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Upper intertidal
drier habitat with crabs and birds
Lower intertidal
less dry habitat with clams and worms
gravel, sand, silt/clay, mud
sediment classified by size, biggest to smallest
wave action
what results in smaller grain sizes of sediment further away from shore
well sorted (coarse)
all large grain size so water drains quickly
greater O2 availability, animals dry faster
positives of well sorted (coarse)
less detritus, shifting rocks create instability
negative of well sorted (coarse)
well sorted (fine)
all small grain size, water drains slowly
more detritus builds up
positive of well sorted (fine)
harder to burrow, dries slower, less O2 available
negatives of well sorted (fine)
poorly sorted
all different grain sizes with little to no draining of water
dig-and-pull
muscular foot that expands and contracts to burrow in sediment
digging
moving particle grains out of the way, and sometimes eating it as they burrow
meiofauna
live between sediment grains due to small body size
bioturbation
burrowing activity that can alter the physical and chemical characteristics of sediments
siphon and increased hemoglobin
adaptations for animals to live within sediment
detritus (decomposing organic material)
main food source of organisms in sediment
primary and secondary producers
suspension feeders role