|
The
intertidal habitats consist of unvegetated creek banks and mud flats,
including small tidal creeks that drain completely at low tide,
and the vegetated marsh surface, which contains several distinct
zones (see figure above). Plant zonation is controlled by a combination
of interacting factors including elevation and hydrology.
Although
the marsh surface is covered by water less than half of each tidal
cycle, there is a perched water table which maintains the sediments
of all but the highest intertidal elevations in a near waterlogged
condition. Near creek channels the hydraulic head created by difference
in the level of the water table and water level in the channel results
in a slow seepage of interstitial water through the creekbanks into
the channels. At a distance from the creeks, however, there is little
subsurface water movement except that due to water loss near the
surface via evaporation and transpiration. That water is replenished
by the subsequent flood tide, but the difference in water exchange
near creeks and at a distance from them results in large and constant
differences in redox potential, salinity, sulfide concentration
and plant productivity.
more
on marshes
|
|