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Near-tropical early eocene terrestrial temperatures at the Australo-Antarctic margin, western Tasmania

机译:塔斯马尼亚西部Australo-Antarctic边缘的近热带初新世陆温

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摘要

A worldwide greenhouse warm climate prevailed in the Early Eocene, and nowhere was warming more dramatic than at high latitudes. Sea-surface temperatures of ~34 °C have been estimated for a site at paleolatitude 65°S on the East Tasman Plateau of the southwest Pacific Ocean, but these estimates require independent validation, including from terrestrial proxies. Here we determine a near-tropical terrestrial mean annual temperature estimate of ~24 °C at sea level for an Early Eocene site in Tasmania, Australia, using three proxies based on welldated estuarine plant fossils. This estimate is lower than the nearby sea estimates to the east, but similarly suggests that, as in the southwest Pacific, Early Eocene climates in the eastern Australo-Antarctic region were warmer than inferred elsewhere at high latitudes, including on the Antarctic Peninsula. Such data are essential for improving our understanding of climatic and biotic evolution in the Southern Hemisphere.
机译:始新世早期普遍存在全球性的温室温暖气候,没有哪个地方比高纬度地区的气候变暖更为剧烈。在西南太平洋东塔斯曼高原的古纬度65°S处,估计海表温度约为34°C,但这些估算值需要独立验证,包括来自陆地代理。在这里,我们使用基于井口植物化石的三个代理人,确定了澳大利亚塔斯马尼亚早期始新世海平面的热带近海年平均气温估计值〜24°C。该估计值低于东部的附近海域估计值,但同样表明,与西南太平洋地区一样,Australo-Antarctic东部地区的始新世气候要比其他高纬度地区(包括南极半岛)的推测要温暖。这些数据对于增进我们对南半球气候和生物演化的理解至关重要。

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