N-cycle gene abundance determination of N mineralization rate following re-afforestation in the Loess Plateau of China
Abstract Afforestation effectively improved soil microbial communities and significantly increased soil nitrogen mineralization rate (Rm).Soil microorganisms drive Rm by regulating soil N-cycling genes.Soil nitrification genes had a major effect on soil Rm than denitrification genes after afforestat...
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| Autor*in: |
Zhao, Yaping [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2024 |
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| Schlagwörter: |
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| Anmerkung: |
© Higher Education Press 2023 |
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| Übergeordnetes Werk: |
Enthalten in: Soil ecology letters - [Beijing] : Higher Education Press, 2019, 6(2024), 1 vom: 18. Jan. |
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| Übergeordnetes Werk: |
volume:6 ; year:2024 ; number:1 ; day:18 ; month:01 |
| Links: |
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| DOI / URN: |
10.1007/s42832-023-0188-0 |
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| Katalog-ID: |
SPR054513626 |
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| 520 | |a Abstract Afforestation effectively improved soil microbial communities and significantly increased soil nitrogen mineralization rate (Rm).Soil microorganisms drive Rm by regulating soil N-cycling genes.Soil nitrification genes had a major effect on soil Rm than denitrification genes after afforestation. Assessing the function of forest ecosystems requires an understanding of the mechanism of soil nitrogen mineralization. However, it remains unclear how soil N-cycling genes drive soil nitrogen mineralization during afforestation. In this study, we collected soil samples from a chrono-sequence of 14, 20, 30, and 45 years of Robinia pseudoacacia L. (RP14, RP20, RP30, and RP45) with a sloped farmland (FL) as a control. Through metagenomic sequencing analysis, we found significant changes in the diversity and composition of soil microbial communities involved in N-cycling along the afforestation time series, with afforestation effectively increasing the diversity (both alpha and beta diversity) of soil microbial communities. We conducted indoor culture experiments and analyzed correlations, which revealed a significant increase in both soil nitrification rate (Rn) and soil nitrogen mineralization rate (Rm) with increasing stand age. Furthermore, we found a strong correlation between soil Rm and soil microbial diversity (both alpha and beta diversity) and with the abundance of soil N-cycling genes. Partial least squares path modeling (PLS-PM) analysis showed that nitrification genes (narH, narY, nxrB, narG, narZ, nxrA, hao, pmoC-amoC) and denitrification genes (norB, nosZ, nirK) had a greater direct effect on soil Rm compared to their effect on soil microbial communities. Our results reveal the relationships between soil nitrogen mineralization rate and soil microbial communities and between the mineralization rate and functional genes involved in N-cycling, in the context of Robinia pseudoacacia L. restoration on the Loess Plateau. This study enriches the understanding of the effects of microorganisms on soil nitrogen mineralization rate during afforestation and provides a new theoretical basis for evaluating soil nitrogen mineralization mechanisms during forest succession. | ||
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10.1007/s42832-023-0188-0 doi (DE-627)SPR054513626 (SPR)s42832-023-0188-0-e DE-627 ger DE-627 rakwb eng Zhao, Yaping verfasserin aut N-cycle gene abundance determination of N mineralization rate following re-afforestation in the Loess Plateau of China 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Higher Education Press 2023 Abstract Afforestation effectively improved soil microbial communities and significantly increased soil nitrogen mineralization rate (Rm).Soil microorganisms drive Rm by regulating soil N-cycling genes.Soil nitrification genes had a major effect on soil Rm than denitrification genes after afforestation. Assessing the function of forest ecosystems requires an understanding of the mechanism of soil nitrogen mineralization. However, it remains unclear how soil N-cycling genes drive soil nitrogen mineralization during afforestation. In this study, we collected soil samples from a chrono-sequence of 14, 20, 30, and 45 years of Robinia pseudoacacia L. (RP14, RP20, RP30, and RP45) with a sloped farmland (FL) as a control. Through metagenomic sequencing analysis, we found significant changes in the diversity and composition of soil microbial communities involved in N-cycling along the afforestation time series, with afforestation effectively increasing the diversity (both alpha and beta diversity) of soil microbial communities. We conducted indoor culture experiments and analyzed correlations, which revealed a significant increase in both soil nitrification rate (Rn) and soil nitrogen mineralization rate (Rm) with increasing stand age. Furthermore, we found a strong correlation between soil Rm and soil microbial diversity (both alpha and beta diversity) and with the abundance of soil N-cycling genes. Partial least squares path modeling (PLS-PM) analysis showed that nitrification genes (narH, narY, nxrB, narG, narZ, nxrA, hao, pmoC-amoC) and denitrification genes (norB, nosZ, nirK) had a greater direct effect on soil Rm compared to their effect on soil microbial communities. Our results reveal the relationships between soil nitrogen mineralization rate and soil microbial communities and between the mineralization rate and functional genes involved in N-cycling, in the context of Robinia pseudoacacia L. restoration on the Loess Plateau. This study enriches the understanding of the effects of microorganisms on soil nitrogen mineralization rate during afforestation and provides a new theoretical basis for evaluating soil nitrogen mineralization mechanisms during forest succession. afforestation (dpeaa)DE-He213 soil N mineralization rate (dpeaa)DE-He213 denitrification genes (dpeaa)DE-He213 nitrification genes (dpeaa)DE-He213 the Loess Plateau (dpeaa)DE-He213 Zhao, Yuqing aut Zhang, Shuohong aut Xu, Yulin aut Han, Xinhui aut Yang, Gaihe aut Ren, Chengjie aut Enthalten in Soil ecology letters [Beijing] : Higher Education Press, 2019 6(2024), 1 vom: 18. Jan. (DE-627)1688167331 (DE-600)3006232-9 2662-2297 nnns volume:6 year:2024 number:1 day:18 month:01 https://dx.doi.org/10.1007/s42832-023-0188-0 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_65 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_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_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_2232 GBV_ILN_2336 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 6 2024 1 18 01 |
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10.1007/s42832-023-0188-0 doi (DE-627)SPR054513626 (SPR)s42832-023-0188-0-e DE-627 ger DE-627 rakwb eng Zhao, Yaping verfasserin aut N-cycle gene abundance determination of N mineralization rate following re-afforestation in the Loess Plateau of China 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Higher Education Press 2023 Abstract Afforestation effectively improved soil microbial communities and significantly increased soil nitrogen mineralization rate (Rm).Soil microorganisms drive Rm by regulating soil N-cycling genes.Soil nitrification genes had a major effect on soil Rm than denitrification genes after afforestation. Assessing the function of forest ecosystems requires an understanding of the mechanism of soil nitrogen mineralization. However, it remains unclear how soil N-cycling genes drive soil nitrogen mineralization during afforestation. In this study, we collected soil samples from a chrono-sequence of 14, 20, 30, and 45 years of Robinia pseudoacacia L. (RP14, RP20, RP30, and RP45) with a sloped farmland (FL) as a control. Through metagenomic sequencing analysis, we found significant changes in the diversity and composition of soil microbial communities involved in N-cycling along the afforestation time series, with afforestation effectively increasing the diversity (both alpha and beta diversity) of soil microbial communities. We conducted indoor culture experiments and analyzed correlations, which revealed a significant increase in both soil nitrification rate (Rn) and soil nitrogen mineralization rate (Rm) with increasing stand age. Furthermore, we found a strong correlation between soil Rm and soil microbial diversity (both alpha and beta diversity) and with the abundance of soil N-cycling genes. Partial least squares path modeling (PLS-PM) analysis showed that nitrification genes (narH, narY, nxrB, narG, narZ, nxrA, hao, pmoC-amoC) and denitrification genes (norB, nosZ, nirK) had a greater direct effect on soil Rm compared to their effect on soil microbial communities. Our results reveal the relationships between soil nitrogen mineralization rate and soil microbial communities and between the mineralization rate and functional genes involved in N-cycling, in the context of Robinia pseudoacacia L. restoration on the Loess Plateau. This study enriches the understanding of the effects of microorganisms on soil nitrogen mineralization rate during afforestation and provides a new theoretical basis for evaluating soil nitrogen mineralization mechanisms during forest succession. afforestation (dpeaa)DE-He213 soil N mineralization rate (dpeaa)DE-He213 denitrification genes (dpeaa)DE-He213 nitrification genes (dpeaa)DE-He213 the Loess Plateau (dpeaa)DE-He213 Zhao, Yuqing aut Zhang, Shuohong aut Xu, Yulin aut Han, Xinhui aut Yang, Gaihe aut Ren, Chengjie aut Enthalten in Soil ecology letters [Beijing] : Higher Education Press, 2019 6(2024), 1 vom: 18. Jan. (DE-627)1688167331 (DE-600)3006232-9 2662-2297 nnns volume:6 year:2024 number:1 day:18 month:01 https://dx.doi.org/10.1007/s42832-023-0188-0 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_65 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_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_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_2232 GBV_ILN_2336 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 6 2024 1 18 01 |
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10.1007/s42832-023-0188-0 doi (DE-627)SPR054513626 (SPR)s42832-023-0188-0-e DE-627 ger DE-627 rakwb eng Zhao, Yaping verfasserin aut N-cycle gene abundance determination of N mineralization rate following re-afforestation in the Loess Plateau of China 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Higher Education Press 2023 Abstract Afforestation effectively improved soil microbial communities and significantly increased soil nitrogen mineralization rate (Rm).Soil microorganisms drive Rm by regulating soil N-cycling genes.Soil nitrification genes had a major effect on soil Rm than denitrification genes after afforestation. Assessing the function of forest ecosystems requires an understanding of the mechanism of soil nitrogen mineralization. However, it remains unclear how soil N-cycling genes drive soil nitrogen mineralization during afforestation. In this study, we collected soil samples from a chrono-sequence of 14, 20, 30, and 45 years of Robinia pseudoacacia L. (RP14, RP20, RP30, and RP45) with a sloped farmland (FL) as a control. Through metagenomic sequencing analysis, we found significant changes in the diversity and composition of soil microbial communities involved in N-cycling along the afforestation time series, with afforestation effectively increasing the diversity (both alpha and beta diversity) of soil microbial communities. We conducted indoor culture experiments and analyzed correlations, which revealed a significant increase in both soil nitrification rate (Rn) and soil nitrogen mineralization rate (Rm) with increasing stand age. Furthermore, we found a strong correlation between soil Rm and soil microbial diversity (both alpha and beta diversity) and with the abundance of soil N-cycling genes. Partial least squares path modeling (PLS-PM) analysis showed that nitrification genes (narH, narY, nxrB, narG, narZ, nxrA, hao, pmoC-amoC) and denitrification genes (norB, nosZ, nirK) had a greater direct effect on soil Rm compared to their effect on soil microbial communities. Our results reveal the relationships between soil nitrogen mineralization rate and soil microbial communities and between the mineralization rate and functional genes involved in N-cycling, in the context of Robinia pseudoacacia L. restoration on the Loess Plateau. This study enriches the understanding of the effects of microorganisms on soil nitrogen mineralization rate during afforestation and provides a new theoretical basis for evaluating soil nitrogen mineralization mechanisms during forest succession. afforestation (dpeaa)DE-He213 soil N mineralization rate (dpeaa)DE-He213 denitrification genes (dpeaa)DE-He213 nitrification genes (dpeaa)DE-He213 the Loess Plateau (dpeaa)DE-He213 Zhao, Yuqing aut Zhang, Shuohong aut Xu, Yulin aut Han, Xinhui aut Yang, Gaihe aut Ren, Chengjie aut Enthalten in Soil ecology letters [Beijing] : Higher Education Press, 2019 6(2024), 1 vom: 18. Jan. (DE-627)1688167331 (DE-600)3006232-9 2662-2297 nnns volume:6 year:2024 number:1 day:18 month:01 https://dx.doi.org/10.1007/s42832-023-0188-0 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_65 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_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_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_2232 GBV_ILN_2336 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 6 2024 1 18 01 |
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10.1007/s42832-023-0188-0 doi (DE-627)SPR054513626 (SPR)s42832-023-0188-0-e DE-627 ger DE-627 rakwb eng Zhao, Yaping verfasserin aut N-cycle gene abundance determination of N mineralization rate following re-afforestation in the Loess Plateau of China 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Higher Education Press 2023 Abstract Afforestation effectively improved soil microbial communities and significantly increased soil nitrogen mineralization rate (Rm).Soil microorganisms drive Rm by regulating soil N-cycling genes.Soil nitrification genes had a major effect on soil Rm than denitrification genes after afforestation. Assessing the function of forest ecosystems requires an understanding of the mechanism of soil nitrogen mineralization. However, it remains unclear how soil N-cycling genes drive soil nitrogen mineralization during afforestation. In this study, we collected soil samples from a chrono-sequence of 14, 20, 30, and 45 years of Robinia pseudoacacia L. (RP14, RP20, RP30, and RP45) with a sloped farmland (FL) as a control. Through metagenomic sequencing analysis, we found significant changes in the diversity and composition of soil microbial communities involved in N-cycling along the afforestation time series, with afforestation effectively increasing the diversity (both alpha and beta diversity) of soil microbial communities. We conducted indoor culture experiments and analyzed correlations, which revealed a significant increase in both soil nitrification rate (Rn) and soil nitrogen mineralization rate (Rm) with increasing stand age. Furthermore, we found a strong correlation between soil Rm and soil microbial diversity (both alpha and beta diversity) and with the abundance of soil N-cycling genes. Partial least squares path modeling (PLS-PM) analysis showed that nitrification genes (narH, narY, nxrB, narG, narZ, nxrA, hao, pmoC-amoC) and denitrification genes (norB, nosZ, nirK) had a greater direct effect on soil Rm compared to their effect on soil microbial communities. Our results reveal the relationships between soil nitrogen mineralization rate and soil microbial communities and between the mineralization rate and functional genes involved in N-cycling, in the context of Robinia pseudoacacia L. restoration on the Loess Plateau. This study enriches the understanding of the effects of microorganisms on soil nitrogen mineralization rate during afforestation and provides a new theoretical basis for evaluating soil nitrogen mineralization mechanisms during forest succession. afforestation (dpeaa)DE-He213 soil N mineralization rate (dpeaa)DE-He213 denitrification genes (dpeaa)DE-He213 nitrification genes (dpeaa)DE-He213 the Loess Plateau (dpeaa)DE-He213 Zhao, Yuqing aut Zhang, Shuohong aut Xu, Yulin aut Han, Xinhui aut Yang, Gaihe aut Ren, Chengjie aut Enthalten in Soil ecology letters [Beijing] : Higher Education Press, 2019 6(2024), 1 vom: 18. Jan. (DE-627)1688167331 (DE-600)3006232-9 2662-2297 nnns volume:6 year:2024 number:1 day:18 month:01 https://dx.doi.org/10.1007/s42832-023-0188-0 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_65 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_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_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_2232 GBV_ILN_2336 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 6 2024 1 18 01 |
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10.1007/s42832-023-0188-0 doi (DE-627)SPR054513626 (SPR)s42832-023-0188-0-e DE-627 ger DE-627 rakwb eng Zhao, Yaping verfasserin aut N-cycle gene abundance determination of N mineralization rate following re-afforestation in the Loess Plateau of China 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Higher Education Press 2023 Abstract Afforestation effectively improved soil microbial communities and significantly increased soil nitrogen mineralization rate (Rm).Soil microorganisms drive Rm by regulating soil N-cycling genes.Soil nitrification genes had a major effect on soil Rm than denitrification genes after afforestation. Assessing the function of forest ecosystems requires an understanding of the mechanism of soil nitrogen mineralization. However, it remains unclear how soil N-cycling genes drive soil nitrogen mineralization during afforestation. In this study, we collected soil samples from a chrono-sequence of 14, 20, 30, and 45 years of Robinia pseudoacacia L. (RP14, RP20, RP30, and RP45) with a sloped farmland (FL) as a control. Through metagenomic sequencing analysis, we found significant changes in the diversity and composition of soil microbial communities involved in N-cycling along the afforestation time series, with afforestation effectively increasing the diversity (both alpha and beta diversity) of soil microbial communities. We conducted indoor culture experiments and analyzed correlations, which revealed a significant increase in both soil nitrification rate (Rn) and soil nitrogen mineralization rate (Rm) with increasing stand age. Furthermore, we found a strong correlation between soil Rm and soil microbial diversity (both alpha and beta diversity) and with the abundance of soil N-cycling genes. Partial least squares path modeling (PLS-PM) analysis showed that nitrification genes (narH, narY, nxrB, narG, narZ, nxrA, hao, pmoC-amoC) and denitrification genes (norB, nosZ, nirK) had a greater direct effect on soil Rm compared to their effect on soil microbial communities. Our results reveal the relationships between soil nitrogen mineralization rate and soil microbial communities and between the mineralization rate and functional genes involved in N-cycling, in the context of Robinia pseudoacacia L. restoration on the Loess Plateau. This study enriches the understanding of the effects of microorganisms on soil nitrogen mineralization rate during afforestation and provides a new theoretical basis for evaluating soil nitrogen mineralization mechanisms during forest succession. afforestation (dpeaa)DE-He213 soil N mineralization rate (dpeaa)DE-He213 denitrification genes (dpeaa)DE-He213 nitrification genes (dpeaa)DE-He213 the Loess Plateau (dpeaa)DE-He213 Zhao, Yuqing aut Zhang, Shuohong aut Xu, Yulin aut Han, Xinhui aut Yang, Gaihe aut Ren, Chengjie aut Enthalten in Soil ecology letters [Beijing] : Higher Education Press, 2019 6(2024), 1 vom: 18. Jan. (DE-627)1688167331 (DE-600)3006232-9 2662-2297 nnns volume:6 year:2024 number:1 day:18 month:01 https://dx.doi.org/10.1007/s42832-023-0188-0 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_65 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_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_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 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_2232 GBV_ILN_2336 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 6 2024 1 18 01 |
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Enthalten in Soil ecology letters 6(2024), 1 vom: 18. Jan. volume:6 year:2024 number:1 day:18 month:01 |
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Enthalten in Soil ecology letters 6(2024), 1 vom: 18. Jan. volume:6 year:2024 number:1 day:18 month:01 |
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Zhao, Yaping @@aut@@ Zhao, Yuqing @@aut@@ Zhang, Shuohong @@aut@@ Xu, Yulin @@aut@@ Han, Xinhui @@aut@@ Yang, Gaihe @@aut@@ Ren, Chengjie @@aut@@ |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">SPR054513626</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20240125064812.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">240125s2024 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s42832-023-0188-0</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR054513626</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s42832-023-0188-0-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhao, Yaping</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">N-cycle gene abundance determination of N mineralization rate following re-afforestation in the Loess Plateau of China</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2024</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Higher Education Press 2023</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Afforestation effectively improved soil microbial communities and significantly increased soil nitrogen mineralization rate (Rm).Soil microorganisms drive Rm by regulating soil N-cycling genes.Soil nitrification genes had a major effect on soil Rm than denitrification genes after afforestation. Assessing the function of forest ecosystems requires an understanding of the mechanism of soil nitrogen mineralization. However, it remains unclear how soil N-cycling genes drive soil nitrogen mineralization during afforestation. In this study, we collected soil samples from a chrono-sequence of 14, 20, 30, and 45 years of Robinia pseudoacacia L. (RP14, RP20, RP30, and RP45) with a sloped farmland (FL) as a control. Through metagenomic sequencing analysis, we found significant changes in the diversity and composition of soil microbial communities involved in N-cycling along the afforestation time series, with afforestation effectively increasing the diversity (both alpha and beta diversity) of soil microbial communities. We conducted indoor culture experiments and analyzed correlations, which revealed a significant increase in both soil nitrification rate (Rn) and soil nitrogen mineralization rate (Rm) with increasing stand age. Furthermore, we found a strong correlation between soil Rm and soil microbial diversity (both alpha and beta diversity) and with the abundance of soil N-cycling genes. Partial least squares path modeling (PLS-PM) analysis showed that nitrification genes (narH, narY, nxrB, narG, narZ, nxrA, hao, pmoC-amoC) and denitrification genes (norB, nosZ, nirK) had a greater direct effect on soil Rm compared to their effect on soil microbial communities. Our results reveal the relationships between soil nitrogen mineralization rate and soil microbial communities and between the mineralization rate and functional genes involved in N-cycling, in the context of Robinia pseudoacacia L. restoration on the Loess Plateau. 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|
| author |
Zhao, Yaping |
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Zhao, Yaping misc afforestation misc soil N mineralization rate misc denitrification genes misc nitrification genes misc the Loess Plateau N-cycle gene abundance determination of N mineralization rate following re-afforestation in the Loess Plateau of China |
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2662-2297 |
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N-cycle gene abundance determination of N mineralization rate following re-afforestation in the Loess Plateau of China afforestation (dpeaa)DE-He213 soil N mineralization rate (dpeaa)DE-He213 denitrification genes (dpeaa)DE-He213 nitrification genes (dpeaa)DE-He213 the Loess Plateau (dpeaa)DE-He213 |
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misc afforestation misc soil N mineralization rate misc denitrification genes misc nitrification genes misc the Loess Plateau |
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misc afforestation misc soil N mineralization rate misc denitrification genes misc nitrification genes misc the Loess Plateau |
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misc afforestation misc soil N mineralization rate misc denitrification genes misc nitrification genes misc the Loess Plateau |
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N-cycle gene abundance determination of N mineralization rate following re-afforestation in the Loess Plateau of China |
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N-cycle gene abundance determination of N mineralization rate following re-afforestation in the Loess Plateau of China |
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Zhao, Yaping |
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Soil ecology letters |
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Zhao, Yaping Zhao, Yuqing Zhang, Shuohong Xu, Yulin Han, Xinhui Yang, Gaihe Ren, Chengjie |
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Zhao, Yaping |
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n-cycle gene abundance determination of n mineralization rate following re-afforestation in the loess plateau of china |
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N-cycle gene abundance determination of N mineralization rate following re-afforestation in the Loess Plateau of China |
| abstract |
Abstract Afforestation effectively improved soil microbial communities and significantly increased soil nitrogen mineralization rate (Rm).Soil microorganisms drive Rm by regulating soil N-cycling genes.Soil nitrification genes had a major effect on soil Rm than denitrification genes after afforestation. Assessing the function of forest ecosystems requires an understanding of the mechanism of soil nitrogen mineralization. However, it remains unclear how soil N-cycling genes drive soil nitrogen mineralization during afforestation. In this study, we collected soil samples from a chrono-sequence of 14, 20, 30, and 45 years of Robinia pseudoacacia L. (RP14, RP20, RP30, and RP45) with a sloped farmland (FL) as a control. Through metagenomic sequencing analysis, we found significant changes in the diversity and composition of soil microbial communities involved in N-cycling along the afforestation time series, with afforestation effectively increasing the diversity (both alpha and beta diversity) of soil microbial communities. We conducted indoor culture experiments and analyzed correlations, which revealed a significant increase in both soil nitrification rate (Rn) and soil nitrogen mineralization rate (Rm) with increasing stand age. Furthermore, we found a strong correlation between soil Rm and soil microbial diversity (both alpha and beta diversity) and with the abundance of soil N-cycling genes. Partial least squares path modeling (PLS-PM) analysis showed that nitrification genes (narH, narY, nxrB, narG, narZ, nxrA, hao, pmoC-amoC) and denitrification genes (norB, nosZ, nirK) had a greater direct effect on soil Rm compared to their effect on soil microbial communities. Our results reveal the relationships between soil nitrogen mineralization rate and soil microbial communities and between the mineralization rate and functional genes involved in N-cycling, in the context of Robinia pseudoacacia L. restoration on the Loess Plateau. This study enriches the understanding of the effects of microorganisms on soil nitrogen mineralization rate during afforestation and provides a new theoretical basis for evaluating soil nitrogen mineralization mechanisms during forest succession. © Higher Education Press 2023 |
| abstractGer |
Abstract Afforestation effectively improved soil microbial communities and significantly increased soil nitrogen mineralization rate (Rm).Soil microorganisms drive Rm by regulating soil N-cycling genes.Soil nitrification genes had a major effect on soil Rm than denitrification genes after afforestation. Assessing the function of forest ecosystems requires an understanding of the mechanism of soil nitrogen mineralization. However, it remains unclear how soil N-cycling genes drive soil nitrogen mineralization during afforestation. In this study, we collected soil samples from a chrono-sequence of 14, 20, 30, and 45 years of Robinia pseudoacacia L. (RP14, RP20, RP30, and RP45) with a sloped farmland (FL) as a control. Through metagenomic sequencing analysis, we found significant changes in the diversity and composition of soil microbial communities involved in N-cycling along the afforestation time series, with afforestation effectively increasing the diversity (both alpha and beta diversity) of soil microbial communities. We conducted indoor culture experiments and analyzed correlations, which revealed a significant increase in both soil nitrification rate (Rn) and soil nitrogen mineralization rate (Rm) with increasing stand age. Furthermore, we found a strong correlation between soil Rm and soil microbial diversity (both alpha and beta diversity) and with the abundance of soil N-cycling genes. Partial least squares path modeling (PLS-PM) analysis showed that nitrification genes (narH, narY, nxrB, narG, narZ, nxrA, hao, pmoC-amoC) and denitrification genes (norB, nosZ, nirK) had a greater direct effect on soil Rm compared to their effect on soil microbial communities. Our results reveal the relationships between soil nitrogen mineralization rate and soil microbial communities and between the mineralization rate and functional genes involved in N-cycling, in the context of Robinia pseudoacacia L. restoration on the Loess Plateau. This study enriches the understanding of the effects of microorganisms on soil nitrogen mineralization rate during afforestation and provides a new theoretical basis for evaluating soil nitrogen mineralization mechanisms during forest succession. © Higher Education Press 2023 |
| abstract_unstemmed |
Abstract Afforestation effectively improved soil microbial communities and significantly increased soil nitrogen mineralization rate (Rm).Soil microorganisms drive Rm by regulating soil N-cycling genes.Soil nitrification genes had a major effect on soil Rm than denitrification genes after afforestation. Assessing the function of forest ecosystems requires an understanding of the mechanism of soil nitrogen mineralization. However, it remains unclear how soil N-cycling genes drive soil nitrogen mineralization during afforestation. In this study, we collected soil samples from a chrono-sequence of 14, 20, 30, and 45 years of Robinia pseudoacacia L. (RP14, RP20, RP30, and RP45) with a sloped farmland (FL) as a control. Through metagenomic sequencing analysis, we found significant changes in the diversity and composition of soil microbial communities involved in N-cycling along the afforestation time series, with afforestation effectively increasing the diversity (both alpha and beta diversity) of soil microbial communities. We conducted indoor culture experiments and analyzed correlations, which revealed a significant increase in both soil nitrification rate (Rn) and soil nitrogen mineralization rate (Rm) with increasing stand age. Furthermore, we found a strong correlation between soil Rm and soil microbial diversity (both alpha and beta diversity) and with the abundance of soil N-cycling genes. Partial least squares path modeling (PLS-PM) analysis showed that nitrification genes (narH, narY, nxrB, narG, narZ, nxrA, hao, pmoC-amoC) and denitrification genes (norB, nosZ, nirK) had a greater direct effect on soil Rm compared to their effect on soil microbial communities. Our results reveal the relationships between soil nitrogen mineralization rate and soil microbial communities and between the mineralization rate and functional genes involved in N-cycling, in the context of Robinia pseudoacacia L. restoration on the Loess Plateau. This study enriches the understanding of the effects of microorganisms on soil nitrogen mineralization rate during afforestation and provides a new theoretical basis for evaluating soil nitrogen mineralization mechanisms during forest succession. © Higher Education Press 2023 |
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| title_short |
N-cycle gene abundance determination of N mineralization rate following re-afforestation in the Loess Plateau of China |
| url |
https://dx.doi.org/10.1007/s42832-023-0188-0 |
| remote_bool |
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| author2 |
Zhao, Yuqing Zhang, Shuohong Xu, Yulin Han, Xinhui Yang, Gaihe Ren, Chengjie |
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Zhao, Yuqing Zhang, Shuohong Xu, Yulin Han, Xinhui Yang, Gaihe Ren, Chengjie |
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10.1007/s42832-023-0188-0 |
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2024-07-04T01:58:44.706Z |
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| score |
7.3997383 |