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The production of K∗(892)± meson resonance is measured at midrapidity (|y|<0.5) in Pb−Pb collisions at √sNN=5.02 TeV using the ALICE detector at the CERN Large Hadron Collider. The resonance is reconstructed via its hadronic decay channel K∗(892)±→K0Sπ±. The transverse momentum distributions are obtained for various centrality intervals in the pT range of 0.4−16 GeV/c . Measurements of integrated yields, mean transverse momenta, and particle yield ratios are reported and found to be consistent with previous ALICE measurements for K∗(892)0 within uncertainties. The pT-integrated yield ratio 2K∗(892)±/(K++K−) in central Pb−Pb collisions shows a significant suppression at a level of 9.3σ relative to pp collisions. Thermal model calculations result in an overprediction of the particle yield ratio. Although both hadron resonance gas in partial chemical equilibrium (HRG-PCE) and music + smash simulations consider the hadronic phase, only HRG-PCE accurately represents the measurements, whereas music + smash simulations tend to overpredict the particle yield ratio. These observations, along with the kinetic freeze-out temperatures extracted from the yields measured for light-flavored hadrons using the HRG-PCE model, indicate a finite hadronic phase lifetime, which decreases with increasing collision centrality percentile. The pT-differential yield ratios 2K∗(892)±/(K++K−) and 2K∗(892)±/(π++π−) are presented and compared with measurements in pp collisions at √s=5.02 TeV. Both pa rticle ratios are found to be suppressed by up to a factor of five at pT<2.0 GeV/c in central Pb−Pb collisions and are qualitatively consistent with expectations for rescattering effects in the hadronic phase. The nuclear modification factor (RAA) shows a smooth evolution with centrality and is found to be below unity at pT>8 GeV/c, consistent with measurements for other light-flavored hadrons. The smallest values are observed in most central collisions, indicating larger energy loss of partons traversing the dense medium.
The production of K∗(892)± meson resonance is measured at midrapidity (|y|<0.5) in Pb-Pb collisions at sNN−−−√=5.02 TeV using the ALICE detector at the LHC. The resonance is reconstructed via its hadronic decay channel K∗(892)±→K0Sπ±. The transverse momentum distributions are obtained for various centrality intervals in the pT range of 0.4-16 GeV/c. The reported measurements of integrated yields, mean transverse momenta, and particle yield ratios are consistent with previous ALICE measurements for K∗(892)0. The pT-integrated yield ratio 2K∗(892)±/(K++K−) in central Pb-Pb collisions shows a significant suppression (9.3σ) relative to pp collisions. Thermal model calculations overpredict the particle yield ratio. Although both simulations consider the hadronic phase, only HRG-PCE accurately represents the measurements, whereas MUSIC+SMASH tends to overpredict them. These observations, along with the kinetic freeze-out temperatures extracted from the yields of light-flavored hadrons using the HRG-PCE model, indicate a finite hadronic phase lifetime, which increases towards central collisions. The pT-differential yield ratios 2K∗(892)±/(K++K−) and 2K∗(892)±/(π++π−) are suppressed by up to a factor of five at pT<2 GeV/c in central Pb-Pb collisions compared to pp collisions at s√= 5.02 TeV. Both particle ratios and are qualitatively consistent with expectations for rescattering effects in the hadronic phase. The nuclear modification factor shows a smooth evolution with centrality and is below unity at pT>8 GeV/c, consistent with measurements for other light-flavored hadrons. The smallest values are observed in most central collisions, indicating larger energy loss of partons traversing the dense medium.
Long- and short-range correlations for pairs of charged particles are studied via two-particle angular correlations in pp collisions at s√=13 TeV and p−Pb collisions at sNN−−−√=5.02 TeV. The correlation functions are measured as a function of relative azimuthal angle Δφ and pseudorapidity separation Δη for pairs of primary charged particles within the pseudorapidity interval |η|<0.9 and the transverse-momentum interval 1<pT<4 GeV/c. Flow coefficients are extracted for the long-range correlations (1.6<|Δη|<1.8) in various high-multiplicity event classes using the low-multiplicity template fit method. The method is used to subtract the enhanced yield of away-side jet fragments in high-multiplicity events. These results show decreasing flow signals toward lower multiplicity events. Furthermore, the flow coefficients for events with hard probes, such as jets or leading particles, do not exhibit any significant changes compared to those obtained from high-multiplicity events without any specific event selection criteria. The results are compared with hydrodynamic-model calculations, and it is found that a better understanding of the initial conditions is necessary to describe the results, particularly for low-multiplicity events.
Long- and short-range correlations for pairs of charged particles are studied via two-particle angular correlations in pp collisions at √s = 13 TeV and p–Pb collisions at √sNN = 5.02 TeV. The correlation functions are measured as a function of relative azimuthal angle ∆φ and pseudorapidity separation ∆η for pairs of primary charged particles within the pseudorapidity interval |η| < 0.9 and the transverse-momentum interval 1 < pT < 4 GeV/c. Flow coefficients are extracted for the long-range correlations (1.6 < |∆η| < 1.8) in various high-multiplicity event classes using the low-multiplicity template fit method. The method is used to subtract the enhanced yield of away-side jet fragments in high-multiplicity events. These results show decreasing flow signals toward lower multiplicity events. Furthermore, the flow coefficients for events with hard probes, such as jets or leading particles, do not exhibit any significant changes compared to those obtained from high-multiplicity events without any specific event selection criteria. The results are compared with hydrodynamic-model calculations, and it is found that a better understanding of the initial conditions is necessary to describe the results, particularly for low-multiplicity events.
The knowledge of the material budget with a high precision is fundamental for measurements of direct photon production using the photon conversion method due to its direct impact on the total systematic uncertainty. Moreover, it influences many aspects of the charged-particle reconstruction performance. In this article, two procedures to determine data-driven corrections to the material-budget description in ALICE simulation software are developed. One is based on the precise knowledge of the gas composition in the Time Projection Chamber. The other is based on the robustness of the ratio between the produced number of photons and charged particles, to a large extent due to the approximate isospin symmetry in the number of produced neutral and charged pions. Both methods are applied to ALICE data allowing for a reduction of the overall material budget systematic uncertainty from 4.5% down to 2.5%. Using these methods, a locally correct material budget is also achieved. The two proposed methods are generic and can be applied to any experiment in a similar fashion.
Dielectrons are unique observables in ultra-relativistic heavy-ion collisions. Thanks to their penetrating nature, they carry information from all stages of the collision and can provide knowledge about pre-equilibirium dynamics, QGP temperature and transport coefficients, and chiral symmetry restoration. On the other hand, experimental challenges are enormous because production cross sections are small and the signal of interest is eclipsed by a huge combinatorial and physics background from light- and heavy-flavour hadron decays. In this talk the status of dielectron measurements with ALICE is shown and the perspectives with the recently installed and planned ALICE detector upgrades are discussed.
Der Hirntumor Glioblastom (GBM) ist aufgrund seines infiltrativen Wachstums, der hohen intra- und intertumoralen Heterogenität, der hohen Therapieresistenz als auch aufgrund der sogenannten gliomartigen Stammzellen sehr schwer zu behandeln und führt fast immer zu Rezidiven. Da es in den letzten Jahrzehnten kaum Fortschritte in der Behandlung des GBMs gab, bis auf die Therapie mit Tumortherapiefeldern, wird weiterhin nach alternativen Zelltodtherapien geforscht, wie zum Beispiel dem Autophagie-abhängigen Zelltod. Der Autophagie-abhängige Zelltod ist durch einen erhöhten autophagischen Flux gekennzeichnet und obwohl die Autophagie, als auch selektive Formen wie die Lysophagie und Mitophagie, normalerweise als überlebensfördernde Mechanismen gelten, konnten viele Studien eine duale Rolle in der Tumorentstehung, -progression und -behandlung aufzeigen, die vor allem vom Tumortyp und stadium abhängt. Um die zugrunde liegenden Mechanismen des durch Medikamente induzierten Autophagie-abhängigen Zelltods im GBM weiter zu entschlüsseln, habe ich in meiner Dissertation verschiedene Substanzen untersucht, die einen Autophagie-abhängigen Zelltod induzieren.
In einer zuvor in unserem Labor durchgeführten Studie konnte gezeigt werden, dass das Antipsychotikum Pimozid (PIMO) und der Opioidrezeptor-Antagonist Loperamid (LOP) einen Autophagie-abhängigen Zelltod in GBM Zellen induzieren können. Darauf aufbauend habe ich die Fähigkeit zur Induktion des Autophagie-abhängigen Zelltods in weiteren Zellmodellen validiert. Dies bestätigte einen erhöhten autophagischen Flux nach PIMO und LOP Behandlung, während der Zelltod als auch der autophagische Flux in Autophagie-defizienten Zellen reduziert war. In weiteren Versuchen konnte ich die Involvierung der LC3-assoziierten Phagozytose (LAP), ein Signalweg der auf die Funktion einiger autophagischer Proteine angewiesen ist, ausschließen. Weiterhin konnte ich eine massive Störung des Cholesterin- und Lipidstoffwechsels beobachten. Unter anderem akkumulierte Cholesterin in den Lysosomen gefolgt von massiven Schäden des lysosomalen Kompartiments und der Permeabiliserung der lysosomalen Membran. Dies trug einerseits zur Aktivierung überlebensfördernder Lysophagie als auch der Zell-schädigenden „Bulk“-Autophagie bei. Letztendlich konnte aber die erhöhte Lysophagie die Zellen nicht vor dem Zelltod retten und die Zellen starben einen Autophagie-abhängigen lysosomalen Zelltod. Da die Eignung von LOP als Therapie für das GBM aufgrund der fehlenden Blut-Hirn-Schranken Permeabilität und von dem Antipsychotikum PIMO aufgrund teils schwerer Nebenwirkungen eingeschränkt ist, habe ich mich im weiteren Verlauf meiner Dissertation mit einer Substanz mit einem anderen Wirkmechanismus beschäftigt.
Der Eisenchelator und oxidative Phosphorylierungs (OXPHOS) Inhibitor VLX600 wurde zuvor berichtet mitochondriale Dysfunktion und Zelltod in Kolonkarzinomzellen zu induzieren. Allerdings hat meines Wissens nach bisher noch keine Studie die therapeutische Eignung von VLX600 für das GBM untersucht. Hier zeige ich eine neuartige Autophagie-abhängige Zelltod-induzierende Fähigkeit von VLX600 für GBM Zellen, da der Zelltod signifikant in Autophagie-defizienten Zellen aber nicht durch Caspase-Inhibitoren gehemmt wurde und der autophagische Flux erhöht war. Darüber hinaus konnte ich die Hemmung der OXPHOS und die Induktion von mitochondrialem Stress in GBM Zellen bestätigen und weiterhin aufzeigen, dass VLX600 nicht nur die mitochondriale Homöostase stört, sondern auch zu einer BNIP3-BNIP3L-abhängigen Mitophagie führt, die wahrscheinlich durch HIF1A reguliert wird aber keinen erkennbaren Nettoeffekt auf den von VLX600 induzierten Zelltod hat. Demnach induziert VLX600 letale „Bulk“-Autophagie in den hier verwendeten Zellmodellen. Darüber hinaus konnte ich zeigen, dass die Eisenchelatierung durch VLX600 eine große Rolle für den von VLX600-induzierten Zelltod spielt aber auch für die Mitophagie Induktion, Histon Lysin Methylierung und den ribosomalen Stress. Letztendlich ist es wahrscheinlich ein Zusammenspiel all dieser Faktoren, die zur Zelltodinduktion durch VLX600 führen und interessanterweise werden Eisenchelatoren bereits in präklinischen und klinischen Studien für Krebstherapien untersucht. Dabei könnten gewisse metabolische Eigenschaften verschiedener Tumorzellen die Sensitivität von Wirkstoffen, die auf den Metabolismus wirken wie VLX600, beeinflussen was in zukünftigen Studien beachtet werden sollte um den bestmöglichsten Therapieerfolg zu erzielen. Zusammenfassend unterstützt meine Dissertation die duale Rolle der Autophagie, die stark vom jeweiligen Kontext abhängt und befürwortet die weitere Forschung von Substanzen, die einen Autophagie-abhängigen Zelltod induzieren, für das GBM.
Highligthts
• Marburg virus infects and replicates in primary human proximal tubular cells (PTC).
• Transcriptome analyses at multiple time points revealed a profound inflammatory response by IFNα, -y and TNFα signaling.
• Among the strongly downregulated gene sets were targets of the transcription factors MYC and E2F, the G2M checkpoint, as well as oxidative phosphorylation.
• Importantly, the downregulated factors comprise PGC-1α, a key factor in mitochondrial biogenesis and renal energy homeostasis, to be substantially downregulated in MARV-infected PTC.
• Our results suggest inflammation-induced changes in tubular energy metabolism as a possible factor in MARV-associated tubular dysfunction.
Abstract
Marburg virus, a member of the Filoviridae, is the causative agent of Marburg virus disease (MVD), a hemorrhagic fever with a case fatality rate of up to 90 %. Acute kidney injury is common in MVD and is associated with increased mortality, but its pathogenesis in MVD remains poorly understood. Interestingly, autopsies show the presence of viral proteins in different parts of the nephron, particularly in proximal tubular cells (PTC). These findings suggest a potential role for the virus in the development of MVD-related kidney injury. To shed light on this effect, we infected primary human PTC with Lake Victoria Marburg virus and conducted transcriptomic analysis at multiple time points. Unexpectedly, infection did not induce marked cytopathic effects in primary tubular cells at 20 and 40 h post infection. However, gene expression analysis revealed robust renal viral replication and dysregulation of genes essential for different cellular functions. The gene sets mainly downregulated in PTC were associated with the targets of the transcription factors MYC and E2F, DNA repair, the G2M checkpoint, as well as oxidative phosphorylation. Importantly, the downregulated factors comprise PGC-1α, a well-known factor in acute and chronic kidney injury. By contrast, the most highly upregulated gene sets were those related to the inflammatory response and cholesterol homeostasis. In conclusion, Marburg virus infects and replicates in human primary PTC and induces downregulation of processes known to be relevant for acute kidney injury as well as a strong inflammatory response.
Carbonate archives record a brief snapshot of the ambient Earth’s surface conditions at their deposition. However, the geologically reasonable extraction and interpretation of geochemical proxy data from ancient, diagenetically altered rock archives is fraught with problems. Three issues stand out: the dichotomy between petrographic and geochemical alteration; the lack of quantitative age constraints for specific diagenetic phases resulting in a poorly constrained admixture of local, basin-wide and over-regional (far-field) features; and an often insufficient understanding of the temperatures and compositions of diagenetic fluids. Here, the archive of Devonian marine limestones exposed to multiple far-field diagenetic events is used as an example to explore the above-listed issues. Methods applied include petrography, micro XRF, fluid inclusion data, clumped isotopes, δ13C and δ18O isotopes, 87Sr/86Sr ratios and quartz trace element data. Devonian limestones studied here were overprinted by two cross-cutting regional fault zones (T ≈ 230 °C) by multiple events between the Variscan Orogeny and the late Paleogene. The following processes are recorded: (i) protolith deposition and partial dolomitisation during rapid burial in the Middle/Late Devonian (T ≈ 180 °C); (ii) deep burial to ca 6.5 km and tectonic/hydrothermal overprint during the Variscan Orogeny in the Carboniferous (T ≈ 90–230 °C); (iii) rapid uplift to 1–2 km burial depth at the end of the Variscan Orogeny and hypogene karstification (T ≈ 50 to 100 °C) initiated by regional geology in the Permian/Triassic; (iv) tectonic/hydrothermal overprint during the opening of the Proto-Atlantic Ocean between the Early Jurassic and the Early Cretaceous (T ≈ 50 to 130 °C); (v) tectonic/hydrothermal overprint including renewed hypogene karstification and hydrothermal calcite cement precipitation (T ≈ 50 to 180 °C) during Alpine Orogeny between the Late Cretaceous and late Paleogene. Despite this complex series of diagenetic events, the protolith limestones largely preserved their respective Middle/Late Devonian dissolved inorganic carbon (DIC) and 87Sr/86Sr signatures. This study documents that geochemical proxy data, placed into their petrographic, paleotemperature, and local to over-regional context, significantly increases the ability to extract quantitative information from ancient carbonate rock archives. Research shown here has wider relevance for carbonate archive research in general.