Long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils
Anaerobic oxidation of methane coupled to nitrate reduction (nitrate-coupled AOM) is performed by Candidatus Methanoperedens nitroreducens (M. nitroreducens)-related archaea, and is recently recognized as a crucial component of the global carbon cycle. The input of fertilizers is an essential agricu...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Yang, Yuling [verfasserIn] Shen, Lidong [verfasserIn] Zhao, Xu [verfasserIn] Agathokleous, Evgenios [verfasserIn] Wang, Shuwei [verfasserIn] Ren, Bingjie [verfasserIn] Yang, Wangting [verfasserIn] Liu, Jiaqi [verfasserIn] Jin, Jinghao [verfasserIn] Huang, Hechen [verfasserIn] Wu, Hongsheng [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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| Übergeordnetes Werk: |
Enthalten in: Soil biology & biochemistry - Amsterdam [u.a.] : Elsevier Science, 1969, 185 |
|---|---|
| Übergeordnetes Werk: |
volume:185 |
| DOI / URN: |
10.1016/j.soilbio.2023.109130 |
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| Katalog-ID: |
ELV063221640 |
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| 245 | 1 | 0 | |a Long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils |
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| 520 | |a Anaerobic oxidation of methane coupled to nitrate reduction (nitrate-coupled AOM) is performed by Candidatus Methanoperedens nitroreducens (M. nitroreducens)-related archaea, and is recently recognized as a crucial component of the global carbon cycle. The input of fertilizers is an essential agricultural practice that greatly impacts methane (CH4) production and emission. However, the significance of nitrate-coupled AOM in CH4 cycling and its response to fertilization in rice fields remain unclear. In this study, the potential nitrate-coupled AOM rates and the communities of M. nitroreducens-related archaea in rice fields were examined at different soil layers (0–10, 10–20, and 30–40 cm) at tillering, elongation, flowering, and ripening stages under three long-term fertilization treatments (CK-without fertilizer, CF-chemical fertilization, or CFS-chemical fertilization with straw incorporation). The results indicated that both CF (1.07 nmol 13CO2 g−1 d−1) and CFS (1.21 nmol 13CO2 g−1 d−1) treatments significantly promoted the potential nitrate-coupled AOM rates compared to CK (0.53 nmol 13CO2 g−1 d−1). A greater response of potential activity to fertilization was observed at plough layer (upper 20 cm) and during elongation stage. The abundance of M. nitroreducens-related archaea under CF (1.12 × 107 copies g−1) and CFS (1.62 × 107 copies g−1) treatments was significantly greater than that under CK (6.93 × 106 copies g−1). Conversely, the growth response of these archaeal to fertilization was stronger at deeper layer (30–40 cm). Moreover, no significant change was observed in the community composition of M. nitroreducens-related archaea among treatments. Correlation analysis suggested that the variations of soil organic carbon, NH4 +, and NO3 − contents caused by fertilization were key factors influencing the potential nitrate-coupled AOM rates and M. nitroreducens-related archaeal abundance. Our findings provide the first evidence for positive response of nitrate-coupled AOM to long-term fertilization, demonstrating its potential to act as an important process for mitigating CH4 emission in rice fields. | ||
| 650 | 4 | |a Long-term fertilization | |
| 650 | 4 | |a Nitrate-coupled AOM | |
| 650 | 4 | |a Different response | |
| 650 | 4 | |a Methane emission mitigation | |
| 650 | 4 | |a Paddy ecosystem | |
| 700 | 1 | |a Shen, Lidong |e verfasserin |4 aut | |
| 700 | 1 | |a Zhao, Xu |e verfasserin |4 aut | |
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| 700 | 1 | |a Wang, Shuwei |e verfasserin |4 aut | |
| 700 | 1 | |a Ren, Bingjie |e verfasserin |4 aut | |
| 700 | 1 | |a Yang, Wangting |e verfasserin |4 aut | |
| 700 | 1 | |a Liu, Jiaqi |e verfasserin |4 aut | |
| 700 | 1 | |a Jin, Jinghao |e verfasserin |4 aut | |
| 700 | 1 | |a Huang, Hechen |e verfasserin |4 aut | |
| 700 | 1 | |a Wu, Hongsheng |e verfasserin |4 aut | |
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10.1016/j.soilbio.2023.109130 doi (DE-627)ELV063221640 (ELSEVIER)S0038-0717(23)00192-X DE-627 ger DE-627 rda eng 570 540 VZ BIODIV DE-30 fid 38.60 bkl 48.32 bkl Yang, Yuling verfasserin aut Long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Anaerobic oxidation of methane coupled to nitrate reduction (nitrate-coupled AOM) is performed by Candidatus Methanoperedens nitroreducens (M. nitroreducens)-related archaea, and is recently recognized as a crucial component of the global carbon cycle. The input of fertilizers is an essential agricultural practice that greatly impacts methane (CH4) production and emission. However, the significance of nitrate-coupled AOM in CH4 cycling and its response to fertilization in rice fields remain unclear. In this study, the potential nitrate-coupled AOM rates and the communities of M. nitroreducens-related archaea in rice fields were examined at different soil layers (0–10, 10–20, and 30–40 cm) at tillering, elongation, flowering, and ripening stages under three long-term fertilization treatments (CK-without fertilizer, CF-chemical fertilization, or CFS-chemical fertilization with straw incorporation). The results indicated that both CF (1.07 nmol 13CO2 g−1 d−1) and CFS (1.21 nmol 13CO2 g−1 d−1) treatments significantly promoted the potential nitrate-coupled AOM rates compared to CK (0.53 nmol 13CO2 g−1 d−1). A greater response of potential activity to fertilization was observed at plough layer (upper 20 cm) and during elongation stage. The abundance of M. nitroreducens-related archaea under CF (1.12 × 107 copies g−1) and CFS (1.62 × 107 copies g−1) treatments was significantly greater than that under CK (6.93 × 106 copies g−1). Conversely, the growth response of these archaeal to fertilization was stronger at deeper layer (30–40 cm). Moreover, no significant change was observed in the community composition of M. nitroreducens-related archaea among treatments. Correlation analysis suggested that the variations of soil organic carbon, NH4 +, and NO3 − contents caused by fertilization were key factors influencing the potential nitrate-coupled AOM rates and M. nitroreducens-related archaeal abundance. Our findings provide the first evidence for positive response of nitrate-coupled AOM to long-term fertilization, demonstrating its potential to act as an important process for mitigating CH4 emission in rice fields. Long-term fertilization Nitrate-coupled AOM Different response Methane emission mitigation Paddy ecosystem Shen, Lidong verfasserin aut Zhao, Xu verfasserin aut Agathokleous, Evgenios verfasserin aut Wang, Shuwei verfasserin aut Ren, Bingjie verfasserin aut Yang, Wangting verfasserin aut Liu, Jiaqi verfasserin aut Jin, Jinghao verfasserin aut Huang, Hechen verfasserin aut Wu, Hongsheng verfasserin aut Enthalten in Soil biology & biochemistry Amsterdam [u.a.] : Elsevier Science, 1969 185 Online-Ressource (DE-627)306591596 (DE-600)1498740-5 (DE-576)100704522 nnns volume:185 GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-FOR GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 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_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.60 Bodenkunde: Allgemeines Geowissenschaften VZ 48.32 Bodenkunde Bodenbewertung Land- und Forstwirtschaft VZ AR 185 |
| spelling |
10.1016/j.soilbio.2023.109130 doi (DE-627)ELV063221640 (ELSEVIER)S0038-0717(23)00192-X DE-627 ger DE-627 rda eng 570 540 VZ BIODIV DE-30 fid 38.60 bkl 48.32 bkl Yang, Yuling verfasserin aut Long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Anaerobic oxidation of methane coupled to nitrate reduction (nitrate-coupled AOM) is performed by Candidatus Methanoperedens nitroreducens (M. nitroreducens)-related archaea, and is recently recognized as a crucial component of the global carbon cycle. The input of fertilizers is an essential agricultural practice that greatly impacts methane (CH4) production and emission. However, the significance of nitrate-coupled AOM in CH4 cycling and its response to fertilization in rice fields remain unclear. In this study, the potential nitrate-coupled AOM rates and the communities of M. nitroreducens-related archaea in rice fields were examined at different soil layers (0–10, 10–20, and 30–40 cm) at tillering, elongation, flowering, and ripening stages under three long-term fertilization treatments (CK-without fertilizer, CF-chemical fertilization, or CFS-chemical fertilization with straw incorporation). The results indicated that both CF (1.07 nmol 13CO2 g−1 d−1) and CFS (1.21 nmol 13CO2 g−1 d−1) treatments significantly promoted the potential nitrate-coupled AOM rates compared to CK (0.53 nmol 13CO2 g−1 d−1). A greater response of potential activity to fertilization was observed at plough layer (upper 20 cm) and during elongation stage. The abundance of M. nitroreducens-related archaea under CF (1.12 × 107 copies g−1) and CFS (1.62 × 107 copies g−1) treatments was significantly greater than that under CK (6.93 × 106 copies g−1). Conversely, the growth response of these archaeal to fertilization was stronger at deeper layer (30–40 cm). Moreover, no significant change was observed in the community composition of M. nitroreducens-related archaea among treatments. Correlation analysis suggested that the variations of soil organic carbon, NH4 +, and NO3 − contents caused by fertilization were key factors influencing the potential nitrate-coupled AOM rates and M. nitroreducens-related archaeal abundance. Our findings provide the first evidence for positive response of nitrate-coupled AOM to long-term fertilization, demonstrating its potential to act as an important process for mitigating CH4 emission in rice fields. Long-term fertilization Nitrate-coupled AOM Different response Methane emission mitigation Paddy ecosystem Shen, Lidong verfasserin aut Zhao, Xu verfasserin aut Agathokleous, Evgenios verfasserin aut Wang, Shuwei verfasserin aut Ren, Bingjie verfasserin aut Yang, Wangting verfasserin aut Liu, Jiaqi verfasserin aut Jin, Jinghao verfasserin aut Huang, Hechen verfasserin aut Wu, Hongsheng verfasserin aut Enthalten in Soil biology & biochemistry Amsterdam [u.a.] : Elsevier Science, 1969 185 Online-Ressource (DE-627)306591596 (DE-600)1498740-5 (DE-576)100704522 nnns volume:185 GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-FOR GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 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_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.60 Bodenkunde: Allgemeines Geowissenschaften VZ 48.32 Bodenkunde Bodenbewertung Land- und Forstwirtschaft VZ AR 185 |
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10.1016/j.soilbio.2023.109130 doi (DE-627)ELV063221640 (ELSEVIER)S0038-0717(23)00192-X DE-627 ger DE-627 rda eng 570 540 VZ BIODIV DE-30 fid 38.60 bkl 48.32 bkl Yang, Yuling verfasserin aut Long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Anaerobic oxidation of methane coupled to nitrate reduction (nitrate-coupled AOM) is performed by Candidatus Methanoperedens nitroreducens (M. nitroreducens)-related archaea, and is recently recognized as a crucial component of the global carbon cycle. The input of fertilizers is an essential agricultural practice that greatly impacts methane (CH4) production and emission. However, the significance of nitrate-coupled AOM in CH4 cycling and its response to fertilization in rice fields remain unclear. In this study, the potential nitrate-coupled AOM rates and the communities of M. nitroreducens-related archaea in rice fields were examined at different soil layers (0–10, 10–20, and 30–40 cm) at tillering, elongation, flowering, and ripening stages under three long-term fertilization treatments (CK-without fertilizer, CF-chemical fertilization, or CFS-chemical fertilization with straw incorporation). The results indicated that both CF (1.07 nmol 13CO2 g−1 d−1) and CFS (1.21 nmol 13CO2 g−1 d−1) treatments significantly promoted the potential nitrate-coupled AOM rates compared to CK (0.53 nmol 13CO2 g−1 d−1). A greater response of potential activity to fertilization was observed at plough layer (upper 20 cm) and during elongation stage. The abundance of M. nitroreducens-related archaea under CF (1.12 × 107 copies g−1) and CFS (1.62 × 107 copies g−1) treatments was significantly greater than that under CK (6.93 × 106 copies g−1). Conversely, the growth response of these archaeal to fertilization was stronger at deeper layer (30–40 cm). Moreover, no significant change was observed in the community composition of M. nitroreducens-related archaea among treatments. Correlation analysis suggested that the variations of soil organic carbon, NH4 +, and NO3 − contents caused by fertilization were key factors influencing the potential nitrate-coupled AOM rates and M. nitroreducens-related archaeal abundance. Our findings provide the first evidence for positive response of nitrate-coupled AOM to long-term fertilization, demonstrating its potential to act as an important process for mitigating CH4 emission in rice fields. Long-term fertilization Nitrate-coupled AOM Different response Methane emission mitigation Paddy ecosystem Shen, Lidong verfasserin aut Zhao, Xu verfasserin aut Agathokleous, Evgenios verfasserin aut Wang, Shuwei verfasserin aut Ren, Bingjie verfasserin aut Yang, Wangting verfasserin aut Liu, Jiaqi verfasserin aut Jin, Jinghao verfasserin aut Huang, Hechen verfasserin aut Wu, Hongsheng verfasserin aut Enthalten in Soil biology & biochemistry Amsterdam [u.a.] : Elsevier Science, 1969 185 Online-Ressource (DE-627)306591596 (DE-600)1498740-5 (DE-576)100704522 nnns volume:185 GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-FOR GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 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_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.60 Bodenkunde: Allgemeines Geowissenschaften VZ 48.32 Bodenkunde Bodenbewertung Land- und Forstwirtschaft VZ AR 185 |
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10.1016/j.soilbio.2023.109130 doi (DE-627)ELV063221640 (ELSEVIER)S0038-0717(23)00192-X DE-627 ger DE-627 rda eng 570 540 VZ BIODIV DE-30 fid 38.60 bkl 48.32 bkl Yang, Yuling verfasserin aut Long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Anaerobic oxidation of methane coupled to nitrate reduction (nitrate-coupled AOM) is performed by Candidatus Methanoperedens nitroreducens (M. nitroreducens)-related archaea, and is recently recognized as a crucial component of the global carbon cycle. The input of fertilizers is an essential agricultural practice that greatly impacts methane (CH4) production and emission. However, the significance of nitrate-coupled AOM in CH4 cycling and its response to fertilization in rice fields remain unclear. In this study, the potential nitrate-coupled AOM rates and the communities of M. nitroreducens-related archaea in rice fields were examined at different soil layers (0–10, 10–20, and 30–40 cm) at tillering, elongation, flowering, and ripening stages under three long-term fertilization treatments (CK-without fertilizer, CF-chemical fertilization, or CFS-chemical fertilization with straw incorporation). The results indicated that both CF (1.07 nmol 13CO2 g−1 d−1) and CFS (1.21 nmol 13CO2 g−1 d−1) treatments significantly promoted the potential nitrate-coupled AOM rates compared to CK (0.53 nmol 13CO2 g−1 d−1). A greater response of potential activity to fertilization was observed at plough layer (upper 20 cm) and during elongation stage. The abundance of M. nitroreducens-related archaea under CF (1.12 × 107 copies g−1) and CFS (1.62 × 107 copies g−1) treatments was significantly greater than that under CK (6.93 × 106 copies g−1). Conversely, the growth response of these archaeal to fertilization was stronger at deeper layer (30–40 cm). Moreover, no significant change was observed in the community composition of M. nitroreducens-related archaea among treatments. Correlation analysis suggested that the variations of soil organic carbon, NH4 +, and NO3 − contents caused by fertilization were key factors influencing the potential nitrate-coupled AOM rates and M. nitroreducens-related archaeal abundance. Our findings provide the first evidence for positive response of nitrate-coupled AOM to long-term fertilization, demonstrating its potential to act as an important process for mitigating CH4 emission in rice fields. Long-term fertilization Nitrate-coupled AOM Different response Methane emission mitigation Paddy ecosystem Shen, Lidong verfasserin aut Zhao, Xu verfasserin aut Agathokleous, Evgenios verfasserin aut Wang, Shuwei verfasserin aut Ren, Bingjie verfasserin aut Yang, Wangting verfasserin aut Liu, Jiaqi verfasserin aut Jin, Jinghao verfasserin aut Huang, Hechen verfasserin aut Wu, Hongsheng verfasserin aut Enthalten in Soil biology & biochemistry Amsterdam [u.a.] : Elsevier Science, 1969 185 Online-Ressource (DE-627)306591596 (DE-600)1498740-5 (DE-576)100704522 nnns volume:185 GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-FOR GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 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_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.60 Bodenkunde: Allgemeines Geowissenschaften VZ 48.32 Bodenkunde Bodenbewertung Land- und Forstwirtschaft VZ AR 185 |
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10.1016/j.soilbio.2023.109130 doi (DE-627)ELV063221640 (ELSEVIER)S0038-0717(23)00192-X DE-627 ger DE-627 rda eng 570 540 VZ BIODIV DE-30 fid 38.60 bkl 48.32 bkl Yang, Yuling verfasserin aut Long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils 2023 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Anaerobic oxidation of methane coupled to nitrate reduction (nitrate-coupled AOM) is performed by Candidatus Methanoperedens nitroreducens (M. nitroreducens)-related archaea, and is recently recognized as a crucial component of the global carbon cycle. The input of fertilizers is an essential agricultural practice that greatly impacts methane (CH4) production and emission. However, the significance of nitrate-coupled AOM in CH4 cycling and its response to fertilization in rice fields remain unclear. In this study, the potential nitrate-coupled AOM rates and the communities of M. nitroreducens-related archaea in rice fields were examined at different soil layers (0–10, 10–20, and 30–40 cm) at tillering, elongation, flowering, and ripening stages under three long-term fertilization treatments (CK-without fertilizer, CF-chemical fertilization, or CFS-chemical fertilization with straw incorporation). The results indicated that both CF (1.07 nmol 13CO2 g−1 d−1) and CFS (1.21 nmol 13CO2 g−1 d−1) treatments significantly promoted the potential nitrate-coupled AOM rates compared to CK (0.53 nmol 13CO2 g−1 d−1). A greater response of potential activity to fertilization was observed at plough layer (upper 20 cm) and during elongation stage. The abundance of M. nitroreducens-related archaea under CF (1.12 × 107 copies g−1) and CFS (1.62 × 107 copies g−1) treatments was significantly greater than that under CK (6.93 × 106 copies g−1). Conversely, the growth response of these archaeal to fertilization was stronger at deeper layer (30–40 cm). Moreover, no significant change was observed in the community composition of M. nitroreducens-related archaea among treatments. Correlation analysis suggested that the variations of soil organic carbon, NH4 +, and NO3 − contents caused by fertilization were key factors influencing the potential nitrate-coupled AOM rates and M. nitroreducens-related archaeal abundance. Our findings provide the first evidence for positive response of nitrate-coupled AOM to long-term fertilization, demonstrating its potential to act as an important process for mitigating CH4 emission in rice fields. Long-term fertilization Nitrate-coupled AOM Different response Methane emission mitigation Paddy ecosystem Shen, Lidong verfasserin aut Zhao, Xu verfasserin aut Agathokleous, Evgenios verfasserin aut Wang, Shuwei verfasserin aut Ren, Bingjie verfasserin aut Yang, Wangting verfasserin aut Liu, Jiaqi verfasserin aut Jin, Jinghao verfasserin aut Huang, Hechen verfasserin aut Wu, Hongsheng verfasserin aut Enthalten in Soil biology & biochemistry Amsterdam [u.a.] : Elsevier Science, 1969 185 Online-Ressource (DE-627)306591596 (DE-600)1498740-5 (DE-576)100704522 nnns volume:185 GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-BIODIV SSG-OLC-PHA SSG-OPC-GGO SSG-OPC-FOR GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_100 GBV_ILN_101 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 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_2034 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2106 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2470 GBV_ILN_2507 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 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_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 38.60 Bodenkunde: Allgemeines Geowissenschaften VZ 48.32 Bodenkunde Bodenbewertung Land- und Forstwirtschaft VZ AR 185 |
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Long-term fertilization Nitrate-coupled AOM Different response Methane emission mitigation Paddy ecosystem |
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Yang, Yuling @@aut@@ Shen, Lidong @@aut@@ Zhao, Xu @@aut@@ Agathokleous, Evgenios @@aut@@ Wang, Shuwei @@aut@@ Ren, Bingjie @@aut@@ Yang, Wangting @@aut@@ Liu, Jiaqi @@aut@@ Jin, Jinghao @@aut@@ Huang, Hechen @@aut@@ Wu, Hongsheng @@aut@@ |
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The input of fertilizers is an essential agricultural practice that greatly impacts methane (CH4) production and emission. However, the significance of nitrate-coupled AOM in CH4 cycling and its response to fertilization in rice fields remain unclear. In this study, the potential nitrate-coupled AOM rates and the communities of M. nitroreducens-related archaea in rice fields were examined at different soil layers (0–10, 10–20, and 30–40 cm) at tillering, elongation, flowering, and ripening stages under three long-term fertilization treatments (CK-without fertilizer, CF-chemical fertilization, or CFS-chemical fertilization with straw incorporation). The results indicated that both CF (1.07 nmol 13CO2 g−1 d−1) and CFS (1.21 nmol 13CO2 g−1 d−1) treatments significantly promoted the potential nitrate-coupled AOM rates compared to CK (0.53 nmol 13CO2 g−1 d−1). A greater response of potential activity to fertilization was observed at plough layer (upper 20 cm) and during elongation stage. The abundance of M. nitroreducens-related archaea under CF (1.12 × 107 copies g−1) and CFS (1.62 × 107 copies g−1) treatments was significantly greater than that under CK (6.93 × 106 copies g−1). Conversely, the growth response of these archaeal to fertilization was stronger at deeper layer (30–40 cm). Moreover, no significant change was observed in the community composition of M. nitroreducens-related archaea among treatments. Correlation analysis suggested that the variations of soil organic carbon, NH4 +, and NO3 − contents caused by fertilization were key factors influencing the potential nitrate-coupled AOM rates and M. nitroreducens-related archaeal abundance. 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Yang, Yuling |
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Yang, Yuling ddc 570 fid BIODIV bkl 38.60 bkl 48.32 misc Long-term fertilization misc Nitrate-coupled AOM misc Different response misc Methane emission mitigation misc Paddy ecosystem Long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils |
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570 540 VZ BIODIV DE-30 fid 38.60 bkl 48.32 bkl Long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils Long-term fertilization Nitrate-coupled AOM Different response Methane emission mitigation Paddy ecosystem |
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ddc 570 fid BIODIV bkl 38.60 bkl 48.32 misc Long-term fertilization misc Nitrate-coupled AOM misc Different response misc Methane emission mitigation misc Paddy ecosystem |
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Long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils |
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Long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils |
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Yang, Yuling Shen, Lidong Zhao, Xu Agathokleous, Evgenios Wang, Shuwei Ren, Bingjie Yang, Wangting Liu, Jiaqi Jin, Jinghao Huang, Hechen Wu, Hongsheng |
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10.1016/j.soilbio.2023.109130 |
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long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils |
| title_auth |
Long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils |
| abstract |
Anaerobic oxidation of methane coupled to nitrate reduction (nitrate-coupled AOM) is performed by Candidatus Methanoperedens nitroreducens (M. nitroreducens)-related archaea, and is recently recognized as a crucial component of the global carbon cycle. The input of fertilizers is an essential agricultural practice that greatly impacts methane (CH4) production and emission. However, the significance of nitrate-coupled AOM in CH4 cycling and its response to fertilization in rice fields remain unclear. In this study, the potential nitrate-coupled AOM rates and the communities of M. nitroreducens-related archaea in rice fields were examined at different soil layers (0–10, 10–20, and 30–40 cm) at tillering, elongation, flowering, and ripening stages under three long-term fertilization treatments (CK-without fertilizer, CF-chemical fertilization, or CFS-chemical fertilization with straw incorporation). The results indicated that both CF (1.07 nmol 13CO2 g−1 d−1) and CFS (1.21 nmol 13CO2 g−1 d−1) treatments significantly promoted the potential nitrate-coupled AOM rates compared to CK (0.53 nmol 13CO2 g−1 d−1). A greater response of potential activity to fertilization was observed at plough layer (upper 20 cm) and during elongation stage. The abundance of M. nitroreducens-related archaea under CF (1.12 × 107 copies g−1) and CFS (1.62 × 107 copies g−1) treatments was significantly greater than that under CK (6.93 × 106 copies g−1). Conversely, the growth response of these archaeal to fertilization was stronger at deeper layer (30–40 cm). Moreover, no significant change was observed in the community composition of M. nitroreducens-related archaea among treatments. Correlation analysis suggested that the variations of soil organic carbon, NH4 +, and NO3 − contents caused by fertilization were key factors influencing the potential nitrate-coupled AOM rates and M. nitroreducens-related archaeal abundance. Our findings provide the first evidence for positive response of nitrate-coupled AOM to long-term fertilization, demonstrating its potential to act as an important process for mitigating CH4 emission in rice fields. |
| abstractGer |
Anaerobic oxidation of methane coupled to nitrate reduction (nitrate-coupled AOM) is performed by Candidatus Methanoperedens nitroreducens (M. nitroreducens)-related archaea, and is recently recognized as a crucial component of the global carbon cycle. The input of fertilizers is an essential agricultural practice that greatly impacts methane (CH4) production and emission. However, the significance of nitrate-coupled AOM in CH4 cycling and its response to fertilization in rice fields remain unclear. In this study, the potential nitrate-coupled AOM rates and the communities of M. nitroreducens-related archaea in rice fields were examined at different soil layers (0–10, 10–20, and 30–40 cm) at tillering, elongation, flowering, and ripening stages under three long-term fertilization treatments (CK-without fertilizer, CF-chemical fertilization, or CFS-chemical fertilization with straw incorporation). The results indicated that both CF (1.07 nmol 13CO2 g−1 d−1) and CFS (1.21 nmol 13CO2 g−1 d−1) treatments significantly promoted the potential nitrate-coupled AOM rates compared to CK (0.53 nmol 13CO2 g−1 d−1). A greater response of potential activity to fertilization was observed at plough layer (upper 20 cm) and during elongation stage. The abundance of M. nitroreducens-related archaea under CF (1.12 × 107 copies g−1) and CFS (1.62 × 107 copies g−1) treatments was significantly greater than that under CK (6.93 × 106 copies g−1). Conversely, the growth response of these archaeal to fertilization was stronger at deeper layer (30–40 cm). Moreover, no significant change was observed in the community composition of M. nitroreducens-related archaea among treatments. Correlation analysis suggested that the variations of soil organic carbon, NH4 +, and NO3 − contents caused by fertilization were key factors influencing the potential nitrate-coupled AOM rates and M. nitroreducens-related archaeal abundance. Our findings provide the first evidence for positive response of nitrate-coupled AOM to long-term fertilization, demonstrating its potential to act as an important process for mitigating CH4 emission in rice fields. |
| abstract_unstemmed |
Anaerobic oxidation of methane coupled to nitrate reduction (nitrate-coupled AOM) is performed by Candidatus Methanoperedens nitroreducens (M. nitroreducens)-related archaea, and is recently recognized as a crucial component of the global carbon cycle. The input of fertilizers is an essential agricultural practice that greatly impacts methane (CH4) production and emission. However, the significance of nitrate-coupled AOM in CH4 cycling and its response to fertilization in rice fields remain unclear. In this study, the potential nitrate-coupled AOM rates and the communities of M. nitroreducens-related archaea in rice fields were examined at different soil layers (0–10, 10–20, and 30–40 cm) at tillering, elongation, flowering, and ripening stages under three long-term fertilization treatments (CK-without fertilizer, CF-chemical fertilization, or CFS-chemical fertilization with straw incorporation). The results indicated that both CF (1.07 nmol 13CO2 g−1 d−1) and CFS (1.21 nmol 13CO2 g−1 d−1) treatments significantly promoted the potential nitrate-coupled AOM rates compared to CK (0.53 nmol 13CO2 g−1 d−1). A greater response of potential activity to fertilization was observed at plough layer (upper 20 cm) and during elongation stage. The abundance of M. nitroreducens-related archaea under CF (1.12 × 107 copies g−1) and CFS (1.62 × 107 copies g−1) treatments was significantly greater than that under CK (6.93 × 106 copies g−1). Conversely, the growth response of these archaeal to fertilization was stronger at deeper layer (30–40 cm). Moreover, no significant change was observed in the community composition of M. nitroreducens-related archaea among treatments. Correlation analysis suggested that the variations of soil organic carbon, NH4 +, and NO3 − contents caused by fertilization were key factors influencing the potential nitrate-coupled AOM rates and M. nitroreducens-related archaeal abundance. Our findings provide the first evidence for positive response of nitrate-coupled AOM to long-term fertilization, demonstrating its potential to act as an important process for mitigating CH4 emission in rice fields. |
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| title_short |
Long-term fertilization enhances the activity of anaerobic oxidation of methane coupled to nitrate reduction and associated microbial abundance in paddy soils |
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Shen, Lidong Zhao, Xu Agathokleous, Evgenios Wang, Shuwei Ren, Bingjie Yang, Wangting Liu, Jiaqi Jin, Jinghao Huang, Hechen Wu, Hongsheng |
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Shen, Lidong Zhao, Xu Agathokleous, Evgenios Wang, Shuwei Ren, Bingjie Yang, Wangting Liu, Jiaqi Jin, Jinghao Huang, Hechen Wu, Hongsheng |
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| doi_str |
10.1016/j.soilbio.2023.109130 |
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2024-07-06T19:30:18.801Z |
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