Aim

Millennial-scale biogeographic changes are well understood in many parts of the world, but little is known about long-term vegetation dynamics in subtropical regions. Here we investigate shifts in C₃/C₄ plant abundance occurred in central Argentina during the past few millennia

Methods

We determined present day soil organic matter δ¹³C signatures of grasslands, shrublands and woodlands, containing different mixtures of C₃ and C₄ plants. We measured past changes in the relative cover of C₃/C₄ plants by comparing δ¹³C values in soil profiles with present day δ¹³C signatures. We analyzed ¹⁴C activity in soil depths that showed major changes in vegetation.

Results

Present day relative cover of C₃/C₄ plants determines whole ecosystem δ¹³C signatures integrated as litter and superficial soil organic matter (R² = 0.78; p < 0.01). Deeper soils show a consistent shift in δ¹³C, indicating a continuous replacement of C₄ by C₃ plants since 3,870 (±210) YBP. During this period, the relative abundance of C₃ plants increased 32% (average across sites) with significant changes being observed in all studied ecosystems.

Conclusions

Our results show that C₄ species were more abundant in the past, but C₃ species became dominant during the late Holocene. We identified increases in the relative C₃/C₄ cover in grasslands, shrublands and woodlands, suggesting a physiological basis for changes in vegetation. The replacement of C₄ by C₃ plants coincided with changes in climate towards colder and wetter conditions and could represent a climatically driven shift in the C₄ species optimum range.