

11

"mud mussels" 1960s-2013

AN sp

S

L
11

Thurston Sportsman
Okanog
an
Retiree
16 Osoyoos Lake

85

Works Cited
Adair, B., G. Silver, T. Whitesel, and K. Kittel. 2009. Preliminary Evidence that Sculpin
Species Native to the Pacific Northwest do not Serve as a Host in the Reproductive Cycle
of the Western Pearlshell Mussel (Margaritifera falcata). Government, USFWS,
Vancouver WA.
Allard, D., M. Koski, and T. Whitesel. 2012. Western Pearlshell Mussel Reproduction in
Merrill Creek, Oregon: Timing. Page 17. USFWS, U.S. Fish and Wildlife Service
Columbia River Fisheries Program Office 1211 SE Cardinal Court, Suite 100.
Azzurro, E., P. Moschella, and F. Maynou. 2011. Tracking Signals of Change in
Mediterranean Fish Diversity Based on Local Ecological Knowledge. PLoS ONE
6:e24885.Bauer, G. 1988. Threats to the freshwater pearl mussel Margaritifera
margaritifera L. in Central Europe. Biological Conservation 45:239–253.
Bauer, G. 1992. Variation in the Life Span and Size of the Freshwater Pearl Mussel.
Journal of Animal Ecology 61:425–436.
Bauer, Gerhard, and Klaus Wächtler. 2001. Ecology and Evolution of the Freshwater
Mussels Unionoida. Springer.Bishop, and Pemberton. 2006. The Third Way: Spermcast
Mating in Sessile Marine Invertebrates. Integr. Comp. Biol. 46.
Black, B. A., J. B. Dunham, B. W. Blundon, M. F. Raggon, and D. Zima. 2010. Spatial
Variability in Growth-Increment Chronologies of Long-Lived Freshwater Mussels:
Implications for Climate Impacts and Reconstructions. Ecoscience 17:240–250.
Bogan, A. 2008. Global Diversity of Freshwater Mussels (Mollusca, Bivalvia) in
Freshwater. pages 139–147 in E. V. Balian, C. Lévêque, H. Segers, and K. Martens,
editors. Freshwater Animal Diversity Assessment. Springer Netherlands.
Bogan, A. E. 1993. Freshwater Bivalve Extinctions (Mollusca: Unionoida): A Search for
Causes. American Zoologist 33:599–609.
Brook, R. K., and S. M. McLachlan. 2008. Trends and Prospects for Local Knowledge in
Ecological and Conservation Research and Monitoring. Biodiversity and Conservation
17:3501–3512.
Cope, W. G., R. B. Bringolf, D. B. Buchwalter, T. J. Newton, C. G. Ingersoll, N. Wang,
T. Augspurger, F. J. Dwyer, M. C. Barnhart, R. J. Neves, and E. Hammer. 2008.
Differential Exposure, Duration, and Sensitivity of Unionoidean Bivalve Life Stages to
Environmental Contaminants. Journal of the North American Benthological Society
27:451–462.

86

Counts III, C. L. 1986. "The Zoogeography and History of the Invasion of the United
States by Corbicula fluminea (Bivalvia: Corbiculidae). American Malacological Bulletin.
Cowles, D. L. 2012, March 21. Between a Rock and a Silty Place: Margaritifera falcata
Mussels and Dams in the Elwha River. Society for Northwest Vertebrate Biology Annual
Meeting. Hood River, Oregon.
Douda, K., M. Vrtílek, O. Slavík, and M. Reichard. 2012. The Role of Host Specificity in
Explaining the Invasion Success of the Freshwater Mussel Anodonta woodiana in
Europe. Biological Invasions 14:127–137.
Dudgeon, D., A. Arthington, Mark Gessner, Z.-I. Kawabata, D. J. Knowler, C. Lévêque,
R. J. Naiman, A.-H. Prieur-Richard, D. Soto, M. L. J. Stiassny, and C. A. Sullivan. 2006.
Freshwater Biodiversity: Importance, Threats, Status and Conservation Challenges.
Biological Reviews 81:163–182.
Haag, W. R. 2012. North American Freshwater Mussels: Natural History, Ecology, and
Conservation. Cambridge University Press.
Haag, W. R., D. J. Berg, D. W. Garton, and J. L. Farris. 1993. Reduced Survival and
Fitness in Native Bivalves in Response to Fouling by the Introduced Zebra Mussel
(Dreissena polymorpha) in Western Lake Erie. Canadian Journal of Fisheries and
Aquatic Sciences 50:13–19.
Hastie, L. C., P. J. Cosgrove, N. Ellis, and M. J. Gaywood. 2003. The Threat of Climate
Change to Freshwater Pearl Mussel Populations. Ambio 32:40–46.
Hastie, L. C., and K. Toy. 2008. Changes in Density, Age Structure and Age-specific
Mortality in Two Western Pearlshell (Margaritifera falcata) Populations in Washington
(1995-2006). Aquatic Conservation: Marine and Freshwater Ecosystems 18:671 – 678.
Helmstetler, H., and D. L. Cowles. 2008. Population Characteristics of Native Freshwater
Mussels in the mid-Columbia and Clearwater Rivers, Washington State. Northwest
Science 82:211.
Hornbach, D. J., V. J. Kurth, and M. C. Hove. 2010. Variation in Freshwater Mussel
Shell Sculpture and Shape Along a River Gradient. The American Midland Naturalist
164:22–36.
Hovingh, P. 2004. Intermountain Freshwater Mollusks, USA (Margaritifera, Anodonta,
Gonidea, Valvata, Ferrissia): Geography, Conservation, and Fish Management
Implications. Monographs of the Western North American Naturalist 2:109–135.

87

Howard, J. K., and K. M. Cuffey. 2003. Freshwater Mussels in a California North Coast
Range River: Occurrence, Distribution, and Controls. Journal of the North American
Benthological Society 22:63–77.
Howard, J. K., and K. M. Cuffey. 2005. Factors Controlling the Age Structure of
Margaritifera falcata in Two Northern California Streams. AGU Spring Meeting
Abstracts -1:03.
Howard, J. K., and K. M. Cuffey. 2006. Factors Controlling the Age Structure of
Margaritifera falcata in 2 Northern California Streams. Journal of the North American
Benthological Society 25:677–690.
Jespen, S. 2012, March 21. The Conservation Status of Western Freshwater Mussels.
Society for Northwest Vertebrate Biology Annual Meeting. Hood River, Oregon.
Jespen, S., C. LaBar, and J. Zarnoch. 2010a. Freshwater mussels: California floater
(Anodonta californiensis)/Winged floater (Anodonta nuttalliana). Literature Review,
Xerces Society.
Jespen, S., C. LeBar, and J. Zarnoch. 2010b. Freshwater Mussels: Western Pearlshell
(Margaritifera falcata). Pages 1 – 24. Literature Review, Xerces Society.
Jespen, S., C. LeBar, and J. Zarnoch. 2010c. Freshwater Mussels: Western Ridged
Mussel (Gonidea angulata). Pages 1 – 19. Literature Review, Xerces Society, Portland,
OR.
Krueger, K., P. Chapman, M. Hallock, and T. Quinn. 2007. Some Effects of Suction
Dredge Placer Mining on the Short-term Survival of Freshwater Mussels in Washington.
Northwest Science 81:323–332.
Leff, L. G., J. L. Burch, and J. V. Mcarthur. 1990. Spatial Distribution, Seston Removal,
and Potential Competitive Interactions of the Bivalves Corbicula fluminea and Elliptio
complanata, in a Coastal Plain Stream. Freshwater Biology 24:409–416.
Limm, M. P., and M. E. Power. 2011. Effect of the Western Pearlshell Mussel
Margaritifera falcata on Pacific Lamprey Lampetra tridentata and Ecosystem Processes.
Oikos 120:1076–1082.
Lohr, S., and J. Glasgow. 2005. Freshwater Mussel Observations in Five Clark County,
Washington Streams. Page 40. Wild Fish Unlimited, Duvall, WA.
Lucey, John. 2006. The Pearl Mussel, Margaritifera margaritifera (L.), in Hard Water in
Ireland. Biology and Environment: Proceedings of the Royal Irish Academy 106B(2):
143–53.
88

MacLellan, S. E. 1976. How to Age Rockfish (Sebastes) Using S. alutus as an Example The Otolith Burnt Section Technique. Technical Report, Canadian Technical Report of
Fisheries and Aquatic Science.
Mazzacano, C. 2012, March 21. Working with Watershed Councils to Conserve
Freshwater Mussels: Volunteer-based Surveys in Urban areas. Society for Northwest
Vertebrate Biology Annual Meeting. Hood River, Oregon.
Moorkens, Evelyn A., Mark J. Costello, and Martin C. D. Speight. 1992. “Status of the
Freshwater Pearl Mussels Margaritifera Margaritifera and M. M. Durrovensis in the
Nore, Barrow and Suir River Tributaries, South-East Ireland.” The Irish Naturalists’
Journal 24(3): 127–31.
Mote, P., and E. Salathe. 2010. Future Climate in the Pacific Northwest. Climatic Change
102:29–50.
Murphy, G. 1942. Relationship of the Fresh Water Mussel to Trout in the Truckee River.
Pages 89 – 102. Government, California Fish and Game.
Naimo, T. J. 1995. A Review of the Effects of Heavy Metals on Freshwater Mussels.
Ecotoxicology 4, no. 6 (1995): 341-362. Ecotoxicology 4:341 – 362.
Nedeau, E. J., A. K. S. (membre du P. N. N. F. M. Workgroup), and J. Stone. 2009. Field
Guide to the Freshwater Mussels of the Pacific Northwest. Fish and Wildlife Service.
Neves, Richard J., and Michael C. Odom. 1989. Muskrat Predation on Endangered
Freshwater Mussels in Virginia. The Journal of Wildlife Management 53(4): 934.
O’Brien, C., D. Nez, D. Wolf, and J. B. Box. 2013. Reproductive Biology of Anodonta
californiensis, Gonidea angulata, and Margaritifera falcata (Bivalvia: Unionoida) in the
Middle Fork John Day River, Oregon. Northwest Science 87:59–72.
Oliver, G. 2000. Conservation Objectives for the Freshwater Pearl Mussel (Margaritifera
margaritifera). English Nature, Peterborough, UK.
Ortmann, A. E. 1909. The Destruction of the Fresh-water Fauna in Western
Pennsylvania. 48.191 (1909): 90-110. Proceedings of the American Philosophical
Society 48:90 – 110.
Ortmann, A. E. 1920. Correlation of Shape and Station in Fresh-Water Mussels
(Naiades). Proceedings of the American Philosophical Society 59:269–312.
Pandolfo, T. J., W. G. Cope, C. Arellano, R. B. Bringolf, M. C. Barnhart, and E.
Hammer. 2010, June 29. Upper Thermal Tolerances of Early Life Stages of Freshwater
Mussels.
89

Pleus, A. E., D. Schuett-Hames, and L. Bullchild. 1999. TFW Monitoring Program
Method Manuel for the Habitat Unit Survey. DNR.
Poos, M., A. J. Dextrase, A. N. Schwalb, and J. D. Ackerman. 2010. Secondary Invasion
of the Round Goby into High Diversity Great Lakes Tributaries and Species at Risk
Hotspots: Potential New Concerns for Endangered Freshwater Species. Biological
Invasions 12:1269–1284.
Preston, S. J., A. Harrison, M. Lundy, D. Roberts, N. Beddoe, and D. Rogowski. 2010.
Square Pegs in Round Holes — the Implications of Shell Shape Variation on the
Translocation of Adult Margaritifera margaritifera (L.). Aquatic Conservation: Marine
and Freshwater Ecosystems 20:568–573.
Richter, B. D., D. P. Braun, M. A. Mendelson, and L. L. Master. 1997. Threats to
Imperiled Freshwater Fauna. Conservation Biology 11:1081 – 1093.
Sime, I. 2005. A Literature Review of the Water Quality Requirements of the Freshwater
Pearl Mussel (Margaritifera margaritifera) and Related Freshwater Bivalves. Scottish
Natural History Commissioned Report, Scottish Natural History.
Skinner, A., M. Young, and L. Hastie. 2003. Ecology of the Freshwater Pearl Mussel:
Margaritifera margaritifera. English Nature, Peterborough, UK.
Spooner, D. E., and C. C. Vaughn. 2006. Context-dependent Effects of Freshwater
Mussels on Stream Benthic Communities. Freshwater Biology 51:1016–1024.
Stagliano, D. 2010. Freshwater Mussels in Montana: Comprehensive Results from 3
years of SWG Funded Surveys. Page 74. Montana Fish Wildlife and Parks.
Stanley, S. M. 1981. Infaunal Survival: Alternative Functions of Shell Ornamentation in
the Bivalvia (Mollusca). Paleobiology 7:384–393.
Stein, B. A., L. S. Kutner, and J. S. Adams. 2000. Precious Heritage: The Status of
Biodiversity in the United States. Oxford University Press, USA.
Stock, A. L. 1996. Habitat and Population Characteristics of the Freshwater Mussel
Margaritifera falcata in Nason Creek, Washington. The Evergreen State College,
Olympia, WA.
Stokstad, E. 2012. Nearly Buried, Mussels Get a Helping Hand. Science 338:876–878.
Stone, J., S. Barndt, and M. Gangloff. 2004. Spatial Distribution and Habitat Use of the
Western Pearlshell Mussel (Margaritifera falcata) in a Western Washington Stream.
Journal of Freshwater Ecology 19:341–352.

90

Strayer, D. L. 1999. Statistical Power of Presence‐Absence Data to Detect Population
Declines. Conservation Biology 13:1034–1038.
Strayer, D. L. 2008. Freshwater Mussel Ecology: A Multifactor Approach to Distribution
and Abundance. University of California Press.
Strayer, D. L. 2010. Alien species in Fresh Waters: Ecological Effects, Interactions with
other Stressors, and Prospects for the Future. Freshwater Biology 55:152–174.
Strayer, D. L., and D. Dudgeon. 2010. Freshwater Biodiversity Conservation: Recent
Progress and Future Challenges. Journal of the North American Benthological Society
29:344–358.
Strayer, D. L., and D. R. Smith. 2003. A Guide to Sampling Freshwater Mussel
Populations. American Fisheries Society.
Strayer, D. L., and L. C. Smith. 1996. Relationships between Zebra Mussels (Dreissena
polymorpha) and Unionid Clams during the Early Stages of the Zebra Mussel Invasion of
the Hudson River. Freshwater Biology 36:771–779.
Toy, K. 1998. Growth, Reproduction, and Habitat Preference of the Freshwater Mussel,
Margaritifera margaritifera falcata, in Western Washington. Masters of Science,
Fisheries, University of Washington, Seattle, WA.
Turvey, S. T. 2009. Holocene Extinctions. Oxford University Press, Oxford; New York.
United States Geological Survey. 2013, May 13. USGS 12031000 Chehalis River at
Porter, WA. Government.
United States Geological Survey. 2013. Chehalis River Basin. USGS Washington Water
Science Center. Federal Government. Retrieved from
http://wa.water.usgs.gov/projects/chehalis/
United States Geological Survey. 2013. USGS 12031000 Chehalis River at Porter,
WA. National Water Information System: Web Interface. Federal Government. Retrieved
from http://waterdata.usgs.gov/wa/nwis/uv?site_no=12031000
USGS. (2013). USGS 12035000 Satsop River near Satsop, WA. National Water
Information System: Web Interface. Federal Government. Retrieved from
http://waterdata.usgs.gov/wa/nwis/uv?site_no=12035000
Valovirta, I. 1990. Conservation of Margaritifera margaritifera in Finland.
Environmental Encounters, Council of Europe.

91

Vannote, R. L., and G. W. Minshall. 1982. Fluvial Processes and Local Lithology
Controlling Abundance, Structure, and Composition of Mussel Beds. Proceedings of the
National Academy of Sciences 79:4103–4107.
Vaughn, C. C., S. J. Nichols, and D. E. Spooner. 2008. Community and Foodweb
Ecology of Freshwater Mussels. The Society for Freshwater Science.
Vaughn, C. C., and C. M. Taylor. 1999. Impoundments and the Decline of Freshwater
Mussels: a Case Study of an Extinction Gradient. Conservation Biology 13:912–920.
Washington Department of Fish and Wildlife. 2012. WDFW, Priority Habitat Species
Database. Washington Department of Fish and Wildlife.
Watters, G. Thomas. 1994. Form and Function of Unionoidean Shell Sculpture and Shape
(Bivalvia). American Malacological Bulletin 11:1–20.
Watters, G. Thomas, and S. H. O’Dee. 1998. Metamorphosis of Freshwater Mussel
Glochidia (Bivalvia: Unionidae) on Amphibians and Exotic Fishes. The American
Midland Naturalist 139:49–57.
Watters, G. Thomas. 1999. Freshwater Mussels and Water Quality: A Review of the
Effects of Hydrologic and Instream Habitat Alterations. Proceedings of the First
Freshwater Mollusk Conservation Society Symposium. Vol. 1.
Williams, J. D., M. L. Warren, K. S. Cummings, J. L. Harris, and R. J. Neves. 1993.
Conservation Status of Freshwater Mussels of the United States and Canada. Fisheries
18:6–22.
Wong, W. 1993, July 8. County Makes It Official: Indian Midden Is Landmark. Seattle
Times. Seattle, WA.
Wydoski, R. S., and R. R. Whitney. 2003. Inland Fishes of Washington. American
Fisheries Society in Association with University of Washington Press, Bethesda, MD.
Young, M. R., L. C. Hastie, and S. Cooksley. 2003. Monitoring the Freshwater Pearl
Mussel Margaritifera margaritifera. University of Aberdeen, Peterborough, UK.
Ziuganov, V., E. S. Miguel, R. J. Neves, A. Longa, C. Fernández, R. Amaro, V. Beletsky,
E. Popkovitch, S. Kaliuzhin, and T. Johnson. 2000. Life Span Variation of the Freshwater
Pearl Shell: A Model Species for Testing Longevity Mechanisms in Animals. AMBIO: A
Journal of the Human Environment 29:102–105.

92