The countable characters of Qingdao, Zhejiang, Liaoning and Japanese Ayu are compared. There are no substantial different
characters among the former three Ayu, so the comprehensive values of them are taken as representative of Chinese Ayu, which
is in turn compared with Japanese Ayu (Plecoglossus altivelis altivelis and Plecoglossus altivelis ryukyuensis). By the coefficient of difference test, 3 and 4 characters are found to be beyond the subspecies level between Chinese Ayu
and nominate subspecies (Plecoglossus altivelis altivelis) and between Chinese Ayu (Plecoglossus altivelis chinensis) and Ryukyus subspecies (Plecoglossus altivelis ryukyuensis), respectively, which shows that they belong to different subspecies. The China mainland Ayu is a new subspecies, Plecoglossus altivelis chinensis Wu & Shan, the establishment of which and its forming causes are discussed. 相似文献
Long-period RS CVn-type binary CQ Aur was observed in 1987 and 1988.B andV light curves for the 1987 and 1988 epochs have been analyzed for the photometric solution by the modified Wilson and Devinney computing code with adjustable spot parameters. One-spot fit is good enough for the 1987 epoch while a wider distribution of spots in longitude is required for the 1988 epoch. The spot covers approximately 3% of total surface area of the cooler component. Absolute dimensions were deduced by combining Popper's spectroscopic results. The volume of the cooler component is approximately 100 times larger than that of the hotter component. Both components are subgiants but the cooler component evolved more than the hotter component. 相似文献
A correlative study of geology and metallogenic process in the bordering zones between China, Russia and Mongolia shows that the region of the western slope of the Da Hingan Mts. -Eastern Transbaikalia-Eastern Mongolia is a metallogenic focus-area associated with Late Mesozoic intraplate tectono-magmatic activation. During the period of 160–120 Ma a great number of multiplex deposits with similar genesis including large and superlarge mineral deposits were formed.