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Sequence variants in the autophagy gene IRGM and multiple other replicating loci contribute to Crohn's disease susceptibility 总被引:14,自引:0,他引:14
Parkes M Barrett JC Prescott NJ Tremelling M Anderson CA Fisher SA Roberts RG Nimmo ER Cummings FR Soars D Drummond H Lees CW Khawaja SA Bagnall R Burke DA Todhunter CE Ahmad T Onnie CM McArdle W Strachan D Bethel G Bryan C Lewis CM Deloukas P Forbes A Sanderson J Jewell DP Satsangi J Mansfield JC;Wellcome Trust Case Control Consortium Cardon L Mathew CG 《Nature genetics》2007,39(7):830-832
A genome-wide association scan in individuals with Crohn's disease by the Wellcome Trust Case Control Consortium detected strong association at four novel loci. We tested 37 SNPs from these and other loci for association in an independent case-control sample. We obtained replication for the autophagy-inducing IRGM gene on chromosome 5q33.1 (replication P = 6.6 x 10(-4), combined P = 2.1 x 10(-10)) and for nine other loci, including NKX2-3, PTPN2 and gene deserts on chromosomes 1q and 5p13. 相似文献
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Parkes RJ Webster G Cragg BA Weightman AJ Newberry CJ Ferdelman TG Kallmeyer J Jørgensen BB Aiello IW Fry JC 《Nature》2005,436(7049):390-394
The sub-seafloor biosphere is the largest prokaryotic habitat on Earth but also a habitat with the lowest metabolic rates. Modelled activity rates are very low, indicating that most prokaryotes may be inactive or have extraordinarily slow metabolism. Here we present results from two Pacific Ocean sites, margin and open ocean, both of which have deep, subsurface stimulation of prokaryotic processes associated with geochemical and/or sedimentary interfaces. At 90 m depth in the margin site, stimulation was such that prokaryote numbers were higher (about 13-fold) and activity rates higher than or similar to near-surface values. Analysis of high-molecular-mass DNA confirmed the presence of viable prokaryotes and showed changes in biodiversity with depth that were coupled to geochemistry, including a marked community change at the 90-m interface. At the open ocean site, increases in numbers of prokaryotes at depth were more restricted but also corresponded to increased activity; however, this time they were associated with repeating layers of diatom-rich sediments (about 9 Myr old). These results show that deep sedimentary prokaryotes can have high activity, have changing diversity associated with interfaces and are active over geological timescales. 相似文献
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