Biology · Reference sheet

Energy Flow and Biogeochemical Cycles

How energy flows through producers, consumers, and decomposers via food chains and food webs, why only about 10% of energy passes between trophic levels, and how carbon, nitrogen, and water cycle through an ecosystem.

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Producers, consumers, and decomposers

Every ecosystem runs on two different things moving through it at the same time. Energy flows in one direction, starting with the sun and ending as heat, and it is never reused. Matter (carbon, nitrogen, water, and other nutrients) cycles around again and again, reused by one organism after another. This sheet covers both halves: how energy flows through feeding relationships, and how key nutrients cycle through the ecosystem. Every organism in an ecosystem fits one of three feeding roles. Producers (autotrophs) make their own food, almost always through photosynthesis, and form the base of every food chain. Green plants, algae, and cyanobacteria are producers. Consumers (heterotrophs) eat other organisms to get energy. Primary consumers (herbivores) eat producers. Secondary consumers eat primary consumers, and tertiary consumers eat secondary consumers. Many consumers are omnivores that eat at more than one level. Decomposers (fungi and bacteria) break down dead organisms and waste, releasing the nutrients locked inside back into the soil, water, and air, where producers can absorb them again.

RoleExample organismsHow they get energy
ProducerGrass, oak trees, algae, cyanobacteriaPhotosynthesis, using sunlight to build glucose
Primary consumerGrasshopper, rabbit, deerEating producers
Secondary consumerFrog, foxEating primary consumers
Tertiary consumerHawk, large fishEating secondary consumers
DecomposerMushrooms, soil bacteriaBreaking down dead organisms and waste

Energy flows, matter cycles

Keep these two ideas separate as you read the rest of this sheet. Energy arrives from the sun, moves through a food chain, and leaves as heat, so it must be constantly resupplied. Carbon, nitrogen, and water atoms stay on Earth and pass from organism to environment to organism over and over.

Food chains show one pathway of energy flow

A food chain is a single pathway showing who eats whom, drawn with arrows pointing from the organism being eaten to the organism that eats it. The arrow shows the direction energy flows, not the direction of eating. Each step in the chain is a trophic level, a feeding level counted from the producer up. Example: grass → grasshopper → frog → hawk. Read this as grass is eaten by the grasshopper, the grasshopper is eaten by the frog, and the frog is eaten by the hawk. Energy from the sun, captured by the grass, flows up the chain in that same direction.

OrganismTrophic levelRole
Grass1Producer
Grasshopper2Primary consumer
Frog3Secondary consumer
Hawk4Tertiary consumer

The arrow means "energy flows to"

A common mix-up is reading the arrow as "eats." Grass → grasshopper means the grasshopper eats the grass, and energy flows FROM the grass TO the grasshopper. Always read the arrow as the direction energy travels, not the direction of the bite.

Food webs show the real feeding picture

Real ecosystems are never just one tidy chain. Most consumers eat more than one type of food and are eaten by more than one type of predator. A food web is a diagram of many overlapping food chains, showing all the feeding connections in an ecosystem at once. A hawk might eat frogs, snakes, and mice, and a frog might be eaten by both hawks and snakes, all in the same web. Food webs matter because they show how ecosystems stay connected. If one species disappears, every food chain that passed through it is disrupted, which is why food webs are a far more realistic model of a real ecosystem than any single food chain.

Removing one species has ripple effects

Because species share connections in a food web, losing one organism does not just affect the organisms directly next to it. If frogs disappeared, hawks and snakes would lose a food source and grasshopper populations could grow unchecked, which then affects the grass. This ripple effect through a food web is called a trophic cascade.

Energy pyramids and the ten percent rule

An energy pyramid stacks trophic levels from producers at the bottom to top predators at the top, with the width of each level showing how much energy is available there. The pyramid gets narrower going up because of the ten percent rule: on average, only about 10% of the energy at one trophic level gets passed on to the next trophic level. The other roughly 90% is used up or lost as heat through the consumer's own cellular respiration, movement, and everyday life, or it leaves as waste that was never digested. Example: if producers in a field store 10,000 kcal of energy, primary consumers that eat them gain only about 1,000 kcal (10% of 10,000). Secondary consumers gain about 100 kcal (10% of 1,000), and tertiary consumers gain about 10 kcal (10% of 100).

Trophic levelEnergy availablePercent of original
Producers10,000 kcal100%
Primary consumers1,000 kcal10%
Secondary consumers100 kcal1%
Tertiary consumers10 kcal0.1%

Why food chains rarely go past 4 or 5 levels

Each trophic level up the pyramid has so much less energy available that there usually is not enough left to support another full level of predators. This is also why top predators, like hawks and large sharks, tend to be far less numerous than the producers and primary consumers below them.

The carbon cycle

Carbon moves between the atmosphere, living things, and long-term storage through a few key processes. Photosynthesis removes CO₂ from the atmosphere and builds it into glucose: 6CO₂ + 6H₂O → C₆H₁₂O₆ + 6O₂. Cellular respiration does the reverse, breaking glucose down for energy and releasing CO₂ back into the atmosphere: C₆H₁₂O₆ + 6O₂ → 6CO₂ + 6H₂O. Decomposition releases the carbon stored in dead organisms back into the air and soil as decomposers break them down. Combustion, burning wood or fossil fuels, releases stored carbon quickly. Fossil fuels formed from the remains of ancient organisms buried and compressed over millions of years, so burning them releases carbon that had been locked away for a very long time.

ProcessWhat happensEffect on atmospheric CO₂
PhotosynthesisProducers convert CO₂ and H₂O into glucoseRemoves CO₂
Cellular respirationOrganisms break down glucose for energyAdds CO₂
DecompositionDecomposers break down dead organismsAdds CO₂
CombustionBurning wood or fossil fuelsAdds CO₂

Photosynthesis and respiration are mirror equations

Notice that the cellular respiration equation is the photosynthesis equation written backward. Producers run both reactions, photosynthesis to build glucose during the day and respiration to release energy from it around the clock.

The nitrogen cycle

About 78% of the atmosphere is nitrogen gas, N₂, but most organisms cannot use N₂ directly because the bond holding the two nitrogen atoms together is very strong. Getting nitrogen into a usable form takes several steps carried out by different bacteria. Nitrogen fixation converts N₂ into ammonia (NH₃) or ammonium (NH₄⁺), done mainly by nitrogen-fixing bacteria that live in the root nodules of legume plants like beans and peas, and to a smaller extent by lightning. Nitrification converts ammonium into nitrites (NO₂⁻) and then nitrates (NO₃⁻), done by nitrifying bacteria in the soil. Assimilation is producers absorbing nitrates through their roots to build proteins and DNA, which then pass to consumers that eat those producers. Ammonification happens when decomposers break down waste and dead organisms, releasing nitrogen back into the soil as ammonium. Denitrification converts nitrates back into N₂ gas, done by denitrifying bacteria, returning nitrogen to the atmosphere and completing the cycle.

ProcessWhat happensWho does it
Nitrogen fixationN₂ → NH₃ / NH₄⁺Nitrogen-fixing bacteria (root nodules), lightning
NitrificationNH₄⁺ → NO₂⁻ → NO₃⁻Nitrifying bacteria
AssimilationProducers absorb NO₃⁻ to build proteins and DNAPlants and algae
AmmonificationDead matter and waste → NH₄⁺Decomposers
DenitrificationNO₃⁻ → N₂Denitrifying bacteria

Why farmers rotate in legumes

Legume roots host nitrogen-fixing bacteria in small nodules, giving the plant, and the soil around it, a steady supply of usable nitrogen. Planting legumes like soybeans in rotation with other crops naturally restores nitrogen to farmland without needing as much fertilizer.

The water cycle

Water moves between the atmosphere, land, and oceans through a repeating cycle. Evaporation turns liquid water from oceans, lakes, and rivers into water vapor, driven by heat from the sun. Transpiration is water vapor released from the leaves of plants. Evaporation and transpiration together are often called evapotranspiration. Water vapor rises, cools, and undergoes condensation, forming the tiny water droplets that make up clouds. Once droplets grow large and heavy enough, precipitation (rain, snow, or sleet) falls back to Earth. From there, water either runs off into rivers and lakes as runoff or soaks into the ground as infiltration, refilling groundwater, and the cycle repeats.

ProcessWhat happens
EvaporationLiquid water from oceans, lakes, and rivers becomes water vapor
TranspirationPlants release water vapor from their leaves
CondensationWater vapor cools and forms cloud droplets
PrecipitationRain, snow, or sleet falls to Earth
Runoff / infiltrationWater flows into surface water or soaks into groundwater

The water cycle carries the other cycles along with it

Water is not just its own cycle. Dissolved carbon and nitrogen compounds travel through soil and waterways riding along in water, so a healthy water cycle helps keep the carbon and nitrogen cycles running too.

Try it yourself

Download energy-flow-trophic-levels.csvenergy-flow-trophic-levels.csv

Measured energy, in kJ, at each trophic level of a food chain in a fictional lake (Lake Kestrel): producers (phytoplankton), primary consumers (zooplankton), secondary consumers (minnows), and tertiary consumers (bass).

Open it in a spreadsheet

Open it in Google Sheets or Excel. Add a column that divides each row's energy by the row above it and multiplies by 100, so the spreadsheet calculates transfer efficiency for you.

1. In the food chain oak leaves → caterpillar → songbird → hawk, which organism is the secondary consumer? 2. If producers in a pond store 5,000 kcal of energy, about how much energy is available to primary consumers, and about how much to secondary consumers, using the ten percent rule? 3. Which nitrogen cycle process converts N₂ gas into a form producers can eventually use, and which process returns nitrogen to the atmosphere as N₂ gas? 4. A food web is generally considered more realistic than a single food chain. Why? 5. Using energy-flow-trophic-levels.csv, apply the ten percent rule stated on this sheet to the producers' (phytoplankton) energy to predict how much energy should be available to the primary consumers (zooplankton). Then compare your prediction to the actual value for primary consumers in the file. 6. Using the file, calculate the actual transfer efficiency, as a percent, from primary consumers (zooplankton) to secondary consumers (minnows). Use efficiency = (energy at the higher trophic level ÷ energy at the trophic level below it) × 100. 7. Calculate the transfer efficiency from secondary consumers (minnows) to tertiary consumers (bass) the same way. Is it closer to your answer for Question 6, or to the ten percent rule? 8. If Lake Kestrel had a fifth trophic level, quaternary consumers that feed on bass, use the ten percent rule and the bass energy in the file to predict about how much energy would reach them. Based on this sheet's explanation, why do food chains rarely reach a fifth trophic level?