Ch2 Flashcards
(32 cards)
Turnover
time for water reservoir to renew
- atmosphere 9days
- river 12-20 days
- lake - days-centuries
- oceans 3100 years
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
- epipelagic = 0:200m
- mesophelagic = 200-1000m
- bathypelagic = 1000-4000m
- abyssal = 4000-6000m
- hadal = 6000m (O2 levels higher, fewer organisms)
Benthic
Habitat on bottom of ocean
Pelagic
Habitat off bottom of ocean
Ocean Light
80% absorbed in first 10m
- very little penetrates past 600m
- leaves 3400m deep = black water
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
- thermocline: rapid temperature change with depth causing thermal stratification
Ocean water movement
- always mpving
- deep water current make upwellings
Ocean Salinity
Decreases close to the equator due to precipitation>Evaporation
- increases in subtropics
- uniform proportions of major ions (Ca2+, Mg2+)
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
- overharvesting
- dumping
- plastic
Coral reefs
in shallow marine waters
- fringing reef = corals growing around young islands from a fringing reef
- barrier reef = as island subsides. corals continue to grow upward and outward towards the sea forming a barrier
- atoll = as island subsides, coral growth will from an atoll on top of island when it has subdivided completely below sea level
Reefs and kelp beds
- sufficient light
- limited by temp
- currents bring o2 and nutrients and remove waste = flushing
Waves and ties of marine shores/intertidal
waves and tides most important
- semidiurnal = 2 high tides and 2 low tides
- diurnal = 1 high tide and 1 low tide
Marine shores/Intertidal
- where amphibious life adapted
- tolerance to air exposure causes zonation
- accessibility increasing = exploitation inceases
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
- tides and river
- organisms, nutrients, O2
- remove waste
- vulnerable
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