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Ecological Succession in plants MCQ - Practice Questions with Answers

Edited By admin | Updated on Sep 18, 2023 18:34 AM | #NEET

Quick Facts

  • Ecological Succession is considered one of the most asked concept.

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Ecological Succession
  • An important characteristic of all communities is that composition and structure constantly change in response to the changing environmental conditions. 
  • This change is orderly and sequential, parallel with the changes in the physical environment. 
  • These changes lead finally to a community that is in near equilibrium with the environment and that is called a climax community. 
  • The gradual and fairly predictable change in the species composition of a given area is called ecological succession. 
  • During succession some species colonise an area and their populations become more numerous, whereas populations of other species decline and even disappear.
  • The entire sequence of communities that successively change in a given area are called sere(s). 
  • The individual transitional communities are termed seral stages or seral communities.
  • In the successive seral stages there is a change in the diversity of species of organisms, increase in the number of species and organisms as well as an increase in the total biomass.
  • Succession can be of two types depending on the areas that are colonised:
    • Primary succession: process that starts where no living organisms are there – these could be areas where no living organisms ever existed, say bare rock.
    • Secondary succession: in areas that somehow, lost all the living organisms that existed there.

Primary succession:

  • Examples of areas where primary succession occurs are newly cooled lava, bare rock, newly created pond or reservoir. 
  • The establishment of a new biotic community is generally slow. 
  • Before a biotic community of diverse organisms can become established, there must be soil. 
  • Depending mostly on the climate, it takes natural processes several hundred to several thousand years to produce fertile soil on bare rock.

Secondary succession:

  • Secondary succession begins in areas where natural biotic communities have been destroyed such as in abandoned farm lands, burned or cut forests, lands that have been flooded. 
  • Since some soil or sediment is present, succession is faster than primary succession.
     
Succession of Plants
  • Based on the nature of the habitat – whether it is water (or very wet areas) or it is on very dry areas – succession of plants can be:
    • Hydrarch succession takes place in wetter areas and the successive series progress from hydric to the mesic conditions. 
    • Xerarch succession takes place in dry areas and the series progress from xeric to mesic conditions.
  • Hence, both hydrarch and xerarch succession lead to medium water conditions (mesic) – neither too dry (xeric) nor too wet (hydric)

Hydrarch Succession:

  • In primary succession in water, the pioneers are the small phytoplanktons, they are replaced with time by free-floating angiosperms, then by rooted hydrophytes, sedges, grasses and finally the trees. 
  • The climax would be a forest. With time the water body is converted into land.
  • Hence, it consists of following stages:
    • Submerged stage: a number of submerged aquatic plants, such as Hydrilla, Elodea, Potamogeton, Ceratophyllum, Najas, Vallisneria, Utricularia, Ranunculus and several algae
    • Floating stage: characterized by plants like Nymphaea, Polygonum, Limnanthemum and Castalia etc. These plants are rooted in the mud, and their broad leaves float on the surface of the water
    • Reed-Swamp stage: by amphibious plants like Scirpus, Typha, Phragmites etc. These plants remain only partly submerged in water.
    • Sedge meadow stage: characterized by plants like Carex, Juncus and Eleocharis.
    • Woodland stage: dominated by shrubs and small trees 
    • Climax forest stage: large trees

Xerarch Succession:

  • In primary succession on rocks these are usually lichens which are able to secrete acids to dissolve rock, helping in weathering and soil formation.
  • These later pave way to some very small plants like bryophytes, which are able to take hold in the small amount of soil. 
  • They are, with time succeeded by bigger plants, and after several more stages, ultimately a stable climax forest community is formed. 
  • The climax community remains stable as long as the environment remains unchanged.
  • With time the xerophytic habitat gets converted into a mesophytic one.
     

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