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Fig. 2 | Carbon Balance and Management

Fig. 2

From: Changes of lake organic carbon sinks from closed basins since the Last Glacial Maximum and quantitative evaluation of human impacts

Fig. 2

The lithology and 14C/OSL dating results from 12 terminal lakes in the closed basins of the Qilian Mountains. a Lithology of the 12 lake sections. b Comparison of the calibrated 14C (solid lines) and OSL ages (dashed lines) in the 5 closed basins of the Qilian Mountains. (Lithology data of Qinghai Lake are from Liu et al. [28], other lithology and 14C/OSL data sources see Additional file 1: Table S1)

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