Micropaleontological and isotopic determinations of Pleistocene climates
Micropaleontological and isotopic determinations of Pleistocene climates
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DOI：
10.2307/1484180
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发表时间：
1956-07
影响因子：
1.5
通讯作者：
D. B. Ericson;G. Wollin
中科院分区：
文献类型：
--
作者：
D. B. Ericson;G. Wollin
将由三个深海岩心浮游有孔虫变化得到的气候曲线与Emily iani根据相同岩心绘制的同位素温度曲线进行了比较。剖面上部相关性较强，但向下偏差增大。更新世气候的微古生物和同位素测定纽约哥伦比亚大学帕利塞兹哥伦比亚大学拉蒙特地质观测站
Climatic curves derived from variations in planktonic foraminifera in three deep-sea cores are compared with isotopic temperature curves drawn by Emiliani on the basis of the same cores. There is close correlation in the upper part of the section, but increasing deviation downward. Micropaleontological and isotopic determinations of Pleistocene climates DAVID B. ERICSON AND GOESTA WOLLIN Lamont Geological Observatory Columbia University Palisades, New York