Hagenia from the early Miocene of Ethiopia: Evidence for possible niche evolution?

Fossil pollen believed to be related to extant Hagenia abyssinica were discovered in the early Miocene (21.73 Ma) Mush Valley paleoflora, Ethiopia, Africa. Both the fossil and extant pollen grains of H. abyssinica were examined with combined light microscopy, scanning electron microscopy, and transmission electron microscopy to compare the pollen and establish their relationships. Based on this, the fossil pollen grains were attributed to Hagenia. The presence of Hagenia in the fossil assemblage raises the questions if its habitat has changed over time, and if the plants are/were wind pollinated. To shed light on these questions, the morphology of extant anthers was also studied, revealing specialized hairs inside the anthers, believed to aid in insect pollination. Pollen and anther morphology are discussed in relation to the age and origin of the genus within a molecular dated phylogenetic framework, the establishment of complex topography in East Africa, other evidence regarding pollination modes, and the palynological record. The evidence presented herein, and compiled from the literature, suggests that Hagenia was an insect‐pollinated lowland rainforest element during the early Miocene of the Mush Valley. The current Afromontane habitat and ambophilous (insect and wind) pollination must have evolved in post‐mid‐Miocene times.     

Past grazing habitats for Svalbard reindeer indicated by the pollen content of 3300‐year‐old faeces from Edgeøya,Svalbard

Sedentary populations, like the Svalbard reindeer, tend to select the most nutritious and easily available plants during the different seasons. It has been shown that plants selected during grazing season are reflected in the pollen content of modern faeces from Svalbard reindeer. In this study the pollen and spore content of fossil reindeer faeces and peat from Raddedalen, western Edgeøya, Svalbard, are presented. The pollen content of the fossil faeces is first compared to published pollen data from modern Svalbard reindeer faeces so as to determine which season they were deposited, and second the pollen in the fossil faeces are compared to the pollen content of the peat in which they were found. The lower part of the peat section is dated to 3435±105?cal?yr BP. The faeces are dominated by pollen from early flowering species such as Saxifraga oppositifolia‐type, S. nivalis‐type, Brassicaceae, and Pedicularis spp. thereby indicating that grazing and faeces deposition took place in spring and early summer. The peat and faeces have some similarities in their pollen and spore content, but different methods of deposition and concentration of pollen in faeces and peat result in different fossil assemblages. The results suggests that the climate of Raddedalen was warmer and moister than today, allowing peat to form in the past.     

Inhibition of the activity of aminoacyl-tRNA synthetases in pollen grains of maize

Extracts from pollen grains of maize ( Zea mays L.) show a low activity of aminoacyltRNA synthetases (EC 6. 1. 1). They also contain a specific factor inhibiting the activity of these enzymes. The molecular mass of this factor, which may be a short peptide, is about 3000 Da as determined by column chromatography on Sephadex G-25 Fine. The Michaelis constant (K_m), determined for the amino acid in the presence of this factor, suggests its allosteric influence on the affinity of the enzyme. Short-term incubation of the factor with pronase R resulted in conversion of the inhibiting action into a stimulating one. Kinetics of aminoacylation reactions confirm inhibitory and stimulative influences of the effector on the enzyme activity. High performance liquid chromatography shows that inhibition of the activity of aminoacyl-tRNA synthetases is affected by a group of compounds of similar molecular masses.     

Pollen dispersal and representation in a neotropical rain forest

Results of 3 years of pollen trapping on Barro Colorado Island, Panama, are presented. Minimum pollen dispersal distances are estimated for the most abundant pollen taxa. Dispersal distances for some taxa appear to be as low as 5 m, while for other taxa at least 50% of the trapped pollen had travelled more than 40 m. No consistent pattern of spatial variation was reflected in the pollen rain, however, samples close to large canopy gaps had exceptional abundances of 'disturbance' taxa. A preliminary analysis of the representation of canopy components indicates that as much as 19% of pollen caught in the traps was derived from large tree species.     

人类活动干扰下区域植被动态变化——以西双版纳为例

云南省西双版纳地区是我国典型热带雨林区,随着社会经济发展,人类活动对区域植被格局与动态产生强烈影响。利用NDVI变化趋势分析、土地利用转移矩阵和基于MODIS数据的干扰指数（MGDI）3种方法,分析了2000-2010年人类活动干扰下研究区植被动态变化,构建了人类活动干扰指数,并利用冗余分析的方法,分析其与植被特征的相关性。结果表明：通过NDVI变化趋势得出,2000-2010年间,研究区植被覆盖度总体较高,植被变化趋势的斜率均大于0,说明植被总体趋于改善;基于土地利用转移矩阵结果表明,植被变化主要发生在常绿阔叶林、常绿针叶林转变为乔木园地、灌木园地、人工园地或居住用地;基于MODIS影像结果得出,西双版纳地区MGDI分布很不均匀,且2000-2010不同土地覆被类型MGDI相差不大。构建的人类活动干扰指数结果显示人类干扰强度由中心向边缘呈递增趋势,呈分散分布,这与人类活动的分布规模和强度相关。通过冗余分析可知,NDVI与人类活动相关性较大,MGDI与人类活动相关性不大。总体上来说,上述3种方法能够从不同侧面反映出人类活动干扰下植被长时间的变化趋势。因此,对于西双版纳地区,局地的人类活动特别是旅游、基础设施建设、农业活动等对热带雨林自然生态系统的干扰不容忽视。     

西双版纳热带山地雨林生物量研究

观测了西双版纳山地气候,建立了山地雨林生物量回归方程,调查了海拔1 100~1 820 m范围5块样地(面积0.16~0.25 hm2)的热带山地雨林生物量。结果表明,海拔1 105和1 610 m的年平均温度分别为20.1和16.6℃,年降雨量分别为1 659和2 011 mm,旱季(11~4月)降雨量分别为295和283mm,年平均相对湿度分别为81%和84%;5块样地生物量变化为256.4~368.6 t.hm-2,平均为312.6t.hm-2,其中乔木占97.1%、木质藤本占1.2%、幼树和灌木占1.3%、草本和幼苗占0.4%;采用热带季节雨林生物量回归方程估计山地雨林生物量,会使得总生物量以及树干和树根生物量高估38.3%~61.5%,树枝生物量低估7.6%~30.8%。可见,西双版纳山地海拔增加导致雨季降雨量增加,山地雨林生物量较热带季节雨林降低32.6%,季节雨林生物量方程不适用于山地雨林。     

Influence of genotype and texture on zein content in endosperm of maize grains

The effect of genotypes and texture on the content of proteins in maize grains was examined by assessing absolute amounts of six protein fractions in the whole endosperms of four wild‐type lines with high protein content and four quality protein maize (QPM) varieties and for hand‐dissected hard and soft endosperm regions from eight other lines. As previously reported for six wild‐type lines and their opaque‐2(o2) versions, zeins were predominant for all genetic backgrounds and all types of endosperms. From these data and others the amounts of zeins and true proteins (crude proteins free of non‐protein nitrogen) in developing and mature endosperms of wild‐type lines were correlated. The data points for zeins from hard endosperms lay between the regression line and the upper limit of confidence area. Those for zeins from soft endosperms were located at the lower part of confidence area and on a level with the points corresponding to the most immature endosperms. Furthermore, some data points for zeins from o2 and QPM samples lay near the lower limit while the others were outside the confidence area. This suggested an initial zein accumulation dependent on the genotype at a low relative rate, followed by an accumulation at higher rate. The conditions used for isolating and quantitating zeins are discussed.     

云南热带季雨林及其与热带雨林植被的比较

在中国植物学文献中, 对热带季雨林的解释和运用是不一致的, 特别是易于把季雨林与热带雨林相混淆。季雨林是在具有明显干、湿季变化的热带季风气候下发育的一种热带落叶森林植被, 是介于热带雨林与热带稀树草原(savanna)之间的一个植被类型。云南的热带季雨林在分布生境、生态外貌特征、植物种类组成和地理成分构成上, 均与热带雨林有明显区别, 季雨林主要分布在海拔1 000 m以下的几大河流开阔河段两岸和河谷盆地, 其群落结构相对简单, 乔木一般仅有1至2层, 上层树种在干季落叶或上层及下层树种在干季都落叶; 在生活型组成上, 季雨林的木质藤本相对较少, 大高位芽植物及地上芽植物很少, 但地面芽植物很丰富, 地下芽植物和一年生植物也相对丰富; 在叶级和叶型特征上, 季雨林植物的小叶和复叶比例相对较高, 分别占到24%和44%; 在植物区系地理成分构成上, 季雨林的热带分布属合计也占绝对优势, 但以泛热带分布属的比例相对较高, 约占到总属数的30%, 热带亚洲至热带非洲分布属的比例也较高, 约占总属数的12%。季雨林的地理成分更为多样性, 起源与发展历史也更复杂和古老。     

瑞丽莫里热带雨林种子植物区系的初步研究

初步分析了鲜为人知的滇西南瑞丽莫里的热带雨林植物区系组成与地理成分。该植物区系中热带和主产热带的科占总科数的80%以上,热带分布属占总属数的84.1%;典型热带分布种占总种数的82.1%,该区系在科、属和种水平上均以热带成分占优势,明显属于热带性质的植物区系。在其热带分布属中,又以热带亚洲分布属最多,占总属数的26.5%;典型热带分布种中也以热带亚洲分布及其变型的种占绝对优势,占总种数的72.9%,反映了该植物区系具有热带亚洲植物区系的性质特点。在其热带亚洲成分中,又具体以南亚—大陆东南亚成分比例最高,反映了滇西南的热带雨林植物区系由于地域邻接关系,受印度(喜马拉雅)—缅甸植物区系的强烈影响。     

Isolation and characterization of Azotobacter chroococcum from the roots of Zea mays

Abstract Bacteria showing rapid growth on a nitrogenfree medium and acetylene-reducing activity were isolated from maize roots collected from agricultural soils in Spain. The isolates were Gram-negative motile rods and were identified as Azotobacter chroococcum . Acetylene-reducing activity and microbial counts were determined on root segments from 7- and 30-day-old plants. Rates obtained were in the range of 0.0053–0.848 nmol C₂H₂· g⁻¹· h⁻¹. Root populations were 1.4–6.0 × 10⁴ micro-organisms · g⁻¹. These results showed that there was an association between A. chroococcum strains and roots of maize planted in some Spanish soils.     

西双版纳地区六种林型地表蜘蛛多样性比较研究

为探索地表蜘蛛多样性及其变化与森林类型和管理方式的关系, 在西双版纳勐仑自然保护区选择热带季节雨林、石灰山季节雨林和山地常绿阔叶林, 在自然保护区附近选择人工纯林、胶茶群落和橡胶林, 共6种林型, 每种林型选择3块样带, 共设置研究样地18块, 分别于2006年12月上旬（雾凉季）、2007年3月下旬（干热季）和2007年7月上旬（雨季）, 以单位地表面积法收集地表蜘蛛的物种组成和数量数据, 并以蜘蛛种类和数量分布为属性进行典范对应分析（CCA）, 探讨不同类型植被与地表蜘蛛多样性的关系。共采集蜘蛛标本9 849头, 用于统计分析的成熟蜘蛛3 119头, 归属于30科, 其中幽灵蛛科、皿蛛科、球蛛科和小密蛛科是地表蜘蛛的优势类群。各林型科的数量为: 热带季节雨林24科, 石灰山季节雨林22科, 山地常绿阔叶林22科, 人工纯林20科, 胶茶群落21科, 橡胶林19科; 各林型特有科数量: 热带季节雨林2科, 山地常绿阔叶林2科, 橡胶林1科; 而仅在雨林中分布的科4个（占全部30个科的13.3%）, 仅在自然林中分布的科6个（20.0%）, 仅在人工林中分布的科1个（3.3%）。从蜘蛛的数量分布看, 个体密度在热带季节雨林显著高于其他5种林型; 橡胶林多样性指数和丰富度指数显著低于3种自然林, 而均匀度指数的最低值也同样在橡胶林出现。CCA分析和聚类分析的结果表明, 6种林型趋于分成2组, 即: 自然林和人工林; 在自然林中两种次生林的相似程度更高; 人工林中人工纯林（非橡胶林）与胶茶群落的相似程度更高。以上结果表明: （1）森林砍伐后种植人工林措施改变了该地区地表蜘蛛群落的物种分布格局; （2）蜘蛛多样性随着人为干扰程度增加有减少的趋势; （3）减少人为干扰和增加植被群落多样性（橡胶林中种植茶树）对保护和恢复物种多样性有重要意义。