地中海生物多样性的中新世纪晚期转变
Konstantina Agiadi1, Niklas Hohmann2,3, Elsa Gliozzi4
1Department of Geology, University of Vienna, Josef-Holaubek-Platz 2, Geozentrum, 1090 Vienna, Austria.
Science advances
|September 25, 2024
概括
地中海的海洋生态系统在米奥森晚期-普略森早期经历了显著的重组. 气候冷却和海洋连接的变化导致了各种海洋群体的物种大量流动.
科学领域:
- 古生物学的古生物学
- 海洋生物学 海洋生物学
- 气候科学 气候科学
背景情况:
- 深海生物多样性变化对于了解半封闭海洋的现代气候影响至关重要.
- 过去的气候和连接性转变显著影响了海洋生态系统.
研究的目的:
- 量化地中海的分类学多样性变化,从中新世纪晚期到新世纪早期 (11.633.6万年前).
- 评估全球气候变冷和改变大西洋连接对海洋生物的影响.
主要方法:
- 对石灰质的纳米浮游生物,恐龙囊,,,珊瑚,软体动物,,,鱼类和海洋哺乳动物进行分析.
- 在托尔顿,梅西尼和桑克莱阶段对分类学多样性和物种周转量进行量化.
主要成果:
- 在所有研究的群体中,物种周转率超过了30%,这表明了生态系统的重大重组.
- 即使在弥赛尼盐度危机 (7.255.97万年前) 之前,也观察到了显著的生态扰乱.
- 生物多样性模式在不同的海洋群体和地中海分盆地之间存在差异.
结论:
- 地中海生态系统由于气候和连接变化而经历了实质性的重组.
- 梅西尼海盐度危机和之前的环境变化对海洋生物多样性产生了深远的影响.
- 了解过去的变化对于预测海洋生态系统对气候变化的未来反应至关重要.
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