大气中PCO2扰动与大西洋中部岩地区相关
Morgan F Schaller1, James D Wright, Dennis V Kent
1Department of Earth and Planetary Sciences, Rutgers University, Piscataway, NJ 08854, USA. schaller@rci.rutgers.edu
概括
大型火山区对大气中的二氧化碳 (PCO2) 有显著影响. 这项研究揭示了CAMP火山活动导致PCO2峰值,随后由于酸盐气候变化而下降.
科学领域:
- 地质科学是地球科学.
- 古气候学 古气候学
- 火山学 火山学是一门学科.
背景情况:
- 大型火山区对大气中的二氧化碳 (PCO2) 的影响在很大程度上仍未得到量化.
- 了解这些影响对于重建过去的气候动态至关重要.
研究的目的:
- 为了估计过去大气中PCO2水平在中大西洋岩地区 (CAMP) 事件期间.
- 研究CAMP火山活动与大气二氧化碳度之间的关系.
主要方法:
- 在纽瓦克盆地与CAMP火山交织在一起的pedogenic碳酸盐的稳定同位素分析.
- 使用已确定的地化学代理来重建PCO2度.
主要成果:
- 营前的PCO2水平约为每百万分之2000个 (ppm).
- 在火山活动之后,PCO2增加到4400 ppm,然后在30万年内下降.
- 这种模式在随后的CAMP流量单位中重复.
结论:
- 坎普火山活动直接导致大气PCO2的显著,尽管是暂时的增加.
- 由新鲜的火山物质增强的酸盐气候变化是二氧化碳吸收的关键机制.
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