he deep-sea floor (below 200 m) is presently, along with Antarctica, the only area on Earth where mineral resources are not currently extracted commercially 1. However, the twenty-first century has seen rising concerns over the depletion of the most readily available and highest-grade ores of selected minerals on land, as well as increasing vulnerabilities to political control over resource access 2-4. Demand for some minerals is also projected to increase, particularly from electrification of the transport sector and renewable energy generation 5-8. A recent Intergovernmental Panel on Climate Change (IPCC) report indicates that 70-85% of all electricity would need to come from renewable sources by 2050 to limit global warming to 1.5 °C 9. These factors, combined with the development of a governance structure for international mineral resources established under the United Nations Convention on the Law of the Sea (UNCLOS) and its 1994 Implementing Agreement, have led to renewed interest in deep-seabed mining 4,10. Many metals occur together at economically interesting concentrations in the deep ocean. These include copper, cobalt, nickel, zinc, silver and gold, as well as lithium and rare-earth elements (Table 1). The metals are found in different ore types in different settings (Fig.