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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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November 2014Dissolved hydrogen and methane in the oceanic basaltic biosphere

Lin, H-T., Cowen, J. P., Olson, E. J., Lilley, M. D., Jungbluth, S. P., Wilson, S. T., & Rappé, M. S. (2014). Earth and Planetary Science Letters, 405(None), 62–73. doi:10.1016/j.epsl.2014.07.037

Evidence of Titan’s climate history from evaporite distribution

MacKenzie, S. M., Barnes, J. W., Sotin, C., Soderblom, J. M., Le Mouélic, S., Rodriguez, S., … Baines, K. H. (2014). Icarus, 243(None), 191–207. doi:10.1016/j.icarus.2014.08.022

Dissolution of benzene, naphthalene, and biphenyl in a simulated Titan lake

Malaska, M. J., & Hodyss, R. (2014). Icarus, 242(None), 74–81. doi:10.1016/j.icarus.2014.07.022

The affect of the space environment on the survival of Halorubrum chaoviator and Synechococcus (Nägeli): data from the Space Experiment OSMO on EXPOSE-R

Mancinelli, R. L. (2014). International Journal of Astrobiology, 14(01), 123–128. doi:10.1017/s147355041400055x

In-situ characterization of oxalic acid breakdown at elevated P and T: Implications for organic C-O-H fluid sources in petrologic experiments

McCubbin, F. M., Sverjensky, D. A., Steele, A., & Mysen, B. O. (2014). American Mineralogist, 99(11-12), 2258–2271. doi:10.2138/am-2014-4947

Nitrogen stable isotope composition and the origins of cupric nitrate mineralization

Melchiorre, E. B., & Talyn, B. C. (2014). Chemical Geology, 388(None), 1–8. doi:10.1016/j.chemgeo.2014.08.031

Thermostable Artificial Enzyme Isolated by In Vitro Selection

Morelli, A., Haugner, J., & Seelig, B. (2014). PLoS ONE, 9(11), e112028. doi:10.1371/journal.pone.0112028

Proposal to rename Carnobacterium inhibens as Carnobacterium inhibens subsp. inhibens subsp. nov. and description of Carnobacterium inhibens subsp. gilichinskyi subsp. nov., a psychrotolerant bacterium isolated from Siberian permafrost

Nicholson, W. L., Zhalnina, K., De Oliveira, R. R., & Triplett, E. W. (2014). INTERNATIONAL JOURNAL OF SYSTEMATIC AND EVOLUTIONARY MICROBIOLOGY, 65(Pt 2), 556–561. doi:10.1099/ijs.0.067983-0

VOLATILE-RICH CIRCUMSTELLAR GAS IN THE UNUSUAL 49 CETI DEBRIS DISK

Roberge, A., Welsh, B. Y., Kamp, I., Weinberger, A. J., & Grady, C. A. (2014). The Astrophysical Journal, 796(1), L11. doi:10.1088/2041-8205/796/1/l11

Path-integral calculation for the emergence of rapid evolution from demographic stochasticity

Shih, H-Y., & Goldenfeld, N. (2014). Phys. Rev. E, 90(5), None. doi:10.1103/physreve.90.050702