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中华山蓼化学成分研究 总被引:7,自引:1,他引:6
bk中华山蓼(Dxyria sinensis Hemsl.)全草中首次分离得到十四个化合物,通过波谱学方法分别鉴定为(-)-表没食子儿茶素(1)、(-)-儿茶素没食子酸酯(2)、(-)-表儿茶素(3)、(-)-表儿茶素-3-没食子酸酯(4)、槲皮素-3-O-α-L-鼠李糖苷(5)、tiliroside(6)、山萘酚-3-O-β-D-吡喃葡萄糖苷(7)、桷皮素(8)、2,4-二羟基-6-甲氧基-乙酰基苯-4-O-β-D-吡喃葡萄糖苷(9)、反-N-(4-羟基苯乙基)阿魏酸酰胺(10)、顺-N-(4-羟基苯乙基)阿魏酸酰胺(11)、icariol A2(12)、(+)-松脂素(13)、Helonioside B(14). 相似文献
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WANG XIAOFENG GERHARD H. BACHMANN† HANS HAGDORN‡ P. MARTIN SANDER§ GILLES CUNY¶ CHEN XIAOHONG WANG CHUANSHANG CHEN LIDE CHENG LONG MENG FANSONG and XU GUANGHONG 《Palaeontology》2008,51(1):27-61
Abstract: Black shales of the lower member of the Carnian Xiaowa Formation (previously known as the Wayao Member of the Falang Formation or as the Wayao Formation) in the Guanling area, Guizhou Province, south-west China, are yielding a rich marine reptile fauna and exceptional remains of pelagic crinoids. The black shales represent deposition on the drowned southern margin of the Yangtze Platform during a Maximum Flooding Interval. The relatively reduced sedimentation rates led to the formation of the Lagerstätte through the accumulation of fossils in the anoxic bottom sediments over a prolonged period of time. Invertebrate fossils represent almost exclusively pelagic forms, such as a diverse ammonite fauna and halobiid bivalves. The spectacular finds of colonies of large (stem lengths > 11 m) crinoids of the genus Traumatocrinus attached to driftwood prove that this crinoid was the first to evolve a pseudoplanktonic life style. The other crinoid is the planktonic roveacrinid Osteocrinus . The marine reptile fauna, represented by probably hundreds of skeletons, is numerically dominated by three species of ichthyosaurs and four species of thalattosaurs. The thalattosaurs fill a palaeobiogeographic gap between the Alpine thalattosaur faunas and those from western North America. Two species of placodonts are rare finds. As for the thalattosaurs, the placodont occurrences greatly expand the geographic range of the group because placodonts have been known previously only from the Mediterranean region, the Alps and the Muschelkalk Basin. The unique abundance of thalattosaurs contrasts with a scarcity of fishes. Although we suggest that the fauna is authochthonous and inhabited surface waters, it must have represented an unusual ecosystem. However, the possibility remains that both the marine reptiles and the Traumatocrinus colonies were concentrated in the region by currents and do not reflect the biocoenosis. 相似文献
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目的探究耐甲氧西林金黄色葡萄球菌(MRSA)感染性创面与创面旁菌种组成的差异并寻找可能的有益菌,为从皮肤微生态角度治疗MRSA感染性创面提供理论依据。方法采集湖南省人民医院MRSA感染性创面及创面旁的皮肤样本,其中创面部位样本22份为D组,创面旁样本11份为N组,提取样本DNA,采用高通量测序技术对16S rRNA基因V3-V4区测序并进行生物信息学分析。结果根据Alpha多样性分析,D组的Chao1指数、Ace指数和Shannon指数明显低于N组(Z=62, P=0.023 8;Z=66, P=0.035 9;Z=30, P=0.000 2),而Simpson指数明显高于N组(Z=211, P=0.000 3)。Beta多样性分析显示2组皮肤菌群组成具有差异,表明分组合理(R=0.584 3、0.467 3, P=0.001 0)。D组葡萄球菌属(Staphylococcus)及韦荣球菌属(Veillonella)丰度显著性升高(Z=213, P=0.000 5;Z=48.5, P=0.004 8),其他常驻菌群均下降。N组的乳杆菌属(Lactobacillus)相对丰度均值较D组高(Z=38, P=0.000 8)。结论MRSA感染性创面的菌群结构较创面旁组具有一定变化,Lactobacillus为皮肤有益菌,可能对创面的恢复有益。 相似文献
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KENNETH R. N. ANTHONY JEFFREY A. MAYNARD GUILLERMO DIAZ‐PULIDO PETER J. MUMBY PAUL A. MARSHALL LONG CAO OVE HOEGH‐GULDBERG 《Global Change Biology》2011,17(5):1798-1808
Ocean warming and acidification from increasing levels of atmospheric CO2 represent major global threats to coral reefs, and are in many regions exacerbated by local‐scale disturbances such as overfishing and nutrient enrichment. Our understanding of global threats and local‐scale disturbances on reefs is growing, but their relative contribution to reef resilience and vulnerability in the future is unclear. Here, we analyse quantitatively how different combinations of CO2 and fishing pressure on herbivores will affect the ecological resilience of a simplified benthic reef community, as defined by its capacity to maintain and recover to coral‐dominated states. We use a dynamic community model integrated with the growth and mortality responses for branching corals (Acropora) and fleshy macroalgae (Lobophora). We operationalize the resilience framework by parameterizing the response function for coral growth (calcification) by ocean acidification and warming, coral bleaching and mortality by warming, macroalgal mortality by herbivore grazing and macroalgal growth via nutrient loading. The model was run for changes in sea surface temperature and water chemistry predicted by the rise in atmospheric CO2 projected from the IPCC's fossil‐fuel intensive A1FI scenario during this century. Results demonstrated that severe acidification and warming alone can lower reef resilience (via impairment of coral growth and increased coral mortality) even under high grazing intensity and low nutrients. Further, the threshold at which herbivore overfishing (reduced grazing) leads to a coral–algal phase shift was lowered by acidification and warming. These analyses support two important conclusions: Firstly, reefs already subjected to herbivore overfishing and nutrification are likely to be more vulnerable to increasing CO2. Secondly, under CO2 regimes above 450–500 ppm, management of local‐scale disturbances will become critical to keeping reefs within an Acropora‐rich domain. 相似文献
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