全文获取类型
收费全文 | 1250篇 |
免费 | 81篇 |
国内免费 | 326篇 |
出版年
2024年 | 6篇 |
2023年 | 12篇 |
2022年 | 15篇 |
2021年 | 40篇 |
2020年 | 26篇 |
2019年 | 36篇 |
2018年 | 20篇 |
2017年 | 14篇 |
2016年 | 24篇 |
2015年 | 33篇 |
2014年 | 33篇 |
2013年 | 61篇 |
2012年 | 77篇 |
2011年 | 68篇 |
2010年 | 52篇 |
2009年 | 54篇 |
2008年 | 66篇 |
2007年 | 82篇 |
2006年 | 73篇 |
2005年 | 66篇 |
2004年 | 80篇 |
2003年 | 70篇 |
2002年 | 93篇 |
2001年 | 85篇 |
2000年 | 65篇 |
1999年 | 40篇 |
1998年 | 51篇 |
1997年 | 37篇 |
1996年 | 48篇 |
1995年 | 34篇 |
1994年 | 27篇 |
1993年 | 28篇 |
1992年 | 30篇 |
1991年 | 24篇 |
1990年 | 26篇 |
1989年 | 25篇 |
1988年 | 8篇 |
1987年 | 3篇 |
1986年 | 8篇 |
1985年 | 3篇 |
1984年 | 4篇 |
1982年 | 3篇 |
1981年 | 1篇 |
1980年 | 1篇 |
1979年 | 1篇 |
1978年 | 1篇 |
1958年 | 1篇 |
1957年 | 1篇 |
1950年 | 1篇 |
排序方式: 共有1657条查询结果,搜索用时 16 毫秒
71.
72.
重新描述了凹颚叶蜂属Aneugmenus Hartig, 1837的属征,指出了凹颚叶蜂属与柄臀叶蜂属Birka Malaise, 1944、微齿叶蜂属Atoposelandria Enslin, 1912 及狭眶叶蜂属Linorbita Wei & Nie, 1998之间的鉴别特征。简要讨论了与凹颚叶蜂属相关的一些种的分类地位以及凹颚叶蜂属种类的寄主植物资料。从凹颚叶蜂属移出2种,建立了2个新组合和1个新异名:短齿狭眶叶蜂Linorbita ungulica (Wei, 1997), n. comb. 和白足近颚叶蜂Paraneugmenus frontalis (Wei, 1997), n. comb., Aneugmenus mandibularis Wei, 1997, syn. nov., 是Paraneugmenus frontalis (Wei, 1997) 的新异名。提出了凹颚叶蜂属世界种类目录,编制了凹颚叶蜂属分种团以及除新热带界以外的世界种类分种检索表。描述了中国凹颚叶蜂属1新种:Aneugmenus nigrofemoratus sp. nov.。凹颚叶蜂属已知25种被划分为6个种团。 相似文献
73.
记述中国顶背瘿螨属3新种,分别是:马蹄荷顶背瘿螨Tegonotus exbucklandiae sp. nov.,为害马蹄荷 (金缕梅科Hamamelidaceae),连蕊藤顶背瘿螨Tegonotus parabaenae sp. nov.,为害连蕊藤 (防己科科Menispermaceae),松顶背瘿螨Tegonotus pini sp. nov.,为害马尾松Pinus massoniana Lamb. (松科Pinaceae)。所有瘿螨均在叶背自由活动。文中还提供了中国顶背瘿螨属种的检索表。 相似文献
74.
Responses of the distribution pattern of Quercus chenii to climate change following the Last Glacial Maximum 下载免费PDF全文
《植物生态学报》2016,40(11):1164
Aims Quercus chenii is a representative species of the flora in East China, with high ecological and economic values. Here, we aim to simulate the changes in the distribution pattern of this tree species following the Last Glacial Maximum (LGM) and to explore how climatic factors constrain the potential distribution, so as to provide scientific basis for protection and management of the germplasm resources in Q. chenii.
Methods Based on 55 presence point records and data on eight environmental variables, we simulated the potential distribution of Q. chenii during the Last Glacial Maximum, mid-Holocene, present and the year 2070 (the scenario of greenhouse gas emission is Representative Concentration Pathway 8.5) with MaxEnt model. The novel climate area and main factors influencing the changes in distribution pattern were evaluated by multivariate environmental similarity surface analysis and the most dissimilar variable analysis. The importance of environmental variables was evaluated by percent contribution, permutation importance and Jackknife test. Response curves were used to estimate the suitable value range of each variable.
Important findings The accuracy of MaxEnt model is very high, as indicated by the value of the area under the receiver operator characteristic curve of 0.9869 ± 0.0045. The highly suitable region for the present distribution covers southern Anhui, western Zhejiang, northeastern Jiangxi and eastern Hubei. The main factors affecting the potential distribution of Q. chenii are temperature and precipitation, with the former being more important. Mean temperature of the driest quarter is likely the main factor restricting Q. chenii growing in the north. During the LGM, the East China Sea Shelf occurs as the highly suitable region for the distribution of Q. chenii. In the mid-Holocene, the outline of the suitable area for the distribution of Q. chenii is similar to the present. The potential distribution region will likely move northward and experience an area expansion under the climate condition in 2070. At that time, climate anomaly will also be most severe compared to the LGM, mid-Holocene and present. Temperature seasonality and precipitation seasonality may be the main climatic factors promoting changes in the distribution pattern of Q. chenii. 相似文献
Methods Based on 55 presence point records and data on eight environmental variables, we simulated the potential distribution of Q. chenii during the Last Glacial Maximum, mid-Holocene, present and the year 2070 (the scenario of greenhouse gas emission is Representative Concentration Pathway 8.5) with MaxEnt model. The novel climate area and main factors influencing the changes in distribution pattern were evaluated by multivariate environmental similarity surface analysis and the most dissimilar variable analysis. The importance of environmental variables was evaluated by percent contribution, permutation importance and Jackknife test. Response curves were used to estimate the suitable value range of each variable.
Important findings The accuracy of MaxEnt model is very high, as indicated by the value of the area under the receiver operator characteristic curve of 0.9869 ± 0.0045. The highly suitable region for the present distribution covers southern Anhui, western Zhejiang, northeastern Jiangxi and eastern Hubei. The main factors affecting the potential distribution of Q. chenii are temperature and precipitation, with the former being more important. Mean temperature of the driest quarter is likely the main factor restricting Q. chenii growing in the north. During the LGM, the East China Sea Shelf occurs as the highly suitable region for the distribution of Q. chenii. In the mid-Holocene, the outline of the suitable area for the distribution of Q. chenii is similar to the present. The potential distribution region will likely move northward and experience an area expansion under the climate condition in 2070. At that time, climate anomaly will also be most severe compared to the LGM, mid-Holocene and present. Temperature seasonality and precipitation seasonality may be the main climatic factors promoting changes in the distribution pattern of Q. chenii. 相似文献
75.
黄土丘陵区辽东栎和刺槐树干液流时滞效应与蒸腾特征的关联性 总被引:3,自引:0,他引:3
运用Granier热扩散探针法,于2016年7-9月对半干旱黄土丘陵区天然次生林树种辽东栎和人工林树种刺槐的树干液流进行连续测定,并同步监测气象因子和土壤含水量,用错位相关法分析液流通量密度与空气水汽压亏缺日变化的时滞长度,研究2个树种不同径级个体在不同土壤水分条件下液流通量密度与蒸腾驱动因子之间的时滞效应.结果表明:辽东栎和刺槐液流通量密度的日变化节律与气象因子显著相关,空气水汽压亏缺峰值的出现较辽东栎树干液流通量密度滞后118.2 min,较刺槐树干液流通量密度滞后39.5 min;而光合有效辐射的峰值通常滞后于辽东栎12.4 min,提前于刺槐68.5 min.液流通量密度和空气水汽压亏缺的时滞长度与树种和土壤含水量显著相关,辽东栎、刺槐在土壤含水量较高时段的时滞长度分别大于土壤含水量较低时段32.2和68.2 min.时滞长度与径级的相关性整体上未达到显著水平,但在土壤含水量较低时段小径级刺槐的时滞长度大于大径级21.4 min,差异达到了显著水平.两树种液流通量密度与空气水汽压亏缺之间的时滞效应反映了对蒸腾驱动因子的敏感性,较好的土壤水分条件有利于液流通量密度提早达到峰值,较低土壤水分会导致树干液流对气象环境因子响应的敏感性降低;刺槐树干液流受土壤水分的影响更显著. 相似文献
76.
传统的元素限制模型认为氮是温带森林生长的限制元素, 不过该结论更多是从地上生物量以及群落水平进行阐述, 忽视了不同物种以及不同径级树木对外源氮的响应差异。辽东栎(Quercus wutaishanica)林是华北地区常见的森林类型, 该研究以北京东灵山辽东栎林为研究对象, 通过设置3个氮添加水平的实验, 即对照CK (0 kg·hm -2·a -1), N50 (50 kg·hm -2·a -1)和N100 (100 kg·hm -2·a -1), 模拟氮沉降对群落和物种水平以及不同径级树木生长的影响。经过7年氮添加, 实验结果显示: 物种水平上, 氮添加明显促进了优势树种辽东栎的生长; 群落水平上, 树木生长随氮浓度增加有不断上升趋势, 但统计学差异不显著; 氮添加显著抑制了辽东栎以及群落内小径级(3-10 cm)树木生长, 中(10-20 cm)、大径级(>20 cm)树木生长随氮沉降水平增加呈上升趋势, 但统计学差异不显著。表明氮是辽东栎以及温带森林树木生长的限制元素; 不同径级的辽东栎和群落内其他植物对氮添加响应不一致, 氮添加抑制了小径级树木生长, 中、大径级树木生长对氮添加响应不明显。 相似文献
77.
78.
繁殖器官在竹类植物的分类学研究中具有重要意义,研究组在广西马山县观察到竹亚科单枝竹属芸香竹正在开花,该文根据观察到的开花状况和采集到的标本解剖观察结果,对其花枝和繁殖器官特征做了详细的中文及拉丁文补充描述。经对比芸香竹与属内已知繁殖器官结构的单枝竹和小花单枝竹的繁殖器官,3个竹种有相同的繁殖器官结构特征,但在小花数目和大小等方面具有差异。繁殖器官比较表明该属竹种的繁殖器官对喀斯特地貌环境有特殊的适应性,也支持依据营养器官差异划分为3个独立竹种。 相似文献
79.
80.
金小蜂科一新属(膜翅目:小蜂总科) 总被引:1,自引:1,他引:0
本文记述了我国金小蜂科、寡金小蜂亚科的1新属和1新种。模式标本存于中国科学院动物研究所动物标本馆。 相似文献