[Amino acids in marine particulate matters and sediments and their role as indicators for organic matter degradation.]

Q3 Environmental Science 应用生态学报 Pub Date : 2018-09-01 DOI:10.13287/j.1001-9332.201809.035
Bu Zhou, Hua Mao Yuan, Jin Ming Song, Xue Gang Li, Ning Li, Li Qin Duan, Cheng Zhe Ren
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引用次数: 3

Abstract

As important components of marine organic matters especially of organic nitrogen, amino acids play an important role in organic matter cycles owing to their lability. The concentration, composition, and distribution of amino acids have been widely used to indicate the degradation state of organic matters in particulates and sediments of marine. Here, the distribution, influencing factors of amino acids and their role in indicating degradation of organic matters were systematically summarized. Gly, Glu, Ala, and Asp were the major components of amino acids in marine particulates and sediments. The contents of amino acids in the particles and sediments showed a decreasing tendency from the coastal waters to the open sea, and adecreased with the water depth. The lower value of %AA-C/TOC, %AA-N/TN and degradation index (DI) based on changes in the composition of amino acids indicated the higher degradation degrees of organic matters. The reactivity index (RI) and ratios of D-AA and L-AA (D/L) based on non-protein amino acids and D-AA were used to indicate the degradation of organic matter according to the bacterial transformation of amino acids, in which RI value closer to 0, higher D/L, and lower ratios of protein amino acids to non-protein amino acids (Asp/β-Ala and Glu/γ-Aba) indicated the higher degree of degradation in organic matters. The migration and transformation of amino acid were mainly affected by dissolved oxygen, nutrient concentrations, sources of organic matter, depositional environments and microbial activities. Further studies should focus on the synergistic effects of particles and sediments, and also the effects and the specific regulatory roles of microorganisms on amino acids.

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[海洋微粒物质和沉积物中的氨基酸及其作为有机物降解指标的作用。]
氨基酸是海洋有机质尤其是有机氮的重要组成部分,由于其不稳定性,在有机质循环中起着重要作用。氨基酸的浓度、组成和分布已被广泛用于指示海洋颗粒物和沉积物中有机物的降解状态。本文系统综述了氨基酸的分布、影响因素及其在有机质降解中的指示作用。Gly、Glu、Ala和Asp是海洋颗粒和沉积物中氨基酸的主要组成部分。颗粒和沉积物中氨基酸含量从近海向外海呈下降趋势,并随水深的增加而降低。%AA-C/TOC、%AA-N/TN和基于氨基酸组成变化的降解指数DI值越低,表明有机质的降解程度越高。以非蛋白质氨基酸和D- aa为基础的反应性指数(RI)和D- aa与L- aa的比值(D/L)表示细菌对氨基酸的降解,其中RI值接近于0,D/L越高,蛋白质氨基酸与非蛋白质氨基酸(Asp/β-Ala和Glu/γ-Aba)的比值越低,表明有机物的降解程度越高。氨基酸的迁移转化主要受溶解氧、营养物浓度、有机质来源、沉积环境和微生物活动的影响。进一步的研究应关注颗粒和沉积物的协同作用,以及微生物对氨基酸的影响和具体调节作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
应用生态学报
应用生态学报 Environmental Science-Ecology
CiteScore
2.50
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0.00%
发文量
11393
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