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Question

The process of "coral bleaching" within the Indian Ocean is most directly linked to:

This question was previously asked in
SSC CGL 2025 Tier 2 Paper 1 Question Paper (19-Jan-2026)
The correct answer is
Anthropogenically induced sea surface temperature increases

Indian Ocean Coral Bleaching Causes

Coral bleaching is a stress response where corals expel the vital symbiotic algae (zooxanthellae) residing in their tissues. This results in the coral turning white and can lead to mortality if stress persists.

Analysis of Potential Causes

  • Anthropogenically induced sea surface temperature increases: Scientific consensus identifies rising sea surface temperatures, largely driven by human activities (anthropogenic factors) like greenhouse gas emissions, as the primary cause of mass coral bleaching events worldwide. Elevated temperatures directly stress the coral-algae symbiosis.
  • Increased deep-sea mining: Deep-sea mining activities can cause localized physical damage and sedimentation, harming marine ecosystems. However, they do not represent the widespread, large-scale stressor responsible for extensive coral bleaching across regions like the Indian Ocean.
  • Increased ocean acidification from river runoff: While ocean acidification, exacerbated by increased atmospheric CO2 absorption and potentially influenced by runoff, poses a long-term threat to coral reef structure, it is not the direct, immediate trigger for the bleaching phenomenon itself. Temperature stress is the more direct cause of bleaching.
  • The effects of increased Arctic ice melt: Melting Arctic ice contributes significantly to global sea-level rise and can alter ocean currents and salinity. While part of broader climate change impacts, its effect is less direct on inducing the specific thermal stress that causes coral bleaching in the Indian Ocean compared to direct ocean warming.

Direct Link Identification

The most significant and direct factor causing coral bleaching within the Indian Ocean, aligning with global patterns, is the increase in sea surface temperatures attributable to human activities.

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