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北部湾北部表层沉积物中碳、氮、磷的空间分布、化学形态及来源解析。

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

机构信息

Key Laboratory of Environment Change and Resources Use in Beibu Gulf, Ministry of Education, Nanning Normal University, Nanning 530001, China; Guangxi Beibu Gulf Intelligent Marine Ranching Engineering Research Center, Nanning Normal University, Nanning 530001, China; Guangxi Beibu Gulf carbon sink and low carbon Engineering Research Center, Guangxi Academy of Sciences, Nanning 530007, China.

Guangxi Academy of Marine Sciences, Guangxi Academy of Sciences, Nanning 530007, China; Guangxi Beibu Gulf carbon sink and low carbon Engineering Research Center, Guangxi Academy of Sciences, Nanning 530007, China.

出版信息

Mar Pollut Bull. 2024 Dec;209(Pt A):117202. doi: 10.1016/j.marpolbul.2024.117202. Epub 2024 Nov 4.

Abstract

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 CN 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 ± 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 ± 5.92 % of total phosphorus (TP), and the average proportions of P fractions followed the order of organic P (OP) > Fe-bound P (FeP) > authigenic P (CaP) > 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.

摘要

本研究展示了北部湾沉积物中碳(C)、氮(N)和磷(P)的空间分布和化学形态,并通过 CN 同位素组成和元素比值追踪了沉积物有机质(SOM)的来源。生物成因元素的空间分布与粒径组成和陆源输入有显著关系。易态氮(LN)占总氮(TN)的 20.74±14.84%,而 LN 的四种形态中以有机-硫化物结合态氮(OSF-N)为主。生物有效磷(BAP)占总磷(TP)的 76.49±5.92%,磷各形态的平均比例顺序为有机磷(OP)>铁结合态磷(FeP)>自生磷(CaP)>碎屑磷(De-P)>可交换磷(Ex-P)。廉州湾和涠洲海的 SOM 主要来源于陆源,而其他沿海海湾的 SOM 则主要来源于海洋浮游植物。

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