Vegetation cover dynamics on the northeastern Qinghai-Tibet Plateau since late Marine Isotope Stage 3

Knowledge of long-term changes in vegetation cover is essential for paleoenvironmental reconstruction and Earth system modeling. The vegetation on the northeastern Qinghai-Tibet Plateau (QTP) is highly sensitive to climatic changes, but studies of long-term changes in the vegetation cover of this region are lacking. To better understand the changes in the regional vegetation cover since late Marine Isotope Stage (MIS) 3, we obtained a pollen record from Luanhaizi Lake and used it to quantitatively reconstruct changes in the cover of trees and grasses using the random forest method. The pollen spectra show that the vegetation of the Luanhaizi Lake area was probably alpine tundra from late MIS3 to the Last Glacial Maximum, after which it changed to alpine steppe with alpine shrub and sparse forest at lower elevations during the last deglaciation. Alpine steppe and alpine meadow dominated the vegetation during the Holocene, with sparse forest in the surrounding low-elevation areas. The quantitative vegetation cover reconstruction suggests that the vegetation cover of the Luanhaizi Lake area was low (20-30%) during 47.0-20.0 ka. The tree cover then increased from-3% to-10%, and the grass cover increased from-20% to-45% during the last deglaciation (20.0-11.9 ka). The increasing Northern Hemisphere summer insolation caused increases in the regional temperature, meltwater supply, and monsoon precipitation, which promoted the development of steppe vegetation. The continued increases in insolation and monsoonal precipitation during the Holocene further increased the tree cover, which reached a maximum of 17.4% at-7.2 ka. Vegetation cover reconstructions from two other sites on the eastern QTP for the last deglaciation indicate contrasting patterns of changes, likely due to contrasts in elevation, climate, and environment.

Automated summary

This study reconstructs the long-term changes in vegetation cover on the northeastern Qinghai-Tibet Plateau using a pollen record from Luanhaizi Lake. The findings show that the vegetation in this region was alpine tundra during the late Marine Isotope Stage 3 and changed to alpine steppe, shrub, and sparse forest during the last deglaciation. The Holocene was dominated by alpine steppe and meadow, with sparse forest in lower elevations. The reconstructions also suggest that changes in insolation and monsoonal precipitation played a significant role in shaping the vegetation cover.