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BIOMES
DESERTS
DESERT BIOME
FLORA
- Wax coated leaves, deep roots
to tap into groundwater,
shallow roots to collect water,
and drop leaves to survive in
dormant state during dry
spells.
- Store biomass in seeds and
remain inac9ve during dry
periods.
germinate, grow, bloom,
produce new seed, and die.
FAUNA
- Hide in cool burrows or rocky
crevices by day & come out at
night
conserving water. Insects and
rep9les have thick outer
coverings and dry feces, dry
urine.
- Spiders get water from dew
and the food they eat
periods of heat
TROPICAL DESERT
Fig. 5-‐12a, p. 109
Tropical Desert
Mean monthly temperature ( ° C) Mean monthly precipitation (mm)
Month
Freezing point
- High temps all year & liCle rain (1 or 2 months per year.)
- Few plants with windblown surface sand.
- Example: Sahara in Africa
POLAR DESERT
Fig. 5-‐12c, p. 109
Polar Desert
Mean monthly precipitation (mm)
Month
Freezing point Mean monthly temperature (°C)
- Winters are cold, summers hot.
- Precipita9on low.
- Example: Gobi in China
TEMPERATE DESERT
FOOD WEB
Fig. 5-‐13, p. 110 Producer to primary consumer Primary to secondary consumer Secondary to higher-‐level consumer All producers and consumers to decomposers Kangaroo rat Diamondback raLlesnake Fungi Bacteria Darkling Beetle Roadrunner Prickly pear cactus Agave Gambel's Quail Collared lizard Jack rabbit Yucca Red-‐tailed hawk
GRASSLANDS
GRASSLANDS AND
CHAPARRAL BIOMES
- Located between 55 N and 30 S
- Grasslands are regions with enough average annual precipita9on to
allow grass to grow. Precipita9on is erra9c and fires prevent large
stands of trees. Most found in interiors of con9nents.
- Grasslands (prairies) occur in areas too moist for desert and too dry for
forests. The cold winters and hot dry summers have deep and fer9le soil
that make them ideal for growing crops and grazing caCle.
- Savannas are tropical grasslands with scaCered tree and herds of
hoofed animals.
- Chaparral has a moderate climate but its dense thickets of spiny shrubs
are subject to periodic fires.
- The cold winters and hot dry summers have deep and fer9le soil that
make them ideal for growing crops and grazing caCle.
TROPICAL GRASSLAND
Fig. 5-‐14a, p. 112
Tropical grassland (savanna)
Mean monthly temperature ( ° C) Mean monthly precipitation (mm)
Month
Freezing point
Savanna: Warm temps year around, prolonged dry season, a lot of rain remainder
of the year. Largest in Africa. Provide grazing and browsing for hoofed animals.
Herbivores have evolved for ea9ng habits that minimize compe99on between
species for vegeta9on.
High temps, low to moderate precip, prolonged dry seasons. Occur on
either side of the equator beyond borders of tropical rainforests.
Fig. 5-‐15, p. 113
Golden eagle
Pronghorn
antelope
Grasshopper
Prairie
Coneflower
Fungi
Bacteria
Prairie
dog
Blue stem
grass
Grasshopper
sparrow
Coyote
Producer to primary consumer Primary to secondary consumer Secondary to higher-‐level consumer All producers and consumers to decomposers
POLAR GRASSLAND
Fig. 5-‐14c, p. 112
Polar grassland (arctic tundra)
Mean monthly temperature ( ° C) Mean monthly precipitation (mm)
Month
Freezing point
Polar grasslands or tundras occur south of the arc9c polar ice cap. Cold, frigid winds,
covered with ice and snow, winters are long and dark. Precip is rare and is mostly snow.
One effect of extreme cold is permafrost: frozen layer of soil. Water near the surface
thaws but permafrost soil layer stays frozen preven9ng liquid water at surface from
seeping into the ground. Soil on upper level remains soggy and forms shallow lakes,
marshes, and wetlands Due to slow cold decomposi9on, soil is low in organic maCer.
HUMAN IMACT
- Conversion of savanna and
temperate grasslands to
cropland
atmosphere from burning
and conversion to cropland
- Overgrazing of tropical and
temperate grassland by
livestock
tundra by oil produc9on, air
and water pollu9on, and
vehicles. – long 9me to
recover.
Fig. 5-‐27, p. 123
Oil producWon and off-‐road
vehicles in arcWc tundra
Overgrazing by livestock
Release of CO 2 to atmosphere
from grassland burning
Conversion to cropland
Grassland s Natural Capital DegradaWon
FORESTS