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   221篇
  免费   20篇
  国内免费   108篇
测绘学   7篇
地球物理   19篇
地质学   91篇
海洋学   172篇
综合类   30篇
自然地理   30篇
  2023年   6篇
  2022年   7篇
  2021年   11篇
  2020年   18篇
  2019年   7篇
  2018年   23篇
  2017年   7篇
  2016年   7篇
  2015年   10篇
  2014年   13篇
  2013年   32篇
  2012年   12篇
  2011年   20篇
  2010年   17篇
  2009年   15篇
  2008年   12篇
  2007年   15篇
  2006年   5篇
  2005年   14篇
  2004年   12篇
  2003年   10篇
  2002年   10篇
  2001年   12篇
  2000年   3篇
  1999年   10篇
  1998年   7篇
  1997年   3篇
  1996年   3篇
  1995年   2篇
  1994年   4篇
  1993年   4篇
  1992年   1篇
  1991年   2篇
  1990年   2篇
  1989年   2篇
  1985年   1篇
  1984年   1篇
  1982年   1篇
  1977年   1篇
  1976年   2篇
  1973年   3篇
  1971年   2篇
排序方式: 共有349条查询结果,搜索用时 62 毫秒
61.
1 IntroductionIn January 2003, undisturbed sediments were tak-en from a grid of 22 sampling stations (from 32.5° to37°N, 122° to 125°E) during the cruise of an ecologi-cal survey of the over-winter ground for anchovy inthe Huanghai Sea. Meiofaunal abundance varied from55.3 to 152.0 ind/cm2 [(95.4 ±27.0) ind/cm2], with81% to 93% [(83.1 ±22.7) ind/cm2] of the specimensbeing nematodes. Up to now, twenty-nine species ofmarine nematodes have been recorded from theHuanghai Sea (Zhang and P…  相似文献   
62.
太白山北坡成土因素及不同土壤垂直带谱的比较   总被引:1,自引:2,他引:1  
雷梅  陈同斌  冯立  常庆瑞  阎湘 《地理研究》2001,20(5):583-592
在系统地考察太白山北坡地质、地貌、气候和植被等成土因素的基础上,总结和回顾了用土壤发生分类和土壤系统分类两种分类体系划定的太白山北坡土壤垂直带谱。根据最新的土壤系统分类,太白山北坡的土壤垂直带谱是:暗瘠寒冻雏形土(3500~3767m)———暗沃寒冻雏形土(3300~3500m)———酸性湿润雏形土(2500~3300m)———简育湿润淋溶土(1400~2500m)———简育干润淋溶土(<1400m)。分析、比较表明:两种体系有密切联系,均以成土因素为依据,建立在土壤发生学理论之上;与土壤地理发生分类相比,土壤系统分类用可以度量的诊断层和诊断特性进行土壤分类,不仅能够反映出山地土壤成土因素的垂直变化趋势,而且避免了太白山北坡土壤类型鉴定上的许多歧义。  相似文献   
63.
Inoceramid bivalves of the upper Albian and lower Cenomanian of the United States Western Interior are revised, Eleven species-level taxa and three genera are described. Two new species, Gnesioceramus mowriensis, characterizing the Mowry Shale of the early, but not the earliest, Cenomanian, and Posidonioceramus merewetheri, of the lower Cenomanian, and on new genus, Posidonioceramus, are recognised. The Western Interior inoceramid species from this interval are strongly endemic and are not good tools for long-distance correlations, although they are very effective in regional dating.In terms of the inoceramid biostratigraphy, middle and upper parts of the upper Albian can be referred to the Gnesioceramus Biozone, represented by G. comancheanus (Cragin) and G. bellvuensis (Reeside). These taxa are endemic to the Western Interior and some adjacent areas (Gulf Coast; Greenland?), but are closely allied to the cosmopolitan species, Gnesioceramus anglicus (Woods). At approximately the Albian-Cenomanian boundary, the endemic clade of ‘Inoceramus’ nahwisi appears, now referred to the newly erected Posidonioceramus, resulting in a distinct P. nahwisi biozone. This zone corresponds to the lower part of the ammonite Neogastroplites’ stratigraphic range. Gnesioceramids re-appear in the early Cenomanian. Close to base of the Cenomanian, for the first in the Western Interior, the genus Inoceramus, represented by Inoceramus irenensis Warren and Stelck, 1958, apparently immigrated into the Western Interior Basin.The Western Interior inoceramids do not allow for direct correlation to chronostratigraphic standard subdivision. The Albian-Cenomanian boundary, as earlier recognized on geochronologic correlations and confirmed, to some extent, based on ammonites, may approximately be located close to the appearance level of the genus Posidonioceramus.  相似文献   
64.
The across shore variability and trophodynamics of meiofauna were studied in a microtidal beach of the Thyrrenian Sea (NW Mediterranean). Two sites were sampled at Collelungo beach (Maremma Park, Italy) subjected to different regimes of sediment erosion and deposition. At each site, four levels were sampled in November 2002 and May 2003 along a transect from the supralittoral zone to the surf zone. Sediment cores were taken down to a depth of 10 cm and meiofaunal abundance and community structure were analyzed and related to the principal trophic resources (quantity and quality of organic matter, chlorophyll a, bacteria density and biomass).Meiofaunal abundance ranged between 14 ind. 10 cm−2 and 716 ind. 10 cm−2 in the top 0–10 cm of sediment. Abundance was lower in the surface (0–2 cm) than in the deeper (5–10 cm) sediment layers but no significant differences were found between the two sites.Multivariate BIOENV analysis showed that dryness, grain size (related to physical processes) and bacterial biomass, were the main variables explaining meiofauna distribution in these beaches. Meiofaunal densities and number of taxa were always higher at the swash level, while lower abundances were observed at the dry sampling level (+5 m). This across shore trend was also observed for the quality of the organic matter (PRT/CHO) and bacterial densities. Nematode assemblage structure at the swash sampling level showed a dominance of non-selective deposit feeders (1B), with Xyalidae as the dominant family (56%), followed by Thoracostomopsidae (14%) and Selachnematidae (12%).According to the findings, physical and biological variables at the swash level create optimal living conditions for the meiobenthos, making the swash a key area within the beach ecosystem, with potential implications within basic and applied ecological studies.  相似文献   
65.
Abstract. Hydrothermal vent ecosystems have been extensively investigated during the last 20 years; shallow water hot springs (typically found below 50 m depth) have also been studied, and from these ecosystems many thermophilic and hyperthermophilic organisms were isolated and described.
The submarine caves of Cape Palinuro were discovered long ago, but only during the last decades were geological and biological investigations carried out, yielding a large number of reports on this fascinating environment. During the last two years, several samples of water, mud, and/or bacterial mat were collected within the "Grotta Azzurra", and enrichment experiments were performed using peptone, starch, glucose or pullulan as main organic nutrients. Many heterotrophic strains were isolated and most of them grew optimally between 37 and 43 ° C with the addition of 0-2 % NaCl. Growth was usually observed between 10 and 50 ° C the range of growth pH was 4 to 9, and NaCl concentrations up to 10–12 % were tolerated in most cases.
The analysis of 16S rDNA performed with the most representative isolates showed a close phylogenetic relationship with the genera Bacillus, Vibrio, Citrobacter and Escherichia. Moreover, an isolate showing morphological and physiological similarities with the genus Enterococcus was characterised and taxonomically described based on the 16S rDNA sequence.  相似文献   
66.
记述了渤海中部在站位DA18、水深27m采到的海洋线虫一新种,渤海海线虫Thalassironus bohaiensis sp nov该新种的个体大小和De Man比值(a.b.c)与Thalassiro-nus bipartitus(Wieser,1953)十分相似,但雄性副交接刺的结构,两种有显著的差异。新种的副交接刺末端钝且内凹,在腹侧近末端有一明显的小突起,而相近种的副交接刺末端尖锐,没有任何突起。此外,新种雄性交接刺长度也与相近种有明显的差别(62—67μmvs 52μm)列表比较了新种与相近种以及该属目前已报导的其他三个种的详细形态学特征。模式标本保存在青岛海洋大学海洋生物系。  相似文献   
67.
本文报道和描述了中国东海双栉虫科颈栉虫属一新记录种,沃氏颈栉虫。本文标本与沃氏颈栉虫的原始描述非常吻合,包括具有两对鳃,胸齿片刚节具有两对加长的腹疣足和具有12个腹部齿片刚节。本文的标本具有长的须状的鳃,可延伸到胸部第9刚节,这在原始描述中没有提及。本文首次在中国海域记录本种。  相似文献   
68.
车轮虫是一类主要寄生于贝类和鱼类体表的缘毛类纤毛虫原生动物。本文对分别寄生于海洋贝类--虾夷扇贝Mizuhopecten yessoensis,半咸水鱼类--鲻鱼Mugil cephalus和双色鳗鲡Anguilla bicolor bicolor,以及淡水鱼类--光唇鱼Acrossocheilus fasciatus鳃表和体表的虾夷扇贝车轮虫Trichodina pectenis,亚卓车轮虫T.jadranica,急尖车轮虫T.acuta和喙状车轮虫T.rostrata,进行了详细的分类学研究。本文第一次报道了虾夷扇贝车轮虫的活体和蛋白银染色后特征,该虫体也是国内新记录种。其它三个车轮虫物种感染的鱼类,均属新纪录宿主。同时,也报道了这四种车轮虫对宿主的感染率和感染强度。  相似文献   
69.
利用平板涂布法从南海海绵生物样品中分离海绵共栖细菌,以枯草芽孢杆菌、金黄色葡萄球菌、大肠杆菌及酿酒酵母作为实验用指示菌对海绵共栖细菌进行了抗菌活性筛选。利用气相质谱联用仪(GC-MS)建立了群体感应信号分子酰基高丝氨酸内酯类化合物(AHLs)的检测方法,分析了活性菌株粗提液中信号分子的产生及种类。同时采用16S rDNA同源性和系统发育分析对活性菌株进行种属鉴定和系统发生学研究。结果表明,在分离到的94株海绵共栖细菌中18株(占19.1%)细菌具有抗菌活性。通过GC-MS检测确定大多数活性菌株都含有AHLs,因此提出了海绵共栖细菌抗菌活性与群体感应之间可能存在必然联系的推测。通过细菌分类鉴定,结果显示具有抗菌活性的细菌大部分属于芽孢杆菌属(Bacillus)。  相似文献   
70.
许多终生浮游软体动物接近全球分布或呈环球分布,是海洋酸化和谱系地理学研究的良好材料。本文以西北太平洋和北印度洋的长角螺属(Clio)种类为材料,通过测定其线粒体COI基因(mtCOI,55条)和核18S rRNA基因(9条)序列,结合数据库中已有的序列,对该属进行了分类学和谱系地理学研究。结果表明,矛头长角螺(C. pyramidata)和尖棘长角螺(C. cuspidata)在mtCOI基因系统树中均形成4个明显分化的谱系分支,分别为支系A–D和支系E–H。矛头长角螺的支系A为全球分布,中国海及邻近海域可能仅有支系A的存在,支系B、C和D分布于特定海域。尖棘长角螺也存在明显的谱系地理结构,西北太平洋北赤道流南北两侧存在2个不同的支系,分布于吕宋海峡的支系E为一新的谱系分支。各支系内mtCOI基因的K2P遗传距离在0~0.026之间,支系间的遗传距离在0.031~0.089之间。膨凸长角螺(C. convexa)和曲形长角螺(C. recurva)没有明显的地理遗传分化。18S rRNA基因支持支系D为独立种,但不支持其他支系的划分。矛头长角螺和尖棘长角螺内部可能存在隐存多样性。洋流可能会成为物种扩布和基因交流的障碍。  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