黒海の微生物のサンゴ礁は,メタンの無酸素酸化によって作動しています
Walter Michaelis1, Richard Seifert, Katja Nauhaus
1Institute of Biogeochemistry and Marine Chemistry, University of Hamburg, Bundesstrasse 55, 20146 Hamburg, Germany. michaelis@geowiss.uni-hamburg.de
まとめ
ブラック海のメタンの浸出地にある微生物マットは,メタンの炭素をバイオマスと炭酸塩に組み込む. これらのアーカイアとバクテリアのコンソーシアムは,炭酸の降水とバイオマスの蓄積を駆動し,地球に影響を及ぼします.
科学分野:
- ゲオミクロバイオロジー
- バイオジオケミカルサイクル
- マリンサイエンス マリンサイエンス・サイエンス
背景:
- 巨大な微生物マットは,無酸素の黒海シェルフ水域のメタン浸出で繁栄します.
- これらのマットは,広範囲にわたる炭酸塩の蓄積を形成し,高さ4メートルに達します.
- 以前の研究では,炭酸塩の形成における微生物活動の役割が強調されています.
研究 の 目的:
- 炭酸塩の降水と黒海メタン漏れで生体質の蓄積を促す微生物のプロセスを調査する.
- 微生物マットと関連する炭酸塩に組み込まれた炭素の源を決定する.
- これらのプロセスが古代の炭素循環に及ぼす影響を理解する.
主な方法:
- 古代生物 (ANME-1) と硫酸塩を減少させる細菌 (Desulfosarcina/Desulfococcus) を中心に微生物マットの組成を分析した.
- 炭素の組み込みを追跡するための安定同位体分析 (13C減少)
- メタン (AOM) の無酸素酸化と硫酸縮小を観察するためのインビトロインキュベーション実験.
主要な成果:
- 13Cの大幅な減少は,炭酸塩,バイオマス,脂質にメタン炭素の組み込みを確認しています.
- 微生物マットは,ANME-1アーカイアとDesulfosarcina/Desulfococcusバクテリアによって支配されています.
- 実験室内インキュベーションでは,これらの微生物コンソーシアムが硫酸還元と結合したメタンの無酸素酸化を実行することを実証しました.
結論:
- メタン浸出における無酸素微生物のコンソーシアムは,炭酸塩の降水と重要なバイオマス生産の両方を誘発することができる.
- これらの発見は,無酸素環境における炭素循環機構の洞察を提供します.
- この研究は,地球の地質学的な過去における同様のプロセスを理解するための意味を持つ.
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