Strangled Waters: First Wave

S. Levy
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Abstract

On a balmy day in June 1955, George Anderson took his sailboat out on Lake Washington, the long stretch of fresh water that separates Seattle from its eastern suburbs. Anderson had recently finished his doctoral research on phytoplankton, and knew the lake well. The water that day looked odd; he noticed a strange brown tinge. So he collected a sample in an empty beer bottle and brought it back to the University of Washington lab where he worked with his mentor, W.T. Edmondson, the ranking authority on the lake. Under the microscope, Anderson and Edmondson found a life form they’d never seen before. It grew in long, narrow chains, striated with lines that separated one cell from the next. They thought this might be a species infamous among limnologists, the cyanobacterium Oscillatoria rubescens. (Cyanobacteria, popularly known as blue-green algae, are in fact distinct from and far more ancient than algae. They appeared more than 3 billion years ago, when the planet was inhabited only by microbes, and were the first organisms to evolve photosynthesis. Their proliferation and release of great volumes of oxygen profoundly changed the chemical makeup of Earth’s atmosphere, making the evolution of complex life possible.) The researchers needed to be sure, so they sent a sample off to an expert, who confirmed their suspicions. O. rubescens signaled deteriorating conditions in Lake Washington. To Edmondson, it also meant an unprecedented opportunity to track the impacts of nutrient overload. O. rubescens had been the harbinger of drastic change in a number of western European lakes. The best-known case was that of Lake Zurich in Switzerland. Fed by Alpine glaciers, Lake Zurich was, until the late 1800s, an expanse of blue known for its abundant populations of whitefish and lake trout, which thrive in deep water. The lake is made up of two basins separated by a narrow passage. In the late nineteenth century towns at the edge of the lower basin, the Untersee, abandoned privies for flush toilets, and began to release their raw sewage into the lake.
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窒息的水:第一波
1955年6月一个和煦的日子,乔治·安德森(George Anderson)驾着他的帆船在华盛顿湖(Lake Washington)上航行。华盛顿湖是一条长长的淡水湖,将西雅图与其东郊分开。安德森刚刚完成了他关于浮游植物的博士研究,对这个湖非常了解。那天的水看起来很奇怪;他注意到一种奇怪的褐色。于是,他在一个空啤酒瓶里收集了一个样本,并把它带回了华盛顿大学的实验室,在那里他和他的导师埃德蒙森(W.T. Edmondson)一起工作,埃德蒙森是该湖的最高权威。在显微镜下,安德森和埃德蒙森发现了一种他们从未见过的生命形式。它生长在长而窄的链上,有条纹,将一个细胞与另一个细胞分开。他们认为这可能是一种在湖沼学家中臭名昭著的物种,蓝藻振荡藻。(蓝藻,俗称蓝绿藻,实际上与藻类不同,而且比藻类古老得多。它们出现在30多亿年前,当时地球上只有微生物,它们是第一批进化出光合作用的生物。它们的扩散和大量氧气的释放深刻地改变了地球大气的化学组成,使复杂生命的进化成为可能。)研究人员需要确定,所以他们把样本寄给了专家,专家证实了他们的怀疑。O. rubescens标志着华盛顿湖环境的恶化。对埃德蒙森来说,这也意味着一个前所未有的机会来追踪营养过剩的影响。O. rubescens曾是许多西欧湖泊剧烈变化的先兆。最著名的例子是瑞士的苏黎世湖。苏黎世湖由阿尔卑斯冰川滋养,直到19世纪末,它还是一片广阔的蓝色湖泊,以其丰富的白鱼和湖鳟鱼种群而闻名,它们在深水中茁壮成长。这个湖由两个由一条狭窄通道隔开的盆地组成。19世纪晚期,位于下游盆地边缘的城镇昂特湖(Untersee)放弃了私人厕所,改为抽水马桶,并开始将未经处理的污水排放到湖中。
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