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BIOL 250
Page history last edited by Anonymous 3 yrs ago
Ecology
textbook UWD1595
Marks
intro
- ecology: scientific study of relationships(with world, same/diff species) between organisms and their environment(physical/biological); multidisciplinary etc
- field and/or lab experiments
- large or small scales in space and time
- natural history: study of how an area's organisms are affected by climate/soil/predators/competitors/evolutionary history via field analysis
- climate diagrams: temperature (left axis) and precipitation (right axis) over time, plus other stuff
on land
- biome: major division (via diff wildlife, climate) of land
- tropical rain forest: (<10 latitude) soil poor as water leaches nutrients, organic stuff decomposes quickly
- tropical dry forest: (10-25 latitude) most trees dormant in dry season (1/2 year)
- tropical savannah: (10-20 latitude) seasonal drought, fire (with first rain), impermeable soil; few trees unlike rainforest so 2Dish, nomadic wildlife
- desert: drought, (30 latitude; 20% of Earth's land) flash floods, heat, bitter cold; cold when wet (huh??); leaves small/angled/reflective to reduce heat; animals deal via behaviour
- temperate woodland/shrubland: (30-40 latitude) usually hot/dry summer otherwise cool/moist, fires frequent so thick/tough barked trees and fast resprouting shrubs and some grow just during moist/wet time
- temperate grassland: flat prarie; wetter than desert but sometimes drought; winters cold and summers hot; fires
- temperate forest
- boreal forest
- tundra
- mountains
- soil structure affected by
- climate: rates of weathering of parent material, leaching, erosion, particle transport, decomposition, also wildlife
- organisms: organic matter, burrowing animals' soil mixing
- topography: rate/direction of water flow, erosion
- parent material (part above bedrock): duh
- time: duh
- latitude/season climate diff due to uneven heating of Earth by sun + axis tilt; biomes due to this (especially temperature/precipitation)
- three air circulation cells per hemisphere needs work here
in water
- 71% of Earth: 97% ocean, 2% ice caps/glaciers, <1% fresh; most of terrestrial life needs freshwater
- biology environments due to light/temperature/water movement/chemistry(salinity/oxygen)
temperature
- microclimate (few kms to cms; hours to mins) = macroclimate + local landscape (altitude-temperature, topographic/etc-shade, albedo-temperature)
- varies less in water since high heat capacity; much heat absorbed during evaporation, given off during freezing (high latent heat of vapourization and fusion)
- species need specific narrow temperature range
- photosynthesis CO2+12H2O --light energy, chlorophyll--> C6H12O6+6O2+6H2O
- acclimation: short-term physiological adjustment to environment, reversible
organisms' heat balance
- heat gain: metabolism (due to cell respiration)
- heat gain/loss: conduction, convection (between fluids), electromagnetic radiation, evaporation
- poikilothermic (temp varies with environment) ectotherms (external sources of heat) = "cold blooded"
- low metabolic rate, high thermal conductance with environmnet; most energy production from anaerobic respiration (depletes stored energy) so only short energy bursts (3-5 mins)
- can allocate more energy to growth (although not too big as hard to exchange heat fast); can lower metabolism during harsh conditions (better extreme survival)
- homeothermic (constant temp) endotherms (internal (metabolic) heat) = "warm blooded"; some fish and insects heat critical organs
- rely on insulation, evaporative cooling, changing metabolism
- less energy for growth, small organisms use more metabolic activity per mass relatively
- aquatic endothermy: high conductive/convective heat loss so few species; heavy insulation (blubber=fat), countercurrent heat exchange in dolphin fins etc
- plants: in desert minimize heat via narrow, reflective leaves that dont touch the ground and open to wind; in arctic dense (no wind) and close to ground etc
- avoid extremes via resting: inactivity or reduced metabolism:
- torpor: short term (eg 1 day/night) eg hummingbird if scarce nectar
- hibernation: dormant state during winter
- estivation: dorman state during summer
water
- challenges: water loss (in desert, salt water), dilution of body fluid (in fresh water); water balance related to thermal balance (evaporative cooling)
- water moves from low to high concentration areas, rate depends on concentration diff
- terrestrial evaporation form organism depends on temperature, water content
- measure water vapour via density or pressure; relative humidity = water vapour density / saturation density; saturation density proportional to temperature
- vapour pressure deficit (vpd) = X water pressure (of air) - Y water pressure (??)
- aquatic: solutes inversely proprotional to water; increasing solutes is freshwater, ocean, saline lakes
- osmosis: water diffusion; osmotic pressure: across semi=permeable membrane due to water moving down concentration gradient; organisms are:
- isomotic: everything equal
- hyperosmotic: osmosis to internal
- hypoosmotic: osmosis to external
- water potential: capacity of water to do work = its free energy content; water flows to lower energy; water (inversely?) potential proportional to solute content
- pure water is 0 Pa, so stuff in nature is -# Pa; dry air=-100Pa; top of plant=-4Pa; soil -0.6Pa
- plants: water potential increases upwards
- qualified potential gradient mechanisms: evaporation, matric forces, solutes; hydrogen bonding in water means that evaporation from leaves pulls up more water
water regulation
- animals on land: gain (drinking, food (moisture+metabolic), absorption) - loss (evaporation, secretion/excretion)
- plants on land: gain (roots, air absorption) - loss (transpiration, secretion/reproductive structures(eg seeds))
- absorbing water from air important mostly for (??)
- metabolic water: oxidizes carbohydrates, protiens, fats via aerobic respiration (reverse of photosynthesis)
- C6H12O6+6O2 --> 6CO2+6H2O
- plants' root:shoot biomass ratio goes up for dry places
- animals reduce loss via waterproofing (eg wax), concentrated excrement, condense+reclaim vapour in breath, inactivity (eg diapause=arrested development stage mostly in insects)
argh need to put stuff in here :-(
- energy sources: light, organic stuff, inorganic stuff
- stomata exchange CO2 and O2
- diffusion of CO2 into (slower) and H2O out of (transpiration-faster)leaves
- photosynthetic pathways related to water stress
- branches have lower nitrogen
A
1 false
2 true
3 false
4 false
B
5 d
6 c
7 d
8 a
9 b
10 b
11 ?
12 e
13 bla
14 bla
15 phenotype
16 endotherm? read slides bla
17 osmosis
18 for a home ?
19 nutrients washed away, some other thing that i forget, it's in my own notes
20 tilt on our axis, spin on axis, move along orbit
21 stuff looking like other stuff, presumably
22 more leaf-growing?
- macronutrients C O H N P = 93%+ of biomass
- herbivore problem: plants have relatively C>N, but ratio is better "farther from trunk"; dead anything is even worse
- mimicry: mullerian when animals are also noxious, but batesian when actually harmless
BIOL 250
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