Positive trends between salinity and chromophoric and fluorescent dissolved organic matter in a seasonally inverse estuary

Estuaries present high content of chromophoric and fluorescent dissolved organic matter (CDOM, FDOM) affecting the attenuation of ultraviolet and blue radiation. In temperate and tropical estuaries, the main CDOM source is riverine input that generally mixes conservatively with the oceanic waters leading to negative relationships between CDOM and salinity. In Mediterranean estuaries, riverine inputs are more limited or absent during the dry season producing a negative hydrological budget and, consequently, hypersalinity and an inverse circulation pattern. Much remains to be understood about CDOM and FDOM dynamics during rainy and dry periods in these last estuaries. In this study, we determined DOM absorbance and fluorescence in the Bay of Cadiz, Spain during a rainy (high riverine inputs) and dry (hypersaline conditions) period. We determined the absorption coefficients at 355 nm (a(355)) and acquired excitation emission matrices (EEMs). The EEMs showed two fluorescence peaks associated with terrestrial humic-like components (peaks A and C), one peak considered to be a marine humic-like component (peak M), and two peaks considered to be amino acid-like components (peaks T and B). The a(355) values ranged from 030 to 1.99 m(-1) with the highest values during the dry season. From the rainy season to the dry season, the overall fluorescence intensity increased and fluorescent peaks M, B, and T increased by greater than two orders of magnitude, whereas the fluorescence intensities of peaks A and C changed less than one order of magnitude. Unlike temperate and tropical estuaries, the a(355) values and fluorescence of the five peaks were positive and significantly related to salinity, but with different slopes. The inverse nature of the Bay of Cadiz during the dry season could be responsible for these positive trends between CDOM/FDOM and salinity. The slopes of the humic-like peaks A and C were lower than the a(355) slope suggesting their preferential losses, likely due to photobleaching. By contrast, the slopes of the amino acid-like peaks B and T were higher than the a(355) slope suggesting an in situ production of these fluorophores, likely due to diffusion from salt marsh and coastal sediments. (C) 2013 Elsevier Ltd. All rights reserved.