“…The La Brava and La Punta lacustrine systems, located in the Tilopozo sector in the extreme south of the Salar de Atacama, are high-altitude Andean lakes (HAALs) along the central Andes of South America ( 2 , 3 ). Seasonal and long-term variations in precipitation and evaporation, among other natural factors, generate changes in the behavioral dynamics of the water column in La Brava and La Punta lakes ( 4 , 5 ), developing areas with greater persistence over time, as well as others with retreat or disappearance during the dry season, called temporary waters ( 6 – 8 ). These dynamics causes physicochemical changes in the water column and superficial sediments, such as low nutrient availability ( 3 ), pH change ( 9 ), dissolved metals ( 10 , 11 ), and other factors that can influence the composition and species richness of the microbiota ( 12 , 13 ).…”