ClassApna

Class 12 Biology Notes

Ecosystem Class 12 Notes

Complete revision notes for NCERT Class 12 Biology Chapter 12 — ecosystem structure and components, productivity and energy flow, the 10% (Lindeman) law, ecological pyramids, decomposition, carbon and nitrogen cycles, ecological succession and the services ecosystems provide.

Class12SubjectBiologyCoversCBSE · NEET

Written byDeep Narayan· Science & Mathematics EducatorReviewed byPushpanjali

What is an ecosystem in one line?

An ecosystem is a functional unit of nature where living organisms (biotic) interact with each other and with non-living components (abiotic) through the flow of energy and the cycling of matter.

Ecosystem Structure and Components

Ecosystem

A functional unit of ecology that includes both abiotic (non-living) and biotic (living) components interacting through energy flow and nutrient cycling. Each ecosystem has two major structural parts: abiotic factors and biotic communities.

  • Abiotic components — physical factors like temperature, water, light, soil and air.
  • Producers (autotrophs) — plants, algae and some bacteria that fix energy via photosynthesis; the base of every ecosystem.
  • Consumers (heterotrophs) — herbivores (primary), carnivores (secondary and tertiary) that eat producers or other consumers.
  • Decomposers — bacteria and fungi that break down dead organic matter and return nutrients to the soil (saprophytes).
  • Examples of ecosystems: forest, grassland, pond, marine and desert; man-made ones include croplands and aquariums.

Role of decomposers

Decomposers are essential but often overlooked: they complete nutrient cycling by mineralising dead organic matter, making nutrients available to producers again.

Productivity — GPP, NPP and R

Gross Primary Productivity (GPP)

The rate at which producers capture solar energy and convert it into chemical energy (biomass) by photosynthesis. It is the total primary production before any losses to respiration.

Net Primary Productivity (NPP)

NPP=GPPRNPP = GPP - R

The amount of energy or biomass left after the producer's own respiration (R) is subtracted from GPP. It is the energy actually available to consumers and decomposers — the net gain stored by the ecosystem.

  • Secondary productivity is the rate at which consumers convert ingested food into their own biomass.
  • NPP is highest in tropical rainforests (about 2.2 kg C m⁻² yr⁻¹) and lowest in deserts and deep seas.
  • Productivity can be measured as kilocalories, biomass or carbon fixed per unit area per unit time.

Exam preference

Remember the relationship NPP = GPP − R. A common MCQ asks which productivity is available to consumers — the answer is always NPP.

Energy Flow and the 10% Law

Energy flows through an ecosystem in a single direction — from the sun into producers, then to consumers — and is never recycled. The producers capture solar energy that enters the ecosystem, but this energy does not flow back to the sun and cannot be reused because energy is lost as heat at each step.

Lindeman's 10% law

Only about 10% of the energy available at one trophic level is transferred to the next level; the rest is lost as heat in respiration, in undigested food and in non-predatory death. This is why food chains have few trophic levels.

  • Food chain — a linear sequence: grass → grasshopper → frog → snake → hawk.
  • Food web — many interconnected food chains in an ecosystem; a web is more stable than a single chain.
  • Trophic levels — the positions an organism occupies in a food chain (producer, primary consumer, etc.).
  • Detritus food chain starts with dead organic matter (detritivores and decomposers); grazing food chain starts with green plants.

Ecological Pyramids

Ecological pyramid

A graphical representation of the number, biomass or energy at successive trophic levels. The base is the producer level and the apex is the top carnivore.

  • Pyramid of numbers — usually upright, but inverted in some cases (e.g. a single tree supporting many herbivore insects).
  • Pyramid of biomass — upright in most terrestrial ecosystems, but inverted in the sea where a large mass of phytoplankton supports smaller zooplankton and fish.
  • Pyramid of energy — always upright, because energy decreases at each successive trophic level and can never be greater than the level below.

Energy pyramid is never inverted

Only the energy pyramid is always upright. Number and biomass pyramids can be inverted, as with a tree and its many insects, or the phytoplankton–zooplankton sea relationship.

Decomposition

Decomposition

The breakdown of dead organic matter (detritus) into simpler inorganic substances by decomposers — bacteria and fungi. Decomposition releases nutrients back to the soil and is vital for nutrient cycling.

  • Fragmentation — detritus is broken into smaller pieces by detritivores such as earthworms.
  • Leaching — water-soluble inorganic nutrients drain into the soil (downward).
  • Catabolism — fungi and bacteria digest detritus and release inorganic substances; enzymes break down complex molecules.
  • Humification — accumulation of a dark coloured, amorphous humus layer that is resistant to further microbial action.
  • Mineralisation — the release of inorganic minerals (e.g. nitrates, phosphates) from the humus.

Conditions that speed decomposition

Decomposition is faster in warm, moist conditions with good oxygen and aeration, and slower at low temperatures and in waterlogged or acidic conditions.

Nutrient Cycling

Nutrient cycle (biogeochemical cycle)

The movement of nutrients between the biotic (organisms) and abiotic (soil, air, water) components of an ecosystem. Carbon and nitrogen cycle mostly through the atmosphere (gaseous cycles); phosphorus cycles mainly through sediments (sedimentary cycle).

  • Carbon cycle — carbon moves between the atmosphere (CO₂), producers (photosynthesis) and consumers, and returns via respiration, decomposition and combustion.
  • Nitrogen cycle — nitrogen fixation (by Rhizobium, Azotobacter, cyanobacteria), nitrification (Nitrosomonas, Nitrobacter), assimilation, ammonification and denitrification (Pseudomonas).
  • Phosphorus cycle — a sedimentary cycle; phosphorus moves through rocks, soil, water and organisms, with no atmospheric phase, so it is slower and can limit productivity.

Gaseous vs sedimentary

Carbon and nitrogen are gaseous cycles because their reservoirs are in the atmosphere; phosphorus is a sedimentary cycle because its reservoir is in rocks. This is a frequent distinction question.

Ecological Succession and Ecosystem Services

Ecological succession

The gradual, directional and predictable change in the species composition of a community over time, ending in a stable climax community that is in equilibrium with the local environment.

  • Primary succession — starts from bare rock or barren land with no soil (e.g. a newly exposed lava or glacier), taking very long to form soil.
  • Secondary succession — starts where soil already exists (e.g. after a forest fire or abandoned farmland) and is faster than primary succession.
  • Hydrarch succession — begins in water (ponds, marshes) and leads to a terrestrial climax.
  • Xerarch succession — begins in dry, bare conditions (e.g. bare rock or sand) and leads to a terrestrial climax.
  • Seral stages — the intermediate communities in succession; the final stable community is the climax community.

Ecosystem services are the benefits humans receive from ecosystems — purification of air and water, nutrient cycling, crop pollination, climate regulation and the prevention of soil erosion. These services have enormous economic value and underscore why ecosystems must be conserved.

Hydrarch vs xerarch

Notice both hydrarch and xerarch reach the same kind of climax — a terrestrial community — but they start from aquatic (hydrarch) and dry/rocky (xerarch) beginnings respectively.

Solved Examples

Example: An ecosystem has a Gross Primary Productivity (GPP) of 10,000 kcal/m²/year and respiration (R) of 3,000 kcal/m²/year. What is its Net Primary Productivity (NPP), and what does it mean?

Solution: NPP = GPP − R = 10,000 − 3,000 = 7,000 kcal/m²/year. This is the energy stored by producers after their own respiration, and it is the amount actually available to consumers and decomposers in the ecosystem.

Example: If a producer stores 10,000 kcal and the 10% law applies, how much energy reaches the third trophic level?

Solution: Only 10% transfers at each step. Primary consumer receives 10% of 10,000 = 1,000 kcal; secondary (third trophic level) receives 10% of 1,000 = 100 kcal. This rapid loss explains why food chains are short and why the energy pyramid is always upright.

Revision

Key formulas at a glance

Memorise these before attempting numericals — most exam questions hinge on one of them.

Net Primary Productivity

NPP=GPPRNPP = GPP - R

Lindeman's 10% law

energy transferred=10% of previous level\text{energy transferred} = 10\%\ \text{of previous level}

Photosynthesis energy capture

R=GPPNPPR = GPP - NPP

Trophic energy loss

energy at level n+1=0.1×energy at level n\text{energy at level } n+1 = 0.1 \times \text{energy at level } n

Food chain

grassgrasshopperfrogsnakehawk\text{grass} \to \text{grasshopper} \to \text{frog} \to \text{snake} \to \text{hawk}

Succession types

hydrarch (water)climax; xerarch (dry)climax\text{hydrarch (water)} \to \text{climax; } \text{xerarch (dry)} \to \text{climax}

Carbon fixation

CO2+H2O    carbohydrate+O2\text{CO}_2 + H_2O \;\to\; \text{carbohydrate} + O_2

Exam tips

How this chapter is asked

Where this topic appears in CBSE, JEE Main and NEET papers.

  • NPP = GPP − R; NPP is what consumers receive.
  • Energy flows one direction and is recycled nowhere; matter is cycled.
  • Lindeman's 10% law — only 10% transfers per trophic level.
  • Energy pyramid is always upright; number and biomass pyramids can be inverted.
  • Decomposition steps: fragmentation, leaching, catabolism, humification, mineralisation.
  • Carbon and nitrogen are gaseous cycles; phosphorus is sedimentary.
  • Primary succession starts on bare rock; secondary starts where soil exists.
  • Hydrarch starts in water, xerarch in dry land; both end in a terrestrial climax.

FAQ

Common questions

What is the difference between GPP, NPP and secondary productivity?

GPP is the total energy producers capture through photosynthesis. NPP is GPP minus the producer's own respiration (NPP = GPP − R) and is available to consumers. Secondary productivity is the rate at which consumers convert ingested food into their own biomass.

Why is the 10% law important and why are food chains short?

Only about 10% of energy transfers to the next trophic level, the rest being lost as heat. Because this loss is so rapid, little energy remains after a few levels, so food chains generally have only 3–4 trophic levels.

What are the steps of decomposition?

The five steps are fragmentation (breaking detritus into pieces), leaching (draining of soluble nutrients), catabolism (enzymatic digestion by bacteria and fungi), humification (forming resistant humus) and mineralisation (releasing inorganic minerals).

What is primary vs secondary succession?

Primary succession begins on bare rock or land with no soil and takes very long (e.g. after lava or glacial retreat). Secondary succession begins where soil already exists, such as after a forest fire or abandoned farmland, and completes much faster.

Mastering this chapter with live help

Notes help, but doubts clear fastest in a live class. Narayan Gurukul Academy (ClassApna) runs small-batch CBSE, JEE and NEET coaching from our Mohali centre and online — with daily doubt support and mock tests.

One-on-one guidance available · Live online classes across India