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Human Biology
Sylvia S. Mader
Michael Windelspecht
Chapter 23
Global Ecology and Human
Interferences
Lecture Outline
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Points to Ponder• What is an ecosystem and what are its biotic components?
• What are the energy flow and chemical cycling in an ecosystem?
• What are the two major ecosystems on earth?
• Describe the 3 types of terrestrial ecosystems and the 2 types of aquatic ecosystems.
• Compare and contrast food webs and food pyramids.
• What is a biogeochemical cycle?
• What is a reservoir and an exchange pool.
• Explain the water, carbon, nitrogen, and phosphorus cycles.
• What human activities interfere with these cycles?
• What problems are we creating by altering these pathways?
• What is ozone depletion and why is this important?
• What are the pros and cons to drilling in the Arctic National Wildlife refuge?
The nature of ecosystems
• Biosphere – the regions of the Earth’s waters,
crust, and atmosphere inhabited by living
organisms
• Ecosystem – a place where organisms interact
between each other and their environment
– Terrestrial: several distinct types based on
temperature and waterfall
– Aquatic: freshwater and marine
23.1 The nature of ecosystems
Terrestrial ecosystems
• Forests – dominated by trees
• Tropical rain forest
• Coniferous forests (taiga)
• Temperate deciduous forests
• Grasslands – dominated by grass
• Tropical grasslands
• Temperate grasslands (prairie)
• Deserts – characterized by lack of available
moisture
• Tundra
• Deserts
23.1 The nature of ecosystems
taiga
temperate forest desert
tropical rain forest tropical grassland (savanna)
temperate grassland (prairie)
Terrestrial ecosystems23.1 The nature of ecosystems
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tropical rain forest
temperate grassland (prairie)
desert
tropical grassland (savanna)
taiga
winter tundraautumn tundra
temperate forest
(temperate, desert, rain forest, prairie): © Corbis RF; (savanna): © Gregory Dimijan/Photo Researchers, Inc.; (taiga): © Brand X Pictures/PunchStock RF;
(autumn tundra): © Joseph Van Os/Getty Images; (winter tundra): © Oxford Scientifi c/Getty Images
Aquatic ecosystems
• Marine
• Seashores
• Oceans
• Coral reefs
• Estuaries
• Freshwater
• Lakes
• Ponds
• Rivers
• Streams
23.1 The nature of ecosystems
Aquatic ecosystems23.1 The nature of ecosystems
Components of an ecosystem
• Abiotic components – nonliving environment
• Biotic components - living components• Autotrophs – producers
• Heterotrophs – consumers• Herbivores – feed on plant and algae
• Carnivores – feed on other animals
• Omnivores – eat both plants and animals
• Detritus feeders – feed on decomposing organic matter
• Niche – the role an organism plays in an ecosystem such as how it gets its food, what it eats, and how it interacts with other organisms
23.1 The nature of ecosystems
Biotic components of an ecosystem
23.1 The nature of ecosystems
Energy flow and chemical cycling
• Energy flow:• Begins and continues when producers absorb solar energy
• Occurs as nutrients pass from one population to another
• This energy is converted to heat that dissipates into the environment
• Only a portion of energy is passed to organisms as they consume one another
• Chemical cycling: • Inorganic nutrients are returned to producers from the
atmosphere or soil
• Chemicals recycle within and between ecosystems
23.1 The nature of ecosystems
Energy flow and chemical cycling
23.1 The nature of ecosystems
Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
solar
energy heat
consumers
producers
inorganic
nutrient pool
heat decomposers
heat
energy
nutrients
Fate of food energy taken
in by a herbivore
23.1 The nature of ecosystems
Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
Heat to
environment
Energy to
carnivores
Energy
to detritus
feeders
growth and reproduction
© George D. Lepp/Photo Researchers, Inc.
Energy flow
• Food web – describes who eats whom• Grazing food web
• Detrital food web
• Trophic levels – composed of all organisms that feed at a particular link in the food chain
• Producers, primary consumers, and secondary consumers
• Ecological pyramid – reflects the loss of energy from one trophic level to another
• Only about 10% of the energy of one trophic level is available to the next trophic level
23.2 Energy flow
Food webs23.2 Energy flow
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shrewssalamanderscarnivorous invertebrates
(beetles)
invertebrates
(earthworms)
b. Detrital food web
fungi and bacteria
(decomposers)
a. grazing food web
skunks
foxes
detritussnakes
mice
rabbitschipmunks
owls
CarnivoresHerbivores/OmnivoresAutotrophs (Producers)
fruits and
nuts
leaf-eating
insects
hawksbirds
deer
mice
detritus
detritus
leaves
An example of a food pyramid23.2 Energy flow
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producers
809g/m2
herbivores
37g/m2
carnivores
11g/m2
top carnivores
1.5g/m2
Biogeochemical cycles
• Biogeochemical cycles are pathways by which chemicals circulate through an ecosystem including both living and nonliving components
1. Water cycle
2. Carbon cycle
3. Nitrogen cycle
4. Phosphorus cycle
• Reservoir – fossil fuels, minerals in rocks, and sediment in oceans that contain inorganic nutrients that are limited in availability
• Exchange pools – atmosphere, soil, and water that are ready sources of inorganic nutrients
23.3 Global Biogeochemical cycles
Biogeochemical cycles
23.3 Global Biogeochemical cycles
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Community
Exchange
Pool
• atmosphere
• soil
• water
Reservoir
• fossilfuels
• mineral
in rocks
• sediment
in oceans
Water cycle
• Water evaporates from the bodies of water, land, and plants and returns when water falls on land to enter the ground, surface waters, or aquifers
• Human activities that interfere:• Withdraw water from aquifers
• Clear vegetation from the land and build structures that prevent percolation and increase runoff
• Add pollutants to water such as sewage and chemicals
23.3 Global Biogeochemical cycles
Water cycle
23.3 Global Biogeochemical cycles
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Ice
1 2
4
5
3 2
6
H2O in Atmosphere
evaporation
from ocean
precipitation
to ocean
transport of water vapor by wind
transpiration from plants
and evaporation from soilprecipitation
over land
lake
fresh water runoff
aquifer
Groundwaters
Ocean
Carbon cycle
• CO2 is exchanged between the atmosphere
and living organisms
• Plants incorporate atmospheric CO2 into
nutrients through photosynthesis that can be
used by living organisms
• CO2 is returned to the atmosphere through
respiration
23.3 Global Biogeochemical cycles
Carbon cycle23.3 Global Biogeochemical cycles
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7
1
7
24
3
5
6
CO2 in Atmosphere
Ocean
bicarbonate (HCO3–)
diffusion
destruction
of vegetation
Land plants
Soils
dead
organisms
and animal
waste
photosynthesis
combustion
decay
respiration
coal
oil
natural gas
Carbon cycle
• Human activities that interfere:
• Burning of fossil fuels and the destruction of forests
are depositing CO2 to the atmosphere faster than it
is being removed
• CO2 and other gases (N2O and CH4) are being
emitted due to human activities
• These gases are called greenhouse gases because
they trap heat that contributes to global warming
23.3 Global Biogeochemical cycles
Greenhouse gases and global warming
23.3 Global Biogeochemical cycles
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solar radiation solar radiation reflectedsolar radiation
reflected
green house gases
in atmosphere
Greenhouse
effect
reradiated
clouds
absorbed
Solar radiation that
passes through
the atmosphere
warms the Earth’s
surface.
Clouds, which contain
water vapor, absorb
infrared rays (heat) from the
earth’s surface and warm
the surface by downward
reradiation of a portion of
these rays.
Green house gases, including carbon
dioxide and methane, also cause the
atmosphere to absorb and reradiate infrared
rays toward the surface of the Earth. As the
concentration of green house gases
increases, the temperature of the Earth is
expected to increase also.
Nitrogen cycle
• 78% of the atmosphere is nitrogen gas but it is
not in a usable form by plants
• Nitrogen-fixing bacteria convert nitrogen gas to
ammonium that can be used by plants
• Nitrifying bacteria convert ammonium to nitrate
• Bacteria convert nitrate back to nitrogen gas
through a process called dentrification
23.3 Global Biogeochemical cycles
Fig. 23.12
Nitrogen cycle23.3 Global Biogeochemical cycles
Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
NO3–
3
4
5
6
8
8
2
2
7
1
7
1
phytoplankton
N2 in Atmosphere
N2 fixation
nitrogen-fixing
bacteria in nodules
And soil
plants
denitrifying
bacteria
decomposers
Biotic
Community
nitrifying
bacteria
NH4+
NO2
NO2
denitrification NH4+
cyanobacteria
Biotic
Community
denitrifying bacteria
nitrification
human
activities
runoff
decomposers
dead organisms
and animal waste
denitrificationN2 fixation
Nitrogen cycle
• Human activities interfere:
• We add nitrogen fertilizers that run off into lakes and
streams that cause major fish kills by eutrophication
• Burning of fossil fuels
- puts nitrogen oxides and sulfur dioxide into the atmosphere
where they combine with water vapor to form acids that
return to earth as acid deposition
- Result in nitrogen oxides and hydrocarbons that react with
one another to produce smog
23.3 Global Biogeochemical cycles
Nitrogen cycle23.3 Global Biogeochemical cycles
Phosphorus cycle
• Phosphate ions become available to living organisms by the slow weathering of rocks
• Phosphate is a limiting nutrient in ecosystems
23.3 Global Biogeochemical cycles
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1
4
3
5
8
6
7
8
2
8
minable rock
phosphate mining
geologic uplift
plants
animals and
animal wastes
decomposers
sewage treatment
plants
phosphate
in solution
biota
detritus
sediments
Biotic
Community phosphate
in soil
fertilizer
runoff
weathering
Phosphorus cycle
• Human activities interfere:
• Runoff of phosphate due to fertilizer and discharge
from sewage treatment plants results in
eutrophication
• Sources of pollution:
- Point source – specific sources
- Nonpoint sources – runoff from land
23.3 Global Biogeochemical cycles
Sources of pollution
23.3 Global Biogeochemical cycles
Biodegradable organic compounds
(e.g., sewage, wastes from food-processing
plants, paper mills, and tanneries)
Nitrates and phosphates from detergents,
fertilizers, and sewage treatment plants
Bacteria and viruses from sewage and
barnyard waste (causing, for example,
cholera, food poisoning, and hepatitis)
Acids from mines and air pollution;
dissolved salts; heavy metals
(e.g., mercury) from industry
Radioactive substances from nuclear
power plants, medical and research facilities
Sources of Water Pollution
Leading to Cultural Eutrophication
Oxygen-demanding
waste
Plant nutrients
Sediments
Thermal discharges
Enriched soil in water due to soil erosion
Heated water from power plants
Health Hazards
Disease-causing agents
Synthetic organic
compounds
Inorganic chemicals
and minerals
Radiation
Pesticides, industrial chemicals
(e.g., PCBs)
acidic water
from mines sediments
crop dusting
industrial wastes
city
biomedical
wastes
barnyard wastes
suburban
development
sewage
treatment plant
fertilizer runoffnuclear reactoroil pollution
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Science focus: ozone shield depletion
• Ozone shield – a layer of ozone in the stratosphere that absorbs UV rays preventing them from reaching the earth
• Causes of depletion:– Chlorine atoms primarily from chlorofluorocarbons(CFCs)
• Freon used as a coolant
• Cleaning agents
• Agents used to make Styrofoam
• Concerns about loss of ozone:– Increases mutations leading to skin cancer
– Adversely affects the immune system
– Impairs crop and tree growth
– Can kill off algae and krill that sustain oceanic life
23.3 Global Biogeochemical cycles
Science focus: ozone shield depletion
23.3 Global Biogeochemical cycles
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Ozone (Dobson Units)
110 220 330 440 550Courtesy NASA