The plankton ecology of Lake St. Clair, 1984

Lake St. Clair phytoplankton and zooplankton abundance and composition was analyzed during the period of May to September 1984. In addition, size-fractionated primary productivity and other limnological parameters were measured. Highest phytoplankton biomass was observed during spring (May) with high values for the southern and southeastern regions of the lake. Seasonally, the mean phytoplankton biomass ranged between 0.17 and 1.18 g m^-3 with high values recorded during spring (May, June) compared to summer. In the spring the phytoplankton was dominated by Diatomeae followed by Chrysophyceae and Cryptophyceae. During the summer the diatoms showed a decreasing trend due to the relative prevalence of Chrysophyceae, Cryptophyceae, and Chlorophyta. The species composition was oligotrophic-mesotrophic with mixed occurrence of some eutrophic species. The phytoplankton size composition indicated dominance of microplankton/netplankton (> 20 µm) and ultraplankton (< 20 µm) during spring and summer respectively. On an overall basis ultraplankton contributed overwhelmingly to primary productivity, as much as 75 percent in the summer.The mean zooplankton biomass ranged from 173.0 to 1306.0 mg l^- dominated by Cladocerans (bosminids) in contrast to the other Great Lakes. Statistical evaluation of the phytoplankton — nutrient-contaminant interactions revealed positive correlations with heavy metals, suggestive of a physiological adaptation to contamination from the chemical valley. Based on low biomass, high Production/Biomass ratio, dominance of ultraplankton, characteristic species composition and plankton spectra, the lake appears to be an oligotrophic-mesotrophic perturbed ecosystem.     

Skeletal formation in the modern but ultraconservative chaetetid spongeSpirastrella (Acanthochaetetes) wellsi (demospongiae,porifera)

Summary The modern hadromerid coralline spongeSpirastrella (Acanthochaetetes) wellsi exhibits a unique secondary high-Mg calcite (>19 mol % MgCO₃) basal skeleton. The basal skeleton is constructed of bundles of elongated crystals more or less tangentially orientated. The initial formation of these crystals is controlled by soluble highly acidic aspartic and glutamic-rich (40%) macromolecules. The skeletal mineralization occurs in four different loci: in the top of the calicles, at the tabulae, on collagenous anchor fibres, and within closed spaces between the tabulae. The clicle walls are formed on the uppermost top of the basal skeleton as a continuous process. Based on long term stainings with Ca²⁺-chelating fluorochroms (calcein, chlorotetracyclines) the growth rate of this sponge is extremely low with ca. 50–100μm/a. The skeletal formation takes places outside the sponge, within a narrow zone (300–500 nm) between the basopinacoderm and the mature basal skeleton. The sponge produces thread-like folded templates (‘spaghetti fibres’) of 0,5–2 μm size, the shape controlling insoluble organic matrix. These templates become mineralized in a first step as MgCO₃, then are stretched. A soluble organic matrix is also secreted, and remains are included inside the mineralized skeleton. This organic matrix consists of in a complex mixture containing small very acidic proteins (5, 13, 31 KD; 40% Asp and Glu and therefore most probably Ca²⁺-binding) and high molecular weight glycoproteins among several other organic compounds. The mature crystals are high-Mg calcites. During calcification large cells with large reserve granules (LCG) are always present in a tight connection with the basopinacoderm. These cells form also the collagenous anchor fibres. Primary tabulae are formed by a non-collagenous organic sheet. Calcification happens only when LCG cells are enriched on the organic sheet. Randomly oriented high-Mg calcite crystals are growing on the collagenous anchor fibres. The same type of the mineralization is observed within the spaces of the tabulae. This particular case of mineralization is controlled by decaying sponge tissue (ammonification). The δ¹³C values are in equilibrium with the ambient sea water and vary between +3.2 and +2.8 ‰. The mode of mineralization of the basal skeleton can be described as biologically induced resp. matrix mediated.     

Predation of zebra mussels by round gobies, Neogobius melanostomus

Preliminary gut analysis of a recent Great Lakes invader, the round goby, Neogobius melanostomus (7.0–8.4 cm), collected from the Detroit River, showed that they ate zebra mussels (58%), snails (6%), and other invertebrates (36%), including aquatic insects (Hexagenia), softshelled crayfish, and zooplankton. Because zebra mussels, Dreissena polymorpha, predominated as prey, we investigated the ability of round gobies to consume different size classes of zebra mussels. In laboratory experiments, we examined feeding preferences of three size classes of round gobies (5.5–6.9 cm; 7.0–8.4 cm; 8.5–10.3 cm standard length) on four different size classes of zebra mussels (6.0–9.9 mm, 10.0–12.9 mm, 13.0–15.9 mm, 16.0–18.9 mm). All sizes of round gobies ate zebra mussels < 10.0 mm. Only the largest size class of round gobies ate larger zebra mussels (10.0–12.9 mm) when all prey sizes were presented. The association between the total mass of zebra mussels available and the amount consumed by round gobies increased positively up to about 6.5 g of available mussels and then levelled off. Round gobies consumed an average of 1.0 g of mussels in 24 h. There was a significant positive relationship between gape size and standard length of round gobies. Although larger round gobies (over the size range of fish in our study) are able to consume larger zebra mussels, small mussels were preferred. Our findings suggest that the preference of small zebra mussels by round gobies has the potential to alter the size structure of zebra mussel populations. This revised version was published online in July 2006 with corrections to the Cover Date.     

秦岭南坡锐齿栎林的生态环境及其营养积累

秦岭锐齿栎林 (含 0～ 6 0cm土层 )营养元素总储量达 182 .6 4 5～ 394 .70 1t·hm-2 ,植被占 0 .5 9%～2 .13% ;林分生物量为 131.713～ 5 0 3.82 2t·hm-2 ,乔木层占 92 .1%～ 99.2 % ;凋落物层现存量和营养元素积累量分别为 2 .897～ 33.999t·hm-2 和 10 4 .339～ 1136 .5 36kg·hm-2 .在一定范围内 ,林分生物量和营养元素积累量随密度的增加而增大 ;立地、林分条件相似的林分 ,生物量和营养元素积累量与林龄呈正相关 .林分针叶树占的比例越大 ,营养元素积累量越小 ,而且对生物量的影响远小于对营养元素积累量的影响 .在同一地区 ,立地、林分状况相似 ,林型不同 ,生物量及营养元素积累量差别不大 ,树种组成和林型不同林分的生物量和营养元素积累量均不同 .不同地区 ,生态和林分条件相似的林分的生物量和营养元素积累量也有差异 ;林型、结构相似林分生物量和营养元素积累量南坡 >北坡 ,中段 东段≈西段 .林分对营养元素利用率与海拔呈负相关 ,且南坡 >北坡 ,中段 >东西段 ,中段 >西段 >东段 .     

三峡大老岭山地常绿落叶阔叶混交林林隙干扰研究 I．林隙基本特征

为探讨我国亚热带山地常绿落叶阔叶混交林的林隙干扰特征,对三峡大老岭地区这一植被类型进行调查,分析了植被中林隙的数量、类型及成因;林隙形成木（GM）的类型、数量、物种构成和径级结构,以及林隙和GM的多尺度空间格局特征。结果表明1）林隙密度为11.7个*hm-2;冠林隙和扩展林隙分别占森林面积的11.09%和27.06%。平均每个林窗的形成木为4.5株;单株GM形成的林隙只占17.46%,其中翻倒木集群性最强。对林隙形成的贡献大小次序是翻倒木>折干>枯立>折枝。2）林隙成因方面冬雪和春、秋冻雨的影响最大;病害影响其次;树木间的牵连和撞击扩大了林隙的范围;陡峭的地形增大林隙形成的机率;干旱的影响很小。3）68种GM主要是森林建群种;常绿树种形成林隙的平均机率高于落叶种。4）GM的胸径结构表明本地森林林隙干扰十分频繁。     

黄山苔类植物区系研究

黄山位于安徽省南部,根据调查和统计,共有苔类植物28科、48属、117种（包括亚种和变种）。该区苔类植物的优势科为细鳞苔科Lejeuneaceae、羽苔科Plagiochilaceae、光萼苔科Porellaceae、耳叶苔科Frullaniaceae;优势属为耳叶苔属Frullania、羽苔属Plagiochila、光萼苔属Porella、鞭苔属Bazzania、细鳞苔属Lejeunea。区系成分以热带成分和东亚成分为主,分别占到40％和39．09％,北温带成分占有一定的比例为20％。无毛拳叶苔Nowellia aciliata（P．C．Chen＆P．C．Wu）Mizut．和新绒苔Neotrichocolea bissetii（Mitt．）S．Hatt被列入我国濒危苔藓植物红色名录。     

Classification of plant associations based on a 20 hm2 dynamics plot of evergreen broad- leaved forest in Mt. Tiantong,Zhejiang, China

为获取能够代表浙江天童山的森林植被典型群丛类型, 同时也为植被分类中如何发现过渡类型和确定典型类型提供参考, 该研究利用天童20 hm ²森林大样地资料, 运用双向指示种分析(TWINSPAN)与除趋势对应分析(DCA), 剔除过渡群落, 进行群丛划分。结果表明, 去除过渡地段后更利于研究区域典型群丛类型的确定。大样地的植被类型可划分为宜昌荚蒾-厚皮香/港柯+云山青冈群丛(Viburnum erosum-Ternstroemia gymnanthera/Lithocarpus harlandii + Cyclobalanopsis sessilifolia Ass.); 虎皮楠-柯/木荷+米槠群丛(Daphniphyllum oldhami-Lithocarpus glaber/Schima superba + Castanopsis carlesii Ass.); 红毒茴-紫楠/南酸枣+薄叶润楠群丛(Illicium lanceolatum-Phoebe sheareri/Choerospondias axillaries + Machilus leptophylla Ass.)。DCA排序同时能反映各群丛类型分布与环境的相关关系, 结果显示, 海拔和凹凸度对群丛分布有较大影响, 坡度和坡向对群丛分布影响较小。     

云南高黎贡山蚤类的生态区系

本文报道了１９８５年以来对我甸横断山南端高黎贡山东、西坡蚤类生态区系的调查及研究结果。共发现蚤类５科２３属４７种（亚种）。文中对该山脉蚤类在不同森林植物带的群落结构、种的多样性及均匀度,各种蚤的栖境幅度、宿主多样性进行了陈述和比较,并对蚤类的区系特征、特有种的区系划分等问题进行了讨论。     

五台山山地草甸自然保护区11种化学元素生物积累的研究

五台山山地草甸自然保护区可划分为亚高山草甸带、山地五花草甸带、常绿针叶林草甸带。本文研究了各生态带土壤和植被中１１种化学元素的含量、分布及生物积累特征。研究表明：（１）各带土壤中化学元素含量均在全国同类型土壤含量范围之内,就平均含量而言,Ｃｏ＇Ｎｉ含量较高,其它元素含量较低,整体属清洁理想水平,合乎自然保护区土壤环境标准。（２）各带植被中营养元素含量较高,营养丰富。尤其是亚高山草甸带是饲用价值很高     

南迦巴瓦峰地区的大型真菌资源

本文记载了西藏南迦巴瓦峰地区的各类大型真菌292种,隶属于120属,42科。其中食用真菌166种,药用真菌109种,有毒真菌5D种,菌根菌68种,树木腐朽菌41种。另有点柄铦囊蘑(Melanoleuca verrucipes)、南牛肝菌(Austroboletus gracilis)、簇生小管菌(Filoboletus manipularis)、多鳞口蘑(Tricholoma squarrulosum)等21种为我国新记录。西藏地区的新记录76种。新种将另文发表。目前认为重要的或经济用途比较大的百种以上,如冬虫夏草(Cordyceps sinensis)、茯苓(Poria cocos)、木耳(Auricularia auricula)、金顶侧耳(Pleurotus citrinopileatus)、蜜环菌(Armillariella mellea)、松口蘑(Tricholoma matsutake)、鸡零售(土从)菌(Termitomyces albuminosus)、白毒伞(Amanita verna)、半卵圆斑褶伞(Anellaria semiovata)等。南峰地区真菌资源丰富,研究利用潜力很大。