Chapter 4 (Part 2): Plant Succession
Chapter 4 (Part 2): Plant Succession
Primary Seres, Secondary Dynamics, Climax Theories and Silvicultural Applications
1. Riverain Succession on Gangetic Alluvium
Primary succession on new alluvial deposits in Northern India progresses through six stages.
Saccharum spontaneum + Tamarix dioica
Acacia catechu + Dalbergia sissoo
Acacia catechu + Holoptelea + Adina cordifolia + Albizia procera
Holoptelea + Adina + Lagerstroemia parviflora + Bombax ceiba + Terminalia bellirica
Adina + Lagerstroemia parviflora + Terminalia spp. + Shorea robusta
Shorea robusta + Lagerstroemia + Terminalia spp. + Adina
Stage-wise reference table
| Stage | Characteristic species |
|---|---|
| 1 | Saccharum spontaneum, Tamarix dioica |
| 2 | Acacia catechu, Dalbergia sissoo |
| 3 | Acacia catechu, Holoptelea, Adina cordifolia, Albizia procera |
| 4 | Holoptelea, Adina, Lagerstroemia parviflora, Bombax ceiba, Terminalia bellirica |
| 5 | Adina, Lagerstroemia parviflora, Terminalia spp., Shorea robusta |
| 6 | Shorea robusta, Lagerstroemia, Terminalia spp., Adina |
2. Coniferous Succession in Temperate Himalayas
Succession on new mountain soils progresses through four stages.
3. Estuarine Succession on Tidal Mudflats
Estuarine succession occurs on tidal mudflats and deltaic deposits.
4. Retrogression and Secondary Succession
Retrogression (Regression)
Reversion of vegetation to an earlier successional stage following the introduction of an adverse factor such as fire, clearing, overgrazing or severe drought.
Retrogressive stages are generally lower in height and more xerophytic in character.
Secondary pioneers after disturbance
| Habitat / Site | Characteristic secondary pioneers |
|---|---|
| Moist tropical evergreen clearings | Macaranga spp., Trema orientalis, Acrocarpus fraxinifolius, Callicarpa |
| Himalayan secondary hill clearings | Woodfordia fruticosa, Indigofera pulchella, Berberis lycium |
| General colonizers | Pinus wallichiana, Trema, Anthocephalus cadamba |
5. Theories of Climax
Mono-climax Theory — Clements (1916)
Climate is the sole master factor governing vegetation. Given sufficient time without disturbance, all seral communities in a region ultimately converge towards one climatic climax.
Poly-climax Theory
Permanent differences in soil, relief and drainage prevent complete convergence, producing multiple stable edaphic or topographic climaxes within a climatic region.
Aubreville's Mosaic Theory
Tropical climax forests are dynamic mosaics of small constituent units undergoing cyclic alternations of species replacement.
Whittaker's Climax Pattern Theory
Rejects fixed absolute climaxes and views climax as a continuous steady state adapted along multi-variable environmental gradients.
Comparison of climax theories
| Theory | Main proposition | Key emphasis |
|---|---|---|
| Mono-climax | One regional climatic climax. | Climate as master factor. |
| Poly-climax | Multiple stable climaxes. | Soil, relief and drainage. |
| Mosaic | Dynamic patchwork of forest units. | Cyclic species replacement. |
| Climax pattern | Climax varies continuously along environmental gradients. | Multiple environmental variables. |
6. Categories of Climax Formations
| Climax category | Definition / ecological status | Indian forestry examples |
|---|---|---|
| Climatic climax | Governed by regional climate and natural biotic interactions. | Southern Tropical Wet Evergreen (Type 1A/C1); Moist Sal Forest (Type 3C/C2); Western Mixed Coniferous (Type 12/C1d). |
| Edaphic climax | Stable community differing from regional climatic climax due to soil peculiarities. | Cane brakes (Type 1B/E1); Wet bamboo brakes (Type 1A/E2); Terminalia tomentosa on heavy clay; Anogeissus pendula (5B/E1); Boswellia serrata (5B/E2); Babul (5B/E3); Hardwickia (5B/E4). |
| Pre-climax | Community preceding regional climatic climax, occurring under drier conditions. | Pinus roxburghii on dry ridges within Subtropical Broad-leaved Forest; very moist Teak adjoining Evergreen forest at Mt. Stuart. |
| Post-climax | Community more exacting than climatic climax on exceptionally moist microsites. | Evergreen / Semi-evergreen patches such as Golatappar, Dehradun, within Moist Deciduous Sal forest. |
| Biotic sub-climax / Disclimax | Stable community held short of climatic climax by persistent biotic interference. | Grassy riverain subclimax; Chir pine where Quercus incana is climatic climax; Sal, Teak and Deodar maintained by periodic controlled fire. |
7. Important Differences Between Climax Categories
Climatic climax
Determined by regional climate.Edaphic climax
Determined by persistent soil conditions.Pre-climax
Associated with relatively drier conditions than the regional climatic climax.Post-climax
Associated with exceptionally moist microsites and more exacting vegetation.Disclimax
Maintained by persistent disturbance or biotic interference such as fire and grazing.8. Importance of Plant Succession in Silviculture
Forest classification
Provides the ecological foundation for classifying forests into climatic, edaphic and seral forest types.
Choice of plantation species
Helps avoid planting exacting climax species on raw, immature seral soils where they may fail to establish.
Management of economic sub-climaxes
Guides the use of controlled disturbance, such as periodic burning or grazing, to maintain economically valuable species as stable sub-climaxes.
9. Important Species and Succession Associations
| Species | Successional association |
|---|---|
| Saccharum spontaneum | Riverain pioneer on Gangetic alluvium. |
| Tamarix dioica | Riverain pioneer on Gangetic alluvium. |
| Pinus wallichiana | Pioneer forest in temperate Himalayan succession. |
| Shorea robusta | Gangetic alluvial climax community; also cited as an economic sub-climax. |
| Macaranga spp. | Secondary pioneer in moist tropical evergreen clearings. |
| Trema orientalis | Secondary pioneer in moist tropical evergreen clearings. |
| Woodfordia fruticosa | Secondary pioneer in Himalayan hill clearings. |
| Acacia catechu | Early and intermediate riverain stages. |
| Heritiera | Intermediate stages of estuarine succession. |
10. Quick Revision Box — Chapter 4 Complete
- Thoreau (1863): Coined "forest succession".
- Clements (1916): Mono-climax theory and six-step succession mechanism.
- Ecesis: Establishment from germination to reproduction.
- Reaction: Vegetation modifies its own habitat.
- Riverain pioneers: Saccharum spontaneum and Tamarix dioica.
- Conifer pioneer: Pinus wallichiana (Kail).
- Secondary pioneers: Macaranga and Trema in tropical evergreen clearings; Woodfordia in hill clearings.
- Mono-climax: One climatic climax.
- Poly-climax: Multiple climaxes due to soil, relief and drainage.
- Mosaic theory: Dynamic forest patches.
- Whittaker: Climax pattern along environmental gradients.
- Disclimax: Maintained by persistent biotic interference.
- Commercial sub-climaxes: Sal, Teak and Deodar are cited in relation to disturbance management.
11. Interactive MCQ Quiz
15 questions. Tap an option to see the correct answer and explanation straight away, then go to the next question.
Chapter 4 (Part 2) | Plant Succession
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