Sediment resuspension as a driving force for organic carbon transference and rebalance in marginal seas

• Published in: Water research (Oxford) 2024-06, Vol.257, p.121672-121672, Article 121672
• Main Authors: Liu, Xiaoqing, Lan, Chunyuan, Zhu, Longhai, Yan, Caiqing, Wang, Nan, Chen, Haibiao, Zheng, Guangjin, Che, Yangli, Yang, Zuosheng, Bao, Rui
• Format: Article
• Language: English
• Subjects: Carbon; Carbon Cycle; Geologic Sediments - chemistry; Grain size; Oceans and Seas; Organic carbon burial; Organic carbon transfer; Radiocarbon (14C); Seawater - chemistry; Sediment resuspension; Shallow marginal sea
• ISSN: 0043-1354; 1879-2448
• DOI: 10.1016/j.watres.2024.121672

•Sediment resuspension drives refractory organic carbon (OC) transfer into seawater.•OC transfer results in the enhancement of dissolved OC bioavailability.•Refractory OC accumulates on particles during sediment resuspension.•The magnitudes of OC transfer are affected by sediment grain sizes. The transfer of particulate organic carbon (POC) to dissolved organic carbon (DOC; OC transferP-D) is crucial for the marine carbon cycle. Sediment resuspension driven by hydrodynamic forcing can affect the burial of sedimentary POC and benthic biological processes in marginal sea. However, the role of sediment grain size fraction on OC transferP-D and the subsequent impact on OC cycling remain unknown. Here, we conduct sediment resuspension simulations by resuspending grain-size fractionated sediments (< 20, 20–63, and > 63 μm) into filtered seawater, combined with analyses of OC content, optical characteristics, 13C and 14C isotope compositions, and molecular dynamics simulations to investigate OC transferP-D and its regulations on OC bioavailability under sediment resuspension. Our results show that the relative intensities of terrestrial humic-like OC (refractory DOC) increase in resuspension experiments of < 20, 20–63, and > 63 μm sediments by 0.14, 0.01, and 0.03, respectively, likely suggesting that sediment resuspension drives refractory DOC transfer into seawater. The variations in the relative intensities of microbial protein-like DOC are linked to the change of terrestrial humic-like OC, accompanied by higher DOC content and reactivity in seawater, particularly in finer sediments resuspension experiments. This implies that transferred DOC likely fuels microbial growth, contributing to the subsequent enhancement of DOC bioavailability in seawater. Our results also show that the POC contents increase by 0.35 %, 0.66 %, and 0.93 % in < 20, 20–63, and > 63 μm resuspension experiments at the end of incubation, respectively. This suggests that the re-absorption of OC on particles may be a significant process, but previously unrecognized during sediment resuspension. Overall, our findings suggest that sediment resuspension promotes the OC transferP-D, and the magnitudes of OC transferP-D further influence the DOC and POC properties by inducing microbial production and respiration. These processes significantly affect the dynamics and recycling of biological carbon pump in shallow marginal seas. [Display omitted]