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Phytoplankton-Specific Response to Enrichment of Phosphorus-Rich Surface Waters with Ammonium, Nitrate, and Urea

机译:浮游植物对富含铵,硝酸盐和尿素的富磷地表水的响应

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摘要

Supply of anthropogenic nitrogen (N) to the biosphere has tripled since 1960; however, little is known of how in situ response to N fertilisation differs among phytoplankton, whether species response varies with the chemical form of N, or how interpretation of N effects is influenced by the method of analysis (microscopy, pigment biomarkers). To address these issues, we conducted two 21-day in situ mesocosm (3140 L) experiments to quantify the species- and genus-specific responses of phytoplankton to fertilisation of P-rich lake waters with ammonium (NH4 +), nitrate (NO3 ), and urea ([NH2]2CO). Phytoplankton abundance was estimated using both microscopic enumeration of cell densities and high performance liquid chromatographic (HPLC) analysis of algal pigments. We found that total algal biomass increased 200% and 350% following fertilisation with NO3 and chemically-reduced N (NH4 +, urea), respectively, although 144 individual taxa exhibited distinctive responses to N, including compound-specific stimulation (Planktothrix agardhii and NH4 +), increased biomass with chemically-reduced N alone (Scenedesmus spp., Coelastrum astroideum) and no response (Aphanizomenon flos-aquae, Ceratium hirundinella). Principle components analyses (PCA) captured 53.2–69.9% of variation in experimental assemblages irrespective of the degree of taxonomic resolution of analysis. PCA of species-level data revealed that congeneric taxa exhibited common responses to fertilisation regimes (e.g., Microcystis aeruginosa, M. flos-aquae, M. botrys), whereas genera within the same division had widely divergent responses to added N (e.g., Anabaena, Planktothrix, Microcystis). Least-squares regression analysis demonstrated that changes in phytoplankton biomass determined by microscopy were correlated significantly (p<0.005) with variations in HPLC-derived concentrations of biomarker pigments (r 2 = 0.13–0.64) from all major algal groups, although HPLC tended to underestimate the relative abundance of cyanobacteria. Together, these findings show that while fertilisation of P-rich lakes with N can increase algal biomass, there is substantial variation in responses of genera and divisions to specific chemical forms of added N.
机译:自1960年以来,向生物圈提供的人为氮(N)的数量增加了两倍。但是,对于浮游植物之间对氮肥的原位响应如何不同,物种响应是否随氮的化学形式而变化,或者分析方法(显微镜,色素生物标志物)如何影响氮效应的解释,知之甚少。为解决这些问题,我们进行了两个为期21天的原位中观宇宙(3140 L)实验,以量化浮游植物对富含P的湖水铵盐施肥(NH4 + ),硝酸盐(NO3 -)和尿素([NH2] 2CO)。浮游植物的丰度是通过细胞密度的显微计数和藻类色素的高效液相色谱(HPLC)分析来估算的。我们发现,虽然有144个单独的分类单元显示,但NO3 -和化学还原的N(NH4 + ,尿素)施肥后,藻类总生物量分别增加了200%和350%。对N的独特反应,包括化合物特异性刺激(Planktothrix agardhii和NH4 + ),仅通过化学还原的N(Scenedesmus spp。,Coelastrum astroideum)增加的生物量,而无响应(Aphanizomenon flos-aquae,陶瓷角叉菜)。无论分类学分析的程度如何,主成分分析(PCA)捕获了实验组合中53.2–69.9%的变化。物种水平数据的PCA显示,同类生物对施肥制度表现出共同的反应(例如,铜绿微囊藻,弗洛斯水藻,葡萄孢菌),而同一分区内的属对添加的N的反应却大相径庭(例如,鱼腥藻) ,Planktothrix,微囊藻)。最小二乘回归分析表明,通过显微镜确定的浮游植物生物量变化与HPLC衍生的生物标志物色素浓度( r 2 ==)显着相关(p <0.005)。 0.13–0.64),尽管HPLC倾向于低估了蓝藻的相对丰度。在一起,这些发现表明,尽管富磷湖泊中的氮肥可以增加藻类生物量,但对添加的氮的特定化学形式,属和种的响应存在很大差异。

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