Abstract
Abstract. Dissolved organic carbon (DOC) concentration in the Pearl River estuary (PRE) of China was measured in May, August, and October 2015 and January 2016. Chromophoric and fluorescent dissolved organic matter (CDOM and FDOM) in the latter three seasons were characterized by absorption and fluorescence spectroscopy. CDOM and FDOM exhibited negligible seasonal variations, while DOC displayed a significant seasonality, with the average concentration being highest in May (156 µmol L−1), lowest in November (87 µmol L−1), and comparable between January (118 µmol L−1) and August (112 µmol L−1). Although DOC, CDOM, and FDOM in surface water were generally higher than in bottom water, the difference between the two layers was statistically insignificant. DOC showed little cross-estuary variations in all seasons, while CDOM and FDOM in January were higher on the west side of the estuary than on the east side. All three variables showed rapid drawdowns in the head region of the estuary (salinity <5); their dynamics in the main estuary were primarily controlled by conservative mixing, leading to linearly declining or relatively constant (for DOC in May and November only) contents with increasing salinity. The decrease in FDOM with salinity was 5 %–35 % faster than that of CDOM, which in turn was 2–3 times quicker than that of DOC. Salinity and CDOM absorption coefficients could serve as indicators of DOC in August and January. Freshwater endmembers in all seasons mainly contained fresh, protein-rich DOM of microbial origin, a large part of it likely being pollution-derived. Protein-like materials were preferentially consumed in the head region but the dominance of the protein signature was maintained throughout the estuary. Exports of DOC and CDOM (in terms of the absorption coefficient at 330 nm) into the South China Sea were estimated as 195×109 g and 266×109 m2 for the PRE and 362×109 g and 493×109 m2 for the entire Pearl River Delta. The PRE presents the lowest concentrations and export fluxes of DOC and CDOM among the world's major estuaries. DOM delivered from the PRE is, however, protein-rich and thus may enhance heterotrophs in the adjacent coastal waters. Overall, the PRE manifests lower abundance and smaller spatiotemporal variability of DOM than expected for a sizable estuary with a marked seasonality of river runoff due supposedly to the poorly forested watershed of the Pearl River, the rapid degradation of the pollution-derived DOM in the upper reach, and the short residence time of freshwater.
Highlights
River runoff is an important contribution of dissolved organic matter (DOM) to the ocean (Raymond and Spencer, 2015)
The discharge rates to the Pearl River estuary (PRE) were estimated as 8.9 × 103 m3 s−1 in May, 5.7 × 103 m3 s−1 in August, 6.7 × 103 m3 s−1 in November, and 5.0 × 103 m3 s−1 in January based on the fact that the PRE receives 54 % of the total discharge from the Pearl River (Mikhailov et al, 2006)
The present study confirms the large variations in the abundance of DOM in the head region of the PRE observed by previous studies (Callahan et al, 2004; Chen et al, 2004; Lin, 2007; He, 2010; Wang et al, 2014; Lei et al, 2018; Ye et al, 2018)
Summary
River runoff is an important contribution of dissolved organic matter (DOM) to the ocean (Raymond and Spencer, 2015). DOM in river water originates from soil leaching (terrigenous DOM) and in situ microbial production. During its transit through estuaries, riverine DOM may be subject to physical (e.g., flocculation and coagulation, Asmala et al, 2014), biological (e.g., microbial uptake, Benner and Kaiser, 2011), and photochemical (Del Vecchio and Blough, 2002) removals, thereby reducing its abundance and modifying its chemical and optical properties before reaching the ocean. Biological production in estuaries can add organic matter to the riverine DOM pool (Bianchi et al, 2004; Fellman et al, 2010; Benner and Kaiser, 2011; Deutsch et al, 2012). Pollution directly brings anthropogenic DOM and carries nutrients that enhance biological DOM production
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