Ma. Moran et al., Biodegradation of riverine dissolved organic carbon in five estuaries of the southeastern United States, ESTUARIES, 22(1), 1999, pp. 55-64
The biological turnover of riverine dissolved organic carbon (DOC) discharg
ed into five southeastern United States estuaries was examined in long-term
respiration bioassays. Measures of bacterial oxygen consumption indicated
surprisingly large differences in the inherent biodegradability of DOC amon
g the five estuaries, despite their close geographic proximity. Differences
of up to 13-fold in biodegradation rates were also found temporally within
a single estuary. For most of the southeastern United States estuaries, me
asured rates of riverine DOC biodegradation were low relative to rates repo
rted for other freshwater and marine environments. This was particularly tr
ue for the coastal plain ("blackwater") rivers that contribute about 35% of
the riverine DOC exported to coastal marine environments in this region; e
xtrapolation of biodegradation rates to the adjacent continental shelf pred
ict biodegradation of a maximum of 11% of exported blackwater DOC within th
e estuary-shelf system (with transit times of up to 140 d). DOC from Piedmo
nt rivers was more biologically labile, with maximum losses of 30% predicte
d within the estuary and adjacent shelf. Short exposures to natural sunligh
t increased the lability of the riverine DOC and enhanced biodegradation ra
tes by over 3-fold in some cases, although significant inter-estuary differ
ences in susceptibility of riverine DOC to photolysis were also evident.