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Biology HL · Chapter 12: Ecological Relationships

12.4 Stability, Change and Succession in Ecosystems

Explain resistance, resilience and tipping points, evaluate agricultural impacts, and compare primary, secondary and cyclical succession.

Estimated time: 165 minutes

IB syllabus: D4.2 · SL and HL

Stability Is Dynamic, Not Motionless

An ecosystem is stable when its structure and processes remain within a characteristic range or recover after disturbance. Resistance is the ability to change little during a disturbance; resilience is the ability to return after change. A grassland may burn readily and therefore have low resistance to fire, yet regrow rapidly from protected roots and therefore have high resilience. Stability must be attached to a variable and time scale: species composition, productivity and nutrient retention can respond differently.

Biodiversity can support stability because species may respond differently to stress and partly replace one another's functions. Complex food webs can provide alternate pathways, genetic diversity can supply tolerant variants, and spatial heterogeneity can preserve refuges. Diversity does not guarantee stability under every disturbance, however. Strongly connected networks can transmit effects, and a stress that affects many species through the same mechanism can overwhelm redundancy.

Negative feedback opposes displacement and can stabilize a system: rising prey density supports predators, which then reduce prey. Positive feedback amplifies change. Vegetation loss can expose soil, erosion can reduce plant establishment and further vegetation can be lost. A tipping point is a threshold beyond which feedback drives the system toward a different state, potentially with hysteresis: reversing the original pressure may not be sufficient to restore the previous community.

Mesocosms and Evidence for Sustainability

A mesocosm is a bounded experimental ecosystem that preserves more ecological complexity than a laboratory flask while allowing greater control and replication than a whole landscape. Aquatic tanks, enclosed soil communities and field chambers can test temperature, nutrients, pollutants or species removal. Investigators standardize starting conditions, include controls, replicate independent units and monitor variables such as oxygen, biomass, nutrient concentration and species abundance.

A sealed mesocosm is materially closed but energetically open: light enters and heat leaves. Producers must capture enough energy, organisms must remain within compatible population ranges, and decomposers must return mineral nutrients. Persistence for a short experiment does not prove indefinite sustainability, because slow depletion, genetic change or rare disturbance may not appear. Mesocosm walls also alter dispersal and predator behavior, so results must be transferred to natural ecosystems cautiously.

Agriculture Changes Energy, Carbon and Diversity

Agriculture redirects ecological production toward human harvest. Land clearance removes biomass and habitat, fragments populations and can release carbon from vegetation and soil. Monocultures simplify species and genetic diversity; machinery and tillage disturb soil; livestock require feed and produce methane; irrigation changes water movement; and fertilizers add reactive nitrogen and phosphorus. These effects depend on practice and landscape, but they are not captured by yield alone.

Fertilizer manufacture and application accelerate the nitrogen cycle. Crops absorb some added nitrate or ammonium, but surplus nitrate can leach into groundwater or run into surface water. Denitrification can produce nitrous oxide, a greenhouse gas, while ammonia can volatilize and later deposit elsewhere. Harvest removes mineral nutrients from the field, so agriculture often relies on replacement through fertilizer, manure, crop rotation or nitrogen-fixing symbioses.

Sustainable agriculture aims to maintain production while preserving soil, water, biodiversity and future options. Practices include reduced tillage, cover crops, crop rotation, integrated pest management, precise nutrient application, agroforestry, habitat strips and matching livestock density to carrying capacity. Each has trade-offs and must be evaluated using long-term evidence: reducing one pressure can shift another, and local yield, total land demand and off-site impacts all matter.

HL extensionD4.2 AHL

Succession and Stability Laboratory

Disturb a landscape, compare primary and secondary succession, and observe how soil inheritance and grazing alter recovery.

flow · populations · feedback · recovery

Ecological relationships laboratory

DISTURBANCE → LEGACY → COLONIZATION → COMMUNITY CHANGEpioneergrass + herbsshrub mosaicmature woodlandsecondary succession: soil and biological legacies remain

Primary and Secondary Succession

Ecological succession is a directional change in community composition through time. Primary succession begins where no developed soil and little biological legacy remain, such as new lava, exposed rock or recently deglaciated sediment. Pioneer organisms tolerate harsh conditions. Weathering, trapped particles, organic inputs and microbial activity gradually build soil. Later colonists alter shade, moisture and nutrient availability, changing which species can establish.

Secondary succession begins after disturbance removes a community but leaves soil, seed banks, roots, microorganisms or nearby colonists. Recovery is usually faster because those legacies bypass slow soil formation. Annual plants may be followed by perennial herbs, shrubs and woodland, but the sequence depends on climate, dispersal, herbivory, soil and repeated disturbance. Succession is not a universal ladder with one inevitable endpoint.

Early stages often have rapid growth, high light at ground level and simple food webs. As biomass and structural complexity rise, more niches become available and gross productivity may increase. Community respiration also rises, and net ecosystem production may approach balance in a mature system. Nutrient cycles often become tighter as deeper roots, litter and decomposer networks retain matter, although storms, fire and herbivores continue to create patches.

Climax, Plagioclimax and Cyclical Change

A climax community is a relatively persistent community compatible with prevailing conditions. It remains dynamic: organisms die and recruit, populations fluctuate and small disturbances occur. Climate strongly influences the broad endpoint, but soil, topography, fire and animals can maintain several stable or shifting states. Modern ecology therefore treats climax as a useful approximation rather than a single predetermined final community.

Repeated human activity can arrest succession at a plagioclimax. Grazing, mowing, burning or cutting may maintain grassland or heath that would otherwise develop more woody vegetation. When management stops, succession may resume, but depleted seed sources or altered soil can delay or redirect it. Conservation may deliberately maintain a plagioclimax when its species depend on the managed habitat.

Cyclical succession occurs when communities replace one another in a repeating pattern rather than progressing toward a permanent endpoint. Heather growth, degeneration and regeneration can form a patch cycle; tree gaps pass through establishment, growth and senescence; grazing fronts can move across vegetation mosaics. The larger ecosystem can remain stable while individual patches occupy different stages.

Test Yourself

Two burned sites have equal plant biomass after five years. Site X regained its original species composition; site Y is dominated by a different stable community. Which conclusion is best?

Exam questions on this topic

Practice focused questions or see how IB combines this topic with ideas from elsewhere in the course.