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the Martian southern hemispheric highlands, and stand as a reflect of an ancient past characterized by active hydrology and surface liquid water. After a peak of valley network formation around ~3.8 Byr ago
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to the oceans. In the ECZ, soils are metal sinks, especially wetlands. Their hydrological cycle (high water/low water) favors the formation of chemical gradients and biogeochemical processes controlling the metal
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