在黄岛半岛记录的海平面的快速波动是在最后一次降冰的前半部分
1T. M. Esat, M. T. McCulloch, J. Chappell, B. Pillans, Research School of Earth Sciences, Australian National University, Canberra, ACT 0200, Australia. A. Omura, Kanazawa University, Kanazawa, Ishikawa 920, Japan.
概括
最后的冰河间期经历了海平面的显著变化,由于较冷的洞穴珊瑚生长,海平面显著下降. 大约13万年前,海平面再次开始上升.
科学领域:
- 古气候学 古气候学
- 四年纪地质学四年纪地质学
背景情况:
- 最后的冰河间时期始于大约14万年前,大陆冰盖的破裂.
- 在此期间,海平面上升,在约135,000年前达到峰值,比现在水平低14米.
研究的目的:
- 通过使用华半岛 (巴布亚新几内亚) 的珊瑚记录,重建最后一个冰河间的海平面.
- 调查明显的海平面波动及其与古气候条件的相关性.
主要方法:
- 对珊瑚生长条件的分析和来自黄岛半岛的升起珊瑚露台 (珊瑚礁VII) 的约会.
- 使用魔鬼洞时间表进行时间相关联.
主要成果:
- 在礁石VII下方的一个洞穴中采集的珊瑚样本,可追溯到13万+/-2000年前,显示珊瑚在比现在低6°C的条件下生长.
- 这些发现表明,在这段时间内,海平面大幅下降60至80米.
- 海平面重建显示,在13万年前之后,海平面上升,这与阳光照射最大值有关.
结论:
- 最后的间冰期经历了复杂的海平面动态,包括意想不到的下降.
- 大约14万年前的早期降冰早于阳光峰值,与独立的时间表保持一致.
- 珊瑚礁记录为了解过去的海平面变化和气候变化提供了关键数据.
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