Spatial distribution, chemical speciation and source apportionment of carbon, nitrogen and phosphorus in surface sediments of northern Beibu Gulf, South China

被引:1
|
作者
Guo, Jing [1 ,3 ,4 ]
Yan, Xiaomin [1 ,3 ,4 ]
Wu, Man [2 ,4 ]
Qiu, Hengtong [1 ,3 ,4 ]
Li, Wan-Yi [1 ,3 ,4 ]
Huang, Wenlong [1 ,3 ,4 ]
Wu, Di [1 ,3 ,4 ]
Xue, Baoming [6 ]
Xu, Guilin [1 ,3 ,4 ]
Pan, Zihan [2 ]
Mo, Zhiming [5 ]
机构
[1] Nanning Normal Univ, Key Lab Environm Change & Resources Use Beibu Gulf, Minist Educ, Nanning 530001, Peoples R China
[2] Guangxi Acad Sci, Guangxi Acad Marine Sci, Nanning 530007, Peoples R China
[3] Nanning Normal Univ, Guangxi Beibu Gulf Intelligent Marine Ranching Eng, Nanning 530001, Peoples R China
[4] Guangxi Acad Sci, Guangxi Beibu Gulf Carbon Sink & Low Carbon Engn R, Nanning 530007, Peoples R China
[5] Guangxi Univ Finance & Econ, Nanning 530003, Peoples R China
[6] Guangdong Polytech Environm Protect Engn, Foshan 528216, Peoples R China
关键词
Spatial variations; Chemical speciation; delta C-13 and delta N-15; Source apportionment; Northern Beibu Gulf; ORGANIC-MATTER; GEOCHEMICAL CHARACTERISTICS; ISOTOPE COMPOSITION; BAY; RATIOS; SEA; EUTROPHICATION; PRESERVATION; MARICULTURE; DELTA-C-13;
D O I
10.1016/j.marpolbul.2024.117202
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study presents the spatial distribution and chemical speciation of carbon (C), nitrogen (N) and phosphorus (P) in sediments, and traces the origins of sedimentary organic matter (SOM) with C-N isotopes composition and elemental ratios in the northern Beibu Gulf. The spatial distribution of biogenic elements was significantly related to the grain size composition and terrestrial inputs. The liable nitrogen (LN) accounted for 20.74 f 14.84 % of total nitrogen (TN), and organic matter-sulfide form-N (OSF-N) was the dominant part among four LN forms. The bio-available P (BAP) accounted for 76.49 f 5.92 % of total phosphorus (TP), and the average proportions of P fractions followed the order of organic P (OP) > Fe-bound P (Fe-P) > authigenic P (Ca-P) > detrital P (De-P) > exchangeable P (Ex-P). The SOM was mainly derived from terrestrial sources in Lianzhou Bay and Maowei Sea, whereas marine phytoplankton primarily contributed to the SOM in other coastal bays.
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页数:8
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