1/21
Looks like no tags are added yet.
Name | Mastery | Learn | Test | Matching | Spaced |
---|
No study sessions yet.
definition of succession
how the species composition of an ecosystem changes in time
comparable characteristics of succession
dynamic
temporal - long time periods
progressive changes over time
definition of zonation
how an ecosystem changes along an environmental gradient (e.g. altitude)
comparable characteristic of zonation
spacial
static
caused by an abiotic gradient
seral stage: bare, inorganic surface
soil = mineral particles
nutrient poor
erratic water supply
e.g. eruptions, sand dunes
seral stage 1 - colonisation
pioneer species adapt to extreme conditions
usually r species
soil starts from dust/windblown particles
seral stage 2 - establishment
species diversity increases
invertebrates visit
humus increases
weathering of rock increases nutrients
seral stage 3 - competition
microclimate changes as new species colonise
larger plants provide shade
shelter enables K species to establish
abiotic factors start to stabilise
pioneer species are out-competed
seral stage 4 - stabilisation
arrival rate of new species decreases
narrowing niches
more complex food webs
seral stage 5 - climax community
stable, self-perpeptuating
dynamic equilibrium
maximum possible development under abiotic factors
human impacts on succession
can divert succession to plagioclimax community through
burning
agriculture
grazing pressure
resource extraction
direct & indirect impacts
change abiotic & biotic components
impact depends on ecosystem’s reslience
definition of resilience
ability of an ecosystem to recover from a disturbance & return to its natural state
biotic changes during succession
size of organisms increases
biodiversity increases
niches appear
species diversity increases then falls
NPP & GPP rise then fall
productivity & respiration ratio falls
energy flow becomes more complex
abiotic changes during succession
following increase:
soil depth
humus
water capacity
mineral content & cycling
hydrosere
succession in water
continuous sediment input from streams/lakes
build allows rooted plants to invade
secondary succession
occurs when established community is destroyed
e.g. natural disasters, plowing
shortened number of seral stages as components already established
5 major types of biome
aquatic
forest
grassland
desert
tundra
definition of biomes
large-scale ecological communities that are characterised by their dominant vegetation, climate, and other abiotic factors that shape their biotic communitie
description of the Hadley Cell
largest
equator → 40° north and south
trade winds blow easterly
trade winds meet at equator, hot air rises
tropical storms are formed
air flows from the stop of the storms to higher latitudes
it becomes cooler & sinks over subtropical regions
this = dry, cloudless air, warmed by the sun as it descends
description of Ferrel Cell
middle cell
edge of Hadley → 70° north and south
joins sinking air of Hadley cell which travels close to earth until it rises at border of polar cell
accounts for frequent, unsettled weather
description of Polar Cell
smallest & weakest
edge of Ferrel → poles
cold air sinks = high pressure
cold air flows towards lower latitudes
warms & returns at altitude to poles
role of global atmospheric circulation model
Air moves from high → low pressure, generating wind
Wind = large scale movements of air due to air pressure difference
This pressure is due to uneven insolation
hot air rises
cool air sinks
this creates pressure cells