BEE Flashcards
(169 cards)
Chemosynthesis
Process of producing organic molecules using the oxidation of inorganic molecules, involving in electron donors and water or oxygen molecules
Problems of Herbivores
- Acquiring lack of protein and acquiring too much-sugar
- Carbon removed via metabolism
- Sugars may also be excreted from the body
Ecosystem dynamics
Changes within a system; infuenced by state factors and interactive controls
State factors and Interactive controls
- State factors: climate, soil/parent material, topography (the altitude of the ecosystem), potential biota (potential maximum growth of population), time; determine biomes in a broad scale
- Interactive controls: resources (energy from sunlight and matter/nutrients and micro-mineral — animals only need a small amount of these, modulators (physical and chemical properties of the ecosystem), human activities, disturbance regime including flood, fire and storm, biotic communities (functional types within a community)
Toposequence
Looking/studying for patterns of organisms living in certain altitudes
Chronosequence
Looking/studying for patterns of organisms living in different time periods
Ecological succession
Structure of biological communities over time
Primary succession
Formation of community from nothing
Secondary succession
Formation of community after another is destroyed
Rock cycle
Igneous (from magma), sedimentary rock (small pieces formed from weathering), then Metamorphic rocks (heat and pressure)
Weathering
Formation of sediments, a key component of soil
Physical Weathering
Frost wedging/freeze thaw, Thermal expansion or isolation leading to exofoliation
Chemical Weathering
Oxidation, carbonation, hydrolysis, hydration, solution (Together 5)
Soil profile
On a deck of Andy’s silty classy mint from Sainsbury, leans an Egg Battered acutely after Castrations
Cation-exchange capacity
Number of exchangeable cations per dry weight that a soil is capable of holding, at a given pH value, and available for exchange with the soil water solution.
Climate
Amount of raindrop + temperature
Direct solar radiation/ Diffused solar radiation and their effects on differing latitude
- Solar radiation traveling on a straight line from the sun down to the surface of the earth.
- Solar radiation reaching the Earth’s surface after having been scattered from the direct solar beam by molecules or suspensoids in the atmosphere
Latitude
A geographic coordinate that specifies the north–south position of a point on the Earth’s surface
Tilt earth’s influences
- Seasonality
2. Non-syncing seasonality of north and south hemisphere
Latitudinal atmosphere circulation and biome formation
- Warm air rises at ITZC via maximum solar input and moist air descends 30 degrees N and S, leading to formation of frequent rain and formation of rainforests
- Formation of desserts with dry wind after the deposition of water it once acquired
Formation of tradewinds
Earth spins anti-clockwise, and the wind act against the direction
Being in high altitude
- Lower temperature
2. Higher rainfall
Land cover’s influence on climate
- Albedo, fraction of solar energy (shortwave radiation) reflected from the Earth back into space. e.g. Ice, ocean, vegetation
- Evapotranspiration, water is transferred from the land to the atmosphere by evaporation from the soil, other surfaces and by transpiration from plants, to remove heat
Causes of long term variation
- Milankovitch cycles
Orbital eccentricity: two forms, elliptical and circular orbit, cycle once every 100,000 years
Precession: Earth’s axis itself rotating on another axis; cycle once every 21,000 years (think wobble of Gyro as it is about to stop)
Axial tilt: angle variation Earth’s obliquity oscillates between 22.1 and 24.5 degrees on a 41,000-year cycle - Interannual climate variation
- El-Nino-southern Oscillation: Easterly trade wind does not pushs warm water to the normal direction, leading to drought