Question:

Source of calcareous ooze in the sea bottom

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Calcareous oozes cannot accumulate below a certain depth known as the Carbonate Compensation Depth (CCD, typically 4000-5000m), where high pressure and low temperature cause calcium carbonate to dissolve completely.
  • Glaciers
  • Precipitation of dissolved nutrients
  • Radiolarians
  • Coccolithophores
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The Correct Option is D

Solution and Explanation

Step 1: Understanding the Concept:
Pelagic sediments covering the deep ocean floor are classified based on their origin.
Biogenic sediments composed of shell remnants are known as oozes.

Step 2: Detailed Explanation:

Pelagic biogenic oozes must contain at least \(30\%\) skeletal remains of microscopic marine organisms. They are divided into:
- Calcareous oozes: Composed of calcium carbonate (\(\text{CaCO}_3\)), primarily derived from the shells of planktonic Foraminifera and Coccolithophores (unicellular marine algae).
- Siliceous oozes: Composed of silica (\(\text{SiO}_2\)), primarily derived from Radiolarians and Diatoms.

Step 3: Final Answer:

The source of calcareous ooze is Coccolithophores, which corresponds to option (D).
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