The slowing of wave (action) (and) currents means
that seagrass beds tend to accumulate sediment.
However,
this is not universal
and depends
on (the) currents
under which the bed exists.
Seagrass beds
under the influence (of) strong currents
tend to have many of (the) lighter particles,
including seagrass (debris,)
moved out,
whereas beds
in weak current (areas)
accumulate (lighter detrital) material.
It is interesting
that temperate seagrass beds accumulate sediments
from sources outside the beds,
whereas tropical seagrass beds
derive most (of) their sediments from within.
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