Conversion of degraded forests to oil palm plantations in the Peruvian Amazonia: Shifts in soil and ecosystem-level greenhouse gas fluxes

Oil palm (OP) expansion and associated forest clearance can significantly impact greenhouse gas (GHG) fluxes. We investigated carbon stocks and soil GHG (N 2 O, CO 2 , CH 4 ) fluxes in a degraded forest and an adjacent 17-year-old OP plantation in Peruvian Amazonia. The plantation comprised three nitrogen (N) fertilizer treatments: 0 (OPN0), 84 (OPN1), 168 (OPN2) kg N ha −1 y −1 . Carbon stocks were inventoried across all pools. GHG and environmental parameters were monitored monthly for 11 months and (bi)daily when fertilizing the OP, with measurements taken both near and far from trees/palms. Ecosystem-scale CO 2 equivalent losses from the conversion were computed by balancing carbon stock losses against N 2 O emission changes. N 2 O emissions (kg N ha −1 y −1 ) in the forest (6.7 ± 1.2) where litterfall N inputs were large (213 kg N ha −1 y −1 ) were 11, 5, and 3 times the emissions in OPN0 (0.6 ± 0.2), OPN1 (1.4 ± 0.2), and OPN2 (2.3 ± 0.3). In the plantation, 1 % of the N fertilizer applied was released as N 2 O. Across ecosystems, N inputs primarily controlled N 2 O emissions. Soil respiration (Mg C ha −1 y −1 ) was 1.4 times higher in the forest (9.1 ± 0.6) than in the plantation (7.3 ± 1, 5.5 ± 0.5, 6.5 ± 0.3 in OPN0, OPN1, OPN2). The forest was a soil CH 4 (kg C ha −1 y −1 ) sink (-1.5 ± 0.3) while all OP treatments were sources (0.2 ± 0.3, 0.7 ± 0.5, 0.2 ± 0.4 in OPN0, OPN1, OPN2). Ecosystem carbon stock losses from forest-to-OP conversion were substantial (196.8 ± 44.0 Mg CO 2 ha −1 15 y −1 ) and partially offset (14–20 %) by decreased N 2 O emissions. Complementary studies for this transition are needed to improve global GHG assessments. • Soil N 2 O emissions were higher in the degraded forest than the oil palm plantation. • Soil respiration was higher in the degraded forest than the oil palm plantation. • The soil was a CH 4 sink in the degraded forest, a CH 4 source in the oil palm plantation. • Degraded forest conversion to oil palm plantation substantially reduced ecosystem C stocks. • C stock losses from the conversion were 14–20 % offset by decreased N 2 O emissions.

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Publication Details

Journal
Agriculture Ecosystems & Environment
Published
2025-03-12
DOI
https://doi.org/10.1016/j.agee.2025.109603
Citations
4
Primary Topic
Oil Palm Production and Sustainability
Type
article
Field-Weighted Citation Impact
6.87

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article

Conversion of degraded forests to oil palm plantations in the Peruvian Amazonia: Shifts in soil and ecosystem-level greenhouse gas fluxes

Mariela López Gonzales, Natalia Málaga, Kristell Hergoualc’h, Christopher Martius
4 citations
Agriculture Ecosystems & Environment
Oil Palm Production and Sustainability
6.87
article

Conversion of degraded forests to oil palm plantations in the Peruvian Amazonia: Shifts in soil and ecosystem-level greenhouse gas fluxes

Mariela López Gonzales, Natalia Málaga, Kristell Hergoualc’h, Christopher Martius
article en
4 citations

Abstract

Oil palm (OP) expansion and associated forest clearance can significantly impact greenhouse gas (GHG) fluxes. We investigated carbon stocks and soil GHG (N 2 O, CO 2 , CH 4 ) fluxes in a degraded forest and an adjacent 17-year-old OP plantation in Peruvian Amazonia. The plantation comprised three nitrogen (N) fertilizer treatments: 0 (OPN0), 84 (OPN1), 168 (OPN2) kg N ha −1 y −1 . Carbon stocks were inventoried across all pools. GHG and environmental parameters were monitored monthly for 11 months and (bi)daily when fertilizing the OP, with measurements taken both near and far from trees/palms. Ecosystem-scale CO 2 equivalent losses from the conversion were computed by balancing carbon stock losses against N 2 O emission changes. N 2 O emissions (kg N ha −1 y −1 ) in the forest (6.7 ± 1.2) where litterfall N inputs were large (213 kg N ha −1 y −1 ) were 11, 5, and 3 times the emissions in OPN0 (0.6 ± 0.2), OPN1 (1.4 ± 0.2), and OPN2 (2.3 ± 0.3). In the plantation, 1 % of the N fertilizer applied was released as N 2 O. Across ecosystems, N inputs primarily controlled N 2 O emissions. Soil respiration (Mg C ha −1 y −1 ) was 1.4 times higher in the forest (9.1 ± 0.6) than in the plantation (7.3 ± 1, 5.5 ± 0.5, 6.5 ± 0.3 in OPN0, OPN1, OPN2). The forest was a soil CH 4 (kg C ha −1 y −1 ) sink (-1.5 ± 0.3) while all OP treatments were sources (0.2 ± 0.3, 0.7 ± 0.5, 0.2 ± 0.4 in OPN0, OPN1, OPN2). Ecosystem carbon stock losses from forest-to-OP conversion were substantial (196.8 ± 44.0 Mg CO 2 ha −1 15 y −1 ) and partially offset (14–20 %) by decreased N 2 O emissions. Complementary studies for this transition are needed to improve global GHG assessments. • Soil N 2 O emissions were higher in the degraded forest than the oil palm plantation. • Soil respiration was higher in the degraded forest than the oil palm plantation. • The soil was a CH 4 sink in the degraded forest, a CH 4 source in the oil palm plantation. • Degraded forest conversion to oil palm plantation substantially reduced ecosystem C stocks. • C stock losses from the conversion were 14–20 % offset by decreased N 2 O emissions.

Agriculture Ecosystems & EnvironmentVol. 386
Centre de Coopération Internationale en Recherche Agronomique pour le Développement (FR), BICC - Bonn International Centre for Conflict Studies (DE), Ecologie fonctionnelle & biogéochimie des sols & des agro-systèmes (FR), Center for International Forestry Research (PE), Wageningen University & Research (NL)
Consortium of International Agricultural Research Centers
Openalex Percentile: Top 4%
Oil Palm Production and Sustainability
6.87
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