Fig. 4: Reconstructed lake water CO2 concentrations and pH values over the past 26 kyr based on δ13C data from Tibetan Plateau lakes (4 newly sampled lakes and 9 previously reported lakes). | Communications Earth & Environment

Fig. 4: Reconstructed lake water CO2 concentrations and pH values over the past 26 kyr based on δ13C data from Tibetan Plateau lakes (4 newly sampled lakes and 9 previously reported lakes).

From: Tibetan lakes have been persistent CO2 sources since the Last Glacial Maximum

Fig. 4: Reconstructed lake water CO2 concentrations and pH values over the past 26 kyr based on δ13C data from Tibetan Plateau lakes (4 newly sampled lakes and 9 previously reported lakes).The alternative text for this image may have been generated using AI.

Solid black lines represent mean CO2 concentrations and pH values calculated at 300-year intervals and grey shadings indicate standard deviation. a Reconstructed CO2 concentrations in lake water. The red line indicates atmospheric equilibrium CO2 concentrations (derived from ice core data8). Values above this line represent lakes acting as CO2 sources to the atmosphere, while values below indicate CO2 sinks. b Calculated CO2 concentration changes relative to modern lake water. For lakes with data extending to ~4 ka, we used the youngest data point as the modern reference. For lakes without data after 4 ka (Lake Qinghai, Zhari Namco, Pumoyum Co, and Heihai), we used contemporary measured CO2 concentrations as the baseline. c Reconstructed pH values of lake water.

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