Nash, MerindaUthicke, S.Negri, A.P.Cantin, N.2016-06-141726-4170http://hdl.handle.net/1885/103262There are concerns that Mg-calcite crustose coralline algae (CCA), which are key reef builders on coral reefs, will be most susceptible to increased rates of dissolution under higher pCO<inf>2</inf> and ocean acidification. Due to the higher solubility of Mg-calcite, it has been hypothesised that magnesium concentrations in CCA Mg-calcite will decrease as the ocean acidifies, and that this decrease will make their skeletons more chemically stable. In addition to Mg-calcite, CCA Porolithon onkodes, the predominant encrusting species on tropical reefs, can have dolomite (Ca<inf>0.5</inf>Mg<inf>0.5</inf>CO<inf>3</inf>) infilling cell spaces which increases their stability. However, nothing is known about how bio-mineralised dolomite formation responds to higher pCO<inf>2</inf>. Using P. onkodes grown for 3 and 6 months in tank experiments, we aimed to determine (1) if mol % MgCO<inf>3</inf> in new crust and new settlement was affected by increasing CO<inf>2</inf> levels (365, 444, 676 and 904 μatm), (2) whether bio-mineralised dolomite formed within these time frames, and (3) if so, whether this was effected by CO<inf>2</inf>. Our results show that there was no significant effect of CO<inf>2</inf> on mol % MgCO<inf>3</inf> in any sample set, indicating an absence of a plastic response under a wide range of experimental conditions. Dolomite within the CCA cells formed within 3 months and dolomite abundance did not vary significantly with CO<inf>2</inf> treatment. While evidence mounts that climate change will impact many sensitive coral and CCA species, the results from this study indicate that reef-building P. onkodes will continue to form stabilising dolomite infill under near-future acidification conditions, thereby retaining its higher resistance to dissolution.201510.5194/bg-12-5247-20152016-06-14