Week 8 Flashcards
How will global climate change affect terrestrial biomes
migration will occur
it will occur at different rates because organisms move at different rates
Four key physical factors affecting the distribution and abundance of organisms in aquatic biomes
salinity
water depth
water flow
nutrient availability
Salinity as a factor affecting distrubution
Def: the concentration of solutes
affects water balance of organisms (OSMOSIS)
Water depth as a factor affecting distribution
water absorbs and scatters light causing turbidity
light required for productivity
Zones of the ocean
Intertidal- consists of rocky shoreline, sandy beach or mud flat exposed to the air at low tide but submerged at high tide
Neritic- extends from intertidal zone to edge of continental shelf
Oceanic zone- Deep water region beyond continental shelf
benthic zone - bottom of ocean at all depths
photic zone - depth where sunlight reaches
aphotic zone- depth where sunlight does not reach
Zones of Lakes
litteral zone- along shore in regions that are shallow enough form plants to take root
Limnetic Zone- offshore region where enough sunlight for photosynthesis
Also contains photic and aphotic zones, as well as benthic zone
Water flow as a mechanism of distrubution
-flow rate can determine how much oxygen is available
-can determine body shapes or behavioral adaptations of organisms
Nutrient availability as a mechanism of distrubution
photic zone has the most sunlight but nutrients are limited
-when organisms die they sink to the benthic zones
-organisms in the benthic zone survive by consuming materials from the photic zone
Where does the photic zone get nutrients
coastal runoff
ocean upwelling
lake turnover
How does ocean upwelling work
- along the coast, the prevailing winds blow moving water at surface
- As the earth rotates, the moving surface water is forced offshore
- as the surface water leaves, it is replaced by nutrient-laden water welling up form the bottom
How does lake turn over work
- winter stratification - dense water at bottom, ice rests on top
- Spring turnover - surface water warms to 4 and sinks
- summer stratification - cooler water at the bottom, warmer water at the top
- Fall turnover - surface water cools to 4 and sinks
Population density
Number of individuals per unit area - varies throughout the range
Types of distributions
Random, Clumped, Uniform
Random distributions
if the position of each individual is independent of the others
Clumped distributions
a patchy habitat or the organisms are social