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131.
Holzenberger M Dupont J Ducos B Leneuve P Géloën A Even PC Cervera P Le Bouc Y 《Nature》2003,421(6919):182-187
Studies in invertebrates have led to the identification of a number of genes that regulate lifespan, some of which encode components of the insulin or insulin-like signalling pathways. Examples include the related tyrosine kinase receptors InR (Drosophila melanogaster) and DAF-2 (Caenorhabditis elegans) that are homologues of the mammalian insulin-like growth factor type 1 receptor (IGF-1R). To investigate whether IGF-1R also controls longevity in mammals, we inactivated the IGF-1R gene in mice (Igf1r). Here, using heterozygous knockout mice because null mutants are not viable, we report that Igf1r(+/-) mice live on average 26% longer than their wild-type littermates (P < 0.02). Female Igf1r(+/-) mice live 33% longer than wild-type females (P < 0.001), whereas the equivalent male mice show an increase in lifespan of 16%, which is not statistically significant. Long-lived Igf1r(+/-) mice do not develop dwarfism, their energy metabolism is normal, and their nutrient uptake, physical activity, fertility and reproduction are unaffected. The Igf1r(+/-) mice display greater resistance to oxidative stress, a known determinant of ageing. These results indicate that the IGF-1 receptor may be a central regulator of mammalian lifespan. 相似文献
132.
To understand the physical processes that occur in nature we need to obtain a solid concept about the 'fundamental' forces acting between pairs of elementary particles. It is also necessary to describe the temporal and spatial evolution of many mutually interacting particles under the influence of these forces. This latter step, known as the few-body problem, remains an important unsolved problem in physics. Experiments involving atomic collisions represent a useful testing ground for studying the few-body problem. For the single ionization of a helium atom by charged particle impact, kinematically complete experiments have been performed since 1969 (ref. 7). The theoretical analysis of such experiments was thought to yield a complete picture of the basic features of the collision process, at least for large collision energies. These conclusions are, however, almost exclusively based on studies of restricted electron-emission geometries. Here, we report three-dimensional images of the complete electron emission pattern for the single ionization of helium by the impact of C6+ ions of energy 100 MeV per a.m.u. (a four-body system) and observe features that have not been predicted by any published theoretical model. We propose a higher-order ionization mechanism, involving the interaction between the projectile and the target nucleus, to explain these features. 相似文献
133.
The tumour suppressor CYLD negatively regulates NF-kappaB signalling by deubiquitination 总被引:1,自引:0,他引:1
Kovalenko A Chable-Bessia C Cantarella G Israël A Wallach D Courtois G 《Nature》2003,424(6950):801-805
134.
Molecular farming of recombinant antibodies in plants 总被引:15,自引:0,他引:15
Antibodies represent a large proportion of therapeutic drugs currently in development. In most cases, they are produced in mammalian cell lines or transgenic animals because these have been shown to fold and assemble the proteins correctly and generate authentic glycosylation patterns. However, such expression systems are expensive, difficult to scale up and there are safety concerns due to potential contamination with pathogenic organisms or oncogenic DNA sequences. Plants represent an inexpensive, efficient and safe alternative for the production of recombinant antibodies. Research over the last 10 years has shown that plants can produce a variety of functional antibodies and there is now intense interest in scaling up production to commercial levels. In this review, we discuss the advantages of plants over traditional expression systems, describe how antibody expression in plants is achieved and optimized and then consider the practical issues concerning large-scale molecular farming in plants. The first plant-produced therapeutic antibodies are already in clinical trials, and, given the economic benefits of this production system, we are likely to see many more recombinant antibodies produced in this manner in the future. 相似文献
135.
Elisabeth K SHAGHAGHI WU Yue Alain M GARDIER Christian JACQUOT Marc PALLARDY 《石河子大学学报(自然科学版)》2004,22(1):11-19
在F344雄性大鼠腹腔注射血蓝蛋白(KLH),研究T 细胞依赖抗原初始免疫反应对中枢神经系统5 羟色胺(5 HT)代谢的影响。当免疫刺激大鼠4天后,其下丘脑匀浆5 羟色胺水平出现降低,同时应用在体脑微透析技术研究发现清醒大鼠腹腔注射血蓝蛋白4天后,其下丘脑前叶细胞外液的5 羟色胺水平增加。为了评价在免疫反应中大鼠下丘脑5 羟色胺释放效应,本文应用氯苯丙胺(PCA)选择性预先耗竭5 羟色胺释放,并测定这些动物在注射血蓝蛋白后抗体产生情况。结果显示在应用氯苯丙胺预处理的血蓝蛋白免疫动物特异抗体IgM和IgG与未用氯苯丙胺预处理的动物比较均有明显增加(P<0.01)。上述资料表明,对于T 细胞依赖抗原,其初始抗体产生的量是由位于下丘脑5 羟色胺神经终端抑制性递质释放所调节。 相似文献
136.
A cluster of phosphorylation sites on the cyclic AMP-regulated nuclear factor CREB predicted by its sequence 总被引:130,自引:0,他引:130
G A Gonzalez K K Yamamoto W H Fischer D Karr P Menzel W Biggs W W Vale M R Montminy 《Nature》1989,337(6209):749-752
137.
138.
The existence in the ocean of deep western boundary currents, which connect the high-latitude regions where deep water is formed with upwelling regions as part of the global ocean circulation, was postulated more than 40 years ago. These ocean currents have been found adjacent to the continental slopes of all ocean basins, and have core depths between 1,500 and 4,000 m. In the Atlantic Ocean, the deep western boundary current is estimated to carry (10-40) x 10(6) m3 s(-1) of water, transporting North Atlantic Deep Water--from the overflow regions between Greenland and Scotland and from the Labrador Sea--into the South Atlantic and the Antarctic circumpolar current. Here we present direct velocity and water mass observations obtained in the period 2000 to 2003, as well as results from a numerical ocean circulation model, showing that the Atlantic deep western boundary current breaks up at 8 degrees S. Southward of this latitude, the transport of North Atlantic Deep Water into the South Atlantic Ocean is accomplished by migrating eddies, rather than by a continuous flow. Our model simulation indicates that the deep western boundary current breaks up into eddies at the present intensity of meridional overturning circulation. For weaker overturning, continuation as a stable, laminar boundary flow seems possible. 相似文献
139.
Clément G Ahlberg PE Blieck A Blom H Clack JA Poty E Thorez J Janvier P 《Nature》2004,427(6973):412-413
Several discoveries of Late Devonian tetrapods (limbed vertebrates) have been made during the past two decades, but each has been confined to one locality. Here we describe a tetrapod jaw of about 365 million years (Myr) old from the Famennian of Belgium, which is the first from western continental Europe. The jaw closely resembles that of Ichthyostega, a Famennian tetrapod hitherto known only from Greenland. The environment of this fossil provides information about the conditions that prevailed just before the virtual disappearance of tetrapods from the fossil record for 20 Myr. 相似文献
140.
High-resolution record of Northern Hemisphere climate extending into the last interglacial period 总被引:4,自引:0,他引:4
Andersen KK Azuma N Barnola JM Bigler M Biscaye P Caillon N Chappellaz J Clausen HB Dahl-Jensen D Fischer H Flückiger J Fritzsche D Fujii Y Goto-Azuma K Grønvold K Gundestrup NS Hansson M Huber C Hvidberg CS Johnsen SJ Jonsell U Jouzel J Kipfstuhl S Landais A Leuenberger M Lorrain R Masson-Delmotte V Miller H Motoyama H Narita H Popp T Rasmussen SO Raynaud D Rothlisberger R Ruth U Samyn D Schwander J Shoji H Siggard-Andersen ML Steffensen JP Stocker T Sveinbjörnsdóttir AE Svensson A Takata M 《Nature》2004,431(7005):147-151
Two deep ice cores from central Greenland, drilled in the 1990s, have played a key role in climate reconstructions of the Northern Hemisphere, but the oldest sections of the cores were disturbed in chronology owing to ice folding near the bedrock. Here we present an undisturbed climate record from a North Greenland ice core, which extends back to 123,000 years before the present, within the last interglacial period. The oxygen isotopes in the ice imply that climate was stable during the last interglacial period, with temperatures 5 degrees C warmer than today. We find unexpectedly large temperature differences between our new record from northern Greenland and the undisturbed sections of the cores from central Greenland, suggesting that the extent of ice in the Northern Hemisphere modulated the latitudinal temperature gradients in Greenland. This record shows a slow decline in temperatures that marked the initiation of the last glacial period. Our record reveals a hitherto unrecognized warm period initiated by an abrupt climate warming about 115,000 years ago, before glacial conditions were fully developed. This event does not appear to have an immediate Antarctic counterpart, suggesting that the climate see-saw between the hemispheres (which dominated the last glacial period) was not operating at this time. 相似文献