Research Article

Can Carbon Sequestration in Tasmanian “Wet” Eucalypt Forests Be Used to Mitigate Climate Change? Forest Succession, the Buffering Effects of Soils, and Landscape Processes Must Be Taken into Account

Figure 6

Site 5 Ferralsols: NMR spectra of fPOM, oPOM, and clay fractions from the B1 horizons (uppermost mineral soil horizons) under rainforest (a) and mixed forest (b). The prominent aryl-C peak in the fPOM fraction under mixed forest is arrowed.