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 M (領域外・複数領域) » M-IS ジョイント

[M-IS26] 生物地球化学

2015年5月28日(木) 11:00 〜 12:45 104 (1F)

コンビーナ:*楊 宗興(東京農工大学)、柴田 英昭(北海道大学北方生物圏フィールド科学センター)、大河内 直彦(海洋研究開発機構)、山下 洋平(北海道大学 大学院地球環境科学研究院)、座長:高野 淑識(海洋研究開発機構)、長尾 誠也(金沢大学環日本海域環境研究センター)、渡邉 泉(東京農工大学大学院農学研究院)、横尾 頼子(同志社大学理工学部)

11:15 〜 11:30

[MIS26-09] 西部北太平洋における天然海洋細菌群集および懸濁態有機物のアミノ酸組成

*高巣 裕之1宮島 利宏1永田 俊1 (1.東京大学大気海洋研究所)

キーワード:海洋細菌, アミノ酸, プロリン, 鏡像異性体, 懸濁態有機物

Amino acid compositions were determined for natural marine bacterial assemblages (bacterium-size particles separated from other organisms and particles) and suspended particulate organic matter (POM) collected at subarctic and subtropical stations in the western North Pacific. We found that L-proline (L-Pro) content was remarkably high [38 - 57% of total hydrolysable amino acids (THAA)] in natural marine bacterial assemblages. These values were much higher than the corresponding values reported in the literature or those determined by ourselves for isolated bacterial strains (typical range, 4.3 - 8.8%). In POM, L-Pro content was low (<5% of THAA) in the upper layer (0 - 200 m), whereas it was high (24 - 26% of THAA) at the depth of 1000 m. Determination of enantiomeric amino acids in POM revealed that the ratio of D-/L- amino acids at the depth of 1000 m (0.054 - 0.061) was higher than that in the upper layer (0.012 - 0.039). These results confirm and add to the previous proposition that amino acid composition is systematically altered during bacterial reworking of marine organic matter, indicating that, in addition to the conventional indicator using enantiomeric amino acid ratio, L-Pro content can be a new indicator of the enrichment of POM by the organic matter derived from bacteria. Our results also underscore the importance of identifying bacterial constituents rich in L-Pro, which might play an important role in biochemical processes mediated by uncultured natural marine bacteria.