OXYGEN ISOTOPES AND SEA-LEVEL
OXYGEN ISOTOPES AND SEA-LEVEL
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DOI：
10.1038/324137a0
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发表时间：
1986-11-13
期刊：
影响因子：
64.8
通讯作者：
SHACKLETON, NJ
中科院分区：
文献类型：
--
作者：
CHAPPELL, J;SHACKLETON, NJ
从生活在深海恒温环境中的有孔虫获得的详细氧同位素记录开始，这些记录所暗示的冰量记录与世界各地年代久远的珊瑚梯地的高度记录之间就存在差异。在这里，我们重新检查了数据并得出结论，深海的温度一直是气候系统中一个积极变化的组成部分。
From the time that detailed oxygen isotope records derived from foraminifera living in the constant-temperature environment of the abyssal ocean became available, there has been a discrepancy between the ice volume record that these records imply, and that derived from the altitude of dated coral terraces around the world. Here, we re-examine the data and conclude that the temperature of the abyssal ocean has been an actively varying component of the climate system.