Spatiotemporal changes in C4 plant abundance in China since the Last Glacial Maximum and their driving factors.

Abstract Knowledge of changes in the distribution of C 3 and C 4 plants in relation to climate change is the key to predicting the biosphere's response to future climatic warming. There are significant differences in the spatiotemporal evolution of C 4 plant abundance at different latitudes since the Last Glacial Maximum (LGM), and the factors responsible remain debated. In this study, we reconstructed the spatiotemporal pattern of C 4 plants in China since the LGM, based on a synthesis of δ13C records of soil organic matter from paleosol sequences and δ13C records of individual n-alkanes from lake and marine sediments. The results indicate that, spatially, maximum C 4 abundance during the LGM was in South China; while maximum C 4 abundance occurred in the Chinese Loess Plateau in North China during the early and mid-Holocene. Temporally, in North China, C 4 plant abundance initially increased since the LGM, reached a maximum during the early and mid-Holocene and then decreased; however, the opposite trend occurred in South China. Combined with a physiological-process model used to study the sensitivity of C 3 and C 4 plants to changes in climate and atmospheric p CO 2 in different regions, our results reveal that temperature was the dominant factor driving C 4 plant expansion in North China, whereas atmospheric p CO 2 and precipitation were the main factors controlling C 4 plant abundance in South China. Highlights • Spatiotemporal pattern of C 4 plant abundance across China since the LGM was reconstructed. • Increase in C 4 abundance in mid-latitude China was triggered by increased temperature. • Decrease in C 4 abundance in low-latitude China was a response to increasing atmospheric p CO 2 and precipitation. [ABSTRACT FROM AUTHOR]