Syllabus topics (RTMNU)
- Ecology: Definition, Branches and significance of ecology
- Climatic factors: Atmospheric (Gaseous composition), Effect of light and temperature on vegetation
- Edaphic factors: Pedogenesis, soil profile, physical and chemical properties of soil
- Biogeochemical cycles: Carbon cycle, Nitrogen cycle and Phosphorous cycle
Ecology: Definition, Branches and Significance
Definition: Ecology is the study of the relationships of living organisms with each other and with their environment. The term "Oekologie" was coined by Ernst Haeckel (1866) — from Greek oikos (house) + logos (study). Indian ecology owes much to Prof. R. Misra, the "father of Indian ecology".
Branches:
- Autecology: ecology of a single species or individual in relation to its environment.
- Synecology: ecology of groups — communities and ecosystems.
- Habitat-based: freshwater, marine, terrestrial, forest, grassland ecology.
- Applied: population ecology, community ecology, ecosystem ecology, conservation ecology, pollution ecology, human ecology, palaeoecology.
Significance: helps in conservation of biodiversity and natural resources; pollution control; forest, grassland and wildlife management; agriculture (crop–weed–pest relations); understanding climate change; environmental impact assessment; land-use planning.
Climatic Factors: Atmosphere (Gaseous Composition)
The atmosphere is the gaseous layer around the earth. Composition of dry air by volume: nitrogen about 78%, oxygen about 21%, argon about 0.93%, carbon dioxide about 0.04%, and traces of neon, helium, methane, ozone, hydrogen; plus variable water vapour and dust.
- O2 — for respiration of all organisms.
- CO2 — raw material of photosynthesis; greenhouse gas that keeps earth warm; its rise causes global warming.
- N2 — fixed by microbes into usable nitrogen.
- Ozone in the stratosphere absorbs harmful UV rays.
- Water vapour — humidity, rainfall, affects transpiration.
Effect of Light and Temperature on Vegetation
Light (intensity, quality, duration):
- Photosynthesis depends on light intensity and red/blue wavelengths.
- Heliophytes (sun plants) vs sciophytes (shade plants) — differ in leaf thickness, chlorophyll and stomata.
- Photoperiodism: day length controls flowering (SDP, LDP).
- Phototropism and germination (some seeds need light, e.g. lettuce).
- Very high light causes solarisation (destruction of chlorophyll) and higher transpiration.
- Layering (stratification) of forest vegetation depends on light.
Temperature:
- Controls rates of enzyme activity, photosynthesis, respiration and transpiration.
- Each plant has cardinal temperatures — minimum, optimum, maximum.
- Determines distribution of vegetation — tropical, temperate, alpine zones (Raunkiaer's and Köppen's classifications use it).
- Vernalisation: low temperature promotes flowering in some plants (e.g. winter wheat).
- Extremes cause injury — frost injury, chilling, heat injury and desiccation.
- Plants classed as megatherms, mesotherms, microtherms, hekistotherms by temperature need.
Edaphic Factors: Pedogenesis and Soil Profile
Edaphic factors are soil-related factors affecting plants.
Pedogenesis (soil formation): (1) Weathering of parent rock — physical (temperature change, frost, wind, water), chemical (hydration, oxidation, carbonation, solution) and biological (lichens, roots, microbes) — forms regolith. (2) Humification — decomposition of dead organic matter into humus. (3) Mineralisation — release of inorganic nutrients. (4) Eluviation (washing down of materials) and illuviation (deposition in lower layers) produce horizons. Factors: climate, parent material, organisms, topography and time.
Soil profile: a vertical section of soil showing layers (horizons).
| Horizon | Name | Features |
|---|---|---|
| O | Organic horizon | Fresh litter (O1) and partly decomposed matter/humus (O2) |
| A | Topsoil (zone of eluviation) | Dark, rich in humus, roots and microbes |
| B | Subsoil (zone of illuviation) | Accumulated clay, iron and aluminium oxides |
| C | Weathered parent material | Partly broken rock, little life |
| R | Bedrock | Unweathered parent rock |
Physical and Chemical Properties of Soil
Physical: (1) Texture — proportion of sand (2–0.02 mm), silt and clay (< 0.002 mm); loam is best for plants. (2) Structure — arrangement of particles into crumbs/aggregates. (3) Porosity — pore space for air and water. (4) Water holding capacity — high in clay, low in sand; forms of soil water: gravitational, capillary (available to plants), hygroscopic. (5) Soil air and temperature. (6) Colour — black soils of Vidarbha (regur) are rich in clay and good for cotton.
Chemical: (1) Soil pH — acidic, neutral, alkaline; most crops prefer 6–7.5. (2) Mineral nutrients — macro (N, P, K, Ca, Mg, S) and micro (Fe, Zn, Cu, Mn, B, Mo). (3) Cation exchange capacity — ability of clay–humus to hold cations. (4) Organic matter/humus — improves fertility. (5) Salinity and alkalinity.
Biogeochemical Cycles: Carbon, Nitrogen and Phosphorus Cycles
Biogeochemical cycle: circulation of elements between living organisms and the non-living environment (air, water, rocks).
Carbon cycle (gaseous): CO2 of air → fixed by photosynthesis into organic matter → passes along food chains → returned as CO2 by respiration of plants, animals and decomposers. Some carbon gets locked as fossil fuels and limestone; returned by burning and weathering. Oceans dissolve large amounts of CO2. Human activities (fossil fuels, deforestation) increase atmospheric CO2.
Nitrogen cycle (gaseous):
- Nitrogen fixation: N2 → NH3 by Rhizobium (in legume nodules), Azotobacter, Nostoc, Anabaena; also by lightning and industry (Haber process).
- Assimilation: plants absorb NH4+/NO3− and form proteins.
- Ammonification: decomposers convert dead protein to NH3.
- Nitrification: NH3 → NO2− (Nitrosomonas) → NO3− (Nitrobacter).
- Denitrification: NO3− → N2 (Pseudomonas, Thiobacillus denitrificans).
Phosphorus cycle (sedimentary — no gaseous phase): phosphate rocks weather → phosphate in soil and water → absorbed by plants → animals → returned by decomposition of dead bodies and excreta; some lost to ocean sediments and returns only over geological time (uplift); guano and fertilisers add phosphate. Phosphate is often a limiting nutrient; runoff causes eutrophication.
Likely exam questions
- (Long, 8 marks) Define ecology. Describe the effect of light and temperature on vegetation.
- (Long, 8 marks) What are edaphic factors? Explain pedogenesis, soil profile and the physical and chemical properties of soil.
- (Short, 4 marks) Explain the nitrogen cycle.
- (Short, 4 marks) Write the gaseous composition of the atmosphere.
- (Short, 4 marks) Why is the phosphorus cycle called a sedimentary cycle?