Policymakers faced with the challenge of limiting greenhouse gas emissions need to know more than simply how much carbon dioxide (CO2) comes from, and is absorbed by, forests. To understand how forests will respond to climate change it is essential to know how much CO2 comes from different components of the forest, and emissions from the soil are poorly understood. For over six years, we measured CO2 emissions from longleaf pine forest soils which differed in their ability to hold water and represented different regions within the southeastern coastal plain. The information on CO2 from the soil was combined with data on CO2 taken up or released by the whole forest, measured from towers extending beyond the treetops.
Carbon dioxide emissions were higher under warm or dry climate conditions, and averaged over six years, there was no increase in the carbon stored in dry and intermediate forest soils.
In forests on moist soils, however, there was an increase of 8 tons per hectare of carbon. Approximately half of the CO2 that was released from the forest to the atmosphere came from soils, and this proportion changed little with year-to-year variation in climate. The results advance the science of predicting climate effects on soil CO2 emissions across the diverse and growing expanse of longleaf pine forests of the southeastern coastal plain.
Wiesner, S., C. L. Staudhammer, H. W. Loescher, A. Baron-Lopez, L. R. Boring, R. J. Mitchell, and G. Starr. 2018. Interactions among abiotic drivers, disturbance and gross ecosystem carbon exchange on soil respiration from subtropical pine savannas. Ecosystems, 20 pp. https://doi.org/10.1007/s10021-018-0246-0.