EGU26-17403, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-17403
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Thursday, 07 May, 09:55–10:05 (CEST)
 
Room 0.16
Small tree patches enhance soil carbon stabilization in pastoral landscapes
Kara Allen1, Ziva Louisson1, Sam McNally1, Kate Orwin1, Dan Richards1, Manpreet Dhami1,2, Scott Graham1, David Whitehead1, and Edward Brzostek3
Kara Allen et al.
  • 1Bioeconomy Science Institute, Lincoln, New Zealand
  • 2School of Biological Sciences, Waipapa Taumata Rau/University of Auckland, Auckland, New Zealand
  • 3Department of Biology, West Virginia University, Morgantown, West Virginia, USA

Small tree patches (<1 ha) embedded within pastoral landscapes can enhance soil carbon (C) storage, yet these gains remain poorly represented in soil C decomposition models that assume spatially uniform plant inputs and microbial processes. Sharp vegetation boundaries at tree-pasture edges generate strong gradients in rooting, litter quality, and microbial activity over short distances, with important implications for soil C stabilization that uniform models fail to capture. Using Aotearoa New Zealand as a model system, where pastoral landscapes are widespread and small tree patches are common features, we quantified plant inputs, microbial community composition and function, and soil processes across established tree-pasture boundaries to inform a microbially explicit soil C decomposition model. Tree-pasture edges exhibited elevated root biomass and lower leaf litter C:N ratios, indicating greater belowground C allocation and higher-quality organic inputs, while rhizosphere extracellular enzyme activity tended to be lower. Shotgun metagenomic analyses revealed a shift from microbial communities in forest soils characterized by greater investment in resource acquisition to microbial communities in grassland soils prioritizing faster growth and resource use, with edge communities displaying intermediate functional profiles. Together, these patterns suggest that tree-pasture edges function as biogeochemical ecotones, where increased root inputs and reduced enzyme investment are consistent with a shift toward microbial utilization of root-derived substrates rather than enzyme-mediated decomposition of more complex organic matter. To examine whether these rhizosphere-associated mechanisms could account for observed soil C gains beneath small tree patches, we refined a microbially explicit soil C decomposition model (FUN-CORPSE) to represent edge-driven root-microbe interactions. Simulations of small tree patch establishment in long-term pasture systems produced higher soil C stocks than pasture alone, with spatially explicit root inputs associated with increased soil C protection beneath tree-pasture edges. These findings highlight small tree patches as important landscape features with the potential to enhance soil C stabilization and contribute meaningfully to climate mitigation in pastoral systems.

How to cite: Allen, K., Louisson, Z., McNally, S., Orwin, K., Richards, D., Dhami, M., Graham, S., Whitehead, D., and Brzostek, E.: Small tree patches enhance soil carbon stabilization in pastoral landscapes, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-17403, https://doi.org/10.5194/egusphere-egu26-17403, 2026.