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Deep-Sea Mining Risks: The Environmental and Regulatory Challenge in the Clarion-Clipperton Zone

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New oceanographic studies indicate that sediment plumes from deep-sea mining could travel hundreds of kilometers, threatening vast marine ecosystems. This highlights a critical conflict between the demand for transition minerals and the protection of the global commons under international law.

The Clarion-Clipperton Zone (CCZ), a vast abyssal plain in the Pacific Ocean, has become the focal point of a global debate over deep-sea mining. As the International Seabed Authority (ISA) works toward finalizing a 'Mining Code,' new research suggests that the environmental risks are far more extensive than previously estimated. Specifically, oceanographic models show that sediment plumes—clouds of silt and chemicals stirred up during the extraction of polymetallic nodules—could travel hundreds of kilometers from the mining site. This movement threatens to smother benthic organisms and disrupt the ocean’s delicate carbon cycling processes. Polymetallic nodules are rich in cobalt, nickel, and manganese—minerals essential for the global transition to renewable energy and the production of electric vehicle batteries. However, the deep sea is one of the most stable and least understood environments on Earth. The potential for 'transboundary' environmental damage across international waters challenges the legal principle of the 'Common Heritage of Mankind.' This principle, enshrined in the United Nations Convention on the Law of the Sea (UNCLOS), dictates that the seabed and its resources in international waters belong to all humanity and must be managed for the collective benefit.

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