首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   854980篇
  免费   87429篇
  国内免费   269篇
  2018年   8532篇
  2017年   8115篇
  2016年   11425篇
  2015年   14466篇
  2014年   17253篇
  2013年   24917篇
  2012年   27831篇
  2011年   28578篇
  2010年   19605篇
  2009年   18052篇
  2008年   25583篇
  2007年   26562篇
  2006年   24792篇
  2005年   23826篇
  2004年   23612篇
  2003年   22733篇
  2002年   22153篇
  2001年   37094篇
  2000年   36457篇
  1999年   29342篇
  1998年   10836篇
  1997年   10937篇
  1996年   10417篇
  1995年   9587篇
  1994年   9237篇
  1993年   9288篇
  1992年   23789篇
  1991年   23350篇
  1990年   22814篇
  1989年   22197篇
  1988年   20350篇
  1987年   19525篇
  1986年   18265篇
  1985年   18096篇
  1984年   14920篇
  1983年   13029篇
  1982年   9851篇
  1981年   8952篇
  1980年   8306篇
  1979年   13921篇
  1978年   10995篇
  1977年   9911篇
  1976年   9479篇
  1975年   10647篇
  1974年   11377篇
  1973年   11319篇
  1972年   10337篇
  1971年   9221篇
  1970年   8092篇
  1969年   7977篇
排序方式: 共有10000条查询结果,搜索用时 928 毫秒
211.
212.
213.
214.
215.
216.
217.
218.
Vaterite otoliths were sampled from two reared populations (Celtic and Clyde Seas) of juvenile herring Clupea harengus. The crystallography, elemental composition and morphometry were analysed and compared with those of normal aragonite otoliths. The incidence of vaterite otoliths in the juveniles sampled (n = 601) ranged from 7·8% in the Clyde population to 13·9% in the Celtic Sea population, and was 5·5% in the small sample (n = 36) of wild adults examined. In all but one case fish had only one vaterite otolith; the corresponding otolith of the pair was completely aragonite. Although the majority of the juveniles sampled showed craniofacial deformities, there was no link between the skull or jaw malformation and the incidence of vaterite otoliths. All vaterite otoliths had an aragonite inner area, and vaterite deposition began sometime after the age of 90 days. The vaterite otoliths were larger and lighter than their corresponding aragonite partners, and were less dense as a consequence of the vaterite crystal structure. The vaterite areas of the otoliths were depleted in Sr, Na and K. Concentrations of Mn were higher in the vaterite areas. The transition between the aragonite inner areas and the vaterite areas was sharply delineated. Within a small spatial scale (20 μm3) in the vaterite areas, however, there was co‐precipitation of both vaterite and aragonite. The composition of the aragonite cores in the vaterite otoliths was the same as in the cores of the normal aragonite otoliths indicating that the composition of the aragonite cores did not seed the shift to vaterite. Vaterite is less dense than aragonite, yet the concentrations of Ca analysed with wavelength‐dispersive spectrometry (WDS) were the same between the two polymorphs, indicating that Ca concentrations measured with WDS are not a good indicator of hypermineralized zones with high mineral density. The asymmetry in density and size of the otoliths may cause disruptions of hearing and pressure sensitivity for individual fish with one vaterite otolith, however, the presence of vaterite otoliths did not seem to affect the growth of these laboratory reared juvenile herring.  相似文献   
219.
In many species of actinomycetes, carotenogenesis can be photoinduced. The capacity to respond to photoinduction is, however unstable and, in various strains of Streptomyces, is lost at a relatively high frequency. In Streptomyces setonii ISP5395, which normally produces no carotenoids, carotenoid-producing mutants can be obtained following protoplast regeneration. We report here the characterization of a gene, crtS, which was isolated from one such mutant and can confer on wild-type S. setonii ISP5395 cells the capacity to synthesize carotenoids. Sequence analysis of crtS reveals an open reading frame, which shows homology to genes that encode alternative sigma factors in Bacillus subtilis. We propose that crtS encodes a sigma factor which is necessary for the expression of a cryptic gene(s) for carotenoid biosynthesis in S. setonii ISP5395.  相似文献   
220.
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号