77 results on '"Pivetta T"'
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2. Continuous Gravity Observations at Mt. Somma-Vesuvius with a gPhoneX Gravimeter: In-Depth Instrumental Response Characterization and Tidal Model
- Author
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Riccardi, U., Carlino, S., Pivetta, T., Hinderer, J., Rosat, S., and Ricciardi, G.
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- 2023
- Full Text
- View/download PDF
3. Geophysical Challenges for Future Satellite Gravity Missions: Assessing the Impact of MOCASS Mission
- Author
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Pivetta, T., Braitenberg, C., and Barbolla, D. F.
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- 2021
- Full Text
- View/download PDF
4. Tumour infiltrating lymphocytes and PD-L1 expression as potential predictors of outcome in patients with malignant pleural mesothelioma
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Sobhani, N., Roviello, G., Pivetta, T., Ianza, A., Bonazza, D., Zanconati, F., Giudici, F., Bottin, C., Corona, S. P., Guglielmi, A., Rizzardi, C., Milione, M., Cortale, M., Confalonieri, M., and Generali, D.
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- 2019
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5. Mass-change And Geosciences International Constellation (MAGIC) expected impact on science and applications.
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Daras, I, March, G, Pail, R, Hughes, C W, Braitenberg, C, Güntner, A, Eicker, A, Wouters, B, Heller-Kaikov, B, Pivetta, T, and Pastorutti, A
- Abstract
The joint ESA/NASA Mass-change And Geosciences International Constellation (MAGIC) has the objective to extend time-series from previous gravity missions, including an improvement of accuracy and spatio-temporal resolution. The long-term monitoring of Earth's gravity field carries information on mass change induced by water cycle, climate change and mass transport processes between atmosphere, cryosphere, oceans and solid Earth. MAGIC will be composed of two satellite pairs flying in different orbit planes. The NASA/DLR-led first pair (P1) is expected to be in a near-polar orbit around 500 km of altitude; while the second ESA-led pair (P2) is expected to be in an inclined orbit of 65°–70° at approximately 400 km altitude. The ESA-led pair P2 Next Generation Gravity Mission shall be launched after P1 in a staggered manner to form the MAGIC constellation. The addition of an inclined pair shall lead to reduction of temporal aliasing effects and consequently of reliance on de-aliasing models and post-processing. The main novelty of the MAGIC constellation is the delivery of mass-change products at higher spatial resolution, temporal (i.e. subweekly) resolution, shorter latency and higher accuracy than the Gravity Recovery and Climate Experiment (GRACE) and Gravity Recovery and Climate Experiment Follow-On (GRACE-FO). This will pave the way to new science applications and operational services. In this paper, an overview of various fields of science and service applications for hydrology, cryosphere, oceanography, solid Earth, climate change and geodesy is provided. These thematic fields and newly enabled applications and services were analysed in the frame of the initial ESA Science Support activities for MAGIC. The analyses of MAGIC scenarios for different application areas in the field of geosciences confirmed that the double-pair configuration will significantly enlarge the number of observable mass-change phenomena by resolving smaller spatial scales with an uncertainty that satisfies evolved user requirements expressed by international bodies such as IUGG. The required uncertainty levels of dedicated thematic fields met by MAGIC unfiltered Level-2 products will benefit hydrological applications by recovering more than 90 per cent of the major river basins worldwide at 260 km spatial resolution, cryosphere applications by enabling mass change signal separation in the interior of Greenland from those in the coastal zones and by resolving small-scale mass variability in challenging regions such as the Antarctic Peninsula, oceanography applications by monitoring meridional overturning circulation changes on timescales of years and decades, climate applications by detecting amplitude and phase changes of Terrestrial Water Storage after 30 yr in 64 and 56 per cent of the global land areas and solid Earth applications by lowering the Earthquake detection threshold from magnitude 8.8 to magnitude 7.4 with spatial resolution increased to 333 km. [ABSTRACT FROM AUTHOR]
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- 2024
- Full Text
- View/download PDF
6. Hydrological and volcano-related gravity signals at Mt. Somma–Vesuvius from ∼20 yr of time-lapse gravity monitoring: implications for volcano quiescence.
- Author
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Pivetta, T, Riccardi, U, Ricciardi, G, and Carlino, S
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GRAVIMETRY , *VOLCANOES , *GRAVITY , *AQUIFERS , *GLOBAL Positioning System - Abstract
We report on about 20 yr of relative gravity measurements, acquired on Mt. Somma–Vesuvius volcano in order to investigate the hydrological and volcano-tectonic processes controlling the present-day activity of the volcano. The retrieved long-term field of time gravity change (2003–2022) shows a pattern essentially related to the subsidence, which have affected the central part of the volcano, as detected by the permanent GNSS network and InSAR data. After reducing the observations for the effect of vertical deformation, no significant residuals are found, indicating no significant mass accumulation or loss within the volcanic system. In the north-western sector of the study area, at the border of the volcano edifice, however, significant residual positive gravity changes are detected which are associated to ground-water rebound after years of intense exploitation of the aquifers. On the seasonal timescale, we find that stations within the caldera rim are affected by the seasonal hydrological effects, while the gravity stations at the base of the Vesuvius show a less clear correlation. Furthermore, within the caldera rim a multiyear gravity transient is detected with an increase phase lasting about 4 yr followed by a slower decrease phase. Analysis of rain data seem to exclude a hydrological origin, hence, we hypothesize a deeper source related to the geothermal activity, which can be present even if the volcano is in a quiescent state. We infer the depth and volume of the source by inverting the spatial pattern of the gravity field at the peak of the transient. A volume of fluids of 9.5 × 107 m3 with density of 1000 kg m−3 at 2.3 km depth is capable to fit reasonably well the observations. To explain the gravity transient, simple synthetic models are produced, that simulate the ascent of fluids from a deep reservoir up to the depth of 2.3 km and a successive diffusion within the carbonate aquifer hosting the geothermal system. The whole process appears to not significantly affect the seismicity rate and the deformation of the volcano. This study demonstrates the importance of a 4-D gravity monitoring of a volcano to understand its complex gravity signals that cover different spatial and temporal scales. Discriminating the different contributions that mix up in the observed gravity changes, in particular those due to hydrologic/anthropogenic activities form those due to the geothermal dynamics, is fundamental for a complete and reliable evaluation of the volcano state. [ABSTRACT FROM AUTHOR]
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- 2023
- Full Text
- View/download PDF
7. Regression parameters between topograpy and gravity as proxies of crustal densities on Earth and other planets
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Pivetta T., Braitenberg C., International Union of Geodesy and Geophysics, Pivetta, T., and Braitenberg, C.
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South Atlantic ,Mar ,isostasy ,global gravity field ,Mars ,South America - Abstract
The statistical evaluation of the correlation between gravity and topography bears information on the isostatic state and the density inhomogeneities of the lithosphere. In appropriate spectral bands, the relation between gravity and topography is linear, and the coefficients depend on the underlying crust and subcrustal densities. We first explore the mutual linear gravity-topography spectral-dependent relations with synthetic lithosphere models, considering different geodynamic situations involving lateral crustal density variation, superficial density changes in topography, and different types of isostatically compensated models. We demonstrate the sensitivity of the regression parameters to the subsurface structure. A second important application is the residualization of the gravity field, useful in areas in which other geophysical constraints are scarse. On other planets topography and gravity field are globally available, and the regression analysis can be used for subsurface exploration and structural characterisation. We demonstrate the usefulness on the African and South American continent, and across the Atlantic ocean, using the gravity data of GOCE. One focus are the Greenstone belts, which are geologically interesting structures to which often mineralizations are associated.
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- 2019
8. A ground based gravity network for monitoring water mass movements in the Classical Karst region
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Pivetta, T., Braitenberg, C., Gabrovšek, F., Meurers, B., Gabriel, G., EGU General Assembly 2019, Pivetta, T., Braitenberg, C., Gabrovšek, F., Meurers, B., and Gabriel, G.
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gravity field ,Karst ,hydrogravimetry ,timevarying ,groundwater monitoring - Abstract
The Classical Karst is a limestone plateau stretching between Italy and Slovenia over an area of about 600km2.The aquifer of Classical Karst contains a complex network of conduits, shafts and large voids that are fed by theautogenic recharge and allogenic input of the Reka River. The Reka River sinks underground in the Škocjan Cavesand continues its underground flow for almost 40km until it reaches the Adriatic Sea at the Timavo Springs. Theriver shows high discharge variations; with minimal discharge below 0.3 m3/s and maximal discharge reachingover 350 m3/s. As the conduit system cannot efficiently drain large discharge, huge water masses are stored inthe epiphreatic voids of the aquifer during flood events. Škocjan Caves present such storage, where a vast amountof water is temporary stored during intense rain. Further evidences of the impressive water movements in thissystem could be found in the geodetic time-series recorded by the Grotta Gigante horizontal pendulums, whichshow deformation transients during Reka flood events. Gravimetry could be a useful tool to obtain local mass balances of such complex system, contributing together withthe other classical hydrologic prospections in depicting the water dynamics in this karstic environment. In additionto this gravimetry represents the ideal completion to the already set up geodetic instrumentation in the ClassicalKarst region. In the last year, we installed two continuous recording gravity stations, near the Škocjan caves and inside the GrottaGigante cave. The Škocjan caves serve as a test site because the cave geometry and the hydraulic system here arewell known. The Grotta Gigante site offers a quiet place and long term geodetic time-series but on the other hand,the hydrodynamics here are less clear. In this contribution, we present the simulations in support to the placement of the instruments and the first analysisconducted on the observed gravity time-series. For the Škocjan caves our simulations estimate that this mass accu-mulation could generate gravity signals up to 30 microGal for extreme events with peak discharge over 250m3/slasting for 1-1.5 days, accumulating over 35 106m3of water. The recorded data in Škocjan supports our simula-tions: a prominent peak up to 5 microGal of amplitude was recorded during a 14 106m3flood event on October2018. We believe that the Classical Karst represents an interesting study case for both the geodetic and hydrologic com-munities; the Škocjan cave offers a natural laboratory to optimally assess the contribution of gravimetry as a toolfor monitoring underground fluid mass movements.
- Published
- 2019
9. Seamount growth to be observed in future satellite gravity missions
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Braitenberg, C., Barbolla, D. F., Brandolin, F., Pivetta, T., International Union of Geodesy and Geophysics, Braitenberg, C., Barbolla, D. F., Brandolin, F., and Pivetta, T.
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seamount - Abstract
Growing seamounts bear a hazard to navigation, especially if their summit reaches shallow depths and they reach the ocean surface. A seamount that expands up to the surface and creates an island, is detectable by remote sensing images, but not if the island retracts below the surface. Real time gravity observations detect the mass change independently of the optical detection, the limiting factor being only the noise level of the data acquisition in relation to the signal generated by the mass change. Starting from realistic size-frequency distributions of seamounts, we estimate the expected signals of seamount growth. We develop a method to compare the signal to the spectral noise characteristics of a GRACE-type mission, expandable to a possible mission with improved noise curve. We evaluate the expected gravity changes of seamounts and find that a noise curve of GRACE improved by a factor 10 would be sufficient to detect a realistic sea mount growth with a latency of 1 year. The detection threshold though has a tradeoff with the time resolution, since resolution improves for increased time periods over which the satellite observation can be averaged.
- Published
- 2019
10. Tectonic and climate induced mass changes - competing signals in long term gravity signals
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Braitenberg, C., Pivetta, T., EGU General Assembly 2019, Braitenberg, C., and Pivetta, T.
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Tibet - Abstract
Several mountain ranges as Alps, Himalaya and Tibet are presently subject to uplift, as documented by GNSSvertical movement rates. Uplift occurs in response to climatic mass loss (deglaciation or hydrologic mass loss)or due to the dynamic forces (crustal compression or mantle inflow below uplifting crust). The uplift generates amass change, which produces a time variation of the gravity field. The deglaciation and changes in the subsurfacehydrologic budget, also generate a mass change, which sums to the tectonic change. Satellite remote sensingis useful in determining the shrinking outlines of glaciers, using both multispectral imaging as well as Radarobservations, thus allowing to determine the surface geometry change. The essential value for climate change andestimate of the hydrologic budget is though the total volume budget estimate, which requires also the thicknessvariation. Remote sensing catches the surface height changes, but these must be corrected for the crustal uplift. Thegeodetic measurements of the crustal dynamics of the Alpine and Himalayan mountain ranges in terms of heightand gravity changes, are therefore in close relation to the estimate of the climatic changes inducing glacier andhydrologic budget changes. We estimate the hydrologic and glacier signal for the Alps and Himalaya-Tibet, usingresults from remote sensing and subsurface hydrologic observations, where available (for the methodologicalrationale see Chen et al. 2018). We estimate the contribution of the dynamic uplift by direct observations ofGNSS. We find that the hydrologic and glacier gravity signal calculated at satellite heights of GRACE andGOCE are superposed to the tectonic signal, and discuss to which amount the signals can be resolved by gravitymeasurements. We compare the predicted signals with the satellite observations of GRACE and GOCE, findingthat the tectonic uplift signal is small relative to the expected glacier/hydrologic signals, but that it cannot beneglected. We define the requirements to future gravity satellites in order to make a significante contribution to thedetection of hydro-glacial mass changes and the separation of the tectonic signal.Reference:Chen W., Braitenberg, C., Serpelloni, E. (2018) Interference of tectonic signals in subsurface hydrologic monitor-ing through gravity and GPS due to mountain building, Global and Planetary Change, Volume 167, August 2018,Pages 148-159.
- Published
- 2019
11. Hydrologic induced deformation : Distinguish surface loading from pressure induced uplift
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Braitenberg, C., Pivetta, T., Grillo, B., Nagy, I., Barbolla, D. F., Devoti, R., Gabrovsek, F., Societa’ Italiana di Fisica, Giovanna Bianchi Bazzi, Braitenberg, C., Pivetta, T., Grillo, B., Nagy, I., Barbolla, D. F., Devoti, R., and Gabrovsek, F.
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uplift - Abstract
The observation of crustal deformation is a means to calculate the strain rates and the stress loading at faults. The strain rate is expected to vary in time during the earthquake cycle, but also due to hydrologic masses and fluxes. Hydrologic mass is an elastic loading of the crust, with a consequent lowering and return to the starting position. The opposite effect occurs in places in which the subsurface waters are constrained to flow in channels with consequent buildup of pressure of the water, which determines a surface uplift and deformation. This latter effect is present in karst areas, and in particular in the classical karst shared between Italy and Slovenia, where crustal deformation is measured with tiltmeters in caves and GPS at the surface.
- Published
- 2019
12. GOCE mission follow-on by cold atom technology: the MOCASS study
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Migliaccio F., Reguzzoni M., Batsukh K., Tino G., Rosi G., Sorrentino F., Braitenberg C., Pivetta T, Barbolla D. B., Zoffoli S., Rene Forsberg, Migliaccio, F., Reguzzoni, M., Batsukh, K., Tino, G., Rosi, G., Sorrentino, F., Braitenberg, C., Pivetta, T, Barbolla, D. B., and Zoffoli, S.
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Next generation gravity mission ,Next generation gravity mission, tectonic gravity signal ,tectonic gravity signal - Abstract
MOCASS (Mass Observation with Cold Atom Sensors in Space) is a study project funded by the Italian Space Agency in the framework of preparatory activities for future missions and payloads of Earth Observation. The idea is to propose a GOCE mission follow-on, launching a unique spacecraft with an on-board gradiometer based on advanced cold atom interferometry (CAI) accelerometers and capable of measuring Earth’s gravity gradients along one or two orthogonal directions. The MOCASS project aims at investigating whether this mission concept can improve GOCE results in terms of accuracy and resolution of the estimated gravity field model, and the capability of detecting mass distribution and monitoring mass variations. To this purpose, firstly the instrument characteristics are defined in terms of long-term stability, accuracy, and spectral responses. Then simulations on gravity field recovery based on the space-wise approach already used for the GOCE data processing are implemented. Finally, an analysis on the geophysical signals that can be detected given the simulated mission performance is made. Simulations were assembled by considering real GOCE orbits at different altitudes, but assuming that a CAI gradiometer is on board the spacecraft. This allows a direct comparison between GOCE and MOCASS performances. Instrumental error spectra were defined depending on the orbit and the orientation of the CAI gradiometer arms, considering both a nadir-pointing satellite and an inertial-pointing one. For each configuration, the effect of the satellite angular velocity was computed from the time series of the GOCE orbit coordinates at different altitudes. The resulting instrumental error shows a flat spectrum in the low frequencies, differently from the one of the GOCE electrostatic accelerometers. On the other hand, the interferometer transfer function introduces a strong correlation between close observations. Given the error spectra and the interferometer integration spectral response, observations of gravity gradients were first simulated and then processed by the space-wise approach, which basically consists in a sequential application of a Wiener filter deconvolution, a local collocation gridding and a spherical harmonic analysis. From Monte Carlo sample statistics, the estimation error of the retrieved gravity field model was evaluated for the different mission configurations, showing an improvement in both accuracy and resolution with respect to GOCE. This estimation error was finally compared with the expected gravity signal from selected geophysical phenomena. In particular, the focus was on the India-Tibet region, which involves important and different movements of mass through time and comprises several different crustal structures. The results show that both time-varying gravity signals, like those due to the Tibet-Himalaya glacier melting and crustal uplift, and static gravity signals, like those due to the India seamounts, could be detected by the MOCASS mission.
- Published
- 2018
13. Gravity changes due to mountain-building processes and their detectability with satellite gravity missions
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Braitenberg, C., Pivetta, T., International Symposium on Geodesy and Geodynamics (ISGG2018), Braitenberg, C., and Pivetta, T.
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Next generation gravity mission ,tectonic gravity signal - Abstract
The Himalaya and Alps mountain ranges, and Tibetan plateau are presently subject to uplift, as documented by GNSS vertical movement rates. Uplift occurs in response to climatic mass loss (deglaciation or hydrologic mass loss) or due to the dynamic forces (crustal compression or mantle inflow below uplifting crust). The uplift generates a mass change, which produces a time variation of the gravity field. The deglaciation and changes in the subsurface hydrologic budget, also generate a mass change, which sums to the tectonic change. The shrinking outlines of glaciers are revealed by remote sensing, but the total volume budget estimate requires also the thickness variation. Remote sensing catches the surface height changes, but these must be corrected for the crustal uplift. The geodetic measurements of the crustal dynamics of the Alpine range in terms of height and gravity changes, is therefore in close relation to the estimate of the climatic changes inducing glacier and hydrologic budget changes. We show that for the Alps and Himalayas the hydrologic gravity signal is superposed to the tectonic signal, and discuss to which amount the signal can be resolved by gravity measurements (Braitenberg and Shum, 2015; Chen et al., 2018). We consider the satellite observations of GRACE and GOCE and propose what kind of error curve would be necessary for possible future gravity satellites to significantly increase the resolution.
- Published
- 2018
14. Gravity from space by Cold Atom Interferometry: the MOCASS study and preliminary results
- Author
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Migliaccio, F., Reguzzoni, M., Batsukh, K., Tino, G., Rosi, G., Sorrentino, F., Braitenberg, C., Pivetta, T., Barbolla, DORA FRANCESCA, Zoffoli, S., European Geosciences Union, Migliaccio, F., Reguzzoni, M., Batsukh, K., Tino, G., Rosi, G., Sorrentino, F., Braitenberg, C., Pivetta, T., Barbolla, DORA FRANCESCA, and Zoffoli, S.
- Subjects
GOCE ,Atom Interferometry ,geodetic satellite - Abstract
MOCASS (Mass Observation with Cold Atom Sensors in Space) is an on-going study project funded by the Italian Space Agency in the framework of preparatory activities for future missions and payloads of Earth Observation. The object of the proposal is an innovative satellite gravity mission based on advanced cold atom interferometry (CAI) accelerometers, with the aim of modelling the static and time-variable gravity field of the Earth with high accuracy and resolution and of monitoring mass variations that occur on and below the Earth surface. The basic idea is a GOCE mission follow-on, launching a unique spacecraft with an on-board instrument capable of measuring some functionals of the Earth gravitational potential. The improvement with respect to the GOCE mission concept can only be achieved by going beyond the technology of electrostatic gradiometers, taking advan- tage of a new generation of sensors, such as cold atom interferometers. In the framework of the MOCASS study, the instrument characteristics are defined in terms of long-term stability, accuracy, and spectral responses. Then simulations on gravity field recovery based on the space-wise approach already used for the GOCE data processing are implemented. Finally an analysis on the geophysical signals that can be detected given the simulated mission performance are performed, with particular attention to hydrologic and tectonic modelling of changing masses. First simulations have already been performed by considering the GOCE orbit parameters but assuming that a CAI gradiometer is on board the spacecraft. This allows direct comparisons between GOCE and MOCASS per- formances. Instrument error spectra have been defined depending on the orbit and CAI configurations, all of them characterized by a flat error spectrum in the low frequencies, differently from the one of the GOCE electrostatic accelerometers. Given the error spectrum and the interferometer integration spectral response, simulated obser- vations have been produced and processed by the space-wise approach, which basically consists in a sequential application of a Wiener filter, a local collocation gridding and a spherical harmonic analysis. From sample statis- tics, the accuracy of the recoverable gravity field model can then be evaluated and compared with the expected gravity signal from selected geophysical phenomena, e.g. orogen geodynamics and glacier melting. Although the study is at this time not complete, these preliminary investigations show promising results.
- Published
- 2018
15. Alps uplift dynamic gravity signal
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Braitenberg C., Pivetta T., Serpelloni E., Chen W., European Geosciences Union, Braitenberg, C., Pivetta, T., Serpelloni, E., and Chen, W.
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Goce ,Grace ,geodynamic uplift ,gravity change ,Goce, Grace, geodynamic uplift, gravity change - Abstract
The Alpine and neighboring Dinarides and Appennine orogens are subject to uplift, as documented by the GNSS vertical movement rates. The uplift is caused by crustal compression and thickening and/or mantle inflow below an uplifting crust. The two end-members can be distinguished by the amount of gravity change rate, the thickening having a smaller gravity signal than the crustal uplift, because the mass surplus at the surface is compensated at the level of lower crust. We calculate the expected rates using the observed GNSS determined uplift rates as geometrical surface constraints, and defining the two end-member geodynamic models. We analyze the gravity change rates of GOCE and GRACE and compare them with the expected rates. Hydrology must be considered in this context, as it contributes to a competing gravity change rate signal that is superposed to the tectonic signal. We find that the predicted signal is measurable, and that lateral changes in the sign of the observed gravity rates over the Alpine range have no counterpart in the ongoing uplift. We analyze possible candidates for this latter signal.
- Published
- 2018
16. Gravimetry for monitoring water movements : the Classic Karst as a natural laboratory
- Author
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Pivetta T., Braitenberg C., European Geosciences Union, Pivetta, T., and Braitenberg, C.
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hydrogeophysic ,hydrogeophysics ,ground water monitoring ,classical Karst ,gravimetry - Abstract
The Karst environment is characterized by a peculiar water system circulation, governed by a network of conduits in which the water flows. The name Karst is derived from the Classic Karst region which is located across Italy, Slovenia and Croatia borders. This area gave name to the phenomenon because it was one of the first worldwide to be studied and it is still object of many researches and hosts an important monitoring network. In this area the water is supplied mainly by infiltration during the autumn-spring rainfall events but also from the Reka river that sinks in the Škocjan caves and then flows underground up to the Timavo Springs. The water path is very well known near the Škocjan cave where the water inflow from the Reka river and the rain fall are continuously monitored and also the karst conduits have been mapped directly by speleology inspection. Such data are indispensable in order to construct and constrain 2D hydraulic models that explain very well the water dynamics in the area. However in Skocjan the water circulation is superficial while in other parts of the Karst the water flows deeper underground: in the Grotta Gigante, a natural cave, the water flow is located over 200m below the surface. Its movement could be hardly monitored by direct observation and also modelling is limited due to the lack of a 3D model of the aquifer. Indirect geophysical methods, in particular gravimetry, could be exploited in order to obtain some constraints for the underground conduits and cavities and also to gain information about the water mass movements through time. In this contribution we present some preliminary synthetic models for assessing the gravity signals expected for the underground cavities typical for the karstic area. In addition we evaluate the time gravity field change during strong rainfall events where the water is expected to fill the conduits and cavities. In future we will take advantage of these models to place a continuous gravity meter that cuold be useful to constrain the water fluxes in area where a direct observation of the water is difficult.
- Published
- 2018
17. 800P Number needed to treat (NNT) and number needed to harm (NNH) to estimate clinical efficacy and safety of new adjuvant (Adj) therapies for resected stage (St) II-III melanoma
- Author
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Zara, D., Pastò, B., Garutti, M., Bartoletti, M., Palmero, L., Bertoli, E., Noto, C., Cucciniello, L., Totaro, F., Rizzetto, M., Pivetta, T., Membrino, A., Freschi, A., Bolzonello, S., and Puglisi, F.
- Published
- 2022
- Full Text
- View/download PDF
18. Gravimetry and petrophysics of the Chad Basin area : Determining the depth of the basement and implication for defining a scientific drilling site (ICDP – CHADRILL Project)
- Author
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Maddaloni F., Braitenberg C., De Min A., Schuster M., Pivetta T., Morsut F., Slejko D., Riggio A., Maddaloni, F., Braitenberg, C., De Min, A., Schuster, M., Pivetta, T., and Morsut, F.
- Subjects
inversion ,Chad ,regression ,rift ,gravity - Published
- 2017
19. GOCE and future gravity missions for geothermal energy exploitation
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Alberto Pastorutti, Braitenberg, C., Pivetta, T., Mariani, P., L. Ouwehand, Pastorutti, Alberto, Braitenberg, Carla, Pivetta, TOMMASO FERRUCCIO MARIA, and Mariani, P.
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GOCE ,geothermal energy, gravity, GOCE, renewable energy ,geothermal energy ,renewable energy ,gravity - Abstract
Geothermal energy is a valuable renewable energy source the exploitation of which contributes to the worldwide reduction of consumption of fossil fuels oil and gas. The exploitation of geothermal energy is facilitated where the thermal gradient is higher than average leading to increased surface heat flow. Apart from the hydrologic circulation properties which depend on rock fractures and are important due to the heat transportation from the hotter layers to the surface, essential properties that increase the thermal gradient are crustal thinning and radiogenic heat producing rocks. Crustal thickness and rock composition form the link to the exploration with the satellite derived gravity field, because both induce subsurface mass changes that generate observable gravity anomalies. The recognition of gravity as a useful investigation tool for geothermal energy lead to a cooperation with ESA and the International Renewable Energy Agency (IRENA) that included the GOCE derived gravity field in the online geothermal energy investigation tool of the IRENA database. The relation between the gravity field products as the free air gravity anomaly, the Bouguer and isostatic anomalies and the heat flow values is though not straightforward and has not a unique relationship. It is complicated by the fact that it depends on the geodynamical context, on the geologic context and the age of the crustal rocks. Globally the geological context and geodynamical history of an area is known close to everywhere, so that a specific known relationship between gravity and geothermal potential can be applied. In this study we show the results of a systematic analysis of the problem, including some simulations of the key factors. The study relies on the data of GOCE and the resolution and accuracy of this satellite. We also give conclusions on the improved exploration power of a gravity mission with higher spatial resolution and reduced data error, as could be achieved in principle by flying an atom interferometer sensor on board a satellite.
- Published
- 2016
20. Relevance of GOCE gradients to detect unknown geologic structures in areas of natural resources
- Author
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Braitenberg, Carla, Mariani, Patrizia, Pivetta, T., Uieda, L., European Space Agency, Braitenberg, Carla, Mariani, Patrizia, Pivetta, T., and Uieda, L.
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GOCE ,Africa ,GOCE, modeling, gravity gradients, Africa, Chad anomaly ,modeling ,Chad anomaly ,gravity gradients - Published
- 2011
21. GOCE observations in exploration geophysics
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Braitenberg, Carla, Mariani, Patrizia, Pivetta, T., ESA, Braitenberg, Carla, Mariani, Patrizia, and Pivetta, T.
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GOCE ,geologic structures ,EGM08 ,quality data ,terrestrial data - Abstract
The satellite GOCE has produced an extraordinary global gravity field with a spatial resolution of 80 km at a precision of 1-2 mGal. When considering geologic structures, the wavelengths of interest for exploration purposes are smaller. We show that the GOCE data produce a new quality assessment tool for fields of higher resolution, which all necessarily rely on terrestrial data. The space-borne control of terrestrial data is necessary in order to obtain 100% reliability of existing data or to assess the quality of newly acquired data. We propose a scheme for controlling and testing the quality of higher resolution data, for example airborne campaigns or the EGM08 global gravity field. EGM08 has the higher resolution of 10 km, but with varying quality, depending on the terrestrial data availability. We show how the quality assessment can be made using the GOCE data, giving confidence in the successive modelling results. Specifically we consider the African continent. Africa is an example where terrestrial data area scarce and where the reliability of EGM08 is very variable, jeopardizing the usefulness of the field if the quality assessment with the GOCE da is not fulfilled.
- Published
- 2011
22. Kojic Acid Derivatives as Iron (III) and Aluminium (III) Chelators
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Pivetta, T., Nurchi, V. M., Crisponi, G., Lachowicz, J., Remelli, Maurizio, Gonzalez Perez, J. M., Niclós Gutiérrez, J., and Castiñeiras, A.
- Published
- 2008
23. Kojic acid derivatives as iron(III) and aluminum(III) chelators
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Pivetta, T., Nurchi, V. M., Remelli, Maurizio, Castiñeiras, A., Gonzalez Perez, J. M., Crisponi, G., Niclós Gutiérrez, J., and Lachowicz, J.
- Published
- 2008
24. A thermodynamic study on complex formation between iron(III) and 1,2-dimethyl-3-hydroxypirydine-4-one
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Crisponi, G., Nurchi, V. M., Pinna, R., Pivetta, T., and Remelli, Maurizio
- Published
- 2003
25. A Spectrophotometric Study on Complex Formation Between Iron(III) and a New Hydroxypyridonate Ligand
- Author
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Crisponi, G., Nurchi, V. M., Pinna, R., Pivetta, T., Formica, Mauro, Fusi, Vieri, Lucarini, Simone, Micheloni, MAURO SERGIO, and Zappia, Giovanni
- Published
- 2003
26. Essential oil composition and variability of Laurus nobilis L. growing in Tunisia, comparison and chemometric investigation of different plant organs.
- Author
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Marzouki, H., Piras, A., Salah, K. Bel Haj, Medini, H., Pivetta, T., Bouzid, S., Marongiu, B., and Falconieri, D.
- Abstract
Stems, leaves, buds and flowers of Laurus nobilis L. growing wild in Tunisia were analysed for their essential oil composition. The essential oil of Laurus nobilis L. gathered from different stations were isolated by hydrodistillation and analysed by GC/MS. The oil yields on a dry weight basis ranged between 0.4% and 1.1%. The major component identified was 1,8-cineole, other predominant components were α-terpinyl acetate, methyl eugenol, eugenol and linalool. Although the same compounds were present in all plant organs, the leaves differed from the stems in the concentration of 1,8-cineole and methyl eugenol, buds and flowers in the concentration of 1,8-cineole and the stem's oil composition differs from the others in content of methyl eugenol. The results obtained from GC/MS analysis of the volatile oils from individual plant organs were submitted to principal component analysis. Chemometric investigations led to differentiation of stems, leaves and buds-flowers with the respect to the content of 1,8-cineole, metyhyl eugenol and α-terpynil acetate; flowers and buds were non-differentiated. Finally, the antibacterial activity of the leaves' essential oils has been assayed. [ABSTRACT FROM AUTHOR]
- Published
- 2009
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27. Structural correlations in nickel(II)–thiodiacetato complexes: molecular and crystal structures and properties of [Ni(tda)(H2O)3]
- Author
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Alarcón-Payer, C., Pivetta, T., Choquesillo-Lazarte, D., González-Pérez, J.M., Crisponi, G., Castiñeiras, A., and Niclós-Gutiérrez, J.
- Published
- 2004
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28. Gravimetry and petrophysics for defining the intracratonic and rift basins of the Western-Central Africa zone
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Carla Braitenberg, Tommaso Pivetta, Francesca Maddaloni, Maddaloni, F., Pivetta, T., and Braitenberg, C.
- Subjects
Rift ,Chad ,Ocean current ,Petrophysics ,Central africa ,gravimetry ,Paleontology ,Geophysics ,Gravitational field ,Geochemistry and Petrology ,Satellite ,Gravimetry ,Geology - Abstract
The global gravity field obtained from the observations of the satellite Gravity Field and Steady-State Ocean Circulation Explorer (GOCE) satellite offers new opportunities in defining density variations of earth’s crust and mantle, allowing new insights into the structure of specific geologic features. The Central African Rift is a key feature in understanding the dismemberment of Gondwana, and we contribute to defining the crustal density structure underlying the rift. The presence of a narrow and up to 12 km deep basin implies crustal stretching allowed the sediment to accumulate, but a key question is whether the stretching processes also affected the deeper layers of the crust or was limited to the upper crust. The study area includes a subbasin of the greater Chad sag basin, which extends over 1500 × 1500 km and occupies the center of North-Central Africa, shared between the countries of Chad, Sudan, Nigeria, Niger, Algeria, Libya, and Cameroon. We find that the rifting affected the lower crust of the West African Rift, and we evaluate evidence for a 1500 km long and several km thick magmatic crustal intrusion presumably associated with underplating and crustal thinning. We estimate that the stretching factor must be at least 1.5 and had affected the entire crust. To our knowledge, the identification of a continuous body of magmatic intrusions is new and has been only possible through the recent global gravity field. The magmatism has altered the thermal conditions from the time of emplacement on, and it is relevant for the maturation of hydrocarbons present in the sediments. The timing of the magmatism is presumably tied to two pulses of volcanism documented in the rift, associated with the first postrift phase from 96 to 88 Ma and the second postrift phase from 23 Ma up to the Quaternary.
- Published
- 2021
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29. Gravity as a tool to improve the hydrologic mass budget in karstic areas
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Carla Braitenberg, Gerald Gabriel, Bruno Meurers, Tommaso Pivetta, Franci Gabrovšek, Pivetta, T., Braitenberg, C., Gabrovsek, F., Gabriel, G., and Meurers, B.
- Subjects
Water mass ,Technology ,subsurface hydrologic monitoring ,subsurface mass changes ,Environmental technology. Sanitary engineering ,oceanic tidal variations ,Drainage system (geomorphology) ,non-tidal oceanic variations ,gravity field ,oceanic tidal variation ,Geography. Anthropology. Recreation ,GE1-350 ,Gravimetry ,TD1-1066 ,General Environmental Science ,Hydrology ,geography ,geography.geographical_feature_category ,Water Movements ,Gravimeter ,Water storage ,General Engineering ,Groundwater recharge ,Karst ,Environmental sciences ,non-tidal oceanic variation ,Environmental science ,General Earth and Planetary Sciences - Abstract
Monitoring the water movements in karstic areas is a fundamental but challenging task due to the complexity of the drainage system and the difficulty in deploying a network of observations. Gravimetry offers a valid complement to classical hydrologic measurements in order to characterize such systems in which the recharge process causes temporarily accumulation of large water volumes in the voids of the epi-phreatic system. We show an innovative integration of gravimetric and hydrologic observations that constrains a hydrodynamic model of the Škocjan cave system (Slovenia). We demonstrate how the inclusion of gravity observations improves water mass budget estimates for the Škocjan area based on hydrological observations only. Finally, the detectability of water storage variations in other karstic contexts is discussed with respect to the noise performances of spring and super-conducting gravimeters.
- Published
- 2021
30. Sensitivity of gravity and topography regressions to earth and planetary structures
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Carla Braitenberg, Tommaso Pivetta, Pivetta, T., and Braitenberg, C.
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Gravity (chemistry) ,Topography ,Isostasy ,010504 meteorology & atmospheric sciences ,Planets ,Mars ,010502 geochemistry & geophysics ,01 natural sciences ,Physics::Geophysics ,Oceanic crust ,Lithosphere ,Bathymetry ,Physics::Atmospheric and Oceanic Physics ,0105 earth and related environmental sciences ,Earth-Surface Processes ,geography ,geography.geographical_feature_category ,Continental crust ,Crustal units ,Crust ,Geophysics ,Ridge ,Global gravity field ,Geology ,Global gravity field, Topography, Isostasy, Crustal units, Planets, Mars - Abstract
The availability of global gravity fields and topography through calculation services like the International Centre for Global Earth Models, allows easy access to gravity data, greatly enlarging the spectrum of users. The applications extend much farther than the classic modeling through the gravity-specialist. We investigate the sensitivity of the joint analysis of topography and gravity data based on linear regression analysis and clustering of the response to particular characteristics of the lithosphere structure. The parameters of the regression analysis are predicted to have characteristic values, which allow to distinguish continental crust from oceanic crust, and signalize the presence of crustal inhomogeneity. Predictions are made through theoretical considerations and on synthetic models. We use the South Atlantic Ocean and the confining South American and African continents for illustration, where the regression parameters distinguish oceanic crust from the ridge up to the bathymetric inflection point, from the transitional crust and the continental crust, allowing to map these units. The general properties of the parameters are statistically relevant, since the errors on the parameters are less than 10% the amplitude of the parameters. We compare the regression parameters with those produced by a global crustal model (CRUST1.0), and find good correspondence between the observed and predicted fields. The analysis can be applied with machine learning algorithms, without the need of specific forward or inverse gravity modeling skills. It is therefore particularly useful in view of the enhanced access to the data through the calculation service, and could be implanted as an add-on tool, since it allows to efficiently distinguish isostatic contribution to the gravity field from crustal sources. Given the experience on the gravity field of the Earth, the analysis can be analogously extended to other planets. For illustration, we show that for Mars a coherent class of Martian crust can be identified.
- Published
- 2020
31. Water mass movements in Classical Karst depicted by continuous gravity measurements
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Pivetta, TOMMASO FERRUCCIO MARIA, Braitenberg, Carla, Franci, Gabrovšek, Bruno, Meurers, Gerald, Gabriel, Pivetta, T., Braitenberg, C. F., Gabrovšek, F., Meurers, B., Gabriel, G., Pivetta, TOMMASO FERRUCCIO MARIA, Braitenberg, Carla, Gabrovšek, Franci, Meurers, Bruno, and Gabriel, Gerald
- Subjects
Monitoring and Modeling Environmental Processes ,Applied Terrestrial Gravimetry ,Hydrology ,Applied Terrestrial Gravimetry, Monitoring and Modeling Environmental Processes, Hydrology - Abstract
Depicting the water dynamics in a Karst environment frequently represents a challenge due to the more complex drainage system compared to porous media and to logistic difficulties in deploying an efficient monitoring network. The observations of key physical parameters such as discharge are usually carried out sparsely and only if a direct access to the drainage channels is possible. For this reason, indirect geophysical methods, such as gravimetry, could be a valid complement to hydrological prospections to study the hydrodynamics of such systems. A typical karst environment is the “Carso/Kars” region, which is a 600km2 limestone aquifer, shared between Italy and Slovenia. The aquifer is constituted by an extended network of caves, shafts, and conduits fed by autogenic water and the allogenic contribution of the Reka river. The Reka river sinks in the Škocjan caves and continues its underground flow for over 30 km, finally outflowing in the Adriatic sea at the Timavo Springs. The river shows high discharge variability between dry and wet periods (0.3- 350 m3/s) and as the karst conduit system cannot efficiently drain large discharge, huge water masses are temporarily stored in the epiphreatic voids during flood events. In July 2018 we installed a gravimeter near the Škocjan caves with the aim to monitor continuously the water variations. In this contribution, we present the gravity data and the processing in order to remove tidal and other non-hydrologic components and, thus, to decipher the gravity variations linked to the Karst water circulation. Some challenges in the processing arise since the study area is close to the Adriatic sea, where marine tidal and non-tidal contributions are unneglectable. Our gravity measurements revealed many effects that are linked to the local hydrology: one important event flooded the caves in February 2019 causing a gravity change of 40 microGal. The event is compatible with the gravity estimate derived from a hydraulic model of the cave which reported an accumulation of about 10 106 m3 of water in the whole cave system in 1.5 days. The case discussed in this contribution represents a first promising application of gravimetry for tracking the water paths in the Classical Karst, easily applicable to other sectors of the Karst for which only little information about the hydrological system exist.
- Published
- 2019
32. Metabolism of primary high-grade serous ovarian carcinoma (HGSOC) cells under limited glutamine or glucose availability.
- Author
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Šimčíková D, Gardáš D, Pelikán T, Moráň L, Hruda M, Hložková K, Pivetta T, Hendrych M, Starková J, Rob L, Vaňhara P, and Heneberg P
- Abstract
Background: High-grade serous ovarian carcinoma (HGSOC) is the most common and aggressive subtype of epithelial ovarian carcinoma. It is primarily diagnosed at stage III or IV when the 5-year survival rate ranges between 20% and 40%. Here, we aimed to validate the hypothesis, based on HGSOC cell lines, that proposed the existence of two distinct groups of HGSOC cells with high and low oxidative phosphorylation (OXPHOS) metabolism, respectively, which are associated with their responses to glucose and glutamine withdrawal., Methods: We isolated and cultivated primary cancer cell cultures from HGSOC and nontransformed ovarian fibroblasts from the surrounding ovarium of 45 HGSOC patients. We tested the metabolic flexibility of the primary cells, particularly in response to glucose and glutamine depletion, analyzed and modulated endoplasmic reticulum stress, and searched for indices of the existence of previously reported groups of HGSOC cells with high and low OXPHOS metabolism., Results: The primary HGSOC cells did not form two groups with high and low OXPHOS that responded differently to glucose and glutamine availabilities in the cell culture medium. Instead, they exhibited a continuum of OXPHOS phenotypes. In most tumor cell isolates, the responses to glucose or glutamine withdrawal were mild and surprisingly correlated with those of nontransformed ovarian fibroblasts from the same patients. The growth of tumor-derived cells in the absence of glucose was positively correlated with the lipid trafficking regulator FABP4 and was negatively correlated with the expression levels of HK2 and HK1. The correlations between the expression of electron transport chain (ETC) proteins and the oxygen consumption rates or extracellular acidification rates were weak. ER stress markers were strongly expressed in all the analyzed tumors. ER stress was further potentiated by tunicamycin but not by the recently proposed ER stress inducers based on copper(II)-phenanthroline complexes. ER stress modulation increased autophagy in tumor cell isolates but not in nontransformed ovarian fibroblasts., Conclusions: Analysis of the metabolism of primary HGSOC cells rejects the previously proposed hypothesis that there are distinct groups of HGSOC cells with high and low OXPHOS metabolism that respond differently to glutamine or glucose withdrawal and are characterized by ETC protein levels., (© 2024. The Author(s).)
- Published
- 2024
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33. Intact cell mass spectrometry coupled with machine learning reveals minute changes induced by single gene silencing.
- Author
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Pečinka L, Moráň L, Kovačovicová P, Meloni F, Havel J, Pivetta T, and Vaňhara P
- Abstract
Intact (whole) cell MALDI TOF mass spectrometry is a commonly used tool in clinical microbiology for several decades. Recently it was introduced to analysis of eukaryotic cells, including cancer and stem cells. Besides targeted metabolomic and proteomic applications, the intact cell MALDI TOF mass spectrometry provides a sufficient sensitivity and specificity to discriminate cell types, isogenous cell lines or even the metabolic states. This makes the intact cell MALDI TOF mass spectrometry a promising tool for quality control in advanced cell cultures with a potential to reveal batch-to-batch variation, aberrant clones, or unwanted shifts in cell phenotype. However, cellular alterations induced by change in expression of a single gene has not been addressed by intact cell mass spectrometry yet. In this work we used a well-characterized human ovarian cancer cell line SKOV3 with silenced expression of a tumor suppressor candidate 3 gene (TUSC3). TUSC3 is involved in co-translational N-glycosylation of proteins with well-known global impact on cell phenotype. Altogether, this experimental design represents a highly suitable model for optimization of intact cell mass spectrometry and analysis of spectral data. Here we investigated five machine learning algorithms (k-nearest neighbors, decision tree, random forest, partial least squares discrimination, and artificial neural network) and optimized their performance either in pure populations or in two-component mixtures composed of cells with normal or silenced expression of TUSC3. All five algorithms reached accuracy over 90 % and were able to reveal even subtle changes in mass spectra corresponding to alterations of TUSC3 expression. In summary, we demonstrate that spectral fingerprints generated by intact cell MALDI-TOF mass spectrometry coupled to a machine learning classifier can reveal minute changes induced by alteration of a single gene, and therefore contribute to the portfolio of quality control applications in routine cell and tissue cultures., Competing Interests: The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper., (© 2024 The Author(s).)
- Published
- 2024
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34. A novel heteroleptic Cu(II)-phenanthroline-UDCA complex as lipoxygenase inhibitor and ER-stress inducer in cancer cell lines.
- Author
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Masuri S, Moráň L, Vesselá T, Cadoni E, Cabiddu MG, Pečinka L, Gabrielová V, Meloni F, Havel J, Vaňhara P, and Pivetta T
- Subjects
- Ursodeoxycholic Acid pharmacology, Phenanthrolines chemistry, Copper pharmacology, Copper chemistry, Molecular Docking Simulation, Endoplasmic Reticulum Stress, Cell Line, Enzyme Inhibitors pharmacology, Apoptosis, Pancreatic Neoplasms, Lipoxygenase Inhibitors pharmacology, Neoplasms
- Abstract
A new heteroleptic copper(II) compound named C0-UDCA was prepared by reaction of [Cu(phen)
2 (OH2 )](ClO4 )2 (C0) with the bile ursodeoxycholic acid (UDCA). The resulting compound is able to inhibit the lipoxygenase enzyme showing more efficacy than the precursors C0 and UDCA. Molecular docking simulations clarified the interactions with the enzyme as due to allosteric modulation. The new complex shows antitumoral effect on ovarian (SKOV-3) and pancreatic (PANC-1) cancer cells at the Endoplasmic Reticulum (ER) level by activating the Unfolded Protein Response. In particular, the chaperone BiP, the pro-apoptotic protein CHOP and the transcription factor ATF6 are upregulated in the presence of C0-UDCA. The combination of Intact Cell MALDI-MS and statistical analysis have allowed us to discriminate between untreated and treated cells based on their mass spectrometry fingerprints., Competing Interests: Declaration of Competing Interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper., (Copyright © 2023 Elsevier Inc. All rights reserved.)- Published
- 2023
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35. Cyclin-Dependent Kinase 4/6 Inhibitors Beyond Progression in Metastatic Breast Cancer: A Retrospective Real-World Biomarker Analysis.
- Author
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Gerratana L, Davis AA, Velimirovic M, Reduzzi C, Clifton K, Bucheit L, Hensing WL, Shah AN, Pivetta T, Dai CS, D'Amico P, Wehbe F, Medford A, Wander SA, Gradishar WJ, Behdad A, Ma CX, Puglisi F, Bardia A, and Cristofanilli M
- Subjects
- Humans, Female, Cyclin-Dependent Kinase 4, Retrospective Studies, Genomics, Breast Neoplasms drug therapy, Breast Neoplasms genetics, Circulating Tumor DNA
- Abstract
Purpose: As the continuation beyond progression (BP) of cyclin-dependent kinase 4/6 inhibitors (CDK4/6i) is becoming increasingly attractive for the treatment of patients with hormone receptor (HR)-positive, human epidermal growth factor receptor 2 (HER2)-negative metastatic breast cancer (MBC), the definition of resistance factors is crucial. The aim of the study was to investigate the impact of CDK 4/6i BP and to explore potential genomic stratification factors., Materials and Methods: We retrospectively analyzed a multi-institutional cohort of patients with HR-positive HER2-negative MBC characterized for circulating tumor DNA through next-generation sequencing before treatment start. Differences across subgroups were analyzed by chi-square test, and survival was tested by univariable and multivariable Cox regression. Further correction was applied by propensity score matching., Results: Among the 214 patients previously exposed to CDK4/6i, 172 were treated with non-CDK4/6i-based treatment (non-CDK) and 42 with CDK4/6i BP. Multivariable analysis showed a significant impact of CDK4/6i BP, TP53 single-nucleotide variants, liver involvement, and treatment line on both progression-free survival (PFS) and overall survival (OS). Propensity score matching confirmed the prognostic role of CDK4/6i BP both for PFS and OS. The favorable impact of CDK4/6i BP was consistent across all subgroups, and a differential benefit was suggested for ESR1 -mutated patients. ESR1 and RB1 mutations were more represented in the CDK4/6i BP subgroup with respect to CDK4/6i upfront., Conclusion: The study highlighted a significant prognostic impact of the CDK4/6i BP strategy with a potential added benefit in patients with ESR1 mutations suggesting the need for an extensive biomarker characterization.
- Published
- 2023
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36. Hydroxylated Coumarin-Based Thiosemicarbazones as Dual Antityrosinase and Antioxidant Agents.
- Author
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Masuri S, Era B, Pintus F, Cadoni E, Cabiddu MG, Fais A, and Pivetta T
- Subjects
- Monophenol Monooxygenase, Melanocytes, Coumarins, Melanins, Enzyme Inhibitors pharmacology, Antioxidants pharmacology, Thiosemicarbazones pharmacology
- Abstract
The design of novel antityrosinase agents appears extremely important in medical and industrial sectors because an irregular production of melanin is related to the insurgence of several skin-related disorders (e.g., melanoma) and the browning process of fruits and vegetables. Because melanogenesis also involves a nonenzymatic oxidative process, developing dual antioxidant and antityrosinase agents is advantageous. In this work, we evaluated the antioxidant and tyrosinase inhibition ability of two new bishydroxylated and two new monohydroxylated derivatives of (1 E )-2-(1-(2-oxo-2 H -chromen-3-yl)ethylidene)hydrazine-1-carbothioamide ( T1 ) using different experimental and computational approaches. The study was also carried out on another monohydroxylated derivative of T1 for comparison. Interestingly, these molecules have more potent tyrosinase-inhibitory properties than the reference compound, kojic acid. Moreover, the antioxidant activity appears to be influenced according to the number and substitution pattern of the hydroxyl groups. The safety of the compounds without ( T1 ), with one ( T3 ), and with two ( T6 ) hydroxyl groups, has also been assessed by studying their cytotoxicity on melanocytes. These results indicate that (1 E )-2-(1-(2-oxo-2H-chromen-3-yl)ethylidene)hydrazine-1-carbothioamide and its hydroxylated derivatives are promising molecules for further drug development studies.
- Published
- 2023
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37. Role of the Solvent in the Reactivity of Bis-4-imidazoline-2-selone Derivatives toward I 2 : An Experimental and Theoretical Approach.
- Author
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Aragoni MC, Arca M, Caltagirone C, Castellano C, Demartin F, Jones PG, Pivetta T, Podda E, Lippolis V, Murgia S, and Picci G
- Abstract
The reactivity of 1,1'-bis(3-methyl-4-imidazolin-2-selone)methane ( L1 ) and 1,2-bis(3-methyl-4-imidazolin-2-selone)ethane ( L2 ) toward I
2 has been explored in MeCN under different experimental conditions and compared with that in CH2 Cl2 . The compounds [ L1' ](I)2 ( I ), [ L1 I]n (I)n ( II ), [ L1 (μ-Se)](I)2 ·1/2H2 O ( III ), [ L1 I](I3 )·2I2 ( IV ), and [ L2 ](I)2 ·MeCN ( V ) were obtained and characterized. X-ray diffraction analyses point out an ionic nature for these compounds, which is presumably favored by the polarity of the solvent used. In particular, [ L1 I]n (I)n ( II ) represents the first example of an iodonium complex of imidazoline-2-selone derivatives, while [ L1 (μ-Se)](I)2 ·1/2H2 O ( III ) represents a unique example of a dicationic [RSeSeSeR] triselane. Density functional theory calculations have allowed us to better understand the nature of the obtained compounds and to justify their formations in polarizing reaction conditions rather than in low polar solvents.- Published
- 2022
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38. BSA fragmentation specifically induced by added electrolytes: An electrospray ionization mass spectrometry investigation.
- Author
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Lusci G, Pivetta T, Carucci C, Parsons DF, Salis A, and Monduzzi M
- Subjects
- Bromides, Chlorides, Electrolytes chemistry, Iodides, Peptides, Potassium, Salts, Sodium, Sodium Chloride, Thiocyanates, Serum Albumin, Bovine chemistry, Spectrometry, Mass, Electrospray Ionization methods
- Abstract
Biointerfaces are significantly affected by electrolytes according to the Hofmeister series. This work reports a systematic investigation on the effect of different metal chlorides, sodium and potassium bromides, iodides and thiocyanates, on the ESI/MS spectra of bovine serum albumin (BSA) in aqueous solution at pH = 2.7. The concentration of each salt was varied to maximize the quality of the ESI/MS spectrum, in terms of peak intensity and bell-shaped profile. The ESI/MS spectra of BSA in the absence and in the presence of salts showed a main protein pattern characterized by the expected mass of 66.5 kDa, except the case of BSA/RbCl (mass 65.3 kDa). In all systems we observed an additional pattern, characterized by at least three peaks with low intensity, whose deconvolution led to suggest the formation of a BSA fragment with a mass of 19.2 kDa. Only NaCl increased the intensity of the peaks of the main BSA pattern, while minimizing that of the fragment. NaCl addition seems to play a crucial role in stabilizing the BSA ionized interface against hydrolysis of peptide bonds, through different synergistic mechanisms. To quantify the observed specific electrolyte effects, two "Hofmeister" parameters (H
s and Ps ) are proposed. They are obtained using the ratio of (BSA-Salt)/BSA peak intensities for both the BSA main pattern and for its fragment. SYNOPSIS: NaCl stabilizes BSA ion and almost prevents fragmentation due to denaturing pH., Competing Interests: Declaration of Competing Interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper., (Copyright © 2022 Elsevier B.V. All rights reserved.)- Published
- 2022
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39. Specific electrolyte effects on hemoglobin in denaturing medium investigated through electro spray ionization mass spectrometry.
- Author
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Pivetta T, Lusci G, Carucci C, Parsons DF, Salis A, and Monduzzi M
- Subjects
- Cations, Chlorides, Hemoglobins, Metals, Myoglobin chemistry, Sodium chemistry, Sodium Chloride, Electrolytes, Spectrometry, Mass, Electrospray Ionization methods
- Abstract
We examine Hofmeister specific ion effects of electrolytes added to protein solution under conditions minimizing electrostatic attraction between cations and positively charged protein. Hemoglobin (Hb) in aqueous solution at the denaturing pH = 2.7 is investigated in the presence of several metal chlorides, along with sodium and potassium bromides, iodides and thiocyanates, using electrospray ionization mass spectrometry (ESI-MS). Salt concentration was varied to maximize peak intensity and bell-shaped profile in the ESI-MS spectrum. The α-chain of myoglobin is identified as the main pattern of the ESI-MS spectra in all Hb-salt systems. Both peak intensity and quality of the bell-shaped profile of the protein spectrum decrease in the cation order: K
+ > > Mg2+ > Li+ > > Na+ > Ca2+ ≈ Cs+ > Rb+ for Hb-Metal Chloride systems, and decrease in the anion order: Cl- > Br- > I- > SCN- for systems of both Hb-NaX and Hb-KX salts. To quantify salt addition effects two Hofmeister specific electrolyte parameters HS , and PS are proposed. HS is the mean (Hb-salt)/Hb peak intensity ratio, measured for the nine peaks used for ESI-MS spectra deconvolution, taken at the same m/z values of the Hb profile. PS is the ratio between HS standard deviation and HS , and provides a specific perturbation parameter measuring the loss of protein structure. These two Hofmeister parameters give clear evidence of the effects induced either by KCl, MgCl2 and LiCl that enhance protein peak intensity, or by NaBr, NaI, NaSCN and KSCN that induce the protein fragmentation, due to electrolyte-mediated dissociation., (Copyright © 2022 Elsevier Inc. All rights reserved.)- Published
- 2022
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40. An Exceptional Response to Dostarlimab in Mismatch Repair Deficient, Microsatellite Instability-High and Platinum Refractory Endometrial Cancer.
- Author
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Bartoletti M, Giorda G, Viel A, Fornasarig M, Zdjelar A, Segatto E, Sorio R, Corsetti S, Scalone S, Nicoloso MS, Pivetta T, Lucia E, Clemente N, Palazzari E, Canzonieri V, and Puglisi F
- Subjects
- Antibodies, Monoclonal, Humanized, Brain Neoplasms, Colorectal Neoplasms, DNA Mismatch Repair, Female, Humans, Immune Checkpoint Inhibitors, Microsatellite Instability, Platinum therapeutic use, Programmed Cell Death 1 Receptor, Endometrial Neoplasms drug therapy, Endometrial Neoplasms genetics, Neoplastic Syndromes, Hereditary
- Abstract
Until recently, effective therapies for advanced endometrial cancer progressing to a platinum-based combination were lacking. In this setting, immunotherapy with anti PD-1/PDL-1 monoclonal antibodies is rising as a new paradigm in particular for patients with microsatellites instability/mismatch repair deficiency. In this case report, we describe an exceptional and rapid response to dostarlimab in a platinum refractory endometrial cancer patient with high disease burden harboring a mismatch repair deficiency.
- Published
- 2022
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41. Copper(II) Phenanthroline-Based Complexes as Potential AntiCancer Drugs: A Walkthrough on the Mechanisms of Action.
- Author
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Masuri S, Vaňhara P, Cabiddu MG, Moráň L, Havel J, Cadoni E, and Pivetta T
- Subjects
- Antineoplastic Agents chemical synthesis, Cell Line, Tumor, Cell Survival, Chemistry Techniques, Synthetic, Coordination Complexes chemical synthesis, Dose-Response Relationship, Drug, Humans, Inhibitory Concentration 50, Ligands, Molecular Structure, Antineoplastic Agents chemistry, Antineoplastic Agents pharmacology, Coordination Complexes chemistry, Copper chemistry, Phenanthrolines chemistry
- Abstract
Copper is an endogenous metal ion that has been studied to prepare a new antitumoral agent with less side-effects. Copper is involved as a cofactor in several enzymes, in ROS production, in the promotion of tumor progression, metastasis, and angiogenesis, and has been found at high levels in serum and tissues of several types of human cancers. Under these circumstances, two strategies are commonly followed in the development of novel anticancer Copper-based drugs: the sequestration of free Copper ions and the synthesis of Copper complexes that trigger cell death. The latter strategy has been followed in the last 40 years and many reviews have covered the anticancer properties of a broad spectrum of Copper complexes, showing that the activity of these compounds is often multi factored. In this work, we would like to focus on the anticancer properties of mixed Cu(II) complexes bearing substituted or unsubstituted 1,10-phenanthroline based ligands and different classes of inorganic and organic auxiliary ligands. For each metal complex, information regarding the tested cell lines and the mechanistic studies will be reported and discussed. The exerted action mechanisms were presented according to the auxiliary ligand/s, the metallic centers, and the increasing complexity of the compound structures.
- Published
- 2021
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42. The first copper(ii) complex with 1,10-phenanthroline and salubrinal with interesting biochemical properties.
- Author
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Masuri S, Cadoni E, Cabiddu MG, Isaia F, Demuru MG, Moráň L, Buček D, Vaňhara P, Havel J, and Pivetta T
- Subjects
- Antiviral Agents pharmacology, Cell Line, Tumor, Cell Survival drug effects, DNA Damage drug effects, DNA Damage genetics, Humans, Lipid Peroxidation drug effects, Magnetic Resonance Spectroscopy, Microscopy, Electron, Transmission, Molecular Structure, Taurochenodeoxycholic Acid pharmacology, Thiourea pharmacology, Transcription Factor CHOP genetics, Transcription Factor CHOP metabolism, Cinnamates pharmacology, Copper pharmacology, Phenanthrolines pharmacology, Thiourea analogs & derivatives
- Abstract
The novel copper complex [Cu(phen)2(salubrinal)](ClO4)2 (C0SAL) has been synthesised and characterised. Copper(ii) is coordinated by salubrinal through the thionic group, as shown by the UV-Vis, IR, ESI-MS and tandem mass results, together with the theoretical calculations. The formed complex showed a DPPH radical scavenging ability higher than that of salubrinal alone. Studies on lipid oxidation inhibition showed that the C0SAL concentration, required to inhibit the enzyme, was lower than that of salubrinal. The inhibition of the enzyme could take place via allosteric modulation, as suggested by docking calculations. C0SAL showed a good cytotoxic activity on A2780 cells, 82 fold higher than that of the precursor salubrinal and 1.4 fold higher than that of [Cu(phen)2(H2O)](ClO4)2. Treatment with C0SAL in SKOV3 ovarian cancer cells induced expression of GRP-78 and DDIT3 regulators of ER-stress response. The cytotoxic effect of C0SAL was reverted in the presence of TUDCA, suggesting that C0SAL induces cell death through ER-stress. In A2780 cells treated with C0SAL γ-H2AX was accumulated, suggesting that DNA damage was also involved.
- Published
- 2020
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43. Correction to: Synthesis, protonation constants and biological activity determination of amino acid-salicylaldehyde‑derived Schiff bases.
- Author
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Fattuoni C, Vascellari S, and Pivetta T
- Abstract
Unfortunately in the online published article, the name of compound "L-salicylidenealanine" was published with incorrect spelling in the section "Synthesis of L‑salicylideneaniline (1a)". The section should correctly read as "Synthesis of L-salicylidenealanine".
- Published
- 2020
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44. Synthesis, protonation constants and biological activity determination of amino acid-salicylaldehyde-derived Schiff bases.
- Author
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Fattuoni C, Vascellari S, and Pivetta T
- Subjects
- Cell Line, Tumor, Humans, Hydrogenation, Inhibitory Concentration 50, Magnetic Resonance Spectroscopy, Spectrophotometry, Infrared, Aldehydes chemistry, Amino Acids chemical synthesis, Antineoplastic Agents chemical synthesis, Antineoplastic Agents pharmacology, Schiff Bases chemical synthesis, Schiff Bases pharmacology
- Abstract
Schiff bases represent a class of molecules widely studied for their importance in organic and coordination chemistry. Despite the large amount of studies on the chemical and biological properties of the Schiff bases, the different experimental conditions prevent a useful comparison to search for a correlation structure-activity. Moreover, literature is lacking in comprehensive data on the spectroscopic characterization of these compounds. For this reason, six Schiff bases, derived from salicylaldehyde and natural amino acids were fully characterized by nuclear magnetic resonance and infrared spectroscopy, and their aqueous solution equilibria, antiproliferative activity and DNA-binding activity were examined. All experimental conditions were kept constants to achieve comparable information and useful insights about their structure-activity correlation. The synthesized compounds showed DNA binding constants in the 10
1 -102 M-1 range, depending on the substituent present in the amino acid side-chain, and resulted devoid of significant cytotoxic activity against the different human tumor cell lines showing IC50 values higher than 100 µM.- Published
- 2020
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45. Mixed copper(ii)-phenanthroline complexes induce cell death of ovarian cancer cells by evoking the unfolded protein response.
- Author
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Moráň L, Pivetta T, Masuri S, Vašíčková K, Walter F, Prehn J, Elkalaf M, Trnka J, Havel J, and Vaňhara P
- Subjects
- Antineoplastic Agents chemistry, Cell Line, Tumor, Coordination Complexes chemistry, Coordination Complexes pharmacology, Copper chemistry, Female, Humans, Ovarian Neoplasms metabolism, Phenanthrolines chemistry, Antineoplastic Agents pharmacology, Copper pharmacology, Ovarian Neoplasms drug therapy, Phenanthrolines pharmacology, Unfolded Protein Response drug effects
- Abstract
There is an ongoing need for the development of new cancer therapeutics that combine high cytotoxic efficiency with low side effects, and also override resistance to the first-line chemotherapeutics. Copper(ii)-phenanthroline complexes are promising compounds that were shown previously to induce an immediate cytotoxic response over a panel of tumor cell lines in vitro. The molecular mechanism, however, remained unresolved. In this work we performed a thorough study of the copper(ii)-phenanthroline complexes containing different imidazolidine-2-thione ligands in ovarian cancer cells, and revealed that these complexes induce endoplasmic reticulum (ER) stress and subsequently cell death mediated by the unfolded protein response. Alleviation of the ER-stress by tauroursodeoxycholic acid (TUDCA) attenuated the cytotoxic effects. In summary, we have identified a novel, ER-dependent, molecular mechanism mediating cytotoxic effects of copper(ii)-phenanthroline complexes.
- Published
- 2019
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46. Terrain uplift due to natural hydrologic overpressure in karstic conduits.
- Author
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Braitenberg C, Pivetta T, Barbolla DF, Gabrovšek F, Devoti R, and Nagy I
- Abstract
Water supply from karst sources is a worldwide natural resource and the exploitation is tied to the knowledge of the positions of the hydrologic channels. We show that surface deformation induced by flood events in karst conduits is observable, and consists in uplift and outward movement from the hydraulic channel. Precipitation events produce the natural occurrence of subsurface hydraulic overpressure up to 1 MPa. Numerical modeling shows that the stresses are so strong to uplift and dislocate the surface by several mm and induce tilts in the order of microradians. The naturally induced deformation is compatible with a transient internal pressure loading of a channel. The results can be used to find new channels with dense GNSS networks. Sea water incursion and channels accessed for tourism could be monitored. Seismicity has been shown to have a seasonal variation in some areas, which could be explained by the subsurface stresses induced by the natural subsurface overpressure. The pressure induced deformation is expected to be observed in all karstic systems worldwide.
- Published
- 2019
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47. Cisplatin, glutathione and the third wheel: a copper-(1,10-phenanthroline) complex modulates cisplatin-GSH interactions from antagonism to synergism in cancer cells resistant to cisplatin.
- Author
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Vascellari S, Valletta E, Perra D, Pinna E, Serra A, Isaia F, Pani A, and Pivetta T
- Abstract
The antagonistic effect of glutathione (GSH) against the cytotoxicity of cisplatin was observed in both wild type and cisplatin-resistant human leukaemia and ovarian carcinoma cell lines. The simultaneous presence of the cytotoxic copper complex [Cu(phen)
2 (OH2 )](ClO4 )2 (C0) restored the sensitivity of the cells to cisplatin, and, at selected concentrations, led to strong synergistic effects. The C0-cisplatin-glutathione system showed a synergistic toxic effect even in the presence of 1000 μM GSH. The three-drug cocktail exerted a higher potency against leukemic cells than against freshly isolated lymphocytes from healthy donors. Compared to actively proliferating normal lymphocytes, leukaemia cells were much more susceptible to the cytocide effect of the three-drug combination and underwent the dying process(es) much faster. When the ovarian carcinoma cells were treated with cisplatin, alone or in combination with C0, late apoptotic effects were mainly observed, suggesting that DNA interactions with the C0-cisplatin complex trigger a process of programmed cell death. In contrast, the ternary combination induced apoptotic effects similar to that shown by C0 in single treatment, that is, early apoptosis. One possible explanation is that C0 and cisplatin compete for GSH-binding in the culture medium. GSH in combination with C0 and cisplatin caused a significant induction of the apoptotic process(es), through a pathway which does not compromise the integrity of the plasma membrane of cells., Competing Interests: There are no conflicts of interest to declare., (This journal is © The Royal Society of Chemistry.)- Published
- 2019
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48. Mass spectrometric discrimination of phospholipid patterns in cisplatin-resistant and -sensitive cancer cells.
- Author
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Cadoni E, Vanhara P, Valletta E, Pinna E, Vascellari S, Caddeo G, Isaia F, Pani A, Havel J, and Pivetta T
- Subjects
- Antineoplastic Agents pharmacology, Cell Line, Tumor, Female, Humans, Ovarian Neoplasms chemistry, Ovarian Neoplasms drug therapy, Ovarian Neoplasms pathology, Phospholipids chemistry, Precursor T-Cell Lymphoblastic Leukemia-Lymphoma drug therapy, Precursor T-Cell Lymphoblastic Leukemia-Lymphoma pathology, Solid Phase Extraction, Spectrometry, Mass, Electrospray Ionization, Tandem Mass Spectrometry, Cisplatin pharmacology, Drug Resistance, Neoplasm, Phospholipids analysis
- Abstract
Rationale: Development of therapy-resistant cancer is a major problem in clinical oncology, and there is an urgent need for novel markers identifying development of the resistant phenotype. Lipidomics represents a promising approach to discriminate lipid profiles of malignant phenotype cells. Alterations in phospholipid distribution or chemical composition have been reported in various pathologies including cancer. Here we were curious whether quantitative differences in phospholipid composition between cisplatin-resistant and -sensitive model cancer cell lines could be revealed by mass spectrometric means., Methods: The phospholipid contents of cell membranes of the cancer cell lines CCRF-CEM and A2780, both responsive and resistant to cisplatin, were analyzed by solid-phase extraction (SPE) and electrospray ionization mass spectrometry (ESI-MS and tandem mass spectrometry (MS/MS)). Extracts were obtained by disruption of cells with a dounce tissue grinder set followed by centrifugation. To minimize the enzymatic activity, phospholipids were extracted from cell extracts by SPE immediately after the cell lysis and analyzed by MS. Both supernatant and pellet fractions of cell extracts were analyzed., Results: A phospholipid profile specific for cell lines and their phenotypes was revealed. We have documented by quantitative analysis that phosphocholines PC P-34:0, PC 34:1, PC 20:2_16:0, LPC 18:1 and LPC 16:0 PLs were present in the 200-400 μM concentration range in CCRF-CEM cisplatin-responsive cells, but absent in their cisplatin-resistant cells. Similarly, PC 34:1, LPC 18:1 and LPC 16:0 were increased in cisplatin-responsive A2780 cells, and PC 20:2_16:0 was downregulated in cisplatin-resistant A2780 cells., Conclusions: In this work we showed that the ESI-MS analysis of the lipid content of the therapy-resistant and -sensitive cells can clearly distinguish the phenotypic pattern and determine the potential tumor response to cytotoxic therapy. Lipid entities revealed by mass spectrometry and associated with development of therapy resistance can thus support molecular diagnosis and provide a potential complementary cancer biomarker., (© 2018 John Wiley & Sons, Ltd.)
- Published
- 2019
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49. Novel coumarins and related copper complexes with biological activity: DNA binding, molecular docking and in vitro antiproliferative activity.
- Author
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Pivetta T, Valletta E, Ferino G, Isaia F, Pani A, Vascellari S, Castellano C, Demartin F, Cabiddu MG, and Cadoni E
- Subjects
- Antineoplastic Agents chemical synthesis, Antineoplastic Agents chemistry, Antineoplastic Agents toxicity, Cell Line, Tumor, Coordination Complexes chemical synthesis, Coordination Complexes chemistry, Coordination Complexes toxicity, Coumarins chemical synthesis, Coumarins chemistry, Coumarins toxicity, Humans, Ligands, Molecular Docking Simulation, Quantitative Structure-Activity Relationship, Antineoplastic Agents pharmacology, Coordination Complexes pharmacology, Copper chemistry, Coumarins pharmacology, DNA chemistry
- Abstract
Coumarins show biological activity and are widely exploited for their therapeutic effects. Although a great number of coumarins substituted by heterocyclic moieties have been prepared, few studies have been carried out on coumarins containing pyridine heterocycle, which is known to modulate their physiological activities. We prepared and characterized three novel 3-(pyridin-2-yl)coumarins and their corresponding copper(II) complexes. We extended our investigations also to three known similar coumarins, since no data about their biochemical activity was previously been reported. The antiproliferative activity of the studied compounds was tested against human derived tumor cell lines and one human normal cell line. The DNA binding constants were determined and docking studies with DNA carried out. Selected Quantitative Structure-Activity Relationship (QSAR) descriptors were calculated in order to relate a set of structural and topological descriptors of the studied compounds to their DNA interaction and cytotoxic activity., (Copyright © 2017 Elsevier Inc. All rights reserved.)
- Published
- 2017
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50. Advances in systemic therapy for malignant mesothelioma: future perspectives.
- Author
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Sobhani N, Corona SP, Bonazza D, Ianza A, Pivetta T, Roviello G, Cortale M, Guglielmi A, Zanconati F, and Generali D
- Subjects
- Antineoplastic Combined Chemotherapy Protocols adverse effects, Antineoplastic Combined Chemotherapy Protocols therapeutic use, Clinical Trials as Topic, Combined Modality Therapy, Humans, Immunotherapy, Lung Neoplasms mortality, Lung Neoplasms pathology, Mesothelioma mortality, Mesothelioma pathology, Mesothelioma, Malignant, Molecular Targeted Therapy, Treatment Outcome, Lung Neoplasms therapy, Mesothelioma therapy
- Abstract
Malignant mesothelioma is a rare and aggressive form of cancer affecting the mesothelium. This mainly occupational disease is becoming more common in those countries where asbestos has been used for industrial applications. Notwithstanding the progress made in the field, patients do not survive more than 12 months on average with standard treatment. With the advent of next generation sequencing, it is now possible to study the mutational landscape of each tumor with the aim of identifying the genetic aberrations driving tumorigenesis. This review encompasses the latest research in the field, with particular attention to new chemotherapy combinatorial regimens, molecular targets and immunotherapies, providing a comprehensive picture of the current and future treatment options for malignant mesothelioma patients.
- Published
- 2017
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