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Phytoplankton response to climate changes and anthropogenic activities recorded by sedimentary pigments in a shallow eutrophied lake

机译:浅水富营养化湖泊中沉积色素记录的浮游植物对气候变化和人类活动的响应

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Studies that address the potential effects of climate and anthropogenic activities on lacustrine phytoplankton succession are scarce in the shallow lakes. In the present work, the succession of phytoplankton community inferred from sedimentary pigments has been investigated; the impacts of climate and anthropogenic activities on the succession have been evaluated by the generalized additive models (GAMs) in a shallow eutrophied lake, Lake Chaohu, located eastern China. The results show that phytoplankton succession can be divided into two periods: pre-1960s and post 1960s. The mean values of beta beta Car and Chl a increased after the 1960s at both sites sampled, from 0.013 to 0.359, and 0.013 to 1.382 mu g g(-1), respectively (site C4), and from 0.015 to 0.530, and 0.010 to 0.921 mu g g(-1), respectively (site C14), reflecting significant increases of primary productivity since the 1960s. The percentage of diatoms and dinoflagellates preserved in sediments decreased from similar to 90% to similar to 15% since the 1960s, while cyanobacteria and green algae increased from similar to 5% to similar to 35%, respectively, reflecting the shift of the lake phytoplankton community. This succession was related to construction of the Chaohu Dam in 1963, increasing discharges of anthropogenic N and P into the Lake, and a generally warming environment as reflected by increasing average air temperatures. The results of GAMs showed aquatic total phosphorus (TP) concentration is the dominant contributor to phytoplankton community change, explaining 42.74%, 40.27%, 40.77% and 72.28% of the variance of total algae, cyanobacteria, green algae, and diatoms and dinoflagellates, respectively. The positive impacts of increasing TP concentrations on abundances of total algae, cyanobacteria, and green algae were observed during periods of relatively high TP concentrations since the mid-1970s. The positive responses of total algae, cyanobacteria, green algae and diatoms and dinoflagellates to increasing average air temperatures were observed since the mid-1990s, showing that a generally warmer environment facilitated algae proliferation. (C) 2018 Elsevier B.V. All rights reserved.
机译:在浅湖中,缺乏针对气候和人为活动对湖泊浮游植物演替的潜在影响的研究。在目前的工作中,已经研究了从沉积色素推断出的浮游植物群落的演替。气候变化和人为活动对演替的影响已通过广义加性模型(GAM)进行了评估,该模型位于中国东部巢湖浅水富营养化湖泊中。结果表明,浮游植物的演替可以分为两个时期:1960年代之前和1960年代之后。 1960年代以后,在两个采样点,βbeta Car和Chl a的平均值分别从0.013增加到0.359,从0.013增加到1.382 mu gg(-1)(站点C4),从0.015到0.530,以及0.010分别为0.921 mu gg(-1)(地点C14),反映了自1960年代以来初级生产力的显着提高。自1960年代以来,沉积物中保存的硅藻和鞭毛藻的百分比从相似的90%降低到相似的15%,而蓝细菌和绿藻的比例分别从相似的5%增加到了35%,这反映了浮游植物的变化社区。这一演替与1963年巢湖大坝的建设,向湖中人为氮和磷的排放量增加以及平均气温升高所反映的总体变暖环境有关。 GAMs结果表明,水体总磷(TP)浓度是浮游植物群落变化的主要因素,解释了总藻,蓝藻,绿藻以及硅藻和鞭毛藻的变异的42.74%,40.27%,40.77%和72.28%,分别。自1970年代中期以来,在TP浓度相对较高的时期,观察到TP浓度增加对总藻类,蓝细菌和绿藻数量的积极影响。自1990年代中期以来,观察到总藻类,蓝细菌,绿藻,硅藻和鞭毛鞭毛虫对平均气温升高的积极反应,这表明总体上较暖的环境促进了藻类的繁殖。 (C)2018 Elsevier B.V.保留所有权利。

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