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  • Mineralogical Association of Canada  (4)
  • Nature Publishing Group (NPG)  (1)
  • 1
    Publication Date: 2016-03-25
    Description: Focal amplifications of chromosome 3p13-3p14 occur in about 10% of melanomas and are associated with a poor prognosis. The melanoma-specific oncogene MITF resides at the epicentre of this amplicon. However, whether other loci present in this amplicon also contribute to melanomagenesis is unknown. Here we show that the recently annotated long non-coding RNA (lncRNA) gene SAMMSON is consistently co-gained with MITF. In addition, SAMMSON is a target of the lineage-specific transcription factor SOX10 and its expression is detectable in more than 90% of human melanomas. Whereas exogenous SAMMSON increases the clonogenic potential in trans, SAMMSON knockdown drastically decreases the viability of melanoma cells irrespective of their transcriptional cell state and BRAF, NRAS or TP53 mutational status. Moreover, SAMMSON targeting sensitizes melanoma to MAPK-targeting therapeutics both in vitro and in patient-derived xenograft models. Mechanistically, SAMMSON interacts with p32, a master regulator of mitochondrial homeostasis and metabolism, to increase its mitochondrial targeting and pro-oncogenic function. Our results indicate that silencing of the lineage addiction oncogene SAMMSON disrupts vital mitochondrial functions in a cancer-cell-specific manner; this silencing is therefore expected to deliver highly effective and tissue-restricted anti-melanoma therapeutic responses.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Leucci, Eleonora -- Vendramin, Roberto -- Spinazzi, Marco -- Laurette, Patrick -- Fiers, Mark -- Wouters, Jasper -- Radaelli, Enrico -- Eyckerman, Sven -- Leonelli, Carina -- Vanderheyden, Katrien -- Rogiers, Aljosja -- Hermans, Els -- Baatsen, Pieter -- Aerts, Stein -- Amant, Frederic -- Van Aelst, Stefan -- van den Oord, Joost -- de Strooper, Bart -- Davidson, Irwin -- Lafontaine, Denis L J -- Gevaert, Kris -- Vandesompele, Jo -- Mestdagh, Pieter -- Marine, Jean-Christophe -- England -- Nature. 2016 Mar 24;531(7595):518-22. doi: 10.1038/nature17161.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Laboratory For Molecular Cancer Biology, Center for Human Genetics, KULeuven, Herestraat 49, 3000 Leuven, Belgium. ; Center for the Biology of Disease, VIB, Herestraat 49, 3000 Leuven, Belgium. ; Institut de Genetique et de Biologie Moleculaire et Cellulaire (IGBMC), Rue Laurent Fries 1, 67404 Illkirch, France. ; Laboratory of Translational Cell and Tissue Research, Department of Pathology, KULeuven and UZ Leuven, Herestraat 49, 3000 Leuven, Belgium. ; Mouse Histopathology Core Facility, Center for the Biology of Disease, VIB-KULeuven, Herestraat 49, 3000 Leuven, Belgium. ; Medical Biotechnology Center, VIB, Albert Baertsoenkaai 3, 9000 Gent, Belgium. ; Department of Biochemistry, Gent University, Albert Baertsoenkaai 3, 9000 Gent, Belgium. ; Center for Medical Genetics, Gent University, De Pintelaan 185, 9000 Gent, Belgium. ; Cancer Research Institute Gent, Gent University, De Pintelaan 185, 9000 Gent, Belgium. ; Gynaecologische Oncologie, KU Leuven, Herestraat 49, 3000 Leuven, Belgium. ; Laboratory of Computational Biology, Center for Human Genetics, KULeuven, Herestraat 49, 3000 Leuven, Belgium. ; Department of Applied Mathematics, Computer Science and Statistics, Gent University, De Pintelaan 185, 9000 Gent, Belgium. ; Department of Mathematics, KU Leuven, Celestijnenlann 200B, 3001 Leuven, Belgium. ; RNA Molecular Biology, Center for Microscopy and Molecular Imaging, Universite Libre de Bruxelles (ULB), rue des Professeurs Jeener et Brachet 12, 6041 Charleroi, Belgium.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/27008969" target="_blank"〉PubMed〈/a〉
    Keywords: Animals ; Carcinogenesis/genetics/pathology ; Cell Lineage ; Cell Proliferation ; Cell Survival ; Chromosomes, Human, Pair 3/genetics ; Clone Cells/metabolism/pathology ; Female ; Gene Amplification/genetics ; Gene Knockdown Techniques ; Humans ; Melanoma/*genetics/*pathology/therapy ; Mice ; Microphthalmia-Associated Transcription Factor/genetics ; Mitochondria/genetics/metabolism/pathology ; Mitochondrial Proteins/metabolism ; Mitogen-Activated Protein Kinases/antagonists & inhibitors/metabolism ; Molecular Targeted Therapy ; Oncogenes/*genetics ; RNA, Long Noncoding/*genetics/therapeutic use ; SOXE Transcription Factors/metabolism ; Xenograft Model Antitumor Assays
    Print ISSN: 0028-0836
    Electronic ISSN: 1476-4687
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2013-02-01
    Description: Zavalíaite, (Mn 2+ ,Fe 2+ ,Mg) 3 (PO 4 ) 2 , belongs to the sarcopside group of minerals and corresponds to the Mn 2+ equivalent of sarcopside and chopinite. It occurs at the La Empleada pegmatite, San Luis Province, Argentina. Zavalíaite forms colorless and transparent exsolution-lamellae up to 70 μm thick and 1.5 mm long in lithiophilite. Owing to hydration, the mineral partially hydrates to reddingite, (Mn 2+ ,Fe 2+ ) 3 (PO 4 ) 2 ·3H 2 O. Lamellae of zavalíaite display a perfect cleavage along the {100} or {001} direction. The luster is vitreous to resinous, and the streak is white. Optically, the mineral is biaxial (–), with an average index of refraction of 1.66(1) (for = 589 nm), 2 V meas = 15(5)°. It is non-pleochroic, without dispersion; the cleavage plane shows an angle of ca . 45° with the elongation of the lamellae; X is perpendicular to this cleavage plane. Zavalíaite is non-fluorescent under short-wave and long-wave ultraviolet light, and its calculated density is 3.68 g/cm 3 . The mineral is brittle, with a Mohs hardness of 4. The mean chemical composition, determined with an electron microprobe from 27 point analyses (wt.%), is: P 2 O 5 41.38, FeO 24.94, MgO 6.09, MnO 27.08, total 99.49. The empirical formula, calculated on the basis of eight atoms of oxygen per formula unit, is (Mn 2+ 1.31 Fe 2+ 1.19 Mg 0.52 ) 3.02 (P 1.00 O 4 ) 2 . Zavalíaite is monoclinic, space group P 2 1 / c , a 6.088(1), b 4.814(1), c 10.484(2)Å, β 89.42(3)°, V 307.2(1) Å 3 , and Z = 2. The crystal structure is identical to that of sarcopside and chopinite, with the M 1 site occupied by 0.5 Fe 2+ + 0.35Mn 2+ + 0.15 Mg, and the M 2 site occupied by 0.475 Mn 2+ + 0.35 Fe 2+ + 0.175 Mg. The strongest eight lines in the X-ray powder pattern [ d in Å (intensities estimated visually) ( hkl )] are: 6.75 (very strong) (100), 3.54 (weak) (012)(11), 2.964 (strong) (200), 2.816 (weak) (013), 2.537 (strong) (11), 1.894 (very strong) (220), 1.848 (very strong) (311), and 1.652 (very strong) (313)(31). The mineral has been approved by the Commission on New Minerals and Mineral Names of the International Mineralogical Association [IMA 2011–012], and is named in honor of María Florencia de Fátima Márquez Zavalía [or Márquez-Zavalía], investigator of Argentinian minerals and ore assemblages and Head of the Department of Mineralogy, Petrography and Geochemistry, IANIGLA, CCT Mendoza, CONICET (National Research Council of Argentina).
    Print ISSN: 0008-4476
    Topics: Geosciences
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  • 3
    Publication Date: 2012-10-29
    Description: A sample from the Koktokay No. 3 granitic pegmatite, Altai Mountains, northwestern China, which shows a transition from lithiophilite [LiMn 2+ PO 4 ] to sicklerite [Li 1– x Mn 2+ PO 4 ], was investigated by single-crystal X-ray diffraction, electron-microprobe analysis, and secondary-ion mass spectrometry (SIMS) techniques. Under the polarizing microscope, the sample shows colorless lithiophilite and deep-orange sicklerite, as well as several intermediate phases. The chemical compositions change from Li 0.96 (Mn 2+ 0.81 Fe 2+ 0.09 Fe 3+ 0.08 )PO 4 to Li 0.69 (Mn 2+ 0.62 Mn 3+ 0.19 Fe 3+ 0.16 )PO 4 , and show a progressive decrease of the lithium content from lithiophilite to sicklerite. Five crystals were extracted from the thin section, and their crystal structures were refined in space group Pbnm , with unit-cell parameters from a 4.736(1), b 10.432(2), c 6.088(1) Å (lithiophilite), to a 4.765(1), b 10.338(1), c 6.060(1) Å (sicklerite). The olivine-type structures of these phosphates are identical to that of triphylite, and are characterized by two chains of edge-sharing octahedra parallel to the c axis. The first chain consists of M 1 octahedra containing Li atoms and vacancies, and the second chain consists of M 2 octahedra occupied by Fe and Mn. The significant Mn 3+ content in sicklerite necessitates a more careful interpretation of the electron-microprobe data, and demonstrates the different mechanisms of oxidation affecting the lithiophilite–sicklerite and triphylite–ferrisicklerite series, respectively.
    Print ISSN: 0008-4476
    Topics: Geosciences
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  • 4
    Publication Date: 2012-08-01
    Print ISSN: 0008-4476
    Electronic ISSN: 1499-1276
    Topics: Geosciences
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  • 5
    Publication Date: 2012-12-01
    Print ISSN: 0008-4476
    Electronic ISSN: 1499-1276
    Topics: Geosciences
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