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一个巨大的西南极冰层解释了早期的新纪海平面幅度
J W Marschalek1, L Zurli2, F Talarico2
1Department of Earth Science and Engineering, Imperial College London, London, UK. j.marschalek18@imperial.ac.uk.
早期米奥森时期的地质证据显示,一个巨大的西南极冰层 (WAIS) 横跨罗斯海大陆架. 这一发现与过去的海平面数据和冰盖模型相协调, 表明南极冰的演变处于一个关键的转折点.
科学领域:
- 古气候学
- 冰川学
- 海洋地质学
背景情况:
- 早期至中期米奥森时期的海平面波动 (~40-60米) 仍在争论中,一些研究表明,在温暖时期,东南极的冰几乎完全消失.
- 然而,冰盖模型表明,即使在更温暖的中米欧时代间隔中,东南极冰仍然存在.
- 这些对比的解释需要考虑来自其他南极地区的大量冰.
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