《Table 3 Rare earth element (REE) concentrations (ppb) of Wudaoliang stromatolites and reference sam

《Table 3 Rare earth element (REE) concentrations (ppb) of Wudaoliang stromatolites and reference sam   提示：宽带有限、当前游客访问压缩模式
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《"Palaeoenvironmental setting of lacustrine stromatolites in the Miocene Wudaoliang Group, northern Tibetan Plateau"》


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Wudaoliang stromatolites showδ13C values ranging from2.43‰to 4.12‰，about 1.20‰higher than skeletal limestones（Yi et al.2008）and marlstones（Wu et al.2009）of the same formation.Highδ13C values might point to a significant photosynthetic effect in the water body.In photosynthetic process12C is preferentially assimilated by primary producers，resulting13CDICenrichment in lake water and highδ13C in the carbonates（Kerby and Raven1985；Hollander and Mc Kenzie 1991；Gu et al.1996）.Therefore，despite high salinity，a significant primary carbon production is evident for this depositional period of the lake in the Hoh Xil Basin.

图表编号XD0061548200    严禁用于非法目的
绘制时间2019.07.01
作者Ling-Qi Zeng、Hai-Sheng Yi、Guo-Qing Xia、Klaus Simon、Christine Heim、Gernot Arp
绘制单位Institute of Sedimentary Geology, Chengdu University of Technology、Institute of Sedimentary Geology, Chengdu University of Technology、State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation、Institute of Sedimentary Geology, Chengdu Universi
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