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131.
Unicellular gametophytes ofUndaria pinnatifida (Harv.) Sur. were isolated in Qingdao, P. R. China in April 1993 and in Tokushima, southern Japan in March 1995. Different intraspecific crossings by using unicellular male and female gametophytes were successfully undertaken in Sept. of 1995 in Qingdao. Sporophytes were transplanted to two different locations for open sea cultivation. One was at Zhanqiao (ZQ) Bay where the water current was slower than that of another location—Taipingjiao(TPJ). A total of 218 adult sporophytes were harvested on January 12 and 18 from TPJ and ZQ respectively. For eacn combination, 10 sporophytes were cultivated. Analysis of the morphological characteristics of adult sporophytes indicated that the longest length between two bases of the serration of pinnate blades (W2) is a morphological characteristic that can be transferred from the parent plant to the next generations regardless of environmental variations. There was evidence that W2 was apparently determined by sex-linked factors, i.e., by male parental gametophyte. Sporophytes from certain crossing combinations showed more vigorous growth than those from other crossing combinations. It is therefore possible to select gametophyte strains which can be used as parental gametophytes for the seedling production of sporophytes with more vigorous growth within shorter cultivation period. The morphology of hybrids from a Qingdao strain and a Tokushima cultivated strain resembled that of both parental plants in frond features (wrinkled or smooth) and W2. Sporophyll formation also varied with strains. The fact that adult sporophytes resulting from the same crossing combinations have identical morphological characteristics under the same environmental conditions indicates the possibility of a new way to select strains which are expected to be ideal for commerical production by purposely selecting, propagating, and seeding unicellular gametophytes for sporeling production through freeliving techniques of gametophytes. Project 39400102 supported by NSFC, also supported by National Climbing Plan B (PD-B642); and Bioengineering Center, SSTC.  相似文献   
132.
The distribution and abundance of benthic foraminifera and a range of elements have been analysed in six long cores (up to 10 m long) from the Bilbao estuary, N. Spain, to document environmental transformation of this estuarine ecosystem and to determine sediment contamination levels. Three different environmental zones could be distinguished in the recent sedimentary record based on its microfaunal and geochemical contents. Initially, a pre-industrial zone containing very abundant and diverse foraminiferal assemblages together with baseline metal levels. Secondly, an older industrial zone exhibiting co-existence of abundant and diverse foraminiferal assemblages with high concentrations of metals. Finally, a younger industrial zone with extreme concentrations of metals and barren of indigenous foraminifera. This environmental transformation has been caused by the discharge of untreated domestic and industrial effluents during the last 150 years. The occurrence of foraminifera in the two industrial zones and along the estuary is not related to defined levels of metals, and this seems to confirm oxygen limitation as the key factor to explain complete estuarine defaunation during deposition of the younger industrial zone (period 1950-2000). Effectiveness of current regeneration schemes could be assessed using microfaunal and geochemical proxies as environmental quality indicators.  相似文献   
133.
东湾背斜位于准噶尔盆地南缘,采用多种地球物理及地质方法,通过多次论证,证明构造是落实的,且其烃源岩、储集层以及盖层条件都较好,但2003年完钻的东湾1井钻探结果却无任何油气显示。在深入了解准噶尔盆地南缘区域构造背景的基础上,探讨了东湾背斜的构造特征、构造演化过程及油气成藏条件,总结出东湾背斜的油气聚集规律,指出在东湾地区可能存在的两种油气藏模式,最后提出下步有利勘探目标区。  相似文献   
134.
Abstract   A continuous, well-preserved core was obtained from the Choshi area, on the Pacific side of Japan, to investigate paleoceanographic and paleoclimatic changes around the northwestern Pacific region during the middle Pleistocene. Siliciclastic sequences in the core are divided into five formations – the Obama, Yokone, Kurahashi and Toyosato Formations in the Inubo Group and the Katori Formation, in ascending order. Examination of calcareous nannofossils and magnetic polarities detected four datums in the core sediments of the Inubo Group: the top of Reticulofenestra asanoi , the base of Helicosphaera inversa , the top of Pseudoemiliania lacunosa and the Brunhes–Matuyama boundary. Fourteen marine isotope stages (MIS24–MIS11) were identified in the δ18O and δ13C records based on detected datums and the graphic correlation with the standard stack oxygen isotope curve. Magnetic susceptibility and gamma-ray attenuation porosity evaluator density were also measured and low values characterize the glacial intervals. Biogenic sedimentation by primary production may be larger during the glacial periods because of invasions of nutrient-rich northern surface-waters related to the southward shift of the Kuroshio front in the Choshi area.  相似文献   
135.
成像光谱数据特征选择及小麦品种识别实验研究   总被引:6,自引:0,他引:6  
针对河北栾城获得的MAIS成像光谱仪数据用于小麦品种识别进行了特征选择和分类研究。利用遗传算法以JM距离为准则并结合实验区小麦的生物物理特性,进行了最佳波段选择;利用Fuzzy—Anmap分类器及选出的最佳波段对成像光谱数据进行了分类,区分出了4种小麦品种,小麦的总体分类精度超过97%。  相似文献   
136.
在信息定义和结构化选取的基础上,根据图斑的空间分布与距离联系,给出图斑数据地理要素层结构的定义和建立过程,从而实现图斑数据制图概括中对象选取的模型化。  相似文献   
137.
基于偏最小二乘回归技术时纹理特征进行线性组合,得到新的纹理特征来进行分类。实验表明,组合后的纹理特征不但提高了纹理分类的性能,而且具有一定的数据自适应能力。  相似文献   
138.
高山雷达站选址对估测降水的影响分析   总被引:1,自引:0,他引:1  
高山雷达站天线高度对雷达的垂直探测范围影响较大,加之中小尺度灾害性天气演生、发展的关键区域在高度1500~4500 m左右,所以高山雷达站在选址时应考虑当地零度层平均高度和雷达的垂直探测范围。通过定量估测层状云降水的个例实践,发现探测高度会限制定量估测降水,探测高度对近距离降水估测影响较小,但对远距离降水估测影响较大,原因主要是雷达的垂直探测范围及当地零度层亮带高度的影响。故在高山雷达站选址中应考虑雷达的垂直探测范围及当地零度层亮带高度的影响,同时对已建设完成的高山天气雷达应考虑对高山雷达做0°仰角的观测可行性研究。  相似文献   
139.
首先,分析了中国石油天然气股份有限公司优选出的3个战略选区重点目标,即河套盆地、塔里木东南坳陷和羌塘盆地的油气资源条件,认为这3个目标都具有资源量大、资源丰度较高的特点,具有开展战略选区的油气资源基础.其次,论述了3个目标的储盖组合和油气显示情况,指出每个地区虽然具有不同的特点,但都具有基本的油气成藏条件和较好的勘探前景.最后,在分析3个目标存在的主要问题的基础上,提出了相应的勘探工作建议.  相似文献   
140.
综合分析了西藏阿里札达盆地早更新世早期的多种与气候环境变化密切相关的地质记录,结果表明该区早更新世早期的沉积可划分为3种不同的沉积相和4个岩性段;古气候与古环境变化可划分为4个阶段:(1)2.68-2.45Ma。为冲洪积相沉积。冻融褶皱开始出现,植被以乔木为主,主要为松、藜、蒿,属山地寒温气候;(2)2.45-2.11Ma,为冲洪积相,地层中冻融褶皱多呈扭曲状,草本植物迅速上升,显示出灌木草原气候特征,气候变得凉爽干燥;(3)2.11-1.49Ma,沉积相为冲洪积相-冰缘沉积相,以冰缘沉积相为主,冻融褶皱层开始增多,出现了喜凉的介形类化石。草本植物数量和种类达到最大,灌木也相对增加,显示气候进一步趋于干旱;(4)1.49-1.36Ma,为冰湖沉积相。地层中普遍出现冻融褶皱,喜凉的介形类化石丰度很高,草本植物有小幅下降,但蕨类植物增加幅度较大,显示了干冷草原气候特征。气候干旱寒冷。  相似文献   
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