Transformation of dissolved inorganic carbon (DIC) into particulate organic carbon (POC) in the lower Xijiang River, SE China: an isotopic approach

Abstract

The sources and dynamics of riverine carbon have been discussed extensively, but knowledge about the transformation from DIC into organic carbon (OC) is still poorly understood. In this study, we conducted a comprehensive investigation on the river-ine carbon, stable carbon isotopic components and C/N ratios for different seasons, 5 including an extreme flood event, in the lower Xijiang and its three tributaries. Detailed analyses are also performed for soil samples across the study region. Downstream increase in δ 13 C DIC and downstream decrease in both δ 13 C POC and C/N have been observed for all the tributaries. Meanwhile, positive shift of δ 13 C DIC and negative shift of δ 13 C POC are also observed from summer to winter. These observations likely indicate 10 that the isotopic compositions of both DIC and POC are significantly affected by in-river primary production that converts DIC into organic matter through photosynthesis. It is estimated that the percentage contribution of the riverine aquatic primary production to the riverine POC in the Xijiang and three tributaries of Guijiang, Hejiang and Luoding is respectively 7.1 %, 43.2 %, 36.4 % and 9.9 % in rainy season, and 35.6 %, 47.3 %, 15 50.3 % and 40.1 % in dry season. Based on the stoichiometry involved in chemical weathering of the bedrocks, the transformation of the carbonate-sourced DIC to POC is further quantified to be 3.4-20.5 % in rainy season, and 12.3-22.1 % in dry season. This may suggest an important sink of atmospheric CO 2 in river systems that was largely ignored previously.