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大气磷沉积可能会导致湖泊从磷限制重新回到氮限制。

Atmospheric phosphorus deposition may cause lakes to revert from phosphorus limitation back to nitrogen limitation.

机构信息

Biogeodynamics and Biodiversity Group, Centre for Advanced Studies of Blanes, CEAB-CSIC, C/Accés Cala Sant Francesc 14, Blanes, Catalonia E-17300, Spain.

出版信息

Nat Commun. 2012;3:1118. doi: 10.1038/ncomms2125.

Abstract

Recent findings indicate that increased atmospheric deposition of nitrogen of human origin has caused changes in the pattern of ecological nutrient limitation in lakes in the northern hemisphere. An increase in the nitrogen to phosphorus ratio, and hence a shift from pristine nitrogen limitation to human-induced phosphorus limitation of phytoplankton growth, seems to have been driven by deposition of atmospheric nitrogen. These findings challenge the classical paradigm of lake phytoplankton productivity being naturally limited by phosphorus availability. However, atmospheric phosphorus deposition may also be highly relevant. Here we show how dissolved inorganic nitrogen concentration has decreased in the Pyrenean lake district over recent decades, despite there being an increase in deposition of atmospheric nitrogen. This is related to an increased atmospheric phosphorus load in the lake water, as a result of higher atmospheric inputs. These changes are causing phytoplankton to revert from being phosphorus-limited to being nitrogen-limited.

摘要

最近的研究结果表明,人为造成的大气氮沉降增加,已经导致北半球湖泊生态养分限制模式发生变化。氮磷比的增加,以及由此导致的从原始氮限制向人为磷限制的浮游植物生长的转变,似乎是由大气氮沉降驱动的。这些发现挑战了经典的湖泊浮游植物生产力受磷供应自然限制的范式。然而,大气磷沉降也可能非常重要。在这里,我们展示了尽管大气氮沉降增加,但最近几十年来,比利牛斯山区湖泊地区的溶解无机氮浓度是如何下降的。这与由于更高的大气输入,导致湖水中的大气磷负荷增加有关。这些变化正在使浮游植物从磷限制转变为氮限制。

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