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      Man and the Last Great Wilderness: Human Impact on the Deep Sea

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          Abstract

          The deep sea, the largest ecosystem on Earth and one of the least studied, harbours high biodiversity and provides a wealth of resources. Although humans have used the oceans for millennia, technological developments now allow exploitation of fisheries resources, hydrocarbons and minerals below 2000 m depth. The remoteness of the deep seafloor has promoted the disposal of residues and litter. Ocean acidification and climate change now bring a new dimension of global effects. Thus the challenges facing the deep sea are large and accelerating, providing a new imperative for the science community, industry and national and international organizations to work together to develop successful exploitation management and conservation of the deep-sea ecosystem. This paper provides scientific expert judgement and a semi-quantitative analysis of past, present and future impacts of human-related activities on global deep-sea habitats within three categories: disposal, exploitation and climate change. The analysis is the result of a Census of Marine Life – SYNDEEP workshop (September 2008). A detailed review of known impacts and their effects is provided. The analysis shows how, in recent decades, the most significant anthropogenic activities that affect the deep sea have evolved from mainly disposal (past) to exploitation (present). We predict that from now and into the future, increases in atmospheric CO 2 and facets and consequences of climate change will have the most impact on deep-sea habitats and their fauna. Synergies between different anthropogenic pressures and associated effects are discussed, indicating that most synergies are related to increased atmospheric CO 2 and climate change effects. We identify deep-sea ecosystems we believe are at higher risk from human impacts in the near future: benthic communities on sedimentary upper slopes, cold-water corals, canyon benthic communities and seamount pelagic and benthic communities. We finalise this review with a short discussion on protection and management methods.

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          Most cited references363

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          Ecology. Physiology and climate change.

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            Volcanic carbon dioxide vents show ecosystem effects of ocean acidification.

            The atmospheric partial pressure of carbon dioxide (p(CO(2))) will almost certainly be double that of pre-industrial levels by 2100 and will be considerably higher than at any time during the past few million years. The oceans are a principal sink for anthropogenic CO(2) where it is estimated to have caused a 30% increase in the concentration of H(+) in ocean surface waters since the early 1900s and may lead to a drop in seawater pH of up to 0.5 units by 2100 (refs 2, 3). Our understanding of how increased ocean acidity may affect marine ecosystems is at present very limited as almost all studies have been in vitro, short-term, rapid perturbation experiments on isolated elements of the ecosystem. Here we show the effects of acidification on benthic ecosystems at shallow coastal sites where volcanic CO(2) vents lower the pH of the water column. Along gradients of normal pH (8.1-8.2) to lowered pH (mean 7.8-7.9, minimum 7.4-7.5), typical rocky shore communities with abundant calcareous organisms shifted to communities lacking scleractinian corals with significant reductions in sea urchin and coralline algal abundance. To our knowledge, this is the first ecosystem-scale validation of predictions that these important groups of organisms are susceptible to elevated amounts of p(CO(2)). Sea-grass production was highest in an area at mean pH 7.6 (1,827 (mu)atm p(CO(2))) where coralline algal biomass was significantly reduced and gastropod shells were dissolving due to periods of carbonate sub-saturation. The species populating the vent sites comprise a suite of organisms that are resilient to naturally high concentrations of p(CO(2)) and indicate that ocean acidification may benefit highly invasive non-native algal species. Our results provide the first in situ insights into how shallow water marine communities might change when susceptible organisms are removed owing to ocean acidification.
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              Submarine thermal sprirngs on the galapagos rift.

              The submarine hydrothermal activity on and near the Galápagos Rift has been explored with the aid of the deep submersible Alvin. Analyses of water samples from hydrothermal vents reveal that hydrothermal activity provides significant or dominant sources and sinks for several components of seawater; studies of conductive and convective heat transfer suggest that two-thirds of the heat lost from new oceanic lithosphere at the Galápagos Rift in the first million years may be vented from thermal springs, predominantly along the axial ridge within the rift valley. The vent areas are populated by animal communities. They appear to utilize chemosynthesis by sulfur-oxidizing bacteria to derive their entire energy supply from reactions between the seawater and the rocks at high temperatures, rather than photosynthesis.
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                Author and article information

                Contributors
                Role: Editor
                Journal
                PLoS One
                plos
                plosone
                PLoS ONE
                Public Library of Science (San Francisco, USA )
                1932-6203
                2011
                1 August 2011
                12 August 2011
                : 6
                : 8
                : e22588
                Affiliations
                [1 ]Institut de Ciències del Mar, Consejo Superior de Investigaciones Científicas, Barcelona, Spain
                [2 ]School of Ocean and Earth Science, University of Southampton, National Oceanography Centre Southampton, Southampton, United Kingdom
                [3 ]Institute of Marine Research, Flødevigen, Norway
                [4 ]National Institute of Water and Atmospheric Research, Wellington, New Zealand
                [5 ]Universidad Nacional Autónoma de México, Instituto de Ciencias del Mar y Limnología, México, D.F., Mexico
                [6 ]Integrative Oceanography Division, Scripps Institution of Oceanography, La Jolla, California, United States of America
                [7 ]Ifremer, Brest, DEEP/LEP, Plouzane, France
                [8 ]Department of Oceanography, University of Hawaii, Honolulu, Hawaii, United States of America
                [9 ]Division of Marine Science and Conservation, Nicholas School of the Environment, Duke University, Beaufort, North Carolina, United States of America
                California Academy of Sciences, United States of America
                Author notes

                Conceived and designed the experiments: ERL PAT MCB OAB MRC EE LAL LM AAR CRS CLVD. Wrote the paper: ERL PAT MCB OAB MRC EE LAL LM AAR CRS CLVD.

                Article
                PONE-D-10-05097
                10.1371/journal.pone.0022588
                3148232
                21829635
                8d647c45-f0a2-485e-a808-1b46a49ae3de
                Ramirez-Llodra et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
                History
                : 22 November 2010
                : 30 June 2011
                Page count
                Pages: 25
                Categories
                Review
                Biology
                Ecology
                Biodiversity
                Biogeography
                Environmental Protection
                Marine Ecology
                Marine Biology
                Fisheries Science
                Marine Conservation
                Marine Ecology
                Marine Monitoring
                Science Policy
                Research Assessment
                Science Education

                Uncategorized
                Uncategorized

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