Evolution and variation of the Tsushima warm current during the late quaternary: Evidence from planktonic foraminifera, oxygen and carbon isotopes
Evolution and variation of the Tsushima warm current during the late quaternary: Evidence from planktonic foraminifera, oxygen and carbon isotopes
复制标题
DOI：
10.1007/s11430-007-0003-2
复制
发表时间：
2007-05
影响因子：
5.7
通讯作者：
L. Tiegang;Su Rongtao;Zhang De-yu;Liu Zhenxia;Li Qing;Jiang Bo
中科院分区：
文献类型：
--
作者：
L. Tiegang;Su Rongtao;Zhang De-yu;Liu Zhenxia;Li Qing;Jiang Bo
