《Table 2 Stable carbon and oxygen isotope results of Wudaoliang stromatolites (Continued)》

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《"Palaeoenvironmental setting of lacustrine stromatolites in the Miocene Wudaoliang Group, northern Tibetan Plateau"》

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Except for WDL-13-D-1，the stromatolite samples showed positive Eu anomalies（Eu/Eu*SN）from 1.006 to 1.260（Table 4）.And，14 of the 17 laminae in sample WDL-13-A showed positive Eu anomalies with a highest value of 1.608（Table 6）.In samples WDL-10-C-1，WDL-10-C-2 and WDL-13-A，La/LuSNratios ranged from 0.568 to 0.794；and，La/LuSNratios ranged from 0.944 to 0.955 in samples WDL-13-D-1 and WDL-13-D-2（Table 4）.Sample WDL-13-D-1 had a positive Ce anomaly of 1.300（Table 4）.However，2 laminae in sample WDL-13-A showed negative Ce anomalies（0.360 and 0.627；Table 6）.