Microbial traits, necromass accumulation, and soil carbon persistence are shaped by oil palm-based agroforestry in the Amazon

Alberto Vinicius S. Rochaa, b, Kate M. Buckeridgeb, Alice Ferreira Alvesa, Felipe Martins do Rêgo Barrosa, c, Acácio Tarciso Moreira de Melod, Rodrigo Floriano Pimpinatoe, Valdemar Luiz Tornisieloe, Carlos Eduardo Pellegrino Cerria, f, Maurício Roberto Cherubina, f, Fernando Dini Andreotea, f

a Department of Soil Science, “Luiz de Queiroz” College of Agriculture (ESALQ), University of São Paulo (USP), Piracicaba, São Paulo, Brazil
b Luxembourg Institute of Science and Technology (LIST), Belvaux, Luxembourg
c Brazilian Agricultural Research Corporation (Embrapa Roraima), Boa Vista, Roraima, Brazil
d Federal Institute of Education, Science, and Technology of Pará (IFPA), Castanhal, Pará, Brazil
e Center for Nuclear Energy in Agriculture (CENA), University of São Paulo (USP), Piracicaba, São Paulo, Brazil
f Center for Carbon Research in Tropical Agriculture (CCARBON), University of São Paulo (USP), Piracicaba, São Paulo, Brazil

Highlights

  • Agroforestry enhances soil microbial activity and shapes trait-based strategies associated with substrate-use versatility and growth rate.
  • SOC sequestration increases under agroforestry, with POM-C and MAOM-C rising by ∼300% and ∼200% (respectively).
  • Agroforestry promotes microbial necromass C accumulation, yet this does not translate into a greater contribution to total SOC.

Abstract

Oil palm-based agroforestry systems (AFS) can promote soil organic carbon (SOC) sequestration, but the links among plant richness, microbial communities, and SOC persistence remain only partially understood. Here, using long-term AFS plots and oil palm (Elaeis guineensis) monocultures in the Amazon, we show that AFS enhances microbial activity and assembles distinct microbial communities, while selects for contrasting microbial life strategies associated with resource acquisition and growth. These changes are accompanied by increases in particulate (POM-C; up to ∼300% and assumed as more labile) and mineral-associated (MAOM-C; up to ∼200% and assumed to be more persistent) SOC, with effects primarily dependent on plant species composition. Microbial necromass carbon (MNC) accumulation in AFS demonstrated similar increase and it was dominated by fungal necromass (∼64%) vs. bacterial necromass (∼36%). However, the contribution of MNC to SOC was decoupled from increases in MNC contents, accounting for a maximum of ∼27% of the bulk SOC in AFS (while ∼25% in monoculture), challenging the prevailing paradigm that multi-species plant cultivation and high microbial activity are major drivers of MNC contributions to SOC. These findings highlight ecosystem-level interactions as determinants of SOC sequestration and offer the first insights into MNC accumulation pathways in Amazonian agricultural systems.
Keywords
Agroforestry systems; Elaeis guineensis; Soil organic carbon; Microbial necromass carbon; Soil microbial community assembly

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