Periodic Reporting for period 1 - Phycosphere Fe (Iron speciation in the microenvironment surrounding phytoplankton cells and the consequences for Fe bioavailability)

More than a half of atmospheric CO2 on earth is taken up by phytoplankton, but iron (Fe) limits their growth in large regions of the oceans. Ongoing ocean acidification and global warming would influence Fe-stress in marine phytoplankton and hence the biological carbon...