JpGU-AGU Joint Meeting 2017

講演情報

[JJ] 口頭発表

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-CG10] [JJ] 生命-水-鉱物-大気相互作用

2017年5月22日(月) 13:45 〜 15:15 201B (国際会議場 2F)

コンビーナ:中村 謙太郎(東京大学大学院工学系研究科システム創成学専攻)、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)、座長:中村 謙太郎(東京大学大学院工学系研究科システム創成学専攻)、座長:上野 雄一郎(東京工業大学大学院地球惑星科学専攻)

15:00 〜 15:15

[BCG10-06] Abiotic Nitrogen Fixation and Organic Synthesis by Photochemistry on Early Mars

*Zang Xiaofeng1Waka Kawade1Norio Kitadai1,2Yuichiro Ueno1,2 (1.Tokyo Institute of Technology Department of Earth and Planetary Sciences、2.Tokyo Institute of Technology Earth-Life Science Institute)

キーワード:Mars, Nitrogen fixation, amino acid synthesis, UV

Detailed studies of Mars in recent years have provided many progress on understanding the possible view of environment on early Mars. With the fact that liquid water was present on early Mars, and the discovery of organic molecules as well as nitrogen-bearing compounds on Mars, there is possibility that life could have emerged on early Mars. Thus, it is important to understand the abiotic organic synthesis and nitrogen fixation process to evaluate the possible origin of life on Mars or other terrestrial planet. Previous studies suggested that organic matters can be produced by photochemistry. Total pressure of Martian atmosphere is lower than Earth. Thus, UV may penetrated down to the surface and can directly photolyze liquid water. This suggests that UV-induced photochemistry may have been more important. However, little is known about abiotic nitrogen fixation by UV light. This experimental study examines the nitrogen photochemistry at the surface of water. In the experiment, initial gas contains N2O or N2 with or without CO under the presence of liquid water. The starting condition may have existed on early Mars. The results showed that NH3, methylamine, glycine and other amino acids was produced from N2O + CO + H2O, whereas only trace amount of NH3 was formed from N2 + CO + H2O. When gas phase do not contain CO, nitrate and nitrite were produced instead of NH3. A numerical model including 296 photochemical reactions was constructed, and can qualitatively explain the formation of NH3 from N2O. However, the concentration of NH3 in the model is order of magnitude lower than the observed amount in the experiment, suggesting that current photochemical model still lack some possible reactions to generate NH3. The results provide important insights on chemical evolution theory that lead to the origin of life and the atmospheric evolution on Mars when the reaction pathway of NH3 starting from N2O and N2 by UV light is confirmed.