New approach to surface seawater palaeotemperatures using 18O/16O ratios in silica of diatom frustules
New approach to surface seawater palaeotemperatures using 18O/16O ratios in silica of diatom frustules
复制标题
利用硅藻壳二氧化硅中的 18O/16O 比例测量表层海水古温度的新方法
作者：
L. Labeyrie
水中生物沉积的碳酸钙和二氧化硅的氧同位素组成取决于水的温度和同位素组成。
THE oxygen isotopic composition of calcium carbonate and silica deposited by organisms in water depends on the temperature and the isotopic composition of the water1.