The isotopic composition of organic carbon, nitrogen and provenance of organic matter in surface sediment from the Jiangsu tidal flat, southwestern Yellow Sea

The Jiangsu tidal flat is a significant organic matter reservoir, but quantitative studies of organic matter sources are scarce. In this study, total organic carbon (TOC) and total nitrogen (TN) concentrations and δ13Corg and δ15Ntotal values of surface sediment from Jiangsu tidal flat were investig...

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Veröffentlicht in:Marine pollution bulletin 2022-09, Vol.182, p.114010-114010, Article 114010
Hauptverfasser: Li, Tianning, Zhang, Gucheng, Wang, Shuai, Mao, Changping, Tang, Zhen, Rao, Wenbo
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Sprache:eng
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Zusammenfassung:The Jiangsu tidal flat is a significant organic matter reservoir, but quantitative studies of organic matter sources are scarce. In this study, total organic carbon (TOC) and total nitrogen (TN) concentrations and δ13Corg and δ15Ntotal values of surface sediment from Jiangsu tidal flat were investigated for their distributions, influencing factors, and sources of organic matter. TOC and TN were high in the center of study area and correlated well with grain size, indicating hydrodynamic influence on organic matter. High TOC/TN and low δ13Corg and δ15Ntotal in estuaries were characteristic of C3 plants, soil, and fertilizer sources, suggesting source effect on the distribution of organic matter. The MixSIAR model revealed that marine sources were dominant with a contribution reaching 56.9 %, followed by uniform of C3 plants, soil and fertilizer, while domestic sewage was least prominent. This study enriched theories of the biogeochemical cycle and ecological protection in the southwestern Yellow Sea. •Distribution of organic matter was affected by hydrodynamic conditions and sources.•Marine sources were the main provenance of organic matter through MixSIAR model.•Estuary organic matter was characterized of fertilizer, soil and C3 plants sources.•OM sources showed spatial variability.
ISSN:0025-326X
1879-3363
DOI:10.1016/j.marpolbul.2022.114010