炭酸性物質の炭素同位体組成は,ウィットウォーターズランド系のプレカンブリア時代からのものです
まとめ
南アフリカのウィトワーターズランド系におけるポリメリ化炭化水素は,有機的起源を示唆している. 炭素同位体分析は,生物学的活動が215億年以上前に存在していたことを示しています.
科学分野:
- 地質化学 地質化学
- パレオバイオロジーの古生物学
- 同位体地質学とは,同位体地質学である.
背景:
- 南アフリカのウィトワターズランド系には,金とウランの合体が含まれています.
- これらの集積は,起源不明のポリメリ化炭化水素を宿している.
研究 の 目的:
- ウィトワーターズランド系で発見されたポリメリ化炭化水素の起源を調査する.
- これらの炭化水素が有機的または無機的由来であるかどうかを判断する.
主な方法:
- ポリマー化炭化水素における炭素同位体比 (デルタC(13) の分析.
- 堆積有機炭素の既知の範囲と同位体値の比較.
主要な成果:
- デルタC(13) の値は,1万人に22.4から32.8の範囲でした.
- これらの同位体組成は,堆積有機炭素の典型的な範囲に属する.
結論:
- 同位体データは,炭化水素の有機的起源を強く示唆しています.
- この発見は,21億5千万年前の初期の生物活動と有機進化のモデルを裏付けている.
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