Late Pliocene–Pleistocene expansion of C4 vegetation in semiarid East Asia linked to increased burning

Abstract

Plants using the C 4 photosynthetic pathway, commonly tropical and subtropical grasses, increased in abundance in East Asia dur- ing the late Cenozoic. Determining the exact timing and likely fac- tors leading to this major vegetation change requires region-specific studies. Here variations in pyrogenic carbon mass accumulation rate (PyC-MAR) and isotope composition (δ 13 C PyC ) from an ~7-m.y.- long depositional sequence from the central Loess Plateau, China, suggest increased biomass burning and an increased contribution to combusted material from C 4 taxa from 2.6 Ma. Changes in the composition of PyC after 0.6 Ma likely reflect the effects of lower temperatures, particularly during glacial periods, and changes in seasonality of precipitation. Increased PyC-MAR without concomi- tant changes in δ 13 C PyC at ca. 0.15 Ma appears to indicate a decou- pling of feedbacks between changes in climate, fire regime, and veg- etation, and may mark the onset of anthropogenic burning in the region. These new data suggest that C 4 taxa were present on the Loess Plateau from at least the late Miocene, rising to prominence at ca. 2.6 Ma following changes in climate and, critically, an increase in biomass fires.