Grazing exclusion increases soil organic C through microbial necromass of root-derived C as traced by 13C labelling photosynthate
Grasslands store large amounts of C; however, the underlying mechanisms of soil C sequestration after grazing exclusion are not well known. This study aimed to elucidate the drivers of soil organic C (SOC) sequestration from plant and microbial residues in temperate grasslands after long-term (~ 40...
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| Published in | Biology and fertility of soils Vol. 60; no. 3; pp. 407 - 420 |
|---|---|
| Main Authors | , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Berlin/Heidelberg
Springer Berlin Heidelberg
01.04.2024
Springer Nature B.V |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Grasslands store large amounts of C; however, the underlying mechanisms of soil C sequestration after grazing exclusion are not well known. This study aimed to elucidate the drivers of soil organic C (SOC) sequestration from plant and microbial residues in temperate grasslands after long-term (~ 40 years) grazing exclusion. We conducted in situ
13
C-CO
2
labelling experiments in the field and traced
13
C in plant-soil systems paired with biomarkers to assess the C input from plants into soils. Long-term grazing exclusion increased all plant and soil pools including shoots, roots, microbial biomass and necromass.
13
C allocation in these pools also increased, whereas
13
C was lost via respiration as CO
2
from soils decreased.
13
C incorporation into the soil and microbial biomass increased with
13
C allocation into the roots. Grazing exclusion for over 40 years increased the total SOC content by 190%, largely due to increases in fungal necromass C, and there was a minor contribution of lignin phenols to SOC accrual (0.8%). Consequently, grazing exclusion boosts not only aboveground biomass, but also larger roots and rhizodeposition, leading to microbial biomass and necromass formation. Microbial necromass and lignin phenols contribute to SOC accrual under grazing exclusion, and microbial necromass, especially fungal necromass, makes a larger contribution than lignin phenols. |
|---|---|
| AbstractList | Grasslands store large amounts of C; however, the underlying mechanisms of soil C sequestration after grazing exclusion are not well known. This study aimed to elucidate the drivers of soil organic C (SOC) sequestration from plant and microbial residues in temperate grasslands after long-term (~ 40 years) grazing exclusion. We conducted in situ ¹³C-CO₂ labelling experiments in the field and traced ¹³C in plant-soil systems paired with biomarkers to assess the C input from plants into soils. Long-term grazing exclusion increased all plant and soil pools including shoots, roots, microbial biomass and necromass. ¹³C allocation in these pools also increased, whereas ¹³C was lost via respiration as CO₂ from soils decreased. ¹³C incorporation into the soil and microbial biomass increased with ¹³C allocation into the roots. Grazing exclusion for over 40 years increased the total SOC content by 190%, largely due to increases in fungal necromass C, and there was a minor contribution of lignin phenols to SOC accrual (0.8%). Consequently, grazing exclusion boosts not only aboveground biomass, but also larger roots and rhizodeposition, leading to microbial biomass and necromass formation. Microbial necromass and lignin phenols contribute to SOC accrual under grazing exclusion, and microbial necromass, especially fungal necromass, makes a larger contribution than lignin phenols. Grasslands store large amounts of C; however, the underlying mechanisms of soil C sequestration after grazing exclusion are not well known. This study aimed to elucidate the drivers of soil organic C (SOC) sequestration from plant and microbial residues in temperate grasslands after long-term (~ 40 years) grazing exclusion. We conducted in situ 13 C-CO 2 labelling experiments in the field and traced 13 C in plant-soil systems paired with biomarkers to assess the C input from plants into soils. Long-term grazing exclusion increased all plant and soil pools including shoots, roots, microbial biomass and necromass. 13 C allocation in these pools also increased, whereas 13 C was lost via respiration as CO 2 from soils decreased. 13 C incorporation into the soil and microbial biomass increased with 13 C allocation into the roots. Grazing exclusion for over 40 years increased the total SOC content by 190%, largely due to increases in fungal necromass C, and there was a minor contribution of lignin phenols to SOC accrual (0.8%). Consequently, grazing exclusion boosts not only aboveground biomass, but also larger roots and rhizodeposition, leading to microbial biomass and necromass formation. Microbial necromass and lignin phenols contribute to SOC accrual under grazing exclusion, and microbial necromass, especially fungal necromass, makes a larger contribution than lignin phenols. Grasslands store large amounts of C; however, the underlying mechanisms of soil C sequestration after grazing exclusion are not well known. This study aimed to elucidate the drivers of soil organic C (SOC) sequestration from plant and microbial residues in temperate grasslands after long-term (~ 40 years) grazing exclusion. We conducted in situ 13C-CO2 labelling experiments in the field and traced 13C in plant-soil systems paired with biomarkers to assess the C input from plants into soils. Long-term grazing exclusion increased all plant and soil pools including shoots, roots, microbial biomass and necromass. 13C allocation in these pools also increased, whereas 13C was lost via respiration as CO2 from soils decreased. 13C incorporation into the soil and microbial biomass increased with 13C allocation into the roots. Grazing exclusion for over 40 years increased the total SOC content by 190%, largely due to increases in fungal necromass C, and there was a minor contribution of lignin phenols to SOC accrual (0.8%). Consequently, grazing exclusion boosts not only aboveground biomass, but also larger roots and rhizodeposition, leading to microbial biomass and necromass formation. Microbial necromass and lignin phenols contribute to SOC accrual under grazing exclusion, and microbial necromass, especially fungal necromass, makes a larger contribution than lignin phenols. |
| Author | Deng, Lei Kuzyakov, Yakov Deng, Jun Hai, Xuying Shangguan, Zhouping Qu, Qing Gunina, Anna |
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| Keywords | Particulate organic C Plant-microbe interaction Amino sugars C persistence Terrestrial C cycle Vegetation restoration Lignin phenols Mineral-associated organic C |
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| SubjectTerms | aboveground biomass Agriculture Biomarkers Biomass Biomedical and Life Sciences Carbon dioxide carbon sequestration Fungi Grasslands Grazing Labeling Life Sciences Lignin microbial biomass Microorganisms necromass Original Paper Phenols Plants rhizodeposition Roots Soil Soil microorganisms soil organic carbon Soil Science & Conservation Soils |
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| Title | Grazing exclusion increases soil organic C through microbial necromass of root-derived C as traced by 13C labelling photosynthate |
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