Leibniz-Institute of Freshwater Ecology and Inland Fisheries, Müggelseedamm 301, 12587 Berlin, Germany.
J Environ Qual. 2010 Feb 19;39(2):725-33. doi: 10.2134/jeq2009.0122. Print 2010 Mar-Apr.
Feedback between submerged macrophytes and water transparency stabilizing the clear, macrophyte-dominated regime has been described so far for shallow lakes. Based on data of total phosphorus (TP) concentrations, underwater light supply, phytoplankton and submerged macrophyte abundance from narrow, stratified Lake Scharmützelsee (mean depth: 9 m, retention time: 16 yr) of the period 1994-2006 we hypothesize that submerged macrophytes may influence transparency and trophic state in deep lakes. The lake was characterized by summer epilimnion TP concentrations of 38 to 57 mug L(-1), turbid water due to mass development of cyanobacteria, and low abundance of few submerged macrophyte species until 2003. Thereafter, a sudden increase in water transparency was followed by a rapid submerged macrophyte colonization of the littoral down to about 5 m depth corresponding to the depth of a light supply of 3 E m(-2) d(-1). Initially, this recolonization was probably a consequence of decreased turbidity. We argue that the increase of submerged macrophyte coverage from < 10% in 1994 to 2003 to about 24% in 2005-2006 has contributed to the stabilization of the clear-water regime during the subsequent years. This is supported by the fact that earlier shifts to clear-water regimes in 1994 and 2000 without a significant spread of submerged macrophytes were not stable. We discuss potential mechanisms that may have resulted in a positive effect of plants on transparency such as P uptake and immobilization by the dominant rootless macrophyte species Nitellopsis obtusa and Ceratophyllum demersum and other macrophyte-related mechanisms such as increased zooplankton grazing and allelopathy.
目前为止,人们已经描述了浅水湖泊中沉水植物与水透明度之间的反馈关系,这种反馈关系稳定了以沉水植物为主的清水态。基于 1994-2006 年期间来自狭窄分层的沙米茨湖(平均深度:9 m,停留时间:16 年)的总磷(TP)浓度、水下光照、浮游植物和沉水植物丰度的数据,我们假设沉水植物可能会影响深水湖中透明度和营养状态。该湖的特点是夏季上湖层 TP 浓度为 38 至 57 微克/升,由于蓝藻大量繁殖导致水浑浊,以及少数沉水植物物种的丰度很低,直到 2003 年。此后,湖水透明度突然增加,随后沉水植物迅速在沿岸带定居,直到约 5 米深,这一深度对应着 3 E m(-2)d(-1)的光照供应。最初,这种再定殖可能是浊度降低的结果。我们认为,沉水植物覆盖率从 1994 年的<10%增加到 2003 年的 20%左右,到 2005-2006 年增加到约 24%,这有助于在随后几年稳定清水态。事实上,1994 年和 2000 年更早的向清水态的转变,而沉水植物没有显著扩散,这些转变并不稳定。我们讨论了可能导致植物对透明度产生积极影响的潜在机制,例如由优势无根沉水植物 Nitellopsis obtusa 和 Ceratophyllum demersum 吸收和固定磷,以及其他与沉水植物相关的机制,如增加浮游动物的摄食和化感作用。