Salt crystals in Chile show how Mars might preserve traces of life
Salar de Pajonales gives Mars researchers a working model for sulfate-hosted biosignatures.๐ท AI-generated / Tech&Space
- โ Salar de Pajonales sits about 3,500 meters above sea level in the extremely dry Andean Altiplano
- โ Gypsum stromatolites contain fossil biosignatures about 4,000 to 6,400 years old and living microbes
- โ Mars has widespread sulfates, including gypsum, so similar sites can guide the search for ancient life
Salar de Pajonales is not a comfortable place for life. It sits about 3,500 meters above sea level in Chile's Andean Altiplano, where temperature swings are sharp, ultraviolet radiation is intense, rainfall is rare, and winds can exceed 100 kilometers per hour. That is exactly why it is scientifically useful. Universe Today describes a new study in Frontiers in Astronomy and Space Sciences showing that gypsum stromatolites in this salt flat preserve two time layers of life. In deeper layers, researchers found fossilized traces of microscopic algae, filamentous structures, and chemical signs of ancient photosynthesis. Only a few millimeters higher, in shallower layers, living microbial communities persist today. That is a rare combination: the same mineral archive shows past and present at once. Gypsum is translucent enough to let in some light, and its crystal structure can retain tiny amounts of water. For microbes in extreme dryness, that can be the difference between disappearance and slow survival.
Salar de Pajonales preserves fossil and living microbes in gypsum, giving researchers a working model for the search in Martian sulfates.
Gypsum can transmit light, hold traces of water, and preserve biological signals in layers.๐ท AI-generated / Tech&Space
Mars is not Salar de Pajonales, but it does have sulfates, including gypsum. Orbital surveys have already shown widespread sulfate deposits, and Perseverance is examining calcium sulfates in Jezero Crater up close. If gypsum on Earth can preserve biosignatures for thousands of years in an extreme environment, Martian sulfates become a reasonable search target. Caution is essential. The Chilean finding does not prove that Mars had life. It also does not prove that organic structures on Mars would necessarily survive. Mineral alteration, radiation, and geological time can erase or distort evidence. But the analog gives researchers a practical map: look for layers, textures, and chemical signatures in minerals that may have protected water and organic remnants. That makes the story stronger than the romantic phrase that life "finds a way." It shows how a trace of life can hide in an ordinary mineral, close enough to the surface to receive light, but protected enough to survive dryness and radiation. Future Mars missions will not be looking for shell-like fossils. They will be looking for tiny chemical and structural differences in rock. Salar de Pajonales shows what such a trace can look like when nature stores it inside a crystalline time capsule.
