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261.
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
262.
1 Spacial Organization Optimizing Theory 1.1 The centeral place theoryThe "centeral place theory" hypothesizes that there is a region: (1) the region is a uniform plain; (2) the motion of economic activities in regions can be carried through in every directions forever; (3) the purchasing power of residents is a successive and uniform distribution; (4) the movement of consumers has rationality in space, namely, proceeding by the shortest distance. The rural settlements as the central place of… 相似文献
263.
在坪北油田应用岩心观察、岩心分析化验资料、测井解释成果、测试及开发动态等方面的资料分析长6储层的非均质性,重点解剖层内非均质性特点,总结了正韵律,反韵律,复合韵律和交互韵律4种类型的层内非均质性。夹层分布较广泛,加剧了层间非均质性。 相似文献
264.
南海是中国唯一发育有洋壳的边缘海,是世界四大海洋油气聚集中心之一。油气勘探表明,南海的油气田分布在北部、西部和南部陆缘沉积盆地内,而大中型油气田集中分布在西部海域盆地中,自北而南有莺歌海—琼东南盆地、万安盆地、湄公盆地、曾母盆地和文莱—沙巴盆地,且以含气为主,含油次之。此外,这一区域深水区还存在多个潜在的大型含油气盆地。研究发现,南海的油气分布与深部岩石圈结构有密切关系。在构造上,南海的含油气盆地位于岩石圈块体边缘或之上,受控于大型岩石圈断裂的发育与演化。在油气富集的盆地中,莫霍面显著凸起,与盆地基底形成镜像,地壳厚度最薄处仅数千米厚,热流值明显较周围地区高,热岩石圈厚度大大减薄。地震层析成像结果反映,这些盆地深部发育一条规模宏大的北西向上地幔隆起带,自红河口向东南穿越南海西部海盆,一直延伸到婆罗州东北部地区,在宏观上控制了南海的油气分布与富集。 相似文献
265.
提出以资源生产量作为生态足迹分析中生态容量计算依据的资源产量法。该方法更全面地考虑了林地、可耕地、水域等具有的多重生态生产性功能,扩大了生态容量的内涵,将可再生能源、可回收利用废物等作为生态容量的供给,使生态容量与生态足迹的计算依据更为协调。以湖北省襄樊市2001年的生态容量计算为实例,说明了资源产量法的合理性。 相似文献
266.
267.
YAO Tandong GUO Xuejun Lonnie Thompson DUAN Keqin WANG Ninglian PU Jianchen XU Baiqing YANG Xiaoxin SUN Weizhen 《中国科学D辑(英文版)》2006,49(1)
The 213 m ice core from the Puruogangri Ice Field on the Tibetan Plateau facilitates the study of the regional temperature changes with its δ18O record of the past 100 years. Here we combine information from this core with that from the Dasuopu ice core (from the southern Tibetan Plateau), the Guliya ice core (from the northwestern Plateau) and the Dunde ice core (from the northeastern Plateau) to learn about the regional differences in temperature change across the Tibetan Plateau. The δ18O changes vary with region on the Plateau, the variations being especially large between South and North and between East and West. Moreover, these four ice cores present increasing δ18O trends, indicating warming on the Tibetan Plateau over the past 100 years. A comparative study of Northern Hemisphere (NH) temperature changes, the δ18O-reflected temperature changes on the Plateau, and available meteorological records show consistent trends in overall warming during the past 100 years. 相似文献
268.
Relationships between δ18O in summer precipitation and temperature and moisture trajectories at Muztagata, western China 总被引:1,自引:0,他引:1
Based on summer observations of stable isotope of precipitation at Muztagata, western China, during 2002―2003, this paper presents the relationship between δ18O in precipitation and air temperature, and discusses the effect of moisture transport on δ18O in precipitation. Results show that air temperature correlates positively with δ18O in precipitation, and the temperature effect controls the δ18O of precipitation in this area. The Muztagata region exhibits high δ18O values in summer precipitation, similar to those shown at stations in adjacent regions. According to the results of our model set up to trace the moisture trajectories, the westerlies and local moisture circulation contribute to variations of oxygen isotopes in precipitation. In addition, the impacts of the moisture transport distance, the moisture transport level, and the incursion of the polar air mass also influence the variations of δ18O in precipitation. The moisture origins and transport mechanisms also contribute to the variation of δ18O in precipitation at Muztagata. 相似文献
269.
270.
δ~(18)O record and temperature change over the past 100 years in ice cores on the Tibetan Plateau 总被引:6,自引:0,他引:6
Lonnie Thompson 《中国科学D辑(英文版)》2006,(1)
1 IntroductionMeteorological stations on the Tibetan Plateau are few in number and uneven in distribution, with a majority concentrated in the east and south. No stations exist so far within the large expanse in the middle or west of the Plateau. Moreover… 相似文献