A volcanically active planet is shown in closeup at the left side of the image with glowing eruptions and lines of lava on the surface. To the right and in the distance is a faint blue glowing ball representing the more massive planet in the system.Sixteen frames from Voyager 1's flyby of Jupiter in 1979 were merged to create this image. Jupiter's Great Red Spot is visible in the center. Jupiter's moon Europa can be seen in the foreground at the bottom left of the image.The frame is a horizontal rainbow of color on a grid. Shadows of molecules can be seen through the light as well as the jagged peaks and troughs of spectral lines.
Fizzy Super Earths and Lava Worlds“Fizzy Super-Earths: Impacts of Magma Composition on the Bulk Density and Structure of Lava Worlds.” in The Astrophysical Journal.01/03
Identifying Hydrothermal Activity on Icy Ocean Worlds“Ethene-ethanol ratios as potential indicators of hydrothermal activity at Enceladus, Europa, and other icy ocean worlds.” In Icarus.02/03
NASA Raman Spectroscopic Database"The NASA Raman spectroscopic database: Ramdb version 1.00.” In Icarus.03/03
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April 2014Elemental, isotopic, and structural changes in Tagish Lake insoluble organic matter produced by parent body processes

Alexander, C. M. O. D., Cody, G. D., Kebukawa, Y., Bowden, R., Fogel, M. L., Kilcoyne, A. L. D., … Nittler, L. R. (2014). Meteoritics & Planetary Science, 49(4), 503–525. doi:10.1111/maps.12282

Chirality of meteoritic free and IOM-derived monocarboxylic acids and implications for prebiotic organic synthesis

Aponte, J. C., Tarozo, R., Alexandre, M. R., Alexander, C. M. O. D., Charnley, S. B., Hallmann, C., … Summons, R. E. (2014). Geochimica et Cosmochimica Acta, 131(None), 1–12. doi:10.1016/j.gca.2014.01.035

Effects of Extreme Obliquity Variations on the Habitability of Exoplanets

Armstrong, J. C., Barnes, R., Domagal-Goldman, S., Breiner, J., Quinn, T. R., & Meadows, V. S. (2014). Astrobiology, 14(4), 277–291. doi:10.1089/ast.2013.1129

Reconciling early impacts and the rise of life

Cavosie, A. J. (2014). Geology, 42(5), 463–464. doi:10.1130/focus052014.1

Isotopic links between atmospheric chemistry and the deep sulphur cycle on Mars

Franz, H. B., Kim, S-T., Farquhar, J., Day, J. M. D., Economos, R. C., McKeegan, K. D., … Schmitt, A. K. (2014). Nature, 508(7496), 364–368. doi:10.1038/nature13175

Solubility and stability investigation of Titan aerosol analogs: New insight from NMR analysis

He, C., & Smith, M. A. (2014). Icarus, 232(None), 54–59. doi:10.1016/j.icarus.2014.01.007

Highly siderophile elements in Earth’s mantle as a clock for the Moon-forming impact

Jacobson, S. A., Morbidelli, A., Raymond, S. N., O'Brien, D. P., Walsh, K. J., & Rubie, D. C. (2014). Nature, 508(7494), 84–87. doi:10.1038/nature13172

The Potential for Biologically Catalyzed Anaerobic Methane Oxidation on Ancient Mars

Marlow, J. J., LaRowe, D. E., Ehlmann, B. L., Amend, J. P., & Orphan, V. J. (2014). Astrobiology, 14(4), 292–307. doi:10.1089/ast.2013.1078

Follow the Plume: The Habitability of Enceladus

McKay, C. P., Anbar, A. D., Porco, C., & Tsou, P. (2014). Astrobiology, 14(4), 352–355. doi:10.1089/ast.2014.1158

Speciation of and D/H partitioning between fluids and melts in silicate-D-O-H-C-N systems determined in-situ at upper mantle temperatures, pressures, and redox conditions

Mysen, B. O., Tomita, T., Ohtani, E., & Suzuki, A. (2014). American Mineralogist, 99(4), 578–588. doi:10.2138/am.2014.4575