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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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December 2022A sedimentary record of the evolution of the global marine phosphorus cycle

Planavsky, N. J., Asael, D., Rooney, A. D., Robbins, L. J., Gill, B. C., Dehler, C. M., … Reinhard, C. T. (2022). A sedimentary record of the evolution of the global marine phosphorus cycle. Geobiology. doi:10.1111/gbi.12536

Inclusion of early-career researchers in space missions

Fernando, B., Daubar, I. J., Irving, J. C. E., Johnson, C. L., Marusiak, A. G., Baker, M. M., & Stanley, S. (2022). Inclusion of early-career researchers in space missions. Nature Astronomy, 6(12), 1339–1341. doi:10.1038/s41550-022-01861-2

Mineral-catalysed formation of marine NO and N2O on the anoxic early Earth

Buessecker, S., Imanaka, H., Ely, T., Hu, R., Romaniello, S. J., & Cadillo-Quiroz, H. (2022). Mineral-catalysed formation of marine NO and N2O on the anoxic early Earth. Nature Geoscience, 15(12), 1056–1063. doi:10.1038/s41561-022-01089-9

Surface‐To‐Ocean Exchange by the Sinking of Impact Generated Melt Chambers on Europa

Carnahan, E., Vance, S. D., Cox, R., & Hesse, M. A. (2022). Surface‐To‐Ocean Exchange by the Sinking of Impact Generated Melt Chambers on Europa. Geophysical Research Letters, 49(24), None. doi:10.1029/2022gl100287

Evidence for the volatile-rich composition of a 1.5-Earth-radius planet

Piaulet, C., Benneke, B., Almenara, J. M., Dragomir, D., Knutson, H. A., Thorngren, D., … Wong, I. (2022). Evidence for the volatile-rich composition of a 1.5-Earth-radius planet. Nature Astronomy. doi:10.1038/s41550-022-01835-4

Co‐Creating Ethical Practices and Approaches for Fieldwork

Ryan‐Davis, J., & Scalice, D. (2022). Co‐Creating Ethical Practices and Approaches for Fieldwork. AGU Advances, 3(6), None. doi:10.1029/2022av000762

New interpretations of lunar mare basalt flow emplacement from XCT analysis of Apollo samples

Gawronska, A. J., McLeod, C. L., Blumenfeld, E. H., Hanna, R. D., & Zeigler, R. A. (2022). New interpretations of lunar mare basalt flow emplacement from XCT analysis of Apollo samples. Icarus, 388, 115216. doi:10.1016/j.icarus.2022.115216

Creative destruction: New protein folds from old

Alvarez-Carreño, C., Gupta, R. J., Petrov, A. S., & Williams, L. D. (2022). Creative destruction: New protein folds from old. Proceedings of the National Academy of Sciences, 119(52), None. doi:10.1073/pnas.2207897119

Close Trans-Neptunian Object Passages as a Driver of the Origin and Evolution of Ultrawide Kuiper Belt Binaries

Campbell, H. M., Stone, L. R., & Kaib, N. A. (2022). Close Trans-Neptunian Object Passages as a Driver of the Origin and Evolution of Ultrawide Kuiper Belt Binaries. The Astronomical Journal, 165(1), 19. doi:10.3847/1538-3881/aca08e

Cycling of CO2 and H2O constrained by experimental investigation of a model ophicarbonate at deep subduction zone conditions

Eguchi, J., & Dasgupta, R. (2022). Cycling of CO2 and H2O constrained by experimental investigation of a model ophicarbonate at deep subduction zone conditions. Earth and Planetary Science Letters, 600, 117866. doi:10.1016/j.epsl.2022.117866