Ostensibly, the deep sea seems to be nothing more than this faraway, effectively irrelevant realm - a place surely too dark, too cold, and too deep to hold any ecological or societal significance. However, though once thought to be completely devoid of life, the deep sea is actually host to biodiversity among the highest on the planet, with over 30,000 known organisms spanning a wide range of phyla (Ramirez-Llodra et al. 2010, World Register of Deep-Sea species 2025). Furthermore, the deep sea, defined as the whole open ocean and seabed below 200 meters, is extremely vast, with a surface area estimated to cover well over 50% of Earth's surface (Paulus 2021). The deep sea is the most expansive environment on Earth. In this way, the deep sea, as opposed to the terrestrial land we humans inhabit, is the ecological norm on Earth.
The deep sea can be characterized by: 1) darkness and coldness, being defined by the depth beyond which sunlight can reach in the ocean; 2) extreme food limitation, with a general reliance on marine snow, or detritus, sinking from waters above for energy; and 3) high biodiversity, with highly specialized organisms, adaptations, and organismal interactions wholly unique to life in the deep sea (Ramirez-Llodra et al. 2010).
There are many different types of environments within the deep sea, each with their own unique geological features, organisms, and minerals. Among the most significant are abyssal plains, seamounts, and hydrothermal vents. Abyssal plains account for the greatest area by far in the deep sea, covering over 50% of Earth's surface (Smith et al. 2008). They can be characterized by cold waters and slow ocean currents, biogenetic sediment, extremely limited food access, and the presence of polymetallic nodules. Within abyssal plains, detrital aggregates (aka 'clumps' of fallen detritus from spring algal blooms in higher waters) and whale falls (aka dead whales that have sunk to the ocean floor) can cause spontaneous, opportunistic species to evolve, diversify, and proliferate dramatically, effectively creating highly unique, localized ecosystems from the sudden, concentrated food source (Paulus 2021). Seamounts are underwater volcanoes, and can be characterized by strong upwelling and hydrodynamics. The unique structure and geology of seamounts allows for extremely high biodiversity, including specialized deep-sea corals, benthic filter-feeders, fishes, and even turtles and marine mammals (Morato et al. 2010). Hydrothermal vents are described as chemically unique, superheated water penetrating deep into the Earth's crust being ejected upwards. This enables wholly unique ecosystems with highly specialized organisms around chemosynthesis, a biological process that converts inorganic compounds like hydrogen sulfide or methane (as opposed to sunlight) into food (Paulus 2021).
Every night, billions of zooplankton, fish, squid, and other midwater organisms travel from the deep sea up to the surface to feed, then return to the depths for safety by morning. This cycle of diel vertical migration supports the pelagic food web, which directly sustains the seafood that we rely on both economically and biotically (Le & Sato).
When surface-dwelling organisms like phytoplankton die or produce waste, some of this organic material sinks to the deep ocean. The biological pump transports carbon from the ocean surface all the way to the deep sea, where microbes and scavengers consume it, storing the carbon in deep sea sediments for centuries to millennia (Agusti et al. 2015). This process is particularly significant in light of anthropogenic climate change.
Deep sea sediments can capture and isolate pollutants like heavy metals and organic toxins, preventing them from circulating in surface waters. Furthermore, certain deep sea microbes are capable of breaking down hydrocarbons, playing a critical role in natural bioremediation (Siscar et al. 2014).
While the exploitation of these minerals has not yet begun, the deep sea is host to high quantities of precious metal deposits, including nickel, cobalt, copper, manganese, and rare earth elements (Paulus 2021). These are key materials for developing and producing electronics, renewable energy, and military technologies.
Like the rest of the ocean, deep sea ecosystems are already vulnerable to well-known impacts of climate change, including ocean acidification and warming. However, they're also at risk of an additional, particularly severe threat: disruption from deep sea mining.
Deep sea mining would seek to exploit three particular forms of precious metals: sulfide deposits found at hydrothermal vents, cobalt-rich ferromanganese crusts from seamounts, and, most significantly, manganese nodules found on abyssal plains. These deposits include metals such as nickel, cobalt, copper, manganese, and rare earth elements, which could be used to produce electronics and technology.
Deep sea mining involves deploying large, remote-controlled machines to collect these nodules scattered across abyssal plains. These machines are designed to scoop or vacuum the nodules, along with surrounding sediments and organismal by-catch, and pump the slurry up to a surface vessel through riser pipes. Onboard, the nodules would be separated from water and sediment, and excess seabed material would be indiscriminately discharged into the mid-ocean, creating widespread sediment plumes that can impair deep sea and mid-ocean life alike (including commercial fisheries), disrupting life-sustaining, necessary ecological processes, and inundating the open ocean with excess carbon.
Deep sea mining threatens one of the most fragile and least understood ecosystems on Earth, hosting unique and often endemic species that have evolved over millennia (Simon-Lledó et al. 2019). Mining operations can crush or bury these organisms and irreversibly alter their habitats. Recovery, if it happens at all, would take centuries, if not longer.
Wastewater and sediment plumes from mining could spread toxic heavy metals and fine particulates over vast areas, smothering life and contaminating feeding grounds for filter feeders and other benthic organisms (van der Grient and Drazen 2022). These pollutants could ascend the food chain, inevitably affecting commercial fisheries and human health.
Mining operations introduce artificial light and intense mechanical noise into otherwise dark, quiet environments, affecting species that rely on darkness and acoustic signals for navigation, communication, and survival. These disturbances ripple outward through food webs and may have unpredictable consequences on biodiversity.
Mining activities, both the collection and discharge processes, will disturb deep sea sediment layers and the open ocean, releasing stored carbon and methane back into the water column and atmosphere. This could greatly exacerbate ocean acidification and global climate change in unpredictable ways at a time when mitigation is already urgent.
The United Nations Convention on the Law of the Sea of 10 December 1982 (UNCLOS) is the international treaty that governs all aspects of the world's oceans and seas. Essentially, UNCLOS serves as the international "Constitution for the Oceans," defining the legal framework for nations' rights and responsibilities of all ocean activities, and establishing rules for activities like navigation, resource exploitation, and environmental protection. This includes regulations on deep sea exploration and mining.
On January 29, 1982, President Reagan gave a statement on the United States' participation in UNCLOS. Notably, he said that the United States will not participate, specifically citing necessary revisions to Part XI of UNCLOS that "will not deter development of any deep seabed mineral resources to meet national and world demand" (Reagan 1982). That's to say, since the very beginning of international efforts to regulate deep sea mining, the United States has refused to formally comply explicitly because of concerns regarding rights to deep sea mining.
The United States did NOT sign the convention in 1982, and, despite the particular effort of President George W. Bush to "urge the Senate to act favorably on U.S. accession to the United Nations Convention on the Law of the Sea" (Bush 2007), the United States has never ratified UNCLOS, maintaining autonomy to regulate deep sea mining within its exclusive economic zone (EEZ) AND in international waters.
The International Seabed Authority (ISA), established under UNCLOS, is the primary international regulatory body for activities related to the common heritage of humankind in the Area (defined as the seabed under the high seas) beyond national jurisdiction. This includes protecting the marine environment from harmful effects of deep-sea activities, promoting and regulating scientific exploration, and weighing the social benefits with environmental risks of mining efforts (Lodge 2017). So far, the ISA has not finalized regulations for commercial-scale seabed extraction, effectively preventing international deep sea exploitation efforts from proceeding (Ackerman 2025). Regardless of the United States' historical compliance, the United States has never been legally bound to the rules and regulations established by the ISA.
On April 24, 2025, President Donald J. Trump signed the executive order titled "Unleashing America's Offshore Critical Minerals and Resources". The following day, April 25, 2025, the National Oceanic and Atmospheric Administration (NOAA) published an article (featured below) in support of the executive order, citing the Deep Seabed Hard Mineral Act (DSHMRA) to justify the agency's authority to review applications and issue licensure for United States entities to explore and commercially exploit deep sea resources in international waters.
DSHMRA, enacted in 1980, is a law established in the United States that allows US citizens to explore and recover hard mineral resources from the deep seabed beyond national jurisdiction. It's intended to serve as an interim measure, designed to be a temporary framework until a global agreement is agreed to (such as the now-established UNCLOS).
President Trump’s Deep Seabed Executive Order, which aims to expand the United States' access to deep sea mining opportunities beyond national jurisdiction, carries significant political, ethical, and ecological implications. Politically, the order asserts unilateral United States interests in international waters, undermining multilateral governance frameworks like UNCLOS and the ISA, despite a history of compliance. Furthermore, President Trump outright cites the necessity to "counter China’s growing influence over seabed mineral resources" among his primary reasons to expedite deep sea mining by United States entities. Ethically, it challenges global norms around the equitable use of the common heritage of mankind, as it blatantly prioritizes national gain over shared stewardship of ocean resources. Ecologically, deep sea mining poses major risks to fragile and largely unexplored marine ecosystems, including the potential loss of biodiversity and irreversible damage to habitats critical to ocean health and climate regulation. The order exemplifies the tension between short-term independent resource exploitation, and long-term planetary sustainability and international goodwill.
Sources
Ackerman, D. (2025, March 28). The world has no rulebook for deep-sea mining. One company is pushing forward anyway. NPR. https://www.npr.org/2025/03/27/nx-s1-5336319/international-deep-sea-mining-critical-metals-seabed
Agusti, S., González-Gordillo, J. I., Vaqué, D., Estrada, M., Cerezo, M. I., Salazar, G., Gasol, J. M., & Duarte, C. M. (2015). Ubiquitous healthy diatoms in the deep sea confirm deep carbon injection by the biological pump. Nature Communications, 6(1), 7608–7608. https://doi.org/10.1038/ncomms8608
Bush, G. W. (2007, May 15). President’s Statement on Advancing U.S. Interests in the World’s Oceans. The White House: President George W. Bush Archives. https://georgewbush-whitehouse.archives.gov/news/releases/2007/05/20070515-2.html
Le, J. T., & Sato, K. N. (n.d.). Ecosystem Services of the Deep Ocean. Ocean-Climate.Org.
Lodge, M. (2017, May 16). The International Seabed Authority and Deep Seabed Mining. United Nations; United Nations. https://www.un.org/en/chronicle/article/international-seabed-authority-and-deep-seabed-mining
Morato, T., Hoyle, S. D., Allain, V., & Nicol, S. J. (2010). Seamounts are hotspots of pelagic biodiversity in the open ocean. Proceedings of the National Academy of Sciences, 107(21), 9707–9711. https://doi.org/10.1073/pnas.0910290107
Paulus, E. (2021). Shedding Light on Deep-Sea Biodiversity—A Highly Vulnerable Habitat in the Face of Anthropogenic Change. Frontiers in Marine Science, 8. https://doi.org/10.3389/fmars.2021.667048
Ramirez-Llodra, E., Brandt, A., Danovaro, R., De Mol, B., Escobar, E., German, C. R., Levin, L. A., Martinez Arbizu, P., Menot, L., Buhl-Mortensen, P., Narayanaswamy, B. E., Smith, C. R., Tittensor, D. P., Tyler, P. A., Vanreusel, A., & Vecchione, M. (2010). Deep, diverse and definitely different: Unique attributes of the world’s largest ecosystem. Biogeosciences, 7(9), 2851–2899. https://doi.org/10.5194/bg-7-2851-2010
Reagan, R. (1982, January 29). Statement on United States Participation in the Third United Nations Conference on the Law of the Sea. Ronald Reagan Presidential Library & Museum. https://www.reaganlibrary.gov/archives/speech/statement-united-states-participation-third-united-nations-conference-law-sea
Siscar, R., Koenig, S., Torreblanca, A., & Solé, M. (2014). The role of metallothionein and selenium in metal detoxification in the liver of deep-sea fish from the NW Mediterranean Sea. The Science of the Total Environment, 466–467, 898–905. https://doi.org/10.1016/j.scitotenv.2013.07.081
Simon-Lledó, E., Bett, B. J., Huvenne, V. A. I., Köser, K., Schoening, T., Greinert, J., & Jones, D. O. B. (2019). Biological effects 26 years after simulated deep-sea mining. Scientific Reports, 9(1), 8040. https://doi.org/10.1038/s41598-019-44492-w
Smith, C. R., De Leo, F. C., Bernardino, A. F., Sweetman, A. K., & Arbizu, P. M. (2008). Abyssal food limitation, ecosystem structure and climate change. Trends in Ecology & Evolution, 23(9), 518–528. https://doi.org/10.1016/j.tree.2008.05.002
Thiel, H., Schriever, G., Ahnert, A., Bluhm, H., Borowski, C., & Vopel, K. (2001). The large-scale environmental impact experiment DISCOL—reflection and foresight. Deep Sea Research Part II: Topical Studies in Oceanography, 48(17), 3869–3882. https://doi.org/10.1016/S0967-0645(01)00071-6
van der Grient, J. M. A., & Drazen, J. C. (2022). Evaluating deep-sea communities’ susceptibility to mining plumes using shallow-water data. Science of The Total Environment, 852, 158162. https://doi.org/10.1016/j.scitotenv.2022.158162
World Register of Deep-Sea species. (2025). Marinespecies.org. https://www.marinespecies.org/deepsea/aphia.php?p=browser&id%5B%5D=2