Ecosystems: Components,
Energy Flow, and Matter
Cycling
“All things come from earth, and to
earth they all return”—Menander
Ecosystem Organization
Organisms
Biosphere
Made of cells
Eukaryotic vs Prokaryotic
Species
Groups of organisms that resemble one
another in appearance, behavior, and
genetic make up
Sexual vs Asexual reproduction
Production of viable offspring in nature
1.5 million named; 10-14 million likely
Ecosystems
Communities
Populations
Genetic diversity
Communities
Ecosystems
Biosphere
Populations
Organisms
Fig. 4.2, p. 66
Earth’s Life Support Systems
Troposphere
To 11 miles
Air is here
Atmosphere
Biosphere
Vegetation and animals
Soil
Stratosphere
Crust
Rock
11 to 30 miles
Ozone layer
Hydrosphere
Solid, liquid, and
gaseous water
Lithosphere
Crust and upper
mantle
Contains nonrenewable res.
core
Lithosphere
Mantle
Crust
Crust
(soil and rock)
Biosphere
(Living and dead
organisms)
Hydrosphere
(water)
Lithosphere
(crust, top of upper mantle)
Atmosphere
(air)
Sustaining Life on Earth…
One way flow of
high quality
energy
The cycling of
matter (the
earth is a closed
system)
Gravity
Biosphere
Carbon
cycle
Phosphorus Nitrogen
cycle
cycle
Causes
downward
movement of
matter
Water
cycle
Heat in the environment
Heat
Heat
Heat
Oxygen
cycle
Major Ecosystem Components
Abiotic Components
Water, air,
temperature, soil,
light levels,
precipitation, salinity
Sets tolerance limits
for populations and
communities
Some are limiting
factors that structure
the abundance of
populations
Biotic Components
Producers, consumers,
decomposers
Plants, animals,
bacteria/fungi
Biotic interactions with
biotic components
include predation,
competition, symbiosis,
parasitism,
commensalism etc.
Limiting Factors on Land & in H2O
Terrestrial
Sunlight
Temperature
Precipitation
Soil nutrients
Fire frequency
Wind
Latitude
Altitude
Aquatic/Marine
Light penetration
• Water clarity
Water currents
Dissolved nutrient
concentrations
• Esp. N, P, Fe
Dissolved Oxygen
concentration
Salinity
The Source of High Quality Energy
Energy of sun
lights and
warms the
planet
Supports PSN
Powers the
cycling of
matter
Drives climate
and weather
that distribute
heat and H2O
Solar
radiation
Energy in = Energy out
Reflected by
atmosphere (34%)
Radiated by
atmosphere
as heat (66%)
UV radiation
Absorbed
by ozone
Lower Stratosphere
Visible (ozone layer)
Greenhouse
light
Troposphere
effect
Heat
Absorbed
by the earth
Heat radiated
by the earth
Earth
Fate of Solar Energy…
Earth gets 1/billionth of sun’s output of energy
34% is reflected away by atmosphere
66% is absorbed by chemicals in atmosphere
= re-radiated into space
Visible light, Infrared radiation (heat), and a
small amount of UV not absorbed by ozone
reaches the atmosphere
Energy warms troposphere and land
Evaporates water and cycles it along with gravity
Generates winds
A tiny fraction is captured by photosynthesizing
organisms
Natural greenhouse effect vs. Global Warming
Primary Productivity
The conversion of light
energy to chemical
energy is called “gross
primary production.”
Plants use the energy
captured in
photosynthesis for
maintenance and
growth.
The energy that is
accumulated in plant
biomass is called “net
primary production.”
Primary Productivity
NPP=GPP-respiration rate
GPP= RATE at which producers convert solar
energy into chemical energy as biomass
Rate at which producers use photosynthesis to fix
inorganic carbon into the organic carbon of their
tissues
These producers must use some of the total
biomass they produce for their own respiration
NPP= Rate at which energy for use by
consumers is stored in new biomass
(available to consumers)
Units Kcal/m2/yr or g/m2/yr
How do you measure it? AP Lab Site
Most productive vs. least productive
What are the most productive
Ecosystems?
Estuaries
Swamps and marshes
Tropical rain forest
Temperate forest
Northern coniferous forest (taiga)
Savanna
Agricultural land
Woodland and shrubland
Temperate grassland
Lakes and streams
Continental shelf
Open ocean
Tundra (arctic and alpine)
Desert scrub
Extreme desert
800
1,600
2,400
3,200
4,000
4,800
5,600
6,400
7,200
Average net primary productivity (kcal/m2/yr)
8,000
8,800
9,600
Fate of Primary Productivity and
Some important questions…
Since producers are ultimate source of all
food, why shouldn’t we just harvest the
plants of the world’s marshes?
Why don’t we clear cut tropical rainforests to
grow crops for humans?
Why not harvest primary producers of the
world’s vast oceans?
Vitousek et al: Humans now use, waste,
or destroy about 27% of earth’s total
potential NPP and 40% of the NPP of
the planet’s terrestrial ecosystems
Biotic Components of Ecosystems
Producers (autotrophs)
Source of all food
Photosynthesis
Heat
Consumers=heterotroph
Aerobic respiration
Anaerobic respiration
Methane, H2S
Abiotic chemicals
(carbon dioxide,
oxygen, nitrogen,
minerals)
Heat
Heat
Decomposers
(bacteria, fungus)
Producers
(plants)
Decomposers
Matter recyclers…
Release organic compounds Heat
into soil and water where they
can be used by producers
Consumers
(herbivores,
carnivores)
Heat
Solar
energy
Trophic Levels
Each organism in an ecosystem is assigned to
a feeding (or Trophic) level
Primary Producers
Primary Consumers (herbivores)
Secondary Consumer (carnivores)
Tertiary Consumers
Omnivores
Detritus feeders and scavengers
Directly consume tiny fragments of dead stuff
Decomposers
Digest complex organic chemicals into inorganic
nutrients that are used by producers
Complete the cycle of matter
Detritivores vs Decomposers stop
Detritus feeders
Bark beetle
engraving
Long-horned
beetle holes
Carpenter
ant
galleries
Decomposers
Termite and
carpenter
ant
work
Dry rot fungus
Wood
reduced
to powder
Time progression
Mushroom
Powder broken down by decomposers
into plant nutrients in soil
Fig. 4.15, p. 75
Energy Flow and Matter Cycling in Ecosystems…
Food Chains vs. Food Webs
KEY: There is little if no matter waste
in natural ecosystems!
First Trophic
Level
Producers
(plants)
Heat
Second Trophic
Level
Third Trophic
Level
Fourth Trophic
Level
Primary
consumers
(herbivores)
Secondary
consumers
(carnivores)
Tertiary
consumers
(top carnivores)
Heat
Heat
Heat
Solar
energy
Heat
Heat
Detritvores
(decomposers and detritus feeders)
Heat
Generalized Food Web of the Antarctic
Humans
Blue whale Sperm whale
Killer
whale
Note:
Arrows
Go in direction
Of energy
flow…
Elephant
seal
Crabeater seal
Leopard
seal
Emperor
penguin
Adélie
penguins
Petrel
Squid
Fish
Carnivorous plankton
Herbivorous
zooplankton
Krill
Fig. 4.18, p. 77
Phytoplankton
Food Webs and the Laws of matter and energy
Food chains/webs show how matter and
energy move from one organism to another
through an ecosystem
Each trophic level contains a certain amount
of biomass (dry weight of all organic matter)
Chemical energy stored in biomass is transferred
from one trophic level to the next
With each trophic transfer, some usable energy
is degraded and lost to the environment as low
quality heat
• Thus, only a small portion of what is eaten and
digested is actually converted into an organisms’
bodily material or biomass (WHAT LAW ACCOUNTS
FOR THIS?)
Food Webs and the Laws of matter and energy
Food chains/webs show how matter and energy
move from one organism to another through an
ecosystem
Each trophic level contains a certain amount of
biomass (dry weight of all organic matter)
Chemical energy stored in biomass is transferred from one
trophic level to the next
With each trophic transfer, some usable energy is degraded
and lost to the environment as low quality heat
• Thus, only a small portion of what is eaten and digested is
actually converted into an organisms’ bodily material or
biomass (WHAT LAW ACCOUNTS FOR THIS?)
Ecological Efficiency:
The % of usable nrg transferred as biomass from one
trophic level to the next (ranges from 5-20% in most
ecosystems, use 10% as a rule of thumb)
Thus, the more trophic levels or steps in a food chain, the
greater the cumulative loss of useable energy…
Food Webs and the Laws of matter and energy
Ecological Efficiency:
The % of usable energy transferred
as biomass from one trophic level to
the next (ranges from 5-20% in most
ecosystems, use 10% as a rule of
thumb)
Thus, the more trophic levels or steps
in a food chain, the greater the
cumulative loss of useable energy…
Pyramids of Energy and Matter
Pyramid of Energy Flow
Pyramid of Biomass
Heat
Tertiary
consumers
(human)
Heat
Decomposers
Heat
10
Secondary
consumers
(perch)
100
1,000
10,000
Usable energy
Available at
Each tropic level
(in kilocalories)
Heat
Primary
consumers
(zooplankton)
Producers
(phytoplankton)
Heat
Ecological Pyramids of Energy
Ecological Pyramids of Biomass
Implications of Pyramids….
Why could the earth support more people if
the eat at lower trophic levels?
Why are food chains and webs rarely more
than four or five trophic levels?
Why do marine food webs have greater
ecological efficiency and therefore more
trophic levels than terrestrial ones?
Why are there so few top level carnivores?
Why are these species usually the first to
suffer when the the ecosystems that support
them are disrupted?
ATMOSPHERE
LITHOSPHERE
HYDROSPHERE
ECOSPHERE
Ecosystem Services and Sustainability
Solar
Capital
Lessons
From
Nature!
Water
resources
and
purification
Air
resources
and
purification
Soil
formation
and
renewal
Waste
removal and
detoxification Natural
pest and
disease
control
Climate
control
Natural
Capital
Biodiversity
and gene
pool
Recycling
vital
chemicals
Renewable
energy
resources
Nonrenewable
energy
resources
Nonrenewable
mineral
Potentially resources
renewable
matter
resources
1. Use Renewable Solar Energy As Energy Source
2. Recycle the chemical nutrients needed for life
Matter Cycles
You are responsible for knowing the
water, carbon, nitrogen, sulfur, and
phosphorus cycles
Know major sources and sinks
Know major flows
Know how human activities are
disrupting these cycles
BIOGEOCHEMICAL CYCLES
‘Fundamentals’ of biogeochemical cycles
All matter cycles...it is neither created nor
destroyed...
As the Earth is essentially a closed system with
respect to matter, we can say that all matter on
Earth cycles .
Biogeochemical cycles: the movement (or
cycling) of matter through a system
by matter we mean: elements (carbon, nitrogen, oxygen)
or molecules (water)
so the movement of matter (for example carbon)
between these parts of the system is, practically
speaking, a biogeochemical cycle
The Cycling Elements:
macronutrients : required in relatively large amounts
"big six":
carbon , hydrogen , oxygen , nitrogen , phosphorous
sulfur
HYDROLOGIC CYCLE
CONNECTS
ALL OF
THE
CYCLES
AND
SPHERES
TOGETHER
Water Quality Degradation
IMPORTANCE OF CARBON
CYCLE
CARBON IS THE
BACKBONE OF LIFE!
Carbon Cycle
MARINE CARBON CYCLE
Diffusion between
atmosphere and ocean
Carbon dioxide
dissolved in
ocean water
photosynthesis
Combustion of fossil fuels
aerobic
respiration
Marine food webs
Producers, consumers,
decomposers, detritivores
incorporation
death,
sedimentation
into sediments
uplifting over
geologic time
sedimentation
Marine sediments, including
formations with fossil fuels
Figure 4-29a
Page 78
Slide 35
TERRESTRIAL CARBON CYCLE
Atmosphere
(most carbon is in carbon dioxide)
Combustion
of fossil
fuels
volcanic action
photosynthesis
Terrestrial
rocks
weathering
combustion of wood (for
aerobic
clearing land; or for fuel
respiration
Land food webs
producers,
consumers,
decomposers,
detritivores
Soil water
(dissolved
carbon)
leaching
runoff
death, burial, compaction
over geologic time
sedimentation
Peat,
fossil fuels
14
CO2 emissions from fossil fuel
(billion metric tons of carbon equivalent)
13
High
projection
12
11
10
Low
projection
9
8
7
6
5
4
3
2
1
0
1850
1900
1950
Year
2000
2030
Figure 4-30
Page 79
Slide 38
The Nitrogen Cycle
Nitrogen is a key element for
amino acids
nucleic acids (purine, pyrimidine)
cell wall components of bacteria (NAM).
Nitrogen Cycle
IMPORTANCE OF
PHOSPHOROUS CYCLE
1.Phosphorous is an essential nutrient of both
plants and animals.
2. It is part of DNA molecules which carry genetic
information.
3. It is part of ATP and ADP) that store chemical
energy for use by organisms in cellular respiration.
4. Forms phospholipids in cell membranes of
plants and animal cells.
5. Forms bones, teeth, and shells of animals as
calcium phosphate compounds.
PHOSPHOROUS CYCLE
mining
excretion
FERTILIZER
GUANO
agriculture
uptake by
autotrophs
MARINE
FOOD
WEBS
weathering
DISSOLVED
IN OCEAN
WATER
uptake by
autotrophs
leaching, runoff
DISSOLVED IN
SOIL WATER,
LAKES, RIVERS
death,
decomposition
sedimentation
death,
decomposition
weathering
settling out
uplifting over
geologic time
MARINE SEDIMENTS
ROCKS
LAND
FOOD
WEBS
http://3.bp.blogspot.com/_n9nytwY_jek/TS8oQCN8xHI/AAAAAAA
AACU/v5pYyLVVZkU/s640/eutrophication.gif
https://iboess.wikispaces.com/5.4+Eutrophication
SULFUR CYCLE
Water
Sulfur trioxide
Acidic fog and
precipitation
Sulfuric acid
Ammonia
Oxygen
Sulfur dioxide
Ammonium
sulfate
Hydrogen
sulfide
Plants
Volcano
Dimethyl
sulfide
Industries
Animals
Ocean
Sulfate salts
Metallic
sulfide
deposits
Decaying
matter
Sulfur
Hydrogen
sulfide
ROCK CYCLE
HUMAN IMPACTS ON ROCK
CYCLE
1. Humans are excavating minerals and
removing rock material. It takes millions of
years for rock to form.
2. Humans remove sediments for building
materials. This removes sediments that may
form sedimentary rocks in the future.
3. Humans are filling in wetlands
(peatlands), area that will form future coal
beds.
Works Cited
1. http://science.pppst.com/carboncycle.html
2. westernreservepublicmedia.org/earthmotion3/im
ages/Carbon_Cycle.ppt
3. climadods.ictp.it/d3/annalisa/ocean_sv/lecture1.ppt
4. www.geology.wmich.edu/Koretsky/envs2150/Pcyc
le_1.ppt