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Ecosystems
species
group of individuals able to produce fertile offspring
ecosystem
how living & non-living organisms interact with e/o in a habitat
community
all the living organisms in an area
population
the # of organisms within the same species living in a habitat
biomass
the total mass of organisms in a given area
abiotic factors definition
non-living chemicals & physical factors influencing the living components of an ecosystem
3 main abiotic factors
soil
physical aspect
climactic factors
soil
pH determines type of plants
diff water capacity/air content
humus(dead organic matter) influences nutrients
climactic factors + effects (4)
light(germination, growth, photosynthesis)
temperature(enzymes, hibernation)
wind (water loss, pollination)
water
biotic factors
how living components interact with each other in an ecosystem
producers
the only living things using inorganic(non-carbon based) substances to make carbs
competition
the organism best adapted to compete for resources they need will win competition & survive
intraspecific competition
between individuals of the same species
i.e. mates
interspecific competition
between individuals of different species
i.e. prey, light intensity, water
mutualism
mutually beneficial interspecies co-operation
symbiosis
if both species cannot survive w/o e/o when mutualism is unavailable
parasitism
interspecies where host doesn’t benefit
predator-prey relationship graph
here, prey # higher than predator #, leading to higher peaks

prey-predator relationship simplified
prey # increase, predator # increase(from food source » mating » offspring)
more comp from hunting, predator # decrease
prey # increases again
carbon cycle
the movement of carbon from living things into earth’s atmosphere & back
importance of carbon
main component of all living cells
can form polymers(bases of fats, carbs & nucleic acids)
fuel component
carbon cycle diagram

CO2 atmospheric » photosynthesis
6CO2 + 6H2O » C6H12O6 + 6O2
producers(photosynthesis) » animals
consumption » eat » digest » monomers synthesize their own molecules
aerobic respiration (releases CO2)
poo and death
» decomposers
producers(photosynthesis)
aerobic respiration (releases CO2)
death
» decomposers
decomposers
break down of dead materials by bacteria & fungi » releases CO2
fossilization
dead material not broken down from fossils becoming fossil fuels
combustion, burned to release CO2
the water cycle
the continuous movement of water on, above & below the surface of the earth
1 reservoir to another (river to ocean)
requires exchange of heat(solid, liquid, gas)
importance of water
maintains habitats & transports nutrients
all organisms take in water
precipitation
condensed water falling to the earth’s surface
evapotranspiration
total of all evaporation + transpiration
advection
movement of water in any state through the atmosphere
percolation
water flows horizontally through soil & rocks due to gravity
runoff
variety of ways water moves across the land
can evaporate/infiltrate ground otw
human activities influencing water cycle
agriculture
urbanization
deforestation
decomposers
break down dead organic material by releasing extra-cellular enzymes
broken down into soluble material
detritivores
small animals that speed up decomposition into small pieces to increase SA (thus site of reaction)
3 factors affecting rate of decay
temp
O2
water
temperature’s effect on RoDecay
high temp denatures enzymes & proteins
low temp slows enzyme RoR preventing growth & reproduction
O2 effect on RoDecay
oxygen needed for aerobic respiration, lack thereof = no decay
water effect on RoDecay
water for transport of nutrients
helps digestion inside organisms
no water = slow
rate of decay
proportion of a material that decays in a given period of time
use comparatives!
rate of decay equation
(g/day) = change in mass(g) / time(days)
large # = high RoDecay
nitrogen fixing definition + 3 diff types
nitrogen » nitrates
in the soil
legumes
lighting- in the air
nitrogen fixing(in the soil)
nitrogen fixing bacteria in the soil converts nitrogen to nitrates in the soil, which is taken up by the roots of a plant
nitrogen fixing(legumes)
root nodules containing rhizobium(bacteria) converts nitrogen into nitrates directly
the bacteria uses sugar from the roots, mutualism
nitrification
ammonia » nitrites » nitrates
ammonia = poo & death, by nitrifying bacteria
NH4+ » NO2- » NO3-
denitrification
nitrates converted into nitrogen gas via denitrifying bacteria
NO3- » N2
nitrogen cycle diagram

trophic levels
feeding levels in a food web
same level = same nutritional relationship to primary source of energy
always starts /w producers
limitations of the foodchain
doesn’t show biomass & # of organisms
arrows = energy direction
limitations of pyramid of numbers
# of organisms not always equal to biomass
pyramid of biomass drawing rules + example
produces always on bottom
always symmetrical(height is same for all, width = value)
draw the scale & adapt scale to values
MUST LABEL

energy transfer
energy transferred between trophic levels when an organism is eaten
not all energy transferred = biomass decrease overall
how energy is lost between trophic levels
not all parts eaten
heat to surroundings
movement
growth & repair
death » detrivores
calculations of efficiency
trophic levels are limited as energy can’t sustain another population (more energy hunting than received)
only 1% of energy from the sun is transferred into biomass
10% between trophic levels