Secondary succession is generally faster because soil, nutrients, propagules, decomposer communities, and sometimes resprouting plants survive the disturbance. Primary succession must begin with substrate weathering and soil formation, processes that can delay the establishment of larger and more resource-demanding species for decades or centuries. Successional trajectories emerge from dispersal, establishment, species interactions, and organism-driven environmental change. Priority effects can make arrival order important, while retained soil and propagules strongly accelerate recovery after disturbance. Facilitation, tolerance, and inhibition are alternative mechanisms rather than mandatory universal stages; more than one may operate at the same site or at different times. The eventual assemblage also depends on climate, substrate, disturbance frequency, and the regional species pool, so a climax is better viewed as dynamic persistence than permanent equilibrium. In this context, the keyed term, Secondary, identifies the relevant mechanism or quantitative relationship and links the observed pattern to its underlying ecological cause. The distinction is testable by measuring changes in organisms, resources, or process rates through time rather than relying on the label alone.
Ref:
Ecology: Concepts and Applications, Molles, 9th Ed., Ch. 20