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The present review discusses the concept of mineral neoformation which describes the formation of gypsum as the end-product of analogous processes occurring in the atmosphere, in the lichen thallus and on lithic substrates colonized by lichens. The formation of gypsum occurs as a result of H2SO4 reacting with CaCO3. Climate change, e.g. global warming and desertification led to an increasing number of annual dust storms originating in North African deserts, from 5 days in 1958 to 30 days in 2006, i.e. sixfold in 48 years. Calcium is a major constituent of desert dust. The enlarged dust load in the Eastern Mediterranean coincides with the amount of calcium accumulated in lichens: from 6300 mu g g(-1) in 1978 to 36,603 +/- 7563 mu g g(-1) in 2002, i.e. about sixfold in 24 years. Desert dust carrying Ca-containing particles reacts with sulfuric acid produced in the atmosphere following both volcanic and anthropogenic activities. Gypsum produced via neoformation in the atmosphere, precipitates in varying formations, e.g. iberulites. A process of neutralization leads to the formation of biominerals. CaCO3-containing particles entrapped in the lichen thallus react with sulfuric acid to produce gypsum as its end-product, detected in the form of crystals on the outer surface of the thallus. The formation of biogenic gypsum occurs also via the reaction of intra- and extracellular Ca2+ cations with SO42- anions, penetrating into, or found inside thallial cells. The catalytic capability of lichens is evident in the process of neoformation of gypsum on lithic substrates, e.g. granite. (C) 2010 Elsevier B.V. All rights reserved.