阳宗海中紫色非硫光合细菌的生态研究

为得到高原深水湖泊中的微生物生态分布信息,运用统计学软件,在2002年对阳宗海中的紫色非硫光合细菌的数量进行了数学分析。影响湖泊中PNSB数量分布的主要因素是水平位点、深度和采水期,溶氧、温度、透明度、COD和叶绿素a含量等环境因子对PNSB数量也有影响。各环境因子如叶绿素a含量和透明度之间也有相关性,对其进行了分析并计算出环境因子之间关系的一元回归方程。     

武汉东湖磷细菌种群结构的研究

对东湖磷细菌种群结构研究结果表明,至少有芽孢杆菌属,微球菌属,不动细菌属,气单胞菌属,产碱杆菌属,贝内克氏菌属,无色杆菌属,短杆菌属,肠杆菌属,黄杆菌尾,微杆菌 ,假单胞菌属,沙雷氏菌属,黄单胞菌属和发酵单胞菌属15个属的不同菌株以其对有机磷,无机磷化合物的分解能力推动着湖泊中磷的循环,其中以芽孢杆菌属和微球菌属居于明显的优势。磷细菌在湖泊中的分布随水质的污染程度和磷化合物含量的不同而表现有明显的判别：在数量上,湖泥高于湖水,污染较重的I站高于水质较好的II站,在调查期间,有机磷细菌数在多数情况下亦高于无机磷细菌,在种群结构上,1站湖水中种类最多,Ⅲ站次之,II站最少。     

云南阳宗海酵母菌种群结构及产胞外酶测试北大核心CSCD

【目的】研究阳宗海酵母菌种群结构,分析生物因子及非生物因子对酵母菌种群分布的影响;测试阳宗海酵母菌产胞外酶活性。【方法】水样用醋酸纤维素滤膜过滤,原位培养分离酵母菌;梯度稀释法分离土样和底泥样品;对分离得到的菌株进行DNA提取和测序,分析26S rDNA的D1/D2区域,并结合形态及生理生化指标进行鉴定;用产酶筛选培养基对分离得到的酵母菌进行产胞外酶活性测试。【结果】共分离得到201株酵母菌,鉴定分属于15个属48个种,其中包括10个潜在的新种;普鲁兰类酵母(Aureobasidium pullulans),库德里阿兹威氏毕赤酵母(Pichia kudriavzevii),胶红酵母(Rhodotorula mucilaginosa),Cryptococcus podzolicus是优势种;15.9%的酵母菌具有产胞外酶活性,主要是脂肪酶和淀粉酶。【结论】阳宗海酵母菌有较为丰富的多样性,人为活动对阳宗海酵母菌分布影响较大,其次浊度、电导率也是影响酵母菌种群分布的重要因素;阳宗海产胞外酶酵母菌可能参与湖泊生态系统的自然循环。     

氧化塘中细菌种群组成动态

对武汉地区氧化塘中的细菌数量、细菌种类、种群组成、优势种及群落多样性进行了初步研究。从氧化塘中分离的细菌经鉴定属于12个属,主要有假单胞菌属(Pseudomonas)、棒杆菌属(corynebacterium)、无色杆菌属(Achromobacter)和微杆菌属(Microbacterium),其它菌属是芽孢杆菌属(Bacillus)、色杆菌属(Chromobacterium)、短杆菌属(Brevibacterium)、葡萄球菌属(Staphylococcus)、微球菌属(Micrococcus)、黄杆菌属(Flavobacterium)、埃希氏菌属(Escherichia)和链球菌属(Streptococcus)。在5个小塘中,细菌数量、种群组成和群落多样性指数都有不同,这与各塘的污染程度有关。由此,多样性指数可用于监测氧化塘的净化效果。     

贫营养湖泊花神湖和紫霞湖浮游细菌群落结构分析

以南京市花神湖和紫霞湖两个贫营养型湖泊为研究对象,通过构建花神湖和紫霞湖16S rRNA基因克隆文库探讨了浮游细菌群落结构组成的变化。结果表明,花神湖和紫霞湖两湖泊水体中浮游细菌群落结构相似,主要隶属于放线菌门(Actinobacteria)、蓝藻门(Cyanobacteria)、α-变形菌门(Alphaproteobacteria)、β-变形菌门(Betaproteobacteria)、杆菌门(Bacteroidetes)、浮霉菌门(Planctomycetes)、疣微菌门(Verrucomicrobia)和芽单胞菌门(Gemmatimonadetes),其中放线菌门(Actinobacteria)、蓝藻门(Cyanobacteria)、β-变形菌门(Betaproteobacteria)是优势细菌类群。两个湖泊水体中75%的细菌与GenBank中已有的未培养细菌同源性高于97%,同时在两个克隆文库中还发现了6个淡水细菌新类群。通过对低纬度区域贫营养型湖泊浮游细菌群落结构的分析,加深了我们对浮游细菌多样性的了解,表明湖泊浮游细菌多样性有待进一步认识。     

大水面放养水葫芦对富营养化湖泊水体可培养细菌群落结构的影响

【目的】了解大水面放养水葫芦对富营养化湖泊水体可培养细菌群落结构和多样性的影响。【方法】采用稀释平板法,分别对云南滇池紫根水葫芦放养区(ZW)、野生型普通水葫芦放养区(PW)、未放养水葫芦对照区(CK)水体中细菌进行分离,并对其16S r RNA序列进行分析。【结果】分别从ZW、PW、CK 3种水体分离得到54、49、40株菌落形态差异的细菌,Shannon-Wiener多样性指数分别为3.17、3.07、2.73,细菌数量分别为1.35×107、8.35×106、2.70×106 CFU/L。16S r RNA序列分析表明,ZW、PW、CK 3种水体可培养细菌主要包括变形菌门α亚群(Alphaproteobacteria,35.1%、32.4%和40%)、放线菌门(Actinobacteria,18.9%、32.4%和20%)、变形菌门β亚群(Betaproteobacteria,13.5%、5.9%和16.0%)、变形菌门γ亚群(Gammaproteobacteria,13.5%、14.6%和12.0%)、拟杆菌门(Bacteroidetes,13.5%、8.8%和8.0%)和厚壁菌门(Firmicutes,2.7%、5.9%和4.0%)。在属的水平上,3种水体仅有鞘氨醇盒菌属(Sphingopyxis)、红细菌属(Rhodobacter)、黄色杆菌属(Xanthobacter)、新鞘脂菌属(Novosphingobium)、鞘氨醇单胞菌属(Sphingomonas)、假单胞菌属(Pseudomonas)、微杆菌属(Microbacterium)、链霉菌属(Steptomyces)、黄杆菌属(Flavobacterium)、芽孢杆菌属(Bacillus)等10个属的细菌为共有菌属。【结论】大水面放养水葫芦提高了富营养化湖泊水体中可培养细菌的多样性,改变了细菌的群落结构。     

云南湖泊鱼类的区系及其类型分化

云南境内约有十二个大小湖泊,由于多数分布在高原面上,故习惯称为高原湖泊。这些湖泊按地理位置可分为东、南、西、北四群。东部湖群有滇池(昆明湖)、抚仙湖、阳宗海、星云湖、杞麓湖等,坐落在昆明弧上,其中除滇池属金沙江水系外,其余均归南盘江(西江上游);西部湖群包括洱海、茨碧湖、剑湖、莫汉沼等,皆注入澜沧江;滇北之程海(黑乌海)属金沙江水系;南部湖群计有异龙湖和大屯海,都属南盘江水系。     

辉腾锡勒草原干涸湖泊中氨氧化微生物群落结构分析

【目的】以内蒙古辉腾锡勒草原九十九泉湿地为对象,研究湖泊干涸过程中氨氧化微生物的群落结构及其变化。【方法】通过MPN-PCR定量测定氨氧化古菌(AOA)和氨氧化细菌(AOB)的数量;构建amoA基因克隆文库,进行系统发育分析;结合土壤环境因子,探讨湿地退化过程中影响氨氧化微生物的潜在因素。【结果】依湖泊湿地退水梯度的不同样点中,有75%的样点AOB的数量高于AOA,AOB与AOA的数量比率为0.3-18.1。从湖心到湖岸草原带,AOA和AOB的数量有明显增加,但生物多样性呈降低趋势,二者没有呈现正相关。研究发现,AOB的数量与土壤中NH 4+-N的变化存在良好响应。系统发育分析显示,退化湖泊湿地AOA克隆序列均来自于泉古菌门(Crenarchaeota);AOB的amoA基因的克隆序列大部分与亚硝化单胞菌属(Nitrosomonas)有一定同源性,较少部分与亚硝化螺菌属(Nitrosospira)有一定同源性。【结论】湖泊退水过程增加了湿地土壤氨氧化微生物的数量,而氨氧化微生物的种群丰度有所降低。AOA和AOB群落对湖泊湿地的退化过程做出了响应,其中AOB的响应较为明显,氧化条件和土壤铵浓度的改变可能是促成这种响应的重要原因。     

典型高原湖滨带底泥细菌群落结构及多样性特征

【背景】高原湖泊的富营养化日趋严重,而湖滨带作为湖泊的保护屏障对外源污染物具有拦截净化等作用,水环境变化则会对底泥细菌产生深刻影响。【目的】探究高原湖滨带底泥细菌群落结构特征及与水体富营养化之间的联系。【方法】基于16S rRNA基因高通量测序技术分析了阳宗海南岸湖滨带8个不同样点的底泥细菌群落结构及多样性,并结合样品水体环境因子,采用主成分分析(PCA)和冗余分析(redundancy analysis,RDA)探讨了水体富营养化对底泥细菌群落结构及丰富度的影响。【结果】湖滨带底泥细菌与水体富营养化程度存在响应关系,在水体富营养化程度高的区域(S3)细菌丰富度较高,操作分类单元(operationaltaxonomicunits,OTU)高达1473。反之,在富营养化程度低的区域(S1)细菌丰富度较低,OTU为730。阳宗海南岸湖滨带底泥中主要优势菌门为变形菌门(Proteobacteria)和绿弯菌门(Chloroflexi),含有少量的放线菌门(Actinobacteria)、酸杆菌门(Acidobacteria)和厚壁菌门(Firmicutes);绿弯菌门(Chloroflexi)与水体富营养化程度具有相关性,在中度富营养化区域,绿弯菌门(Chloroflexi)的比重高达44.1%,而在轻度富营养化区域绿弯菌门(Chloroflexi)的比重仅为15.6%。通过环境因子分析发现,阳宗海湖滨底泥细菌受总磷(TP)、叶绿素a (Chla)和总氮(TN)影响较强。【结论】研究结果明确了高原湖泊湖滨带底泥细菌种群的结构、变化特征及其对于水体富营养化的响应,加深了高原湖泊底泥细菌的了解,为高原湖泊水体富营养化的防治提供理论基础。     

湖光岩玛珥湖可培养浮游细菌的BOX-PCR图谱及生物多样性分析

玛珥湖是一类具有独特地质构造特征的火山口湖泊, 目前国内外对玛珥湖内微生物多样性的研究还鲜有报道。为了解具有典型玛珥特征的湖光岩湖泊中可培养浮游细菌的种群资源特征, 采用盒式PCR (BOX-PCR) 筛选技术, 通过通用贫营养和原位湖水培养基研究在冬夏两季各水层内获得的可培养细菌种群的差异。结果表明: 不同培养基在不同水层上表现的细菌数量的变化相一致, 为夏季的5 m>1 m>13 m, 冬季的1 m>5 m>13 m, 变形菌占据优势地位, 其它为放线菌、厚壁菌和拟杆菌; 两类培养基上所获培养菌BOX-PCR图谱的多样性相似, 但菌群结构不同; 而细菌多样性在季节上的变化表现为冬季高于夏季, 这与相关湖泊内细菌微生物多样性在夏季会发生减少的特点相似; 相同季节同一水层上不同培养基上获得的培养菌门类不同, 表明此类通用性培养基在培养该环境微生物中的局限。研究的结果为探讨此类型湖泊微生物多样性与环境的关系及分离该环境下特定微生物菌株提供参考。     

太湖湖滨带生态系统健康评价

根据湖滨带生态系统的特点,运用综合健康指数法建立了湖滨带生态系统健康评价体系,由目标层、准则层、指标层构成,其中准则层由湖滨带水质状况、底泥状况、植被状况、其它生物状况(浮游动物、浮游植物、底栖动物)、岸带物理状况5项组成,指标层由总氮、总磷、溶解氧、挺水植物覆盖率等15项指标构成。采用专家打分法、熵值法分别确定了准则层、指标层的权重系数。对太湖湖滨带33个点位进行了采样分析,并进行无量纲化处理后应用到所建立的评价体系中。评价结果显示33个点位中为"很健康"、"健康"、"亚健康"、"疾病"、"严重疾病"的分别占0%、24.2%、21.2%、51.5%及3.0%,也即超过一半的点位处于"疾病"状态。只有东太湖刚刚超过"健康"分数的下限,东部沿岸、贡湖、南部沿岸均处于"亚健康"状态,而梅梁湾、竺山湾、西部沿岸属于"疾病"状态,且竺山湾的生态健康状态最差。该评价结果与太湖湖滨带各分区的实际调查情况相符合,评价方法可靠性、可行性较强,可为其它湖泊湖滨带的生态系统健康评价提供一定的参照。     

Oxygen concentration profiles in sediments of two ancient lakes: Lake Baikal (Siberia,Russia) and Lake Malawi (East Africa)

Oxygen concentration profiles have been measured, by means of with microelectrodes in sediments of Lake Baikal and Lake Malawi, along transects allowing to give a survey of two major ancient Rift lakes: Lake Baikal (Eastern Siberia) and Lake Malawi (East Africa), along depth transects in the constitutive basins of the lakes and/or of relevant depths with regard to oxygen (including including the deepest point, 1680 m, in Lake Baikal). Sediment oxygen penetration depths (SOPs) display very different patterns, depending on the lake in the two lakes. In Lake Baikal, SOPs are variable, show no significant relationship with bathymetric depth and are surprisingly deep on Akademichesky ridge (> 50.0 mm), emphasizing the distinctive feature of this region in the lake. While the Selenga river is an important source of eutrophication, the similarity of SOP-values in the Selenga shallow with those of most other sites suggests either a dilution of organic material by allochthonous matter, or a strong south-to-north transport of particles. In Lake Malawi, available oxygen is restricted to a maximum of three millimetres of the sediment, and there is a negative relationship with bathymetric depth, as a result of a steady decline of oxygen concentration with depth through the water column. Amongst the few parameters known to affect SOPs, the oxygen consumption by the sediment seems the most significant in both lakes. SOP-values furthermore confirm differences in the trophic status of Baikal and Malawi, respectively. The importance of oxygen as a factor likely to create ecological segregation for benthic organisms is discussed. Lake Malawi offers possibilities of bathymetric segregation but no vertical segregation in the sediment. In contrast, no bathymetric segregation related to oxygen is possible in Lake Baikal, but vertical segregation in the sediment is very likely. This revised version was published online in July 2006 with corrections to the Cover Date.     

星云湖硅藻群落响应近现代人类活动与气候变化的过程

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。     

博斯腾湖小湖区湿地景观变化特征研究

以博斯腾湖小湖区为研究区,采用5个不同时期的Landsat影像为主要数据源,运用景观转换系数和重心迁移模型对1996~2015年研究区湿地景观变化进行分析,以揭示博斯腾湖小湖区的景观变化类型与景观的重心变化特征。结果显示:(1)近20年有地表水的湿地与旱地的重心变化强烈,1996~2001年有地表水的湿地重心变化达到最大值,向西南迁移10.57km,旱地重心变化也达到最大值,向东南迁移8.78km。(2)近20年明水与旱地的重心迁移呈顺时针向心偏移。(3)稳定型景观是研究区的主要构成类型,占总类型的89.72%,非稳定型景观保持在总类型的11.28%,研究区湿地景观变化逐渐呈稳定趋势。研究表明,气候因素、湖泊水位和区域湿地保护措施是影响研究区湿地景观变化的主要驱动因素。     

基于水质管理目标的博斯腾湖生态水位研究

人类开发活动导致湖泊生态功能严重退化,研究湖泊生态水位对于维持湖泊生态系统健康意义重大。针对博斯腾湖化学需氧量(COD)浓度较高的水环境现状,分析博斯腾湖水位和COD浓度关系,研究提出基于水质管理目标的生态水位,以期为博斯腾湖水资源、水环境管理提供参考。结果表明,博斯腾湖水位与水体COD浓度显著负相关,但由于COD浓度空间差异较大以及影响因素不唯一,水位与COD浓度两者之间曲线估计结果不理想。为实现博斯腾湖COD浓度小于20 mg/L的水质管理目标,引入累计水位概念进行统计分析得到两个特征水位:所有COD浓度大于等于20 mg/L的数据对应水位的平均值为1046.02 m,该水位在历史丰水期水位的频率为60.83%,可作为最小生态水位;所有COD`浓度小于等于20 mg/L的数据对应水位的平均值为1046.4 m,该水位在历史丰水期水位的频率为44.70%,可作为适宜生态水位。适宜生态水位1046.4 m与已有研究成果基本相符,博斯腾湖在1046.4 m时既有利于水质管理,也可保障湖泊整体生态系统健康。     

An ecological study of two shallow,equatorial lakes: Lake Mburo and Lake Kachera,Uganda

Lake Mburo and Lake Kachera are shallow, eutrophic lakes in mid‐western Uganda. Lake Mburo recorded higher values of Secchi and eutrophic depths and lower extinction coefficient (k) values. The lakes showed a ‘red shift’ phenomenon in maximum light transmission. The average values of electrical conductivity in Lake Mburo and Lake Kachera were 136 and 244 μS cm^?1, respectively. The pH values indicated high photosynthetic activity. Dissolved oxygen concentration averaged 6.9 and 7.8 mg l^?1 in Lake Mburo and Lake Kachera, respectively. The lakes had high total nitrogen (TN) : total phosphorus (TP) ratios averaging 200 and 280 in Lake Mburo and Lake Kachera, respectively. The lakes are dominated by cyanobacterial blooms that reduce light penetration to less than 1 m. Lake Mburo had a lower algal biomass than Lake Kachera. Chlorophyll a concentrations correlated positively (r = 0.73, P < 0.05) with the extinction coefficient in Lake Mburo but not in Lake Kachera. The correlations between chlorophyll a and TN and TP were also high. Both lakes recorded high primary productivity, Lake Mburo showing higher values. The study highlighted the need to investigate the organism–community interrelationships in the two water bodies.     

Ancient Lake Ohrid: biodiversity and evolution

Worldwide ancient lakes have been a major focal point of geological, biological, and ecological research, and key concepts in, for example, evolutionary biology are partly based on ancient lake studies. Ancient lakes can be found on most continents and climate zones with most actual or putative ancient lakes in Europe being restricted to the Balkan Region. The arguably most outstanding of them is the oligotrophic and karstic Lake Ohrid, a steep-sided graben of rift formation origin situated in the central Balkans. Here, an attempt is made to summarize current knowledge of the geological, limnological, and faunal history of Lake Ohrid. Additionally, existing data on biodiversity and endemism in Lake Ohrid are updated and evaluated, and patterns and processes of speciation are reviewed in the context of the Ohrid watershed, including its sister lake, Lake Prespa. Whereas the geological history of the Ohrid Graben is relatively well studied, there is little knowledge about the limnological and biotic history of the actual lake (e.g., the age of the extant lake or from where the lake first received its water, along with its first biota). Most workers agree on a time frame of origin for Lake Ohrid of 2–5 million years ago (Mya). However, until now, the exact limnological origin and the origin of faunal or floral elements of Lake Ohrid remain uncertain. Two largely contrasting opinions either favour the theory of de novo formation of Lake Ohrid in a dry polje with a spring or river hydrography or a palaeogeographical connection of Lake Ohrid to brackish waters on the Balkan Peninsula. Whereas neither theory can be rejected at this point, the data summarized in the current review support the de novo hypothesis. An assessment of the fauna and flora of Lake Ohrid confirms that the lake harbours an incredible endemic biodiversity. Despite the fact that some biotic groups are poorly studied or not studied at all, approximately 1,200 native species are known from the lake, including 586 animals, and at least 212 species are endemic, including 182 animals. The adjusted rate of endemicity is estimated at 36% for all taxa and 34% for Animalia. In terms of endemic biodiversity, Lake Ohrid is with these 212 known endemic species and a surface area of 358 km² probably the most diverse lake in the world, taking surface area into account. Preliminary phylogeographical analyses of endemic Lake Ohrid taxa indicate that the vast majority of respective sister taxa occurs in the Balkans and that therefore the most recent common ancestors of Ohrid- and non-Ohrid species likely resided in the region when Lake Ohrid came into existence. These data also indicate that there is relatively little faunal exchange and overlap between Lake Ohrid and its sister lake, Lake Prespa, despite the fact that the latter lake is a major water supplier for Lake Ohrid. Studies on selected species flocks and scatters, mostly in molluscs, point towards the assumption that only few lineages originally colonized Lake Ohrid from the Balkans and that the majority of endemic species seen today probably started to evolve within the lake during the early Pleistocene. Within the Ohrid watershed, endemism occurs at different spatial and taxonomic scales, ranging from species endemic to certain parts of Lake Ohrid to species endemic to the whole watershed and from subspecies to genus level and possibly beyond. Modes of speciation in the Ohrid watershed are largely affected by its degree of isolation. Observational evidence points towards both allopatric (peripatric) and parapatric speciation. Though sympatric speciation within a habitat is conceivable, so far there are no known examples. Today, the lake suffers from increasing anthropogenic pressure and a “creeping biodiversity crisis”. Some endemic species presumably have already gone extinct, and there are also indications of invasive species penetrating Lake Ohrid. The comparatively small size of Lake Ohrid and the extremely small range of many endemic species, together with increasing human pressure make its fauna particularly vulnerable. It is thus hoped that this review will encourage future research on the ecology and evolutionary biology of the lake’s taxa, the knowledge of which would ultimately help protecting this unique European biodiversity hot spot. Guest editors: T. Wilke, R. V?in?l? & F. Riedel Patterns and Processes of Speciation in Ancient Lakes: Proceedings of the Fourth Symposium on Speciation in Ancient Lakes, Berlin, Germany, September 4–8, 2006     

巢湖崩岸湖滨基质-水文-生物一体化修复

湖滨带生态修复不是简单的水生植物移种,还必须提供其适于生存的基质、水文等外部物理条件。基质作为水生植被的载体,既需要适宜的柔度,也要求一定的刚度。在巢湖崩岸湖滨综合调查的基础上,系统分析了崩岸湖滨带生态退化的成因,研发了基质、水文、生物一体化修复技术,解决了水生植物在恢复生长时期受基质流失和水力切割影响的问题,为水生植物营造了适宜的水生环境。通过西北岸万年埠湖滨的示范工程建设,取得了良好的治理效果,为巢湖崩岸湖滨的生态修复提供一种生态型的、可工程化实施的技术方法。     

Biological diversity of the Yala Swamp lakes, with special emphasis on fish species composition, in relation to changes in the Lake Victoria Basin (Kenya): threats and conservation measures

During the second half of the last century, the Lake Victoria ecosystem has undergone drastic ecological changes. Most notable has been the decline in the populations of many endemic cichlid fishes. The lake has lost nearly 200 haplochromines and one tilapiine, Oreochromis esculentus. The above changes have been attributed to effects of species stocking and, in particular, from predation pressure by the introduced Nile perch, Lates niloticus. Other factors that have led to the decline of the endemic species include intensive non-selective fishing, extreme changes in the drainage basin, increased eutrophication, and the invasion of the lake by the water hyacinth, Eichhornia crassipes. However, the remnants of some species that had disappeared from Lake Victoria occur abundantly in the Yala Swamp lakes (Kanyaboli, Sare and Namboyo). This paper discusses the biodiversity of the swamp and the three lakes and gives suggestions for their conservation.     

300年来鄱阳湖营养盐演化重建与模拟

水体富营养化已经成为全球性的问题而受到广泛关注,然而其发生的过程和机制尚未完全明了。在湖泊营养演化过程中,水文和生态是两个最基本的制约因素。相对于短期的和试验性的研究,长时间尺度的营养盐变化过程能更全面地揭示营养盐的演化机制。以我国最大的淡水湖——鄱阳湖为例,采用湖泊水体交换周期模型和湖泊生态-营养盐动力耦合模型,重建鄱阳湖营养盐的长期变化,并利用沉积钻孔代用指标加以验证。在此基础上探讨其演化机制,模拟的时间序列中营养盐变化对气候水文与生态系统存在两种不同的响应模式。敏感因子分析显示:典型同步响应期中(1812—1828 AD),气候水文因子的贡献率达79.1%,生态因子为20.9%;典型异步响应期中(1844—1860 AD),两者贡献率分别为36.4%和63.6%。在模拟的营养盐变化时间序列中同步期占62.5%,说明气候因子在营养盐演化过程中起重要的作用;异步期虽只占12.5%,但对湖泊营养盐作用、营养盐反馈生物量同样至关重要。相关分析结果显示,生物量增长与TP含量基本呈线性关系,但存在一个阈值。在没有超过阈值前,生物量对TP具有较好的调节作用;当超过阈值之后,生物量的调节作用减弱。