B43L-07
Grassland Degradation Alters Soil Carbon Turnover through Depth
Thursday, 17 December 2015: 15:10
2008 (Moscone West)
Courtney Creamer1, Suzanne M. Prober2, Adrian Chappell3, Mark Farrell1 and Jeff Baldock4, (1)CSIRO, Agriculture, Glen Osmond, SA, Australia, (2)CSIRO Land and Water Flagship, Wembley, WA, Australia, (3)CSIRO, Land and Water Flagship, Canberra, ACT, Australia, (4)CSIRO Land and Water, Glen Osmond, Australia
Abstract:
Ecosystem degradation is widespread and changes in aboveground plant communities alter belowground soil processes. In Australia, grassy eucalyptus woodlands dominated by kangaroo grasses (Themeda trianda) were widely cleared during European settlement for agriculture, with only fragments remaining of this now threatened ecosystem. As remnant grassland fragments are used for livestock grazing, Themeda transitions through states of degradation, starting with red grasses (Bothriochloa spp) and then proceeding to less productive, increasingly degraded states dominated by either annual exotic weeds or native wallaby grasses (Rytidosperma spp) and spear grasses (Austrastipa spp). The aim of our experiment was to determine how soil organic matter dynamics (including erosion, root biomass, C storage and turnover) have been altered by the transition from deeply-rooted Themeda grass systems to more shallowly-rooted annual exotic weeds and wallaby/spear grass states. We sampled soils in five depth-based increments (0-5, 5-15, 15-30, 30-60, 60-100 cm) across this ecosystem transition at five sites across New South Wales, Australia. Caseium-137 analysis indicated erosion rates were similar among all ecosystems and were consistent with levels for grasslands in the region. Compared to the remnant Themeda grass systems, the degraded states had lower root biomass, lower carbon stocks and C:N ratios in the coarse fraction (> 50 µm), lower fungal : bacterial ratios, higher available phosphate, higher alkyl : O-alkyl C ratios, and faster mineralization of synthetic root-exudate carbon. All these metrics indicate the surprising finding of more microbially processed OM and faster turnover of newly added C in the degraded sites. Compared to one another, the two degraded sites differed in both C and N turnover, with the exotic weeds having higher dissolved organic N, inorganic N, and coarse fraction N, higher fine fraction C stocks, and greater microbial biomass. These differences likely arise from the greater aboveground productivity of exotic weeds relative to the wallaby and spear grasses. Although microbial C turnover through depth is altered with grassland degradation in both states, the trajectory of the soil organic matter dynamics with degradation is also impacted by plant community dynamics.