Title : The early heat loss evolution of Mars and their implications for internal and environmental history.

Pub. Date : 2014 Mar 11

PMID : 24614056






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1 The time around 3.7 Ga ago was an epoch when substantial changes in Mars occurred: a substantial decline in aqueous erosion/degradation of landscape features; a change from abundant phyllosilicate formation to abundant acidic and evaporitic mineralogy; a change from olivine-rich volcanism to olivine-pyroxene volcanism; and maybe the cessation of the martian dynamo. olivine methionyl-tRNA synthetase 1 Homo sapiens