Ma. Moran et al., Carbon loss and optical property changes during long-term photochemical and biological degradation of estuarine dissolved organic matter, LIMN OCEAN, 45(6), 2000, pp. 1254-1264
Terrestrially derived dissolved organic matter (DOM) impacts the optical pr
operties of coastal seawater and affects carbon cycling on a global scale.
We studied sequential long-term photochemical and biological degradation of
estuarine dissolved organic matter from the Satilla River, an estuary in t
he southeastern United States that is dominated by vascular plant-derived o
rganic matter. During photodegradation, dissolved organic carbon (DOC) loss
(amounting to 31% of the initial DOC) was much less extensive than colored
dissolved organic matter (CDOM) or fluorescent dissolved organic matter (F
DOM) loss (50% and 56% of the initial CDOM and FDOM), and analysis of kinet
ics suggested a reservoir of DOC that was resistant to photodegradation. In
contrast, CDOM photodegradation closely followed first-order kinetics over
two hall-lives with no indication of a nondegradable component. FDOM loss
was slightly biased toward fluorophores considered representative of terres
trial humic substances. Additional changes in optical properties included i
ncreases in spectral slope and shifts in fluorescence excitation/emission m
axima that were generally consistent with previous observations from field
studies of photobleached DOM. Biological degradation of photobleached DOM w
as more rapid than that of unbleached material, and this net positive effec
t was evident even for extensively photodegraded material. Bacterial degrad
ation caused shifts in the opposite direction from photochemical degradatio
n for both spectral slope and excitation/emission maxima and thus dampened
but did not eliminate changes in optical properties caused by photobleachin
g.