University of North Carolina at Chapel Hill, Institute of Marine Sciences, 3431 Arendell St. Morehead City, NC 28557, United States.
National Oceanic and Atmospheric Administration, National Ocean Service, National Centers for Coastal Ocean Science, Beaufort Laboratory, 101 Pivers Island Rd. Beaufort, NC 28516, United States.
Harmful Algae. 2018 Mar;73:30-43. doi: 10.1016/j.hal.2018.01.003. Epub 2018 Feb 4.
A brown tide bloom of Aureoumbra lagunensis developed in Guantánamo Bay, Cuba during a period of drought in 2013 that followed heavy winds and rainfall from Hurricane Sandy in late October 2012. Based on satellite images and water turbidity measurements, the bloom appeared to initiate in January 2013. The causative species (A. lagunensis) was confirmed by microscopic observation, and pigment and genetic analyses of bloom samples collected on May 28 of that year. During that time, A. lagunensis reached concentrations of 900,000 cells ml (28 ppm by biovolume) in the middle portion of the Bay. Samples could not be collected from the northern (Cuban) half of the Bay because of political considerations. Subsequent sampling of the southern half of the Bay in November 2013, April 2014, and October 2014 showed persistent lower concentrations of A. lagunensis, with dominance shifting to the cyanobacterium Synechococcus (up to 33 ppm in April), an algal group that comprised a minor bloom component on May 28. Thus, unlike the brown tide bloom in Laguna Madre, which lasted 8 years, the bloom in Guantánamo Bay was short-lived, much like recent blooms in the Indian River, Florida. Although hypersaline conditions have been linked to brown tide development in the lagoons of Texas and Florida, observed euhaline conditions in Guantánamo Bay (salinity 35-36) indicate that strong hypersalinity is not a requirement for A. lagunensis bloom formation. Microzooplankton biomass dominated by ciliates was high during the observed peak of the brown tide, and ciliate abundance was high compared to other systems not impacted by brown tide. Preferential grazing by zooplankton on non-brown tide species, as shown in A. lagunensis blooms in Texas and Florida, may have been a factor in the development of the Cuban brown tide bloom. However, subsequent selection of microzooplankton capable of utilizing A. lagunensis as a primary food source may have contributed to the short-lived duration of the brown tide bloom in Guantánamo Bay.
2012 年 10 月下旬,桑迪飓风过后狂风暴雨,古巴关塔那摩湾遭遇了一场干旱,在此期间,夜光藻棕潮在该地区爆发。根据卫星图像和水体浊度测量结果,此次棕潮似乎于 2013 年 1 月开始出现。通过对当年 5 月 28 日采集的水样进行微观观察、色素分析和基因分析,确定了优势种为夜光藻。当时,夜光藻在湾内中部的浓度达到了 90 万个细胞/毫升(以生物体积计为 28ppm)。由于政治因素,无法从湾的北部(古巴)采集样本。2013 年 11 月、2014 年 4 月和 2014 年 10 月对湾的南部进行了后续采样,结果显示夜光藻浓度持续较低,优势种转为聚球藻(4 月时达到 33ppm),而聚球藻在 5 月 28 日的棕潮中只占很小的一部分。因此,与持续了 8 年的拉古纳马德雷湖棕潮不同,关塔那摩湾的棕潮是短暂的,与佛罗里达州印第安河近期的棕潮类似。尽管高盐度条件与德克萨斯州和佛罗里达州泻湖中的棕潮发展有关,但在关塔那摩湾观察到的等盐度条件(盐度 35-36)表明,强烈的高盐度不是夜光藻形成棕潮的必要条件。在观察到的棕潮高峰期,以纤毛虫为主的微型浮游动物生物量很高,纤毛虫的丰度与其他未受棕潮影响的系统相比也很高。正如在德克萨斯州和佛罗里达州的夜光藻棕潮中所观察到的那样,浮游动物对非棕潮物种的优先摄食可能是古巴棕潮爆发的一个因素。然而,随后选择能够将夜光藻作为主要食物来源的微型浮游动物,可能是导致关塔那摩湾棕潮持续时间短暂的一个因素。