Energy enters most ecosystems through photosynthesis by primary producers and flows through trophic levels: producers, primary consumers, secondary consumers, and so on. Only about 10% of energy transfers to the next trophic level because the rest is lost as heat during cellular respiration. Chemosynthetic organisms capture energy from inorganic molecules and support ecosystems without sunlight. Matter, unlike energy, is conserved and cycles through biogeochemical cycles including the carbon, nitrogen, phosphorus, and water cycles. Changes in energy availability, such as a reduction in producer biomass, ripple through all trophic levels.
- 10% rule: Approximately 10% of energy at one trophic level is available to the next, because the rest is lost as heat through metabolism.
- Gross vs. net primary productivity: GPP is total energy fixed by producers; NPP is GPP minus energy used by producers in respiration, representing energy available to consumers.
- Biogeochemical cycles: Pathways through which matter moves between biotic organisms and abiotic reservoirs such as the atmosphere, soil, and water.
- Chemosynthesis: Energy capture from inorganic molecules by organisms such as deep-sea vent bacteria, supporting ecosystems in the absence of sunlight.
- Decomposers: Bacteria and fungi that break down dead organic matter, returning nutrients to abiotic reservoirs and completing biogeochemical cycles.
If a drought reduces plant biomass by 50%, predict the effect on primary consumer and secondary consumer populations and explain your reasoning using energy flow.
| Feature | Energy Flow | Matter Cycling |
|---|
| Direction | One-way: sun to producers to consumers | Cyclical: between biotic and abiotic reservoirs |
| Lost at each step? | Yes, as heat during respiration | No, matter is conserved |
| Key process | Photosynthesis and cellular respiration | Biogeochemical cycles (carbon, nitrogen, water, phosphorus) |
| Measured by | Calories or joules per trophic level | Mass of element in each reservoir |