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01 augustus 2023, Item does not contain fulltext, Understanding the timing and spectrum of genetic alterations that contribute to the development of pancreatic cancer is essential for effective interventions and treatments. The aim of this study was to characterize somatic ATM alterations in noninvasive pancreatic precursor lesions and invasive pancreatic adenocarcinomas from patients with and without pathogenic germline ATM variants. DNA was isolated and sequenced from the invasive pancreatic ductal adenocarcinomas and precursor lesions of patients with a pathogenic germline ATM variant. Tumor and precursor lesions from these patients as well as colloid carcinoma from patients without a germline ATM variant were immunolabeled to assess ATM expression. Among patients with a pathogenic germline ATM variant, somatic ATM alterations, either mutations and/or loss of protein expression, were identified in 75.0% of invasive pancreatic adenocarcinomas but only 7.1% of pancreatic precursor lesions. Loss of ATM expression was also detected in 31.0% of colloid carcinomas from patients unselected for germline ATM status, significantly higher than in pancreatic precursor lesions [pancreatic intraepithelial neoplasms (p = 0.0013); intraductal papillary mucinous neoplasms, p = 0.0040] and pancreatic ductal adenocarcinoma (p = 0.0076) unselected for germline ATM status. These data are consistent with the second hit to ATM being a late event in pancreatic tumorigenesis. © 2023 The Authors. The Journal of Pathology published by John Wiley & Sons Ltd on behalf of The Pathological Society of Great Britain and Ireland.

Oncogenic mutations in the small GTPase RAS contribute to ~30% of human cancers. In a Drosophila genetic screen, we identified novel and evolutionary conserved cancer genes that affect Ras-driven tumorigenesis and metastasis in Drosophila including confirmation of the tetraspanin Tsp29Fb. However, it was not known whether the mammalian Tsp29Fb orthologue, TSPAN6, has any role in RAS-driven human epithelial tumors. Here we show that TSPAN6 suppressed tumor growth and metastatic dissemination of human RAS activating mutant pancreatic cancer xenografts. Whole-body knockout as well as tumor cell autonomous inactivation using floxed alleles of Tspan6 in mice enhanced KrasG12D-driven lung tumor initiation and malignant progression. Mechanistically, TSPAN6 binds to the EGFR and blocks EGFR-induced RAS activation. Moreover, we show that inactivation of TSPAN6 induces an epithelial-to-mesenchymal transition and inhibits cell migration in vitro and in vivo. Finally, low TSPAN6 expression correlates with poor prognosis of patients with lung and pancreatic cancers with mesenchymal morphology. Our results uncover TSPAN6 as a novel tumor suppressor receptor that controls epithelial cell identify and restrains RAS-driven epithelial cancer.

The aim of the YOKOSUKA 91 cruise (October 1991) of the Japanese submersible Shinkai 6500 was to come back on two hydrothermal sites of the axis of the North Fiji Basin ridge which had already been explored by the submersible Nautile in 1989. This cruise gave us the opportunity to show that the hydrothermal manifestations vary a lot in terms of geology, geochemistry or biology during a very short time. A new site which is located in a deep graben of the N 160 ridge axis showed only activity along a fault system marked by sulphide deposits., La campagne YOKOSUKA 91 du sous-marin japonais Shinkai 6500 (octobre 1991) a eu pour objectif de retourner sur deux sites hydrothermaux de l'axe de la dorsale du Bassin Nord-Fidjien explorés en 1989 par le Nautile. On a pu montrer que les manifestations hydrothermales présentent de grandes variations d'ordre géologique, géochimique ou biologique, sur de très courts espaces de temps. Un nouveau site, situé dans un profond graben de l'axe N160 de la dorsale, présente une activité principalement tectonique le long d'un système de failles jalonné par des dépôts de sulfures.

Since 1987, Japanese and French geologists, geophysicists, and biologists have been studying the North Fiji Basin Ridge within the framework of a joint project named STARMER (Science and Technology Agency of Japan—IFREMER of France). This ridge was first geologically, geophysically, and geochemically surveyed during the 1985 SEAPSO 3 cruise of the R/V Jean Charcot [Auzende et al., 1988]. At that time, water sampling and morphotectonic analysis indicated that the North Fiji Basin Ridge was technically and hydrothermally active. Within the STARMER project, four surface ship cruises have been conducted {Kaiyo 87‐88‐89 and Yokosuka 90). One significant result of these surveys is the complete mapping of the entire ridge between 14°S and 22°S (Figure 1), an area approximately 900 km long and more than 50 km wide (Sea Beam and Furuno multibeam swath‐mapping systems were used). During the Kaiyo 87 cruise, the presence of active hydrothermalism (sulfide deposits, chimneys expelling shimmering water, and associated living animal colonies) was discovered through water sampling and video deep towing.

The aim of the YOKOSUKA 91 cruise (October 1991) of the Japanese submersible Shinkai 6500 was to come back on two hydrothermal sites of the axis of the North Fiji Basin ridge which had already been explored by the submersible Nautile in 1989. This cruise gave us the opportunity to show that the hydrothermal manifestations vary a lot in terms of geology, geochemistry or biology during a very short time. A new site which is located in a deep graben of the N 160 ridge axis showed only activity along a fault system marked by sulphide deposits., La campagne YOKOSUKA 91 du sous-marin japonais Shinkai 6500 (octobre 1991) a eu pour objectif de retourner sur deux sites hydrothermaux de l'axe de la dorsale du Bassin Nord-Fidjien explorés en 1989 par le Nautile. On a pu montrer que les manifestations hydrothermales présentent de grandes variations d'ordre géologique, géochimique ou biologique, sur de très courts espaces de temps. Un nouveau site, situé dans un profond graben de l'axe N160 de la dorsale, présente une activité principalement tectonique le long d'un système de failles jalonné par des dépôts de sulfures.

Since 1987, Japanese and French geologists, geophysicists, and biologists have been studying the North Fiji Basin Ridge within the framework of a joint project named STARMER (Science and Technology Agency of Japan—IFREMER of France). This ridge was first geologically, geophysically, and geochemically surveyed during the 1985 SEAPSO 3 cruise of the R/V Jean Charcot [Auzende et al., 1988]. At that time, water sampling and morphotectonic analysis indicated that the North Fiji Basin Ridge was technically and hydrothermally active. Within the STARMER project, four surface ship cruises have been conducted {Kaiyo 87‐88‐89 and Yokosuka 90). One significant result of these surveys is the complete mapping of the entire ridge between 14°S and 22°S (Figure 1), an area approximately 900 km long and more than 50 km wide (Sea Beam and Furuno multibeam swath‐mapping systems were used). During the Kaiyo 87 cruise, the presence of active hydrothermalism (sulfide deposits, chimneys expelling shimmering water, and associated living animal colonies) was discovered through water sampling and video deep towing.

The aim of the YOKOSUKA 91 cruise (October 1991) of the Japanese submersible Shinkai 6500 was to come back on two hydrothermal sites of the axis of the North Fiji Basin ridge which had already been explored by the submersible Nautile in 1989. This cruise gave us the opportunity to show that the hydrothermal manifestations vary a lot in terms of geology, geochemistry or biology during a very short time. A new site which is located in a deep graben of the N 160 ridge axis showed only activity along a fault system marked by sulphide deposits., La campagne YOKOSUKA 91 du sous-marin japonais Shinkai 6500 (octobre 1991) a eu pour objectif de retourner sur deux sites hydrothermaux de l'axe de la dorsale du Bassin Nord-Fidjien explorés en 1989 par le Nautile. On a pu montrer que les manifestations hydrothermales présentent de grandes variations d'ordre géologique, géochimique ou biologique, sur de très courts espaces de temps. Un nouveau site, situé dans un profond graben de l'axe N160 de la dorsale, présente une activité principalement tectonique le long d'un système de failles jalonné par des dépôts de sulfures.

Since 1987, Japanese and French geologists, geophysicists, and biologists have been studying the North Fiji Basin Ridge within the framework of a joint project named STARMER (Science and Technology Agency of Japan—IFREMER of France). This ridge was first geologically, geophysically, and geochemically surveyed during the 1985 SEAPSO 3 cruise of the R/V Jean Charcot [Auzende et al., 1988]. At that time, water sampling and morphotectonic analysis indicated that the North Fiji Basin Ridge was technically and hydrothermally active. Within the STARMER project, four surface ship cruises have been conducted {Kaiyo 87‐88‐89 and Yokosuka 90). One significant result of these surveys is the complete mapping of the entire ridge between 14°S and 22°S (Figure 1), an area approximately 900 km long and more than 50 km wide (Sea Beam and Furuno multibeam swath‐mapping systems were used). During the Kaiyo 87 cruise, the presence of active hydrothermalism (sulfide deposits, chimneys expelling shimmering water, and associated living animal colonies) was discovered through water sampling and video deep towing.

The aim of the YOKOSUKA 91 cruise (October 1991) of the Japanese submersible Shinkai 6500 was to come back on two hydrothermal sites of the axis of the North Fiji Basin ridge which had already been explored by the submersible Nautile in 1989. This cruise gave us the opportunity to show that the hydrothermal manifestations vary a lot in terms of geology, geochemistry or biology during a very short time. A new site which is located in a deep graben of the N 160 ridge axis showed only activity along a fault system marked by sulphide deposits., La campagne YOKOSUKA 91 du sous-marin japonais Shinkai 6500 (octobre 1991) a eu pour objectif de retourner sur deux sites hydrothermaux de l'axe de la dorsale du Bassin Nord-Fidjien explorés en 1989 par le Nautile. On a pu montrer que les manifestations hydrothermales présentent de grandes variations d'ordre géologique, géochimique ou biologique, sur de très courts espaces de temps. Un nouveau site, situé dans un profond graben de l'axe N160 de la dorsale, présente une activité principalement tectonique le long d'un système de failles jalonné par des dépôts de sulfures.