地殻の炭素の再動員が火山弧の排出を支配する可能性がある
Emily Mason1, Marie Edmonds2, Alexandra V Turchyn1
1Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK.
まとめ
火山の炭素同位体データによると 地球は
科学分野:
- 地化学
- 同位体地化学
- 火山学
背景:
- 炭素の流れは地球の気候と居住可能性に影響を与えます
- 火山ガスは世界の炭素循環の 重要な構成要素です
研究 の 目的:
- 地球上の火山のイソトープを分析する
- 火山ガスの炭素同位体成分を決定する.
- 火山の炭素の源を調査する
主な方法:
- 炭素とヘリウムの同位体に関するグローバルデータセットの作成.
- 火山弧のサンプルからの同位体組成の分析.
- 火山ガスの同位体値と海中の玄武岩の比較
主要な成果:
- 平均的な地球規模の火山ガスの炭素同位体組成は,海中の玄武岩 (-6.0‰) よりも重い.
- 成長した炭酸基板を持つ成熟した大陸の弧は,より高いδ13Cの主要な火山の炭素放出源である.
- 地殻の石灰岩の再処理は火山炭の重要な源である.
結論:
- 火山による炭素の発生源は これまで考えられていたよりも多様です
- 有機炭素の分量埋葬は低い可能性があり,地質学的な時間とともに変化しています.
- 超大陸の循環は,大気への火山による炭素の供給に影響を与えます.
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