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   902篇
  免费   31篇
  国内免费   14篇
耳鼻咽喉   1篇
儿科学   9篇
妇产科学   9篇
基础医学   106篇
口腔科学   6篇
临床医学   120篇
内科学   221篇
皮肤病学   5篇
神经病学   59篇
特种医学   81篇
外科学   144篇
综合类   6篇
一般理论   3篇
预防医学   46篇
眼科学   7篇
药学   67篇
肿瘤学   57篇
  2023年   5篇
  2022年   9篇
  2021年   18篇
  2020年   7篇
  2019年   9篇
  2018年   22篇
  2017年   16篇
  2016年   15篇
  2015年   14篇
  2014年   37篇
  2013年   36篇
  2012年   65篇
  2011年   73篇
  2010年   33篇
  2009年   28篇
  2008年   67篇
  2007年   83篇
  2006年   63篇
  2005年   61篇
  2004年   51篇
  2003年   59篇
  2002年   51篇
  2001年   7篇
  2000年   2篇
  1999年   11篇
  1998年   14篇
  1997年   11篇
  1996年   5篇
  1995年   10篇
  1994年   11篇
  1993年   9篇
  1992年   3篇
  1991年   6篇
  1990年   3篇
  1989年   4篇
  1988年   7篇
  1987年   3篇
  1985年   2篇
  1984年   2篇
  1983年   3篇
  1982年   3篇
  1981年   1篇
  1980年   2篇
  1976年   1篇
  1975年   1篇
  1974年   1篇
  1973年   1篇
  1972年   1篇
  1971年   1篇
排序方式: 共有947条查询结果,搜索用时 31 毫秒
31.
The Canadian Cardiovascular Society (CCS) Atrial Fibrillation Guidelines Committee provides periodic reviews of new data to produce focused updates that address clinically important advances in atrial fibrillation (AF) management. This 2018 Focused Update addresses: (1) anticoagulation in the context of cardioversion of AF; (2) the management of antithrombotic therapy for patients with AF in the context of coronary artery disease; (3) investigation and management of subclinical AF; (4) the use of antidotes for the reversal of non-vitamin K antagonist oral anticoagulants; (5) acute pharmacological cardioversion of AF; (6) catheter ablation for AF, including patients with concomitant AF and heart failure; and (7) an integrated approach to the patient with AF and modifiable cardiovascular risk factors. The recommendations were developed using the Grading of Recommendations, Assessment, Development, and Evaluation (GRADE) standards. Individual studies and literature were reviewed for quality and bias; the literature review process and evidence tables are included as Supplementary Material and are available on the CCS Web site. Details of the updated recommendations are presented, along with their background and rationale. This document is linked to an updated summary of all CCS AF guidelines recommendations, from 2010 to the present 2018 Focused Update, which is provided in the Supplementary Material.  相似文献   
32.
The authors describe a rare case in which blunt abdominal trauma resulted in mesenteric injury with delayed double ischemic ileal stenosis. Abdominal computed tomography demonstrated stenotic ileal loop with mural thickening. At surgery, a double stenotic bowel loop was found adjacent to a healed defect in the mesentery. Histological examination of the two resected segments showed fibrotic and ischemic lesions within the mesentery. Ischemic intestinal stenosis from mesenteric injury should be considered in the differential diagnosis in patients suffering from intestinal occlusion with a history of blunt abdominal trauma.  相似文献   
33.
34.
Fossil fuel combustion and agriculture result in atmospheric deposition of 0.8 Tmol/yr reactive sulfur and 2.7 Tmol/yr nitrogen to the coastal and open ocean near major source regions in North America, Europe, and South and East Asia. Atmospheric inputs of dissociation products of strong acids (HNO(3) and H2SO(4)) and bases (NH(3)) alter surface seawater alkalinity, pH, and inorganic carbon storage. We quantify the biogeochemical impacts by using atmosphere and ocean models. The direct acid/base flux to the ocean is predominately acidic (reducing total alkalinity) in the temperate Northern Hemisphere and alkaline in the tropics because of ammonia inputs. However, because most of the excess ammonia is nitrified to nitrate (NO(3)(-)) in the upper ocean, the effective net atmospheric input is acidic almost everywhere. The decrease in surface alkalinity drives a net air-sea efflux of CO(2), reducing surface dissolved inorganic carbon (DIC); the alkalinity and DIC changes mostly offset each other, and the decline in surface pH is small. Additional impacts arise from nitrogen fertilization, leading to elevated primary production and biological DIC drawdown that reverses in some places the sign of the surface pH and air-sea CO(2) flux perturbations. On a global scale, the alterations in surface water chemistry from anthropogenic nitrogen and sulfur deposition are a few percent of the acidification and DIC increases due to the oceanic uptake of anthropogenic CO(2). However, the impacts are more substantial in coastal waters, where the ecosystem responses to ocean acidification could have the most severe implications for mankind.  相似文献   
35.
A sea change in the management of diabetes is occurring with the publication of clinical trials showing unequivocal cardiovascular (CV) protection through the use of certain antihyperglycemic agents. This change is similar to the change that occurred when lipid lowering with statins was first shown to have CV benefits, an event necessitating changes in training and the proactive treatment of lipids by CV specialists. As was the case then, many CV specialists currently feel poorly equipped to address diabetes with this new information even though diabetes is common in CV practice. The purpose of this overview is to provide an updated, comprehensive, and evidence-based CV protection plan for patients with type 2 diabetes, intended specifically for cardiologists and vascular medicine specialists. We attempt to elucidate a set of “CardioDiabetes” core competencies by merging the CV-relevant elements of the Diabetes Canada 2018 guidelines within a framework of comprehensive vascular protection as supported by other CV guidelines. We review the rationale for measuring hemoglobin A1C, understanding its use for establishing a diagnosis and for monitoring treatment. We also provide a brief review of the medications most important for a CV specialist to know. We provide useful memory aids and a succinct set of reminders and tips (“ABCDEFR’S”) that can serve as a comprehensive checklist in the clinic and help to motivate trainees and clinicians to consult the original guideline source documents to enrich their knowledge and improve treatment in this rapidly changing arena.  相似文献   
36.
Deferoxamine mesylate (DFO) reduces morbidity and mortality associated with transfusional iron overload. Data on the utilization and costs of care among U.S. patients receiving DFO in typical clinical practice are limited however. This was a retrospective study using a large U.S. health insurance claims database spanning 1/97-12/04 and representing 40 million members in >70 health plans. Study subjects (n = 145 total, 106 sickle cell disease [SCD], 39 thalassemia) included members with a diagnosis of thalassemia or SCD, one or more transfusions (whole blood or red blood cells), and one or more claims for DFO. Mean transfusion episodes were 12 per year. Estimated mean DFO use was 307 g/year. Central venous access devices were required by 20% of patients. Cardiac disease was observed in 16% of patients. Mean total medical costs were $59,233 per year including $10,899 for DFO and $8,722 for administration of chelation therapy. In multivariate analyses, potential complications of iron overload were associated with significantly higher medical care costs. In typical clinical practice, use of DFO in patients with thalassemia and SCD receiving transfusions is low. Administration costs represent a large proportion of the cost of chelation therapy. Potential complications of iron overload are associated with increased costs.  相似文献   
37.
Very short-lived brominated substances (VSLBr) are an important source of stratospheric bromine, an effective ozone destruction catalyst. However, the accurate estimation of the organic and inorganic partitioning of bromine and the input to the stratosphere remains uncertain. Here, we report near-tropopause measurements of organic brominated substances found over the tropical Pacific during the NASA Airborne Tropical Tropopause Experiment campaigns. We combine aircraft observations and a chemistry−climate model to quantify the total bromine loading injected to the stratosphere. Surprisingly, despite differences in vertical transport between the Eastern and Western Pacific, VSLBr (organic + inorganic) contribute approximately similar amounts of bromine [∼6 (4−9) parts per thousand] to the stratospheric input at the tropical tropopause. These levels of bromine cause substantial ozone depletion in the lower stratosphere, and any increases in future abundances (e.g., as a result of aquaculture) will lead to larger depletions.Until the end of the last century, it was believed that only long-lived species, like bromomethane (CH3Br) and halons, contributed to the global burden of stratospheric bromine. However, disagreement between the observed amount of reactive stratospheric bromine and the sources of long-lived trace gases suggested the existence of an additional contributor: Very short-lived brominated substances (VSLorg) [VSLorg = bromoform (3CHBr3) + dibromomethane (2CH2Br2) + minorVSLBr, where minorVSLBr = bromochloromethane (CH2BrCl) + dibromochloromethane (2CHBr2Cl) + bromodichloromethane (CHBrCl2)] that originate mainly from ocean biogenic sources (1, 2).Several studies have described the processes involved in the transformation of biogenic bromocarbons to inorganic bromine, and their transport through the tropical tropopause layer (TTL) (15). These studies have led to significant progress in modeling the VSLorg contribution to the formation of stratospheric inorganic bromine (Bry) (3, 4, 611). However, the scarcity of observations to constrain the emissions, the impact of deep convection, and the effect of dehydration processes limit the prediction of short-lived source gases that reach the stratosphere (3). On the other hand, atmospheric observations of VSLorg have been provided by ground measurements and cruise, balloon, and airborne campaigns (1214), but the different instruments used between campaigns, and the low spatial and temporal coverage of each study, contribute to the uncertainties in the estimations of total bromine and its partitioning (15). In an attempt to reduce these limitations, we present unique measurements of organic bromine substances carried out with the same instrument, the Global Hawk Whole Air Sampler (GWAS), deployed during the NASA Airborne Tropical Tropopause Experiment (ATTREX), which covered the tropical Pacific region during 2013 and 2014 (see SI Text for details of the campaign).Because coastal areas of tropical waters (like the Maritime Continent) are an important source for VSLorg (1618) and highly convective zones can transport air masses from the troposphere into the stratosphere through the TTL (19), we focus this study on observations taken over the Western Pacific (120°E−165°E) and the Eastern Pacific (187°E−268°E) (Fig. S1). We compared these regions in terms of VSLorg mixing ratios at the tropopause level (∼17 km; Fig. S2), which defines the chemical composition of air that enters the stratosphere.Open in a separate windowFig. S1.GWAS sample locations during ATTREX campaign. Dotted lines define the Western (120°E–165°E) and Eastern Pacific (187°E–268°E) limits for this study.Open in a separate windowFig. S2.Sample density of measurements of organic bromine species (A) during ATTREX-2014 (Western Pacific) and (B) during ATTREX-2013 (Eastern Pacific).Whole air samples were collected during two deployments of the ATTREX campaigns, on board the unmanned aerial vehicle Global Hawk. Measurements of VSLorg were carried out in the field using a combination of gas chromatography with mass selective, flame ionization, and electron capture detectors (Materials and Methods). Fig. 1 A and B displays the observations of CHBr3, CH2Br2, and minorVSLBr, as well as the total organic bromine mixing ratio, in the upper troposphere/lower stratosphere (UTLS) of the Western and Eastern Pacific. GWAS observations indicate that the total amount of VSLorg that enters the stratosphere over the Western and Eastern Pacific is approximately similar, 3.27 ± 0.47 parts per thousand (ppt) and 2.96 ± 0.42 ppt, respectively. These observations are compared with the state-of-the-art Community Atmosphere Model (CAM-Chem) simulations (4, 20) (see Materials and Methods). The results show good agreement with the measurements, and simulate the injection of VSLorg to the stratosphere of 3.84 ± 0.64 ppt and 3.18 ± 1.49 ppt organic Br for the Western and Eastern Pacific, respectively (Fig. 1 A and B).Open in a separate windowFig. 1.GWAS measurements and CAM-Chem simulations ±1 SD. Filled symbols are the 1 km average bins from GWAS measurements. Lines are the CAM-Chem simulation. Values from the arrows represent the mean mixing ratio (ppt) of VSLorg and Bry at the tropopause level (∼17 km) derived from CAM-Chem simulations. (A and B) Organic brominated species multiplied by their atomicity for (A) Western Pacific and (B) Eastern Pacific. (C and D) CAM-Chem estimations of inorganic bromine (Bry) from measured brominated VSLS with shaded ±1 SD for (C) Western Pacific and (D) Eastern Pacific.Although negligible differences of the organic fraction of VSLBr were observed between the Western and Eastern Pacific, we quantified the inorganic fraction coming from the degradation of VSLorg. Estimations of inorganic bromine (Bry = Br + BrO + HOBr + BrONO2 + HBr + BrCl + 2Br2 + BrNO2 + IBr), with a focus at ∼17 km, were calculated with the CAM-Chem model using assimilated meteorological fields for each Global Hawk flight. According to these simulations, the amount of Bry over the Eastern Pacific is 3.02 ± 1.90 ppt, whereas, in the Western Pacific, the mixing ratio of Bry is 1.97 ± 0.21 ppt (Fig. 1 C and D). Bry/VSLorg ratios show that at ∼17 km, the abundance of Bry over the Western Pacific is almost half the amount of VSLorg, in contrast to the Eastern Pacific, where the abundance of Bry is similar to the value of VSLorg (
Values at 17 kmWestern PacificEastern Pacific
From CAM-Chem
 VSLorg, ppt3.84 ± 0.643.18 ± 1.49
 Bry, ppt1.97 ± 0.213.02 ± 1.90
 Bry/VSLorg0.51 ± 0.040.95 ± 0.32
 VSLBr (Bry + VSLorg),* ppt5.81 ± 0.676.20 ± 2.41
From GWAS
 VSLorg, ppt3.27 ± 0.472.96 ± 0.42
 VSLBr (Bry + VSLorg), ppt5.24 ± 0.515.98 ± 1.95
Open in a separate window*VSLBr from CAM-Chem. Both VSLorg and Bry are estimates from CAM-Chem model.VSLBr from GWAS. VSLorg are the measurements from GWAS, and Bry are estimates from CAM-Chem model.We evaluated these different Bry/VSLorg ratios with 12-d back-trajectory analyses using the Numerical Atmospheric dispersion Modeling Environment (NAME) (21) (see Materials and Methods). These analyses indicate that a variety of source regions influenced our samples in the TTL during the ATTREX flights (see SI Text for details). However, the majority of air transported to the tropopause region (∼17 km) of the Eastern and Western Pacific last encountered the boundary layer in the area between 90°E and −140°E (Fig. S3). Fig. 2 A and B shows two representative cases of the locations where the back-trajectories first crossed the 1-km-altitude surface for samples collected over the Western and Eastern Pacific, respectively. This similarity on the source location of the air mass could explain the similar amount of VSLorg observed over both the Western and Eastern Pacific. The NAME analysis indicates that the mean time for the boundary layer (<1 km) air to reach the air sampled at 17 km was 9.8 d in the West Pacific samples and 11.1 d in the East Pacific. This difference in mean times, along with the difference between East and West Pacific in the fraction of trajectories that reach 1 km, is consistent with the observed differences in the mixing ratios of the shorter-lived gases such as methyl iodide, bromoform, and propane (Fig. 2C and Fig. S4D). This is supported by 30-d back-trajectories calculated by NAME, which show that the influence of convective events between days 12 and 30 was small. The same analyses show that differences of Bry could be due to transport dynamics, mixing processes, and age of air masses targeted during the field campaigns. Flights over the Western Pacific tracked fresh air from the air masses detrained into the TTL by Tropical Storm Faxai and air from the South Pacific Convection Zone. Thus, most of the air masses that reached ∼17 km during these two events moved from the boundary layer to the upper troposphere (UT) rather than following the horizontal pattern seen on most of the air masses tracked over the Eastern Pacific (Fig. 2 C and D). We suggest that these “fresh” air masses, quickly transported to the UT, limit the chemistry that leads to the formation of Bry, and reduce their abundance over the Western Pacific. From another point of view, the higher stratospheric injection of Br over the Eastern Pacific could be also related to transport time and distance. For example, as the air masses travel from West to East, heterogeneous recycling reactions could put more Br back into the troposphere than washout is removing. Previous studies have pointed out that rapid uplift of air masses, due to convection events, as well as the colder temperatures within the TTL, can considerably enhance the efficiency of heterogeneous reactions relative to complete washout or ice removal (3, 4, 22, 23). However, the impact of heterogeneous reactions depends on several factors, including the microphysical environment and the partitioning of the inorganic bromine species. Hence, further analysis of the Bry chemical speciation over the Eastern and Western Pacific could provide insight into these fundamental processes.Open in a separate windowFig. 2.NAME 12-d back-trajectories for samples collected over the Western Pacific (A and C) on 4 March 2014 (at 16.58 km, 18.341°N, 147.494°E), and over the Eastern Pacific (B and D) on 22 February 2013 (at 16.54 km, 12.007 °N, 107.82°W). (A and B) Location at which trajectories first crossed 1 km, with the color indicating the time taken to reach this altitude. Black line indicates the ATTREX flight path. Light blue mark represents the location of the GWAS sample where the trajectories start. (C and D) Probability distribution of trajectory altitude as a function of time traveled backward. The median trajectory altitude is marked with a solid line, 25th and 75th percentiles are marked with dotted lines, and 10th and 90th percentiles are marked with dot−dash lines.Open in a separate windowFig. S3.The dots mark the location of all particles released for samples collected between 16.5 km and 17.5 km (average ∼17 km) that passed through the 1-km surface. The color code indicates the time taken to reach this altitude. (A) Eastern Pacific and (B) Western Pacific.

Table S1.

Mixing ratio of other trace gases measured by GWAS during ATTREX campaign, and estimates of decrease from Western Pacific source location
Mixing ratio, pptPercent difference of average mixing ratio between Western and Eastern PacificMean time of air fraction below 1 km, daysTropics lifetime,* daysExponential decayFraction of decrease
Western PacificEastern PacificWestern PacificEastern PacificWestern PacificEastern Pacific
CHBr31.15 ± 0.430.93 ± 0.38199.811.1170.5620.5210.07
Propane22.91 ± 13.4918.53 ± 6.24199.811.113.50.4840.4390.09
CH3I0.07 ± 0.060.03 ± 0.01579.811.13.50.0610.0420.31
Open in a separate window*The 2014 WMO O3 assessment: 10 km tropics (25°S–25°N) annually averaged local lifetime (days) from total loss process.Mixing ratios multiplied by Br atomicity.Open in a separate windowFig. S4.NAME 12-d back-trajectories over the Western Pacific (A and C) on 4 March 2014 (origin at 14.43 km, 17.65°N, 147.43°E), and over the Eastern Pacific (B and D) on 22 February 2013 (origin at 14.34 km, 6.77°N, 101.69°W). (A and B) Location at which trajectories first crossed 1 km, with the color indicating the time taken to reach this altitude. Black line indicates the ATTREX flight path. Light blue marks represent the location of the GWAS sample where the trajectories start. (C and D) Probability distribution of trajectory altitude as a function of time traveled backward. The median trajectory altitude is marked with a solid line, 25th and 75th percentile are marked with dotted lines, and 10th and 90th percentile are marked with dot−dash lines.Based on the CAM-Chem simulation results, the overall contribution of VSL substances (VSLorg + Bry) to total stratospheric bromine, quantified at ∼17 km, show 5.81 (5.14–6.48) ppt over the Western Pacific and 6.20 (3.79–8.61) ppt over the Eastern Pacific (24). Note that this estimate based on model results is slightly higher and has a slightly narrower range than the 2014 WMO O3 assessment. However, using the same methodology as the 2014 WMO O3 assessment, GWAS measurements show that the contribution of VSL substances to total stratospheric bromine would be slightly lower [i.e., 5.24 (4.73–5.75) ppt over the Western Pacific and 5.98 (4.03–7.93) ppt over the Eastern Pacific (Fig. S5 A and B). Halon 1301 was not measured during ATTREX, and its contribution to the Br budget was estimated from measurements at surface sites (25). Remarkably, the results show similar profiles in the UTLS, and relatively little variation, between the Eastern and Western Pacific. In addition, CAM-Chem model simulations clearly capture the distribution and variability of these three major groups. The total organic bromine budgets at the tropopause (17 km, θ ≈ 370 K) resulted in 18.02 ± 0.66 ppt and 17.68 ± 0.49 ppt in the Western and Eastern Pacific, respectively (26, 27) and to the total organic bromine of 17.5 ± 0.6 ppt found over the Eastern Pacific during NASA-Costa Rica-Aura Validation Experiment (NASA-CRAVE) 2006 (https://espoarchive.nasa.gov/archive/browse/cr_ave). The similarity between campaigns over this extended time period reflects the changing abundances of the long-lived species (bromomethane and halons) and the variable amounts of short-lived bromine compounds found during the few campaigns that have collected data in the tropical TTL (25, 28, 29). During the time period from 1996 until 2014, methyl bromide has been declining globally (28). The global average of CH3Br has been reduced by ∼3.5 parts per trillion volume (pptv) during this time. At the same time, the total amount of halons has seen an increasing trend that reached a broad maximum during 2004–2008, and has slowly declined since then. For the missions shown in STRAT 1996*CRAVE 2006ATTREX 2013–2014Campaign locationCentral Pacific, ppt (%)Eastern Pacific, ppt (%)Western Pacific, ppt (%)Eastern Pacific, ppt (%)Halons6.63 ± 0.22 (38)8.26 ± 0.09 (47)7.59 ± 0.19 (42)7.92 ± 0.11 (45)CH3Br9.45 ± 0.39 (54)7.83 ± 0.16 (45)7.16 ± 0.41 (40)6.80 ± 0.23 (38)VSLorg1.30 ± 0.40 (7)1.42 ± 0.52 (8)3.27 ± 0.49 (18)2.96 ± 0.42 (17)Total organic bromine budget17.4 ± 0.917.5 ± 0.618.02 ± 0.6617.68 ± 0.49Open in a separate window*Values calculated from data presented in tables and text in Schauffler et al. (26, 27).Open in a separate windowFig. S5.Vertical profiles of halons, CH3Br, and VSLorg. (A) Western Pacific (B) Eastern Pacific. Solid marks represent the 1-km bin average of GWAS measurements ±1 SD. Solid lines represent the average from CAM-Chem model with shaded ±1 SD limits.We calculated that, during ATTREX, the average level of measured bromine resulted in 20% of total ozone destruction in the tropical lower stratosphere. However, potential changes in the ocean−air flux or a rise in seaweed cultivation could increase VSLorg emissions, leading to an even larger percentage of ozone depletion. Further observations with high-altitude aircraft will improve our understanding of the role of VSLorg in the composition of the tropopause region and the processes occurring in the TTL, diminish the uncertainties of the amount of Bry that enters the stratosphere, and ascertain whether VSLBr is changing in this critical region.  相似文献   
38.
Involvement of BAFF and APRIL in the resistance to apoptosis of B-CLL through an autocrine pathway   总被引:26,自引:11,他引:26       下载免费PDF全文
Kern C  Cornuel JF  Billard C  Tang R  Rouillard D  Stenou V  Defrance T  Ajchenbaum-Cymbalista F  Simonin PY  Feldblum S  Kolb JP 《Blood》2004,103(2):679-688
Tumor necrosis factor (TNF) superfamily members BAFF, or B-cell activation factor of the TNF family, and APRIL, a proliferation-inducing ligand, are involved in normal B-cell survival and differentiation. They interact with 3 receptors: BAFF-R, specific to BAFF; and TACI and BCMA, which are shared by BAFF and APRIL. We tested the potential role of these proteins in B-cell chronic lymphocytic leukemia (B-CLL) resistance to apoptosis. TACI and BAFF-R mRNAs were found in leukemic B cells. BAFF and APRIL mRNAs and proteins were detected in B-CLL leukemic cells and normal blood or tonsil-derived B lymphocytes. Yet, in contrast to normal B lymphocytes, BAFF and APRIL were expressed at the membranes of leukemic cells. Adding soluble BAFF or APRIL protected B-CLL cells against spontaneous and drug-induced apoptosis and stimulated NF-kappaB activation. Conversely, adding soluble BCMA-Fc or anti-BAFF and anti-APRIL antibodies enhanced B-CLL apoptosis. Moreover, a soluble form of BAFF was detected using surface-enhanced laser desorption/ionization-time-of-flight mass spectrometry (SELDI-TOF MS) in the sera of B-CLL patients but not of healthy donors. Taken together, our results indicate that B-CLL cells can be rescued from apoptosis through an autocrine process involving BAFF, APRIL, and their receptors. Inhibiting BAFF and APRIL pathways may be of therapeutic value for B-CLL treatment.  相似文献   
39.
Saccharomyces boulardii interferes with enterohemorrhagic Escherichia coli-induced signaling pathways in T84 cells          下载免费PDF全文
Dahan S  Dalmasso G  Imbert V  Peyron JF  Rampal P  Czerucka D 《Infection and immunity》2003,71(2):766-773
Enterohemorrhagic Escherichia coli (EHEC) infections are associated with the modification of tight-junction permeability and synthesis of proinflammatory cytokine interleukin-8 (IL-8). In a previous study, it was demonstrated that EHEC-induced IL-8 secretion is due to the involvement of the mitogen-activated protein kinase (MAPK), AP-1, and NF-kappaB pathways. In this study, we investigated the effect of the yeast Saccharomyces boulardii on EHEC infection in T84 cells. For this purpose, cells were (i) incubated with bacteria and yeast at the same time or (ii) incubated overnight with yeast cells that were maintained during infection or eliminated by several washes before infection. Coincubation is sufficient to maintain the transmonolayer electrical resistance (TER) of EHEC-infected cells, whereas the preincubation of cells with the yeast without elimination of the yeast during infection is necessary to significantly decrease IL-8 secretion. We thus analyzed the mechanisms of S. boulardii action. We showed that S. boulardii has no effect on EHEC growth or on EHEC adhesion. Kinetics studies revealed that EHEC-induced myosin light chain (MLC) phosphorylation precedes the decrease of TER. ML-7, an MLC kinase inhibitor, abolishes the EHEC-induced MLC phosphorylation and decrease of TER. Studies show that S. boulardii also abolishes EHEC-induced MLC phosphorylation. We demonstrated that the preincubation of cells with S. boulardii without washes before EHEC infection inhibits NF-kappaB DNA binding activity, phosphorylation and degradation of IkappaB-alpha, and activation of the three members of a MAPK group (extracellular signal-regulated protein kinases 1 and 2, p38, and c-jun N-terminal kinase). These findings demonstrate that S. boulardii exerts a preventive effect on EHEC infection by (i) interfering with one of the transduction pathways implicated in the control of tight-junction structure and (ii) decreasing IL-8 proinflammatory secretion via inhibition of the NF-kappaB and MAPK signaling pathways in infected T84 cells.  相似文献   
40.
稳定层流剪应力对内皮细胞骨架调节蛋白VASP表达的影响   总被引:1,自引:0,他引:1  
魏蕾  刘肖珩  欧阳静萍  李柯  Sylvaine Muller  Wang Xiong 《生物医学工程学杂志》2003,20(2):193-196,201
为探讨生理强度的稳定层流剪应力对内皮细胞骨架actin相关蛋白VASP特征影响规律,我们采用胰蛋白酶消化法分离人脐静脉内皮细胞(HUVECs),模拟体内流动环境,建立平行板流动腔模型。利用细胞图像分析系统和ALEXA488—若丹明一次毒蕈环肽双标记法,观察内皮细胞在稳态层流下形态、actin排列变化与VASP分布变化之间的规律。采用Western blot定量动态检测细胞内VASP表达及磷酸化的水平。结果表明,内皮细胞在10dyn/cm^2剪切作用后,随时间细胞逐渐延长,长轴趋于剪应力作用方向排列,细胞与静息态的细胞相比,细胞内骨架沿剪应力方向重组,与此同时VASP表达增强,沿着actin纤维呈点状分布,尤其集中在细胞膜下actin末端区域;Western blot检测显示在剪切后,细胞内VASP出现快速磷酸化,VASP总体表达量增加,2h达高峰后逐渐恢复,8h后再次逐渐升高。以上结果提示血流动力学特性中剪应力引起了细胞胞质内骨架蛋白分子重组,血管内皮细胞形态改变,在此过程中,VASP发挥骨架调节蛋白的作用。  相似文献   
[首页] « 上一页 [1] [2] [3] 4 [5] [6] [7] [8] [9] [10] [11] 下一页 » 末  页»
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