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intertidal zone
area between the highest high tide and the lowest low tide
also known as: coasts
“where the land meets the sea”
soft bottom community
soft sandy bottom (gravel, sand, silt, clay)
consists mostly of infaunal organisms (sand crabs, bivalves)
consists of meiofaunal organisms (worms, copepods)
more common along the East Coast of US
commonly known as beaches
less geologically active
rocky shore community
regularly exposed to air (due to tidal flow)
known as the "littoral zone" (due to Littorina planaxis -periwinkle snail )
more common on the West Coast of US
hard "rocky" bottom
occur on recently uplifted or geologically young coasts or where erosion occurs (edge of tectonic plate)
temperature and salinity fluctuate greatly (due to tidal flow)
consists mostly of epifaunal organisms ↳some motile (move), some sessile (attached) - snails, anemones, mussels, crabs, seastars
periwinkle snail
commonly found along rocky shorelines in the intertidal zone
small, marine snails
spread rapidly along the eastern coast of North America, especially in the intertidal zones.
graze on algae
it can create a ripple effect throughout the food web, impacting species that rely on algae as their primary food source.
epifaunal
organisms that live ON top of substrate
motile
mobile
can move
sessile
attached
lichens
looks like tar
fungus and plant symbiosis
provide structure, protection, and moisture retention.
perform photosynthesis, producing food for both the fungal partner and themselves.
↳allows lichens to survive in harsh conditions, where individual organisms might struggle.
ecological succession
replacement of organisms
the natural process of change in the species composition of an ecosystem over time, influenced by a variety of factors
↳plays a critical role in shaping biodiversity and ecosystem structure.
competitive exclusion principle
when dominant species takes over
when two species that are too similar in their use of resources cannot live in the same place indefinitely, and one will eventually prevail (take over)
wave shock
force of striking waves
effect of high tide
affects intertidal organisms bc they cant withstand the force of wave shock
hydraulic pressure
to the pressure exerted by water within organisms or environments.
plays a role in supporting the structure and movement of marine animals, circulating fluids in their bodies, and influencing the functioning of marine ecosystems.
the weight of the water above creates immense pressure on organisms that live there
byssal threads
strong fibers made of protein that mussels use to attach to substrates to prevent being washed away by strong tides
adaption for high tides
swim bladder
adaptation for high tides
A gas-filled sac that provides many bony fishes with buoyancy.
intertidal fishes lack this to be able to sink down to the bottom to prevent being washed away by tides
abrasion
effect of high tides
injuries or tiny cuts on skin/surfacec
closing down
adaptation for high tides
when organisms use their covering or shell that closes and is able to hold water
helps contain water and prevent drying out
desiccation
substrate remains wet after the tide goes out,
not a huge problem
drying out?
suspension feeding
used by sessile organisms like sea anemones
the capture and ingestion of food particles that are suspended in water
deposit feeding
used by sessile organisms
Animals that eat organic matter that settles to the bottom.
grazing
feeding used by mobile organisms like snails
when a herbivore feeds on low-growing plants such as grasses or other multicellular organisms, such as algae
filter feeding
Animals that actively filter food particles from the water.
They are a common type of suspension feeder
infaunal
organisms that live IN the substrate
meiofaunal
organisms that live IN BETWEEN the sediments
coarse sediment
(gravel, sand)
large, gritty (sandy bottom)
water drains quickly due to interstitial space
desiccation increases
no organic matter
no cellular respiration, more oxygen
↳food poor; oxygen rich
fine sediment
(silt, clay, both comprise mud)
small, smooth (muddy bottom)
water drains slowly due to little space
desiccation decreases
organic matter trapped
cellular respiration (anaerobic), no oxygen (anoxic)
smelly (hydrogen sulfide)
↳food rich; oxygen poor
drainage
large/coarse - water drains quickly
small/fine - water drains slowly
poorly sorted/mixed - water movement is inefficient (water is blocked)
interstitial space
the small spaces or voids between particles in sediment or rock
anoxic
an environment or condition where there is a complete lack of oxygen.
detritus
the organic material that is dead or decaying, typically derived from plant and animal matter