追踪碳从俯冲到排气沿着阿列乌提亚-阿拉斯加火山弧
Taryn Lopez1,2, Tobias P Fischer3, Terry Plank4
1Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USA.
Science advances
|June 28, 2023
概括
俯冲通过火山弧回收碳,但效率各不相同. 快速的沉降回收更多的有机碳,而缓慢的沉降回收更多的地碳,影响大气中的碳水平.
科学领域:
- 地质化学 地质化学
- 火山学 火山学是一门学科.
- 构造学 构造学 构造学 构造学
背景情况:
- 俯冲区对于地球的可居住性至关重要,它调节了地幔,地和大气之间的挥发性交换.
- 通过沉积来理解碳循环是理解长期气候调节的关键.
研究的目的:
- 通过同位素分析,追踪沿阿列乌提亚 - 阿拉斯加弧线从沉降产生的碳到其排气.
- 调查潜水特征的变化如何影响碳回收到大气中的效率.
主要方法:
- 沿着阿拉斯加-阿勒岛弧线的火山气体的同位素分析.
- 同位素组成与潜水参数 (例如速度,温度) 的相关性.
主要成果:
- 观察到火山气体同位素组成的显著沿冲击变化.
- 快速和冷的沉降 (中阿勒群岛) 可回收43-61%的沉积物衍生的有机碳.
- 缓慢和温暖的沉积 (西阿列乌提群岛) 将6-9%的改变的海洋地碳回收.
结论:
- 潜伏区的碳循环效率是高度可变的,并取决于构造学设置.
- 与此前估计的相比,返回深层地幔的碳量较少.
- 在地质时间尺度上,降解有机碳不是一个始终可靠的大气碳汇.
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