NASA's Curiosity rover has uncovered evidence of a robust ancient carbon cycle on Mars, shedding light on the planet's climate history.
The study, published in Science, found high concentrations of siderite, an iron carbonate mineral, in Martian rock samples collected by the rover.
These findings challenge prior data and suggest Mars once had a thicker, warmer atmosphere capable of supporting liquid water.
The presence of siderite hints at large carbon deposits on Mars, hinting at an ancient carbon cycle that may have sustained habitable conditions.
Scientists believe that Mars had a significantly higher amount of atmospheric CO₂ in the past, with processes like volcanic activity contributing to the planet's climate.
The discovery of carbonate-rich sediments implies that Mars could have trapped substantial amounts of CO₂, impacting its climate transition over time.
The identification of iron oxyhydroxides in the sediments suggests that some trapped CO₂ may have been released back into the atmosphere, temporarily delaying Mars' cooling.
Understanding Mars' ancient carbon cycle provides insights into the planet's habitability over time and may inform future Mars exploration missions.
The study also offers lessons for Earth's climate, as researchers study Mars' natural carbon storage mechanisms to develop strategies for combating climate change.
The delicate balance of habitability on Mars serves as a cautionary tale, highlighting the importance of preserving Earth's environment for sustainable life.