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Chapter 24
Lecture Outline
See separate PowerPoint slides for all figures and tables pre-
inserted into PowerPoint without notes.
Copyright © 2016 McGraw-Hill Education. Permission required for reproduction or display.
2
Global Ecology and
Human Interferences
3
Points to ponder • What is an ecosystem and what are its biotic
components?
• What are energy flow and chemical cycling in an ecosystem?
• What are the two major ecosystems on earth?
• Describe the three types of terrestrial ecosystems and the two 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?
4
Points to ponder
• 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 biomagnification and why is mercury a concern?
5
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
with each other and their environment
– Terrestrial: several distinct types based on
temperature and waterfall
– Aquatic: freshwater and marine
24.1 The Nature of Ecosystems
6
• Forests – dominated by trees
• Tropical rain forest
• Coniferous forests (taiga)
• Temperate deciduous forests
• Grasslands – dominated by grass
• Tropical grasslands
• Temperate grasslands (prairie)
24.1 The Nature of Ecosystems
Terrestrial ecosystems
7
• Deserts – characterized by lack of
available moisture
• Tundra
• Deserts
24.1 The Nature of Ecosystems
Terrestrial ecosystems
8
Terrestrial ecosystems
Figure 24.1 The
distribution of the
major terrestrial
biomes.
24.1 The Nature of Ecosystems
9
Aquatic ecosystems • Marine
• Seashores
• Oceans
• Coral reefs
• Estuaries
• Freshwater
• Lakes
• Ponds
• Rivers
• Streams
24.1 The Nature of Ecosystems
10
Aquatic ecosystems Figure 24.2 Examples of freshwater and saltwater ecosystems.
24.1 The Nature of Ecosystems
Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
a. b.
c. d.
a: © Francois Gohier/Photo Researchers; b: © The McGraw-Hill Companies, Inc. Carlyn Iverson, photographer;
c: © David Hall/Photo Researchers; d: © Vol. 121/Corbis RF
11
Components of an ecosystem
• Abiotic components – nonliving environment
• Biotic components - living components
• Autotrophs – producers
• Heterotrophs – consumers
• Herbivores – feed on plants and algae
• Carnivores – feed on other animals
• Omnivores – eat both plants and animals
• Detritus feeders – feed on decomposing
organic matter
24.1 The Nature of Ecosystems
12
• 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
24.1 The Nature of Ecosystems
Components of an ecosystem
13
Biotic components of an ecosystem
Figure 24.3 The biotic components of
an ecosystem.
24.1 The Nature of Ecosystems
14
• Energy flow
• It begins and continues when producers
absorb solar energy.
• Energy flow 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.
24.1 The Nature of Ecosystems
Energy flow and chemical cycling
15
• Chemical cycling
• Inorganic nutrients are returned to producers
from the atmosphere or soil.
• Chemicals recycle within and between
ecosystems.
24.1 The Nature of Ecosystems
Energy flow and chemical cycling
16
Energy flow and chemical cycling 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
Figure 24.4 Energy flow and
chemical cycling in an
ecosystem.
24.1 The Nature of Ecosystems
17
Fate of food energy taken
in by an herbivore 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.
Figure 24.5 The fate of
food energy taken in by an
herbivore.
24.1 The Nature of Ecosystems
18
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
24.2 Energy Flow
19
Energy flow
• 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
24.2 Energy Flow
20
Food webs
Figure 24.6 Food webs
illustrate ecological
relationships.
24.2 Energy Flow
Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
shrews salamanders carnivorous invertebrates invertebrates
b.
fungi and bacteria in detritus
a.
rabbits chipmunks
owls
Carnivores Herbivores/Omnivores Autotrophs
nuts
hawks birds
mice
detritus
leaves
mice
snakes
skunks
foxes
deer
leaf-eating insects
death death
death
21
An example of a food pyramid Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
producers
809g/m2
herbivores
37g/m2
carnivores
11g/m2
top carnivores
1.5g/m2
Figure 24.7 The
influence of
trophic level on
biomass.
24.2 Energy Flow
22
• Biogeochemical cycles are pathways by
which chemicals circulate through an
ecosystem.
1. Water cycle
2. Carbon cycle
3. Nitrogen cycle
4. Phosphorus cycle
24.3 Global Biogeochemical Cycles
Biogeochemical cycles
23
• Reservoir – fossil fuels, minerals in rocks,
and sediments in oceans contain inorganic
nutrients that are limited in availability
• Exchange pools – atmosphere, soil, and
water are ready sources of inorganic
nutrients
24.3 Global Biogeochemical Cycles
Biogeochemical cycles
24
Biogeochemical cycles Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
Community
Exchange
Pool
• atmosphere
• soil
• water
Reservoir
• fossilfuels
• mineral
in rocks
• sediment
in oceans
Figure 24.8
The cycling of
nutrients
between biotic
communities
and
biogeochemical
reservoirs.
24.3 Global Biogeochemical Cycles
25
• Water evaporates from bodies of water, land, and plants, and returns when water falls on land to enter the ground, surface waters, or aquifers.
24.3 Global Biogeochemical Cycles
Water cycle
26
• Human activities that interfere
• Withdrawing water from aquifers
• Clearing vegetation from the land and building structures that prevent percolation and increase runoff
• Adding pollutants to water such as sewage and chemicals
24.3 Global Biogeochemical Cycles
Water cycle
27
Water cycle Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
I c e
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 soil precipitation
over land
lake
fresh water runoff
aquifer
Groundwaters
Ocean
Figure 24.9 The hydrologic (water) cycle.
24.3 Global Biogeochemical Cycles
28
• CO2 is exchanged between the atmosphere
and living organisms.
• Plants incorporate atmospheric CO2 into
nutrients through photosynthesis, providing
food for themselves and other organisms.
• CO2 is returned to the atmosphere through
respiration.
24.3 Global Biogeochemical Cycles
Carbon cycle
29
Carbon cycle
Figure 24.10 The
carbon cycle.
24.3 Global Biogeochemical Cycles
30
• Human activities that interfere
• Burning of fossil fuels and the destruction of forests are adding 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; this contributes to global warming.
24.3 Global Biogeochemical Cycles
Carbon cycle
31
Global warming and climate change
Figure 24.11 Global warming and climate change.
24.3 Global Biogeochemical Cycles
32
• 78% of the atmosphere is nitrogen gas (N2) but
plants cannot use this form.
• Nitrogen-fixing bacteria convert nitrogen gas to
ammonium (NH4+), which can be used by plants.
• Nitrifying bacteria convert ammonium to nitrate
(NO3-).
• Bacteria convert nitrate back to nitrogen gas
through a process called denitrification.
24.3 Global Biogeochemical Cycles
Nitrogen cycle
33
Nitrogen cycle
Figure 24.12 The nitrogen cycle.
24.3 Global Biogeochemical Cycles
34
• Human activities that interfere
• We add nitrogen fertilizers that run off into lakes
and streams, causing major fish kills by
eutrophication.
• Burning of fossil fuels
- It 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.
- It results in nitrogen oxides and hydrocarbons
that react with one another to produce smog.
24.3 Global Biogeochemical Cycles
Nitrogen cycle
35
Thermal inversions and smog • During a thermal inversion, pollutants are
trapped near the Earth.
– The air does not circulate, so pollutants can build
up to dangerous levels.
Figure 24.14 Thermal inversions.
24.3 Global Biogeochemical Cycles
Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
cooler air
cool air
warm air
a. Normal pattern
cool air
warm inversion layer
cool air
b. Thermal inversion
36 Figure 24.13 The effects of acid deposition.
24.3 Global Biogeochemical Cycles
Nitrogen cycle Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
a.
b.
c.
a: © Larry Lee Photography/Corbis RF; b: © Oxford Scientific/Photolibrary/Getty Images;
c: © Sue Baker/Photo Researchers
37
Phosphorus cycle
• Phosphate ions become available to living organisms by the slow weathering of rocks.
• Phosphate is a limiting nutrient in ecosystems.
Figure 24.15 The phosphorus cycle.
24.3 Global Biogeochemical Cycles
38
Phosphorus cycle
• Human activities that interfere
• Runoff of phosphate due to fertilizer and
discharge from sewage treatment plants
results in eutrophication.
• Sources of water pollution
- Point sources are the easily identifiable
sources.
- Nonpoint sources cannot be specifically
identified (e.g., runoff).
24.3 Global Biogeochemical Cycles
39
Biomagnification of mercury
• Emissions of mercury into the environment can lead to serious health effects for humans, fish, and wildlife.
• There is widespread mercury contamination in streams, wetlands, reservoirs, and lakes throughout most of the U.S.
• Bioaccumulation occurs when an organism accumulates a contaminant such as mercury faster than it can eliminate it.
• Mercury enters ecosystems at the base of the food chain and increases in concentration as it moves up higher trophic levels.
24.3 Global Biogeochemical Cycles
40
Sources of water pollution
Figure 24.16 Some sources of surface water pollution.
24.3 Global Biogeochemical Cycles
Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
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 runoff nuclear reactor oil pollution