初期の生命の証拠 地球の最も古い水熱噴出孔の沈殿物
Matthew S Dodd1,2, Dominic Papineau1,2, Tor Grenne3
1London Centre for Nanotechnology, 17-19 Gordon Street, London WC1H 0AH, UK.
Nature
|March 3, 2017
まとめ
ケベック で 発見 さ れ た 古代 の 微生物 の 証拠 は,おそらく 428 億 年 前の もの です
科学分野:
- 地質学
- 古生物学
- 天体生物学
背景:
- 海底の熱水噴出孔は 地球上の生命の早期生息地と考えられています
- カナダ の クエベック 州 の ヌヴワギットゥク 帯 に は,古代 の 鉄質 の 堆積 岩 が 含ま れ て い ます.
研究 の 目的:
- ヌブワギトク帯の 古代岩石の化石化微生物を調査する
- 岩の微小構造の 年代と起源を特定するためです
主な方法:
- 微生物化石の証拠のための鉄質の堆積岩の分析.
- 現代の熱水噴出孔の微生物との形態学的および鉱物学的比較.
- 岩石サンプル内の炭素の同位体分析
主要な成果:
- 微米規模のヘマタイト管とフィラメントが発見され,その年代は377億年から428億年です.
- これらの構造は,現代の熱水噴出孔の微生物に似た形態と鉱物組成を示しています.
- 同位体的に軽い炭素が 推定微生物化石と関連して 生物学的活性を示す
結論:
- この発見は37億7千万年前の 海底熱水環境で 生物学的活動があった証拠です
- 発見された微小構造は 古代の微生物の 酸化バイオマスと一致しています
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