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A 200-year perspective on alternative stable state theory and lake management from a biomanipulated shallow lake

机译:从生物操纵的浅湖中寻找替代稳态理论和湖泊管理的200年观点

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Multiple stressors to a shallow lake ecosystem have the ability to control the relative stability of alternative states (clear, macrophyte-dominated or turbid, algaldominated). As a consequence, the use of remedial biomanipulations to induce trophic cascades and shift a turbid lake to a clear state is often only a temporary solution. Here we show the instability of short-term manipulations in the shallow Lake Christina (Minnesota, USA) is governed by the long-term state following a regime shift in the lake. During the modern, managed period of the lake, three top-down manipulations (fish kills) were undertaken inducing temporary (5-10 years) unstable clear-water states. Paleoecological remains of diatoms, along with proxies of primary production (total chlorophyll a and total organic carbon accumulation rate) and trophic state (total P) from sediment records clearly show a single regime shift in the lake during the early 1950s; following this shift, the functioning of the lake ecosystem is dominated by a persistent turbid state. We find that multiple stressors contributed to the regime shift. First, the lake began to eutrophy (from agricultural land use and/or increased waterfowl populations), leading to a dramatic increase in primary production. Soon after, the construction of a dam in 1936 effectively doubled the depth of the lake, compounded by increases in regional humidity; this resulted in an increase in planktivorous and benthivorous fish reducing phytoplankton grazers. These factors further conspired to increase the stability of a turbid regime during the modern managed period, such that switches to a clear-water state were inherently unstable and the lake consistently returned to a turbid state. We conclude that while top-down manipulations have had measurable impacts on the lake state, they have not been effective in providing a return to an ecosystem similar to the stable historical period. Our work offers an example of a well-studied ecosystem forced by multiple stressors into a new long-term managed period, where manipulated clearwater states are temporary, managed features.
机译:浅湖生态系统的多个压力源具有控制替代状态(透明,大型植物为主或混浊,藻类为主)的相对稳定性的能力。结果,使用补救性的生物操作来诱导营养级联反应并使浑浊的湖水转变为清澈的状态通常只是暂时的解决方案。在这里,我们显示了克里斯蒂娜湖(美国明尼苏达州)的短时操纵的不稳定性是由湖政权转移后的长期状态决定的。在现代的,管理的湖泊时期,进行了三项自上而下的操纵(杀死鱼类),导致暂时的(5-10年)不稳定的清水状态。沉积物中记录的硅藻的古生态遗迹以及主要产量(总叶绿素a和总有机碳积累速率)和营养状态(总P)的代表清楚地表明,在1950年代初期,湖中发生了单一的政权转移。随着这一转变,湖泊生态系统的功能以持续的浑浊状态为主导。我们发现,多个压力源促成了政权转移。首先,该湖开始富营养化(由于农业土地利用和/或水禽数量增加),导致初级产量急剧增加。此后不久,1936年修建的大坝有效地使湖的深度增加了一倍,同时区域湿度增加。这导致浮游和弯曲食鱼的增加,减少了浮游植物的放牧。这些因素进一步合谋在现代管理时期增加了浑浊状态的稳定性,从而使切换到清水状态本质上是不稳定的,并且湖泊始终返回浑浊状态。我们得出的结论是,尽管自上而下的操作对湖泊状态产生了可观的影响,但它们并不能有效地提供类似于稳定历史时期的生态系统回报。我们的工作提供了一个经过充分研究的生态系统的例子,该生态系统是由多个压力源强迫进入一个新的长期管理时期的,其中受控的清水状态是临时的,受控的特征。

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