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We tested whether the abundance of C 4  vegetation in grasslands of the Mongolian plateau is influenced by grazing conditions. The analysis exploited the politically originated contrast that exists between Mongolia (low stocking rate, transhumant system) and the district of Inner Mongolia, China (high stocking rate, sedentary system). We estimated the proportion of C 4  carbon (P C4 ) in grazed vegetation from the relative carbon isotope ratio (δ 13 C) of sheep wool sampled from 298 annual shearings originating from 1996 to 2007. Annual stocking rates varying over time and between the districts of both countries were taken from regional statistics. The P C4  pattern within the 0.7 million km 2  sampling area was geostatistically analyzed and related to stocking rates and temperature gradients. For similar climatic conditions, P C4  was the same in both countries. Further, a unique relationship was found between P C4  and July temperature on both sides of the border, which explained 71% of the pattern. Stocking rate and grazing system had no significant influences on present-day C 3 /C 4  abundance ratio. This finding suggests that recent changes in the C 3 /C 4  ratio of these grasslands are mainly a consequence of regional warming, not overgrazing.

Sheep Wool δ13C Reveals No Effect of Grazing on the C3/C4 Ratio of Vegetation in the Inner Mongolia–Mongolia Border Region Grasslands