June 2026·12 min read·Succession · Disturbance · Fire Ecology
Forest Succession: How Ecosystems Rebuild Themselves
Walk across a lava flow that cooled a century ago, an abandoned farm field, or a hillside
scorched by wildfire, and you are watching the same story unfold at different stages:
life methodically reclaiming bare ground. Ecological succession is the orderly, predictable
process by which communities of organisms replace one another over time, transforming
sterile substrate into towering old-growth forest. This article explains the difference
between primary and secondary succession, the role of pioneer species and climax
communities, the three classic mechanisms by which one stage gives way to the next, why
moderate disturbance can maximise diversity, and how some forests have evolved to depend
on fire.
1. Primary versus Secondary Succession
Ecologists distinguish two fundamentally different starting points for succession,
separated by one critical resource: soil.
Primary succession
Primary succession begins on lifeless substrate where no soil exists —
newly cooled lava, land exposed by a retreating glacier, fresh volcanic ash, or a
sandbar. With no organic matter, no seed bank, and no microbial community, the first
colonists must survive on bare mineral rock. Primary succession is slow, often taking
centuries to millennia to build the deep, fertile soils a forest requires. The classic
textbook example is the retreating glaciers of Glacier Bay, Alaska.
Secondary succession
Secondary succession follows a disturbance that removes much of the
existing community but leaves the soil — and usually a seed bank, roots, and surviving
organisms — intact. Abandoned farmland, logged plots, and burned forests all undergo
secondary succession. Because the soil and biological legacy already exist, recovery is
far faster, often producing a recognisable forest in decades rather than centuries.
The key distinction: Primary succession must build soil from scratch;
secondary succession inherits it. This single difference accounts for the order-of-
magnitude gap in how long the two processes take to reach a mature community.
2. Pioneer Species and the Seral Stages
The first organisms to colonise open ground are the pioneer species.
In primary succession these are typically lichens and mosses — organisms that can cling
to bare rock, fix atmospheric nitrogen (often via cyanobacterial partners), and survive
extremes of temperature and desiccation. As lichens secrete acids and trap dust, they
begin the slow manufacture of soil.
Pioneer species share a characteristic life-history strategy, often called
r-selected: rapid growth, early reproduction, prolific output of small,
wind-dispersed seeds or spores, high tolerance of harsh, sunny, exposed conditions, and
short lifespans. They are excellent colonisers but poor competitors.
The intermediate communities that follow are called seral stages (each
a sere). A typical secondary sequence on abandoned farmland runs:
Annual weeds and grasses — fast, sun-loving colonisers (years 1–3)
Perennial herbs and shrubs — taller, longer-lived (years 3–15)
Fast-growing pioneer trees — birch, aspen, pine; shade-intolerant (years 15–80)
Shade-tolerant hardwoods — oak, maple, beech; the eventual canopy
3. The Climax Community
The endpoint that succession tends toward is the climax community — a
relatively stable, self-perpetuating assemblage in equilibrium with the regional climate
and soils. In a temperate climate this is typically a closed-canopy forest dominated by
shade-tolerant, slow-growing, long-lived trees. These late-successional species are
K-selected: they invest in fewer, larger seeds, grow slowly, tolerate
shade as seedlings, and persist for centuries.
The early 20th-century ecologist Frederic Clements imagined the climax as a single,
deterministic endpoint dictated by climate — a "superorganism" developing toward
maturity. Henry Gleason countered that communities are individualistic and contingent on
chance and dispersal. Modern ecology sits between them: succession is directional and
partly predictable, but the precise endpoint depends on local conditions, history, and
ongoing disturbance. Many ecologists now prefer to speak of a shifting
climax mosaic rather than a single fixed community.
Net primary productivity (NPP) over succession:
NPP rises rapidly in early stages, peaks in mid-succession,
then declines as the forest matures.
Biomass accumulation: B(t) ≈ B_max · (1 − e^(−k·t))
where B_max = carrying-capacity biomass of the climax stand
k = growth-rate constant set by climate and soil
4. Facilitation, Inhibition, Tolerance
In 1977 Joseph Connell and Ralph Slatyer proposed three distinct mechanisms by which one
successional stage gives way to the next. Real successions usually combine all three.
Facilitation
In the facilitation model, early species modify the environment in ways
that make it more suitable for later species — and often less suitable for
themselves. Nitrogen-fixing pioneers enrich the soil, leaf litter builds humus, and
shade reduces evaporation. The pioneers literally prepare the ground for their
successors. This dominates classic primary succession.
Inhibition
In the inhibition model, whoever arrives first holds the site and
actively resists invasion — through shading, allelopathic chemicals, or pre-empting
space and nutrients. Succession proceeds only when the incumbents die or are removed by
disturbance, releasing the site to the next colonist. Order of arrival, not facilitation,
drives the sequence.
Tolerance
In the tolerance model, later species are simply those able to tolerate
the lower resource levels (especially light) that develop as the community matures. Early
and late species can establish at the same time, but the shade-tolerant ones persist and
eventually dominate because they can survive where the sun-demanding pioneers cannot.
5. The Intermediate Disturbance Hypothesis
If succession always ran to a single climax dominated by a few superior competitors, we
would expect mature forests to be relatively species-poor. Yet many of the most diverse
ecosystems on Earth are far from undisturbed. The
Intermediate Disturbance Hypothesis (IDH), also from Connell, resolves
the paradox.
Species diversity as a function of disturbance:
Low disturbance → competitive exclusion → few dominant climax species → low diversity
High disturbance → only fast pioneers survive → low diversity
Intermediate → pioneers AND late species coexist → MAXIMUM diversity
Diversity D(disturbance) is hump-shaped, peaking at intermediate frequency/intensity.
At intermediate levels of disturbance frequency and intensity, the system never settles
into competitive exclusion (which would let dominant climax species crowd everyone out)
and never collapses to only the hardiest pioneers. Both early- and late-successional
species coexist across a patchwork of recently disturbed and recovering ground, and total
diversity peaks. Coral reefs and many forests fit this hump-shaped pattern, though the
IDH is now understood as one important mechanism among several rather than a universal law.
6. Fire Ecology and Disturbance-Dependent Forests
For some ecosystems, disturbance is not an interruption of succession but an integral
part of it. Many forests are fire-adapted and even
fire-dependent, having evolved over millions of years with recurring
burns as a normal feature of the landscape.
The adaptations are striking:
Serotiny: lodgepole pine, jack pine and many eucalypts hold their
seeds in resin-sealed cones or capsules that open only when heated by fire, releasing
seed onto freshly cleared, nutrient-rich, competitor-free ground.
Thick insulating bark: ponderosa pine and giant sequoia survive
low-intensity surface fires that kill their competitors.
Epicormic and lignotuber resprouting: many eucalypts and oaks
regenerate rapidly from protected buds beneath the bark or underground after the canopy
burns.
Fire-stimulated germination: chemicals in smoke (karrikins) trigger
dormant seeds in chaparral and fynbos to germinate.
A century of aggressive fire suppression in western North America illustrates the danger
of removing a disturbance an ecosystem evolved to need. Without periodic low-intensity
burns, fuel — dead wood, litter, dense understorey — accumulates for decades. When fire
inevitably comes, it burns hotter and higher, becoming a catastrophic crown fire that
even fire-adapted species cannot survive. Modern forest management increasingly uses
prescribed burning to restore the natural disturbance regime, keep fuel
loads low, and maintain the mosaic of seral stages that sustains biodiversity. Fire, used
well, is a tool of succession rather than its enemy.