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                               Dr Jean-Pierre Gattuso
                               CNRS Research Director and President of the Monegasque
                               Association on Ocean Acidification (AMAO)


                                                                            Unfortunately, species such as corals and
                                                                            gorgonians are attached to the seabed and cannot
                                                                            move. Their larvae are not attached to the seabed,
                                                                            but move very slowly. Excessively high temperatures
                                                                            have already caused large-scale mortality within
                                                                            certain corals, such as the Great Barrier Reef
                                                                            in Australia where two thirds were affected by
                                                                            bleaching in 2016 and 2017.

                                                                            How does acidification affect oceans?
                                                                            Acidity levels have already risen by 34% in the past
                                                                            two centuries. Increased sea water acidity has
                               Why is the ocean at the heart of the climate   reduced carbonates which are an essential building
                               regulation system?                           block in generating calcareous skeletons and shells.
                               The carbon dioxide which we emit into the    Acidification, therefore, is impacting many organisms
                               atmosphere increases the greenhouse effect and   with calcareous skeletons and shells, such as
                               generates heat. The ocean stores more than 90%   oysters and corals.
                               of this excess heat, and in doing so, limits air
                               warming. It also stores a quarter of carbon dioxide
                               emissions, which is 26 million tonnes of CO  per day.
                                                                 2
                               This also limits global warming. Lastly, the ocean
                               receives almost all the global ice-melt water. Sea-
                               water warming and acidification, including
                               increasing sea water levels, create mainly
                               negative consequences.

                               How can the ocean be
                               a global warming victim?                                            RISING SEA LEVELS
                                                                                                     +0,2m since 1900
                               Sea-water warming causes                                              +0,3 to 1m in 2100
                               massive migrations,
                               large-scale mortality
                               and the demise of
                               certain species. We                                                  GLOBAL WARMING
                               have witnessed impressive                                              +0,5°C since 1971
                               species migrations of several                                         +0,6 to 2°C in 2100
                               hundred kilometres per
                               decade. This is the case, for
                               example, for tropical species
                               which tend to migrate to cooler                                             ACIDITY
                               waters. The balance in biodiversity                                    +30% since 1900
                               is disrupted and creates a predicted                                    +150% in 2100
                               weakening in the tropics and an
                               increase in the polar regions.
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