黄海大气中的孢粉及其对海底沉积物中孢粉组合的影响

１９７８—１９７９ 年在黄海上空共收集到孢粉３２１ 粒,属２３ 个属种。春季大气中所含孢粉数量最多,秋季次之,夏季和冬季较少。大气中木本花粉含量达７４％ ,草本花粉２３％ ,孢子３％ 。通过大气中孢粉与１９９０ 年黄海表层沉积物中孢粉组合的对比,反映出大气中孢粉与海洋沉积物中孢粉属种具有明显的对应关系。海洋沉积物中的孢粉分布显现近岸草本花粉含量高,远海木本花粉含量高的规律     

Comparison between airborne pollens in Torino and Perugia (Italy) 1982–83–84

Summary By means of two Burkard Volumetric Spore-Traps situated in the center of Torino and Perugia, pollen was sampled between March and August for three years (1982–83–84). The two pollen spectra, with special reference to trees, were compared for pollen levels and duration of season in the two cities. Comments on vegetation in and around Torino and Perugia and meteorological data are compared with the two pollen spectra.      

我国微型硅藻类的新记录属--拟脆杆藻属

利用透射电镜（TEM）对东海、黄海海域典型站位的微型硅藻进行了研究,观察到我国的一个新记录属——拟脆杆藻属Fragilariopsis Hustedt。该属的主要特征是：1．细胞以壳面全部或大部分相连成带状群体：2．壳缝靠近壳缘,强烈偏心;3．点条纹数目与船骨点大致相等;4．壳面纵轴通常异极;5．点条纹由两列孔纹组成,很少一列或两列以上的。对该属以及在东海、黄海海域发现的该属的两个种——克氏拟脆杆藻E kerguelensis（0’Meara）Hustedt和菱形拟脆杆藻Frhombica（0’Meara）Hustedt进行了较详细的分类特征、生态习性和分布的描述并配有相应的透射电镜照片。     

东海表层沉积硅藻组合与环境关系研究

对东海表层沉积硅藻分析研究,共发现有103种和变种,根据其中分布特征和规律,结合因子负荷变化曲线,把东海表层沉积分为六个硅藻组合和分布区,并探讨影响硅藻分布的环境因素,为恢复古环境提供科学依据。     

Airborne pollen, spores, and dust across the East Mediterranean Sea

Airborne pollen and spores, as well as airflow directions, were continuously monitored during a cruise across the East Mediterranean from Tel Aviv, Israel, to Istanbul, Turkey. In spite of the fact that a high-altitude dust cloud moved, at that, time from North Africa, across the East Mediterranean, only a few dust particles were monitored on the boat. The numbers of counted airborne pollen along the cruise path were rather small. This is, in part, because the trip was taken after the main flowering season in the East Mediterranean region. Nevertheless, airborne pollen grains were still found, either as a result of remnant pollen releases by late-flowering plants or because of secondary lift-up of previously settled pollen. The presented pollen counts are average pollen counts /m³ air /6 h. The counts ranged between ∼5 pollen/m³ of air in mid-sea (July 16th–July 17th) or ∼6 pollen/m³ of air on the Israeli coast (July 16–July 17th), and 30 pollen/m³ of air near the coasts of Turkey and of the Greek Islands (July 18th–July 19th) and some 18 taxa of pollen were identified, most of them at the family level. Some 30 taxa of different spores were recorded. The numbers of airborne spores were relatively low in mid-sea (300–750 spores/m³ air), but were high near the coasts of Turkey (1,200–2,400 spores/m³ air) and of Israel (340–1,695 spores/m³ air).     

我国硅藻类的新记录属--微舟藻属及其一新种

利用透射电镜对采自东黄海海域典型站位的微型硅藻(nanodiatom,〈20μm)进行了研究.观察到我国微型硅藻类的一个新记录属:微舟藻属Nanoneis R.E.Norris以及该属的一个新种:长微舟藻Nanoneislongta sp.nov..该属的主要特征是:壳面两侧对称,具有不完全壳缝,壳面除中轴区外都有横肋纹或长室孔分布.本文描述该属的两个种,其中海斯微舟藻(Nanoneis hasleae R.E.Norris)为我国的新记录种,长微舟藻为新种,两种之间主要的区别特征是壳面外形、长宽比例以及壳面横肋纹的密度.并较详细地描述了该属种类的分类特征、生态习性和分布.     

我国硅藻类的新记录属——微舟藻属及其一新种(英文)

利用透射电镜对采自东黄海海域典型站位的微型硅藻(nanodiatom,<20mm)进行了研究。观察到我国微型硅藻类的一个新记录属微舟藻属NanoneisR.E.Norris以及该属的一个新种长微舟藻Nanoneislongtasp.nov.。该属的主要特征是壳面两侧对称,具有不完全壳缝,壳面除中轴区外都有横肋纹或长室孔分布。本文描述该属的两个种,其中海斯微舟藻(NanoneishasleaeR.E.Norris)为我国的新记录种,长微舟藻为新种,两种之间主要的区别特征是壳面外形、长宽比例以及壳面横肋纹的密度。并较详细地描述了该属种类的分类特征、生态习性和分布。     

南海陆坡沉积物细菌丰度预测

分别利用参数模型和无参数估计法预测南海陆坡沉积物柱MD05-2896中的细菌丰度.基于非培养的PCR-RFLP的16SrRNA基因分子技术,扩增了沉积物柱中的细菌16S rRNA基因序列,并构建16S rRNA基因文库.系统发育分析表明16S rRNA基因文库中,大多数序列属于17个已知的“门”.分别以99％、97％、90％和80％序列一致性作为分类单元分界点,将16SrRNA基因序列组群为分类单元.使用逆高斯分布模型、对数正态分布模型、负二项式分布模型、帕雷托分布模型、双指数分布模型以及ACE、ACE-1等估计方法预测不同分类单元分类水平下的细菌丰度.结果表明在“种”级分类水平上,负二项式分布为最优估计模型,估计细菌丰度为244±10(SE).不过,受实验条件的限制,该估计值可能偏低.     

北部湾中部海域底质沉积物中的有孔虫

本文对北部湾中部海域水深2.4m到61m、共计184个站位表层沉积物中的有孔虫进行研究。结果显示浮游有孔虫丰度非常低,种类也较稀少,仅在南侧水深较大的少数站位有发现,且含量不超过5%;而底栖有孔虫则较丰富,多数样品中以含有螺旋式与平旋式的玻璃质壳类型为主,暖水或大型底栖有孔虫分子常见。和其它海区相较而言,该海域底栖有孔虫中胶结壳类含量偏高,可能与沉积物底质颗粒较粗及海水盐度较低有关。该研究详细报道了底栖有孔虫主要属种在北部湾的分布特征。与海洋环境对比显示,水深和沉积物底质类型是影响这些属种平面分布的主要因素,而湾外温暖水团则是控制暖水种分子分布的另一重要因素。     

南海断面春季放射虫残骸的空间分布及其与表层沉积记录对比

放射虫是揭示古海洋环境信息的重要载体。本文采用虎红染色方法,首次揭示了南海典型断面现代放射虫残骸群的空间分布特征,并比较分析现代水体中放射虫残骸群与海底表层沉积物中放射虫化石群的相互关系。结果表明:南海春季放射虫残骸群比较丰富,其丰度一般呈现出随深度增加而增高的趋势,最高值主要出现在75—300m深即位于叶绿素最大值层和活体高峰深度之下;分析发现研究区放射虫残骸丰度的深度分布受到海流的横向输运影响;春季水体和表层沉积物中放射虫属种组成和丰度分布的差异表明,除了现代放射虫具有季节性变化之外,海流的横向传输也是一个很重要的原因。在150—300m水体中除了Cornutella profunda和Cyrtopera laguncula,还发现了Cycladophora davisiana的残骸,推测典型冷水种C.davisiana由于受到径向翻转流的作用,从中深层水被带到了中上层水体中。     

南海某些表层沉积硅藻的分布及其古环境意义

本文通过对南海表层沉积物样品的硅藻分析,试图揭示南海某些表层沉积硅藻的分布规律,以便为南海古海洋学研究提供科学依据。研究发现,Thalassionema nitzshioides为南海地区表层沉积硅藻的优势种,且其百分含量无明显的区域差异,体现了南海与周围海洋水体交换相对较弱的特征。除此之外,南海表层沉积硅藻的分布主要受到海洋环流的影响,表现在黑潮暖流、印度洋暖水的入侵以及沿岸流对南海表层沉积硅藻分布的影响。其中,Nitzshia marina, Azpeitia neocrenulata , Azpeitia africana , Rhizosolenia bergonii等暖水硅藻可作为黑潮暖流及印度洋暖水入侵南海强度的指标种。而Cyclotella stylorum , Cyclotella striata , Diploneis bombus , Traychneis aspera , Tabularia tabulata等则可看作判断沿岸流对南海水体影响强度的标志种。     

Late Devonian–Early Carboniferous palynology of the CSDP-2 Borehole in the southern Yellow Sea,China

Late Devonian–Early Carboniferous spores recovered from the depths of 2140 m to 2031.3 m in the CSDP-2 Borehole in the southern Yellow Sea are systematically documented to characterize palynological associations for the stratigraphic correlation. The taxonomic study identifies 96 species belonging to 48 genera, including a re-examination of 33 previously described and indeterminate species. Three palynological associations are established for the Wutong Formation in the CSDP-2 Borehole. In ascending order, these are the late Famennian Aneurospora asthenolabrata–Geminospora lemurata (AL) Association from the proposed Guanshan Member, the latest Famennian Cymbosporites circinatus–Asperispora acuta (CA) Association from the lower part of the proposed Leigutai Member, and the Tournaisian Auroraspora macra–Lophozonotriletes involutus (MI) Association of the upper part of the latter member. The AL and CA associations are correlated with the palynological assemblages in the Guanshan Member, and those in the lower to middle parts of the Leigutai Member of the Wutong Formation that outcrops in the suburbs of Nanjing and southern Jiangsu. The MI Association is similar to those derived from the uppermost beds of the subsurface Wutong Formation and is dated as early Tournaisian.     

红树林恢复对潮滩表层沉积物氮素的影响

研究了不同树种的红树林恢复对潮滩表层沉积物氮素的影响。结果表明,红树林恢复提高了潮滩表层沉积物中总氮(TN)含量。以光滩为对照,外来树种和乡土树种的恢复使表层沉积物中的可交换态无机态N(IEF-N)分别朝着相反的方向发展:外来树种——无瓣海桑(Sonneratia apetala)和海桑(S. caseolaris)提高了IEF-N的含量,而乡土树种——秋茄(Kandelia candel)和桐花树(Aegiceras corniculatum)使IEF-N的含量下降。当与近岸水体发生物质营养交换作用时,乡土树种和外来树种的恢复可能导致营养盐在潮滩沉积物水界面间的迁移和交换过程中存在不同的潜在环境效应。     

Factors of influence on microbial pollution in the atmosphere over Beijing area

Summary The atmospheric microbial pollutants are potentially correlated to population density and activity as well as to human health. The higher the population density is, the heavier the air microbial pollution will become. Some meteorological factors exert great influence on air microbial pollution. Generally, wind, solar radiation and rainfalls purify air and, consequently cause a decrease in atmospheric microbial pollution. On the other hand, prevailing strong winds may favour this pollution, especially in dry conditions and in absence of vegetation. Obviously, relatively high temperatures associated with high RH enhance the growing of microbes. However, the higher the temperature is, the lower the viability of airborne microbes will be; nonetheless, with high RH a decrease in suspended particles may be recorded.     

基于模拟降雨试验的喀斯特坡耕地土壤侵蚀特征

探索喀斯特坡耕地土壤侵蚀过程及机理对该区水土流失及石漠化治理具有重要的现实和指导意义.本文采用人工模拟降雨的试验方法,探索喀斯特坡耕地土壤侵蚀过程及特征.结果表明: 降雨强度较小时(30、50 mm·h^-1),水土流失以地下孔(裂)隙流失为主,当降雨强度较大时(80 mm·h^-1),土壤侵蚀以地表流失为主;地表径流模数和输沙率均随坡度的增加而增大,随孔(裂)隙度的增加而减小.地下径流模数在0.37～0.52 L·m^-2·min^-1,地下输沙率在0.81～1.93 g·min^-1,二者均随坡度的增加而减小,随降雨强度的增加呈先增大后减小的变化趋势.     

Determination of nitrite in lake sediments

Abstract

An evaluation of nitrite determination in marine lake sediments has shown that spectrophotometric measurements can be in error due to light scattering by colloidal (<0.2 μm) matter in extract solutions and incomplete nitrite recovery. The scatter error can be minimised by using uncoloured extract in the reference beam but precision at low levels remains poor (RSD 25 to 100%). Recovery tests on ‘spiked’ sediment indicated that optimum retrieval (～85%) occurred with 30 minute mixing with 0.2 M NH₄Cl, using a sediment to extractant ratio of 1:30. To counter this variable, calibration based on standard addition to sample suspensions is recommended. Modified procedure proposed is suitable for measuring up to 10 μg g^?1 of nitrite N; the lake sediments tested contained <100 ng g^?1