Skills you'll gain in this topic:
- Explain how energy flows from producers to consumers in ecosystems.
- Describe the roles of producers, consumers, and decomposers in food webs.
- Predict ecosystem impacts when energy flow is disrupted.
- Relate energy transfer efficiency to food chain length and ecosystem stability.
- Analyze how energy changes influence entire ecosystems.
How Energy Moves Through Food Chains and Webs
All organisms in an ecosystem need energy. Remember, all the energy that we have on Earth originates from the sun ☀️. Photosynthetic organisms convert this energy into usable forms through photosynthesis.
Energy flows through ecosystems, starting with energy from the sun and traveling through photosynthetic organisms and the organisms that consume them. The majority of energy is lost in the form of heat between levels of the ecosystem. This is because energy is used by the individual in order to produce heat, digest, and go through basic daily functioning.
Trophic Levels
As energy flows through an ecosystem it travels through trophic levels. A trophic level is the energy level in which an organism exists based on what it eats:
- 🌱 Producers (Autotrophs): Produce their own energy through photosynthesis or chemosynthesis (think: plants, algae, and photosynthetic bacteria).
- 🐐 Consumers (Heterotrophs): Get their energy from other organisms (think: everyone else!):
- Primary consumers: Herbivores that eat producers (deer, rabbits, caterpillars)
- Secondary consumers: Carnivores that eat primary consumers (foxes, small birds of prey)
- Tertiary consumers: Carnivores that eat secondary consumers (hawks, wolves)
- Quaternary consumers: Top predators with few natural enemies (orcas, eagles)
- Decomposers and Scavengers: Special heterotrophs that break down dead organic matter:
- Decomposers: Bacteria and fungi that chemically break down dead material
- Scavengers: Animals that consume dead organisms (vultures, hyenas)
- Omnivores: Consume both plants and animals, operating at multiple trophic levels (humans, bears)
The maintenance of energy levels is essential to the survival of all organisms. If an organism is using more energy than it is consuming, creating a net loss of energy, the organism will lose mass and may eventually die. A net gain ⬆️ in energy results in energy storage as fat reserves in animals or starch in plants, providing resources for future use. A net loss ⬇️ of energy results in loss of mass and, ultimately, the death of an organism.
Trophic Pyramids and Energy Transfer
Trophic pyramids (also called energy pyramids) visually represent energy flow through ecosystems. Each level shows:
- Only about 10% of energy transfers to the next trophic level
- 90% is lost as heat, movement, and metabolic processes
- This explains why food chains rarely exceed 4-5 levels
- Biomass typically decreases at higher trophic levels
Temperature Regulation Strategies
Organisms have evolved different strategies for maintaining body temperature, which impacts their energy requirements:
- Endotherms (warm-blooded animals) maintain an even temperature in their bodies. We are examples of endotherms, as we maintain a body temperature between 97 and 99°F. These organisms use a great deal of the energy that they get from food sources in order to maintain their internal temperature.
- Ectotherms (cold-blooded animals) do not maintain an even temperature in their bodies. Snakes and fish are examples of ectotherms. These organisms must change their behaviors in order to maintain an internal temperature. This may involve hibernating in the winter and lying in a sunny spot during the summer.
Biogeochemical Cycles
Energy flow involves essential biogeochemical cycles:
The Hydrologic Cycle
- Water movement within the hydrosphere involves processes like evaporation, condensation, precipitation, and transpiration.
The Carbon Cycle
- Carbon atoms recycle through photosynthesis, cellular respiration, decomposition, and combustion.
The Nitrogen Cycle
- Nitrogen fixation: Bacteria convert atmospheric nitrogen gas (N₂) to ammonia (NH₃), which immediately ionizes to ammonium (NH₄⁺) in soil water
- Assimilation: Plants absorb NH₄⁺ and NO₃⁻ to make proteins and nucleic acids
- Ammonification: Decomposers convert organic nitrogen back to NH₄⁺
- Nitrification: Bacteria oxidize NH₄⁺ to NO₂⁻ then NO₃⁻
- Denitrification: Anaerobic bacteria convert NO₃⁻ back to N₂ gas
The Phosphorus Cycle
- Rocks release phosphate into the soil and groundwater, supporting plant growth.
Chemosynthetic Organisms
Chemosynthetic organisms harness energy from inorganic molecules, enabling life in environments devoid of sunlight.
Life-History Strategies and Reproductive Timing
Organisms have evolved various life-history strategies to optimize energy use and reproductive success:
Life-History Strategies
- Biennial plants: Complete their life cycle over two years, storing energy in roots during year one, then flowering and dying in year two (e.g., carrots, foxglove)
- Reproductive diapause: A delay in development during unfavorable conditions, allowing organisms to conserve energy until conditions improve (e.g., some insects pause development as pupae)
- Seasonal reproduction: Many organisms time reproduction to coincide with peak resource availability (e.g., deer breeding in fall for spring births when food is abundant)
Reproductive Strategies in Response to Energy Availability
Organisms alter their reproductive strategies based on the availability of free energy in their environment:
- When energy is abundant: Organisms often invest in sexual reproduction, which requires more energy but increases genetic diversity
- When energy is limited: Many organisms switch to asexual reproduction, which requires less energy and allows rapid population growth
For example, many plants and animals can alternate between sexual and asexual reproduction depending on environmental conditions. Water fleas (Daphnia) reproduce asexually when food is plentiful but switch to sexual reproduction when stressed. Similarly, strawberry plants produce runners (asexual) during favorable conditions but invest in seeds (sexual) when preparing for winter.
Ecological Levels of Organization
Energy flow affects various ecological levels:
- Populations: Groups of the same species.
- Communities: Interacting species in a common environment.
- Ecosystems: Combined living and non-living elements.
- Biomes: Large climate-specific regions with distinctive life forms.
Energy Availability and Ecosystem Disruptions
Changes in energy availability directly affect population sizes and can cause ecosystem disruptions:
Effects on Population Size:
- When energy increases (e.g., nutrient enrichment), populations grow rapidly until reaching carrying capacity
- When energy decreases (e.g., drought reducing plant growth), populations decline through starvation and reduced reproduction
- Energy limitations create competition, affecting which species dominate
Ecosystem Disruptions:
- Bottom-up effects: Changes in producer energy availability cascade up through all trophic levels
- Trophic cascades: Removal of predators can cause prey explosions, depleting producer populations
- Energy subsidies: Human additions (fertilizer runoff) can cause algal blooms and ecosystem collapse
- Climate change: Alters energy availability patterns, disrupting migration, reproduction, and species interactions
Understanding these interactions deepens our comprehension of energy dynamics within ecosystems, highlighting the importance of maintaining balance and the critical impacts of energy disruptions on entire ecological communities.
Check out the AP Bio Unit 8 Replays or watch the 2021 Unit 8 Cram
Vocabulary
The following words are mentioned explicitly in the College Board Course and Exam Description for this topic.
| Term | Definition |
|---|---|
| abiotic reservoirs | Non-living components of ecosystems that store matter, such as atmosphere, soil, and water. |
| ammonification | The process by which decomposers break down organic nitrogen compounds into ammonia. |
| asexual reproduction | Reproduction that produces offspring genetically identical to the parent without the fusion of gametes. |
| assimilation | The process by which organisms take up and incorporate nutrients into their biological molecules. |
| autotrophs | Organisms that capture energy from physical or chemical sources in the environment and convert it into organic compounds to fuel their own growth and metabolism. |
| biogeochemical cycles | Cycles that move matter and nutrients between biotic and abiotic reservoirs in ecosystems. |
| biomass | The total mass of living organisms in a population or trophic level. |
| biomes | Large geographic areas with similar climate, vegetation, and animal life. |
| biotic reservoirs | Living organisms and organic matter that store matter within ecosystems. |
| carbon cycle | The cycle involving the movement of carbon atoms through the biosphere, atmosphere, and organisms. |
| carnivores | Heterotrophs that obtain energy by consuming other animals. |
| cellular respiration | The metabolic process by which cells break down biological macromolecules to release energy and synthesize ATP. |
| chemosynthetic organisms | Autotrophs that capture energy from inorganic chemical compounds in their environment, independent of sunlight. |
| combustion | The burning of organic matter or fossil fuels, which releases carbon dioxide into the atmosphere. |
| community | A group of interacting populations of different species that live in the same area and change over time based on interactions between those populations. |
| condensation | The process by which water vapor cools and changes into liquid form in the atmosphere. |
| conservation of matter | The principle that matter is neither created nor destroyed but is recycled through biogeochemical cycles. |
| decomposer | Organisms, such as bacteria and fungi, that break down dead organic matter and return nutrients to the ecosystem. |
| decomposition | The process by which decomposers break down dead organic matter, releasing carbon dioxide and nutrients. |
| denitrification | The process by which soil microorganisms convert nitrate back into nitrogen gas, returning it to the atmosphere. |
| ecosystem | A community of living organisms interacting with each other and their physical environment. |
| ecosystem disruption | A disturbance to the normal functioning and balance of an ecosystem caused by changes in environmental factors. |
| ectotherms | Organisms that lack efficient internal mechanisms for regulating body temperature and rely on behavioral or environmental factors to regulate their temperature. |
| endotherms | Organisms that use thermal energy generated by their own metabolism to maintain a relatively constant body temperature. |
| energy availability | The amount of energy accessible to organisms in an ecosystem, which can change based on factors like sunlight or food resources. |
| energy flow | The movement of energy through an ecosystem from the sun through producers and consumers to decomposers. |
| energy storage | The accumulation of energy in an organism, resulting from a net gain of energy that can be used for growth and reproduction. |
| evaporation | The process by which water changes from liquid to gas and enters the atmosphere. |
| food chain | A linear sequence showing the transfer of energy from one organism to the next through feeding relationships. |
| food web | A network of interconnected food chains showing multiple feeding relationships in an ecosystem. |
| herbivores | Heterotrophs that obtain energy by consuming plants and other autotrophs. |
| heterotrophs | Organisms that obtain energy by consuming organic matter derived from autotrophs or other organisms. |
| homeostasis | The maintenance of stable internal environmental conditions in an organism despite external and internal changes. |
| hydrologic cycle | The cycle involving water movement and storage through evaporation, condensation, precipitation, and transpiration. |
| matter cycles | The movement and recycling of chemical elements and compounds between organisms and the physical environment. |
| metabolism | The sum of all chemical reactions in an organism that produce energy and build or break down molecules. |
| nitrification | The process by which soil microorganisms convert ammonia into nitrite and nitrate. |
| nitrogen cycle | The cycle involving the movement of nitrogen between the atmosphere, soil, and organisms through various microbial processes. |
| nitrogen fixation | The process by which nitrogen gas from the atmosphere is converted into ammonia by microorganisms. |
| omnivores | Heterotrophs that obtain energy by consuming both plants and animals. |
| phosphorus cycle | The cycle involving the movement of phosphorus through soil, organisms, and water in ecosystems. |
| photosynthesis | The series of reactions that use carbon dioxide, water, and light energy to produce carbohydrates and oxygen, allowing organisms to capture and store energy from the sun. |
| photosynthetic organisms | Autotrophs that capture energy from sunlight and convert it into chemical energy stored in organic compounds. |
| population | A group of organisms of the same species living in the same geographic area. |
| population size | The total number of individual organisms of the same species in a population at a given time. |
| precipitation | Water falling from clouds to Earth's surface as rain, snow, sleet, or hail. |
| primary consumer | An organism that feeds directly on producers; a herbivore. |
| primary productivity | The rate at which photosynthetic organisms capture solar energy and convert it into organic matter in an ecosystem. |
| producer | Organisms, primarily plants and photosynthetic organisms, that convert light energy into chemical energy through photosynthesis. |
| quaternary consumer | An organism that feeds on tertiary consumers; a carnivore at the fourth trophic level. |
| reproductive diapause | A period of suspended or delayed reproduction in response to unfavorable environmental conditions or limited energy availability. |
| reproductive strategies | Different approaches organisms use to reproduce in response to environmental conditions and energy availability. |
| scavengers | Heterotrophs that obtain energy by consuming dead organisms or organic waste. |
| secondary consumer | An organism that feeds on primary consumers; a carnivore or omnivore at the second trophic level. |
| sexual reproduction | Reproduction involving the fusion of gametes from two parents, producing genetically diverse offspring. |
| tertiary consumer | An organism that feeds on secondary consumers; a carnivore at the third trophic level. |
| transpiration | The process by which water is released from plants into the atmosphere. |
| trophic level | A position in a food chain or food web occupied by organisms that obtain energy in the same way, including producers, consumers, and decomposers. |
| trophic pyramid | A diagram representing the relative amounts of energy or biomass at each trophic level in an ecosystem. |
| weathering | The process by which rocks break down, releasing minerals such as phosphate into soil and water. |
Frequently Asked Questions
What is the difference between endotherms and ectotherms and how do they regulate body temperature?
Endotherms generate most of their body heat from internal metabolism (think birds and mammals). They maintain fairly constant internal temperatures using metabolic heat and physiological mechanisms—shivering, changing metabolic rate, vasodilation/vasoconstriction, sweating or panting—to keep homeostasis (EK 8.2.A.1.i). Ectotherms (reptiles, many amphibians, fishes, invertebrates) don’t produce enough metabolic heat to regulate temperature internally; instead they rely mainly on behavioral strategies—basking in sun, seeking shade, changing posture, or aggregating—and sometimes microhabitat selection to control body temp. Those differences affect energy budgets: endothermy needs higher metabolic input (affects growth and reproduction), while ectothermy saves energy but limits activity in cold (ties to LO 8.2.A and energy flow concepts). For more review and AP-style practice on thermoregulation and energy strategies, see the Topic 8.2 study guide (https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd) and practice problems (https://library.fiveable.me/practice/ap-biology).
How does energy actually flow through ecosystems step by step?
Energy flows through ecosystems in a one-way, step-by-step path: 1. Producers (autotrophs) capture energy—mostly sunlight via photosynthesis (or chemical energy via chemosynthesis)—producing organic molecules. Gross primary productivity (GPP) is total captured energy; net primary productivity (NPP ≈ GPP – plant respiration) is what’s available to consumers (LO 8.2.D, EK 8.2.D.1). 2. Primary consumers (herbivores) eat producers and convert some organic matter into biomass; most energy is lost as heat/metabolism (EK 8.2.A.1). 3. Secondary/tertiary consumers (carnivores/omnivores) eat lower trophic levels; at each step ~10% of energy is transferred (the “10% rule”), so energy and biomass decline up the trophic pyramid (LO 8.2.B, keywords: trophic levels, trophic pyramid). 4. Decomposers/detritivores break down dead matter, returning nutrients to the abiotic environment (matter cycles like C, N, P) and completing nutrient recycling (EK 8.2.B.2–7). 5. Changes in producer energy input (e.g., less sunlight or NPP) alter population sizes and trophic structure (LO 8.2.C). This matches AP expectations for energy flow and ties to nutrient cycles—review the Topic 8.2 study guide (https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd) and unit page (https://library.fiveable.me/ap-biology/unit-8). For more practice, try the AP problems (https://library.fiveable.me/practice/ap-biology).
What's the difference between autotrophs and heterotrophs in terms of getting energy?
Autotrophs make their own energy-rich organic molecules by capturing energy from the environment—usually sunlight (photosynthesis) or inorganic chemicals (chemosynthesis). They’re the primary producers at the base of trophic levels and drive primary productivity (EK 8.2.D.1). Heterotrophs can’t make organic carbon from inorganic sources, so they get energy by eating (or decomposing) organic matter made by autotrophs—metabolizing carbs, lipids, and proteins for ATP and biomass (EK 8.2.D.2). In ecosystems, that’s how energy flows upward through consumers (herbivores → carnivores → decomposers); only a fraction of energy is passed to the next trophic level (think ~10% transfer rule), so fewer trophic levels are supported as you go up. For AP exam focus, connect these ideas to trophic pyramids, energy transfer, and LO 8.2.D (see the Topic 8.2 study guide for a quick review) (https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd). For extra practice on these concepts, try the AP Bio practice problems (https://library.fiveable.me/practice/ap-biology).
I'm confused about biogeochemical cycles - do they involve energy flow or just matter cycling?
Short answer: biogeochemical cycles are about matter (nutrients) cycling, not energy flow. More detail: energy in ecosystems flows one-way—from sunlight (or chemical sources) into producers and up trophic levels, with ~90% lost as heat at each transfer (EK 8.2.D and LO 8.2.C). Biogeochemical cycles (carbon, nitrogen, phosphorus, water) describe how atoms and nutrients move between abiotic reservoirs and living things and are conserved (EK 8.2.B.2–B.7). Microbial processes (e.g., nitrogen fixation, nitrification, denitrification) and physical processes (evaporation, precipitation, weathering, decomposition, combustion) move matter between reservoirs (EK 8.2.B.3–B.7). They’re linked: matter cycles let energy be stored and passed in organic molecules, but the cycle itself tracks atoms, not energy flow direction. If you want a quick CED-aligned refresher, check the Topic 8.2 study guide (https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd) and practice questions (https://library.fiveable.me/practice/ap-biology).
Why do organisms sometimes switch between sexual and asexual reproduction based on energy availability?
Switching happens because sex and asex have different energy costs and benefits. Asexual reproduction is cheap and fast (clonal offspring)—good when an organism has a net energy gain and the environment is stable, so maximizing reproductive output is favored. Sexual reproduction is energetically costly (finding mates, meiosis, gamete production) but creates genetic variation and often durable or stress-resistant offspring (e.g., seeds, cysts). So many species reproduce asexually when energy and conditions are good, then switch to sex when energy becomes limited or conditions are unpredictable to increase offspring survival and adaptive potential. This ties directly to EK 8.2.A.1–2 and the life-history examples in the CED (seasonal reproduction, diapause). For more examples and AP-aligned review, see the Topic 8.2 study guide (https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd) and practice questions (https://library.fiveable.me/practice/ap-biology). On the exam, this concept can show up under LO 8.2.A or LO 8.2.C in free-response or multiple-choice items.
Can someone explain the nitrogen cycle in simple terms because I keep forgetting all the steps?
Think of the nitrogen cycle as a loop that moves N between the air, soil, and living things—mainly driven by microbes. Steps (simple): - Reservoir: Most N is N₂ gas in the atmosphere (biggest reservoir). - Nitrogen fixation: Special bacteria (e.g., Rhizobium in legumes) or lightning convert N₂ → ammonia (NH₃) or ammonium (NH₄⁺). This makes nitrogen usable. - Assimilation: Plants take up NH₄⁺ or nitrate (NO₃⁻) and build amino acids, proteins, nucleic acids. Animals get N by eating plants. - Ammonification (decomposition): Decomposers break dead organisms and waste into NH₄⁺. - Nitrification: Soil bacteria convert NH₄⁺ → NO₂⁻ → NO₃⁻ (nitrate), which plants can also use. - Denitrification: Other bacteria convert NO₃⁻ back to N₂ gas, returning N to the atmosphere. Remember: microbes do most steps, energy flows in while matter cycles (EK 8.2.B). For a concise AP-aligned review, check the Topic 8.2 study guide (https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd) and practice questions (https://library.fiveable.me/practice/ap-biology).
What happens to an ecosystem when there's a change in the number of producers at the bottom of the food chain?
If the number (or biomass) of producers changes, the whole ecosystem shifts because producers set primary productivity—the energy base for all consumers (LO 8.2.C, EK 8.2.B/D). Fewer producers → less available energy for herbivores, so primary consumer populations usually drop; that propagates upward (secondary/tertiary consumers decline). Because only about ~10% of energy is transferred between trophic levels, small drops in producer biomass can cause big decreases in consumer abundance and may shrink the number of trophic levels or simplify food webs (EK 8.2.C.2.i). You can also get trophic cascades, altered nutrient cycling (carbon, nitrogen, phosphorus), and less biodiversity. The reverse (more producers) can increase consumer populations and possibly add trophic complexity. For AP review, focus on energy flow, trophic pyramids, net primary productivity, and examples of disruptions (see the Topic 8.2 study guide on Fiveable: https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd). For extra practice, try problems at (https://library.fiveable.me/practice/ap-biology).
How do chemosynthetic organisms get energy without sunlight and where would you find them?
Chemosynthetic organisms are autotrophs that harvest energy from inorganic molecules instead of sunlight. They oxidize compounds like hydrogen sulfide (H2S), methane (CH4), ammonia (NH3), or ferrous iron (Fe2+) and use that energy to fix CO2 into organic matter (chemosynthesis). This lets them be primary producers in places without light—think deep-sea hydrothermal vents, cold seeps, sulfur-rich hot springs, and some anoxic soils or subsurface habitats. You’ll also find chemosynthetic bacteria inside host animals (e.g., tubeworms, clams) forming symbioses that fuel whole communities. In AP terms (EK 8.2.D.1.ii), they capture chemical energy and enable energy flow through trophic levels where sunlight-driven photosynthesis is absent. For a quick review of energy flow and where chemosynthesis fits, check the Topic 8.2 study guide (https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd) and hit the practice problems (https://library.fiveable.me/practice/ap-biology) to see related Qs.
What's the difference between the carbon cycle and the phosphorus cycle?
Short answer: both cycle matter through ecosystems, but they move differently. Carbon cycles rapidly between the atmosphere and living things (photosynthesis puts CO2 into organic molecules; cellular respiration, decomposition, and combustion return CO2 to the atmosphere). Carbon has a large gaseous reservoir (atmosphere) and also long-term geological reservoirs (fossil fuels, sediments), so it moves via gas exchange as well as storage/release. Phosphorus cycles without a gaseous phase—its main reservoir is rocks and soils. Weathering releases phosphate (PO4^3–) into soil and water; producers take it up, consumers get it by eating producers, and decomposition/excretion returns phosphate to soils or sediments. Because P is mostly bound in solids and is less mobile, it’s often a limiting nutrient in ecosystems (adding P can fuel eutrophication). Both illustrate conservation of matter and link to productivity and trophic transfer (AP LO 8.2.B; see the Topic 8.2 study guide on Fiveable for a quick review: https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd). For practice, try problems at https://library.fiveable.me/practice/ap-biology.
I don't understand trophic pyramids - why do they get smaller as you go up?
Trophic pyramids get smaller going up because energy is lost at each transfer between trophic levels. Producers (autotrophs) capture sunlight and make biomass (net primary productivity), but most of that energy is used for metabolism, movement, reproduction, and lost as heat (cellular respiration) or excreted as waste. Only a fraction—commonly about 10%—is incorporated into the next level (herbivores), so secondary consumers get ~1% of original plant energy, and so on. That’s why pyramids of energy and usually biomass narrow upward (fewer trophic levels can be supported when primary productivity is low). This idea is exactly what LO 8.2.B/EK 8.2.D describe (energy flows through ecosystems; heterotrophs metabolize organic matter). On the AP exam you may need to apply the 10% rule or explain how changes in producer biomass affect higher trophic levels (LO 8.2.C). For a quick review, check the Topic 8.2 study guide (https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd) or the Unit 8 overview (https://library.fiveable.me/ap-biology/unit-8). For extra practice problems, see (https://library.fiveable.me/practice/ap-biology).
How does transpiration fit into the water cycle and why is it important for ecosystems?
Transpiration is the loss of water vapor from plant leaves (stomata) and is a key process in the hydrologic cycle—it moves water from soil/plant tissues into the atmosphere alongside evaporation (CED EK 8.2.B.4). Mechanistically, transpiration creates a negative pressure (cohesion–tension) that pulls water and dissolved nutrients up through xylem, helping producers get the water they need for photosynthesis (EK 8.2.D.1). Ecologically, transpiration regulates local microclimate (cooling, humidity), helps distribute nutrients from soil to aboveground tissues, and links water availability to primary productivity—changes in transpiration (e.g., drought, deforestation) can cascade through trophic levels (LO 8.2.B and LO 8.2.C). For AP review, make sure you can place transpiration in the hydrologic cycle and explain how it affects producers and energy flow (see the Topic 8.2 study guide for quick review: https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd). For broader unit review and practice questions, check the unit page (https://library.fiveable.me/ap-biology/unit-8) and practice set (https://library.fiveable.me/practice/ap-biology).
What are some real world examples of how energy availability affects population sizes?
Energy availability sets the size of populations because producers (autotrophs) capture energy that fuels every trophic level (think EK 8.2.D and the 10% rule). Real-world examples: - Seasonal sunlight: In temperate lakes, spring light + nutrients spike phytoplankton (producers) → zooplankton and fish populations rise; winter light drop reduces biomass and consumer numbers. - Nutrient pulses: Fertilizer runoff adds phosphorus → algal blooms (huge producer increase) then dead zones as decomposition depletes O2, collapsing fish/shellfish populations (EK 8.2.B, 8.2.C). - Upwelling zones: Cold-water upwelling brings nutrients → high net primary productivity and large fisheries (more trophic levels supported). - Drought/heatwaves: Lower NPP (net primary productivity) in grasslands/forests → herbivore numbers fall, then predator populations decline. These link directly to LO 8.2.C (changes in energy availability change population size and trophic structure). For a focused review, check the Topic 8.2 study guide (https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd) and more unit resources (https://library.fiveable.me/ap-biology/unit-8). For practice, try problems at (https://library.fiveable.me/practice/ap-biology).
Why do decomposers play such an important role in energy flow if they're at the bottom of most food webs?
Even though decomposers sit at the “bottom” of many food webs, they’re essential for energy flow because they recycle matter and keep energy moving through the system. Producers (autotrophs) capture sunlight or chemical energy (EK 8.2.D.1); decomposers break down dead organic matter and waste, releasing nutrients (C, N, P) back into the soil or water so producers can rebuild biomass (EK 8.2.B.5–B.7). Without decomposers, nutrients would stay locked in dead tissue and primary productivity (and every higher trophic level) would collapse. They also form detrital food webs that channel energy from dead material to consumers. Remember the ~10% energy-transfer rule: energy is lost as heat at each trophic step (LO 8.2.B), so efficient nutrient recycling by decomposers is critical to sustain net primary productivity. For a quick AP-aligned refresher, check the Topic 8.2 study guide (https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd) and more practice problems (https://library.fiveable.me/practice/ap-biology).
I missed the lab on biogeochemical cycles - what's the main difference between abiotic and biotic reservoirs?
Abiotic reservoirs are nonliving places where elements or compounds are stored (like the atmosphere for CO2, oceans/groundwater in the hydrosphere for water, and rocks/minerals in the lithosphere for phosphorus). Biotic reservoirs are the living parts of the ecosystem—producers, consumers, decomposers—where matter is incorporated into biomass (plants holding carbon, animals holding nitrogen in proteins, microbes in soil). The main difference: abiotic reservoirs store matter in nonliving pools; biotic reservoirs store matter in living organisms. Biogeochemical cycles move matter between these reservoirs by processes such as photosynthesis, cellular respiration, decomposition, nitrogen fixation, nitrification/denitrification, and weathering (CED EK 8.2.B.2–B.7). Remember on the AP exam they often ask you to ID reservoirs and the processes that move matter between them (LO 8.2.B). For a quick review, check the Topic 8.2 study guide (https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd) and practice problems (https://library.fiveable.me/practice/ap-biology).
How does photosynthesis connect to both energy flow and the carbon cycle at the same time?
Photosynthesis is the bridge between energy flow and the carbon cycle. As an autotroph process, it captures sunlight (energy) and uses CO2 from the atmosphere to build organic carbon (glucose)—that’s where energy enters an ecosystem and producers set primary productivity (GPP → NPP). Energy then flows up trophic levels when herbivores and carnivores eat producers (most energy lost as heat; remember ~10% transfer rule). At the same time, the carbon atoms fixed in organic molecules cycle back to the atmosphere or soil via cellular respiration, decomposition, and combustion (EK 8.2.B.5). So photosynthesis both inputs usable energy and moves carbon from an abiotic reservoir (atmosphere) into biotic reservoirs (biomass), linking energy transfer and matter cycling. For review and practice on these AP ideas (LO 8.2.B, LO 8.2.D), see the Topic 8.2 study guide (https://library.fiveable.me/ap-biology/unit-8/energy-flow-through-ecosystems/study-guide/A1PeQD1Zy3BIMu1zSMzd) and the Unit 8 overview (https://library.fiveable.me/ap-biology/unit-8). For more practice questions, try https://library.fiveable.me/practice/ap-biology.