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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July 2013 MODELING THE HD 32297 DEBRIS DISK WITH FAR-INFRARED HERSCHEL DATA

Donaldson, J. K., Lebreton, J., Roberge, A., Augereau, J-C., & Krivov, A. V. (2013). The Astrophysical Journal, 772(1), 17. doi:10.1088/0004-637x/772/1/17

Glycine's Radiolytic Destruction in Ices: First in situ Laboratory Measurements for Mars

Gerakines, P. A., & Hudson, R. L. (2013). Astrobiology, 13(7), 647–655. doi:10.1089/ast.2012.0943

Low simulated radiation limit for runaway greenhouse climates

Goldblatt, C., Robinson, T. D., Zahnle, K. J., & Crisp, D. (2013). Nature Geosci, 6(8), 661–667. doi:10.1038/ngeo1892

Universal labeling of 5′-triphosphate RNAs by artificial RNA ligase enzyme with broad substrate specificity

Haugner III, J. C., & Seelig, B. (2013). Chem. Commun., 49(66), 7322. doi:10.1039/c3cc44454f

KETENE FORMATION IN INTERSTELLAR ICES: A LABORATORY STUDY

Hudson, R. L., & Loeffler, M. J. (2013). The Astrophysical Journal, 773(2), 109. doi:10.1088/0004-637x/773/2/109

MrpA Functions in Energy Conversion during Acetate-Dependent Growth of Methanosarcina acetivorans

Jasso-Chavez, R., Apolinario, E. E., Sowers, K. R., & Ferry, J. G. (2013). Journal of Bacteriology, 195(17), 3987–3994. doi:10.1128/jb.00581-13

The persistent activity of Jupiter-family comets at 3–7AU

Kelley, M. S., Fernández, Y. R., Licandro, J., Lisse, C. M., Reach, W. T., A’Hearn, M. F., … Bauer, J. (2013). Icarus, 225(1), 475–494. doi:10.1016/j.icarus.2013.04.012

HERSCHEL 's “COLD DEBRIS DISKS”: BACKGROUND GALAXIES OR QUIESCENT RIMS OF PLANETARY SYSTEMS?

Krivov, A. V., Eiroa, C., Löhne, T., Marshall, J. P., Montesinos, B., Del Burgo, C., … Absil, O. (2013). The Astrophysical Journal, 772(1), 32. doi:10.1088/0004-637x/772/1/32

Texture-specific isotopic compositions in 3.4Gyr old organic matter support selective preservation in cell-like structures

Lepot, K., Williford, K. H., Ushikubo, T., Sugitani, K., Mimura, K., Spicuzza, M. J., & Valley, J. W. (2013). Geochimica et Cosmochimica Acta, 112(None), 66–86. doi:10.1016/j.gca.2013.03.004

Archaeal and bacterial glycerol dialkyl glycerol tetraether lipids in chimneys of the Lost City Hydrothermal Field

Lincoln, S. A., Bradley, A. S., Newman, S. A., & Summons, R. E. (2013). Organic Geochemistry, 60(None), 45–53. doi:10.1016/j.orggeochem.2013.04.010