Ecological succession is change in community composition and associated conditions over time. Primary succession begins where soil is initially absent, such as newly exposed rock. Secondary succession occurs after a disturbance where soil remains. Early colonisers can alter shade, organic matter and substrate conditions, affecting later species. Pathways depend on the setting and disturbance history; there is no single sequence for every ecosystem.
Biotic and abiotic changes influence one another. A decline in light at ground level can accompany canopy development, changing which plants establish. Fossils and sediments provide evidence of longer-term environmental changes. Marine fossils in a rock layer support a past marine setting, but one finding does not provide an exact past temperature. Interpret the stated evidence at the level it supports.
Example 1
Vegetation returns to a burnt grassland where soil remains. Classify the succession.
Secondary succession: the disturbance removed vegetation but did not remove the soil.
Example 2
A sequence shows bare rock, lichens, shallow soil and later grasses. Identify one relevant change.
Soil development changes the substrate and permits establishment of plants requiring soil.
Watch out: Succession depends on available species, conditions and disturbances, so trajectories can differ.