Distribution of phyllosilicates on the surface of Ceres
E. Ammannito, M. C. DeSanctis, M. Ciarniello, A. Frigeri, F. G. Carrozzo, J.-Ph. Combe, B. L. Ehlmann, S. Marchi, H. Y. McSween, A. Raponi, M. J. Toplis, F. Tosi, J. C. Castillo-Rogez, F. Capaccioni, M. T. Capria, S. Fonte, M. Giardino, R. Jaumann, A. Longobardo, S. P. Joy, G. Magni, T. B. McCord, L. A. McFadden, E. Palomba, C. M. Pieters, C. A. Polanskey, M. D. Rayman, C. A. Raymond, P. M. Schenk, F. Zambon, C. T. Russell
Science 02 Sep 2016:
Vol. 353, Issue 6303, pp. 1006
DOI: 10.1126/science.aaf4279
“INTRODUCTION
The surface of the dwarf planet Ceres is known to host phyllosilicate minerals, but their distribution and origin have not previously been determined. Phyllosilicates are hydrated silicates, and their presence on the surface of Ceres is intriguing given that their structure evolves through an aqueous alteration process. In addition, some phyllosilicates are known to bear NH4, which places a constraint on the pH and redox conditions during the evolution of Ceres. We studied the distribution of phyllosilicates across the planet’s surface to better understand the evolutionary pathway of Ceres.
RATIONALE
Using the data acquired by the mapping spectrometer (VIR) onboard the Dawn spacecraft, we mapped the spatial distribution of different minerals on Ceres on the basis of their diagnostic absorption features in visible and infrared spectra. We studied the phyllosilicates through their OH-stretch fundamental absorption at about 2.7 µm and through the NH4 absorption at about 3.1 µm. From our composition maps, we infer the origin of the materials identified.
RESULTS
We found that Mg- and NH4-bearing phyllosilicates are ubiquitous across the surface of Ceres and that their chemical composition is fairly uniform. The widespread presence of these two types of minerals is a strong indication of a global and extensive aqueous alteration—i.e., the presence of water at some point in Ceres’ geological history. Although the detected phyllosilicates are compositionally homogeneous, we found variations in the intensity of their absorption features in the 3-µm region of the reflectance spectrum. Such variations are likely due to spatial variability in relative mineral abundance (see the figure).
CONCLUSION
The large-scale regional variations evident in the figure suggest lateral heterogeneity in surficial phyllosilicate abundance on scales of several hundreds of kilometers. Terrains associated with the Kerwan crater (higher concentration of phyllosilicates) appear smooth, whereas the Yalode crater (lower concentration of phyllosilicates) is characterized by both smooth and rugged terrains. These distinct morphologies and phyllosilicate concentrations observed in two craters that are similar in size may reflect different compositions and/or rheological properties. On top of this large-scale lateral heterogeneity, small-scale variations associated with individual craters could result from different proportions of mixed materials in a stratified upper crustal layer that has been exposed by impacts. Variations associated with fresh craters, such as the 34-km-diameter Haulani, indicate the presence of crustal variations over a vertical scale of a few kilometers, whereas much larger craters, such as the 126-km-diameter Dantu, suggest that such stratification may extend for at least several tens of kilometers.”
