| Q29029771 | A cold-wet middle-latitude environment on Mars during the Hesperian-Amazonian transition: Evidence from northern Arabia valleys and paleolakes |
| Q59795012 | Chaos terrain, storms, and past climate on Mars |
| Q123473422 | High and Dry: Billion‐Year Trends in the Aridity of River‐Forming Climates on Mars |
| Q59153042 | Infrared Spectroscopic Biosignatures from Hidden Cave, New Mexico: Possible Applications for Remote Life Detection |
| Q90884468 | Knickpoints in Martian channels indicate past ocean levels |
| Q104697661 | Late Noachian to Hesperian climate change on Mars: Evidence of episodic warming from transient crater lakes near Ares Vallis |
| Q56114474 | Methane bursts as a trigger for intermittent lake-forming climates on post-Noachian Mars |
| Q101121108 | The Kasei Valles, Mars: a unified record of episodic channel flows and ancient ocean levels |
| Q56939304 | The Nature and Origin of Deposits in Uzboi Vallis on Mars |
| Q60132544 | Thermokarst in Siberian ice-rich permafrost: Comparison to asymmetric scalloped depressions on Mars |