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本文借助扫描电镜和光学显微镜系统地观察和研究了中国紫草科42属129种植物的花粉形态,并对其中39属45种植物花粉壁做了起薄切片,并用透射电镜研究其外壁内部的超微结构。 并根据花粉形态特征,做了聚类分析。 紫草科花粉是一个多类型的类群。大多数属种为等极花粉,少数为异极,稀为亚等极。形状以茧形花粉占优势,其次是长球形或近长球形,还有少数为球形或近球形、椭球形、卵球形,个别种为哑铃形。花粉大小变异也很大,从最小的6.09×3.4num到最大的69.16um。萌发孔结构复杂,类型繁多,在本文观察的129种植物中就有二十三种萌发孔类型,它们不仅在萌发孔数量上面且在其形状和结构上也有差别,其中以三孔沟、 三孔沟和三假沟为本科的主要类型。外壁主要为光滑和具或多或少的孔穴,少数种还具有刺状、网状、瘤状或短棒等纹饰。外壁在透射电镜下分层性明显,为完全覆盖层,偶具穿孔,柱状层大多数分化较好,小柱直立, 少数柱状层分化不明显,成团块状或结构模糊,柱状层厚度不等,有的稍厚,但有的很薄,基层一般都存在,个别种不明显,但有的的种又特别厚,外壁内层一般在萌发孔区加厚,少数加厚不明显或稍加厚。内壁明显或否。根据花粉形态特征,编了属的检索表。 根据花粉形态的演化规律,本文讨论了紫草科花粉的萌发孔、形状、大小、外壁纹饰及壁的结构等的演化趋势。 在研究花粉形态特征的基础上, 对紫草科的系统分类进行了探讨;对其中归属争议比较大的某些类群, 从花粉形态上提出了自己的观点。 最后讨论了花粉的形态与其适应性的关系。 从其花粉形态特征和高度的适应性上,显示出紫草科是一个适应昆虫传粉, 并且比较进化的类群。

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松科植物的叶绿体和线粒体基因分别为父系和母系遗传,二者的联合分析为系统发育重建,特别是揭示网状进化过程提供了便利条件。此外,松科中的多个属(如黄杉属、铁杉属等)呈洲际间断分布,是研究生物地理学问题的良好试材。 本文选择来自于叶绿体和线粒体基因组的5个DNA片段,通过序列分析对黄杉属的所有8个种进行了系统发育重建;同时结合已有的对黄杉属的各方面研究,讨论了该属典型的东亚-北美间断分布式样的形成过程。主要结果如下: (1) 叶绿体DNA片段trnfM-trnS、rpl20和trnP的序列分析 无论叶绿体基因两两组合分析还是3个叶绿体片段的联合分析均强烈支持东亚的6种黄杉属植物聚为一支(支持率>96%),其中日本黄杉位于最基部,其他分布于中国的5个种聚在一起。 (2) 线粒体基因nad5和cox1的序列分析 线粒体基因序列的进化速率较慢,信息位点相对较少,因此分辨率较低。本文中线粒体DNA序列在黄杉属的东亚物种间几乎没有分辨率,但是仍以>60%的Bootstrap支持率将该属分为东亚与北美两个姐妹支。 (3) 5个DNA片段的联合分析 5个细胞质DNA片段(trnfM-trnS, rpl20, trnP, nad5, cox1)的联合数据矩阵长4351 bp,其中含变异位点129个(3.0%),信息位点109个(2.5%)。利用最大简约法进行的系统发育分析表明:黄杉属分成北美和东亚两支,与地理分布相吻合,并分别得到了66%和100%的支持;中国的5个物种形成一个单系分支,该分支与日本黄杉为姐妹群关系。 根据上述叶绿体和线粒体DNA片段的序列分析结果,并结合前人的研究资料,我们认为黄杉属通过白令陆桥扩散后,在北美和东亚独立进化,但该属的起源地尚需要进一步研究。

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Tubular graphite cones (TGCs) with a single-crystal nanotip have been achieved by means of microwave plasma-assisted chemical vapor deposition using in-situ-evaporated Fe catalysts. The absence of the disorder-induced D band in Raman spectra revealed the single-crystalline feature of the nanotip. TGCs were found to stem from Fe catalytic carbon spherules on the order of 100 mum diameter, whose critical role in promoting both nucleation and plasma annealing in the formation of highly crystalline TGCs is discussed. The crystalline quality of such TGCs can be further verified by the investigation of their oxidative stability in air. All TGCs can survive up to 600 degrees C without any structural variations, and a few TGCs still survive with an anisotropic etched and stepped nanotip at temperatures up to 800 degrees C, much better than CNTs. Thus, TGCs with single crystalline nanotips are potential candidates for scanning probes in high-temperature oxygen-containing environments.

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In June 2008, the NOAA National Ocean Service (NOS), in conjunction with the EPA National Health and Environmental Effects Laboratory (NHEERL), conducted an assessment of the status of ecological condition of soft-bottom habitat and overlying waters within the boundaries of Stellwagen Bank National Marine Sanctuary (SBNMS). The sanctuary lies approximately 20 nautical miles east of Boston, MA in the southwest Gulf of Maine between Cape Ann and Cape Cod and encompassing 638 square nautical miles (2,181 km2). A total of 30 stations were targeted for sampling using standard methods and indicators applied in prior NOAA coastal studies and EPA’s Environmental Monitoring and Assessment Program (EMAP) and National Coastal Assessment (NCA). A key feature adopted from these studies was the incorporation of a random probabilistic sampling design. Such a design provides a basis for making unbiased statistical estimates of the spatial extent of ecological condition relative to various measured indicators and corresponding thresholds of concern. Indicators included multiple measures of water quality, sediment quality, and biological condition (benthic fauna, fish tissue contaminant levels). Depths ranged from 31 – 137 m throughout the study area. About 76 % of the area had sediments composed of sands (< 20 % silt-clay), 17 % of the area was composed of intermediate muddy sands (20 – 80 % silt-clay), and 7 % of the sampled area consisted of mud (> 80 % siltclay). About 70 % of the area (represented by 21 sites) had sediment total organic carbon (TOC) concentrations < 5 mg/g and all but one site (located in Stellwagen Basin) had levels of TOC < 20 mg/g, which is well below the range potentially harmful to benthic fauna (> 50 mg/g). Surface salinities ranged from 30.6 – 31.5 psu, with the majority of the study region (approximately 80 % of the area) having surface salinities between 30.8 and 31.4 psu. Bottom salinities varied between 32.1 and 32.5 psu, with bottom salinities at all sites having values above the range of surface salinities. Surface-water temperatures varied between 12.1 and 16.8 ºC, while near-bottom waters ranged in temperature from 4.4 – 6.2 ºC. An index of density stratification (Δσt) indicated that the waters of SBNMS were stratified at the time of sampling. Values of Δσt at 29 of the 30 sites sampled in this study (96.7 % of the study area) varied from 2.1 – 3.2, which is within the range considered to be indicative of strong vertical stratification (Δσt > 2) and typical of the western Gulf of Maine in summer. Levels of dissolved oxygen (DO) were confined to a fairly narrow range in surface (8.8 – 10.4 mg/L) and bottom (8.5 – 9.6 mg/L) waters throughout the survey area. These levels are within the range considered indicative of good water quality (> 5 mg/L) with respect to DO. None of these waters had DO at low levels (< 2 mg/L) potentially harmful to benthic fauna and fish.

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Loligo opalescens live less than a year and die after a short spawning period before all oocytes are expended. Potential fecundity (EP), the standing stock of all oocytes just before the onset of spawning, increased with dorsal mantle length (L), where EP = 29.8L. For the average female squid (L of 129 mm), EP was 3844 oocytes. During the spawning period, no oogonia were produced; therefore the standing stock of oocytes declined as they were ovulated. This decline in oocytes was correlated with a decline in mantle condition and an increase in the size of the smallest oocyte in the ovary. Close agreement between the decline in estimated body weight and standing stock of oocytes during the spawning period indicated that maturation and spawning of eggs could largely, if not entirely, be supported by the conversion of energy reserves in tissue. Loligo opalescens, newly recruited to the spawning population, ovulated about 36% of their potential fecundity during their first spawning day and fewer ova were released in subsequent days. Loligo opalescens do not spawn all of their oocytes; a small percentage of the spawning population may live long enough to spawn 78% of their potential fecundity. Loligo opalescens are taken in a spawning grounds fishery off California, where nearly all of the catch are mature spawning adults. Thirty-three percent of the potential fecundity of L. opalescens was deposited before they were taken by the fishery (December 1998−99). This observation led to the development of a management strategy based on monitoring the escapement of eggs from the fishery. The strategy requires estimation of the fecundity realized by the average squid in the population which is a function of egg deposition and mortality rates. A model indicated that the daily total mortality rate on the spawning ground may be about 0.45 and that the average adult may live only 1.67 days after spawning begins. The rate at which eggs escape the fishery was modeled and the sensitivity of changing daily rates of fishing mortality, natural mortality, and egg deposition was examined. A rapid method for monitoring the fecundity of the L. opalescens catch was developed.

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An assessment of the total biomass of shortbelly rockfish (Sebastes jordani) off the central California coast is presented that is based on a spatially extensive but temporally restricted ichthyoplankton survey conducted during the 1991 spawning season. Contemporaneous samples of adults were obtained by trawl sampling in the study region. Daily larval production (7.56 × 1010 larvae/d) and the larval mortality rate (Z=0.11/d) during the cruise were estimated from a larval “catch curve,” wherein the logarithm of total age-specific larval abundance was regressed against larval age. For this analysis, larval age compositions at each of the 150 sample sites were determined by examination of otolith microstructure from subsampled larvae (n=2203), which were weighted by the polygonal Sette-Ahlstrom area surrounding each station. Female population weight-specific fecundity was estimated through a life table analysis that incorporated sex-specific differences in adult growth rate, female maturity, fecundity, and natural mortality (M). The resulting statistic (102.17 larvae/g) was insensitive to errors in estimating M and to the pattern of recruitment. Together, the two analyses indicated that a total biomass equal to 1366 metric tons (t)/d of age-1+ shortbelly rockfish (sexes combined) was needed to account for the observed level of spawning output during the cruise. Given the long-term seasonal distribution of spawning activity in the study area, as elucidated from a retrospective examination of California Cooperative Oceanic Fisheries Investigation (CalCOFI) ichthyoplankton samples from 1952 to 1984, the “daily” total biomass was expanded to an annual total of 67,392 t. An attempt to account for all sources of error in the derivation of this estimate was made by application of the delta-method, which yielded a coefficient of variation of 19%. The relatively high precision of this larval production method, and the rapidity with which an absolute biomass estimate can be obtained, establishes that, for some species of rockfish (Sebastes spp.), it is an attractive alternative to traditional age-structured stock assessments.