Molecular characterization of marine and terrestrial dissolved organic matter using ultrahigh resolution mass spectrometry.

DOM represents the largest reservoir of organic carbon stored in the oceans. Its source has been proposed to originate from marine primary and bacterial production, with limited land-derived contributors. Marine DOM is a complex mixture of biomolecules that either exist naturally or have been transformed from living and decaying organisms in the ocean. Previous research has identified only a small portion of deep sea DOM, due to the complexity of the mixture and lack of advanced techniques available; however, ultrahigh resolution mass spectrometry has succeeded for DOM characterization where other techniques have failed. In Chapter 3, we compare ultrahigh resolution mass spectra of marine DOM isolated from two sites in the Weddell Sea (Antarctica) using ESI and Atmospheric Pressure Photoionization (APPI). These spectra, obtained on a 9.4 Tesla FT-ICR-MS, indicate the two ionization techniques are complementary. Ions produced by APPI extend to higher carbon undersaturation compared to ESI, indicated by higher double-bond equivalence minus oxygen (DBE-O) values, while ions in the ESI spectra are more oxygenated. Moreover, many sulfur-containing compounds were efficiently ionized by ESI but not detected by APPI. These results show that the differences in mass spectra obtained by ESI and APPI FT-ICR-MS are significant and that both are necessary to obtain a complete description of the molecular composition of marine DOM. Peatlands are extraordinary carbon reservoirs due to their sequestration and emission of greenhouse gases. Chapter 4 depicts the importance of investigating the molecular characterization of terrestrial DOM from the Glacial Lake Agassiz Peatlands (GLAP) of northern Minnesota, to reveal the potentially pivotal role it plays in global carbon cycling. ESI-FT-ICR-MS was used to identify the qualitative differences between DOM in fen and bog porewaters of the Red Lake II system in the GLAP. Approximately 80% of molecular composition observed in surface porewater was maintained throughout the bog profile (0.17 to 2.50m). The qualitative stability of the molecular composition of DOM was accompanied by a quantitative increase in Dissolved Organic Carbon (DOC) with depth. The composition of DOM in the fen was significantly different at depth with slightly varying DOC levels. Using Aromaticity Index (AI) values we identified condensed aromatic phenol-type compounds in the porewaters of both peatlands. Surface bog and deep fen DOM had surprising similar molecular compositions. We suggest that enzymatic degradation via phenol oxidase and slower hydrologic transport down the bog vertical profile are responsible for the observed variations in DOM composition. In Chapter 5, molecular composition and optical properties were correlated for two samples of DOM from different peat formations in the GLAP. Fen and bog DOM were analyzed using 9.4 T FT-ICR-MS to determine the aromatic content as a function of depth. UV/Vis absorbance and Excitation Emission Matrix Fluorescence Spectroscopy (EEMS) were used to identify changes in the optical properties associated with the chromophoric fractions of DOM (CDOM). Higher specific UV absorbance (SUVA) at 254 nm indicated more abundant aromatic content for surface bog and deep fen DOM. EEMS results were also found to be in agreement with the absorption spectra and molecular characterization as determined by FT-ICR-MS. The strong correlations we have observed suggest that optical spectroscopy techniques represent an effective surrogate approach to characterizing DOM provided some detailed molecular information is available for calibrating the observed correlations. Finally, comparative analysis of...