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碳酸盐的埋葬模式,中新纪的气候和纳米浮游生物的扩张
Tristan Salles1, Laurent Husson2, Thran Trung Nguyen1,3
1School of Geosciences, University of Sydney, Camperdown, NSW 2006, Australia.
概括
浅水碳酸盐平台通过调节碳循环恢复,对地球气候产生重大影响. 它们的生产力,在可居住性和性极限之间交替,在地质时间尺度上调节气候.
科学领域:
- 地球科学 地球科学 地球科学
- 古气候学 古气候学
- 海洋学 海洋学 海洋学
背景情况:
- 地球的长期气候是由大气中的二氧化碳调节的,而酸盐气候作为一个关键的反.
- 碳酸盐埋葬区分于海底和海底地区影响了碳循环回收率.
- 在海洋化学和纳米浮游生物生产力中,神经碳酸盐积累的作用还未得到充分研究.
研究的目的:
- 研究碳酸盐积累对海洋和性流量的影响.
- 评估神经碳酸盐平台对纳米浮游生物生产率和碳库的影响.
- 了解浅水碳酸盐系统如何调节地球的气候系统和海底生态系统.
主要方法:
- 板块构造重建与气候和生理学模拟相结合.
- 采用宏观生态模型来估计中高新生态时期的温水碳酸盐息地和生产力.
- 分析的重点是地化学流入和碳酸盐积累潜力之间的平衡.
主要成果:
- 地化学流入仅在白纪早期和古纪期间超过了碳酸盐积累潜力.
- 对于大部分中代代,地化学流入不足以满足碳酸盐积累潜力.
- 确定了两种不同的制度:居住性有限的时期和性有限的时期.
结论:
- 尼里特基平台作为碳循环的关键调节器,影响恢复时间表 (10^3到10^5年).
- 这些系统调节纳米浮游生物的发展和生产力,从而影响生物.
- 浅水碳酸盐系统在调节地球气候和海底生态系统方面发挥着重要作用.
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