NASA Astrobiology



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

NextPrevious

Go Explore

May 2011Debris 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. (2011). A&A, 530(None), A62. doi:10.1051/0004-6361/201116456

Aragonite Kinetics in Dilute Solutions

Romanek, C. S., Morse, J. W., & Grossman, E. L. (2011). Aquat Geochem, 17(4-5), 339–356. doi:10.1007/s10498-011-9127-2

Field-portable Mossbauer spectroscopy on Earth, the Moon, Mars, and beyond

Schroder, C., Klingelhofer, G., Morris, R. V., Bernhardt, B., Blumers, M., Fleischer, I., … Rodionov, D. S. (2011). Geochemistry: Exploration, Environment, Analysis, 11(2), 129–143. doi:10.1144/1467-7873/09-iags-018

Hydrothermal systems in peridotites at slow-spreading ridges. Modeling phase transformations and material balance: Role of gabbroids

Silantyev, S. A., Novoselov, A. A., & Mironenko, M. V. (2011). Petrology, 19(3), 217–236. doi:10.1134/s0869591111030027

Molecular paleobiological insights into the origin of the Brachiopoda

Sperling, E. A., Pisani, D., & Peterson, K. J. (2011). Evolution & Development, 13(3), 290–303. doi:10.1111/j.1525-142x.2011.00480.x

Molecular Dynamics Simulation of the Antiamoebin Ion Channel: Linking Structure and Conductance

Wilson, M. A., Wei, C., Bjelkmar, P., Wallace, B. A., & Pohorille, A. (2011). Biophysical Journal, 100(10), 2394–2402. doi:10.1016/j.bpj.2011.03.054

Response to Comments on "A Bacterium That Can Grow Using Arsenic Instead of Phosphorus"

Wolfe-Simon, F., Blum, J. S., Kulp, T. R., Gordon, G. W., Hoeft, S. E., Pett-Ridge, J., … Stolz, J. F. (2011). Science, 332(6034), 1149–1149. doi:10.1126/science.1202098

Formation of nitric oxide and nitrous oxide in electron-irradiated H218O/N2 ice mixtures—evidence for the existence of free oxygen atoms in interstellar and solar system analog ices

Zheng, W., Kim, Y. S., & Kaiser, R. I. (2011). Physical Chemistry Chemical Physics, 13(35), 15749. doi:10.1039/c1cp20528e

April 2011THE EFFECTS OF GRAIN SIZE AND GRAIN GROWTH ON THE CHEMICAL EVOLUTION OF COLD DENSE CLOUDS

Acharyya, K., Hassel, G. E., & Herbst, E. (2011). The Astrophysical Journal, 732(2), 73. doi:10.1088/0004-637x/732/2/73

Using CRISPRs as a metagenomic tool to identify microbial hosts of a diffuse flow hydrothermal vent viral assemblage

Anderson, R. E., Brazelton, W. J., & Baross, J. A. (2011). FEMS Microbiology Ecology, 77(1), 120–133. doi:10.1111/j.1574-6941.2011.01090.x

1...329/330/331/332/333...412