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   1860篇
  免费   184篇
  国内免费   410篇
  2024年   3篇
  2023年   40篇
  2022年   27篇
  2021年   54篇
  2020年   106篇
  2019年   124篇
  2018年   66篇
  2017年   56篇
  2016年   101篇
  2015年   124篇
  2014年   104篇
  2013年   158篇
  2012年   66篇
  2011年   50篇
  2010年   81篇
  2009年   126篇
  2008年   120篇
  2007年   97篇
  2006年   110篇
  2005年   81篇
  2004年   77篇
  2003年   70篇
  2002年   58篇
  2001年   46篇
  2000年   58篇
  1999年   38篇
  1998年   51篇
  1997年   26篇
  1996年   31篇
  1995年   33篇
  1994年   28篇
  1993年   25篇
  1992年   27篇
  1991年   16篇
  1990年   19篇
  1989年   26篇
  1988年   13篇
  1987年   15篇
  1986年   12篇
  1985年   21篇
  1984年   13篇
  1982年   13篇
  1981年   10篇
  1980年   5篇
  1979年   7篇
  1978年   6篇
  1977年   4篇
  1976年   7篇
  1972年   1篇
  1971年   1篇
排序方式: 共有2454条查询结果,搜索用时 406 毫秒
1.
2.
3.
4.
《Plant Ecology & Diversity》2013,6(2-3):227-241
Background: Although forest floor forms a large biomass pool in forested peatlands, little is known about its role in ecosystem carbon (C) dynamics.

Aim: We aimed to quantify forest floor photosynthesis (P FF) and respiration (R FF) as a part of overall C dynamics in a drained peatland forest in southern Finland.

Methods: We measured net forest floor CO2 exchange with closed chambers and reconstructed seasonal CO2 exchange in the prevailing plant communities.

Results: The vegetation was a mosaic of plant communities that differed in CO2 exchange dynamics. The reconstructed growing season P FF was highest in the Sphagnum community and lowest in the feather moss communities. On the contrary, R FF was highest in the feather moss communities and lowest in the Sphagnum community. CO2 assimilated by the forest floor was 20–30% of the total CO2 assimilated by the forest. The forest floor was a net CO2 source to the atmosphere, because respiration from ground vegetation, tree roots and decomposition of soil organic matter exceeded the photosynthesis of ground vegetation.

Conclusions: Tree stand dominates C fluxes in drained peatland forests. However, forest floor vegetation can have a noticeable role in the C cycle of peatlands drained for forestry. Similarly to natural mires, Sphagnum moss-dominated communities were the most efficient assimilators of C.  相似文献   
5.
6.
7.
8.
Densities of red mullet Mullus surmuletus have declined since 1996 at Cap Martin, Alpes‐Maritimes, France, following colonization by Caulerpa taxifolia . Foraging M. surmuletus were rarely observed over C. taxifolia or the seagrass Posidonia oceanica , but were observed over bare sand and endemic macroalgae. Within colonized sites (where the mean cover of C. taxifolia was 30–100%), fish were concentrated on areas with low cover of C. taxifolia (<21%). A difference in the frequency of observations of foraging groups (17%) was observed between sites with and without C. taxifolia . The observed patterns were probably due to a physical barrier to foraging that is presented by meadows of C. taxifolia . Changes to habitat structure that occur when the substratum is colonized by C. taxifolia influence the accessibility to benthic food resources, and consequently the foraging activities of fish that feed on benthic invertebrates. The decline in density of M. surmuletus at Cap Martin could be the result of fish emigration from colonized sites (unfavourable to the species) to uncolonized sites.  相似文献   
9.
Summary An electrical fusion method has been used to form somatic hybrids between protoplasts of two mutant cell lines of sycamore tissue culture cells. Both mutants will not grow in a hypoxanthine-aminopterin-thymidine (HAT) medium. It was possible to select the fused hybrids from homospecific fusion products and nonfused protoplasts by the use of HAT medium. In this way the viability and regeneration of the fused cells during the first few weeks of culture could be evaluated. An electron microscopic examination of the fusion process showed that it occurred at a series of points along the surface of the plasmalemma. Cytoplasmic bridges between the two cells were formed separated by vesicles which later dispersed to give complete cytoplasmic continuity between the cells.  相似文献   
10.
A three month experimental acidification was carried out on lotic bottom communities. Experiments were conducted under semi-natural conditions in plasticized wooden channels. Acidified communities (pH 4.0), with or without added aluminum, were compared with a reference community (pH 6.3–6.9). Added aluminum concentrations were respectively 0.2 and 0.4 mg 1–1 in experiments performed in 1982 and 1983. Water chemistry and taxonomic composition of the macroinvertebrate communities were monitored. Under acidified conditions, results were similar, with or without added aluminum. Mean abundances of all groups of organisms were lowered. Mayflies nearly completely disappeared from the acidified channels. The only organism not affected by the acidification was Microtendipes sp. Differences in the organism response were observed: Orthocladiinae (Rheocricotopus, Parametriocnemus, Corynoneura, Thienemanniella, Nanocladius, Cricotopus) and Ephemeroptera (Baetis, Habrophlebia, Habrophlebiodes, Paraleptophlebia, Ephemerella), especially early instars, were very sensitive to low pH, Chironomini and Tanypodinae were much less sensitive, while Tanytarsini were intermediate; Oligochaeta and Nematoda were difficult to classify, their response being different from one year to another. Organisms inhabiting the surface of artificial substrates disappeared very rapidly from the system, while those buried inside had a delayed reaction to acidification. Aluminum which was mainly in the monomeric form was not responsible for community modifications. Direct action of hydrogen ions through a physiological stress seems a more credible explanation. These results, induced by a continuous experimental acidification, suggest that if this small headwater stream undergoes acidification, the resulting invertebrate community will be very simplified, with only resistant species able to cope with the acid conditions.  相似文献   
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