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   1077篇
  免费   86篇
  国内免费   3篇
耳鼻咽喉   8篇
儿科学   39篇
妇产科学   8篇
基础医学   148篇
口腔科学   7篇
临床医学   171篇
内科学   249篇
皮肤病学   25篇
神经病学   55篇
特种医学   47篇
外科学   167篇
综合类   1篇
现状与发展   1篇
一般理论   1篇
预防医学   55篇
眼科学   23篇
药学   52篇
肿瘤学   109篇
  2023年   13篇
  2022年   14篇
  2021年   59篇
  2020年   28篇
  2019年   57篇
  2018年   63篇
  2017年   36篇
  2016年   36篇
  2015年   37篇
  2014年   57篇
  2013年   51篇
  2012年   86篇
  2011年   76篇
  2010年   47篇
  2009年   53篇
  2008年   61篇
  2007年   49篇
  2006年   59篇
  2005年   47篇
  2004年   50篇
  2003年   31篇
  2002年   26篇
  2001年   9篇
  2000年   14篇
  1999年   6篇
  1998年   8篇
  1997年   3篇
  1996年   3篇
  1995年   4篇
  1994年   2篇
  1993年   2篇
  1992年   4篇
  1991年   3篇
  1990年   7篇
  1989年   10篇
  1988年   12篇
  1987年   4篇
  1986年   5篇
  1985年   4篇
  1984年   4篇
  1983年   2篇
  1981年   2篇
  1977年   5篇
  1973年   2篇
  1972年   2篇
  1967年   1篇
  1965年   1篇
  1964年   2篇
  1962年   2篇
  1960年   1篇
排序方式: 共有1166条查询结果,搜索用时 31 毫秒
961.
Fungal rhinosinusitis (FRS) has a worldwide distribution, comprises distinct clinical entities but is mostly due to Aspergillus among which Aspergillus fumigatus plays a major role in European countries. Although, there is accumulating evidence for the emergence of environmentally acquired‐azole resistance in A. fumigatus (such as TR34/L98H) in various clinical settings, there is few data for patients with FRS. In this study, we aimed to investigate the prevalence of A. fumigatus azole resistance due to TR34/L98H in a multicentre cohort of patients with FRS. One hundred and thirty‐seven patients with FRS admitted between 2002 and 2016 at four French medical centres were retrospectively enrolled. Clinical and mycological findings were collected. Aspergillus fumigatus and the TR34/L98H alteration conferring azole resistance were investigated directly from clinical samples using the commercial CE‐IVD marked MycoGENIE® A. fumigatus real‐time PCR assay. Fungal ball was the more frequent clinical form (n = 118). Despite the presence of fungal hyphae at direct microscopic examination, mycological cultures remained negative for 83 out of the 137 patients (60.6%). The PCR assay proved to be useful allowing the identification of A. fumigatus and etiological diagnosis in 106 patients (77.4%) compared with 44 patients (32.1%) when using culture as the reference method. Importantly, neither TR34 nor L98H alterations were evidenced.  相似文献   
962.

Purpose

The aim of this study was to quantify the association between the CRP value and 18F–FDG PET vascular positivity in Takayasu arteritis (TAK) through a structured dedicated systematic review and meta-analysis.

Methods

From January 2000 to December 2016, the PubMed/MEDLINE database was searched for articles specifically dealing with the assessment of vascular inflammation using 18F–FDG PET and CRP biomarkers in TAK. Inclusion criteria for the qualitative analysis were (1) 18F–FDG PET used to assess the disease activity, (2) The use of the ACR criteria for the diagnosis of TAK, (3) No case mixed vasculitis (i.e., no giant cell arteritis), and (4) CRP concentration and clinical disease activity available. For the meta-analysis, PET-positive and PET-negative subgroups with the corresponding CRP concentrations were generated based on per patient data. The standard mean difference, which represents the effect of the CRP concentrations on the 18F–FDG PET vascular uptake, was computed for all studies, and then the results were pooled together.

Results

Among the 33 initial citations, nine complete articles including 210 patients fulfilled the inclusion criteria. Five studies found a significant correlation between the 18F–FDG PET and CRP concentration, one provided a trend towards association and three did not find any association between the two biomarkers. Six studies found a significant association between 18F–FDG PET and clinical disease activity, one found a trend towards association and the last two studies did not evaluate this correlation. The meta-analysis (121 patients) provided the following results: Standard Mean Deviation = 0.54 [0.15;0.92]; Chi2 = 3.35; I2 = 0%; Test for overall effect: Z = 2.70 (P = 0.007).

Conclusion

The CRP concentration only moderately reflects the 18F–FDG PET vascular positivity in TAK, suggesting dissociated information. Standardized longitudinal prospective studies are necessary to assess the value of 18F–FDG PET as an independent biomarker for subtle vascular wall inflammation detection.
  相似文献   
963.
964.
Enhanced renal CT scanners were performed in 38 children (82% girls) to rule out acute pyelonephritis. Patients were divided in 2 groups on the basis of clinical presentation and bacteriology data. In patients of group A (n=16, preliminary study), upper urinary tract infection (UTI) was certain. CT confirmed the diagnosis in all but 3 patients (a 2-year-old child and 2 patients with UTI developed on prior obstruction). In subsequently studied patients of group B (n=22), clinical findings or bacteriology data were negative or questionable. CT made the diagnosis of acute pyelonephritis in 11 patients. As well as DMSA scintigraphy, CT scanner can help to diagnose or to rule out upper UTIs in difficult cases. In all boys of both groups, ipsilateral vesico-ureteric reflux (VUR) was found by subsequent voiding cystourethrography (VCUG) on the side of pyelonephritis. In girls, this correlation was shown in only 7 of the 25 kidneys with pyelonephritis. This result supports the hypothesis of a gender-dependent contamination. We believe that absence of radiologic reflux cannot exclude the possibility of bacterial crossings of ureteric meatus capable to lead to genuine upper UTIs.  相似文献   
965.
966.
BackgroundPhase 3 trials have demonstrated the safety and efficacy of lumacaftor-ivacaftor (LUMA-IVA) in patients with cystic fibrosis (CF) homozygous for the Phe508del CFTR mutation and percent predicted forced expiratory volume in 1 s (ppFEV1) between 40 and 90. Marketing authorizations have been granted for patients at all levels of ppFEV1.MethodsTo evaluate the safety and effectiveness of LUMA-IVA over the first year of treatment in patients with ppFEV1<40 or ppFEV1≥90 in comparison with those with ppFEV1 [40–90[. Analysis of data collected during a real world study, which included all patients aged ≥12 years who started LUMA-IVA in 2016 across all 47 French CF centers.Results827 patients were classified into 3 subgroups according to ppFEV1 at treatment initiation (ppFEV1<40, n = 121; ppFEV1 [40–90[, n = 609; ppFEV1≥90, n = 97). Treatment discontinuation rate was higher in ppFEV1<40 patients (28.9%) than in those with ppFEV1 [40–90[(16.4%) or ppFEV1≥90 (17.5%). In patients with uninterrupted treatment, significant increase in ppFEV1 occurred in the ppFEV1 [40–90[subgroup (+2.9%, P<0.001), and in those ppFEV1<40 (+0.5%, P = 0.03) but not in those with ppFEV1≥90 (P = 0.46). Compared with the year prior to initiation, the number of days of intravenous antibiotics were reduced in all subgroups, although 72% of patients with ppFEV1<40 still experienced at least one exacerbation/year under LUMA-IVA. Comparable increase in body mass index was seen in the three subgroups.ConclusionPhe508del homozygous CF patients benefit from LUMA-IVA at all levels of baseline lung function, but the characteristics and magnitude of the response vary depending on ppFEV1 at baseline.  相似文献   
967.
Inflammatory skin diseases including atopic dermatitis (AD) and psoriasis (PSO) are underpinned by dendritic cell (DC)–mediated T cell responses. Currently, the heterogeneous human cutaneous DC population is incompletely characterized, and its contribution to these diseases remains unclear. Here, we performed index-sorted single-cell flow cytometry and RNA sequencing of lesional and nonlesional AD and PSO skin to identify macrophages and all DC subsets, including the newly described mature LAMP3+BIRC3+ DCs enriched in immunoregulatory molecules (mregDC) and CD14+ DC3. By integrating our indexed data with published skin datasets, we generated a myeloid cell universe of DC and macrophage subsets in healthy and diseased skin. Importantly, we found that CD14+ DC3s increased in PSO lesional skin and co-produced IL1B and IL23A, which are pathological in PSO. Our study comprehensively describes the molecular characteristics of macrophages and DC subsets in AD and PSO at single-cell resolution, and identifies CD14+ DC3s as potential promoters of inflammation in PSO.  相似文献   
968.
The absolute benefit (AB) is extensively used to summarize the results of clinical trials. As the AB depends directly on the patient's baseline risk, therapeutic decisions based on AB tend to favor patients at high risk. To evaluate the consequences of this decision's procedure for life-long therapy, we compare the AB with the gain in event-free life expectancy in a simulated hypertensive population. Our results show that the AB goes through a maximum and then declines as the duration of treatment increases. The amplitude of the variation of AB is independent of the baseline risks but the maximum is reached more quickly in the high-risk patients. Considering the gain in event-free life expectancy, low-risk patients benefit more than high-risk patients do, at the expense of a longer treatment exposure. The interpretation of the AB changes depending on follow-up.  相似文献   
969.
970.
Increasing atmospheric partial pressure of CO2 (pCO2) is a major threat to coral reefs, but some argue that the threat is mitigated by factors such as the variability in the response of coral calcification to acidification, differences in bleaching susceptibility, and the potential for rapid adaptation to anthropogenic warming. However the evidence for these mitigating factors tends to involve experimental studies on corals, as opposed to coral reefs, and rarely includes the influence of multiple variables (e.g., temperature and acidification) within regimes that include diurnal and seasonal variability. Here, we demonstrate that the inclusion of all these factors results in the decalcification of patch-reefs under business-as-usual scenarios and reduced, although positive, calcification under reduced-emission scenarios. Primary productivity was found to remain constant across all scenarios, despite significant bleaching and coral mortality under both future scenarios. Daylight calcification decreased and nocturnal decalcification increased sharply from the preindustrial and control conditions to the future scenarios of low (reduced emissions) and high (business-as-usual) increases in pCO2. These changes coincided with deeply negative carbonate budgets, a shift toward smaller carbonate sediments, and an increase in the abundance of sediment microbes under the business-as-usual emission scenario. Experimental coral reefs demonstrated highest net calcification rates and lowest rates of coral mortality under preindustrial conditions, suggesting that reef processes may not have been able to keep pace with the relatively minor environmental changes that have occurred during the last century. Taken together, our results have serious implications for the future of coral reefs under business-as-usual environmental changes projected for the coming decades and century.Tropical coral reef ecosystems face significant challenges from anthropogenic changes in ocean temperature and chemistry (1). Short periods of anomalously high sea temperatures have triggered mass coral bleaching and mortality events since the early 1980s (2, 3), and projected pH and carbonate ion concentrations reduce the calcification rate of many organisms such as reef-building corals and crustose coralline algae (reviewed in ref. 4). Generally, the projected impacts associated with future increases in sea temperature have been examined independently of those associated with ocean acidification (2, 58). When multiple drivers have been considered, extrapolation of the results to the future outlook of coral reefs has been complicated by a lack of replication, the use of artificial light, and/or experimental designs that exclude the potentially important influence of natural variation in ocean temperature and chemistry over diel and seasonal cycles (911). Furthermore, most studies have focused on corals or calcareous algae in isolation rather than on broader communities that may better represent the responses of coral reefs (911). Excluding the interaction of changing temperature and ocean chemistry, natural variability, and the wider set of organisms and processes places important limitations on our ability to understand the future and ascertain whether, for coral reefs, there is any real difference between action and no action regarding CO2 emissions. This issue is fundamentally important given the time lag between reducing CO2 emissions and establishing atmospheric stability, but has not been addressed adequately via studies that seek mechanistic understandings for the individual effects of temperature and acidification on specific organisms, because the sum of the parts may not equal the whole.Some argue that the potential and imminent threat to coral reefs posed by anthropogenic CO2 emissions is mitigated by potential rapid evolutionary adaptation by key reef organisms such as corals (12). Within this argument, greater inherent environmental variability is seen as a facilitator of adaptation (13), and the transition within some corals to thermally tolerant symbionts is presented as a current coral plasticity that is likely to enhance adaptation toward warmer water (12). The latter suggestion is debatable because the enhancement in host performance is not typically recorded in terms of a property that belongs uniquely to the host (e.g., coral survival, growth, or reproduction) but rather as properties (bleaching tolerance, sustained maximum quantum yields of photosystem II) that may be more attributable to the symbiont than to the host (14). That is, it is not always clear that the statement “having thermally tolerant symbionts leads to thermally tolerant hosts” is anything more than a tautology. Especially given observations in the current literature that corals harboring thermally tolerant symbionts experience reduced growth (15, 16), that heterotrophic feeding can sustain some coral species postbleaching (17), and finally that while food may be relatively unavailable in the oceans that surround reefs, this is not typically the case on a reef (reviewed in ref. 18). Evolution will occur over multiple generations. Presently, however, we lack the experimental evidence to support scientifically the contention that organism evolution over the next decades will protect features such as the maintenance of a positive carbonate balance that are essential to reef viability and the functional utility of reefs to mankind (1). However, the ocean environment has changed significantly over the last 100 y in terms of both ocean temperature and acidification (19, 20), suggesting that reefs in the Southern Great Barrier Reef (GBR), where seasonal environmental variability is great, should provide ample opportunity to evaluate experimentally the degree to which key ecosystem features are retained over decadal time frames.In the present study, we simulated past and future ocean temperature and chemistry on replicated patches of coral reef reconstructed from a broad range of organisms collected from the growth zone of a coral reef (Harry’s Bommie, Heron Island, GBR, 151.9357°E, 23.4675°S) (Fig. S1). The experiment was designed to answer two major questions. The first was whether processes such as the maintenance of maximum net reef calcification rates, measured independently of episodic events such as cyclones, are optimal under the preindustrial (PRE) or present-day (control) scenarios. The second was whether the response of coral reefs differs between action scenarios that result in business-as-usual unabated rates of CO2 emission (A1FI) as compared to reduced rates of CO2 emission (B1) through 2050. Here, the Special Report on Emission Scenarios (SRES) A1FI is equivalent to a Representation Concentration Pathway (RCP) 8.5; and, SRES B1 is equivalent to RCP4.5 (21).

Table 1.

November composition of the reassembled patch-reefs
TypePrincipal components% cover
Hard coralAcropora formosa; Seriatopora hystrix*; Stylophora pistillata; Porites cylindrical; Plating Montipora sp.; Goniastrea aspera; Lobophyllia sp.*; Fungia sp.35 ± 1
MacroalgaeCrustose calcareous algae; red, green, brown filamentous algae; Halimeda sp.; Lobophora sp.; Chlorodesmis fastigiata; Hypnea sp.15 ± 3
Other invertebratesZoanthids; Xenia sp.; sponges (Cliona orientalis); sea cucumbers (Holothuria atra); snails (herbivorous); xanthid crabs2 ± 0
VertebratesThree lawnmower blennies (Salarias fasciatus)
SedimentsSkeletons of corals, crustose calcareous algae, foraminifers, mollusks, and Halimeda (39)48 ± 3
Open in a separate windowAll organisms were collected from a depth of ca. 5 m at Harry’s Bommie, Heron Island Reef, GBR, Australia.*Corals excluded from buoyant weight assessment.To incorporate natural variability at day and seasonal scales, a computer-control system tracked water temperature and ocean partial pressure of CO2 (pCO2) look-up tables established from two or three hourly measurements made at our reference site (Harry’s Bommie, www.pmel.noaa.gov/co2/story/Heron+Island) during 2010 and 2011 (Fig. S1). Then treatment conditions (with similar natural levels of diurnal and seasonal variability) were established by applying past and projected future anomalies as offsets to these look-up table values (Fig. 1). The precision and accuracy of the control system is evident from the comparison of the data from 2010 and 2011 (black trace in Fig. 1) with the condition replicated in the control (today) mesocosms (blue symbols). PRE conditions were established by reducing the seawater (SW) pCO2 by 104 ± 11 µatm and temperature by 1 °C. Future conditions were established using anomalies appropriate to the lower (B1: +174 ± 9 µatm, +2 °C) and upper (A1FI: +572 ± 11 µatm, +4 °C) ends of respective scenarios. Temperature profiles for representative mesocosms are shown in Fig. 1, along with the average pH conditions (± SE) measured at 30-min intervals. Experimental treatments were preceded by 2.5 mo in which the coral reef communities were acclimatized to treatment conditions by slowly increasing the relative proportion of treatment water to inner reef flat water [control (field) rates of changes over acclimatization period were 0.04 °C d−1 and 6 μatm·pCO2·d−1; A1FI rates were 0.09 °C·d−1 and 14 μatm·pCO2·d−1]. Full treatments were applied over the austral summer from early November 2011 to early February 2012 under light conditions appropriate to the reference site.Open in a separate windowFig. 1.Treatment conditions established over the experimental period: daily temperature profiles and average treatment pH obtained through the course of the experiment. PRE, pre-industrial treatment; C, control treatment set to mimic conditions at the reference site (Harry’s Bommie, GBR, Australia, indicated by the solid black line) measured by the Commonwealth Scientific and Industrial Research Organization between November 2010 and February 2011; B1, SRES B1/RCP4.5, reduced CO2 emission scenario; A1FI, SRES A1FI/RCP 8.5 business-as-usual emissions scenario. The upper dashed line represents the maximum monthly mean (MMM) + 1 °C, established for Heron Island using 50-km pixel satellite data (http://coralreefwatch.noaa.gov). The lower dashed line represents MMM+1 specific to the reference site established by relating satellite nighttime temperatures to same-day average night temperatures logged at Harry’s Bommie. Triangles represent sampling days for community O2 flux and calcification measurements. Average pCO2s across sampling days were PRE = 301 ± 11 µatm, C = 405 ± 25 µatm, B1 = 611 ± 17 µatm, and A1FI = 1,009 ± 8 µatm (Table S1).  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