Characterization of dissolved organic matter in Lake Superior and its watershed using ultrahigh resolution mass spectrometry

Elizabeth C Austin-Minor, Carla J. Steinbring, Krista Longnecker, Elizabeth B. Kujawinski

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140 Scopus citations

Abstract

With the advent of ultrahigh resolution mass spectrometry (MS), recent studies have begun to resolve molecular relationships between terrestrial and aquatic dissolved organic matter (DOM) in rivers, estuaries, mangrove swamps and their receiving oceans and lakes. Here, we extend ultrahigh resolution MS techniques to Lake Superior, the largest freshwater lake in the world by area. Solid-phase extracted samples from the western arm of the lake and its watershed, including swamp, creek, river, lake-river confluence and offshore lake sites were compared using electrospray ionization (ESI), Fourier transform ion cyclotron resonance MS (FT-ICR-MS). Results were analyzed using cluster analysis and van Krevelen diagrams. Chemical similarity appears related to hydrological proximity, terrestrial impact and flow conditions. For example, higher and lower flow samples from the same stream differ from one another. Toivola Swamp, Lake Superior and the south shore river have diverse arrays of unique molecular formulae relative to the north shore river and stream sampled in the data set. The lake's unique elemental formulae, relative to its watershed samples, are primarily in the lignin-like and reduced hydrocarbon regions of van Krevelen diagrams. The ESI-amenable lake DOM also has a higher proportion of formulae containing nitrogen or sulfur relative to the other samples. The degree of overlap among formulae within the data set is consistent with previous ESI FT-ICR-MS characterization of terrestrial, estuarine and marine OM. There appears to be a conserved portion of formulae across natural OM samples, perhaps because these compounds are intrinsically refractory or because they are commonly generated as products of natural reworking processes.

Original languageEnglish (US)
Pages (from-to)1-11
Number of pages11
JournalOrganic Geochemistry
Volume43
DOIs
StatePublished - Feb 2012

Bibliographical note

Funding Information:
The study was supported in part by NSF Grant OCE-0825600 (to E.C.M.). C.S. was supported in part by a National Science Foundation Graduates in K-12 Education grant to the University of Minnesota Duluth. Travel support was provided to C.S. through the travel fund at the WHOI FT-MS facility which was funded by the WHOI Director of Research and NSF grant OCE-0751897. The authors thank M. Kido Soule for FT-ICR-MS assistance and the funding sources of the WHOI FT-MS facility (NSF Grant OCE-0619608 and the Gordon and Betty Moore Foundation). Thanks also go to B. Stephens and B. Kruger (Large Lakes Observatory) for sharing samples, S. Stark (UMD Geology) for assistance in generating Fig. 1 and three anonymous reviewers for constructive comments.

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