Lec 5- aquatic biomes Flashcards
(39 cards)
biomes
- way of categorizing ecosystems
- distinguished by dominant plants and climates (terrestrial) or movement and physical properties of water (aquatic)
kinds of marine biomes (5)
ocean/salty
- open ocean
- deep ocean and thermal vents
- kelp forests and coral gardens
- intertidal
- salt marshes and mangroves
open ocean
pelagic
deep ocean
benthic
intertidal
littoral
kinds of aquatic biomes
freshwater
- lakes
- rives and streams
- wetlands
lakes
lentic
rivers and streams
lotic
aquatic sys in Canada (8)
ocean
- open ocean, kelp forests, intertidal zone, estuaries (salt marshes and mangroves)
- lakes
- ponds
- rivers
- streams
- wetlands
- bogs
- fens
Oceans
70% of world
zones:
- littoral (intertidal) zone
- neritic zone
- oceanic (pelagic) zone
- zonation of habitat: benthic and pelagic
littoral zone
shallow shoreline, under influence of tides
neritic zone
coast to margin of continental shelf
oceanic zone
beyond continental shelf
- epipelagic 0-200
- mesopelagic 200-1000
- bathypelagic 1000-4000
- abyssal 4000-6000
- hadal 6000+
benthic
habitat at bottom of ocean
pelagic
habitat off the bottom, in open water
open ocean
pelagic
physical: light and temp dependent on depth, gyres, light decreases w depth
chemical: salty, o2 concentration correlated with depth
biological: photic zone, low densities
deep ocean and thermal vents
physical/chemical: chemosynthesis-based ecosystems, no light
biological: highly adapted organisms, little known, hard to study b/c adapted to high pressure
kelp forests and coral reefs
higher latitudes, ocean currents
biomes analogous to terrestrial forest
between Tropics
kelp across rocky shores and eat coast
kelp: 30 degrees latitude or high cooler temp
coral reef/garden: 30 degrees latitude or lower warm temp
- highly vulnerable
- high productive organisms
Ekman spiral
starts at surface then moves down in specific movements
- Coriolis effect and wind move large water masses in vertical fashion
- with increasing depth, forces diminishes and changes direction due to friction in water
- wind directed water movement resembles vertical spiral
- net transport direction will be 90 degrees than surface wind direction
- key to transport of energy
Coastal upwelling
- wind driven off-shore movement of water
- deeper waters replace displaced water nearshore
- deeper waters nutrient-enriched
- kelp forest
intertidal
littoral
- ocean meets land
- rise and fall of tides
physical/chemical: tides, high light, temp closer to air temp, oxygenated
biological: amphibious. part marine and part terrestrial, starfish, mussels, algae
salt marshes and mangroves
- saltwater and freshwater mix
- river into ocean
physical/chemical: highly variable and dynamic like intertidal, salinity fluxes
biological: marshes = grass, mangroves = trees, low diversity but high productivity
lotic ecosystems
rivers and streams- natural channels of moving water, differ in sizes
rivers, streams, creeks/brooks
canals are human-made channels of flowing water integrated into an ecosystem
size depends on substrate, energy, photosynthesis
smaller have higher turbidity and less photosynthetic organisms
rivers
physical/chemical: water moves, turbid, lots of suspended sediment, temp similar to air
biological: fish-variety, macroinvertebrates-benthic invertebrates