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Mars Simulation Laboratory

Mars seen from Phoenix lander — Photo: NASA

Phoenix lander — Photo: NASA

Interdisciplinary research

Biology
Chemistry
Geology
Physics

Search for answers to questions such as:

Could Mars ever have support life?

Could life today be present below the surface?

Which processes formed the morphology of Mars?

What causes the oxidizing state of the surface?

Does the atmospheric CO₂pressure vary?

How did the dust on Mars become red?

Publications - Mars Simulation Laboratory

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Gunnlaugsson, H. P., Höskuldsson, Á., Steinthorsson, S., Óskarsson, , N., Madsen, M. B., Nørnberg, P., Merrison, J. P. & Larsen, G. (2014). Mössbauer spectroscopy of samples from the 2010 Fimmvörðuháls/Eyjafjallajökull eruption. Hyperfine Interactions, 226(1-3), 601-612. https://doi.org/10.1007/s10751-013-0915-5

Gunnlaugsson, H. P., Rasmussen, H., Kristjansson, L., Steinthorsson, S., Helgason, O., Nørnberg, P., Madsen, M. B. & Morup, S. (2008). Mossbauer spectroscopy of magnetic minerals in basalt on Earth and Mars. Hyperfine Interactions, 182(1-3), 87-101.

Mølholt, T. E., Gunnlaugsson, H. P., Merrison, J. P., Morris, R. V. & Nørnberg, P. (2008). Mössbauer and VNIR study of dust generated from olivine basalt: application to Mars. Hyperfine Interactions, 127–133. https://doi.org/10.1007/s10751-008-9842-2

Nørnberg, P., Schwertmann, U., Stanjek, H., Andersen, T. & Gunnlaugsson, H. P. (2004). Mineralogy of a burned soil compared with four anomalously red Quaternary deposits in Denmark. Clay Minerals, 39, 85.

Merrison, J. P., Gunnlaugsson, H. P., Jensen, S. K. & Nørnberg, P. (2010). Mineral alteration induced by sand transport: a source for the reddish color of martian dust: A source for the reddish color of Martian dust. Icarus, 205(2), 716-718. https://doi.org/10.1016/j.icarus.2009.09.004

Kolchev, I., Marshall, I. P. G., Jones, E., Yde, J. C., Nørnberg, P., Rivera, A. M., Hodson, A. J., Bak, E. N. & Finster, K. (2022). Microbial iron reduction and greenhouse gas production in response to organic matter amendment and temperature increase of periglacial sediments, Bolterdalen, Svalbard. Arctic, Antarctic, and Alpine Research, 54(1), 314-334. https://doi.org/10.1080/15230430.2022.2097757

Bak, E. N., Jensen, S. K., Nørnberg, P. & Finster, K. (2016). Methylated silicates may explain the release of chlorinated methane from Martian soil. Earth and Planetary Science Letters, 433, 226-231. https://doi.org/10.1016/j.epsl.2015.10.044

Nørnberg, P., Finster, K., Thøgersen, J., Golbek, T. W., Weidner, T., Hassenkam, T., Goetz, W., Oehlke, M. & Knak Jensen, S. J. (2022). Methane as a reddish coating agent. Icarus, 382, Article 115023. https://doi.org/10.1016/j.icarus.2022.115023

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Revised 14.02.2025

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Kai Finster