The past of Mars has become even more complex after data collected by NASA's Perseverance rover showed that one area in Jezero Crater was exposed to water at least three different times. Each episode altered the chemical composition and appearance of the rocks.
This discovery was made when the rover reached the inner boundary of the crater in September 2023. The area, named the 'Margin Unit,' extends along the edge of an ancient Martian lake.
Scientists initially expected to find sedimentary rocks formed by the accumulation of sand layers over millennia. These expectations were also based on the strong presence of carbonate minerals detected by orbital probes. On Earth, carbonates often form in shallow marine environments of oceans and lakes capable of supporting life.
However, Perseverance found igneous rocks that can form deep underground from magma or as a result of volcanic activity on the surface. According to NASA, these rocks are important chronicles of the past because mineral crystals preserve details of their formation moment. In the case of the Margin Unit, they recorded a particularly complex history of water activity in early Mars.
The team managed to determine the sequence of water interactions with the rocks, although the age of each episode could not yet be established. The first episode occurred when groundwater rich in carbon dioxide reacted with olivine present in the rocks. This process created carbonate in the rock fissures in lower-lying areas. Currently, these carbonate-filled fissures remain elevated structures, while the softer surrounding rocks have undergone erosion.
The second episode may be related to an ancient lake that occupied the crater. Some rocks in the Margin Unit also contain silica. According to planetary scientist Eleni Ravanis from the University of Hawaii at Manoa and co-author of the study, the transformation of olivine into carbonate can leave behind silica. The team found more of this mineral in rocks located below the water level.
The third and last identified event involved the formation of mineral veins in one spot in the eastern part of the Margin Unit. These structures are about 25 centimeters thick and contain minerals such as calcium sulfate and fluorite. The presence of fluorite attracted the researchers' attention, as this mineral usually forms during the circulation of hot water through volcanic rocks. This discovery indicates that the region subsequently experienced an episode of heated groundwater.
The Perseverance rover traveled approximately 265 meters in elevation while exploring the Margin Unit. On the highest parts, it found granular and crystalline rocks characteristic of olivine, with slight signs of contact with water. This olivine unit formed from magma deep within the crust. Cooling occurred slowly, allowing crystals to grow. The rocks only reached the surface after the overlying soil underwent erosion.
In the lowest parts, near the old lakebed, the rocks show signs of transformation: olivine grains are fractured, and silica is present between them. Carbonates and silica are important for studying ancient life. When water interacts with olivine on Earth, the reaction can release hydrogen, which serves as a food source for some microorganisms. The process also leaves behind carbonate and silica—minerals capable of preserving traces of the existence of these microorganisms.


