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2023
DOI: 10.1029/2022je007474
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Samples Collected From the Floor of Jezero Crater With the Mars 2020 Perseverance Rover

Abstract: Nine samples, consisting of four pairs of rock cores and a tube of atmospheric gas, were collected from the floor of Jezero Crater, Mars.• In situ observations of crater floor outcrops, used as proxies for the samples, reveal aqueously altered igneous lithologies.• Perseverance will leave one sample from each pair at the Three Forks depot and retain a second to be cached with future samples.

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Cited by 38 publications
(69 citation statements)
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References 171 publications
(350 reference statements)
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“…The crater density is in N/km 2 . The pink stars denote the two locations of the 4 collected samples of the floor unit by Perseverance (Simon et al., 2023). (b) Map of the craters >170 m of both the main delta fan and the dark floor unit with a color code as a function of their size.…”
Section: Methodsmentioning
confidence: 99%
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“…The crater density is in N/km 2 . The pink stars denote the two locations of the 4 collected samples of the floor unit by Perseverance (Simon et al., 2023). (b) Map of the craters >170 m of both the main delta fan and the dark floor unit with a color code as a function of their size.…”
Section: Methodsmentioning
confidence: 99%
“…During the first ∼380 sols of the mission, the dark crater floor unit, referred to as the Máaz formation by the Mars 2020 team (Farley et al, 2022), has been investigated using the payload on the Perseverance rover. Four samples have been collected from this unit: Montagnac and Montdenier from the Rochette member of the Artuby ridge, a widespread caprock layer within Máaz, and Hahonih and Atsah from the upper crater-retaining top of Maaz (Simon et al, 2023). The results of Perseverance's crater floor scientific campaign (Sun et al, 2022) show that the dark floor unit is composed of holocrystalline igneous rocks dominated by pyroxene and plagioclase with limited aqueous alteration (Farley et al, 2022;Mandon et al, 2022;Udry et al, 2022;Wiens et al, 2022).…”
Section: Introductionmentioning
confidence: 99%
“…Science observations would be made and analyzed quickly to establish the database of Séítah formation compositions and facies and to determine which Séítah outcrops to sample. Early images of Séítah showed apparent layering (Figure 3g), which raised the possibility that Séítah could potentially be a sedimentary deposit with fine‐grained rocks that would be of high sampling interest (Section 3.3.2; Farley et al., 2020; Simon et al., 2023). If a sedimentary fine‐grained Séítah rock could not be found or sampled, the team would instead sample a representative rock from Séítah that is olivine‐rich and potentially carbonate‐bearing, as this could be correlated to the major olivine‐bearing unit inside and potentially outside Jezero and would likely be the best indication of past water activity and thus habitability so far observed (Section 2.2.1).…”
Section: Crater Floor Campaign Objectives and Notional Planmentioning
confidence: 99%
“…Purple coatings (purple arrows in Figure 17d) were once again observed on the natural surface of the rock, and even though the Brac rock appears layered, no evidence of layering was observed in the Dourbes abrasion patch. The first Séítah sample, Salette, was then collected on sol 262 and its sample pair, Coulettes, was acquired on sol 271 (Simon et al., 2023).…”
Section: Crater Floor Campaign Narrativementioning
confidence: 99%
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