在超深海沉积物中的地震增强的溶解碳循环
Mengfan Chu1, Rui Bao2, Michael Strasser3
1Frontiers Science Center for Deep Ocean Multispheres and Earth System, and Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, 266100, China.
Nature communications
|September 11, 2023
概括
地震触发的流石在海拔沟中增强了碳循环. 这些事件推动微生物甲基生成和深沉积物中的碳积累,可能加速碳出口到俯冲区.
科学领域:
- 海洋地质 海洋地质学
- 地质化学 地质化学
- 微生物学 微生物学
背景情况:
- 哈达尔沟是潜水带的独特的地质和生态系统.
- 地震触发的流岩是有机碳 (OC) 运输的关键途径.
- 在战中的OC重矿化和转化仍然不太了解.
研究的目的:
- 研究日本沟地下沉积物中溶解有机碳 (DOC) 和溶解无机碳 (DIC) 的动态.
- 了解地震触发的流石在碳循环中的作用.
- 评估微生物甲基生成和碳出口在 hadal沟系统.
主要方法:
- 对DOC和DIC度的分析.
- 溶解碳的稳定和放射性碳同位素特征.
- 从日本沟地下沉积物中取取间歇性水的样本 (IODP探险队386).
主要成果:
- 在地下沉积物中观察到的DOC和DIC的积累和老化.
- 有证据表明,与矿相关的可变溶解碳产量增加.
- 密集的微生物甲基生成由沟沉积物中的不稳定碳支持.
结论:
- 像地震这样的构造事件显著增强了沟系统中的碳积累和转化.
- 剩余的溶解碳为海底沟中的深层生物圈提供燃料.
- 由于这些过程,可能会出现加速的碳出口到俯冲区.
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