Ecosystems are dynamic; they change due to climate shifts, invasive species, natural disasters, seasonal cycles, and time.
The gradual sequence of community changes over time is called ecological succession.
Comparable to royal succession: when one community “dies,” another “inherits” the habitat.
Time scale ranges from a few \text{decades} to \text{millions of years}.
Begins on newly formed, lifeless surfaces.
Examples: volcanic lava flows, land exposed by retreating glaciers.
No pre-existing soil; surface is bare rock or ash.
Pioneer species (algae, fungi, lichens) are first colonizers; they break down rock and start soil formation.
Few organisms initially ⇒ biodiversity rises gradually as soil develops and plants, then animals, establish.
Rebuilding of a previously existing ecosystem after a major disturbance (fire, flood, storm, human clearing).
Soil already present; seed bank and microorganisms often survive.
Pioneer species + early plants (grasses, herbs) arrive quickly, followed by shrubs, trees, and animals.
Starts with low biodiversity, which increases over time as community complexity returns.
Undersea volcanic eruption 1963–1967 created a brand-new island ⇒ classic primary succession site.
First plant colonization recorded 1965 via ocean-borne seeds.
Early pioneers: sea rocket, sea sandwort, sea lyme grass.
Ongoing observations show gradual soil development and rising biodiversity.
Primary vs. Secondary: presence of soil is the main difference; primary starts from bare rock, secondary from existing soil.
Pioneer species kick-start both processes but face harsher conditions in primary succession.
Biodiversity trajectory: both forms move from low to higher diversity, but secondary succession is usually faster due to existing soil and seed banks.