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Chapter 10: Cycles and
Patterns in the Biosphere
McKnight’s Physical Geography:
A Landscape Appreciation,
Tenth Edition, Hess
Cycles and Patterns in the
Biosphere
• The Impact of Plants and Animals on the
Landscape
• The Geographic Approach to the Study of
Organisms
• Biogeochemical Cycles
• Food Chains
• Natural Distributions
• Environmental Relationships
2© 2011 Pearson Education, Inc.
The Impact of Plants and Animals
on the Landscape
• Vegetation grew profusely
at one time
• Human modification of
vegetation
• Animal life less apparent
• Both interact with
components of the
landscape
3© 2011 Pearson Education, Inc.
Figure 10-1b
The Geographic Approach to the
Study of Organisms
• Simplest organisms still extraordinarily complex
• Seek patterns of distribution of living organisms—
biogeography
• Several biological classification schemes
– Most common, binomial, “two name”
• 600,000 species of plants; twice that of animals
• Biota—total complex of plant and animal life
– Flora: plant life
– Fauna: animal life
• Ocean biota—plankton, nekton, and benthos
4© 2011 Pearson Education, Inc.
Biogeochemical Cycles
• Organisms survive through
complex of systemic flows
of energy, water, and
nutrients
• Cycles through which
Earth’s chemical elements
are absorbed by
organisms and returned to
Earth through
decomposition—
biogeochemical cycles
5© 2011 Pearson Education, Inc.
Figure 10-2
Biogeochemical Cycles
• The flow of energy
– Sun is source on which all
life depends
– Photosynthesis and
respiration
– Food chain
– Energy must be converted
to a usable form and
recycled
6© 2011 Pearson Education, Inc.
Figure 10-3
Biogeochemical Cycles
• Photosynthesis
– Biosphere receives solar energy
– Chlorophyll
– Chemical equation
• CO2 + H2O = Carbohydrates + O2
– Energy distributed by animals eating plants or each
other
– Energy distributed in the plants through respiration
– Plant respiration equation
• Carbohydrates + O2 = CO2 + H2O + Energy (heat)
7© 2011 Pearson Education, Inc.
Biogeochemical Cycles
• Net primary production
– Net photosynthesis—
difference in
carbohydrates produced
to those lost to respiration
– Net primary production is
the net photosynthesis
over a year (Figure 10-4)
– Measure of chemical
energy in a plant
– Reflected in the dry
weight, or biomass, of the
material
8© 2011 Pearson Education, Inc.
Figure 10-4
Biogeochemical Cycles
• The Hydrologic Cycle
– Every living thing
depends on water supply
– Water dissolves nutrients
and carries them to all
parts of the organism
– Two ways water is found
in biosphere
• In residence: chemically
bound to plant and animal
tissue
• In transit: part of
transpiration-respiration
9© 2011 Pearson Education, Inc.
Biogeochemical Cycles
• The Carbon Cycle
– Biosphere contains
complex mixture of carbon
compounds
– Main components
• Transfer of carbon from CO2 to
living matter and back to CO2
– Rapid process (years not
centuries)
– Gradual incorporation of
stored carbon in rock
– Fossil fuels increase CO2
10© 2011 Pearson Education, Inc.
Figure 10-6
Biogeochemical Cycles
• The Oxygen Cycle
– Building block in most
organic molecules
– By-product of plant life
– Occurs in many forms
and is released in many
ways
– Sources include water,
carbon dioxide, ozone,
oxygen stored in rocks
11© 2011 Pearson Education, Inc.
Figure 10-7
Biogeochemical Cycles
• The Nitrogen Cycle
– Nitrogen only usable in gas
form by a few bacteria
– Nitrogen usable by other
organisms as nitrates that
are used in plants—nitrogen
fixation
– Waste converts nitrates to
waste nitrites
– Bacteria convert nitrites
back to nitrates and nitrogen
gas (denitrification)
12© 2011 Pearson Education, Inc.
Figure 10-8
Biogeochemical Cycles
• Other mineral cycles—other minerals critical to the
biosphere
– Phosphorous
– Sulfur
– Calcium
• Gaseous pathways—interchange between biota and
atmosphere-ocean environment
• Sedimentary pathways—element is weathered and
reaches the groundwater; returned to the ocean and is
consumed by ocean organisms
13© 2011 Pearson Education, Inc.
Food Chains
• Food chain—direct
passage from one
organism to another of
nutrients
• More complex—food
“web”
• Primary energy
transformation
mechanism
14© 2011 Pearson Education, Inc.
Figure 10-9
Food Chains
• Fundamental unit: producers
(autotrophs), self feeders
• Producers eaten by
consumers (heterotrophs)
– Primary consumers:
herbivores
– Secondary consumers:
carnivores
• Food pyramid
• Decomposers begin the food
pyramid again
15© 2011 Pearson Education, Inc.
Figure 10-10
Food Chains
• Energy is inefficiently
consumed between different
food pyramid levels
• Pollutants in the food chain
– Biological amplification
– Chemical pesticides and
heavy metals (mercury, lead)
– Irrigation-related issues
16© 2011 Pearson Education, Inc.
Figure 10-11
Natural Distributions
• Four basic conditions
• Evolutionary development
– Survival of the fittest
– Where did the genus
(closely related organism
group) evolve?
• Some localized
• Several scattered localities of
the same genus
17© 2011 Pearson Education, Inc.
Figure 10-12
Natural Distributions
• Migration and dispersal
– Animals move from one
place to another
– Plants move through seed
dispersal
– Distribution pattern of
organisms results from
natural migration or
dispersal from the original
development center
18© 2011 Pearson Education, Inc.
Figure 10-14
Natural Distributions
• Reproductive success
– Ability for organisms to
reproduce affects
distribution
– Factors resulting in poor
reproductive success
• Heavy predation
• Climate change
• Food supply failure
• Changing environmental
conditions
19© 2011 Pearson Education, Inc.
Figure 10-16
Natural Distributions
• Extinction and die-off
– Range diminution
• Small areal changes
• Mass extinction
– Plant succession—one
vegetation type replaced by
another (Figure 10-17)
• Occur after catastrophic events
• Primary succession—pioneer
community
• Secondary succession
– Extinction versus succession
20© 2011 Pearson Education, Inc.
Figure 10-17
Environmental Relationships
• Relationships of plants and animals depends on
environment
• Influences depend on the area of interest
– Large area: seasonal characteristics, location
– Small area: localized terrain, topsoil
• Interspecific versus intraspecific competition
• Limiting factor: most important variable for the
survival of an organism
21© 2011 Pearson Education, Inc.
Environmental Relationships
• The influence of climate
– Light
• green plants need light to survive
• Light changes shapes of plants
(Figure 10-19)
• Photoperiodism: stimulates
seasonal plant behavior
– Moisture
• Distribution of biota governed
more by moisture than any other
factor
• Biota evolution dictated by
adaptation to moisture conditions
22© 2011 Pearson Education, Inc.
Figure 10-19
Figure 10-20
Environmental Relationships
• The influence of climate
– Temperature
• Different species can survive in
different temperatures
• Plants have limited cold
temperature tolerance
– Wind
• Wind effects generally limited
• Persistent winds can have
limiting effects through increased
drying
• Strong winds can be destructive
to biota
23© 2011 Pearson Education, Inc.
Figure 10-21
Environmental Relationships
• Topographic influences
– Plants and animals in a plains
region vastly different from a
mountainous region
– Slope and drainage
• Wildfires
– Result in complete or partial
devastation of plant live and
death or driving away of animals
– Can be helpful for regrowth and
maintaining of plant type
24© 2011 Pearson Education, Inc.
Figure 10-22
Environmental Relationships
• Example of selva (rainforest)
– Occurs when climate is warm and
has abundant precipitation
– Abundance of precipitation and
warmth leads to abundance of
natural vegetation (flora), jungle
– Numerous plants allow for fauna
– Leaves, trees, branches
decomposed by abundant fauna
on floor, put into soil
– Water runoff
25© 2011 Pearson Education, Inc.
Figure 10-24
Summary
• Plants and animals impact and interact with the
landscape in numerous ways
• Need a classification scheme for biota to understand
geographically
• Flora and fauna refer to plants and animals,
respectively
• Energy originates from the Sun and flows to organisms
through photosynthesis
• The hydrologic cycle describes the transition of water
through the biosphere
• The interaction of carbon with the biosphere is the
carbon cycle 26© 2011 Pearson Education, Inc.
Summary
• Oxygen and nitrogen cycle through the biosphere
through the oxygen and nitrogen cycles, respectively
• Other minerals cycle through the biosphere as well, but
they are not as commonly observed
• Food chains describe the passage of energy from one
organism to another
• There are four primary components to the natural
distributions of biota
• Numerous environmental relationships affect which
biota exist in which regions
27© 2011 Pearson Education, Inc.

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Ch10

  • 1. Chapter 10: Cycles and Patterns in the Biosphere McKnight’s Physical Geography: A Landscape Appreciation, Tenth Edition, Hess
  • 2. Cycles and Patterns in the Biosphere • The Impact of Plants and Animals on the Landscape • The Geographic Approach to the Study of Organisms • Biogeochemical Cycles • Food Chains • Natural Distributions • Environmental Relationships 2© 2011 Pearson Education, Inc.
  • 3. The Impact of Plants and Animals on the Landscape • Vegetation grew profusely at one time • Human modification of vegetation • Animal life less apparent • Both interact with components of the landscape 3© 2011 Pearson Education, Inc. Figure 10-1b
  • 4. The Geographic Approach to the Study of Organisms • Simplest organisms still extraordinarily complex • Seek patterns of distribution of living organisms— biogeography • Several biological classification schemes – Most common, binomial, “two name” • 600,000 species of plants; twice that of animals • Biota—total complex of plant and animal life – Flora: plant life – Fauna: animal life • Ocean biota—plankton, nekton, and benthos 4© 2011 Pearson Education, Inc.
  • 5. Biogeochemical Cycles • Organisms survive through complex of systemic flows of energy, water, and nutrients • Cycles through which Earth’s chemical elements are absorbed by organisms and returned to Earth through decomposition— biogeochemical cycles 5© 2011 Pearson Education, Inc. Figure 10-2
  • 6. Biogeochemical Cycles • The flow of energy – Sun is source on which all life depends – Photosynthesis and respiration – Food chain – Energy must be converted to a usable form and recycled 6© 2011 Pearson Education, Inc. Figure 10-3
  • 7. Biogeochemical Cycles • Photosynthesis – Biosphere receives solar energy – Chlorophyll – Chemical equation • CO2 + H2O = Carbohydrates + O2 – Energy distributed by animals eating plants or each other – Energy distributed in the plants through respiration – Plant respiration equation • Carbohydrates + O2 = CO2 + H2O + Energy (heat) 7© 2011 Pearson Education, Inc.
  • 8. Biogeochemical Cycles • Net primary production – Net photosynthesis— difference in carbohydrates produced to those lost to respiration – Net primary production is the net photosynthesis over a year (Figure 10-4) – Measure of chemical energy in a plant – Reflected in the dry weight, or biomass, of the material 8© 2011 Pearson Education, Inc. Figure 10-4
  • 9. Biogeochemical Cycles • The Hydrologic Cycle – Every living thing depends on water supply – Water dissolves nutrients and carries them to all parts of the organism – Two ways water is found in biosphere • In residence: chemically bound to plant and animal tissue • In transit: part of transpiration-respiration 9© 2011 Pearson Education, Inc.
  • 10. Biogeochemical Cycles • The Carbon Cycle – Biosphere contains complex mixture of carbon compounds – Main components • Transfer of carbon from CO2 to living matter and back to CO2 – Rapid process (years not centuries) – Gradual incorporation of stored carbon in rock – Fossil fuels increase CO2 10© 2011 Pearson Education, Inc. Figure 10-6
  • 11. Biogeochemical Cycles • The Oxygen Cycle – Building block in most organic molecules – By-product of plant life – Occurs in many forms and is released in many ways – Sources include water, carbon dioxide, ozone, oxygen stored in rocks 11© 2011 Pearson Education, Inc. Figure 10-7
  • 12. Biogeochemical Cycles • The Nitrogen Cycle – Nitrogen only usable in gas form by a few bacteria – Nitrogen usable by other organisms as nitrates that are used in plants—nitrogen fixation – Waste converts nitrates to waste nitrites – Bacteria convert nitrites back to nitrates and nitrogen gas (denitrification) 12© 2011 Pearson Education, Inc. Figure 10-8
  • 13. Biogeochemical Cycles • Other mineral cycles—other minerals critical to the biosphere – Phosphorous – Sulfur – Calcium • Gaseous pathways—interchange between biota and atmosphere-ocean environment • Sedimentary pathways—element is weathered and reaches the groundwater; returned to the ocean and is consumed by ocean organisms 13© 2011 Pearson Education, Inc.
  • 14. Food Chains • Food chain—direct passage from one organism to another of nutrients • More complex—food “web” • Primary energy transformation mechanism 14© 2011 Pearson Education, Inc. Figure 10-9
  • 15. Food Chains • Fundamental unit: producers (autotrophs), self feeders • Producers eaten by consumers (heterotrophs) – Primary consumers: herbivores – Secondary consumers: carnivores • Food pyramid • Decomposers begin the food pyramid again 15© 2011 Pearson Education, Inc. Figure 10-10
  • 16. Food Chains • Energy is inefficiently consumed between different food pyramid levels • Pollutants in the food chain – Biological amplification – Chemical pesticides and heavy metals (mercury, lead) – Irrigation-related issues 16© 2011 Pearson Education, Inc. Figure 10-11
  • 17. Natural Distributions • Four basic conditions • Evolutionary development – Survival of the fittest – Where did the genus (closely related organism group) evolve? • Some localized • Several scattered localities of the same genus 17© 2011 Pearson Education, Inc. Figure 10-12
  • 18. Natural Distributions • Migration and dispersal – Animals move from one place to another – Plants move through seed dispersal – Distribution pattern of organisms results from natural migration or dispersal from the original development center 18© 2011 Pearson Education, Inc. Figure 10-14
  • 19. Natural Distributions • Reproductive success – Ability for organisms to reproduce affects distribution – Factors resulting in poor reproductive success • Heavy predation • Climate change • Food supply failure • Changing environmental conditions 19© 2011 Pearson Education, Inc. Figure 10-16
  • 20. Natural Distributions • Extinction and die-off – Range diminution • Small areal changes • Mass extinction – Plant succession—one vegetation type replaced by another (Figure 10-17) • Occur after catastrophic events • Primary succession—pioneer community • Secondary succession – Extinction versus succession 20© 2011 Pearson Education, Inc. Figure 10-17
  • 21. Environmental Relationships • Relationships of plants and animals depends on environment • Influences depend on the area of interest – Large area: seasonal characteristics, location – Small area: localized terrain, topsoil • Interspecific versus intraspecific competition • Limiting factor: most important variable for the survival of an organism 21© 2011 Pearson Education, Inc.
  • 22. Environmental Relationships • The influence of climate – Light • green plants need light to survive • Light changes shapes of plants (Figure 10-19) • Photoperiodism: stimulates seasonal plant behavior – Moisture • Distribution of biota governed more by moisture than any other factor • Biota evolution dictated by adaptation to moisture conditions 22© 2011 Pearson Education, Inc. Figure 10-19 Figure 10-20
  • 23. Environmental Relationships • The influence of climate – Temperature • Different species can survive in different temperatures • Plants have limited cold temperature tolerance – Wind • Wind effects generally limited • Persistent winds can have limiting effects through increased drying • Strong winds can be destructive to biota 23© 2011 Pearson Education, Inc. Figure 10-21
  • 24. Environmental Relationships • Topographic influences – Plants and animals in a plains region vastly different from a mountainous region – Slope and drainage • Wildfires – Result in complete or partial devastation of plant live and death or driving away of animals – Can be helpful for regrowth and maintaining of plant type 24© 2011 Pearson Education, Inc. Figure 10-22
  • 25. Environmental Relationships • Example of selva (rainforest) – Occurs when climate is warm and has abundant precipitation – Abundance of precipitation and warmth leads to abundance of natural vegetation (flora), jungle – Numerous plants allow for fauna – Leaves, trees, branches decomposed by abundant fauna on floor, put into soil – Water runoff 25© 2011 Pearson Education, Inc. Figure 10-24
  • 26. Summary • Plants and animals impact and interact with the landscape in numerous ways • Need a classification scheme for biota to understand geographically • Flora and fauna refer to plants and animals, respectively • Energy originates from the Sun and flows to organisms through photosynthesis • The hydrologic cycle describes the transition of water through the biosphere • The interaction of carbon with the biosphere is the carbon cycle 26© 2011 Pearson Education, Inc.
  • 27. Summary • Oxygen and nitrogen cycle through the biosphere through the oxygen and nitrogen cycles, respectively • Other minerals cycle through the biosphere as well, but they are not as commonly observed • Food chains describe the passage of energy from one organism to another • There are four primary components to the natural distributions of biota • Numerous environmental relationships affect which biota exist in which regions 27© 2011 Pearson Education, Inc.