David T. Vaniman

TL;DR: The Curiosity rover discovered fine-grained sedimentary rocks, which are inferred to represent an ancient lake and preserve evidence of an environment that would have been suited to support a martian biosphere founded on chemolithoautotrophy.

TL;DR: The present status of lunar knowledge based on U.S. and USSR lunar missions and the continuing analysis of lunar samples and data is reviewed in this paper, with particular attention given to exploration, samples, and recent concepts of the moon; the lunar environment; lunar surface processes; the moon minerals, rocks, and regolith; chemical elements in the moon, physical properties of the lunar surface; and global and regional data about the moon.

TL;DR: The Curiosity rover has a designed lifetime of at least one Mars year (∼23 months) and drive capability of up to 20 km as discussed by the authors, and is a scaled version of the Mars Exploration Rovers (MER) Spirit and Opportunity and the Mars Pathfinder Sojourner.

TL;DR: The observations suggest that individual lakes were stable on the ancient surface of Mars for 100 to 10,000 years, a minimum duration when each lake was stable both thermally (as liquid water) and in terms of mass balance (with inputs effectively matching evaporation and loss of water to colder regions).

TL;DR: Sedimentary rocks at Yellowknife Bay (Gale crater) on Mars include mudstone sampled by the Curiosity rover, indicating that clay mineral formation on Mars extended beyond Noachian time.