岩层碳的重新动员可能会主导火山弧的排放
Emily Mason1, Marie Edmonds2, Alexandra V Turchyn1
1Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK.
概括
火山碳同位素数据显示,地球
科学领域:
- 地质化学
- 同位素地质化学
- 火山学
背景情况:
- 碳流影响地球的气候和可居住性.
- 火山气体是全球碳循环的重要组成部分.
研究的目的:
- 在全球范围内分析火山弧的碳和同位素.
- 确定火山气体的碳同位素组成.
- 调查火山碳的来源.
主要方法:
- 全球碳和同位素数据集的编制.
- 来自火山弧样本的同位素组成分析.
- 火山气体同位素值与中海基岩的比较.
主要成果:
- 平均全球火山气体的碳同位素组成比中海基岩 (-6.0 ‰) 重.
- 成熟的大陆弧与积累的碳酸盐平台是主要的火山碳排放,具有更高的 δ 13 C.
- 岩层石灰岩的再加工是火山碳的重要来源.
结论:
- 火山的碳来源比之前所认为的多样化.
- 有机碳的分量埋葬可能较低,并且随着地质时间的推移而变化.
- 超大陆的循环影响了火山对大气的碳贡献.
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