8.2 Energy Flow Through Ecosystems

Syllabus
2025
Topic
8.2
Level

Learning objectives

8.2A—Describe the strategies organisms use to acquire and use energyDescribe the strategies organisms use to acquire and use energy.• Organisms use energy to organize, grow, reproduce, and maintain homeostasis.- i. Organisms use different strategies to r egulate body temperature and metabolism. Endotherms use thermal energy generated by metabolism to maintain homeostatic body temperatures. Ectotherms lack efficient internal mechanisms for maintaining body temperature, although they may regulate their temperature behaviorally by moving into the sun or shade or by aggregating with other individuals.- ii. A net gain in energy results in energy stor age, the growth of an organism, and increased reproductive output.- iii. A net loss of energy results in loss of mass, a decreas e in reproductive output, and, eventually, the death of an organism.• Different organisms use various reproductive strategies in response to energy availability. Some organisms alternate between asexual and sexual reproduction in response to energy availability.8.2B—Explain how energy flows and matter cycles through trophic levelsExplain how energy flows and matter cycles through trophic levels.• Ecological levels of organization include populations, communities, ecosystems, and biomes.• Energy flows through ecosystems, while matter and nutrients cycle between the environment and organisms via biogeochemical cycles. The cycles are essential for life, and each cycle demonstrates the conservation of matter. The cycles are interdependent.• Biogeochemical cycles include abiotic and biotic reservoirs, as well as processes that cycle matter between reservoirs.• The hydrologic (water) cycle involves water movement and storage within the hydrosphere. Reservoirs include oceans, surface water, the atmosphere, and living organisms. Processes include evaporation, condensation, precipitation, and transpiration.• The carbon cycle involves recycling carbon atoms through Earth’s biosphere into organisms as carbohydrates and back into the atmosphere as carbon dioxide ()CO At the highest levels of organization, 2 . the carbon cycle can be simplified into four parts: photosynthesis, cellular respiration, decomposition, and combustion.• The nitrogen cycle involves several steps, including nitrogen fixation, assimilation, ammonification, nitrification, and denitrification. These steps are performed by microorganisms in the soil. The largest reservoir of nitrogen is the atmosphere. In nitrogen fixation, nitrogen gas ()N2 is fixed into ammonia ()NH3 , which ionizes to ammonium (NH + 4 ) by acquiring hydrogen ions from the soil solution.• The phosphorus cycle involves weathering rocks releasing phosphate ()PO 3− 4 into soil and groundwater. Producers take in phosphate, which is incorporated into biological molecules; consumers eat producers, transferring phosphate to animals. Phosphorus returns to the soil via decomposition of biomass, or excretion. Phosphate can also be incorporated back into the environment via decomposition of decaying organic matter.8.2C—Explain how changes in energy availability affect populations, communities, and ecosystemsExplain how changes in energy availability affect populations, communities, and ecosystems.• Changes in energy availability can result in changes in population size.• Changes in energy availability can result in disruptions to an ecosystem.- i. A change in energy resources such as sunlight can affect the number and size of the trophic levels. Trophic levels include producers; primary, secondary, tertiary, and quaternary consumers; and decomposers.- ii. A change in the biomass or number of producers in a given geographic area can affect the number and size of other trophic levels.8.2D—Explain how the activities of autotrophs and heterotrophs enable the flow of energy within an ecosystemExplain how the activities of autotrophs and heterotrophs enable the flow of energy within an ecosystem.• Autotrophs capture energy from physical or chemical sources in the environment.- i. Photosynthetic organisms capture energy present in sunlight contributing to primary productivity.- ii. Chemosynthetic organisms capture energy from small inorganic molecules present in their environment, which can occur in the absence of oxygen.• Heterotrophs, which include carnivores, herbivores, omnivores, decomposers, and scavengers, metabolize carbohydrates, lipids, and proteins as sources of energy. Heterotrophs capture the energy present in carbon compounds by consuming organic matter derived from autotrophs incorporating matter into their tissues. 156AP Biology Course and Exam Description Ecology UNIT 8

Organism Energy Budgets and Life Strategies

Organisms acquire and allocate energy to maintain organization and homeostasis, grow, and reproduce. Because available energy is limited, using more for one function can leave less for another.

Strategy Source of body-temperature regulation Energy implication
Endotherm Metabolism generates thermal energy that maintains a homeostatic body temperature Internal heat production requires metabolic energy
Ectotherm Internal temperature control is less efficient; behavior such as moving between sun and shade or aggregating can regulate temperature Environmental heat and behavior reduce reliance on metabolic heat production
Energy balance Biological outcomes
Net gain Energy storage, growth, and increased reproductive output
Net loss Loss of mass, decreased reproductive output, and eventually death if the loss persists

Energy availability can also change reproductive strategy. Some organisms alternate between asexual and sexual reproduction as energy conditions change, linking current resources to how energy is invested in offspring.

Ectotherms do regulate body temperature, but often through behavior rather than efficient internal heat production. Endothermy does not mean body temperature never varies or that energy supply is unlimited.

Energy Flows; Matter Cycles

Energy flows through trophic levels, whereas matter and nutrients cycle between organisms and the environment. Matter is conserved: atoms move among biotic and abiotic reservoirs through linked biogeochemical processes.

Population: one species in an area → community: interacting populations → ecosystem: community plus abiotic environment → biome: large region with characteristic ecological conditions.

Cycle Major reservoirs Processes moving matter
Water Oceans, surface water, atmosphere, organisms Evaporation, condensation, precipitation, transpiration
Carbon Atmosphere and carbon in organisms or other Earth reservoirs Photosynthesis, cellular respiration, decomposition, combustion
Nitrogen Atmosphere is the largest reservoir; soil and organisms also store nitrogen Nitrogen fixation, assimilation, ammonification, nitrification, denitrification; soil microorganisms perform these transformations
Phosphorus Rocks, soil, groundwater, organisms Weathering releases PO₄³⁻; uptake, feeding, excretion, and decomposition transfer or return it

During nitrogen fixation, atmospheric N₂ is converted to NH₃, which can acquire H⁺ in soil solution to form NH₄⁺. Producers assimilate usable forms, and feeding transfers nitrogen through trophic levels.

Decomposers recycle matter but do not recycle energy back to producers. The cycles are interdependent because organisms and physical processes move several kinds of matter at the same time.

How Energy Availability Reshapes Trophic Levels

Energy availability limits how much biomass and how many organisms an ecosystem can support. Because producers form the energy-entry point, changes in sunlight or producer biomass can propagate through every consumer level.

Available energy changes → producer productivity or biomass changes → energy available to primary consumers changes → higher consumer populations and trophic structure change → the community and ecosystem may be disrupted.

Initial change Likely trophic consequence
Less sunlight or fewer producers Less energy enters the food web, so supported consumer biomass and population sizes may fall; upper trophic levels are especially constrained
More usable energy and producer biomass More energy can support larger populations or additional consumer levels, provided other resources are not limiting

Trophic levels include producers; primary, secondary, tertiary, and quaternary consumers; and decomposers. A change at one level can alter feeding relationships and population sizes at several others.

Energy availability is not the only ecological limit. A predicted increase may not occur if nutrients, water, habitat, or another required factor remains limiting.

Autotrophs Bring Energy In; Heterotrophs Transfer It

Autotrophs capture energy from the environment and store it in organic matter; heterotrophs obtain that stored chemical energy by consuming organic matter derived from autotrophs. Together, these activities enable energy flow through ecosystems.

Organism role Energy source and activity Ecosystem consequence
Photosynthetic autotroph Captures sunlight and stores energy in organic molecules Adds to primary productivity and supplies food-web energy
Chemosynthetic autotroph Captures energy from small inorganic molecules, including in environments without oxygen Provides an energy-entry route where sunlight is unavailable
Heterotroph Consumes organic matter and metabolizes carbohydrates, lipids, and proteins Transfers energy and incorporates matter into tissues

Herbivores, carnivores, omnivores, scavengers, and decomposers are all heterotrophs. Their feeding and metabolism connect autotroph-derived carbon compounds to successive trophic roles.

Sunlight or inorganic chemical energy → autotroph organic matter → heterotroph consumption → metabolism, growth, and transfer to other consumers or decomposers.

Autotrophs do not create energy; they capture and transform it. Heterotrophs depend ultimately on organic matter made by autotrophs, even when the first energy source is chemical rather than sunlight.