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      Biotic and Human Vulnerability to Projected Changes in Ocean Biogeochemistry over the 21st Century

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          Abstract

          Mora and colleagues show that ongoing greenhouse gas emissions are likely to have a considerable effect on several biogeochemical properties of the world's oceans, with potentially serious consequences for biodiversity and human welfare.

          Abstract

          Ongoing greenhouse gas emissions can modify climate processes and induce shifts in ocean temperature, pH, oxygen concentration, and productivity, which in turn could alter biological and social systems. Here, we provide a synoptic global assessment of the simultaneous changes in future ocean biogeochemical variables over marine biota and their broader implications for people. We analyzed modern Earth System Models forced by greenhouse gas concentration pathways until 2100 and showed that the entire world's ocean surface will be simultaneously impacted by varying intensities of ocean warming, acidification, oxygen depletion, or shortfalls in productivity. In contrast, only a small fraction of the world's ocean surface, mostly in polar regions, will experience increased oxygenation and productivity, while almost nowhere will there be ocean cooling or pH elevation. We compiled the global distribution of 32 marine habitats and biodiversity hotspots and found that they would all experience simultaneous exposure to changes in multiple biogeochemical variables. This superposition highlights the high risk for synergistic ecosystem responses, the suite of physiological adaptations needed to cope with future climate change, and the potential for reorganization of global biodiversity patterns. If co-occurring biogeochemical changes influence the delivery of ocean goods and services, then they could also have a considerable effect on human welfare. Approximately 470 to 870 million of the poorest people in the world rely heavily on the ocean for food, jobs, and revenues and live in countries that will be most affected by simultaneous changes in ocean biogeochemistry. These results highlight the high risk of degradation of marine ecosystems and associated human hardship expected in a future following current trends in anthropogenic greenhouse gas emissions.

          Author Summary

          Climate change caused by human activity could damage biological and social systems. Here we gathered climate, biological, and socioeconomic data to describe some of the events by which ocean biogeochemical changes triggered by ongoing greenhouse gas emissions could cascade through marine habitats and organisms, eventually influencing humans. Our results suggest that the entire world's ocean surface will be simultaneously impacted by varying intensities of ocean warming, acidification, oxygen depletion, or shortfalls in productivity. Only a very small fraction of the oceans, mostly in polar regions, will face the opposing effects of increases in oxygen or productivity, and almost nowhere will there be cooling or pH increase. The biological responses to such biogeochemical changes could be considerable since marine habitats and hotspots for several marine taxa will be simultaneously exposed to biogeochemical changes known to be deleterious. The social ramifications are also likely to be massive and challenging as some 470 to 870 million people – who can least afford dramatic changes to their livelihoods – live in areas where ocean goods and services could be compromised by substantial changes in ocean biogeochemistry. These results underline the need for urgent mitigation of greenhouse gas emissions if degradation of marine ecosystems and associated human hardship are to be prevented.

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          Most cited references23

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          Ecology. Physiology and climate change.

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            Climate change affects marine fishes through the oxygen limitation of thermal tolerance.

            A cause-and-effect understanding of climate influences on ecosystems requires evaluation of thermal limits of member species and of their ability to cope with changing temperatures. Laboratory data available for marine fish and invertebrates from various climatic regions led to the hypothesis that, as a unifying principle, a mismatch between the demand for oxygen and the capacity of oxygen supply to tissues is the first mechanism to restrict whole-animal tolerance to thermal extremes. We show in the eelpout, Zoarces viviparus, a bioindicator fish species for environmental monitoring from North and Baltic Seas (Helcom), that thermally limited oxygen delivery closely matches environmental temperatures beyond which growth performance and abundance decrease. Decrements in aerobic performance in warming seas will thus be the first process to cause extinction or relocation to cooler waters.
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              Meta-analysis reveals negative yet variable effects of ocean acidification on marine organisms.

              Ocean acidification is a pervasive stressor that could affect many marine organisms and cause profound ecological shifts. A variety of biological responses to ocean acidification have been measured across a range of taxa, but this information exists as case studies and has not been synthesized into meaningful comparisons amongst response variables and functional groups. We used meta-analytic techniques to explore the biological responses to ocean acidification, and found negative effects on survival, calcification, growth and reproduction. However, there was significant variation in the sensitivity of marine organisms. Calcifying organisms generally exhibited larger negative responses than non-calcifying organisms across numerous response variables, with the exception of crustaceans, which calcify but were not negatively affected. Calcification responses varied significantly amongst organisms using different mineral forms of calcium carbonate. Organisms using one of the more soluble forms of calcium carbonate (high-magnesium calcite) can be more resilient to ocean acidification than less soluble forms (calcite and aragonite). Additionally, there was variation in the sensitivities of different developmental stages, but this variation was dependent on the taxonomic group. Our analyses suggest that the biological effects of ocean acidification are generally large and negative, but the variation in sensitivity amongst organisms has important implications for ecosystem responses. © 2010 Blackwell Publishing Ltd/CNRS.
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                Author and article information

                Contributors
                Role: Academic Editor
                Journal
                PLoS Biol
                PLoS Biol
                plos
                plosbiol
                PLoS Biology
                Public Library of Science (San Francisco, USA )
                1544-9173
                1545-7885
                October 2013
                October 2013
                15 October 2013
                : 11
                : 10
                : e1001682
                Affiliations
                [1 ]Department of Geography, University of Hawaii, Honolulu, Hawaii, United States of America
                [2 ]Ocean Science Centre, Memorial University of Newfoundland, St. John's, Newfoundland, Canada
                [3 ]Pacific Islands Fisheries Science Center, Honolulu, Hawaii, United States of America
                [4 ]Norwegian Institute for Water Research, Bergen, Norway
                [5 ]Florida State University, Tallahassee, Florida, United States of America
                [6 ]National Oceanography Centre, University of Southampton Waterfront Campus, Southampton, United Kingdom
                [7 ]Institut Pierre Simon Laplace/Laboratoire des Sciences du Climat et de l'Environnement, Centre National de la Recherche Scientifique, Gif sur Yvette, France
                [8 ]The Centre for Australian Weather and Climate Research, Commonwealth Scientific and Industrial Research Organisation Marine and Atmospheric Research, Aspendale, Victoria, Australia
                [9 ]Department of Life and Environmental Sciences, Polytechnic University of Marche, Ancona, Italy
                [10 ]Center for Marine Biodiversity and Conservation, Scripps Institution of Oceanography, La Jolla, California, United States of America
                [11 ]Met Office Hadley Centre, Exeter, United Kingdom
                [12 ]College of Life and Environmental Sciences, University of Exeter, Exeter, United Kingdom
                [13 ]Marine Biology Research Group, Biology Department, Ghent University, Ghent, Belgium
                [14 ]Plymouth Marine Laboratory, Plymouth, United Kingdom
                [15 ]Meteorological Research Institute, Tsukuba, Japan
                [16 ]Norwegian Institute for Water Research, Oslo, Norway
                [17 ]Institut de Ciències Marines, Consejo Superior de Investigaciones Científicas, Barcelona, Spain
                [18 ]Department of Biology, University of Massachusetts, Boston, Massachusetts, United States of America
                [19 ]Department of Oceanography, University of Hawaii at Manoa, Hawaii, United States of America
                [20 ]International Research Institute of Stavanger, Thormøhlensgate, Bergen, Norway
                [21 ]College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, Oregon, United States of America
                [22 ]Uni Climate, Uni Research, Bergen, Norway
                [23 ]Department of Biology, University of Hawaii at Manoa, Hawaii, United States of America
                [24 ]Centro de innovacion Fundacion In-nova Castilla La Mancha, Madrid, Spain
                [25 ]Beijing Climate Center, China Meteorological Administration, Beijing, China
                [26 ]School of Biological Sciences, Swire Institute of Marine Science, and Department of Earth Sciences, University of Hong Kong, Hong Kong, China
                University College London, United Kingdom
                Author notes

                The authors have declared that no competing interests exist.

                The author(s) have made the following declarations about their contributions: Conceived and designed the experiments: CM CLW AR TA ARB DB LB QC MC RD AJG BMG PRH JI DOBJ LAL HN KN ERL MR HAR CRS AKS ART JFT PU LW TW MY. Performed the experiments: CM AR. Analyzed the data: CM QC CLW. Wrote the paper: CM CLW AR TA ARB DB LB QC MC RD AJG BMG PRH JI DOBJ LAL HN KN ERL MR HAR CRS AKS ART JFT PU LW TW MY.

                Article
                PBIOLOGY-D-13-01193
                10.1371/journal.pbio.1001682
                3797030
                24143135
                522c203c-a45c-4ee0-9570-e8929f699534
                Copyright @ 2013

                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
                : 26 March 2013
                : 3 September 2013
                Page count
                Pages: 14
                Funding
                This study was funded by the University of Hawaii Sea Grant ( http://seagrant.soest.hawaii.edu/). We thank the Norwegian Research Council ( www.forskningsradet.no/en/) for funding a workshop on Climate Change Stress on Deep-Sea Benthic Ecosystems (CLIDEEP), the Sloan Foundation through the Census of Marine Life Program ( www.coml.org) and the Total Foundation ( http://foundation.total.com/) for funding several meetings as part of the International Network for Scientific Investigations of Deep-Sea Ecosystems ( INDEEP, www.indeep-project.org) and the First Global Synthesis of Biodiversity, Biogeography and Ecosystem Function in the Deep Sea (SYNDEEP) that led to the idea of this paper. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
                Categories
                Research Article

                Life sciences
                Life sciences

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