Department of Geosciences/Princeton Environmental Institute, 153 Guyot Hall, Princeton University, Princeton, NJ 08544, USA
Abstract:
In cultures and in nature, ferric (oxyhydro-)oxides (FeOx) precipitate and become associated with phytoplankton surfaces. Other trace elements adsorb on FeOx and it is thus difficult to differentiate between cellular- and oxide-associated concentrations of both iron and these elements. Existing techniques to selectively dissolve the FeOx associated with phytoplankton surfaces often contaminate the sample or necessitate elaborate pre-cleaning procedures and/or proceed by unknown and thus uncontrolled mechanisms.