Research news on diagenesis

Diagenesis is the suite of physical, chemical, and biological processes that alter unconsolidated sediments after deposition and during and after lithification, excluding surface weathering and high-grade metamorphism. It encompasses compaction, cementation, dissolution, recrystallization, authigenic mineral formation, and fluid–rock interaction within low-temperature and low-pressure regimes of the upper crust. Diagenetic reactions modify porosity, permeability, mineralogy, and geochemical signatures, critically influencing reservoir quality, basin evolution, and the preservation or alteration of primary paleoenvironmental and paleoecological signals. Diagenetic pathways are controlled by factors such as sediment composition, burial history, pore-fluid chemistry, redox conditions, and thermal gradients.

Organic carbon detected in Bright Angel rock formation on Mars

In September 2025, NASA announced that its Perseverance rover had discovered a potential biosignature, which is a substance or structure that might have a biological origin. A new paper, published in Science Advances, unambiguously ...

The time capsule in the salt flat

There is a place in northern Chile, 3,500 meters above sea level in the Andean Altiplano, where almost nothing survives. The Salar de Pajonales is a salt flat of savage extremes temperatures swinging from −23°C to 26°C, solar ...