Publication Details

Category Text Publication
Reference Category Journals
DOI 10.1016/j.watres.2020.115532
Document accepted manuscript
Title (Primary) Dissolved organic matter in a tropical saline-alkaline lake of the East African Rift Valley
Author Butturini, A.; Herzsprung, P.; Lechtenfeld, O.J. ORCID logo ; Venturi, S.; Amalfitano, S.; Vazquez, E.; Pacini, N.; Harper, D.M.; Tassi, F.; Fazi, S.
Source Titel Water Research
Year 2020
Department SEEFO; ANA
Volume 173
Page From art. 115532
Language englisch
Keywords Dissolved organic carbon; African soda lake; Meromixis; FT-ICR-MS; CDOM
UFZ wide themes ProVIS;

Saline-alkaline lakes of the East African Rift are known to have an extremely high primary production supporting a potent carbon cycle. To date, a full description of carbon pools in these lakes is still missing. More specifically, there is not detailed information on the quality of dissolved organic matter (DOM), the main carbon energy source for heterotrophs prokaryotes. We report the first exhaustive description of DOM molecular properties in the water column of a meromictic saline-alkaline lake of the East African Rift. DOM availability, fate and origin were studied either quantitatively, in terms of dissolved organic carbon (DOC) and nitrogen (DON) or qualitatively, in terms of optical properties (absorbance) and molecular characterization of solid-phase extracted DOM (SPE-DOM) through negative electrospray ionization Fourier-transform ion cyclotron resonance mass spectrometry (FT-ICR-MS). DOM availability was high (DOC ∼ 8.1 mM in surface waters) and meromixis imprinted a severe quantitative and qualitative change on DOM pool. At the surface, DOM was rich in aliphatic and moderately in aromatic molecules and thus mirroring autochthonous microbial production together with photodegradation. At the bottom changes were extreme: DOC increased up to 5 times (up to 50 mM) and, molecular signature drifted to saturated, reduced and non-aromatic DOM suggesting intense microbial activity within organic sediments. At the chemocline, DOC was retained indicating that this interface is a highly reactive layer in terms of DOM processing. These findings underline that saline-alkaline lakes of the East African Rift are carbon processing hot spots and their investigation may broaden our understanding of carbon cycling in inland waters at large.

Persistent UFZ Identifier
Butturini, A., Herzsprung, P., Lechtenfeld, O.J., Venturi, S., Amalfitano, S., Vazquez, E., Pacini, N., Harper, D.M., Tassi, F., Fazi, S. (2020):
Dissolved organic matter in a tropical saline-alkaline lake of the East African Rift Valley
Water Res. 173 , art. 115532 10.1016/j.watres.2020.115532