Abstract

Ulva is the dominant genus in the green tide events and is considered to have efficient CO2 concentrating mechanisms (CCMs). However, little is understood regarding the impacts of ocean acidification on the CCMs of Ulva and the consequences of thalli’s acclimation to ocean acidification in terms of responding to environmental factors. Here, we grew a cosmopolitan green alga, Ulva linza at ambient (LC) and elevated (HC) CO2 levels and investigated the alteration of CCMs in U. linza grown at HC and its responses to the changed seawater carbon chemistry and light intensity. The inhibitors experiment for photosynthetic inorganic carbon utilization demonstrated that acidic compartments, extracellular carbonic anhydrase (CA) and intracellular CA worked together in the thalli grown at LC and the acquisition of exogenous carbon source in the thalli could be attributed to the collaboration of acidic compartments and extracellular CA. Contrastingly, when U. linza was grown at HC, extracellular CA was completely inhibited, acidic compartments and intracellular CA were also down-regulated to different extents and thus the acquisition of exogenous carbon source solely relied on acidic compartments. The down-regulated CCMs in U. linza did not affect its responses to changes of seawater carbon chemistry but led to a decrease of net photosynthetic rate when thalli were exposed to increased light intensity. This decrease could be attributed to photodamage caused by the combination of the saved energy due to the down-regulated CCMs and high light intensity. Our findings suggest future ocean acidification might impose depressing effects on green tide events when combined with increased light exposure.

Highlights

  • MethodsThalli of U. linza were collected from the coastal water of Lianyungang (119.3 ̊E, 34.5 ̊N), Jiangsu province of China in April 2013

  • Due largely to burning fossil fuel and change of net land use, the carbon dioxide level in the air has increased by 40% since 1750 [1]

  • AZ, and EZ inhibited the net photosynthetic rate of thalli grown at LC, which means that acidic compartments, external and internal carbonic anhydrase (CA) work together in the thalli grown in natural seawater medium and the acquisition of exogenous carbon in the thalli may be achieved by the collaboration of acidic compartments and external CA

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Summary

Methods

Thalli of U. linza were collected from the coastal water of Lianyungang (119.3 ̊E, 34.5 ̊N), Jiangsu province of China in April 2013. The natural temperature and salinity in the seawater were 12 ̊C and 31 respectively. The thalli were transported to the lab in a cooling box (4–6 ̊C) within one hour and washed gently with 0.2 μm filtered seawater to remove any sediment, epiphytes or small grazers. The concentrations of nitrate and phosphate in natural seawater were 20 and 2 μM respectively and the artificial addition of nitrate and phosphate was to avoid the limit of nutrients during the laboratory culture. The light conditions were set as 100 μmol photons m-2 s-1 (light/dark 12:12 h) and the temperature was set as 12 ̊C, in accordance with where U. linza was found in its natural conditions. The culture lasted three weeks and five replicates were conducted under each treatment. Three weeks should be enough for thalli to acclimatise to the condition of ocean acidification

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