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definition
- partially enclosed coastal body of brackish water with one or more rivers or streams flowing into it, and with free connection to the open sea
geologic: drowned river valley
- sea level rise
- much wider than deep
- V shaper cross sections
- unobstructed sea connection
geologic: bar built
- mixed zone somewhat separated from sea by sand spits or barrier islands
- = "semi-enclosed"
= sedimentation = high
geologic: fjord (glacial)
pleistocene glaciers deepened existing rivers
- width:depth = small
- steep sides and u shaped cross sections
- mouths = sill (glacial deposits)
geologic: tectonic
- geologic subsidence associated with faults
- san fran bay
less dense water means
inflowing freshwater
salt-wedge estuary
- freshwater flow larger than marine input
- less dense freshwater flows on top and thins as it mixes forming a wedge (depends on flow)
- strong halocline
- mouth = same as river flow
partially mixed estuary
- freshwater flow moderate and moderate tidal influence
- bottom sediments: friction stress and salinity changes
- volume of water flowing out of mouth >> river flow
well mixed estuary
- broad shallow estuary with strong tides
-- no halocline
-- strong horizontal salinity gradient river
-- wide basin means coriolis force significant
negative circulation
- common along arabian gulf
- low FW inputs
- seawater flows in at he surface
- high evap at head of estuary --> hypersaline
estuaries are at the top of
unit value
what are the adaptations for salinity variations
- physiology (osmoregulators and osmoconformers)
- avoidance behavior
- life histories
avoidance behavior
- moves as tides flow
- find less variable habitat in the sediments
- most molluscs able to clam up to avoid suboptimal conditions
life history adaptations
- anadromy (lamprey and salmon, migrate to freshwater to reproduce)
- catadromy (eels, migrate to ocean to reproduce)
property:property plots
- salinity is approximately 'conservative' in estuaries (mixing of freshwater and saltwater)
- net source v net sink
- freshwater --> marine
mixing diagrams
easy way to understand what is happening to a substance as it flows through estuary
ETM (estuarine turbidity maxima)
- common feature
- very fine sediments in rivers hits saltier water --> flocculation
- very light sediments easily disturbed by inflowing seawater
estuary productivity
- most productive natural ecosystems in the world
- due to 3 types of primary producers (phytoplankton, benthic algae, marsh grasses)
- ebb and flow of tides
- nutrients from rivers
- year round productivity
- 2K
what are some energy sources from estuaries
- autochthonous NPP
- allochthonous (DOM and POM)
phytoplankton NPP
- rarely nutrient limited due to rivers and tides
- LIMITED by light and flushing out
benthic algae NPP
- mudflats form in estuaries with large tidal range
- very rich habitat
- birds feed during low tides
most estuaries are heavily dominated by
detrital energy flow
threats to estuaries: human devo
- 7/10 largest cities= on an estuary
- 13% land mass, 40% human pop
threats to estuaries: pollution
- sewage
- shipping centers= industrial centers
- cole matson lab = evolutionary adaptation to pollution
threats to estuaries: non-indigenous species
- transportation centers
- brackish water species can travel better
- brackish water= few species, so higher potential of establishment
threats to estuaries: altered hydrology
dams
- keep seawater out
- no tides= pastures
- pooled water
reduced river flow --> increased salinity