Pine afforestation improves the biological soil attributes linked to methane oxidation in a temperate zone of Argentina

ABSTRACT

Background:

Atmospheric methane (CH ₄) is responsible for approximately 20% of global warming since the preindustrial era. Forests are land ecosystems whose role is crucial for mitigating the greenhouse effect due to their capacity to capture and store C and preserve other processes such as CH ₄ oxidation in the soil. On the other hand, in the particular case of afforestation, there are contradictory results about the magnitude of CH ₄ uptake variation due to changes in methanotrophic bacteria activity and its relationship with micro-environmental conditions.

Results:

The average potential CH ₄ oxidation rate in the laboratory (MOL) of afforested soil was 186% greater than that of the grassland, which could be marginally attributed to differences in soil physicochemical parameters like bulk density, pH and organic matter. A seasonal pattern in MOL was observed in both land uses, with the highest values at the warm and rainy season. MOL magnitude increased with soil depth up to 10-15 cm, which corresponds with the mineral layer.

Conclusion:

Pine afforestation would improve the biological soil attributes linked to methane oxidising bacteria compared to the grassland systems.

Keywords:
Land use change; Methanotrophic bacteria; methane uptake; GHG mitigation; ecological services

HIGHLIGHTS

Afforested soils showed the highest methane oxidation rates.

Methane oxidation rate was higher in the warm and wet season of the year.

The higher methane oxidation rates were obtained at 10-15 cm depth.

The methane oxidation rate variation was marginally explained by soil parameters