空中火山活动打破了原生代中期的环境静止
Shuichang Zhang1, Huajian Wang1, Xiaomei Wang1
1Key Laboratory of Petroleum Geochemistry, Research Institute of Petroleum Exploration and Development, China National Petroleum Corporation, Beijing 100083, China.
Science advances
|March 29, 2024
概括
大约14亿年前的火山活动促进了营养物质的流失,增加了海洋初级生产力 (MPP) 和有机碳埋葬. 这表明前生代中期的地球并不像以前认为的那样停滞不前.
科学领域:
- 地质科学是地球科学.
- 古气候学 古气候学
- 生物地质化学生物地质化学
背景情况:
- 长生代中期 (1.80.8亿年前) 的特点是海洋无氧,低海洋初级生产力 (MPP),和有限的真核生物多样性.
- 这一时期一直被视为环境停滞不前,但最近的发现表明间歇性干扰和进化事件.
研究的目的:
- 为了调查火山活动对陆地气候和MPP在中期Proterozoic期间的影响.
- 通过检查环境动态来挑战静态地球的概念.
主要方法:
- 分析了14亿年前的热带海上沉积物.
- 精确的 (Hg) 和 (Li) 同位素分析.
主要成果:
- 当地的火山活动引入了新鲜的岩石基板,增强了热带低地地区的化学气候变化和脱皮.
- 增加的营养物质流入,特别是来自火山衍生物的,刺激了MPP率.
- 观察到有机碳埋葬的增加,与增加的MPP有关.
结论:
- 火山活动在中原生代中期起到了重要的环境干扰作用.
- 这些由火山活动驱动的干扰,可能有助于增加MPP和有机碳埋葬,可能打破了这个时代的长期静态状态.
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