Desert varnish is a thin, dark coating found on rock surfaces in arid environments. It is primarily composed of clay minerals, manganese () oxides, and iron () oxides. Two scientists discuss the mechanism behind its formation.
Scientist 1
Desert varnish is formed biochemically by manganese-oxidizing bacteria (such as the genus ). These bacteria inhabit rock surfaces and utilize soluble divalent manganese () from windborne dust as an energy source, oxidizing it to insoluble tetravalent manganese () oxides. These oxides, along with clay particles, are cemented to the rock surface by bacterial extracellular polymeric substances (EPS). This biochemical process requires living microbial cells, organic carbon nutrients, and trace liquid water.
Scientist 2
Desert varnish forms through a purely inorganic chemical-physical process. During wet periods, dew or light rain dissolves amorphous silica () and trace metals from windborne dust on rock surfaces. As the rock heats and dries, the silica precipitates, forming a silica-rich glaze. This glaze physically traps ambient, pre-oxidized manganese and iron oxides from the dust, cementing them to the rock. This process does not require living organisms, organic nutrients, or biological activity, and can occur in completely sterile environments.
Which of the following experimental procedures would provide the most definitive evidence to resolve the conflict between the two scientists' models?
- Place sterile rock slabs and sterile, synthetic dust (containing , , and no organic carbon or microbes) in a sealed chamber, subject them to repeated wetting and drying cycles under high heat and UV light, and analyze if a manganese-rich glaze forms.Answer
- BCollect desert varnish samples from various geographic regions and measure both the total organic carbon content and the ratio of to in the coating.
- CInoculate a nutrient-rich agar plate containing soluble with bacteria, expose the plates to different temperatures, and measure the rate of bacterial colony growth.
- DIntroduce bacteria to rock samples in a humid, nutrient-rich environment, then vary the concentrations of both silica () and iron () oxides simultaneously to observe which component is deposited faster.