What is AP Environmental Science unit 1?
Unit 1 asks you to think about Earth as a system where living organisms, physical processes, and chemical cycles are all connected. You will explain how resource availability shapes species interactions, identify biomes by their climate and organisms, trace carbon, nitrogen, phosphorus, and water through their cycles, and calculate how energy decreases as it moves up a food chain.
Unit 1 covers ecosystem structure and function: species interactions (predation, symbiosis, competition), terrestrial and aquatic biome distribution, the four major biogeochemical cycles, primary productivity (GPP vs. NPP), trophic levels, the 10% rule, and food web dynamics including feedback loops.
Species interactions and biomes
Topics 1.1-1.3 establish how resource availability drives predator-prey relationships, symbiosis, and competition, and how climate shapes the global distribution of terrestrial biomes (taiga through tropical rainforest) and aquatic biomes (freshwater and marine).
Biogeochemical cycles
Topics 1.4-1.7 trace carbon, nitrogen, phosphorus, and water through sources, sinks, and reservoirs. Key distinctions include short-term vs. long-term carbon storage, the role of bacteria in the nitrogen cycle, the absence of an atmospheric phase in the phosphorus cycle, and the sun as the driver of the hydrologic cycle.
Energy flow through ecosystems
Topics 1.8-1.11 connect primary productivity (GPP and NPP), trophic levels, the 10% rule, and food web structure. Energy decreases at each trophic level due to the second law of thermodynamics, while matter is conserved and recycled through biogeochemical cycles.
The core idea: Earth as an interconnected systemEvery concept in Unit 1 reflects the same principle: matter cycles and energy flows through interconnected living and nonliving components. Disrupting one part, such as burning fossil fuels to release stored carbon or adding excess nitrogen through fertilizers, ripples through the entire system. This systems thinking is the lens you need for every unit that follows.
Unit 1 review notes
1.1
Species Interactions and Resource Availability
Resource availability determines how species interact. When resources are limited, species compete; when one species relies on another, symbiotic or predator-prey relationships form. Understanding these interactions explains population dynamics and ecosystem stability.
- Predator-prey relationship: The predator eats the prey; predator and prey populations cycle together, with predator numbers lagging behind prey numbers.
- Symbiosis types: Mutualism: both species benefit. Commensalism: one benefits, one is unaffected. Parasitism: one benefits, one is harmed.
- Intraspecific vs. interspecific competition: Intraspecific competition occurs within a species; interspecific competition occurs between species competing for the same limited resource.
- Resource partitioning: Species reduce competition by using resources differently in space, time, or method, allowing coexistence rather than competitive exclusion.
- Keystone species: A species with a disproportionately large effect on ecosystem structure relative to its abundance; removing it can collapse the food web.
Can you give one example each of mutualism, commensalism, and parasitism, and explain how resource partitioning allows two competing species to coexist?
| Interaction | Species A outcome | Species B outcome | Example |
|---|
| Mutualism | Benefits (+) | Benefits (+) | Legume roots and Rhizobium bacteria |
| Commensalism | Benefits (+) | Unaffected (0) | Barnacles on a whale |
| Parasitism | Benefits (+) | Harmed (-) | Tapeworm in a host |
| Competition | Harmed (-) | Harmed (-) | Two plant species competing for soil nitrogen |
| Predation | Benefits (+) | Harmed (-) | Wolf eating a rabbit |
1.2
Terrestrial Biomes
A biome is defined by its climate, especially temperature and precipitation, which determines the characteristic plants and animals found there. Biome boundaries are not fixed; they shift as climate changes. The global distribution of resources like water and timber also varies by latitude, altitude, and soil type.
- Major terrestrial biomes: Taiga, temperate rainforest, temperate seasonal forest, tropical rainforest, shrubland, temperate grassland, savanna, desert, and tundra. Each has a distinct climate profile.
- Tundra and permafrost: Found at high latitudes; permanently frozen subsoil (permafrost) limits plant growth and stores large amounts of carbon.
- Tropical rainforest productivity: High year-round temperature and rainfall produce the highest net primary productivity of any terrestrial biome and the greatest biodiversity.
- Biome distribution factors: Climate, latitude, altitude, nutrient availability, and soil type together determine where nonmineral resources like water and timber are found.
- Dynamic biome boundaries: Biome ranges have shifted in the past and are projected to shift again as global temperatures and precipitation patterns change.
Given a description of annual temperature range and precipitation, can you identify the correct terrestrial biome and name one characteristic plant or animal adaptation?
| Biome | Climate signature | Key vegetation |
|---|
| Tundra | Very cold, low precipitation | Mosses, lichens, sedges |
| Taiga | Cold winters, moderate precipitation | Coniferous trees (spruce, fir) |
| Temperate seasonal forest | Distinct seasons, moderate precipitation | Deciduous broadleaf trees |
| Tropical rainforest | Warm year-round, very high precipitation | Broadleaf evergreen trees, lianas |
| Desert | Low precipitation, extreme temperature swings | Cacti, xerophytes |
1.3
Aquatic Biomes
Aquatic biomes are divided into freshwater and marine systems. The distribution of organisms and resources in aquatic biomes depends on salinity, depth, turbidity, nutrient availability, and temperature. Algae are the primary photosynthetic organisms in most aquatic systems.
- Freshwater biomes: Streams, rivers, ponds, lakes, and freshwater wetlands. Wetlands are especially productive and filter pollutants.
- Marine biomes: Oceans, coral reefs, marshes, and estuaries. Estuaries are highly productive transition zones between fresh and salt water.
- Photic zone: The upper layer of water where enough sunlight penetrates for photosynthesis. Most red light is absorbed in the top 1 m; blue light can reach beyond 100 m in clear water.
- Salinity and turbidity: Salinity determines which organisms can survive; turbidity (suspended particles) limits light penetration and reduces photosynthesis.
- Coral reefs: Among the most biodiverse marine ecosystems; depend on warm, clear, shallow water and the mutualistic relationship between coral polyps and zooxanthellae algae.
What four factors most directly control the distribution of marine resources like fish populations, and how does light availability differ between the top 1 m and depths below 100 m?
| System | Salinity | Key productivity factor | Example biome |
|---|
| Freshwater | Very low | Nutrient input, light | Lake, river, wetland |
| Estuarine | Variable (brackish) | Nutrient mixing, tidal flow | Salt marsh, estuary |
| Marine (coastal) | High | Upwelling, nutrient availability | Coral reef, continental shelf |
| Open ocean | High | Nutrient scarcity limits productivity | Pelagic zone |
1.4
The Carbon Cycle
The carbon cycle moves carbon between the atmosphere, living organisms, soil, oceans, and geological reservoirs. The key distinction for the exam is between short-term reservoirs (living organisms, atmosphere) and long-term reservoirs (fossil fuels, deep ocean sediments). Human combustion of fossil fuels rapidly transfers long-stored carbon into the atmosphere as CO2.
- Short-term carbon reservoirs: Living organisms and the atmosphere hold carbon for years to decades; carbon moves quickly through photosynthesis and cellular respiration.
- Long-term carbon reservoirs: Fossil fuels, deep ocean sediments, and carbonate rocks store carbon for millions of years; burning fossil fuels bypasses the slow natural release.
- Photosynthesis and respiration: Photosynthesis removes CO2 from the atmosphere and stores it in organic molecules; cellular respiration releases CO2 back to the atmosphere.
- Decomposition: Decomposers break down dead organic matter, releasing CO2 (aerobic) or methane (anaerobic) back to the atmosphere.
- Fossil fuel combustion: Burning coal, oil, and natural gas rapidly moves millions of years of stored carbon into the atmosphere, increasing atmospheric CO2 concentrations.
Trace a carbon atom from atmospheric CO2 through photosynthesis, a food chain, decomposition, and back to the atmosphere. Then explain why fossil fuel combustion disrupts this cycle.
1.5
The Nitrogen Cycle
The atmosphere is the major nitrogen reservoir, holding nitrogen as N2 gas that most organisms cannot use directly. Bacteria are essential at every step of the nitrogen cycle, converting nitrogen into usable forms and returning it to the atmosphere. Most nitrogen reservoirs hold compounds for relatively short periods.
- Nitrogen fixation: Bacteria (including Rhizobium in legume root nodules and free-living cyanobacteria) convert atmospheric N2 into ammonia (NH3), making nitrogen available to plants.
- Nitrification: Soil bacteria convert ammonia to nitrite and then to nitrate (NO3-), the form most easily absorbed by plant roots.
- Assimilation: Plants absorb nitrate or ammonium and incorporate nitrogen into proteins and nucleic acids; consumers get nitrogen by eating plants.
- Ammonification: Decomposers break down nitrogen-containing organic matter and release ammonia back into the soil.
- Denitrification: Bacteria in low-oxygen environments convert nitrate back to N2 gas, returning nitrogen to the atmosphere and completing the cycle.
List the five main steps of the nitrogen cycle in order and name the type of organism responsible for each step.
1.6
The Phosphorus Cycle
Phosphorus cycles through rock, soil, water, and living organisms but has no atmospheric phase. Rock weathering is the primary natural source of phosphate. Because phosphorus is often scarce in soils and water, it frequently limits plant and algae growth. Excess phosphorus from agricultural runoff causes eutrophication in aquatic systems.
- Major reservoir: Rock and sediments containing phosphate minerals are the primary long-term phosphorus reservoir; weathering slowly releases phosphate into soil and water.
- No atmospheric phase: Unlike carbon and nitrogen, phosphorus does not cycle through the atmosphere, so it moves only between land, water, and organisms.
- Phosphate uptake: Plant roots absorb phosphate (PO4^3-) from soil; phosphorus is incorporated into DNA, RNA, and ATP in all living organisms.
- Limiting nutrient: Phosphorus availability often limits primary productivity in freshwater systems because it is scarce and does not cycle through the air.
- Eutrophication: Excess phosphate from fertilizer runoff or sewage triggers algal blooms; when algae die and decompose, oxygen is depleted, creating hypoxic dead zones.
Why does the phosphorus cycle have no atmospheric component, and what environmental problem results when excess phosphorus enters a freshwater lake?
| Cycle | Atmospheric reservoir? | Major long-term reservoir | Key limiting factor role |
|---|
| Carbon | Yes (CO2) | Fossil fuels, ocean sediments | Greenhouse gas; climate driver |
| Nitrogen | Yes (N2) | Atmosphere | Limits productivity in many terrestrial systems |
| Phosphorus | No | Rock and sediments | Limits productivity in most freshwater systems |
| Water | Yes (water vapor) | Oceans | Limits productivity in arid terrestrial biomes |
1.7
The Hydrologic Cycle
The hydrologic cycle is powered by solar energy and moves water between the atmosphere, land surface, and subsurface reservoirs. The oceans are the primary surface reservoir. Water moves through evaporation, transpiration, condensation, precipitation, surface runoff, infiltration, and groundwater flow.
- Evapotranspiration: The combined loss of water from soil and open water surfaces (evaporation) and from plant leaves (transpiration); returns water vapor to the atmosphere.
- Precipitation: Water returns to Earth's surface as rain, snow, sleet, or hail after condensation in the atmosphere.
- Surface runoff and infiltration: Precipitation either flows over the land surface into streams (runoff) or soaks into the soil (infiltration) to recharge groundwater.
- Groundwater: Water stored in underground aquifers; a smaller reservoir than the oceans but critical for drinking water and irrigation in many regions.
- Ocean as primary reservoir: Oceans hold the vast majority of Earth's surface water; ice caps and glaciers are the next largest reservoirs, followed by groundwater.
Trace a water molecule from the ocean surface through evaporation, precipitation, surface runoff, and infiltration back to groundwater. What energy source drives this entire cycle?
1.8
Primary Productivity
Primary productivity measures how fast producers convert solar energy into organic matter. Gross primary productivity (GPP) is the total rate of photosynthesis; net primary productivity (NPP) is what remains after producers use energy for their own respiration. NPP is the energy available to the rest of the ecosystem.
- GPP vs. NPP: GPP = total photosynthesis rate. NPP = GPP minus autotrophic respiration. NPP represents the biomass actually available to consumers.
- Units of productivity: Measured in energy per unit area per unit time, such as kcal/m2/yr or gC/m2/yr.
- Light and aquatic productivity: Most red light is absorbed in the top 1 m of water; blue light penetrates beyond 100 m only in the clearest water. This limits where photosynthesis can occur in aquatic systems.
- Photic zone: The layer of water with enough light for photosynthesis; depth varies with turbidity and water clarity.
- Terrestrial vs. aquatic NPP: Tropical rainforests have the highest terrestrial NPP; open ocean has low NPP per unit area due to nutrient scarcity, though its total area makes it globally significant.
If a forest ecosystem has a GPP of 8,000 kcal/m2/yr and producers use 3,000 kcal/m2/yr for respiration, what is the NPP, and what does that value represent ecologically?
1.9
Trophic Levels and the 10% Rule
Energy enters ecosystems at the producer level and flows upward through consumers, but only about 10% transfers from one trophic level to the next. The remaining 90% is lost as heat through metabolic processes, which is explained by the second law of thermodynamics. This limits food chain length and determines how much biomass each level can support.
- Trophic levels: Producers (autotrophs) form the base; primary consumers eat producers; secondary consumers eat primary consumers; and so on up to apex predators.
- 10% rule: Approximately 10% of energy at one trophic level is transferred to the next; the rest is lost as heat through respiration and metabolic activity.
- Energy pyramid: A diagram showing decreasing energy at each successive trophic level; always widest at the producer base and narrowest at the top consumer level.
- Second law of thermodynamics: Energy conversions are never 100% efficient; heat is always lost, which explains why energy decreases as it moves up trophic levels.
- Conservation of matter: Unlike energy, matter is not lost; nutrients cycle through biogeochemical cycles and are recycled by decomposers back into the system.
If producers in an ecosystem fix 10,000 kcal/m2/yr, how much energy is available to secondary consumers? Show your calculation using the 10% rule.
1.11
Food Chains and Food Webs
A food chain shows a single linear path of energy transfer; a food web shows the full network of overlapping food chains in an ecosystem. Because species are interconnected, adding or removing one species triggers feedback effects throughout the web. Positive feedback amplifies change; negative feedback dampens it.
- Food web: An interlocking model of multiple food chains showing how energy and matter flow through an ecosystem among producers, consumers, and decomposers.
- Decomposers: Bacteria and fungi break down dead organic matter, releasing nutrients back into the soil and water for producers to use again.
- Trophic cascade: When a top predator is removed, prey populations increase, which can reduce vegetation and alter the entire ecosystem structure.
- Negative feedback loop: A change in one part of the food web triggers a response that reduces the original change, stabilizing the system.
- Positive feedback loop: A change in one part of the food web amplifies the original change, potentially destabilizing the system.
If a keystone predator is removed from a food web, describe the sequence of changes that would occur at two other trophic levels and identify whether this is a positive or negative feedback loop.
Practice AP Environmental Science unit 1 questions
Try stimulus-based AP practice questions and written prompts after you review the notes.
In a coastal kelp forest, 10 years of data show sea urchin population density and kelp biomass. In year 4, disease sharply reduced the sea otter population. The researchers want to test how the decline in this secondary consumer affected energy flow from kelp to sea urchins.
QuestionWhich statement is the appropriate null hypothesis for the investigation?
The decline in sea otters will have a significant positive effect on kelp biomass.
The decline in sea otters will have no significant effect on kelp biomass.
The decline in sea otters will have no significant effect on sea urchin population density.
The decline in sea otters will have no significant effect on energy available to tertiary consumers.
The figure below shows the average net primary productivity for six different terrestrial biomes, along with their typical latitude ranges.
QuestionWhich statement accurately describes the pattern of net primary productivity across the biomes?
Biomes located near the equator exhibit higher productivity than biomes at higher latitudes.
Net primary productivity shows a perfect negative correlation with latitude across all biomes.
Extreme environments like deserts and tundras show the highest rates of carbon assimilation.
Net primary productivity remains relatively constant across all latitudes shown in the chart.
3. Lake Mendota is a temperate freshwater lake ecosystem that supports diverse aquatic life. The lake has experienced increased algal blooms in recent years due to agricultural runoff from surrounding farmland. Scientists are studying the lake's energy flow and nutrient cycling to develop management strategies.
Trophic Level | Biomass (kg/m²) | Phosphorus Input Source | Annual P Load (kg/yr) |
|---|
Producers (Phytoplankton) | 0.45 | Agricultural runoff | 2,850 |
Primary Consumers (Zooplankton) | 0.082 | Urban stormwater | 640 |
Secondary Consumers (Small fish) | 0.015 | Atmospheric deposition | 210 |
Tertiary Consumers (Large fish) | 0.0028 | Natural sources | 180 |
Figure 1. Lake Mendota Trophic Structure and Energy Flow
1. A freshwater lake ecosystem contains phytoplankton (photosynthetic algae), zooplankton (small herbivorous animals), small fish, and large predatory fish. Energy flows through this ecosystem as organisms consume those at lower trophic levels. The productivity of the ecosystem depends on the availability of limiting nutrients, particularly nitrogen and phosphorus.
Figure 1. Dissolved Nutrient Concentrations at Different Depths in a Freshwater Lake (Nitrogen and Phosphorus)
Figure 2. Phytoplankton Biomass at Different Depths in a Freshwater Lake
i. Identify the independent variable in the students' investigation.
ii. Identify one variable that was held constant in the experimental design.
Lake Zone | Species 1 | Species 2 | Species 3 | Species 4 | Species 5 | Species 6 |
|---|
High nutrient zone | X | X | | | | |
Low nutrient zone | X | X | X | X | X | X |
i. Explain why the low nutrient zone would be more resilient to environmental disturbances, such as temperature changes or disease outbreaks, than the high nutrient zone would.
ii. Explain one reason why excess phosphorus from agricultural runoff could lead to decreased dissolved oxygen concentrations in the lake, negatively affecting fish populations.
2. A coastal estuary ecosystem supports diverse marine life and serves as a critical nursery habitat for commercial fish species. The estuary receives freshwater input from a river that drains an agricultural watershed. Recent monitoring has detected changes in water quality parameters and shifts in the phytoplankton community structure.
Figure 1. Nitrogen Cycle and Estuary Food Web in a Coastal Estuary Ecosystem (with Agricultural Runoff Input)
Figure 2. Water Quality and Biological Data from Estuary Monitoring (2015 and 2024)