The Risks and Impacts of Deep-Seabed Mining to Marine Ecosystems
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Deep Sea Mining on the Horizon?
May 2014 Home Subscribe Archive Contact Thematic focus: Environmental governance, Resource efficiency Wealth in the Oceans: Deep sea mining on the horizon? 2 The deep ocean, the largest biome on Earth at over 1 000 metres below the surface of the ocean, holds vast quantities of untapped energy resources, precious metals and minerals. Advancements in technology have enabled greater access to these treasures. As a result, deep sea mining is becoming increasingly possible. To date no commercial deep sea mining operation has taken place, but plans to open a deep sea mine have recently been announced. Our ability to anticipate the impacts of mining is limited by the lack of knowledge about deep sea biodiversity, ecosystem complexity, and the extent of environmental BYCC NC and social impacts from mining operations. As such, it is important that policies guiding mineral extraction from the deep seas are rooted into adaptive management – allowing for the integration of new scientific information alongside advances in technology. Governance mechanisms for international waters and the seabed need to be strengthened. The tanley Zimny/Flickr/ precautionary approach should be used to avoid repeating instances of S well-known destructive practices associated with conventional mining. Why is this issue important? Minerals and the metals they contain are an essential component of the modern high-tech world. As global stocks of raw mineral resources continue to dwindle due to increasing material consumption, intense demand for valuable metals has pushed up global prices. The result is that manufacturing industries are now seeking access to previously unattainable mineral deposits in the ocean depths. -
Polymetallic Nodules Are Essential for Food-Web Integrity of a Prospective Deep-Seabed Mining Area in Pacific Abyssal Plains
www.nature.com/scientificreports OPEN Polymetallic nodules are essential for food‑web integrity of a prospective deep‑seabed mining area in Pacifc abyssal plains Tanja Stratmann1,2,3*, Karline Soetaert1, Daniel Kersken4,5 & Dick van Oevelen1 Polymetallic nodule felds provide hard substrate for sessile organisms on the abyssal seafoor between 3000 and 6000 m water depth. Deep‑seabed mining targets these mineral‑rich nodules and will likely modify the consumer‑resource (trophic) and substrate‑providing (non‑trophic) interactions within the abyssal food web. However, the importance of nodules and their associated sessile fauna in supporting food‑web integrity remains unclear. Here, we use seafoor imagery and published literature to develop highly‑resolved trophic and non‑trophic interaction webs for the Clarion‑Clipperton Fracture Zone (CCZ, central Pacifc Ocean) and the Peru Basin (PB, South‑East Pacifc Ocean) and to assess how nodule removal may modify these networks. The CCZ interaction web included 1028 compartments connected with 59,793 links and the PB interaction web consisted of 342 compartments and 8044 links. We show that knock‑down efects of nodule removal resulted in a 17.9% (CCZ) to 20.8% (PB) loss of all taxa and 22.8% (PB) to 30.6% (CCZ) loss of network links. Subsequent analysis identifed stalked glass sponges living attached to the nodules as key structural species that supported a high diversity of associated fauna. We conclude that polymetallic nodules are critical for food‑web integrity and that their absence will likely result in reduced local benthic biodiversity. Abyssal plains, the deep seafoor between 3000 and 6000 m water depth, have been relatively untouched by anthropogenic impacts due to their extreme depths and distance from continents 1. -
Deep-Sea Mining: the Basics
A fact sheet from June 2018 NOAA Office of Ocean Exploration and Research Deep-sea Mining: The Basics Overview The deepest parts of the world’s ocean feature ecosystems found nowhere else on Earth. They provide habitat for multitudes of species, many yet to be named. These vast, lightless regions also possess deposits of valuable minerals in rich concentrations. Deep-sea extraction technologies may soon develop to the point where exploration of seabed minerals can give way to active exploitation. The International Seabed Authority (ISA) is charged with formulating and enforcing rules for all seabed mining that takes place in waters beyond national jurisdictions. These rules are now under development. Environmental regulations, liability and financial rules, and oversight and enforcement protocols all must be written and approved within three to five years. Figure 1 Types of Deep-sea Mining Production support vessel Return pipe Riser pipe Cobalt Seafloor massive Polymetallic crusts sulfides nodules Subsurface plumes 800-2,500 from return water meters deep Deposition 1,000-4,000 meters deep 4,000-6,500 meters deep Cobalt-rich Localized plumes Seabed pump Ferromanganeseferromanganese from cutting crusts Seafloor production tool Nodule deposit Massive sulfide deposit Sediment Source: New Zealand Environment Guide © 2018 The Pew Charitable Trusts 2 The legal foundations • The United Nations Convention on the Law of the Sea (UNCLOS). Also known as the Law of the Sea Treaty, UNCLOS is the constitutional document governing mineral exploitation on the roughly 60 percent of the world seabed that lies beyond national jurisdictions. UNCLOS took effect in 1994 upon passage of key enabling amendments designed to spur commercial mining. -
The Mid-Atlantic Ridge Underwater Mountains and Hydrothermal Vent Zones Are Home to Distinctive Species and Valuable Minerals
A fact sheet from Jan 2018 NOAA The Mid-Atlantic Ridge Underwater mountains and hydrothermal vent zones are home to distinctive species and valuable minerals Overview The depths of the Atlantic Ocean are home to fascinating geological features and unusual life forms. The Mid- Atlantic Ridge (MAR) is a massive underwater mountain range, 1,700 to 4,200 meters (1 to 2.6 miles) below sea level, that runs from the Arctic Ocean to the Southern Ocean. It is a hot spot for hydrothermal vents, which provide habitat for unique species that could provide insight into the origins of life on Earth. Hydrothermal vents are fueled by underwater volcanic activity or seafloor spreading, and they spew superheated, mineral-laden water from beneath the ocean floor. As the water cools, minerals precipitate out, forming towers containing copper, gold, silver, and zinc. These minerals are used in electronics such as mobile phones and laptop computers and in cars, appliances, and bridges. Vent ecosystems support unique species, mostly bacteria, that derive their energy from mineral-rich vent waters rather than sunlight. These microbes form thick, nutrient-rich mats along the seafloor that support shrimp, mussels, worms, snails, and fish. The MAR’s vent fields were discovered only in 1985, and scientists expect future expeditions to reveal new vents and species.1 The International Seabed Authority (ISA), which is responsible for managing deep-sea mining and protecting the marine environment from its impacts, has entered into exploration contracts along the MAR with France, Poland, and Russia. Once mining begins, equipment will remove or degrade habitats and create sediment plumes that could smother nearby life, while noise and light could also negatively affect deep-sea species. -
Deep Sea Mining MINERAL EXPLORATION in the PACIFIC
MARCH 2021 Deep sea mining MINERAL EXPLORATION IN THE PACIFIC Overview KEY STATS The Pacific Islands are already producers of transition minerals, including copper, cobalt and nickel, mined onshore in Papua New Guinea, Fiji and 2 New Caledonia. But the real opportunity to dramatically expand transition 1.5M+ km in the Pacific and Indian mineral production is offshore, in the deep sea. This opportunity comes oceans set aside for with significant human rights risks. mineral exploration In the last decade, companies and governments have increasingly pursued exploration of the deep sea, where minerals essential to renewable energy technology may be found in large quantities. Copper, nickel, cobalt, lithium, manganese and rare earth elements (REEs) are all mineral exploration found on or below the Pacific seabed; none have yet been commercially contracts awarded mined. Given the current geographic concentration of some of these 30 to 21 companies minerals, companies and governments are eager to expand production to new geographies to diversify supply chains and guard against disruption. Exploration has begun in earnest, with more than 1.5 million squared kilometers in the Pacific and Indian oceans already set aside for mineral exploration, an area nearly the size of Mongolia. However, Indigenous groups and civil society organisations have raised 18/30 contracts are held by companied from: concerns about the potential for human rights abuse associated with seabed mining, including the potential destruction of Indigenous China S. Korea cultures and livelihoods and irreparable environmental damage to France India sensitive and critical ecosystems, including potential impacts on ocean biodiversity and sensitive food chains. -
4. a Growth Model for Polymetallic Nodules
A GEOLOGICAL MODEL OF POLYMETALLIC NODULE DEPOSITS IN THE CLARION‐CLIPPERTON FRACTURE ZONE ISA TECHNICAL STUDY SERIES Technical Study No. 1 Global Non‐Living Resources on the Extended Continental Shelf: Prospects at the year 2000 Technical Study No. 2 Polymetallic Massive Sulphides and Cobalt‐Rich Ferromanganese Crusts: Status and Prospects Technical Study No. 3 Biodiversity, Species Ranges and Gene Flow in the Abyssal Pacific Nodule Province: Predicting and Managing the Impacts of Deep Seabed Mining Technical Study No. 4 Issues associated with the Implementation of Article 82 of the United Nations Convention on the Law of the Sea Technical Study No. 5 Non‐Living resources of the Continental Shelf beyond 200 nautical miles: Speculations on the Implementation of Article 82 of the United Nations Convention on the Law of the Sea PAGE | II A GEOLOGICAL MODEL OF POLYMETALLIC NODULE DEPOSITS IN THE CLARION‐ CLIPPERTON FRACTURE ZONE This report contains a summary of two documents – A Geological Model of Polymetallic Nodule Deposits in the Clarion‐Clipperton Fracture Zone and a Prospector’s Guide prepared under the project ‘Development of a Geological Model of Polymetallic Nodule Deposits in the Clarion‐Clipperton Fracture Zone, Pacific Ocean’. ISA TECHNICAL STUDY: NO. 6 International Seabed Authority Kingston, Jamaica PAGE | III The designation employed and the presentation of materials in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the International Seabed Authority concerning the legal status of any country or territory or of its authorities, or concerning the delimitation of its frontiers or maritime boundaries. All rights reserved. -
Seabed Mapping: a Brief History from Meaningful Words
geosciences Review Seabed Mapping: A Brief History from Meaningful Words Pedro Smith Menandro and Alex Cardoso Bastos * Marine Geosciences Lab (Labogeo), Departmento Oceanografia, Universidade Federal do Espírito Santo, Vitória-ES 29075-910, Brazil; [email protected] * Correspondence: [email protected] Received: 19 May 2020; Accepted: 7 July 2020; Published: 16 July 2020 Abstract: Over the last few centuries, mapping the ocean seabed has been a major challenge for marine geoscientists. Knowledge of seabed bathymetry and morphology has significantly impacted our understanding of our planet dynamics. The history and scientific trends of seabed mapping can be assessed by data mining prior studies. Here, we have mined the scientific literature using the keyword “seabed mapping” to investigate and provide the evolution of mapping methods and emphasize the main trends and challenges over the last 90 years. An increase in related scientific production was observed in the beginning of the 1970s, together with an increased interest in new mapping technologies. The last two decades have revealed major shift in ocean mapping. Besides the range of applications for seabed mapping, terms like habitat mapping and concepts of seabed classification and backscatter began to appear. This follows the trend of investments in research, science, and technology but is mainly related to national and international demands regarding defining that country’s exclusive economic zone, the interest in marine mineral and renewable energy resources, the need for spatial planning, and the scientific challenge of understanding climate variability. The future of seabed mapping brings high expectations, considering that this is one of the main research and development themes for the United Nations Decade of the Oceans. -
Intern Report
Insights from abyssal lebensspuren Jennifer Durden, University of Southampton, UK Mentors: Ken Smith, Jr., Christine Huffard, Katherine Dunlop Summer 2014 Keywords: lebensspuren, traces, abyss, megafauna, deposit-feeding, benthos, sediment ABSTRACT The seasonal input of food to the abyss impacts the benthic community, and changes to that temporal cycle, through changes to the climate and surface ocean conditions impact the benthic assemblage. Most of the benthic fauna are deposit feeders, and many leave traces (‘lebensspuren’) of their activity in the sediment. These traces provide an avenue for examining the temporal variations in the activity of these animals, with insights into the usage of food inputs to the system. Traces of a variety of functions were identified in photographs captured in 2011 and 2012 from Station M, a soft-sedimented abyssal site in the northeast Pacific. Lebensspuren creation, holothurian tracking, and lebensspuren duration were estimated from hourly time-lapse images, while trace densities, diversity and seabed coverage were assessed from photographs captured with a seabed- transiting vehicle. The creation rates and duration of traces on the seabed appeared to vary over time, and may have been related to food supply, as may tracking rates of holothurians. The density, diversity and seabed coverage by lebensspuren of different types varied with food supply, with different lag times for POC flux and salp coverage. These are interpreted to be due to selectivity of 1 deposit feeders, and different response times between trace creators. These variations shed light on the usage of food inputs to the abyss. INTRODUCTION Deep-sea benthic communities rely on a seasonal food supply of detritus from the surface ocean (Billett et al., 1983, Rice et al., 1986). -
Where Are They Seeking to Mine First? Much of the Deep Ocean Floor Is Composed of Vast, Flat, Sediment- Covered Areas Called Abyssal Plains
Deep-sea mining: fact sheet 4 Deep-sea mining: where are they seeking to mine first? Much of the deep ocean floor is composed of vast, flat, sediment- covered areas called abyssal plains. Extensive deposits of manganese or polymetallic nodules have been found on the abyssal plains of the Eastern Pacific Ocean between Mexico and Hawaii. The nodules are of commercial interest The ISA has already granted 16 contracts to because they contain cobalt, copper, nickel and explore for metals across more than a million manganese, which have precipitated around square kilometers of the CCZ. Some of the fish bones, teeth and other small objects over contractors want to start mining the nodules. millions of years. These metals are in demand (See map 'Clarion Clipperton Fracture Zone' on to build batteries, electronic equipment and page 2.) renewable energy technologies. The largest deposits of nodules found to Clarion Clipperton Fracture Zone date lie at depths of four to six kilometers in Research expeditions have continuously an area called the Clarion Clipperton Fracture identified new species in this area, leading marine Zone (CCZ), in the eastern Pacific Ocean scientists to speculate that the vast majority of Below:octopod hanging between Mexico and Hawaii. This is the area life there has yet to be discovered. They believe underneath her brood of of the seabed where the International Seabed that the CCZ may be one of the most biologically 30 eggs, 2–2.7cm-long, Authority (ISA), which regulates deep-sea diverse areas of deep sea on the planet. each individually attached mining in all marine areas outside national Major research projects, such as the JPI to the sponge stalk. -
Worksheets on Climate Change: Sea Level Rise
EDUCATION FOR SUSTAINABLE DEVELOPMENT WORKSHEETS ON CLIMATE CHANGE Sea level rise Consequences for coastal and lowland areas: Bangladesh and the Netherlands Sea level rise – Consequences for coastal and lowland areas: Bangladesh and the Netherlands © Germanwatch 2014 Sea level rise Consequences for coastal and lowland areas: Bangladesh and the Netherlands As a consequence of the anthropogenic greenhouse effect A comparison of the two countries, the Netherlands and the scientific community predicts an increase in average Bangladesh, both of which are potentially very much jeop- global temperature and resulting sea level rise. Heated ardised by sea level rise, clearly illustrates the likely im- water, however, expands only slowly because of the heat pacts for humans and the environment, but also shows transfer from the atmosphere to the sea. For this reason, how different the capacities of individual countries are the sea responds to climate change like a slow-to-react concerning their ability to adapt and to protect them- monster – slow but persistent. In the 20th century the selves from the consequences. Bangladesh, one of the sea level already rose by an average of 12 to 22 cm. The poorest and at the same time most densely populated Intergovernmental Panel on Climate Change (IPCC) con- countries in the world, is also one of the countries which cludes that, as a result of climate change, by 2100 the rise will be most affected by the expected sea level rise. in sea levels could increase worldwide by up to almost 1 metre compared to the mean sea level in the years Flooding has already caused damage up to 100 km inland 1986–2005. -
Polymetallic Nodules Are Essential for Food-Web Integrity of a Prospective
bioRxiv preprint doi: https://doi.org/10.1101/2021.02.11.430718; this version posted February 12, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Polymetallic nodules are essential for food-web integrity of a prospective 2 deep-seabed mining area in Pacific abyssal plains 3 4 Tanja Stratmann1,2,3, Karline Soetaert1, Daniel Kersken4,5, Dick van Oevelen1 5 1 Department of Estuarine and Delta Systems, NIOZ Royal Netherlands Institute for Sea 6 Research, P.O. Box 140, 4400 AC Yerseke, The Netherlands. 7 2 Department of Earth Sciences, Utrecht University, Vening Meineszgebouw A, Princetonlaan 8 8a, 3584 CB Utrecht, The Netherlands. 9 3 HGF MPG Joint Research Group for Deep-Sea Ecology and Technology, Max Planck Institute 10 for Marine Microbiology, Celsiusstraße 1, 28359 Bremen, Germany. 11 4 German Centre for Marine Biodiversity Research (DZMB), Senckenberg am Meer, Südstrand 12 44, 26382 Wilhelmshaven, Germany. 13 5 Marine Zoology, Senckenberg Research Institute and Nature Museum, Senckenberganlage 25, 14 60325 Frankfurt am Main, Germany. 15 16 *corresponding author: Tanja Stratmann, [email protected] 17 18 Keywords: binary food web, DISCOL, anthropogenic impact, interaction matrix 19 20 Abstract 21 Polymetallic nodule fields provide hard substrate for sessile organisms on the abyssal seafloor 22 between 3,000 and 6,000 m water depth. Deep-seabed mining targets these mineral-rich nodules 23 and will likely modify the consumer-resource (trophic) and substrate-providing (non-trophic) 24 interactions within the abyssal food web. -
International Seabed Authority the Eighth Session of the International
International Seabed Authority The eighth session of the International Seabed Authority was held at Kingston, Jamaica, from 5 to 16 August 2002. Among the most important substantive matters discussed by the Authority during the session were the first set of annual reports of the seven contractors for exploration for polymetallic nodules and future regulations for prospecting and exploration for polymetallic sulphides and cobalt-rich ferromanganese crusts. The eighth session also included a one-day seminar, open to all members and observers, on the prospects for hydrothermal polymetallic sulphides and cobalt-rich ferromanganese crusts in the Area. The seminar consisted of presentations by marine geologists and biologists of the latest findings about these resources and their environment and was intended to provide participants with background information on the status and characteristics of deep sea polymetallic sulphides and cobalt-rich ferromanganese crusts as well as information on the marine environment where these minerals are located. The essential problem for the Authority is that many of the same hydrothermal vent sites that are being targeted by scientific researchers and bioprospectors are also of considerable interest to prospective seabed miners. There is therefore considerable overlap, as well as potential for conflict, between the Authority’s responsibilities in respect of the marine environment and activities directed at bioprospecting. The papers presented at the seminar have been published by the Authority as a technical study. Most of the substantive work during the eighth session was carried out by the Legal and Technical Commission. In pursuance of the supervisory functions of the Authority with respect to contracts for exploration, the Commission made an evaluation of the first set of annual reports submitted by the contractors in accordance with the Authority’s regulations for prospecting and exploration for polymetallic nodules in the Area.