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Algal co-limitation by N and P persists after 30 years in Mirror Lake (New Hampshire, USA)

机译:在镜子湖(美国新罕布什尔州新罕布什尔州)后,N和P在N和P持续的藻类合并限制

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The fundamental question of limits to ecosystem productivity is a continually important topic in the field of limnology. Historically, phosphorus (P) has usually been considered the most important limiting nutrient for primary production in freshwater lakes (SCHINDLER 1977). However, the recognition of limitation or co-limitation by other nutrients, in particular nitrogen (N), has generated further interest and understanding about processes that control lake productivity (ELSER et al. 1990). In light of persistent nitrogen pollution in many regions, including the northeastern United States (GALLOWAY & COWLING 2002, ABER et al. 2003), there is even more impetus to examine the potential for nitrogen limitation. Nonpoint sources of nitrogen pollution are considered to be a key factor in eutrophication of inland waters (CARPENTER et al. 1998). Indeed many examples show lakes becoming less limited by nitrogen, or increased productivity due to nitrogen stimulation (JASSBY et al. 1995, BERGSTROM & JANSSON 2006). Several methods were used to asses the nutrient limitation status of Mirror Lake in the early 1970s (GERHART 1975, GERHART & LIKENS 1975). In those studies, N and P co-limited phytoplankton primary production. Mirror Lake is located in New Hampshire, United States (LIKENS 1985) in an area known for moderately high deposition of atmospheric nitrogen (OLLINGER et al. 1993). Long-term studies of chemical mass balances conducted from 1980 to 2000 suggested the possibility that the nutrient limitation status of Mirror Lake may have changed; therefore, we repeated one of Gerhart's experiments with the intent of discovering whether there had been any change in nutrient limitation in Mirror Lake. Specifically we addressed the question of whether N and P were still co-limiting in Mirror Lake. Surprisingly, we again found co-limitation by N and P after 30 years of continued atmospheric nitrogen pollution.
机译:对生态系统生产力的基本问题是湖沼科领域不断重要的话题。从历史上看,磷(P)通常被认为是淡水湖泊中主要生产最重要的限制营养素(Schindler 1977)。然而,识别其他营养素的限制或限制,特别是氮气(n),产生了进一步的兴趣和理解控制湖泊生产率的过程(Elser等,1990)。鉴于许多地区的持续氮污染,包括美国东北部(加洛韦和Cowling 2002,Aber等,2003年),甚至有更多的推动来检查氮气限制的可能性。非点氮污染来源被认为是内陆水域富营养化的关键因素(Carpenter等,1998)。实际上,许多例子显示湖泊因氮气而变得不受限制,或由于氮刺激而增加的生产率(Jassby等,1995,Bergstrom&Jansson 2006)。使用了几种方法来判断20世纪70年代初期(Gerhart 1975,Gerhart&Liskens 1975)的镜湖营养限制状态。在这些研究中,N和P共同限制浮游植物初级生产。镜湖位于美国新罕布什尔(1985年)的新罕布什尔州(比较1985年),该区域在众所周知的大气氮气沉积(Ollinger等,1993)。 1980年至2000年进行的化学质量余额的长期研究表明镜湖的营养限制状态可能发生变化;因此,我们重复了Gerhart的实验,意图发现镜湖中是否存在营养限制的任何变化。具体而言,我们解决了N和P是否仍然共同限制在镜子湖中的问题。令人惊讶的是,在持续的大气氮污染30年后,我们再次发现了N和P的合并限制。

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