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Deep‐sea Environmental Disturbance and Recovery Potential
Author(s) -
Thiel Hjalmar
Publication year - 1992
Publication title -
internationale revue der gesamten hydrobiologie und hydrographie
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.524
H-Index - 52
eISSN - 1522-2632
pISSN - 0020-9309
DOI - 10.1002/iroh.19920770213
Subject(s) - deep sea , benthic zone , seabed , abyssal zone , sediment , disturbance (geology) , abyssal plain , substrate (aquarium) , seafloor spreading , environmental science , oceanography , scale (ratio) , ecology , earth science , geology , geography , paleontology , biology , cartography
Mining the abyssal seafloor for manganese nodules will destroy the hard substrate and it will severely disturb the seabed and the benthic soft substrate community. Recolonization will occur from unmined areas. Reestablishment of a community similar to that originally present is, however, not possible, since the nodules will be removed and epigrowth on hard substrates is thereby precluded. Small scale experiments using azoic sediment in trays exposed to ambient deep‐sea conditions, may not be appropriate models for large scale recolonization processes. Results of such experiments and general knowledge of deep‐sea ecology suggest that decades may be required for reestablishment of a balanced community. With respect to evaluation of some ecological consequences of mining an ongoing large scale experiment, termed DISCOL (DIS‐turbance and re‐COL‐onization) is shortly described as a new approach in deep‐sea risk assessment.