989 resultados para 3C 273


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 毛茛科乌头属全世界约有300余种,主要分布在北半球温带地区,包括三个亚属,即牛扁亚属、乌头亚属和露蕊乌头亚属。我国西南横断山区是乌头属植物的重要分布区,已记载的种类达100余种,很多种都为地方特有。由于缺乏野外观察和标本不够丰富等原因,有些种类的分类处理尚不能令人满意,应予修订。乌头属的属下系统以及与近缘属之间的关系也不十分清楚,还需进一步研究。本文对我国乌头属植物的重要分布区四川的乌头属植物进行了分类修订,同时通过形态学、细胞学和分子系统学等方面的研究对乌头属的系统发育进行了探讨。结果如下:   1.分类修订 通过广泛的野外观察、文献查阅和标本研究,对乌头属的形态性状在居群间和居群内的变异式样进行了比较分析,发现叶分裂程度、上萼片的形状和花梗毛被等性状是较为可靠的分种依据,但是在个别情况,这些性状也会在同一种的同一居群内或不同居群间发生变化。花瓣和种子的特征对于属下划分有重要意义。 本文确认四川乌头属植物有45种、11变种,另有2种和1变种暂存疑。30种、22变种降为异名;作出新组合2个,其中包括1个改级新组合。紫乌头和保山乌头为四川新分布记录。对康定乌头、川鄂乌头和狭裂乌头进行了模式选定。初步澄清了东俄洛乌头和狭裂乌头等种类中长期存在的名实混乱。本文还给出了各个种的形态描述、地理分布图以及分亚属、分系和分种检索表。   2.细胞学 对国产14种乌头属植物进行了细胞学研究。染色体基数为x=8。研究的所有种都为二倍体(2n=16)。各个种的核型公式如下:狭盔高乌头2n=2m+10sm+4st; 赣皖乌头2n=2m+8sm+6st; 西南乌头2n=4m+10sm+2st; 镰形乌头2n=4m+12sm; 弯喙乌头2n=4m+12sm; 东俄洛乌头2n=2m+12sm+2st; 毛瓣乌头, 来自两个居群, 2n=2m+14sm(1sat)和2n=2m+14sm(2sat); 狭裂乌头2n=2m+10sm+4st; 大渡乌头2n=8m+8sm; 展毛大渡乌头2n=6m(1sat)+8sm(2sat)+2st; 贡嘎乌头2n=2m+14sm; 刷经寺乌头, 来自四个居群, 分别为2n=4m+10sm+2st, 2n=6m+10sm, 2n=2m+14sm, 2n=2m+14sm; 工布乌头,来自两个居群, 2n=2m+10sm+4st和 2n=6m+10sm; 岩乌头2n=2m+14sm; 美丽乌头2n=4m+12sm; 康定乌头2n=4m+12sm。其中赣皖乌头、弯喙乌头、东俄洛乌头、狭裂乌头、大渡乌头、展毛大渡乌头、贡嘎乌头、工布乌头和康定乌头9种的染色体数目和核型为首次报道。乌头属植物通常都有两对较大的染色体,即第一对为中部着丝点染色体,第二对为近中部着丝点染色体,其余染色体相对较小,为中部着丝点、近中部着丝点或近端部着丝点染色体。牛扁亚属的核型与乌头亚属在染色体大小、形态及不对称性等方面有明显的区别。随体的数目和位置在同一种内的不同居群中都有变化。核型不对称性表现有2B、3B、2C和3C型。 对国产乌头属植物的染色体数目资料进行了统计。国产61种乌头属植物已有染色体报道,占国产乌头属植物的41%。二倍体、四倍体、六倍体和八倍体都有发现,有5种乌头属植物表现为种内多倍性。横断山区分布的乌头亚属植物多为二倍体,多倍体通常在主要分布于华北和东北地区的乌头亚属的乌头系中观察到。横断山区的牛扁亚属植物多数为四倍体。少数种的染色体具有B-染色体。   3.分子系统学 通过对翠雀族23种植物两个DNA片段ITS和trnL-F进行简约分析和邻接法分析,构建了乌头属三个亚属之间及其与近缘属的系统关系树。结果如下:翠雀族作为单系类群得到了较强的支持;翠雀族中,与乌头属关系较近的是翠雀属;在乌头属中,乌头属作为单系类群未得到支持,除非将露蕊乌头亚属排除在外;牛扁亚属和乌头亚属均为单系群,二者互为姐妹群;新建的唐古特乌头亚属与乌头亚属聚在一起不能分开,其亚属的地位未得到支持。 采用ITS序列,选取代表乌头亚属植物不同组、系以及不同地理分布区的54个样品,进行了乌头亚属的系统发育研究。乌头亚属的单系发生得到了支持。多果乌头位于乌头亚属的基部,与其他乌头亚属植物构成姐妹群关系。岩乌头系和褐紫乌头系也各自成为分支, 但唐古特乌头系、圆叶乌头系、保山乌头系与短柄乌头系共同组成一个单系类群,而显柱乌头系、兴安乌头系、乌头系、蔓乌头系和准噶尔乌头系共同组成一个单系类群。从上述结果来看,这些系或组是否应当划分及其系统关系均应重新考虑。在ITS系统树中,中国北方分布的乌头亚属植物与欧洲、北美及东亚的乌头亚属植物有较近的关系;来自横断山区的种类外部形态差异显著,但遗传差异却很小,说明这一地区的种可能是近期形成的。本研究的ITS序列分析结果与种子和花瓣的形态相吻合,种子和花瓣的特征有可能在一定程度上反映了乌头亚属的系统发育关系。

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上新世时期是地球环境发展变化过程中由温暖的中新世向冰期-间冰期交替出现的更新世的过渡时期,研究上新世的气候有助于研究现代全球气候变化趋势。我国上新世植物群研究不多,尤其缺乏早上新世植物群的研究。在研究化石植物群的过程中,叶角质层的信息通常被忽视。迄今,我国古气候的定量研究主要集中在山东山旺和云南地区,研究的主要是中新世和晚上新世的古气候,早上新世气候的定量研究国内外都未见报道。 本论文以采自浙江中部嵊州地区硅藻土中的植物叶和果实为材料,通过光学显微镜、荧光显微镜和扫描电镜观察,对提取的化石叶角质层和叶结构进行研究,对比研究现代相关类群植物的叶片,确定了化石植物类群计15科24属(或亚科)34种。同时参照现代植物分布,恢复了早上新世嵊州地区古植被情况,进一步运用共存分析(Co-existence Approch)定量重建了当时的古气候,得到古年均温、古年较差和古年降水量等7个参数。 研究表明,叶结构和叶角质层可以应用于化石植物类群的鉴定。光学显微镜和荧光显微镜下可以获得的信息有:气孔、表皮细胞形状及大小、表皮细胞垂周壁、分泌结构、表皮毛或毛基等。扫描电镜观察的是叶表皮细胞表面的情况,如细胞外壁是否被蜡质以及蜡质的交结情况,气孔外壁是否增厚呈环等。 经化石植物类群鉴定,早上新世(约4Ma)嵊州地区植被属亚热带常绿阔叶林。推测:该地区当时存在一个较大的湖泊,湖泊边缘水中生长有菱角,湖泊周边可能有海拔超过1400m的山地。 常绿阔叶林主要成分是壳斗科植物,其中青冈属植物可能是建群植物。自低海拔到高海拔地区都有分布的是:栎属、栗属、桤木属植物,青杨梅。低海拔地区(<600m)分布的植物有:海南锥,樟。中低海拔地区(300-1000m)分布着:柯属、黄杨属植物,水青冈,海南油丹,江南油杉,福建柏。中高海拔地区(>700m)分布有:高山栎、黄肉楠属植物,米心水青冈,榉树,建始槭,天台鹅耳枥和昌化鹅耳枥。除了上述类群,林中还散布着鼠李属、杜鹃花属和冬青属的植物,豆科崖豆藤属植物则缠绕一些较大乔木生长。另外,在一些土壤、有机质易堆积的洼地生长有竹林,山地贫瘠的地方生长着柏属植物。 嵊州早上新世化石植物群反映的植被同浙江地区现代植被相似。第三纪浙江地区从针叶林或阔叶树为主的针-阔叶混交林过渡到常绿-落叶阔叶林,再发展为常绿阔叶林。 依据23个植物类群分析获得7个古气候参数:年均温17.7-21.4°C,最热月均温22.2-27°C,最冷月均温8.4-13.4°C,年较差12.1-15.3°C,年降水量1136-1869.9mm,最大月降水量211.8-283.3mm,最小月降水量20.3-36.8mm。 对比现代嵊州地区气候参数,早上新世嵊州地区年降水量略高于现代,年均温比现代高1.3-5°C,年较差为12.1-15.3°C。早上新世期嵊州地区四季气温比现代平稳。

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We report a Monte Carlo representation of the long-term inter-annual variability of monthly snowfall on a detailed (1 km) grid of points throughout the southwest. An extension of the local climate model of the southwestern United States (Stamm and Craig 1992) provides spatially based estimates of mean and variance of monthly temperature and precipitation. The mean is the expected value from a canonical regression using independent variables that represent controls on climate in this area, including orography. Variance is computed as the standard error of the prediction and provides site-specific measures of (1) natural sources of variation and (2) errors due to limitations of the data and poor distribution of climate stations. Simulation of monthly temperature and precipitation over a sequence of years is achieved by drawing from a bivariate normal distribution. The conditional expectation of precipitation. given temperature in each month, is the basis of a numerical integration of the normal probability distribution of log precipitation below a threshold temperature (3°C) to determine snowfall as a percent of total precipitation. Snowfall predictions are tested at stations for which long-term records are available. At Donner Memorial State Park (elevation 1811 meters) a 34-year simulation - matching the length of instrumental record - is within 15 percent of observed for mean annual snowfall. We also compute resulting snowpack using a variation of the model of Martinec et al. (1983). This allows additional tests by examining spatial patterns of predicted snowfall and snowpack and their hydrologic implications.

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NOAA’s National Centers for Coastal Ocean Science (NCCOS)-Center for Coastal Monitoring and Assessment’s (CCMA) Biogeography Branch, National Park Service (NPS), US Geological Survey, and the University of Hawaii used acoustic telemetry to quantify spatial patterns and habitat affinities of reef fishes around the island of St. John, US Virgin Islands. The objective of the study was to define the movements of reef fishes among habitats within and between the Virgin Islands Coral Reef National Monument (VICRNM), the Virgin Islands National Park (VIIS), and Territorial waters surrounding St. John. In order to better understand species’ habitat utilization patterns among management regimes, we deployed an array of hydroacoustic receivers and acoustically tagged reef fishes. Thirty six receivers were deployed in shallow near-shore bays and across the shelf to depths of approximately 30 m. One hundred eighty four individual fishes were tagged representing 19 species from 10 different families with VEMCO V9-2L-R64K transmitters. The array provides fish movement information at fine (e.g., day-night and 100s meters within a bay) to broad spatial and temporal scales (multiple years and 1000s meters across the shelf). The long term multi-year tracking project provides direct evidence of connectivity across habitat types in the seascape and among management units. An important finding for management was that a number of individuals moved among management units (VICRNM, VINP, Territorial waters) and several snapper moved from near-shore protected areas to offshore shelf-edge spawning aggregations. However, most individuals spent the majority of their time with VIIS and VICRNM, with only a few wide-ranging species moving outside the management units. Five species of snappers (Lutjanidae) accounted for 31% of all individuals tagged, followed by three species of grunts (Haemulidae) accounting for an additional 23% of the total. No other family had more than a single species represented in the study. Bluestripe grunt (Haemulon sciurus) comprised 22% of all individuals tagged, followed by lane snappers (Lutjanus synagris) at 21%, bar jack (Carangoides ruber) at 11%, and saucereye porgy (Calamus calamus) at 10%. The largest individual tagged was a 70 cm TL nurse shark (Ginglymostoma cirratum), followed by a 65 cm mutton snapper (Lutjanus analis), a 47 cm bar jack, and a 41 cm dog snapper (Lutjanus jocu). The smallest individuals tagged were a 19 cm blue tang (Acanthurus coeruleus) and a 19.2 cm doctorfish (Acanthurus chirurgus). Of the 40 bluestriped grunt acoustically tagged, 73% were detected on the receiver array. The average days at large (DAL) was 249 (just over 8 months), with one individual detected for 930 days (over two and a half years). Lane snapper were the next most abundant species tagged (N = 38) with 89% detected on the array. The average days at large (DAL) was 221 with one individual detected for 351 days. Seventy-one percent of the bar jacks (N = 21) were detected on the array with the average DALs at 47 days. All of the mutton snapper (N = 12) were detected on the array with an average DAL of 273 and the longest at 784. The average maximum distance travelled (MDT) was ca. 2 km with large variations among species. Grunts, snappers, jacks, and porgies showed the greatest movements. Among all individuals across species, there was a positive and significant correlation between size of individuals and MDT and between DAL and MDT.

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藻胆体在低浓度磷酸缓冲溶液中发生解离,我们通过藻胆体在解离过程中荧光发射光谱的变化研究藻胆体中藻胆蛋白之间的光能传递. 1.发菜(Nostoc flagelliforme)藻胆体在0.9M磷酸缓冲溶液中较稳定,其77K荧光发射光谱中只有一个荧光峰F686,属于别藻蓝蛋白-B的荧光峰。当藻胆体在低浓度缓冲溶液中时,荧光峰除了686nm,还出现F648和F666肩,而且F648先于F666肩出现.这说明C-藻蓝蛋白(F'648)所捕获的光能已不能全部传给别藻蓝蛋白-B,并说明藻蓝蛋白与别藻蓝蛋白之间的断裂先于别藻蓝蛋白与别藻蓝蛋白-B之间的断裂。当进一步解离时,主峰仍位于648nm,次峰位于686nm.而666nm荧光肩消失,说明C-藻蓝蛋白所捕获的光能已不能传给别藻蓝蛋白,但能传给别藻蓝蛋白-B.我们因此提出在该藻胆体中藻胆蛋白之间的光能传递途径如下: C一藻红蛋白一C-藻蓝蛋白一别藻蓝蛋白_-别藻蓝蛋白-B 在藻胆体的结构方面,我们提出一部分C-藻蓝蛋白与别藻蓝蛋白相连接,另一部分与别藻蓝蛋白-B相连接. 2.聚球藻( synechococcus leopoliensis 625)藻胆体在0.6M,0.3M和0.1M磷酸缓冲液中解离时,其77K荧光光谱中只出现别藻蓝蛋白-B(F'684)和C-藻蓝蛋白(F655)的荧光峰消长变化,没有出现别藻蓝蛋白(F666)的荧光,我们为此提出在该藻胆体中光能从C-藻蓝蛋白传给别藻蓝蛋白-B有两条途径:一是直接传给别藻蓝蛋白-B,另一是传递给别藻蓝蛋白和别藻蓝蛋白-B的复合物,此复合物在0.lM到0,6M磷酸缓冲液中比较稳定.即: c-藻红蛋白→c—藻蓝蛋白—①别藻蓝蛋白-别藻蓝蛋白-B复合物、②别藻蓝蛋白-B

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Ninety-six bigeye tuna (88– 134 cm fork length) were caught and released with implanted archival (electronic data storage) tags near fish-aggregating devices (FADs) in the equatorial eastern Pacific Ocean (EPO) during April 2000. Twenty-nine fish were recaptured, and the data from twenty-seven tags were successfully downloaded and processed. Time at liberty ranged from 8 to 446 days, and data for 23 fish at liberty for 30 days or more are presented. The accuracy in geolocation estimates, derived from the light level data, is about 2 degrees in latitude and 0.5 degrees in longitude in this region. The movement paths derived from the filtered geolocation estimates indicated that none of the fish traveled west of 110°W during the period between release and recapture. The null hypothesis that the movement path is random was rejected in 17 of the 22 statistical tests of the observed movement paths. The estimated mean velocity was 117 km/d. The fish exhibited occasional deep-diving behavior, and some dives exceeded 1000 m where temperatures were less than 3°C. Evaluations of timed depth records, resulted in the discrimination of three distinct behaviors: 54.3% of all days were classified as unassociated (with a floating object) type-1 behavior, 27.7% as unassociated type-2 behavior, and 18.7% as behavior associated with a floating object. The mean residence time at floating objects was 3.1 d. Data sets separated into day and night were used to evaluate diel differences in behavior and habitat selection. When the fish were exhibiting unassociated type-1 behavior (diel vertical migrations), they were mostly at depths of less than 50 m (within the mixed layer) throughout the night, and during the day between 200 and 300 m and 13° and 14°C. They shifted their average depths in conjunction with dawn and dusk events, presumably tracking the deep-scattering layer as a foraging strategy. There were also observed changes in the average nighttime depth distributions of the fish in relation to moon phase.

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近二十年来,碳同位素技术己被广泛应用于植物生态学,特别是植物“碳一水”关系的研究中。植物的碳同位素组成(δ13C值)是叶片组织合成过程中光合活动的整合,它反映了植物长期的水分利用效率。内蒙古锡林河流域位于我国温带典型草原的核心区域,水分是制约本区植物生产力和群落稳定性的限制因素。因此关于本区植物水分利用效率和水分利用状况的研究,对探讨植物对生境干旱化的适应与响应机制具有十分重要的理论和实践意义。本研究沿土壤水分梯度在锡林河流域选取了沼泽化草甸、盐化草甸、草甸草原、典型草原、退化草地和疏林沙地等8个代表性植物群落,研究主要植物种、功能群和群落的碳同位素组成及叶片含水量、脯氨酸含量等与植物抗旱性相关的生理指标的变化,从植物种、功能群和群落三个层次研究了不同水分条件下植物水分利用效率的变化及其对不同水分生境的响应与适应机制。   1)在所调查的8个植物群落中,C3植物占绝对优势;C3植物的δ13C值和水分利用效率越大,其在整个流域中的分布频度越高,生物量也越大;与生长在湿润生境中的植物相比,生长在较干旱生境中的植物能积累更高水平的脯氨酸。以上结果表明,锡林河流域的植物可能通过两种机制适应当地的干旱生境:一是通过调节气孔导度提高植物的水分利用效率;止是通过积累高水平的脯氨酸增强植株的渗透调节能力并维持相对稳定的水分含量。   2)依照生活型将锡林河流域主要植物种划分成6个植物功能群:乔木、灌木、半灌木、多年生禾草、多年生杂类草和一年生植物。在较湿润生境,多年生杂类草更加丰富并构成了群落地上生物量的绝大部分;而在较干旱生境下,多年生禾草在群落中起更重要的作用;随着土壤含水量下降,灌木和半灌木逐渐增多,且在退化草地和沙地中其相对生物量迅速增加;多年生禾草别3c值显著高于其它功能群;随着土壤水分可利用性降低,多年生禾草和杂类草的别3c值表现出增加的趋势,而灌木/半灌木则表现出相反的趋势。以上结果进一步证明了,在典型草原区以生活型为基础划分的植物功能群可以用来进行较大尺度植物一水分关系的研究。   3)依照植物的水分生态类群,将锡林河流域主要植物种划分为六个植物功能群:旱生植物、中旱生植物、旱中生植物、中生植物、湿中生植物和湿生植物。在较湿润生境中(沼泽化草甸和盐化草甸),湿中生和湿生植物成为优势种并构成地上生物量的主体;在干旱生境中(草甸草原、典型草原和退化草地),旱生和中早生植物占绝对优势并构成群落生物量的90%以上;随着不同水分生态类群所适应的生境从干旱到湿润逐渐转变,植物的δ13C值和水分利用效率显著降低;旱生植物叶片脯氨酸含耸最高,湿中生和湿生植物脯氨酸含量最低,不同水分生态类群脯氨酸含量与其δ13C值和地上生物星.显著正相关关系。   4)不同群落类型的平均δ13C值有显著不同,表现为:典型草原>退化草地>沙地>退化恢复草地>草甸草原之盐化草甸>沼泽化草甸。C4植物的出现、不同物种δ13C值的差异和同一物种在不同生境下δ13C值的变化是影响群落平均δ13C值的主要因素,而这些因素与土壤水分状况和干扰历史(特别是放牧)密切相关。   此外,本文还研究了氮素添加对羊草和大针茅光合和水分利用效率的影响。土壤含氮量的增加可以显著提高羊草叶片光合能力和叭JE,而对大针茅的影响不大。作为锡林河流域两种优势植物,羊草和大针茅通过不同的生理机制来维持较高的WUE适应干旱生境:羊草为高光合、高蒸腾,而大针茅为低光合、低蒸腾。羊草较高的WUE是以降低氮利用效率 (NuE)为代价的;而大针茅在维持较高WUE的同时仍能维持较高的NUE,这一特征使大针茅可以广泛分布于更加干旱和贫瘩的地区。   以上研究结果,为深入开展典型草原生态系统植物与水分关系的研究提供了有价值的信息,进一步证实了稳定性碳同位素技术可以有效地指示不同群落类型中主要植物种长期水分利用效率。同时,通过对其它相关生理指标的测定,可以更好地探讨植物对水分限制的适应策略。我们的研究结果从植物种、功能群和群落三个层次进一步揭示了植物对干旱生境的适应机制,并初步阐明了人类干扰特别是过度放牧对草原群落建群种和优势种的生态替代或/和灌丛入侵的影响。这些研究对生物多样性保护、全球变化和区域可持续发展等热点问题的研究都具有重要的意义。在今后的研究中,结合其它稳定性同位素(如2H,18O和15N)技术,将有助于我们进一步深入研究蒙古高原植物对气候变化和过度放牧的适应与响应机制。