日本地球惑星科学連合2015年大会

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セッション記号 B (地球生命科学) » B-CG 地球生命科学複合領域・一般

[B-CG28] 生命-水-鉱物-大気相互作用

2015年5月26日(火) 18:15 〜 19:30 コンベンションホール (2F)

コンビーナ:*白石 史人(広島大学大学院理学研究科地球惑星システム学専攻)、大竹 翼(北海道大学大学院工学研究院 環境循環システム部門)、鈴木 庸平(東京大学大学院理学系研究科)、高井 研(海洋研究開発機構極限環境生物圏研究センター)、上野 雄一郎(東京工業大学大学院地球惑星科学専攻)、長沼 毅(広島大学大学院生物圏科学研究科)、掛川 武(東北大学大学院理学研究科地学専攻)、横山 正(大阪大学大学院理学研究科宇宙地球科学専攻)、中村 謙太郎(独立行政法人海洋研究開発機構 (JAMSTEC) システム地球ラボ プレカンブリアンエコシステムラボユニット)

18:15 〜 19:30

[BCG28-P02] 衝撃波によるストレッカー型アミノ酸合成の実験的検討

*梅田 悠平1永露 健太1関根 利守1網本 智子1小林 敬道2 (1.広島大学理学研究科、2.物質材料研究機構)

Amino acid is thought to be one of the most primary biomolecules related to the origin of life. The prebiotic syntheses of amino acids under early Earth condition were simulated in experiments using by several energies such as electric discharge, light, heat and shock wave. According to a previous study by Aubrey et al., 2009, it is considered that amino acid formation from ammonium formate (NH4HCO2) depends mainly on concentration of starting materials. It has been known that ammonium formate can produce HCN above 180 oC, and that HCN is a necessary material in order to synthesize amino acid via strecker reaction. Strecker reaction is used for syntheses of amino acids in the presence of NH3 and HCN. These molecules can be easily formed from ammonium formate at high temperature. They performed hydrothermal experiments at concentrations of 0.1 M and 0.001 M. Then, amino acids such as glycine and alanine were formed from only a high concentration sample (0.1 M). However, this concentration is unrealistically too high for natural marine conditions. We need to know the effect of shock energy on the formation.
In this study, we carried out shock recovery experiments using a propellant gun for aqueous solutions of ammonium formate and formamide. Starting material, encapsulated in steel container as a target, was ammonium formate or formamide aqueous solution immersed in the pressed olivine powder. We used two concentrations (5 mM and 100 mM) to compare with the results of hydrothermal experiments. Olivine was simulated as ordinary chondrite. The peak pressure in this study was about 5 GPa. Recovered solutions were analyzed by using hybrid/MS for biomolecules of the m/z values between 50 and 500 with analytical errors within 3 mmu (0.003). The results indicated that glycine and glycylglycine were detected in all samples and that benzoic acid as carboxylic acid was detected in only formamide samples. Present results suggest that glycine formation by shock reaction might be more effective than that of hydrothermal reaction because glycine was formed from low concentration samples. Detailed discussions will be given as poster.