Vegetation Succession
The vegetation at any given place also represents a point of time in the interactions among
available plants, physical and biological disturbances that vary in severity, frequency and
duration, changeable weather, and large scale climate changes.
Succession is the process of revegetation after disturbance. Complete successions begin on bare
surfaces. Usually the pioneering plants form open communities that, except in the harshest of
environments, are soon replaced by denser, taller communities, which are dominated by a
different set of plant species. In the absence of further massive disturbances or environmental
changes, steady-state or climax vegetation eventually establishes, which may change locally in
time and space. However, it remains uniform overall.
Successions are primary if they begin on unweathered parent material, and secondary if they
begin on soil developed under preceding vegetation. Succession in tussock grasslands is therefore
secondary.
Regeneration is the process whereby species remain in a community- the death of individual plants is compensated by the establishment of seedlings or be vegetative reproduction. Information taken from Wardle, 1991. Vegetation of New Zealand, Cambridge University Press.
At conservation workshops held in 1996, ecologists and land managers highlighted the factors
influencing plant succession, which are presented in the table below.
Below is a vegetation succession model developed by Colin Meurk. Assuming that a grassland
is no longer disturbed by grazing or burning activities, the rate of vegetation change will be
determined to a large extent by the degree of environmental stress present. Grassland sites which
are cold or drought prone are likely to remain as grasslands. Those which occur in humid areas
are more likely to revert to shrubland, woodland and eventually forest, given that a suitable seed
source is available.
![]() Vegetation Succession Model (after Meurk)
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