This document discusses plant succession, including the causes, types, and theories of succession. It provides details on primary and secondary succession. There are two main types of succession: primary succession, which occurs in newly exposed bare areas, and secondary succession, which occurs in areas where vegetation has been disturbed but soil remains. Succession proceeds through a series of plant communities called seral stages and over time progresses toward a climax community. Major theories of succession include the monoclimax theory, polyclimax theory, and climax pattern theory. The document also outlines the main stages of hydrosere and xerosere, or aquatic and dry land succession.
2. Succession
Succession may be defined as an orderly process of
community change”.
In the words of Salisbury,
“Plant succession is a competitive drift in which at each
phase until the climax the constituent species render the
habitat more favorable to their successors than to
themselves.”
Pioneer community :
The first community to become establish
in an area
Climax community:
The final community stage is called climax
community
3. 2. Causes of Succession:
The main causes of succession are as follows:
Climatic causes
Topographic causes
Biotic causes
4. Climatic causes:
plants cannot adjust with the long
range variations in the climate.
The fluctuating climate sometimes
leads the vegetation towards total or
partial destruction and, as a result,
the bare area develops which
becomes occupied by such plants as
are better adapted for changed
climatic conditions.
The fluctuating climate sometimes
leads the vegetation towards total or
partial destruction and, as a result,
the bare area develops which
becomes occupied by such plants as
are better adapted for changed
climatic conditions.
5. Topographic causes
These are concerned with the changes in the
soil.
Erosion of the soil:
Sometimes surface soil is removed by a
number of agents, such as wind, water
currents, and rainfall. This process is known
as soil erosion. In the process of erosion new
and bare area is exposed in which new plant
communities begin to appear one after
another.
Soil deposition:
If the deposition of soil takes place over an
area already covered with vegetation, the
plants occurring over there may be
suppressed and destroyed. Deposition results
in a new bare area on which succession of
vegetation starts.
6. Biotic causes:
Many biological or living agencies also affect the vegetation
in many respects.
Grazing, cutting, clearing, cultivation, harvesting, and
deforestation, all caused by living agencies, are directly
responsible for vegetation change.
The parasitic plants and animals also affect the vegetation
and destroy it.
7. 3. Types of succession
Plant succession may be of two kinds:
Primary succession
Secondary succession
8. Primary succession
“Primary succession, type of
ecological succession (the
evolution of a biological
community’s ecological structure)
in which plants and animals first
colonize a barren, lifeless habitat”
10. Secondary succession
“This kind of succession begins wherever the existing
vegetation has been destroyed without denuding the
area of soil.”
It usually starts after forest fires, cutting of the trees, flood
and erosions. It is also of common occurrence in abandoned
agricultural lands.
12. Sere and seral stages:
A single case of plant succession at a particular kind of habitat is usually referred to as a
sere, and the various stages of a sere are called seral stages.
A single case of plant succession at a particular kind of habitat is usually referred to as a
sere, and the various stages of a sere are called seral stages.
Hydrosere:
When succession starts in aquatic habitat
Xerosere:
When succession initiates on a dry, bare land.
Lithosere
It starts on a bare rock surface.
Psammosere:
Initiating on sandy habitats
Senile
It is the succession of micro-organisms and lower plants on dead plant parts and bodies.
Eosere or Geosere
It is the development of vegetation in an era.
14. Monoclimax theory
This theory was put forward by an American ecologist Frederick Clements in 1916.
According to this theory there is only one climax community in a climatic or geographical
region. But topographic differences and different soil types form other communities in the
same zone. These communities are known as subordinate communities .the subordinate
communities may be proclimax, post climax, disclimax, preclimax, and subclimax
communities.
Proclimax:
The community which is more or less stable resembling the climax community is called
proclimax.
Disclimas:
The community disturbed by man or other animals is called disclimax community. Its example is
grassland in forest area.
Subclimax or preclimax:
The community in which development is stopped in the subtinal matte of succession due to
burning, cutting or grazing and flooding is called subclimax or preclimax community.
Post climax:
The community in which a strip of vegetation of higher life form is found within a climax is called
post climax community. Its example is forest strip along a stream in grassland.
15. Polyclimax Theory
“this theory was put forward by European ecologists Nicholos.
Champion and Whitaxer in 1953.
According to this theory a number of different climax communities
are present in climatic or geographical region.
Thus preclimax, postelimax and disclimax communities are all climax
communities. They are all self-reproducing communities. They can
maintain themselves or an indefinite period of time.
This theory does not rule out climax communities. But it gives other
stages of communities as full status of climax communities. Thus
these are not regarded as in minor communities
16. 3.Climax Pattern Theory
This theory was put forward h Whitaker (1963). McIntosh (1958) and
Sellech (1913).
According to this theory the structure, composition and other
characters of the climax communities are determined by the total
environment of the ecosystem. It is not determined by single factor.
Climax community is composed of an communities. These
communities have close interrelationship the flora and fauna of the
area soil and climate
A particular plant cannot survive. Its seeds must be properly
distributed. Similarly an animal cannot survive without food of plants.
The climatic climax is the most popular community.
The community which expresses the climate of the area is called
cilmatric community.
17. 5. Stages of hydrosere and
xerosere
A ) stages of hydrosere
18. 1.Phytoplankton stage:
They will be pioneer community
Blue green algae , green algae, diatoms bacteria etc.
They multiply and grow for some time
Fix light energy
Add nutrients to soil and water
2.Rooted submerged stage:
Nutrients are added to the soil by the death and decomposition of
planktons
Soft muddy bottoms forms
Bottom rich with silt
Water depth becomes shallower
Light penetration become easy
This promote the growth of rooted hydrophytes
Example: Hydrilla,Vallisneria,utricullaria
19. 3.Rooted floating stage:
More reduction in water depth
Increase in the width of bottom soil/silt
Death and decomposition of rooted plants and nutrients
Rooted floating plants starts to appear
Example :Nelumbo, Nymphea, Trapa
Free floating plants can also develops :Azolla, Lemna, Wolffia, Pistia,
Salvinia
4 .Reed-swamp stage:
Also called amphibious stage
Water level very much reduced
Soil and silt level increases
Soil become more fertile by death and decay of plants
Most of the plant will be rooted, but their shoots exposed to air
Have well develop rhizome
Forms very dense vegetation
Example :Typha, sagitaria
20. 5. Sedge Meadow Stage
Water level further decreases
Soil level further increases
Plants of cyoeraceae and poaceae predominate
They forms mat like vegetation over the top of the soil
Rhizome well developed and interconnected
Have high rate of transpiration, water level further reduced
Soil exposed to air
Nutrients like ammonia and sulfides become oxidized to nitrates & sulfates
Terrestrial soil formation proceeds
Woodland stage:
Soil become drier most of the times
Marshy vegetation replaced terrestrial plants
Shrubs and herbs predominates
Small trees also occurs
Huge accumulation of humus occurs
Variety of decomposers in the soil
Fertility of soil increases
Example of plants : Salix ,Eupatorium ,Alnus
21. 7. Forest stage
Climax community
Wood land community is invaded by tree forms
Tree forms predominate
Canopy cover the entire area
Light penetration to the lower canopy reduced
Herbs and shrubs highly reduced
Wooded climbers also predominates
Climate determines the type of forest (evergreen ,deciduous etc.)
Example of plants: Shorea, Quercus,Acer
23. Stages of xerosere
1. bare rocks
The first form of life originate
2.Crustose lichen :
Lichen is important pioneer in primary succession
composed of phosynthesizing algae and fungi absorbing
nutrient from rocks
They break down rocks
Soil accumulate as particles trapped in cracks of ricks
Lichen decompose provide food for mosses
24. Foliose of lichen stage
The can be absorb more water and able to accumulate more
soil particle
The shallow depression in rocks filled with sold and topsoil
further increase
These autogenic changes favor growth and establishment of
mosses
Mosses stage
Mosses develop in patches they catch soil particles from air
and increase the amount of substratum
The changing environment leads to migration of lichen and
help in invasion of herbaceous vegetation that out compete
mosses
25. Herb stage:
Herbaceous weeds such as milk weed and evening primroses
invade the rocks
Their root penetrate deep secrete acid and enhance weathering
Leaf liter and the death of herbs add humus to the soil
Shrub stage
The herb and grass mixture is invaded by shrub species, such as
Rhus and Phytocarpus.
Early invasion of shrub is slow, but once a few bushes have
become established, birds invade the area and help disperse scrub
seeds.
Climax stage :
The succession culminates in a climax community, the forest. Many
intermediate tree stages develop prior to establishment of a climax
community.