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刘俊  何秀凤  刘炎雄 《大地测量与地球动力学》2014,34(4):117-122

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李黎  龙四春  沈军  李浩军  张立亚 《大地测量与地球动力学》2014,34(2):74-78

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Seasonal Variations in Phytoplankton Community Structure in the Sanggou,Ailian, and Lidao Bays     

YUAN Mingli  ;ZHANG Cuixia  ;JIANG Zengjie  ;GUO Shujin  ;SUN Jun 《青岛海洋大学学报(英文版)》2014,(6):1012-1024

The seasonal variations in phytoplankton community structure were investigated for the Sanggou Bay （SGB） and the adjacent Ailian Bay （ALB） and Lidao Bay （LDB） in Shandong Peninsula,eastern China.The species composition and cell abundance of phytoplankton in the bay waters in spring （April 2011）,summer （August 2011）,autumn （October 2011）,and winter （January 2012） were examined using the Uterm6hl method.A total of 80 taxa of phytoplankton that belong to 39 genera of 3 phyla were identified.These included 64 species of 30 genera in the Phylum Bacillariophyta,13 species of 8 genera in the Phylum Dinophyta,and 3 species of 1 genus in the Phylum Chrysophyta.During the four seasons,the number of phytoplankton species （43） was the highest in spring,followed by summer and autumn （40）,and the lowest number ofphytoplankton species （35） was found in winter.Diatoms,especially Paralia sulcata （Ehrenberg） Cleve and Coscinodiscus oculus-iridis Ehrenberg,were predominant in the phytoplankton community throughout the study period,whereas the dominance of dinoflagellate appeared in summer only.The maximum cell abundance of phytoplankton was detected in summer （average 8.08 × 103 cells L-1） whereas their minimum abundance was found in autumn （average 2.60 x 103 cellsL-1）.The phytoplankton abundance was generally higher in the outer bay than in the inner bay in spring and autumn.In summer,the phytoplankton cells were mainly concentrated in the south of inner SGB,with peak abundance observed along the western coast.In winter,the distribution of phytoplankton cells showed 3 patches,with peak abundance along the western coast as well.On seasonal average,the Shannon-Wiener diversity indices of phytoplankton community ranged from 1.17 to 1.78 （autumn 〉 summer 〉 spring 〉 winter）,and the Pielou＇s evenness indices of phytoplankton ranged from 0.45 to 0.65 （autumn 〉 spring 〉 summer〉 winter）.According to the results of canonical correspondence analysis,phosphate level w  相似文献   

基于GIS的广东冬种辣椒气候适宜性区划   总被引：3，自引：0，他引：3  

王华  胡飞  黄俊 《气象与环境科学》2014,37(3):76-80

基于广东省86个气象站1980-2012年气候资料和1991-2010年冬季寒害灾情资料,采用冬季(12月一翌年2月)≥15℃有效积温作为冬种辣椒的气候资源指标,选取寒害过程中最低气温＜10℃的天数、日最低气温＜10.0℃积寒量构建冬种辣椒的寒害风险指标,完善了冬种辣椒的种植气候适宜性指标.构建指标的空间分析模型,采用ArcGIS的空间分析和多层复合方法,对广东冬种辣椒的气候适宜性进行了区域划分.结果表明,冬种辣椒的气候最适宜种植区主要分布在雷州半岛、茂名、阳江等地区,适宜种植区主要分布在南部沿海地区和中部偏南地区,次适宜种植区主要分布在中部偏北地区和北部偏南地区,不适宜种植区主要分布在肇庆、清远、韶关、河源及梅州等地的北部.  相似文献   

EMD方法在广西夏季降水量预测中的应用     

马军  陆甲  赵金彪 《气象研究与应用》2014,35(3):31-35

对广西夏季降水量进行EMD分解后,利用均生函数相关法,比较不同IMF分量组合建模的预测,不同组合试验预测显示,用前二个IMF分量组合建模预测是最佳的组合方案。经对2001—2010年共10年广西夏季降水量实际预测检验表明,趋势预测准确率达70%以上,对夏季降水量预测较有参考价值。为基层台站的气候预测及服务提供一个客观预测方法。  相似文献   

颗粒态有机物在长江口及其邻近海域的夏季分布和影响因素初析   总被引：1，自引：1，他引：0  

邵锡斌  吴莹  胡俊  鲍红艳 《海洋与湖沼》2014,45(6):1288-1294

利用气相色谱法对长江口及其邻近海域的表层颗粒态木质素(p-lignin)进行测定和分析,结合粒度、有机碳(OC%)、叶绿素a(Chl a)、碳稳定同位素(δ13C)等参数研究颗粒态有机物的夏季分布,并对其分布影响因素进行了初步分析。结果表明,悬浮颗粒物粒度组成以粘土和粉砂为主,平均粒径为7.9μm;OC%的值为0.57—7.41%,Chl a的值为0.35—3.71μg/L,δ13C的值为-25.7‰—–16.6‰,在口门外水华站位出现OC%、Chl a和δ13C的最大值,表明浮游生物的现场生产是主要贡献;紫丁香基酚类(S)、香草基酚类(V)和肉桂基酚类(C)8种木质素酚单体的含量Λ8(相对于总有机碳的含量)为0.0406—1.47mg/100mg OC;紫丁香基系列与香草基系列的质量比值(S/V)的分布范围较宽,为0.5—1.6之间,均值为0.8;肉桂基含量与香草基含量比值(C/V)的分布范围为0.02—0.2之间,均值为0.09;香草基酚类的酸醛比值[(Ad/Al)v]在0.24—2.30之间。盐度、总悬浮颗粒物(TSM)浓度是控制长江口内区与邻近海域颗粒态有机物来源与分布差异的重要控制因素,颗粒态木质素在向海输送过程中还会受到矿物组分、生物降解、浮游生物现场生产等各种因素的作用,使其组成成分和性质发生改变。木质素等参数表明最大浑浊带尽管对颗粒态有机物向海输送有改造作用,但是影响区域有限。  相似文献   

Phylogenomic analysis of transcriptomic sequences of mitochondria and chloroplasts for marine red algae (Rhodophyta) in China   总被引：1，自引：1，他引：0  

JIA Shangang  WANG Xumin  QIAN Hao  LI Tianyong  SUN Jing  WANG Liang  YU Jun  LI Xingang  YIN Jinlong  LIU Tao  WU Shuangxiu 《海洋学报(英文版)》2014,33(2):86-93

The chloroplast and mitochondrion of red algae （Phylum Rhodophyta） may have originated from different endosymbiosis. In this study, we carried out phylogenomic analysis to distinguish their evolutionary lin-eages by using red algal RNA-seq datasets of the 1 000 Plants （1KP） Project and publicly available complete genomes of mitochondria and chloroplasts of Rhodophyta. We have found that red algae were divided into three clades of orders, Florideophyceae, Bangiophyceae and Cyanidiophyceae. Taxonomy resolution for Class Florideophyceae showed that Order Gigartinales was close to Order Halymeniales, while Order Graci-lariales was in a clade of Order Ceramials. We confirmed Prionitis divaricata （Family Halymeniaceae） was closely related to the clade of Order Gracilariales, rather than to genus Grateloupia of Order Halymeniales as reported before. Furthermore, we found both mitochondrial and chloroplastic genes in Rhodophyta under negative selection （Ka/Ks〈1）, suggesting that red algae, as one primitive group of eukaryotic algae, might share joint evolutionary history with these two organelles for a long time, although we identified some dif-ferences in their phylogenetic trees. Our analysis provided the basic phylogenetic relationships of red algae, and demonstrated their potential ability to study endosymbiotic events.  相似文献   

Transcriptome characterization of Ishige okamurae (Phaeophyceae) shows strong environmental acclimation     

QU Jieqiong  WANG Xumin  CHI Shan  WU Shuangxiu  SUN Jing  LIU Cui  CHEN Shengping  YU Jun  LIU Tao 《海洋学报(英文版)》2014,33(2):20-26

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Transcriptome-wide evolutionary analysis on essential brown algae (Phaeophyceae) in China   总被引：1，自引：1，他引：0  

SUN Jing  WANG Liang  WU Shuangxiu  WANG Xumin  XIAO Jingf  CHI Shan  LIU Cui  REN Lufeng  ZHAO Yuhui  LIU Tao  YU Jun 《海洋学报(英文版)》2014,33(2):13-19

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琼东南盆地深水区构造热演化特征及其影响因素分析   总被引：5，自引：1，他引：4  

王振峰  施小斌  杨军  黄保家  孙珍  WANG Yahui  蒋海燕  于传海  杨小秋 《海洋学报(英文版)》2014,33(12):107-117

To reveal the tectonic thermal evolution and influence factors on the present heat flow distribution, based on 154 heat flow data, the present heat flow distribution features of the main tectonic units are first analyzed in detail, then the tectonic thermal evolution histories of 20 profiles are reestablished crossing the main deep-water sags with a structural, thermal and sedimentary coupled numerical model. On the basis of the present geothermal features, the Qiongdongnan Basin could be divided into three regions: the northern shelf and upper slope region with a heat flow of 50–70 m W/m2, most of the central depression zone of 70–85 m W/m2, and a NE trending high heat flow zone of 85–105 m W/m2 lying in the eastern basin. Numerical modeling shows that during the syn-rift phase, the heat flow increases generally with time, and is higher in basement high area than in its adjacent sags. At the end of the syn-rift phase, the heat flow in the deepwater sags was in a range of 60–85 m W/m2, while in the basement high area, it was in a range of 75–100 m W/m2. During the post-rift phase, the heat flow decreased gradually, and tended to be more uniform in the basement highs and sags. However, an extensive magmatism, which equivalently happened at around 5 Ma, has greatly increased the heat flow values, and the relict heat still contributes about 10–25 m W/m2 to the present surface heat flow in the central depression zone and the southern uplift zone. Further analyses suggested that the present high heat flow in the deep-water Qiongdongnan Basin is a combined result of the thermal anomaly in the upper mantle, highly thinning of the lithosphere, and the recent extensive magmatism. Other secondary factors might have affected the heat flow distribution features in some local regions. These factors include basement and seafloor topography, sediment heat generation, thermal blanketing, local magmatic injecting and hydrothermal activities related to faulting and overpressure.  相似文献