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Estuarine
Communities
-
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‰)

1. Saltmarsh Community
(intertidal)
-
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

2. Seagrass bed (inter-
to subtidal)
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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
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habitat
for sessile animals (hydroids)
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seagrass
biomass ends up in detritus
-
manatees
and sea turtles graze Turtlegrass

3. Mud/Sandflats
-
Primary
producers: epipsammic algae, mostly benthic diatoms and dinoflagellates
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cyanobacteria
mats on mudflats
-
production
10% or less of seagrass beds and saltmarshes, decreasing with grain size
of sediment (mud more productive than sand)
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macro-
and meiobenthos, often detrivores, living of deposits from seagrasses and
marshes
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birds
important grazers

4. Plankton Community
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High production
by nutrients imported by the freshwater inflow
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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)

5. Mangroves
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