Significance of a halocline to nutrient cycles in shallow brackish Lake Nakanoumi,Japan

The significance of a halocline for nutrient cycles in a shallow coastal lagoon, Lake Nakanoumi, was investigated. The study was made possible when the northern part of the lagoon was enclosed by polder dikes prior to land reclamation for agricultural purposes. The disappearance of the halocline allowed vertical mixing to extend to the whole depth and vertical gradients in water properties then decreased remarkably. Despite the disappearance of the halocline, dissolved oxygen content of bottom waters decreased considerably during summer months. Summer peaks in inorganic nitrogen and phosphate were still observed after disappearance of the halocline.     

Circulation and the nutrient budget in Myall Lakes

A two-dimensional model is used to study transport of material within Myall Lakes and is coupled to the ocean using a one-dimensional model of Lower Myall River. Runoff from the catchment is calculated from water levels and compares favourably with rainfall assuming an average runoff yield of 28% and a runoff coefficient of 47% for events above the 90th percentile. Most of the runoff enters Bombah Broadwater which is also the only basin connected to the ocean. Intermittent runoff events rapidly displace water from Bombah Broadwater into Boolambayte Lake and from Boolambayte Lake into Myall Lake. Displaced water is mixed within basins by wind-driven circulation within the time scale that levels fall as water drains from the lakes to the ocean. Only 7% of the nutrient load entering Bombah Broadwater becomes resident Myall Lake. About 40% of the nutrient load entering Boolambayte Lake becomes resident in Myall Lake. Median time scales for loss of conservative material entering each basin with the runoff are: 140 days for Bombah Broadwater, 118 days for Boolambayte Lake, and 535 days for Myall Lake. Salinity fluctuates greatly in Bombah Broadwater but is stable in Myall Lake. Material loss from Bombah Broadwater is characterized by many time scales associated with runoff from the catchment and low-frequency changes in ocean water level. Comparison of observed distributions of total nitrogen with simulations indicates that there are sources of total nitrogen in Boolambayte Lake and Myall Lake and sinks of total nitrogen in Bombah Broadwater. There appear to be sinks of total phosphorus throughout the Myall Lakes.     

应用多种生物类群评价白洋淀水环境质量变化

白洋淀是华北平原最大的浅水湖泊。近几十年来,白洋淀上游耗水增加,天然入淀水量急剧减少,使白洋淀水位明显降低;同时,随着淀泊周边农村生活污水的排入,白洋淀发生了严重的富营养化。2017年雄安新区设立,白洋淀环境治理工作的重要性空前提高。近几年通过上游水库和跨流域生态补水,白洋淀水位明显抬升,同时淀中和淀边农村实施了生活污水收集。为了解白洋淀当前水环境状况,对前期补水和治污的效果进行评估,2019年8月对白洋淀水体理化指标及水生生物进行调查,采用水质、浮游植物、浮游动物、底栖动物指标评价白洋淀水环境质量,并与2010年的调查数据进行对比,辅以沉水植物指标评价水体生态状况。结果表明: 白洋淀2019年总磷达到优于Ⅲ类水平,总氮优于Ⅱ类水平,水环境状况比2010年有较大改善。其中,总磷浓度下降了88.6%,总氮浓度下降了83.9%,叶绿素a浓度下降了47.8%,透明度增大了43.4%;浮游动物、底栖动物等生物多样性明显提高,浮游植物密度显著降低,优势种从普遍的重富营养型转变为富营养型;沉水植物清洁型种类分布范围缩小。这说明沉水植物物种评价法不适于白洋淀水环境质量评价,浮游动物多样性评价方法也不适用于当前白洋淀水环境质量评价。早期,由于污染源集中在西部,白洋淀西部水质差于东部;现在,由于自西、北、南多方向补水,淀区的水动力条件发生显著改变,加之西部实施治污工程,淀区水质呈现空间均一化的特点。     

基于遥感技术的鄱阳湖采砂对水体透明度的影响

采砂是一项具有巨大生态影响的经济活动。其引起沉积泥沙的再悬浮,降低水体透明度,减弱水下光环境以及产生一系列的生态影响。旨在利用遥感技术监测鄱阳湖自2001年开始的采砂活动对水体透明度的影响。时间序列的IANDSAT影像用于船只的识别和同期的水体透明度反演,MODIS影像用于估计湖区2000—2005年6—10月期间水体透明度的动态变化。结果显示鄱阳湖北部自2001年以来随着船只数目的增加水体透明度显著下降。结合对船只最终目的地以及船只分布与水体透明度变化一致性等方面的分析,可以确认采砂是引起此区域水体透明度下降的主要原因。夏季频繁发生的长江江水倒灌推动鄱阳湖北部的浑浊水体向南移动,从而扩大采砂的影响范围至鄱阳湖中部,甚至南部。采砂繁荣了地方经济,同时也对鄱阳湖生态系统具有重大的负面影响。平衡经济发展与生态保护之间的关系,将因采砂而造成的负面影响下降到最低限度,使鄱阳湖的各种生态功能全面发挥是当务之急。     

鄱阳湖不同水文连通性子湖水生植被覆盖度对年际水位变化的响应

水位变化是影响水生植被生长的主控环境因子,研究其对不同水文管控模式子湖的水生植被覆盖度的影响具有重要的现实意义.本研究基于谷歌地球引擎(GEE)遥感云计算平台,以鄱阳湖自由连通子湖蚌湖、局部控制子湖大湖池为研究对象,采用像元二分法估算2000-2019年间水生植被生长期的植被覆盖度并分析其时空分异特征,运用Sen+M-...     

Using stable hydrogen and oxygen isotopes to study water movement in soil-plant-atmosphere continuum at Poyang Lake wetland,China

Water movement in the soil-plant-atmosphere continuum (SPAC) has a significant effect on the biogeochemical process in wetlands. This study investigated the water movement in the SPAC in Poyang Lake wetland, which is a protected area with an important ecological function within the Yangtze River basin, under different water-level conditions by analyzing the responses of river, groundwater, soil and plants to precipitation using stable hydrogen and oxygen isotopes. The results show that the stable hydrogen and oxygen isotopic compositions (δ¹⁸O and δD) of soil water decrease with increasing depth due to the near surface evaporation. During the dry season the water-level in Poyang Lake is low, when it rains the influencing depth of precipitation and evaporation on soil water isotopic signatures was 20 cm below the ground surface. The rain water infiltrates into the soil, recharges groundwater and flows to the river. When the water-level in Poyang Lake is low, the Xiu River is recharged by the groundwater, which recharges the soil water by capillary rise. During the flood season, the water-level is high and the water in Poyang Lake reaches or covers the meadows, recharges the groundwater and soil water. In the meantime, the water in Poyang Lake can be recharged by rain water when it rains. During the dry season when it doesn’t rain, plants mainly use groundwater, but soil water is preferred and plants don’t use rainwater directly when it rains. When the lake water-level is extremely low, the plants in Poyang Lake wetland may suffer from water stress, which is harmful for plant growth.     

Interannual and between-site variability in the occurrence of clear water phases in two shallow Mediterranean lakes

It is widely accepted that clear water phases constitute a regular stage in the seasonal succession of plankton in dimictic lakes and reservoirs (i.e. PEG Model). The occurrence of such a phenomenon in Mediterranean shallow lakes is characterised by a marked interannual variability, which makes it difficult to establish reliable predictions on the dynamics and functioning of plankton in these ecosystems. In the present paper we analyse the factors influencing the occurrence of the clear water phases in the two shallow lakes of the Albufera of Adra, a coastal wetland region of south-eastern Spain: Lake Honda and Lake Nueva. Despite their geographical proximity, both lakes depicted large hydrological and limnological differences. Lake Honda is an epigenic and recharge lake that is strongly influenced by the hydrological conditions in its watershed, while Lake Nueva can be classified as a hypogenic and discharge lake and, as such, is less affected by the hydrological regime. In contrast, the morphometry, exposure and fetch of Lake Nueva make this ecosystem especially sensitive to wind forcing. Clear water phases in these shallow lakes were linked with periods of low thermal stability and the dominance of small-edible algae in the phytoplankton community, both of which allowed a Daphnia magna population to grow up and induce the algae collapse by grazing. In Lake Honda, those conditions were met during the spring of 2002 under the influence of intense rainfall-events, while in Lake Nueva the clear water phase was induced in the spring of 2003 by the occurrence of strong and frequent wind events. In both lakes, a relatively high water column thermal stability and the abundance of cyanobacteria early in the spring prevented the development of the Daphnia magna population and the occurrence of the clear water phase.     

Responses to food web manipulation in a shallow waterfowl lake

The effects of fish stock reduction have been studies in 3 Dutch lakes (Lake Zwemlust, Lake Bleiswijkse Zoom and Lake Noorddiep) and 1 Danish lake (Lake Væng) during 4–5 years. A general response id described. The fish stock reduction led in general to a low fish stock, low chlorophyii-a, high transparency and high abunuance of macrophytes. Large Daphnia became abundant, but their density decreased, due to food limitation and predation by fish. The total nitrogen concentration became low due to N-uptake by macrophytes and enhanced denitrification. In Lake Bleiswijkse Zoom the water transparency deteriorated and the clear water state was not stable. The fish stock increased and the production of young fish in summer was high. lear water occurred only in spring. Large daphnids were absent in summer and the macrophytes decreased.In Lake Zwemlust, Lake Væng and Lake Noorddiep the water remained clear during the first five years. In summer of the sixth year (1992) transparency decreased in Lake Zwemlust (with high P-concentration of 1.0 mg P l^-1). Also in Lake Væng (with a low nutrient concentration of 0.15 mg P.^-1) a short term turbid stage (1.5 month) occurred in summer 1992 after a sudden collapse of the macrophytes. Deterioration of the water quality seems to start in summer and seems related to a collapse in macrophytes. At a low planktivorous fishstock (e.g. Lake Væng)thhe duration of the turbid state is shorter. than in presence of a high planktivorous fish biomass (e.g. Lake Zwemlust, and later years of Lake Bleiswijkse Zoom).     

Zinc in water and sediments of two finnish lakes

The distribution of zinc in Lake Vanajavesi and Lake Mallasvesi, South Finland, was determined on the basis of water and sediment studies. Lake Vanajavesi is one of the most polluted of large inland lakes, in Finland. The zinc load comes mainly from industrial sources. Lake Mallasvesi, situated near Vanajavesi, is in almost natural condition. The water samples were taken by a Ruttner sampler. In collecting sediment samples, a freezing technique was used. The results of zinc analyses indicate that, during several winters, zinc has spread with waste water to different parts of L. Vanaja against the main course of flow. A close correlation between sedimentation of zinc and waste discharge from a textile factory was found in the present study.     

Is speciation of demersal fishes in Lake Tanganyika restrained by physical limnological conditions?

Both Lake Malawi and Lake Victoria have many species of offshore demersal cichlids, most of which are stenotopic. In Lake Tanganyika there are fewer, more eurytopic, demersal species. These differences may be the effect of the physical regimes of the lakes. In Lake Victoria there is no permanent anoxic layer. In both the other lakes, water below 250 m depth is permanently anoxic and the seasonal cycle is dominated by upwelling. In Lake Malawi this is mainly derived from intermediate water containing free oxygen. In Lake Tanganyika upwelling involves hypolimnetic water, which may rise to within 80 m of the surface, causing great short-term changes in oxygen concentration over the depth range 50–250 m. This has inhibited the development of deep water species restricted to narrow depth ranges.     

太湖春季沉积物间隙水中磷的分布特征及界面释放的影响

通过对太湖春季不同湖区水体和沉积物间隙水中磷的分布特征研究,探讨了间隙水中磷的释放对上覆水环境的影响。结果表明,颗粒态磷(PP)和溶解态有机磷(DOP)是太湖水体中主要的磷形态,占总磷的58%～95%。不同湖区沉积物间隙水磷的剖面变化可能与生态特征及水动力引起的沉积物-水界面的扰动强度密切相关。湖心和西部沿岸沉积物扰动强烈,致使间隙水中磷含量向上逐渐降底,而梅梁湾和贡湖间隙水磷的垂向变化不大。东太湖和竺山湖沉积物界面间隙水中磷含量偏高,可能是由于表层沉积物的有氧环境使Fe2+被氧化固定下来,并促进了总磷(TP)和溶解态活性磷(DRP)的扩散释放。总体而言,间隙水中各形态磷具有向上覆水体释放的趋势,其中DRP的扩散潜力最大,竺山湖沉积物-水界面DRP扩散通量高达11.42mg.m-2.d-1,表明春季浮游植物的复苏生长对DRP的迫切需求。     

Suitability Modeling of Lake Sturgeon Habitat in Five Northern Lake Michigan Tributaries: Implications for Population Rehabilitation

The availability of lotic spawning, staging, and nursery habitats is considered a major factor limiting the recovery of Lake sturgeon ( Acipenser fulvescens ) in Lake Michigan. Despite efforts to better understand the population biology and habitat use of remnant Lake sturgeon stocks, little information exists on the quantity, quality, and spatial distribution of habitats for riverine life stages. We applied georeferenced habitat information on substrate, water depth, and stream gradient to a Lake sturgeon habitat suitability index in a geographic information system to produce spatially explicit models of life stage–specific habitat characteristics in the Menominee River, Michigan–Wisconsin; the Peshtigo, Oconto, and lower Fox rivers, Wisconsin; and the Manistique River, Michigan. High-quality Lake sturgeon spawning habitat associated with coarse substrates (≥2.1 mm) and moderate- to high-stream gradients (≥0.6 m/km) comprised 1–6% of the available habitat in each system. Staging habitat characterized by water depths greater that 2 m located near potential spawning habitat comprised an additional 17–41%. However, access to a majority of these habitat types (range 30–100%) by Lake sturgeon from Lake Michigan is currently impeded by dams. High-quality juvenile Lake sturgeon habitat associated with finer substrates, lower stream gradients, and a broad range of water depths (i.e., 0.5–8 m) was relatively ubiquitous throughout each system and comprised 69–100% of the available habitat. Our study suggests that efforts to rehabilitate Lake sturgeon populations should consider providing fish passage and creating supplemental spawning habitat to increase reproductive and recruitment potential.     

艾比湖流域生态环境演变与人类活动关系初探

艾比湖流域生态环境演变与人类活动关系初探杨云良阎顺贾宝全陈利军（中国科学院新疆地理研究所,乌鲁木齐８３００１１）ＡＰｒｅｌｉｍｉｎａｒｙＳｔｕｄｙｏｎｔｈｅＲｅｌａｔｉｏｎｓｈｉｐＢｅｔｗｅｅｎｔｈｅＥｎｖｉｒｏｎｍｅｎｔａｌＥｖｏｌｕｔｉｏｎａｎｄ...     

Diversity of extremophilic purple phototrophic bacteria in Soap Lake, a Central Washington (USA) Soda Lake

Culture-based and culture-independent methods were used to explore the diversity of phototrophic purple bacteria in Soap Lake, a small meromictic soda lake in the western USA. Among soda lakes, Soap Lake is unusual because it consists of distinct upper and lower water bodies of vastly different salinities, and its deep waters contain up to 175 mM sulfide. From Soap Lake water new alkaliphilic purple sulfur bacteria of the families Chromatiaceae and Ectothiorhodospiraceae were cultured, and one purple non-sulfur bacterium was isolated. Comparative sequence analysis of pufM, a gene that encodes a key photosynthetic reaction centre protein universally found in purple bacteria, was used to measure the diversity of purple bacteria in Soap Lake. Denaturing gradient gel electrophoresis and subsequent phylogenetic analyses of pufMs amplified from Soap Lake water revealed that a significant diversity of purple bacteria inhabit this soda lake. Although close relatives of several of the pufM phylotypes obtained from cultured species could also be detected in Soap Lake water, several other more divergent pufM phylotypes were also detected. It is possible that Soap Lake purple bacteria are major contributors of organic matter into the ecosystem of this lake, especially in its extensive anoxic and sulfidic deep waters.     

Pelagic zonation of water quality and phytoplankton in the Great Lakes

Analysis of aquatic ecosystem data collected from large water bodies must consider spatial variations. A suite of pelagic survey stations exists for the Laurentian Great Lakes, but little is known about their redundancy. We present a strategy to delineate the lakes into zones based on water quality and phytoplankton biovolume. Water samples were collected from 72 sites in two seasons (spring and summer) from 2007 to 2010 in all five lakes. Integrated samples were analyzed for phytoplankton biovolume and nine water quality parameters. We conducted cluster analysis, principal components analysis and non-metric multidimensional scaling methods for water quality and phytoplankton taxon-specific biovolume for the Great Lakes basin and for each lake separately. There were significant lake-to-lake differences, and based on lake-specific analyses, Lake Superior, Lake Michigan and Lake Erie were each divided into three zones; Lake Huron and Lake Ontario were each grouped into two zones. The zones identified by water quality and phytoplankton provide an understanding of spatial distributions for evaluating monitoring data.     

引水后杭州西湖主要水质参数的因子分析

利用2000年西湖常规监测数据,通过聚类分析选取三个具有代表性的采样点,用因子分析方法探讨了西湖水质各个参数之间的相互影响,结果表明,西湖水质主要受水温和营养盐的影响,各水域由于所处的地理位置和受到钱塘江引水影响程度的不同又有各自的主要水质影响因子,说明引水工程对改善西湖水质具有一定的作用。     

Temporal variation of energy reserves in mayfly nymphs (Hexagenia spp.) from Lake St Clair and western Lake Erie

1. We analysed changes in energy reserves (lipid and glycogen) and length–weight relationships of burrowing mayflies (Hexagenia spp.) in 1997–99 to compare an established population in Lake St Clair with a recovering population in western Lake Erie of the Laurentian Great Lakes. In addition, we measured changes in water temperature and potential food in both water columns and sediments. 2. Although overall mean values of lipid and glycogen levels of Hexagenia nymphs from Lake St Clair and western Lake Erie were not significantly different, there were differences in seasonal patterns between the two lakes. In Lake St Clair, levels were highest in early spring, declined throughout the year, and reached their lowest levels in fall during all 3 years of study. In contrast, levels in western Lake Erie were lower in spring, increased to a maximum in summer, then declined in fall. Seasonal patterns in length–weight relationships were similar to those for lipid and glycogen. 3. Total lipid as a percentage of dry weight did not increase with developmental stage of nymphs until just prior to metamorphosis and emergence from water. However, the major reserve lipid, triacylglycerols, increased systematically with development stage. In the final stage of development, triacylglycerols declined, probably as a result of energy consumption and its conversion to other biochemical components for metamorphosis and reproduction. 4. Indicators of potential food (algal fluorescence in the water column and chlorophyll a and chlorophyll a/phaeophytin ratio in sediments) suggest that Hexagenia in Lake St Clair have a food source that is benthic based, especially in early spring, whereas in western Lake Erie nymphs have a food source that is water column based and settles to the lake bottom during late spring and summer.     

小型湖泊水生植物栽培对轮虫群落结构的影响

为了解水生植物栽培对水环境及轮虫群落结构的影响,于2015年10月至2016年9月,对广州市暨南大学校园两个小型湖泊——明湖和南湖进行了周年调查.明湖无水生植物生长,南湖3—10月有水生植物轮叶黑藻生长,其中6—9月为植物旺盛生长时期.调查发现: 两湖共记录轮虫50种,分属于23个属,其中臂尾轮属、异尾轮属和腔轮属种类较多,均有8种.明湖记录轮虫32种,南湖记录39种. 明湖优势种主要有广布多肢轮虫、暗小异尾轮虫和微型多突轮虫;南湖优势种主要有螺形龟甲轮虫、爱德里亚狭甲轮虫和囊形腔轮虫.明湖轮虫丰度在2015年10月最高,达到3790 ind·L^-1,2016年3月最低,为854 ind·L^-1.南湖轮虫丰度在2015年11月最高,达到3555 ind·L^-1,2016年1月最低,为977 ind·L^-1.相似性分析表明,明湖与南湖水体轮虫群落结构差异显著,其中螺形龟甲轮虫为两湖群落结构差异贡献率最高的物种,其次为广布多肢轮虫.冗余分析表明,明湖轮虫群落结构主要受总磷、叶绿素a、水温的影响;南湖水生植物旺盛生长期,轮虫群落结构受总磷、温度、叶绿素a、深度的影响较大,优势种为底栖的无棘鳞冠轮虫、爱德里亚狭甲轮虫和囊形腔轮虫;水生植物开始生长时期主要受总氮和透明度的影响,优势种为浮游的广布多肢轮虫和等棘异尾轮虫;而无水生植物生长期主要受pH和溶解氧的影响较大,优势种亦为浮游性种,广布多肢轮虫、裂痕龟纹轮虫等.水生植物生长可有效降低N、P营养盐浓度,改善水质,增加空间异质性,支持更多轮虫种类生存,对水域生态系统的稳定具有重要作用.     

近十年太湖生态系统服务功能价值变化评估

理解和把握近年来湖泊生态系统服务功能退化规律的最佳手段是评估其生态系统服务功能价值的变化。以太湖为例,基于近十年来太湖生态系统的科学调查数据,综合运用生态学及经济学方法,对太湖生态系统的四大类功能和11个亚类的服务价值进行了综合评估。研究结果表明,2000年、2003年、2007年和2009年太湖生态系统服务总价值分别为1627.98亿元、1908.68亿元、1503.99亿元和3528.73亿元,保持逐渐升高的趋势,但是在2007年却意外降低。从2000年到2009年太湖生态系统服务功能价值构成发生了一些变化,2000年以供水功能为主体,约占总价值的43%,2003年和2007年变为以航运功能为主体,分别占总价值的41.31%和38.73%,而2009年又变为以旅游功能为主体,约占总价值的52.52%,总体上由供给功能向文化功能转变。航运功能和旅游功能急剧上升而供水功能急剧下降不利于长远发挥的太湖生态服务功能。蓝藻水华的发生可能降低太湖供给功能、支持服务功能和文化服务功能,进而对太湖生态服务的总价值产生负面影响。研究认为太湖生态系统对支持和保护人类社会具有重要的作用,为管理者和决策者有效的保护和管理湖泊生态系统提供了重要的信息。     

应用原生动物群落评价枯水期白洋淀的水质现状

应用PFU微型生物群落监测方法,对长期处于低水位状态下的白洋淀水质进行了综合评价。结果表明,白洋淀水域受府河污水的影响,淀内的内源性污染,对原生动物群落造成了极大的影响。与20世纪90年代的资料相比,淀内中心区4个采样点原生动物的群集种类数(1d)急剧下降,而丰度上升了1．28倍,表明内源性污染对白洋淀水质的影响加剧。