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长江口及其邻近海域颗粒态氨基酸的分布以及对有机质降解和来源的指示
引用本文:张敬慧,陈岩,杨剑,杨桂朋.长江口及其邻近海域颗粒态氨基酸的分布以及对有机质降解和来源的指示[J].海洋环境科学,2022,41(2):283-292, 302.
作者姓名:张敬慧  陈岩  杨剑  杨桂朋
作者单位:1.中国海洋大学 化学化工学院,海洋化学理论与工程技术教育部重点实验室,山东 青岛 266100
基金项目:国家重点研发计划;烟台市科技计划项目;国家自然科学基金;中国科学院重点实验室开放基金
摘    要:本研究于2018年3月采集长江口及其邻近海域50个站位样品,对颗粒态氨基酸(PAA)的分布与组成进行了分析。结果表明:PAA的平均浓度为(1.86 ± 1.02)μmol/L(0.76~5.55 μmol/L),其主要组分为天门冬氨酸(Asp)、谷氨酸(Gly)、丝氨酸(Ser)、丙氨酸(Ala)和甘氨酸(Glu)。颗粒有机碳(POC)和颗粒氮(PN)的平均浓度分别为(74.21 ± 37.70)μmol/L(18.06~238.66 μmol/L)和(7.52 ± 3.46)μmol/L(2.27~19.86 μmol/L)。PAA、POC与PN具有相似的分布特征,长江口内浓度低于近岸浓度,近岸浓度高于远岸浓度,垂直分布上较为均匀。研究海域中的C/N由近岸向远海逐渐降低,表明陆源输入有机质的影响逐渐降低。基于氨基酸的衍生参数Asp/Gly和Ser + Thr(苏氨酸)mol%]表明该海域颗粒物中有机质主要源于硅质碳源,与硅藻在该海域中相对较高的生物量有关。碳、氮归一化产率PAA-C(N)%]以及降解因子(DI)所指示的降解趋势并不完全一致,这或许与PAA-C(N)%和DI适用于不同降解阶段以及氨基酸来源与转化的多样性有关。

关 键 词:颗粒态氨基酸    颗粒有机碳    来源    降解    长江口
收稿时间:2020-12-01

Distribution of particulate amino acids in the Changjiang Estuary and its adjacent sea and their indications for degradation and sources of organic matter
ZHANG Jing-hui,CHEN Yan,YANG Jian,YANG Gui-peng.Distribution of particulate amino acids in the Changjiang Estuary and its adjacent sea and their indications for degradation and sources of organic matter[J].Marine Environmental Science,2022,41(2):283-292, 302.
Authors:ZHANG Jing-hui  CHEN Yan  YANG Jian  YANG Gui-peng
Affiliation:1.College of Chemistry and Chemical Engineering, Ocean University of China, Key Laboratory of Marine Chemistry Theory and Technology, MOE, Qingdao 266100,China
Abstract:A total of 50 samples were collected to investigate the distribution and composition of particulate amino acids (PAA) in the Changjiang Estuary and its adjacent East China Sea in March, 2018. The results showed that the average concentration of PAA was (1.86 ± 1.02) μmol/L (0.76~5.55 μmol/L). The major components of PAA in this study were Asp (aspartic acid), Gly (glycine acid), Ser (serine acid), Ala (alanine acid) and Glu (glutamic acid). The average concentrations of particulate organic carbon (POC) and particulate nitrogen (PN) were (74.21 ± 37.70) μmol/L (18.06~238.66 μmol/L) and (7.52 ± 3.46) μmol/L (2.27~19.86 μmol/L), respectively. The distributions of PAA, POC and PN showed similar trends, with elevated concentrations were found at the mouth of the Changjiang River and nearshore stations of the study area. The vertical distributions of PAA, POC and PN exhibited a uniform pattern. The C/N ratio in this study gradually decreased seaward, reflecting the influence of terrestrial input. Derivative parameters Asp/Gly and Ser + Thr mol%] based on amino acids indicated that POM was dominated by diatomaceous organic matter, which might be due to the dominant growth of diatoms in the study area. No correlation were found between the PAA-C (N)% and the degradation index (DI), respectively. This discrepancy may be related to the application of PAA-C (N)% and DI to different stages of degradation and the diversity of sources and transformations of amino acids.
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