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意大利南部伊奥尼亚海塔兰托的马尔皮科洛湾沉积物 - 水界面的氧气、碳和养分交换

Oxygen, carbon, and nutrient exchanges at the sediment-water interface in the Mar Piccolo of Taranto (Ionian Sea, southern Italy).

作者信息

De Vittor Cinzia, Relitti Federica, Kralj Martina, Covelli Stefano, Emili Andrea

机构信息

OGS (Istituto Nazionale di Oceanografia e di Geofisica Sperimentale), Sezione Oceanografia, Via A. Piccard 54, 34151, Trieste, Italy.

Dipartimento di Scienze della Vita, Università degli Studi di Trieste, Via Licio Giorgieri 5, 34128, Trieste, Italy.

出版信息

Environ Sci Pollut Res Int. 2016 Jul;23(13):12566-81. doi: 10.1007/s11356-015-4999-0. Epub 2015 Jul 9.

Abstract

In the shallow environment, the nutrient and carbon exchanges at the sediment-water interface contribute significantly to determine the trophic status of the whole water column. The intensity of the allochthonous input in a coastal environment subjected to strong anthropogenic pressures determines an increase in the benthic oxygen demand leading to depressed oxygen levels in the bottom waters. Anoxic conditions resulting from organic enrichment can enhance the exchange of nutrients between sediments and the overlying water. In the present study, carbon and nutrient fluxes at the sediment-water interface were measured at two experimental sites, one highly and one moderately contaminated, as reference point. In situ benthic flux measurements of dissolved species (O2, DIC, DOC, N-NO3 (-), N-NO2 (-), N-NH4 (+), P-PO4 (3-), Si-Si(OH)4, H2S) were conducted using benthic chambers. Furthermore, undisturbed sediment cores were collected for analyses of total and organic C, total N, and biopolymeric carbon (carbohydrates, proteins, and lipids) as well as of dissolved species in porewaters and supernatant in order to calculate the diffusive fluxes. The sediments were characterized by suboxic to anoxic conditions with redox values more negative in the highly contaminated site, which was also characterized by higher biopolymeric carbon content (most of all lipids), lower C/N ratios and generally higher diffusive fluxes, which could result in a higher release of contaminants. A great difference was observed between diffusive and in situ benthic fluxes suggesting the enhancing of fluxes by bioturbation and the occurrence of biogeochemically important processes at the sediment-water interface. The multi-contamination of both inorganic and organic pollutants, in the sediments of the Mar Piccolo of Taranto (declared SIN in 1998), potentially transferable to the water column and to the aquatic trophic chain, is of serious concern for its ecological relevance, also considering the widespread fishing and mussel farming activities in the area.

摘要

在浅水环境中,沉积物 - 水界面的营养物质和碳交换对确定整个水柱的营养状态起着重要作用。在受到强烈人为压力的沿海环境中,外源输入的强度决定了底栖生物需氧量的增加,导致底层水体中的氧含量降低。有机富集导致的缺氧条件可增强沉积物与上覆水之间的营养物质交换。在本研究中,在两个实验地点测量了沉积物 - 水界面的碳和营养物质通量,一个是高度污染的地点,另一个是中度污染的地点,作为参考点。使用底栖室对溶解物质(O2、DIC、DOC、N - NO3(-)、N - NO2(-)、N - NH4(+)、P - PO4(3-)、Si - Si(OH)4、H2S)进行原位底栖通量测量。此外,采集未扰动的沉积物岩芯,分析总碳和有机碳、总氮以及生物聚合物碳(碳水化合物、蛋白质和脂质),以及孔隙水和上清液中的溶解物质,以计算扩散通量。沉积物的特征是从亚缺氧到缺氧条件,在高度污染的地点氧化还原值更负,该地点还具有较高的生物聚合物碳含量(主要是脂质)、较低的C/N比和通常较高的扩散通量,这可能导致污染物的更高释放。观察到扩散通量和原位底栖通量之间存在很大差异,这表明生物扰动增强了通量,并且在沉积物 - 水界面发生了具有生物地球化学重要性的过程。塔兰托小港(1998年宣布为特殊保护区域)沉积物中无机和有机污染物的多重污染,有可能转移到水柱和水生营养链中,考虑到该地区广泛的捕鱼和贻贝养殖活动,其生态相关性令人严重关切。

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