148 results on '"Meslin, Pierre-Yves"'
Search Results
2. The Pyrenean Platform for Observation of the Atmosphere: Site, long-term dataset and science
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Lothon, Marie, primary, Gheusi, François, additional, Lohou, Fabienne, additional, Pont, Véronique, additional, Soula, Serge, additional, Derrien, Solène, additional, Bezombes, Yannick, additional, Leclerc, Emmanuel, additional, Athier, Gilles, additional, Vial, Antoine, additional, Philibert, Alban, additional, Campistron, Bernard, additional, Saïd, Frédérique, additional, Jambert, Corinne, additional, Sonke, Jeroen, additional, Amestoy, Julien, additional, Bargain, Erwan, additional, Bosser, Pierre, additional, Boulanger, Damien, additional, Bret, Guillaume, additional, Bodichon, Renaud, additional, Cabanas, Laurent, additional, Canut, Guylaine, additional, Estrampes, Jean-Bernard, additional, Gardrat, Eric, additional, Gomez Kuri, Zaida, additional, Gueffier, Jérémy, additional, Guesdon, Fabienne, additional, Lopez, Morgan, additional, Masson, Olivier, additional, Meslin, Pierre-Yves, additional, Meyerfeld, Yves, additional, Pascal, Nicolas, additional, Pique, Eric, additional, Ramonet, Michel, additional, Starck, Felix, additional, and Vidal, Romain, additional
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- 2024
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3. Retrieval of Water Vapor Column Abundance and Aerosol Properties from ChemCam Passive Sky Spectroscopy
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McConnochie, Timothy H., Smith, Michael D., Wolff, Michael J., Bender, Steve, Lemmon, Mark, Wiens, Roger C., Maurice, Sylvestre, Gasnault, Olivier, Lasue, Jeremie, Meslin, Pierre-Yves, Harri, Ari-Matti, Genzer, Maria, Kemppinen, Osku, Martínez, Germán M., DeFlores, Lauren, Blaney, Diana, Johnson, Jeffrey R., and Bell III, James F.
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Astrophysics - Earth and Planetary Astrophysics - Abstract
We derive water vapor column abundances and aerosol properties from Mars Science Laboratory (MSL) ChemCam passive mode observations of scattered sky light. Each ChemCam passive sky observation acquires spectra at two different elevation angles. We fit these spectra with a discrete-ordinates multiple scattering radiative transfer model, using the correlated-k approximation for gas absorption bands. The retrieval proceeds by first fitting the continuum of the ratio of the two elevation angles to solve for aerosol properties, and then fitting the continuum-removed ratio to solve for gas abundances. The final step of the retrieval makes use of the observed CO2 absorptions and the known CO2 abundance to correct the retrieved water vapor abundance for the effects of the vertical distribution of scattering aerosols and to derive an aerosol scale height parameter. The ChemCam-retrieved water abundances show, with only a few exceptions, the same seasonal behavior and the same timing of seasonal minima and maxima as the TES, CRISM, and REMS-H data sets that we compare them to. However ChemCam-retrieved water abundances are generally lower than zonal and regional scale from-orbit water vapor data, while at the same time being significantly larger than pre-dawn REMS-H abundances. Pending further analysis of REMS-H volume mixing ratio uncertainties, the differences between ChemCam and REMS-H pre-dawn mixing ratios appear to be much too large to be explained by large scale circulations and thus they tend to support the hypothesis of substantial diurnal interactions of water vapor with the surface. Our preliminary aerosol results, meanwhile, show the expected seasonal pattern in dust particle size but also indicate a surprising inter-annual increase in water-ice cloud opacities., Comment: 64 pages with embedded figures; this is the accepted version of the manuscript; the meta-data version of the abstract has been shorted to meet arXiv rules
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- 2017
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4. Cryogenic origin of fractionation between perchlorate and chloride under modern martian climate
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Li, Dongdong, Zhao, Yu-Yan Sara, Meslin, Pierre-Yves, Vals, Margaux, Forget, François, and Wu, Zhongchen
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- 2022
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5. Post-landing major element quantification using SuperCam laser induced breakdown spectroscopy
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Anderson, Ryan B., Forni, Olivier, Cousin, Agnes, Wiens, Roger C., Clegg, Samuel M., Frydenvang, Jens, Gabriel, Travis S.J., Ollila, Ann, Schröder, Susanne, Beyssac, Olivier, Gibbons, Erin, Vogt, David S., Clavé, Elise, Manrique, Jose-Antonio, Legett, Carey, IV, Pilleri, Paolo, Newell, Raymond T., Sarrao, Joseph, Maurice, Sylvestre, Arana, Gorka, Benzerara, Karim, Bernardi, Pernelle, Bernard, Sylvain, Bousquet, Bruno, Brown, Adrian J., Alvarez-Llamas, César, Chide, Baptiste, Cloutis, Edward, Comellas, Jade, Connell, Stephanie, Dehouck, Erwin, Delapp, Dorothea M., Essunfeld, Ari, Fabre, Cecile, Fouchet, Thierry, Garcia-Florentino, Cristina, García-Gómez, Laura, Gasda, Patrick, Gasnault, Olivier, Hausrath, Elisabeth M., Lanza, Nina L., Laserna, Javier, Lasue, Jeremie, Lopez, Guillermo, Madariaga, Juan Manuel, Mandon, Lucia, Mangold, Nicolas, Meslin, Pierre-Yves, Nelson, Anthony E., Newsom, Horton, Reyes-Newell, Adriana L., Robinson, Scott, Rull, Fernando, Sharma, Shiv, Simon, Justin I., Sobron, Pablo, Fernandez, Imanol Torre, Udry, Arya, Venhaus, Dawn, McLennan, Scott M., Morris, Richard V., and Ehlmann, Bethany
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- 2022
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6. Effects of environmental factors on the monitoring of environmental radioactivity by airborne gamma-ray spectrometry
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Amestoy, Julien, Meslin, Pierre-Yves, Richon, Patrick, Delpuech, Aude, Derrien, Solène, Raynal, Hugo, Pique, Éric, Baratoux, David, Chotard, Pascal, Van Beek, Pieter, Souhaut, Marc, and Zambardi, Thomas
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- 2021
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7. Experimental Wind Characterization with the SuperCam Microphone under a Simulated martian Atmosphere
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Chide, Baptiste, Murdoch, Naomi, Bury, Yannick, Maurice, Sylvestre, Jacob, Xavier, Merrison, Jonathan P., Iversen, Jens J., Meslin, Pierre-Yves, Bassas-Portús, Marti, Cadu, Alexandre, Sournac, Anthony, Dubois, Bruno, Lorenz, Ralph D., Mimoun, David, and Wiens, Roger C.
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- 2021
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8. Recording laser-induced sparks on Mars with the SuperCam microphone
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Chide, Baptiste, Maurice, Sylvestre, Cousin, Agnès, Bousquet, Bruno, Mimoun, David, Beyssac, Olivier, Meslin, Pierre-Yves, and Wiens, Roger C.
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- 2020
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9. Disambiguating the soils of Mars
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Certini, Giacomo, Karunatillake, Suniti, Zhao, Yu-Yan Sara, Meslin, Pierre-Yves, Cousin, Agnes, Hood, Donald R., and Scalenghe, Riccardo
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- 2020
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10. Listening to laser sparks: a link between Laser-Induced Breakdown Spectroscopy, acoustic measurements and crater morphology
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Chide, Baptiste, Maurice, Sylvestre, Murdoch, Naomi, Lasue, Jérémie, Bousquet, Bruno, Jacob, Xavier, Cousin, Agnès, Forni, Olivier, Gasnault, Olivier, Meslin, Pierre-Yves, Fronton, Jean-François, Bassas-Portús, Marti, Cadu, Alexandre, Sournac, Anthony, Mimoun, David, and Wiens, Roger C.
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- 2019
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11. CALOTRITON: a convective boundary layer height estimation algorithm from ultra-high-frequency (UHF) wind profiler data.
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Philibert, Alban, Lothon, Marie, Amestoy, Julien, Meslin, Pierre-Yves, Derrien, Solène, Bezombes, Yannick, Campistron, Bernard, Lohou, Fabienne, Vial, Antoine, Canut-Rocafort, Guylaine, Reuder, Joachim, and Brooke, Jennifer K.
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ATMOSPHERIC boundary layer ,THERMAL boundary layer ,BOUNDARY layer (Aerodynamics) ,CONVECTIVE boundary layer (Meteorology) ,ATMOSPHERIC circulation ,ATMOSPHERIC composition - Abstract
Long time series of observations of atmospheric dynamics and composition are collected at the French Pyrenean Platform for Observation of the Atmosphere (P2OA). Planetary boundary layer depth is a key variable of the climate system, but it remains difficult to estimate and analyse statistically. In order to obtain reliable estimates of the convective boundary layer height (Zi) and to allow long-term series analyses, a new restitution algorithm, named CALOTRITON, has been developed. It is based on the observations of an ultra-high-frequency (UHF) radar wind profiler (RWP) from P2OA with the help of other instruments for evaluation. Estimates of Zi are based on the principle that the top of the convective boundary layer is associated with both a marked inversion and a decrease in turbulence. Those two criteria are respectively manifested by larger RWP reflectivity and smaller vertical-velocity Doppler spectral width. With this in mind, we introduce a new UHF-deduced dimensionless parameter which weighs the air refractive index structure coefficient with the inverse of vertical velocity standard deviation to the power of x. We then search for the most appropriate local maxima of this parameter for Zi estimates with defined criteria and constraints such as temporal continuity. Given that Zi should correspond to fair-weather cloud base height, we use ceilometer data to optimize our choice of the power x and find that x=3 provides the best comparisons. The estimates of Zi by CALOTRITON are evaluated using different Zi estimates deduced from radiosounding according to different definitions. The comparison shows excellent results with a regression coefficient of up to 0.96 and a root-mean-square error of 71 m, which is close to the vertical resolution of the UHF RWP of 75 m, when conditions are optimal. In more complex situations, that is when the atmospheric vertical structure is itself particularly ambiguous, secondary retrievals allow us to identify potential thermal internal boundary layers or residual layers and help to qualify the Zi estimations. Frequent estimate errors are observed nevertheless; for example, when Zi is below the UHF RWP first reliable gate or when the boundary layer begins its transition to a stable nocturnal boundary layer. [ABSTRACT FROM AUTHOR]
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- 2024
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12. Manganese-Iron Phosphate Nodules at the Groken Site, Gale Crater, Mars
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Treiman, Allan H., primary, Lanza, Nina L., additional, VanBommel, Scott, additional, Berger, Jeff, additional, Wiens, Roger, additional, Bristow, Thomas, additional, Johnson, Jeffrey, additional, Rice, Melissa, additional, Hart, Reginald, additional, McAdam, Amy, additional, Gasda, Patrick, additional, Meslin, Pierre-Yves, additional, Yen, Albert, additional, Williams, Amy J., additional, Vasavada, Ashwin, additional, Vaniman, David, additional, Tu, Valerie, additional, Thorpe, Michael, additional, Swanner, Elizabeth D., additional, Seeger, Christina, additional, Schwenzer, Susanne P., additional, Schröder, Susanne, additional, Rampe, Elizabeth, additional, Rapin, William, additional, Ralston, Silas J., additional, Peretyazhko, Tanya, additional, Newsom, Horton, additional, Morris, Richard V., additional, Ming, Douglas, additional, Loche, Matteo, additional, Le Mouélic, Stéphane, additional, House, Christopher, additional, Hazen, Robert, additional, Grotzinger, John P., additional, Gellert, Ralf, additional, Gasnault, Olivier, additional, Fischer, Woodward W., additional, Essunfeld, Ari, additional, Downs, Robert T., additional, Downs, Gordon W., additional, Dehouck, Erwin, additional, Crossey, Laura J., additional, Cousin, Agnes, additional, Comellas, Jade M., additional, Clark, Joanna V., additional, Clark, Benton, additional, Chipera, Steve, additional, Caravaca, Gwenaël, additional, Bridges, John, additional, Blake, David F., additional, and Anderson, Ryan, additional
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- 2023
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13. Background levels of methane in Mars’ atmosphere show strong seasonal variations
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Webster, Christopher R., Mahaffy, Paul R., Atreya, Sushil K., Moores, John E., Flesch, Gregory J., Malespin, Charles, McKay, Christopher P., Martinez, German, Smith, Christina L., Martin-Torres, Javier, Gomez-Elvira, Javier, Zorzano, Maria-Paz, Wong, Michael H., Trainer, Melissa G., Steele, Andrew, Archer, Doug, Sutter, Brad, Coll, Patrice J., Freissinet, Caroline, Meslin, Pierre-Yves, Gough, Raina V., House, Christopher H., Pavlov, Alexander, Eigenbrode, Jennifer L., Glavin, Daniel P., Pearson, John C., Keymeulen, Didier, Christensen, Lance E., Schwenzer, Susanne P., Navarro-Gonzalez, Rafael, Pla-García, Jorge, Rafkin, Scot C. R., Vicente-Retortillo, Álvaro, Kahanpää, Henrik, Viudez-Moreiras, Daniel, Smith, Michael D., Harri, Ari-Matti, Genzer, Maria, Hassler, Donald M., Lemmon, Mark, Crisp, Joy, Sander, Stanley P., Zurek, Richard W., and Vasavada, Ashwin R.
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- 2018
14. The SuperCam Instrument Suite on the NASA Mars 2020 Rover: Body Unit and Combined System Tests
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Wiens, Roger C., Maurice, Sylvestre, Robinson, Scott H., Nelson, Anthony E., Cais, Philippe, Bernardi, Pernelle, Newell, Raymond T., Clegg, Sam, Sharma, Shiv K., Storms, Steven, Deming, Jonathan, Beckman, Darrel, Ollila, Ann M., Gasnault, Olivier, Anderson, Ryan B., André, Yves, Michael Angel, S., Arana, Gorka, Auden, Elizabeth, Beck, Pierre, Becker, Joseph, Benzerara, Karim, Bernard, Sylvain, Beyssac, Olivier, Borges, Louis, Bousquet, Bruno, Boyd, Kerry, Caffrey, Michael, Carlson, Jeffrey, Castro, Kepa, Celis, Jorden, Chide, Baptiste, Clark, Kevin, Cloutis, Edward, Cordoba, Elizabeth C., Cousin, Agnes, Dale, Magdalena, Deflores, Lauren, Delapp, Dorothea, Deleuze, Muriel, Dirmyer, Matthew, Donny, Christophe, Dromart, Gilles, George Duran, M., Egan, Miles, Ervin, Joan, Fabre, Cecile, Fau, Amaury, Fischer, Woodward, Forni, Olivier, Fouchet, Thierry, Fresquez, Reuben, Frydenvang, Jens, Gasway, Denine, Gontijo, Ivair, Grotzinger, John, Jacob, Xavier, Jacquinod, Sophie, Johnson, Jeffrey R., Klisiewicz, Roberta A., Lake, James, Lanza, Nina, Laserna, Javier, Lasue, Jeremie, Le Mouélic, Stéphane, Legett, IV, Carey, Leveille, Richard, Lewin, Eric, Lopez-Reyes, Guillermo, Lorenz, Ralph, Lorigny, Eric, Love, Steven P., Lucero, Briana, Madariaga, Juan Manuel, Madsen, Morten, Madsen, Soren, Mangold, Nicolas, Manrique, Jose Antonio, Martinez, J. P., Martinez-Frias, Jesus, McCabe, Kevin P., McConnochie, Timothy H., McGlown, Justin M., McLennan, Scott M., Melikechi, Noureddine, Meslin, Pierre-Yves, Michel, John M., Mimoun, David, Misra, Anupam, Montagnac, Gilles, Montmessin, Franck, Mousset, Valerie, Murdoch, Naomi, Newsom, Horton, Ott, Logan A., Ousnamer, Zachary R., Pares, Laurent, Parot, Yann, Pawluczyk, Rafal, Glen Peterson, C., Pilleri, Paolo, Pinet, Patrick, Pont, Gabriel, Poulet, Francois, Provost, Cheryl, Quertier, Benjamin, Quinn, Heather, Rapin, William, Reess, Jean-Michel, Regan, Amy H., Reyes-Newell, Adriana L., Romano, Philip J., Royer, Clement, Rull, Fernando, Sandoval, Benigno, Sarrao, Joseph H., Sautter, Violaine, Schoppers, Marcel J., Schröder, Susanne, Seitz, Daniel, Shepherd, Terra, Sobron, Pablo, Dubois, Bruno, Sridhar, Vishnu, Toplis, Michael J., Torre-Fdez, Imanol, Trettel, Ian A., Underwood, Mark, Valdez, Andres, Valdez, Jacob, Venhaus, Dawn, and Willis, Peter
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- 2021
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15. Retrieval of water vapor column abundance and aerosol properties from ChemCam passive sky spectroscopy
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McConnochie, Timothy H., Smith, Michael D., Wolff, Michael J., Bender, Steve, Lemmon, Mark, Wiens, Roger C., Maurice, Sylvestre, Gasnault, Olivier, Lasue, Jeremie, Meslin, Pierre-Yves, Harri, Ari-Matti, Genzer, Maria, Kemppinen, Osku, Martínez, Germán M., DeFlores, Lauren, Blaney, Diana, Johnson, Jeffrey R., and Bell, James F., III
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- 2018
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16. Methane seasonal cycle at Gale Crater on Mars consistent with regolith adsorption and diffusion
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Moores, John E., Gough, Raina V., Martinez, German M., Meslin, Pierre-Yves, Smith, Christina L., Atreya, Sushil K., Mahaffy, Paul R., Newman, Claire E., and Webster, Christopher R.
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- 2019
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17. CALOTRITON: A convective boundary layer height estimation algorithm from UHF wind profiler data
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Philibert, Alban, primary, Lothon, Marie, additional, Amestoy, Julien, additional, Meslin, Pierre-Yves, additional, Derrien, Solène, additional, Bezombes, Yannick, additional, Campistron, Bernard, additional, Lohou, Fabienne, additional, Vial, Antoine, additional, Canut-Rocafort, Guylaine, additional, Reuder, Joachim, additional, and Brooke, Jennifer, additional
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- 2023
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18. Observations of the Perseverance rover at the Jezero crater delta front using the SuperCam instrument
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Mangold, Nicolas, primary, Caravaca, Gwenael, additional, Dehouck, Erwin, additional, Beyssac, Olivier, additional, Beck, Pierre, additional, Clavé, Elise, additional, Cousin, Agnès, additional, Dromart, Gilles, additional, Forni, Olivier, additional, Fouchet, Thierry, additional, Gasnault, Olivier, additional, Gupta, Sanjeev, additional, Le Mouélic, Stéphane, additional, Mandon, Lucia, additional, Maurice, Sylvestre, additional, Meslin, Pierre-Yves, additional, Quantin-Nataf, Cathy, additional, Royer, Clément, additional, and Wiens and SuperCam team, Roger, additional
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- 2023
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19. Observations of the Perseverance rover at the Jezero crater delta front using the SuperCam instrument
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Mangold, Nicolas, Caravaca, Gwénaël, Dehouck, Erwin, Beyssac, Olivier, Beck, Pierre, Clavé, Elise, Cousin, Agnès, Dromart, Gilles, Forni, Olivier, Fouchet, Thierry, Gasnault, Olivier, Gupta, Sanjeev, Le Mouélic, Stéphane, Mandon, Lucia, Maurice, Sylvestre, Meslin, Pierre-Yves, Quantin-Nataf, Cathy, Royer, Clément, Wiens, Roger, Team, The Supercam, Laboratoire de Planétologie et Géosciences [UMR_C 6112] (LPG), Université d'Angers (UA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes université - UFR des Sciences et des Techniques (Nantes univ - UFR ST), Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ), Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Muséum national d'Histoire naturelle (MNHN)-Institut de recherche pour le développement [IRD] : UR206-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Institut de Planétologie et d'Astrophysique de Grenoble (IPAG), Centre National d'Études Spatiales [Toulouse] (CNES)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ), Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France -Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France, Centre d'Etudes Lasers Intenses et Applications (CELIA), Université de Bordeaux (UB)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS), Pôle Planétologie du LESIA, Laboratoire d'études spatiales et d'instrumentation en astrophysique = Laboratory of Space Studies and Instrumentation in Astrophysics (LESIA), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Department of Earth Science and Engineering [Imperial College London], Imperial College London, Division of Geological and Planetary Sciences [Pasadena], California Institute of Technology (CALTECH), Purdue University [West Lafayette], European Geosciences Union, and EGU
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jezero crater ,delta ,[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology ,SuperCam ,[SDU]Sciences of the Universe [physics] ,[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,Mars 2020 ,perseverance ,Mars ,[SDU.STU]Sciences of the Universe [physics]/Earth Sciences - Abstract
International audience; The Perseverance rover landed on the floor of Jezero crater in February 2021. The initial set of images taken from the landing site of the residual butte Kodiak showed a deltaic architecture consistent with a paleolake, but at a level ~100 m lower than expected, suggestive of a closed lake system. After spending ~1 year studying the crater floor, the rover reached the front of the deltaic fan in April 2022. Here, we report observations of the facies, structure and composition of these sedimentary deposits using the SuperCam instrument. SuperCam can take images for texture analysis with the Remote Micro-Imager (RMI), visible and infrared reflectance (VISIR) spectra as well as Raman spectra for mineralogical analysis, and data from laser induced breakdown spectroscopy (LIBS) for chemical analysis. The rover investigated the basal strata of the delta along two traverses at the SE of the delta front. The transition between the crater floor and the delta is not well determined due to regolith and strongly degraded outcrops, and is currently under assessment. The ~20 m thick basal layers that are well-visible on orbital data consist of fine-grained sandstones and siltstones deposited in sub-horizontal planar beds with millimeter thick laminations. These deposits display a substantial alteration highlighted by the detection of both sulfates and phyllosilicates, with exception of local boulders of igneous texture lacking alteration. Texture and composition are both consistent with a quiet regime of deposition such as in lake deposits or distal delta slopes. These beds are considered of topmost importance for sample return and were cored in two locations. Pebbly sandstones and conglomerates with pebbles limited to a few centimeters are observed immediately above these strata. The texture is matrix-supported suggesting an emplacement through gravity sliding or turbidity flows below water rather than fluvial deposition. The composition is more variable than in underlying finer-grained beds and includes local carbonate detections. Uppermost deposits have not been reached by the rover yet, but have been analyzed remotely by RMI images, and VISIR for some of them. They consist of cross-bedded sandstones and conglomerates in all locations of the delta front. The diversity in texture of these deposits suggests a variability in depositional regimes including high-energy floods, either during the lacustrine phase, or subsequently. Boulders present within these layers are rounded suggesting a substantial abrasion by fluvial transport. These boulders are also interesting targets for sampling distant crustal rocks. The top of the delta will be analyzed and sampled along the traverse of the rover in 2023.
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- 2023
20. Detection of Copper by the ChemCam Instrument Along Curiosity's Traverse in Gale Crater, Mars: Elevated Abundances in Glen Torridon
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Goetz, Walter, primary, Dehouck, Erwin, additional, Gasda, Patrick J., additional, Johnson, Jeffrey R., additional, Meslin, Pierre‐Yves, additional, Lanza, Nina L., additional, Wiens, Roger C., additional, Rapin, William, additional, Frydenvang, Jens, additional, Payré, Valerie, additional, and Gasnault, Olivier, additional
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- 2023
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21. Comparison of orbital and Supercam in situ investigation of the floor Units of Jezero crater
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Quantin-Nataf, Cathy, primary, Beyssac, Olivier, additional, Udry, Arya, additional, Mandon, Lucia, additional, Clave, Elise, additional, Benzerara, Karim, additional, Dehouck, Erwin, additional, Poulet, François, additional, Beck, Pierre, additional, LeMouelic, Stephane, additional, Mangold, Nicolas, additional, Cousin, Agnes, additional, Meslin, Pierre Yves, additional, Forni, Olivier, additional, Gasnault, Olivier, additional, Wiens, Roger, additional, and Maurice, Sylvestre, additional
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- 2023
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22. Geochemistry and Mineralogy of Ancient Sedimentary Rocks Analyzed by the SuperCam Instrument in the Jezero Delta, Mars
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Dehouck, Erwin, primary, Forni, Olivier, additional, Quantin-Nataf, Cathy, additional, Beck, Pierre, additional, Mangold, Nicolas, additional, Royer, Clément, additional, Clavé, Elise, additional, Beyssac, Olivier, additional, Johnson, Jeffrey, additional, Mandon, Lucia, additional, Poulet, Francois, additional, Le Mouélic, Stéphane, additional, Caravaca, Gwénaël, additional, Kalucha, Hemani, additional, Gibbons, Erin, additional, Dromart, Gilles, additional, Gasda, Patrick, additional, Meslin, Pierre-Yves, additional, Williams, Amy, additional, Schroeder, Susanne, additional, Udry, Arya, additional, Anderson, Ryan, additional, Clegg, Sam, additional, Cousin, Agnes, additional, Gabriel, Travis, additional, Lasue, Jérémie, additional, Fouchet, Thierry, additional, Pilleri, Paolo, additional, Pilorget, Cédric, additional, Hurowitz, Joel, additional, Núñez, Jorge, additional, Russell, Patrick, additional, Simon, Justin, additional, Maurice, Sylvestre, additional, and Wiens, Roger, additional
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- 2023
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23. Investigation of the petrogenetic relationship between the two igneous formations in Jezero crater by using trace element concentrations acquired by the Perseverance SuperCam instrument
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Debaille, Vinciane, primary, Forni, Olivier, additional, Anderson, Ryan, additional, Beck, Pierre, additional, Beyssac, Olivier, additional, Clavé, Elise, additional, Clegg, Sam, additional, Cousin, Agnes, additional, Dehouck, Erwin, additional, Fouchet, Thierry, additional, Gabriel, Travis, additional, Johnson, Jeffrey, additional, Le Mouélic, Stéphane, additional, Mandon, Lucia, additional, Maurice, Sylvestre, additional, Meslin, Pierre-Yves, additional, Pilleri, Paolo, additional, Poulet, Francois, additional, Quantin-Nataf, Cathy, additional, Royer, Clément, additional, Udry, Arya, additional, and Wiens, Roger, additional
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- 2023
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24. Magmatic complexity on early Mars as seen through a combination of orbital, in-situ and meteorite data
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Sautter, Violaine, Toplis, Michael J., Beck, Pierre, Mangold, Nicolas, Wiens, Roger, Pinet, Patrick, Cousin, Agnes, Maurice, Sylvestre, LeDeit, Laetitia, Hewins, Roger, Gasnault, Olivier, Quantin, Cathy, Forni, Olivier, Newsom, Horton, Meslin, Pierre-Yves, Wray, James, Bridges, Nathan, Payré, Valérie, Rapin, William, and Le Mouélic, Stéphane
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- 2016
- Full Text
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25. A JOURNEY ACROSS THE TRANSITION BETWEEN THE IGNEOUS SÉÍTAH FLOOR UNIT AND THE DELTA WITH THE MARS2020 SUPERCAM INSTRUMENT AT JEZERO CRATER, MARS
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Beyssac, Olivier, Clavé, Elise, Dehouck, Erwin, Forni, Olivier, Udry, Arya, Beck, Pierre, Cousin, Agnès, Mangold, Nicolas, Quantin-Nataf, Cathy, Royer, Clément, Mandon, Lucia, Johnson, Jeffrey, Simon, Justin I., Meslin, Pierre-Yves, Fouchet, Thierry, Le Mouélic, Stéphane, Pilorget, Cédric, Caravaca, Gwénaël, Poulet, François, Lasue, Jérémie, Pilleri, Paolo, M. Ollila, Ann, Clegg, Samuel, Núñez, Jorge, Maurice, Sylvestre, Wiens, Roger, Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Muséum national d'Histoire naturelle (MNHN)-Institut de recherche pour le développement [IRD] : UR206-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Centre d'Etudes Lasers Intenses et Applications (CELIA), Université de Bordeaux (UB)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), University of Nevada [Las Vegas] (WGU Nevada), Institut de Planétologie et d'Astrophysique de Grenoble (IPAG), Centre National d'Études Spatiales [Toulouse] (CNES)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ), Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France -Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France, Laboratoire de Planétologie et Géosciences [UMR_C 6112] (LPG), Université d'Angers (UA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes université - UFR des Sciences et des Techniques (Nantes univ - UFR ST), Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ), Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, Division of Geological and Planetary Sciences [Pasadena], California Institute of Technology (CALTECH), Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), NASA Johnson Space Center (JSC), NASA, Laboratoire d'études spatiales et d'instrumentation en astrophysique = Laboratory of Space Studies and Instrumentation in Astrophysics (LESIA), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Institut d'astrophysique spatiale (IAS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Centre National d’Études Spatiales [Paris] (CNES), Los Alamos National Laboratory (LANL), and Lunar and Planetary Institute
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Jezero crater ,[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology ,SuperCam ,[SDU]Sciences of the Universe [physics] ,[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,Mars 2020 ,seitah ,[SDU.STU]Sciences of the Universe [physics]/Earth Sciences ,mars ,mineralogy - Abstract
International audience; During the first scientific campaign, Perseverance explored the Jezero crater floor and found two main igneous formations: the basaltic Máaz unit, and Séítah, consisting of an olivine-rich cumulate. Then the rover did a rapid traverse towards the second campaign region, Jezero’s delta. Just before reaching the lowest part of the delta, Perseverance encountered the Séítah formation again, with some variability in the degree of alteration. Here, we use the data obtained by the SuperCam instrument to document the structure and texture of rocks at the transition between Séítah and the delta front, its geochemistry and its primary and secondary mineralogy. Then, we discuss the simi-larities/differences between these rocks and discuss a geological scenario to account for these observations.
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- 2023
26. THE FIRST FROST DETECTION CAMPAIGN BY THE MARS 2020 PERSEVERANCE ROVER: IMPLEMENTATION AND RESULTS
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Martínez, Germán, Lasue, Jérémie, Meslin, Pierre-Yves, Chide, Baptiste, Caravaca, Gwénaël, López-Reyes, Guillermo, Tamppari, Leslie K., Beyssac, Olivier, Polkko, J., Hieta, M., Genzer, M., Harri, A.-M., Newman, Claire, Gillespie, Hartzel, Fischer, Erik, Mora, Luis, Sebastián, Eduardo, Wiens, Roger, Rodríguez Manfredi, Jose, Lunar and Planetary Institute [Houston] (LPI), Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Los Alamos National Laboratory (LANL), Universidad de Valladolid [Valladolid] (UVa), Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Muséum national d'Histoire naturelle (MNHN)-Institut de recherche pour le développement [IRD] : UR206-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Finnish Meteorological Institute (FMI), Aeolis Research, University of Michigan [Ann Arbor], University of Michigan System, Centro de Astrobiologia [Madrid] (CAB), Instituto Nacional de Técnica Aeroespacial (INTA)-Consejo Superior de Investigaciones Científicas [Madrid] (CSIC), Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, and Lunar and Planetary Institute
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Jezero crater ,[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology ,SuperCam ,[SDU]Sciences of the Universe [physics] ,[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,Mars 2020 ,Mars ,[SDU.STU]Sciences of the Universe [physics]/Earth Sciences ,frost - Abstract
International audience; Here we describe the first campaign launched by the Perseverance rover to detect frost during the first Martian year of operations (669 sols as of Jan 5, 2023). This campaign was conceived, developed and executed following lessons learnt from the Mars Science Laboratory Mission, where frost was likely detected [1].Between sols 546 and 548 during northern winter (Ls ~297), measurements of ground temperature and relative humidity by the Mars Environmental Dynamics Analyzer (MEDA, [2]) were used to predict frost formation, while SuperCam laser-induced breakdown spectroscopy (LIBS) and Raman spectrometer measurements [3,4] were used to detect frost formation on a target informally called Snowy Mountain. While the measured ground temperature fell below the estimated frost point, and therefore frost was predicted by MEDA, neither H enrichment in LIBS measurements nor Raman peaks associated with water ice were detected by SuperCam.
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- 2023
27. OVERVIEW OF THE BEDROCK GEOCHEMISTRY AND MINERALOGY OBSERVED BY SUPERCAM DURING PERSEVERANCE'S DELTA FRONT CAMPAIGN
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Dehouck, Erwin, Forni, Olivier, Quantin-Nataf, Cathy, Beck, Pierre, Mangold, Nicolas, Royer, Clément, Clavé, Elise, Beyssac, Olivier, Johnson, Jeffrey, Mandon, Lucia, Poulet, François, Le Mouélic, Stéphane, Caravaca, Gwénaël, Kalucha, Hemani, Gibbons, Erin, Dromart, Gilles, Gasda, Patrick, Meslin, Pierre-Yves, Schroeder, Susanne, Udry, Arya, Anderson, Ryan B., Clegg, Samuel, Cousin, Agnès, Gabriel, Travis, Lasue, Jérémie, Fouchet, Thierry, Pilleri, Paolo, Pilorget, Cédric, Hurowitz, Joel, Núñez, Jorge, Williams, Amy, Russell, Patrick, Simon, Justin I., Maurice, Sylvestre, Wiens, Roger, Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Institut de Planétologie et d'Astrophysique de Grenoble (IPAG), Centre National d'Études Spatiales [Toulouse] (CNES)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ), Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France -Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France, Laboratoire de Planétologie et Géosciences [UMR_C 6112] (LPG), Université d'Angers (UA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes université - UFR des Sciences et des Techniques (Nantes univ - UFR ST), Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ), Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, Centre d'Etudes Lasers Intenses et Applications (CELIA), Université de Bordeaux (UB)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS), Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Muséum national d'Histoire naturelle (MNHN)-Institut de recherche pour le développement [IRD] : UR206-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), Division of Geological and Planetary Sciences [Pasadena], California Institute of Technology (CALTECH), Institut d'astrophysique spatiale (IAS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Centre National d’Études Spatiales [Paris] (CNES), McGill University = Université McGill [Montréal, Canada], Los Alamos National Laboratory (LANL), Deutsches Zentrum für Luft- und Raumfahrt [Berlin] (DLR), University of Nevada [Las Vegas] (WGU Nevada), US Geological Survey [Flagstaff], United States Geological Survey [Reston] (USGS), United States Geological Survey (USGS), Laboratoire d'études spatiales et d'instrumentation en astrophysique = Laboratory of Space Studies and Instrumentation in Astrophysics (LESIA), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Stony Brook University [SUNY] (SBU), State University of New York (SUNY), Department of Geological Sciences [Gainesville] (UF|Geological), University of Florida [Gainesville] (UF), Department of Earth, Planetary and Space Sciences [Los Angeles] (EPSS), University of California [Los Angeles] (UCLA), University of California (UC)-University of California (UC), NASA Johnson Space Center (JSC), NASA, and Lunar and Planetary Institute
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jezero crater ,[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology ,[SDU]Sciences of the Universe [physics] ,[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,Mars 2020 ,[SDU.STU]Sciences of the Universe [physics]/Earth Sciences ,mars ,delta front ,geochemistry - Abstract
International audience; In February 2021, the Perseverance rover landed in Jezero crater, Mars. The crater floor was found to be composed of lava flows and cumulate rocks [1-5]. These magmatic rocks appear to have undergone some limited aqueous alteration; however, it is not clear whether this alteration is related to the lacustrine phase of the crater [1,3,6,7].After completing its exploration of the crater floor, Perseverance reached the foot of the Jezero western fan in late April 2022 (sol ~422). Long-distance images acquired earlier in the mission had already confirmed the deltaic nature of the fan [8], which had long been suspected from orbital observations [9,10]. Between April and December 2022, Perseverance investigated the basal layers of the delta at two locations named Hawksbill Gap and Cape Nukshak, which are ~400 m apart [11]. Here, we present an overview of the geo-chemistry and mineralogy of the delta rocks as observed by SuperCam, and show that these rocks record a diver-sity of past aqueous alteration environments.
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- 2023
28. Light-toned veins and material in Jezero crater, Mars, as seen in-situ via NASA's Perseverance rover (Mars 2020 mission): stratigraphic distribution and compositional results from the supercam instrument
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Nachon, Marion, López-Reyes, Guillermo, Meslin, Pierre-Yves, M. Ollila, Ann, Mandon, Lucia, Clavé, Elise, Forni, Olivier, Maurice, Sylvestre, Wiens, Roger, Gasnault, Olivier, Quantin-Nataf, Cathy, Mangold, Nicolas, Clegg, Samuel, Cousin, Agnès, Lasue, Jérémie, Dehouck, Erwin, Pilleri, Paolo, Team, The Supercam, Bell III, J.F., Horgan, Briony, Núñez, Jorge, Stack‐Morgan, Katie, Tebolt, Michelle, Caravaca, Gwénaël, Gupta, Sanjeev, Calef, Fred J., Crumpler, Larry, Siljeström, Sandra, Russell, Patrick, Williams, Amy, Shuster, David L., Rice, James, Brown, Adrian, Holm-Alwmark, Sanna, Kanine, Oak, Texas A&M University [College Station], Universidad de Valladolid [Valladolid] (UVa), Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Los Alamos National Laboratory (LANL), Division of Geological and Planetary Sciences [Pasadena], California Institute of Technology (CALTECH), Centre d'Etudes Lasers Intenses et Applications (CELIA), Université de Bordeaux (UB)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS), Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie et Géosciences [UMR_C 6112] (LPG), Université d'Angers (UA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes université - UFR des Sciences et des Techniques (Nantes univ - UFR ST), Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ), Arizona State University [Tempe] (ASU), Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), Department of Geological Sciences [Austin], Jackson School of Geosciences (JSG), University of Texas at Austin [Austin]-University of Texas at Austin [Austin], Department of Earth Science and Engineering [Imperial College London], Imperial College London, New Mexico Museum of Natural History and Science (NMMNHS), RISE Research Institutes of Sweden, Department of Earth, Planetary and Space Sciences [Los Angeles] (EPSS), University of California [Los Angeles] (UCLA), University of California (UC)-University of California (UC), Department of Geological Sciences [Gainesville] (UF|Geological), University of Florida [Gainesville] (UF), Berkeley Geochronology Center (BGC), School of Earth and Space Exploration [Tempe] (SESE), NASA Headquarters, Plancius Research LLC, University of Copenhagen = Københavns Universitet (UCPH), and Lunar and Planetary Institute
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Jezero crater ,[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology ,[SDU]Sciences of the Universe [physics] ,Mars 2020 ,[SDU.ASTR.EP]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP] ,sedimentology ,veins ,diagenesis - Abstract
International audience; Within Jezero crater, the Perseverance rover currently explores the lowermost-exposed scarp of the delta (Fig. 1) [1,2]. Here we: (1) present the distribution of light-toned veins currently observed via the rover along its route in Jezero crater; (2) introduce compositional results of veins as analyzed via Perseverance’s SuperCam instrument, and place them into the context of results from the other instruments.
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- 2023
29. Understanding the signature of rock coatings in laser-induced breakdown spectroscopy data
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Lanza, Nina L., Ollila, Ann M., Cousin, Agnes, Wiens, Roger C., Clegg, Samuel, Mangold, Nicolas, Bridges, Nathan, Cooper, Daniel, Schmidt, Mariek, Berger, Jeffrey, Arvidson, Raymond, Melikechi, Noureddine, Newsom, Horton E., Tokar, Robert, Hardgrove, Craig, Mezzacappa, Alissa, Jackson, Ryan S., Clark, Benton, Forni, Olivier, Maurice, Sylvestre, Nachon, Marion, Anderson, Ryan B., Blank, Jennifer, Deans, Matthew, Delapp, Dorothea, Léveillé, Richard, McInroy, Rhonda, Martinez, Ronald, Meslin, Pierre-Yves, and Pinet, Patrick
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- 2015
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30. Overview of the Morphology and Chemistry of Diagenetic Features in the Clay‐Rich Glen Torridon Unit of Gale Crater, Mars
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Gasda, Patrick J., primary, Comellas, Jade, additional, Essunfeld, Ari, additional, Das, Debarati, additional, Bryk, Alexander B., additional, Dehouck, Erwin, additional, Schwenzer, Susanne P., additional, Crossey, Laura, additional, Herkenhoff, Kenneth, additional, Johnson, Jeffrey R., additional, Newsom, Horton, additional, Lanza, Nina L., additional, Rapin, William, additional, Goetz, Walter, additional, Meslin, Pierre‐Yves, additional, Bridges, John C., additional, Anderson, Ryan, additional, David, Gael, additional, Turner, Stuart M. R., additional, Thorpe, Michael T., additional, Kah, Linda, additional, Frydenvang, Jens, additional, Kronyak, Rachel, additional, Caravaca, Gwénaël, additional, Ollila, Ann, additional, Le Mouélic, Stéphane, additional, Nellessen, Matthew, additional, Hoffman, Megan, additional, Fey, Deirdra, additional, Cousin, Anges, additional, Wiens, Roger C., additional, Clegg, Samuel M., additional, Maurice, Sylvestre, additional, Gasnault, Olivier, additional, Delapp, Dorothea, additional, and Reyes‐Newell, Adriana, additional
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- 2022
- Full Text
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31. Bedrock Geochemistry and Alteration History of the Clay‐Bearing Glen Torridon Region of Gale Crater, Mars
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Dehouck, Erwin, primary, Cousin, Agnès, additional, Mangold, Nicolas, additional, Frydenvang, Jens, additional, Gasnault, Olivier, additional, Forni, Olivier, additional, Rapin, William, additional, Gasda, Patrick J., additional, Caravaca, Gwénaël, additional, David, Gaël, additional, Bedford, Candice C., additional, Lasue, Jérémie, additional, Meslin, Pierre‐Yves, additional, Rammelkamp, Kristin, additional, Desjardins, Marine, additional, Le Mouélic, Stéphane, additional, Thorpe, Michael T., additional, Fox, Valerie K., additional, Bennett, Kristen A., additional, Bryk, Alexander B., additional, Lanza, Nina L., additional, Maurice, Sylvestre, additional, and Wiens, Roger C., additional
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- 2022
- Full Text
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32. Early Mars sub-aerial environments conducive to prebiotic evolution
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Rapin, William, primary, Dromart, Gilles, additional, Clark, Benton, additional, Schieber, Jürgen, additional, Kite, Edwin, additional, Kah, Linda, additional, Thompson, Lucy, additional, Gasnault, Olivier, additional, Lasue, Jérémie, additional, Meslin, Pierre-Yves, additional, Gasda, Patrick, additional, and Lanza, Nina, additional
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- 2022
- Full Text
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33. Jezero Crater Floor and Delta Chemistry and Mineralogy Observed by SuperCam in the First 1.5 Years of the Perseverance Rover Mission
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Wiens, Roger, Maurice, Sylvestre, Clegg, Samuel, Cousin, Agnès, Dehouck, Erwin, Udry, Arya, Beyssac, Olivier, Quantin-Nataf, Cathy, Mangold, Nicolas, Mandon, Lucia, Forni, Olivier, Benzerara, Karim, Johnson, Jeffrey Roy, Anderson, Ryan, Gasda, Patrick, Royer, Clément, Madariaga, Juan Manuel, Pinedo, Kepa Castro Ortiz De, Arana, Gorka, Meslin, Pierre-Yves, Ollila, Ann, Legett, Carey, Poulet, François, Sharma, Shiv, Comellas, Jade, Chide, Baptiste, Acosta-Maeda, Tayro, Clave, Elise, Hausrath, Elisabeth, Simon, Justin, Bosak, Tanja, Brown, Adrian, Laserna, Javier, Alvarez, César, Lasue, Jérémie, Cloutis, Edward, Caravaca, Gwénaël, Connell, Stephanie, Wolf, Uriah, Sidhu, Sahejpal, Turenne, Nathalie, Ostwald, Amanda, Mouélic, Stéphane Le, Lopez-Reyes, Guillermo, Manrique, José, Veneranda, Marco, Pilleri, Paolo, Fouchet, Thierry, Pilorget, Cédric, Gabriel, Travis, Gibbons, Erin, Lanza, Nina, Larmat, Carene, Horgan, Briony, Nachon, Marion, Rapin, William, Manelski, Henry, Martinez-Frias, Jesus, Pinet, Patrick, Los Alamos National Laboratory (LANL), Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), University of Nevada [Las Vegas] (WGU Nevada), Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Muséum national d'Histoire naturelle (MNHN)-Institut de recherche pour le développement [IRD] : UR206-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie et Géosciences [UMR_C 6112] (LPG), Université d'Angers (UA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes université - UFR des Sciences et des Techniques (Nantes univ - UFR ST), Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ), Laboratoire d'études spatiales et d'instrumentation en astrophysique = Laboratory of Space Studies and Instrumentation in Astrophysics (LESIA), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Muséum national d'Histoire naturelle (MNHN)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut de recherche pour le développement [IRD] : UR206-Centre National de la Recherche Scientifique (CNRS), Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), United States Geological Survey (USGS), University of the Basque Country/Euskal Herriko Unibertsitatea (UPV/EHU), Institut d'astrophysique spatiale (IAS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Centre National d’Études Spatiales [Paris] (CNES), University of Hawaii, University of Hawai‘i [Mānoa] (UHM), Centre d'Etudes Lasers Intenses et Applications (CELIA), Université de Bordeaux (UB)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS), NASA Johnson Space Center (JSC), NASA, Department of Earth, Atmospheric and Planetary Sciences [MIT, Cambridge] (EAPS), Massachusetts Institute of Technology (MIT), NASA Headquarters, Plancius Research LLC, Universidad de Málaga [Málaga] = University of Málaga [Málaga], University of Winnipeg, Universidad de Valladolid [Valladolid] (UVa), Astrogeology Science Center [Flagstaff], United States Geological Survey [Reston] (USGS), McGill University = Université McGill [Montréal, Canada], Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, Texas A&M University [Galveston], Purdue University [West Lafayette], Instituto de Geociencias [Madrid] (IGEO), Universidad Complutense de Madrid = Complutense University of Madrid [Madrid] (UCM)-Consejo Superior de Investigaciones Científicas [Madrid] (CSIC), and American Geophysical Union
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Jezero crater ,[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology ,SuperCam ,[SDU]Sciences of the Universe [physics] ,[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,Mars 2020 ,sedimentology ,[SDU.STU]Sciences of the Universe [physics]/Earth Sciences ,mineralogy ,geochemistry ,petrography - Abstract
International audience; Jezero crater was chosen for exploration and sample collection by Perseverance due to its history as a lake with river deltas, its diverse mineralogy, including carbonates observed from orbit, and as a potential site to calibrate crater counting ages with radiometric dates of samples to be returned to Earth. This presentation focuses on the results of SuperCam, which uses LIBS for remote elemental chemistry, VISIR and remote Raman spectroscopy for mineral compositions and alteration, includes a microphone, and performs high-resolution imaging for textures and morphology. In the first year after landing, SuperCam and other instruments were used to explore Jezero’s floor. We found that all of the floor units are igneous, with lava flows comprising the upper units as part of the Máaz formation, while the lower formation, Séítah, is an olivine cumulate, produced by gravitational settling of olivine crystals in a large melt body. Artuby ridge, just outside the SW portion of Séítah and stratigraphically just above it, contains up to 60% pyroxene. The upper portions of the Máaz formation are more enriched in plagioclase, with the uppermost Ch’al member having the most evolved composition, along with the Content member, pitted rocks directly overlying the main cumulate portion of Séítah. After exploring the floor, Perseverance drove to the delta formation and began a walk-about style of observations starting at Enchanted Lake, just below an arm of the delta formation, and then moving into Hawksbill Gap, climbing 18 m in elevation between Devil’s Tanyard, Sunset Hill, and Hogwallow flats. Delta compositions initially displayed higher phyllosilicate contents, identified by absorptions at 1.4, 1.9, and 2.3 µm, and by higher LIBS H peak areas. Farther up, compositions changed to sulfur-bearing in lower locations within the continuous fine-grained light-toned strata (e.g., Pignut Mountain, Sol 463) and carbonate-rich in upper strata. Veins were observed, consisting of Mg-Fe carbonate (Elder Ridge, Sol 459) and anhydrite (Reid’s Gap, Sol 466). The sulfates suggest precipitation of these salts at a later stage, as the lake was evaporating. Carbonates and sulfates in veins in different locations indicate that groundwater was active in the lithified sediments and had significantly different chemistry at different intervals.
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- 2022
34. Mars methane detection and variability at Gale crater
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the MSL Science Team, Webster, Christopher R., Mahaffy, Paul R., Atreya, Sushil K., Flesch, Gregory J., Mischna, Michael A., Meslin, Pierre-Yves, Farley, Kenneth A., Conrad, Pamela G., Christensen, Lance E., Pavlov, Alexander A., Martín-Torres, Javier, Zorzano, María-Paz, McConnochie, Timothy H., Owen, Tobias, Eigenbrode, Jennifer L., Glavin, Daniel P., Steele, Andrew, Malespin, Charles A., Archer, P. Douglas, Sutter, Brad, Coll, Patrice, Freissinet, Caroline, McKay, Christopher P., Moores, John E., Schwenzer, Susanne P., Bridges, John C., Navarro-Gonzalez, Rafael, Gellert, Ralf, and Lemmon, Mark T.
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- 2015
35. Formation and destruction of clay minerals in Glen Torridon, Gale crater, Mars
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Dehouck, Erwin, Cousin, Agnès, Mangold, Nicolas, Frydenvang, Jens, Gasnault, Olivier, Forni, Olivier, Rapin, William, Gasda, Patrick, Caravaca, Gwénaël, David, Gaël, Bedford, Candice, Lasue, Jérémie, Meslin, Pierre-Yves, Rammelkamp, Kristin, Desjardin, Marine, Le Mouélic, Stéphane, Thorpe, Michael, Fox, Valerie, Bennett, Kristen, Bryk, Alexander, Lanza, Nina, Maurice, Sylvestre, Wiens, Roger, Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie et Géosciences [UMR_C 6112] (LPG), Université d'Angers (UA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes université - UFR des Sciences et des Techniques (Nantes univ - UFR ST), Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ), University of Copenhagen = Københavns Universitet (UCPH), Los Alamos National Laboratory (LANL), Lunar and Planetary Institute [Houston] (LPI), UniLaSalle, NASA Johnson Space Center (JSC), NASA, University of Minnesota [Twin Cities] (UMN), University of Minnesota System, Astrogeology Science Center [Flagstaff], United States Geological Survey [Reston] (USGS), Department of Earth and Planetary Science [UC Berkeley] (EPS), University of California [Berkeley] (UC Berkeley), and University of California (UC)-University of California (UC)
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[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology ,[SDU]Sciences of the Universe [physics] ,[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy ,[SDU.STU]Sciences of the Universe [physics]/Earth Sciences - Abstract
International audience; From 2019 to 2021, the Curiosity rover explored the Glen Torridon (GT) region, a topographic troughlocated on the slope of Aeolis Mons, the central mound of Gale crater. GT corresponds to what was previously referred toas the “clay-bearing unit”, due to the detection of smectite signatures by orbital spectro-imagers. One of the objectives ofthis campaign was to better understand the context of formation of the clay minerals, as well as the overall alterationhistory of GT.Here, we used the ChemCam instrument to survey the major-element composition of the bedrock throughout the region.Overall, the GT bedrock is characterized by elevated values of the Chemical Index of Alteration (CIA), which indicatesthat the clay minerals were formed in a context of open-system weathering, i.e., through the interaction of the sediments(or their source rocks) with dilute meteoric fluids at relatively high water-to-rock ratio. We also observed geochemicalvariations correlated with outcrop expression – for example, in the northern part of GT, the spatially dominant type ofbedrock has a distinctive “rubbly” appearance and displays enrichments in both K2O and SiO2, which are best explainedby the presence of illite or a mixed-layer illite/smectite phase.Finally, in the southern part GT, in an area of lighter-toned rocks named the Hutton interval, we found significantly lowerCIA values that are correlated with reduced abundances of clay minerals. We interpret these “anomalous” compositionsas a local diagenetic overprint, and propose that the clay minerals of the Hutton interval have been partially destroyed bythe circulation of concentrated fluids late in the history of Gale.
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- 2022
36. On the occurrence of Jahnsite/Whiteite phases on Mars: a thermodynamic study
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Drouet, Christophe, primary, Loche, Matteo, additional, Fabre, Sébastien, additional, and Meslin, Pierre-Yves, additional
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- 2022
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37. Time-resolved Raman and luminescence spectroscopy of synthetic REE-doped hydroxylapatites and natural apatites
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Fau, Amaury, primary, Beyssac, Olivier, additional, Gauthier, Michel, additional, Panczer, Gérard, additional, Gasnault, Olivier, additional, Meslin, Pierre-Yves, additional, Bernard, Sylvain, additional, Maurice, Sylvestre, additional, Forni, Olivier, additional, Boulliard, Jean-Claude, additional, Bosc, Françoise, additional, and Drouet, Christophe, additional
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- 2022
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38. CALOTRITON: A convective boundary layer height estimation algorithm from UHF wind profiler data.
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Philibert, Alban, Lothon, Marie, Amestoy, Julien, Meslin, Pierre-Yves, Derrien, Solène, Bezombes, Yannick, Campistron, Bernard, Lohou, Fabienne, Vial, Antoine, Canut-Rocafort, Guylaine, Reuder, Joachim, and Brooke, Jennifer
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CONVECTIVE boundary layer (Meteorology) ,ATMOSPHERIC boundary layer ,THERMAL boundary layer ,BOUNDARY layer (Aerodynamics) ,STANDARD deviations ,ATMOSPHERIC circulation - Abstract
Long series of observation of the atmospheric dynamics and composition are collected at the French Pyrenean Platform for the Observation of the Atmosphere (P2OA). Planetary boundary layer depth is a key variable of the climate system, but it remains difficult to estimate and analyse statistically by use of long series. In order to obtain reliable estimates of the convective boundary layer height (Zi) and to allow long-term series analyses, a new restitution algorithm, named CALOTRITON, has been developed, based on the observations of a Ultra High Frequency (UHF) wind profiler radar from P2OA, with the help of other instruments for evaluation. Zi estimates are based on the principle that the top of the convective boundary layer is associated with both a marked inversion and a decrease of turbulence. Those two criteria are respectively manifested by larger radar reflectivity and smaller vertical velocity Doppler spectral width. With this in mind, we introduce a new UHF- deduced dimensionless parameter which weights the air refractive index coefficient with the inverse of vertical velocity standard deviation to the power x. We then search for the most appropriate local maxima of this parameter for Zi estimates, with defined criteria and constraints, like temporal continuity. Given that Zi should correspond to fair weather cloud base height, we use ceilometer data to optimize our choice of the power x, and find that x = 3 gives the best comparisons/results. The estimates of Zi by CALOTRITON are evaluated using different Zi estimates deduced from radiosounding, according to different definitions. The comparison shows excellent results with a regression coefficient of up to 0.96 and a root mean square error of 80 m, close to the vertical resolution of the UHF of 75 m, when conditions are optimal. In more complex situations, that is when the atmospheric vertical structure is itself particularly ambiguous, secondary retrievals allow us to identify potential thermal internal boundary layers or residual layers, and help to qualify the Zi estimations. Frequent estimate errors are nevertheless observed when Zi is below the UHF first reliable gate, but also at the end of the day, when the boundary layer begins its transition to a stable nighttime boundary layer. [ABSTRACT FROM AUTHOR]
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- 2023
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39. Compositionally and density stratified igneous terrain in Jezero crater, Mars
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Wiens, Roger C., Udry, Arya, Beyssac, Olivier, Quantin-Nataf, Cathy, Mangold, Nicolas, Cousin, Agnès, Mandon, Lucia, Bosak, Tanja, Forni, Olivier, McLennan, Scott M., Sautter, Violaine, Brown, Adrian, Benzerara, Karim, Johnson, Jeffrey R., Mayhew, Lisa, Maurice, Sylvestre, Anderson, Ryan B., Clegg, Samuel M., Crumpler, Larry, Gabriel, Travis S. J., Gasda, Patrick, Hall, James, Horgan, Briony H. N., Kah, Linda, Legett, Carey, Madariaga, Juan Manuel, Meslin, Pierre-Yves, Ollila, Ann M., Poulet, Francois, Royer, Clement, Sharma, Shiv K., Siljeström, Sandra, Simon, Justin I., Acosta-Maeda, Tayro E., Alvarez-Llamas, Cesar, Angel, S. Michael, Arana, Gorka, Beck, Pierre, Bernard, Sylvain, Bertrand, Tanguy, Bousquet, Bruno, Castro, Kepa, Chide, Baptiste, Clavé, Elise, Cloutis, Ed, Connell, Stephanie, Dehouck, Erwin, Dromart, Gilles, Fischer, Woodward, Fouchet, Thierry, Francis, Raymond, Frydenvang, Jens, Gasnault, Olivier, Gibbons, Erin, Gupta, Sanjeev, Hausrath, Elisabeth M., Jacob, Xavier, Kalucha, Hemani, Kelly, Evan, Knutsen, Elise, Lanza, Nina, Laserna, Javier, Lasue, Jeremie, Le Mouélic, Stéphane, Leveille, Richard, Lopez Reyes, Guillermo, Lorenz, Ralph, Manrique, Jose Antonio, Martinez-Frias, Jesus, McConnochie, Tim, Melikechi, Noureddine, Mimoun, David, Montmessin, Franck, Moros, Javier, Murdoch, Naomi, Pilleri, Paolo, Pilorget, Cedric, Pinet, Patrick, Rapin, William, Rull, Fernando, Schröder, Susanne, Shuster, David L., Smith, Rebecca J., Stott, Alexander E., Tarnas, Jesse, Turenne, Nathalie, Veneranda, Marco, Vogt, David S., Weiss, Benjamin P., Willis, Peter, Stack, Kathryn M., Williford, Kenneth H., Farley, Kenneth A., Los Alamos National Laboratory (LANL), University of Nevada [Las Vegas] (WGU Nevada), Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Muséum national d'Histoire naturelle (MNHN)-Institut de recherche pour le développement [IRD] : UR206-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement (LGL-TPE), École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Université Jean Monnet - Saint-Étienne (UJM)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie et Géosciences [UMR_C 6112] (LPG), Université d'Angers (UA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes université - UFR des Sciences et des Techniques (Nantes univ - UFR ST), Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ), Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Laboratoire d'études spatiales et d'instrumentation en astrophysique = Laboratory of Space Studies and Instrumentation in Astrophysics (LESIA), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Department of Earth, Atmospheric and Planetary Sciences [MIT, Cambridge] (EAPS), Massachusetts Institute of Technology (MIT), Stony Brook University [SUNY] (SBU), State University of New York (SUNY), Plancius Research LLC, Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), Department of Geological Sciences [Boulder], University of Colorado [Boulder], Astrogeology Science Center [Flagstaff], United States Geological Survey [Reston] (USGS), New Mexico Museum of Natural History and Science (NMMNHS), Department of Earth, Atmospheric, and Planetary Sciences [West Lafayette] (EAPS), Purdue University [West Lafayette], Department of Earth and Planetary Sciences [Knoxville], The University of Tennessee [Knoxville], University of the Basque Country/Euskal Herriko Unibertsitatea (UPV/EHU), Institut d'astrophysique spatiale (IAS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Centre National d’Études Spatiales [Paris] (CNES), University of Hawai'i [Honolulu] (UH), RISE Research Institutes of Sweden, Center for Isotope Cosmochemistry and Geochronology, NASA Johnson Space, Universidad de Málaga [Málaga] = University of Málaga [Málaga], Department of Chemistry and Biochemistry [Columbia, South Carolina], University of South Carolina [Columbia], Institut de Planétologie et d'Astrophysique de Grenoble (IPAG), Centre National d'Études Spatiales [Toulouse] (CNES)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ), Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France -Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France, Centre d'Etudes Lasers Intenses et Applications (CELIA), Université de Bordeaux (UB)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS), University of Winnipeg, California Institute of Technology (CALTECH), Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), University of Copenhagen = Københavns Universitet (UCPH), McGill University = Université McGill [Montréal, Canada], Department of Earth Science and Engineering [Imperial College London], Imperial College London, Institut de mécanique des fluides de Toulouse (IMFT), Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP), Université de Toulouse (UT), PLANETO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Universidad de Valladolid [Valladolid] (UVa), Consejo Superior de Investigaciones Científicas [Madrid] (CSIC), University of Maryland [College Park], University of Maryland System, Department of Physics and Applied Physics [Lowell], University of Massachusetts [Lowell] (UMass Lowell), University of Massachusetts System (UMASS)-University of Massachusetts System (UMASS), Institut Supérieur de l'Aéronautique et de l'Espace (ISAE-SUPAERO), DLR Institute of Optical Sensor Systems, Deutsches Zentrum für Luft- und Raumfahrt [Berlin] (DLR), Department of Earth and Planetary Science [UC Berkeley] (EPS), University of California [Berkeley] (UC Berkeley), and University of California (UC)-University of California (UC)
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emplacement ,LIBS ,shergottites ,Multidisciplinary ,Mars2020 ,Mars ,Perseverance ,system ,rocks ,reflectance spectra ,Vis ,in-situ ,SuperCam ,[SDU]Sciences of the Universe [physics] ,rover ,IR ,origin ,surface ,identification ,Raman ,olivine - Abstract
Before Perseverance, Jezero crater's floor was variably hypothesized to have a lacustrine, lava, volcanic airfall, or aeolian origin. SuperCam observations in the first 286 Mars days on Mars revealed a volcanic and intrusive terrain with compositional and density stratification.The dominant lithology along the traverse is basaltic, with plagioclase enrichment in stratigraphically higher locations. Stratigraphically lower, layered rocks are richer in normative pyroxene. The lowest observed unit has the highest inferred density and is olivine-rich with coarse (1.5 millimeters) euhedral, relatively unweathered grains, suggesting a cumulate origin. This is the first martian cumulate and shows similarities to martian meteorites, which also express olivine disequilibrium. Alteration materials including carbonates, sulfates, perchlorates, hydrated silicates, and iron oxides are pervasive but low in abundance, suggesting relatively brief lacustrine conditions. Orbital observations link the Jezero floor lithology to the broader Nili-Syrtis region, suggesting that density-driven compositional stratification is a regional characteristic. Funding was provided by the following sources: NASA's Mars exploration program, including contracts NNH15AZ24I and NNH13ZDA018O to LANL. LANL LDRD code XWHW contributed to calibrations. A portion of this research was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration (80NM0018D0004). NASA RSSPS grants supported J.I.S., grantnumber 80NSSC20K0239 supported L. Hausrath, grant number 80NSSC20K0240 supported L. Mayhew, and grant number 80NSSC21K0330 supported A.U. CNRS and CNES supported the work in France. DLR supported S.Sc. and D.S.V. The Swedish National Space Agency (contracts 137/19 and 2021-00092) supported S.Si. The Natural Sciences and Engineering Research Council of Canada (NSERC) and the Canadian Space Agency (CSA) supported E.C., S.C., and N.T. The Ministry of Economy and Competitiveness (MINECO, SPAIN) grant PID2019-107442RB-C31 supported F.R., G.L.R., J.A.M., and M.
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- 2022
40. Overview of Secondary Phosphate Facies observed by Chemcam in Gale Crater, Mars
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Meslin, Pierre-Yves, primary, Forni, Olivier, additional, Loche, Matteo, additional, Fabre, Sébastien, additional, Lanza, Nina, additional, Gasda, Patrick, additional, Treiman, Allan, additional, Berger, Jeff, additional, Cousin, Agnès, additional, Gasnault, Olivier, additional, Rapin, William, additional, Lasue, Jérémie, additional, Mangold, Nicolas, additional, Dehouck, Erwin, additional, Dromart, Gilles, additional, Maurice, Sylvestre, additional, and Wiens, Roger C., additional
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- 2022
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41. Mafic chemistry and mineralogy (including olivine) of the coarse-grained regolith analyzed by SuperCam at Jezero crater, Mars
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Beyssac, Olivier, Gasnault, Olivier, Chide, Baptiste, Clave, Elise, Cousin, Agnès, Forni, Olivier, Royer, Clément, Johnson, Jeffrey, Benzerara, Karim, Clegg, Samuel, Meslin, Pierre‐Yves, Pilleri, Paolo, Willis, Peter, Lasue, Jérémie, Mandon, Lucia, Ollila, Ann, Beck, Pierre, Kelemen, Peter, Dehouck, Erwin, Anderson, Ryan, Institut de minéralogie et de physique des milieux condensés (IMPMC), Université Pierre et Marie Curie - Paris 6 (UPMC)-Université Paris Diderot - Paris 7 (UPD7)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS), Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Institut Supérieur de l'Aéronautique et de l'Espace (ISAE-SUPAERO), Centre d'Etudes Lasers Intenses et Applications (CELIA), Université de Bordeaux (UB)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS), Laboratoire d'études spatiales et d'instrumentation en astrophysique = Laboratory of Space Studies and Instrumentation in Astrophysics (LESIA), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Muséum national d'Histoire naturelle (MNHN)-Institut de recherche pour le développement [IRD] : UR206-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Los Alamos National Laboratory (LANL), NASA Astrobiology Institute (NAI), Université Grenoble Alpes (UGA), Lamont-Doherty Earth Observatory (LDEO), Columbia University [New York], Université de Toulouse (UT), United States Geological Survey (USGS), and AGU Advancing Earth and Space Science
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[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology ,[SDU.ASTR.EP]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP] ,mars exploration ,mars geology ,mineralogy ,geochemistry - Abstract
International audience; On February 18, 2021 NASAs Perseverance rover landed in Jezero Crater where the floor consists of various rock lithologies and abundant regolith. Using the rovers imagery and the LIBS and VISIR spectroscopies from SuperCam, we focus on the chemistry and mineralogy of coarse-grained regolith. Such regolith has been observed all along the rover traverse since the landing: it is widespread either on flat surfaces/rocks or in aeolian ripples. This coarse regolith is composed of rounded granules rather homogeneous in size (~1-2 mm), shape (nearly isotropic) and color. Some VISIR spectra are highly consistent with the presence of olivine in the regolith. No hydration band is detected, and no H is detected by LIBS, suggesting that this olivine is rather pristine. SuperCam LIBS has a laser spot size of 300 mm and is operated by performing rasters of up to 10 sampling points, each accumulating up to 50 laser shots. Combining high-resolution RMI images with microphone recordings during the laser shots, we can assess whether the LIBS laser sampled dust/fine sand or granules during the shot series, and if the laser significantly ablates a granule. Careful analysis of the LIBS spectra and derived chemical compositions, including comparison with data from calibration targets and shot to shot variability, reveal the presence at the LIBS spot size of (i) olivine only, (ii) olivine and andesine mixtures, and (iii) other assemblages including the former and/or other minerals such as pyroxenes. Most olivine grains are Fo# 60-75, but locally some grains may be lower Fo#; they all exhibit low content of Cr and Mn, Ni is below detection limit. Interestingly, this coarse regolith displays a different chemistry and mineralogy compared to the surrounding rocks raising questions about its provenance. The rover is currently making its way toward the adjacent Seitah unit which is a possible source as it may contain olivine based on orbital data. There are also some differences in composition between these granules and the finer fractions of the regolith. All these data will be compared to orbital data and observations by Curiosity on similar coarse-grained regolith at Gale crater. They will also be discussed in light of knowledge from Martian meteorites to place constraints on the formation of olivine and magmatic processes on Mars.
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- 2021
42. First Sounds from Mars
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Maurice, sylvestre, primary, Chide, Baptiste, additional, Murdoch, Naomi, additional, Lorenz, Ralph, additional, Mimoun, David, additional, Wiens, Roger, additional, Stott, Alexander, additional, Jacob, Xavier, additional, Bertrand, Tanguy, additional, Montmessin, Franck, additional, Lanza, Nina, additional, Llamas, Cesar Alvarez, additional, Angel, S. M., additional, Aung, M., additional, Balaram, J., additional, Beyssac, Olivier, additional, Cousin, Agnès, additional, Delory, Greg, additional, Forni, Olivier, additional, Fouchet, Thierry, additional, Gasnault, Olivier, additional, Grip, Havard, additional, hecht, Mike, additional, Hoffman, Jeff, additional, Laserna, Javier, additional, Lasue, Jérémie, additional, Maki, Justin, additional, McClean, John, additional, Meslin, Pierre-Yves, additional, Mouélic, Stéphane Le, additional, Munguira, Asier, additional, Newman, Claire, additional, Rodriguez-Manfredi, Jose, additional, Moros, Javier, additional, Pilleri, Paolo, additional, Schroeder, Susanne, additional, Torre, Manuel de la, additional, Ollila, Ann, additional, Tzanetos, Thoedore, additional, Farley, Ken, additional, Stack, Kathryn, additional, and Williford, Ken, additional
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- 2021
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43. The K and Th concentration in the Martian crust: insights from multi-scale analyses
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Baratoux, David, primary, Makhoudia, Fall, additional, Meslin, Pierre-Yves, additional, Ndiaye, Papa Moussa, additional, Baratoux, Lenka, additional, Moyen, Jean-François, additional, Jessell, Mark, additional, and Vanderhaeghe, Olivier, additional
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- 2021
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44. Observations of Rocks in Jezero Landing Site: SuperCam/LIBS technique overview of results from the first six months of operations
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Cousin, Agnès, Anderson, Ryan, Forni, Olivier, Benzerara, Karim, Mangold, Nicolas, Beck, Pierre, Dehouck, Erwin, Ollila, Ann, Meslin, Pierre-Yves, Gibbons, Erin, Gasnault, Olivier, Beyssac, Olivier, Lassue, Jérémie, Frydenvang, Jens, Vogt, David, Pilleri, Paolo, Schröder, Susanne, Clegg, Sam, Maurice, Sylvestre, Wiens, Roger, Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), United States Geological Survey (USGS), Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Muséum national d'Histoire naturelle (MNHN)-Institut de recherche pour le développement [IRD] : UR206-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Laboratoire de Planétologie et Géosciences [UMR_C 6112] (LPG), Université d'Angers (UA)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Nantes université - UFR des Sciences et des Techniques (Nantes univ - UFR ST), Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ)-Nantes Université - pôle Sciences et technologie, Nantes Université (Nantes Univ)-Nantes Université (Nantes Univ), Institut de Planétologie et d'Astrophysique de Grenoble (IPAG), Centre National d'Études Spatiales [Toulouse] (CNES)-Observatoire des Sciences de l'Univers de Grenoble (OSUG ), Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France -Institut national des sciences de l'Univers (INSU - CNRS)-Université Savoie Mont Blanc (USMB [Université de Savoie] [Université de Chambéry])-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Université Grenoble Alpes (UGA)-Météo-France, Los Alamos National Laboratory (LANL), McGill University = Université McGill [Montréal, Canada], University of Copenhagen = Københavns Universitet (UCPH), and Deutsches Zentrum für Luft- und Raumfahrt [Berlin] (DLR)
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[SDU.STU.PL]Sciences of the Universe [physics]/Earth Sciences/Planetology - Abstract
International audience
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- 2021
45. Transition Metals in Gale Crater, Mars: Perspectives on Global Abundances and Future Exploration
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Payré, Valérie, primary, Nachon, Marion, additional, Wiens, Roger C., additional, Lasue, Jérémie, additional, Salvatore, Mark, additional, Ollila, Ann M., additional, Lanza, Nina L., additional, and Meslin, Pierre-Yves, additional
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- 2021
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46. Bedrock geochemistry measured by ChemCam along a 2-km eastward traverse in the Glen Torridon region, Gale crater, Mars
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Dehouck, Erwin, primary, Cousin, Agnès, additional, Mangold, Nicolas, additional, Frydenvang, Jens, additional, Gasnault, Olivier, additional, Rammelkamp, Kristin, additional, Rapin, William, additional, Forni, Olivier, additional, Gasda, Patrick J., additional, David, Gaël, additional, Caravaca, Gwénaël, additional, Lasue, Jérémie, additional, Meslin, Pierre-Yves, additional, Bedford, Candice C., additional, Lanza, Nina L., additional, Fox, Valerie K., additional, Bennett, Kristen A., additional, Bryk, Alexander B., additional, Maurice, Sylvestre, additional, and Wiens, Roger C., additional
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- 2021
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47. Observations of Rocks in Jezero Landing Site: SuperCam/LIBS technique overview of results from the first six months of operations.
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Cousin, Agnès, primary, Anderson, Ryan, additional, Forni, Olivier, additional, Benzerara, Karim, additional, Mangold, Nicolas, additional, Beck, Pierre, additional, Dehouck, Erwin, additional, Ollila, Ann, additional, Meslin, Pierre-Yves, additional, Gibbons, Erin, additional, Gasnault, Olivier, additional, Beyssac, Olivier, additional, Lassue, Jérémie, additional, Frydenvang, Jens, additional, Vogt, David, additional, Pilleri, Paolo, additional, Schröder, Susanne, additional, Clegg, Sam, additional, Maurice, Sylvestre, additional, and Wiens, Roger, additional
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- 2021
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48. Comparing SuperCam first shots at Jezero with ChemCam eolian dust analysis at Gale
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Lasue, Jeremie, primary, Meslin, Pierre-Yves, additional, Cousin, Agnes, additional, Forni, Olivier, additional, Anderson, Ryan, additional, Dehouck, Erwin, additional, Frydenvang, Jens, additional, Gasnault, Olivier, additional, Rapin, William, additional, Pilleri, Paolo, additional, Clegg, Sam, additional, and Wiens, Roger, additional
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- 2021
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49. MARS ATMOSPHERE: Mars methane detection and variability at Gale crater
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Webster, Christopher R., Mahaffy, Paul R., Atreya, Sushil K., Flesch, Gregory J., Mischna, Michael A., Meslin, Pierre-Yves, Farley, Kenneth A., Conrad, Pamela G., Christensen, Lance E., Pavlov, Alexander A., Martín-Torres, Javier, Zorzano, María-Paz, McConnochie, Timothy H., Owen, Tobias, Eigenbrode, Jennifer L., Glavin, Daniel P., Steele, Andrew, Malespin, Charles A., Archer, Douglas P., Jr., Sutter, Brad, Coll, Patrice, Freissinet, Caroline, McKay, Christopher P., Moores, John E., Schwenzer, Susanne P., Bridges, John C., Navarro-Gonzalez, Rafael, Gellert, Ralf, and Lemmon, Mark T.
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- 2015
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50. The SuperCam Microphone and Expected First Sounds at Jezero Crater, Mars
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Chide, Baptiste, Lanza, N. L., Alvarez, C., Angel, Stanley M., Bernardi, Pernelle, Beyssac, Olivier, Bousquet, Bruno, Cadu, A., Clavé, E., Forni, Olivier, Fouchet, Thierry, Gasnault, Olivier, Jacob, X., Lacombes, G., Laserna, J., Lasue, Jérémie, Lorenz, Ralph D., Meslin, Pierre-Yves, Montmessin, Franck, Moros, J., Murdoch, N., Ollila, Ann, Pilleri, Paolo, Puhorit, P., Reyes-Newell, A. L., Schroder, S., Stott, A., Vogt, D., Maurice, Sylestre, Wiens, Roger, Mimoun, David, Institut de recherche en astrophysique et planétologie (IRAP), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France -Centre National de la Recherche Scientifique (CNRS), Institut Supérieur de l'Aéronautique et de l'Espace (ISAE-SUPAERO), Los Alamos National Laboratory (LANL), Universidad de Málaga [Málaga] = University of Málaga [Málaga], University of South Carolina [Columbia], Laboratoire d'études spatiales et d'instrumentation en astrophysique = Laboratory of Space Studies and Instrumentation in Astrophysics (LESIA), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Pôle Planétologie du LESIA, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de Paris, Institut de minéralogie, de physique des matériaux et de cosmochimie (IMPMC), Muséum national d'Histoire naturelle (MNHN)-Institut de recherche pour le développement [IRD] : UR206-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Centre d'Etudes Lasers Intenses et Applications (CELIA), Université de Bordeaux (UB)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS), Institut de mécanique des fluides de Toulouse (IMFT), Université de Toulouse (UT)-Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP), Université de Toulouse (UT), Johns Hopkins University Applied Physics Laboratory [Laurel, MD] (APL), PLANETO - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), DLR Institut für Planetenforschung, and Deutsches Zentrum für Luft- und Raumfahrt [Berlin] (DLR)
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[PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph] - Abstract
International audience; This presentation aims to show the expected first results from the SuperCam microphone onboard the NASA Perseverance rover.
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- 2021
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