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3–3 Cycles of Matter
Photo Credit: ©Bruce Coleman, LTD/Natural Selection
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3-3 Cycles of Matter
How does matter move among the living and nonliving parts of an ecosystem?
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3. Recycling in the Biosphere
Energy and matter move through the biosphere very differently.
Unlike the one-way flow of energy, matter is recycled within and between ecosystems.
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4. Recycling in the Biosphere
Matter (elements, chemical compounds, etc.) are passed from one organism to another
Matter is assembled into living tissue, passed out of the body, or decomposed.
AND from one part of the biosphere to another through biogeochemical cycles.
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What are the two reasons we need food?
Energy. Organic compounds (carbs, lipids, proteins, and nucleic acids)
Build us. Organic compounds contain the carbon, hydrogen, oxygen, nitrogen, phosphorus, and sulfur that make up most of our bodies.
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The Water Cycle
The Water Cycle
All living things require water to survive.
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The Water Cycle
Water moves between the ocean, atmosphere, and land.
This diagram shows the main processes involved in the water cycle. Scientists estimate that it can take a single water molecule as long as 4000 years to complete one cycle.
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Nutrient Cycles
How are nutrients important in living systems?
Remember the two reasons why you need food (nutrients):
--For energy and building materials
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Nutrient Cycles
Nutrient Cycles
All the chemical substances that an organism needs to sustain life are its nutrients.
Every living organism needs nutrients to build tissues and carry out essential life functions.
Similar to water, nutrients are passed between organisms and the environment through biogeochemical cycles.
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10. Rembember this chart? Matter is neither created nor destroyed
Group Name
Chemical composition (made up of…)
Examples
Function (job) in living things
CARBOHYDRATES
C,H,O
LIPIDS
NUCLEIC ACIDS
C,H,O,N, P
PROTEINS
C,H,O,N, S
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Nutrient Cycles
The Carbon Cycle
Carbon is a key ingredient of living tissue.
Biological processes
such as photosynthesis, respiration, and decomposition, take up and release carbon and oxygen.
Geochemical processes
such as erosion and volcanic activity, release carbon dioxide to the atmosphere and oceans.
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Nutrient Cycles
CO2 in Atmosphere
Photosynthesis
Volcanic activity
feeding
Respiration
Erosion
Human activity
Respiration
Decomposition
CO2 in Ocean
Uplift
Carbon is found in several large reservoirs in the biosphere. In the atmosphere, it is found as carbon dioxide gas; in the oceans as dissolved carbon dioxide; on land in organisms, rocks, and soil; and underground as coal, petroleum, and calcium carbonate rock. 
Deposition
Photosynthesis
feeding
Fossil fuel
Deposition
Carbonate Rocks
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Nutrient Cycles
The Nitrogen Cycle
All organisms require nitrogen to make nucleic acids and proteins!
Although nitrogen gas is the most abundant form of nitrogen on Earth-80% of atmosphere is N2 gas. THIS IS UNUSABLE BY ALMOST EVERYTHING, EXCEPT…
Bacteria live in the soil and on the roots of plants called legumes (beans, clover, etc.).
They convert nitrogen gas (unusable form) into ammonia (usable form) in a process known as nitrogen fixation.
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Nutrient Cycles
THEN…
Other bacteria in the soil convert ammonia into nitrates and nitrites.
Once these products are available, producers can use them to make proteins.
Consumers then eat the producers and reuse the nitrogen to make their own proteins or nucleic acids.
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15. NH3 N2 in Atmosphere NO3 and NO2 Nutrient Cycles
Synthetic fertilizer manufacturer
Atmospheric nitrogen fixation
Denitrification
Uptake by producers
Reuse by consumers
Uptake by producers
Reuse by consumers
The atmosphere is the main reservoir of nitrogen in the biosphere. Nitrogen also cycles through the soil and through the tissues of living organisms. 
Decomposition, excretion
Decomposition, excretion
Bacterial nitrogen fixation
NO3 and NO2
NH3
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Nutrient Cycles
When organisms die, decomposers return nitrogen to the soil as ammonia.
The ammonia may be taken up again by producers.
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Nutrient Cycles
Other soil bacteria convert nitrates into nitrogen gas in a process called denitrification.
This process releases nitrogen into the atmosphere once again.
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Nutrient Cycles
The Phosphorus Cycle
Phosphorus is essential to organisms because it helps forms important molecules like DNA and RNA.
Most phosphorus exists in the form of inorganic phosphate—in rocks. Inorganic phosphate is released into the soil and water as sediments wear down.
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Nutrient Cycles
Organic phosphate moves through the food web and to the rest of the ecosystem.
Organisms
Phosphorus in the biosphere cycles among the land, ocean sediments, and living organisms.
Land
Ocean
Sediments
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Nutrient Limitation
Nutrient Limitation
The primary productivity of an ecosystem is the rate at which organic matter (carbohydrates) is created by producers through photosynthesis.
One factor that controls the primary productivity of an ecosystem is the amount of available nutrients.
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Nutrient Limitation
If a nutrient is in short supply, it will limit an organism's growth.
When an ecosystem is limited by a single nutrient that is scarce or cycles very slowly, this substance is called a limiting nutrient.
Therefore: lower amounts of nitrogen or phosphorus LIMIT the growth of plants.
If a plant can’t make proteins or nucleic acids it can’t build or run itself.
What happens if large amounts of N or P are added?
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3–3
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3–3
Transpiration is part of the
water cycle.
carbon cycle.
nitrogen cycle.
phosphorus cycle.
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3–3
Carbon is found in the atmosphere in the form of
carbohydrates.
carbon dioxide.
calcium carbonate.
ammonia.
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3–3
Biologists describe nutrients as moving through cycles because the substances
start as simple organic forms that plants need.
provide “building blocks” and energy that organisms need.
are passed between organisms and the environment and then back to organisms.
are needed by organisms to carry out life processes.
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3–3
The only organisms that can convert nitrogen in the atmosphere into a form useful to living things are nitrogen-fixing
plants.
bacteria.
detritivores.
animals.
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3–3
When an aquatic ecosystem receives a large input of a limiting nutrient, the result is
runoff.
algal death.
algal bloom.
less primary productivity.
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