Utilisation and transformation of organic and inorganic nitrogen by soil microorganisms and its regulation by excessive carbon and nitrogen availability
Abstract The process of nitrogen (N) transformation after microbial utilisation of organic and inorganic N is unclear. 15N-glycine (Gly), 15$ NH_{4} $+ and 15$ NO_{3} $− were used to investigate the uptake, release and reutilisation of N by microorganisms over 9 days. In addition, high amounts of un...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Pan, Wankun [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2023 |
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| Schlagwörter: |
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| Anmerkung: |
© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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| Übergeordnetes Werk: |
Enthalten in: Biology and fertility of soils - Springer Berlin Heidelberg, 1985, 59(2023), 4 vom: 09. März, Seite 379-389 |
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| Übergeordnetes Werk: |
volume:59 ; year:2023 ; number:4 ; day:09 ; month:03 ; pages:379-389 |
| Links: |
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| DOI / URN: |
10.1007/s00374-023-01712-w |
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OLC2134521465 |
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| 520 | |a Abstract The process of nitrogen (N) transformation after microbial utilisation of organic and inorganic N is unclear. 15N-glycine (Gly), 15$ NH_{4} $+ and 15$ NO_{3} $− were used to investigate the uptake, release and reutilisation of N by microorganisms over 9 days. In addition, high amounts of unlabelled carbon (C) or N were added to explore how C or N availability affects the cycling of inorganic and organic N by microorganisms. Within 15 min, 67% of the added 15N-Gly was taken up by soil microorganisms; within 1 h, 8% was released as $ NH_{4} $+. The released 15$ NH_{4} $+ was reutilised by the microorganisms within hours. Microorganisms took up 50% of the added 15$ NH_{4} $+ (15 min) and released 13% of the taken up $ NH_{4} $+ (1 h). Microorganisms prefer to take up Gly rather than $ NH_{4} $+ because they can directly acquire C from Gly for maintaining its growth and synthesising more complex compounds. $ NO_{3} $− was taken up by microorganisms within minutes but not released into the soil. $ NO_{3} $− was likely stored in the cytoplasm, to be used as an N source to face future N-deficient environments. When high concentrations of C or N were added, the assimilation of Gly and $ NH_{4} $+ increased, whereas N mineralisation and nitrification rates decreased, and the uptake of $ NO_{3} $− remained stable. Overall, Gly and $ NH_{4} $+ were taken up, released and re-taken up by microorganisms and were preferentially utilised under excess C or N sources, while $ NO_{3} $− was stored in the microbiome. These findings provide new insights into N uptake by microorganisms in short-term. | ||
| 650 | 4 | |a Organic nitrogen uptake | |
| 650 | 4 | |a Inorganic nitrogen uptake | |
| 650 | 4 | |a C and N bioavailability | |
| 650 | 4 | |a Isotopic labelling | |
| 700 | 1 | |a Zhou, Jingjie |4 aut | |
| 700 | 1 | |a Tang, Sheng |4 aut | |
| 700 | 1 | |a Wu, Lianghuan |4 aut | |
| 700 | 1 | |a Ma, Qingxu |0 (orcid)0000-0003-2050-7725 |4 aut | |
| 700 | 1 | |a Marsden, Karina A. |4 aut | |
| 700 | 1 | |a Chadwick, David R. |4 aut | |
| 700 | 1 | |a Jones, Davey L. |4 aut | |
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10.1007/s00374-023-01712-w doi (DE-627)OLC2134521465 (DE-He213)s00374-023-01712-w-p DE-627 ger DE-627 rakwb eng 570 630 640 VZ 12 ssgn BIODIV DE-30 fid Pan, Wankun verfasserin aut Utilisation and transformation of organic and inorganic nitrogen by soil microorganisms and its regulation by excessive carbon and nitrogen availability 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract The process of nitrogen (N) transformation after microbial utilisation of organic and inorganic N is unclear. 15N-glycine (Gly), 15$ NH_{4} $+ and 15$ NO_{3} $− were used to investigate the uptake, release and reutilisation of N by microorganisms over 9 days. In addition, high amounts of unlabelled carbon (C) or N were added to explore how C or N availability affects the cycling of inorganic and organic N by microorganisms. Within 15 min, 67% of the added 15N-Gly was taken up by soil microorganisms; within 1 h, 8% was released as $ NH_{4} $+. The released 15$ NH_{4} $+ was reutilised by the microorganisms within hours. Microorganisms took up 50% of the added 15$ NH_{4} $+ (15 min) and released 13% of the taken up $ NH_{4} $+ (1 h). Microorganisms prefer to take up Gly rather than $ NH_{4} $+ because they can directly acquire C from Gly for maintaining its growth and synthesising more complex compounds. $ NO_{3} $− was taken up by microorganisms within minutes but not released into the soil. $ NO_{3} $− was likely stored in the cytoplasm, to be used as an N source to face future N-deficient environments. When high concentrations of C or N were added, the assimilation of Gly and $ NH_{4} $+ increased, whereas N mineralisation and nitrification rates decreased, and the uptake of $ NO_{3} $− remained stable. Overall, Gly and $ NH_{4} $+ were taken up, released and re-taken up by microorganisms and were preferentially utilised under excess C or N sources, while $ NO_{3} $− was stored in the microbiome. These findings provide new insights into N uptake by microorganisms in short-term. Organic nitrogen uptake Inorganic nitrogen uptake C and N bioavailability Isotopic labelling Zhou, Jingjie aut Tang, Sheng aut Wu, Lianghuan aut Ma, Qingxu (orcid)0000-0003-2050-7725 aut Marsden, Karina A. aut Chadwick, David R. aut Jones, Davey L. aut Enthalten in Biology and fertility of soils Springer Berlin Heidelberg, 1985 59(2023), 4 vom: 09. März, Seite 379-389 (DE-627)130468681 (DE-600)742137-0 (DE-576)016061675 0178-2762 nnns volume:59 year:2023 number:4 day:09 month:03 pages:379-389 https://doi.org/10.1007/s00374-023-01712-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO SSG-OPC-FOR GBV_ILN_2018 GBV_ILN_4277 AR 59 2023 4 09 03 379-389 |
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10.1007/s00374-023-01712-w doi (DE-627)OLC2134521465 (DE-He213)s00374-023-01712-w-p DE-627 ger DE-627 rakwb eng 570 630 640 VZ 12 ssgn BIODIV DE-30 fid Pan, Wankun verfasserin aut Utilisation and transformation of organic and inorganic nitrogen by soil microorganisms and its regulation by excessive carbon and nitrogen availability 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract The process of nitrogen (N) transformation after microbial utilisation of organic and inorganic N is unclear. 15N-glycine (Gly), 15$ NH_{4} $+ and 15$ NO_{3} $− were used to investigate the uptake, release and reutilisation of N by microorganisms over 9 days. In addition, high amounts of unlabelled carbon (C) or N were added to explore how C or N availability affects the cycling of inorganic and organic N by microorganisms. Within 15 min, 67% of the added 15N-Gly was taken up by soil microorganisms; within 1 h, 8% was released as $ NH_{4} $+. The released 15$ NH_{4} $+ was reutilised by the microorganisms within hours. Microorganisms took up 50% of the added 15$ NH_{4} $+ (15 min) and released 13% of the taken up $ NH_{4} $+ (1 h). Microorganisms prefer to take up Gly rather than $ NH_{4} $+ because they can directly acquire C from Gly for maintaining its growth and synthesising more complex compounds. $ NO_{3} $− was taken up by microorganisms within minutes but not released into the soil. $ NO_{3} $− was likely stored in the cytoplasm, to be used as an N source to face future N-deficient environments. When high concentrations of C or N were added, the assimilation of Gly and $ NH_{4} $+ increased, whereas N mineralisation and nitrification rates decreased, and the uptake of $ NO_{3} $− remained stable. Overall, Gly and $ NH_{4} $+ were taken up, released and re-taken up by microorganisms and were preferentially utilised under excess C or N sources, while $ NO_{3} $− was stored in the microbiome. These findings provide new insights into N uptake by microorganisms in short-term. Organic nitrogen uptake Inorganic nitrogen uptake C and N bioavailability Isotopic labelling Zhou, Jingjie aut Tang, Sheng aut Wu, Lianghuan aut Ma, Qingxu (orcid)0000-0003-2050-7725 aut Marsden, Karina A. aut Chadwick, David R. aut Jones, Davey L. aut Enthalten in Biology and fertility of soils Springer Berlin Heidelberg, 1985 59(2023), 4 vom: 09. März, Seite 379-389 (DE-627)130468681 (DE-600)742137-0 (DE-576)016061675 0178-2762 nnns volume:59 year:2023 number:4 day:09 month:03 pages:379-389 https://doi.org/10.1007/s00374-023-01712-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO SSG-OPC-FOR GBV_ILN_2018 GBV_ILN_4277 AR 59 2023 4 09 03 379-389 |
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10.1007/s00374-023-01712-w doi (DE-627)OLC2134521465 (DE-He213)s00374-023-01712-w-p DE-627 ger DE-627 rakwb eng 570 630 640 VZ 12 ssgn BIODIV DE-30 fid Pan, Wankun verfasserin aut Utilisation and transformation of organic and inorganic nitrogen by soil microorganisms and its regulation by excessive carbon and nitrogen availability 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract The process of nitrogen (N) transformation after microbial utilisation of organic and inorganic N is unclear. 15N-glycine (Gly), 15$ NH_{4} $+ and 15$ NO_{3} $− were used to investigate the uptake, release and reutilisation of N by microorganisms over 9 days. In addition, high amounts of unlabelled carbon (C) or N were added to explore how C or N availability affects the cycling of inorganic and organic N by microorganisms. Within 15 min, 67% of the added 15N-Gly was taken up by soil microorganisms; within 1 h, 8% was released as $ NH_{4} $+. The released 15$ NH_{4} $+ was reutilised by the microorganisms within hours. Microorganisms took up 50% of the added 15$ NH_{4} $+ (15 min) and released 13% of the taken up $ NH_{4} $+ (1 h). Microorganisms prefer to take up Gly rather than $ NH_{4} $+ because they can directly acquire C from Gly for maintaining its growth and synthesising more complex compounds. $ NO_{3} $− was taken up by microorganisms within minutes but not released into the soil. $ NO_{3} $− was likely stored in the cytoplasm, to be used as an N source to face future N-deficient environments. When high concentrations of C or N were added, the assimilation of Gly and $ NH_{4} $+ increased, whereas N mineralisation and nitrification rates decreased, and the uptake of $ NO_{3} $− remained stable. Overall, Gly and $ NH_{4} $+ were taken up, released and re-taken up by microorganisms and were preferentially utilised under excess C or N sources, while $ NO_{3} $− was stored in the microbiome. These findings provide new insights into N uptake by microorganisms in short-term. Organic nitrogen uptake Inorganic nitrogen uptake C and N bioavailability Isotopic labelling Zhou, Jingjie aut Tang, Sheng aut Wu, Lianghuan aut Ma, Qingxu (orcid)0000-0003-2050-7725 aut Marsden, Karina A. aut Chadwick, David R. aut Jones, Davey L. aut Enthalten in Biology and fertility of soils Springer Berlin Heidelberg, 1985 59(2023), 4 vom: 09. März, Seite 379-389 (DE-627)130468681 (DE-600)742137-0 (DE-576)016061675 0178-2762 nnns volume:59 year:2023 number:4 day:09 month:03 pages:379-389 https://doi.org/10.1007/s00374-023-01712-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO SSG-OPC-FOR GBV_ILN_2018 GBV_ILN_4277 AR 59 2023 4 09 03 379-389 |
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10.1007/s00374-023-01712-w doi (DE-627)OLC2134521465 (DE-He213)s00374-023-01712-w-p DE-627 ger DE-627 rakwb eng 570 630 640 VZ 12 ssgn BIODIV DE-30 fid Pan, Wankun verfasserin aut Utilisation and transformation of organic and inorganic nitrogen by soil microorganisms and its regulation by excessive carbon and nitrogen availability 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract The process of nitrogen (N) transformation after microbial utilisation of organic and inorganic N is unclear. 15N-glycine (Gly), 15$ NH_{4} $+ and 15$ NO_{3} $− were used to investigate the uptake, release and reutilisation of N by microorganisms over 9 days. In addition, high amounts of unlabelled carbon (C) or N were added to explore how C or N availability affects the cycling of inorganic and organic N by microorganisms. Within 15 min, 67% of the added 15N-Gly was taken up by soil microorganisms; within 1 h, 8% was released as $ NH_{4} $+. The released 15$ NH_{4} $+ was reutilised by the microorganisms within hours. Microorganisms took up 50% of the added 15$ NH_{4} $+ (15 min) and released 13% of the taken up $ NH_{4} $+ (1 h). Microorganisms prefer to take up Gly rather than $ NH_{4} $+ because they can directly acquire C from Gly for maintaining its growth and synthesising more complex compounds. $ NO_{3} $− was taken up by microorganisms within minutes but not released into the soil. $ NO_{3} $− was likely stored in the cytoplasm, to be used as an N source to face future N-deficient environments. When high concentrations of C or N were added, the assimilation of Gly and $ NH_{4} $+ increased, whereas N mineralisation and nitrification rates decreased, and the uptake of $ NO_{3} $− remained stable. Overall, Gly and $ NH_{4} $+ were taken up, released and re-taken up by microorganisms and were preferentially utilised under excess C or N sources, while $ NO_{3} $− was stored in the microbiome. These findings provide new insights into N uptake by microorganisms in short-term. Organic nitrogen uptake Inorganic nitrogen uptake C and N bioavailability Isotopic labelling Zhou, Jingjie aut Tang, Sheng aut Wu, Lianghuan aut Ma, Qingxu (orcid)0000-0003-2050-7725 aut Marsden, Karina A. aut Chadwick, David R. aut Jones, Davey L. aut Enthalten in Biology and fertility of soils Springer Berlin Heidelberg, 1985 59(2023), 4 vom: 09. März, Seite 379-389 (DE-627)130468681 (DE-600)742137-0 (DE-576)016061675 0178-2762 nnns volume:59 year:2023 number:4 day:09 month:03 pages:379-389 https://doi.org/10.1007/s00374-023-01712-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO SSG-OPC-FOR GBV_ILN_2018 GBV_ILN_4277 AR 59 2023 4 09 03 379-389 |
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10.1007/s00374-023-01712-w doi (DE-627)OLC2134521465 (DE-He213)s00374-023-01712-w-p DE-627 ger DE-627 rakwb eng 570 630 640 VZ 12 ssgn BIODIV DE-30 fid Pan, Wankun verfasserin aut Utilisation and transformation of organic and inorganic nitrogen by soil microorganisms and its regulation by excessive carbon and nitrogen availability 2023 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. Abstract The process of nitrogen (N) transformation after microbial utilisation of organic and inorganic N is unclear. 15N-glycine (Gly), 15$ NH_{4} $+ and 15$ NO_{3} $− were used to investigate the uptake, release and reutilisation of N by microorganisms over 9 days. In addition, high amounts of unlabelled carbon (C) or N were added to explore how C or N availability affects the cycling of inorganic and organic N by microorganisms. Within 15 min, 67% of the added 15N-Gly was taken up by soil microorganisms; within 1 h, 8% was released as $ NH_{4} $+. The released 15$ NH_{4} $+ was reutilised by the microorganisms within hours. Microorganisms took up 50% of the added 15$ NH_{4} $+ (15 min) and released 13% of the taken up $ NH_{4} $+ (1 h). Microorganisms prefer to take up Gly rather than $ NH_{4} $+ because they can directly acquire C from Gly for maintaining its growth and synthesising more complex compounds. $ NO_{3} $− was taken up by microorganisms within minutes but not released into the soil. $ NO_{3} $− was likely stored in the cytoplasm, to be used as an N source to face future N-deficient environments. When high concentrations of C or N were added, the assimilation of Gly and $ NH_{4} $+ increased, whereas N mineralisation and nitrification rates decreased, and the uptake of $ NO_{3} $− remained stable. Overall, Gly and $ NH_{4} $+ were taken up, released and re-taken up by microorganisms and were preferentially utilised under excess C or N sources, while $ NO_{3} $− was stored in the microbiome. These findings provide new insights into N uptake by microorganisms in short-term. Organic nitrogen uptake Inorganic nitrogen uptake C and N bioavailability Isotopic labelling Zhou, Jingjie aut Tang, Sheng aut Wu, Lianghuan aut Ma, Qingxu (orcid)0000-0003-2050-7725 aut Marsden, Karina A. aut Chadwick, David R. aut Jones, Davey L. aut Enthalten in Biology and fertility of soils Springer Berlin Heidelberg, 1985 59(2023), 4 vom: 09. März, Seite 379-389 (DE-627)130468681 (DE-600)742137-0 (DE-576)016061675 0178-2762 nnns volume:59 year:2023 number:4 day:09 month:03 pages:379-389 https://doi.org/10.1007/s00374-023-01712-w lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC FID-BIODIV SSG-OLC-GEO SSG-OLC-FOR SSG-OPC-GGO SSG-OPC-FOR GBV_ILN_2018 GBV_ILN_4277 AR 59 2023 4 09 03 379-389 |
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Utilisation and transformation of organic and inorganic nitrogen by soil microorganisms and its regulation by excessive carbon and nitrogen availability |
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Abstract The process of nitrogen (N) transformation after microbial utilisation of organic and inorganic N is unclear. 15N-glycine (Gly), 15$ NH_{4} $+ and 15$ NO_{3} $− were used to investigate the uptake, release and reutilisation of N by microorganisms over 9 days. In addition, high amounts of unlabelled carbon (C) or N were added to explore how C or N availability affects the cycling of inorganic and organic N by microorganisms. Within 15 min, 67% of the added 15N-Gly was taken up by soil microorganisms; within 1 h, 8% was released as $ NH_{4} $+. The released 15$ NH_{4} $+ was reutilised by the microorganisms within hours. Microorganisms took up 50% of the added 15$ NH_{4} $+ (15 min) and released 13% of the taken up $ NH_{4} $+ (1 h). Microorganisms prefer to take up Gly rather than $ NH_{4} $+ because they can directly acquire C from Gly for maintaining its growth and synthesising more complex compounds. $ NO_{3} $− was taken up by microorganisms within minutes but not released into the soil. $ NO_{3} $− was likely stored in the cytoplasm, to be used as an N source to face future N-deficient environments. When high concentrations of C or N were added, the assimilation of Gly and $ NH_{4} $+ increased, whereas N mineralisation and nitrification rates decreased, and the uptake of $ NO_{3} $− remained stable. Overall, Gly and $ NH_{4} $+ were taken up, released and re-taken up by microorganisms and were preferentially utilised under excess C or N sources, while $ NO_{3} $− was stored in the microbiome. These findings provide new insights into N uptake by microorganisms in short-term. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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Abstract The process of nitrogen (N) transformation after microbial utilisation of organic and inorganic N is unclear. 15N-glycine (Gly), 15$ NH_{4} $+ and 15$ NO_{3} $− were used to investigate the uptake, release and reutilisation of N by microorganisms over 9 days. In addition, high amounts of unlabelled carbon (C) or N were added to explore how C or N availability affects the cycling of inorganic and organic N by microorganisms. Within 15 min, 67% of the added 15N-Gly was taken up by soil microorganisms; within 1 h, 8% was released as $ NH_{4} $+. The released 15$ NH_{4} $+ was reutilised by the microorganisms within hours. Microorganisms took up 50% of the added 15$ NH_{4} $+ (15 min) and released 13% of the taken up $ NH_{4} $+ (1 h). Microorganisms prefer to take up Gly rather than $ NH_{4} $+ because they can directly acquire C from Gly for maintaining its growth and synthesising more complex compounds. $ NO_{3} $− was taken up by microorganisms within minutes but not released into the soil. $ NO_{3} $− was likely stored in the cytoplasm, to be used as an N source to face future N-deficient environments. When high concentrations of C or N were added, the assimilation of Gly and $ NH_{4} $+ increased, whereas N mineralisation and nitrification rates decreased, and the uptake of $ NO_{3} $− remained stable. Overall, Gly and $ NH_{4} $+ were taken up, released and re-taken up by microorganisms and were preferentially utilised under excess C or N sources, while $ NO_{3} $− was stored in the microbiome. These findings provide new insights into N uptake by microorganisms in short-term. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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Abstract The process of nitrogen (N) transformation after microbial utilisation of organic and inorganic N is unclear. 15N-glycine (Gly), 15$ NH_{4} $+ and 15$ NO_{3} $− were used to investigate the uptake, release and reutilisation of N by microorganisms over 9 days. In addition, high amounts of unlabelled carbon (C) or N were added to explore how C or N availability affects the cycling of inorganic and organic N by microorganisms. Within 15 min, 67% of the added 15N-Gly was taken up by soil microorganisms; within 1 h, 8% was released as $ NH_{4} $+. The released 15$ NH_{4} $+ was reutilised by the microorganisms within hours. Microorganisms took up 50% of the added 15$ NH_{4} $+ (15 min) and released 13% of the taken up $ NH_{4} $+ (1 h). Microorganisms prefer to take up Gly rather than $ NH_{4} $+ because they can directly acquire C from Gly for maintaining its growth and synthesising more complex compounds. $ NO_{3} $− was taken up by microorganisms within minutes but not released into the soil. $ NO_{3} $− was likely stored in the cytoplasm, to be used as an N source to face future N-deficient environments. When high concentrations of C or N were added, the assimilation of Gly and $ NH_{4} $+ increased, whereas N mineralisation and nitrification rates decreased, and the uptake of $ NO_{3} $− remained stable. Overall, Gly and $ NH_{4} $+ were taken up, released and re-taken up by microorganisms and were preferentially utilised under excess C or N sources, while $ NO_{3} $− was stored in the microbiome. These findings provide new insights into N uptake by microorganisms in short-term. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law. |
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The released 15$ NH_{4} $+ was reutilised by the microorganisms within hours. Microorganisms took up 50% of the added 15$ NH_{4} $+ (15 min) and released 13% of the taken up $ NH_{4} $+ (1 h). Microorganisms prefer to take up Gly rather than $ NH_{4} $+ because they can directly acquire C from Gly for maintaining its growth and synthesising more complex compounds. $ NO_{3} $− was taken up by microorganisms within minutes but not released into the soil. $ NO_{3} $− was likely stored in the cytoplasm, to be used as an N source to face future N-deficient environments. When high concentrations of C or N were added, the assimilation of Gly and $ NH_{4} $+ increased, whereas N mineralisation and nitrification rates decreased, and the uptake of $ NO_{3} $− remained stable. Overall, Gly and $ NH_{4} $+ were taken up, released and re-taken up by microorganisms and were preferentially utilised under excess C or N sources, while $ NO_{3} $− was stored in the microbiome. 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März, Seite 379-389</subfield><subfield code="w">(DE-627)130468681</subfield><subfield code="w">(DE-600)742137-0</subfield><subfield code="w">(DE-576)016061675</subfield><subfield code="x">0178-2762</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:59</subfield><subfield code="g">year:2023</subfield><subfield code="g">number:4</subfield><subfield code="g">day:09</subfield><subfield code="g">month:03</subfield><subfield code="g">pages:379-389</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s00374-023-01712-w</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">FID-BIODIV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-FOR</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-FOR</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2018</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4277</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">59</subfield><subfield code="j">2023</subfield><subfield code="e">4</subfield><subfield code="b">09</subfield><subfield code="c">03</subfield><subfield code="h">379-389</subfield></datafield></record></collection>
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