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TR EL-82-4 ~iological Report 82(1 1.85) September 1988 Species Profiles: ~hvironmental Requirements of Coastal Fishes and Invertebrates (Pacific Northwest) PACIFIC OYSTER Coastal Ecology Group Fish and Wildlife Service Waterways Experiment Station U.S. Department of the Interior U.S. Army Corps of Engineers

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TR EL-82-4 ~iological Report 82(1 1.85)

September 1988

Species Profiles: ~hvironmental Requirements of Coastal Fishes and Invertebrates (Pacific Northwest)

PACIFIC OYSTER

Coastal Ecology Group Fish and Wildlife Service Waterways Experiment Station U.S. Department of the Interior U.S. Army Corps of Engineers

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B i o l o g i c a l Repor t 82(11.85) TR EL-82-4 September 1988

Species P r o f i l e s : L i f e H i s t o r i e s and Envi ronmenta l Requirements of Coasta l F ishes and I n v e r t e b r a t e s ( P a c i f i c Nor thwest )

PACIFIC OYSTER

G i l b e r t B. Pauley, B i r g i t t a Van Der Raay, and Dav id T r o u t t Washington Coopera t i ve F i she ry Research U n i t

Co l lege of Ocean and F i she ry Sciences U n i v e r s i t y o f Washington

Sea t t l e , WA 98195

P r o j e c t Manager C a r r o l l Cordes P r o j e c t O f f i c e r

Dav id Moran U.S. F i s h and W i l d l i f e Se rv i ce

Na t i ona l Wetlands Research Center 1010 Gause Bou levard

S l i d e l l , LA 70458

Performed f o r

Coasta l Ecology Group Waterways Exper iment S t a t i o n U.S. Army Corps o f Eng ineers

Vicksburg, MS 39180

and

U. S. Department o f t h e I n t e r i o r F i s h and W i l d l i f e Se rv i ce Research and Development

Na t i ona l Wet1 ands Research Center Washington, DC 20240

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DISCLAIMER

The ment ion o f t r a d e names does n o t c o n s t i t u t e endorsement o r recommendation f o r use by t h e Federa l Government.

T h i s s e r i e s may be r e f e renced as f o l l o w s :

U.S. F i s h and W i l d l i f e Serv ice . 1983-19-. Species p r o f i l e s : l i f e h i s t o r i e s and env i ronmenta l requ i rements o f coas ta l f i s h e s and i n v e r t e b r a t e s . U. S. F i s h W i l d l . Serv. B i o l . Rep. 82(11). U.S. Army Corps o f Engineers, TR EL-82-4.

T h i s p r o f i l e may be c i t e d as f o l l o w s :

Pauley, G.B., B. Van Der Raay, and D. T r o u t t . 1988. Species p r o f i l e s : l i f e h i s t o r i e s and env i ronmenta l requi rements o f coas ta l f i s h e s and i n v e r t e b r a t e s ( P a c i f i c Nor thwes t ) - -Pac i f i c oys te r . U. S. F i s h W i l d l . Serv. B i o l . Rep. 82(11.85). U.S. Army Corps o f Engineers, TR EL-82.4. 28pp.

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PREFACE

This species p r o f i l e i s one o f a se r i es on coasta l aquat ic organisms, p r i n c i p a l l y f i s h , o f spor t , commercial, o r eco log ica l importance. The p r o f i l e s are designed t o provide coasta l managers, engineers, and b i o l o g i s t s w i t h a b r i e f comprehensive sketch o f the b i o l o g i c a l c h a r a c t e r i s t i c s and env i ronmental requirements o f the species and t o descr ibe how populat ions o f t he species may be expected t o r e a c t t o environmental changes caused by coasta l development. Each p r o f i l e has sec t ions on taxonomy, 1 i f e h i s t o r y , eco log ica l r o l e , environmental requirements, and economic importance, i f appl i cab le . A t h r e e - r i n g b inde r i s used f o r t h i s se r i es so t h a t new p r o f i l e s can be added as they are prepared. This p r o j e c t i s j o i n t l y planned and f inanced by the U.S. Army Corps o f Engineers and the U.S. F ish and W i l d l i f e Service.

Permission was obta ined from the Canada Department o f F i she r ies and Oceans t o use copyr igh ted ma te r i a l from P a c i f i c Oyster Cu l tu re j~ B r i t i s h Columbia by D.B. Quay1 e (1969).

Suggestions o r quest ions regard ing t h i s r e p o r t should be d i r e c t e d t o one o f the f o l 1 owing addresses.

In fo rmat ion Trans fer Speci a1 i s t Nat iona l Wetlands Research Center U.S. F i sh and W i l d l i f e Serv ice NASA-Sl i d e l 1 Computer Complex 1010 Gause Boul evard S l i d e l l , LA 70458

U.S. Army Engineer Waterways Experiment S t a t i o n A t ten t i on : WESER-C Post O f f i c e Box 631 Vicksburg, MS 39180

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CONVERSION TABLE

M e t r i c t o U. S. Customary

Mu1 t i p l y

m i l l i m e t e r s (mm) cent imeters (cm) meters (m) meters (m) k i 1 ometers (km) k i l omete rs (km)

square meters (m2) 10.76 square k i lomete rs (km2) 0.3861 hectares (ha) 2.471

l i t e r s (1) cub ic meters (m3) cub ic meters (m3)

m i l l i g r a m s (mg) grams (g) k i 1 ograms (kg) m e t r i c tons (t) m e t r i c tons (t)

k i l o c a l o r i e s ( k c a l ) Ce ls ius degrees ( O C )

inches inches f e e t ( f t ) fathoms s t a t u t e m i l e s ( m i ) n a u t i c a l m i l e s (nmi)

square f e e t ( f t2) square m i l e s ( m i 2 ) acres

gal l ons (ga l ) cub ic f e e t ( f t 3 ) a c r e - f e e t

ounces (oz) ounces (02)

pounds ( l b ) pounds ( l b ) s h o r t tons ( t o n )

B r i t i s h thermal u n i t s (Btu) Fahrenhei t degrees (OF)

U.S . Customary t o M e t r i c

25.40 2.54 0.3048 1.829 1.609 1.852

To Obta in

i nches inches f e e t fathoms s t a t u t e m i l e s n a u t i c a l m i l e s

square f e e t square m i l e s acres

ga l lons cub ic f e e t a c r e - f e e t

ounces ounces pounds pounds s h o r t tons

B r i t i s h thermal u n i t s Fahrenhe i t degrees

m i l l i m e t e r s cen t imete rs meters meters k i 1 ometers k i 1 ometers

square meters square k i lometers hectares

1 i t e r s cub ic meters cub ic meters

m i l l i g r a m s grams k i 1 ograms m e t r i c tons m e t r i c tons

k i l o c a l o r i e s Ce ls ius degrees

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CONTENTS

Page

PREFACE . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . i i i CONVERSION TABLE . . . . . . . . . . . . . . . . . . . . . . . . . . i v ACKNOWLEDGMENTS . . . . . . . . . . . . . . . . . . . . . . . . . . . v i

NaMENCLATURE/TAXONOMY/RANGE . . . . . . . . . . . . . . . . . . . . . 1 MORPHOLOGY AND IDENTIFICATION AIDS . . . . . . . . . . . . . . . . . 1 REASON FOR INCLUSION I N SERIES . . . . . . . . . . . . . . . . . . . 4

. . . . . . . . . . . . . . . . . . . . . . . . . . . . LIFE HISTORY 4 Reproduct ive P h y s i o l ogy . . . . . . . . . . . . . . . . . . . . 5 Spawning . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5

. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Eggs 5 . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Larvae 5

A d u l t s . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 6 GROWTH CHARACTERISTICS . . . . . . . . . . . . a . m . . . . . . . . 7 THE FISHERY . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 8 . . . . . . . . . . . . . . . . . . . . . . . . Economic S t a t u s 8

Farming . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1 0 ECOLOGICAL ROLE . . . . . . . . . . . . . . . . . . . . . . . . . . . 12

Feeding Behav io r . . . . . . . . . . . . . . . . . . . . . . . . 12 Summer M o r t a l i t y . . . . . . . . . . . . . . . . . . . . . . . . 1 3 P r e d a t o r s . . . . . . . . . . . . . . . . . . . . . . . . . . . 1 3 P a r a s i t e s . . . . . . . . . . . . . . . . . . . . . . . . . . . 15 Disease . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1 5 Red T i d e . . . . . . . . . . . . . . . . . . . . . . . . . . . . 1 5

ENVIRONMENTAL REQUIREMENTS . . . . . . . . . . . . . . . . . . . . . 17 Temperature . . . . . . . . . . . . . . . . . . . . . . . . . . 1 7 S a l i n i t y . . . . . . . . . . . . . . . . . . . . . . . . . . . . 18 S i l t a t i o n and S u b s t r a t e . . . . . . . . . . . . . . . . . . . . 19 Water C i r c u l a t i o n . . . . . . . . . . . . . . . . . . . . . . . 19 P o l l u t i o n . . . . . . . . . . . . . . . . . . . . . . . . . . . 20

. . . . . . . . . . . . . . . . . . . . . . . . . . LITERATURE CITED 23

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ACKNOWLEDGMENTS

We are g ra te fu l f o r peer reviews by Ne i l Bourne o f the Canada Department o f Fisheries and Oceans, Kenneth Chew o f the Univers i ty o f Washington, and Alber t Sparks o f the National Marine Fisheries Service.

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Figure 1. P a c i f i c oys te r (Crassostrea g igas ) , showing ex terna l anatomy of s h e l l valves.

P A C I F I C OYSTER

S c i e n t i f i c name . . . . . Crassostrea g igas (Thunberg)

Pre er red common name . . . . P a c i f i c oyster (F igure 1)

Other common names . . . Giant oyster , Japanese oyster , Giant P a c i f i c oys ter

Class . . . . . . . . . . . . B i v a l v i a Order . . . . . . . . . . .Anisomyaria Family . . . . . . . . . . . Ostre idae

Geographic Range: Morro Bay, C a l i f o r n i a , t o nor thern B r i t i s h Columbia; Japan (Quayle 1960; F i t c h 1953). Quayle (1969a) repor ted t h a t breeding occurs na tu ra l l y on l y between Wi l lapa Harbour ( l a t . 46O N.) and Pendrel l Sound ( l a t . 50° N. ) Consistent breeding occurs on l y i n Dabob and Qui lcene Bays i n Washington and Pendrel l Sound and Pipestem I n l e t i n B r i t i s h Col umbia; breeding i s r a r e o r sporadic i n o the r loca t ions . Since the P a c i f i c oys ter has been moved i n t o a l l t h e p o t e n t i a l oys ter

growing areas i n Washington, t he species i s a t o r near i t s geographical breeding 1 i m i t (Quayle 1960). Major areas of commercial and rec rea t i ona l harves t o f P a c i f i c oys ters are shown i n F igure 2.

MORPHOLOGY AND IDENTIFICATION AIDS

The s h e l l i s extremely rough, ex tens i ve l y f l u t e d , and 1ami nated. The lower va lve i s deeply cupped and the upper valve i s gene ra l l y f l a t . The s h e l l s a re u s u a l l y w h i t i s h w i t h many pu rp le st reaks and spots r a d i a t i n g away from t h e umbo. The shape o f t he s h e l l va r i es w i t h t h e environment (see Growth sect ion) . 'The i n t e r i o r o f t he s h e l l i s wh i te , w i t h a s i n g l e muscle scar t h a t i s sometimes dark, b u t never pu rp le o r black. Maximum leng th i s 10 inches, b u t normal ly l eng th i s 4-6 inches. D i f f e r s from Crassostrea v i r g i n i c a i n never having a pu rp le o r b lack muscle scar , and from Ostrea l u r i d a i n i t s

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VANCOUVER I.

BELLINGHAM UCKANUT BAY

TRAIT OF GEORGIA

SAN JUAN ISLANDS

GRA YS HARBOR

WILLAPA BAY

WASHINGTON

Figure 2. Geographic d i s t r i b u t i o n o f t h e P a c i f i c oys te r i n t h e P a c i f i c North- west, showing major areas o f harvest , commercial and rec rea t i ona l .

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YAQUINA BAY

Recreational and cornmerclal harvest

KILOMETERS

-'\

HUMBOLDT BAY

CALIFORNIA

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ex t reme ly l a r g e s i z e and heavy s h e l l . I n a d d i t i o n , t h e i n s i d e o f an c. l u r i d a s h e l l i s i r i d e s c e n t green. Fo r a comparison o f C. g a s , C. v i r g i n i c a , and 0. l u r i d a see Table 1. D e t a i l e d d e s c r i p t i o n s o f o y s t e r anatomy have been pub1 i shed ( G a l t s o f f 1964 ; Quay le 1969a).

REASON FOR INCLUSION I N SERIES

The commercial f i s h e r y f o r t h e P a c i f i c o y s t e r has grown r a p i d l y s i n c e i t s i n t r o d u c t i o n f rom Japan t o t h e wes te rn coas t o f t h e Un i t ed S t a t e s i n 1903 (Glude and Chew 1982). The Un i t ed S ta tes now consumes a lmost 60% of t h e w o r l d ' s t o t a l o y s t e r produc- t i o n . The P a c i f i c o y s t e r i s a domi- nan t s h e l l f i s h i n a g row ing Un i t ed S t a t e s aquacu l tu re i n d u s t r y a l ong t h e

P a c i f i c Coast because o f i t s l a r g e s i z e , m a r k e t a b i l i t y , and t h e ease o f p r o d u c t i o n i n s u i tab1 e areas ( G l ude and Chew 1982). Approx imate ly 60%-70% o f P a c i f i c o y s t e r p r o d u c t i o n i s marketed i n t h e P a c i f i c Coast S ta tes , b u t markets o u t s i d e t h e r e g i o n have been developed (Glude and Chew 1982). Washington S t a t e 1 eads a1 1 o t h e r P a c i f i c Coast S ta tes combined by a l a r g e marg in i n t h e p r o d u c t i o n o f P a c i f i c o y s t e r s (Chew 1983; 1984), which compr ise about 25% o f a1 1 she1 l- f i s h l and ings i n Washington S ta te .

LIFE HISTORY

The b a s i c l i f e h i s t o r i e s o f t h e P a c i f i c o y s t e r (C. g a s ) and t h e - Eas te rn o y s t e r (&. v i r g i n i c a ) a r e s i m i l a r .

Tab le 1. C h a r a c t e r i s t i c s o f t h e o y s t e r spec ies found i n B r i t i s h Columbia, Oregon, and Washi ng ton (adapted f rom Quay1 e 1969a).

Oys te rs N a t i v e o r Olympia ~ m e r i c a n o r Eas te rn P a c i f i c o r Japanese

C h a r a c t e r i s t i c (Os t rea l u r i d a ) (Crassos t rea v i r g i n i c a ) (Crassos t rea g i g a s )

Promyal chamber Lack ing Presen t Present

Adductor muscle scar :

Color Uncolored Dark p u r p l e o r brown Mauve o r w h i t e O u t l i n e C l e a r l y o u t l i n e d C l e a r l y O u t l i n e d Not c l e a r l y o u t l i n e d

Length ( i n ches ) 2 i n 3-4 i n 4-6 i n

Concen t r i c growth I n d i s t i n c t F l a t b u t c l e a r P r o j e c t i n g w i t h

f l u t i n g s

Rad ia l grooves Not apparent Ba re l y apparent General l y deep

I n s i d e s h e l l c o l o r Green i r i d e s c e n t Whi te White

Outs ide s h e l l c o l o r Gray-green w i t h Ye1 1 ow brown Gray w i t h p u r p l e

dark p u r p l e

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Reproduct ive Phys io logy

P a c i f i c oys te r s a re p ro tandrous hermaphrodi tes ( F r e t t e r and Graham 1964; Katkansky and Sparks 1966); t h e y change sex, b u t t h e i r t i m i n g i s e r r a t - i c and seasonal. The young a r e f u n c t i o n a l l y male d u r i n g t h e i r f i r s t spawning, w h i l e about h a l f remain males f o r t h e i r second spawning. The a d u l t s f u n c t i o n as separa te male o r female an imals i n any g i v e n r ep ro - d u c t i v e season, b u t a change o f sex f r om male t o female o f t e n occurs a t some p o i n t i n l i f e (Katkansky and Sparks 1966). Sexual m a t u r i t y i s reached d u r i n g t h e f i r s t year .

Spawning

P a c i f i c o y s t e r s spawn a n n u a l l y i n c e r t a i n c o a s t a l waters of B r i t i s h Columbia (Quay le 1969a) when t h e wa te r temperature i s approx imate ly 19.5-C. Once t h e spawning tempera tu re has been reached, which i s u s u a l l y sometime i n J u l y o r August, spawning i s synchronous (Quay1 e 1969a).

Under n a t u r a l cond i t i ons , s imul taneous r e l e a s e o f sperm and eggs i n t o t h e wate r column i s a t t a i n e d th rough mutual s t i m u l a t i o n ( G a l t s o f f 1964). The gametogenesis and h i s - t o l o g y o f deve lop ing ova and sperm i n C . g i g a s have been desc r i bed - (Katkansky and Sparks 1966; Quay le 1969a), as have those aspec ts i n C. v i r g i n i c a (Gal t s o f f 1964; - ~ e n n e d ~ and B a t t l e 1964).

Oysters a re h i g h l y p r o l i f i c . An average marke t -s i zed female o y s t e r (3 inches l o n g ) can produce 50-100 m i l l i o n eggs i n a s i n g l e spawning (Quay le 1969a). F e r t i l i z e d eggs o f t h e P a c i f i c o y s t e r a r e s p h e r i c a l , and 45-62 pm i n d iameter . The egg i s m u l t i l a y e r e d , w i t h membranes t h a t d i v i d e t h e j e l l y l i k e o u t e r c o a t f rom t h e smal l nuc leus ( G a l t s o f f 1964). The germina l v e s i c l e i s e c c e n t r i c a l l y l o c a t e d w i t h i n t h e nuc leo lus .

Temperature p l a y s a ma jo r r o l e i n t h e d e v e l o ~ m e n t o f t h e f e r t i l i z e d , ~

o y s t e r egg. A decrease o f 2'C ( f r om 24.5OC t o 22.5OC) doubled t h e t i m e r e q u i r e d f o r t h e f o r m a t i o n o f t h e t rochophore l a r v a e ( G a l s t o f f 1964). F e r t i 1 i z e d eggs reached t h e v e l i g e r s tage i n 72 hours a t 14'C, and i n 28 hours a t 22'C (Loosano f f and Davis 1963).

Larvae

I f p r e v a i l i n g c o n d i t i o n s a re f avo rab le , 90%-95% o f t h e f e r t i l i z e d eggs develop t o t h e s h e l l e d v e l i g e r s tage w i t h i n 48 hours. The r e s u l t i n g p e l a g i c l a r v a e a re p l a n k t o t r o p h i c , f eed ing on phy top l ank ton and growing over a p e r i o d o f 2 t o 3 weeks (Kennedy and B re i sch 1981).

As t h e l a r v a e grow, t h e i r l e n g t h con t i nues t o be 5-10 g r e a t e r t han t h e i r w i d th . T h i s c o n d i t i o n p e r s i s t s u n t i l t h e l a r v a e r each about 90 pm. A t 100 pm, t h e l e n g t h and t h e w i d t h a r e equal , b u t beyond 125 pm t h e w i d t h grows f a s t e r t han t h e leng th , f o rm ing what i s g e n e r a l l y observed as an o y s t e r l a r v a (Loosano f f 1965; Loosano f f e t a l . 1966). Complete l e n g t h and w i d t h r e l a t i o n s h i p s i n C. g!gas, as w e l l as o t h e r b i v a l v e s a r e g i v e n by Loosano f f e t a l . (1966).

Growth o f t he free-swimminq l a r - vae depends on many f a c t o r s ; t h e l e n g t h o f t he l a r v a l p e r i o d i s depen- den t on t h e wate r tempera tu re . Temper- a t u r e s must be 20°C o r g r e a t e r f o r a t l e a s t t h r e e weeks f o r near op t ima l g rowth (Magoon and V i n i n g 1981). A l though l a r v a e can s u r v i v e s l i g h t l y lower water temperatures, t h i s p ro - 1 ongs t h e i r development and i nc reases t h e i r exposure t o p e l a g i c p r e d a t o r s (Kennedy and B re i sch 1981).

D e t a i l e d d e s c r i p t i o n s o f t h e ana- t o m i c a l development o f C. v i r g i n i c a l a r v a e f r om f i r s t c leavage t o s e t t i n g a r e p rov i ded by G a l t s o f f (1964) . Pho- tog raphs o f C. gi-gas l a r v a l develop- ment a t va r i ous s i z e s i s presented by

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Loosano f f e t a1 . (1966). A d d i t i o n a l i n f o r m a t i o n concern ing t h e e f f e c t s o f temperature, s a l i n i t y , and t u r b i d i t y on eggs and l a r v a e i s presented i n Loosano f f ( 1965).

The p r imary de te rminan t o f d i s - t r i b u t i o n o f a p e l a g i c p lankton, ic spec ies t h a t e v e n t u a l l y s e t t l e s on t h e bot tom i s t h e p r e v a l e n t wa te r c u r r e n t s d u r i n g t h e c r i t i c a l f ree-swimming s tages o f t h e l a r v a (West ley 1968; Quay le 1969a). D i s p e r s a l can be q u i t e broad, b u t o n l y areas w i t h s u i t a b l e h a b i t a t s u s t a i n p o p u l a t i o n s o f oy- s t e r s . When t h e o y s t e r l a r v a e r each a l e n g t h o f about 0.30 mm, t h e i r f r e e swimming e x i s t e n c e ends and they a t t a c h t o t h e bo t tom o r a hard s u b s t r a t e as spa t (Quay le 1969a)

An eyespot develops when t h e l a r - va s h e l l l e n g t h reaches 250-175 pm. T h i s "eye" remains th roughou t t h e free-swimming stage, and may serve as a defense mechanism (Loosano f f 1965). Develop ing i n c o n j u n c t i o n w i t h t h e eyespot i s a f o o t c o n t a i n i n g a byssa l g l and (Loosano f f 1965). T h i s f o o t i s extended when t h e l a r v a i s ready t o se t . The f o o t w i l l a t t a c h t o any s o l i d s u r f a c e w i t h which i t comes i n t o con tac t . When c o n t a c t i s made, t h e l a r v a c raw l s on to t h e su r f ace and, i f i t i s s u i t a b l e , a t t aches by t h e l e f t va l ve (Kennedy and B re i sch 1981). A t t h i s p o i n t , o y s t e r s a r e no longer free-swimming and a r e c a l l e d spat. L u t z e t a l . (1970) found t h a t t h e l a r v a e can be s t i m u l a t e d t o s e t by temperature man ipu la t ion . 0 t h e r f a c t o r s c r i t i c a l t o s e t t i n g i n c l u d e t h e presence o f oys te r s h e l l s o r o t h e r s u i t a b l e s u b s t r a t e (C r i ps 1967), s u f f i c i e n t 1 i g h t ( R i t c h i e and Menzel 1969), and sur face i r r e g u l a r i t i e s on t h e s u b s t r a t e (Gal t s o f f 1964). The presence o f a water-borne "g rega r i ous f a c t o r , " a substance r e l eased by newly s e t C. v i r i n i c a spa t t h a t appa ren t l y + a t t r a c t s o e r spat , was demonstrated by H idu e t a l . 1978.

T h i s metamorphosis f rom f r e e - swimming l a r v a e t o s p a t i s accompanied

by some marked morpho log ica l changes, such as t h e disappearance o f t h e velum and f o o t as w e l l as t h e a n t e r i o r adduc to r muscle, and t he development o f an en l a rged s e t o f g i l l s (Loosano f f 1965; Quay le 1969a). A f t e r s e t t i n g , t h e j u v e n i l e o y s t e r i s a s e s s i l e animal, which w i l l grow t o a d u l t s i z e and d i e i n t h e a rea o f s e t t i n g , unable t o v o l u n t a r i l y move around. Kennedy and B re i sch (1981) p r o v i d e a d e t a i l e d d e s c r i p t i o n o f t h e p reda to r s o f j uve- n i l e oys te rs . Loosanof f (1965) de- t a i l s t h e va r i ous d iseases common t o j u v e n i l e oys te rs .

Adu l t s

There a re c o n t r a s t i n g r e p o r t s concern ing t h e e f f ec t o f p o p u l a t i o n d e n s i t i e s on o y s t e r growth. S tud ies o f 0 . e d u l i s have found s h e l l growth i s r n a m d by c o n t a c t w i t h ad j acen t oys te r s , bu t t h e volume o f meat i s reduced (Cole and Waugh 1959; Sheldon 1968), which may be due t o c o m p e t i t i o n o r some o t h e r v a r i a b l e . The problem o f t o o many o y s t e r s and t o o l i t t l e food i s a major l i m i t i n g f a c t o r i n any h i gh-densi t y area.

The mechanical process o f f i l t e r feeding i n a d u l t o y s t e r s i s w e l l documented (Nelson 1938; Ko r r i nga 1952; Menzel 1955; Owen 1974). D u r i n g feeding, va r i ous p a r t i c l e s a r e s o r t e d accord ing t o s i z e by mucous secre- t i o n s . Bernard (1974) found t h a t t h e amount o f mucus secre ted depends on t h e degree o f mucous g l a n d s t i m u l a t i o n by f o r e i g n p a r t i c l e s . Larger p a r t i c l e s evoke copious mucous s e c r e t i o n , w h i l e sma l l p a r t i c l e s evoke less. Th i s s o r t i n g o f food p a r t i c l e s takes p lace on t h e c i l i a t e d l a b i a l p a l p s (Kennedy and B re i sch 1981). The anatomy and phys io logy o f t h e pa lps, which a re a c t i v e l y i n v o l v e d i n t h e feed ing process was descr ibed i n d e t a i l (Yonge 1960; G a l t s o f f 1964). The h i s t o l o g i c a l anatomy o f t h e e n t i r e d i g e s t i v e t r a c t has been desc r i bed i n C. v i r g i n i c a by Shaw and B a t t l e - ( 1957).

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GROWTH CHARACTERISTICS l o n g as 40 years, w i t h l onge r l i f e a t t a i n e d a t t h e more n o r t h e r n l a t i t u d e s .

L a r v a l growth seems t o be d i r e c t l y r e l a t e d t o water temperature w i t h f a s t e r growth a t h i ghe r temperatures (Quay le 1969a). I n t h e temperature range 64OF t o 75OF, l a r v a e o f t h e P a c i f i c o y s t e r i n B r i t i s h Columbia w i l l grow f rom 75 pm i n l e n g t h t o about 300 pm d u r i n g t h e p e r i o d from mid -Ju ly t o mid-August (Quayle 1969a). Loosanof f e t a l . (1966) showed t h a t t h e shapes and t h e r e f o r e t h e r e l a t i o n s h i p of w i d t h t o l e n g t h of l a r v a e v a r i e s a t d i f f e r e n t growth stages. Langton and McKay (1974, 1976) d iscussed t h e e f f e c t s o f f eed ing v a r i a t i o n s on t h e g rowth of - C. j i g a s spa t .

Oyster s i z e i n Washington S t a t e a f t e r 2 years of growth i s d i r e c t l y r e l a t e d t o t h e i n i t i a l p l a n t i n g s i z e and t h e month p l an ted , w i t h e a r l i e r p l a n t i n g (about A p r i 1 ) p roduc ing t h e l a r g e s t oys te r s (Scholz and Westley 1971a, 1971b). Growth o f t r a y - r e a r e d seed o y s t e r s (seed o y s t e r s a r e a l r eady s e t b u t sma l l ) and ground-reared seed oys te r s was t h e same i n Washington, a l though t r a y - r e a r e d seed o y s t e r s had t w i c e t h e s u r v i v a l r a t e (Scholz 1973). I n Alaska, m o r t a l i t y was 3% i n r a f t - grown o y s t e r s p a t conpared t o 63% mor- t a l i t y i n nearby bo t tom-p lan ted spa t (Yancey 1966). Crowded spa t grow more s l o w l y d u r i n g t h e i r i n i t i a l 6 months a f t e r p l a n t i n g (Scho lz 1974).

Seed oys te r s shou ld reach a l e n g t h o f 4 t o 5 cm d u r i n g t h e i r f i r s t year . Oysters g e n e r a l l y grow more r a p i d l y when they a re young w i t h a r e d u c t i o n i n g rowth r a t e when t h e y a r e 4 o r 5 years o f age (Quay le 1969a).

Growth i n o y s t e r s v a r i e s w i d e l y w i t h t i d a l he i gh t , growing area, and env i ronmenta l c o n d i t i o n s . Oyster g rowth can be measured by inc reases i n s h e l l s i z e o r body s i ze . As a genera l r u l e , growth i s f a s t e r as water tem- p e r a t u r e inc reases (Loosanof f 1965). Oys te rs have been known t o l i v e as

S h e l l d e p o s i t i o n i s c o n t r o l l e d by t h e a c t i v i t y o f t h e mant le su r f ace ( G a l t s o f f 1964; Quay le 1969a). She1 1 growth occurs ma in ly i n summer when e l eva ted water temperatures r e s u l t i n inc reased food supply and inc reased metabol ism, u s i n g t h e a v a i l a b l e ca l c i um f o r shel 1 d e p o s i t i o n (Quay le 1969a). S t a r t i n g i n t h e f a l l , as wa te r temperatures decrease, growth drops g r e a t l y , w i t h o n l y m i no r she l 1 growth o c c u r r i n g d u r i n g t h e w i n t e r (Sparks and Chew 1961).

Oysters e x h i b i t compensatory growth, growing wider when l eng thw i se g rowth i s p h y s i c a l l y r e t a rded , o r v i c e versa. Therefore, s h e l l s i z e as an i n d i c a t o r o f growth i s g i ven as t h e p roduc t o f l e n g t h and w i d t h (Katkansky e t a l . 1967). Oys te r growth can appear t o be a f f e c t e d by hand l ing , due t o t h e l o s s o f f r a g i l e ex tens ions o f new s h e l l growth (Sparks and Chew 1961), b u t t h i s does n o t seem t o a f f e c t o y s t e r s u r v i v a l . Foul i ng organisms assoc i a t ed w i t h o y s t e r s sometimes have a s i g n i f i c a n t l y nega- t i v e e f f e c t on growth, even caus ing i t t o cease (Michael and Chew 1976).

The shape o f t h e o y s t e r depends g r e a t l y on t h e t ype o f su r f ace upon which i t i s grown. I f i t i s a t t ached t o a s o l i d ob j ec t , t he l e f t , o r l ower va lve f o l l o w s t h e con tour o f t h a t o b j e c t (Quay le 1969a). Oysters grow l o n g and narrow on s o f t mud o r i n c l u s t e r s , and a r e round and deep ly cupped, w i t h ex tens i ve f 1 u t i ng o f t h e s h e l l , when grown on a ha rd su r face , such as g rave l (Quay le 1969a).

Weighing an o y s t e r by f i n d i n g t h e we igh t o f t h e wa te r i t d i sp l aces e s s e n t i a l l y p rov i des t h e we igh t o f t h e s h e l l s i nce t h e s p e c i f i c g r a v i t y o f o y s t e r meat i s v e r y near t o t h a t o f water . A t i m e s e r i e s o f such measurements p rov i des a r e c o r d o f shel 1 growth (Quay le 1969a).

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The bas i c measure o f o y s t e r p r o d u c t i v i t y i s volume (Quay le 1969a). The r a t i o o f whole volume t o s h e l l volume i n d i c a t e s t h e volume o f meat an oys te r can produce f o r i t s s i ze . The l e n g t h t o volume r a t i o w i l l change i n P a c i f i c oys te rs depending upon t h e age o f t h e animals (F igure 3). These volume r e l a t i o n s h i p s have impor tan t i m p l i c a t i o n s t o oys te r growers.

The market va lue o f o y s t e r meat depends on a h i gh c o n d i t i o n index, which i s def ined as the amount o f s t o red glycogen, 1 i p id , and germinal t i s s u e of an o y s t e r i n p r o p o r t i o n t o i t s i n t e r n a l s h e l l volume (Kennedy and Bre isch 1981). Westley (1964) found t h a t a bushel o f C. g i gas i n pr ime c o n d i t i o n y i e l d e d - one g a l l o n o f shucked meats, whereas a bushel o f oys te rs i n poor c o n d i t i o n y i e l d e d o n l y h a l f a ga l lon . The c o n d i t i o n index o f an oys te r depends on i t s feed ing behavior , t h e n u t r i t i o n a l va lue of i t s food, and i t s r ep roduc t i ve s t a t e (Kor r inga 1952). Oysters t h a t a r e ready t o spawn, o r t h a t f a i l t o spawn because o f low water temperatures a r e n o t considered t o be o f good market-

F i gu re 3. Length and volume increases o f P a c i f i c oys te rs f o l l owed over 4 consecut ive years i n B r i t i s h Columbia ( a f t e r Quayle 1969a, P a c i f i c Oyster Cu l t u re fi B r i t i s h Columbia, F i s h e r i e s Research Board o f Canada, w i t h per- m iss ion o f t h e Department o f F i s h e r i e s and Oceans).

a b l e q u a l i t y (Quayle 1969a), even though they may have a h igh c o n d i t i o n index.

THE FISHERY

Economic S ta tus

The Un i t ed S ta tes i s t h e l a r g e s t o y s t e r producing and consuming n a t i o n i n the world. The Un i ted States annua l l y produces 50 m i l l i o n pounds of o y s t e r meats and impor ts over 20 m i 11 i on pounds, thereby consuming ap- p rox imate ly 56% o f the w o r l d ' s t o t a l annual p roduc t i on (Glude and Chew 1982).

Washington S t a t e i s t he l a r g e s t producer o f o y s t e r s on t he P a c i f i c Coast (Chew 1983, 1984). The Washing- t on S ta te p roduc t i on o f approx imate ly 5 m i l l i o n pounds o f o y s t e r meat i s about 5 t imes g r e a t e r t han t h e com- b ined p roduc t i on o f B r i t i s h Columbia, Oregon, and C a l i f o r n i a (F igu re 4). The annual oys te r harves t i n Washing- t o n S ta te amounts t o 33% o f t h e t o t a l s h e l l f i s h weight harves ted and 26% o f t he landed d o l l a r va lue a t $3.8 m i l - l i o n o u t o f $14.6 m i l l i o n i n 1982 (Washington S t a t e Department o f F i s h e r i e s 1983). Th is comprises t he l a r g e s t l and ing percentage and d o l l a r va lue f o r any commercial s h e l l f i s h species harvested i n Washington S t a t e (F igure 5 ) . Peak oys te r p roduc t i on on t h e P a c i f i c Coast was from 1954-56, when harves ts exceeded 10 m i l l i o n pounds o f meats (Glude and Chew 1982). Since 1965, annual p r o d u c t i o n has been 4 t o 7 m i l l i o n pounds o f meats i n t h e coas ta l s t a t e s o f Washington, Oregon, and C a l i f o r n i a . The decrease i n p roduc t i on a f t e r 1956 i s a t t r i b u t a b l e t o the i m p o r t a t i o n o f lower p r i c e d canned oys te rs f rom Japan and Korea (Glude and Chew 1982). Improper seeding o f oys te r beds and increased p o l l u t i o n have caused decreases i n some areas. L i m i t e d s h e l f l i f e and market ing problems r e s t r i c t t h e market f o r r e f r i g e r a t e d f r e s h o y s t e r meats (Magoon and V in ing 1981).

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--- California -Washington ------- Oregon - British Columbia

Year

Figure 4 . Commercial p roduct ion o f oys ters i n C a l i f o r n i a , Oregon, Washington and B r i t i s h Columbia ( a f t e r Chew 1983).

OTHER SHELLFISH ($0.3 MILLION)

OYSTERS

($3.2 MILLION)

Figure 5. Oysters made up 26% o f t he $14.6 m i l l i o n t o t a l landed value o f a l l Washington Sta te she1 1 f i s h i n 1982 (modif ied from Washington Sta te Department o f F i she r ies 1983).

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A p p r o x i m a t e l y 60%-70% o f C. 9i igas p r o d u c t i o n i s marketed i n t h e - ~ a c i f i c Coast s t a t e s . N e a r l y a1 1 t h e P a c i f i c Coast p r o d u c t i o n o f o y s t e r s i s shucked and s o l d a s f r e s h o r f r o z e n p r o d u c t . On ly 5%-10% i s s o l d i n t h e s h e l l f o r s h u c k i n g by t h e consumer f o r t h e h a l f - s h e l l t r a d e . T h i s demand i s e s p e c i a l l y h i g h f o r o y s t e r s grown o f f t h e b o t t o m o r on h a r d s u b s t r a t e s , s i n c e t h e s e have a r e p o r t e d l y m i l d e r f l a v o r t h a n o y s t e r s r a i s e d on muddy s u b s t r a t e s (Glude and Chew 1982) . T h i s t y p e o f o y s t e r commands a premium p r i c e .

Farming

There i s p o t e n t i a l f o r r e s t o r i n g West Coast o y s t e r p r o d u c t i o n t o 10 m i l l i o n pounds by a p p l y i n g p r e s e n t b o t t o m c u l t u r e t e c h n i q u e s i n under - u t i l i z e d a r e a s (Glude and Chew 1982) . The re i s a c o n s i d e r a b l e amount o f un- d e r u t i l i z e d a r e a a v a i l a b l e ( T a b l e 2 ) . W i t h i n c r e a s e d consumer demand, t h e a v a i l a b i l i t y o f adequate o y s t e r seed, and t h e a p p l i c a t i o n o f o f f - b o t t o m c u l t u r e t e c h n i q u e s , f u t u r e p r o d u c t i o n o f P a c i f i c o y s t e r s c o u l d exceed 20 m i l l i o n pounds o f meats p e r y e a r (Glude and Chew 1982).

The P a c i f i c Nor thwes t wa te rs a r e g e n e r a l l y t o o c o o l f o r C . i as a d u l t s t o spawn s u c c e s s f u l ly -or% t h e i r

Tab le 2. T i d e l a n d s i n a c r e s u s a b l e f o r o y s t e r c u l t u r e i n Washington, Oregon and C a l i f o r n i a .

T o t a l a r e a S t a t e T o t a l Area i n p r o d u c t i o n

Wash i n g t o n 42,000 16,000 Oregon 4,000 1,350 C a l i f o r n i a 17,150 2,120

TOTAL 63,150 19,470

l a r v a e t o s e t t l e i n q u a n t i t i e s app re - c i a b l e f o r commerc ia l u s e ( K o r r i n g a 1976) . E x c e p t i o n s t o t h i s a r e Dabob Bay and Q u i l c e n e Bay i n Washington, where y e a r l y s p a t f a l l ave rages about 25 p e r s h e l l o f c u l t c h , w h i l e i n P e n d r e l l Sound i n B r i t i s h Columbia, commercial s e t s o f o v e r 1,000 s p a t p e r s h e l l a r e n o t uncommon ( K o r r i n g a 1976; Chew, pers. comm.). B o t h a r e a s a r e r e l a t i v e l y p r o t e c t e d ; summer w a t e r t empera tu res r e g u l a r l y exceed 20'C and where h y d r o g r a p h i c f e a t u r e s f a c i l i t a t e o y s t e r l a r v a l r e t e n t i o n ( Q u a y l e 1969a; K o r r i n g a 1976). H y d r o g r a p h i c c o n d i t i o n s o c c a s i o n a l l y a l l o w commerc ia l c o l l e c t i o n o f n a t u r - a l l y produced o y s t e r s p a t i n W i l l a p a Bay, Washington, o r i n Ladysmi t h Harbour , B r i t i s h Columbia, b u t i n most y e a r s t h e spa t do n o t s e t t l e i n commerc ia l q u a n t i t i e s ( Q u a y l e 1969a; K o r r i n g a 1976) . Comnerc ia l s e t s may o c c u r i r r e g u l a r l y i n abou t 6 o u t o f 10 y e a r s i n W i l l a p a Bay w i t h 10 s p a t p e r s h e l l c o n s i d e r e d a good s e t (Chew, pe rs . comm.). P a c i f i c o y s t e r s a r e c u l t u r e d t o t h e s p a t s tage and t r a n s p l a n t e d t o many a r e a s shown i n F i g u r e 2 f o r r e a r i n g t o a d u l t s i z e and subsequent h a r v e s t .

I n warmer summers, t h e s e n a t u r a l sou rces s u p p l y as much as t w o - t h i r d s o f t h e seed needed f o r t h e P a c i f i c Nor thwes t o y s t e r a q u a c u l t u r e i n d u s t r y (Washington S t a t e Depar tment o f F i s h e r i e s 1983) . U n t i l about 1982, o y s t e r seed was i m p o r t e d f r o m Japan, wh ich h i s t o r i c a l l y p r o v i d e d t h e b u l k o f t h e i n d u s t r i a l seed demanded (G lude and Chew 1982). Today, commerc ia l h a t c h e r i e s a l o n g t h e P a c i f i c Coast a r e s u c c e s s f u l l y p r o d u c i n g o y s t e r seed a t compe t i t i v e p r i c e s (Glude and Chew 1982) . One h a t c h e r y t e c h n i q u e i n - v o l v e s s h i p p i n g eyed o y s t e r l a r v a e t o g rowers (Breese 1979; Chew 1983) . The l a r v a e a r e a l l o w e d t o s e t and f o r m s p a t o n t h e g r o w e r ' s c u l t c h .

Oys te r seed, a t t a c h e d t o c u l t c h ( u s u a l l y shucked o y s t e r s h e l l s ) , i s g e n e r a l l y " i m p l a n t e d " d i r e c t l y o n t o g r o w i n g beds, o r sometimes o n t o g r a v e l

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nursery beds f o r t h e f i r s t yea r o r two (Glude and Chew 1982). Much o f t h e P a c i f i c o y s t e r c u l t u r e i n Washington ana B r i t i s h Columbia i s done on i n - t e r t i d a l beds w i t h g rave l , sand, o r mud bottoms. A t r e l a t i v e l y h i g h t i d e s , l e s s s i l t a t i o n and fewer preda- t o r s a l l o w b e t t e r o y s t e r seed s u r v i v a l (Quay le 1969a), w i t h s u r v i v a l improved f rom 22% a t t he zero t i d a l l e v e l t o 61% a t a p o i n t 6 ft above zero t i d a l l e v e l .

Dur ing t h e growing per iod , c l u s - t e r s o f o y s t e r s need t o be broken up, separated, and t h i nned . Oys te rs a r e o f t e n t r a n s f e r r e d a f t e r 1 o r 2 years t o b e t t e r growing beds t o improve t h e i r c o n d i t i o n (Ko r r i nga 1976). Best growth was r epo r t ed a t t h e zero t i d e l e v e l , w h i l e f a t t e n i n g was g r e a t e s t a t t he 3- t o 4 - f t mark (Quay le 1969a). The s e l e c t i o n o f ground s u i t a b l e f o r o y s t e r c u l t u r e i s based ma in ly on t h r e e f a c t o r s : t i d a l l e v e l , bot tom cons is tency , and pro- t e c t i o n f r a n wave a c t i o n (Quay le 1969a).

Growth t o market s i z e v a r i e s w i t h l a t i t u d e , r ang ing f rom l e s s t han 2 years i n C a l i f o r n i a , t o 2 t o 4 yea rs i n Oregon and sou thern Washington, and 4 t o 6 yea rs i n n o r t h e r n Washington, B r i t i s h Columbia and Alaska (Glude and Chew 1982). Oysters a re harves ted e i t h e r by hand a t l ow t i d e o r by v a r i - ous dredges a t h i g h t i d e (Glude and Chew 1982). Bottom c u l t u r e i s used by most Washington commercial o y s t e r growers because i t i s most economical and r e q u i r e s a minimum o f l a b o r (Magoon and V i n i n g 1981).

Stake c u l t u r e techn iques a re used t o grow C. g i g a s on t h e i n t e r t i d a l beds a t C ~ O S Bay, Oregon, and Tomales Bay, C a l i f o r n i a , where t h e bot tom sediments a re g e n e r a l l y t o o s o f t f o r c u l t u r e . Wooden s takes 4 t o 5 f t l o n g a r e pushed i n t o t h e s u b s t r a t e a t 3 f t i n t e r v a l s , and severa l l a r g e o y s t e r s h e l l s w i t h spa t a r e a t t ached t o them (Glude and Chew 1982; Magoon and V i n i n g 1981). The a d d i t i o n a l

l a b o r c o s t o f s take c u l t u r e i s o f f s e t by t h e acce le ra ted growth and e x c e l l e n t q u a l i t y o f t h e o y s t e r s (Glude and Chew 19821.

I n Tomales and Drakes Bay, i n C a l i f o r n i a , o y s t e r s h e l l s w i t h a t - tached spa t a re suspended from l o n g fences o r r acks 4-5 f t h igh , l o c a t e d i n t h e lower p a r t o f t h e i n t e r t i d a l zone. T h i s method no t o n l y inc reases t h e i r growth r a t e , bu t a l s o p r o t e c t s them f rom ~ r e d a t o r v b a t ravs. Ho lo rh i nus c a i i f o r n i c i s (Glude i n d Chew 1982).

Off-bottom o y s t e r c u l t u r e , u s i n g r a f t s , racks, o r s takes, has been t r i e d i n va r i ous l o c a t i o n s a l ong t h e P a c i f i c Coast. R a f t c u l t u r e i s used a t Yaquina Bay, Oregon, because s u i t - a b l e i n t e r t i d a l beds a r e l a c k i n g and p r o t e c t e d e s t u a r i n e wate rs a r e ava i 1 - a b l e (Glude and Chew 1982).

Cu l t ch , w i t h o y s t e r spa t a t - tached, a r e s t r u n g on rope o r w i r e and suspended f rom l o g r a f t s (Magoon and V i n i n g 1981). Th i s method o f o y s t e r c u l t u r e has t h r e e advantages over beach c u l t u r e . F i r s t , growth t o mar- k e t a b l e s i z e i s reduced by l t o a lmos t 2 years (Quay le 1969a), perhaps be- cause o y s t e r s a re immersed con t i n u - ous l y and t hus have more o p p o r t u n i t y t o feed (Pereyra 1961; Magoon and V i n i n g 1981). Second, a t a l l t i m e s o f t h e year, o y s t e r s grown by r a f t c u l t u r e a r e f a t t e r t h a n t h o s e grown on beaches o n l y a few hundred yards away (Quay le 1969a). Th i r d , m o r t a l i t y caused by s i l t a t i o n o r p r e d a t i o n doe'$ n o t occur (Quay le 1969a).

Quay l e (197 1) recommended o n l y one growing season by r a f t c u l t u r e , c l a i m i n g r e l a t i v e l y l i t t l e a d d i t i o n a l growth i n t h e second year, w i t h s i g n i f i c a n t f o u l i n g . We l l e r (1978) found good p o t e n t i a l f o r commercial r a f t c u l t u r e o f P a c i f i c o y s t e r s near Squaxin I s l a n d i n sou thern Puget Sound and r e p o r t e d a s i g n i f i c a n t i n - c rease i n p r o d u c t i o n d u r i n g t h e second year o f growth.

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A t t h i s t i m e , o f f - b o t t o m c u l t u r e s accoun t f o r a r e l a t i v e l y s m a l l p r o - p o r t i o n o f West Coast o y s t e r p roduc - t i o n due t o a low p r o f i t marg in asso- c i a t e d w i t h h i g h c o s t s o f p r o d u c t i o n (G lude and Chew 1982). I n t h e f u t u r e , t h e s e methods may have g r e a t e r p romise , when s u i t a b l e i n t e r t i d a l beds a r e f u l l y u t i l i z e d and t h e p r i c e and demand f o r P a c i f i c o y s t e r s i n c r e a s e .

ECOLOGICAL ROLE

Feed ing Behav io r

O y s t e r s f e e d on p l a n k t o n i c o r - ganisms wh ich a r e f i l t e r e d by t h e g i l l s , en t rapped, and bound i n mucus. S t r i n g s o f mucus t h e n c a r r y t h e p a r t i c u l a t e m a t t e r t o t h e l a b i a l p a l p s , where i t i s s o r t e d and e i t h e r passed i n t o t h e mouth o r r e j e c t e d as pseudofeces ( K o r r i n g a 1976; Kennedy and B r e i s h 1981) . Pseudofeces a r e f i l t e r e d m a t e r i a l s wh ich have n o t been passed t h r o u g h t h e d i g e s t i v e system. Food i s c a r r i e d by t h e mucous s t r i n g s t o t h e a l i m e n t a r y c a n a l , and s o r t e d a g a i n by t h e caecum (Menzel 1955). O y s t e r s use an o r g a n u n i q u e t o b i - v a l v e s and g a s t r o p o d s c a l l e d a c r y s t a l l i n e s t y l e t o a s s i s t i n t h e d i g e s t i o n p r o c e s s ( G a l t s o f f 1964; Q u a y l e 1969a).

Some o y s t e r s c a n f i l t e r p a r t i c l e s s m a l l e r t h a n 2 pm, b u t r e t e n t i o n e f f i - c i e n c y i n c r e a s e s w i t h l a r q e r p a r t i c l e s 3-10 pm (Kusuk i 1977a, 1977b). O y s t e r s seem t o d i f f e r e n t i a l l y s e l e c t p a r t i c l e s t o consume o r r e j e c t , s i n c e stomach c o n t e n t s do n o t f u l l y r e p r e - s e n t t h e p h y t o p l a n k t o n c o m p o s i t i o n t o w h i c h o y s t e r s a r e exposed (Grave 1916; Morse 1944) .

O y s t e r s i n g e s t b a c t e r i a , p r o t o - zoa, a w ide v a r i e t y of p h y t o p l a n k t o n , l a r v a l f o rms o f o t h e r i n v e r t e b r a t e an ima ls , i n a n i m a t e o r g a n i c m a t e r i a l c a l l e d d e t r i t u s , and some i n o r g a n i c m a t e r i a l (Quay l e 1969a). L i t t l e i s known o f wha t p o r t i o n o f t h e v a r i o u s i n g e s t e d i t ems !s a c t u a l l y u s a b l e

food , o r o f wha t n u t r i t i o n a l v a l u e t h e y a r e t o o y s t e r s . Some o y s t e r g rowers a s s o c i a t e s p r i n g f a t t e n i n g o f o y s t e r s w i t h t h e u s u a l s p r i n g b loom o f d ia toms , caused b y an i d e a l c o m b i n a t i o n o f l i g h t , t e m p e r a t u r e , and n u t r i e n t s (Quay le 1969a).

I t i s s t i l l u n c l e a r whe the r o y s t e r s f e e d and d i g e s t f o o d con- t i n u o u s l y o r i n d a i l y p a t t e r n s . M o r t o n (1977) p o s t u l a t e d t h a t i n t e r - t i d a l p o p u l a t i o n s o f C. g i g a s f e e d d i s c o n t i n u o u s l y , c o r r e s p o n d i n g t o t i d - a l c y c l e s . O y s t e r s c u l t u r e d by o f f - b o t t o m t e c h n i q u e s show i n c r e a s e d growth, pe rhaps as a r e s u l t o f con- t i n u o u s f e e d i n g ( P e r e y r a 1961, Q u a y l e 1969a). However, Lang ton and McKay (1974) r e p o r t e d c o n s i s t e n t l y h i g h e r g r o w t h i n s p a t s u b j e c t e d t o a d i s c o n - t i n u o u s f e e d i n g reg ime. Feed ing i s c l o s e l y t i e d t o t h e r a t e o f w a t e r t r a n s p o r t t h r o u g h an o y s t e r , wh ich i n t u r n i s a f f e c t e d by such e n v i r o n m e n t a l c o n d i t i o n s as w a t e r s a l i n i t y , wa te r t empera tu re , w a t e r c i r c u l a t i o n , p o l l u - t i o n , and suspended s i l t and by b i o l o - g i c a l c o n d i t i o n s such as c o m p e t i t i o n and f o o d c o n c e n t r a t i o n ( Q u a y l e 1969a).

Loosano f f and E n g l e (1947) f o u n d t h a t when a l g a l c o n c e n t r a t i o n s were h i g h , pumping r a t e s decreased and o y s t e r s o f t e n became s l u g g i s h i n r e - sponse t o s t i m u l i . They h y p o t h e s i z e d t h a t t h i s l a b o r a t o r y o b s e r v a t i o n was caused e i t h e r by t o x i c m e t a b o l i t e s e x c r e t e d f r o m dense a l g a l concen- t r a t i o n s o r by t h e h i g h l y c o n c e n t r a t e d l e v e l o f n u t r i e n t s used t o c u l t u r e t h e a lgae . B a c t e r i a l p o p u l a t i o n s can be a s s o c i a t e d w i t h l a r g e numbers o f a l g a l c u l t u r e s , and t o g e t h e r w i t h h i g h tem- p e r a t u r e s may cause o y s t e r m o r t a l i t y ( L i p o v s k y and Chew 1973, 1974) .

F i e l d s t u d i e s i n Washington showed a r e a s w i t h u n s t r a t i f i e d w a t e r s h a v i n g modera te t o r a p i d volume ex - change, s u s t a i n e d p h y t o p l a n k t o n p r o - d u c t i o n , and h i g h l e v e l s o f n i t r a t e and phosphate n u t r i e n t s produced o y s t e r s i n good c o n d i t i o n (West ley 1968) . Under l a b o r a t o r y c o n d i t i o n s ,

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l a r v a l s e t t i n g o f P a c i f i c o y s t e r s was reduced by poor n u t r i t i o n and a l g a l concen t ra t i ons o f l e s s t han 5,000 c e l l s l m l (Lund 1971). Optima1 l a b - o r a t o r y growth r a t e f o r o y s t e r l a r vae occur red a t an a l g a l i n f l o w d e n s i t y of 20,000 c e l l s l m l (Malouf 1971). The r a t e of food consumption inc reased as a l g a l d e n s i t i e s decreased o r as water temperatures increased from 10 t o 24°C. Grea te r f eed ing r a t e s do n o t necessar i l y correspond t o p r o p o r t i o n - a t e l y g r e a t e r l a r v a l growth, f o r some food was incomple te ly ass imi l a t e d o r r e j e c t e d as pseudofeces (Malouf and Breese 1977).

Summer M o r t a l i t y

Throughout t h e l a t e 1960's and 1970's mass m o r t a l i t i e s i n P a c i f i c o y s t e r s o f up t o 65% have occur red d u r i n g warmer t han usua l summers i n Washington, C a l i f o r n i a , and a t Boundry Bay i n B r i t i s h Columbia (Quay le 1969a; B e a t t i e 1978; B e a t t i e e t a l . 1980). M o r t a l i t i e s have genera l l y occur red du r i ng l a t e summer when water temperatures approached o r exceeded 20°C among o y s t e r s tocks t h a t were 2 years o r o l de r , had r e l a t i v e l y h i gh c o n d i t i o n i nd i ces , and were l o c a t e d i n areas o f h i gh n u t r i e n t l e v e l s (Perdue e t a l . 1981). Glude (1975) no ted t h a t t h i s c o n d i t i o n i n t h e o y s t e r s was ac- companied by degenerat ive n e c r o s i s of t h e d i g e s t i v e d i v e r t i c u l u m . The l a r g - e s t oys te rs , e x h i b i t i n g heavy gonadal development, comprised t h e g r e a t e s t p r o p o r t i o n o f t h e m o r t a l i t i e s (Glude 1975). Al though m o r t a l i t y seemed se- l e c t i v e a g a i n s t females, male o y s t e r s d i e d a l s o (Perdue e t a l . 1981). How- ever, Glude (1975) d i d n o t observe t h i s sex d i f f e r e n c e .

L ipovsky and Chew (1972) simu- l a t e d sgmmer m o r t a l i t y i n t he l abo ra - t o r y and suggested t h a t a V i b r i o bac te r ium was invo lved . A l though t h e cause of mass o y s t e r m o r t a l i t y has n o t been p o s i t i v e l y i d e n t i f i e d , V i b r i o were i m p l i c a t e d as f a c u l t a t i v e patho- gens (Grischkowsky and L i s t o n 1974; L i p p e t a l . 1975). Brown (1977) found

t h a t on l y a sma l l number o f V i b r i o s t r a i n s a re v i r u l e n t , and t h e a b i l i t y o f b a c t e r i a t o cause d i sease depends g r e a t l y on t h e i r a b i l i t y t o pass t h e o y s t e r ' s defense mechanisms i n l a r g e numbers. He found V i b r i o an u i l l a r u m t o be the o r g a n i s m m o s t i s o l a t e d f rom o y s t e r s t h a t d i e d i n t h e l a b o r a t o r y .

Environmental pressures, such as l o n g pe r i ods o f exposure t o a i r , warm temperatures, o r d i n o f l a g e l l a t e blooms, may t r i g g e r m o r t a l i t y i n oys te r s a l r eady i n a s t r essed s t a t e ( B e a t t i e 1978). B e a t t i e e t a l . (1978) found good p o t e n t i a l f o r development o f a s t r a i n o f oys te r s r e s i s t a n t t o 1 abo ra to r y - i nduced summer mor ta l i t y . Expe r imen ta l l y se lec ted , g e n e t i c a l l y r e s i s t a n t oys te r s were p l a n t e d i n Rocky Bay, Washington, and subse- q u e n t l y exper ienced summer m o r t a l i t y i n 1978 t h a t was lower than f o r t h e c o n t r o l o y s t e r s ( B e a t t i e e t a l . 1980). V a r i a b i 1 i ty i n t h e carbohydrate c y c l e and gonadal development o f s e l e c t i v e l y b red o y s t e r s i n d i c a t e d a p o s s i b l e gene t i c component t o o y s t e r response t o env i ronmenta l cues (Purdue e t a l . 1981).

Predators

Crabs and s t a r f i s h can be s e r i o u s p reda to r s on young and a d u l t P a c i f i c o y s t e r s i n Oregon, Washington, and B r i t i s h Columbia (Quay le 1969a). I n Puget Sound and t h e S t r a i t o f Georgia, o y s t e r seed stocks a l s o can be s i g - n i f i c a n t l y reduced by t he i n a d v e r t - e n t l y impor ted Japanese o y s t e r d r i l l Ocinebra j apon i ca and by t h e preda- t o r y f 1 atworm Pseudostyl ochus os t r e o - phagus (Quay le 1969a; B e a t t i e 1982).

The Dungeness c rab Cancer ma i s t e r , t he rock c rab C. roductus, d3-F t e g race fu l c rab T. + g r a c l IS,

c h i p and open young oys te r s and o y s t e r seed w i t h t h e i r c laws (Quay le 1969a). Genera l ly , c rab p r e d a t i o n i s n o t a major problem, a l though few o y s t e r beds escape damage complete ly . The most devas ta t i ng e f f e c t i s t o t h e

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young seed oys te r s . Crab p r e d a t i o n can be c o n t r o l l e d by keeping o y s t e r seed o f f t h e bottom, o r by a s imp le c rab t r a p p i n g program (Quayl e 1969a; Magoon and V i n i ng 1981).

The most s e r i o u s o y s t e r p r e d a t o r s i n B r i t i s h Columbia. ~ a r t i c u l a r l v i n s u b t i d a l c u l t u r e s , a rb t h e sun - s t a r Pycnopodia he1 i an tho i des , t h e m o t t l e d s t a r s t a r s t a r 1969a

t h e ochre I t h e p i nk

( Quay 1 e an o y s t e r

s h e l l - open by a p p l y i n g .more t h a n t e n pounds p ressure t o t h e o y s t e r s h e l l w i t h i t s s u c t i o n - t i p p e d tube f e e t . The e v e r t i b l e stomach i s t hen f o r c e d i n t o t h e narrow opening between t h e va lves, and t h e v i c t i m i s d i g e s t e d w i t h i n i t s s h e l l i n l e s s t h a n 24 hours (Magoon and V i n i n g 1981). E i g h t months a f t e r t e r m i n a t i n g a s t a r f i s h removal program i n Depar ture Bay, B r i t i s h Columbia a d u l t o y s t e r s had s u f f e r e d 70% m o r t a l i t y , and o y s t e r seed 100% mor ta l i t y (Quay l e 1969a).

I n i n t e r t i d a l areas, s t a r f i s h can be c o n t r o l l e d by removal o r by app ly - i n g a teaspoon o f qu ick l ime t o t h e i r backs (Quay l e 1969a). Chopping s t a r - f i s h up w i l l g e n e r a l l y r e s u l t i n more s t a r f i s h , due t o t h e i r amazing regen- e r a t i v e a b l i t i e s . A f t e r an o y s t e r bed has been c l e a r e d o f s t a r f i s h , i t may become r e i n f e s t e d by free-swimmming s t a r f i s h l a r v a e d u r i n g s p r i n g and summer. Young s t a r f i s h up t o 3 inches (75 mm) i n d iamete r appear t o be l i g h t shy. S t a r f i s h 12.5 mm i n d iameter a t t acked oys te r spa t , and those t h a t were 125 mm cou ld a t t a c k o y s t e r s o f market s i z e (Quay le 1969a).

The Japanese o y s t e r d r i l l i s con- s i d e r e d t o be one o f t h e most se r i ous p reda to r s on P a c i f i c o y s t e r s and a l s o w i l l a t t a c k a v a r i e t y o f mo l luscan b i v a l v e s (Chew and E i s l e r 1958). A c c i d e n t a l l y i n t r oduced f rom Japan, t h e Japanese d r i l l i s now w e l l - e s t a b l i s h e d a l ong t h e P a c i f i c coas t and i n t h e bays o f Puget Sound (Chew 1960). The Japanese oys te r d r i l l i s a

s n a i l t h a t uses a c i d and i t s raspy tongue ( r a d u l a ) t o d r i l l a h o l e th rough t h e o y s t e r ' s she1 1. I t then uses t h e r a d u l a t o t e a r ou t t h e meat (Quay le 1969a; Magoon and V in i ng 1981). T h i s process i s completed i n 5-6 days on young o y s t e r s (Chew 1960). Oys te rs over 2 years o l d a r e r e l a - t i v e l y s a f e f rom t h i s p reda t i on , due t o t h e t h i c k n e s s o f t h e i r s h e l l s (Ma- goon and V i n i n g 1981). Under l abo ra - t o r y c o n d i t i o n s , i t was found t h a t g i ven a cho ice , Japanese o y s t e r d r i l l s p r e f e r r e d Man i la clams (Venerupis

aponi ca) , Olympic o y s t e r s (Os t rea and bay mussels ( M y t i l u s

e d u l i s ) t o P a c i f i c o y s t e r s (Chew and Eisler 1958; Chew 1960). I n a subsequent s tudy by E l 1 i fri t (1971), d r i l l s showed no d e f i n i t e p re fe rence between P a c i f i c oys te r s , bay mussels, n a t i v e l i t t l e - n e c k clams (Pro to thaca s taminea) , o r ba rnac les (Balanus spp.). I n some areas, t h e Japanese o y s t e r d r i l l can cause a 90% l o s s o f o v s t e r s t ocks IGlude and Chew 19821. he n a t i v e d r 1 1 , Tha i s lame l losa , a l thouah ~ r e s e n t on o v s t e r beds. a t tack; baknacl es, clams ,- and mussels r a t h e r t h a n oys te r s (Quay le 1969a).

More than 50,000 Japanese d r i l l s were found per a c r e a t L i b e r t y Bay i n t h e Hood Canal area o f Washington (L indsay 1961). The a rea became un- s u i t a b l e f o r seed oys te r s , a l though h a l f -grown and adu 1 t o y s t e r s cou l d s t i l l be grown and f a t t e n e d there . Gravel t r e a t e d w i t h o r t h o d i c h l o r o - benzene and Sev in appeared t o c o n t r o l d r i l l s i n t h e i n t e r t i d a l area, by f o rm ing a permanent b a r r i e r around oys te r seed beds (L indsay 1961).

The Japanese o y s t e r d r i l l can be c o n t r o l l e d somewhat by c o l l e c t i n g i t s egg cases b e f o r e t h e eggs hatch, and by c a r e f u l o y s t e r f a rm ing p r a c t i c e s (Glude and Chew 1982). The Washington Department o f F i s h e r i e s must be con- t a c t e d b e f o r e o y s t e r s o r o y s t e r s h e l l s a r e moved w i t h i n t h e S ta te , t o he lp p reven t t h e spread o f Japanese d r i l l s (Magoon and V in i ng 1981). I n s p e c t i o n a t t h e pack ing s i t e s i n Japan helped

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p reven t f u r t h e r i m p o r t a t i o n o f d r i l l s and o t h e r pes t s on seed oys te r s (Quay l e 1969a).

I n a reas where Japanese o y s t e r d r i l l s a r e a l ready a problem, on ly o y s t e r s over 2 years o f age shou ld be p lan ted . A f t e r t h e o y s t e r s a re harves ted , t h e beds should be c leaned as t ho rough l y as poss i b l e , t h e ground raked, and t h e d e b r i s taken ashore. D r i l l s can a l s o be b u r i e d by p u l l i n g d rags over t h e a rea (Quay l e 1969a).

Mud shr imp (Upogebia puge t ten- s i s) , and ghos t shr imp ( C a l l ianassa - c a l i f o r n i e n s i s ) , cause s e r i o u s damage t o o y s t e r beds (Quay le 1969a). They d i g "U"-shaped burrows w i t h two openings which r e t a i n wa te r a t low t i d e , making t h e beds t o o s o f t f o r o y s t e r c u l t u r e . The tremendous t u r n o v e r of sediment by t h e s e an imals r e s u l t s i n t h e b u r i a l o f bo t tom c u l t u r e d oys te r s . The p e s t i c i d e Sev in has been used c o n t r o v e r s i a l l y as a c o n t r o l agen t i n Washington f o r ghost shr imp.

P a r a s i t e s

The p a r a s i t i c copepod M t i l i c o l a o r i e n t a l i s i s a sma l l b F k j F X 7 3 c rus tacean i n t r oduced t o t h e West Coast w i t h o y s t e r s impor ted f rom Japan. The maximum l e n g t h o f t h e o r - ganism i s abou t 10 mm and i t occurs i n t h e sma l l i n t e s t i n e o f v a r i o u s mo l - l u s c s (Quayle 1969a). S tud i es o f M. o r i e n t a l i s i n t h r e e areas a l o n g tTie P a c i f i c Coast found t h a t i n f e s t a t i o n was h i g h e s t a t Yaquina Bay, Oregon, i n t e r m e d i a t e a t Humboldt Bay, C a l i - f o r n i a , and l owes t a t Oys te r Bay, Washington (Chew e t a l . 1964) . The p a r a s i t e was found t o be con t i nuous l y r e p r o d u c t i v e th roughou t t h e year, a1 - though fewer egg c a r r y i n g females were found d u r i n g w i n t e r (Chew e t a l . 1964). High i n f e s t a t i o n s d i d no t ap- pea r t o a f f e c t o y s t e r g rowth (Chew e t a l . 1964), o r s u r v i v a l (Katkansky e t a l . 1967). I n f e s t a t i o n was assoc i a t ed w i t h a lower c o n d i t i o n o f P a c i f i c oys te r s , a l though i t was n o t c l e a r

whether t h e copepod caused t h e poor c o n d i t i o n o r whether o y s t e r s i n poor c o n d i t i o n were more s u s c e p t i b l e t o copepod i n v a s i o n (Chew e t a l . 1964). Ex tens i ve l o c a l t i s s u e damage can occur i n t h e g u t o f t h e o y s t e r (Sparks 1962; S i ndermann 1974).

Consumption o f o y s t e r s i n f e s t e d w i t h M t i l i c o l a poses no human t h r e a t , X-- but t e presence o f M. o r i e n t a l i s im- p a i r s t h e o y s t e r ' s appearance (Katkansky e t a l . 1967).

B o r i n g sponges (C 1 i ona ce 1 a ta ) and sea worms (P lydora c i - m , wh ich weaken t h e s h e l l b y b o r i n g ho les i n t o it, have been seiious pists t o o y s t e r s grown i n o t h e r p a r t s o f t h e wor ld . A l though b o t h spec i es occu r i n t h e Northwest, t hey have n o t been a prob lem t h e r e (Quay le 1969a).

Disease

P a c i f i c o y s t e r s do n o t seem t o be g r e a t l y a f f e c t e d by d iseases, a l t hough occas iona l d i sease ou tb reaks have occu r red (Quay le 1969a).

Focal nec ros i s , caused by an u n i d e n t i f i e d g ram-pos i t i ve bacter ium, has been found i n seed and market - s i z e d o y s t e r s i n W i l l a p a Bay, Wash- i n g t o n (Sindermann 1974). Gross d isease s i gns i n c l u d e p a l e d i g e s t i v e g lands, gaping, and sporad ic m o r t a l i - t i e s . No t r ea tmen t has been repo r t ed .

Bac i 1 l a r y necros is . caused by V i b r i o an u i 1-larum, has been r e p o r t e d i o y s t e r l a r v a e ( B e a t t i e 1978), where l a r v a l m o t i l i t y decreases, f o l lowed by m o r t a l i t y . Sindermann (1974) suggests t r ea tmen t by a d m i n i s t e r i n g a n t i b i o t i c s , accom- pan ied by improvements i n t h e water q u a l i t y and genera l s a n i t a t i o n t o h e l p p reven t t h i s disease.

Red T i d e

Occasional l y , env i ronmenta l con- d i t i o n s encourage epidemic g rowth o f v a r i o u s a l gae o r p l a n k t o n i c organisms,

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c o l o r i n g t h e waters o f a f f e c t e d bays d u l l orange t o che r r y red. O f p a r t i - c u l a r concern a re ou tb reaks o f t h e m ic roscop ic d i n o f l a g e l l a t e , - Protogony- - aulax c a t e n e l l a , which produces a m y v i r u l e n t p o i son (Quay l e 1969b). ~ o n y a u l a x -- catene l l a , a long - w i t h seve- r a l o t h e r members o f t h e aenus, have been r e c e n t l y t r a n s f e r r e d t t h e genus ~ r o t o g o n ~ a u l a x ( T a y l o r 1979). organ- isms i n t h i s arouD a r e d i f f i c u l t t o separa te taxo iomic 'a l l y , w i t h seve ra l t ypes resembl i n g P. ca tene l l a (To r i um i and Takano 19797. F i l t e r - f e e d i ng s h e l l f i s h do n o t seem t o be a f f e c t e d by t h e po ison, a l though they accumu- l a t e t h e t o x i n i n t h e i r t i s s u e s (Quay le 1969b). Human consumpti on o f t h e i n f e c t e d s h e l l f i s h causes p a r a l y t - i c s h e l l f i s h po ison ing , a p o t e n t i a l l y l e t h a l c o n d i t i o n a f f e c t i n g t h e nervous System ( N i s h i t a n i and Chew 1983).

Blooms o f P. c a t e n e l l a occur a l ong t h e p a c i f i c Coast, f rom Alaska t o c e n t r a l C a l i f o r n i a (Quay le 1969b; B e a t t i e 1982). The o y s t e r market i s n o t g e n e r a l l y a f f e c t e d , s i n c e o y s t e r s a r e u s u a l l y harves ted i n w i n t e r when p a r a l y t i c s h e l l f i s h po i son ing i s l e s s l i k e l y t o occur (Glude and Chew 1982). However, a number o f people became ill a f t e r e a t i n g i n f e c t e d o y s t e r s i n t h e Comox-Courtenay a rea a l ong t h e e a s t coas t o f Vancouver I s l a n d , B r i t i s h Columbia, i n October 1957 (Quayle 1969b). Common e d i b l e marine b i v a l v e s t h a t become h i g h l y t o x i c a r e l i t t l e - neck clams (P ro to thaca s taminea) , Man i la clams (1. j a p o n i c a ) , b u t t e r clams (Saxidomus g i gan teus ) , bay mus- s e l s (M. e d u l i s ) , and C a l i f o r n i a sea m u s s e l s ( M y t i l u s c a l i f o r n i a n u s ) , accord ing t o Quay le (1969b). I n t h e f a l l o f 1978, a severe outbreak o f p a r a l y t i c s h e l l f i s h po i son ing occur red as f a r sou th as Vashon I s l a n d i n sou thern Puget Sound, Washington ( N i s h i t a n i and Chew 1983). She1 l f i s h i n t h a t a rea remained t o x i c f o r t h e unusua l l y l o n g t ime o f 10 months, perhaps as a r e s u l t o f i n g e s t i n g t h e c y s t s formed by P. c a t a n e l l a , which a r e 10 t imes more t o x i c t han t h e d i n o f l a g e l l a t e i n t h e swimni ng stage

(Magoon and V in i ng 1981). Win te r storms may have k e p t c ys t s f rom s e t t l i n g as they norma l l y do, a l l o w i n g s h e l l f i s h t o i n g e s t them. An a l - t e r n a t i v e ~ o s s i b i l i t y i s t h a t enormous amounts o f ' ~ r o t o ~ o n ~ i u l a x were c a r r i e d i n t o t he area by wa te r movina t o sou thern Puget sound ( ~ i s h i t a n i - and Chew 1983).

P a c i f i c o y s t e r s l o s e t h e i r t o x i - c i t y q u i c k l y , i n a few weeks, conpared t o some s h e l l f i s h spec ies which may remain t o x i c f o r as l o n g as a year . Oysters c o n t a i n i n g 176 mg o f t o x i n were found t o c o n t a i n l e s s t h a n 32 mg a f t e r 4 weeks ( Q u a y l e 1969a).

Dupuy and Sparks (1968) found t h a t P a c i f i c oys te r s f e d u n i a l g a l mass

washingtonensis up take o f t o x i n

a f t e r 3 months. A t ~ e q u i m Bay, Wash- i ng ton , t o x i n l e v e l s were 3 o r 4 t imes lower i n oys te r s than i n C a l i f o r n i a mussels (Dupuy and Sparks 1968).

The Hea l t h Serv ices D i v i s i o n o f t h e Washington S ta te Department o f S o c i a l and Hea l th Serv ices and l o c a l county h e a l t h d i s t r i c t s a r e respons- i b l e f o r t e s t i n g she l l f i s h semimonthly i n bo th commercial and r e c r e a t i o n a l beaches, and c l o s i n g beaches f o r she l l f i s h h a r v e s t when accep tab le l e v - e l s o f t o x i n a re exceeded ( N i s h i t a n i and Chew 1983). I n B r i t i s h Columbia, t h e Department o f N a t i o n a l Hea l t h and Wel fare per forms t h e t e s t i n g f o r p a r a l y t i c s h e l l f i s h po ison ( Q u a y l e 1969b). I n Washington, beaches f rom Dungeness S p i t t o t h e Columbia R ive r a r e c losed annua l l y f rom A p r i l 1 t o October 31 due t o r e l a t i v e l y r e g u l a r occurrences o f p a r a l y t i c s h e l l f i s h po ison ( N i s h i t a n i and Chew 1983).

I n bays w i t h poor c i r c u l a t i o n i n sou thern Puget Sound and sou thern Hood Canal i n Washinaton. huae blooms o f Cerat ium fusu; and a Gymnodinium s l e n d i c e s can occur f rom June t o

ecember w i t h t he heav i es t concen- + t r a t i o n i n August th rough October (Cardwe l l 1978; Magoon and V i n i n g

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1981). The Washington S t a t e Depar t - ment o f F i s h e r i e s has determined t h a t blooms c o n t a i n i n g c e l l s a t a d e n s i t y of 10,00O/ml a re ex t reme ly t o x i c t o o y s t e r l a r vae . S ince P a c i f i c o y s t e r s spawn d u r i n g t he h e i g h t o f t h e bloom pe r i od , t h e occur rence of t hese blooms migh t e x p l a i n some o f t h e v a r i a b i l i t y i n y e a r l y s e t t i n g success o f o y s t e r s (Magoon and V i n i n g 1981).

ENV I R O N MENTAL REQUIREMENTS

Temperature

Water temperature i s c r i t i c a l t o o y s t e r growth and r ep roduc t i on , and appears t o be t h e main l i m i t i n g f a c t o r i n b reed ing success (Quay l e 1969a). Temperature p robab ly has an i n d i r e c t e f f e c t on l a r v a e by a f f e c t i n g t h e p ro - d u c t i o n of l a r v a l food (Quay le 1969a).

P a c i f i c o y s t e r s l i v e and grow i n wa te r w i t h temperatures o f 4 t o 24'C, and a r e a b l e t o s u r v i v e a i r tempera- t u r e s as low as -4'C when e x p ~ s e d by t h e t i d e (Quay le 1969a). Dur ing feeding, water movement th rough t h e o y s t e r i s inc reased a t h i g h e r tem- pera tu res ; consequent ly, more food i s f i l t e r e d by t h e g i l l s . Optimum tem- p e r a t u r e f o r water t r a n s p o r t through a d u l t oys te r s appears t o be about 20'C (Quay le 1969a).

W i l lapa Bay, Washington, serves as an example o f average wate r temper- a t u r e c o n d i t i o n s encountered by P a c i f i c oys te r s . W in te r wa te r temper- a t u r e s t h e r e range f rom 5 t o 6OC. The wate r temperatures beg in r i s i n g i n March and reach an upper range o f 12 t o 15'C near mid-June ( K o r r i n g a 1976). Increases i n water temperature t h e r e a f t e r a r e ex t reme ly v a r i a b l e , and determine whether o r n o t o y s t e r s i n t h a t a rea w i l l s u c c e s s f u l l y reproduce.

Oysters c a r r y spawn d u r i n g J u l y and August, b u t do n o t r e l e a s e these gametes u n t i 1 t h e water tempera tu re reaches 19'C (Magoon and V i n i n g 1981). Larvae can s u r v i v e temperatures below

15'C f o r a s h o r t t ime (Magoon and V in i ng 1981). La rvae can s u r v i v e tem- pe ra tu res as h i g h as 30°C. The l a r v a l p e r i o d inc reases f r om 18 days a t 72'F (22°C) t o 30 days a t 64'F (18'C) (F i gu re 6 ) .

West1 ey (1968) found a p o s i t i v e r e l a t i o n between t h e dep th o f t h e warm water l a ye r , t h e number o f oys te r la rvae , and t h e i n t e n s i t y o f o y s t e r s p a t f a l l i n Dabob Bay. High wate r temperatures and exce l l e n t l a r v a l r e - t e n t i o n o f Dabob Bay, Washington, and P e n d r e l l Sound, B r i t i s h Columbia, p rov i de c o n d i t i o n s conducive t o t h e n a t u r a l s e t t i n g o f P a c i f i c o y s t e r l a r v a e (Ko r r i nga 1976). Accord ing t o Chew (1983), l a r v a l s e t t i n g inc reases as temperature i nc reases between 15 and 30°C, but a t 35'C t h e r e was a d e c l i n e i n s e t t i n g ( F i g u r e 7 ) . Commercial l e v e l s o f s p a t f a l l a re a t t r i b u t e d t o t he r e g u l a r s u m e r occur rence o f a warm wate r l a y e r , up t o 7 m deep, i n which average tem- p e r a t u r e s exceed 20'C (Quay l e 1969a). A s t r o n g t he rmoc l i ne occu rs a t a dep th o f about 4 m (12 f t ) i n P e n d r e l l Sound (Quay le 1969a). Water above t h e t he rmoc l i ne i s 21'C o r more, w h i l e below t h i s l e v e l t h e tempera tu re decreases r a p i d l y . Most P a c i f i c

60 10 2 0 3 0 4 0

LARVAL PERIOD (DAYS)

F i g u r e 6. D u r a t i o n o f t h e l a r v a l p e r i o d i n P a c i f i c o y s t e r s a t v a r i o u s temperatures i n B r i t i s h Columbia ( a f t e r Quay1 e 1969a).

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'Ir I I I 1 I5 2 0 25 3 0 35

SALINITY X o

F i g u r e 7. Remote s e t t i n g o f P a c i f i c o y s t e r eyed l a r v a e a t va r i ous s a l i n i - t i e s and temperatures i n Washington ( a f t e r Chew 1983).

o y s t e r l a r v a e do n o t descend below t h e t he rmoc l i ne (Quay le 1969a).

Oyster spa t g r o m f o r 5 months i n sea water warmed t o 25°C e x p e r i - enced 28% m o r t a l i t y , compared t o 18% f o r spa t grown i n 12°C water (Breese 1971). Diaz (1973) showed t h a t l a r g e sudden inc reases i n temperature o f 10. t o 20°C can have d e t r i m e n t a l e f f e c t s on growth r a t e s , m o r t a l i t y , and s e t t i n g r a t e s o f American o y s t e r l a r vae . I n i t i a l growth o f spa t i n heated wate r , however, was 14 t imes g r e a t e r t han spa t grown i n unheated wate r (Breese 1971).

S a l i n i t y

The i n s h o r e waters, bays, and e s t u a r i e s where o y s t e r s a r e grown a r e s u b j e c t t o f r equen t seasonal changes i n wa te r s a l i n i t y . S a l i n i t y i s f a i r l y

u n i f o r m th roughou t t h e w i n t e r a t about 28-29 pp t i n t h e S t r a i t o f Georg ia i n B r i t i s h Columbia, b u t can change d r a s t i c a l l y i n May as h i l l s i d e r u n o f f and r i v e r d ischarge add f r e s h water, the reby r educ i ng t h e s a l i n i t y d u r i n g summer (Quay1 e 1969a).

Oys te rs a r e s e n s i t i v e t o changes i n s a l i n i t y , and respond t o a l t e r e d s a l i n i t i e s by c o n t r o l l i n g t h e degree of s h e l l opening ( G a l t s o f f 1964). Consequent ly, s a l i n i t y p l a y s a ma jo r r o l e i n t h e volume o f wa te r t r a n s - por ted , and hence t h e f eed ing o f oys te r s . Optimum s a l i n i t y f o r maximum water t r a n s p o r t through t h e body o f Crassos t rea i as i s 25-35 p p t ( Q u a y l e 1969a). Pa% o y s t e r s become i n c r e a s i n g l y s e n s i t i v e t o s a l i n i t i e s below 20 p p t . A t 13 pp t , l i t t l e wa te r i s pumped th rough t h e g i l l s , even a f t e r seve ra l days o f a c c l imat ion. Normal a c t i v i t y i s q u i c k l y resumed a f t e r r e t u r n i n g t h e o y s t e r s t o h i ghe r s a l i n i t i e s . Harmful e f f e c t s a r e apparent i n t h e g i l l s a t a s a l i n i t y of 10.5 ppt , a f t e r wh ich recovery i n wa te r of h i ghe r s a l i n i t y i s ex t reme ly s low (Hopkins 1936).

Labora to ry s t u d i e s i n d i c a t e d t h a t s e t t i n g o f P a c i f i c o y s t e r l a r v a e was una f fec ted by cons tan t s a l i n i t i e s be- tween 16-34 ppt, b u t s e t t i n g was r e t a r d e d by r a p i d l y f l u c t u a t i n g s a l i n - i t i e s (Lund 1971). Oys te r l a r v a e beg in dy i ng a t a s a l i n i t y o f 10 p p t ( Q u a y l e 1969a). Chew (1983) i n d i c a t e d t h a t as s a l i n i t i e s inc reased f rom 15 p p t t o 30 p p t remote s e t t i n g o f ha t che ry - r ea red l a r v a e i n a r t i f i c i a l tanks increased, bu t a t 35 p p t t h e r e was a d e c l i n e i n s e t t i n g (F i gu re 7) . S e t t i n g seems t o i n c rease w i t h b o t h inc reases i n tempera tu re and s a l i n i t y ( F i g u r e 7) . However, t h e r e i s a d rama t i c d e c l i n e i n s e t t i n g a t t h e combined h i gh temperature o f 35°C and h i g h s a l i n i t y o f 35 p p t ( F i g u r e 7 ) . Optimum c o n d i t i o n s f o r s e t t i n g o f eyed o y s t e r l a r v a e i n t h e l a b o r a t o r y were observed a t temperatures o f about 30°C and s a l i n i t i e s o f about 30 p p t (F i gu re 7 ) .

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S a l i n i t y r e d u c t i o n can r e s u l t i n t h e e l i m i n a t i o n o f p r e d a t o r species, such as t h e o y s t e r d r i l l and some f o u l i n g organisms, which a r e l e s s euryha l i n e t han oys te rs . The e l i m i - n a t i o n o f p reda to rs o r f o u l i n g organisms r e s u l t s i n a h i ghe r l e v e l o f o y s t e r p r o d u c t i v i t y (Michael and Chew 1976).

S i l t a t i o n and Subs t ra te

Oysters a r e unable t o move when faced w i t h d e t r i m e n t a l env i ronmenta l cond i t i ons . Suspended bot tom sed i - ments can cause o y s t e r s t o e i t h e r s t op f eed ing o r expend cons iderab le energy i n sepa ra t i ng mud and sand f rom e d i b l e p a r t i c l e s (Quayl e 1969a). M o r t a l i t y o f seed oys te r s p l a n t e d i n Ladysmith Harbour, B r i t i s h Columbia, reached 9% d u r i n g t h e f i r s t yea r , w i t h s i 1 t a t i o n as t h e causa t i ve f a c t o r (Quayle 1969a). Pereyra (1961, 1964) found s i l t a t i o n t o cause m o r t a l i t i e s as h i g h as 22% i n t r a y - r ea red oys te r s , whi 1 e b iweek ly r a i s i n g and r e s e t t i n g o f baskets kep t them r e l a t i v e l y f r e e f rom mud and p robab l y he lped reduce f u r t h e r m o r t a l i t i e s .

Many o y s t e r growers a s s o c i a t e t h e y e a r l y inc rease i n o y s t e r cond i t i on , known as fa tness, w i t h t h e inc reased t u r b i d i t y o f water o c c u r r i n g f rom March th rough November (Quay le 1969a). T h i s t u r b i d i t y i s caused by severa l t h i n g s , i n c l u d i n g qu ick blooms o f m ic roscop ic mar ine organisms, s i 1 t, suspended d e t r i t u s , o r a v a r y i n g m i x t u r e o f a l l o f these.

The e f f e c t s o f suspended sed i - ments on P a c i f i c o y s t e r eggs and l a r v a e s t i l l need t o be i n v e s t i g a t e d . The eggs o f t he Eas te rn oys te r , C . v i r g i n ica, exper ienced 20% m o r t a l i T y a t s i l t concen t ra t i ons of 0.25 g / l , and 1 a r v a l mo r ta l i t y o f approx imate ly 27% a t s i l t concen t ra t i ons o f 0.50 g / l a f t e r 12 days o f exposure (Davis and Hidu 1969).

Kennedy and Br iesch (1981) r e - viewed seve ra l s t u d i e s o f d redg ing e f - f e c t s on Eas te rn oys te rs , and concluded t h a t t h e response o f oys te r s t o d redg ing i s a f f e c t e d by t h e t y p e o f sediment, the c i r c u l a t i o n o f water i n t h e area, t h e amount o f sediment suspended and r e d i s t r i b u t e d , and t h e topography o f t h e o y s t e r grounds. They suggested avo id i ng ex tens i ve d redg ing i n oys te r -p roduc ing areas d u r i n g t h e oys te r r e p r o d u c t i v e season, o r d u r i n g per iods o f e l eva ted temper- a tu res o r lowered s a l i n i t i e s t h a t might inc rease t h e s t r e s s on oys te rs .

Water C i r c u l a t i o n

Due t o t he s e s s i l e l i f e s t y l e o f t h e oys te r , water c i r c u l a t i o n p l a y s a paramount r o l e i n p r o v i d i n g c o n d i t i o n s f o r feed ing and c leans ing , as w e l l as f o r success fu l r e p r o d u c t i o n and f o r t h e d i s p e r s a l o f o y s t e r la rvae . West ley (1964) found t h a t areas (15 m deep w i t h u n s t r a t i f i e d waters and hav ing moderate ly r a p i d wate r ex- change, were areas of good o y s t e r c o n d i t i o n . I n a d d i t i o n , t h e depth o f a warm (>17OC) wate r l a y e r i n l a t e summer i s j u s t as impo r tan t as t h e number o f o y s t e r l a r v a e p e r sample i n de te rmin ing t h e d e n s i t y o f s e t t i n g oys te r s (West ley 1968). I n Pendrel 1 Sound, B r i t i s h Columbia, su r f ace c u r r e n t s a r e weak, a l l o w i n g o n l y a smal l p o r t i o n o f t h e n a t u r a l l y produced o y s t e r l a r v a e t o move o u t of t h e sound, thereby a1 1 owing heavy spa t s e t t i ng (Quayl e 1969a). Grea te r f 1 ush i ng r a t e s can cause un favorab le s e t t i n g c o n d i t i o n s f o r o y s t e r l a r vae , by washing them away f rom p r e f e r r e d s e t t i n g s i t e s ( K o r r i nga 1976).

Excessive wave ac t i on , however, can tumble oys te r s about , knock ing o f f t h e i r f r a g i l e s h e l l edges (Quay le 1969a). High wave a c t i o n a l s o i n - creases water t u r b i d i t y by s t i r r i n g up bot tom sediments, causing s i l t accumu- l a t i o n over t h e o y s t e r s (Kor r inga 1976).

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P o l l u t i o n

A major long- te rm concern t o t h e o y s t e r i n d u s t r y i n t h e P a c i f i c Nor th - west i s t h e p resen t and p o t e n t i a l f u t u r e l o s s o f wa te r q u a l i t y because o f p o l l u t i o n . The va r i ous l i f e s tages o f oys te r s (eggs, la rvae , spat , and a d u l t s ) have d i f f e r e n t l e v e l s o f s u s c e p t i b i l i t y t o p o l l u t i o n (Woelke 1960b, 1960c; Quay le 1969a). Var ious t ypes o f p o l l u t a n t s can be concen t ra ted i n t h e i r body t i s sues , pos i ng hazards t o humans consumi ng a f f e c t e d o y s t e r s (Kennedy and B re i sch 1981). I n d i r e c t l y , p o l l u t i o n can r e s u l t i n l o s s o f o y s t e r f o o d supply , poor growth, l o ss o f l a r v a l v i go r , i nc reased s u s c e p t i b i l i t y t o d isease, pests , o r p reda t ion , con tam ina t i on o f s e t t l i n g sur faces, decreased fecun- d i t y , and reduced spawning (Quay l e 1969a; Kennedy and B re i sch 1981). The e f f e c t s o f p o l l u t a n t s can be exacer- ba ted by o t h e r env i ronmenta l s t r esses , such as changes i n water temperature o r s a l i n i t y , even though o y s t e r s a re t o l e r a n t o f wide v a r i a t i o n s i n b o t h of these f a c t o r s (Quay l e 1969a).

P a c i f i c o y s t e r c u l t u r e has been i n h i b i t e d by t h e t o x i c o r pa thogen ic p o l l u t i o n o f wa te rs by sewage, i n - d u s t r i a l waste, o r p u l p m i l 1 e f f l u e n t s (Gunn and Saxby 1982). P o l l u t i o n r e s u l t s p a r t l y f rom t h e d i r e c t d i s - charge o f sewage i n t o an a rea , o r f rom t h e curnu l a t i ve d ra inage f rom i n d i - v i d u a l , improper l y i n s t a l led, o r i m - p r o p e r l y f u n c t i o n i n g s e p t i c t anks (Quay l e 1969a). Pol l u t i on can occur i n d i r e c t l y by r u n o f f f rom su r round ing a g r i c u l t u r a l l a n d o r urban areas, o r th rough seepage f rom ground wate r f o l l owing r a i n f a l l (Quay1 e 1969a; B e a t t i e e t a1 . 1982).

The embryonic and l a r v a l s tages o f an o y s t e r a re t h e most s u s c e p t i b l e t o poor wa te r q u a l i t y (Woelke 1960a, 1960b, 1960c; B e a t t i e e t a l . 1982). Domestic sewage p o l l u t i o n can enhance a l g a l blooms t o x i c t o s h e l l f i s h l a r - vae, t h u s r educ i ng o r e l i m i n a t i n g n a t u r a l oys te r r ep roduc t i o n ( B e a t t i e

e t a l . 1982). One o y s t e r ha tchery i n Washington was c l osed because o f p o l - l u t e d bay water ( B e a t t i e e t a l . 1982).

P i e r ce County, one o f t h e coun t i es su r round ing South Puget Sound, has p l aced r e s t r i c t i o n s on l and use on bays where o y s t e r s a r e grown, r e g u l a t i n g minimum l o t s i z e and s e p t i c system requ i rements i n an a t t emp t t o reduce non-po in t source p o l 1 u t i o n ( B e a t t i e e t a l . 1982). Over 90% o f Coos Bay, Oregon, has been ba r red f rom o y s t e r p r o d u c t i o n due t o h i g h c o n t e n t o f c o l i f o r m b a c t e r i a (Qualman 1982). Sewage p o l l u t i o n i n B r i t i s h Columbia has r e s u l t e d i n t h e c l o s u r e o r r e s t r i c t i o n o f a s i g n i f i c a n t p ro - p o r t i o n o f t h e p o t e n t i a l o y s t e r p roduc ing areas, i n c l u d i ng Boundary Bay and Ladysmith Harbour (Gunn and Saxby 1982). Var ious methods have been developed t o p u r i f y o y s t e r s t a i n t e d by p o l 1 u t i o n (Quayle 1969a; Conte and Dupuy 1982).

The d e t e r i o r a t i o n o f o y s t e r g row ing areas can a l s o be caused by t h e f o r e s t i n d u s t r y , ma in ly as a consequence o f p u l p m i l l e f f l u e n t s and l o g p rocess i ng procedures. Pulp m i 11 e f f l u e n t i s known as s u l p h i t e waste l i q u o r o r k r a f t m i l l e f f l u e n t depend- i n g upon t h e process used (Quay le 1969a), and bo th e f f l u e n t s c o n s i s t o f water, chemical waste, and some wood f i b e r . Upon d ischarge i n t o t h e water , bo th chemical waste and f i b e r s mhy a f f e c t oys te r s d i r e c t l y by caus i ng m o r t a l i t y , reduc ing t h e growth r a t e , r educ i ng f a t ness ( t he reby changing t h e c o n d i t i o n index) , and by a l t e r i n g t h e spawning c y c l e (Quay le 1969a). The measurement o f these f a c t o r s , whi 1 e n o t p a r t i c u l a r l y d i f f i c u l t i n i t s e l f , becomes complex when e f f l u e n t e f f e c t s have t o be separated f r om t h e wide v a r i a t i o n s t h a t occur i n t h e absence o f p o l l u t i o n . M o r t a l i t y i s t h e s i m p l e s t of these f a c t o r s t o measure, b u t o n l y r a r e l y a r e e f f l u e n t concen- t r a t i o n s h i g h enough t o cause s i g n i - f i c a n t m o r t a l i t y i n t h e hardy P a c i f i c o y s t e r (Quay le 1969a). Concen t ra t ions of k r a f t m i l 1 e f f l u e n t between 10 t o

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40 ppm e x e r t a s i g n i f i c a n t e f f e c t on t h e c o n d i t i o n f a c t o r o f P a c i f i c o y s t e r s i n B r i t i s h Columbia (Quay le 1969a). I n Washington S ta te , f r e s h s u l p h i t e waste l i q u o r adverse ly a f - f e c t e d 48-hr P a c i f i c o y s t e r l a r v a e development a t 2 ppm and i t caused n e a r l y 100% l a r v a l a b n o r m a l i t i e s a t 18 ppm (Woelke 1 9 6 0 ~ ) . I n d i r e c t l y , s u l - p h i t e waste l i q u o r can a f f e c t o y s t e r s by k i l l i n g t h e i r f o o d organisms. A t 1,000 t o 10,000 ppm, s u l p h i t e waste l i q u o r i s l e t h a l t o Monas spp., a f l a g e l l a t e protozoan t h a t i s an i m - p o r t a n t o y s t e r food (Woe'l ke 1960a) , and a t concen t ra t i ons as low as 2.5 ppn o v e r severa l months t ime, i t seemed t o depress growth i n Monas spp. Other fl age1 l a t e s , Cryptanonas and I s o c h r y s i s , and a d ia tom, Ac t ino - c yc l us , t h a t o y s t e r feed upon were n o t g r e a t l y a f f e c t e d by concen t ra - t i o n s o f s u l p h i t e waste l i q u o r as h i gh as 304 ppn (Woelke 1960b).

I n genera l , s u l p h i t e waste l i q u o r was p resen t a t ext remely h i gh concen- t r a t i o n s o n l y i n t h e v i c i n i t y o f p u l p m i l l s , a l t hough some was found i r ~ n e a r l y a1 1 a reas o f Puget Sound, Grays Harbor, and P o r t Angeles i n Washington S t a t e (Woelke 1960a). A r a p i d d e c l i n e occur red i n open bays, e s p e c i a l l y i n t h e summer (Woelke 1960b); t h i s was r e l a t e d t o t h e movement o f t h e su r f ace l a y e r o f wa te r (Woelke 1 9 6 0 ~ ) .

Organic m a t e r i a l s i n p u l p m i l l e f f l u e n t s r e q u i r e l a r g e amounts o f oxygen f o r decomposit ion. A s u f f i - c i e n t l o w e r i n g o f t h e oxygen concen- t r a t i o n i n sea wate r can v i r t u a l l y su f foca te mar ine l i f e (Quay le 1969a). I n a d d i t i o n , l a r g e q u a n t i t i e s o f suspended wood f i b r e can c l o g t h e g i 11s o f f i l t e r - f e e d i ng an imals such as oys te r s (Quay le 1960a).

Log boomi ng s i t e s o f t e n occur c l o s e t o oys te r beds. Debr i s , such as

bark and wood ch ips , g e n e r a l l y s i nk d i r e c t l y below t h e l o g booms, bu t some d e b r i s remains a f l o a t l o n g enough t o be depos i t ed i n a mat on t h e surround- i n g bottom. Not o n l y does t h i s smother bo t t om-dwe l l i ng organisms by p r e v e n t i n g adequate water c i r c u l a t i o n , bu f t h e decompos i t i on o f these m a t e r i - a l s dep le tes t h e oxygen supp ly and produces t o x i c hydrogen s u l f i d e (Quayle 1969a). Log s to rage i n Ladysmi t h Harbor, B r i t i s h Columbia, has appa ren t l y ended o y s t e r p r o d u c t i o n i n t h a t a rea (Gunn and Saxby 1982).

The e f f e c t o f chemica l p o l l u t i o n on 5. g i g a s i n t h e P a c i f i c Nor thwest has n o t been t ho rough l y s tud ied . How- ever , Kennedy and B re i sch (1981) r e - viewed t h e l i t e r a t u r e d e a l i n g w i t h t h e chemica l e f f e c t s o f pH, c h l o r i n e , heavy meta l , pe t ro leum hydrocarbons, and de te rgen t s on t h e Eas te rn oys te r . Oys te rs near a former copper sme l t e r i n B r i t i s h Columbia con ta i ned 20,000 ppm o f copper and 36,000 ppm o f z i nc , compared t o average va lues o f 600 ppm o f copper and 10,000 ppm o f z i n c found i n o t h e r areas (Quay le 1969a). The s e t t i n g o f P a c i f i c o y s t e r l a r v a e under l a b o r a t o r y c o n d i t i o n s was r e t a r d e d by copper concen t ra t i ons exceeding 0.1 mg/l (Lund 1971). Oys te rs have accu- mulated very low c o n c e n t r a t i o n s o f a r s e n i c leached f r om s h i p s sprayed w i t h an a r s e n i c compound t o p r e v e n t shipworm a t t a c k ( Q u a y l e 1969a).

Tests i n v o l v i n g o y s t e r l a r v a e a r e used as a s tandard f o r t h e e v a l u a t i o n o f env i ronmenta l degrada t ion (LeGore 1974). However, t e s t i n g f o r contami - na ted o y s t e r s shou ld be done by com- prehensive mon i t o r i ng , s i n c e i s o l a t e d t e s t s can r e s u l t i n a wide range o f va lues due t o t i d a l o r seasonal f l u c - t u a t i o n s i n po l l u t a n t l e v e l s (Mor ton and S h o r t r i d g e 1975).

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10172 -101

REPORT DOCUMEhTATION 1- "E'ORT i I L Rec~wmw'n kcmaatan No.

PACE ( B i o l o g i c a l Report 82(11.85) 1 I I

r. n t l e EMI I. S p e c ~ e s t r o f i l e s : L i f e H i s t o r i e s and Environmental Requirements o f Coastal Fishes and I n v e r t e b r a t e s ( P a c i f i c Nor thwes t ) - -Pac i f i c Oyster

Na t iona l Wet1 ands Research Center coas ta l - ~ c o l ogy Group Washington, DC 20240 P.O. Box 631

Vicksburg, MS 39180

% rmwa oate

September 1988

7. I r r ( k r ( s l

G i l b e r t B. Pauley, B i r g i t t a Van Der Raay, and David T r o u t t 9. h d o r m ~ n a Oqanrrat~an Nmme and ~ d d r m a

Washington Cooperat ive F i she ry Research U n i t Co l lege o f Ocean and F i she ry Sciences U n i v e r s i t y o f Washington S e a t t l e , WA 98195

1% SaoncMna Or#anhtbm Namm and A d d m a

U. S. Department o f t h e I n t e r i o r U. S. Army Corps o f Engineers F i s h and W i l d l i f e Se rv i ce Waterways Experiment S t a t i o n

15 Suop(am8ntaq Not- I

L Prdarmana Oraantrat~or Rmac. ((a

10. P r n ~ u t n m a k t W ~ r r Unrt I*

18. bntracc(C) w GI.W(G) ~ e .

IC)

la

IS. TYW 01 Rmooa L h n o d - n d

U.S. Army Corps o f Engineers Report No. TR EL-82-4

IL Abu- ( U m i t IOQ w r d . )

Species p r o f i l e s a r e l i t e r a t u r e summaries o f t h e taxonomy, morphology, range, l i f e h i s t o r y , and environmental requirements o f coas ta l aqua t i c species. They a r e designed t o a s s i s t i n environmental impact assessments. The P a c i f i c o y s t e r i s found i n t h e e s t u a r i n e waters o f C a l i f o r n i a , Oregon, Washington, and B r i t i s h Columbia. I t i s sought b o t h commerc ia l ly and r e c r e a t i o n a l l y . Washington leads a l l o t h e r areas combined w i t h a commercial p r o d u c t i o n o f 5.5 m i l l i o n pounds valued a t $3.8 m i l l i o n . T h i s i s 26% o f Washington S t a t e ' s t o t a l shel l f i s h p r o d u c t i o n value. These a r e very pro1 i f i c animals, r e l e a s i n g up t o 70 m i l l i o n eggs p e r year . Larvae a r e s e n s i t i v e t o a v a r i e t y o f environmental cond i t i ons , p r i m a r i l y temperature and s a l i n i t y , and t o p o l 1 u t a n t s i n c l u d i n g s u l p h i t e waste l i q u o r . Growth i s r a p i d and most n o t i c e a b l e i n t h e t h i r d and f o u r t h years . A1 ong w i t h o t h e r shel 1 f i s h , P a c i f i c oys te rs may accumulate t o x i n f rom Gonyaulax cantenel l a ( respons ib le f o r p a r a l y t i c shel l f i s h po ison ing) , b u t they l o s e t h e t o x i n more r a p i d l y than o t h e r s h e l l f i s h . Optimum water temperature f o r a d u l t s i s 20 O C and optimum s a l i n i t i e s a r e above 20 p p t f o r adu l t s . Ambient temperature i s t h e s i n g l e most c r i t i c a l i t e m t o breed ing success i n t h e P a c i f i c Northwest.

Temperature Feeding h a b i t s Suspended sediments Es tua r ies Growth Contaminants Oysters Sediments Water p o l l u t i o n S a l i n i t y L i f e c y c l e s b ldantlfbmn/Omn.Cnded T o m

P a c i f i c Oyster Eco log i ca l r o l e Crassostrea g igas Environmental Requirements L i f e h i s t o r y

I

2 2 Pncm 1 c wun ~ ~ I ~ I C ~ W

21. No. of Pa#*-

28 1L Avm.r.llabllity Stmcmmmnl 19. Scunty Class nhla R-W-1

u n c l a s s i f i e d

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TME PRIDE in Amerzca

DEPARTMENT OF THE INTERIOR U.S. FISH AH1 WllDLlR SERVICE

As the Nation's principal conservation agency. the Department of the Interior has respon- sibility for most of our .nationally owned public lands and natural resources. This includes fostering the wisest use of our land and water resources, protecting our fish and wildlife, preserving thsenvironmental and cultural values of our national parks and historical places, and providing for the enjoyment of life through outdoor recreation. The Department as- sesses our energy and mineral resources and works to assure that their development is in the best interests of all our people. The Department also has a major responsibility for American Indian reservation communities and for people who live in island territories under U.S. administration.