Soil aggregates reveal tree species and land-use legacy effects on early carbon storage pathways during reforestation
Preprint
Abstract
Reforestation is a leading natural climate solution, but bulk soil organic carbon (C) often responds slowly, obscuring early belowground change. We tested whether soil aggregates reveal early structural reorganization that affects C retention pathways at a three-year-old experimental reforestation planting established on former pasture in Oregon, USA. We sampled soils at 0-20 and 20-40 cm beneath incense cedar ( Calocedrus decurrens ; arbuscular mycorrhizal [AM]), black cottonwood ( Populus trichocarpa ; AM and ectomycorrhizal [EcM]), ponderosa pine ( Pinus ponderosa ; EcM), and treeless controls. We measured bulk soil C concentration and C:N, aggregate size distribution and mean weight diameter (MWD), fraction-associated C, and, in a subset of surface aggregate fractions, natural-abundance δ¹³C to evaluate soil C pools, physical structure, C distribution, and C processing. After three years, reforestation did not produce significant differences in bulk soil C between planted trees and treeless controls. In surface soil, MWD averaged 36% higher under incense cedar and 58% higher under black cottonwood than under controls, whereas ponderosa pine remained similar to controls. The clearest treatment differences in C distribution occurred in macroaggregates. Incense cedar and black cottonwood had higher large (>2000 µm) macroaggregate-associated C than controls, while black cottonwood combined a greater proportion of large macroaggregates with lower C concentrations, indicating that structural development and C accumulation were partly decoupled. Species patterns were broadly consistent with stronger early aggregate responses under AM-compatible species in former-pasture legacy conditions; by contrast, the EcM-associated ponderosa pine remained closer to treeless controls across multiple aggregate measures. Treatment effects weakened with depth and were limited in microaggregates (250-53 µm) and silt-and-clay (Open Research Statement: All raw data and metadata are provided for peer-review with Dryad at xxxxx, where it will be permanently archived for public access upon acceptance.Keywords
Funding Information
- Eugene Water and Electric Board
- Environmental Science Summer Research Fellowship of the Environmental Studies Program at the University of Oregon
This publication has 95 references indexed in Scilit:
- Mycorrhizal legacy mediates seedling success following timber harvesting in Northeastern forestsEcological Applications, 2026
- Dual-mycorrhizal colonization is determined by plant age and host identity in two species of PopulusMycorrhiza, 2025
- Ecological Restoration Enhances the Stability and Associated Organic Carbon of Soil Aggregates in a Tibetan Alpine MeadowLand Degradation & Development, 2024
- Nature versus nurture: Quantifying the effects of management, region, and hillslope position on soil health indicators in an on‐farm survey in MinnesotaSoil Science Society of America Journal, 2024
- The linkage of 13C and 15N soil depth gradients with C:N and O:C stoichiometry reveals tree species effects on organic matter turnover in soilBiogeochemistry, 2020
- Microaggregates in soilsJournal of Plant Nutrition and Soil Science, 2017
- Carbon isotopes for estimating soil decomposition and physical mixing in well‐drained forest soilsJournal of Geophysical Research: Biogeosciences, 2013
- Ectomycorrhizas and water relations of trees: a reviewMycorrhiza, 2010
- Review: Factors affecting rhizosphere priming effectsJournal of Plant Nutrition and Soil Science, 2002
- Soil organic matter and structural stability: mechanisms and implications for managementPlant and Soil, 1984