6,320 results on '"Crosta A"'
Search Results
152. Integrating Kinematic Analysis and Infrared Thermography for Instability Processes Assessment in the Rupestrian Monastery Complex of David Gareja (Georgia)
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Frodella, William, Spizzichino, Daniele, Gigli, Giovanni, Elashvili, Mikheil, Margottini, Claudio, Villa, Alberto, Frattini, Paolo, Crosta, Giovanni, Casagli, Nicola, Sassa, Kyoji, Series Editor, Mikoš, Matjaž, editor, Sassa, Shinji, editor, Bobrowsky, Peter T., editor, Takara, Kaoru, editor, and Dang, Khang, editor
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- 2021
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153. Discrete Element Modeling of Compound Rockfall Fence Nets
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Previtali, Marco, Ciantia, Matteo Oryem, Spadea, Saverio, Castellanza, Riccardo, Crosta, Giovanni, di Prisco, Marco, Series Editor, Chen, Sheng-Hong, Series Editor, Vayas, Ioannis, Series Editor, Kumar Shukla, Sanjay, Series Editor, Sharma, Anuj, Series Editor, Kumar, Nagesh, Series Editor, Wang, Chien Ming, Series Editor, Barla, Marco, editor, Di Donna, Alice, editor, and Sterpi, Donatella, editor
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- 2021
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154. How does the Southern Ocean palaeoenvironment during Marine Isotope Stage 5e compare to the modern?
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Chadwick, M., Allen, C.S., Sime, L.C., Crosta, X., and Hillenbrand, C.-D.
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- 2022
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155. Sea ice changes in the southwest Pacific sector of the Southern Ocean during the last 140 000 years
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J. Jones, K. E. Kohfeld, H. Bostock, X. Crosta, M. Liston, G. Dunbar, Z. Chase, A. Leventer, H. Anderson, and G. Jacobsen
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Environmental pollution ,TD172-193.5 ,Environmental protection ,TD169-171.8 ,Environmental sciences ,GE1-350 - Abstract
Sea ice expansion in the Southern Ocean is believed to have contributed to glacial–interglacial atmospheric CO2 variability by inhibiting air–sea gas exchange and influencing the ocean's meridional overturning circulation. However, limited data on past sea ice coverage over the last 140 ka (a complete glacial cycle) have hindered our ability to link sea ice expansion to oceanic processes that affect atmospheric CO2 concentration. Assessments of past sea ice coverage using diatom assemblages have primarily focused on the Last Glacial Maximum (∼21 ka) to Holocene, with few quantitative reconstructions extending to the onset of glacial Termination II (∼135 ka). Here we provide new estimates of winter sea ice concentrations (WSIC) and summer sea surface temperatures (SSST) for a full glacial–interglacial cycle from the southwestern Pacific sector of the Southern Ocean using the modern analog technique (MAT) on fossil diatom assemblages from deep-sea core TAN1302-96. We examine how the timing of changes in sea ice coverage relates to ocean circulation changes and previously proposed mechanisms of early glacial CO2 drawdown. We then place SSST estimates within the context of regional SSST records to better understand how these surface temperature changes may be influencing oceanic CO2 uptake. We find that winter sea ice was absent over the core site during the early glacial period until MIS 4 (∼65 ka), suggesting that sea ice may not have been a major contributor to early glacial CO2 drawdown. Sea ice expansion throughout the glacial–interglacial cycle, however, appears to coincide with observed regional reductions in Antarctic Intermediate Water production and subduction, suggesting that sea ice may have influenced intermediate ocean circulation changes. We observe an early glacial (MIS 5d) weakening of meridional SST gradients between 42 and 59∘ S throughout the region, which may have contributed to early reductions in atmospheric CO2 concentrations through its impact on air–sea gas exchange.
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- 2022
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156. Reconstructing Antarctic winter sea-ice extent during Marine Isotope Stage 5e
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M. Chadwick, C. S. Allen, L. C. Sime, X. Crosta, and C.-D. Hillenbrand
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Environmental pollution ,TD172-193.5 ,Environmental protection ,TD169-171.8 ,Environmental sciences ,GE1-350 - Abstract
Environmental conditions during Marine Isotope Stage (MIS) 5e (130–116 ka) represent an important “process analogue” for understanding the climatic responses to present and future anthropogenic warming. The response of Antarctic sea ice to global warming is particularly uncertain due to the short length of the observational record. Reconstructing Antarctic winter sea-ice extent during MIS 5e therefore provides insights into the temporal and spatial patterns of sea-ice change under a warmer-than-present climate. This study presents new MIS 5e records from nine marine sediment cores located south of the Antarctic Polar Front between 55 and 70∘ S. Winter sea-ice extent and sea-surface temperatures are reconstructed using marine diatom assemblages and a modern analogue technique transfer function, and changes in these environmental variables between the three Southern Ocean sectors are investigated. The Atlantic and East Indian sector records show much more variable MIS 5e winter sea-ice extent and sea-surface temperatures than the Pacific sector records. High variability in the Atlantic sector winter sea-ice extent is attributed to high glacial meltwater flux in the Weddell Sea, indicated by increased abundances of the diatom species Eucampia antarctica and Fragilariopsis cylindrus. The high variability in the East Indian sector winter sea-ice extent is conversely believed to result from large latitudinal migrations of the flow bands of the Antarctic Circumpolar Current, inferred from latitudinal shifts in the sea-surface temperature isotherms. Overall, these findings suggest that Pacific sector winter sea ice displays a low sensitivity to warmer climates. The different variability and sensitivity of Antarctic winter sea-ice extent in the three Southern Ocean sectors during MIS 5e may have significant implications for the Southern Hemisphere climatic system under future warming.
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- 2022
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157. Triggering and recovery of earthquake accelerated landslides in Central Italy revealed by satellite radar observations
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Song, Chuang, Yu, Chen, Li, Zhenhong, Utili, Stefano, Frattini, Paolo, Crosta, Giovanni, and Peng, Jianbing
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- 2022
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158. Coat Color Genetics
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Crosta, Maria Cristina, Noli, Chiara, editor, and Colombo, Silvia, editor
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- 2020
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159. The Southern Ocean Radiolarian (SO-RAD) dataset: a new compilation of modern radiolarian census data
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K.-A. Lawler, G. Cortese, M. Civel-Mazens, H. Bostock, X. Crosta, A. Leventer, V. Lowe, J. Rogers, and L. K. Armand
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Environmental sciences ,GE1-350 ,Geology ,QE1-996.5 - Abstract
Radiolarians (holoplanktonic protozoa) preserved in marine sediments are commonly used as palaeoclimate proxies for reconstructing past Southern Ocean environments. Generating reconstructions of past climate based on microfossil abundances, such as radiolarians, requires a spatially and environmentally comprehensive reference dataset of modern census counts. The Southern Ocean Radiolarian (SO-RAD) dataset includes census counts for 238 radiolarian taxa from 228 surface sediment samples located in the Atlantic, Indian, and southwest Pacific sectors of the Southern Ocean. This compilation is the largest radiolarian census dataset derived from surface sediment samples in the Southern Ocean. The SO-RAD dataset may be used as a reference dataset for palaeoceanographic reconstructions, or for studying modern radiolarian biogeography and species diversity. As well as describing the data collection and collation, we include recommendations and guidelines for cleaning and subsetting the data for users unfamiliar with the procedures typically used by the radiolarian community. The SO-RAD dataset is available to download from https://doi.org/10.1594/PANGAEA.929903 (Lawler et al., 2021).
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- 2021
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160. Exploring the use of compound-specific carbon isotopes as a palaeoproductivity proxy off the coast of Adélie Land, East Antarctica
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K. E. Ashley, X. Crosta, J. Etourneau, P. Campagne, H. Gilchrist, U. Ibraheem, S. E. Greene, S. Schmidt, Y. Eley, G. Massé, and J. Bendle
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Ecology ,QH540-549.5 ,Life ,QH501-531 ,Geology ,QE1-996.5 - Abstract
The Antarctic coastal zone is an area of high primary productivity, particularly within coastal polynyas, where large phytoplankton blooms and drawdown of CO2 occur. Reconstruction of historical primary productivity changes and the associated driving factors could provide baseline insights on the role of these areas as sinks for atmospheric CO2, especially in the context of projected changes in coastal Antarctic sea ice. Here we investigate the potential for using carbon isotopes (δ13C) of fatty acids in marine sediments as a proxy for primary productivity. We use a highly resolved sediment core from off the coast of Adélie Land spanning the last ∼ 400 years and monitor changes in the concentrations and δ13C of fatty acids along with other proxy data from the same core. We discuss the different possible drivers of their variability and argue that C24 fatty acid δ13C predominantly reflects phytoplankton productivity in open-water environments, while C18 fatty acid δ13C reflects productivity in the marginal ice zone. These new proxies have implications for better understanding carbon cycle dynamics in the Antarctica coastal zone in future palaeoclimate studies.
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- 2021
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161. Updating the Chieti Affective Action Videos database with older adults
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Pasquale La Malva, Irene Ceccato, Adolfo Di Crosta, Anna Marin, Mirco Fasolo, Riccardo Palumbo, Nicola Mammarella, Rocco Palumbo, and Alberto Di Domenico
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Science - Abstract
Measurement(s) emotion - valence & arousal Technology Type(s) Self-Assessment Manikin scale (SAM) Factor Type(s) emotional video stimuli • age group Sample Characteristic - Organism Homo sapiens Machine-accessible metadata file describing the reported data: https://doi.org/10.6084/m9.figshare.14992173
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- 2021
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162. Modeling the formation of Menrva impact crater on Titan: Implications for habitability
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Crósta, A.P., Silber, E.A., Lopes, R.M.C., Johnson, B.C., Bjonnes, E., Malaska, M.J., Vance, S.D., Sotin, C., Solomonidou, A., and Soderblom, J.M.
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- 2021
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163. Relationship between the spatial distribution of landslides and rock mass strength, and implications for the driving mechanism of landslides in tectonically active mountain ranges
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Wang, Xueliang, Clague, John J., Crosta, Giovanni Battista, Sun, Juanjuan, Stead, Douglas, Qi, Shengwen, and Zhang, Luqing
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- 2021
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164. Characterization of the subsurface urban heat island and its sources in the Milan city area, Italy
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Previati, Alberto and Crosta, Giovanni B.
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- 2021
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165. Sensitivity of Holocene East Antarctic productivity to subdecadal variability set by sea ice
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Johnson, Katelyn M., McKay, Robert M., Etourneau, Johan, Jiménez-Espejo, Francisco J., Albot, Anya, Riesselman, Christina R., Bertler, Nancy A. N., Horgan, Huw J., Crosta, Xavier, Bendle, James, Ashley, Kate E., Yamane, Masako, Yokoyama, Yusuke, Pekar, Stephen F., Escutia, Carlota, and Dunbar, Robert B.
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- 2021
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166. Gaia Data Release 1: Astrometry - one billion positions, two million proper motions and parallaxes
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Lindegren, L., Lammers, U., Bastian, U., Hernández, J., Klioner, S., Hobbs, D., Bombrun, A., Michalik, D., Ramos-Lerate, M., Butkevich, A., Comoretto, G., Joliet, E., Holl, B., Hutton, A., Parsons, P., Steidelmüller, H., Abbas, U., Altmann, M., Andrei, A., Anton, S., Bach, N., Barache, C., Becciani, U., Berthier, J., Bianchi, L., Biermann, M., Bouquillon, S., Bourda, G., Brüsemeister, T., Bucciarelli, B., Busonero, D., Carlucci, T., Castañeda, J., Charlot, P., Clotet, M., Crosta, M., Davidson, M., de Felice, F., Drimmel, R., Fabricius, C., Fienga, A., Figueras, F., Fraile, E., Gai, M., Garralda, N., Geyer, R., González-Vidal, J. J., Guerra, R., Hambly, N. C., Hauser, M., Jordan, S., Lattanzi, M. G., Lenhardt, H., Liao, S., Löffler, W., McMillan, P. J., Mignard, F., Mora, A., Morbidelli, R., Portell, J., Riva, A., Sarasso, M., Serraller, I., Siddiqui, H., Smart, R., Spagna, A., Stampa, U., Steele, I., Taris, F., Torra, J., van Reeven, W., Vecchiato, A., Zschocke, S., de Bruijne, J., Gracia, G., Raison, F., Lister, T., Marchant, J., Messineo, R., Soffel, M., Osorio, J., de Torres, A., and O'Mullane, W.
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Astrophysics - Astrophysics of Galaxies ,Astrophysics - Instrumentation and Methods for Astrophysics - Abstract
Gaia Data Release 1 (Gaia DR1) contains astrometric results for more than 1 billion stars brighter than magnitude 20.7 based on observations collected by the Gaia satellite during the first 14 months of its operational phase. We give a brief overview of the astrometric content of the data release and of the model assumptions, data processing, and validation of the results. For stars in common with the Hipparcos and Tycho-2 catalogues, complete astrometric single-star solutions are obtained by incorporating positional information from the earlier catalogues. For other stars only their positions are obtained by neglecting their proper motions and parallaxes. The results are validated by an analysis of the residuals, through special validation runs, and by comparison with external data. Results. For about two million of the brighter stars (down to magnitude ~11.5) we obtain positions, parallaxes, and proper motions to Hipparcos-type precision or better. For these stars, systematic errors depending e.g. on position and colour are at a level of 0.3 milliarcsecond (mas). For the remaining stars we obtain positions at epoch J2015.0 accurate to ~10 mas. Positions and proper motions are given in a reference frame that is aligned with the International Celestial Reference Frame (ICRF) to better than 0.1 mas at epoch J2015.0, and non-rotating with respect to ICRF to within 0.03 mas/yr. The Hipparcos reference frame is found to rotate with respect to the Gaia DR1 frame at a rate of 0.24 mas/yr. Based on less than a quarter of the nominal mission length and on very provisional and incomplete calibrations, the quality and completeness of the astrometric data in Gaia DR1 are far from what is expected for the final mission products. The results nevertheless represent a huge improvement in the available fundamental stellar data and practical definition of the optical reference frame., Comment: Accepted for publication in Astronomy & Astrophysics
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- 2016
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167. Fault controls on spatial variation of fracture density and rock mass strength within the Yarlung Tsangpo Fault damage zone (southeastern Tibet)
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Wang, Xueliang, Crosta, Giovanni Battista, Clague, John J., Stead, Douglas, Sun, Juanjuan, Qi, Shengwen, and Liu, Haiyang
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- 2021
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168. Reproduction Management of Herds/Flocks of Exotic Animals: Investigating Breeding Failures in Birds, Reptiles, and Small Mammals
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Crosta, Lorenzo, Petrini, Daniele, and Sawmy, Shivananden
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- 2021
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169. Production-induced instability of a gentle submarine slope: Potential impact of gas hydrate exploitation with the huff-puff method
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Tan, Lin, Liu, Fang, Huang, Yu, Crosta, Giovanni, Frattini, Paolo, and Cen, Xueqi
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- 2021
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170. Antarctic Polar Front migrations in the Kerguelen Plateau region, Southern Ocean, over the past 360 kyrs
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Civel-Mazens, M., Crosta, X., Cortese, G., Michel, E., Mazaud, A., Ther, O., Ikehara, M., and Itaki, T.
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- 2021
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171. Changing Decisions: The Interaction between Framing and Decoy Effects
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Adolfo Di Crosta, Anna Marin, Rocco Palumbo, Irene Ceccato, Pasquale La Malva, Matteo Gatti, Giulia Prete, Riccardo Palumbo, Nicola Mammarella, and Alberto Di Domenico
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cognitive bias ,framing effect ,decoy effect ,congruent decoy ,incongruent decoy ,decision making ,Psychology ,BF1-990 - Abstract
Background: Cognitive biases are popular topics in psychology and marketing, as they refer to systematic cognitive tendencies in human thinking that deviate from logical and rational reasoning. The framing effect (FE) and the decoy effect (DE) are examples of cognitive biases that can influence decision making and consumer preferences. The FE involves how options are presented, while the DE involves the addition of a third option that influences the choice between the other two options. Methods: We investigated the interaction between the FE and the DE in the case of both incongruent (ID) and congruent (CD) decoys in a sample of undergraduates (n = 471). The study had a two (positive vs. negative valence) × three (original, congruent decoy, incongruent decoy) within-subject design. Results: The ID option reduces the FE in both positive- and negative-framed conditions compared to the controls, while adding the CD option increases the FE only in the positive-framed condition. Additionally, the inclusion of the CD option enhances the level of decision confidence, whereas no significant differences were found in the ID condition. Conclusions: Our findings gave new insights into the interplay between two of the most frequent cognitive biases.
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- 2023
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172. Contributors
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Bovenga, F., primary, Bowman, E.T., additional, Brideau, Marc-André, additional, Clague, John J., additional, Crosta, Giovanni B., additional, Davies, Tim, additional, Delcamp, Audray, additional, Deline, P., additional, Hewitt, K., additional, Jakob, Matthias, additional, Korup, Oliver, additional, Massey, Chris, additional, McColl, Samuel T., additional, Moretti, Danilo, additional, Murphy, Bill, additional, Reznichenko, N., additional, Roberts, Nicholas J., additional, Rosser, Nick, additional, Shugar, D., additional, Sosio, Rosanna, additional, Utili, Stefano, additional, van Wyk de Vries, Benjamin, additional, Wang, Gonghui, additional, Warburton, Jeff, additional, and Wasowski, J., additional
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- 2022
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173. Retinal Microvasculature in Schizophrenia
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Silverstein SM, Lai A, Green KM, Crosta C, Fradkin SI, and Ramchandran RS
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schizophrenia ,retina ,oct angiography (octa) ,venule ,arteriole ,Ophthalmology ,RE1-994 ,Neurology. Diseases of the nervous system ,RC346-429 - Abstract
Steven M Silverstein,1– 4 Adriann Lai,1 Kyle M Green,3 Christen Crosta,5 Samantha I Fradkin,6 Rajeev S Ramchandran3,7 1Department of Psychiatry, University of Rochester Medical Center, Rochester, NY, USA; 2Department of Neuroscience, University of Rochester Medical Center, Rochester, NY, USA; 3Department of Ophthalmology, University of Rochester Medical Center, Rochester, NY, USA; 4Center for Visual Science, University of Rochester, Rochester, NY, USA; 5Department of Cell Biology and Neuroscience, Rutgers University, Piscataway, NJ, USA; 6Department of Psychology, University of Rochester, Rochester, NY, USA; 7Department of Public Health Sciences, University of Rochester Medical Center, Rochester, NY, USACorrespondence: Steven M SilversteinDepartment of Psychiatry, University of Rochester Medical Center, 300 Crittenden Boulevard, Rochester, NY, 14642, USATel +1 585 275-6742Fax +1 585 276-2094Email steven_silverstein@urmc.rochester.eduPurpose: Schizophrenia is associated with alterations in neural structure and function of the retina that are similar to changes seen in the retina and brain in multiple neurodegenerative disorders. Preliminary evidence suggests that retinal microvasculature may also be compromised in schizophrenia. The goal of this study was to determine, using optical coherence tomography angiography (OCTA), whether 1) schizophrenia is associated with alterations in retinal microvasculature density; and 2) microvasculature reductions are associated with retinal neural layer thinning and performance on a measure of verbal IQ.Patients and Methods: Twenty-eight outpatients with schizophrenia or schizoaffective disorder and 37 psychiatrically healthy control subjects completed OCT and OCTA exams, and the Wechsler Test of Adult Reading.Results: Schizophrenia patients were characterized by retinal microvasculature density reductions, and enlarged foveal avascular zones, in both eyes. These microvascular abnormalities were generally associated with thinning of retinal neural (macular and peripapillary nerve fiber layer) tissue (but the data were stronger for the left than the right eye) and lower scores on a proxy measure of verbal IQ. First- and later-episode patients did not differ significantly on OCTA findings.Conclusion: The retinal microvasculature impairments seen in schizophrenia appear to be a biomarker of overall brain health, as is the case for multiple neurological conditions. Additional research is needed, however, to clarify contributions of social disadvantage and medical comorbidities to the findings.Keywords: schizophrenia, retina, OCT angiography, OCTA, venule, arteriole
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- 2021
174. Vulnerability of the North Water ecosystem to climate change
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Sofia Ribeiro, Audrey Limoges, Guillaume Massé, Kasper L. Johansen, William Colgan, Kaarina Weckström, Rebecca Jackson, Eleanor Georgiadis, Naja Mikkelsen, Antoon Kuijpers, Jesper Olsen, Steffen M. Olsen, Martin Nissen, Thorbjørn J. Andersen, Astrid Strunk, Sebastian Wetterich, Jari Syväranta, Andrew C. G. Henderson, Helen Mackay, Sami Taipale, Erik Jeppesen, Nicolaj K. Larsen, Xavier Crosta, Jacques Giraudeau, Simone Wengrat, Mark Nuttall, Bjarne Grønnow, Anders Mosbech, and Thomas A. Davidson
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Science - Abstract
The North Water polynya is a unique but vulnerable ecosystem, home to Indigenous people and Arctic keystone species. New palaeoecological records from Greenland suggest human abandonment c. 2200–1200 cal yrs BP occurred during climate-forced polynya instability, foreshadowing future ecosystem declines.
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- 2021
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175. “What's next?” Individual differences in expected repercussions of the COVID-19 pandemic
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Ceccato, Irene, Palumbo, Rocco, Di Crosta, Adolfo, Marchetti, Daniela, La Malva, Pasquale, Maiella, Roberta, Marin, Anna, Mammarella, Nicola, Verrocchio, Maria Cristina, and Di Domenico, Alberto
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- 2021
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176. Respiratory Diseases of Parrots: Anatomy, Physiology, Diagnosis and Treatment
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Crosta, Lorenzo
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- 2021
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177. Cost-sensitive rainfall thresholds for shallow landslides
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Sala, Gianluca, Lanfranconi, Camilla, Frattini, Paolo, Rusconi, Giulia, and Crosta, Giovanni B.
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- 2021
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178. Semi-automated regional classification of the style of activity of slow rock-slope deformations using PS InSAR and SqueeSAR velocity data
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Crippa, Chiara, Valbuzzi, Elena, Frattini, Paolo, Crosta, Giovanni B., Spreafico, Margherita C., and Agliardi, Federico
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- 2021
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179. Regional-scale assessment of the thermal potential in a shallow alluvial aquifer system in the Po plain (northern Italy)
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Previati, Alberto and Crosta, Giovanni B.
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- 2021
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180. Impact of the Agulhas Return Current on the oceanography of the Kerguelen Plateau region, Southern Ocean, over the last 40 kyrs
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Civel-Mazens, M., Crosta, X., Cortese, G., Michel, E., Mazaud, A., Ther, O., Ikehara, M., and Itaki, T.
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- 2021
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181. Discovery of a dormant 33 solar-mass black hole in pre-release Gaia astrometry
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Panuzzo, P., Mazeh, T., Arenou, F., Holl, B., Caffau, E., Jorissen, A., Babusiaux, C., Gavras, P., Sahlmann, J., Bastian, U., Wyrzykowski, Ł., Eyer, L., Leclerc, N., Bauchet, N., Bombrun, A., Mowlavi, N., Seabroke, G. M., Teyssier, D., Balbinot, E., Helmi, A., Brown, A. G.A., Vallenari, A., Prusti, T., De Bruijne, J. H.J., Barbier, A., Biermann, M., Creevey, O. L., Ducourant, C., Evans, D. W., Guerra, R., Hutton, A., Jordi, C., Klioner, S. A., Lammers, U., Lindegren, L., Luri, X., Mignard, F., Nicolas, C., Randich, S., Sartoretti, P., Smiljanic, R., Tanga, P., Walton, N. A., Aerts, C., Bailer-Jones, C. A.L., Cropper, M., Drimmel, R., Jansen, F., Katz, D., Lattanzi, M. G., Soubiran, C., Thévenin, F., Van Leeuwen, F., Andrae, R., Audard, M., Bakker, J., Blomme, R., Castañeda, J., De Angeli, F., Fabricius, C., Fouesneau, M., Frémat, Y., Galluccio, L., Guerrier, A., Heiter, U., Masana, E., Messineo, R., Nienartowicz, K., Pailler, F., Riclet, F., Roux, W., Sordo, R., Gracia-Abril, G., Portell, J., Altmann, M., Benson, K., Berthier, J., Burgess, P. W., Busonero, D., Busso, G., Cacciari, C., Cánovas, H., Carrasco, J. M., Carry, B., Cellino, A., Cheek, N., Clementini, G., Damerdji, Y., Davidson, M., De Teodoro, P., Delchambre, L., Della Oro, A., Fraile Garcia, E., Garabato, D., García-Lario, P., Haigron, R., Hambly, N. C., Harrison, D. L., Hatzidimitriou, D., Hernández, J., Hestroffer, D., Hodgkin, S. T., Jamal, S., Jevardat De Fombelle, G., Jordan, S., Krone-Martins, A., Lanzafame, A. C., Löffler, W., Lorca, A., Marchal, O., Marrese, P. M., Moitinho, A., Muinonen, K., Nuñez Campos, M., Oreshina-Slezak, I., Osborne, P., Pancino, E., Pauwels, T., Recio-Blanco, A., Riello, M., Rimoldini, L., Robin, A. C., Roegiers, T., Sarro, L. M., Schultheis, M., Smith, M., Sozzetti, A., Utrilla, E., Van Leeuwen, M., Weingrill, K., Abbas, U., Ábrahám, P., Abreu Aramburu, A., Ahmed, S., Altavilla, G., Álvarez, M. A., Anders, F., Anderson, R. I., Anglada Varela, E., Antoja, T., Baig, S., Baines, D., Baker, S. G., Balaguer-Núñez, L., Balog, Z., Barache, C., Barros, M., Barstow, M. A., Bartolomé, S., Bashi, D., Bassilana, J. L., Baudeau, N., Becciani, U., Bedin, L. R., Bellas-Velidis, I., Bellazzini, M., Beordo, W., Bernet, M., Bertolotto, C., Bertone, S., Bianchi, L., Binnenfeld, A., Blanco-Cuaresma, S., Bland-Hawthorn, J., Blazere, A., Boch, T., Bossini, D., Bouquillon, S., Bragaglia, A., Braine, J., Bratsolis, E., Breedt, E., Bressan, A., Brouillet, N., Brugaletta, E., Bucciarelli, B., Butkevich, A. G., Buzzi, R., Camut, A., Cancelliere, R., Cantat-Gaudin, T., Capilla Guilarte, D., Carballo, R., Carlucci, T., Carnerero, M. I., Carretero, J., Carton, S., Casamiquela, L., Casey, A., Castellani, M., Castro-Ginard, A., Ceraj, L., Cesare, V., Charlot, P., Chaudet, C., Chemin, L., Chiavassa, A., Chornay, N., Chosson, D., Cooper, W. J., Cornez, T., Cowell, S., Crosta, M., Crowley, C., Cruz Reyes, M., Dafonte, C., Dal Ponte, M., David, M., De Laverny, P., De Luise, F., De March, R., De Torres, A., Del Peloso, E. F., Delbo, M., Delgado, A., Delisle, J. B., Demouchy, C., Denis, E., Dharmawardena, T. 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G., Buzzi, R., Camut, A., Cancelliere, R., Cantat-Gaudin, T., Capilla Guilarte, D., Carballo, R., Carlucci, T., Carnerero, M. I., Carretero, J., Carton, S., Casamiquela, L., Casey, A., Castellani, M., Castro-Ginard, A., Ceraj, L., Cesare, V., Charlot, P., Chaudet, C., Chemin, L., Chiavassa, A., Chornay, N., Chosson, D., Cooper, W. J., Cornez, T., Cowell, S., Crosta, M., Crowley, C., Cruz Reyes, M., Dafonte, C., Dal Ponte, M., David, M., De Laverny, P., De Luise, F., De March, R., De Torres, A., Del Peloso, E. F., Delbo, M., Delgado, A., Delisle, J. B., Demouchy, C., Denis, E., Dharmawardena, T. E., Di Giacomo, F., Diener, C., Distefano, E., Dolding, C., Dsilva, K., Enke, H., Fabre, C., Fabrizio, M., Faigler, S., Fatoviä, M., Fedorets, G., Fernández-Hernández, J., Fernique, P., Figueras, F., Fouron, C., Fragkoudi, F., Gai, M., Galinier, M., Garcia-Serrano, A., García-Torres, M., Garofalo, A., Gerlach, E., Geyer, R., Giacobbe, P., Gilmore, G., Girona, S., Giuffrida, G., Gomboc, A., Gomez, A., González-Santamaría, I., Gosset, E., Granvik, Mikael, Gregori Barrera, V., Gutiérrez-Sánchez, R., Haywood, M., Helmer, A., Hidalgo, S. L., Hilger, T., Hobbs, D., Hottier, C., Huckle, H. E., Jiménez-Arranz, Ó., Juaristi Campillo, J., Kaczmarek, Z., Kervella, P., Khanna, S., Kontizas, M., Kordopatis, G., Korn, A. J., Kóspál, Á., Kostrzewa-Rutkowska, Z., Kruszyåà  Ska, K., Kun, M., Lambert, S., Lanza, A. F., Lebreton, Y., Lebzelter, T., Leccia, S., Lecoutre, G., Liao, S., Liberato, L., Licata, E., Livanou, E., Lobel, A., López-Miralles, J., Loup, C., Madarász, M., Mahy, L., Mann, R. G., Manteiga, M., Marcellino, C. P., Marchant, J. M., Marconi, M., Marín Pina, D., Marinoni, S., Marshall, D. J., Martín Lozano, J., Martin Polo, L., Martín-Fleitas, J. M., Marton, G., Mascarenhas, D., Masip, A., Mastrobuono-Battisti, A., McMillan, P. J., Meichsner, J., Merc, J., Messina, S., Millar, N. R., Mints, A., Mohamed, D., Molina, D., Molinaro, R., Molnár, L., Monguió, M., Montegriffo, P., Monti, L., Mora, A., Morbidelli, R., Morris, D., Mudimadugula, R., Muraveva, T., Musella, I., Nagy, Z., Nardetto, N., Navarrete, C., Oh, S., Ordenovic, C., Orenstein, O., Pagani, C., Pagano, I., Palaversa, L., Palicio, P. A., Pallas-Quintela, L., Pawlak, M., Penttilä, A., Pesciullesi, P., Pinamonti, M., Plachy, E., Planquart, L., Plum, G., Poggio, E., Pourbaix, D., Price-Whelan, A. M., Pulone, L., Rabin, V., Rainer, M., Raiteri, C. M., Ramos, P., Ramos-Lerate, M., Ratajczak, M., Re Fiorentin, P., Regibo, S., Reylé, C., Ripepi, V., Riva, A., Rix, H. W., Rixon, G., Robert, G., Robichon, N., Robin, C., Romero-Gómez, M., Rowell, N., Ruz Mieres, D., Rybicki, K. A., Sadowski, G., Sagristà Sellés, A., Sanna, N., Santoveña, R., Sarasso, M., Sarmiento, M. H., Sarrate Riera, C., Sciacca, E., Ségransan, D., Semczuk, M., Shahaf, S., Siebert, A., Slezak, E., Smart, R. L., Snaith, O. N., Solano, E., Solitro, F., Souami, D., Souchay, J., Spitoni, E., Spoto, F., Squillante, L. A., Steele, I. A., Steidelmüller, H., Surdej, J., Szabados, L., Taris, F., Taylor, M. B., Teixeira, R., Tepper-Garcia, T., Thuillot, W., Tolomei, L., Tonello, N., Torra, F., Torralba Elipe, G., Trabucchi, M., Trentin, E., Tsantaki, M., Turon, C., Ulla, A., Unger, N., Valtchanov, I., Vanel, O., Vecchiato, A., Vicente, D., Villar, E., Weiler, M., Zhao, H., Zorec, J., Zucker, S., Župiä, A., and Zwitter, T.
- Abstract
Context. Gravitational waves from black-hole (BH) merging events have revealed a population of extra-galactic BHs residing in short-period binaries with masses that are higher than expected based on most stellar evolution models-And also higher than known stellar-origin black holes in our Galaxy. It has been proposed that those high-mass BHs are the remnants of massive metal-poor stars. Aims. Gaia astrometry is expected to uncover many Galactic wide-binary systems containing dormant BHs, which may not have been detected before. The study of this population will provide new information on the BH-mass distribution in binaries and shed light on their formation mechanisms and progenitors. Methods. As part of the validation efforts in preparation for the fourth Gaia data release (DR4), we analysed the preliminary astrometric binary solutions, obtained by the Gaia Non-Single Star pipeline, to verify their significance and to minimise false-detection rates in high-mass-function orbital solutions. Results. The astrometric binary solution of one source, Gaia BH3, implies the presence of a 32.70a ±a 0.82aM- BH in a binary system with a period of 11.6 yr. Gaia radial velocities independently validate the astrometric orbit. Broad-band photometric and spectroscopic data show that the visible component is an old, very metal-poor giant of the Galactic halo, at a distance of 590 pc. Conclusions. The BH in the Gaia BH3 system is more massive than any other Galactic stellar-origin BH known thus far. The low metallicity of the star companion supports the scenario that metal-poor massive stars are progenitors of the high-mass BHs detected by gravitational-wave telescopes. The Galactic orbit of the system and its metallicity indicate that it might belong to the Sequoia halo substructure. Alternatively, and more plausibly, it could belong to the ED-2 stream, which likely originated from a globular cluster that had been disrupted by the Milky Way., Funder: for funder information see Appendix F in https://doi.org/10.1051/0004-6361/202449763;Full text license: CC BY 4.0
- Published
- 2024
- Full Text
- View/download PDF
182. Gaia Focused Product Release: A catalogue of sources around quasars to search for strongly lensed quasars
- Author
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Krone-Martins, A., Ducourant, C., Galluccio, L., Delchambre, L., Oreshina-Slezak, I., Teixeira, R., Braine, J., Le Campion, J. F., Mignard, F., Roux, W., Blazere, A., Pegoraro, L., Brown, A. G.A., Vallenari, A., Prusti, T., De Bruijne, J. H.J., Arenou, F., Babusiaux, C., Barbier, A., Biermann, M., Creevey, O. L., Evans, D. W., Eyer, L., Guerra, R., Hutton, A., Jordi, C., Klioner, S. A., Lammers, U., Lindegren, L., Luri, X., Randich, S., Sartoretti, P., Smiljanic, R., Tanga, P., Walton, N. A., Bailer-Jones, C. A.L., Bastian, U., Cropper, M., Drimmel, R., Katz, D., Soubiran, C., Van Leeuwen, F., Audard, M., Bakker, J., Blomme, R., Castañeda, J., De Angeli, F., Fabricius, C., Fouesneau, M., Frémat, Y., Guerrier, A., Masana, E., Messineo, R., Nicolas, C., Nienartowicz, K., Pailler, F., Panuzzo, P., Riclet, F., Seabroke, G. M., Sordo, R., Thévenin, F., Gracia-Abril, G., Portell, J., Teyssier, D., Altmann, M., Benson, K., Berthier, J., Burgess, P. W., Busonero, D., Busso, G., Cánovas, H., Carry, B., Cheek, N., Clementini, G., Damerdji, Y., Davidson, M., De Teodoro, P., Dell' Oro, A., Fraile Garcia, E., Garabato, D., García-Lario, P., Garralda Torres, N., Gavras, P., Haigron, R., Hambly, N. C., Harrison, D. L., Hatzidimitriou, D., Hernández, J., Hodgkin, S. T., Holl, B., Jamal, S., Jordan, S., Lanzafame, A. C., Löffler, W., Lorca, A., Marchal, O., Marrese, P. M., Moitinho, A., Muinonen, K., Nuñez Campos, M., Osborne, P., Pancino, E., Pauwels, T., Recio-Blanco, A., Riello, M., Rimoldini, L., Robin, A. C., Roegiers, T., Sarro, L. M., Schultheis, M., Siopis, C., Smith, M., Sozzetti, A., Utrilla, E., Van Leeuwen, M., Weingrill, K., Abbas, U., Ábrahám, P., Abreu Aramburu, A., Aerts, C., Altavilla, G., Álvarez, M. A., Alves, J., Anderson, R. I., Antoja, T., Baines, D., Baker, S. G., Balog, Z., Barache, C., Barbato, D., Barros, M., Barstow, M. A., Bartolomé, S., Bashi, D., Bauchet, N., Baudeau, N., Becciani, U., Bedin, L. R., Bellas-Velidis, I., Bellazzini, M., Beordo, W., Berihuete, A., Bernet, M., Bertolotto, C., Bertone, S., Bianchi, L., Binnenfeld, A., Boch, T., Bombrun, A., Bouquillon, S., Bragaglia, A., Bramante, L., Breedt, E., Bressan, A., Brouillet, N., Brugaletta, E., Bucciarelli, B., Butkevich, A. G., Buzzi, R., Caffau, E., Cancelliere, R., Cannizzo, S., Carballo, R., Carlucci, T., Carnerero, M. I., Carrasco, J. M., Carretero, J., Carton, S., Casamiquela, L., Castellani, M., Castro-Ginard, A., Cesare, V., Charlot, P., Chemin, L., Chiaramida, V., Chiavassa, A., Chornay, N., Collins, R., Contursi, G., Cooper, W. J., Cornez, T., Crosta, M., Crowley, C., Dafonte, C., De Laverny, P., De Luise, F., De March, R., De Souza, R., De Torres, A., Del Peloso, E. F., Delbo, M., Delgado, A., Dharmawardena, T. E., Diakite, S., Diener, C., Distefano, E., Dolding, C., Dsilva, K., Durán, J., Enke, H., Esquej, P., Fabre, C., Fabrizio, M., Faigler, S., Fatoviäà ‡, M., Fedorets, G., Fernández-Hernández, J., Fernique, P., Figueras, F., Fournier, Y., Fouron, C., Gai, M., Galinier, M., Garcia-Gutierrez, A., García-Torres, M., Garofalo, A., Gerlach, E., Geyer, R., Giacobbe, P., Gilmore, G., Girona, S., Giuffrida, G., Gomel, R., Gomez, A., González-Núñez, J., González-Santamaría, I., Gosset, E., Granvik, Mikael, Gregori Barrera, V., Gutiérrez-Sánchez, R., Haywood, M., Helmer, A., Helmi, A., Henares, K., Hidalgo, S. L., Hilger, T., Hobbs, D., Hottier, C., Huckle, H. E., Jabåà  Oåà Â., Ska, M., Jansen, F., Jiménez-Arranz, Ó, Juaristi Campillo, J., Khanna, S., Kordopatis, G., Kóspál, Á, Kostrzewa-Rutkowska, Z., Kun, M., Lambert, S., Lanza, A. F., Lebreton, Y., Lebzelter, T., Leccia, S., Lecoeur-Taibi, I., Lecoutre, G., Liao, S., Liberato, L., Licata, E., Lindstrøm, H. E.P., Lister, T. A., Livanou, E., Lobel, A., Loup, C., Mahy, L., Mann, R. G., Manteiga, M., Marchant, J. M., Marconi, M., Marín Pina, D., Marinoni, S., Marshall, D. J., Martín Lozano, J., Martín-Fleitas, J. M., Marton, G., Mary, N., Masip, A., Massari, D., Mastrobuono-Battisti, A., Mazeh, T., McMillan, P. J., Meichsner, J., Messina, S., Michalik, D., Millar, N. R., Mints, A., Molina, D., Molinaro, R., Molnár, L., Monari, G., Monguió, M., Montegriffo, P., Montero, A., Mor, R., Mora, A., Morbidelli, R., Morel, T., Morris, D., Mowlavi, N., Munoz, D., Muraveva, T., Murphy, C. P., Musella, I., Nagy, Z., Nieto, S., Noval, L., Ogden, A., Ordenovic, C., Pagani, C., Pagano, I., Palaversa, L., Palicio, P. A., Pallas-Quintela, L., Panahi, A., Panem, C., Payne-Wardenaar, S., Penttilä, A., Pesciullesi, P., Piersimoni, A. M., Pinamonti, M., Pineau, F. X., Plachy, E., Plum, G., Poggio, E., Pourbaix, D., Prša, A., Pulone, L., Racero, E., Rainer, M., Raiteri, C. M., Ramos, P., Ramos-Lerate, M., Ratajczak, M., Re Fiorentin, P., Regibo, S., Reylé, C., Ripepi, V., Riva, A., Rix, H. W., Rixon, G., Robichon, N., Robin, C., Romero-Gómez, M., Rowell, N., Royer, F., Ruz Mieres, D., Rybicki, K. A., Sadowski, G., Sáez Núñez, A., Sagristà Sellés, A., Sahlmann, J., Sanchez Gimenez, V., Sanna, N., Santoveña, R., Sarasso, M., Sarrate Riera, C., Sciacca, E., Segovia, J. C., Ségransan, D., Shahaf, S., Siebert, A., Siltala, L., Slezak, E., Smart, R. L., Snaith, O. N., Solano, E., Solitro, F., Souami, D., Souchay, J., Spina, L., Spitoni, E., Spoto, F., Squillante, L. A., Steele, I. A., Steidelmüller, H., Surdej, J., Szabados, L., Taris, F., Taylor, M. B., Tisaniäà ‡, K., Tolomei, L., Torra, F., Torralba Elipe, G., Trabucchi, M., Tsantaki, M., Ulla, A., Unger, N., Vanel, O., Vecchiato, A., Vicente, D., Voutsinas, S., Weiler, M., Wyrzykowski, Ł, Zhao, H., Zorec, J., Zwitter, T., Balaguer-Núñez, L., Leclerc, N., Morgenthaler, S., Robert, G., Zucker, S., Krone-Martins, A., Ducourant, C., Galluccio, L., Delchambre, L., Oreshina-Slezak, I., Teixeira, R., Braine, J., Le Campion, J. F., Mignard, F., Roux, W., Blazere, A., Pegoraro, L., Brown, A. G.A., Vallenari, A., Prusti, T., De Bruijne, J. H.J., Arenou, F., Babusiaux, C., Barbier, A., Biermann, M., Creevey, O. L., Evans, D. W., Eyer, L., Guerra, R., Hutton, A., Jordi, C., Klioner, S. A., Lammers, U., Lindegren, L., Luri, X., Randich, S., Sartoretti, P., Smiljanic, R., Tanga, P., Walton, N. A., Bailer-Jones, C. A.L., Bastian, U., Cropper, M., Drimmel, R., Katz, D., Soubiran, C., Van Leeuwen, F., Audard, M., Bakker, J., Blomme, R., Castañeda, J., De Angeli, F., Fabricius, C., Fouesneau, M., Frémat, Y., Guerrier, A., Masana, E., Messineo, R., Nicolas, C., Nienartowicz, K., Pailler, F., Panuzzo, P., Riclet, F., Seabroke, G. M., Sordo, R., Thévenin, F., Gracia-Abril, G., Portell, J., Teyssier, D., Altmann, M., Benson, K., Berthier, J., Burgess, P. W., Busonero, D., Busso, G., Cánovas, H., Carry, B., Cheek, N., Clementini, G., Damerdji, Y., Davidson, M., De Teodoro, P., Dell' Oro, A., Fraile Garcia, E., Garabato, D., García-Lario, P., Garralda Torres, N., Gavras, P., Haigron, R., Hambly, N. C., Harrison, D. L., Hatzidimitriou, D., Hernández, J., Hodgkin, S. T., Holl, B., Jamal, S., Jordan, S., Lanzafame, A. C., Löffler, W., Lorca, A., Marchal, O., Marrese, P. M., Moitinho, A., Muinonen, K., Nuñez Campos, M., Osborne, P., Pancino, E., Pauwels, T., Recio-Blanco, A., Riello, M., Rimoldini, L., Robin, A. C., Roegiers, T., Sarro, L. M., Schultheis, M., Siopis, C., Smith, M., Sozzetti, A., Utrilla, E., Van Leeuwen, M., Weingrill, K., Abbas, U., Ábrahám, P., Abreu Aramburu, A., Aerts, C., Altavilla, G., Álvarez, M. A., Alves, J., Anderson, R. I., Antoja, T., Baines, D., Baker, S. G., Balog, Z., Barache, C., Barbato, D., Barros, M., Barstow, M. A., Bartolomé, S., Bashi, D., Bauchet, N., Baudeau, N., Becciani, U., Bedin, L. R., Bellas-Velidis, I., Bellazzini, M., Beordo, W., Berihuete, A., Bernet, M., Bertolotto, C., Bertone, S., Bianchi, L., Binnenfeld, A., Boch, T., Bombrun, A., Bouquillon, S., Bragaglia, A., Bramante, L., Breedt, E., Bressan, A., Brouillet, N., Brugaletta, E., Bucciarelli, B., Butkevich, A. G., Buzzi, R., Caffau, E., Cancelliere, R., Cannizzo, S., Carballo, R., Carlucci, T., Carnerero, M. I., Carrasco, J. M., Carretero, J., Carton, S., Casamiquela, L., Castellani, M., Castro-Ginard, A., Cesare, V., Charlot, P., Chemin, L., Chiaramida, V., Chiavassa, A., Chornay, N., Collins, R., Contursi, G., Cooper, W. J., Cornez, T., Crosta, M., Crowley, C., Dafonte, C., De Laverny, P., De Luise, F., De March, R., De Souza, R., De Torres, A., Del Peloso, E. F., Delbo, M., Delgado, A., Dharmawardena, T. E., Diakite, S., Diener, C., Distefano, E., Dolding, C., Dsilva, K., Durán, J., Enke, H., Esquej, P., Fabre, C., Fabrizio, M., Faigler, S., Fatoviäà ‡, M., Fedorets, G., Fernández-Hernández, J., Fernique, P., Figueras, F., Fournier, Y., Fouron, C., Gai, M., Galinier, M., Garcia-Gutierrez, A., García-Torres, M., Garofalo, A., Gerlach, E., Geyer, R., Giacobbe, P., Gilmore, G., Girona, S., Giuffrida, G., Gomel, R., Gomez, A., González-Núñez, J., González-Santamaría, I., Gosset, E., Granvik, Mikael, Gregori Barrera, V., Gutiérrez-Sánchez, R., Haywood, M., Helmer, A., Helmi, A., Henares, K., Hidalgo, S. L., Hilger, T., Hobbs, D., Hottier, C., Huckle, H. E., Jabåà  Oåà Â., Ska, M., Jansen, F., Jiménez-Arranz, Ó, Juaristi Campillo, J., Khanna, S., Kordopatis, G., Kóspál, Á, Kostrzewa-Rutkowska, Z., Kun, M., Lambert, S., Lanza, A. F., Lebreton, Y., Lebzelter, T., Leccia, S., Lecoeur-Taibi, I., Lecoutre, G., Liao, S., Liberato, L., Licata, E., Lindstrøm, H. E.P., Lister, T. A., Livanou, E., Lobel, A., Loup, C., Mahy, L., Mann, R. G., Manteiga, M., Marchant, J. M., Marconi, M., Marín Pina, D., Marinoni, S., Marshall, D. J., Martín Lozano, J., Martín-Fleitas, J. M., Marton, G., Mary, N., Masip, A., Massari, D., Mastrobuono-Battisti, A., Mazeh, T., McMillan, P. J., Meichsner, J., Messina, S., Michalik, D., Millar, N. R., Mints, A., Molina, D., Molinaro, R., Molnár, L., Monari, G., Monguió, M., Montegriffo, P., Montero, A., Mor, R., Mora, A., Morbidelli, R., Morel, T., Morris, D., Mowlavi, N., Munoz, D., Muraveva, T., Murphy, C. P., Musella, I., Nagy, Z., Nieto, S., Noval, L., Ogden, A., Ordenovic, C., Pagani, C., Pagano, I., Palaversa, L., Palicio, P. A., Pallas-Quintela, L., Panahi, A., Panem, C., Payne-Wardenaar, S., Penttilä, A., Pesciullesi, P., Piersimoni, A. M., Pinamonti, M., Pineau, F. X., Plachy, E., Plum, G., Poggio, E., Pourbaix, D., Prša, A., Pulone, L., Racero, E., Rainer, M., Raiteri, C. M., Ramos, P., Ramos-Lerate, M., Ratajczak, M., Re Fiorentin, P., Regibo, S., Reylé, C., Ripepi, V., Riva, A., Rix, H. W., Rixon, G., Robichon, N., Robin, C., Romero-Gómez, M., Rowell, N., Royer, F., Ruz Mieres, D., Rybicki, K. A., Sadowski, G., Sáez Núñez, A., Sagristà Sellés, A., Sahlmann, J., Sanchez Gimenez, V., Sanna, N., Santoveña, R., Sarasso, M., Sarrate Riera, C., Sciacca, E., Segovia, J. C., Ségransan, D., Shahaf, S., Siebert, A., Siltala, L., Slezak, E., Smart, R. L., Snaith, O. N., Solano, E., Solitro, F., Souami, D., Souchay, J., Spina, L., Spitoni, E., Spoto, F., Squillante, L. A., Steele, I. A., Steidelmüller, H., Surdej, J., Szabados, L., Taris, F., Taylor, M. B., Tisaniäà ‡, K., Tolomei, L., Torra, F., Torralba Elipe, G., Trabucchi, M., Tsantaki, M., Ulla, A., Unger, N., Vanel, O., Vecchiato, A., Vicente, D., Voutsinas, S., Weiler, M., Wyrzykowski, Ł, Zhao, H., Zorec, J., Zwitter, T., Balaguer-Núñez, L., Leclerc, N., Morgenthaler, S., Robert, G., and Zucker, S.
- Abstract
Context. Strongly lensed quasars are fundamental sources for cosmology. The Gaia space mission covers the entire sky with the unprecedented resolution of 0.18âà € ³ in the optical, making it an ideal instrument to search for gravitational lenses down to the limiting magnitude of 21. Nevertheless, the previous Gaia Data Releases are known to be incomplete for small angular separations such as those expected for most lenses. Aims. We present the Data Processing and Analysis Consortium GravLens pipeline, which was built to analyse all Gaia detections around quasars and to cluster them into sources, thus producing a catalogue of secondary sources around each quasar. We analysed the resulting catalogue to produce scores that indicate source configurations that are compatible with strongly lensed quasars. Methods. GravLens uses the DBSCAN unsupervised clustering algorithm to detect sources around quasars. The resulting catalogue of multiplets is then analysed with several methods to identify potential gravitational lenses. We developed and applied an outlier scoring method, a comparison between the average BP and RP spectra of the components, and we also used an extremely randomised tree algorithm. These methods produce scores to identify the most probable configurations and to establish a list of lens candidates. Results. We analysed the environment of 3 760 032 quasars. A total of 4 760 920 sources, including the quasars, were found within 6âà € ³ of the quasar positions. This list is given in the Gaia archive. In 87% of cases, the quasar remains a single source, and in 501 385 cases neighbouring sources were detected. We propose a list of 381 lensed candidates, of which we identified 49 as the most promising ones. Beyond these candidates, the associate tables in this Focused Product Release allow the entire community to explore the unique Gaia data for strong lensing studies further., Full text license: CC BY 4.0;Funder: for funder information see Appendix C in https://doi.org/10.1051/0004-6361/202347273
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- 2024
- Full Text
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183. Methodological approach to predict liquefaction effects on geo-structures: laboratory tests on real cases
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Romice, F, CASTELLANZA, RICCARDO PIETRO, CROSTA, GIOVANNI, ROMICE, FRANCESCA, Romice, F, CASTELLANZA, RICCARDO PIETRO, CROSTA, GIOVANNI, and ROMICE, FRANCESCA
- Abstract
La liquefazione è un fenomeno complesso che potrebbe causare numerosi danni agli edifici e alle infrastrutture. È generalmente identificato come la perdita di resistenza e rigidità di un terreno a causa di scosse sismiche o altri carichi dinamici. Comprendere appieno il suo meccanismo rimane una delle sfide dell’ingegneria geotecnica legata ai terremoti, poiché i geomateriali non mostrano reazioni identiche in condizioni sismiche simili. Dal terremoto di Niigata del 1964, molti ricercatori hanno mostrato interesse per questo campo e si sono impegnati per studiare questo fenomeno. Questa tesi di dottorato si concentra sull'analisi dei terreni liquefacibili partendo da un metodo semplificato per poi esplorare i metodi avanzati, attraverso lo studio di due casi reali, che coinvolgono diverse strutture geotecniche. L'obiettivo è quello di fornire un metodo completo di analisi nel campo della liquefazione, concentrandosi soprattutto su apparecchiature di laboratorio che meglio simulino il comportamento dinamico del terreno. Per ottenere questo risultato, il lavoro è stato sviluppato in più fasi focalizzate principalmente sullo studio sperimentale, teorico e numerico; questo percorso rappresenta il tipico e peculiare approccio ingegneristico per l'analisi di un fenomeno reale. Le prove in situ sono considerate come punto di partenza nella valutazione della liquefazione, poiché forniscono il Fattore di Sicurezza del terreno in esame, necessario per ulteriori analisi. Le apparecchiature di laboratorio consentono di testare il materiale per valutare la sua suscettibilità alla liquefazione, ma soprattutto per definire una curva affidabile da utilizzare nella calibrazione della modellazione costitutiva. A questo scopo sono state eseguite diverse prove triassiali cicliche, a carico controllato e a deformazione controllata, al fine di definire una procedura di prova per ottenere risultati di alta qualità. Un'analisi finale mediante modellazione numerica basata sulla ca, Liquefaction is a complex phenomenon which could lead to several damages in building and infrastructure. It is generally identified as the loose of strength and stiffness of a soil by earthquake shaking or other dynamic loading. Fully understanding its mechanism remains one of the challenges of earthquake-related geotechnical engineering, as geomaterials do not exhibit identical reactions under similar seismic conditions. From Niigata earthquake in 1964, many researchers have shown interest in this field and have worked to study this phenomenon. This PhD thesis is focus on analysis of liquefiable soils starting from a simplified method and then exploring the advanced methods, by means of study of two real cases, which involve different geotechnical structure. The objective is to provide a full method of analysis in liquefaction field, focusing most of all on laboratory equipment which better simulate the dynamic behaviour of the soil. For getting this result, the work has been developed in more phasis focused mostly on experimental, theoretical and numerical study; this path represents the typical and peculiar engineering approach for analysing a real phenomenon. In situ tests are considered as a starting point in liquefaction assessment, since they provide the Factor of Safety of soil under investigation, necessary for further analysis. Laboratory equipment allow to test the material in order to evaluate its susceptibility to liquefaction, but most of all to define reliable curve to be used in constitutive modelling calibration. For this purpose, several cyclic triaxial test have been performed, load-controlled and strain-controlled, in order to define a testing procedure to obtain high quality results. A final analysis by means of numerical modelling based on real test calibration, allows to make prediction not only about susceptibility but also about the actual effects of liquefaction on structure. The work presented reinforces the possibility of using the combin
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- 2024
184. Investigating Rockfall Fragmentation from Numerical and Experimental Perspectives
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Lanfranconi, C, FRATTINI, PAOLO, CROSTA, GIOVANNI, LANFRANCONI, CAMILLA, Lanfranconi, C, FRATTINI, PAOLO, CROSTA, GIOVANNI, and LANFRANCONI, CAMILLA
- Abstract
Questo progetto di ricerca, ha affrontato una vasta gamma di aspetti relativi ai fenomeni di crollo roccioso. L'indagine ha compreso l'analisi di casi di studio reali con l'obiettivo di comprendere la distribuzione dei frammenti in relazione al volume e alla topografia. Inoltre, sono state condotte simulazioni numeriche allo scopo di valutare l'impatto della frammentazione sull'analisi della pericolosità. Allo stesso tempo, sono stati condotti esperimenti in situ e di laboratorio al fine di approfondire la comprensione delle dinamiche di frammentazione. Questo approccio multidisciplinare ha fornito intuizioni sul comportamento dei crolli rocciosi, la frammentazione e le relative implicazioni per la valutazione della pericolosità e la gestione del rischio in regioni montuose. In particolare, la tesi si è concentrata su quattro obiettivi principali: L'analisi di casi di studio di crolli rocciosi, con un focus specifico sull'esame delle distribuzioni delle dimensioni dei blocchi nel deposito finale dei frammenti dei crolli. Questo approccio ha consentito di proporre indicatori che forniscono informazioni dettagliate sulle dinamiche di frammentazione durante gli eventi di crollo. Nello specifico, nel Capitolo 1 sono stati descritti tre indicatori chiave correlati alla frammentazione nei crolli rocciosi: la distanza percorsa rispetto alle dimensioni dei frammenti, la relazione di scala di potenza tra il deposito e le dimensioni dei frammenti, l'angolo di copertura e la dispersione laterale. Questi indicatori forniscono importanti informazioni sulla presenza di frammentazione dinamica durante gli eventi di crollo, permettendo di distinguere tra le caratteristiche del deposito primario e quelle dei blocchi/frammenti, mentre evidenziano la mobilità e il consumo di energia associati alla frammentazione. La quantificazione e la valutazione della frammentazione nelle dinamiche e nella pericolosità dei crolli rocciosi attraverso una modellazione dettagliata e l'analisi di, This research project, titled "Rockfall Volume Distribution, Fragmentation, and Frequency in the Context of Climate Change," aimed to explore various aspects of rockfall phenomena. The investigation included the analysis of real case studies to understand fragment distribution in relation to volume and topography, numerical simulations to assess the impact of fragmentation on hazard analysis, and in-situ and laboratory experiments to enhance the understanding of fragmentation dynamics. This multidisciplinary approach sought to provide some insights into how rockfalls behave, how fragmentation occurs, and the implications for hazard assessment and risk management in mountainous regions. Specifically, the thesis attempted to focus on four main objectives: 1. The analysis of real case studies of rockfalls, with a specific focus on examining the distributions of block sizes in the final deposit of rockfall fragments. This approach aimed to propose some indicators that could provide information about the dynamics of fragmentation during rockfall events. 2. The quantification and evaluation of fragmentation in rockfall dynamics and hazard assessment through detailed modeling and analysis of real case studies. This approach aimed to examine how fragmentation processes influence rockfall hazard and the importance of explicitly modeling fragmentation for accurate hazard assessment. 3. The analysis of the fragmentation process through experiments conducted at different scales (full-scale and laboratory-scale) to investigate behaviors observed in real case studies, focusing on dispersion, deposition, and mobility of rockfalls, as well as the effects of discontinuities. Despite the complexities and challenges in this area of study, the analysis of fragmentation in rockfalls remains of significant importance for various reasons. This work aimed to contribute to the enrichment of the understanding of this topic, impacting context of risk assessment and management in mountainous r
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- 2024
185. Late Miocene onset of the modern Antarctic Circumpolar Current
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Australian Research Council, Ministère de l'Europe et des Affaires étrangères (France), Generalitat de Catalunya, International Ocean Discovery Program, Ministerio de Economía, Industria y Competitividad (España), UK Research and Innovation, Evangelinos, Dimitris, Etourneau, Johan, van de Flierdt, Tina, Crosta, Xavier, Jeandel, Catherine, Flores, José Abel, Harwood, David M., Valero, Luis, Ducassou, Emmanuelle, Sauermilch, Isabel, Klocker, Andreas, Cacho, Isabel, Pena, Leopoldo D., Kreissig, Katharina, Benoit, Mathie, Paredes, Eduardo, García-Solsona, Ester, López-Quirós, Adrián, Escutia, Carlota, Australian Research Council, Ministère de l'Europe et des Affaires étrangères (France), Generalitat de Catalunya, International Ocean Discovery Program, Ministerio de Economía, Industria y Competitividad (España), UK Research and Innovation, Evangelinos, Dimitris, Etourneau, Johan, van de Flierdt, Tina, Crosta, Xavier, Jeandel, Catherine, Flores, José Abel, Harwood, David M., Valero, Luis, Ducassou, Emmanuelle, Sauermilch, Isabel, Klocker, Andreas, Cacho, Isabel, Pena, Leopoldo D., Kreissig, Katharina, Benoit, Mathie, Paredes, Eduardo, García-Solsona, Ester, López-Quirós, Adrián, and Escutia, Carlota
- Abstract
The Antarctic Circumpolar Current plays a pivotal role in global climate through its strong influence on the global overturning circulation, ocean heat and CO uptake. However, when and how the Antarctic Circumpolar Current reached its modern-like characteristics remains disputed. Here we present neodymium isotope and sortable silt records from sediment cores in the Southwest Pacific and South Indian oceans spanning the past 31 million years. Our data indicate that a circumpolar current like that of today did not exist before the late Miocene cooling. These findings suggest that the emergence of a homogeneous and deep-reaching strong Antarctic Circumpolar Current was not linked solely to the opening and deepening of Southern Ocean Gateways triggering continental-scale Antarctic Ice Sheet expansion during the Eocene–Oligocene Transition (∼34 Ma). Instead, we find that besides tectonic pre-conditioning, the expansion of the Antarctic Ice Sheet and sea ice since the middle Miocene Climate Transition (∼14 Ma) played a crucial role. This led to stronger density contrast and intensified Southern Westerly Winds across the Southern Ocean, establishing a vigorous deep-reaching circumpolar flow and an enhanced global overturning circulation, which amplified the late Cenozoic global cooling.
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- 2024
186. Examining the Effect of Increased Aerobic Exercise in Moderately Fit Adults on Psychological State and Cognitive Function
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Julia C. Basso, Douglas J. Oberlin, Medha K. Satyal, Catherine E. O’Brien, Christen Crosta, Zach Psaras, Anvitha Metpally, and Wendy A. Suzuki
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physical activity ,cardiopulmonary fitness ,spatial learning and memory ,episodic memory ,mood ,affective state ,Neurosciences. Biological psychiatry. Neuropsychiatry ,RC321-571 - Abstract
Regular physical exercise can decrease the risk for obesity, diabetes, and cardiovascular disease, increase life expectancy, and promote psychological health and neurocognitive functioning. Cross-sectional studies show that cardiorespiratory fitness level (VO2 max) is associated with enhanced brain health, including improved mood state and heightened cognitive performance. Interventional studies are consistent with these cross-sectional studies, but most have focused on low-fit populations. Few such studies have asked if increasing levels of physical activity in moderately fit people can significantly enhance mood, motivation, and cognition. Therefore, the current study investigated the effects of increasing aerobic exercise in moderately fit individuals on psychological state and cognitive performance. We randomly assigned moderately fit healthy adults, 25–59 years of age, who were engaged in one or two aerobic exercise sessions per week to either maintain their exercise regimen (n = 41) or increase their exercise regimen (i.e., 4–7 aerobic workouts per week; n = 39) for a duration of 3 months. Both before and after the intervention, we assessed aerobic capacity using a modified cardiorespiratory fitness test, and hippocampal functioning via various neuropsychological assessments including a spatial navigation task and the Mnemonic Similarity Task as well as self-reported measures including the Positive and Negative Affect Scale, Beck Anxiety Inventory, State-Trait Anxiety Inventory, Perceived Stress Scale, Rumination Scale, Eating Disorders Examination, Eating Attitudes Test, Body Attitudes Test, and Behavioral Regulation of Exercise Questionnaire. Consistent with our initial working hypotheses, we found that increasing exercise significantly decreased measures of negative affect, including fear, sadness, guilt, and hostility, as well as improved body image. Further, we found that the total number of workouts was significantly associated with improved spatial navigation abilities and body image as well as reduced anxiety, general negative affect, fear, sadness, hostility, rumination, and disordered eating. In addition, increases in fitness levels were significantly associated with improved episodic memory and exercise motivation as well as decreased stress and disordered eating. Our findings are some of the first to indicate that in middle-aged moderately-fit adults, continuing to increase exercise levels in an already ongoing fitness regimen is associated with additional benefits for both psychological and cognitive health.
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- 2022
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187. Francophone African Women Documentary Filmmakers : Beyond Representation
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CROSTA, SUZANNE, NIANG, SADA, TCHEUYAP, ALEXIE, CROSTA, SUZANNE, NIANG, SADA, and TCHEUYAP, ALEXIE
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- 2023
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188. The Ray Tracing Analytical Solution within the RAMOD framework. The case of a Gaia-like observer
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Crosta, Mariateresa, Vecchiato, Alberto, de Felice, Fernando, and Lattanzi, Mario Gilberto
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General Relativity and Quantum Cosmology - Abstract
This paper presents the analytical solution of the inverse ray tracing problem for photons emitted by a star and collected by an observer located in the gravitational field of the Solar System. This solution has been conceived to suit the accuracy achievable by the ESA Gaia satellite (launched on December 19, 2013) consistently with the measurement protocol in General relativity adopted within the RAMOD framework. Aim of this study is to provide a general relativistic tool for the science exploitation of such a revolutionary mission, whose main goal is to trace back star directions from within our local curved space-time, therefore providing a three-dimensional map of our Galaxy. The results are useful for a thorough comparison and cross-checking validation of what already exists in the field of Relativistic Astrometry. Moreover, the analytical solutions presented here can be extended to model other measurements that require the same order of accuracy expected for Gaia., Comment: 29 pages, 1 figure
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- 2015
189. Impact of Southern Ocean surface conditions on deep ocean circulation during the LGM: a model analysis
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F. Lhardy, N. Bouttes, D. M. Roche, X. Crosta, C. Waelbroeck, and D. Paillard
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Environmental pollution ,TD172-193.5 ,Environmental protection ,TD169-171.8 ,Environmental sciences ,GE1-350 - Abstract
Changes in water mass distribution are considered to be a significant contributor to the atmospheric CO2 concentration drop to around 186 ppm recorded during the Last Glacial Maximum (LGM). Yet simulating a glacial Atlantic Meridional Overturning Circulation (AMOC) in agreement with paleotracer data remains a challenge, with most models from previous Paleoclimate Modelling Intercomparison Project (PMIP) phases showing a tendency to simulate a strong and deep North Atlantic Deep Water (NADW) instead of the shoaling inferred from proxy records of water mass distribution. Conversely, the simulated Antarctic Bottom Water (AABW) is often reduced compared to its pre-industrial volume, and the Atlantic Ocean stratification is underestimated with respect to paleoproxy data. Inadequate representation of surface conditions, driving deep convection around Antarctica, may explain inaccurately simulated bottom water properties in the Southern Ocean. We investigate here the impact of a range of surface conditions in the Southern Ocean in the iLOVECLIM model using nine simulations obtained with different LGM boundary conditions associated with the ice sheet reconstruction (e.g., changes of elevation, bathymetry, and land–sea mask) and/or modeling choices related to sea-ice export, formation of salty brines, and freshwater input. Based on model–data comparison of sea-surface temperatures and sea ice, we find that only simulations with a cold Southern Ocean and a quite extensive sea-ice cover show an improved agreement with proxy records of sea ice, despite systematic model biases in the seasonal and regional patterns. We then show that the only simulation which does not display a much deeper NADW is obtained by parameterizing the sinking of brines along Antarctica, a modeling choice reducing the open-ocean convection in the Southern Ocean. These results highlight the importance of the representation of convection processes, which have a large impact on the water mass properties, while the choice of boundary conditions appears secondary for the model resolution and variables considered in this study.
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- 2021
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190. New Perspectives in Online Doctoral Supervision: A Systematic Literature Review
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Gray, Morag A. and Crosta, Lucilla
- Abstract
The aim of this systematic literature review was to ascertain the best practice available to provide high-quality online support to students during their thesis stage of an Online Doctorate in Higher Education programme. The review process involved a synthesis of available research literature to arrive a comprehensive and trustworthy picture. For completeness we reviewed literature related to both online and face-to-face doctoral supervision and how the latter could be applied to the growing area of providing online doctoral supervision. Through a detailed and systematic review of the literature by the two researchers independently we identified good practices which fit under three themes: Enculturation; Emancipation; and Healthy Relationship. We also highlighted aspects of effective online doctoral supervision
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- 2019
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191. Self-Reported Mental Health and Psychosocial Correlates during the COVID-19 Pandemic: Data from the General Population in Italy
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Daniela Marchetti, Roberta Maiella, Rocco Palumbo, Melissa D’Ettorre, Irene Ceccato, Marco Colasanti, Adolfo Di Crosta, Pasquale La Malva, Emanuela Bartolini, Daniela Biasone, Nicola Mammarella, Piero Porcelli, Alberto Di Domenico, and Maria Cristina Verrocchio
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psychological distress ,personality ,trust ,health anxiety ,dataset ,Bibliography. Library science. Information resources - Abstract
The COVID-19 pandemic tremendously impacted people’s day-to-day activities and mental health. This article describes the dataset used to investigate the psychological impact of the first national lockdown on the general Italian population. For this purpose, an online survey was disseminated via Qualtrics between 1 April and 20 April 2020, to record various socio-demographic and psychological variables. The measures included both validated (namely, the Impact of the Event Scale-Revised, the Perceived Stress Scale, the nine-item Patient Health Questionnaire, the seven-item Generalized Anxiety Disorder scale, the Big Five Inventory 10-Item, and the Whiteley Index-7) and ad hoc questionnaires (nine items to investigate in-group and out-group trust). The final sample comprised 4081 participants (18–85 years old). The dataset could be helpful to other researchers in understanding the psychological impact of the COVID-19 pandemic and its related preventive and protective measures. Furthermore, the present data might help shed some light on the role of individual differences in response to traumatic events. Finally, this dataset can increase the knowledge in investigating psychological distress, health anxiety, and personality traits.
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- 2023
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192. A Multivariate Time Series Analysis of Ground Deformation Using Persistent Scatterer Interferometry
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Serena Rigamonti, Giuseppe Dattola, Paolo Frattini, and Giovanni Battista Crosta
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InSAR ,Ground deformation ,Subsidence ,PCA ,ICA ,Hierarchical Clustering ,Science - Abstract
Ground deformations in urban areas can be the result of a combination of multiple factors and pose several hazards to infrastructures and human lives. In order to monitor these phenomena, Interferometric Synthetic Aperture Radar (InSAR) techniques are applied. The obtained signals record the overlapping of the phenomena, and their separation is a relevant issue. In this framework, we explored a new multi-method approach based on the combination of Principal Component Analysis (PCA), Independent Component Analysis (ICA) and Hierarchal Clustering (HC) on the standardized results to distinguish the main trends and seasonal signals embedded in the time series of ground displacements, to understand spatial-temporal patterns, to correlate ground deformation phenomena with geological and anthropogenic factors, and to recognize the specific footprints of different ground deformation phenomena. This method allows us to classify the ground deformations at the site scale in the metropolitan area of Naples, which is affected by uplift cycles, subsidence, cavity instabilities and sinkholes. At the local scale, the results allow a kinematic classification using the extracted components and considering the effect of the radius of influence generated by each cavity, as it is performed from a theoretical point of view when the draw angle is considered. According to the results, among the classified cavities, 2% were assigned to subsidence and 11% to uplift kinematics, while the remaining were found to be stable. Furthermore, our results show that the centering of the Spatial-PCA (S-PCA) is representative of the region’s main trend, whereas Temporal-PCA (T-PCA) gives information about the displacement rates identified by each component.
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- 2023
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193. Detecting the gravito-magnetic field of the dark halo of the Milky Way - the LaDaHaD mission concept: LaDaHaD
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Tartaglia, Angelo, Bassan, Massimo, Casalino, Lorenzo, Crosta, Mariateresa, Lattanzi, Mario, Lorenzini, Enrico, Lucchesi, David, Peron, Roberto, Pucacco, Giuseppe, Ruggiero, Matteo Luca, Santoli, Francesco, Valko, Pavol, Vecchiato, Alberto, Vespe, Francesco, and Visco, Massimo
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- 2021
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194. Ecological interactions in glacier environments: a review of studies on a model Alpine glacier.
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Crosta, Arianna, Valle, Barbara, Caccianiga, Marco, Gobbi, Mauro, Ficetola, Francesco Gentile, Pittino, Francesca, Franzetti, Andrea, Azzoni, Roberto Sergio, Lencioni, Valeria, Senese, Antonella, Corlatti, Luca, Buda, Jakub, Poniecka, Ewa, Novotná Jaroměřská, Tereza, Zawierucha, Krzysztof, and Ambrosini, Roberto
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ALPINE glaciers , *LITERATURE reviews , *TOP predators , *RHEOLOGY , *GLACIERS - Abstract
ABSTRACT Glaciers host a variety of cold‐adapted taxa, many of which have not yet been described. Interactions among glacier organisms are even less clear. Understanding ecological interactions is crucial to unravelling the functioning of glacier ecosystems, particularly in light of current glacier retreat. Through a review of the existing literature, we aim to provide a first overview of the biodiversity, primary production, trophic networks, and matter flow of a glacier ecosystem. We use the Forni Glacier (Central Italian Alps) – one of the best studied alpine glaciers in the world – as a model system for our literature review and integrate additional original data. We reveal the importance of allochthonous organic matter inputs, of Cyanobacteria and eukaryotic green algae in primary production, and the key role of springtails (Vertagopus glacialis) on the glacier surface in sustaining populations of two apex terrestrial predators: Nebria castanea (Coleoptera: Carabidae) and Pardosa saturatior (Araneae: Lycosidae). The cryophilic tardigrade Cryobiotus klebelsbergi is the apex consumer in cryoconite holes. This short food web highlights the fragility of nodes represented by invertebrates, contrasting with structured microbial communities in all glacier habitats. Although further research is necessary to quantify the ecological interactions of glacier organisms, this review summarises and integrates existing knowledge about the ecological processes on alpine glaciers and supports the importance of glacier‐adapted organisms in providing ecosystem services. [ABSTRACT FROM AUTHOR]
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- 2024
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195. EZH2 Inhibition by DS3201 Triggers the Kaposi's Sarcoma-Associated Herpesvirus Lytic Cycle and Potentiates the Effects Induced by SAHA in Primary Effusion Lymphoma Cells.
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Gonnella, Roberta, Collura, Flavia, Corrado, Vincenzo, Di Crosta, Michele, Santarelli, Roberta, and Cirone, Mara
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KAPOSI'S sarcoma-associated herpesvirus ,LYTIC cycle ,VIRAL antigens ,LYSIS ,HYDROXAMIC acids - Abstract
Primary Effusion Lymphoma (PEL) cells carry Kaposi's sarcoma-associated herpesvirus (KSHV) in a latent state, except for a small number of cells in which the virus replicates to ensure its persistence into the infected host. However, the lytic cycle can be reactivated in vitro by exposing these lymphoma cells to various treatments, leading to cell lysis. To restrict viral antigen expression, KSHV induces repressive epigenetic changes, including DNA methylation and histone modifications. Among the latter, histone deacetylation and tri-methylation of Histone H3 lisyne-27 (H3K27me3) have been reported to play a role. Here, we found that the inhibition of H3K27 tri-methylation by valemetostat DS3201 (DS), a small molecule that inhibits Enhancer of Zeste Homolog 2 (EZH2) methyltransferase, induced the KSHV lytic cycle in PEL cells, and that this effect involved the activation of the wtp53–p21 axis and autophagic dysregulation. DS also potentiated the lytic cycle activation mediated by the Histone deacetylases (HDAC) inhibitor Suberoylanilide hydroxamic acid (SAHA) and reinforced its cytotoxic effect, suggesting that such a combination could be used to unbalance the latent/lytic cycle and further impair the survival of PEL cells. [ABSTRACT FROM AUTHOR]
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- 2024
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196. Shaping shallow landslide susceptibility as a function of rainfall events.
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Fumagalli, Micol, Previati, Alberto, Frattini, Paolo, and Crosta, Giovanni B.
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RAINFALL ,LOGISTIC regression analysis ,LANDSLIDES ,COST analysis ,STATISTICAL models ,REGRESSION analysis ,LANDSLIDE hazard analysis - Abstract
This paper tests a multivariate statistical model to simulate rainfall dependent susceptibility scenarios of shallow landslides. To this end, extreme rainfall events spanning from 1977 to 2021 in the Orba basin (a study area of 505 km
2 located in Piedmont, northern Italy), have been considered. First of all, the role of conditioning and triggering factors on the spatial pattern of shallow landslides in areas with complex geological conditions is analysed by comparing their spatial distribution and their influence within logistic regression models, with results showing that rainfall and specific lithological and geomorphological conditions exert the strongest control on the spatial pattern of landslide. Different rainfall-based scenarios were then modelled using logistic regression models trained on different combinations of past events and evaluated using an ensemble of performance metrics. Models calibrated on multi-events outperform the ones based on a single event, since they are capable of compensating for local misleading effects that can arise from the use of a single rainfall event. The best performing developed model considers all the landslide triggering rainfall scenarios and two non-triggering intense rainfall events, with a score of 0.90 out of 1 on the multi-criteria TOPSIS-based performance index. Finally, a new approach based on misclassification costs is proposed to account for false negatives and false positives in the predicted susceptibility maps. Overall, this approach based on a multi-event calibration and on a misclassification costs analysis shows promise in producing rainfall dependent shallow landslide susceptibility scenarios that could be used for hazard analyses, early warning systems and to assist decision-makers in developing risk mitigation strategies. [ABSTRACT FROM AUTHOR]- Published
- 2024
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197. Post-Translational Modifications (PTMs) of mutp53 and Epigenetic Changes Induced by mutp53.
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Benedetti, Rossella, Di Crosta, Michele, D'Orazi, Gabriella, and Cirone, Mara
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RNA regulation , *POST-translational modification , *MUTANT proteins , *PROTEIN stability , *UBIQUITINATION , *P53 protein - Abstract
Simple Summary: Post-translational modifications (PTMs) strongly influence the stability and function of proteins. These modifications have been reported to affect wild-type (wt) p53 as well as the mutant forms of this protein (mutp53), often detected in cancer cells. Thus, PTMs may be key regulators of the oncosuppressor activity of wtp53 and of the pro-oncogenic functions that some mutant forms of p53 may acquire, in terms of tumor survival, progression and resistance to anti-cancer therapies. As treatments that specifically target mutp53 do not exist, manipulating PTMs may represent a promising approach to achieve this goal and even to reactivate the wt functions of mutant proteins, in some cases, as reported in this review. Wild-type (wt) p53 and mutant forms (mutp53) play a key but opposite role in carcinogenesis. wtP53 acts as an oncosuppressor, preventing oncogenic transformation, while mutp53, which loses this property, may instead favor this process. This suggests that a better understanding of the mechanisms activating wtp53 while inhibiting mutp53 may help to design more effective anti-cancer treatments. In this review, we examine possible PTMs with which both wt- and mutp53 can be decorated and discuss how their manipulation could represent a possible strategy to control the stability and function of these proteins, focusing in particular on mutp53. The impact of ubiquitination, phosphorylation, acetylation, and methylation of p53, in the context of several solid and hematologic cancers, will be discussed. Finally, we will describe some of the recent studies reporting that wt- and mutp53 may influence the expression and activity of enzymes responsible for epigenetic changes such as acetylation, methylation, and microRNA regulation and the possible consequences of such changes. [ABSTRACT FROM AUTHOR]
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- 2024
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198. Effects of Presentation Side and Emotional Valence on Auditory Recognition in Younger and Older Adults.
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Prete, Giulia, Malatesta, Gianluca, D'Anselmo, Anita, Palumbo, Rocco, Ceccato, Irene, La Malva, Pasquale, Di Crosta, Adolfo, Mammarella, Nicola, Tommasi, Luca, and Di Domenico, Alberto
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OLDER people ,AUDITORY perception ,AGE factors in memory ,STIMULUS & response (Psychology) ,OPTIMISM ,EAR - Abstract
(1) Background: It is well-established that older persons compared with younger persons show a bias toward positive valence (a positivity effect), together with less pronounced hemispheric asymmetries, but these topics have been scarcely explored in auditory modality. (2) Methods: We presented auditory stimuli with positive, neutral, or negative emotional valence dichotically to 20 younger and 20 older participants and asked them to memorize the stimuli. In a following session, stimuli were presented binaurally, and participants had to decide whether they were new or already presented in the left/right ear. (3) Results: A higher performance by younger compared with older listeners emerged, but neither the expected Right Ear Advantage nor the positivity effect was confirmed. New stimuli were correctly categorized more frequently if they had neutral valence, whereas stimuli already presented were better recognized with negative rather than neutral or positive valence, without any age difference. (4) Conclusions: These results reveal no hemispheric asymmetries and no age difference in a memory task for auditory stimuli and suggest the existence of a bias to better encode negative content, possibly due to the crucial role of negative stimuli in everyday life. [ABSTRACT FROM AUTHOR]
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- 2024
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199. A Study on the Effect of ‘Information Mismatch’ Simulation on Victims’ Quality of Life and Sense of Place in the Post-disaster Period
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Shimizu, Hiroaki, Tomeno, Ryoya, Crosta, Quirino, Merucuri, Micaela, Ono, Satoru, Kanegae, Hidehiko, Rizzi, Paola, Kijima, Kyoichi, Editor-in-Chief, Deguchi, Hiroshi, Editor-in-Chief, Hamada, Ryoju, editor, Soranastaporn, Songsri, editor, Kanegae, Hidehiko, editor, Dumrongrojwatthana, Pongchai, editor, Chaisanit, Settachai, editor, Rizzi, Paola, editor, and Dumblekar, Vinod, editor
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- 2019
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200. Structure of the Colima Volcanic Complex: Origin and Behaviour of Active Fault Systems in the Edifice
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Norini, Gianluca, Agliardi, Federico, Crosta, Giovanni, Groppelli, Gianluca, Zuluaga, Maria Clara, Cimarelli, Corrado, Series Editor, Müller, Sebastian, Series Editor, Varley, Nick, editor, Connor, Charles B., editor, and Komorowski, Jean-Christophe, editor
- Published
- 2019
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