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Stratification of dissolved organic matter in the upper 2000 m water column at the Mariana Trench

机译:玛丽安娜海沟2000 m上方水柱中溶解有机物的分层

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摘要

Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS) and absorbance spectroscopy were utilized to investigate the molecular composition of marine dissolved organic matter (DOM) from the upper 2000 m water column at the Mariana Trench. Molecular indices, calculated based on the relative abundance of 4699 formulas assigned from FT-ICR MS data, showed depth stratification. The degradation index (I-DEG) varied from 0.610 to 0.663 (0.645 +/- 0.014) in the surface layer to 0.668-0.754 (0.722 +/- 0.021) in the deep ocean (below 500 m), indicating that the DOM in the deep layer was more refractory than that of the surface layer. This was confirmed by an increase of modified aromaticity index (AI(mod)) from 0.196 to 0.207 (0.200 +/- 0.003) in the surface layer to 0213-0.225 (0.220 +/- 0.003) at depth. Multivariate analysis based on both bulk molecular parameters and relative abundance of individual formulas showed that the molecular composition of DOM was highly stratified and could be well separated into three groups: the upper layer (5-75 m), the middle layer (200 m) and the deep layer (500-2000 m). In addition, surface-enriched and deep-enriched formulas were identified based on Spearman correlation between relative abundance of individual formulas and depth. The surface-enriched formulas were characterized by higher H/C and lower AI(mod), while deep-enriched formulas showed lower H/C and higher AI(med). Variations in AI(mod) and H/C for these formulas indicated that extracellular release (mainly from primary production) and photochemical processes strongly affected the DOM composition in euphotic zone, while microbial processes likely exerted a tremendous influence on the DOM composition at all depths. Moreover, strong correlations between spectroscopic indices (a(325). S-275(-)295 and S-280(-)400) and FT- ICR MS derived proxies indicated these two approaches can be integrated to provide valuable information on the molecular characterization of open ocean DOM. (C) 2019 Elsevier B.V. All rights reserved.
机译:利用傅里叶变换离子回旋共振质谱(FT-ICR MS)和吸收光谱研究了马里亚纳海沟2000 m水柱上方海洋溶解有机物(DOM)的分子组成。根据从FT-ICR MS数据分配的4699个公式的相对丰度计算出的分子指数显示出深度分层。降解指数(I-DEG)从表层的0.610到0.663(0.645 +/- 0.014)到深海(500 m以下)的0.668-0.754(0.722 +/- 0.021)不等,表明深层比表面层难熔。这可以通过表面层的改性芳香度指数(AI(mod))从0.196增加到深度的0213-0.225(0.220 +/- 0.003)来确认。基于体分子参数和各个分子式的相对丰度的多变量分析表明,DOM的分子组成高度分层,可以很好地分为三类:上层(5-75 m),中层(200 m)深层(500-2000 m)。此外,根据各个公式的相对丰度与深度之间的Spearman相关性,确定了表面富集和深度富集的公式。表面富集的配方的特征在于较高的H / C和较低的AI(mod),而深度富集的配方则具有较低的H / C和较高的AI(med)。这些公式的AI(mod)和H / C的变化表明,细胞外释放(主要来自初级生产)和光化学过程强烈影响了富营养区的DOM组成,而微生物过程可能对所有深度的DOM组成都产生了巨大影响。此外,光谱指数(a(325)。S-27​​5(-)295和S-280(-)400)与FT-ICR MS衍生的代理之间有很强的相关性,这表明可以整合这两种方法以提供有关分子的有价值的信息开放海洋DOM的特征。 (C)2019 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《The Science of the Total Environment》 |2019年第10期|1222-1231|共10页
  • 作者单位

    Southern Univ Sci & Technol, Shenzhen Key Lab Marine Archaea Geoom, Dept Ocean Sci & Engn, Shenzhen 518055, Peoples R China|Nankai Univ, Coll Environm Sci & Engn, Tianjin 300350, Peoples R China;

    Southern Univ Sci & Technol, Shenzhen Key Lab Marine Archaea Geoom, Dept Ocean Sci & Engn, Shenzhen 518055, Peoples R China;

    Woods Hole Oceanog Inst, Dept Geol & Geophys, Woods Hole, MA 02543 USA|Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Ocean & Marginal Sea Geol, Guangzhou 510301, Guangdong, Peoples R China;

    China Univ Petr, State Key Lab Heavy Oil Proc, Beijing 102249, Peoples R China;

    China Univ Petr, State Key Lab Heavy Oil Proc, Beijing 102249, Peoples R China;

    Southern Univ Sci & Technol, Shenzhen Key Lab Marine Archaea Geoom, Dept Ocean Sci & Engn, Shenzhen 518055, Peoples R China;

    Southern Univ Sci & Technol, Shenzhen Key Lab Marine Archaea Geoom, Dept Ocean Sci & Engn, Shenzhen 518055, Peoples R China|Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Shandong, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    DOM; FT-ICR MS; Absorbance spectroscopy; Stratification; Biogeochemical processes;

    机译:DOM;FT-ICR MS;吸收光谱;分层;生物地球化学过程;

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