Abstract
Biological degradation contributes significantly to aquatic dissolved organic matter (DOM) turnover. Yet to date, the specific biological pathways involved in DOM degradation are still obscure. Here, we show how DOM changes in response to 28-d incubation in a karst river, via the combined fluorescent excitation-emission matrix (EEM) with parallel factor analysis (PARAFAC) and peak picking. Tyrosine-, tryptophan- and UV humic-like components were identified as the primary DOM in original waters. Notable decreases of protein-like components were observed after 15 ℃ incubation, suggesting preferential consumption of biogenic DOM. Elevated temperature (30 ℃), however, caused significant decreases in visible humic-like and terrestrial fulvic-like components, but an increase in UV humic-like components in comparison to 15 ℃ incubation (p < 0.05). Humification index (HIX) decreased dramatically after 15 ℃ incubation, indicating that biological processes regulated river DOM properties. Our results highlight the significant biogenic signals in karst rivers, and evidence that fluorescence measurement can decipher riverine DOM biodegradation as a useful approach.
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