Litter chemical traits, microbial and soil stoichiometry regulate organic carbon accrual of particulate and mineral-associated organic matter
Abstract Plant litter quality considerably affects C accrual in soil organic matter (SOM). However, the chemical traits of litter that influence C distribution in SOM fractions, such as particulate organic matter (POM) and mineral-associated organic matter (MAOM), are not fully understood. Thus, we...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Cheng, Xiangrong [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2023 |
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| Schlagwörter: |
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| Anmerkung: |
© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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| Übergeordnetes Werk: |
Enthalten in: Biology and fertility of soils - Berlin : Springer, 1985, 59(2023), 7 vom: 06. Juni, Seite 777-790 |
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| Übergeordnetes Werk: |
volume:59 ; year:2023 ; number:7 ; day:06 ; month:06 ; pages:777-790 |
| Links: |
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| DOI / URN: |
10.1007/s00374-023-01746-0 |
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| Katalog-ID: |
SPR052985830 |
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| 520 | |a Abstract Plant litter quality considerably affects C accrual in soil organic matter (SOM). However, the chemical traits of litter that influence C distribution in SOM fractions, such as particulate organic matter (POM) and mineral-associated organic matter (MAOM), are not fully understood. Thus, we conducted a 150-day incubation experiment with litter addition (poplar leaves, roots, grasses grown under the canopy, and a mixture of these three litter types). We analyzed the organic C concentration in the POM and MAOM fractions and the stoichiometric ratios (C:N:P) of the soil and microbial biomass 50, 100, and 150 days after the initial litter addition. Microbial residue C (amino sugar biomarkers) in SOM fractions was registered at the end of decomposition. High-quality litter (i.e., leaf) increased MAOM-C accrual, and low-quality litter (i.e., root and grass) contributed more to POM-C accrual. The mixed litter addition accumulated more C in the SOM via high POM-C levels compared to single litter input, likely resulting from an antagonistic effect caused by different litter trait dissimilarity. Moreover, POM-C dynamics were dominated by litter chemical traits during litter decomposition, and MAOM-C was controlled mainly by microbial and soil stoichiometry. Furthermore, the contribution of microbial residue C to SOM (especially POM-C) was lower in the mixed litter than in the single litter. These findings highlight the direct or indirect impacts of litter types on the C dynamics of POM and MAOM, and demonstrate that litter diversity is conducive to C accumulation in SOM. | ||
| 650 | 4 | |a Soil organic matter |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Particulate organic matter |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Mineral-associated organic matter |7 (dpeaa)DE-He213 | |
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| 700 | 1 | |a Liu, Jiangwei |4 aut | |
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10.1007/s00374-023-01746-0 doi (DE-627)SPR052985830 (SPR)s00374-023-01746-0-e DE-627 ger DE-627 rakwb eng Cheng, Xiangrong verfasserin (orcid)0000-0001-7253-072X aut Litter chemical traits, microbial and soil stoichiometry regulate organic carbon accrual of particulate and mineral-associated organic matter 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Plant litter quality considerably affects C accrual in soil organic matter (SOM). However, the chemical traits of litter that influence C distribution in SOM fractions, such as particulate organic matter (POM) and mineral-associated organic matter (MAOM), are not fully understood. Thus, we conducted a 150-day incubation experiment with litter addition (poplar leaves, roots, grasses grown under the canopy, and a mixture of these three litter types). We analyzed the organic C concentration in the POM and MAOM fractions and the stoichiometric ratios (C:N:P) of the soil and microbial biomass 50, 100, and 150 days after the initial litter addition. Microbial residue C (amino sugar biomarkers) in SOM fractions was registered at the end of decomposition. High-quality litter (i.e., leaf) increased MAOM-C accrual, and low-quality litter (i.e., root and grass) contributed more to POM-C accrual. The mixed litter addition accumulated more C in the SOM via high POM-C levels compared to single litter input, likely resulting from an antagonistic effect caused by different litter trait dissimilarity. Moreover, POM-C dynamics were dominated by litter chemical traits during litter decomposition, and MAOM-C was controlled mainly by microbial and soil stoichiometry. Furthermore, the contribution of microbial residue C to SOM (especially POM-C) was lower in the mixed litter than in the single litter. These findings highlight the direct or indirect impacts of litter types on the C dynamics of POM and MAOM, and demonstrate that litter diversity is conducive to C accumulation in SOM. Soil organic matter (dpeaa)DE-He213 Particulate organic matter (dpeaa)DE-He213 Mineral-associated organic matter (dpeaa)DE-He213 Microbial residue (dpeaa)DE-He213 Organic carbon accumulation (dpeaa)DE-He213 Xing, Wenli aut Liu, Jiangwei aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 59(2023), 7 vom: 06. Juni, Seite 777-790 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:59 year:2023 number:7 day:06 month:06 pages:777-790 https://dx.doi.org/10.1007/s00374-023-01746-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 59 2023 7 06 06 777-790 |
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10.1007/s00374-023-01746-0 doi (DE-627)SPR052985830 (SPR)s00374-023-01746-0-e DE-627 ger DE-627 rakwb eng Cheng, Xiangrong verfasserin (orcid)0000-0001-7253-072X aut Litter chemical traits, microbial and soil stoichiometry regulate organic carbon accrual of particulate and mineral-associated organic matter 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Plant litter quality considerably affects C accrual in soil organic matter (SOM). However, the chemical traits of litter that influence C distribution in SOM fractions, such as particulate organic matter (POM) and mineral-associated organic matter (MAOM), are not fully understood. Thus, we conducted a 150-day incubation experiment with litter addition (poplar leaves, roots, grasses grown under the canopy, and a mixture of these three litter types). We analyzed the organic C concentration in the POM and MAOM fractions and the stoichiometric ratios (C:N:P) of the soil and microbial biomass 50, 100, and 150 days after the initial litter addition. Microbial residue C (amino sugar biomarkers) in SOM fractions was registered at the end of decomposition. High-quality litter (i.e., leaf) increased MAOM-C accrual, and low-quality litter (i.e., root and grass) contributed more to POM-C accrual. The mixed litter addition accumulated more C in the SOM via high POM-C levels compared to single litter input, likely resulting from an antagonistic effect caused by different litter trait dissimilarity. Moreover, POM-C dynamics were dominated by litter chemical traits during litter decomposition, and MAOM-C was controlled mainly by microbial and soil stoichiometry. Furthermore, the contribution of microbial residue C to SOM (especially POM-C) was lower in the mixed litter than in the single litter. These findings highlight the direct or indirect impacts of litter types on the C dynamics of POM and MAOM, and demonstrate that litter diversity is conducive to C accumulation in SOM. Soil organic matter (dpeaa)DE-He213 Particulate organic matter (dpeaa)DE-He213 Mineral-associated organic matter (dpeaa)DE-He213 Microbial residue (dpeaa)DE-He213 Organic carbon accumulation (dpeaa)DE-He213 Xing, Wenli aut Liu, Jiangwei aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 59(2023), 7 vom: 06. Juni, Seite 777-790 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:59 year:2023 number:7 day:06 month:06 pages:777-790 https://dx.doi.org/10.1007/s00374-023-01746-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 59 2023 7 06 06 777-790 |
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10.1007/s00374-023-01746-0 doi (DE-627)SPR052985830 (SPR)s00374-023-01746-0-e DE-627 ger DE-627 rakwb eng Cheng, Xiangrong verfasserin (orcid)0000-0001-7253-072X aut Litter chemical traits, microbial and soil stoichiometry regulate organic carbon accrual of particulate and mineral-associated organic matter 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Plant litter quality considerably affects C accrual in soil organic matter (SOM). However, the chemical traits of litter that influence C distribution in SOM fractions, such as particulate organic matter (POM) and mineral-associated organic matter (MAOM), are not fully understood. Thus, we conducted a 150-day incubation experiment with litter addition (poplar leaves, roots, grasses grown under the canopy, and a mixture of these three litter types). We analyzed the organic C concentration in the POM and MAOM fractions and the stoichiometric ratios (C:N:P) of the soil and microbial biomass 50, 100, and 150 days after the initial litter addition. Microbial residue C (amino sugar biomarkers) in SOM fractions was registered at the end of decomposition. High-quality litter (i.e., leaf) increased MAOM-C accrual, and low-quality litter (i.e., root and grass) contributed more to POM-C accrual. The mixed litter addition accumulated more C in the SOM via high POM-C levels compared to single litter input, likely resulting from an antagonistic effect caused by different litter trait dissimilarity. Moreover, POM-C dynamics were dominated by litter chemical traits during litter decomposition, and MAOM-C was controlled mainly by microbial and soil stoichiometry. Furthermore, the contribution of microbial residue C to SOM (especially POM-C) was lower in the mixed litter than in the single litter. These findings highlight the direct or indirect impacts of litter types on the C dynamics of POM and MAOM, and demonstrate that litter diversity is conducive to C accumulation in SOM. Soil organic matter (dpeaa)DE-He213 Particulate organic matter (dpeaa)DE-He213 Mineral-associated organic matter (dpeaa)DE-He213 Microbial residue (dpeaa)DE-He213 Organic carbon accumulation (dpeaa)DE-He213 Xing, Wenli aut Liu, Jiangwei aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 59(2023), 7 vom: 06. Juni, Seite 777-790 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:59 year:2023 number:7 day:06 month:06 pages:777-790 https://dx.doi.org/10.1007/s00374-023-01746-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 59 2023 7 06 06 777-790 |
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10.1007/s00374-023-01746-0 doi (DE-627)SPR052985830 (SPR)s00374-023-01746-0-e DE-627 ger DE-627 rakwb eng Cheng, Xiangrong verfasserin (orcid)0000-0001-7253-072X aut Litter chemical traits, microbial and soil stoichiometry regulate organic carbon accrual of particulate and mineral-associated organic matter 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Plant litter quality considerably affects C accrual in soil organic matter (SOM). However, the chemical traits of litter that influence C distribution in SOM fractions, such as particulate organic matter (POM) and mineral-associated organic matter (MAOM), are not fully understood. Thus, we conducted a 150-day incubation experiment with litter addition (poplar leaves, roots, grasses grown under the canopy, and a mixture of these three litter types). We analyzed the organic C concentration in the POM and MAOM fractions and the stoichiometric ratios (C:N:P) of the soil and microbial biomass 50, 100, and 150 days after the initial litter addition. Microbial residue C (amino sugar biomarkers) in SOM fractions was registered at the end of decomposition. High-quality litter (i.e., leaf) increased MAOM-C accrual, and low-quality litter (i.e., root and grass) contributed more to POM-C accrual. The mixed litter addition accumulated more C in the SOM via high POM-C levels compared to single litter input, likely resulting from an antagonistic effect caused by different litter trait dissimilarity. Moreover, POM-C dynamics were dominated by litter chemical traits during litter decomposition, and MAOM-C was controlled mainly by microbial and soil stoichiometry. Furthermore, the contribution of microbial residue C to SOM (especially POM-C) was lower in the mixed litter than in the single litter. These findings highlight the direct or indirect impacts of litter types on the C dynamics of POM and MAOM, and demonstrate that litter diversity is conducive to C accumulation in SOM. Soil organic matter (dpeaa)DE-He213 Particulate organic matter (dpeaa)DE-He213 Mineral-associated organic matter (dpeaa)DE-He213 Microbial residue (dpeaa)DE-He213 Organic carbon accumulation (dpeaa)DE-He213 Xing, Wenli aut Liu, Jiangwei aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 59(2023), 7 vom: 06. Juni, Seite 777-790 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:59 year:2023 number:7 day:06 month:06 pages:777-790 https://dx.doi.org/10.1007/s00374-023-01746-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 59 2023 7 06 06 777-790 |
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10.1007/s00374-023-01746-0 doi (DE-627)SPR052985830 (SPR)s00374-023-01746-0-e DE-627 ger DE-627 rakwb eng Cheng, Xiangrong verfasserin (orcid)0000-0001-7253-072X aut Litter chemical traits, microbial and soil stoichiometry regulate organic carbon accrual of particulate and mineral-associated organic matter 2023 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract Plant litter quality considerably affects C accrual in soil organic matter (SOM). However, the chemical traits of litter that influence C distribution in SOM fractions, such as particulate organic matter (POM) and mineral-associated organic matter (MAOM), are not fully understood. Thus, we conducted a 150-day incubation experiment with litter addition (poplar leaves, roots, grasses grown under the canopy, and a mixture of these three litter types). We analyzed the organic C concentration in the POM and MAOM fractions and the stoichiometric ratios (C:N:P) of the soil and microbial biomass 50, 100, and 150 days after the initial litter addition. Microbial residue C (amino sugar biomarkers) in SOM fractions was registered at the end of decomposition. High-quality litter (i.e., leaf) increased MAOM-C accrual, and low-quality litter (i.e., root and grass) contributed more to POM-C accrual. The mixed litter addition accumulated more C in the SOM via high POM-C levels compared to single litter input, likely resulting from an antagonistic effect caused by different litter trait dissimilarity. Moreover, POM-C dynamics were dominated by litter chemical traits during litter decomposition, and MAOM-C was controlled mainly by microbial and soil stoichiometry. Furthermore, the contribution of microbial residue C to SOM (especially POM-C) was lower in the mixed litter than in the single litter. These findings highlight the direct or indirect impacts of litter types on the C dynamics of POM and MAOM, and demonstrate that litter diversity is conducive to C accumulation in SOM. Soil organic matter (dpeaa)DE-He213 Particulate organic matter (dpeaa)DE-He213 Mineral-associated organic matter (dpeaa)DE-He213 Microbial residue (dpeaa)DE-He213 Organic carbon accumulation (dpeaa)DE-He213 Xing, Wenli aut Liu, Jiangwei aut Enthalten in Biology and fertility of soils Berlin : Springer, 1985 59(2023), 7 vom: 06. Juni, Seite 777-790 (DE-627)269015426 (DE-600)1473419-9 1432-0789 nnns volume:59 year:2023 number:7 day:06 month:06 pages:777-790 https://dx.doi.org/10.1007/s00374-023-01746-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_647 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 59 2023 7 06 06 777-790 |
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Enthalten in Biology and fertility of soils 59(2023), 7 vom: 06. Juni, Seite 777-790 volume:59 year:2023 number:7 day:06 month:06 pages:777-790 |
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Enthalten in Biology and fertility of soils 59(2023), 7 vom: 06. Juni, Seite 777-790 volume:59 year:2023 number:7 day:06 month:06 pages:777-790 |
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Biology and fertility of soils |
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Cheng, Xiangrong @@aut@@ Xing, Wenli @@aut@@ Liu, Jiangwei @@aut@@ |
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Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Plant litter quality considerably affects C accrual in soil organic matter (SOM). However, the chemical traits of litter that influence C distribution in SOM fractions, such as particulate organic matter (POM) and mineral-associated organic matter (MAOM), are not fully understood. Thus, we conducted a 150-day incubation experiment with litter addition (poplar leaves, roots, grasses grown under the canopy, and a mixture of these three litter types). 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Cheng, Xiangrong |
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Cheng, Xiangrong misc Soil organic matter misc Particulate organic matter misc Mineral-associated organic matter misc Microbial residue misc Organic carbon accumulation Litter chemical traits, microbial and soil stoichiometry regulate organic carbon accrual of particulate and mineral-associated organic matter |
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Litter chemical traits, microbial and soil stoichiometry regulate organic carbon accrual of particulate and mineral-associated organic matter Soil organic matter (dpeaa)DE-He213 Particulate organic matter (dpeaa)DE-He213 Mineral-associated organic matter (dpeaa)DE-He213 Microbial residue (dpeaa)DE-He213 Organic carbon accumulation (dpeaa)DE-He213 |
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misc Soil organic matter misc Particulate organic matter misc Mineral-associated organic matter misc Microbial residue misc Organic carbon accumulation |
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misc Soil organic matter misc Particulate organic matter misc Mineral-associated organic matter misc Microbial residue misc Organic carbon accumulation |
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Litter chemical traits, microbial and soil stoichiometry regulate organic carbon accrual of particulate and mineral-associated organic matter |
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litter chemical traits, microbial and soil stoichiometry regulate organic carbon accrual of particulate and mineral-associated organic matter |
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Litter chemical traits, microbial and soil stoichiometry regulate organic carbon accrual of particulate and mineral-associated organic matter |
| abstract |
Abstract Plant litter quality considerably affects C accrual in soil organic matter (SOM). However, the chemical traits of litter that influence C distribution in SOM fractions, such as particulate organic matter (POM) and mineral-associated organic matter (MAOM), are not fully understood. Thus, we conducted a 150-day incubation experiment with litter addition (poplar leaves, roots, grasses grown under the canopy, and a mixture of these three litter types). We analyzed the organic C concentration in the POM and MAOM fractions and the stoichiometric ratios (C:N:P) of the soil and microbial biomass 50, 100, and 150 days after the initial litter addition. Microbial residue C (amino sugar biomarkers) in SOM fractions was registered at the end of decomposition. High-quality litter (i.e., leaf) increased MAOM-C accrual, and low-quality litter (i.e., root and grass) contributed more to POM-C accrual. The mixed litter addition accumulated more C in the SOM via high POM-C levels compared to single litter input, likely resulting from an antagonistic effect caused by different litter trait dissimilarity. Moreover, POM-C dynamics were dominated by litter chemical traits during litter decomposition, and MAOM-C was controlled mainly by microbial and soil stoichiometry. Furthermore, the contribution of microbial residue C to SOM (especially POM-C) was lower in the mixed litter than in the single litter. These findings highlight the direct or indirect impacts of litter types on the C dynamics of POM and MAOM, and demonstrate that litter diversity is conducive to C accumulation in SOM. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
| abstractGer |
Abstract Plant litter quality considerably affects C accrual in soil organic matter (SOM). However, the chemical traits of litter that influence C distribution in SOM fractions, such as particulate organic matter (POM) and mineral-associated organic matter (MAOM), are not fully understood. Thus, we conducted a 150-day incubation experiment with litter addition (poplar leaves, roots, grasses grown under the canopy, and a mixture of these three litter types). We analyzed the organic C concentration in the POM and MAOM fractions and the stoichiometric ratios (C:N:P) of the soil and microbial biomass 50, 100, and 150 days after the initial litter addition. Microbial residue C (amino sugar biomarkers) in SOM fractions was registered at the end of decomposition. High-quality litter (i.e., leaf) increased MAOM-C accrual, and low-quality litter (i.e., root and grass) contributed more to POM-C accrual. The mixed litter addition accumulated more C in the SOM via high POM-C levels compared to single litter input, likely resulting from an antagonistic effect caused by different litter trait dissimilarity. Moreover, POM-C dynamics were dominated by litter chemical traits during litter decomposition, and MAOM-C was controlled mainly by microbial and soil stoichiometry. Furthermore, the contribution of microbial residue C to SOM (especially POM-C) was lower in the mixed litter than in the single litter. These findings highlight the direct or indirect impacts of litter types on the C dynamics of POM and MAOM, and demonstrate that litter diversity is conducive to C accumulation in SOM. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
| abstract_unstemmed |
Abstract Plant litter quality considerably affects C accrual in soil organic matter (SOM). However, the chemical traits of litter that influence C distribution in SOM fractions, such as particulate organic matter (POM) and mineral-associated organic matter (MAOM), are not fully understood. Thus, we conducted a 150-day incubation experiment with litter addition (poplar leaves, roots, grasses grown under the canopy, and a mixture of these three litter types). We analyzed the organic C concentration in the POM and MAOM fractions and the stoichiometric ratios (C:N:P) of the soil and microbial biomass 50, 100, and 150 days after the initial litter addition. Microbial residue C (amino sugar biomarkers) in SOM fractions was registered at the end of decomposition. High-quality litter (i.e., leaf) increased MAOM-C accrual, and low-quality litter (i.e., root and grass) contributed more to POM-C accrual. The mixed litter addition accumulated more C in the SOM via high POM-C levels compared to single litter input, likely resulting from an antagonistic effect caused by different litter trait dissimilarity. Moreover, POM-C dynamics were dominated by litter chemical traits during litter decomposition, and MAOM-C was controlled mainly by microbial and soil stoichiometry. Furthermore, the contribution of microbial residue C to SOM (especially POM-C) was lower in the mixed litter than in the single litter. These findings highlight the direct or indirect impacts of litter types on the C dynamics of POM and MAOM, and demonstrate that litter diversity is conducive to C accumulation in SOM. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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| title_short |
Litter chemical traits, microbial and soil stoichiometry regulate organic carbon accrual of particulate and mineral-associated organic matter |
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https://dx.doi.org/10.1007/s00374-023-01746-0 |
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Xing, Wenli Liu, Jiangwei |
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2024-07-03T16:13:40.132Z |
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|
| score |
7.400017 |