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太湖是一个典型的大型浅水湖泊,在季风影响下,常年受风浪扰动影响。为了解风浪扰动对太湖水体中微囊藻释放藻毒素(MC)的影响,于2018年7月采集含有微囊藻水华的太湖原水,在中国科学院太湖湖泊生态系统研究站设置了对照、间歇扰动和持续扰动3种处理方式来进行模拟实验,研究水体中藻毒素的变化,实验共持续19 d。结果表明:3种处理方式下,MC浓度的变化趋势一致,1～13 d呈升高趋势,其后均有不同幅度的下降;对照组MC浓度最低,平均值为1.69μg·L-1,显著低于间歇扰动组和持续扰动组(P<0.05);间歇扰动组和持续扰动组MC均值分别为1.81和1.86μg·L-1,两者差异不显著; 3种处理方式下,单位藻细胞MC含量1～7 d持续减小,且各组间差异不显著(P>0.05); 10～19 d各组均有一个先增加后减小的过程,且组间差异均显著(P<0.05),对照组、间歇扰动组和持续扰动组单位藻细胞MC含量均值分别为0.55、1.20和1.98μg·108cells-1;本实验条件下MC与氮磷等因子显著负相关,与水温、SS、Chla等之间显著正相关。本研究表明,扰动可促进水体中藻... 相似文献
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随着人类活动的增强与全球气候变暖的持续,近年来云南湖泊的生态系统功能持续退化,而目前对云南湖泊生态系统的研究还主要集中于单一环境压力的生态效应。以星云湖为研究对象,通过沉积物记录与现代监测资料,识别在湖泊富营养化、气候变化以及人类强烈干扰下硅藻群落结构响应的过程,并甄别驱动群落变化的主要环境压力及其强度。结果显示随着湖泊生产力水平(如沉积物叶绿素a浓度)的增加,硅藻物种组成发生了明显的变化,主成分分析表明了水体富营养化是驱动群落变化的主要环境因子(r=-0.63,P0.001)。简约模型与方差分解的结果表明近200年来(钻孔长度38cm),湖泊营养水平和水动力是驱动星云湖硅藻群落变化的主要环境因子,分别解释了群落变化的18.8%和2.9%;而1951年以后,湖泊营养水平和温度分别解释了硅藻群落结构变化的31.4%和26.8%。研究结果表明了硅藻群落长期变化的主控因子是湖泊营养水平,而人类活动及气候变化等可以通过改变湖泊水动力及湖水温度来驱动硅藻群落的演替,同时抚仙湖-星云湖的连通性也对硅藻群落的演替产生了一定影响。 相似文献
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湖泊富营养化治理的生态工程 总被引：55，自引：3，他引：55
1996年对长春南湖的富营养化实施了生治理工作,调查结果表明,通过收获水生高等植物和鱼产品带出湖体的P量分别为149．6和189．9kg,通过蚌体生长固定的P量为153.4kg,三者合计492.9kg,与湖体会年P输入量大体持平,生态工程运转后,水质明显好转,湖水中的总P浓度逐年下降,浮游植物个体密度减小,种类数增加,生态工程是城市湖泊富营养化治理较为理想的方法。 相似文献
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21世纪以来, 全球森林植被正面临由气候变化加剧、干旱胁迫频发及人类活动干扰等多重压力共同导致的系统性衰退。通过文献分析与多学科证据整合, 全面评述了当前森林衰退的表现特征及成因机制。结果表明: (1)森林衰退的量化评估呈现多尺度特征, 其中生物多样性、土壤含水率、碳储量、热响应、蒸散量及营养元素(磷、钾、铁、铜)浓度等指标均与衰退程度呈负相关, 而地表温度则表现为显著正响应; (2)衰退机制可归纳为内源生理机制(如干旱诱导的水力失衡、碳饥饿及遗传机制)与外源胁迫机制(包括病虫害爆发、地质灾害、人类活动及种间竞争)的共同作用, 其中水力失效与碳代谢紊乱的交互效应被证实为干旱环境森林衰退的主导路径。进一步指出当前研究的局限: ①多尺度模型耦合能力不足; ②水力学失效机制多基于均质化假设, 未区分不同植物类型对栓塞的响应差异; ③人为干扰与自然胁迫的定量分离仍存挑战。未来研究需重点关注全球变化背景下森林衰退的临界阈值判定、早期干旱预警系统构建及干旱后森林恢复力探索等。本研究为理解森林退化过程的级联效应及制定适应性管理策略提供了理论框架。 相似文献
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应用人工神经网络评价湖泊的富营养化 总被引：17，自引：1，他引：17
应用人工神经网络方法,以化学需氧量、总氮、总磷和透明度作为评价参数,经反复尝试,构建了具有４层结构用于评价湖泊富营养化的误差逆传播网络．其输入层有４个神经元,２个隐含层也各有４个神经元,输出层有１个神经元．以太湖富营养化评价标准作为样本模式提供给网络,按照误差逆传播网络的学习规则对网络进行训练,经过３７６８４次学习后,网络达到预先给定的收敛标准．使网络具备了识别湖泊富营养化程度的功能．应用该网络对我国１７个湖泊的富营养化程度进行评价,操作过程简便易行,评价结果切合实际,展示了这种方法的一系列优点． 相似文献
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横岗水库富营养化特征分析 总被引：4，自引：0，他引：4
于2005年5月和11月调查了横岗水库的营养盐、叶绿素a(Chl.a)和浮游植物,对水库富营养化特征进行了分析。5月的总氮(TN)平均浓度为3.810mg·L-1,总磷(TP)平均浓度为0.172mg·L-1,Chl.a平均浓度为17.888mg·m-3,综合营养状态指数(TSIM)为73.3,该水库已达重度富营养化;11月份TSIM下降到55.6,处于轻度富营养化状态,TN和TP平均浓度分别下降到1.302mg·L-1和0.096mg·L-1,Chl.a平均浓度却上升到26.935mg·m-3,Chl.a浓度的上升与氨氮(NH3-N)和正磷(PO4-P)浓度上升以及浮游植物群落组成改变有关。从5月到11月,水库由蓝藻型富营养化水体变为绿藻型富营养化水体。5月浮游植物平均细胞密度高达2.75×108cells·L-1,优势种为美丽平裂藻和银灰平裂藻,其中平裂藻细胞数约占总细胞数的90%。11月浮游植物平均细胞密度降低到1.27×107cells·L-1,平裂藻的优势度下降,只占总细胞数的14.89%,绿藻成为主优势类群,其中栅藻是优势种之一,占总细胞数的11.52%。 相似文献
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汤溪水库的富营养化现状研究 总被引：8，自引：1，他引：8
为了解汤溪水库的富营养化现状,于2000年丰水期和枯水期对该水库的水质和浮游生物分布进行了调查。结果表明,汤溪水库综合营养状态指数(TLI)在30～50之间,属中营养水平。浮游植物丰度为0.81×106～6.57×106cells·L-1,丰水期高于枯水期。浮游植物以蓝藻、绿藻和硅藻为主,其优势种主要为水华微囊藻(Microcystis flos-aquae)、颗粒直链藻(Melosira granulata)、极小直链藻(Melosira minmum)和衣藻(Chlamydomonas sp.)等富营养化指示种。浮游动物丰度为43.25～812.2ind.·L-1,其优势种也多为富营养化指示种,如:螺形龟甲轮虫(Keratella cochlearis)、角突臂尾轮虫(Brachionus angularis)、前节晶囊轮虫(Asplanchna priodonta)和广布中剑水蚤(Mesocyclops leuckarti)。与1984年相比,该水库由硅藻型变为蓝藻型,其营养水平与浮游植物丰度都显著增加。在2000年一次微囊藻水华发生时,水体表层浮游植物丰度高达11.97×106cells·L-1。 相似文献
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青藏高原是中国湿地分布最多的区域,其独特的高寒湿地对区域生态环境安全有着不可或缺的作用。梳理了青藏高原湿地变化的时空特征,基于此,重点分析了气候变化与人类活动对不同类型湿地的影响和作用机制。研究发现：(1)主导不同类型湿地变化的气候因素有差异,影响存在区域异质性。湖泊湿地主要受降水量影响,湖泊湿地在北部扩张、南部缩小的趋势与降水量的空间差异存在较强的一致性;沼泽湿地主要受气温影响,气温升高导致水分蒸发、植被群落演替,沼泽湿地向草地转化,江河源区和若尔盖高原等主要分布区域呈现退化趋势;河流湿地主要受气温影响,气温升高加速河源冰川消融、同时也增大河流蒸散发量,共同作用下河流湿地呈现北部减少、南部增加的趋势。(2)过度放牧、泥炭开采、水利建设等是影响湿地变化的主要人类活动。若尔盖高原同时存在过度放牧、泥炭开采和沟渠建设多重人类活动影响,当地沼泽湿地退化明显;柴达木盆地的人工湿地由于盐业开采迅速扩张。(3)当前研究存在数据可对比性不足、大区域尺度和野外定点持续监测数据缺乏等问题,导致对气候变化与人类活动影响机制研究不够深入。未来应加强高寒湿地定期监测与风险评估,完善高寒湿地生态系统与环境变化和... 相似文献
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- Harmful cyanobacterial blooms are an increasing problem at many locations throughout the world but are rarely reported in aquatic habitats at high latitudes. Shallow lakes are a major feature of northern permafrost landscapes and are likely to experience large‐scale changes in their limnological properties in the future as a consequence of climate warming.
- In the present study, we addressed the question of what preconditions would be necessary to stimulate the growth and dominance of bloom‐forming cyanobacteria in northern fresh waters. We analysed the summer phytoplankton of 18 lakes on eroding permafrost (thaw lakes) and on glacier‐scoured rock (rock basin lakes) in subarctic Quebec, Canada, to determine their phytoplankton community structure and the biomass contribution of cyanobacteria. This survey was complemented with an incubation experiment to evaluate the direct warming and indirect phosphorus (P) enrichment effects of climate change on cyanobacterial bloom development.
- All lakes contained diverse phytoplankton communities, often dominated by chrysophytes, dinoflagellates and chlorophytes. Cyanobacteria were present in all waterbodies, but their contribution to the total community biovolume was highly variable (mean of 8.7%, range 0.1%–47%). Cyanobacterial community biovolumes correlated positively with surface water temperatures, and negatively with dissolved organic carbon, soluble reactive phosphorus, iron and manganese concentrations in the surface waters.
- Phosphorus enrichment of water from a thaw lake resulted in a fourfold increase of chlorophyll a (Chl‐a) and an increase in the cyanobacterial pigments echinenone and zeaxanthin. The phytoplankton counts showed that there was a sharp decrease in diversity (expressed as decline of the Shannon–Wiener index from 1.69 to 0.16), accompanied by a shift to cyanobacterial dominance, notably by the heterocystous, potentially toxic species Dolichospermum cf. planctonicum. Increased temperature led to an initial doubling of cyanobacterial biovolume, followed by the development of a chrysophyte bloom. Combined warming and P enrichment led to reduced phytoplankton biodiversity, with a community composed of cyanobacteria and chrysophytes. There was also a pronounced response by the picophytoplankton community; picocyanobacteria were strongly stimulated by P enrichment, while picoeukaryotes increased in response to warming.
- The current inoculum levels of cyanobacteria in subarctic lakes and their responsiveness to temperature and phosphorus indicate the potential for an abrupt increase in their abundance, accompanied by a decrease in phytoplankton diversity. Ongoing climate change will increase the risk of noxious cyanobacterial blooms in northern lakes and ponds, with potentially negative consequences for higher trophic levels.
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REBECCA MORAN IAN HARVEY BRIAN MOSS HEIDRUN FEUCHTMAYR KEITH HATTON TOM HEYES DAVID ATKINSON 《Freshwater Biology》2010,55(2):315-325
1. Shallow lakes and their ectothermic inhabitants are particularly vulnerable to the effects of climatic warming. These impacts are likely to depend on nutrient loading, especially if the combination of warming and eutrophication leads to severe hypoxia. 2. To investigate effects of realistic warming and nutrient loading on a fish species with high tolerance of warming and hypoxia, we observed population changes and timing of reproduction of three‐spined sticklebacks in 24 outdoor shallow freshwater ecosystems with combinations of temperature (ambient and ambient +4 °C) and three nutrient treatments over 16 months. 3. Warming reduced stickleback population biomass by 60% (population size by 76%) and nutrient‐addition reduced biomass by about 80% (population size 95%). Nutrients and warming together resulted in extinction of the stickleback populations. These losses were mainly attributed to the increased likelihood of severe hypoxia in heated and nutrient‐addition mesocosms. 4. Warming of nutrient‐rich waters can thus have dire consequences for freshwater ectotherm populations. The loss even of a hardy fish suggests a precarious future for many less tolerant species in such eutrophic systems under current climate change predictions. 相似文献
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Jonathan S. Lefcheck David J. Wilcox Rebecca R. Murphy Scott R. Marion Robert J. Orth 《Global Change Biology》2017,23(9):3474-3483
Interactions among global change stressors and their effects at large scales are often proposed, but seldom evaluated. This situation is primarily due to lack of comprehensive, sufficiently long‐term, and spatially extensive datasets. Seagrasses, which provide nursery habitat, improve water quality, and constitute a globally important carbon sink, are among the most vulnerable habitats on the planet. Here, we unite 31 years of high‐resolution aerial monitoring and water quality data to elucidate the patterns and drivers of eelgrass (Zostera marina) abundance in Chesapeake Bay, USA, one of the largest and most valuable estuaries in the world, with an unparalleled history of regulatory efforts. We show that eelgrass area has declined 29% in total since 1991, with wide‐ranging and severe ecological and economic consequences. We go on to identify an interaction between decreasing water clarity and warming temperatures as the primary drivers of this trend. Declining clarity has gradually reduced eelgrass cover the past two decades, primarily in deeper beds where light is already limiting. In shallow beds, however, reduced visibility exacerbates the physiological stress of acute warming, leading to recent instances of decline approaching 80%. While degraded water quality has long been known to influence underwater grasses worldwide, we demonstrate a clear and rapidly emerging interaction with climate change. We highlight the urgent need to integrate a broader perspective into local water quality management, in the Chesapeake Bay and in the many other coastal systems facing similar stressors. 相似文献
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Essie M. Rodgers 《Biology letters》2021,17(10)
The threat of excessive nutrient enrichment, or eutrophication, is intensifying across the globe as climate change progresses, presenting a major management challenge. Alterations in precipitation patterns and increases in temperature are increasing nutrient loadings in aquatic habitats and creating conditions that promote the proliferation of cyanobacterial blooms. The exacerbating effects of climate warming on eutrophication are well established, but we lack an in-depth understanding of how aquatic ectotherms respond to eutrophication and warming in tandem. Here, I provide a brief overview and critique of studies exploring the cumulative impacts of eutrophication and warming on aquatic ectotherms, and provide forward direction using mechanistically focused, multi-threat experiments to disentangle complex interactions. Evidence to date suggests that rapid warming will exacerbate the negative effects of eutrophication on aquatic ectotherms, but gradual warming will induce physiological remodelling that provides protection against nutrients and hypoxia. Moving forward, research will benefit from a greater focus on unveiling cause and effect mechanisms behind interactions and designing treatments that better mimic threat dynamics in nature. This approach will enable robust predictions of species responses to ongoing eutrophication and climate warming and enable the integration of climate warming into eutrophication management policies. 相似文献
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《人类与生态风险评估》2012,18(1):152-167
ABSTRACT Salt lakes are significant landscape features in Australia. The three studied lakes, in particular, are recognized as being of national (Gnotuk) and international significance (Keilambete, Bullenmerri) for their ecological, social, and scientific values. The lake levels have been declining since the mid-1800s, the likely cause being a natural climate-driven decrease in precipitation and increase in evaporation. With the prospect of human-induced climate change further altering regional climate, this article presents a framework and results for assessing the impacts and risks of climate change on lake levels and salinity. A lake water balance model was applied with the inputs of climate observations and modeled future climate variables. The latter are generated from 14 general circulation model simulations used in the Intergovernmental Panel on Climate Change Fourth Assessment Report. The resulting scenarios represent the range of likely outcomes of regional climate under enhanced greenhouse conditions to year 2100. Models project that all lake levels are likely to continue to decline, with the declines for Bullenmerri expected to exceed those of the other two lakes. The salinity in the lakes is likely to increase, with the rate of increase likely to become more rapid over time. Some implications of these findings are discussed. 相似文献
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Pirkko Kortelainen Tuula Larmola Miitta Rantakari Sari Juutinen Jukka Alm Pertti J. Martikainen 《Global Change Biology》2020,26(3):1432-1445
Estimates of regional and global freshwater N2O emissions have remained inaccurate due to scarce data and complexity of the multiple processes driving N2O fluxes the focus predominantly being on summer time measurements from emission hot spots, agricultural streams. Here, we present four‐season data of N2O concentrations in the water columns of randomly selected boreal lakes covering a large variation in latitude, lake type, area, depth, water chemistry, and land use cover. Nitrate was the key driver for N2O dynamics, explaining as much as 78% of the variation of the seasonal mean N2O concentrations across all lakes. Nitrate concentrations varied among seasons being highest in winter and lowest in summer. Of the surface water samples, 71% were oversaturated with N2O relative to the atmosphere. Largest oversaturation was measured in winter and lowest in summer stressing the importance to include full year N2O measurements in annual emission estimates. Including winter data resulted in fourfold annual N2O emission estimates compared to summer only measurements. Nutrient‐rich calcareous and large humic lakes had the highest annual N2O emissions. Our emission estimates for Finnish and boreal lakes are 0.6 and 29 Gg N2O‐N/year, respectively. The global warming potential of N2O from lakes cannot be neglected in the boreal landscape, being 35% of that of diffusive CH4 emission in Finnish lakes. 相似文献
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Tyler L. Lewis Mark S. Lindberg Joel A. Schmutz Patricia J. Heglund Jennifer Rover Joshua C. Koch Mark R. Bertram 《Global Change Biology》2015,21(3):1140-1152
Losses in lake area have been observed for several Arctic and Subarctic regions in recent decades, with unknown consequences for lake ecosystems. These reductions are primarily attributed to two climate‐sensitive mechanisms, both of which may also cause changes in water chemistry: (i) increased imbalance of evaporation relative to inflow, whereby increased evaporation and decreased inflow act to concentrate solutes into smaller volumes; and (ii) accelerated permafrost degradation, which enhances sublacustrine drainage while simultaneously leaching previously frozen solutes into lakes. We documented changes in nutrients [total nitrogen (TN), total phosphorus (TP)] and ions (calcium, chloride, magnesium, sodium) over a 25 year interval in shrinking, stable, and expanding Subarctic lakes of the Yukon Flats, Alaska. Concentrations of all six solutes increased in shrinking lakes from 1985–1989 to 2010–2012, while simultaneously undergoing little change in stable or expanding lakes. This created a present‐day pattern, much weaker or absent in the 1980s, in which shrinking lakes had higher solute concentrations than their stable or expanding counterparts. An imbalanced evaporation‐to‐inflow ratio (E/I) was the most likely mechanism behind such changes; all four ions, which behave semiconservatively and are prone to evapoconcentration, increased in shrinking lakes and, along with TN and TP, were positively related to isotopically derived E/I estimates. Moreover, the most conservative ion, chloride, increased >500% in shrinking lakes. Conversely, only TP concentration was related to probability of permafrost presence, being highest at intermediate probabilities. Overall, the substantial increases of nutrients (TN >200%, TP >100%) and ions (>100%) may shift shrinking lakes towards overly eutrophic or saline states, with potentially severe consequences for ecosystems of northern lakes. 相似文献
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Frazer Matthews‐Bird William D. Gosling Angela L. Coe Mark Bush Francis E. Mayle Yarrow Axford Stephen J. Brooks 《Ecology and evolution》2016,6(1):91-112
To predict the response of aquatic ecosystems to future global climate change, data on the ecology and distribution of keystone groups in freshwater ecosystems are needed. In contrast to mid‐ and high‐latitude zones, such data are scarce across tropical South America (Neotropics). We present the distribution and diversity of chironomid species using surface sediments of 59 lakes from the Andes to the Amazon (0.1–17°S and 64–78°W) within the Neotropics. We assess the spatial variation in community assemblages and identify the key variables influencing the distributional patterns. The relationships between environmental variables (pH, conductivity, depth, and sediment organic content), climatic data, and chironomid assemblages were assessed using multivariate statistics (detrended correspondence analysis and canonical correspondence analysis). Climatic parameters (temperature and precipitation) were most significant in describing the variance in chironomid assemblages. Temperature and precipitation are both predicted to change under future climate change scenarios in the tropical Andes. Our findings suggest taxa of Orthocladiinae, which show a preference to cold high‐elevation oligotrophic lakes, will likely see range contraction under future anthropogenic‐induced climate change. Taxa abundant in areas of high precipitation, such as Micropsectra and Phaenopsectra, will likely become restricted to the inner tropical Andes, as the outer tropical Andes become drier. The sensitivity of chironomids to climate parameters makes them important bio‐indicators of regional climate change in the Neotropics. Furthermore, the distribution of chironomid taxa presented here is a vital first step toward providing urgently needed autecological data for interpreting fossil chironomid records of past ecological and climate change from the tropical Andes. 相似文献
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The effects of the recent warming trend in many northern temperate lakes on the species composition of spring phytoplankton remain poorly understood, especially because a recent change in nutrients has complicated efforts, and previous studies have defined spring according to the calendar. We analysed data from 1979 to 2004 from Lake Müggelsee (Berlin, Germany), using physical and biological parameters to define the spring period. We show that a change in timing of spring plankton events in warm years led to the paradox of lower mean water temperatures during the growth period, favouring cold-adapted diatoms over cyanobacteria, and within the diatoms, some cold-adapted centric forms over pennate forms. Under high P : Si ratios, the increased time between phytoplankton and cladoceran peaks opened a loophole for filamentous cyanobacteria (Oscillatoriales) in warm years to establish dominance after the diatoms, which are silicate limited. Therefore, the warming trend promotes filamentous cyanobacteria, a well-known nuisance in eutrophic lakes, and surprisingly, cold-adapted diatoms. 相似文献
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湖泊富营养化模型研究进展 总被引：25，自引：0，他引：25
自多湖泊富营养化引起人类注意以来,科学家们就设法通过使用数学模型来模拟湖泊富营养化的发生,预测湖泊对不同管理措施的响应,以便批出合理的治理措施。总的来说,湖泊富营养化模型大概经历了以下三个发展阶段：（1）单限制因子模型,如磷模型;（2）多限制因子模型,如浮游植物初级生产力估测模型;（3）生态－动力学模型,它是目前也是以后发展的主不充。随着人们对湖泊生态系统认识的提高和计算机技术的发展,生态与水动力耦合模型、面向对象模型和神经网络模型等具有良好的发展前景。 相似文献