Danika Wellington

ORCID: 0000-0002-2130-0075
Publications
Citations
Views
---
Saved
---
About
Contact & Profiles
Research Areas
  • Planetary Science and Exploration
  • Astro and Planetary Science
  • Space Exploration and Technology
  • Space Science and Extraterrestrial Life
  • Geology and Paleoclimatology Research
  • Atmospheric and Environmental Gas Dynamics
  • Isotope Analysis in Ecology
  • Anomaly Detection Techniques and Applications
  • Spaceflight effects on biology
  • Aeolian processes and effects
  • Space exploration and regulation
  • Remote Sensing in Agriculture
  • Geochemistry and Geologic Mapping
  • Climate change and permafrost
  • Land Use and Ecosystem Services
  • Laser-induced spectroscopy and plasma
  • Solar and Space Plasma Dynamics
  • Methane Hydrates and Related Phenomena
  • Calibration and Measurement Techniques
  • Hydrocarbon exploration and reservoir analysis
  • Geological and Geophysical Studies
  • Remote-Sensing Image Classification
  • Marine and environmental studies
  • Geological and Geochemical Analysis
  • Scientific Research and Philosophical Inquiry

United States Geological Survey
2021-2022

KBR (United States)
2022

Arizona State University
2013-2021

Chesapeake Bay Program
2020

Ames Research Center
2020

Institut de Recherche en Astrophysique et Planétologie
2017

Centre National de la Recherche Scientifique
2017

The Curiosity rover discovered fine-grained sedimentary rocks, which are inferred to represent an ancient lake and preserve evidence of environment that would have been suited support a martian biosphere founded on chemolithoautotrophy. This aqueous was characterized by neutral pH, low salinity, variable redox states both iron sulfur species. Carbon, hydrogen, oxygen, sulfur, nitrogen, phosphorus were measured directly as key biogenic elements; inference, is assumed available. probably had...

10.1126/science.1242777 article EN Science 2013-12-10
Donald M. Hassler C. Zeitlin R. F. Wimmer‐Schweingruber Bent Ehresmann Scot Rafkin and 95 more J. L. Eigenbrode D. E. Brinza Gerald Weigle Stephan Böttcher Eckart Böhm Söenke Burmeister Jingnan Guo Jan Köhler César Martı́n G. Reitz Francis A. Cucinotta Myung‐Hee Y. Kim David Grinspoon M. A. Bullock Arik Posner Javier Gómez‐Elvira A. R. Vasavada J. P. Grotzinger MSL Science Team Osku Kemppinen David A. Cremers J. F. Bell Lauren Edgar Jack D. Farmer Austin Godber M. Wadhwa Danika Wellington Ian McEwan Claire Newman M. I. Richardson Antoine Charpentier Laurent Péret P. L. King J. G. Blank M. E. Schmidt Shuai Li R. E. Milliken Kevin Robertson V. Z. Sun Michael B. Baker Christopher S. Edwards B. L. Ehlmann K. A. Farley J. L. Griffes Hayden Miller Megan Newcombe C. Pilorget M. S. Rice K. L. Siebach Katie Stack Edward M. Stolper Claude Brunet V. Hipkin Richard Léveillé Geneviève Marchand Pablo Sobrón Sánchez Laurent Favot George D. Cody A. Steele Lorenzo Flückiger David Lees Ara Nefian Mildred Martin M. Gailhanou Francès Westall Guy Israël Christophe Agard Julien Baroukh Christophe Donny Alain Gaboriaud Philippe Guillemot Vivian Lafaille Eric Lorigny Alexis Paillet R. Pérez M. Saccoccio Charles Yana Carlos Armiens‐Aparicio Javier Caride Rodríguez Isaías Carrasco Blázquez Felipe Gómez Sebastian Hettrich Alain Lepinette Malvitte Mercedes Marín Jiménez Jesús Martínez‐Frías Javier Martín-Soler Javier Martín‐Torres Antonio Molina Jurado Luis Mora‐Sotomayor G. M. Muñoz Sara Navarro López Verónica Peinado-González Jorge Pla-García J. A. Rodríguez‐Manfredi Julio José Romeral-Planelló

The Radiation Assessment Detector (RAD) on the Mars Science Laboratory’s Curiosity rover began making detailed measurements of cosmic ray and energetic particle radiation environment surface 7 August 2012. We report discuss absorbed dose equivalent from galactic rays solar particles martian for ~300 days observations during current maximum. These provide insight into hazards associated with a human mission to an anchor point which model subsurface environment, implications microbial survival...

10.1126/science.1244797 article EN Science 2013-12-10

Samples from the Rocknest aeolian deposit were heated to ~835°C under helium flow and evolved gases analyzed by Curiosity’s Sample Analysis at Mars instrument suite. H 2 O, SO , CO O major released. Water abundance (1.5 3 weight percent) release temperature suggest that is bound within an amorphous component of sample. Decomposition fine-grained Fe or Mg carbonate likely source much . Evolved coincident with Cl, suggesting oxygen produced thermal decomposition oxychloride compound. Elevated...

10.1126/science.1238937 article EN Science 2013-09-26
P. R. Mahaffy Christopher R. Webster S. K. Atreya H. B. Franz Michael Wong and 95 more P. G. Conrad D. N. Harpold John J. Jones L. A. Leshin H. L. K. Manning Tobias Owen R. O. Pepin S. W. Squyres M. G. Trainer Osku Kemppinen Nathan Bridges J. R. Johnson M. E. Minitti David A. Cremers J. F. Bell Lauren Edgar Jack D. Farmer Austin Godber M. Wadhwa Danika Wellington Ian McEwan Claire Newman M. I. Richardson Antoine Charpentier Laurent Péret P. L. King J. G. Blank Gerald Weigle M. E. Schmidt Shuai Li R. E. Milliken Kevin Robertson V. Z. Sun Michael B. Baker Christopher Edwards Bethany Ehlmann Kenneth Farley J. L. Griffes J. P. Grotzinger Hayden Miller Megan Newcombe C. Pilorget M. S. Rice Kirsten Siebach Katie Stack Edward M. Stolper Claude Brunet V. Hipkin Richard Léveillé Geneviève Marchand Pablo Sobrón Sánchez Laurent Favot George D. Cody A. Steele Lorenzo Flückiger David Lees Ara Nefian Mildred Martin M. Gailhanou Francès Westall Guy Israël Christophe Agard Julien Baroukh Christophe Donny Alain Gaboriaud Philippe Guillemot Vivian Lafaille Eric Lorigny Alexis Paillet R. Pérez M. Saccoccio Charles Yana Carlos Armiens‐Aparicio Javier Caride Rodríguez Isaías Carrasco Blázquez Felipe Gómez Javier Gómez‐Elvira Sebastian Hettrich Alain Lepinette Malvitte Mercedes Marín Jiménez Jesús Martínez‐Frías Javier Martín-Soler Javier Martín‐Torres Antonio Molina Jurado Luis Mora‐Sotomayor G. M. Muñoz Sara Navarro López Verónica Peinado-González Jorge Pla-García J. A. Rodríguez‐Manfredi Julio José Romeral-Planelló Sara Alejandra Sans Fuentes Eduardo Sebastian Martinez J. Torres Roser Urqui-O'Callaghan

Volume mixing and isotope ratios secured with repeated atmospheric measurements taken the Sample Analysis at Mars instrument suite on Curiosity rover are: carbon dioxide (CO2), 0.960(±0.007); argon-40 ((40)Ar), 0.0193(±0.0001); nitrogen (N2), 0.0189(±0.0003); oxygen, 1.45(±0.09) × 10(-3); monoxide, < 1.0 (40)Ar/(36)Ar, 1.9(±0.3) 10(3). The (40)Ar/N2 ratio is 1.7 times greater (40)Ar/(36)Ar 1.6 lower than values reported by Viking Lander mass spectrometer in 1976, whereas other are generally...

10.1126/science.1237966 article EN Science 2013-07-18

H 2 O, CO , SO O S, HCl, chlorinated hydrocarbons, NO, and other trace gases were evolved during pyrolysis of two mudstone samples acquired by the Curiosity rover at Yellowknife Bay within Gale crater, Mars. O/OH-bearing phases included 2:1 phyllosilicate(s), bassanite, akaganeite, amorphous materials. Thermal decomposition carbonates combustion organic materials are candidate sources for . Concurrent evolution hydrocarbons suggests presence oxychlorine phase(s). Sulfides likely...

10.1126/science.1245267 article EN Science 2013-12-10

Observations by the Mars Science Laboratory Mast Camera (Mastcam) in Gale crater reveal isolated outcrops of cemented pebbles (2 to 40 millimeters diameter) and sand grains with textures typical fluvial sedimentary conglomerates. Rounded conglomerates indicate substantial abrasion. ChemCam emission spectra at one outcrop show a predominantly feldspathic composition, consistent minimal aqueous alteration sediments. Sediment was mobilized ancient water flows that likely exceeded threshold...

10.1126/science.1237317 article EN Science 2013-05-30

Sedimentary rocks examined by the Curiosity rover at Yellowknife Bay, Mars, were derived from sources that evolved an approximately average martian crustal composition to one influenced alkaline basalts. No evidence of chemical weathering is preserved, indicating arid, possibly cold, paleoclimates and rapid erosion deposition. The absence predicted geochemical variations indicates magnetite phyllosilicates formed diagenesis under low-temperature, circumneutral pH, rock-dominated aqueous...

10.1126/science.1244734 article EN Science 2013-12-10

The ChemCam instrument, which provides insight into martian soil chemistry at the submillimeter scale, identified two principal types along Curiosity rover traverse: a fine-grained mafic type and locally derived, coarse-grained felsic type. component is representative of widespread soils similar in composition to dust. It possesses ubiquitous hydrogen signature spectra, corresponding hydration amorphous phases found by CheMin instrument. This likely accounts for an important fraction global...

10.1126/science.1238670 article EN Science 2013-09-26

Abstract The Curiosity rover has analyzed abundant light‐toned fracture‐fill material within the Yellowknife Bay sedimentary deposits. ChemCam instrument, coupled with Mastcam and ChemCam/Remote Micro Imager images, was able to demonstrate that these fracture fills consist of calcium sulfate veins, many which appear be hydrated at a level expected for gypsum bassanite. Anhydrite is locally present found in location characterized by nodular texture. An intricate assemblage veins crosses...

10.1002/2013je004588 article EN Journal of Geophysical Research Planets 2014-07-15
J. C. Stern B. Sutter Caroline Freissinet R. Navarro‐González Christopher P. McKay and 95 more P. D. Archer A. Buch Anna Brunner Patrice Coll J. L. Eigenbrode Alberto González Fairén H. B. Franz D. P. Glavin Srishti Kashyap A. C. McAdam D. W. Ming A. Steele Cyril Szopa J. J. Wray Javier Martín‐Torres Marìa‐Paz Zorzano P. G. Conrad P. R. Mahaffy Osku Kemppinen N. T. Bridges J. R. Johnson M. E. Minitti David A. Cremers James F. Bell L. A. Edgar Jack D. Farmer Austin Godber M. Wadhwa Danika Wellington Ian McEwan Claire Newman M. I. Richardson Antoine Charpentier Laurent Péret P. L. King J. G. Blank Gerald Weigle M. E. Schmidt Shuai Li R. E. Milliken Kevin Robertson V. Z. Sun Michael B. Baker Christopher S. Edwards B. L. Ehlmann K. A. Farley J. Shechet J. P. Grotzinger Hayden Miller Megan Newcombe C. Pilorget M. S. Rice K. L. Siebach Katie Stack Edward M. Stolper C. Brunet V. Hipkin Richard Léveillé Geneviève Marchand Pablo Sobrón Sánchez Laurent Favot George D. Cody A. Steele Lorenzo Flückiger David Lees Ara Nefian Mildred Martin Francès Westall G. Israël Christophe Agard Julien Baroukh Christophe Donny Philippe Guillemot Vivian Lafaille Eric Lorigny Alexis Paillet R. Pérez M. Saccoccio Charles Yana Carlos Armiens‐Aparicio Javier Caride Rodríguez Isaías Carrasco Blázquez Felipe Gómez Javier Gómez‐Elvira Sebastian Hettrich Alain Lepinette Malvitte Mercedes Marín Jiménez Jesús Martínez‐Frías Javier Martín-Soler F. Javier Martín - Torres Antonio Molina Jurado Luis Mora‐Sotomayor G. M. Muñoz Sara Navarro López Verónica Peinado-González

Significance We present data supporting the presence of an indigenous source fixed nitrogen on surface Mars in form nitrate. This may indicate first stage development a primitive cycle ancient and would have provided biochemically accessible nitrogen.

10.1073/pnas.1420932112 article EN Proceedings of the National Academy of Sciences 2015-03-23
Edward M. Stolper M. B. Baker Megan Newcombe M. E. Schmidt A. H. Treiman and 95 more A. Cousin M. D. Dyar M. R. Fisk R. Gellert P. L. King L. A. Leshin S. Maurice S. M. McLennan M. E. Minitti G. M. Perrett Scott K. Rowland V. Sautter R. C. Wiens Osku Kemppinen Nathan Bridges J. R. Johnson David A. Cremers J. F. Bell Lauren Edgar Jack D. Farmer Austin Godber M. Wadhwa Danika Wellington Ian McEwan Claire Newman M. I. Richardson Antoine Charpentier Laurent Péret J. G. Blank Gerald Weigle Shuai Li R. E. Milliken Kevin Robertson V. Z. Sun Christopher S. Edwards Bethany Ehlmann Kenneth Farley Jennifer Griffes J. P. Grotzinger Hayden Miller Cedric Pilorget M. S. Rice Kirsten Siebach Katie Stack C. Brunet Victoria Hipkin Richard Léveillé Geneviève Marchand Pablo Sobrón Sánchez Laurent Favot George D. Cody A. Steele Lorenzo Flückiger David Lees Ara Nefian Mildred Martin M. Gailhanou Francès Westall Guy Israël Christophe Agard Julien Baroukh Christophe Donny Alain Gaboriaud Philippe Guillemot Vivian Lafaille Eric Lorigny Alexis Paillet R. Pérez M. Saccoccio Charles Yana Carlos Armiens‐Aparicio Javier Caride Rodríguez Isaías Carrasco Blázquez Felipe Gómez Javier Gómez‐Elvira Sebastian Hettrich Alain Lepinette Malvitte Mercedes Marín Jiménez Jesús Martínez‐Frías Javier Martín-Soler Javier Martín‐Torres Antonio Molina Jurado Luis Mora‐Sotomayor G. M. Muñoz Sara Navarro López Verónica Peinado-González Jorge Pla‐García J. A. Rodríguez‐Manfredi Julio José Romeral-Planelló Sara Alejandra Sans Fuentes Eduardo Sebastián J. Torres Roser Urqui-O'Callaghan Marìa‐Paz Zorzano Steve Chipera

"Jake_M," the first rock analyzed by Alpha Particle X-ray Spectrometer instrument on Curiosity rover, differs substantially in chemical composition from other known martian igneous rocks: It is alkaline (>15% normative nepheline) and relatively fractionated. Jake_M compositionally similar to terrestrial mugearites, a type typically found at ocean islands continental rifts. By analogy with these comparable rocks, could have been produced extensive fractional crystallization of primary or...

10.1126/science.1239463 article EN Science 2013-09-26

Abstract The NASA Curiosity rover Mast Camera (Mastcam) system is a pair of fixed‐focal length, multispectral, color CCD imagers mounted ~2 m above the surface on rover's remote sensing mast, along with associated electronics and an onboard calibration target. left Mastcam (M‐34) has 34 mm focal instantaneous field view (IFOV) 0.22 mrad, FOV 20° × 15° over full 1648 1200 pixel span its Kodak KAI‐2020 CCD. right (M‐100) 100 IFOV 0.074 6.8° 5.1° using same detector. cameras are separated by...

10.1002/2016ea000219 article EN cc-by-nc-nd Earth and Space Science 2017-06-28

Abstract The Mars Science Laboratory Curiosity rover performed coordinated measurements to examine the textures and compositions of aeolian sands in active Bagnold dune field. are rounded subrounded, very fine medium sized (~45–500 μm) with ≥6 distinct grain colors. In contrast examined by a dust‐covered, inactive bedform called Rocknest soils at other landing sites, darker, less red, better sorted, have fewer silt‐sized or smaller grains, show no evidence for cohesion. Nevertheless,...

10.1002/2017je005267 article EN cc-by-nc-nd Journal of Geophysical Research Planets 2017-06-12
Christopher R. Webster P. R. Mahaffy Sushil K. Atreya Gregory J. Flesch K. A. Farley and 95 more Osku Kemppinen Nathan Bridges J. R. Johnson M. E. Minitti David A. Cremers J. F. Bell Lauren Edgar Jack D. Farmer Austin Godber M. Wadhwa Danika Wellington Ian McEwan Claire Newman M. I. Richardson Antoine Charpentier Laurent Péret P. L. King J. G. Blank Gerald Weigle M. E. Schmidt Shuai Li R. E. Milliken Kevin Robertson V. Z. Sun Michael B. Baker Christopher Edwards Bethany Ehlmann Kenneth Farley Jennifer Griffes J. P. Grotzinger Hayden Miller Megan Newcombe C. Pilorget M. S. Rice K. L. Siebach Katie Stack Edward M. Stolper C. Brunet Victoria Hipkin Richard Léveillé Geneviève Marchand Pablo Sobrón Sánchez Laurent Favot George D. Cody A. Steele Lorenzo Flückiger David Lees Ara Nefian Mildred Martin M. Gailhanou Francès Westall G. Israël Christophe Agard Julien Baroukh Christophe Donny Alain Gaboriaud Philippe Guillemot Vivian Lafaille Eric Lorigny Alexis Paillet R. Pérez M. Saccoccio Charles Yana Carlos Armiens‐Aparicio Javier Caride Rodríguez Isaías Carrasco Blázquez Felipe Gómez Javier Gómez Elvira Sebastian Hettrich Alain Lepinette Malvitte Mercedes Marín Jiménez Jesús Martínez‐Frías Javier Martín Soler Javier Martín‐Torres Antonio Molina Jurado Luis Mora‐Sotomayor G. M. Muñoz Sara Navarro López Verónica Peinado-González Jorge Pla-García J. A. Rodríguez‐Manfredi Julio José Romeral-Planelló Sara Alejandra Sans Fuentes Eduardo Sebastian Martinez J. Torres Roser Urqui-O'Callaghan Marìa‐Paz Zorzano Steve Chipera Jean-Luc Lacour Patrick Mauchien Jean‐Baptiste Sirven H. L. K. Manning Alberto González Fairén Alexander Hayes Jonathan Joseph

By analogy with Earth, methane in the Martian atmosphere is a potential signature of ongoing or past biological activity. During decade, Earth-based telescopic observations reported "plumes" tens parts per billion by volume (ppbv), and those from Mars orbit showed localized patches, prompting speculation sources subsurface bacteria nonbiological sources. From situ measurements made Tunable Laser Spectrometer (TLS) on Curiosity using distinctive spectral pattern specific to methane, we report...

10.1126/science.1242902 article EN Science 2013-09-20

Abstract This paper provides an overview of the Curiosity rover's exploration at Vera Rubin ridge (VRR) and summarizes science results. VRR is a distinct geomorphic feature on lower Aeolis Mons (informally known as Mount Sharp) that was identified in orbital data based its texture, topographic expression, association with hematite spectral signature. conducted extensive remote sensing observations, acquired dozens contact targets, drilled three outcrop samples from ridge, well one sample...

10.1029/2020je006527 article EN cc-by Journal of Geophysical Research Planets 2020-07-27

Abstract Mars' atmosphere typically supports dust aerosol with an effective radius near 1.5 μm, varying from ~1 μm during low times northern summer solstice to ~2 higher in southern spring and summer. After global events, size variations outside this range have not previously been observed. We report on imaging spectral observations by the Curiosity rover through 2018 event. These show that was seasonally normal prior local onset of increased opacity, rapidly above 4 increasing remained 3...

10.1029/2019gl084407 article EN Geophysical Research Letters 2019-08-22

Abstract. The increasing availability of high-quality remote sensing data and advanced technologies has spurred land cover mapping to characterize change from local global scales. However, most datasets either span multiple decades at a scale or limited time over larger geographic extent. Here, we present new surface dataset created by the Land Change Monitoring, Assessment, Projection (LCMAP) program conterminous United States (CONUS). LCMAP consists annual products period 1985–2017 30 m...

10.5194/essd-14-143-2022 article EN cc-by Earth system science data 2022-01-19

Abstract As part of the Bagnold Dune campaign conducted by Mars Science Laboratory rover Curiosity, visible/near‐infrared reflectance spectra dune sands were acquired using Mast Camera (Mastcam) multispectral imaging (445–1013 nm) and Chemistry (ChemCam) passive point spectroscopy (400–840 nm). By comparing from pristine rover‐disturbed ripple crests troughs within field, through analysis sieved grain size fractions, constraints on mineral segregation sorting could be determined. In general,...

10.1002/2016je005187 article EN Journal of Geophysical Research Planets 2017-04-26

The Mastcam CCD cameras on the Mars Science Laboratory Curiosity Rover each use an 8-position filter wheel in acquiring up to 1600 × 1200 pixel images. set includes a broadband near-infrared cutoff for RGB Bayer imaging camera and 12 narrow-band geology filters distributed between two cameras, spanning wavelength range 445–1013 nm. This region relatively broad charge-transfer crystal-field absorption bands that are most commonly due presence of iron-bearing minerals. To identify such...

10.2138/am-2017-5760ccby article EN cc-by American Mineralogist 2017-06-01

Abstract Images from the Mars Science Laboratory (MSL) mission of lacustrine sedimentary rocks Vera Rubin ridge on “Mt. Sharp” in Gale crater, Mars, have shown stark color variations red to purple gray. These differences crosscut stratigraphy and are likely due diagenetic alteration sediments after deposition. However, chemistry timing these fluid interactions is unclear. Determining how processes may modified chemical mineralogical signatures ancient Martian environments critical for...

10.1029/2019je006322 article EN cc-by-nc Journal of Geophysical Research Planets 2020-09-23

Visible/short-wave infrared spectral data from the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) show absorptions attributed to hematite at Vera Rubin ridge (VRR), a topographic feature on northwest Mt. Sharp. The goals of this study are determine why caused by ferric iron strongly visible orbit VRR and improve interpretation CRISM throughout lower These achieved analyzing coordinated in situ along Curiosity rover's traverse. bedrock within areas that have deepest also has...

10.1029/2019je006294 article EN cc-by Journal of Geophysical Research Planets 2020-08-04

Sample-based estimates augmented by complete coverage land-cover maps were used to estimate area and describe patterns of annual change across the conterminous United States (CONUS) between 1985 2016. Most CONUS land cover remained stable in terms net class over this time, but a substantial gross dynamic was captured cumulative time intervals. The dominant types changes can be grouped into natural resource cycles, increases urbanization, surface-water dynamics. 30-year series showed...

10.3390/land11020298 article EN cc-by Land 2022-02-16

In this work, we present a system based on convolutional autoencoders for detecting novel features in multispectral images. We introduce SAMMIE: Selections Autoencoder Modeling of Multispectral Image Expectations. Previous work using employed the scalar reconstruction error to classify new images as or typical. show that spatial-spectral map can enable both accurate classification novelty well human-comprehensible explanations detection. apply our methodology detection geologic Martian...

10.1609/aaai.v33i01.33019484 article EN Proceedings of the AAAI Conference on Artificial Intelligence 2019-07-17
Coming Soon ...