From Earth to Mars with micrometeorite volatiles

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• 作者：M. Maurette ; J. Duprat ; C. Engrand and G. Kurat
• 关键词：Micrometeorites ; Atmosphere ; Volatiles ; Mars ; Earth
• 刊名：Advances in Space Research
• 出版年：2006
• 出版时间：2006
• 年：2006
• 卷：38
• 期：4
• 页码：701-708
• 全文大小：202 K

文摘

The contribution of the accretion of ȁc;juvenile” micrometeorites to the volatile inventory of the Martian atmosphere had to mostly occur during the period of the late heavy bombardment of the inner solar system, prior to about 3.5 Ga ago, when the flux of micrometeorites was much higher than today. To assess this contribution, a micrometeorite accretion formula, developed and validated for the Earth, and based on the variation of lunar cratering rates with time, is extrapolated to Mars. This extrapolation suggests that the history of Martian volatiles was more complex than on the Earth. It is described with a two ȁc;shots” scenario involving the two last giant impacts on Mars separated by a time interval of about 500 Ma. The first one was triggered by the last planetary embryo that did merge to Mars thus closing its formation time interval and blowing up its complex pre-impact atmosphere. Thus, a new niche was formed for the accumulation of a dominant micrometeoritic atmosphere during the first 200 Ma of the post-merging period, when the partial pressures of H₂O, CO₂ and N₂ reached about 60, 34 and 0.3 bars, respectively (in water equivalent). This huge amount of water was probably not frozen because an early greenhouse effect was triggered during the simultaneous injection of huge amounts of three strong micrometeoritic greenhouse gases (SO₂, H₂O and CO₂) in the Martian atmosphere. Therefore, early microorganisms could have thrived on early Mars, because micrometeorites likely opened a surprising variety of reaction channels in the prebiotic chemistry of life. But they got likely extinguished a few 100 Ma later, when the last giant impactor, which was probably associated with the spike of bodies that invaded the inner solar system around 4 Ga ago, blew off the earlier massive micrometeoritic atmosphere of Mars and all ingredients of the early greenhouse effect. It thus produced the last ȁc;niche” that allowed the accumulation of the thin and sterile present day Martian atmosphere, and threw the Martian regolith and the in falling micrometeorite water and SO₂ into a deep freeze.