Fluorescent dissolved organic matter in lakes: Relationships with heterotrophic metabolism

By W. K. Levi Cammack, J. Kalff, Yves T. Prairie, Erik M. Smith. 2004

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Viral lysis of Micromonas pusilla: impacts on dissolved organic matter production and composition (2013, unknown): “Previous studies have found that F(280/320) is available for bacterial utilization (Cammack et al. 2004; Lønborg et al. 2010), however, different subcomponents of the F(280/320) pool may have different bioavailability, as some fractions are consumed more readily than others (Lønborg et al. 2010).”
Biological lability of streamwater fluorescent dissolved organic matter (2012, background): “…ranged from 24 h for coastal upwelling waters (Nieto-Cid et al. 2006) to 51 d for estuarine waters (Moran et al. 2000) and have been performed with samples from lakes (Cammack et al. 2004), a fjord (Stedmon and Markager 2005), and marine, mid-estuary, and brackish bay waters (Boyd and Osburn 2004).”