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Perseverance Study Maps Multiple Water Episodes in Jezero Crater Showing Increasing Habitability

A MIST analysis of PIXL measurements identifies two dozen minerals that record a transition from hot acidic fluids to low‑temperature alkaline conditions.

Overview

  • The peer‑reviewed study in Journal of Geophysical Research: Planets compiles high‑resolution mineral identifications from Perseverance’s first 1,100 sols, led by Rice University’s Eleanor Moreland.
  • Researchers used the MIST algorithm with uncertainty propagation to assign confidence levels to each mineral match and to inform the rover’s sampling strategy.
  • Results outline three alteration phases: localized high‑temperature acidic fluids on the crater floor, more moderate neutral waters over a larger area, and a widespread low‑temperature alkaline episode marked by sepiolite.
  • The mineral framework provides context for separate Nature findings in the Bright Angel formation that report organics and iron‑phosphate/iron‑sulfide microtextures as potential biosignatures that remain unconfirmed without Earth‑lab testing.
  • Perseverance’s cached samples await a return plan as NASA evaluates approaches for retrieval or in‑situ analysis, with the timeline for bringing them to Earth now pushed into the 2040s.