EGU25-9050, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-9050
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Tuesday, 29 Apr, 16:15–18:00 (CEST), Display time Tuesday, 29 Apr, 14:00–18:00
 
Hall X1, X1.41
Can SOC lost during initial forest-to-agriculture transitions be replenished within timeframes required for effective climate mitigation (typically decades)?
Jordi Buckley Paules1, Athanasios Paschalis2, and Yiannis Moustakis3
Jordi Buckley Paules et al.
  • 1Imperial College London / Grantham Institute
  • 2University of Cyprus / Imperial College London
  • 3Ludwig-Maximilians-Universität München

Soil organic carbon (SOC) dynamics are driven by a complex matrix of factors, including local climate (e.g., temperature, precipitation), soil properties (e.g., mineralogy, clay content, cation-exchange capacity, pH), and land use (e.g., forests, grassland, arable agriculture) and its history. Each parcel of land carries a unique signature within this matrix, resulting in distinct SOC dynamics and varied responses to land-use changes and future climate scenarios.

European political and environmental strategies increasingly emphasize (re) afforestation as a key measure for climate change mitigation. This represents a full-circle transformation for European landscapes, many of which were historically deforested to accommodate grazing and agriculture. With rising reforestation rates, these landscapes are gradually returning to their forested states. However, with this, a critical ecological question arises: can SOC lost during initial forest-to-agriculture transitions be replenished within timeframes required for effective climate mitigation (typically decades)?

This study addresses this question by focusing on irrecoverable carbon stocks—SOC fractions lost during land-use transitions that cannot be restored quickly enough to meet climate targets. Using the terrestrial biosphere model T&C, which incorporates a microbially explicit soil biogeochemistry module to simulate carbon (C), nitrogen (N), and phosphorus (P) dynamics, we investigate SOC recovery potential and how this varies with land management.

Our proof-of-concept approach here presented involves a) validating the T&C model across multiple European sites undergoing forest-to-agriculture and agriculture-to-forest transitions and b) simulating SOC dynamics for a representative European grid cell experiencing these transitions under distinct Shared Socioeconomic Pathway (SSP) climate scenarios.

Such work is imperative to gain critical insights into the persistence of irrecoverable carbon stocks and the feasibility of SOC recovery through European (re)afforestation efforts.

How to cite: Buckley Paules, J., Paschalis, A., and Moustakis, Y.: Can SOC lost during initial forest-to-agriculture transitions be replenished within timeframes required for effective climate mitigation (typically decades)?, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-9050, https://doi.org/10.5194/egusphere-egu25-9050, 2025.