Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/30876
Appears in Collections:Biological and Environmental Sciences Journal Articles
Peer Review Status: Refereed
Title: Laboratory analysis of returned samples from the AMADEE-18 Mars analog mission
Author(s): Lalla, Emmanuel Alexis
Cote, Kristen
Hickson, Dylan
Garnitsching, Stefanie
Konstantinidis, Menelaos
Such, Pamela
Czakler, Christine
Schroeder, Christian
Frigeri, Allesandro
Ercoli, Maurizio
Losiak, Anna
Gruber, Sophie
Groemer, Gernot
Contact Email: christian.schroeder@stir.ac.uk
Keywords: Planetary exploration
combined instrumentation methods
Astrobiology
simulated space mission
Issue Date: 2020
Citation: Lalla E, Cote K, Hickson D, Garnitsching S, Konstantinidis M, Such P, Czakler C, Schroeder C, Frigeri A, Ercoli M, Losiak A, Gruber S & Groemer G (2020) Laboratory analysis of returned samples from the AMADEE-18 Mars analog mission. Astrobiology, 20 (11), pp. 1303-1320. https://doi.org/10.1089/ast.2019.2038
Abstract: Between 01-28. February 2018, the Austrian Space Forum, in cooperation with the Oman Astronomical Society and research teams from 25 nations conducted the AMADEE-18 mission, a human-robotic Mars expedition simulation in the Dhofar region in the Sultanate of Oman As a part of the AMADEE-18 simulated Mars human exploration mission, the Remote Science Support team performed analysis of the Dhofar area, (Oman) in order to characterize it as a potential Mars analog site. The main motivation of this research was to study and register selected samples collected by the analog astronauts during the AMADEE-18 mission with laboratory analytical methods and techniques comparable to the techniques that will be used on Mars in the future. The 25 samples representing unconsolidated sediments obtained during the simulated mission were studied by using optical microscopy, Raman spectroscopy, X-ray diffraction, laser-induced breakdown spectroscopy, and laser-induced fluorescence. The principal results showed the existence of minerals and the detection of alteration processes related to volcanism, hydrothermalism, and weathering. The analogy between the Dhofar region and the Eridana Basin region of Mars is clearly noticeable, particularly as an analog for secondary minerals formed in a hydrothermal seafloor volcanic-sedimentary environment. The synergy between the techniques used in the present work provides a solid basis for the geochemical analyses and organic detection in the context of future human-robotic Mars expeditions. AMADEE-18 has been a prime test bed for geoscientific workflows with astrobiological relevance and has provided valuable insights for future space missions.
DOI Link: 10.1089/ast.2019.2038
Rights: This item has been embargoed for a period. During the embargo please use the Request a Copy feature at the foot of the Repository record to request a copy directly from the author. You can only request a copy if you wish to use this work for your own research or private study. Final publication is available from Mary Ann Liebert, Inc., publishers https://doi.org/10.1089/ast.2019.2038
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