Geological Society of America Bulletin
Geological Society of America Bulletin
复制标题
DOI：
--
复制
发表时间：
2010
期刊：
影响因子：
--
通讯作者：
Samuel Epstein;Ralph Buchsbaum;Heinz Lowenstam
中科院分区：
文献类型：
--
作者：
Samuel Epstein;Ralph Buchsbaum;Heinz Lowenstam
测定了海洋贝壳碳酸钙中氧的相对丰度与温度的关系。如果已知壳生长所在的水的相对氧丰度，则可以确定温度，精确度为±1.0°C。海洋沃茨的相对O含量随盐度增加而增加，在海洋表面沃茨的情况下，随盐度和温度增加而增加。
A relationship between temperature and relative O abundance in calcium carbonate in marine shells has been determined. If the relative O abundance of the water in which the shell grew is known, the temperature can be determined to an accuracy of ±1.0°C. The relative O contents of marine waters increase with salinity and, in the case of surface marine waters, with salinity and temperature.