Transcript Ecosystems
Ecosystems
Chapter 54
I. Energy Flow
A.
B.
Trophic Structures
Energy Budget
Global EB
GPP & NPP
Biomass
Limits of PP- aquatic, terrestrial
C.
Secondary Productivity
Energy Efficiency
Pyramids-production, #s, biomass
D.
Biological Magnification
II. Biogeochemical Cycles
A.
B.
C.
D.
Water
Carbon
Nitrogen
Phosphorous
III. Human Impact
A.
B.
C.
D.
Chemical Cycles
Acid precipitation
Toxins & biological
Magnification
Climate change-CO2 & O3
A. Trophic Structures- Energy
Flow
Energy flow one way- sun is inflow
Food
chains & webs are short b/c trophic
energy level loses 90%
Energy Transfer
Energy in
from
the Sun
captured by autotrophs =
producers
Energy moves through
food
chain
transfer of energy
from autotrophs to
heterotrophs
(herbivores to carnivores)
heterotrophs = consumers
Energy Transfer
Primary
producers primary
consumers secondary consumers
tertiary consumers
Detrivores/Decomposers get
energy from detritus most
important part in an ecosystem
connects all levels
B. Energy Budget Primary
Production
Producers
determine the energy
budget for an ecosystem
GPP
amount of solar energy
converted into chemical energy all
photsynthesis
NPP = GPP- Respiration (cost of staying
alive)
PP J/m2/y or biomass
Primary Production
Aquatic
Systems light &
nutrients are limiting factors
for PP
Terrestrial Systems
temperature, moisture,
nutrients
C. Secondary Production
The mount of chemical energy in
consumers’ food that is converted into
their
Energy Inefficiency
incomplete
digestion
metabolism
Pyramids of Production
represent the loss of energy from a food
chain
how
much energy is turned into biomass
Pyramid of Numbers
levels in pyramids of production are
proportional to number of individuals
present in each trophic level
Implications
Dynamics of energy through ecosystems
have important implications for human
populations
what
food would be more ecologically
sound?
D. Biological Magnification
Toxins can become concentrated in successive
trophic levels of food webs
Humans produce many toxic chemicals that are
dumped into ecosystems.
These substances are ingested and
metabolized by the organisms in the
ecosystems and can accumulate in the fatty
tissues of animals.
These toxins become more concentrated in
successive trophic levels of a food web, a
process called biological magnification.
Fig. 54.24
The pesticide DDT, before it was banned,
showed this affect.
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Fig. 54.25
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Biogeochemical Cycles
Nutrient
cycles
Gases cycle on a global level
Solids cycle slowly and locally
Fig. 54.15
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The water cycle is more of a physical
process than a chemical one.
Fig. 54.16
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The carbon cycle fits the generalized scheme
of biogeochemical cycles better than water.
Fig. 54.17
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The Nitrogen Cycle
Nitrogen
enters ecosystems through
two natural pathways.
Atmospheric
deposition, where usable
nitrogen is added to the soil by rain or
dust.
Nitrogen fixation, where certain
prokaryotes convert N2 to minerals
that can be used to synthesize
nitrogenous organic compounds like
amino acids.
Fig. 54.18
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Fig. 54.19
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III. Human Impact
Rising atmospheric CO2.
Since the Industrial Revolution, the
concentration of CO2 in the
atmosphere has increased greatly as a
result of burning fossil fuels.
Measurements in 1958 read 316 ppm and
increased to 370 ppm today
Fig. 54.26
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The Greenhouse Effect
Rising levels of atmospheric CO2 may have an
impact on Earth’s heat budget.
When
light energy hits the Earth, much of it is
reflected off the surface.
CO2 causes the Earth to retain some of the
energy that would ordinarily escape the
atmosphere.
This phenomenon is called the greenhouse effect.
The Earth needs this heat, but too much could be
disastrous.
Global Warming
Scientists continue to construct models
to predict how increasing levels of CO2 in
the atmosphere will affect Earth.
Several
studies predict a doubling of CO2 in
the atmosphere will cause a 2º C increase in
the average temperature of Earth.
Rising temperatures could cause polar ice cap
melting, which could flood coastal areas.
It is important that humans attempt to
stabilize their use of fossil fuels.
Ozone Depletion
Life on earth is
protected from the
damaging affects of
ultraviolet radiation
(UV) by a layer of O3,
or ozone.
Studies suggest that
the ozone layer has
been gradually
“thinning” since 1975.
Fig. 54.27b
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Ozone Depletion
Probably results from the accumulation of
chlorofluorocarbons, chemicals used in
refrigeration and aerosol cans, and in certain
manufacturing processes.
The result of a reduction in the ozone layer
may be increased levels of UV radiation that
reach the surface of the Earth.
This radiation has been linked to skin cancer
and cataracts.
The impact of human activity
on the ozone layer is one
more example of how much
we are able to disrupt
ecosystems and the entire
biosphere.