BIOL 331
Lecture 17
Intertidal Ecology II
Ecological Interactions in the
Intertidal
Mid-Intertidal Zones (Zones 2-3)
- Starfish is a keystone predator
- Ecological succession
- Balance of disturbance and homeostasis
Lower-Intertidal Zones (Zones 3-4)
- Sea otter is a keystone predator on West Coast
- Factors affecting Enteromorpha & Chondrus dominance
- Seaweeds predominate
Soft-Bottom Ecosystems
Defining the Substrate
- Sediments accumulate where water is calm enough to let it settle out
- Attachment sites unavailable
- No seaweeds, only eel grass in protected areas
- Communities dominated by infauna
- Grain size varies from gravel & sand to silt & clay
- Type of sediment depends on amount of water movement
- Smaller the dominant particles, the richer the community (better water retention)
Nutrients & Oxygen Levels
- Most organisms are detrital feeders
- Finer sediments richer in food
- Oxygen levels lower as particle size decreases
- Muds are richest, but just below surface become anoxic
- Anaerobic, hydrogen sulfide producing bacteria are abundant
- Many invertebrates pump water to get oxygen
- Other invertebrates are adapted to low oxygen levels
Movement
- Worms use expansion and contraction of body to move
- Bivalves use muscular foot as digging & anchoring tool
- Some invertebrates eat their way through sediment
- Meiofauna simply pass between grains
Feeding
- Deposit feeders predominate
- Eat through
- Use tube feet to pass particle of food to mouth
- Clams siphon particles from surface
- Tentacles & mucous nets to catch food as it settles
- Suspension feeders (Olivella, sand crabs)
- Predators (moons snails, birds, fish)
Zonation
- Present on sand, essentially absent on muds
- Arthropods near & above high tide mark
- Worms & bivalves intertidal
- Sand dollars & sea cucumbers subtidal

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