FEATURE ARTICLE
	Oysters . . .
	In the Environment

The Eastern Oyster
(Crassostrea virginica)

Classified Information

Kindgom Animalia
   Phylum Mollusca
      Class Pelecypoda or Bivalvia
         Order Lamellibranchia
            Family Filibranchia
               Genus Crassostrea
                  species virginica

Biologically Speaking

Range: Along the coast of North America from the Gulf of the St. Lawrence to the Gulf of Mexico. It has also been introduced to Hawaii, the West Coast of North America, and other locations worldwide.

Oysters are typically found in estuaries, sounds and bays, from brackish water to very salty lagoons. They are very tolerant organisms, being able to withstand wide variations in temperature, salinity, suspended sediments, and dissolved oxygen. In the Bay, oysters are usually found in areas that have over 5ppt salinity.

Feeding: Oyster are filter-feeders, drawing water in over it's gills through the beating of cillia. Suspended food (plankton) and particles are trapped in the mucus of the gills and transported to the mouth, where they will be eaten, digested and expelled as feces or expelled (spit out) as pseudo-feces. Feeding activity is greatest in oysters when water temperatures are above 50°F (~10°C).

Reproduction: Oysters spawn when water temperatures become greater than 68°F (~20°C). They are broadcast spawners, releasing eggs and sperm into the water column. Fertilized eggs develop into a planktonic or swimming larval form. After about two weeks these larvae will "set", a process of cementing themselves to a hard substrate, and metamorphose. This newly attached oyster is known as a "spat".

Challenging Chesapeake

Oysters have been around for millions of years - they were used for food, tools, weapons and decoration.

During the early 1600's in the Chesapeake region, oyster bars were so numerous and large, that they were reported as navigation hazards by Captain John Smith.

Today, the state of the oyster fishery in the Chesapeake has dwindled to less than one percent of it's historical mass. Key reasons for this decline include:

• Overharvesting
  
• Habitat Destruction
  
• Disease
  
• Sedimentation and pollution
  

Reef Reality

Oysters are the building blocks of one of the most important benthic communities found in Chesapeake Bay, The Oyster Bar. Formed as a result of years of oyster production and settlement in concentrated areas, bars have become home to a complex assemblage of plants and animals.

Benefits of oyster bars to Chesapeake Bay include:

• Providing solid structure within the water column for sessile organism attachment (i.e., barnacles, sea anemones)
  
  
• Creating homes and hiding places for organisms seeking refuge from predation (i.e., polychaete worms, soft-shell blue crabs)
  
  
• Providing spawning substrate (i.e., gobies, blennies, skilletfish)
  
  
• Stablizing bottom sediments for benthic organisms and aquatic plants (i.e., hard clams)
  
  
• Concentrating prey (food) species for larger predator fishes (i.e., striped bass)
  

http://www.mdsg.umd.edu/Extension/msgsnn/msgsnn02_2/oysters_envi.html