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 2012 Nucleobases and Prebiotic Molecules in Organic Residues Produced from the Ultraviolet Photo-Irradiation of Pyrimidine in NH 3 and H 2 O+NH 3 Ices

Nuevo, M., Milam, S. N., & Sandford, S. A. (2012). Astrobiology, 12(4), 295–314. doi:10.1089/ast.2011.0726

Debris disks as signposts of terrestrial planet formation

Raymond, S. N., Armitage, P. J., Moro-Martín, A., Booth, M., Wyatt, M. C., Armstrong, J. C., … Mandell, A. M. (2012). A&A, 541(None), A11. doi:10.1051/0004-6361/201117049

Organic Sulfur Metabolisms in Hydrothermal Environments

Rogers, K. L., & Schulte, M. D. (2012). Geobiology, 10(4), 320–332. doi:10.1111/j.1472-4669.2012.00324.x

Maintenance of permeable habitable subsurface environments by earthquakes and tidal stresses

Sleep, N. H. (2012). International Journal of Astrobiology, 11(04), 257–268. doi:10.1017/s1473550412000122

Chemical ionization in the atmosphere? A model study on negatively charged “exotic” ions generated from Titan's tholins by ultrahigh resolution MS and MS/MS

Somogyi, Á., Smith, M. A., Vuitton, V., Thissen, R., & Komáromi, I. (2012). International Journal of Mass Spectrometry, 316-318(None), 157–163. doi:10.1016/j.ijms.2012.02.026

THE EFFECT OF POPULATION-WIDE MASS-TO-RADIUS RELATIONSHIPS ON THE INTERPRETATION OF KEPLER AND HARPS SUPER-EARTH OCCURRENCE RATES

Wolfgang, A., & Laughlin, G. (2012). The Astrophysical Journal, 750(2), 148. doi:10.1088/0004-637x/750/2/148

March 2012Geobiology of the Archean Eon

Buick, R. (2012). Geobiology of the Archean Eon. Fundamentals of Geobiology, None, 351–370. doi:10.1002/9781118280874.ch19

The Global Oxygen Cycle

Kasting, J. F., & Canfield, D. E. (2012). The Global Oxygen Cycle. Fundamentals of Geobiology, None, 93–104. doi:10.1002/9781118280874.ch7

The Global Iron Cycle

Kendall, B., Anbar, A. D., Kappler, A., & Konhauser, K. O. (2012). The Global Iron Cycle. Fundamentals of Geobiology, None, 65–92. doi:10.1002/9781118280874.ch6

What is Geobiology?

Knoll, A. H., Canfield, D. E., & Konhauser, K. O. (2012). What is Geobiology? Fundamentals of Geobiology, None, 1–4. doi:10.1002/9781118280874.ch1