C/EBP homologous protein contributes to cytokine-induced pro-inflammatory responses and apoptosis in β-cells.

Induction of the C/EBP homologous protein (CHOP) is considered a key event for endoplasmic reticulum (ER) stress-mediated apoptosis. Type 1 diabetes (T1D) is characterized by an autoimmune destruction of the pancreatic β-cells. Pro-inflammatory cytokines are early mediators of β-cell death in T1D. Cytokines induce ER stress and CHOP overexpression in β-cells, but the role for CHOP overexpression in cytokine-induced β-cell apoptosis remains controversial. We presently observed that CHOP knockdown (KD) prevents cytokine-mediated degradation of the anti-apoptotic proteins B-cell lymphoma 2 (Bcl-2) and myeloid cell leukemia sequence 1 (Mcl-1), thereby decreasing the cleavage of executioner caspases 9 and 3, and apoptosis. Nuclear factor-κB (NF-κB) is a crucial transcription factor regulating β-cell apoptosis and inflammation. CHOP KD resulted in reduced cytokine-induced NF-κB activity and expression of key NF-κB target genes involved in apoptosis and inflammation, including iNOS, FAS, IRF-7, IL-15, CCL5 and CXCL10. This was due to decreased IκB degradation and p65 translocation to the nucleus. The present data suggest that CHOP has a dual role in promoting β-cell death: (1) CHOP directly contributes to cytokine-induced β-cell apoptosis by promoting cytokine-induced mitochondrial pathways of apoptosis; and (2) by supporting the NF-κB activation and subsequent cytokine/chemokine expression, CHOP may contribute to apoptosis and the chemo attraction of mononuclear cells to the islets during insulitis.

Biotic effects of the Chicxulub impact, K-T catastrophe and sea level change in Texas

Biotic effects of the Chicxulub impact, the K-T event and sea level change upon planktic foraminifera were evaluated in a new core and outcrops along the Brazos River, Texas, about 1000 km from the Chicxulub impact crater on Yucatan, Mexico. Sediment deposition occurred in a middle neritic environment that shallowed to inner neritic depths near the end of the Maastrichtian. The sea level fall scoured submarine channels, which were infilled by a sandstone complex with reworked Chicxulub impact spherules and clasts with spherules near the base. The original Chicxulub impact ejecta layer was discovered 45-60 cm below the sandstone complex, and predates the K-T mass extinction by about 300,000 years. Results show that the Chicxulub impact caused no species extinctions or any other significant biotic effects. The subsequent sea level fall to inner neritic depth resulted in the disappearance of all larger (>150 mu m) deeper dwelling species creating a pseudo-mass extinction and a survivor assemblage of small surface dwellers and low oxygen tolerant taxa. The K-T boundary and mass extinction was identified 40-80 cm above the sandstone complex where all but some heterohelicids, hedbergellids and the disaster opportunistic guembelitfids went extinct, coincident with the evolution of first Danian species and the global delta(13)C shift. These data reveal that sea level changes profoundly influenced marine assemblages in near shore environments, that the Chicxulub impact and K-T mass extinction are two separate and unrelated events, and that the biotic effects of this impact have been vastly overestimated. (C) 2008 Elsevier B.V. All rights reserved.

Historia morbi atrocis--deux nouveaux cas de ruptures spontanées de l'oesophage (syndrome de Boerhaave) [Historia morbi atrocis--2 new cases of spontaneous rupture of the esophagus (Boerhaave syndrome)].]

We report the case of two patients hospitalized within a few weeks of each other and both presenting with spontaneous rupture of the esophagus whose evolution proved fatal. We take the opportunity of drawing attention to this rare and challenging disease, which is often diagnosed too late.

Un horizon infini. Explorateurs et voyageurs français au Tibet (1846-1912)

Peu reconnus par la critique postcoloniale, souvent assimilés sans nuances aux enjeux géopolitiques du Grand Jeu en Asie centrale à la même période, les récits des explorateurs français du Tibet manifestent pourtant des traits culturels spécifiques dont on se propose ici de mener l'archéologie. Missionnaires, aventuriers, nobles bannis, scientifiques républicains, diplomates, officiers coloniaux, intellectuels et orientalistes éclairés indiquent tous que la culture de l'exploration dont, de 1846 à 1912, ils sont les représentants se conçoit intrinsèquement comme une culture paysagère. Aussi révèlent-ils une évolution originale des savoirs sur le Tibet et des représentations du paysage tibétain qui se découvre progressivement à eux. La description du paysage participe ainsi globalement d'une histoire des sensibilités et d'une histoire des sciences, ce que l'on peut appeler une géosensibilité. Mais la description scientifique du paysage, liée à la pratique du voyage et à une confrontation à l'ailleurs, ne doit pas masquer le primat expérientiel qui lui donne sens. C'est ainsi que le paysage, en tant qu'expérience vécue, en vient à jouer le rôle d'une médiation interculturelle invitant à un renouvellement des questionnaires des explorateurs. Par ailleurs, la description scientifique participe tout autant de différents orientalismes, de différentes perceptions d'un Tibet associé par les voyageurs à un « paysage sacré ». La diversité dont ceux-ci témoignent, mais aussi les croisements de représentations issues d'autres cultures de l'exploration du Tibet - la tradition anglo-saxonne en premier lieu -, nous plongent aux origines de l'« image du Tibet » qui, au loin de la rencontre vivante des explorateurs - la Première Guerre, la Convention de Simla et l'avènement du Guomindang marquent le terme de la culture française de l'exploration du Tibet -, se cristallisera et s'unifiera dans l'imaginaire occidental du XXe siècle.