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Transcript
Ecossistemas: fluxos de matéria e
energia
População Recursos e Ambiente
Ecossistema
†
Um ecossistema é um
complexo dinâmico de
plantas, animais,
comunidades de
microorganismos e o seu
ambiente não vivo
interagindo como uma
unidade funcional
Biosphere
Ecosystems
Communities
Populations
Organisms
1
Oceanic crust
Continental crust
Biosphere
Vegetation
and animals
Soil
Lithosphere
Upper mantle
Asthenosphere
Crust
Rock
Lower mantle
Core
Crust
(soil and rock)
Mantle
Biosphere
(Living and dead
organisms)
Lithosphere
(crust, top of upper mantle)
Solar
radiation
Atmosphere
(air)
Hydrosphere
(water)
Energy in = Energy out
Reflected by
atmosphere (34%)
Radiated by
atmosphere
as heat (66%)
UV radiation
Absorbed
by ozone
Visible
light
Lower stratosphere
(ozone layer)
Greenhouse
Troposphere
effect
Heat
Absorbed
by the earth
Heat radiated
by the earth
Earth
2
Sun
Producers (rooted plants)
Producers (phytoplankton)
Primary consumers (zooplankton)
Secondary consumers (fish)
Dissolved
chemicals
Tertiary consumers
(turtles)
Sediment
Decomposers (bacteria and fungi)
Oxygen (O2)
Sun
Producer
Carbon dioxide (CO2)
Primary consumer
(rabbit)
Falling leaves
Precipitation
and twigs
Secondary consumer
(fox)
Producers
Soil decomposers
Water
3
Heat
Tertiary
consumers
(human)
Heat
Decomposers
Heat
10
Secondary
consumers
(perch)
100
Heat
Primary
consumers
(zooplankton)
1,000
10,000
Usable energy
available at
each tropic level
(in kilocalories)
Heat
Producers
(phytoplankton)
Sun
Ph
ot o
syn
t he
sis
Respiration
Energy lost &
unavailable to
consumers
Gross primary
production
Net primary
production
Growth and reproduction (energy
available to
consumers)
4
Terrestrial Ecosystems
Swamps and marshes
Tropical rain forest
Temperate forest
Northern coniferous forest (taiga)
Savanna
Agricultural land
Woodland and shrubland
Temperate grassland
Tundra (arctic and alpine)
Desert scrub
Extreme desert
Aquatic Ecosystems
Estuaries
Lakes and streams
Continental shelf
Open ocean
800 1,600 2,400 3,200 4,000 4,800 5,600 6,400 7,200 8,000 8,800 9,600
Average net primary productivity (kcal/m2/yr)
Detritus feeders
Bark beetle
engraving
Long-horned
beetle holes
Carpenter
ant
galleries
Decomposers
Termite and
carpenter
ant
work
Dry rot fungus
Wood
reduced
to powder
Time progression
Mushroom
Powder broken down by decomposers
into plant nutrients in soil
5
Abiotic chemicals
(carbon dioxide,
oxygen, nitrogen,
minerals)
Heat
Heat
Solar
energy
Heat
Decomposers
(bacteria, fungus)
Heat
Carbon
cycle
Producers
(plants)
Consumers
(herbivores,
carnivores)
Phosphorus
cycle
Nitrogen
cycle
Heat
Water
cycle
Oxygen
cycle
Heat in the environment
Heat
Heat
Heat
6
Figure 4-28
Page 76Rain clouds
Condensation
Transpiration
Evaporation
Transpiration
from plants
Precipitation to
land
Precipitation
Precipitation
Runoff
Evaporation
from land
Evaporation
from ocean
Surface runoff
(rapid)
Precipitation to
ocean
Surface
runoff
(rapid)
Infiltration and
Percolation
Groundwater movement (slow)
Ocean storage
incorporation
into sediments
sedimentation
7
8
Sulfur trioxide
Water
H2SO4
Sulfuric acid
Acidic fog and
precipitation
Ammonia
Sulfur dioxide
SO2
Oxygen
Hydrogen H S
2
sulfide
NH3
Ammonium
sulfate
(NH4)2SO4
Plants
Volcano
Dimethyl
sulfide
Industries
Animals
Ocean
Sulfate salts
SO4Decaying
matter
Metallic
sulfide
deposits
Sulfur
H2S Hydrogen
sulfide
Mosaic
of closely
packed
pebbles,
boulders
Alkaline,
dark,
and rich
in humus
Weak humusmineral mixture
Dry, brown to
reddish-brown, with
variable accumulations
of clay, calcium
carbonate, and
soluble salts
Desert Soil
(hot, dry climate)
Clay,
calcium
compounds
Grassland Soil
(semiarid climate)
9
Forest litter
leaf mold
Acidic
lightcolored
humus
Humus-mineral
mixture
Light-colored
and acidic
Light, grayishbrown, silt loam
Iron and
aluminum
compounds
mixed with
clay
Tropical Rain Forest Soil
(humid, tropical climate)
Acid litter
and humus
Humus and
iron and
aluminum
compounds
Dark brown
firm clay
Deciduous Forest Soil
(humid, mild climate)
Coniferous Forest Soil
(humid, cold climate)
10