NASA Astrobiology

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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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September 2015Dissolved amino acids in oceanic basaltic basement fluids

Lin, H-T., Amend, J. P., LaRowe, D. E., Bingham, J-P., & Cowen, J. P. (2015). Geochimica et Cosmochimica Acta, 164(None), 175–190. doi:10.1016/j.gca.2015.04.044

The molecular record of Cryogenian sponges - a response to Antcliffe (2013)

Love, G. D., & Summons, R. E. (2015). Palaeontology, 58(6), 1131–1136. doi:10.1111/pala.12196

Single cell activity reveals direct electron transfer in methanotrophic consortia

McGlynn, S. E., Chadwick, G. L., Kempes, C. P., & Orphan, V. J. (2015). Nature, 526(7574), 531–535. doi:10.1038/nature15512

Investigation of the Role of Polysaccharide in the Dolomite Growth at Low Temperature by Using Atomistic Simulations

Shen, Z., Szlufarska, I., Brown, P. E., & Xu, H. (2015). Langmuir, 31(38), 10435–10442. doi:10.1021/acs.langmuir.5b02025

Integrated stratigraphic, geochemical, and paleontological late Ediacaran to early Cambrian records from southwestern Mongolia

Smith, E. F., Macdonald, F. A., Petach, T. A., Bold, U., & Schrag, D. P. (2015). Geological Society of America Bulletin, None(None), B31248.1. doi:10.1130/b31248.1

Depositional and preservational environments of the Ediacara Member, Rawnsley Quartzite (South Australia): Assessment of paleoenvironmental proxies and the timing of ‘ferruginization’

Tarhan, L. G., Droser, M. L., & Gehling, J. G. (2015). Palaeogeography, Palaeoclimatology, Palaeoecology, 434(None), 4–13. doi:10.1016/j.palaeo.2015.04.026

An examination of the evolution of Ediacaran paleoenvironmental and paleoecological research

Tarhan, L., & Laflamme, M. (2015). Palaeogeography, Palaeoclimatology, Palaeoecology, 434(None), 1–3. doi:10.1016/j.palaeo.2015.04.012

Indigenous aliphatic amines in the aqueously altered Orgueil meteorite

Aponte, J. C., Dworkin, J. P., & Elsila, J. E. (2015). Meteoritics & Planetary Science, 50(10), 1733–1749. doi:10.1111/maps.12507

The Proterozoic Record of Eukaryotes

Cohen, P. A., & Macdonald, F. A. (2015). Paleobiology, 41(04), 610–632. doi:10.1017/pab.2015.25

Biotic replacement and mass extinction of the Ediacara biota

Darroch, S. A. F., Sperling, E. A., Boag, T. H., Racicot, R. A., Mason, S. J., Morgan, A. S., … Tweedt, S. (2015). Proc. R. Soc. B, 282(1814), 20151003. doi:10.1098/rspb.2015.1003

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