Department of Oceanography, Texas A&M University, College Station, TX 77843-3146, USA.
Mar Environ Res. 2011 Dec;72(5):248-57. doi: 10.1016/j.marenvres.2011.09.007. Epub 2011 Sep 28.
Here we present results of an initial assessment of the impacts of a water diversion event on the concentrations and chemical composition of dissolved organic matter (DOM) and bacterioplankton community composition in Barataria Bay, Louisiana U.S.A, an important estuary within the Mississippi River Delta complex. Concentrations and spectral properties of DOM, as reflected by UV/visible absorbance and fluorescence, were strikingly similar at 26 sites sampled along transects near two western and two eastern areas of Barataria Bay in July and September 2010. In September 2010, dissolved organic carbon (DOC) was significantly higher (568.1-1043 μM C, x=755.6+/-117.7 μM C, n=14) than in July 2010 (249.1-577.1 μM C, x=383.7+/-98.31 μM C, n=14); conversely, Abs254 was consistently higher at every site in July (0.105-0.314) than in September (0.080-0.221), averaging 0.24±0.06 in July and 0.15±0.04 in September. Fluorescence data via the fluorescence index (FI450/500) revealed that only 30% (8 of 26) of the July samples had an FI450/500 above 1.36, compared to 96% (25 of 26) for the September samples. This indicates a more terrestrial origin for the July DOM. Bacterioplankton from eastern sites differed in composition from bacterioplankon in western sites in July. These differences appeared to result from reduced salinities caused by the freshwater diversion. Bacterioplankton communities in September differed from those in July, but no spatial structure was observed. Thus, the trends in bacterioplankton and DOM were likely due to changes in water masses (e.g., input of Mississippi River water in July and a return to estuarine waters in September). Discharge of water from the Davis Pond Freshwater Diversion (DPFD) through Barataria Bay may have partially mitigated some adverse effects of the oil spill, inasmuch as DOM is concerned.
这里我们呈现了一项初始评估的结果,该评估旨在研究美国路易斯安那州巴拉塔里亚湾的水体转移事件对溶解有机物质(DOM)浓度和化学组成以及浮游细菌群落组成的影响。该研究于 2010 年 7 月和 9 月,在巴拉塔里亚湾的两个西部和两个东部地区附近的横截线上,对 26 个站点进行了采样,结果表明 DOM 的浓度和光谱特性(通过紫外/可见吸收和荧光反映)非常相似。2010 年 9 月,溶解有机碳(DOC)浓度显著高于 7 月(7 月为 568.1-1043μM C,x=755.6+/-117.7μM C,n=14;9 月为 249.1-577.1μM C,x=383.7+/-98.31μM C,n=14);相反,7 月每个站点的 Abs254 始终高于 9 月(7 月为 0.105-0.314,9 月为 0.080-0.221),7 月平均为 0.24±0.06,9 月平均为 0.15±0.04。荧光数据通过荧光指数(FI450/500)表明,7 月只有 30%(26 个样本中的 8 个)的样本 FI450/500 高于 1.36,而 9 月则有 96%(26 个样本中的 25 个)。这表明 7 月 DOM 具有更具陆地起源的特征。7 月,来自东部站点的浮游细菌与西部站点的浮游细菌在组成上存在差异。这些差异似乎是由于淡水分流导致的盐度降低所致。9 月的浮游细菌群落与 7 月不同,但未观察到空间结构。因此,浮游细菌和 DOM 的趋势可能是由于水体变化(例如,7 月输入密西西比河水,9 月回归河口水)所致。戴维斯池塘淡水分流(DPFD)通过巴拉塔里亚湾排放的水可能部分减轻了与溢油有关的一些不利影响。