Ancient alluvial plains at Oxia Planum, Mars

Davis, Joel M.; Balme, Matthew R.; Fawdon, Peter; Grindrod, Peter M.; Favaro, Elena A.; Banham, Steven G.; Thomas, Nicolas (2023). Ancient alluvial plains at Oxia Planum, Mars. Earth and planetary science letters, 601 Elsevier 10.1016/j.epsl.2022.117904

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The geologic origin of the ancient, phyllosilicate-bearing bedrock at Oxia Planum, Mars, the ExoMars rover landing site, is unknown. The phyllosilicates record ancient aqueous processes, but the processes that formed the host bedrock remain elusive. Here, we use high-resolution orbital and topographic datasets from the HiRISE, CaSSIS and CTX instruments to investigate and characterize fluvial sinuous ridges (FSRs), found across the Oxia Planum region. The FSRs form segments up to 70 km long, are 20-600 m wide, and up to 9 m in height, with sub-horizontal layering common in ridge margins. Some FSRs comprise multi-story ridge systems; many are embedded within the phyllosilicate-bearing bedrock. We interpret the FSRs at Oxia Planum as deposits of ancient, episodically active, alluvial river systems (channel-belt and overbank deposits). Thus, at least some of the phyllosilicate-bearing bedrock was formed by ancient alluvial rivers, active across the wider region, though we do not exclude other processes from contributing to its formation as well. The presence of alluvial floodplains at Oxia Planum increases the chances of the ExoMars rover detecting signs of ancient life. Future exploration by the ExoMars rover can verify the alluvial interpretation and provides an opportunity to investigate some of the oldest river deposits in the Solar System.

Item Type:

Journal Article (Original Article)

Division/Institute:

08 Faculty of Science > Physics Institute > Space Research and Planetary Sciences
08 Faculty of Science > Physics Institute
10 Strategic Research Centers > Center for Space and Habitability (CSH)
08 Faculty of Science > Physics Institute > NCCR PlanetS

UniBE Contributor:

Thomas, Nicolas

Subjects:

500 Science > 520 Astronomy
600 Technology > 620 Engineering
000 Computer science, knowledge & systems
500 Science
500 Science > 530 Physics

ISSN:

0012-821X

Publisher:

Elsevier

Language:

English

Submitter:

Agnès Véronique Schär Vuillemin

Date Deposited:

04 Apr 2024 12:07

Last Modified:

04 Apr 2024 12:07

Publisher DOI:

10.1016/j.epsl.2022.117904

Uncontrolled Keywords:

Mars; remote sensing; geomorphology; surface processes; landing sites; planetary science

BORIS DOI:

10.48350/195498

URI:

https://boris.unibe.ch/id/eprint/195498

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