ecosystems and physical laws ecologists view ecosystems as transformers of energy and processors of...
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![Page 1: Ecosystems and Physical Laws Ecologists view ecosystems as transformers of energy and processors of matter Laws of physics and chemistry apply to ecosystems,](https://reader035.vdocument.in/reader035/viewer/2022062421/56649c865503460f9493dcf6/html5/thumbnails/1.jpg)
Ecosystems and Physical Laws
• Ecologists view ecosystems as transformers of energy and processors of matter
• Laws of physics and chemistry apply to ecosystems, particularly energy flow
• Energy is conserved but degraded to heat during ecosystem processes
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Trophic Relationships
• Energy and nutrients pass from primary producers (autotrophs) to primary consumers (herbivores) and then to secondary consumers (carnivores)
• Energy flows through an ecosystem, entering as light and exiting as heat
• Nutrients cycle within an ecosystem
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Microorganismsand other
detritivores
Tertiaryconsumers
Secondaryconsumers
Detritus Primary consumers
Sun
Primary producers
Heat
Key
Chemical cycling
Energy flow
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Decomposition
• Decomposition connects all trophic levels
• Detritivores, mainly bacteria and fungi, recycle essential chemical elements by decomposing organic material and returning elements to inorganic reservoirs
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Physical and chemical factors limit primary production in ecosystems
• Primary production in an ecosystem is the amount of light energy converted to chemical energy by autotrophs during a given time period
• The extent of photosynthetic production sets the spending limit for an ecosystem’s energy budget
• The amount of solar radiation reaching the Earth’s surface limits photosynthetic output of ecosystems
• Only a small fraction of solar energy actually strikes photosynthetic organisms
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Gross and Net Primary Production
• Total primary production is known as the ecosystem’s gross primary production (GPP)
• Net primary production (NPP) is GPP minus energy used by primary producers for respiration
• Only NPP is available to consumers
• Ecosystems vary greatly in net primary production and contribution to the total NPP on Earth
• Overall, terrestrial ecosystems contribute about two-thirds of global NPP and marine ecosystems contribute about one-third
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Open oceanContinental shelf
Upwelling zonesExtreme desert, rock, sand, ice
Swamp and marshLake and stream
Desert and semidesert scrubTropical rain forest
Temperate deciduous forestTemperate evergreen forest
Tropical seasonal forest
SavannaCultivated land
EstuaryAlgal beds and reefs
Boreal forest (taiga)Temperate grassland
Woodland and shrublandTundra
0.40.4
1.01.31.51.61.71.82.42.72.93.33.54.7
0.30.10.1
5.265.0
Freshwater (on continents)
Terrestrial
Marine
Key Percentage of Earth’ssurface area
Average net primaryproduction (g/m2/yr)
6050403020100 2,5002,0001,5001,0005000
Percentage of Earth’s netprimary production
2520151050
125
2,500
3601,500
5003.090
900600
800
2,200
600
250
1,6001,2001,300
2,000
700140
0.3
7.99.19.6
5.43.5
0.67.1
4.93.8
2.3
24.45.6
1.20.9
0.10.040.9
22
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Light Limitation
• Depth of light penetration affects primary production in the photic zone of an ocean or lake
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Nutrient Limitation
• More than light, nutrients limit primary production in geographic regions of the ocean and in lakes
• A limiting nutrient is the element that must be added for production to increase in an area
• Nitrogen and phosphorous are typically the nutrients that most often limit marine production
• Nutrient enrichment experiments confirmed that nitrogen was limiting phytoplankton growth in an area of the ocean
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Atlantic Ocean
ShinnecockBay
Moriches Bay
Long Island
2
45
30
1115
19
21
Coast of Long Island, New York
Great South Bay
Phytoplankton
Inorganicphosphorus
GreatSouth Bay
MorichesBay
ShinnecockBay
Station number2119153011542
8
5
4
3
21
0
6
78
5
4
3
21
0
6
7
Phytoplankton biomass and phosphorus concentration
Ph
yto
pla
nk
ton
(mil
lio
ns
of
cel
ls/m
L)
Ino
rga
nic
ph
os
ph
oru
s(µ
m a
tom
s/L
)
Ammonium enriched
Station number2119153011542
30
Ph
yto
pla
nk
ton
(mil
lio
ns
of
cel
ls p
er m
L)
Startingalgal
density
Phytoplankton response to nutrient enrichment
24
18
12
6
0
Phosphate enrichedUnenriched control
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• The addition of large amounts of nutrients to lakes has a wide range of ecological impacts
• In some areas, sewage runoff has caused eutrophication of lakes, which can lead to loss of most fish species
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Primary Production in Terrestrial and Wetland Ecosystems
• In terrestrial and wetland ecosystems, climatic factors such as temperature and moisture affect primary production on a large scale
• Actual evapotranspiration can represent the contrast between wet and dry climates
• Actual evapotranspiration is the water annually transpired by plants and evaporated from a landscape
• It is related to net primary production
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Control
August 1980JulyJune00
100
200
300L
ive,
ab
ove
-gro
un
d b
iom
ass
(g d
ry w
t/m
2 )
50
150
250N + P
N only
P only
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Energy transfer between trophic levels is usually less than 20% efficient
• Secondary production of an ecosystem is the amount of chemical energy in food converted to new biomass during a given period of time
• When a caterpillar feeds on a leaf, only about one-sixth of the leaf’s energy is used for secondary production
• An organism’s production efficiency is the fraction of energy stored in food that is not used for respiration
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Growth (new biomass)
Cellularrespiration
Feces100 J
33 J
67 J
200 J
Plant materialeaten by caterpillar
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Trophic Efficiency and Ecological Pyramids
• Trophic efficiency is the percentage of production transferred from one trophic level to the next
• It usually ranges from 5% to 20%
• A pyramid of net production represents the loss of energy with each transfer in a food chain
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1,000,000 J of sunlight
10,000 J
1,000 J
100 J
10 JTertiaryconsumers
Secondaryconsumers
Primaryconsumers
Primaryproducers
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Trophic level Dry weight(g/m2)
Tertiary consumers
Secondary consumers
Primary consumers
Primary producers
1.5
11
37
809
Most biomass pyramids show a sharp decrease in biomass at successively higher trophic levels, as illustrated by data from a bog at Silver Springs, Florida.
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Trophic level Dry weight(g/m2)
Primary consumers (zooplankton)
Primary producers (phytoplankton)
21
4
In some aquatic ecosystems, such as the English Channel, a small standing crop of primary producers (phytoplankton) supports a larger standing crop of primary consumers (zooplankton).
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Trophic level Number ofindividual organisms
Tertiary consumers
Secondary consumers
Primary consumers
Primary producers
3
354,904
708,624
5,842,424
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• The green world hypothesis proposes several factors that keep herbivores in check:
– Plant defenses
– Limited availability of essential nutrients
– Abiotic factors
– Intraspecific competition
– Interspecific interactions
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A General Model of Chemical Cycling
• Gaseous carbon, oxygen, sulfur, and nitrogen occur in the atmosphere and cycle globally
• Less mobile elements such as phosphorus, potassium, and calcium cycle on a more local level
• A model of nutrient cycling includes main reservoirs of elements and processes that transfer elements between reservoirs
• All elements cycle between organic and inorganic reservoirs
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Fossilization
Reservoir a Reservoir b
Reservoir c Reservoir d
Organicmaterialsavailable
as nutrients
Organicmaterialsunavailableas nutrients
Inorganicmaterialsavailable
as nutrients
Inorganicmaterialsunavailableas nutrients
Livingorganisms,detritus
Coal, oil,peat
Atmosphere,soil, water
Mineralsin rocks
Assimilation,photosynthesis Burning
of fossil fuels
Weathering,erosion
Formation ofsedimentary rock
Respiration,decomposition,excretion
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Biogeochemical Cycles
• In studying cycling of water, carbon, nitrogen, and phosphorus, ecologists focus on four factors:
1. Each chemical’s biological importance
2. Forms in which each chemical is available or used by organisms
3. Major reservoirs for each chemical
4. Key processes driving movement of each chemical through its cycle
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Transportover land
Precipitationover landEvaporation
from oceanPrecipitationover ocean
Net movement ofwater vapor by wind
Solar energy
Evapotranspirationfrom land
Runoff andgroundwater
Percolationthroughsoil
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Cellularrespiration
Burning offossil fuelsand wood
Carbon compoundsin water
Photosynthesis
Primaryconsumers
Higher-levelconsumers
Detritus
Decomposition
CO2 in atmosphere
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Assimilation
N2 in atmosphere
DecomposersNitrifyingbacteria
Nitrifyingbacteria
Nitrogen-fixingsoil bacteria
Denitrifyingbacteria
NitrificationAmmonification
Nitrogen-fixingbacteria in rootnodules of legumes
NO3–
NO2–NH4
+NH3
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Sedimentation
Plants
Rain
Runoff
Weatheringof rocks
Geologicuplift
SoilLeaching
Decomposition
Plant uptakeof PO4
3–
Consumption
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Decomposition and Nutrient Cycling Rates
• Decomposers (detritivores) play a key role in the general pattern of chemical cycling
• Rates at which nutrients cycle in different ecosystems vary greatly, mostly as a result of differing rates of decomposition
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Concrete dams and weirs built across streams at the bottom of watersheds enabled researchers to monitor the outflow of water and nutrients from the ecosystem.
One watershed was clear cut to study the effects of the loss of vegetation on drainage and nutrient cycling.
The concentration of nitrate in runoff from the deforested watershed was 60 times greater than in a control (unlogged) watershed.
Deforested
Control
Completion oftree cutting
Nit
rate
co
nce
ntr
atio
n in
ru
no
ff(m
g/L
)
1965 19681966 1967
80.0
60.0
40.0
20.0
4.0
3.0
2.0
1.0
0
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Agriculture and Nitrogen Cycling
• Agriculture removes nutrients from ecosystems that would ordinarily be cycled back into the soil
• Nitrogen is the main nutrient lost through agriculture; thus, agriculture greatly impacts the nitrogen cycle
• Industrially produced fertilizer is typically used to replace lost nitrogen, but effects on an ecosystem can be harmful
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Contamination of Aquatic Ecosystems
• Critical load for a nutrient is the amount that plants can absorb without damaging the ecosystem
• When excess nutrients are added to an ecosystem, the critical load is exceeded
• Remaining nutrients can contaminate groundwater and freshwater and marine ecosystems
• Sewage runoff causes cultural eutrophication, excessive algal growth that can greatly harm freshwater ecosystems
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Acid Precipitation
• Combustion of fossil fuels is the main cause of acid precipitation
• North American and European ecosystems downwind from industrial regions have been damaged by rain and snow containing nitric and sulfuric acid
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Field pH
5.35.2–5.35.1–5.25.0–5.14.9–5.04.8–4.94.7–4.84.6–4.74.5–4.64.4–4.54.3–4.4<4.3
5.3
5.3
5.35.3
5.3 5.3
5.3
5.2
5.3
5.6
5.9
5.4
5.2
5.2
5.2
5.2
5.4
5.56.0
5.0
5.4
6.3
5.3
5.3
6.1
5.5
5.4
5.4
5.4
5.4
5.6
5.5
5.5
5.6
5.65.2
5.1
5.15.74.9
5.7
5.0
5.0
5.0
5.04.9
4.9
4.9
4.9
4.14.3
4.3
4.34.4
4.44.4
4.4
4.4
4.5
4.54.5
4.54.5
4.54.5
4.5
4.5
4.54.5
4.5
4.5
4.5
4.54.5
4.5
4.54.5
4.5
4.5
4.64.6
4.64.6
4.6
4.6
4.64.6
4.64.64.6
4.64.6
4.6
4.7
4.7
4.74.74.7
4.7
4.7
4.74.7
4.7
4.74.7
4.7
4.7
4.7
4.84.8
4.8
4.8
4.8
4.8
4.8
4.8
4.8
5.0
5.0
5.3
5.2
5.1
5.1
5.1
5.1
5.2
5.25.2
5.3
5.4
5.4
5.5
5.5
4.74.7
4.7
4.7
4.7
4.7
4.7
4.9
4.8
4.8
4.64.7
4.7
4.7
4.84.8
4.8
4.8
4.9
4.9
4.9
5.0
5.0
5.0
5.1
5.1
5.0
5.0 5.05.1
5.2
5.3
5.45.4
5.7
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Toxins in the Environment
• Humans release many toxic chemicals, including synthetics previously unknown to nature
• In some cases, harmful substances persist for long periods in an ecosystem
• One reason toxins are harmful is that they become more concentrated in successive trophic levels
• In biological magnification, toxins concentrate at higher trophic levels, where biomass is lower
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Zooplankton0.123 ppm
Phytoplankton0.025 ppm
Lake trout4.83 ppm
Smelt1.04 ppm
Herringgull eggs124 ppm
Co
nc
en
tra
tio
n o
f P
CB
s
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Chlorine atoms
O3Chlorine
Cl2O2
CIO
O2
O2
CIO
Chlorine from CFCs interacts with ozone (O3), forming chlorine monoxide (CIO) and oxygen (O2).
Sunlight causes Cl2O2 to break down into O2 and free chlorine atoms. The chlorine atoms can begin the cycle again.
Two CIO molecules react, forming chlorine peroxide (Cl2O2).
Sunlight
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Animations and Videos• Chapter Quiz Questions – 1
• Chapter Quiz Questions – 2
• An Idealized Energy Pyramid
• Energy Flow and The Water Cycle
• The Global Hydrological Cycle
• The Carbon Cycle
• The Global Carbon Cycle
• Nitrogen Cycle
• The Global Nitrogen Cycle
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Animations and Videos• Phosphorus Cycle
• Sulfur Cycle
• Nitrogen Fixation Animation