mfagan

 

BIOL 250

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Ecology

 

textbook UWD1595

 

Marks

  • miderm 25%
  • final 75%

 

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

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