熱帯雨林のゴム農園への転換が土壌炭素の長期保持を損なうことを解明(Conversion of Tropical Rainforest to Rubber Plantations Disrupts Soil Carbon Persistence)

2026-07-02 中国科学院(CAS)

中国科学院西双版納熱帯植物園(XTBG)の研究チームは、熱帯雨林をゴム農園へ転換すると、土壌有機炭素(SOC)の量だけでなく質も変化し、長期的な炭素固定能力が損なわれることを明らかにした。研究では、熱帯雨林跡地に造成された樹齢9年、21年、37年のゴム農園を比較し、植物由来炭素と微生物由来炭素の動態を解析した。その結果、転換直後には表層40cmのSOCが43%減少したが、農園の成熟に伴い落葉や根からの炭素供給増加などにより総量は回復した。一方で、リグニンフェノールとアミノ糖を指標として分析したところ、微生物由来炭素は植物由来炭素の5.2~9.3倍を占める重要な構成要素であるにもかかわらず、その組成は熱帯雨林とは異なる状態のままであり、安定的に土壌へ保持される能力が低下していた。研究は、土壌炭素量の維持だけでは気候変動対策として不十分であり、土壌攪乱の抑制や地下部への炭素投入を促進して、安定な土壌炭素の形成・維持を図る管理が必要であることを示した。

<関連情報>

熱帯雨林をゴム農園に転換すると、植物リグニンと微生物残渣の蓄積の仕方が変化することで、土壌有機炭素の隔離の様相が変化する Conversion of tropical rainforest to rubber plantations reshapes soil organic carbon sequestration through divergent accrual of plant lignin and microbial residues

Xia Yuan, Xiaoyi Cai, Xiai Zhu, Wenjie Liu
Journal of Environmental Management  Available online: 6 June 2026
DOI:https://doi.org/10.1016/j.jenvman.2026.130153

熱帯雨林のゴム農園への転換が土壌炭素の長期保持を損なうことを解明(Conversion of Tropical Rainforest to Rubber Plantations Disrupts Soil Carbon Persistence)

Highlights

  • Rainforest conversion reduced SOC, lignin phenols, and amino sugars.
  • Lignin phenols and amino sugars increased with rubber plantation age.
  • Microbial residues contributed 5.2–9.3 times more to SOC than plant residues.
  • Rubber managements need to consider SOC recovery and long-term C persistence.

Abstract

Tropical forests are being destroyed and converted to tree plantations at an alarming rate, with major consequences for soil organic carbon (SOC) cycling. Although mechanistic insights into SOC formation are fundamental to sustainable land management, how forest-to-plantation conversion modulates plant- and microbial-derived SOC remains unclear. Herein, we evaluated SOC sources using lignin phenols and amino sugars as biomarkers and identified their key drivers across a rubber plantation chronosequence (9, 21, and 37 years) established after tropical rainforest conversion in Southwest China. Both lignin phenol and amino sugar concentrations were positively correlated with total SOC and declined significantly with soil depth. Conversion of rainforest to young rubber plantations was associated with marked reductions in SOC (43%), lignin (18%), and amino sugars (7%) across the 0–40 cm profile. However, both biomarker pools followed an increasing trajectory with rubber stand age, likely driven by enhanced plant litter and root inputs together with reduced microbial lignin degradation. Lignin phenols were mainly regulated by plant properties (e.g., root biomass) and abiotic soil factors (e.g., nutrient availability), whereas amino sugar accumulation was more closely linked to microbial attributes. Notably, lower glucosamine:muramic acid ratios in rubber plantations than in rainforest soils suggest a shift in microbial residue composition that may influence the long-term persistence of microbial-derived SOC. Microbial residues contributed 5.2–9.3 times more to SOC than plant-derived C, highlighting the dominant role of microbial pathways in SOC formation. Moreover, rainforest-to-rubber conversion (regardless of stand age) decreased the relative contribution of plant-derived C to SOC while increasing that of microbial-derived C, particularly bacterial residues. Overall, our results indicate that conversion of tropical forest to rubber plantations was associated with substantial shifts in SOC composition, including an initial loss in both plant- and microbial-derived C and a compositional change in the microbial residue pool that may reduce its persistence potential. These findings highlight the need for rubber plantation managements that promote both SOC recovery and long-term persistence of key C components.

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