δ¹⁸Osw benthic-corrected on planktonic foraminifera of sediment core MD01-2378
收藏官方服务：
资源简介：
AGE follows the GICC05 time scale. To estimate changes of d18Osw of the sea surface and upper thermocline water, we used paired G. ruber and P. obliquiloculata Mg/Ca temperatures and stable isotopes and calculated the d18Osw using the equation of Bemis et al. (1998, doi:10.1029/98PA00070). The ice volume effect was corrected using the benthic d18Osw from the same core.
创建时间：
2009-01-01
