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NCERT Exemplar · Q34

Q.What could be the reason for the faster rate of decomposition in the tropics?

Sikkim CbseShort· 2mImportance★★★★★
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The faster rate of decomposition in the tropics is driven primarily by the region’s consistently high temperatures and abundant moisture, which together create ideal conditions for the decomposer organisms to work at maximum efficiency.

Decomposition is the natural process by which dead organic matter — leaves, wood, animal remains — is broken down into simpler substances, releasing nutrients back into the soil. This process is not a single event but a chain of physical and chemical changes carried out by a host of organisms: bacteria, fungi, earthworms, termites, and other detritivores. The speed at which this happens depends heavily on the environment, and the tropics stand out as the fastest zone on Earth.

The key reason lies in two climatic factors that the NCERT textbook emphasises: temperature and moisture. In the tropics, both are present in abundance throughout the year. High temperatures — typically above 20°C even in the coolest months — accelerate the metabolic rates of decomposer microbes. For every 10°C rise in temperature, the rate of enzymatic reactions in these organisms roughly doubles, a principle known as the Q₁₀ effect. This means that a warm tropical forest floor is a chemical factory running at full speed, while a cold temperate forest floor in winter is nearly dormant.

Moisture is equally critical. Decomposers need water to survive and to transport enzymes and dissolved nutrients. The tropics receive heavy and reliable rainfall, keeping the soil and leaf litter consistently moist. In contrast, deserts or cold regions where water is frozen or scarce see decomposition grind to a halt. The combination of warmth and wetness in the tropics creates a near-ideal environment where decomposer populations are large, diverse, and active year-round.

Note

This is why tropical rainforests, despite having the highest plant growth on Earth, often have surprisingly thin layers of leaf litter on the forest floor. Dead leaves are broken down so quickly that they rarely accumulate, unlike in temperate forests where a thick carpet of decaying leaves builds up over years. …

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