Estuarine Shores Flashcards
Global Patterns
More soft sediment beaches in the tropics.
Related to coastal climate, freshwater inflow and glaciation history.
Local patterns
Soft shores are inhabited by mobile epifauna and infauna
Porosity and permeability
Porosity, volume of pore space in between particles.
Permeability, rate of percolation of water through the sediment.
Water content and mud
Water content related to parcel size, beach profile and water table height.
Dilatant sands:
- When pressure applied, the sand becomes dry and hard pack as water driven out of the interstices. Difficult to borrow.
Thixotrophic sands:
- Sands with high clay content, easy to burrow.
Muds:
- Do not drain and saturated with water. Easy to burrow
Oxygen and sediment chemistry
Aerobic bacteria decompose organic material at the surface when oxygen is abundant.
Oxygen consumption at the surface deprives deep layers of oxygen, so sediments below the surface are anaerobic.
Depth of oxygenated layer varies according to grain size, which determines permeability.
As oxygen concentrations diminish with depth anaerobic bacteria start to dominate.
Transition layer between oxygen rich and oxygen poor layers is the redox discontinuity layer.
Burrowing animals generate a respiratory current within their burrows to receive oxygen.
Macrofauna
Generally, no macroalgae, but sometimes see blooms of Enteromorpha and Ulva on mudflats.
Macrofauna: amphipod and arenicola, deposit feeders.
-Shore crab, heart urchin, lanice, cerianthus, sagartia, nereis, grazers.
Meiofauna
Detritus, bacteria and diatom feeders
Food for higher trophic levels
Macrofauna vs particle size
Species richness, abundance and total biomass increase with increasing sediment stability, decreased wave exposure.
Highest in muddy/sheltered habitatts.
Macrofauna vs tidal heigh
Lack of distinct vertical zonation.
Sediments buffer physical stress and the organisms are mobile.
Organisms burrow deeper in the intertidal.
Distribution related to particle size, emersion period, depth of water table.
On sandy shores, zonation schemes have been related to hydrodynamics.
Not just invertebrates
Burrowing fish.
Rays, eels, and band fish.
Evolutionary history of fauna
Cambrian animals primarily lived in the surface and often no more than 10cm depth.
Somehow Ordovician-Devonian fauna created extensive and deep burrows.
However, most Paleozoic fauna are epifaunal.
Infaunalization goes large scale in the Mesozoic.
Biostabilisers
Increase cohesiveness.
Make sediment surface smoother.
Form protective layer over sediment surface.
Bioturbators
Make sediment surface rougher.
Regrade sediment particle structure.
Reduce sediment strength.
Oxygenate sediment.
modify geochemistry profiles.
Often exclude filter feeders.
What is an estuary
Extended interface between a marine and freshwater flowing system.
Estuarine fauna
Invertebrates dominate epifauna and infauna.
Fish typically use estuaries as nursery grounds or move in with tides.
Birds are migratory visitors are all trophic levels.
Plankton, mainly diatoms and dinoflagellates.