全文获取类型
收费全文 | 16776篇 |
免费 | 34篇 |
国内免费 | 37篇 |
专业分类
系统科学 | 71篇 |
丛书文集 | 263篇 |
教育与普及 | 30篇 |
理论与方法论 | 71篇 |
现状及发展 | 7992篇 |
研究方法 | 693篇 |
综合类 | 7565篇 |
自然研究 | 162篇 |
出版年
2013年 | 76篇 |
2012年 | 185篇 |
2011年 | 364篇 |
2008年 | 222篇 |
2007年 | 241篇 |
2006年 | 279篇 |
2005年 | 270篇 |
2004年 | 376篇 |
2003年 | 254篇 |
2002年 | 254篇 |
2001年 | 479篇 |
2000年 | 442篇 |
1999年 | 326篇 |
1994年 | 74篇 |
1992年 | 286篇 |
1991年 | 221篇 |
1990年 | 238篇 |
1989年 | 235篇 |
1988年 | 202篇 |
1987年 | 234篇 |
1986年 | 278篇 |
1985年 | 335篇 |
1984年 | 230篇 |
1983年 | 226篇 |
1982年 | 205篇 |
1981年 | 217篇 |
1980年 | 224篇 |
1979年 | 563篇 |
1978年 | 475篇 |
1977年 | 437篇 |
1976年 | 341篇 |
1975年 | 404篇 |
1974年 | 564篇 |
1973年 | 452篇 |
1972年 | 472篇 |
1971年 | 553篇 |
1970年 | 696篇 |
1969年 | 538篇 |
1968年 | 539篇 |
1967年 | 536篇 |
1966年 | 430篇 |
1965年 | 371篇 |
1964年 | 121篇 |
1959年 | 193篇 |
1958年 | 330篇 |
1957年 | 247篇 |
1956年 | 190篇 |
1955年 | 192篇 |
1954年 | 190篇 |
1948年 | 127篇 |
排序方式: 共有10000条查询结果,搜索用时 31 毫秒
211.
Carbon loss from an unprecedented Arctic tundra wildfire 总被引:2,自引:0,他引:2
Mack MC Bret-Harte MS Hollingsworth TN Jandt RR Schuur EA Shaver GR Verbyla DL 《Nature》2011,475(7357):489-492
Arctic tundra soils store large amounts of carbon (C) in organic soil layers hundreds to thousands of years old that insulate, and in some cases maintain, permafrost soils. Fire has been largely absent from most of this biome since the early Holocene epoch, but its frequency and extent are increasing, probably in response to climate warming. The effect of fires on the C balance of tundra landscapes, however, remains largely unknown. The Anaktuvuk River fire in 2007 burned 1,039 square kilometres of Alaska's Arctic slope, making it the largest fire on record for the tundra biome and doubling the cumulative area burned since 1950 (ref. 5). Here we report that tundra ecosystems lost 2,016?±?435?g?C?m(-2) in the fire, an amount two orders of magnitude larger than annual net C exchange in undisturbed tundra. Sixty per cent of this C loss was from soil organic matter, and radiocarbon dating of residual soil layers revealed that the maximum age of soil C lost was 50 years. Scaled to the entire burned area, the fire released approximately 2.1?teragrams of C to the atmosphere, an amount similar in magnitude to the annual net C sink for the entire Arctic tundra biome averaged over the last quarter of the twentieth century. The magnitude of ecosystem C lost by fire, relative to both ecosystem and biome-scale fluxes, demonstrates that a climate-driven increase in tundra fire disturbance may represent a positive feedback, potentially offsetting Arctic greening and influencing the net C balance of the tundra biome. 相似文献
212.
213.
Molecular mechanism of anaerobic ammonium oxidation 总被引:7,自引:0,他引:7
Kartal B Maalcke WJ de Almeida NM Cirpus I Gloerich J Geerts W Op den Camp HJ Harhangi HR Janssen-Megens EM Francoijs KJ Stunnenberg HG Keltjens JT Jetten MS Strous M 《Nature》2011,479(7371):127-130
Two distinct microbial processes, denitrification and anaerobic ammonium oxidation (anammox), are responsible for the release of fixed nitrogen as dinitrogen gas (N(2)) to the atmosphere. Denitrification has been studied for over 100 years and its intermediates and enzymes are well known. Even though anammox is a key biogeochemical process of equal importance, its molecular mechanism is unknown, but it was proposed to proceed through hydrazine (N(2)H(4)). Here we show that N(2)H(4) is produced from the anammox substrates ammonium and nitrite and that nitric oxide (NO) is the direct precursor of N(2)H(4). We resolved the genes and proteins central to anammox metabolism and purified the key enzymes that catalyse N(2)H(4) synthesis and its oxidation to N(2). These results present a new biochemical reaction forging an N-N bond and fill a lacuna in our understanding of the biochemical synthesis of the N(2) in the atmosphere. Furthermore, they reinforce the role of nitric oxide in the evolution of the nitrogen cycle. 相似文献
214.
215.
Bos KI Schuenemann VJ Golding GB Burbano HA Waglechner N Coombes BK McPhee JB DeWitte SN Meyer M Schmedes S Wood J Earn DJ Herring DA Bauer P Poinar HN Krause J 《Nature》2011,478(7370):506-510
Technological advances in DNA recovery and sequencing have drastically expanded the scope of genetic analyses of ancient specimens to the extent that full genomic investigations are now feasible and are quickly becoming standard. This trend has important implications for infectious disease research because genomic data from ancient microbes may help to elucidate mechanisms of pathogen evolution and adaptation for emerging and re-emerging infections. Here we report a reconstructed ancient genome of Yersinia pestis at 30-fold average coverage from Black Death victims securely dated to episodes of pestilence-associated mortality in London, England, 1348-1350. Genetic architecture and phylogenetic analysis indicate that the ancient organism is ancestral to most extant strains and sits very close to the ancestral node of all Y. pestis commonly associated with human infection. Temporal estimates suggest that the Black Death of 1347-1351 was the main historical event responsible for the introduction and widespread dissemination of the ancestor to all currently circulating Y. pestis strains pathogenic to humans, and further indicates that contemporary Y. pestis epidemics have their origins in the medieval era. Comparisons against modern genomes reveal no unique derived positions in the medieval organism, indicating that the perceived increased virulence of the disease during the Black Death may not have been due to bacterial phenotype. These findings support the notion that factors other than microbial genetics, such as environment, vector dynamics and host susceptibility, should be at the forefront of epidemiological discussions regarding emerging Y. pestis infections. 相似文献
216.
217.
Cerling TE Wynn JG Andanje SA Bird MI Korir DK Levin NE Mace W Macharia AN Quade J Remien CH 《Nature》2011,476(7358):51-56
The role of African savannahs in the evolution of early hominins has been debated for nearly a century. Resolution of this issue has been hindered by difficulty in quantifying the fraction of woody cover in the fossil record. Here we show that the fraction of woody cover in tropical ecosystems can be quantified using stable carbon isotopes in soils. Furthermore, we use fossil soils from hominin sites in the Awash and Omo-Turkana basins in eastern Africa to reconstruct the fraction of woody cover since the Late Miocene epoch (about 7 million years ago). (13)C/(12)C ratio data from 1,300 palaeosols at or adjacent to hominin sites dating to at least 6 million years ago show that woody cover was predominantly less than ~40% at most sites. These data point to the prevalence of open environments at the majority of hominin fossil sites in eastern Africa over the past 6 million years. 相似文献
218.
Rasmussen SG Choi HJ Fung JJ Pardon E Casarosa P Chae PS Devree BT Rosenbaum DM Thian FS Kobilka TS Schnapp A Konetzki I Sunahara RK Gellman SH Pautsch A Steyaert J Weis WI Kobilka BK 《Nature》2011,469(7329):175-180
G protein coupled receptors (GPCRs) exhibit a spectrum of functional behaviours in response to natural and synthetic ligands. Recent crystal structures provide insights into inactive states of several GPCRs. Efforts to obtain an agonist-bound active-state GPCR structure have proven difficult due to the inherent instability of this state in the absence of a G protein. We generated a camelid antibody fragment (nanobody) to the human β(2) adrenergic receptor (β(2)AR) that exhibits G protein-like behaviour, and obtained an agonist-bound, active-state crystal structure of the receptor-nanobody complex. Comparison with the inactive β(2)AR structure reveals subtle changes in the binding pocket; however, these small changes are associated with an 11?? outward movement of the cytoplasmic end of transmembrane segment 6, and rearrangements of transmembrane segments 5 and 7 that are remarkably similar to those observed in opsin, an active form of rhodopsin. This structure provides insights into the process of agonist binding and activation. 相似文献
219.
220.
Arner P Bernard S Salehpour M Possnert G Liebl J Steier P Buchholz BA Eriksson M Arner E Hauner H Skurk T Rydén M Frayn KN Spalding KL 《Nature》2011,478(7367):110-113
Adipose tissue mass is determined by the storage and removal of triglycerides in adipocytes. Little is known, however, about adipose lipid turnover in humans in health and pathology. To study this in vivo, here we determined lipid age by measuring (14)C derived from above ground nuclear bomb tests in adipocyte lipids. We report that during the average ten-year lifespan of human adipocytes, triglycerides are renewed six times. Lipid age is independent of adipocyte size, is very stable across a wide range of adult ages and does not differ between genders. Adipocyte lipid turnover, however, is strongly related to conditions with disturbed lipid metabolism. In obesity, triglyceride removal rate (lipolysis followed by oxidation) is decreased and the amount of triglycerides stored each year is increased. In contrast, both lipid removal and storage rates are decreased in non-obese patients diagnosed with the most common hereditary form of dyslipidaemia, familial combined hyperlipidaemia. Lipid removal rate is positively correlated with the capacity of adipocytes to break down triglycerides, as assessed through lipolysis, and is inversely related to insulin resistance. Our data support a mechanism in which adipocyte lipid storage and removal have different roles in health and pathology. High storage but low triglyceride removal promotes fat tissue accumulation and obesity. Reduction of both triglyceride storage and removal decreases lipid shunting through adipose tissue and thus promotes dyslipidaemia. We identify adipocyte lipid turnover as a novel target for prevention and treatment of metabolic disease. 相似文献