概括
纳米比亚海域的格拉上游系统可能始于米奥森末期早期,大约1000万年前. 这种启动带来了寒冷的,富含营养的水,建立了现代系统.
科学领域:
- 海洋地质学 海洋地质学
- 古海洋学是古海洋学.
- 古气候学 古气候学
背景情况:
- 班格拉上游系统是大西洋海洋生态系统的关键组成部分.
- 了解它的开始,可以了解过去的海洋学条件和气候动态.
研究的目的:
- 为了确定班格拉上游系统在纳米比亚北部启动的时间.
- 重建与该系统的建立相关的古海洋学条件.
主要方法:
- 从现场362/362A.深海钻探项目核心的分析.
- 检查沉积物的积累速度.
- 对藻的丰度和微化石温度偏好的研究 (浮游生物菌体,石灰质的纳米浮游生物,鞭状体).
- 通过有机碳含量和在石灰岩骨中的融入来评估生产率.
主要成果:
- 沉积物学和古生物学的数据表明,主要的,持续的上游在早期的中新世纪晚期开始.
- 现代的Benguela上游系统可以追溯到大约在现在之前的1000万年.
- 有证据表明,寒冷的,富含营养的水在表面的到来.
结论:
- 早期的中新世纪晚期标志着现代格拉上游系统的启动.
- 这一事件显著改变了纳米比亚北部的海洋环境.
- 这些发现有助于了解主要海洋系统的长期演变.
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