Abstract

The increasing global demand for vegetable oils has resulted in a significant increase in the area under oil palm in the tropics during the last couple of decades, and this is projected to increase further. The Roundtable on Sustainable Palm Oil discourages the conversion of peatlands to oil palm and rubber plantations. However, our understanding of the effects on soil organic carbon (SOC) stocks and associated greenhouse gas (GHG) emissions of land use conversion is incomplete, especially for mineral soils under primary forests, secondary forests, rubber and other perennial plantations in the tropics. In this review we synthesised information on SOC stocks and GHG emissions from tropical mineral soils under forest, oil palm and rubber plantations and other agroecosystems across the tropical regions. We found that the largest SOC losses occurred after land use conversion from primary forest to oil palm and rubber plantations. Secondary forest and pasture lands showed lower SOC losses as well as total GHG (CO2, N2O and CH4) emissions when converted to oil palm and rubber plantations. However, due to the limited data available on all three GHG emissions, there remains high uncertainty in GHG emissions estimates, and regional GHG accounting is more reliable. We recommend long-term monitoring of oil palm and other perennial plantations established on tropical mineral soils on different soil types and regions on SOC stock changes and total GHG emissions and evaluate appropriate management practices to optimise production and sustainable economic returns, and minimise environmental impact.

Highlights

  • The increasing global demand for vegetable oils has resulted in a significant increase in the area under oil palm during the last decade, and this is projected to increase further [1]

  • In this review we synthesise information on soil carbon stocks and greenhouse gas (GHG) emissions from tropical mineral soils under forest, oil palm and rubber plantations and other agroecosystems of land uses across the tropical regions (details available in the tables in the Supplementary Materials for subtropical and tropical (30◦ N–30◦ S) regions)

  • We reviewed the changes in soil organic carbon (SOC) stocks (0–30 cm) and soil GHG emissions following tropical forest conversion on mineral soil

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Summary

Introduction

The increasing global demand for vegetable oils has resulted in a significant increase in the area under oil palm during the last decade, and this is projected to increase further [1]. Our understanding of the effects on soil carbon stocks of conversion of various land use types including tropical forests is still incomplete or even contradictory, especially for mineral soils [10,11]. Because of the very high emissions of major greenhouse gases (carbon dioxide CO2 , nitrous oxide N2 O and methane CH4 ) associated with the conversion of peatlands to oil palm and rubber plantations [12], conversion will increasingly focus on mineral soils [8]. SOC stock changes and associated greenhouse gas (GHG) emissions are poorly known for most land use systems on tropical mineral soils. In this review we synthesise information on soil carbon stocks and GHG emissions from tropical mineral soils under forest, oil palm and rubber plantations and other agroecosystems of land uses across the tropical regions

Materials and Methods
SOC Stocks under Different Ecosystems and Land Use Conversions
Losses
Magnitude of SOC Losses Due to Soil Erosion
Effect of Different Land Uses on GHG Fluxes from Tropical Mineral Soils
Findings
Perspectives
Full Text
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