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  5. Localized aliphatic organic material on the surface of Ceres
 

Localized aliphatic organic material on the surface of Ceres

Journal
SCIENCE  
Date Issued
2017
Author(s)
DE SANCTIS, MARIA CRISTINA  
•
Ammannito, E.
•
McSween, H. Y.
•
RAPONI, Andrea  
•
Marchi, S.
•
CAPACCIONI, FABRIZIO  
•
CAPRIA, MARIA TERESA  
•
CARROZZO, FILIPPO GIACOMO  
•
CIARNIELLO, Mauro  
•
FONTE, SERGIO  
•
FORMISANO, Michelangelo  
•
FRIGERI, ALESSANDRO  
•
Giardino, M.
•
Longobardo, A.  
•
Magni, G.
•
McFadden, L. A.
•
PALOMBA, Ernesto  
•
Pieters, C. M.
•
TOSI, Federico  
•
ZAMBON, Francesca  
•
Raymond, C. A.
•
Russell, C. T.
DOI
10.1126/science.aaj2305
Abstract
Organic compounds occur in some chondritic meteorites, and their signatures on solar system bodies have been sought for decades. Spectral signatures of organics have not been unambiguously identified on the surfaces of asteroids, whereas they have been detected on cometary nuclei. Data returned by the Visible and InfraRed Mapping Spectrometer on board the Dawn spacecraft show a clear detection of an organic absorption feature at 3.4 micrometers on dwarf planet Ceres. This signature is characteristic of aliphatic organic matter and is mainly localized on a broad region of ~1000 square kilometers close to the ~50-kilometer Ernutet crater. The combined presence on Ceres of ammonia-bearing hydrated minerals, water ice, carbonates, salts, and organic material indicates a very complex chemical environment, suggesting favorable environments to prebiotic chemistry.
Volume
355
Issue
6326
Start page
719
Uri
http://hdl.handle.net/20.500.12386/28668
Url
https://science.sciencemag.org/content/355/6326/719
Issn Identifier
0036-8075
Ads BibCode
2017Sci...355..719D
Rights
restricted
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