The role of earthworms in the transformation of labile plant litter into mineral-associated organic matter

Although it has been recognized that the formation of organo-mineral complexes may be fostered by soil fauna, their formation pathways are far from understood. The objective of this study was to investigate the intensity and processes involved in earthworm-mediated mineral-associated organic matter (MAOM) formation. To this end, we used microcosms to produce casts with three different temperate earthworm species (epigeic Lumbricus castaneus [LC], epi-anecic Lumbricus terrestris [LT], endogeic Aporrectodea icterica [AI]) fed with 13 C-enriched Miscanthus litter in two contrasting soil types (Luvisol, Cambisol). To investigate MAOM formation processes, we used 13 C isotope tracing to track litter-derived carbon origin and neutral sugar biomarkers to resolve microbial transformation pathways. Our results indicated that cast MAOM-C content increased compared to the control treatment without earthworms with LC casts in Luvisol exhibiting the highest MAOM-C concentration (24.1 mg g -1 ). MAOM-C contribution to casts decreased in the order LC > LT > AI. Sugar biomarkers revealed species- and soil-dependent stabilization pathways: MAOM of LC casts in Luvisol contained high proportions of plant-derived arabinose, while MAOM of AI casts in Cambisol were enriched in microbial-derived hexoses (mannose) and deoxy-hexoses (rhamnose, fucose). We conclude that earthworms depending on species and soil type accelerated MAOM formation via synergistic pathways: (1) direct stabilization of plant sugars and (2) microbial transformation of labile litter into necromass during cast formation. We suggest that earthworm-driven MAOM formation depends on species-specific traits (e.g., LC’s capacity for litter fragmentation) and soil properties (e.g., clay and Ca content). • Earthworms accelerate formation of mineral-associated organic matter (MAOM) • Amount of MAOM depends on earthworm species • Interaction of soil type and earthworm species control stabilization processes • Earthworm gut passage can lead to direct stabilization of plant litter

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Publication Details

Journal
Soil Biology and Biochemistry
Published
2025-05-20
DOI
https://doi.org/10.1016/j.soilbio.2025.109859
Citations
5
Primary Topic
Invertebrate Taxonomy and Ecology
Type
article
Field-Weighted Citation Impact
15.13

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article

The role of earthworms in the transformation of labile plant litter into mineral-associated organic matter

Cornélia Rumpel, Axel Felbacq, Yacouba Zi, Nicolas Bottinelli et al.
5 citations
Soil Biology and Biochemistry
Invertebrate Taxonomy and Ecology
15.13
article

The role of earthworms in the transformation of labile plant litter into mineral-associated organic matter

Cornélia Rumpel, Axel Felbacq, Yacouba Zi, Nicolas Bottinelli, Chao Song, Shanshan Song, Marie-France Dignac
article en
5 citations

Abstract

Although it has been recognized that the formation of organo-mineral complexes may be fostered by soil fauna, their formation pathways are far from understood. The objective of this study was to investigate the intensity and processes involved in earthworm-mediated mineral-associated organic matter (MAOM) formation. To this end, we used microcosms to produce casts with three different temperate earthworm species (epigeic Lumbricus castaneus [LC], epi-anecic Lumbricus terrestris [LT], endogeic Aporrectodea icterica [AI]) fed with 13 C-enriched Miscanthus litter in two contrasting soil types (Luvisol, Cambisol). To investigate MAOM formation processes, we used 13 C isotope tracing to track litter-derived carbon origin and neutral sugar biomarkers to resolve microbial transformation pathways. Our results indicated that cast MAOM-C content increased compared to the control treatment without earthworms with LC casts in Luvisol exhibiting the highest MAOM-C concentration (24.1 mg g -1 ). MAOM-C contribution to casts decreased in the order LC > LT > AI. Sugar biomarkers revealed species- and soil-dependent stabilization pathways: MAOM of LC casts in Luvisol contained high proportions of plant-derived arabinose, while MAOM of AI casts in Cambisol were enriched in microbial-derived hexoses (mannose) and deoxy-hexoses (rhamnose, fucose). We conclude that earthworms depending on species and soil type accelerated MAOM formation via synergistic pathways: (1) direct stabilization of plant sugars and (2) microbial transformation of labile litter into necromass during cast formation. We suggest that earthworm-driven MAOM formation depends on species-specific traits (e.g., LC’s capacity for litter fragmentation) and soil properties (e.g., clay and Ca content). • Earthworms accelerate formation of mineral-associated organic matter (MAOM) • Amount of MAOM depends on earthworm species • Interaction of soil type and earthworm species control stabilization processes • Earthworm gut passage can lead to direct stabilization of plant litter

Soil Biology and BiochemistryVol. 208
Centre National de la Recherche Scientifique (FR), Université Paris-Est Créteil (FR), China Geological Survey (CN), Chinese Academy of Geological Sciences (CN), Sorbonne Université (FR), Institut d'écologie et des sciences de l'environnement de Paris (FR), Vietnam Academy of Agricultural Sciences (VN), Institut de Recherche pour le Développement (FR), Tsinghua University (CN)
Agence Nationale de la Recherche, National Natural Science Foundation of China, China Scholarship Council
Openalex Percentile: Top 1%
Invertebrate Taxonomy and Ecology
15.13
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