日本地球惑星科学連合2014年大会

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セッション記号 B (地球生命科学) » B-AO 宇宙生物学・生命起源

[B-AO01_28PM1] Astrobiology: Origins, Evolution, Distribution of Life

2014年4月28日(月) 14:15 〜 14:55 502 (5F)

コンビーナ:*小林 憲正(横浜国立大学大学院工学研究院)、山岸 明彦(東京薬科大学生命科学部)、大石 雅寿(国立天文台天文データセンター)、田近 英一(東京大学大学院新領域創成科学研究科複雑理工学専攻)、掛川 武(東北大学大学院理学研究科地学専攻)、井田 茂(東京工業大学大学院理工学研究科地球惑星科学専攻)、座長:山岸 明彦(東京薬科大学生命科学部)、掛川 武(東北大学大学院理学研究科地学専攻)

14:15 〜 14:30

[BAO01-11] 火星初期のハビタブル・トリニティ環境と今後の生命探査計画の候補地

*Dohm James1丸山 茂徳1 (1.東京工業大学地球生命研究所)

キーワード:ハビタブル・トリニティ, 生命の存在可能性

Mars, the most Earth-like planet in our solar system, once had Habitable-Trinity conditions: an interfacing ocean, atmosphere, and nutrient-enriched primordial crustal materials with energy circulation driven by the Sun. Mars is thus considered the best target to search for life beyond Earth, as there are no other planetary bodies in our solar system that record Habitable-Trinity conditions. Following the termination of Habitable Trinity conditions nearly 4.0 Ga, when a strong dynamo shut down prior to the post-heavy-bombardment Hellas and Argyre impact events, the atmosphere was thinning, and plate tectonism was ongoing though waning, life would have found it increasingly difficult to survive at or near the surface, and thus would have migrated to the subterranean to persist. Vent structures, such as those located in the western part of Elysium Planitia where oceans once occupied the Martian surface and long-term magma-water interactions (billions of years) may be still ongoing, as evidenced through pristine lavas, faults that cut youthful surfaces, and geologically-recent flood events, are thus considered to be optimal targets to search for signs of life on Mars. The vent structures were formed by the transferal of subterranean materials to the surface likely due to magma-water interactions. The geologically youthful vent structures could be readily investigated in situ through current mission design.