梅西尼海盐度危机受到竞争性构造学和直布罗陀弧线侵蚀的调节
D Garcia-Castellanos1, A Villaseñor
1Instituto de Ciencias de la Tierra Jaume Almera, CSIC, Solé i Sabarís s/n, 08028 Barcelona, Spain. danielgc@ictja.csic.es
Nature
|December 16, 2011
概括
梅西尼亚盐度危机是由大西洋流入地中海量减少所驱动的. 数字模型显示,海路侵蚀抵消了构造上升,维持了浅层连接,并解释了盐分沉.
科学领域:
- 地球科学 地球科学 地球科学
- 海洋学 海洋学 海洋学
- 地质地质地质地质地质地
背景情况:
- 梅西尼亚盐度危机 (5.96-5.33万年前) 导致地中海从大西洋流入减少,导致大量的盐分降水和海平面下降.
- 以前的解释集中在构造上升和全球海平面变化上,但很难将时间尺度与广泛的盐沉积所需的长时间的浅层连接相协调.
研究的目的:
- 调查海路侵蚀在弥赛尼海盐危机期间维持大西洋和地中海之间浅层连接中的作用.
- 为了使构造上升和海平面变化的时间表与地中海-大西洋连接的持续时间相协调.
主要方法:
- 数字建模以模拟不同构造和侵蚀条件下的海路动态.
- 用地质证据和地力学模型比较模型衍生的侵蚀和提升速度.
主要成果:
- 海路侵蚀,由大西洋的涌入驱动,可以抵消构造上升,维持浅层连接.
- 所需的侵蚀和提升速度与直布罗陀弧和地力学模型的地质数据保持一致.
- 适度升起和侵蚀之间的平衡解释了地中海早期海平面下降和周期性盐降水.
结论:
- 海路侵蚀是在弥赛尼海盐危机期间维持浅层大西洋-地中海连接的关键机制.
- 提升和侵蚀之间的相互作用为早期盐沉积的周期性提供了新的解释.
- 这挑战了以前关于梅西尼海盐度危机的时间和机制的假设.
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