A new study, published in the journal Scientific Reports, has ruled out the possibility that the levels of methane detected in the Martian atmosphere could be produced by the wind erosion of rocks, releasing trapped methane from fluid inclusions and fractures on the planets’ surface. A view of Mars showing the planet’s northern polar ice cap. Image credit: ISRO / ISSDC / Emily Lakdawalla. Methane can be produced over time through both geological...