カワムラ クニオ
KAWAMURA Kunio 川村 邦男 所属 広島修道大学 人間環境学部 職種 教授 |
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言語種別 | 英語 |
発行・発表の年月 | 2011/06 |
形態種別 | 学術論文 |
査読 | 査読有り |
標題 | Mineral-enhanced hydrothermal oligopeptide formation at the second time scale |
執筆形態 | 共著 |
掲載誌名 | Astrobiology |
掲載区分 | 国外 |
出版社・発行元 | Corresponding author |
巻・号・頁 | 11(5),pp.461-469 |
著者・共著者 | ◎Kunio Kawamura, Hitoshi Takeya, Takao Kushibe, Yuka Koizumi |
概要 | Here, we show that enhancement of hydrothermal oligopeptide elongation by naturally occurring minerals was successfully verified for the first time by using a mineral-mediated hydrothermal flow reactor system (MMHF). MMHF consists of a narrow tubular reactor packed with mineral particles, and the enhancement or inhibitory activities of 10 types of naturally occurring minerals were successfully evaluated for an elongation reaction from (Ala)4 to (Ala)5 and higher oligopeptides in the absence of condensation reagents. It was unexpected that calcite and dolomite facilitated the elongation from (Ala)4 to (Ala)5 and higher oligopeptides with 28% yield at pH 7, while tourmaline, galena, apatite, mica, sphalerite, quartz, chalcopyrite, and pyrite did not show enhancement activities. These facts suggest the importance of carbonate minerals for the accumulation of peptide in primitive Earth environments. |