Previous Year Question
In case of which one of the following biogeochemical cycles, is the weathering of rocks the main source of release of nutrient to enter the cycle?
Carbon cycle
Nitrogen cycle
Phosphorus cycle
Sulphur cycle
Correct Answer: C
Detailed Solution
In the phosphorus cycle, weathering of rocks is the main source for the release of the nutrient.
The phosphorus cycle is a major sedimentary biogeochemical cycle.
The principal long-term reservoir of phosphorus is not in the atmosphere but in phosphate-bearing rocks of the Earth’s crust and marine sediments.
Physical and chemical weathering of rocks containing phosphate minerals releases inorganic phosphate into soil and water.
Plants absorb dissolved phosphate ions from the soil through their roots.
Phosphorus passes from plants through the food chain to herbivores and then to carnivores.
Excretion by organisms and decomposition of dead plants and animals return phosphate to soil or water.
Phosphate carried by water may reach lakes and oceans and accumulate in the form of sediments.
Over long geological periods, these sediments may form new phosphate rocks.
Tectonic uplift brings these rocks back to the Earth’s surface, and the process of weathering begins again.
The phosphorus cycle does not have a significant natural gaseous phase.
Due to the absence of a gaseous phase, the phosphorus cycle is comparatively slower than the carbon or nitrogen cycle.
The carbon cycle is not the correct answer.
The principal active reservoirs of carbon occur in the atmosphere, oceans, biosphere and soil.
Carbon dioxide enters the biosphere through photosynthesis.
Respiration, decomposition, combustion and ocean-atmosphere gas exchange are major processes of the carbon cycle.
Weathering of rocks affects the carbon cycle, but it is not the main source through which carbon enters the cycle.
The nitrogen cycle is not the correct answer.
The largest reservoir of nitrogen is the atmosphere, which contains approximately 78% nitrogen gas.
Most organisms cannot directly use atmospheric N₂.
Biological nitrogen fixation, lightning and industrial fixation convert N₂ into useful nitrogen compounds.
Therefore, weathering of rocks is not the main source of the nutrient in the nitrogen cycle.
The sulphur cycle is not the correct answer.
Sulphur occurs in rocks and sediments, and weathering can release sulphate.
However, volcanic emissions, sea spray, biological decomposition and the combustion of fossil fuels are also important sources of sulphur.
The sulphur cycle also includes gaseous compounds such as sulphur dioxide and hydrogen sulphide.
Therefore, among the given options, the cycle most directly dependent upon rock weathering is the phosphorus cycle.
Biological importance of phosphorus
Phosphorus is a component of the phosphate backbone in DNA and RNA.
It is necessary for the storage and transfer of energy in ATP.
It is an important component of cell membranes in the form of phospholipids.
Calcium phosphate provides structure and hardness to bones and teeth.
Phosphorus can be a limiting nutrient in many ecosystems.
Excessive entry of phosphate from fertilisers and sewage into water bodies can accelerate eutrophication.