BIOMES L27 Flashcards
I. Earth's Climate - CC micro, microclimate - SEQ, HD climate change II. Terrestrial biomes - CC features III. Aquatic biomes - CC features - CC aquatic biomes
climate
- long term prevailing weather conditions in an area
- most important influence on species distribution
macroclimate
- global climate patterns
- driven by solar E and movement of Earth in space – temp, wind
solar E
- varies by latitude
- tropics: direct sunlight, most heat, light, E
- higher latitudes: less E, cooler
global air circulation
- starts near equator
- air heated
- rises, flows towards poles
- cools, releases water
- lots of rain in tropics
water
- ocean currents influence climate along coasts
- heat or cool air – passes across land
- high specific heat – can moderate temp of nearby land
mountains
- influence air flow – precipitation – biodiversity
- mountain direction affects sunlight – temp, rainfall
microclimate
- can be influenced by features of local environment
- ex. tree, rotting log, rock
global climate change
- large scale changes in climate
- affects biosphere
- due to increasing CO2 and other gases
- result of burning fossil fuels, deforestation
effects of climate change
- changes to biomes, ocean currents, geographic ranges
biome
- major life zone characterized by vegetation (terrestrial) or physical environment (aquatic)
climograph
- plot of annual mean temp and precipitation in a region
- method of correlating climate and biomes
ecotone
- area of intergradation between adjacent biomes
- transition area
vertical layering of vegetation
- provides diverse habitats – supports different animals
- ex. forests
freshwater aquatic biome
- <0.1% salt
- closely linked to surrounding terrestrial biome
- influenced by patterns and speed of water flow
saltwater marine biome
- average 3% salt
- mostly oceans
zonation
- physical and chemical stratification
- vertical and horizontal
vertical stratification
- light
- benthic zone
- thermocline
light
- H2O selectively reflects and absorbs certain wavelengths
- absorbed by water and photosynthetic organisms
- photic and aphotic zones
photic zone
- upper layer
- sufficient light for photosynthesis
aphotic zone
- little/no light
- not enough to do photosynthesis
benthic zone
- bottom of all aquatic zones
- sand, organic and inorganic sediments
- detritus is food source
- falls from photic zone
thermocline
- narrow layer of abrupt temp change
- surface warmer from sunlight
- deeper water remains cold
horizontal zonation
- zones differ by water depth
- affects microclimate
- drives community diversity
oligotrophic lakes
- nutrient poor
- usually O2 rich
- low amount of organic matter in sediments
eutrophic lakes
- nutrient rich
- often O2 depleted
- high amount of organic matter in sediments