Marine optical biogeochemistry: the chemistry of ocean color.

By P. Coble. Chemical Reviews, 2007

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Optical properties of dissolved organic matter (DOM): Effects of biological and photolytic degradation (2016, methodology): “Both DOM amount and composition vary spatially and temporally due not only to its proximity to source material but also to its exposure to environmental processing (Hood et al. 2005; Coble 2007; Helms et al. 2008).”
Biogeneration of chromophoric dissolved organic matter by bacteria and krill in the Southern Ocean (2009, background): “Chromophoric dissolved organic matter (CDOM) in oceanic waters comprises a broad suite of optically active compounds (Nelson and Siegel 2002; Coble 2007), and these compounds play important roles in the cycling of carbon and other elements as they mediate photochemical reactions (Mopper et al.…”
Production of chromophoric dissolved organic matter by marine phytoplankton (2010, background): “A subfraction of CDOM can emit blue fluorescence when it is irradiated with UV light, and this subfraction is called fluorescent CDOM (FDOM; Coble 1996, 2007).”
Formation of Chromophoric Dissolved Organic Matter by Bacterial Degradation of Phytoplankton-Derived Aggregates (2018, background): “Two types of fluorescence are typically described, amino acid-like compounds and humiclike compounds (Coble, 2007), and have been attributed to autochthonous (e.g., primary production) and allochthonous (e.g., terrestrial) production, respectively (Coble, 1996; Yamashita and Tanoue, 2003).”