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1 September 2008 Dissolved Organic Matter in the Great Lakes: Role and Nature of Allochthonous Material
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Abstract

Dissolved organic matter (DOM) quality and the modifying influence of light on DOM bioavailability were investigated along a natural gradient of allochthonous influence in the lower Great Lakes. Using parallel factor analysis (PARAFAC), three DOM fluorophores were identified. One fluo-rophore, previously identified as peak C, was of allochthonous (component 1) origin and two previously uncharacterized fluorophores were identified as autochthonous (components 2 and 3). Component 1 was photoreactive and the dominant form in creek water samples while components 2 and 3 were dominant in Hamilton Harbour and lake water samples. Components 2 and 3 showed limited photoreactivity. Exposure to full spectrum irradiance decreased the average molecular weight of DOM (i.e., increased the absorbance ratio (a254:a365)) for all water samples. DOM bioavailability was lowest in creek and highest in lake water samples and was inversely related to DOM average molecular weight. Photomodifica-tion of DOM resulted in higher bacterial activity although these differences were not significantly different. This suggests that light plays a significant role in the cycling of terrestrially-derived DOM and to a certain extent autochthonous DOM, potentially increasing metabolism of both terrestrially and microbially derived DOM in the Great Lakes aquatic ecosystems.

Véronique P. Hiriart-Baer, Ngan Diep, and Ralph E. H. Smith "Dissolved Organic Matter in the Great Lakes: Role and Nature of Allochthonous Material," Journal of Great Lakes Research 34(3), 383-394, (1 September 2008). https://doi.org/10.3394/0380-1330(2008)34[383:DOMITG]2.0.CO;2
Received: 10 April 2007; Accepted: 1 March 2008; Published: 1 September 2008
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