Carbon limitation overrides acidification in mediating soil microbial activity to nitrogen enrichment in a temperate grassland
Higher ecosystem nitrogen (N) inputs resulting from human activities often suppress soil microbial biomass and respiration, thereby altering biogeochemical cycling. Soil acidification and carbon (C) limitation may drive these microbial responses, yet their relative importance remains elusive, which...
Saved in:
| Published in | Global change biology Vol. 27; no. 22; pp. 5976 - 5988 |
|---|---|
| Main Authors | , , , , , , , , , , , , , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Oxford
Blackwell Publishing Ltd
01.11.2021
Wiley |
| Subjects | |
| Online Access | Get full text |
Cover
Loading…
| Abstract | Higher ecosystem nitrogen (N) inputs resulting from human activities often suppress soil microbial biomass and respiration, thereby altering biogeochemical cycling. Soil acidification and carbon (C) limitation may drive these microbial responses, yet their relative importance remains elusive, which limits our understanding of the longer term effects of increasing N inputs. In a field experiment with continuous N addition at seven different rates from 0 to 50 g N m−2 year−1 over 6 years in a temperate grassland of Inner Mongolia, China, we examined the responses of soil microbial biomass and respiration to changes in soil acidity and C availability by adding lime and/or glucose to soil samples. Soil microbial biomass and respiration did only weakly respond to increasing soil pH, but increased strongly in response to higher C availability with increasing N addition rates. Soil net N immobilization increased in response to glucose addition, and soil microbial biomass increased at higher rates than microbial respiration along the gradient of previous N addition rates, both suggesting increasingly reinforced microbial C limitation with increasing N addition. Our results provide clear evidence for strong N‐induced microbial C limitation, but only little support for soil acidity effects within the initial pH range of 4.73–7.86 covered by our study. Field data support this conclusion by showing reduced plant C allocation belowground in response to N addition, resulting in soil microbial C starvation over the long term. In conclusion, soil microbial biomass and respiration under N addition were strongly dependent on C availability, most likely originating from plant belowground C inputs, and was much less affected by changes in soil pH. Our data help clarify a long‐standing debate about how increasing N input rates affect soil microbial biomass and respiration, and improve the mechanistic understanding of the linkages between ecosystem N enrichment and C cycling.
Soil acidification and carbon (C) limitation induced by nitrogen (N) enrichment may suppress microbial activity, yet their relative importance remains elusive. Our experiments in the field and laboratory clearly showed that soil microbial C limitation increased with N addition rates, and played the overriding role in modulating soil microbial activity, while soil acidification was of only limited importance. Microbial C limitation is driven by plant, which allocate less C to belowground with increasing N addition. Our study clarifies a long‐standing debate about the mechanisms of N‐induced suppression of soil microbial activity, allowing better predictions of the ecosystem consequences of N deposition. |
|---|---|
| AbstractList | Higher ecosystem nitrogen (N) inputs resulting from human activities often suppress soil microbial biomass and respiration, thereby altering biogeochemical cycling. Soil acidification and carbon (C) limitation may drive these microbial responses, yet their relative importance remains elusive, which limits our understanding of the longer term effects of increasing N inputs. In a field experiment with continuous N addition at seven different rates from 0 to 50 g N m(-2) year(-1) over 6 years in a temperate grassland of Inner Mongolia, China, we examined the responses of soil microbial biomass and respiration to changes in soil acidity and C availability by adding lime and/or glucose to soil samples. Soil microbial biomass and respiration did only weakly respond to increasing soil pH, but increased strongly in response to higher C availability with increasing N addition rates. Soil net N immobilization increased in response to glucose addition, and soil microbial biomass increased at higher rates than microbial respiration along the gradient of previous N addition rates, both suggesting increasingly reinforced microbial C limitation with increasing N addition. Our results provide clear evidence for strong N-induced microbial C limitation, but only little support for soil acidity effects within the initial pH range of 4.73-7.86 covered by our study. Field data support this conclusion by showing reduced plant C allocation belowground in response to N addition, resulting in soil microbial C starvation over the long term. In conclusion, soil microbial biomass and respiration under N addition were strongly dependent on C availability, most likely originating from plant belowground C inputs, and was much less affected by changes in soil pH. Our data help clarify a long-standing debate about how increasing N input rates affect soil microbial biomass and respiration, and improve the mechanistic understanding of the linkages between ecosystem N enrichment and C cycling. Higher ecosystem nitrogen (N) inputs resulting from human activities often suppress soil microbial biomass and respiration, thereby altering biogeochemical cycling. Soil acidification and carbon (C) limitation may drive these microbial responses, yet their relative importance remains elusive, which limits our understanding of the longer term effects of increasing N inputs. In a field experiment with continuous N addition at seven different rates from 0 to 50 g N m-2 year-1 over 6 years in a temperate grassland of Inner Mongolia, China, we examined the responses of soil microbial biomass and respiration to changes in soil acidity and C availability by adding lime and/or glucose to soil samples. Soil microbial biomass and respiration did only weakly respond to increasing soil pH, but increased strongly in response to higher C availability with increasing N addition rates. Soil net N immobilization increased in response to glucose addition, and soil microbial biomass increased at higher rates than microbial respiration along the gradient of previous N addition rates, both suggesting increasingly reinforced microbial C limitation with increasing N addition. Our results provide clear evidence for strong N-induced microbial C limitation, but only little support for soil acidity effects within the initial pH range of 4.73-7.86 covered by our study. Field data support this conclusion by showing reduced plant C allocation belowground in response to N addition, resulting in soil microbial C starvation over the long term. In conclusion, soil microbial biomass and respiration under N addition were strongly dependent on C availability, most likely originating from plant belowground C inputs, and was much less affected by changes in soil pH. Our data help clarify a long-standing debate about how increasing N input rates affect soil microbial biomass and respiration, and improve the mechanistic understanding of the linkages between ecosystem N enrichment and C cycling.Higher ecosystem nitrogen (N) inputs resulting from human activities often suppress soil microbial biomass and respiration, thereby altering biogeochemical cycling. Soil acidification and carbon (C) limitation may drive these microbial responses, yet their relative importance remains elusive, which limits our understanding of the longer term effects of increasing N inputs. In a field experiment with continuous N addition at seven different rates from 0 to 50 g N m-2 year-1 over 6 years in a temperate grassland of Inner Mongolia, China, we examined the responses of soil microbial biomass and respiration to changes in soil acidity and C availability by adding lime and/or glucose to soil samples. Soil microbial biomass and respiration did only weakly respond to increasing soil pH, but increased strongly in response to higher C availability with increasing N addition rates. Soil net N immobilization increased in response to glucose addition, and soil microbial biomass increased at higher rates than microbial respiration along the gradient of previous N addition rates, both suggesting increasingly reinforced microbial C limitation with increasing N addition. Our results provide clear evidence for strong N-induced microbial C limitation, but only little support for soil acidity effects within the initial pH range of 4.73-7.86 covered by our study. Field data support this conclusion by showing reduced plant C allocation belowground in response to N addition, resulting in soil microbial C starvation over the long term. In conclusion, soil microbial biomass and respiration under N addition were strongly dependent on C availability, most likely originating from plant belowground C inputs, and was much less affected by changes in soil pH. Our data help clarify a long-standing debate about how increasing N input rates affect soil microbial biomass and respiration, and improve the mechanistic understanding of the linkages between ecosystem N enrichment and C cycling. Higher ecosystem nitrogen (N) inputs resulting from human activities often suppress soil microbial biomass and respiration, thereby altering biogeochemical cycling. Soil acidification and carbon (C) limitation may drive these microbial responses, yet their relative importance remains elusive, which limits our understanding of the longer term effects of increasing N inputs. In a field experiment with continuous N addition at seven different rates from 0 to 50 g N m−2 year−1 over 6 years in a temperate grassland of Inner Mongolia, China, we examined the responses of soil microbial biomass and respiration to changes in soil acidity and C availability by adding lime and/or glucose to soil samples. Soil microbial biomass and respiration did only weakly respond to increasing soil pH, but increased strongly in response to higher C availability with increasing N addition rates. Soil net N immobilization increased in response to glucose addition, and soil microbial biomass increased at higher rates than microbial respiration along the gradient of previous N addition rates, both suggesting increasingly reinforced microbial C limitation with increasing N addition. Our results provide clear evidence for strong N‐induced microbial C limitation, but only little support for soil acidity effects within the initial pH range of 4.73–7.86 covered by our study. Field data support this conclusion by showing reduced plant C allocation belowground in response to N addition, resulting in soil microbial C starvation over the long term. In conclusion, soil microbial biomass and respiration under N addition were strongly dependent on C availability, most likely originating from plant belowground C inputs, and was much less affected by changes in soil pH. Our data help clarify a long‐standing debate about how increasing N input rates affect soil microbial biomass and respiration, and improve the mechanistic understanding of the linkages between ecosystem N enrichment and C cycling. Soil acidification and carbon (C) limitation induced by nitrogen (N) enrichment may suppress microbial activity, yet their relative importance remains elusive. Our experiments in the field and laboratory clearly showed that soil microbial C limitation increased with N addition rates, and played the overriding role in modulating soil microbial activity, while soil acidification was of only limited importance. Microbial C limitation is driven by plant, which allocate less C to belowground with increasing N addition. Our study clarifies a long‐standing debate about the mechanisms of N‐induced suppression of soil microbial activity, allowing better predictions of the ecosystem consequences of N deposition. Higher ecosystem nitrogen (N) inputs resulting from human activities often suppress soil microbial biomass and respiration, thereby altering biogeochemical cycling. Soil acidification and carbon (C) limitation may drive these microbial responses, yet their relative importance remains elusive, which limits our understanding of the longer term effects of increasing N inputs. In a field experiment with continuous N addition at seven different rates from 0 to 50 g N m−2 year−1 over 6 years in a temperate grassland of Inner Mongolia, China, we examined the responses of soil microbial biomass and respiration to changes in soil acidity and C availability by adding lime and/or glucose to soil samples. Soil microbial biomass and respiration did only weakly respond to increasing soil pH, but increased strongly in response to higher C availability with increasing N addition rates. Soil net N immobilization increased in response to glucose addition, and soil microbial biomass increased at higher rates than microbial respiration along the gradient of previous N addition rates, both suggesting increasingly reinforced microbial C limitation with increasing N addition. Our results provide clear evidence for strong N‐induced microbial C limitation, but only little support for soil acidity effects within the initial pH range of 4.73–7.86 covered by our study. Field data support this conclusion by showing reduced plant C allocation belowground in response to N addition, resulting in soil microbial C starvation over the long term. In conclusion, soil microbial biomass and respiration under N addition were strongly dependent on C availability, most likely originating from plant belowground C inputs, and was much less affected by changes in soil pH. Our data help clarify a long‐standing debate about how increasing N input rates affect soil microbial biomass and respiration, and improve the mechanistic understanding of the linkages between ecosystem N enrichment and C cycling. Higher ecosystem nitrogen (N) inputs resulting from human activities often suppress soil microbial biomass and respiration, thereby altering biogeochemical cycling. Soil acidification and carbon (C) limitation may drive these microbial responses, yet their relative importance remains elusive, which limits our understanding of the longer term effects of increasing N inputs. In a field experiment with continuous N addition at seven different rates from 0 to 50 g N m −2 year −1 over 6 years in a temperate grassland of Inner Mongolia, China, we examined the responses of soil microbial biomass and respiration to changes in soil acidity and C availability by adding lime and/or glucose to soil samples. Soil microbial biomass and respiration did only weakly respond to increasing soil pH, but increased strongly in response to higher C availability with increasing N addition rates. Soil net N immobilization increased in response to glucose addition, and soil microbial biomass increased at higher rates than microbial respiration along the gradient of previous N addition rates, both suggesting increasingly reinforced microbial C limitation with increasing N addition. Our results provide clear evidence for strong N-induced microbial C limitation, but only little support for soil acidity effects within the initial pH range of 4.73–7.86 covered by our study. Field data support this conclusion by showing reduced plant C allocation belowground in response to N addition, resulting in soil microbial C starvation over the long term. In conclusion, soil microbial biomass and respiration under N addition were strongly dependent on C availability, most likely originating from plant belowground C inputs, and was much less affected by changes in soil pH. Our data help clarify a long-standing debate about how increasing N input rates affect soil microbial biomass and respiration, and improve the mechanistic understanding of the linkages between ecosystem N enrichment and C cycling. Higher ecosystem nitrogen (N) inputs resulting from human activities often suppress soil microbial biomass and respiration, thereby altering biogeochemical cycling. Soil acidification and carbon (C) limitation may drive these microbial responses, yet their relative importance remains elusive, which limits our understanding of the longer term effects of increasing N inputs. In a field experiment with continuous N addition at seven different rates from 0 to 50 g N m −2 year −1 over 6 years in a temperate grassland of Inner Mongolia, China, we examined the responses of soil microbial biomass and respiration to changes in soil acidity and C availability by adding lime and/or glucose to soil samples. Soil microbial biomass and respiration did only weakly respond to increasing soil pH, but increased strongly in response to higher C availability with increasing N addition rates. Soil net N immobilization increased in response to glucose addition, and soil microbial biomass increased at higher rates than microbial respiration along the gradient of previous N addition rates, both suggesting increasingly reinforced microbial C limitation with increasing N addition. Our results provide clear evidence for strong N‐induced microbial C limitation, but only little support for soil acidity effects within the initial pH range of 4.73–7.86 covered by our study. Field data support this conclusion by showing reduced plant C allocation belowground in response to N addition, resulting in soil microbial C starvation over the long term. In conclusion, soil microbial biomass and respiration under N addition were strongly dependent on C availability, most likely originating from plant belowground C inputs, and was much less affected by changes in soil pH. Our data help clarify a long‐standing debate about how increasing N input rates affect soil microbial biomass and respiration, and improve the mechanistic understanding of the linkages between ecosystem N enrichment and C cycling. Higher ecosystem nitrogen (N) inputs resulting from human activities often suppress soil microbial biomass and respiration, thereby altering biogeochemical cycling. Soil acidification and carbon (C) limitation may drive these microbial responses, yet their relative importance remains elusive, which limits our understanding of the longer term effects of increasing N inputs. In a field experiment with continuous N addition at seven different rates from 0 to 50 g N m⁻² year⁻¹ over 6 years in a temperate grassland of Inner Mongolia, China, we examined the responses of soil microbial biomass and respiration to changes in soil acidity and C availability by adding lime and/or glucose to soil samples. Soil microbial biomass and respiration did only weakly respond to increasing soil pH, but increased strongly in response to higher C availability with increasing N addition rates. Soil net N immobilization increased in response to glucose addition, and soil microbial biomass increased at higher rates than microbial respiration along the gradient of previous N addition rates, both suggesting increasingly reinforced microbial C limitation with increasing N addition. Our results provide clear evidence for strong N‐induced microbial C limitation, but only little support for soil acidity effects within the initial pH range of 4.73–7.86 covered by our study. Field data support this conclusion by showing reduced plant C allocation belowground in response to N addition, resulting in soil microbial C starvation over the long term. In conclusion, soil microbial biomass and respiration under N addition were strongly dependent on C availability, most likely originating from plant belowground C inputs, and was much less affected by changes in soil pH. Our data help clarify a long‐standing debate about how increasing N input rates affect soil microbial biomass and respiration, and improve the mechanistic understanding of the linkages between ecosystem N enrichment and C cycling. |
| Author | Kardol, Paul Zhang, Yunhai Ning, Qiushi Peñuelas, Josep Lü, Xiaotao Gao, Yingzhi Li, Ang Han, Xingguo Wang, Jing Sardans, Jordi Hättenschwiler, Stephan Xu, Zhihong He, Jizheng Xu, Chengyuan Peng, Yang Wei, Cunzheng Huang, Jianhui Yang, Junjie |
| Author_xml | – sequence: 1 givenname: Qiushi orcidid: 0000-0002-6743-5653 surname: Ning fullname: Ning, Qiushi organization: Griffith University – sequence: 2 givenname: Stephan orcidid: 0000-0001-8148-960X surname: Hättenschwiler fullname: Hättenschwiler, Stephan organization: Univ Montpellier, CNRS, EPHE – sequence: 3 givenname: Xiaotao orcidid: 0000-0001-5571-1895 surname: Lü fullname: Lü, Xiaotao organization: Chinese Academy of Sciences – sequence: 4 givenname: Paul orcidid: 0000-0001-7065-3435 surname: Kardol fullname: Kardol, Paul organization: Swedish University of Agricultural Sciences – sequence: 5 givenname: Yunhai orcidid: 0000-0003-0613-3624 surname: Zhang fullname: Zhang, Yunhai organization: Chinese Academy of Sciences – sequence: 6 givenname: Cunzheng orcidid: 0000-0001-9309-2722 surname: Wei fullname: Wei, Cunzheng organization: Chinese Academy of Sciences – sequence: 7 givenname: Chengyuan surname: Xu fullname: Xu, Chengyuan organization: Central Queensland University – sequence: 8 givenname: Jianhui surname: Huang fullname: Huang, Jianhui organization: Chinese Academy of Sciences – sequence: 9 givenname: Ang surname: Li fullname: Li, Ang organization: Chinese Academy of Sciences – sequence: 10 givenname: Junjie surname: Yang fullname: Yang, Junjie organization: Chinese Academy of Sciences – sequence: 11 givenname: Jing orcidid: 0000-0002-6917-5859 surname: Wang fullname: Wang, Jing organization: Chinese Academy of Sciences – sequence: 12 givenname: Yang surname: Peng fullname: Peng, Yang organization: Chinese Academy of Sciences – sequence: 13 givenname: Josep orcidid: 0000-0002-7215-0150 surname: Peñuelas fullname: Peñuelas, Josep organization: CSIC, Global Ecology Unit CREAF‐CSIC‐UAB – sequence: 14 givenname: Jordi orcidid: 0000-0003-2478-0219 surname: Sardans fullname: Sardans, Jordi organization: CSIC, Global Ecology Unit CREAF‐CSIC‐UAB – sequence: 15 givenname: Jizheng surname: He fullname: He, Jizheng organization: Fujian Normal University – sequence: 16 givenname: Zhihong surname: Xu fullname: Xu, Zhihong organization: Griffith University – sequence: 17 givenname: Yingzhi surname: Gao fullname: Gao, Yingzhi email: gaoyz108@nenu.edu.cn organization: Northeast Normal University – sequence: 18 givenname: Xingguo orcidid: 0000-0002-1836-975X surname: Han fullname: Han, Xingguo email: xghan@ibcas.ac.cn organization: University of Chinese Academy of Sciences |
| BackLink | https://cnrs.hal.science/hal-04960313$$DView record in HAL https://res.slu.se/id/publ/113346$$DView record from Swedish Publication Index |
| BookMark | eNqFkk1v1DAQhiNUJNrCgX8QiQscsvVH7CTHsoIWaSUucLYc72Q7lWMvtrPVXvjtOGShKgLhy4xHzzvy65mL4sx5B0XxmpIVzedqZ_oVFS3tnhXnlEtRsbqVZ3Mu6ooSyl8UFzHeE0I4I_K8-L7WofeutDhi0glz6g8QAm4hltrgFgc0Sx1dOcIW88XtyujRliOa4HvUNpMJD5iOZfKlwxT8DlwJLqC5G8GlWavLBOMegk5Q7oKO0Wq3fVk8H7SN8OoUL4uvHz98Wd9Wm883n9bXm8oIwrqqg6E2tdZCE0Z6EF0rhRG9oW0HDWOspS2jmuuGD4OkHTDedrUhnawHDo0Eflmslr7xAfZTr_YBRx2OymtU0U69DnNQERSlnNcyC94tgjttn9C31xs110jdScIpP9DMvl3YffDfJohJjRgN2GwQ_BQVk1zWXDay-T8qREvaLvvK6Js_0Hs_BZd_KVN5wLVgbH7n1ULlScQYYFDmNMcUNFpFiZr3QuW9UD_34tHZb8Uve39jT90f0MLx36C6Wb9fFD8AFQ3JxQ |
| CitedBy_id | crossref_primary_10_1016_j_catena_2022_106759 crossref_primary_10_3390_agriculture12091366 crossref_primary_10_1016_j_apsoil_2023_104991 crossref_primary_10_1016_j_catena_2023_106913 crossref_primary_10_1016_j_envres_2024_119206 crossref_primary_10_1093_jpe_rtac015 crossref_primary_10_1111_gcb_16669 crossref_primary_10_1111_gcb_16746 crossref_primary_10_1007_s42729_024_01734_9 crossref_primary_10_1016_j_geoderma_2022_116159 crossref_primary_10_3390_agriculture14071018 crossref_primary_10_1016_j_geoderma_2022_116036 crossref_primary_10_1016_j_jes_2024_09_022 crossref_primary_10_1016_j_apsoil_2024_105601 crossref_primary_10_1016_j_agee_2022_108144 crossref_primary_10_3389_fpls_2023_1168111 crossref_primary_10_1016_j_catena_2024_108303 crossref_primary_10_1007_s10661_024_13289_4 crossref_primary_10_1007_s11104_023_06310_1 crossref_primary_10_1016_j_soilbio_2023_108975 crossref_primary_10_1007_s11104_023_06339_2 crossref_primary_10_17221_275_2022_PSE crossref_primary_10_3389_fpls_2023_1109860 crossref_primary_10_1016_j_envres_2024_120155 crossref_primary_10_1111_gcb_17311 crossref_primary_10_1016_j_scitotenv_2024_175717 crossref_primary_10_1007_s11104_023_06354_3 crossref_primary_10_1016_j_agee_2023_108595 crossref_primary_10_1016_j_apsoil_2025_105874 crossref_primary_10_1016_j_scitotenv_2023_169793 crossref_primary_10_1111_1365_2435_14626 crossref_primary_10_24857_rgsa_v18n1_137 crossref_primary_10_1016_j_geoderma_2024_116841 crossref_primary_10_1111_ejss_13564 crossref_primary_10_1016_j_envres_2023_116501 crossref_primary_10_3390_biology11060870 crossref_primary_10_1186_s13717_024_00544_2 crossref_primary_10_1007_s42832_023_0216_0 crossref_primary_10_1016_j_scitotenv_2024_174088 crossref_primary_10_1007_s11104_023_06043_1 crossref_primary_10_1080_00103624_2023_2241500 crossref_primary_10_3389_fpls_2022_834184 crossref_primary_10_1007_s11104_024_06605_x crossref_primary_10_1016_j_still_2023_105864 crossref_primary_10_1016_j_rhisph_2025_101019 crossref_primary_10_1016_j_soilbio_2024_109695 crossref_primary_10_1007_s11104_022_05332_5 crossref_primary_10_1016_j_soilbio_2023_109272 crossref_primary_10_1016_j_geoderma_2023_116429 crossref_primary_10_1016_j_oneear_2024_02_007 crossref_primary_10_1016_j_scitotenv_2024_175867 crossref_primary_10_3389_fpls_2023_1175946 crossref_primary_10_1111_1365_2745_70001 crossref_primary_10_1016_j_ecolind_2022_108852 crossref_primary_10_1016_j_eti_2024_103712 crossref_primary_10_1021_acs_jafc_3c09655 crossref_primary_10_1016_j_apsoil_2024_105509 crossref_primary_10_1111_nph_19140 crossref_primary_10_1016_j_scitotenv_2023_167925 crossref_primary_10_1039_D3SU00295K crossref_primary_10_1002_ldr_4883 crossref_primary_10_3390_microorganisms12081716 crossref_primary_10_1007_s11104_025_07225_9 crossref_primary_10_1186_s40793_022_00441_1 crossref_primary_10_1029_2024GL111238 crossref_primary_10_3389_fmicb_2022_952021 crossref_primary_10_1007_s11104_024_06715_6 crossref_primary_10_1016_j_agee_2024_109368 crossref_primary_10_1016_j_apsoil_2025_105896 crossref_primary_10_1016_j_foreco_2023_121074 crossref_primary_10_1007_s11104_024_06656_0 crossref_primary_10_1111_gcb_17405 crossref_primary_10_1016_j_apsoil_2023_105134 crossref_primary_10_1038_s41559_022_01944_3 crossref_primary_10_1016_j_soilbio_2023_109218 crossref_primary_10_1002_ldr_4792 crossref_primary_10_1016_j_scitotenv_2023_163236 crossref_primary_10_1111_gcb_16272 crossref_primary_10_1007_s11104_025_07372_z crossref_primary_10_1111_gcb_17247 crossref_primary_10_1139_cjfr_2022_0001 crossref_primary_10_1029_2022JG007000 crossref_primary_10_1016_j_jenvman_2023_118807 crossref_primary_10_1016_j_scitotenv_2024_172954 crossref_primary_10_1016_j_scitotenv_2022_156405 crossref_primary_10_1016_j_geoderma_2023_116729 |
| Cites_doi | 10.1016/j.soilbio.2007.05.002 10.1038/srep03763 10.1016/j.soilbio.2015.02.014 10.1007/s00442‐012‐2584‐5 10.1016/j.geoderma.2018.07.008 10.1111/nph.15361 10.1111/gcb.13140 10.1126/science.1231923 10.1016/j.soilbio.2015.05.014 10.1016/0038‐0717(94)00241‐R 10.1016/j.soilbio.2008.07.011 10.1111/j.1469‐8137.2008.02488.x 10.2136/sssaj1989.03615995005300060016x 10.1111/j.1461‐0248.2008.01230.x 10.1111/gcb.12458 10.1111/j.1365‐2389.2008.01103.x 10.1111/1365‐2435.12525 10.1016/j.apsoil.2016.04.015 10.1073/pnas.0912421107 10.1016/S0038‐0717(99)00203‐5 10.1890/06‐2057.1 10.1007/s11104‐014‐2181‐y 10.5194/bg‐4‐769‐2007 10.1111/sum.12270 10.1111/j.1469‐8137.2010.03274.x 10.1080/15324980500299615 10.1016/S0038‐0717(03)00015‐4 10.1111/gcb.12611 10.1016/j.geoderma.2018.05.019 10.1007/s10533‐015‐0173‐5 10.1038/ngeo339 10.1016/j.soilbio.2007.08.019 10.1111/j.1461‐0248.2010.01482.x 10.1007/s11368‐010‐0260‐0 10.1016/j.geoderma.2020.114234 10.1007/s10533‐013‐9892‐7 10.1007/BF00384433 10.1007/s10021‐016‐0031‐x 10.1038/ncomms7707 10.1111/nph.12235 10.1016/j.scitotenv.2017.09.131 10.1016/j.foreco.2011.03.018 10.1890/13‐0274.1 10.1111/gcb.14719 10.1111/gcb.12348 10.1016/j.soilbio.2006.07.016 10.1016/j.soilbio.2015.01.001 10.1111/gcb.15311 10.1038/ngeo844 10.1007/s11355‐018‐0366‐x 10.1016/j.soilbio.2017.07.015 10.1016/j.soilbio.2018.02.003 10.1111/1365‐2435.12377 10.1016/j.soilbio.2019.05.018 10.1016/j.soilbio.2017.09.015 10.1016/j.envpol.2020.115016 10.1088/1748‐9326/10/2/024019 10.1007/s11427‐020‐1894‐8 10.1111/j.1365‐2486.2005.00902.x 10.1016/j.soilbio.2012.12.017 10.1038/s41561‐018‐0258‐6 10.1016/j.soilbio.2014.01.022 |
| ContentType | Journal Article |
| Copyright | 2021 John Wiley & Sons Ltd. Copyright © 2021 John Wiley & Sons Ltd Distributed under a Creative Commons Attribution 4.0 International License |
| Copyright_xml | – notice: 2021 John Wiley & Sons Ltd. – notice: Copyright © 2021 John Wiley & Sons Ltd – notice: Distributed under a Creative Commons Attribution 4.0 International License |
| CorporateAuthor | Sveriges lantbruksuniversitet |
| CorporateAuthor_xml | – name: Sveriges lantbruksuniversitet |
| DBID | AAYXX CITATION 7SN 7UA C1K F1W H97 L.G 7X8 7S9 L.6 1XC ADTPV AOWAS |
| DOI | 10.1111/gcb.15819 |
| DatabaseName | CrossRef Ecology Abstracts Water Resources Abstracts Environmental Sciences and Pollution Management ASFA: Aquatic Sciences and Fisheries Abstracts Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality Aquatic Science & Fisheries Abstracts (ASFA) Professional MEDLINE - Academic AGRICOLA AGRICOLA - Academic Hyper Article en Ligne (HAL) SwePub SwePub Articles |
| DatabaseTitle | CrossRef Aquatic Science & Fisheries Abstracts (ASFA) Professional Ecology Abstracts Aquatic Science & Fisheries Abstracts (ASFA) 3: Aquatic Pollution & Environmental Quality ASFA: Aquatic Sciences and Fisheries Abstracts Water Resources Abstracts Environmental Sciences and Pollution Management MEDLINE - Academic AGRICOLA AGRICOLA - Academic |
| DatabaseTitleList | MEDLINE - Academic Aquatic Science & Fisheries Abstracts (ASFA) Professional CrossRef AGRICOLA |
| DeliveryMethod | fulltext_linktorsrc |
| Discipline | Meteorology & Climatology Biology Environmental Sciences |
| EISSN | 1365-2486 |
| EndPage | 5988 |
| ExternalDocumentID | oai_slubar_slu_se_113346 oai_HAL_hal_04960313v1 10_1111_gcb_15819 GCB15819 |
| Genre | article |
| GeographicLocations | China |
| GeographicLocations_xml | – name: China |
| GrantInformation_xml | – fundername: European Research Council funderid: ERCSyG‐2013‐610028 IMBALANCE‐P – fundername: Catalan Government funderid: SGR2017‐1005 – fundername: Youth Innovation Promotion Association of the Chinese Academy of Sciences funderid: 2018032 – fundername: National Key R&D Program funderid: 2016YFC0500700 – fundername: Open Foundation of the State Key Laboratory of Urban and Regional Ecology of China funderid: SKLURE2021‐2‐1 – fundername: Fundación Ramon Areces |
| GroupedDBID | -DZ .3N .GA .Y3 05W 0R~ 10A 1OB 1OC 29I 31~ 33P 3SF 4.4 50Y 50Z 51W 51X 52M 52N 52O 52P 52S 52T 52U 52W 52X 53G 5GY 5HH 5LA 5VS 66C 702 7PT 8-0 8-1 8-3 8-4 8-5 8UM 930 A03 AAESR AAEVG AAHBH AAHHS AAHQN AAMNL AANHP AANLZ AAONW AASGY AAXRX AAYCA AAZKR ABCQN ABCUV ABEFU ABEML ABJNI ABPVW ACAHQ ACBWZ ACCFJ ACCZN ACGFS ACPOU ACPRK ACRPL ACSCC ACXBN ACXQS ACYXJ ADBBV ADEOM ADIZJ ADKYN ADMGS ADNMO ADOZA ADXAS ADZMN ADZOD AEEZP AEIGN AEIMD AENEX AEQDE AEUQT AEUYR AFBPY AFEBI AFFPM AFGKR AFPWT AFRAH AFWVQ AFZJQ AHBTC AHEFC AITYG AIURR AIWBW AJBDE AJXKR ALAGY ALMA_UNASSIGNED_HOLDINGS ALUQN ALVPJ AMBMR AMYDB ASPBG ATUGU AUFTA AVWKF AZBYB AZFZN AZVAB BAFTC BDRZF BFHJK BHBCM BMNLL BMXJE BNHUX BROTX BRXPI BY8 C45 CAG COF CS3 D-E D-F DC6 DCZOG DDYGU DPXWK DR2 DRFUL DRSTM DU5 EBS ECGQY EJD ESX F00 F01 F04 FEDTE FZ0 G-S G.N GODZA H.T H.X HF~ HGLYW HVGLF HZI HZ~ IHE IX1 J0M K48 LATKE LC2 LC3 LEEKS LH4 LITHE LOXES LP6 LP7 LUTES LW6 LYRES MEWTI MK4 MRFUL MRSTM MSFUL MSSTM MXFUL MXSTM N04 N05 N9A NF~ O66 O9- OIG OVD P2P P2W P2X P4D PALCI PQQKQ Q.N Q11 QB0 R.K RIWAO RJQFR ROL RX1 SAMSI SUPJJ TEORI UB1 UQL VOH W8V W99 WBKPD WIH WIK WNSPC WOHZO WQJ WRC WUP WXSBR WYISQ XG1 Y6R ZZTAW ~02 ~IA ~KM ~WT AAYXX AEYWJ AGHNM AGQPQ AGYGG CITATION 7SN 7UA AAMMB AEFGJ AGXDD AIDQK AIDYY C1K F1W H97 L.G 7X8 7S9 L.6 1XC ADTPV AOWAS |
| ID | FETCH-LOGICAL-c5029-9ef4c4aa5a020be59865c5bc189e722281821a3a73ff619e23894c0964f3e76e3 |
| IEDL.DBID | DR2 |
| ISSN | 1354-1013 1365-2486 |
| IngestDate | Thu Aug 21 06:46:24 EDT 2025 Fri May 09 12:15:11 EDT 2025 Fri Jul 11 18:38:50 EDT 2025 Fri Jul 11 00:01:49 EDT 2025 Fri Jul 25 19:32:49 EDT 2025 Tue Jul 01 03:53:07 EDT 2025 Thu Apr 24 22:56:10 EDT 2025 Wed Jan 22 16:27:41 EST 2025 |
| IsPeerReviewed | true |
| IsScholarly | true |
| Issue | 22 |
| Language | English |
| License | Distributed under a Creative Commons Attribution 4.0 International License: http://creativecommons.org/licenses/by/4.0 |
| LinkModel | DirectLink |
| MergedId | FETCHMERGED-LOGICAL-c5029-9ef4c4aa5a020be59865c5bc189e722281821a3a73ff619e23894c0964f3e76e3 |
| Notes | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 content type line 23 |
| ORCID | 0000-0001-9309-2722 0000-0003-2478-0219 0000-0003-0613-3624 0000-0002-6743-5653 0000-0001-8148-960X 0000-0002-1836-975X 0000-0002-7215-0150 0000-0001-5571-1895 0000-0002-6917-5859 0000-0001-7065-3435 0000-0001-6203-6883 |
| PQID | 2581945226 |
| PQPubID | 30327 |
| PageCount | 13 |
| ParticipantIDs | swepub_primary_oai_slubar_slu_se_113346 hal_primary_oai_HAL_hal_04960313v1 proquest_miscellaneous_2636436767 proquest_miscellaneous_2558089189 proquest_journals_2581945226 crossref_citationtrail_10_1111_gcb_15819 crossref_primary_10_1111_gcb_15819 wiley_primary_10_1111_gcb_15819_GCB15819 |
| ProviderPackageCode | CITATION AAYXX |
| PublicationCentury | 2000 |
| PublicationDate | November 2021 |
| PublicationDateYYYYMMDD | 2021-11-01 |
| PublicationDate_xml | – month: 11 year: 2021 text: November 2021 |
| PublicationDecade | 2020 |
| PublicationPlace | Oxford |
| PublicationPlace_xml | – name: Oxford |
| PublicationTitle | Global change biology |
| PublicationYear | 2021 |
| Publisher | Blackwell Publishing Ltd Wiley |
| Publisher_xml | – name: Blackwell Publishing Ltd – name: Wiley |
| References | 2007; 39 2018; 120 2010; 11 2010; 13 2010; 107 2013; 23 2019; 12 2016; 32 2010; 187 2016; 30 2016; 106 2018; 329 2020; 366 2008; 1 2017; 115 2014; 20 2013; 19 2013; 59 2014; 4 2015; 82 1995; 27 2013; 115 2018; 332 2015; 85 2015; 88 2019; 25 2007; 4 2018; 615 2013; 198 2010; 3 1996; 22 2018; 221 2015; 6 2015; 126 2009; 60 2015; 10 2003; 35 2006; 19 2008; 11 2020; 265 1989; 53 2015; 29 2013; 339 2021 2000; 32 2016; 20 2008; 89 2020; 26 2019; 135 2017 2008; 179 2011; 262 2008; 40 2014; 72 2014; 383 2013; 171 2005; 11 2018; 15 2016; 22 e_1_2_8_28_1 e_1_2_8_24_1 e_1_2_8_47_1 e_1_2_8_26_1 e_1_2_8_49_1 e_1_2_8_3_1 e_1_2_8_5_1 e_1_2_8_7_1 e_1_2_8_9_1 e_1_2_8_20_1 e_1_2_8_43_1 e_1_2_8_22_1 e_1_2_8_45_1 R Development Core Team (e_1_2_8_44_1) 2017 e_1_2_8_62_1 e_1_2_8_41_1 e_1_2_8_60_1 e_1_2_8_17_1 e_1_2_8_19_1 e_1_2_8_13_1 e_1_2_8_36_1 e_1_2_8_59_1 e_1_2_8_15_1 e_1_2_8_38_1 e_1_2_8_57_1 e_1_2_8_32_1 e_1_2_8_55_1 Zheng P. (e_1_2_8_64_1) 2021 e_1_2_8_11_1 e_1_2_8_34_1 e_1_2_8_53_1 e_1_2_8_51_1 e_1_2_8_30_1 e_1_2_8_29_1 e_1_2_8_25_1 e_1_2_8_46_1 e_1_2_8_27_1 e_1_2_8_48_1 e_1_2_8_2_1 e_1_2_8_4_1 e_1_2_8_6_1 e_1_2_8_8_1 e_1_2_8_21_1 e_1_2_8_42_1 e_1_2_8_23_1 e_1_2_8_65_1 e_1_2_8_63_1 e_1_2_8_40_1 e_1_2_8_61_1 e_1_2_8_18_1 e_1_2_8_39_1 e_1_2_8_14_1 e_1_2_8_35_1 e_1_2_8_16_1 e_1_2_8_37_1 e_1_2_8_58_1 e_1_2_8_10_1 e_1_2_8_31_1 e_1_2_8_56_1 e_1_2_8_12_1 e_1_2_8_33_1 e_1_2_8_54_1 e_1_2_8_52_1 e_1_2_8_50_1 |
| References_xml | – volume: 1 start-page: 767 issue: 11 year: 2008 end-page: 770 article-title: Negative impact of nitrogen deposition on soil buffering capacity publication-title: Nature Geoscience – volume: 35 start-page: 549 issue: 4 year: 2003 end-page: 563 article-title: The implications of exoenzyme activity on microbial carbon and nitrogen limitation in soil: A theoretical model publication-title: Soil Biology and Biochemistry – volume: 26 start-page: 6568 issue: 11 year: 2020 end-page: 6580 article-title: Nitrogen‐induced acidification, not N‐nutrient, dominates suppressive N effects on arbuscular mycorrhizal fungi publication-title: Global Change Biology – volume: 115 start-page: 310 year: 2017 end-page: 321 article-title: Indications that long‐term nitrogen loading limits carbon resources for soil microbes publication-title: Soil Biology and Biochemistry – volume: 12 start-page: 46 issue: 1 year: 2019 end-page: 53 article-title: Microbial formation of stable soil carbon is more efficient from belowground than aboveground input publication-title: Nature Geoscience – volume: 23 start-page: 1962 issue: 8 year: 2013 end-page: 1975 article-title: Forest liming increases forest floor carbon and nitrogen stocks in a mixed hardwood forest publication-title: Ecological Applications – volume: 135 start-page: 294 year: 2019 end-page: 303 article-title: Stoichiometric controls of soil carbon and nitrogen cycling after long‐term nitrogen and phosphorus addition in a mesic grassland in South Africa publication-title: Soil Biology and Biochemistry – volume: 53 start-page: 1707 issue: 6 year: 1989 end-page: 1711 article-title: Diffusion method to prepare soil extracts for automated N‐15 analysis publication-title: Soil Science Society of America Journal – year: 2021 – volume: 10 issue: 2 year: 2015 article-title: A global analysis of soil acidification caused by nitrogen addition publication-title: Environmental Research Letters – volume: 179 start-page: 428 issue: 2 year: 2008 end-page: 439 article-title: Global response patterns of terrestrial plant species to nitrogen addition publication-title: New Phytologist – volume: 40 start-page: 2660 issue: 10 year: 2008 end-page: 2669 article-title: Direct experimental evidence for the contribution of lime to CO release from managed peat soil publication-title: Soil Biology and Biochemistry – volume: 32 start-page: 390 issue: 3 year: 2016 end-page: 399 article-title: Soil acidification and the importance of liming agricultural soils with particular reference to the United Kingdom publication-title: Soil Use Management – volume: 4 start-page: 769 issue: 5 year: 2007 end-page: 779 article-title: Community shifts and carbon translocation within metabolically‐active rhizosphere microorganisms in grasslands under elevated CO publication-title: Biogeosciences – volume: 88 start-page: 158 year: 2015 end-page: 164 article-title: Carbon availability regulates soil respiration response to nitrogen and temperature publication-title: Soil Biology and Biochemistry – volume: 3 start-page: 315 issue: 5 year: 2010 end-page: 322 article-title: Reduction of forest soil respiration in response to nitrogen deposition publication-title: Nature Geoscience – volume: 59 start-page: 32 issue: 2 year: 2013 end-page: 37 article-title: Bacterial growth and growth‐limiting nutrients following chronic nitrogen additions to a hardwood forest soil publication-title: Soil Biology and Biochemistry – volume: 39 start-page: 276 issue: 1 year: 2007 end-page: 288 article-title: Carbon and nitrogen mineralization in acidic, limed and calcareous agricultural soils: Apparent and actual effects publication-title: Soil Biology and Biochemistry – volume: 39 start-page: 2485 issue: 10 year: 2007 end-page: 2495 article-title: Comparison of factors limiting bacterial growth in different soils publication-title: Soil Biology and Biochemistry – volume: 15 start-page: 101 issue: 1 year: 2018 end-page: 111 article-title: Effects of repeated fertilization and liming on soil microbial biomass in Regel and Fr. Schmidt stands in Japan publication-title: Landscape and Ecological Engineering – volume: 19 start-page: 299 issue: 4 year: 2006 end-page: 306 article-title: Net nitrogen mineralization or immobilization potential in a residue‐amended calcareous soil publication-title: Arid Land Research and Management – volume: 6 start-page: 6707 year: 2015 article-title: Plant diversity increases soil microbial activity and soil carbon storage publication-title: Nature Communications – volume: 27 start-page: 969 issue: 7 year: 1995 end-page: 975 article-title: Soil microbial biomass and activity in long‐term grassland: Effects of management changes publication-title: Soil Biology and Biochemistry – volume: 107 start-page: 10938 issue: 24 year: 2010 end-page: 10942 article-title: Shifting carbon flow from roots into associated microbial communities in response to elevated atmospheric CO publication-title: Proceedings of the National Academy of Sciences of the United States of America – volume: 332 start-page: 37 year: 2018 end-page: 44 article-title: Microbial carbon use efficiency and priming effect regulate soil carbon storage under nitrogen deposition by slowing soil organic matter decomposition publication-title: Geoderma – volume: 11 start-page: 15 issue: 1 year: 2010 end-page: 24 article-title: Effects of land use type and incubation temperature on greenhouse gas emissions from Chinese and Canadian soils publication-title: Journal of Soils and Sediments – volume: 339 start-page: 1615 issue: 6127 year: 2013 end-page: 1618 article-title: Roots and associated fungi drive long‐term carbon sequestration in boreal forest publication-title: Science – volume: 4 start-page: 3763 year: 2014 article-title: Spatial and decadal variations in inorganic nitrogen wet deposition in China induced by human activity publication-title: Scientific Reports – volume: 89 start-page: 371 issue: 2 year: 2008 end-page: 379 article-title: Nitrogen limitation of net primary productivity in terrestrial ecosystems is globally distributed publication-title: Ecology – volume: 115 start-page: 433 year: 2017 end-page: 441 article-title: Patterns and mechanisms of responses by soil microbial communities to nitrogen addition publication-title: Soil Biology and Biochemistry – volume: 30 start-page: 658 issue: 4 year: 2016 end-page: 669 article-title: Soil acidification exerts a greater control on soil respiration than soil nitrogen availability in grasslands subjected to long‐term nitrogen enrichment publication-title: Functional Ecology – volume: 20 start-page: 3520 year: 2014 end-page: 3529 article-title: Rapid plant species loss at high rates and at low frequency of N addition in temperate steppe publication-title: Global Change Biology – volume: 171 start-page: 639 issue: 3 year: 2013 end-page: 651 article-title: Beyond global change: Lessons from 25 years of CO research publication-title: Oecologia – volume: 82 start-page: 112 year: 2015 end-page: 118 article-title: The effects of simulated nitrogen deposition on plant root traits: A meta‐analysis publication-title: Soil Biology and Biochemistry – volume: 20 start-page: 1943 issue: 6 year: 2014 end-page: 1954 article-title: Labile carbon retention compensates for CO released by priming in forest soils publication-title: Global Change Biology – volume: 85 start-page: 22 year: 2015 end-page: 30 article-title: Greater humification of belowground than aboveground biomass carbon into particulate soil organic matter in no‐till corn and soybean crops publication-title: Soil Biology and Biochemistry – volume: 115 start-page: 33 year: 2013 end-page: 51 article-title: Nitrogen, organic carbon and sulphur cycling in terrestrial ecosystems: Linking nitrogen saturation to carbon limitation of soil microbial processes publication-title: Biogeochemistry – volume: 32 start-page: 725 issue: 5 year: 2000 end-page: 727 article-title: Suitability of the anthrone–sulfuric acid reagent for determining water soluble carbohydrates in soil water extracts publication-title: Soil Biology and Biochemistry – volume: 20 start-page: 354 issue: 2 year: 2016 end-page: 367 article-title: Linking above‐ and belowground responses to 16 years of fertilization, mowing, and removal of the dominant species in a temperate grassland publication-title: Ecosystems – volume: 265 start-page: 115016 issue: Pt A year: 2020 article-title: Soil acidification alters root morphology, increases root biomass but reduces root decomposition in an alpine grassland publication-title: Environmental Pollution – volume: 187 start-page: 485 issue: 2 year: 2010 end-page: 493 article-title: Quantification of effects of season and nitrogen supply on tree below‐ground carbon transfer to ectomycorrhizal fungi and other soil organisms in a boreal pine forest publication-title: New Phytologist – volume: 25 start-page: 2958 issue: 9 year: 2019 end-page: 2969 article-title: Asymmetry in above‐ and belowground productivity responses to N addition in a semi‐arid temperate steppe publication-title: Global Change Biology – volume: 198 start-page: 656 issue: 3 year: 2013 end-page: 669 article-title: Competition between roots and microorganisms for nitrogen: Mechanisms and ecological relevance publication-title: New Phytologist – volume: 29 start-page: 285 issue: 2 year: 2015 end-page: 296 article-title: Priming of the decomposition of ageing soil organic matter: Concentration dependence and microbial control publication-title: Functional Ecology – volume: 262 start-page: 95 issue: 2 year: 2011 end-page: 104 article-title: A meta‐analysis of the effects of nitrogen additions on base cations: Implications for plants, soils, and streams publication-title: Forest Ecology and Management – volume: 60 start-page: 186 issue: 2 year: 2009 end-page: 197 article-title: Contrasting effects of glucose, living roots and maize straw on microbial growth kinetics and substrate availability in soil publication-title: European Journal of Soil Science – volume: 72 start-page: 116 year: 2014 end-page: 122 article-title: Decoupling of soil microbes and plants with increasing anthropogenic nitrogen inputs in a temperate steppe publication-title: Soil Biology and Biochemistry – year: 2021 article-title: Disturbance‐level‐dependent post‐disturbance succession in a Eurasian steppe publication-title: Science China Life Science – volume: 22 start-page: 59 issue: 1 year: 1996 end-page: 65 article-title: The use of phospholipid fatty acid analysis to estimate bacterial and fungal biomass in soil publication-title: Biology and Fertility of Soils – volume: 13 start-page: 819 issue: 7 year: 2010 end-page: 828 article-title: A global perspective on belowground carbon dynamics under nitrogen enrichment publication-title: Ecology Letters – volume: 126 start-page: 301 issue: 3 year: 2015 end-page: 313 article-title: Chronic nitrogen fertilization and carbon sequestration in grassland soils: Evidence of a microbial enzyme link publication-title: Biogeochemistry – volume: 120 start-page: 126 year: 2018 end-page: 133 article-title: Decreasing soil microbial diversity is associated with decreasing microbial biomass under nitrogen addition publication-title: Soil Biology and Biochemistry – volume: 40 start-page: 370 issue: 2 year: 2008 end-page: 379 article-title: Bacterial and fungal response to nitrogen fertilization in three coniferous forest soils publication-title: Soil Biology and Biochemistry – volume: 329 start-page: 61 year: 2018 end-page: 64 article-title: Nitrogen addition aggravates microbial carbon limitation: Evidence from ecoenzymatic stoichiometry publication-title: Geoderma – volume: 383 start-page: 373 issue: 1 year: 2014 end-page: 385 article-title: Nutrient availability and pH jointly constrain microbial extracellular enzyme activities in nutrient‐poor tundra soils publication-title: Plant and Soil – volume: 19 start-page: 3688 issue: 12 year: 2013 end-page: 3697 article-title: Nitrogen deposition weakens plant‐microbe interactions in grassland ecosystems publication-title: Global Change Biology – volume: 106 start-page: 1 year: 2016 end-page: 10 article-title: Mineral nitrogen input decreases microbial biomass in soils under grasslands but not annual crops publication-title: Applied Soil Ecology – year: 2017 – volume: 615 start-page: 1535 year: 2018 end-page: 1546 article-title: Soil acid cations induced reduction in soil respiration under nitrogen enrichment and soil acidification publication-title: Science of the Total Environment – volume: 11 start-page: 266 issue: 2 year: 2005 end-page: 277 article-title: Soil microbial responses to experimental warming and clipping in a tallgrass prairie publication-title: Global Change Biology – volume: 11 start-page: 1111 issue: 10 year: 2008 end-page: 1120 article-title: Nitrogen additions and microbial biomass: A meta‐analysis of ecosystem studies publication-title: Ecology Letters – volume: 22 start-page: 1445 issue: 4 year: 2016 end-page: 1455 article-title: Nitrogen enrichment weakens ecosystem stability through decreased species asynchrony and population stability in a temperate grassland publication-title: Global Change Biology – volume: 221 start-page: 233 issue: 1 year: 2018 end-page: 246 article-title: Evidence for the primacy of living root inputs, not root or shoot litter, in forming soil organic carbon publication-title: New Phytologist – volume: 366 start-page: 114234 year: 2020 article-title: Soil acidification as an additional driver to organic carbon accumulation in major Chinese croplands publication-title: Geoderma – ident: e_1_2_8_11_1 doi: 10.1016/j.soilbio.2007.05.002 – ident: e_1_2_8_23_1 doi: 10.1038/srep03763 – ident: e_1_2_8_39_1 doi: 10.1016/j.soilbio.2015.02.014 – ident: e_1_2_8_31_1 doi: 10.1007/s00442‐012‐2584‐5 – ident: e_1_2_8_36_1 doi: 10.1016/j.geoderma.2018.07.008 – ident: e_1_2_8_50_1 doi: 10.1111/nph.15361 – ident: e_1_2_8_62_1 doi: 10.1111/gcb.13140 – ident: e_1_2_8_10_1 doi: 10.1126/science.1231923 – ident: e_1_2_8_15_1 doi: 10.1016/j.soilbio.2015.05.014 – ident: e_1_2_8_37_1 doi: 10.1016/0038‐0717(94)00241‐R – ident: e_1_2_8_3_1 doi: 10.1016/j.soilbio.2008.07.011 – ident: e_1_2_8_58_1 doi: 10.1111/j.1469‐8137.2008.02488.x – ident: e_1_2_8_6_1 doi: 10.2136/sssaj1989.03615995005300060016x – ident: e_1_2_8_53_1 doi: 10.1111/j.1461‐0248.2008.01230.x – ident: e_1_2_8_43_1 doi: 10.1111/gcb.12458 – ident: e_1_2_8_4_1 doi: 10.1111/j.1365‐2389.2008.01103.x – ident: e_1_2_8_8_1 doi: 10.1111/1365‐2435.12525 – ident: e_1_2_8_18_1 doi: 10.1016/j.apsoil.2016.04.015 – ident: e_1_2_8_14_1 doi: 10.1073/pnas.0912421107 – ident: e_1_2_8_20_1 doi: 10.1016/S0038‐0717(99)00203‐5 – ident: e_1_2_8_30_1 doi: 10.1890/06‐2057.1 – ident: e_1_2_8_51_1 doi: 10.1007/s11104‐014‐2181‐y – ident: e_1_2_8_13_1 doi: 10.5194/bg‐4‐769‐2007 – ident: e_1_2_8_19_1 doi: 10.1111/sum.12270 – volume-title: Effects of different forms of nitrogen addition on litter decomposition of dominant species in meadow steppe year: 2021 ident: e_1_2_8_64_1 – ident: e_1_2_8_21_1 doi: 10.1111/j.1469‐8137.2010.03274.x – ident: e_1_2_8_41_1 doi: 10.1080/15324980500299615 – ident: e_1_2_8_47_1 doi: 10.1016/S0038‐0717(03)00015‐4 – ident: e_1_2_8_63_1 doi: 10.1111/gcb.12611 – ident: e_1_2_8_9_1 doi: 10.1016/j.geoderma.2018.05.019 – ident: e_1_2_8_7_1 doi: 10.1007/s10533‐015‐0173‐5 – ident: e_1_2_8_5_1 doi: 10.1038/ngeo339 – ident: e_1_2_8_12_1 doi: 10.1016/j.soilbio.2007.08.019 – ident: e_1_2_8_34_1 doi: 10.1111/j.1461‐0248.2010.01482.x – ident: e_1_2_8_28_1 doi: 10.1007/s11368‐010‐0260‐0 – ident: e_1_2_8_61_1 doi: 10.1016/j.geoderma.2020.114234 – ident: e_1_2_8_25_1 doi: 10.1007/s10533‐013‐9892‐7 – ident: e_1_2_8_16_1 doi: 10.1007/BF00384433 – ident: e_1_2_8_26_1 doi: 10.1007/s10021‐016‐0031‐x – ident: e_1_2_8_29_1 doi: 10.1038/ncomms7707 – ident: e_1_2_8_27_1 doi: 10.1111/nph.12235 – ident: e_1_2_8_33_1 doi: 10.1016/j.scitotenv.2017.09.131 – ident: e_1_2_8_38_1 doi: 10.1016/j.foreco.2011.03.018 – ident: e_1_2_8_40_1 doi: 10.1890/13‐0274.1 – ident: e_1_2_8_55_1 doi: 10.1111/gcb.14719 – ident: e_1_2_8_57_1 doi: 10.1111/gcb.12348 – ident: e_1_2_8_2_1 doi: 10.1016/j.soilbio.2006.07.016 – ident: e_1_2_8_32_1 doi: 10.1016/j.soilbio.2015.01.001 – ident: e_1_2_8_42_1 doi: 10.1111/gcb.15311 – ident: e_1_2_8_22_1 doi: 10.1038/ngeo844 – ident: e_1_2_8_17_1 doi: 10.1007/s11355‐018‐0366‐x – ident: e_1_2_8_45_1 doi: 10.1016/j.soilbio.2017.07.015 – ident: e_1_2_8_54_1 doi: 10.1016/j.soilbio.2018.02.003 – ident: e_1_2_8_46_1 doi: 10.1111/1365‐2435.12377 – ident: e_1_2_8_48_1 doi: 10.1016/j.soilbio.2019.05.018 – ident: e_1_2_8_65_1 doi: 10.1016/j.soilbio.2017.09.015 – volume-title: R: A language and environment for statistical computing year: 2017 ident: e_1_2_8_44_1 – ident: e_1_2_8_56_1 doi: 10.1016/j.envpol.2020.115016 – ident: e_1_2_8_52_1 doi: 10.1088/1748‐9326/10/2/024019 – ident: e_1_2_8_59_1 doi: 10.1007/s11427‐020‐1894‐8 – ident: e_1_2_8_60_1 doi: 10.1111/j.1365‐2486.2005.00902.x – ident: e_1_2_8_24_1 doi: 10.1016/j.soilbio.2012.12.017 – ident: e_1_2_8_49_1 doi: 10.1038/s41561‐018‐0258‐6 – ident: e_1_2_8_35_1 doi: 10.1016/j.soilbio.2014.01.022 |
| SSID | ssj0003206 |
| Score | 2.6328955 |
| Snippet | Higher ecosystem nitrogen (N) inputs resulting from human activities often suppress soil microbial biomass and respiration, thereby altering biogeochemical... |
| SourceID | swepub hal proquest crossref wiley |
| SourceType | Open Access Repository Aggregation Database Enrichment Source Index Database Publisher |
| StartPage | 5976 |
| SubjectTerms | Acidification Acidity Availability belowground carbon allocation Biodiversity and Ecology Biogeochemical cycles Biological activity Biomass Carbon carbon use efficiency China Cycles ecosystems Environmental Sciences field experimentation global change Glucose Grasslands humans Immobilization Markvetenskap Microbial activity microbial biomass microbial carbon starvation Microorganisms Nitrogen nitrogen deposition Nitrogen enrichment organic matter decomposition pH effects Respiration Soil Soil acidification Soil chemistry Soil lime Soil pH Soil Science Soils Starvation |
| Title | Carbon limitation overrides acidification in mediating soil microbial activity to nitrogen enrichment in a temperate grassland |
| URI | https://onlinelibrary.wiley.com/doi/abs/10.1111%2Fgcb.15819 https://www.proquest.com/docview/2581945226 https://www.proquest.com/docview/2558089189 https://www.proquest.com/docview/2636436767 https://cnrs.hal.science/hal-04960313 https://res.slu.se/id/publ/113346 |
| Volume | 27 |
| hasFullText | 1 |
| inHoldings | 1 |
| isFullTextHit | |
| isPrint | |
| link | http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwnV1Lb9QwEB6VSkhceCxUBAoyCEEvWW1iOw9xKquWFQIOiEo9IEW247RRQ4KSXSQ48NuZcR7tIkCI02aTseLEY-eb5JtvAJ4Z-jaVLoyvIil8IYrQT7mJfKEXgbZBmHPrCLLvo9WJeHMqT3fg5ZgL0-tDTC_caGa49ZomuNLdlUl-ZvQ8kImT_CSuFgGiD5fSUTx0dTUDjl1At-ODqhCxeKaWW8-ia-fEhLwKM3vp0G3U6h47x7fg09jhnm1yMd-s9dx8_0XL8T-v6DbcHOAoO-z95w7s2HoG1_sCld9msHd0mQeHZsNC0M3Ae4dgu2mdGXvOllWJyNf9uws_lqrVTc0qyp1yA8-IJ9qWue2YMmVO7KR-f1kzl7pC3GvWNWXFPpdOGQpPRhkXVNiCrRuG607boKsz9PbSnFN3qK1ipKxFstCWnbUYBhBN8x6cHB99XK78ocyDbySRb1JbCCOUkgqhq7YkGC-N1CZIUhvTCyoMgQLFVcyLAsM9iyAjFQZDL1FwG0eW78Fu3dT2PjCEq0lqYh5zq4UtUs0NlxxBkE0XMs8TDw7GAc_McAuoFEeVjbEQjkHmxsCDp5Ppl17447dG6DXTcZLqXh2-zWgfRl5UwJt_DTzYH50qGxaILgupOanZRx48mQ7j1KbvNaq2zYZsZLJIUrwPf7GJOGJKUt3z4EXvsFvd6aqNVi39ZJ3F3nMu8IwHzg3_fF3Z6-Urt_Hg300fwo2Q-D4uT3Mfdtftxj5CwLbWj93M_AmVuj0n |
| linkProvider | Wiley-Blackwell |
| linkToHtml | http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwnV1Lb9QwEB6VIgQXHgtVAwUMQtBLVpvYeUlcytKywLYH1Eq9oMh2nDYiJCjZRYIDv50ZJ9l2ESDEKa-x4sQzzjfOzDcAzzT9m0om2pVhIFwhct9NuA5doSaeMp6fcWMDZI_C2Yl4dxqcbsDLIRem44dYLbiRZdj5mgycFqQvWfmZVmMviInz8ypV9Cbm_NcfLsijuG8ra3ocO4GKx3teIYrjWTVd-xpdOadYyMtAsyMPXcet9sNzcAs-Dl3u4k0-jZcLNdbff2Fz_N9nug03e0TK9joVugMbphrBta5G5bcRbO1fpMKhWD8XtCNwDhFv140VY8_ZtCwQ_Nqju_BjKhtVV6yk9Ck79oxCRZsiMy2TusgoQKk7X1TMZq9Q-DVr66JknwtLDoU3o6QLqm3BFjXDqaepUdsZKnyhz6k71FYyItciZmjDzhr0BChS8x6cHOwfT2duX-nB1QHF3yQmF1pIGUhEr8oQZ3ygA6W9ODERrVGhF-RJLiOe5-jxGcQZidDofYmcmyg0fAs2q7oy28AQscaJjnjEjRImTxTXPOCIg0wyCbIsdmB3GPFU96-AqnGU6eAO4RikdgwceLoS_dJxf_xWCNVmdZ3Yumd785TOofNFNbz5V8-BnUGr0n6OaFOfmhOhfejAk9VltG76ZSMrUy9JJogncYLv4S8yIUdYScR7DrzoNHatO225VLKhTdoa7D3nAu-4a_Xwz8-Vvpm-sjv3_130MVyfHR_O0_nbo_cP4IZP4T82bXMHNhfN0jxE_LZQj6yZ_gQ_P0FD |
| linkToPdf | http://utb.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwnV3db5RAEJ_UGo0vfpw2olVXY7QvXOB2-YpP9drz1NoYY5M-mJDdZWmJCA3cmeiDf7szC1x7Ro3x6TiYDQM7s_wGZn4D8FTTt6nE064MA-EKkU_chOvQFcrzlfEnGTc2QfYwnB-JN8fB8Qa8GGphOn6I1Qs38gy7XpODn2X5BSc_0WrsBzFRfl4WoZdQ34a9D-fcUXxiG2v6HHVAu-M9rRCl8ayGrj2MLp1SKuRFnNlxh67DVvvcmd2AT4PGXbrJ5_Fyocb6-y9kjv95STfheo9H2W5nQLdgw1QjuNJ1qPw2gq3980I4FOtXgnYEzjtE23VjxdgzNi0LhL723234MZWNqitWUvGUnXlGiaJNkZmWSV1klJ7U7S8qZmtXKPmatXVRsi-FpYbCk1HJBXW2YIua4cLT1GjrDM290KekDo2VjKi1iBfasJMG4wDK07wDR7P9j9O52_d5cHVA2TeJyYUWUgYSsasyxBgf6EBpP05MRG-oMAbyJZcRz3OM9wyijERojL1Ezk0UGr4Fm1VdmbvAEK_GiY54xI0SJk8U1zzgiIJM4gVZFjuwM0x4qvtbQL04ynQIhnAOUjsHDjxZiZ51zB-_FUKrWR0nru757kFK-zD0og7e_KvvwPZgVGm_QrTphIYTnX3owOPVYfRt-mAjK1MvSSaIvTjB-_AXmZAjqCTaPQeedwa7pk5bLpVs6CdtDWrPucAz7lgz_PN1pa-mL-3GvX8XfQRX3-_N0oPXh2_vw7UJ5f7Yms1t2Fw0S_MAwdtCPbRO-hNOoz_y |
| openUrl | ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fsummon.serialssolutions.com&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.atitle=Carbon+limitation+overrides+acidification+in+mediating+soil+microbial+activity+to+nitrogen+enrichment+in+a+temperate+grassland&rft.jtitle=Global+change+biology&rft.au=Qiushi+Ning&rft.au=H%C3%A4ttenschwiler%2C+Stephan&rft.au=L%C3%BC%2C+Xiaotao&rft.au=Kardol%2C+Paul&rft.date=2021-11-01&rft.pub=Blackwell+Publishing+Ltd&rft.issn=1354-1013&rft.eissn=1365-2486&rft.volume=27&rft.issue=22&rft.spage=5976&rft.epage=5988&rft_id=info:doi/10.1111%2Fgcb.15819&rft.externalDBID=NO_FULL_TEXT |
| thumbnail_l | http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/lc.gif&issn=1354-1013&client=summon |
| thumbnail_m | http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/mc.gif&issn=1354-1013&client=summon |
| thumbnail_s | http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/sc.gif&issn=1354-1013&client=summon |