Title: Chapter 7: Environmental Systems and Ecosystem Ecology
1Chapter 7 Environmental Systems and Ecosystem
Ecology
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2Environmental Systems
- community ecology (different species)
- ecosystem level (living and non-living)
- environmental systems
- solar radiation
- geothermal activity
- organism's metabolism
- human activity
- pollution
3Feedback
- Input parts of a system that causes the
condition observed - freshwater
- sediments
- nutrients
- pollution
- Output products obtained from the system
- matter and energy in the form of fish/shellfish
4Feedback loop
- when the output of a system can become the input
- Negative feedback loop input and output
neutralize each other by dynamic equilibrium
resulting in homeostasis (stabilized) - thirst and drinking
- Positive feedback loop drive the ecosystem to
one of the extremes. Rare in nature but common
when humans alter the environment - erosion
5Dead Zone
- area in which oxygen depletion is evident
(hypoxia) - normal oxygenated water has 10ppm
- depletion is 2ppm or less
- below 1.5ppm most organisms die
- caused by several factors
- urban runoff
- fertilizers
- municipal sewage
- industrial discharges
- fossil fuel emissions
6Types of Environmental Systems
- lithosphere (rock and sediment)
- atmosphere (air)
- hydrosphere (water systems)
- biosphere (biotic and abiotic)
- they overlap in some way (Ecosystems)
7Ecosystems
- interaction of living and non-living components
- energy (food) is converted into biomass (growth
and repair) - nutrients can limit productivity
- too much nitrogen causes dead zone in the gulf
- too much phosphorus causes dead zones in fresh
water ponds and lakes - iron seems to be the factor in open ocean waters
8Primary Productivity Worldwide
grams of Carbon per meter squared per year
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9Ecosystems Integration
- from small (simple pond) to large scale
(biosphere) - adjacent ecosystems may share components
- frogs develop in ponds, live in land and
reproduce in pond - salmon lives in the ocean but breeds in
freshwater - these areas where ecosystems meet are known as
ecotones
10Landscape Ecology
- study of different ecosystems that may affect
abundance, distribution and interaction of
organisms - consists of patches and these can be of different
scales - subpopulations can live in different patches
- if a species move among patches to mate it is
called a metapopulation - metapopulation is used to study loss, protection
and restoration of biodiversity
11- 5 ecosystems shown in large patches 3
terrestrial, a marsh and a river - A corridor is shown between the marsh and the
forest - Ecotone is shown between the grassland and forest
showing patches in a smaller scale
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12Geographic Information System (GIS)
- software that takes multiple data
- geology, hydrology, vegetation, animal species,
human development - analyzes their location in the area of study
- analyzes their correlation and interactions with
the other factors
13- GIS integrates different features and human uses
of an area for future development
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14Biochemical Cycles
- carbon cycle
- nitrogen cycle
- water cycle
- phosphorus cycle
- rock cycle
- plate tectonics
15Carbon Cycle
- photosynthesis carbon is fixated in plant growth
- respiration carbon is given back to the
environment in the form of CO2 - food webs carbon is passed along
- sediment storage remains settle to the bottom of
the ocean producing fossil fuels - oceans absorb C from air, runoffs, volcanoes,
waste and detritus of marine organisms. Ocean
acidification
16pool size petagram (1015g) fluxes petagrams of
C per year
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17Shifting carbon from lithosphere to atmosphere
- producing more carbon in the air (CO2) by
combustion than what is put back in the
lithosphere - carbon cycle cannot keep up
- cutting down forests and burning fields converts
that carbon into CO2 releasing it to the air - 1-2 billion metric tons of CO2 is unaccounted
for, so it seems it is been taken up by plants - scientists don't know what ecosystem is doing it
right now.
18Phosphorus Cycle
- essential for production of DNA, RNA, ATP and
other molecules essential for life on earth - present mainly lithosphere and ocean
- humans affect it by extracting it from the
lithosphere and polluting the ocean with
fertilizers
19pool sizes teragrams (10-12g) fluxes teragrams
of P per year
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20Nitrogen Cycle
- 78 of the atmosphere mass as N2
- essential ingredient for DNA and RNA
- essential for plant growth
- N2 is inert but once it transforms into NH3
(ammonia) or NH4 (ammonium), it becomes "fixed" - fixed molecules can be taken by plants (nitrogen
fixation) - nitrifying bacteria- puts nitrogen back in soil
- denitrifying bacteria- puts nitrogen back in
atmosphere
21pool sizes teragrams (10-12g) of N fluxes
teragram of N per year
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22Human Influence in Nitrogen Cycle
- excess nitrogen from agriculture practices
- causes hypoxia
- dead zone in the gulf
- synthetic ammonia increased food production since
1950s - factor in human population growth
- nitrogen fixation has been doubled
- NOx have increased in the atmosphere creating
nitric acid (acid rain) and nitric oxide (smog)
23- Nitrogen Fixation since 1950
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24Hydrologic Cycle
- essential for life
- key role in every cycle already studied
- 97 ocean, 3 fresh water
- carries nutrients
- carries sediments
- distributes pollutants
- evaporation, precipitation, groundwater
25Forms of Fresh Water
- vapor
- evaporation
- transpiration
- liquid
- precipitation
- runoff
- surface water (lakes, rivers)
- groundwater
- aquifers
26pool size cubic kilometers (km3) fluxes km3 per
year
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27Impacts on Hydrologic Cycle
- dams increase evaporation
- lake Mead levels
- dams alter vegetation
- Colorado river dams opening
- agricultural fields decrease water level in
rivers and streams - Rio Grande
- lower water tables
- Edwards aquifer
- pollutants present in water
- Rio Grande and aquifers
- conflicts for water
- Rio Grande delta, Colorado River
28Geological Systems
- very slow process
- rock cycle
- igneous rock
- sedimentary rock
- metamorphic rock
29Igneous Rock
- form from magma when it cools down
- it formes intrusive rocks
- multicolored
- formed by different similar minerals
- metamorphic and sedimentary
- granite is a good example
30Sedimentary Rock
- formed by sediments and dissolved minerals
- weight and pressure aids its formation
- minerals act like glue
- metamorphic and igneous
- fossils and limestone
31Metamorphic Rock
- changes form due to geological forces
- temperature and pressure
- sedimentary and igneous rock
- marble
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33THE END
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