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Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
PowerPoint® Lecture Presentations for
Biology
Eighth Edition
Neil Campbell and Jane Reece
Lectures by Chris Romero, updated by Erin Barley with contributions from Joan Sharp
Chapter 37
Soil and Plant Nutrition
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Overview: “The Nation that Destroys Its Soil
Destroys Itself”
• Farmland productivity often suffers from
chemical contamination, mineral
deficiencies, acidity, salinity, and poor
drainage.
• Healthy soils improve plant growth by
enhancing plant nutrition.
• Typically, plants obtain carbon dioxide from the
air, and water and minerals from the soil.
Dust Bowl ---> Could this Happen Again??
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Soil is a living, finite resource
• Plants obtain most of their water and minerals
from the upper layers of soil.
• Living organisms play an important role in
these soil layers.
• This complex ecosystem is fragile.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Soil Texture
• Soil particles are classified by size; from largest
to smallest they are called sand, silt, and clay.
• Soil is stratified into layers = soil horizons.
• Topsoil consists of mineral particles, living
organisms, and humus = the decaying organic
material.
Soil
horizons
A horizon
B horizon
C horizon
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
• After a heavy rainfall, water drains from the
larger spaces in the soil, but smaller spaces
retain water because of its attraction to clay
and other particles.
• The film of loosely bound water is usually
available to plants.
• Loams are the most fertile topsoils and contain
equal amounts of sand, silt, and clay.
Soil
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Topsoil Composition
• A soil’s composition refers to:
** its inorganic (mineral) AND
** organic chemical components.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Inorganic Components
• Cations (for example K+, Ca2+, Mg2+) adhere to
negatively charged soil particles.
• This adhering of cations prevents them from
leaching out of the soil through percolating
groundwater.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
• During cation exchange, cations are displaced
from soil particles by other cations.
• Displaced cations enter the soil solution and
can be taken up by plant roots.
• Negatively charged ions do not bind with soil
particles and can be lost from the soil by
leaching.
Cation
exchange in
soil
Soil particle
–
–
– –
– – – –
–
K+
K+
K+
Ca2+
Ca2+
Mg2+
H+
H+
H2O + CO2 H2CO3 HCO3
– +
Root hair
Cell wall
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Organic Components
• Humus builds a crumbly soil that retains water
but is still porous.
• It also increases the soil’s capacity to
exchange cations and serves as a reservoir of
mineral nutrients.
• Topsoil contains bacteria, fungi, algae, other
protists, insects, earthworms, nematodes, and
plant roots.
• These organisms help to decompose organic
material and mix the soil -- detrivores.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Soil Conservation and Sustainable Agriculture
• In contrast with natural ecosystems, agriculture
depletes the mineral content of soil, taxes
water reserves, and encourages erosion.
• The goal of sustainable agriculture is to use
farming methods that are conservation-minded,
environmentally safe, and profitable.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Irrigation
• Irrigation is a huge drain on water resources
when used for farming in arid regions.
• The primary source of irrigation water is
underground water reserves called aquifers.
• The depleting of aquifers can result in
subsidence = the settling or sinking of land.
Land subsidence caused by excessive
removal of groundwater
Land subsidence in California Sinkhole in Florida
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
• Irrigation can lead to salinization = the
concentration of salts in soil as water
evaporates.
• Drip irrigation requires less water and reduces
salinization.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fertilization
• Soils can become depleted of nutrients as
plants and the nutrients they contain are
harvested.
• Fertilization replaces mineral nutrients that
have been lost from the soil.
• Commercial fertilizers are enriched in nitrogen,
phosphorus, and potassium.
• Organic fertilizers are composed of manure,
fishmeal, or compost.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Adjusting Soil pH
• Soil pH affects cation exchange and the
chemical form of minerals.
• Cations are more available in slightly acidic
soil, as H+ ions displace mineral cations from
clay particles.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Controlling Erosion
• Topsoil from thousands of acres of farmland is
lost to water and wind erosion each year in the
United States.
• Erosion of soil causes loss of nutrients.
Contour tillage helps reduce soil erosion
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
• Erosion can be reduced by:
– Planting trees as windbreaks
– Terracing hillside crops
– Cultivating in a contour pattern
– Practicing no-till agriculture.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Preventing Soil Compaction
• Soil compaction from heavy equipment
reduces pore space between soil particles.
• Soil compaction slows gas exchange and
reduces root growth.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Phytoremediation
• Some areas are unfit for agriculture because of
contamination of soil or groundwater with toxic
pollutants.
• Phytoremediation is a biological,
nondestructive technology that reclaims
contaminated areas.
• Plants capable of extracting soil pollutants are
grown and are then disposed of safely.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Concept 37.2: Plants require essential elements to
complete their life cycle
• Plants derive most of their organic mass
from the CO2 of air, but they also depend on
soil nutrients such as water and minerals.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Macronutrients and Micronutrients
• A chemical element is considered an essential
element if it is required for a plant to complete its life
cycle.
• Nine of the essential elements are called
macronutrients because plants require them in
relatively large amounts. The macronutrients are
carbon, oxygen, hydrogen, nitrogen, phosphorus,
sulfur, potassium, calcium, and magnesium.
• Eight of the essential elements are called
micronutrients because plants need them in very
small amounts. These are chlorine, iron, manganese,
boron, zinc, copper, nickel, and molybdenum.
Hydroponic culture - used
by researchers to
determine which chemical
elements are essential
TECHNIQUE
Control: Solution
containing all minerals
Experimental: Solution
without potassium
The 17 Essential Elements = Micro- and Macro- Nutrients
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Symptoms of Mineral Deficiency
• Symptoms of mineral deficiency depend on the
nutrient’s function and mobility within the plant.
• Deficiency of a mobile nutrient usually affects
older organs more than young ones.
• Deficiency of a less mobile nutrient usually
affects younger organs more than older ones.
• The most common deficiencies are those of
nitrogen, potassium, and phosphorus.
The most common mineral deficiencies, as seen in maize leaves
Healthy
Phosphate-deficient
Potassium-deficient
Nitrogen-deficient
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Improving Plant Nutrition by Genetic
Modification: Some Examples
Genetic engineering can improve plant nutrition
and fertilizer usage:
• Resistance to Aluminum Toxicity
• Flood Tolerance
• Smart Plants
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Resistance to Aluminum Toxicity
• Aluminum in acidic soils damages roots and
greatly reduces crop yields.
• The introduction of bacterial genes into plant
genomes can cause plants to secrete acids
that bind to and tie up aluminum.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Flood Tolerance
• Waterlogged soils deprive roots of oxygen and
cause buildup of ethanol and toxins.
• The gene Submergence 1A-1 is responsible for
submergence tolerance in flood-resistant rice.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Smart Plants
• “Smart” plants inform the grower of a nutrient
deficiency before damage has occurred.
• A blue tinge indicates when these plants need
phosphate-containing fertilizer.
Deficiency warnings from “smart” plants
No phosphorus
deficiency
Beginning
phosphorus
deficiency
Well-developed
phosphorus
deficiency
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Plant nutrition often involves relationships with
other organisms
• Plants and soil microbes have a mutualistic
relationship ++
– Dead plants provide energy needed by soil-
dwelling microorganisms.
– Secretions from living roots support a wide
variety of microbes in the near-root
environment.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Soil Bacteria and Plant Nutrition
• The layer of soil bound to the plant’s roots is
the rhizosphere.
• The rhizosphere has high microbial activity
because of sugars, amino acids, and organic
acids secreted by roots.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Rhizobacteria
• Free-living rhizobacteria thrive in the
rhizosphere, and some can enter roots.
• Rhizobacteria can play several roles:
– Produce hormones that stimulate plant
growth
– Produce antibiotics that protect roots from
disease
– Absorb toxic metals or make nutrients more
available to roots.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Bacteria in the Nitrogen Cycle
• Nitrogen can be an important limiting nutrient for plant
growth.
• The nitrogen cycle transforms nitrogen and nitrogen-
containing compounds. Most soil nitrogen comes from
actions of soil bacteria.
• Plants absorb nitrogen as either NO3
– or NH4
+
• Bacteria break down organic compounds or use N2 to
produce NH3, which is converted to NH4
+
• Nitrification is carried out by bacteria that convert NH3
into NO3
– .
The role of soil bacteria in the nitrogen nutrition of plants
Atmosphere
Atmosphere
N2
N2
Soil
Nitrogen-fixing bacteria
Soil
H+
(from soil)
Ammonifying
bacteria
NH3
(ammonia)
NH4
+
(ammonium) Nitrifying
bacteria
Organic material (humus)
N2
NO3
–
(nitrate)
Denitrifying
bacteria
NH4
+
Nitrate and
nitrogenous
organic
compounds
exported in
xylem to
shoot system
Root
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Nitrogen-Fixing Bacteria: A Closer Look
• N2 is abundant in the atmosphere, but
unavailable to plants.
• Nitrogen fixation is the conversion of nitrogen
from N2 to NH3.
• Symbiotic relationships with nitrogen-fixing
bacteria provide some plant species with a
built-in source of fixed nitrogen.
• Key symbioses occur between nitrogen-fixing
bacteria and plants, including those in the
legume family (peas, beans, and other similar
plants)
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
• Along a legume’s roots are swellings called
nodules, composed of plant cells “infected” by
nitrogen-fixing Rhizobium bacteria.
• Inside the root nodule, Rhizobium bacteria
assume a form called bacteroids, which are
contained within vesicles formed by the root
cell.
• The bacteria of a root nodule obtain sugar from
the plant and supply the plant with fixed
nitrogen ++ mutualism.
Root nodules on legume plants
Nodules
Roots
(a) Pea plant root (b) Bacteroids in a soybean root
nodule
5 µm
Bacteroids
within
vesicle
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
• Each legume species is associated with a
particular strain of Rhizobium.
• The development of a nitrogen-fixing root
nodule depends on chemical dialogue between
Rhizobium bacteria and root cells of their
specific plant hosts.
Development
of a soybean
root nodule
Rhizobium
bacteria
Infection thread
Chemical signals
attract bacteria
1
1
2
2
3
3
4
4
Infected root hair
Bacteroid
Bacteroids form
Dividing cells
in root cortex
Dividing cells in
pericycle
Developing
root nodule
Bacteroid
Nodule
forms
Nodule
vascular
tissue
Bacteroid
Nodule develops
vascular tissue
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Nitrogen Fixation and Agriculture
• Crop rotation takes advantage of the agricultural
benefits of symbiotic nitrogen fixation.
• A non-legume such as maize is planted one year, and
the next year a legume is planted to restore the
concentration of fixed nitrogen in the soil.
• Instead of being harvested, the legume crop is often
plowed under to decompose as “green manure” and
reduce the need for manufactured fertilizer.
• Non-legumes such as alder trees, certain tropical
grasses, and rice benefit either directly or indirectly
from nitrogen-fixing bacteria.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Fungi and Plant Nutrition
• Mycorrhizae are mutualistic associations of
fungi and roots ++.
• The fungus benefits from a steady supply of
sugar from the host plant.
• The host plant benefits because the fungus
increases the surface area for water uptake
and mineral absorption.
• Mycorrizal relationships are common and might
have helped plants to first colonize land.
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
The Two Main Types of Mycorrhizae
• In ectomycorrhizae, the mycelium of the fungus
forms a dense sheath over the surface of the root.
• These hyphae form a network in the apoplast, but do
not penetrate the root cells.
• In arbuscular endomycorrhizae, microscopic fungal
hyphae extend into the root.
• These mycorrhizae penetrate the cell wall but not the
plasma membrane to form branched arbuscules within
root cells.
Epidermis
Mantle - fungal sheath
(a) Ectomycorrhizae
Cortex Mantle
(fungal
sheath)
Endodermis
Fungal
hyphae
between
cortical
cells (colorized SEM)
100 µm
10 µm
Cortical cells
Endodermis
Fungal
vesicle
Casparian
strip
Arbuscules
Plasma
membrane (LM, stained specimen)
Cortex
Epidermis
Fungal
hyphae
Root
hair
(b) Endomycorrhizae Arbuscular mycorrhizae
In endomycorrhizae, microscopic fungal hyphae extend
into the root
Epidermis
Fungal
hyphae
Cortex
Endodermis
Fungal
vesicle
Casparian
strip
Arbuscules
Plasma
membrane
Root
hair
Arbuscular mycorrhizae (endomycorrhizae)
Cortical cells
10 µm
(LM, stained specimen)
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Agricultural and Ecological Importance of
Mycorrhizae
• Farmers and foresters often inoculate seeds
with fungal spores to promote formation of
mycorrhizae.
• Some invasive exotic plants disrupt interactions
between native plants and their mycorrhizal
fungi.
Question: Does the invasive weed garlic mustard disrupt mutualistic
associations between native tree seedlings and arbuscular mycorrhizal
fungi?
EXPERIMENT
Increase
in
plant
biomass
(%)
RESULTS
Invaded Uninvaded Sterilized
invaded
Sterilized
uninvaded
0
100
200
300
Soil type
Mycorrhizal
colonization
(%)
0
10
20
30
40
Invaded Uninvaded
Soil type
Seedlings
Sugar maple
Red maple
White ash
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
Epiphytes, Parasitic Plants, and Carnivorous
Plants
Some plants have nutritional adaptations that use other
organisms in nonmutualistic ways:
• Epiphyte plants + 0 grows on another plant and
obtains water and minerals from rain.
• Parasitic plants + - absorb sugars and minerals
from their living host plant.
• Carnivorous plants are photosynthetic but obtain
nitrogen by killing and digesting mostly insects.
Unusual nutritional adaptations in plants
Staghorn fern, an epiphyte
Unusual nutritional adaptations in plants
Mistletoe, a photosynthetic parasite
Unusual nutritional adaptations in plants
Dodder, a nonphotosynthetic parasite
Dodder
Host’s phloem
Haustoria
Unusual nutritional adaptations in plants
Carnivorous plants
Unusual nutritional adaptations in plants
Carnivorous plants
Pitcher plants
Unusual nutritional adaptations in plants
Carnivorous plants
Sundews
Review
N2 (from atmosphere)
Nitrogen-fixing
bacteria
H+
(from soil)
(to atmosphere)
Denitrifying
bacteria
N2
NO3
–
(nitrate)
Nitrifying
bacteria
NH4
+
(ammonium)
NH3
(ammonia)
Ammonifying
bacteria
Organic
material (humus) Root
NH4
+
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
You should now be able to:
1. Define soil texture and soil composition.
2. Explain why plants cannot extract all of the
water in soil.
3. Define cation exchange and describe how
plants can stimulate the process.
4. Discuss the problems of topsoil erosion and
farm irrigation in arid regions; suggest actions
that can help mitigate these problems.
5. Distinguish between and list the
macronutrients and micronutrient.s
Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings
6. Explain how a nutrient’s role and mobility
determine the symptoms of a mineral
deficiency.
7. Summarize the ecological role of each of the
following groups of bacteria: ammonifying,
denitrifying, nitrogen-fixing, nitrifying.
8. Describe the basis for crop rotation.
9. Distinguish between ectomycorrhizae and
arbuscular mycorrhizae.
10.Describe the adaptations for nutrition of
parasitic, epiphytic, and carnivorous plants.

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37_lecture_presentation_0.ppt

  • 1. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings PowerPoint® Lecture Presentations for Biology Eighth Edition Neil Campbell and Jane Reece Lectures by Chris Romero, updated by Erin Barley with contributions from Joan Sharp Chapter 37 Soil and Plant Nutrition
  • 2. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Overview: “The Nation that Destroys Its Soil Destroys Itself” • Farmland productivity often suffers from chemical contamination, mineral deficiencies, acidity, salinity, and poor drainage. • Healthy soils improve plant growth by enhancing plant nutrition. • Typically, plants obtain carbon dioxide from the air, and water and minerals from the soil.
  • 3. Dust Bowl ---> Could this Happen Again??
  • 4. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Soil is a living, finite resource • Plants obtain most of their water and minerals from the upper layers of soil. • Living organisms play an important role in these soil layers. • This complex ecosystem is fragile.
  • 5. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Soil Texture • Soil particles are classified by size; from largest to smallest they are called sand, silt, and clay. • Soil is stratified into layers = soil horizons. • Topsoil consists of mineral particles, living organisms, and humus = the decaying organic material.
  • 7. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings • After a heavy rainfall, water drains from the larger spaces in the soil, but smaller spaces retain water because of its attraction to clay and other particles. • The film of loosely bound water is usually available to plants. • Loams are the most fertile topsoils and contain equal amounts of sand, silt, and clay. Soil
  • 8. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Topsoil Composition • A soil’s composition refers to: ** its inorganic (mineral) AND ** organic chemical components.
  • 9. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Inorganic Components • Cations (for example K+, Ca2+, Mg2+) adhere to negatively charged soil particles. • This adhering of cations prevents them from leaching out of the soil through percolating groundwater.
  • 10. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings • During cation exchange, cations are displaced from soil particles by other cations. • Displaced cations enter the soil solution and can be taken up by plant roots. • Negatively charged ions do not bind with soil particles and can be lost from the soil by leaching.
  • 11. Cation exchange in soil Soil particle – – – – – – – – – K+ K+ K+ Ca2+ Ca2+ Mg2+ H+ H+ H2O + CO2 H2CO3 HCO3 – + Root hair Cell wall
  • 12. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Organic Components • Humus builds a crumbly soil that retains water but is still porous. • It also increases the soil’s capacity to exchange cations and serves as a reservoir of mineral nutrients. • Topsoil contains bacteria, fungi, algae, other protists, insects, earthworms, nematodes, and plant roots. • These organisms help to decompose organic material and mix the soil -- detrivores.
  • 13. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Soil Conservation and Sustainable Agriculture • In contrast with natural ecosystems, agriculture depletes the mineral content of soil, taxes water reserves, and encourages erosion. • The goal of sustainable agriculture is to use farming methods that are conservation-minded, environmentally safe, and profitable.
  • 14. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Irrigation • Irrigation is a huge drain on water resources when used for farming in arid regions. • The primary source of irrigation water is underground water reserves called aquifers. • The depleting of aquifers can result in subsidence = the settling or sinking of land.
  • 15. Land subsidence caused by excessive removal of groundwater Land subsidence in California Sinkhole in Florida
  • 16. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings • Irrigation can lead to salinization = the concentration of salts in soil as water evaporates. • Drip irrigation requires less water and reduces salinization.
  • 17. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Fertilization • Soils can become depleted of nutrients as plants and the nutrients they contain are harvested. • Fertilization replaces mineral nutrients that have been lost from the soil. • Commercial fertilizers are enriched in nitrogen, phosphorus, and potassium. • Organic fertilizers are composed of manure, fishmeal, or compost.
  • 18. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Adjusting Soil pH • Soil pH affects cation exchange and the chemical form of minerals. • Cations are more available in slightly acidic soil, as H+ ions displace mineral cations from clay particles.
  • 19. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Controlling Erosion • Topsoil from thousands of acres of farmland is lost to water and wind erosion each year in the United States. • Erosion of soil causes loss of nutrients.
  • 20. Contour tillage helps reduce soil erosion
  • 21. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings • Erosion can be reduced by: – Planting trees as windbreaks – Terracing hillside crops – Cultivating in a contour pattern – Practicing no-till agriculture.
  • 22. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Preventing Soil Compaction • Soil compaction from heavy equipment reduces pore space between soil particles. • Soil compaction slows gas exchange and reduces root growth.
  • 23. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Phytoremediation • Some areas are unfit for agriculture because of contamination of soil or groundwater with toxic pollutants. • Phytoremediation is a biological, nondestructive technology that reclaims contaminated areas. • Plants capable of extracting soil pollutants are grown and are then disposed of safely.
  • 24. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Concept 37.2: Plants require essential elements to complete their life cycle • Plants derive most of their organic mass from the CO2 of air, but they also depend on soil nutrients such as water and minerals.
  • 25. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Macronutrients and Micronutrients • A chemical element is considered an essential element if it is required for a plant to complete its life cycle. • Nine of the essential elements are called macronutrients because plants require them in relatively large amounts. The macronutrients are carbon, oxygen, hydrogen, nitrogen, phosphorus, sulfur, potassium, calcium, and magnesium. • Eight of the essential elements are called micronutrients because plants need them in very small amounts. These are chlorine, iron, manganese, boron, zinc, copper, nickel, and molybdenum.
  • 26. Hydroponic culture - used by researchers to determine which chemical elements are essential TECHNIQUE Control: Solution containing all minerals Experimental: Solution without potassium
  • 27. The 17 Essential Elements = Micro- and Macro- Nutrients
  • 28. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Symptoms of Mineral Deficiency • Symptoms of mineral deficiency depend on the nutrient’s function and mobility within the plant. • Deficiency of a mobile nutrient usually affects older organs more than young ones. • Deficiency of a less mobile nutrient usually affects younger organs more than older ones. • The most common deficiencies are those of nitrogen, potassium, and phosphorus.
  • 29. The most common mineral deficiencies, as seen in maize leaves Healthy Phosphate-deficient Potassium-deficient Nitrogen-deficient
  • 30. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Improving Plant Nutrition by Genetic Modification: Some Examples Genetic engineering can improve plant nutrition and fertilizer usage: • Resistance to Aluminum Toxicity • Flood Tolerance • Smart Plants
  • 31. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Resistance to Aluminum Toxicity • Aluminum in acidic soils damages roots and greatly reduces crop yields. • The introduction of bacterial genes into plant genomes can cause plants to secrete acids that bind to and tie up aluminum.
  • 32. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Flood Tolerance • Waterlogged soils deprive roots of oxygen and cause buildup of ethanol and toxins. • The gene Submergence 1A-1 is responsible for submergence tolerance in flood-resistant rice.
  • 33. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Smart Plants • “Smart” plants inform the grower of a nutrient deficiency before damage has occurred. • A blue tinge indicates when these plants need phosphate-containing fertilizer.
  • 34. Deficiency warnings from “smart” plants No phosphorus deficiency Beginning phosphorus deficiency Well-developed phosphorus deficiency
  • 35. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Plant nutrition often involves relationships with other organisms • Plants and soil microbes have a mutualistic relationship ++ – Dead plants provide energy needed by soil- dwelling microorganisms. – Secretions from living roots support a wide variety of microbes in the near-root environment.
  • 36. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Soil Bacteria and Plant Nutrition • The layer of soil bound to the plant’s roots is the rhizosphere. • The rhizosphere has high microbial activity because of sugars, amino acids, and organic acids secreted by roots.
  • 37. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Rhizobacteria • Free-living rhizobacteria thrive in the rhizosphere, and some can enter roots. • Rhizobacteria can play several roles: – Produce hormones that stimulate plant growth – Produce antibiotics that protect roots from disease – Absorb toxic metals or make nutrients more available to roots.
  • 38. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Bacteria in the Nitrogen Cycle • Nitrogen can be an important limiting nutrient for plant growth. • The nitrogen cycle transforms nitrogen and nitrogen- containing compounds. Most soil nitrogen comes from actions of soil bacteria. • Plants absorb nitrogen as either NO3 – or NH4 + • Bacteria break down organic compounds or use N2 to produce NH3, which is converted to NH4 + • Nitrification is carried out by bacteria that convert NH3 into NO3 – .
  • 39. The role of soil bacteria in the nitrogen nutrition of plants Atmosphere Atmosphere N2 N2 Soil Nitrogen-fixing bacteria Soil H+ (from soil) Ammonifying bacteria NH3 (ammonia) NH4 + (ammonium) Nitrifying bacteria Organic material (humus) N2 NO3 – (nitrate) Denitrifying bacteria NH4 + Nitrate and nitrogenous organic compounds exported in xylem to shoot system Root
  • 40. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Nitrogen-Fixing Bacteria: A Closer Look • N2 is abundant in the atmosphere, but unavailable to plants. • Nitrogen fixation is the conversion of nitrogen from N2 to NH3. • Symbiotic relationships with nitrogen-fixing bacteria provide some plant species with a built-in source of fixed nitrogen. • Key symbioses occur between nitrogen-fixing bacteria and plants, including those in the legume family (peas, beans, and other similar plants)
  • 41. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings • Along a legume’s roots are swellings called nodules, composed of plant cells “infected” by nitrogen-fixing Rhizobium bacteria. • Inside the root nodule, Rhizobium bacteria assume a form called bacteroids, which are contained within vesicles formed by the root cell. • The bacteria of a root nodule obtain sugar from the plant and supply the plant with fixed nitrogen ++ mutualism.
  • 42. Root nodules on legume plants Nodules Roots (a) Pea plant root (b) Bacteroids in a soybean root nodule 5 µm Bacteroids within vesicle
  • 43. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings • Each legume species is associated with a particular strain of Rhizobium. • The development of a nitrogen-fixing root nodule depends on chemical dialogue between Rhizobium bacteria and root cells of their specific plant hosts.
  • 44. Development of a soybean root nodule Rhizobium bacteria Infection thread Chemical signals attract bacteria 1 1 2 2 3 3 4 4 Infected root hair Bacteroid Bacteroids form Dividing cells in root cortex Dividing cells in pericycle Developing root nodule Bacteroid Nodule forms Nodule vascular tissue Bacteroid Nodule develops vascular tissue
  • 45. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Nitrogen Fixation and Agriculture • Crop rotation takes advantage of the agricultural benefits of symbiotic nitrogen fixation. • A non-legume such as maize is planted one year, and the next year a legume is planted to restore the concentration of fixed nitrogen in the soil. • Instead of being harvested, the legume crop is often plowed under to decompose as “green manure” and reduce the need for manufactured fertilizer. • Non-legumes such as alder trees, certain tropical grasses, and rice benefit either directly or indirectly from nitrogen-fixing bacteria.
  • 46. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Fungi and Plant Nutrition • Mycorrhizae are mutualistic associations of fungi and roots ++. • The fungus benefits from a steady supply of sugar from the host plant. • The host plant benefits because the fungus increases the surface area for water uptake and mineral absorption. • Mycorrizal relationships are common and might have helped plants to first colonize land.
  • 47. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings The Two Main Types of Mycorrhizae • In ectomycorrhizae, the mycelium of the fungus forms a dense sheath over the surface of the root. • These hyphae form a network in the apoplast, but do not penetrate the root cells. • In arbuscular endomycorrhizae, microscopic fungal hyphae extend into the root. • These mycorrhizae penetrate the cell wall but not the plasma membrane to form branched arbuscules within root cells.
  • 48. Epidermis Mantle - fungal sheath (a) Ectomycorrhizae Cortex Mantle (fungal sheath) Endodermis Fungal hyphae between cortical cells (colorized SEM) 100 µm 10 µm Cortical cells Endodermis Fungal vesicle Casparian strip Arbuscules Plasma membrane (LM, stained specimen) Cortex Epidermis Fungal hyphae Root hair (b) Endomycorrhizae Arbuscular mycorrhizae
  • 49. In endomycorrhizae, microscopic fungal hyphae extend into the root Epidermis Fungal hyphae Cortex Endodermis Fungal vesicle Casparian strip Arbuscules Plasma membrane Root hair Arbuscular mycorrhizae (endomycorrhizae) Cortical cells 10 µm (LM, stained specimen)
  • 50. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Agricultural and Ecological Importance of Mycorrhizae • Farmers and foresters often inoculate seeds with fungal spores to promote formation of mycorrhizae. • Some invasive exotic plants disrupt interactions between native plants and their mycorrhizal fungi.
  • 51. Question: Does the invasive weed garlic mustard disrupt mutualistic associations between native tree seedlings and arbuscular mycorrhizal fungi? EXPERIMENT Increase in plant biomass (%) RESULTS Invaded Uninvaded Sterilized invaded Sterilized uninvaded 0 100 200 300 Soil type Mycorrhizal colonization (%) 0 10 20 30 40 Invaded Uninvaded Soil type Seedlings Sugar maple Red maple White ash
  • 52. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings Epiphytes, Parasitic Plants, and Carnivorous Plants Some plants have nutritional adaptations that use other organisms in nonmutualistic ways: • Epiphyte plants + 0 grows on another plant and obtains water and minerals from rain. • Parasitic plants + - absorb sugars and minerals from their living host plant. • Carnivorous plants are photosynthetic but obtain nitrogen by killing and digesting mostly insects.
  • 53. Unusual nutritional adaptations in plants Staghorn fern, an epiphyte
  • 54. Unusual nutritional adaptations in plants Mistletoe, a photosynthetic parasite
  • 55. Unusual nutritional adaptations in plants Dodder, a nonphotosynthetic parasite Dodder Host’s phloem Haustoria
  • 56. Unusual nutritional adaptations in plants Carnivorous plants
  • 57. Unusual nutritional adaptations in plants Carnivorous plants Pitcher plants
  • 58. Unusual nutritional adaptations in plants Carnivorous plants Sundews
  • 59. Review N2 (from atmosphere) Nitrogen-fixing bacteria H+ (from soil) (to atmosphere) Denitrifying bacteria N2 NO3 – (nitrate) Nitrifying bacteria NH4 + (ammonium) NH3 (ammonia) Ammonifying bacteria Organic material (humus) Root NH4 +
  • 60. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings You should now be able to: 1. Define soil texture and soil composition. 2. Explain why plants cannot extract all of the water in soil. 3. Define cation exchange and describe how plants can stimulate the process. 4. Discuss the problems of topsoil erosion and farm irrigation in arid regions; suggest actions that can help mitigate these problems. 5. Distinguish between and list the macronutrients and micronutrient.s
  • 61. Copyright © 2008 Pearson Education, Inc., publishing as Pearson Benjamin Cummings 6. Explain how a nutrient’s role and mobility determine the symptoms of a mineral deficiency. 7. Summarize the ecological role of each of the following groups of bacteria: ammonifying, denitrifying, nitrogen-fixing, nitrifying. 8. Describe the basis for crop rotation. 9. Distinguish between ectomycorrhizae and arbuscular mycorrhizae. 10.Describe the adaptations for nutrition of parasitic, epiphytic, and carnivorous plants.