College of Marine Science, University of South Florida, 140 Seventh Avenue South, St. Petersburg, Florida 33701, United States.
Environ Sci Technol. 2013 Sep 3;47(17):9651-9. doi: 10.1021/es401761h. Epub 2013 Aug 21.
The Deepwater Horizon oil spill is unparalleled among environmental hydrocarbon releases, because of the tremendous volume of oil, the additional contamination by dispersant, and the oceanic depth at which this release occurred. Here, we present data on general toxicity and mutagenicity of upper water column waters and, to a lesser degree, sediment porewater of the Northeastern Gulf of Mexico (NEGOM) and west Florida shelf (WFS) at the time of the Deepwater Horizon oil spill in 2010 and thereafter. During a research cruise in August 2010, analysis of water collected in the NEGOM indicated that samples of 3 of 14 (21%) stations were toxic to bacteria based on the Microtox assay, 4 of 13 (34%) were toxic to phytoplankton via the QwikLite assay, and 6 of 14 (43%) showed DNA damaging activity using the λ-Microscreen Prophage induction assay. The Microtox and Microscreen assays indicated that the degree of toxicity was correlated to total petroleum hydrocarbon concentration. Long-term monitoring of stations on the NEGOM and the WFS was undertaken by 8 and 6 cruises to these areas, respectively. Microtox toxicity was nearly totally absent by December 2010 in the Northeastern Gulf of Mexico (3 of 8 cruises with one positive station). In contrast, QwikLite toxicity assay yielded positives at each cruise, often at multiple stations or depths, indicating the greater sensitivity of the QwikLite assay to environmental factors. The Microscreen mutagenicity assays indicated that certain water column samples overlying the WFS were mutagenic at least 1.5 years after capping the Macondo well. Similarly, sediment porewater samples taken from 1000, 1200, and 1400 m from the slope off the WFS in June 2011 were also highly genotoxic. Our observations are consistent with a portion of the dispersed oil from the Macondo well area advecting to the southeast and upwelling onto the WFS, although other explanations exist. Organisms in contact with these waters might experience DNA damage that could lead to mutation and heritable alterations to the community pangenome. Such mutagenic interactions might not become apparent in higher organisms for years.
墨西哥湾深海地平线石油泄漏是环境中碳氢化合物释放的空前事件,这是由于石油的巨大体积、分散剂的额外污染以及该释放发生的海洋深度。在这里,我们提供了 2010 年深海地平线石油泄漏期间及之后墨西哥湾东北部(NEGOM)和西佛罗里达大陆架(WFS)上地表水和沉积物孔隙水的一般毒性和致突变性数据。在 2010 年 8 月的一次研究航行中,对 NEGOM 采集的水样进行分析表明,在基于 Microtox 测定的 14 个站位中的 3 个(21%)、基于 QwikLite 测定的 13 个站位中的 4 个(34%)和基于 λ-Microscreen Prophage 诱导测定的 14 个站位中的 6 个(43%)水样具有细菌毒性。Microtox 和 Microscreen 测定表明,毒性程度与总石油烃浓度相关。通过对 NEGOM 和 WFS 的 8 次和 6 次巡航进行了长期监测。到 2010 年 12 月,墨西哥湾东北部的 Microtox 毒性几乎完全消失(8 次巡航中有 3 次阳性站位)。相比之下,QwikLite 毒性测定在每次巡航中均呈阳性,通常在多个站位或深度上,表明 QwikLite 测定对环境因素更为敏感。Microscreen 致突变性测定表明,在 Macondo 井封盖至少 1.5 年后,WFS 上方的某些水柱样品仍具有致突变性。同样,2011 年 6 月从 WFS 斜坡 1000、1200 和 1400 米处采集的沉积物孔隙水样也具有高度遗传毒性。我们的观察结果与来自 Macondo 井区的一部分分散油向南东南方向漂移并涌向上佛罗里达大陆架的情况一致,尽管还有其他解释。与这些水接触的生物可能会经历 DNA 损伤,从而导致突变和对群落泛基因组的遗传改变。这种致突变的相互作用可能在多年后才会在高等生物中显现出来。