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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September 2012Compound-specific carbon, nitrogen, and hydrogen isotopic ratios for amino acids in CM and CR chondrites and their use in evaluating potential formation pathways

Elsila, J. E., Charnley, S. B., Burton, A. S., Glavin, D. P., & Dworkin, J. P. (2012). Meteoritics & Planetary Science, 47(9), 1517–1536. doi:10.1111/j.1945-5100.2012.01415.x

Understanding measured water rotational temperatures and column densities in the very innermost coma of Comet 73P/Schwassmann–Wachmann 3 B

Fougere, N., Combi, M. R., Tenishev, V., Rubin, M., Bonev, B. P., & Mumma, M. J. (2012). Icarus, 221(1), 174–185. doi:10.1016/j.icarus.2012.07.019

Molybdenum limitation of microbial nitrogen assimilation in aquatic ecosystems and pure cultures

Glass, J. B., Axler, R. P., Chandra, S., & Goldman, C. R. (2012). Frontiers in Microbiology, 3(None), None. doi:10.3389/fmicb.2012.00331

The Enzymatic and Metabolic Capabilities of Early Life

Goldman, A. D., Baross, J. A., & Samudrala, R. (2012). PLoS ONE, 7(9), e39912. doi:10.1371/journal.pone.0039912

Anomalous molybdenum isotope trends in Upper Pennsylvanian euxinic facies: Significance for use of δ98Mo as a global marine redox proxy

Herrmann, A. D., Kendall, B., Algeo, T. J., Gordon, G. W., Wasylenki, L. E., & Anbar, A. D. (2012). Chemical Geology, 324-325(None), 87–98. doi:10.1016/j.chemgeo.2012.05.013

Formation of Amino Acids and Nucleotide Bases in a Titan Atmosphere Simulation Experiment

Hörst, S. M., Yelle, R. V., Buch, A., Carrasco, N., Cernogora, G., Dutuit, O., … Quirico, E. (2012). Astrobiology, 12(9), 809–817. doi:10.1089/ast.2011.0623

ELECTRON IRRADIATION OF KUIPER BELT SURFACE ICES: TERNARY N 2 -CH 4 -CO MIXTURES AS A CASE STUDY

Kim, Y. S., & Kaiser, R. I. (2012). The Astrophysical Journal, 758(1), 37. doi:10.1088/0004-637x/758/1/37

Deformation associated with ghost craters and basins in volcanic smooth plains on Mercury: Strain analysis and implications for plains evolution

Klimczak, C., Watters, T. R., Ernst, C. M., Freed, A. M., Byrne, P. K., Solomon, S. C., … Blair, D. M. (2012). Journal of Geophysical Research: Planets, 117(E12), n/a–n/a. doi:10.1029/2012je004100

Extending the known range of glycerol ether lipids in the environment: structural assignments based on tandem mass spectral fragmentation patterns

Liu, X-L., Summons, R. E., & Hinrichs, K-U. (2012). Rapid Commun. Mass Spectrom., 26(19), 2295–2302. doi:10.1002/rcm.6355

The O/OREOS Mission: First Science Data from the Space Environment Viability of Organics (SEVO) Payload

Mattioda, A., Cook, A., Ehrenfreund, P., Quinn, R., Ricco, A. J., Squires, D., … Bramall, N. (2012). Astrobiology, 12(9), 841–853. doi:10.1089/ast.2012.0861