中国菌藻类煤的成因分类 形成条件及其特征     

解光新  李小彦  庄军 《煤田地质与勘探》2001,29(3):10-13

运用煤岩学和地球化学方法, 对中国山西浑源等4个典型的菌藻类煤进行了综合研究, 结果表明, 菌藻类煤在物理、化学组成和特性上与腐植煤有明显的区别; 其形成环境主要受 p H、Eh值和有机质含量的制约, 其中皮拉藻和轮奇藻具有含量高、生存时间长的特征; 并在此基础上对菌藻类煤作了成因分类。   相似文献   

平邑盆地下第三系官中段核形石成因分析   总被引：23，自引：0，他引：23  

李熙哲  管守锐 《岩石学报》2000,16(2):261-268

平邑盆地下第三系官中段核形石较为发育,类型多样。通过对其内部结构的研究发现核形石单元纹层有六种类型,作为核心的藻类仅在顶端发生碎屑粘结效应,而其底部则发育厚度小,规则的暗色纹层。纹层组合类型多样,主要受藻类发育程度,水动力强度和藻类种属的控制,是不同水动力环境下的产物。根据颗粒大小、纹层组合类型纹层层数、填隙物将核形石分为浅水高能成因核形石和较深水低能成因核形石。核形石成因分析和分类对沉积环境的判  相似文献   

Environmental Factors Affecting the Occurrence and Production of the Spring Phytoplankton Bloom in Funka Bay, Japan     

Isao Kudo  Katsuhiko Matsunaga 《Journal of Oceanography》1999,55(4):505-513

The concentration of nutrients was measured during the spring phytoplankton bloom in Funka Bay over a 5-year period (1988–92). During the winter mixing period, nutrient concentrations were similar in every year except in 1990 when a high concentration of silicate was observed. There was interannual variation in the onset of the bloom, presumably depending on the stability of the water column. The bloom developed in early March when the Oyashio water (OW), which has a lower density than the existing winter water, flowed into the bay and the pycnocline formed near the bottom of the euphotic zone. In this case, high chl a was found only in the euphotic zone and nutrient utilization was limited to this zone. In the year when the inflow of OW was not observed by April, the bloom took place at the end of March without strong stratification and high chl a was found in the whole water column, accompanied by a decrease in nutrients. Interannual differences were found not only at the beginning of the decrease, but also in the thickness of the layer which showed a decrease in nutrients. Primary production from the beginning to the end of the spring bloom was estimated from the nutrient budget before and after the spring bloom. The integrated production over the spring bloom period ranged from 25 to 73 g C m^-2, which accounts for 19–56% of the annual production in this bay. We found that the timing of the bloom was strongly dependent on the inflow of OW, but the amount of production was not clearly related to this timing.  相似文献   

A Massive Coccolithophorid Bloom Observed in Mikawa Bay, Japan     

Masanobu Kai  Tamotsu Hara  Hiroaki Aoyama  Nobuo Kuroda 《Journal of Oceanography》1999,55(3):395-406

In April 1996, a massive algal bloom of the coccolithophorid Gephyrocapsa oceanica developed in both Chita Bay and Atsumi Bay which comprise the bay known as Mikawa Bay of Japan. It was the first record of such a bloom in this area. In Chita Bay, the bloom persisted until the middle of May, however in Atsumi Bay, it remained until early June. From the analysis of salinity, water temperature, and current velocity and direction data, it is considered that the following mechanism accounts for the occurrence and maintenance of the bloom: Before the bloom, the standing crop of phytoplankton was poor, resulting in relatively rich nutrients throughout the bay. Thereafter, with the influx of oceanic water into Mikawa Bay, high salinity occurred firstly in Chita Bay. Under these hydrographic conditions, the bloom occurred first in Chita Bay, and extended throughout the bay with the clockwise circulation of water into Atsumi Bay. In Chita Bay, the bloom was influenced by rainfall and G. oceanica flowed out from this area. Whereas, in Atsumi Bay, the bloom persisted for longer due to the clockwise circulation and another influx of oceanic water.  相似文献   

徐州贾汪地区中—上寒武统藻礁,风暴层与海平面变化   总被引：5，自引：1，他引：4  

彭阳  乔秀夫 《地质论评》1999,45(2):193-207

笔者详细研究了徐州贾汪地区中－上寒武统的二郎山等剖面,将张夏组－凤山组划分为３个各具特色的三级层序,根据各层序内副层序的堆叠形式进一上划分出海侵体系域（ＴＳＴ）凝缩段（ＣＳ）及高位体系域（ＨＳＴ）其中张夏层序的藻礁为中－晚寒武世期间发育的最大规模碳酸盐岩缓坡藻礁,崮山层序凝胶缩代表中－晚寒武世最大海泛（海侵）期沉积,长山－凤山层序顶部白云岩代表中－晚寒武世最小海平面（海退）时期的沉积。  相似文献   

杭州西湖湖底附泥藻群落     

项斯端  吴文卫 《湖泊科学》1999,11(2):177-183

杭州西湖在 ２０世纪 ４０年代湖底附泥藻群落以蓝藻门静水隐杆藻为优势,占 ９８％－ ９９％,而 ９０年代本次调查时发现随着水体富营养化底栖性的附泥藻群落由蓝藻型转变为以硅藻门放射针杆藻为优势的群落．根据１９９１年４月及１２月调查全湖各湖区该群落分为三个组合：（ １）放射针杆藻组合：外湖及北里湖,藻密度高,（ ３０２－ ５７５） ｘ １０_４个· ｇ~（-１）．放射针杆藻占总藻量的４１２％－５２８％．（２）凸腹脆杆藻－放射针杆藻组合：分布在西部三个湖区．藻密度低,仅为前一组合的 １１３或 １１８．（３）静水隐杆藻组合：仅存在于三潭印月内湖．  相似文献   

太湖水质时空特性及其与蓝藻水华的关系   总被引：16，自引：5，他引：11  

张晓晴  陈求稳 《湖泊科学》2011,23(3):339-347

以太湖2005-2007年的连续监测资料为基础,运用聚类分析和自相关分析方法,针对总无机磷,总无机氮、水温等环境理化因素与叶绿素a进行时空序列分析,初步归纳了当前太湖水质指标变化的空间特点、时问周期性及其与蓝藻水华暴发的关系.结果表明,太湖水质的空间分布大致分为三个人湖河口、四个湖湾、湖心区、西部湖区、东部湖区等十个区...  相似文献   

太湖蓝藻水华灾害灾情评估方法初探   总被引：3，自引：0，他引：3  

刘聚涛  杨永生  高俊峰  姜加虎 《湖泊科学》2011,23(3):334-338

通过对太湖蓝藻水华灾害影响分析,探讨了太湖蓝藻水华灾害灾情评估指标的选取和评价标准的划分,并采用模糊评价模型构建太湖蓝藻水华灾害灾情综合评估方法.评价指标分为影响人口、影响范围、生态环境影响和经济损失四个方面,其中影响人口指标为受灾人口,影响范围指标包括蓝藻水华面积发生百分比和影响时间,生态环境影响指标包括藻细胞浓度、...  相似文献   

青岛近海球形棕囊藻的宏条形码分析     

王一奇  丁翔翔  宋会银  陈楠生 《海洋与湖沼》2023,54(5):1351-1362

自1997年球形棕囊藻(Phaeocystis globosa)赤潮首次在我国南海海域暴发以来,该赤潮在我国南海和渤海的多个海域频繁暴发,表明球形棕囊藻在我国海域的分布比较广泛。尽管如此,在此之前开展的分类和生态调查研究均未发现我国海域球形棕囊藻的存在。近年来基于分子标记扩增和高通量测序的宏条形码分析检测到了球形棕囊藻,显示出宏条形码分析对球形棕囊藻鉴定的优势。然而,由于包括球形棕囊藻在内的定鞭藻的18S rDNA序列具有较高的G(Guanine,鸟嘌呤)C(Cytosine,胞嘧啶)含量等特点,导致针对球形棕囊藻的宏条形码分析结果在很大程度上依赖分子标记的选择或PCR扩增引物的选择。以青岛栈桥海域样本为研究对象,评估了扩增通用分子标记18S rDNA V4的两套常用PCR引物(即Stoeck引物和Song引物)对球形棕囊藻的宏条形码分析结果的影响,并利用Song引物对青岛近海2021年冬季突发性球形棕囊藻赤潮样本开展了宏条形码分析。分析发现不同引物对定鞭藻门物种的分析结果具有显著影响。利用Stoeck引物的宏条形码分析没有获得任何对应的定鞭藻的ASV(ampliconsequence...  相似文献   

有害藻华数据分析与可视化平台的设计          下载免费PDF全文

李笑语  于仁成  牟乃夏  耿慧霞  王治鹏  史金浩  薛润生 《海洋与湖沼》2023,54(1):58-66

有害藻华是海洋中最为常见的一类生态灾害问题,对养殖业、旅游业和公众健康等造成了严重威胁,也给海洋管理带来了巨大的挑战。近年来,与有害藻华相关的生物、化学、水文、气象等观测数据以及有害藻华发生记录等统计数据不断积累,统计学方法、地理信息系统(Geographic Information System, GIS)等数据分析方法也在快速发展,为深入挖掘有害藻华时空演变特征、提高有害藻华监测预警水平奠定了重要基础。该研究综合应用数据库、地理信息系统及可视化技术,设计了一套集有害藻华多源异构数据管理、分析与可视化为一体的综合平台,能够实现对有害藻华相关数据的存储和动态关联,并集成了空间分析方法,实现了数据和分析产品的可视化。该研究以渤海有害藻华长期时空演变特征探究为案例,展示了该平台在有害藻华数据分析与可视化方面应用效果。该平台可望为公众科普、科学分析和政府决策等提供支撑。  相似文献