Abstract

The Mars Exploration Rover Opportunity investigated plains at Meridiani Planum, where laminated sedimentary rocks are present. The Opportunity rover’s Athena morphological investigation showed microstructures organized in intertwined filaments of microspherules: a texture we have also found on samples of terrestrial (biogenic) stromatolites and other microbialites. We performed a quantitative image analysis to compare images (n=45) of microbialites with the images (n=30) photographed by the rover (corresponding, approximately, to 25,000/15,000 microstructures). Contours were extracted and morphometric indexes were obtained: geometric and algorithmic complexities, entropy, tortuosity, minimum and maximum diameters. Terrestrial and Martian textures present a multifractal aspect. Mean values and confidence intervals from the Martian images overlapped perfectly with those from the terrestrial samples. The probability of this occurring by chance is 1/2 8 , less than p<0.004. Terrestrial abiogenic pseudostromatolites showed a simple fractal structure and different morphometric values from those of the terrestrial biogenic stromatolite images or Martian images with a less ordered texture (p<0.001). Our work shows the presumptive evidence of microbialites in the Martian outcroppings: i.e., the presence of unicellular life on the ancient Mars.

Highlights

  • The Mars Exploration Rover “Opportunity” investigated the landing site in Eagle crater and the nearby plains within Meridiani Planum where flat-lying sedimentary rocks are present

  • As regards microstructures in stromalites, Walter highlighted a great variety of microfabrics, reporting ribboned, striated and lumpy types, and showing that these microfabrics are due to micro-laminated sequence that could be distinct in diffuse or massive [7]

  • As regards Martian sediments, this study undertakes a systematic analysis of black and white Microscopic Images (MI) obtained by Athena (Fig. 1), a camera mounted on the NASA Mars Exploration Rovers (MER) “Opportunity” and “Spirit” [24]

Read more

Summary

Introduction

The Mars Exploration Rover “Opportunity” investigated the landing site in Eagle crater and the nearby plains within Meridiani Planum where flat-lying sedimentary rocks are present. These rocks are finely laminated, are rich in sulfur, and contain abundant sulfate salts. Not without controversy [2], microbialites, such as stromatolites, are often interpreted as the oldest evidence of life on Earth [3,4,5,6]: an interpretation predicated on the assumption that these rocks are formed by microbial mats trapping, binding and/or precipitating minerals. Stromatolites have been defined as “macroscopically layered authigenic microbial sediments”, namely organosedimentary rocks. The term thrombolites [8] was given for not-layered-generally clotted

Methods
Results
Discussion
Conclusion
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.