Factors controlling phytoplankton primary productivity in Byram Lake,Mt. Kisco,N.Y., summer 1977

Phytoplankton productivity was measured in Byram Lake Reservoir during summer 1977. Depth integrated productivity (0–5 gC m^{– 2} d^–1) increased with station depth, which together with visibility measurements indicated that light did not limit deep station productivity (C1 and S2). Macrophytes at station C5 (shallow) reduced the euphotic zone to 0 in June.On a unit depth basis, C5 was the most productive station. Apparently changes in macrophyte growth, regulated by light and temperature, controlled phytoplankton production. At C1, productivity was related to levels of different nutrients at different depths, the thermocline influencing nutrient availability at mid-depth. At S2, NH₃-N controlled mid-depth productivity. Surface and mid-depth productivity appeared influenced by factors not measured in this study.     

Contribution a l'etude limnologique du lac Pavin (France). II: Relations entre parametres abiotiques-phyto et zooplancton dans la zone 0–20 metres

At 1197 m in the French Massif Central, lake Pavin has a volcanic origin. It is a meromictic lake of 44 ha area and 98 meters depth.Zooplancton samples (250 liters) were collected bimonthly with a water pump from May 1973 to April 1974 at six depths from surface to 20 meters.Countings were made to study the dynamics of two Cladocera: (Daphnia longispina and Ceriodaphnia quadrangula), two copepode populations, the calanoide Acanthodiaptomus denticornis and the cyclopoide Cyclops abyssorum. For the last two species, males, females, ovigerous females, Nauplius larvae and each of the five copepodite stages were differentiated.If Cladocera have a period of development limited from June to September for Ceriodaphnia and from June to December for Daphnia, copepods are presents all around the year with two principals periods of reproduction. The first during spring (March–April), the second during fall (October–November). If this second generation presents an important development for Cyclops abyssorum, that is not the same for Acanthodiaptomus denticornis, in which species nauplius larvae died in winter. The synthetical mathematical model realized by Principal Components Analysis illustrates the relationships between phyto-and zooplancton and bio-physico-chemicals parameters and specially the fact that, in this lake, the highest values of phytoplanctonic primary production and activity coefficient (Production/Standing crop) are found when herbivorous zooplancton presents the more important development and nutrients their lowest concentrations.

     

Genetic analysis of transpositions in the lac region of Escherichia coli

The lac region of Escherichia coli, carried on an F′ lacproB episome, was used as a target for the transposition of several transposable elements. Tn9 shows a preferential integration (by a factor of 50) into a region extending from the end of the Z gene through the Y gene. Throughout the remainder of the lacI, Z and Y genes one other short region, located in the middle of the I gene, is favored for integration. Within these favored regions many different integration points are evident. Inspection of the DNA sequence for the I and Y genes, and parts of the Z gene, shows a strong correlation between A + T richness and regions of preferential integration. Tn5 insertions follow a similar pattern, although with less preference; whereas Tn10 insertions (provided by T. J. Foster), also favor the Y gene and the end of Z, but are distributed among fewer integration points. Most of the Tn3 insertions into the episome are accompanied by a nearby or adjacent deletion.     

Comparison of ageing methods and growth rates for largemouth bass,Micropterus salmoides Lacépède,from northern latitudes

Synopsis Ages determined by counts of apparent annuli on scales, sagittae, vertebrae, pectoral fin ray and dorsal fin spine cross sections of largemouth bass from northern populations, which are older and slower growing fish than in the southern parts of its native range, were compared to establish the accuracy of each method. Linear regression techniques indicated strong agreement (r> 0.9) among ages assigned from the examination of scales, sagittae, and vertebrae. The pattern of growth zones on pectoral fin ray and dorsal fm spine cross sections proved too variable for accurate age determination. Limited data suggest that ages greater than 7+ assigned from scales were more likely to underestimate true ages than the other body parts used, although none of these methods gave satisfactory results. Examination of scales from recovered tagged fish, and the similarity between back-calculated lengths of fish through age 7+ to annulus I and observed lengths of juvenile largemouth bass near the end of their first growing season, support the validity of ages determined from scales. Despite a very limited amount of habitat suitable for largemouth bass and severe climatic conditions, growth of this species in Tadenac Lake was similar to growth in other waters north of the Great Lakes. Differences in physical characteristics among these waters does not appear to influence growth rates of largemouth bass, but probably affects production and biomass.     

鄱阳湖湿地不同土地利用方式下土壤微生物群落功能多样性

于2011年5月分别采集鄱阳湖围垦92、48a和38a的水稻田,退田还湖25a的退耕地以及自然湿地共5个样地的表层土壤,利用Biolog-ECO板技术对土壤微生物群落的单一碳源利用情况进行了测定,并结合群落指数和主成分分析(PCA)对培养72 h土壤微生物群落功能多样性变化进行了分析。结果表明:退耕地和自然湿地土壤微生物群落利用31种碳源的能力较强,来自不同围垦年限的土壤微生物群落利用碳源能力均较弱;且随围垦时间的增长,土壤微生物对碳源的利用能力呈降低的趋势。自然湿地、退耕地与围垦92、38a样地土壤之间存在显著的微生物功能多样性差异;围垦对土壤微生物代谢糖类、羧酸类、氨基酸类物质的影响最为明显。结果提示,围垦改变了湿地土壤微生物群落结构,退田还湖有助于湿地土壤微生物群落结构的恢复。     

气候变化对滇西北碧塔海流域景观演变的影响

气候变化是景观演变的重要驱动力,高海拔地带生态系统对气候变化的响应较为敏感和迅速。选择地处青藏高原东南缘,受人为干扰相对较小的碧塔海流域为研究对象,利用1958—2011年气象资料以及1955、1974、1981、1994、2005和2011年6个年代的景观类型面积,采用气候倾向率估计、Mann-Kendall突变检验方法和Pearson相关系数等统计方法,研究了香格里拉县气候变化背景下碧塔海流域景观演变特征。结果表明:(1)1958—2011年来,滇西北香格里拉县多年平均气温为5.9℃,多年平均活动积温为2146.1℃,多年平均年极端高温为24.3℃,多年平均年极端低温为-18.6℃,多年平均降水量为631.7mm。气温、活动积温和年极端低温呈显著上升趋势,近54年来气温平均上升了1.94℃,升温速率远高于云南和全国水平。年极端高温和降水量呈增加趋势,但增加不明显。滇西北高原碧塔海流域背景气候呈现显著的变暖趋势。(2)1955—2011年来,碧塔海流域自然景观演变规律为草甸和灌草丛向有林地演变,气温、活动积温和年极端低温升高趋势与有林地景观面积的增加趋势大体一致,与草甸和灌草丛变化趋势相反。(3)气温、活动积温和年极端低温与碧塔海流域草甸、灌草丛和有林地的景观面积变化具有显著的相关性,是流域景观演变的主导气候要素,在草甸和灌草丛演变成有林地的过程中发挥着重要作用。极端高温和降水量对流域景观演变的作用相对较弱。     

白洋淀富营养化湖泊湿地厌氧氨氧化菌的分布及对氮循环的影响

随着生物反应器和海洋生态系统中厌氧氨氧化反应的发现,自然生态系统的氮循环过程被重新认识,但是目前厌氧氨氧化过程是否也存在于富营养化湖泊湿地并发挥着重要作用,还未见报道。结合15N同位素示踪与分子生物学技术研究了白洋淀湖泊湿地沉积物中厌氧氨氧化菌的分布、菌群结构特性、生物多样性及其活性。结果表明,在藻类影响导致的高氨氮沉积物中,厌氧氨氧化菌具有广泛存在性。通过构建16S rRNA克隆文库发现,沉积物中厌氧氨氧化菌的生物多样性相对较低,在2%差异度的条件下,30个克隆序列只分为5个操作分类单元(OTUs),代表序列与Genebank数据库中已探明的厌氧氨氧化菌Candidatus Brocadia fulgida和Candidatus Brocadia anammoxidans同源性最高,分别可达97%和96%。同位素示踪结果表明,白洋淀湖泊湿地沉积物中厌氧氨氧化活性为0.19—7.78 nmol N g-1h-1,空间差异较大,产生的氮气占此沉积物总氮气生成量的0.64%—20.65%,体现了湿地的异质性。通过得出的厌氧氨氧化反应速率推算每年由厌氧氨氧化反应损失的氮量为1.8—78gN m-2a-1,对白洋淀氮循环起到非常重要的作用。富营养化湖泊湿地沉积物中厌氧氨氧化反应的发现为研究厌氧氨氧化对氮循环的重要影响提供了新证据。     

近30年来白洋淀湿地景观格局变化及其驱动机制

湿地是水陆相互作用形成的独特生态系统,其景观格局极易受到气候变化和人类活动的影响。利用1984—2014年的11期遥感影像数据,综合运用GIS技术和景观格局指数方法,对白洋淀湿地景观格局变化特征及其驱动力机制进行了分析。结果表明,1984—2014年期间,挺水植物和沉水植物呈减少趋势,农田和居民点持续快速增长,纯水体为"增加—减少—再增加"的趋势,林地和裸土地变化幅度不大。其中挺水植物一直是白洋淀最主要的景观类型,占研究区总面积比例达到37%—61%。农田的平均斑块面积最大,挺水植物的最大斑块指数和分维度指数最高,挺水植物和农田的聚集度指数最大,居民点、林地和裸土地空间分布离散,破碎化程度高,连通性差。1989—2004年白洋淀景观多样性指数呈减少趋势,景观格局趋于不稳定,同期聚集度指数上升,湿地连通性增加;1984—1989年和2004—2014年期间白洋淀多样性指数上涨,聚集度指数逐年下降,景观异质性增加。人口和社会经济发展是影响白洋淀景观格局变化的主要因素。     

Microbiota within the perennial ice cover of Lake Vida, Antarctica

Lake Vida, located in the McMurdo Dry Valleys, Antarctica, is an 'ice-sealed' lake with approximately 19 m of ice covering a highly saline water column (approximately 245 ppt). The lower portions of the ice cover and the lake beneath have been isolated from the atmosphere and land for circa 2800 years. Analysis of microbial assemblages within the perennial ice cover of the lake revealed a diverse array of bacteria and eukarya. Bacterial and eukaryal denaturing gradient gel electrophoresis phylotype profile similarities were low (<59%) between all of the depths compared (five depths spanning 11 m of the ice cover), with the greatest differences occurring between surface and deep ice. The majority of bacterial 16S rRNA gene sequences in the surface ice were related to Actinobacteria (42%) while Gammaproteobacteria (52%) dominated the deep ice community. Comparisons of assemblage composition suggest differences in ice habitability and organismal origin in the upper and lower portions of ice cover. Specifically, the upper ice cover microbiota likely reflect the modern day transport and colonization of biota from the terrestrial landscape, whereas assemblages in the deeper ice are more likely to be persistent remnant biota that originated from the ancient liquid water column of the lake that froze.     

新疆真藓科（Bryaceae）植物新记录

采用经典分类学方法,对1987~2015年采自新疆地区的400余份真藓科植物标本进行了整理和鉴定。结果发现：新疆分布有真藓科植物5属37种,其中3种为新记录种,即尖叶短月藓（Brachymenium acuminatum Harv.）、拟纤枝真藓（Bryum petelotii Thér. & Henr.）和下延真藓（Bryum weigelii Biehler）。该文对此3个新记录种的重点识别特征、生境、地理分布及其与相近种的特征比较作了阐述,并绘制了基本形态特征墨线图。凭证标本存放于河北师范大学植物标本室（HBNU）。