Bulletin of Taras Shevchenko National University of Kyiv. Astronomy, no. 72, p. 5-9 (2025)

ABOUT LIFE IN “DRY RIVERS” OF MARS

Anatoly VIDMACHENKO, DSc (Phys. & Math.), Prof.
ORCID ID: 0000-0002-0523-5234
e-mail: avidmachenko@gmail.com
National University of Life and Environmental Sciences of Ukraine, Kyiv, Ukraine,
Main astronomical observatory of NAS of Ukraine

Yuliana KUZNYETSOVA, Researcher
ORCID ID: 0000-0001-7750-4395
e-mail: juliana@mao.kiev.ua
Main astronomical observatory of NAS of Ukraine


Abstract

The presence of long valleys, resembling dried-up riverbeds on Earth, should indicate that once upon a time there were conditions on the surface of Mars under which liquid water could exist. Now water in various states is located under the surface of the planet. Areas under the surface could be a kind of oases for possible biological activity. Therefore, they, together with clay-covered areas of Mars, can be a promising place to search for traces of life. The Mars rover “Spirit” was sent to the Gusev crater with a diameter of 180 km located near the equator. The channel of an ancient river flows into this crater. In the past, this crater could have been a lake. The Mars rover “Opportunity” descended into the Eagle crater, located near the equator on the opposite side of Mars from the Gusev crater. An increased concentration of hematite, which on Earth is formed only in an aqueous environment was found there. The main mission of the Perseverance rover is to search for signs of modern bacterial life on Mars, or for its past existence. Observations using spectral instruments on the Perseverance rover have shown that organic molecules have been found in some rocks and in fossilized mud. They are the basis of all life on the planet. There is many evidence that from 3.5 to 2.5 billion years ago, a powerful hydrosphere existed on Mars. Measurements by the Curiosity rover have allowed us to indicate the volume of water lost by Mars. The data obtained have led us to conclude that Mars was not just covered in water in the past but could also retain it in liquid form for hundreds of millions of years. A study of the ratio of deuterium to hydrogen in its atmosphere has led us to conclude that greenhouse gases could retain water in liquid form. Greenhouse gases were quite capable of warming Mars enough to provide a stable climate for millions of years. This allowed conditions to be maintained for chemical evolution, a stage that precedes the emergence of life.

Key words
Mars, polar cap, dry river, water, organics, perchlorates.

References

Becerra, P., Sori, M. M., Thomas, N., Pommerol A., Simioni E., Sutton S., Tulyakov S., & Cremonese G. (2019). Timescales of the climate record in the south polar ice cap of Mars. Geophysical Research Letters, 46(13), 7268–7277. https://doi.org/10.1029/2019GL083588 Chevrier, V. (2022) Limited stability of multi-component brines on the surface of Mars. The Planetary Science Journal, 3(5), 125.
Chevrier, V. F., Hanley, J., & Altheide, T. S. (2009). Stability of perchlorate hydrates and their liquid solutions at the Phoenix landing site, Mars. Geophysical Research Letters, 36(10), L10202. https://doi.org/10.1029/2009GL037497
Clancy, R. T., & Nair, H. (1996). Annual (perihelion-aphelion) cycles in the photochemical behavior of the global Mars atmosphere. Journal of Geophysical Research: Planet, 101(E5), 12785–12790. https://doi.org/10.1029/96JE00836
Conway, S. J., Hovius, N., Barnie, T., Besserer, J., Le Mouélic, S., Orosei, R., & Read, N. (2012). Climate-driven deposition of water ice and the formation of mounds in craters in Mars’ north polar region. Icarus, 220(1), 174–193. https://doi.org/10.1016/j.icarus.2012.04.021
Cutts, J. A. (1973). Nature and origin of layered deposits of the Martian polar regions. Journal of Geophysical Research, 78(20), 4231–4249.
https://doi.org/10.1029/JB078i020p04231
Goldspiel, J. M., & Squyres S. W. (2000) Groundwater sapping and valley formation on Mars. Icarus, 148, 176–192.
Gough, R. V., Chevrier, V. F., & Tolbert, M. A. (2014). Formation of aqueous solutions on Mars via deliquescence of chloride–perchlorate binary mixtures. Earth and Planetary Science Letter, 393, 73–82.
Hecht, M., Kounaves, S. P., Quinn, R. C., West, S. J. , Young, S. M. M., Ming, D. W., Catling, D. C., Clark, B. C., Boynton, W. V., Hoffman, J., DeFlores, L. P., Gospodinova, K., Kapit, J., & Smith, P. H. (2009). Detection of Perchlorate and Soluble Chemistry of Martian Soil at the Phoenix Lander Site. Science, 325(5936), 64–67. https://doi.org/10.1126/science.1172466
Heldmann, J. L., Toon, O. B., Pollard, W. H., Mellon, M. T., Pitlick, J., McKay, C. P., & Andersen, D. T. (2005). Formation of Martian gullies by the action of liquid water flowing under current Martian environmental conditions. Journal Geophysical Research, 110, E05004.
Kuznyetsova, Yu. G., Vidmachenko, A. P., & Steklov, A. F. (2019). What can be called “traces” of life on Mars. 6-th Gamow International Conference in Odessa “New Trends in Astrophysics, Cosmology and HEP after Gamow” and 19-th Gamow Summer School “Astronomy and beyond: Astrophysics, Cosmology, Radioastronomy and Astrobiology” (pp. 52–53). Odesa I. I. Mechnikov National University.
McEwen, A. S., Ojha, L., & Dundas, C. M. (2011). Seasonal Flows on Warm Martian Slopes. Science. American Association for the Advancement of Science, 333(6043), 740–743.
Morozhenko, A. V., & Vidmachenko, A. P. (2017). Optical parameters of Martian dust and its influence on the exploration of Mars. Dust in the Atmosphere of Mars and Its Impact on Human Exploration. Proceedings conference Houston, Texas, 1966, id. 6010. LPI Contribution.
Morozhenko, A. V., & Vidmachenko, A. P. (2020). Dust can affect on the mastering of Mars. 22 International scientific conference Astronomical School of Young Scientists (pp. 71–73). State University “Kyiv Aviation Institute”.
Morozhenko, A. V., Vidmachenko, A. P., & Kostogryz, N. M. (2015). Spectrophotometric properties of Moon’s and Mars’s surfaces exploration by shadow mechanism. Highlights of Astronomy, 16, 182. https://doi.org/10.1017/S1743921314005365
Steklov, A. F., & Vidmachenko, A. P. (2019). Where and What Exactly Can Be the “Traces” of Life on Mars? The Mars Extant Life: What’s Next? LPI Contribution, New Mexico, 2108, id.5089.
Vid’machenko, А. P. (2009а). Research of the Mars by space vehicles. Astronomical School’s Report, 6(2), 131–137.
Vidmachenko, A. P. (2009б). Water on Mars. Astron. almanac. 56, 225–249.
Vidmachenko, A. P. (2016а). Is there life on Mars and where necessary to search for its traces. Astronomy and present: materials of 5 Interregional Scientific Conference (с. 43–48). Vinnytsia Mykhailo Kotsiubynskyi State Pedagogical University.
Vidmachenko, A. P. (2016б). Traces of life on Mars must be sought around the valley Hellas in areas where the water coming out from under the planet’s surface. 18 International scientific conference Astronomical School of Young Scientists (с. 14–16). State University “Kyiv Aviation Institute”.
Vidmachenko, A. P. (2016в). Where is Necessary to Search Traces of Life on Mars? Biosignature Preservation and Detection in Mars Analog Environments. LPI Contribution, Lake Tahoe, Nevada, No. 1912, id. 2002.
Vidmachenko, A. P. (2017). Where Should Search Traces of Life, Which Could Appear on Mars in the First 300 Million Years. Fourth ICo on Early Mars: Geologic, Hydrologic, and Climatic Evolution and the Implications for Life, 2014, id. 3005.
Vidmachenko, A. P., & Morozhenko, O. V. (2014). The physical characteristics of surface Earth-like planets, dwarf and small planets, and their companions, according to distance studies. MAO NASU, NULESU. Publishing House “Profi”.
Vidmachenko, A. P., & Morozhenko, O. V. (2019). Physical parameters of terrestrial planets and their satellites. Editorial and Publishing Department of NULES of Ukraine.

Full text PDF

DOI: https://doi.org/10.17721/BTSNUA.2025.72.5-9