Ostrea Lurida

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Ostrea Lurida, commonly known as the Olympia Oyster, is a bivalve native to the west coast of North America. They are found attached to the bottom and top of a variety of substrates in bays and calm estuaries. They are filter feeders, using gills to extract food from the surrounding water. Can survive in waters with varying salinity. Their shells grow to a length of 35-45mm. They are sexual reproducers. This Oysters population has been greatly exploited by the fishing industry and has still not recovered. Many Restoration and Conservation attempts have been made though, few have shown successful.

Olympia Oyster
Ostrea Lurida: Photo by Joop Trausel & Frans Slieker, taken from http://www.nmr-pics.nl/Ostreidae_new/album/slides/Ostrea%20lurida.jpg
Scientific classification
Kingdom: Animalia
Phylum: Mollusca
Class: Bivalvia
Subclass: Pteriomorphia
Order: Pterioida
Family: Ostreidae
Subfamily: Ostreinae
Genus: Ostrea
Species: Lurida
Binomial name
Ostrea Lurida
Carpenter, 1864


Phylogeny & Description

Average length ranges from 6-8cm with a width of 4-6cm. Shell shape can vary extremely. Upper (right) valve is flat and fits into the raised area of the opposite valve. Lower (left) valve is concave and shallow. Upper and Lower valves are usually the same size. Shells growing on substrates will conform in respect to substrate. Free-growing oysters have oval to elongated shells. The exterior of the shell has no organic coating, or periostracum, and varies from white to a black purple. shells may have purplish brown or yellow stripes. The scar of the adductor muscle is not much darker then the white to olive green interior of the valves.

Oysters, like clams, scallops, mussels, and the rest of the Bivalves are a altered group of mollusks. Bivalves are some of the earliest mollusks to be seen evolutionarily. Numerous bivalves, including Fordilla and Pojetaia, date back to the Tommotian Period which is about 535-521 million years ago. Although these bivalves disappeared during the mid-Cambrian period, around 510-501 million years ago, modern bivalves were seen in the early Ordovician period 488-472 million years ago. These dates are based on accumilated fossil records. Bivalves were seen evolving during the early paleozoic and mesozoic around 251-65.5 million years ago.

Ecology & Distribution

Geographic Range

Olympia Oysters Coastal Geographical Range: British Columbia to Baja California

The olympia oyster is native to the Puget Sound, but range from Baja California to Southern Alaksa. It was once plentiful on the west coast, from Sitka, AK to Baja California. Fossil records show presence in mid-California as early as the Miocene and early-Pliocene. Native Indians and early americans may have been responsible for changes in their geographic range. Therefore, by the early 1930's, this oysters natural range had been diminished. It is also indicated by historic evidence that this oyster is indigenous to at least three of Oregon's estuaries. The Yaquina Bay, the Netarts Bay, and Coos Bay, though it seems only the Yaquina Bay population has been continuous since prewestern settlements. This information is backed by large shell deposits buried in the sediment of the polyhaline estuary regions and by numerous fishery landing records in those areas. Other Oregon estuaries such as Umpqua/Winchester, Alsea, and Tillamook Bay might have also sustained populations of Ostrea Lurida.

Can be found growing on pilings, rocks, docks, floats, and on other oyster shells close to low-tide areas in calm estuaries and bays. Can also be found living in small rivers and streams. In higher elevations they are found in mudflat bordered areas. In lower elevations they live in eel grass beds. They need water with temperatures from 6-20 degress celsius and depths of 0-71 meters. They live in waters with an average salinity of 25ppt though, can survive in streams where salinity fluxuates. These oysters are vulnerable to extreme high and low temperatures.

Life History

The Olympia oysters life history is similar to the other oysters of the genus Ostrea. It is indicated by historical evidence that this oyster is indigenous to at least three of Oregon's estuaries. Fossil records and sedimentation along the North American coast show they are native to these waters. Some records may be shown unaccurate due to native indian cultivations effecting Ostrea Lurida populations and their natural flourishing sites.

Reproduction and Behavior


Average Reproductive Cycle of Oyster

The spawning process begins at water temperatures of 13-16 Celsius. Clusters of Sperm are released in the mantle cavity of the males. Contractions of the shell are used by the body to expel these balls. The sperm disintegrates in seawater and spermatozoa is released. The female bring the spermatozoa into the mantle cavity using water pumps. The eggs are then fertilized. Spermatozoa in seawater stimulates synchronous spawning in other Olympia oysters. Veliger larvae develop from the fertilized eggs within the mantle chamber and are discharged 10-12 days later. They develop feet and an eyespot within the 11-16 day veliger stage. Then they metamorphose into spat after crawling on hard substrate. This substrate can range from old oyster shells, rocks, wood, metal, to any other hard material. Due to the swimming position of larvae, the foot being held in a superior position, oyster spat set on the underside and upperside of horizontal surfaces. In the northern area of the oysters geographic range, there may be one or two spawning periods in mid-summer. In the central area of their geographic range, spawning may be one prolonged period or two in mid-summer. In the Southern area, spawning occurs from spring to fall, peaking in the spring.

Life Span

Olympia Oyster Attached to Rock Substrate: Photo by and taken from http://www.elkhornslough.org/research/conserv_oysters.htm

After larvae have been released from female they go through a 11-16 day veliger stage while in search of substrate to live on (See Reproduction). Once larvae have found substrate to live on and have metamorphosed from larvae to spat, shell begins to grow. Oysters grow slow, their shells reaching 35-45mm in three years within Washington. After this three year period, there is little to no increase in growth. As the oyster matures, shell growth decreases. Although shells have been recorded to grow to heights of 50mm. The maximum size of an Olympia oyster recorded was 75mm.


Similar to other bivalves, they are filter feeders which filter the water that surrounds them screening out phytoplankton which they eat. These phytoplankton are found in tidal waters. They filter 9-12 quarts of water daily. In turn, marine waters are kept clean. The water is filtered through ostia-gill openings which are larger on the olympia oyster than the japanese oyster. This larger ostia-gill allows for larger food items and prevents it from consuming nannoplankton. The position of the two mantles coming together considerably reduces the amount of water taken in by gills. Temperature and Salinity of surrounding water effects the oysters ability to feed. When temperatures are low, the shell is forced to close therefore effecting suction of gills. This is the case since the behavior of the adductor muscle is controlled by temperature. The gills, mantle, and adductor muscle are the three sets of organs which control feeding. The ciliae covering the surface of the gills influences the rate of feeding. The ciliaes synchronous beating forces the water through the gills. Therefore, stronger ciliae means improved eating.

Human Use


Fishing for Oysters: Photo by Tom Mattson, taken from http://www.pacificcohistory.org/sw2005_3.htm

The Olympia oyster has supported an Indian sustenance fishery and a commercial fishery, and was used to establish a maricultural industry on the US west coast. They were shown to be an important food item of coastal tribes by the large quantity of shells found in San Francisco Indian kitchen middens. Indians of the southern puget sound located their settlements near oyster populations. In Washington in 1850, 10,000 bushels of wild Olympia oysters were harvested. Production had reached 130,000 bushels a year by the 1890's. In 1910, production declined to 16,000 bushels a year due to Callow Act of 1890 which allowed private ownership of tidelands. Oysters were returned to reefs which would in turn produce new generations. During the early 1900's, dyked oyster beds were created with gravel bottoms which held water at low tides. After 3 to 5 years, oysters reached a marketable size and then were sold as shucked meat rather them in the shell. This led to increases in oyster culture. Production peaked in 1897 to 1908, at 63,000 gallons a year. Production declined in the 1920's to 42,000 gallons a year and continued to fall through the 1980's. This decline was due to anthropogenic pollution along with urbanization.

Conservation & Preservation

Conservation measures have been made due to the exploitation of Ostrea Lurida. Oyster conservation was one of the first measures addressed in 1889 after statehood was granted. The first legislature passed an act regulating the appraisal and disposal of tidelands. The Callow Act and Bush Act were also passed to support cultivation of oysters. Many oyster reserves were created by Washington legislature in 1890 and 1910. These reserves overlapping already existing natural oyster beds. 4,500 acres in Puget Sound and 11,239 acres in Willapa Bay were used as reserves. These reserves were not fully protected and still experienced exploitation. Today the reserves popularity and interest has greatly decreased. Only 10,000 acres reserves in Willapa Bay and 1,000 acres of reserves in Puget Sound still exist today.


Oyster Restoration in Chesapeake Bay: Photo by and taken from http://oysterloversparadise.blogspot.com/2009/05/oyster-management-and-restoration.html

Restoration interest has increased due to oyster growers, nonprofit organizations, state agencies, and tribes. Restoration supports a range of interests including improved water quality, a habitat for other native species, and possible commercial harvests. In 1970, Ostrea Lurida was recognized as a threatened species candidate by Washington State. In 1998 a Stock Rebuilding plan was created for the species. The plan involves habitat recovery and the planting of juvenile hatchery raised oysters. The Habitat recovery consists of the natural recruitment of placed shells. There are at least 41 restoration sites in Washington. These sites have been constructed out of the Puget Sound Restoration fund. The plan aims to restore and preserve populations on public tidelands of their natural range. Restoration sites that have been successful are usually subtidal or moist seeps which prevent predation. These areas also protect the oysters from silt. Biology of the Olympia oyster is being studied to further understand its relationship with the environment. Information gained through these studies will go to support restoration.


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