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Flashcards about salt marshes
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Saltmarsh
Herbaceous vascular vegetation on sheltered particulate shores between consisting of plants of terrestrial originThese plants are adapted to saline conditions and can tolerate periodic inundation by seawater.
Saltmarshes As Coastal Defenses
Saltmarshes dissipate wave energy, reduces damage to, and overtopping of, sea walls, can allow shorter sea walls
Importance of Saltmarshes in primary productivity
Very high primary productivity, most productivity is exported as detritus to food webs in adjacent habitats, habitat to nationally rare species.
Habitat for Birds
Saltmarshes provide convenient (close to food) and relatively undisturbed roosting areas for waders (especially on neap tides from spring to august where upper marshes are not reached by the tide)
Nereis diversicolor
A polychaete that lives in Saltmarshes. Eats diatoms, seeds and seedlings, plankton and small invertebrates. This increases with high pollution levels/eutrophication and can lead to saltmarsh collapse
Carcinus maenas
Larger invertebrates tunnel into the banks of creeks in salt marshes
Fishes in Saltmarshes
Fishes use saltmarshes, especially creeks. e.g. 0 group bass feed only when in saltmarsh or mudflat habitats.
Formation of Saltmarshes
Saltmarshes are assumed to form through facilitated succession. Sand/mudflat with benthic diatoms – secrete EPS (extracellular polymeric substances) that bind and stabilise the sediment. Pioneer zone vascular plant species (e.g. Salicornia europaea) grow here where they cause further sediimentation and stabilisation allowing secondary succession etc
Saltmarsh Vertical Zonation
Plants show a vertical zonation. Lower limit is dependent on their tolerance to environmental factors (esp. salinity) and the upper by interspecific competition.
Saltmarsh Erosion
Saltmarshes are disappearing rapidly with annual losses of 1-2% worldwide.
Causes of Saltmarsh Erosion
Land claim (reclamation) and erosion suggested to be due to nutrient pollution.
Creek Erosion
Nutrient pollution leads to a decrease in root biomass, increase in above-ground biomass, and increased vulnerability of plants to herbivores. Led to collapse of creek banks; saltmarsh converted to mudflat.
Nereis increase
Nereis are more abundant, and their rates of deposit feeding higher, at the saltmarsh-mudflat interface, because of nutrient enrichment, leading to loss of saltmarsh vegetation.
Nereis exclusion
Nereis exclusion experiments demonstrate absence of pioneer zone vegetation where the sediment is high enough is due to bioturbation and herbivory (they eat seeds and seedlings).
Progradation
is the advancement of a coastline due to the accumulation of sediment, often influenced by natural processes and can impact salt marsh formation.
Parts of a salt marsh
mudflat, pioneer zone, low marsh, upper marsh, transition zone, creeks, cliffs, pans
Deposit feeding
encouraged by eutrophication, deposit feeding refers to the ingestion of sediments and organic matter from the bottom of aquatic environments by benthic organisms.