tropical rainforest Flashcards
general facts
20-28 degrees
2000 mm
convectional rainfall
covers only 5% but supports over 50% of biotic species
soil moisture budget
balance between inputs and outputs is high because precipitation is higher than potential evaporation
latosol
high in metal oxides like aluminum
nutrient poor
quick decomposition - ideal microclimate for bacteria
all year growing season - nutrients continuously recycled and reabsorbed
– leaching by heavy rainfall
layers of the rainforest
emergent
main canopy
under canopy
shrub layer
emergent layer
buttress routes - withstand strong winds
30-35m high
example: mahogany
main canopy
continuous layer of trees
most productive layer
dense leaves create shade – prevent sunlight reaching lower layers increases competition
under canopy
younger trees that aren’t fully grown
only survive if there are breaks in the canopy
only recieve about 10% of sunlight
example: lianas - form green corridors
shrubs layer
little sunlight
have large leaves to absorb as much sunlight as possible
drip tips - adaptations
waxy leaves with pointed tips that channel water so it runs off
ensure it does not break off or grow mold
abscission - adaptations
leaves fall yearly to allow the trees and plants to grow all year long
epiphytes - adapatations
lianas that climb up trees to reach the sunlight - also form bridges across the canopy which allow animals to move around
orchids - hold water in the canopy and prevent further soil leaching
sloths - adaptations
slow moving saves energy
algae grown on fur - helps with camouflage
long claws which help them to hang from tall trees and lianas
anteaters - adaptations
under the canopy - low light conditions - adapted a good sense of smell
characteristics of the rainforest
low latitudes within the tropics
low diurnal range at 5 degrees
no seasons - wet and hot all year round
88% humidity
high biodiversity 50%
nutrient cycling
continual yearly growing season
fast recycling of nutrients
– loose leaves all year round
– rapid decomposition due to optimal bacterial conditions
– plants grow quickly when light breaks through the main canopy so nutrient uptake is rapid
leads to large biomass
small litter and soil
npp in rainforests
very high
humus
organic component of soil that helps retain moisture and nutrients
composed mostly of organic plant matter
how does climate impacts the soil
parent rock type can remain the same but different climatic conditions create different soils
high temperatures - determines the rate of chemical and biological decay and influences humification (the formation of humus)
results in a deep profile with many well developed horizons
aerated soils
soils with pore spaces has a rich brown colour
soil texture
determines permeability
smaller mineral particles = decreased permeability
clay - compact and lacks pore space
soils with ample pore space will allow roots to develop and support vegitation growth
soil moisture budget
high - precipitation exceeds potential evapotranspiration
short time lapse between rainfall peaks - never reaches a deficit
water surplus all year round
soil importance
important factor in the development of vegitation that has driven ecological change and succession
completely reliant on the rainforest to remain fertile - deforested: nutrient leaches and humus is no longer being replaced
mining of minerals - human impact
large scale deforestation strips the soil of nutrients and exposes it to erosion
water clogged with silt leads to downstream flooding
eg: carajas, brazil
agricultural practices - human impacts
slash and burn creates pasture for grazing
single cash crops like soy create a monocultural environment - decreases biodiversity and increases vulnerability to ecological change