%0 Figure %A Hohl, Simon V. %A Becker, Harry %A Jiang, Shao-Yong %A Ling, Hong-Fei %A Guo, Qingjun %A Struck, Ulrich %D 2017 %T Fig. A. Eu/Eu* vs. Ba/Sm. Geochemistry of Ediacaran cap dolostones across the Yangtze Platform, South China: implications for diagenetic modification and seawater chemistry in the aftermath of the Marinoan glaciation %U https://geolsoc.figshare.com/articles/figure/Fig_A_Eu_Eu_vs_Ba_Sm_Geochemistry_of_Ediacaran_cap_dolostones_across_the_Yangtze_Platform_South_China_implications_for_diagenetic_modification_and_seawater_chemistry_in_the_aftermath_of_the_Marinoan_glaciation/4970396 %R 10.6084/m9.figshare.4970396.v1 %2 https://geolsoc.figshare.com/ndownloader/files/8360138 %K ICP-MS analysis %K correction %K diagenetic modification %K Marinoan glaciation Fig %K basin cap dolostones %K Yangtze Platform %K South China %K BaO interferences %K Negative Eu anomalies %K Ba content %K Ediacaran cap dolostones %K Eu anomalies %K seawater chemistry %K Geology %X Fig. A. Eu/Eu* vs. Ba/Sm. Eu concentrations obtained by ICP-MS analysis are highly influenced by BaO interferences and therefore need to be corrected. Circles represent platform, x represents slope and diamonds represent basin cap dolostones. Resulting corrected Eu/Eu* ratios (black) have been plotted together with the uncorrected ratios (red). The size of the uncorrected symbols refers to Ba content of the sample. The correlation of Ba/Sm with uncorrected Eu/Eu* diminishes after correction. Remaining apparent positive Eu anomalies after correction may indicate insufficient correction. Negative Eu anomalies (Eu/Eu* < 1) in two corrected samples may be due to overcorrection. %I Geological Society of London