The ocean is a substantial sink for atmospheric carbon dioxide (CO2) released as a result of human activities. Over the coming decades the dissolved inorganic C concentration in the surface ocean is predicted to increase, which is expected to have a direct influence on the efficiency of C utilization (consumption and production) by phytoplankton during photosynthesis. Here, we evaluated the generality of C‐rich organic matter production by examining the elemental C:N ratio of organic matter produced under conditions of varying pCO2.
Full report, as presented by the Youth for the SDGs scholars, of the Arctic voyage on Peace Boat from 24th May to 14th June. Ms Siana Whatarau of the NES and Mr Winton Herman were two Cook Island youths to embark on this voyage.