碳同位素证据表明,甲水合物在四级间阶段期间不稳定
1Geological Sciences and Marine Science Institute, University of California, Santa Barbara, CA 93106, USA. Department of Geological Sciences, California State University, Long Beach, CA 90840, USA.
海洋沉积物中的甲水合物解离导致了6万年来碳同位素的巨大转移. 这些与气候变化相关的事件释放了甲,影响了大气组成.
科学领域:
- 古海洋学是古海洋学.
- 海洋地质化学海洋地质化学
- 气候科学气候科学
背景情况:
- 在圣塔巴巴拉盆地的盆地地藻中观察到的千年级碳同位素振荡.
- 这些振荡表明,在过去的6万年里,沉积物甲梯度和气酸盐解离发生了变化.
研究的目的:
- 为了调查圣巴巴拉盆地千年级碳同位素振荡的原因.
- 了解气体水合物解离在这些振荡中的作用及其对大气甲的潜在影响.
主要方法:
- 在过去的6万年里,对盆地和浮游生物的碳同位素进行了分析.
- 同位素数据与古海洋学代理和气候记录的相关性.
主要成果:
- 大规模的千年级碳同位素振荡 (约. 5每毫克) 反映了在间阶段期间气体水合物解离过程中的甲排气.
- 短暂的负偏差 (高达每毫升 -6) 表明盆地沉积物大量释放甲.
- 气体水合物稳定性受到与热环循环转移相关的中间水温变化的影响.
结论:
- 甲水合物解离和随后的甲释放对千年规模的碳循环产生了重大影响.
- 这些过程可能导致了加利福尼亚边缘和全球范围内大气中广泛的甲振荡.
- 热环循环在调节气酸盐稳定性方面发挥了关键作用.
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