Temporal variability in 13C of respired CO2 in a pine and a hardwood forest subject to similar climatic conditions

Temporal variability in the ¹³C of foliage (¹³C_F), soil (¹³C_S) and ecosystem (¹³C_R) respired CO₂ was contrasted between a 17.2-m tall evenly aged loblolly pine forest and a 35-m tall unevenly aged mature second growth mixed broadleaf deciduous forest in North Carolina, USA, over a 2-year period. The two forests are located at the Duke Forest within a kilometer of each other and are subject to identical climate and have similar soil types. The ¹³C_F, collected just prior to dawn, was primarily controlled by the time-lagged vapor pressure deficit (VPD) in both stands; it was used for calculating the ratio of intercellular to ambient CO₂ (Ci/Ca). A remarkable similarity was observed in the relationship between Ci/Ca and time-lagged VPD in these two forests despite large differences in hydraulic characteristics. This similarity emerged as a result of physiological adjustments that compensated for differences in plant hydraulic characteristics, as predicted by a recently proposed equilibrium hypothesis, and has implications to ecophysiological models. We found that in the broadleaf forest, the ¹³C of forest floor CO₂ efflux dominated the ¹³C_R, while in the younger pine forest, the ¹³C of foliage respired CO₂ dominated ¹³C_R. This dependence resulted in a more variable ¹³C_R in the pine forest when compared to the broadleaf forest due to the larger photosynthetic contribution. Given the sensitivity of the atmospheric inversion models to ¹³C_R, the results demonstrate that these models could be improved by accounting for stand characteristics, in addition to previously recognized effects of moisture availability, when estimating ¹³C_R.