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      No recovery of a large-scale anthropogenic sediment disturbance on the Pacific seafloor after 77 years at 6460 m depth

      , ,
      Marine Pollution Bulletin
      Elsevier BV

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          Alternative stable states in ecology

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            Is Open Access

            Threatened by mining, polymetallic nodules are required to preserve abyssal epifauna

            Polymetallic nodule mining at abyssal depths in the Clarion Clipperton Fracture Zone (Eastern Central Pacific) will impact one of the most remote and least known environments on Earth. Since vast areas are being targeted by concession holders for future mining, large-scale effects of these activities are expected. Hence, insight into the fauna associated with nodules is crucial to support effective environmental management. In this study video surveys were used to compare the epifauna from sites with contrasting nodule coverage in four license areas. Results showed that epifaunal densities are more than two times higher at dense nodule coverage (>25 versus ≤10 individuals per 100 m2), and that taxa such as alcyonacean and antipatharian corals are virtually absent from nodule-free areas. Furthermore, surveys conducted along tracks from trawling or experimental mining simulations up to 37 years old, suggest that the removal of epifauna is almost complete and that its full recovery is slow. By highlighting the importance of nodules for the epifaunal biodiversity of this abyssal area, we urge for cautious consideration of the criteria for determining future preservation zones.
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              Deep impact: the rising toll of fishing in the deep sea

              C Roberts (2002)
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                Author and article information

                Journal
                Marine Pollution Bulletin
                Marine Pollution Bulletin
                Elsevier BV
                0025326X
                February 2022
                February 2022
                : 175
                : 113374
                Article
                10.1016/j.marpolbul.2022.113374
                881e4cb4-da08-41d5-b40a-e83f9a7c843d
                © 2022

                https://www.elsevier.com/tdm/userlicense/1.0/

                https://doi.org/10.15223/policy-017

                https://doi.org/10.15223/policy-037

                https://doi.org/10.15223/policy-012

                https://doi.org/10.15223/policy-029

                https://doi.org/10.15223/policy-004

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