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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February 2008Iron isotope variations in Holocene sediments of the Gotland Deep, Baltic Sea

Fehr, M. A., Andersson, P. S., Hålenius, U., & Mörth, C-M. (2008). Geochimica et Cosmochimica Acta, 72(3), 807–826. doi:10.1016/j.gca.2007.11.033

Detection of cometary amines in samples returned by Stardust

Glavin, D. P., Dworkin, J. P., & Sandford, S. A. (2008). Meteoritics & Planetary Science, 43(1-2), 399–413. doi:10.1111/j.1945-5100.2008.tb00629.x

Reduction of N2 by Fe2+ via Homogeneous and Heterogeneous Reactions

Wander, M. C. F., & Schoonen, M. A. A. (2008). Orig Life Evol Biosph, 38(2), 127–137. doi:10.1007/s11084-008-9122-9

January 2008Iron isotopes constrain biologic and abiologic processes in banded iron formation genesis

Johnson, C. M., Beard, B. L., Klein, C., Beukes, N. J., & Roden, E. E. (2008). Geochimica et Cosmochimica Acta, 72(1), 151–169. doi:10.1016/j.gca.2007.10.013

December 2007Effect of Shadowing on Survival of Bacteria under Conditions Simulating the Martian Atmosphere and UV Radiation

Osman, S., Peeters, Z., La Duc, M. T., Mancinelli, R., Ehrenfreund, P., & Venkateswaran, K. (2007). Applied and Environmental Microbiology, 74(4), 959–970. doi:10.1128/aem.01973-07

June 2007Functional genetic selection of Helix 66 in Escherichia coli 23S rRNA identified the eukaryotic-binding sequence for ribosomal protein L2

Kitahara, K., Kajiura, A., Sato, N. S., & Suzuki, T. (2007). Nucleic Acids Research, 35(12), 4018–4029. doi:10.1093/nar/gkm356

April 2007Formation of Tellurium Nanocrystals during Anaerobic Growth of Bacteria That Use Te Oxyanions as Respiratory Electron Acceptors

Baesman, S. M., Bullen, T. D., Dewald, J., Zhang, D., Curran, S., Islam, F. S., … Oremland, R. S. (2007). Formation of Tellurium Nanocrystals during Anaerobic Growth of Bacteria That Use Te Oxyanions as Respiratory Electron Acceptors. Applied and Environmental Microbiology, 73(7), 2135–2143. doi:10.1128/aem.02558-06

March 2007The Structural Basis of Ribozyme-Catalyzed RNA Assembly

Robertson, M. P., & Scott, W. G. (2007). Science, 315(5818), 1549–1553. doi:10.1126/science.1136231

October 2006A palaeotemperature curve for the Precambrian oceans based on silicon isotopes in cherts

Robert, F., & Chaussidon, M. (2006). A palaeotemperature curve for the Precambrian oceans based on silicon isotopes in cherts. Nature, 443(7114), 969–972. doi:10.1038/nature05239

August 2005Biologically Enhanced Energy and Carbon Cycling on Titan?

Schulze-Makuch, D., & Grinspoon, D. H. (2005). Biologically Enhanced Energy and Carbon Cycling on Titan? Astrobiology, 5(4), 560–567. doi:10.1089/ast.2005.5.560