Autophagy induced by Helicobacter pylori infection is necessary for gastric cancer stem cell emergence

Background: The main cause of gastric cancer is the infection by the bacterium Helicobacter pylori which induces a chronic inflammation and an epithelial-to-mesenchymal transition (EMT) leading to the emergence of cells with cancer stem cell (CSC) properties. However, the underlying mechanisms have not been fully characterized. Moreover, H. pylori modulates the host cell autophagic process, but a few studies have investigated the role of this process in tumoral transformation. The aim of this study was to determine whether H. pylori-induced autophagy has a role in CSC emergence. Methods: Autophagic flux in response to H. pylori infection was characterized in AGS cell line expressing the tandem-tagged mCherry-GFP-LC3 protein and using a ratiometric flow cytometry analysis. Then, AGS and MKN45 cell lines were treated with bafilomycin or chloroquine, two pharmaceutical well-known inhibitors of autophagy, and different EMT and CSC characteristics were analyzed. Results: First, a co-expression of the gastric CSC marker CD44 and the autophagic marker LC3 in mice and human stomach tissues infected with H. pylori was observed. Then, we demonstrated in vitro that H. pylori was able to activate the autophagy process with a reduced autophagic flux. Finally, infected cells were treated with autophagy inhibitors, which reduced (i) appearance of mesenchymal phenotypes and migration ability related to EMT and (ii) CD44 expression as well as tumorsphere formation capacities reflecting CSC properties. Conclusion: In conclusion, all these data show that H. pylori-induced autophagy is implicated in gastric CSC emergence and could represent an interesting therapeutic target.This work was supported by the French foundation Ligue contre le Cancer (Pyrénées Atlantiques)

Leukaemia Inhibitory Factor (LIF) inhibits cancer stem cells tumorigenic properties through hippo kinases activation in gastric cancer

Cancer stem cells (CSCs) present chemo-resistance mechanisms contributing to tumour maintenance and recurrence, making their targeting of utmost importance in gastric cancer (GC) therapy. The Hippo pathway has been implicated in gastric CSC properties and was shown to be regulated by leukaemia inhibitory factor receptor (LIFR) and its ligand LIF in breast cancer. This study aimed to determine LIF’s effect on CSC properties in GC cell lines and patient-derived xenograft (PDX) cells, which remains unexplored. LIF’s treatment effect on CSC markers expression and tumoursphere formation was evaluated. The Hippo kinase inhibitor XMU-MP-1 and/or the JAK1 inhibitor Ruxolitinib were used to determine Hippo and canonical JAK/STAT pathway involvement in gastric CSCs’ response to LIF. Results indicate that LIF decreased tumorigenic and chemo-resistant CSCs, in both GC cell lines and PDX cells. In addition, LIF increased activation of LATS1/2 Hippo kinases, thereby decreasing downstream YAP/TAZ nuclear accumulation and TEAD transcriptional activity. LIF’s anti-CSC effect was reversed by XMU-MP-1 but not by Ruxolitinib treatment, highlighting the opposite effects of these two pathways downstream LIFR. In conclusion, LIF displays anti-CSC properties in GC, through Hippo kinases activation, and could in fine constitute a new CSCs-targeting strategy to help decrease relapse cases and bad prognosis in GC.Ministry of Tertiary Education, Research and Innovation/[]//FranciaLigue Nationale Française Contre le Cancer (French National League against Cancer)/[]//FranciaUniversidad de Costa Rica/[]/UCR/Costa RicaMinisterio de Ciencia, Innovación, Tecnología y Telecomunicaciones/[]/MICITT/Costa RicaFrench National Cancer Institute/[PLBio 2014-152]/INCa/FranciaUCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias de la Salud::Instituto de Investigaciones en Salud (INISA

TAZ Controls Helicobacter pylori-Induced Epithelial–Mesenchymal Transition and Cancer Stem Cell-Like Invasive and Tumorigenic Properties

Helicobacter pylori infection, the main risk factor for gastric cancer (GC), leads to an epithelial–mesenchymal transition (EMT) of gastric epithelium contributing to gastric cancer stem cell (CSC) emergence. The Hippo pathway e ectors yes-associated protein (YAP) and transcriptional co-activator with PDZ binding motif (TAZ) control cancer initiation and progression in many cancers including GC. Here, we investigated the role of TAZ in the early steps of H. pylori-mediated gastric carcinogenesis. TAZ implication in EMT, invasion, and CSC-related tumorigenic properties were evaluated in three gastric epithelial cell lines infected by H. pylori. We showed that H. pylori infection increased TAZ nuclear expression and transcriptional enhancer TEA domain (TEAD) transcription factors transcriptional activity. Nuclear TAZ and zinc finger E-box-binding homeobox 1 (ZEB1) were co-overexpressed in cells harboring a mesenchymal phenotype in vitro, and in areas of regenerative hyperplasia in gastric mucosa of H. pylori-infected patients and experimentally infected mice, as well as at the invasive front of gastric carcinoma. TAZsilencing reduced ZEB1 expression andEMTphenotype, and strongly inhibited invasion and tumorsphere formation induced by H. pylori. In conclusion, TAZ activation in response to H. pylori infection contributes to H. pylori-induced EMT, invasion, and CSC-like tumorigenic properties. TAZ overexpression in H. pylori-induced pre-neoplastic lesions and in GC could therefore constitute a biomarker of early transformation in gastric carcinogenesis.Ligue Nationale Française Contre le Cancer (French National League against Cancer)/[]//FranciaUniversidad de Costa Rica/[]/UCR/Costa RicaMinisterio de Ciencia, Innovación, Tecnología y Telecomunicaciones/[]/MICITT/Costa RicaFrench National Cancer Institute/[PLBio 2014-152]/INCa/FranciaLigue Contre le Cancer/[]//FranciaUCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias de la Salud::Instituto de Investigaciones en Salud (INISA

The Hippo Kinase LATS2 Controls Helicobacter pylori-Induced Epithelial-Mesenchymal Transition and Intestinal Metaplasia in Gastric Mucosa

Gastric carcinoma is related mostly to CagA+-Helicobacter pylori infection, which disrupts the gastric mucosa turnover and elicits an epithelial-mesenchymal transition (EMT) and preneoplastic transdifferentiation. The tumor suppressor Hippo pathway controls stem cell homeostasis; its core, constituted by the large tumor suppressor 2 (LATS2) kinase and its substrate Yes-associated protein 1 (YAP1), was investigated in this context.UCR::Vicerrectoría de Investigación::Unidades de Investigación::Ciencias de la Salud::Instituto de Investigaciones en Salud (INISA

Electrical conductivity during incipient melting in the oceanic low-velocity zone

International audienceThe low-viscosity layer in the upper mantle, the asthenosphere, is a requirement for plate tectonics1. The seismic low velocities and the high electrical conductivities of the asthenosphere are attributed either to subsolidus, water-related defects in olivine minerals2, 3, 4 or to a few volume per cent of partial melt5, 6, 7, 8, but these two interpretations have two shortcomings. First, the amount of water stored in olivine is not expected to be higher than 50 parts per million owing to partitioning with other mantle phases9 (including pargasite amphibole at moderate temperatures10) and partial melting at high temperatures9. Second, elevated melt volume fractions are impeded by the temperatures prevailing in the asthenosphere, which are too low, and by the melt mobility, which is high and can lead to gravitational segregation11, 12. Here we determine the electrical conductivity of carbon-dioxide-rich and water-rich melts, typically produced at the onset of mantle melting. Electrical conductivity increases modestly with moderate amounts of water and carbon dioxide, but it increases drastically once the carbon dioxide content exceeds six weight per cent in the melt. Incipient melts, long-expected to prevail in the asthenosphere10, 13, 14, 15, can therefore produce high electrical conductivities there. Taking into account variable degrees of depletion of the mantle in water and carbon dioxide, and their effect on the petrology of incipient melting, we calculated conductivity profiles across the asthenosphere for various tectonic plate ages. Several electrical discontinuities are predicted and match geophysical observations in a consistent petrological and geochemical framework. In moderately aged plates (more than five million years old), incipient melts probably trigger both the seismic low velocities and the high electrical conductivities in the upper part of the asthenosphere, whereas in young plates4, where seamount volcanism occurs6, a higher degree of melting is expected

La conductivité électrique des liquides riches en volatils (C-O-H) produits lors de la fusion partielle du manteau terrestre

Electromagnetic data images mantle regions more conductive than that of dry olivine. There is no doubt that melt is thermodynamically stable and present in the asthenosphere, but how they can impact on mantle electrical conductivity remains debated. Petrological studies realized some 30 years ago have shown that peridotites exposed at the P-T-fO₂ conditions of the asthenosphere produced H₂O and CO₂ rich-melts, but electrical conductivities of these melts are poorly known. Therefore, electrical conductivity experiments have been performed in piston cylinder on H₂O-CO₂ rich melts. Different melt compositions have been explored, from carbonated melts to basalts. The effects of chemical compositions and volatiles on these melts have been determined. The electrical conductivity measurements have shown that hydrous carbonated melts are very conductive, and the incorporation of basalt decreases the conductivity. With these new data, a semi-empirical law predicting the conductivity as a function of H₂O and CO₂ contents has been produced. Based on this law and the electrical conductivity of olivine, 1D conductivity profiles were constructed. With these profiles, the effect of volatile contents (partitioned between the melt and in the solids), melt fractions (mixing law and interconnection of the melt) and different temperature regimes on conductivity are discussed. These calculations are conducted on oceanic and continental settings with different ages. The electrical conductivities of the mantle is thus a powerful tool to track the fundamental process of mantle partial melting, which is in turn narrowly associated to the cycling of H₂O and CO₂ in the upper mantle.Les données électromagnétiques imagent des zones du manteau plus conductrice que l’olivine sèche. Il y a peu d’ambiguïté sur le fait qu’un liquide est thermodynamiquement stable et présent au niveau de l’asthénosphère, mais son impact sur la conductivité électrique du manteau reste débattu. Les études pétrologiques réalisées ces 30 dernières années ont montré qu’une péridotite exposée aux conditions the P-T-fO₂ de l’asthénosphère produisait des liquides riches en H₂O and CO₂, mais les conductivités électriques de ces liquides sont mal connues. Pour cette raison, des expériences de conductivité électrique ont été réalisées en piston cylindre sur des liquides riches en H₂O and CO₂. Différentes compositions de liquides ont été explorées, des liquides carbonatés aux basaltes. Les effets de la composition chimique et des volatiles sur ces liquides ont été déterminés. Les mesures de conductivités électriques ont montré que les liquides hydratés et carbonatés sont très conducteurs, et que l’incorporation de basalte décroit la conductivité. Avec ces nouvelles données, un modèle semi-empirique calculant la conductivité en fonction des teneurs en H₂O and CO₂ a été produit. Sur la base de ce modèle et de la conductivité électrique de l’olivine, des profils 1D de conductivité ont été construits. Avec ces profils, l’effet des teneurs en volatiles (partagé entre le liquide et le solide), les fractions de liquides (loi de mélange et interconnexion du liquide) et les différents régimes de température sur la conductivité ont été discutés. Ces calculs ont été considérés en milieu océanique et continental pour différents âges. La conductivité électrique du manteau est donc un outil puissant pour suivre les processus fondamentaux de la fusion du manteau, qui est à son tour étroitement liée aux cycles de H₂O and CO₂ dans le manteau supérieur

High electrical conductivities in the mantle: an experimental study on low melt fractions

International audienceMany regions in the Earth's mantle show elevated electrical conductivities. Under mid-oceanic ridges, electrical conductivities are in the range 0.1 S.m1 to 0.3 S.m1whereas off-axis conductivities show slightly lower values, which, however, remains well above expected conductivity for conventional peridotitic rocks. A correct interpretation of the petrological nature of the conductive mantle is critical for our understanding of mantle geodynamics. Conductive mantle regions most likely reflect partial melting. The presence of melts in the Earth's mantle has long been proved by geochemical observations and experimental petrology on peridotite rocks by the presence of volatile species (water, carbon dioxide, halogens) which produce small melt fractions (either silicated or carbonated in composition). Hydrated basalts show elevated conductivities, but high melt fractions that carbonated melts are very conductive: 100 to 300 S.m1. Pressure and chemical compositions have little effect on their electrical conductivities. Using different mixing laws (Hashin-Shtrikman upper bound (HS+) or tube law) between carbonated melts and olivine, it is possible to anticipate that we need less than 1% of carbonated melts in the mantle to explain high electrical conductivities. However the electrical conductivity depends on the melt configuration in grain boundaries (sheets, tube, ...). So it is very important to perform new electrical conductivity measurements on peridotite samples containing carbonated melt fraction less to 1%. Since it is very difficult to observe small melt fractions, we can only compare predicted conductivities using different mixing laws with the electrical response of partially molten peridotitic samples. We will report here new measurements of electrical conductivities of peridotitic rocks impregnated with low fractions of carbonated melts. Measurements of sample containing 0.1 to 1% will be presented. The solid matrix will be constituted of dry forsterite and multi-component synthetic peridotites. With these experiments, we will be able to deduce the melt configuration in grain boundaries and to provide a more quantitative interpretation of elevated electrical conductivities imaged in Earth's mantle