日本地球惑星科学連合2023年大会

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[J] 口頭発表

セッション記号 P (宇宙惑星科学) » P-CG 宇宙惑星科学複合領域・一般

[P-CG20] 宇宙における物質の形成と進化

2023年5月25日(木) 10:45 〜 12:00 展示場特設会場 (2) (幕張メッセ国際展示場)

コンビーナ:荒川 創太(海洋研究開発機構)、大坪 貴文(自然科学研究機構 国立天文台)、野村 英子(国立天文台 科学研究部)、瀧川 晶(東京大学 大学院理学系研究科 地球惑星科学専攻)、座長:古家 健次(国立天文台)、石﨑 梨理(東京大学大学院理学系研究科地球惑星科学専攻)


11:45 〜 12:00

[PCG20-11] Micrometer-scale distributions of small organic compounds in meteorites: implications to organic synthesis before asteroid accretion

★Invited Papers

*古川 善博1、三枝 大輔2、可野 邦行3、宇留野 晃1、齋藤 律水1伊藤 元雄4松本 恵1、青木 淳賢3、山本 雅之1中村 智樹1 (1.東北大学、2.帝京大学、3.東京大学、4.海洋研究開発機構)

キーワード:質量分析イメージング、隕石、有機物、原始太陽系円盤

Carbonaceous chondrites contain diverse small soluble organic compounds that formed and processed in the early solar system, including in the proto-solar nebula, proto-solar disk, and asteroids. These organic compounds may provide hints for understanding the early evolution of the solar system. In most cases, these organic compounds have been investigated in extracts of several hundred milligrams of meteorite powders due to the lack of suitable analytical methods in less than millimeter-scale resolution. Thus, their spatial distributions have been unclear. We investigated micrometer-scale distributions of small organic compounds in two carbonaceous chondrites (Murchison and NWA 801) using a surface-assisted laser desorption/ionization system connected to a high mass-resolution mass spectrometer. Distributions of diverse mass signals (i.e., more than 220,000 signals) with different elemental compositions of organic compounds were acquired from the meteorites. The distributions were categorized into 20 clusters by hierarchical cluster analysis. One cluster is occupied by the signals that have diverse CHN1-2 and CHN1-2O compounds in each meteorite. These compounds contained mutual relationships of ±H2, ±CH2, ±H2O, and ±CH2O and showed highly similar distributions, indicating that they are the products of series reactions. The spatial distributions were highly heterogeneous due to the micro-scale difference in the abundance of these compounds, indicating the formation of these compounds on individual dust particles before asteroid accretion. The compositions of diverse small organic compounds associated with individual dust particles in meteorites are useful for understanding different histories of volatile evolution in the early solar system.