Page 21 - climate-change2013
P. 21

Photo: J.Hall-Spencer
                                                         abundance and productivity (Hall-Spencer et al., 2008;
                                                         Suggett et al., 2012). P. oceanica is, on the other hand,
                                                         highly sensitive to seawater warming, and high mortality
                                                         rates may be expected in natural populations with the
                                                         rise in annual water temperature.

                                                         Effects of sea-level rise


                                                         As seen above, the rise in sea-level is generally consid-
                                                         ered one of the most significant consequences of cli-
                                                         mate warming, yet its effects on biodiversity are poorly
                                                         understood.

               Observed effects on the endemic coral Cladocora   Sea-level rise threatens coastal marshes, sea caves
               caespitosa polyps with marks of dissolution of   and beaches, which are crucial habitats for many spe-
               their skeleton under low pH conditions.   cies, such as endangered populations of sea turtles and
                                                         Mediterranean monk seals, which use them for breeding
                                                         (see page 24). Intertidal bioconstructions such as reefs
          in Mediterranean benthic ecosystems. The natural CO    built by vermetid molluscs together with coralline algae
                                                    2
          emissions from these vents provide a range of pH levels   (such as the vermetid Dendropoma petraeum and the
          that can be used to monitor what benthic ecosystems   red alga  Neogoniolithon brassica-florida) or rims built
          will be like in a high-CO  scenario. These studies have   slightly above sea-level by the encrusting coralline alga
                            2
          shown that nearby rocky shore communities exposed   Lithophyllum byssoides are extremely vulnerable to
          to low-pH waters decrease in species number and shift   water-level changes and to wave erosion during major
          from a calcareous-dominated community structure to   storms (Boudouresque, 2004). Vermetid reefs are found
          one dominated by uncalcified organisms (Hall-Spencer   mostly in the central and southern Mediterranean Sea
          et al., 2008). For example, around the Vulcano vents of   while rims are widely distributed throughout the Mediter-
          Italy, a macroalgae-dominated community decreased   ranean (Chemello and Silenzi, 2011) and have been used
          in species richness, coverage and reproduction capac-  to track past changes in sea-level in the Mediterranean.
          ity in a low-pH environment. Likewise, the abundance   As these habitats are built from calcium carbonate, sea
          of various calcareous organisms such as scleractinian   acidification can also affect vermetid and algal calcifi-
          corals (Cladocora caespitosa and Balanophyllia euro-  cation and have detrimental effects on the organisms’
          paea), macroalgae (Lithophyllum incrustans,  Corallina   growth rate, resulting in local extinction events.
          elongata,  Padina pavonica and  Halimeda tuna), mol-
          luscs (Osilinus turbinatus,  Patella caerulea and  Hexa-  Rising sea temperature, sea-level rise and acidity thus
          plex trunculus) and sea-urchins (Paracentrotus lividus   appear to be associated with various changes in bio-
          and Arbacia lixula) was lower under low-pH/more acidic   diversity in the Mediterranean (Rodolfo-Metalpa et al.,
         conditions (Hall-Spencer et al., 2008; Rodolfo-Metalpa   2010). The synergic effects of different stressors linked
         et al., 2011).                                  to global change will probably exacerbate the impact on
                                                         the biodiversity and functioning of coastal ecosystems.
         Aquarium experiments and transplants in the field into
         naturally acidified waters have confirmed some of the
         observed  negative  effects  of  acidification.  For  exam-
         ple, for the scleractinian corals  Cladocora caespitosa
         and the alien  Oculina patagonica,  low-pH conditions
         reduced calcification rates by about 30% (Movilla et
         al., 2012). Similarly, other species such as the red coral
         Corallium rubrum and the coralline alga  Lithophyl-
         lum cabiochae displayed a significant reduction (by
         up to 60%) in skeleton growth and feeding activity or
         increased necrosis, respectively, in a low-pH environ-
         ment. These and other findings suggest that rich coral-
         ligenous communities are likely to be severely affected
         by the ongoing acidification. Ocean acidification has
         also been shown to have an impact on shellfish growth,
         reproduction and structure.
         In contrast, a number of species seem to be resistant to
         or even to benefit from acidification. For instance, Posi-
         donia oceanica meadows seem remarkably tolerant of
         low pH levels and several algal species, among them
         some aliens (Caulerpa racemosa, Asparagopsis armata
         and  Dictyota dichotoma), and other species such as
         the sea anemone Anemonia viridis can increase their      Vermetid platforms at Torre Guaceto MPA, Italy. Photo: M. Otero


          MEDITERRANEAN MARINE PROTECTED AREAS AND CLIMATE CHANGE: A GUIDE TO REGIONAL MONITORING AND ADAPTATION OPPORTUNITIES  19
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