Constraining the origin of sedimentary organic matter in the eastern Guangdong coast of China using δ13C and δ15N

被引:3
作者
Wu, Junwen [1 ,2 ,3 ]
Chen, Jisheng [1 ,2 ]
Wang, Cui [4 ]
Yan, Xiuli [1 ,2 ]
Yin, Xijie [4 ]
Liu, Qian [5 ,6 ]
机构
[1] Shantou Univ, Guangdong Prov Key Lab Marine Disaster Predict & P, Shantou, Peoples R China
[2] Shantou Univ, Inst Marine Sci, Shantou, Peoples R China
[3] Southern Marine Sci & Engn Guangdong Lab Guangzhou, Guangzhou, Peoples R China
[4] Minist Nat Resource, Inst Oceanog 3, Xiamen, Peoples R China
[5] Ocean Univ China, Frontiers Sci Ctr Deep Ocean Multispheres & Earth, Qingdao, Peoples R China
[6] Ocean Univ China, Key Lab Marine Chem Theory & Technol, Minist Educ, Qingdao, Peoples R China
基金
中国国家自然科学基金;
关键词
terrestrial organic carbon; delta C-13; C/N ratio; marine sediment; eastern Guangdong coast; PEARL RIVER ESTUARY; CONTINENTAL-SHELF; C/N RATIOS; STABLE-ISOTOPE; CARBON-ISOTOPE; BALTIC SEA; NITROGEN; MARINE; BAY; FATE;
D O I
10.3389/fmars.2023.1234116
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The source apportionment of organic carbon is of great scientific significance for understanding the carbon sink pattern in the coastal ocean. The concentrations of total organic carbon (TOC) and total nitrogen (TN) and their isotopic compositions (delta C-13(TOC) and delta N-15(TN)) were determined in surface sediments and sediment cores (Y3 and Y5) collected in the eastern Guangdong coast (EGDC) during spring, summer and winter cruises in 2021, in order to determine the distribution and source of sedimentary organic matter. Spatially, TOC and delta C-13(TOC) distributions in the EGDC have contrasting patterns; TOC concentrations decreased and delta C-13(TOC) values increased with distance offshore. Higher TOC concentrations and enriched delta C-13(TOC) were observed in the marine aquaculture area off EGDC. The measured values of delta C-13(TOC), delta N-15(TN) and the C/N ratio constrained the two dominant sources of organic matter, marine and terrestrial material, in the EGDC. Using a two end-member mixing model, we estimated the proportion of marine organic matter to be 74 +/- 20% in spring, 74 +/- 16% in summer and 75 +/- 12% in winter, respectively. This suggests in situ production of marine phytoplankton dominated the organic carbon pool (average=similar to 74%) in the EGDC sediment. These consistent marine organic matter contributions are also observed in sediment cores, with proportions averaging 59 +/- 5% in core Y3 and 66 +/- 4% in core Y5. The observed variations in biogeochemical proxies in sediments are thus mainly caused by differing relative contributions of marine and terrestrial organic matter. Additionally, the high TOC inventory in the marine aquaculture area indicates increased carbon storage and carbon fixation capacity compared to the other areas investigated. Overall, this study establishes a background carbon database in the coastal environment that can be used in future studies of blue carbon to achieve carbon neutrality in China.
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页数:15
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