Turnover
time for water reservoir to renew
Life in water
Density higher = structure for soft bodied organisms
Buoyancy higher = organisms use lipids/air sacs to stay under pressure
Viscosity higher = more energy to move
Light lower = photosynthesis restricted
Heat conduction higher = difficult to maintain body temp above surrounding temp
Specific heat higher = more stable
Littoral zone
Littoral zone = intertidal shallow zone
Ocean Zone
Benthic
Habitat on bottom of ocean
Pelagic
Habitat off bottom of ocean
Ocean Light
80% absorbed in first 10m
Neritic zone
Neritic zone = coast margin of continental shelf (200m deep)
Ocean Temp
increases velocity of molecules so density decreases with warm water on top and cool water below
Ocean water movement
Ocean Salinity
Decreases close to the equator due to precipitation>Evaporation
Ocean oxygen
increase near surface, decrease to 1000m
increase past 1000m (sometime)
Ocean Biology
Photosynthetic organisms are epipelagic (on top layer)
i. photoplankton/zooplankton
ii. 1/4 of total photosynthesis globally
When no light present organisms will chemosynthesize
Human influences on oceans
Coral reefs
in shallow marine waters
- fringing reef = corals growing around young islands from a fringing reef
Reefs and kelp beds
Waves and ties of marine shores/intertidal
waves and tides most important
Marine shores/Intertidal
Estuaries
river to sea
salt marshes/mangroves
low costs
salt marsh located in northern regions
mangroves located in tropical/subtropical southern regions
Estuaries/salt marshes/mangroves characteristics
Salt marshes and mangroves fluctuations
fluctuations strong and complex for:
- light, temp, O2
- salinity gradient (fresh water will sit on top of salt water until it mixes)
- tides
- primary production
Endemic species
native and only found in one particular area
River and stream - light, water movement, temp
Light
- surface
- water column
Water movement
- cause erosion and suspended sediments
Temperature
- similar to water temp