氨基酸示踪南海东北部溶解有机物的来源与降解状态

迟隆祥, 范承飞, 陈岩, 张洪海

中国环境科学 ›› 2025, Vol. 45 ›› Issue (9) : 5062-5070.

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中国环境科学 ›› 2025, Vol. 45 ›› Issue (9) : 5062-5070.
环境生态

氨基酸示踪南海东北部溶解有机物的来源与降解状态

  • 迟隆祥1,2, 范承飞1,2, 陈岩2, 张洪海1,2
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Amino acid traced the source and degradation state of dissolved organic matter in the Northeastern South China Sea

  • CHI Long-xiang1,2, FAN Cheng-fei1,2, CHEN Yan2, ZHANG Hong-hai1,2
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摘要

于2023年9月调查了南海东北部海域海水中总溶解态氨基酸(TDAA)的浓度分布、分子组成并探究了溶解有机物(DOM)的来源及降解状态.结果表明:海水中TDAA的浓度范围为0.37~2.59μmol/L,平均值为(0.78±0.41)μmol/L,TDAA的水平分布呈现近岸高、远海低的特点,垂直分布呈现表层至底层逐渐降低的趋势.以D-丙氨酸(D-Ala)作为生物标志物量化细菌源有机物对DOM的贡献率(Bacterial-C%),海水中Bacterial-C%的变化范围为9.6%~46.2%,平均值为(23.3±8.1)%,其整体呈现近岸低、远海高的趋势.此外,表层海水的降解因子(DI)平均值为(0.5±1.0),而中层海水和底层海水DI的平均值分别为(-1.2±0.6)和(-1.3±0.6),表明表层海水的DOM相对于中层和底层海水的DOM降解程度较低.本研究揭示了南海东北部海域DOM的来源及降解状态,为深入理解边缘海生物地球化学循环过程提供了重要的科学依据与数据支持.

Abstract

In September 2023, a study was conducted in the Northeastern South China Sea to investigate the concentration distribution and mole composition of total dissolved amino acids (TDAA) in the seawater, as well as the sources and degradation status of dissolved organic matter (DOM). The results showed that the concentration of TDAA ranged from 0.37 to 2.59μmol/L, with an average value of (0.78±0.41) μmol/L. The horizontal distribution of TDAA exhibited a pattern of higher concentrations near the coast and lower concentrations in offshore, while the vertical distribution showed a gradual decrease from the surface to the bottom layer. Using D-alanine (D-Ala) as a biomarker, the contribution of bacterial organic matter to DOM (Bacterial-C%) was quantified. The Bacterial-C% in seawater ranged from 9.6% to 46.2%, with an average value of (23.3±8.1)%, demonstrating an overall trend of lower values near the coast and higher values in offshore areas. Additionally, the mean value of degradation index (DI) in surface seawater was (0.5 ± 1.0), while the average DI values for middle and bottom layers were (-1.2±0.6) and (-1.3±0.6), respectively. This indicates that the DOM in surface seawater was less degraded compared to those in the middle and bottom layers. This study elucidates the sources and degradation status of DOM in the Northeastern South China Sea, providing important scientific insights and data support for a deeper understanding of biogeochemical cycling processes in marginal seas.

关键词

总溶解态氨基酸 / 细菌贡献 / 有机物降解 / 南海

Key words

total dissolved amino acids / bacterial contribution / organic matter degradation / South China Sea

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导出引用
迟隆祥, 范承飞, 陈岩, 张洪海. 氨基酸示踪南海东北部溶解有机物的来源与降解状态[J]. 中国环境科学. 2025, 45(9): 5062-5070
CHI Long-xiang, FAN Cheng-fei, CHEN Yan, ZHANG Hong-hai. Amino acid traced the source and degradation state of dissolved organic matter in the Northeastern South China Sea[J]. China Environmental Science. 2025, 45(9): 5062-5070
中图分类号: X55   

参考文献

[1] Cowie G, Hedges J. Biochemical indicators of diagenetic alteration in natural organic matter mixtures [J]. Nature, 1994,369:304-307.
[2] Tremblay L, Benner R. Organic matter diagenesis and bacterial contributions to detrital carbon and nitrogen in the Amazon River system [J]. Limnology and Oceanography, 2009,54(3):681-691.
[3] Broek T A B, Bour A L, Ianiri H L, et al. Amino acid enantiomers in old and young dissolved organic matter: Implications for a microbial nitrogen pump [J]. Geochimica et Cosmochimica Acta, 2019,247:207-219.
[4] Wang L, Wu S G, Li Q P, et al. Architecture and development of a multi-stage Baiyun submarine slide complex in the Pearl River Canyon, northern South China Sea [J]. Geo-Marine Letters, 2014,34 (4):327-343.
[5] Ji C X, Yang G P, Chen Y, et al. Contrast the distribution, transformation, and degradation of dissolved and particulate organic matter in the South Yellow Sea, the East China Sea, and its adjacent Kuroshio Current [J]. Marine Chemistry, 2023,248:104210.
[6] Li X L, Liu Z, Chen W. et al. Production and transformation of dissolved and particulate organic matter as indicated by amino acids in the Pearl River Estuary, China [J]. Journal of Geophysical Research: Biogeosciences, 2018,123:3523-3537.
[7] Ji C X, Yang G P, Chen Y, et al. Distribution, degradation and bioavailability of dissolved organic matter in the East China Sea [J]. Biogeochemistry, 2019,142(2):189-207.
[8] Ji C X, Chen Y, Yang G. Seasonal Variation, Degradation, and Bioavailability of Dissolved Organic Matter in the Changjiang Estuary and its Adjacent East China Sea [J]. Journal of Geophysical Research: Oceans, 2021,126(3):e2020JC016648.
[9] Zhang P Y, Yang G P, Chen Y, et al. Temporal and spatial variations of particulate and dissolved amino acids in the East China Sea [J]. Marine Chemistry, 2016,186:133-144.
[10] Fitznar H P, Lobbes J M, Kattner G. Determination of enantiomeric amino acids with high-performance liquid chromatography and pre- column derivatisation with o-phthaldialdehyde and N- isobutyrylcysteine in seawater and fossil samples (mollusks) [J]. Journal of Chromatography A, 1999,832(1/2):123-132.
[11] 陈岩,杨桂朋,纪崇霄,等.南海北部海水中氨基酸的分布及其对溶解有机物降解行为的指示研究 [J].海洋学报, 2017,39(9):58-70. Chen Y, Yang G P, Ji C X, et al. Distributions of amino acids and their indications for the degradation of dissolved organic matter in the northern South China Sea [J]. Haiyang Xuebao, 2017,39(9):58-70.
[12] Kaiser K, Benner R. Hydrolysis-induced racemization of amino acids [J]. Limnology and Oceanography Methods, 2005,3:318-325.
[13] Spyres G, Nimmo M, Worsfold P J, et al. Determination of dissolved organic carbon in seawater using high temperature catalytic oxidation techniques [J]. TrAC Trends in Analytical Chemistry, 2000,19(8):498-506.
[14] Wu J W, Xu F, Liu L, et al. Production, distribution and flux of dimethyl sulfide in the East China Sea and its contribution to atmospheric sulfate aerosols [J]. Environmental Chemistry, 2021,18(6):202-213.
[15] Kaiser K, Benner R. Major bacterial contribution to the ocean reservoir of detrital organic carbon and nitrogen [J]. Limnology and Oceanography, 2008,53:99-112.
[16] Benner R, Amon R M W. The Size-Reactivity Continuum of Major Bioelements in the Ocean [J]. Annual Review of Marine Science, 2015,7(1):185-205.
[17] Liu S, Longnecker K, Kujawinski E B, et al. Linkages Among Dissolved Organic Matter Export, Dissolved Metabolites, and Associated Microbial Community Structure Response in the Northwestern Sargasso Sea on a Seasonal Scale [J]. Frontiers in Microbiology, 2022,13:833252.
[18] Choi H, Yang J E, Kang H, et al. Seasonal dynamics of sinking organic matter in the Pacific Arctic Ocean revealed by nitrogen isotope ratios of amino acids [J]. Marine Chemistry, 253,2023,104252.
[19] Wen Y, Zhang W, Shan B. Amino acids as indicators of seasonal variations in organic matter degradation in surface sediments from a shallow lake [J]. Journal of Environmental Sciences, 2023,131:1-10.
[20] Wei J E, Chen Y, Zhang N, et al. Variability and composition of amino acids and amino sugars in sediment cores of the Changjiang Estuary [J]. Organic Geochemistry, 2022,163:104330.
[21] Dauwe B, Middelburg J J. Amino acids and hexosamines as indicators of organic matter degradation state in North Sea sediments [J]. Limnology and Oceanography, 1998,43(5):782-798.
[22] Dauwe B, Middelburg J J, Herman P M J, et al. Linking diagenetic alteration of amino acids and bulk organic matter reactivity [J]. Limnology and Oceanography, 1999,44(7):1809-1814.
[23] Gao Y, Huang R X, Zhu J, et al. Using the Sigma-Pi diagram to analyze water masses in the northern South China Sea in spring [J]. Journal of Geophysical Research, 2020,125:e2019JC015676.
[24] Deng H X, Huang P, Tanhua T, et al. Observations of the intermediate water exchange between the South China Sea and the Pacific Ocean deduced from transient tracer measurements [J]. Journal of Geophysical Research: Oceans, 2018,123(10):7495-7510.
[25] Wu K, Dai M, Chen J, et al. Dissolved organic carbon in the South China Sea and its exchange with the Western Pacific Ocean [J]. Deep Sea Research Part II: Topical Studies in Oceanography, 2015,122:41-51.
[26] Chen C T A, Wang S L, Wang B J, et al. Nutrient budgets for the South China Sea basin [J]. Marine Chemistry, 2001,75:281-300.
[27] 高新芃,景玉婷,苏荣国,等.南黄海浒苔绿潮暴发区氨基酸时空分布特征 [J].中国环境科学, 2021,41(6):2902-2909. Gao J P, Jing Y T, Su R G, et al. Temporal and spatial distribution characteristics of amino acids in the green tide outbreak area of Ulva prolifera in the South Yellow Sea [J]. China Environmental Science, 2021,41(6):2902-2909.
[28] Nagata T, Kirchman D L. Release of dissolved free and combined amino acids by bacterivorous marine flagellates [J]. Limnology and Oceanography, 1991,36(3):433-443.
[29] Liu K K, Chao S Y, Shaw P T, et al. Monsoon-forced chlorophyll distribution and primary production in the South China Sea: observations and a numerical study [J]. Deep Sea Research Part I: Oceanographic Research Papers, 2002,49(8):1387-1412.
[30] He Q, Zhan H, Cai S, et al. A New Assessment of Mesoscale Eddies in the South China Sea: Surface Features, Three-Dimensional Structures, and Thermohaline Transports [J]. Journal of Geophysical Research: Oceans, 2018,123(7):4906-4929.
[31] Amon R M W, Fitznar H P, Benner R. Linkages among the bioreactivity, chemical composition, and diagenetic state of marine dissolved organic matter [J]. Limnology and Oceanography, 2001,46 (2):287-297.
[32] Middelboe M, Jørgensen N O. Viral lysis of bacteria: an important source of dissolved amino acids and cell wall compounds [J]. Journal of the Marine Biological Association of the United Kingdom, 2006, 86:605-612.
[33] Li X L, Wu K, Gu S, et al. Enhanced Biodegradation of Dissolved Organic Carbon in the Western Boundary Kuroshio Current When Intruded to the Marginal South China Sea [J]. Journal of Geophysical Research: Oceans, 2021,126(11):e2021JC017585.
[34] Cowie G L, Hedges J I. Digestion and alteration of the biochemical constituents of a diatom (Thalassiosira weisflogii) ingested by an herbivorous zooplankton (Calanus pacificus) [J]. Limnology and Oceanography, 1996,41(4):581-594.
[35] Shen Y, Guilderson T P, Chavez F P, et al. Important Contribution of Bacterial Carbon and Nitrogen to Sinking Particle Export [J]. Geophysical Research Letters, 2023,50(11):e2022GL102485.
[36] Kawasaki N, Sohrin R, Ogawa H, et al. Bacterial carbon content and the living and detrital bacterial contributions to suspended particulate organic carbon in the North Pacific Ocean [J]. Aquatic Microbial Ecology, 2011,62:165-176.
[37] Kim T H, Kim G, Shen Y, et al. Strong linkages between surface and deep-water dissolved organic matter in the East/Japan Sea [J]. Biogeosciences, 2017,14(9):2561-2570.
[38] Hou P, Eglinton T I, Yu M, et al. Degradation and Aging of Terrestrial Organic Carbon within Estuaries: Biogeochemical and Environmental Implications [J]. Environmental Science & Technology, 2021,55(15): 10852-10861.
[39] Shen Y, Benner R. Molecular properties are a primary control on the microbial utilization of dissolved organic matter in the ocean [J]. Limnology and Oceanography, 2020,65(5):1061-1071.
[40] Park H, Kim G, Kim S, et al. Significant benthic fluxes of bioavailable dissolved amino acids to the ocean: Results from the East/Japan Sea [J]. Limnology and Oceanography Letters, 2024,9(1):52-61.
[41] Davis J, Kaiser K, Benner R. Amino acid and amino sugar yields and compositions as indicators of dissolved organic matter diagenesis [J]. Organic Geochemistry, 2009,40:343-352.

基金

国家自然科学基金资助项目(42276042,41876082)

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