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Transcript
Chapter Concepts
z Terrestrial Primary Production is generally
Chapter 18
PRIMARY PRODUCTION
AND ENERGY FLOW
Molles: Ecology 3RD Ed.
limited by temperature and moisture
z Aquatic Primary Production is generally
limited by nutrient availability
z Consumers can influence rates of primary
production in terrestrial and aquatic
ecosystems
z Energy losses limit the number of trophic
levels found in ecosystems
Molles: Ecology 3RD Ed.
Fundamental Concepts
z Primary Production – fixation of energy by
autotrophs in an ecosystem
z Rate of Primary Production – amount of
energy fixed over a given period of time
™ Gross
– Total amount of energy fixed by
autotrophs
™ Net – Amount of energy leftover after
autotrophs have met their metabolic needs
Molles: Ecology 3RD Ed.
Fundamental Concepts
z Trophic Level – Position in a food web
determined by number of energy transfers
from primary producers to current level:
™ Primary
producers occupy first level
™ Primary consumers occupy second level
™ Secondary consumers occupy third level
™ Tertiary consumers occupy fourth level
Molles: Ecology 3RD Ed.
1
Evapotranspiration and Terrestrial
Primary Production
z Rosenzweig estimated influence of moisture
and temperature on rates of primary
production by plotting relationship between
annual net primary production and annual
actual evapotranspiration (AET)
™ AET
– annual amount of water that
evaporates and transpires off a landscape
ƒ
Cold dry ecosystems tend to have low AET
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
Evapotranspiration and Terrestrial
Primary Production
™ Generally,
there is a positive relationship
between net primary production and AET
ƒ
Sala found east-west variation in primary
production correlated with rainfall
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
2
Soil Fertility and Terrestrial
Primary Production
z Significant variation in terrestrial primary
production can be explained by differences in
soil fertility
z Shaver and Chapin found arctic net primary
production was twice as high on fertilized
plots compared to unfertilized plots
z Bowman suggested N is main nutrient limiting
net primary production in a dry tundra
meadow, and N and P jointly limit production
in a wet meadow
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
Patterns of Aquatic Primary Production
z Several studies have found quantitative
relationship between phosphorus and
phytoplankton biomass
z Several studies support generalization
that nutrient availability controls rate of
primary production in freshwater
ecosystems
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
3
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
Whole Lake Experiments
z Founded in 1968
z In northwestern Ontario, Canada
z The Experimental Lakes Area
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
4
Molles: Ecology 3RD Ed.
Spring
Bloom in
the Arabian
Sea
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
5
50 - 20
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Bigeye Tuna: Catch Per Unit Effort
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BET 1990-2000
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BET
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marine phytoplankton are generally
concentrated in areas with higher levels of
nutrient availability
z Highest rates found along continental
margins
™ Nutrient
run-off from land
™ Sediment disturbance
z Open ocean tends to be nutrient poor
™ Vertical mixing main nutrient source
Molles: Ecology 3RD Ed.
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z Highest rates of primary production by
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The Bigeye Tuna
Global Patterns of Marine Primary
Production
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500
Molles: Ecology 3RD Ed.
! !
! ! ! !
- 20- 50
Equator
!
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<= 0.138
0.138-0.326
0.326-0.553
> 0.553
! !
!
Molles: Ecology 3RD Ed.
Global Patterns of Marine
Primary Production
z Graneli gathered results
suggesting rate or primary
production in Baltic Sea is
nutrient limited
™ Increased
nutrients led to
increased chlorophyll
concentrations
ƒ
N appears to be limiting
nutrient
Molles: Ecology 3RD Ed.
6
Global Patterns of Marine Primary
Production
z Residual Variation – proportion of variation
not explained by the independent variable
™ Dillon
and Rigler suggested environmental
factors besides nutrient availability
significantly influence phytoplankton
biomass
ƒ
Consumer Influences
z Bottom-Up Controls
™ Influences
of physical and chemical factors
of an ecosystem
z Top-Down Controls
™ Influences
of consumers
Intensity of predation on zooplankton
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
Lake Primary Production
z Carpenter proposed piscivores,
planktivorous fish can cause significant
deviations in primary productivity
z Carpenter and Kitchell proposed the
influence of consumers on lake primary
productivity propagate through food webs
™ Trophic
Molles: Ecology 3RD Ed.
Cascade Hypothesis
Molles: Ecology 3RD Ed.
7
Lake Primary Production
(Trophic Cascade hypothesis)
z Carpenter and Kitchell
™ Reduction
in planktivorous fish populations
led to reduced rates of primary production
™ In absence of planktivorous minnows,
predaceous invertebrates (zooplankton)
became more numerous
™ In presence of abundant, large herbivorous
zooplankton, phytoplankton biomass and rate
of primary production declined
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
Experimental manipulation
z Reduced piscivore (bass) biomass,
increased plankitivore biomass
z Increased piscivore biomass, decreased
plankitivore biomass
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
8
Responses
z Decreased herbivores, increased
phytoplankton
z Increased herbivores, Decreased
phytoplankton
Primary Production (PP) in the Serengeti
z McNaughton estimated
Serengeti grazers consume
an average of 66% of annual
primary production
™ Rate
z The responses of herbivores and
phytoplankton to manipulation of piscivore
and planktivore biomass support the trophic
cascade model
Molles: Ecology 3RD Ed.
of primary production
in the Serengeti is positively
correlated with rainfall
quantity
Molles: Ecology 3RD Ed.
Serengeti National Park
z Endless plain
z 14,763 sq. km
z in Northern
Tanzania
Molles: Ecology 3RD Ed.
PP in the Serengeti
z Found grazers can increase primary
production
™ Increased
ƒ
growth rate
Compensatory Growth
¾ Lower respiration rate due to lower
biomass
¾ Reduced self-shading
¾ Improved water balance due to reduced
leaf area
Molles: Ecology 3RD Ed.
9
PP in the Serengeti
z In addition, McNaughton found
compensatory growth highest at
intermediate grazing intensities
™ Light
grazing insufficient to produce
compensatory growth
™ Heavy grazing reduces plant’s capacity to
recover
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
Trophic Dynamic View of Ecosystems
z Lindeman concluded that the ecosystem
concept is fundamental to the study of
energy transfer within an ecosystem
™ Suggested
grouping organisms within an
ecosystem into trophic levels
ƒ
Each feeds on level immediately below
¾ As energy is transferred from one trophic
level to another, energy is degraded
¾ The 10% Law
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
10
Why SP is smaller than PP?
z Not all the plant biomass is consumed
(some is decomposed)
z Not all the eaten parts is assimilated
(some is lost in feces)
z Not all the energy assimilated is actually
converted to biomass (some is lost as
heat)
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
Pattern of
energy flow
through a
trophic
level
Molles: Ecology 3RD Ed.
The laws of thermodynamics
z 1st = Energy is neither created nor
destroyed
z 2nd = No energy conversion process is
100% efficient. Part of the energy is lost
in a form of heat to the environment that
is useless for further transfer
Molles: Ecology 3RD Ed.
11
Consumption efficiency
z Ingested energy
z Herbivores 5% in forests, 25% in grassland
& 50% in aquatic ecosystem
z Carnivore (vertebrate-vertebrate 50-100%,
vertebrate-invertebrate 5%, invertebrateinvertebrate 25%)
Molles: Ecology 3RD Ed.
Assimilation efficiency
z Energy taken that is assimilated
z Bacteria/fungi 100%
z Herbivore, detritivore, microbivore 20-50%
z Carnivore 80%
z Seed/fruit 60-70%
z Leaf 50%
z Wood 15%
Molles: Ecology 3RD Ed.
Production efficiency
“The 10% law”
z Assimilated energy that be included in
z Trophic transfer efficiency = CE*AE*PE
biomass
z Invertebrate 30-40%
z Ethotherm 10%
z Endotherm 1~2%
z Microorganism high
z Highly variable
Molles: Ecology 3RD Ed.
z 2~24% in general
z Mean = 10.1%, SE = 0.49
Molles: Ecology 3RD Ed.
12
Trophic Dynamic View of Ecosystems
™ As
energy is transferred from one trophic
level to another, energy is degraded:
Limited assimilation
ƒ Consumer respiration
ƒ Heat production
¾ Energy quality decreases with each
successive trophic level
– Pyramid-shaped energy distribution
ƒ
Molles: Ecology 3RD Ed.
Energy Flow - A Temperate Deciduous
Forest
z Gosz studied solar energy flow:
™ 15%
reflected
™ 41% converted to heat
™ 42% absorbed during evapotranspiration
™ 2.2% fixed by plants as gross primary
production
™ 1.2% used in plant respiration
™ 1% left for primary production
Molles: Ecology 3RD Ed.
Energy Flow - A Temperate Deciduous
Forest
z 99% of solar energy unavailable for use
by second trophic level
z As energy losses between trophic levels
accumulate, eventually there is
insufficient energy left to support a
viable population at a higher trophic
level
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
13
Summary
z Terrestrial Primary Production is generally
limited by temperature and moisture
z Aquatic Primary Production is generally
limited by nutrient availability
z Consumers can influence rates of primary
production in terrestrial and aquatic
ecosystems
z Energy losses limit the number of trophic
levels found in ecosystems
Molles: Ecology 3RD Ed.
Molles: Ecology 3RD Ed.
14