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Planetary science

Into thin martian air

A dense early atmosphere has been invoked to explain the strong greenhouse effect inferred for early Mars. Yet an analysis of the smallest impact craters suggests that the atmospheric pressure on Mars 3.6 billion years ago was surprisingly low.

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Figure 1: The tenuous modern atmosphere of Mars seen from low-elevation orbit by NASA's Viking 1 spacecraft.

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Correspondence to Sanjoy M. Som.

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Som, S. Into thin martian air. Nature Geosci 7, 329–330 (2014). https://doi.org/10.1038/ngeo2145

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