Ecosystems: The Living Network | Grade 12 Life Sciences
★ Grade 12 Life Sciences ★

The Living
Network

No organism lives in isolation. Every species is connected to dozens of others through feeding relationships, competition, and the cycling of nutrients. Ecosystems are these connections — and understanding them explains why removing one species can collapse a whole system.

Structure · Food Webs · Energy Flow · Nutrient Cycles · Succession · Quiz

Ecosystem Structure

The Cast of Characters

🌿 What Is an Ecosystem?

An ecosystem is a community of living organisms (biotic factors) interacting with each other and with their non-living environment (abiotic factors) in a defined area. Energy flows through ecosystems (one-way) and matter cycles within them (recycled). Every ecosystem has producers that capture energy, consumers that feed on them, and decomposers that break down dead matter and return nutrients to the soil.

🌡️ Abiotic Factors (Non-living)

  • Temperature — affects metabolic rates of all organisms
  • Light intensity — drives photosynthesis; determines plant zone distribution
  • Water availability — limiting factor in most terrestrial ecosystems
  • Soil pH and mineral content — determines plant species composition
  • Salinity — key in aquatic ecosystems
  • Atmospheric gases — O₂ for respiration; CO₂ for photosynthesis
  • Wind and currents — affect temperature, moisture, seed dispersal

🦁 Biotic Factors (Living)

  • Producers (autotrophs) — make their own food via photosynthesis or chemosynthesis
  • Primary consumers (herbivores) — eat producers
  • Secondary consumers — eat primary consumers
  • Tertiary consumers — eat secondary consumers
  • Decomposers (saprotrophs) — bacteria and fungi; break down dead organic matter
  • Detritivores — animals that eat dead matter (earthworms, dung beetles)
TermDefinitionExample
HabitatThe physical place where an organism livesA rock pool; a forest canopy; a river bed
NicheThe role an organism plays in its ecosystem — what it eats, when it is active, how it reproduces, what eats itA barn owl's niche: nocturnal predator of small rodents, nests in buildings/trees, prey of larger raptors
PopulationAll individuals of one species in a defined area at a given timeAll lions in the Kruger National Park
CommunityAll populations of all species in a defined area — all living organisms togetherAll the plants, animals, fungi, and microbes in a grassland
EcosystemA community plus all the abiotic factors it interacts withThe grassland community + soil, rainfall, temperature, light
BiomeA large geographic area with characteristic climate and vegetationSavanna, fynbos, tropical rainforest, desert, tundra
⚠️ Exam Watch — Habitat vs Niche
A common exam error is confusing habitat and niche. Habitat = address (where it lives). Niche = occupation (what it does there — its role, diet, activity time, predators, etc.). Two species cannot occupy exactly the same niche in the same habitat indefinitely — competitive exclusion will result in one outcompeting the other (Gause's Law). Species that appear to occupy the same niche usually differ in subtle ways — feeding on slightly different sizes, active at different times, or using different microhabitats.

Food Chains & Food Webs

Who Eats Whom

🍽️ Energy Pathways Through the Ecosystem

A food chain shows a single linear pathway of energy transfer from producer to top consumer. A food web shows ALL the feeding relationships in an ecosystem simultaneously — a more realistic picture, since most animals eat more than one thing and are eaten by more than one predator. Arrows in food chains and webs point in the direction of energy flow (from eaten to eater).

A Simple Food Web — Savanna Example

Grass / Plants Zebra Wildebeest Impala Wild Dog Cheetah Lion Decomposers Arrows show direction of energy flow (from eaten → to eater)
📖
Key Terms
Food Web Vocabulary You Must Know
Trophic levels, producers, consumers — know every term cold.
TermDefinition
Trophic levelA feeding level in a food chain. Producers = T1; primary consumers = T2; secondary consumers = T3; tertiary = T4
Producer (autotroph)Makes own food from sunlight (photosynthesis) or chemicals (chemosynthesis). Always Trophic Level 1
Primary consumer (herbivore)Eats producers directly. Trophic Level 2
Secondary consumerEats primary consumers. Trophic Level 3. May be carnivore or omnivore
Tertiary consumerEats secondary consumers. Trophic Level 4. Often apex predator
OmnivoreEats both plants and animals — occupies multiple trophic levels simultaneously
DecomposerBreaks down dead organic matter; releases inorganic nutrients back into the soil/water. Not on the main food chain trophic levels
Apex predatorTop predator with no natural predators. Removal causes trophic cascade
📌 Trophic Cascades — Why Apex Predators Matter
When an apex predator is removed (by hunting or habitat loss), its prey population explodes, which then overconsumes the prey's food source. Example: when wolves were removed from Yellowstone, deer populations exploded → overgrazing stripped riverbanks → rivers changed course. When wolves were reintroduced in 1995, the whole ecosystem recovered — even the rivers. This chain reaction is a trophic cascade, demonstrating that food webs are tightly interconnected.

Energy Flow

The 10% Rule

⚡ Energy Flows One Way — It Is Never Recycled

Unlike matter (which cycles), energy flows through ecosystems in one direction only: from the sun through producers to consumers, and is lost as heat at each step. This is why food chains rarely have more than 4–5 trophic levels — there simply isn't enough energy left to support more. Understanding energy transfer efficiency is essential for exam calculations.

The Ecological Pyramid of Energy — 10% Transfer Rule

Tertiary consumer
1 kJ (1%)
Secondary consumer
10 kJ (10%)
Primary consumer
100 kJ (100%)
Producer
1 000 kJ (1 000%)

Only ~10% of energy at each level is transferred to the next. The rest is lost as heat via cellular respiration.

🔢
Must-Know Calculation
The 10% Rule — Worked Examples
Every exam will ask you to calculate energy at a given trophic level. Learn this method.

Rule: Only 10% of energy at one trophic level passes to the next. 90% is lost as heat (via cellular respiration, movement, maintaining body temperature).

Example 1 — Moving UP the pyramid

Producers fix 50 000 kJ. How much energy is available to secondary consumers?
T1 (producers) = 50 000 kJ
T2 (primary consumers) = 50 000 × 10% = 5 000 kJ
T3 (secondary consumers) = 5 000 × 10% = 500 kJ

Example 2 — Moving DOWN the pyramid

Tertiary consumers have 80 kJ available. How much energy was in the producers?
T4 = 80 kJ → T3 = 80 ÷ 10% = 800 kJ → T2 = 800 ÷ 10% = 8 000 kJ → T1 = 8 000 ÷ 10% = 80 000 kJ

Example 3 — Efficiency calculation

Producers have 20 000 kJ; primary consumers have 1 600 kJ. What is the actual transfer efficiency?
Efficiency = (energy at next level ÷ energy at current level) × 100
= (1 600 ÷ 20 000) × 100 = 8%
(Real efficiency varies 5–20%; the 10% figure is an average approximation)

⚠️ Exam Watch — Where Does the 90% Go?
Energy is NOT destroyed — it is lost from the food chain as heat generated during cellular respiration. This heat cannot be recaptured. Additional energy is lost in: undigested material (faeces), urine, movement and maintaining body temperature. Only the energy stored in body tissues (growth) passes to the next trophic level.
📐
Ecological Pyramids
Numbers, Biomass, and Energy
Three ways to represent feeding relationships. Know why some pyramids can be inverted.

🔢 Pyramid of Numbers

  • Shows the number of organisms at each trophic level
  • CAN be inverted — e.g. one oak tree (T1) supports thousands of caterpillars (T2)
  • Least useful pyramid — does not account for organism size

⚖️ Pyramid of Biomass

  • Shows total dry mass of organisms at each trophic level
  • Usually upright — more biomass at lower levels
  • CAN be inverted in aquatic systems — phytoplankton reproduce so fast that large biomass of zooplankton is supported by a small standing crop of phytoplankton

⚡ Pyramid of Energy

  • Shows energy available at each trophic level per unit area per unit time
  • ALWAYS upright — energy is always lost at each level
  • Most accurate and informative pyramid
  • Cannot be inverted under any circumstances

Nutrient Cycles

Matter Is Recycled Forever

♻️ Unlike Energy, Matter Cycles

Carbon, nitrogen, water, and other elements cycle continuously through living and non-living components of ecosystems. Decomposers are the key link — they break down dead organic matter and release nutrients back into the soil and atmosphere, making them available to producers again. Without decomposers, nutrients would become locked in dead organic matter and the ecosystem would collapse.

🌬️
Most Examined Cycle
The Carbon Cycle
Carbon moves between atmosphere, living things, oceans, and fossil fuels. Know every pathway.
🌿
Photosynthesis
Plants remove CO₂ from atmosphere and fix it into organic molecules (glucose) using light energy
🫁
Respiration
All living organisms release CO₂ back to atmosphere through cellular respiration
🍂
Decomposition
Decomposers break down dead organisms, releasing CO₂ through their own respiration
🏭
Combustion
Burning fossil fuels and wood rapidly releases stored carbon as CO₂ — disrupting the cycle

🌊 Carbon Sinks

  • Oceans — dissolve huge amounts of CO₂ from atmosphere
  • Forests — store carbon in wood and soil organic matter
  • Peat bogs — partially decomposed organic matter stores carbon for thousands of years
  • Fossil fuels — ancient carbon locked underground for millions of years

🔥 Human Impact on Carbon Cycle

  • Burning fossil fuels releases ancient carbon rapidly → atmospheric CO₂ increase
  • Deforestation removes carbon sinks AND releases stored carbon
  • Increased CO₂ → enhanced greenhouse effect → global warming
  • Ocean acidification as CO₂ dissolves to form carbonic acid → threatens marine life
🌾
The Complex One
The Nitrogen Cycle
78% of air is N₂ — but most organisms can't use it directly. Bacteria are the key to unlocking it.
ProcessWhat HappensWho Does It
Nitrogen fixationAtmospheric N₂ converted to ammonium (NH₄⁺) or nitrate (NO₃⁻) — forms plants can absorbNitrogen-fixing bacteria (Rhizobium in root nodules of legumes; free-living Azotobacter); lightning; industrial Haber process
NitrificationAmmonium (NH₄⁺) converted to nitrite (NO₂⁻) then nitrate (NO₃⁻) in the soilNitrifying bacteria (Nitrosomonas, Nitrobacter) in soil
AssimilationPlants absorb nitrates from soil through roots; use nitrogen to make proteins and DNAPlants (producers)
AmmonificationDead organic matter (proteins) broken down; nitrogen released as ammonium (NH₄⁺)Decomposers (bacteria and fungi)
DenitrificationNitrates (NO₃⁻) converted back to N₂ gas — returns nitrogen to atmosphere; completes the cycleDenitrifying bacteria in waterlogged/anaerobic soils
⚠️ Exam Watch — Why Nitrogen Fixation Matters
Plants need nitrogen to make amino acids and nucleotides — but they cannot use atmospheric N₂ directly. Only nitrogen-fixing bacteria can break the triple bond in N₂. Legumes (peas, beans, clover) have a mutualistic relationship with Rhizobium bacteria in their root nodules — the bacteria fix nitrogen for the plant in exchange for carbohydrates. This is why legumes improve soil fertility and are used in crop rotation.

Ecological Succession

How Ecosystems Change Over Time

🌱 Communities Don't Stay Still

Ecological succession is the gradual, directional change in the species composition of a community over time. It follows a predictable sequence — from simple pioneer communities to a complex, stable climax community. Each stage modifies the environment in ways that make it more suitable for the next community. Understanding succession explains how ecosystems recover from disturbance and how bare rock eventually becomes forest.

🪨
Starting from Zero
Primary Succession
Begins on bare rock or new land where no soil exists. The slowest type — takes thousands of years.
1
Pioneer species — first colonisers of bare rock. Lichens (fungi + algae) are classic pioneers. They tolerate extreme conditions (drought, temperature extremes, no soil) and slowly break down rock surface. They die and their organic matter begins soil formation.
2
Mosses and small plants — as thin soil accumulates, mosses colonise. They trap more particles, add organic matter, and create a slightly more hospitable environment for the next community.
3
Herbaceous plants (grasses, ferns) — deeper soil allows these. Their roots further break up rock, and decaying material adds humus. Small insects and invertebrates colonise. Soil improves in quality and depth.
4
Shrubs and pioneer trees — fast-growing light-demanding shrubs establish. They create shade and their leaf litter enriches soil. Attract more animal species. Eventually outcompeted by taller trees.
5
Climax community — stable, self-sustaining community that does not change unless disturbed. Species composition is in balance with the local climate. Maximum biodiversity and biomass. In temperate regions often oak woodland; in South Africa, often specific fynbos or savanna communities depending on rainfall and soil.
🔥
Starting from Disturbance
Secondary Succession
Begins where a community was destroyed but soil remains. Much faster than primary — decades, not millennia.

⚡ Key Differences from Primary

  • Soil is already present — no lichen pioneer stage needed
  • Seed bank in soil — dormant seeds germinate rapidly after disturbance
  • Much faster — decades to centuries rather than thousands of years
  • Triggered by: fire, flood, farming abandonment, storm damage, volcanic eruption that preserves soil
  • Same endpoint: climax community

🌿 South African Example — Fynbos After Fire

  • Fynbos is fire-adapted — many species require fire to germinate
  • Within weeks: geophytes (bulbs) re-sprout; annual herbs germinate from seed bank
  • Months: grasses and small shrubs re-establish
  • Years: proteas, ericas, restios re-establish
  • Without periodic fire: alien invasive plants overwhelm fynbos → biodiversity collapses. Fire IS part of the fynbos ecosystem
📌 Climax Community — Stability, Not Stasis
The climax community is stable but not unchanging. It experiences normal turnover as individual organisms die and are replaced. But the SPECIES COMPOSITION remains relatively constant. The climax is determined by climate — same climate = same climax community, regardless of which succession pathway led there (this is called convergence). Disturbances reset succession and are part of many healthy ecosystems (fire in fynbos, gap dynamics in forests).

🎯 Ecosystem Assessment

Eight questions covering the full ecosystem topic.

Question 1 of 8
In a grassland ecosystem, grass fixes 80 000 kJ of energy. How much energy is available to secondary consumers?
Question 2 of 8
Why does the pyramid of energy ALWAYS have a broader base than top, while the pyramid of numbers can be inverted?
Question 3 of 8
Which bacteria are responsible for converting atmospheric nitrogen (N₂) into forms that plants can absorb?
Question 4 of 8
A biologist removes all the lions from a savanna ecosystem. Which sequence of events is most likely?
Question 5 of 8
What is the difference between a species' HABITAT and its NICHE?
Question 6 of 8
Why is the role of decomposers essential to the functioning of an ecosystem?
Question 7 of 8
A forest fire destroys a mature woodland, but the soil and seed bank remain intact. What type of succession will follow, and why will it be faster than succession on newly formed volcanic rock?
Question 8 of 8
In the carbon cycle, how does carbon in atmospheric CO₂ become incorporated into the body of a lion?
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