Mars May Have Supported Life with Ancient Hydrothermal Activity

Curtin University researchers found evidence of ancient hydrothermal activity on Mars through a 4.45 billion-year-old zircon, hinting at the potential for past life.

Evidence of Hydrothermal Activity on Mars

A groundbreaking investigation from Curtin University has offered tantalizing evidence that Mars may have once harbored hydrothermal activity, suggesting the tantalizing possibility that life could have existed on the Red Planet in its distant past. In this pivotal study, researchers analyzed a zircon grain estimated to be 4.45 billion years old, extracted from the renowned Martian meteorite NWA7034, often referred to as Black Beauty.

Their findings reveal crucial geochemical signals of water-rich fluids, shedding light on how ancient Martian hydrothermal systems linked to volcanic occurrences may have operated.

Implications for the Origins of Life

The research team, led by experts in Earth and planetary sciences, emphasized that these insights pave a path toward a deeper understanding of Mars’ early conditions.

The discovery indicates that hydrothermal systems, which have been integral to the development of life on Earth, likely existed on Mars as well, suggesting that the planet was not devoid of water—a vital ingredient for environments capable of supporting life—during the formation of its primordial crust. Employing advanced nano-scale imaging and spectroscopy techniques, the team revealed distinct elemental patterns within the zircon, detecting the presence of iron, aluminum, yttrium, and sodium.

The implication of these elements in the zircon’s formation underscores the role of water in the planet’s early magmatic processes.

Future Research Directions

This study suggests that even amidst the tumult of significant meteorite impacts and surface disruptions, water persisted on Mars during the Pre-Noachian period, a time frame that exceeds 4.1 billion years ago.

This latest research builds upon earlier findings that the zircon grain had been subjected to shock waves from a meteorite impact, making it the first known instance of such a phenomenon for a Martian zircon. Further exploration into the early conditions of Mars appears promising.

The collaborative efforts of researchers from Curtin’s Space Science and Technology Centre, the John de Laeter Centre, and the University of Adelaide, combined with support from the Australian Research Council, point to a vibrant scientific community dedicated to unraveling the mysteries of our planetary neighbor. The full results of this significant research will be published in the journal Science Advances under the title “Zircon evidence for early hydrothermal activity on Mars.” As scientists continue to piece together the story of Mars, each discovery brings us closer to understanding whether life ever took root beyond Earth.

Study Details:

  • Title: Zircon trace element evidence for early hydrothermal activity on Mars
  • Authors: Jack Gillespie, Aaron J. Cavosie, Denis Fougerouse, Cristiana L. Ciobanu, William D. A. Rickard, David W. Saxey, Gretchen K. Benedix, Phil A. Bland
  • Journal: Science Advances
  • Publication Date: 2024
  • DOI: 10.1126/sciadv.adq3694