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The transcription factor ∆Np63 is a master regulator of epithelial cell identity and essential for the survival of squamous cell carcinoma (SCC) of lung, head and neck, oesophagus, cervix and skin. Here, we report that the deubiquitylase USP28 stabilizes ∆Np63 and maintains elevated ∆NP63 levels in SCC by counteracting its proteasome‐mediated degradation. Impaired USP28 activity, either genetically or pharmacologically, abrogates the transcriptional identity and suppresses growth and survival of human SCC cells. CRISPR/Cas9‐engineered in vivo mouse models establish that endogenous USP28 is strictly required for both induction and maintenance of lung SCC. Our data strongly suggest that targeting ∆Np63 abundance via inhibition of USP28 is a promising strategy for the treatment of SCC tumours.
The Miocene is a key time in the evolution of African mammals and their ecosystems witnessing the origin of the African apes and the isolation of eastern coastal forests through an expanding biogeographic arid corridor. Until recently, however, Miocene sites from the southeastern regions of the continent were unknown. Here we report discovery of the first Miocene fossil teeth from the shoulders of the Urema Rift in Gorongosa National Park, Mozambique, at the southern East African Rift System. We provide the first 1) radiometric age determinations of the fossiliferous Mazamba Formation, 2) reconstructions of past vegetation in the region based on pedogenic carbonates and fossil wood, and 3) description of fossil teeth from the southern rift. Gorongosa is unique in the East African Rift System in combining marine invertebrates, marine vertebrates, terrestrial mammals, and fossil woods in coastal paleoenvironments. The Gorongosa fossil sites offer the first evidence of persistent woodlands and forests on the coastal margins of southeastern Africa during the Miocene, and an exceptional assemblage of fossil vertebrates including new species. Further work will allow the testing of hypotheses positing the formation of a northeast-southwest arid corridor isolating species on the eastern coastal forests from those elsewhere in Africa.
Brief The Miocene is a key time in the evolution of African mammals and their ecosystems encompassing hominine origins and the establishment of an arid corridor that isolated eastern Africa’s coastal forests. Until now, however, Miocene sites from southeastern Africa have been unknown. We report the discovery of the first Miocene fossil sites from Gorongosa National Park, Mozambique, and show that these sites formed in coastal settings. We provide radiometric ages for the fossiliferous sediments, reconstructions of past vegetation based on stable isotopes and fossil wood, and a description of the first fossil teeth from the region. Gorongosa is the only paleontological site in the East African Rift that combines fossil woods, marine invertebrates, marine vertebrates, and terrestrial mammals. Gorongosa offers the first evidence of persistent woodlands and forests on the coastal margins of southeastern Africa during the Miocene.
The Miocene was a key time in the evolution of African ecosystems witnessing the origin of the African apes and the isolation of eastern coastal forests through an expanding arid corridor. Until recently, however, Miocene sites from the southeastern regions of the continent were unknown. Here, we report the first Miocene fossil teeth from the shoulders of the Urema Rift in Gorongosa National Park, Mozambique. We provide the first 1) radiometric ages of the Mazamba Formation, 2) reconstructions of paleovegetation in the region based on pedogenic carbonates and fossil wood, and 3) descriptions of fossil teeth. Gorongosa is unique in the East African Rift in combining marine invertebrates, marine vertebrates, reptiles, terrestrial mammals, and fossil woods in coastal paleoenvironments. The Gorongosa fossil sites offer the first evidence of woodlands and forests on the coastal margins of southeastern Africa during the Miocene, and an exceptional assemblage of fossils including new species.
Die Zytomegafie ist eine meist lebenslänglich latent bleibende vertikale und horizontale Herpesvirusinfektion mit gelegentlich schweren Krankheitsbildern, auch als Ursache oder Folge von Immunstörungen. Dem Virus wird ein onkogenes Potential zugeschrieben, zuletzt diskutiert bei AIDS und M. Kaposi. Für die Labordiagnose verfügen wir über die Mikroskopie (Zellkerneinschlüsse) und Elektronenmikroskopie, Nachweis der Virusinfektiosität auf Zellkulturen, DNA- und Polypeptidanalyse zur Virusstammidentifikation, direkte DNA- und Antigennachweise aus Patientenmaterial, immunhistologische Methoden (z.B. Immunperoxydase- Technik). Die Untersuchung der Immunzellen erfolgt bei der Zytomegalie quantitativ (T-ZellQuotient) und qualitativ (Lymphozytenstimulierung, neuerdings auch mit Vollblut). Am leichtesten gelingt die Labordiagnose serologisch, d.h. über den Antikörpernachweis. Dafür sind eine Vielzahl „liquid" und „solid phase"-Assays entwickelt worden. Am meisten haben sich heute neben der KB R (und P H A) Immunofluororeszenz und ELISA durchgesetzt, wobei einerseits unterschiedliche Antigene („early", „late antigens") und Antigenpräparationen (z. B. Viruskapsid, -envelope) zum Einsatz kommen, andererseits verschiedene Ig- Klassen und -Subklassen getestet werden, um die primäre und sekundäre Zytomegalie zu diagnostizieren und zu differenzieren. Speziell für den Ig M -Nachweis wurden viele Testmodifikationen etabliert; Rheumafaktorinterferenz und IgG-Kompetition lassen sich am besten durch IgG-Präzipitation ausschalten. Die neuen Methoden haben nicht nur die Aufklärung vieler interessanter Krankheitsfälle, sondern auch exakte epidemiologische Studien bei Risikogruppen ermöglicht (Blutspender: 47[0], schwangere Frauen 56[13], Patienten mit Hämophilie: 69[0], nach NTPL: 90[24], nach Herz-OP: 87[1], Prostituierte: 90[1]% CMV-IgG[(IgM)- Antikörperträger].