首页> 外文期刊>Elementa: science of the anthropocene >Influence of solar radiation on biogeochemical parameters and fluorescent dissolved organic matter (FDOM) in the sea surface microlayer of the southern coastal North Sea
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Influence of solar radiation on biogeochemical parameters and fluorescent dissolved organic matter (FDOM) in the sea surface microlayer of the southern coastal North Sea

机译:太阳辐射对北海南部沿海海面微层中生物地球化学参数和荧光溶解有机物质(FDOM)的影响

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We investigated the influence of solar radiation on biogeochemical parameters of the sea surface microlayer (SML), including the spectroscopic composition of FDOM, and biotic and abiotic parameters. We calculated the humification index, biological index, and recently produced material index from the ultraviolet spectra to characterize the dynamic environment of the SML. The humification index ranged from 4 to 14 in the SML and 14 to 22 in underlying water (ULW). An inverse relation for this index as a function of solar radiation was observed, indicating photochemical decomposition of complex molecules present in fluorescent dissolved organic matter (FDOM). The biological index (along Leg 2) ranged from 1.0 to 2.0 for the SML and 1.0 to 1.5 for ULW. The index for recently produced material ranged from 0.25 to 0.8 for the SML and 0.5 to 1.0 for ULW. The FDOM enrichment process of the SML was influenced by the photochemical decomposition of highly aromatic-like fluorophores, as indicated by the calculated indices. Fluorescence intensity increased for humic C peaks (0.5 Raman units) in the North Sea samples and for humic M peaks (1.0 Raman units) for Jade Bay. Spearman analysis for FDOM enrichment in the SML as a function of PAR (for Leg 2) showed a weak positive correlation (Rho = 0.676, n = 11, p = 0.022). Abundance of small photoautotrophic cells (Rho = 0.782, n = 11, p = 0.045) and of bacteria (Rho = 0.746, n = 11, p = 0.0082) also showed a positive correlation as a function of PAR. Overall, we found positive trends between the intensity of available light and the response of the constituents within the SML, highlighting the role of the surface microlayer as a distinctive habitat characterized by unique photochemical processes.
机译:我们调查了太阳辐射对海表微层(SML)的生物地球化学参数的影响,包括FDOM的光谱组成以及生物和非生物参数。我们根据紫外线光谱计算了增湿指数,生物学指数和最近产生的物质指数,以表征SML的动态环境。腐殖化指数在SML中为4到14,在下层水(ULW)中为14到22。观察到该指数与太阳辐射成反比关系,表明存在于荧光溶解有机物(FDOM)中的复杂分子发生光化学分解。 SML的生物学指数(沿第2条)范围从1.0到2.0,ULW的范围从1.0到1.5。 SML的最新生产材料的指数范围为0.25至0.8,ULW的指数为0.5至1.0。如计算出的指数所示,SML的FDOM富集过程受高度芳香类荧光团的光化学分解影响。在北海样品中,腐殖质C峰(> 0.5拉曼单位)和翡翠湾腐殖质M峰(> 1.0拉曼单位)的荧光强度增加。 Spearman分析表明SML中的FDOM富集与PAR的关系(对于腿2)显示出弱的正相关性(Rho = 0.676,n = 11,p = 0.022)。小型光合自养细胞(Rho = 0.782,n = 11,p = 0.045)和细菌(Rho = 0.746,n = 11,p = 0.0082)的丰富度也显示出与PAR呈正相关。总体而言,我们发现可用光的强度与SML内各成分的响应之间呈积极趋势,突出了表面微层作为以独特光化学过程为特征的独特生境的作用。

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