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 | Estuarine
Communities 
1. Saltmarsh Community
(intertidal)
Estuaries
are among the most productive marine ecosystems with high biomass of benthic
algae, seagrass and phytoplankton
Nutrients
are imported from land, but also retained within the estuary
Sequence
of communities: saltmarsh, seagrass bed, mudflat/sand,
pelagic
   
Salinity
gradient: mixture of freshwater and marine
organisms, only few real brackish-water species; diversity lowest in brackish
water (5-10‰)
  
2. Seagrass bed (inter-
to subtidal)
Dominated
by marshgrasses (flow- ering plants) as high as 2 m, which trap nutrient-rich
sediments
most
plant tissues are not grazed but get into detrital food web
slow
decay and deep sediment, saltmarshes growh upwards, eventually filling
the estuary and becoming land
  
3. Mud/Sandflats
Eelgrass
(temperate) and Turtlegrass (tropical)
few seaweeds,
which do not grow well on muddy sediment
many
epiphytic diatoms on seagrass contribute to primary production and serve
as food for snails
habitat
for sessile animals (hydroids)
seagrass
biomass ends up in detritus
manatees
and sea turtles graze Turtlegrass
  
4. Plankton Community
Primary
producers: epipsammic algae, mostly benthic diatoms and dinoflagellates
cyanobacteria
mats on mudflats
production
10% or less of seagrass beds and saltmarshes, decreasing with grain size
of sediment (mud more productive than sand)
macro-
and meiobenthos, often detrivores, living of deposits from seagrasses and
marshes
birds
important grazers
  
5. Mangroves
High production
by nutrients imported by the freshwater inflow
Highest production and 
biomass at intermediate salinities. At head of estuary, nutrient concentrations are high 
but turbidity by sediments suspended in river water is high as well so that phytoplankton 
remains light-limited; as sediments sink out of the water column along the river plume and 
water turbidity decreases, phytoplankton can make use of high nutrient concentrations at 
intermediate salinities.
benthic
filter-feeders profit from plankton production
high sedimentation
of plankton from estuarine plumes can cause oxygen consumption and anoxic
sediments at the seaward edge (even hypoxia in the water; for example Mississippi River plume)
 
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