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Bajiu A, Gao K, Zeng G, He Y. Impact of Intercropping Five Medicinal Plants on Soil Nutrients, Enzyme Activity, and Microbial Community Structure in Camellia oleifera Plantations. Microorganisms 2024; 12:1616. [PMID: 39203458 PMCID: PMC11356553 DOI: 10.3390/microorganisms12081616] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/01/2024] [Revised: 07/28/2024] [Accepted: 07/29/2024] [Indexed: 09/03/2024] Open
Abstract
Intercropping medicinal plants plays an important role in agroforestry that can improve the physical, chemical, and biological fertility of soil. However, the influence of intercropping medicinal plants on the Camellia oleifera soil properties and bacterial communities remains elusive. In this study, five intercropping treatment groups were set as follows: Curcuma zedoaria/C. oleifera (EZ), Curcuma longa/C. oleifera (JH), Clinacanthus nutans/C. oleifera (YDC), Fructus Galangae/C. oleifera (HDK), and Ficus simplicissima/C. oleifera (WZMT). The soil chemical properties, enzyme activities, and bacterial communities were measured and analyzed to evaluate the effects of different intercropping systems. The results indicated that, compared to the C. oleifera monoculture group, YDC and EZ showed noticeable impacts on the soil chemical properties with a significant increase in total nitrogen (TN), nitrate nitrogen (NN), available nitrogen (AN), available phosphorus (AP), and available potassium (AK). Among them, the content of TN and AK in the rhizosphere soil of Camellia oleifera in the YDC intercropping system was the highest, which was 7.82 g/kg and 21.94 mg/kg higher than CK. Similarly, in the EZ intercropping system, the content of NN and OM in the rhizosphere soil of Camellia oleifera was the highest, which was higher than that of CK at 722.33 mg/kg and 2.36 g/kg, respectively. Curcuma longa/C. oleifera (JH) and Clinacanthus nutans/C. oleifera (YDC) had the most effect on soil enzyme activities. Furthermore, YDC extensively increased the activities of hydrogen peroxide and acid phosphatase enzymes; the increase was 2.27 mg/g and 3.21 mg/g, respectively. While JH obviously increased the urease activity, the diversity of bacterial populations in the rhizosphere soil of the intercropping plants decreased, especially the Shannon index of YDC and HDK. Compared with the monoculture group, the bacterial community abundance and structure of JH and YDC were quite different. The relative abundance of Actinobacteriota and Firmicutes was increased in YDC, and that of Acidobacteriota and Myxococcota was increased in JH. According to the redundancy analysis (RDA), pH, total potassium, and soil catalase activity were identified as the main factors influencing the microbial community structure of the intercropping systems. In conclusion, intercropping with JH and YDC increased the relative abundance of the dominant bacterial communities, improved the microbial community structure, and enhanced the soil nutrients and enzyme activities. Therefore, in the future, these two medicinal plants can be used for intercropping with C. oleifera.
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Affiliation(s)
- Azuo Bajiu
- Guangxi Key Laboratory of Special Non-Wood Forest Cultivation and Utilization, Nanning 530002, China; (A.B.); (K.G.)
- Key Laboratory of National Forestry and Grassland Administration on Control of Artifcial Forest Diseases and Pests in South China, Hunan Provincial Key Laboratory for Control of Forest Diseases and Pests, Key Laboratory for Non-Wood Forest Cultivation and Conservation of Ministry of Education, Key Laboratory of Forest Bio-Resources and Integrated Pest Management for Higher Education in Hunan Province, College of Forestry, Central South University of Forestry and Technology, Changsha 410004, China
| | - Kai Gao
- Guangxi Key Laboratory of Special Non-Wood Forest Cultivation and Utilization, Nanning 530002, China; (A.B.); (K.G.)
| | - Guangyu Zeng
- Guangxi Key Laboratory of Special Non-Wood Forest Cultivation and Utilization, Nanning 530002, China; (A.B.); (K.G.)
| | - Yuanhao He
- Key Laboratory of National Forestry and Grassland Administration on Control of Artifcial Forest Diseases and Pests in South China, Hunan Provincial Key Laboratory for Control of Forest Diseases and Pests, Key Laboratory for Non-Wood Forest Cultivation and Conservation of Ministry of Education, Key Laboratory of Forest Bio-Resources and Integrated Pest Management for Higher Education in Hunan Province, College of Forestry, Central South University of Forestry and Technology, Changsha 410004, China
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Shang B, Agathokleous E, Calatayud V, Peng J, Xu Y, Li S, Liu S, Feng Z. Drought mitigates the adverse effects of O 3 on plant photosynthesis rather than growth: A global meta-analysis considering plant functional types. PLANT, CELL & ENVIRONMENT 2024; 47:1269-1284. [PMID: 38185874 DOI: 10.1111/pce.14808] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/16/2023] [Accepted: 12/21/2023] [Indexed: 01/09/2024]
Abstract
Tropospheric ozone (O3 ) is a phytotoxic air pollutant adversely affecting plant growth. High O3 exposures are often concurrent with summer drought. The effects of both stresses on plants are complex, and their interactions are not yet well understood. Here, we investigate whether drought can mitigate the negative effects of O3 on plant physiology and growth based on a meta-analysis. We found that drought mitigated the negative effects of O3 on plant photosynthesis, but the modification of the O3 effect on the whole-plant biomass by drought was not significant. This is explained by a compensatory response of water-deficient plants that leads to increased metabolic costs. Relative to water control condition, reduced water treatment decreased the effects of O3 on photosynthetic traits, and leaf and root biomass in deciduous broadleaf species, while all traits in evergreen coniferous species showed no significant response. This suggested that the mitigating effects of drought on the negative impacts of O3 on the deciduous broadleaf species were more extensive than on the evergreen coniferous ones. Therefore, to avoid over- or underestimations when assessing the impact of O3 on vegetation growth, soil moisture should be considered. These results contribute to a better understanding of terrestrial ecosystem responses under global change.
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Affiliation(s)
- Bo Shang
- Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology, Nanjing, Jiangsu, China
- Key Laboratory of Ecosystem Carbon Source and Sink, China Meteorological Administration (ECSS-CMA), School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing, Jiangsu, China
| | - Evgenios Agathokleous
- Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology, Nanjing, Jiangsu, China
- Key Laboratory of Ecosystem Carbon Source and Sink, China Meteorological Administration (ECSS-CMA), School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing, Jiangsu, China
| | - Vicent Calatayud
- Fundación CEAM, c/Charles R. Darwin 14, Parque Tecnológico, Paterna, Valencia, Spain
| | - Jinlong Peng
- Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China
| | - Yansen Xu
- Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology, Nanjing, Jiangsu, China
- Key Laboratory of Ecosystem Carbon Source and Sink, China Meteorological Administration (ECSS-CMA), School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing, Jiangsu, China
| | - Shuangjiang Li
- Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology, Nanjing, Jiangsu, China
- Key Laboratory of Ecosystem Carbon Source and Sink, China Meteorological Administration (ECSS-CMA), School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing, Jiangsu, China
| | - Shuo Liu
- Zhejiang Carbon Neutral Innovation Institute, Zhejiang University of Technology, Hangzhou, Zhejiang, China
| | - Zhaozhong Feng
- Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology, Nanjing, Jiangsu, China
- Key Laboratory of Ecosystem Carbon Source and Sink, China Meteorological Administration (ECSS-CMA), School of Ecology and Applied Meteorology, Nanjing University of Information Science and Technology, Nanjing, Jiangsu, China
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3
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Zhang Y, Cheng X, van Groenigen KJ, García-Palacios P, Cao J, Zheng X, Luo Y, Hungate BA, Terrer C, Butterbach-Bahl K, Olesen JE, Chen J. Shifts in soil ammonia-oxidizing community maintain the nitrogen stimulation of nitrification across climatic conditions. GLOBAL CHANGE BIOLOGY 2024; 30:e16989. [PMID: 37888833 DOI: 10.1111/gcb.16989] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/09/2023] [Revised: 10/01/2023] [Accepted: 10/04/2023] [Indexed: 10/28/2023]
Abstract
Anthropogenic nitrogen (N) loading alters soil ammonia-oxidizing archaea (AOA) and bacteria (AOB) abundances, likely leading to substantial changes in soil nitrification. However, the factors and mechanisms determining the responses of soil AOA:AOB and nitrification to N loading are still unclear, making it difficult to predict future changes in soil nitrification. Herein, we synthesize 68 field studies around the world to evaluate the impacts of N loading on soil ammonia oxidizers and nitrification. Across a wide range of biotic and abiotic factors, climate is the most important driver of the responses of AOA:AOB to N loading. Climate does not directly affect the N-stimulation of nitrification, but does so via climate-related shifts in AOA:AOB. Specifically, climate modulates the responses of AOA:AOB to N loading by affecting soil pH, N-availability and moisture. AOB play a dominant role in affecting nitrification in dry climates, while the impacts from AOA can exceed AOB in humid climates. Together, these results suggest that climate-related shifts in soil ammonia-oxidizing community maintain the N-stimulation of nitrification, highlighting the importance of microbial community composition in mediating the responses of the soil N cycle to N loading.
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Affiliation(s)
- Yong Zhang
- Key Laboratory of Soil Ecology and Health in Universities of Yunnan Province, School of Ecology and Environmental Science, Yunnan University, Kunming, China
- State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, China
| | - Xiaoli Cheng
- Key Laboratory of Soil Ecology and Health in Universities of Yunnan Province, School of Ecology and Environmental Science, Yunnan University, Kunming, China
| | - Kees Jan van Groenigen
- Department of Geography, Faculty of Environment, Science and Economy, University of Exeter, Exeter, UK
| | - Pablo García-Palacios
- Instituto de Ciencias Agrarias, Consejo Superior de Investigaciones Científicas, Madrid, Spain
- Department of Plant and Microbial Biology, University of Zurich, Zurich, Switzerland
| | - Junji Cao
- Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
| | - Xunhua Zheng
- Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China
| | - Yiqi Luo
- School of Integrative Plant Science, Cornell University, New York, Ithaca, USA
| | - Bruce A Hungate
- Department of Biological Sciences, Northern Arizona University, Arizona, Flagstaff, USA
| | - Cesar Terrer
- Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Massachusetts, Cambridge, USA
| | - Klaus Butterbach-Bahl
- Institute for Meteorology and Climate Research, Atmospheric Environmental Research, Karlsruhe Institute of Technology, Garmisch-Partenkirchen, Germany
- Center for Landscape Research in Sustainable Agricultural Futures, Land-CRAFT, Department of Agroecology, Aarhus University, Aarhus, Denmark
| | - Jørgen Eivind Olesen
- Department of Agroecology, Aarhus University, Tjele, Denmark
- Aarhus University Centre for Circular Bioeconomy, Aarhus University, Tjele, Denmark
- iCLIMATE Interdisciplinary Centre for Climate Change, Aarhus University, Roskilde, Denmark
| | - Ji Chen
- State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an, China
- Department of Agroecology, Aarhus University, Tjele, Denmark
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Liu C, Siri M, Li H, Ren C, Huang J, Feng C, Liu K. Drought is threatening plant growth and soil nutrients of grassland ecosystems: A meta-analysis. Ecol Evol 2023; 13:e10092. [PMID: 37250445 PMCID: PMC10208897 DOI: 10.1002/ece3.10092] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 02/28/2023] [Revised: 04/25/2023] [Accepted: 04/28/2023] [Indexed: 05/31/2023] Open
Abstract
As a widespread direct effect of global warming, drought is currently wreaking havoc on terrestrial ecosystems' structure and function, however, the synthesized analysis is lacked to explore the general rules between drought changes and main functional factors of grassland ecosystems. In this work, meta-analysis was used to examine the impacts of drought on grassland ecosystems in recent decades. According to the results, drought greatly reduced aboveground biomass (AGB), aboveground net primary production (ANPP), height, belowground biomass (BGB), belowground net primary production (BNPP), microbial biomass nitrogen (MBN), microbial biomass carbon (MBC) and soil respiration (SR), and increased dissolved organic carbon (DOC), total nitrogen (TN), total phosphorus (TP), nitrate nitrogen (NO3--N), and the ratio of microbial biomass carbon and nitrogen (MBC/MBN). The drought-related environmental factor mean annual temperature (MAT) was negatively correlated with AGB, height, ANPP, BNPP, MBC, and MBN, however, mean annual precipitation (MAP) had positive effect on these variables. These findings indicate that drought is threatening the biotic environment of grassland ecosystem, and the positive steps should be taken to address the negative effects of drought on grassland ecosystems due to climate change.
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Affiliation(s)
- Cheng Liu
- College of Grassland Science and TechnologyChina Agricultural UniversityBeijingChina
| | - Muji Siri
- College of Grassland Science and TechnologyChina Agricultural UniversityBeijingChina
| | - Hui Li
- College of Grassland Science and TechnologyChina Agricultural UniversityBeijingChina
| | - Cheng Ren
- College of Grassland Science and TechnologyChina Agricultural UniversityBeijingChina
| | - Jing Huang
- College of Grassland Science and TechnologyChina Agricultural UniversityBeijingChina
| | - Changliang Feng
- College of Grassland Science and TechnologyChina Agricultural UniversityBeijingChina
| | - Kesi Liu
- College of Grassland Science and TechnologyChina Agricultural UniversityBeijingChina
- National Field Station of Grassland Ecosystem in GuyuanGuyuanChina
- Key Laboratory of Restoration Ecology of Cold Area in Qinghai Province, Northwest Institute of Plateau BiologyChinese Academy of SciencesXiningChina
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Jin X, Wu F, Wu Q, Heděnec P, Peng Y, Wang Z, Yue K. Effects of drying-rewetting cycles on the fluxes of soil greenhouse gases. Heliyon 2023; 9:e12984. [PMID: 36704269 PMCID: PMC9871208 DOI: 10.1016/j.heliyon.2023.e12984] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/02/2023] [Revised: 01/10/2023] [Accepted: 01/11/2023] [Indexed: 01/15/2023] Open
Abstract
Irregular precipitation caused by climate changes has resulted in frequent events of soil drying-rewetting cycles (DWC), which can strongly affect soil carbon (C) and nitrogen (N) cycling, including the fluxes of greenhouse gases (GHGs). The response of soil carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) fluxes to DWC events may differ among different ecosystem types and vary with experimental settings and soil properties, but these processes were not quantitatively assessed. Here, we evaluated the responses of soil GHG fluxes to DWC, compared with consistent moisture, as well as the associated driving factors with 424 paired observations collected from 47 publications of lab incubation experiments. Results showed that: (1) DWC significantly decreased soil CO2 emissions by an average of 9.7%, but did not affect the emissions and uptakes of soil CH4 and N2O; (2) DWC effects on soil GHG emissions varied significantly among different ecosystem types, with CO2 emissions significantly decreased by 6.8 and 16.3% in croplands and grasslands soils, respectively, and CH4 and N2O emissions significantly decreased and increased in wetlands and forests soils, respectively; (3) the effects of DWC on CO2 emissions were also positively regulated by organic C and N concentrations, pH, clay concentration, and soil depth, but negatively by C:N ratio and silt concentration, while DWC effects on N2O emissions were negatively controlled by C:N ratio, silt concentration, and soil depth. Overall, our results showed that CO2 emissions were significantly decreased by DWC, while the fluxes of CH4 and N2O were not affected, indicating an overall decrease of GHGs in response to DWC. Our results will be useful for a better understanding of global GHG emissions under future climate change scenario.
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Affiliation(s)
- Xia Jin
- Key Laboratory for Humid Subtropical Eco-Geographical Processes of the Ministry of Education, School of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China
| | - Fuzhong Wu
- Key Laboratory for Humid Subtropical Eco-Geographical Processes of the Ministry of Education, School of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China,Fujian Sanming Forest Ecosystem National Observation and Research Station, Sanming 365002, China
| | - Qiqian Wu
- State Key Laboratory of Subtropical Silviculture, Zhejiang A & F University, Lin'an 311300, China
| | - Petr Heděnec
- Institute of Tropical Biodiversity and Sustainable Development, University Malaysia Terengganu, Kuala Nerus, 21030, Terengganu, Malaysia
| | - Yan Peng
- Key Laboratory for Humid Subtropical Eco-Geographical Processes of the Ministry of Education, School of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China
| | - Zheng Wang
- College of Forestry, Hebei Agricultural University, Baoding 071000, China
| | - Kai Yue
- Key Laboratory for Humid Subtropical Eco-Geographical Processes of the Ministry of Education, School of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China,Fujian Sanming Forest Ecosystem National Observation and Research Station, Sanming 365002, China,Corresponding author. Wulongjiang Middle Avenue 18, Shangjie Town, Minhou County, Fuzhou 350117, Fujian, China.
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6
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Liang XS, Ma W, Hu JX, Zhang BC, Wang ZW, Lü XT. Extreme drought exacerbates plant nitrogen‑phosphorus imbalance in nitrogen enriched grassland. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 849:157916. [PMID: 35963412 DOI: 10.1016/j.scitotenv.2022.157916] [Citation(s) in RCA: 5] [Impact Index Per Article: 2.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 05/10/2022] [Revised: 08/04/2022] [Accepted: 08/04/2022] [Indexed: 06/15/2023]
Abstract
The nitrogen‑phosphorus (N-P) imbalance induced by N enrichment has received increasing concerns, because N:P ratios play a critical role in driving many fundamental ecological processes. Given the simultaneous occurrence of different global change drivers, it is important to understand whether and how would such N-induced N-P imbalance would be mediated by other global change factors. We examined the interactive effects of N addition (10 g N m-2 yr-1) and extreme drought (-66 % rainfall during the growing season) on species- and community-level N:P ratios in both green and senesced leaves in a temperate grassland of northern China. Extreme drought did not alter soil available N:P ratio under ambient N conditions, but increased that under N enriched conditions. Further, extreme drought did not alter the community-level N:P in both green and senesced leaves under ambient N conditions but significantly enhanced that under N enriched conditions. The drought-induced species turnover made a significant positive contribution to the changes in the community-level N:P ratio under N enriched conditions, but not under ambient N conditions. Our results suggest that the N-induced ecosystem N-P imbalance would be exacerbated by extreme drought event, the frequency of which is predicted to increase across global drylands. Such N-P imbalance would have consequences on litter decomposition, nutrient cycling, and the structures of above- and below-ground food webs. Our findings highlighted the complexity in predicting ecosystem N-P imbalance given the interactions between different global change drivers.
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Affiliation(s)
- Xiao-Sa Liang
- Erguna Forest-Steppe Ecotone Research Station, CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; University of Chinese Academy of Sciences, Beijing 100049, China
| | - Wang Ma
- Erguna Forest-Steppe Ecotone Research Station, CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China
| | - Jia-Xin Hu
- Erguna Forest-Steppe Ecotone Research Station, CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; University of Chinese Academy of Sciences, Beijing 100049, China
| | - Bing-Chuan Zhang
- Erguna Forest-Steppe Ecotone Research Station, CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; University of Chinese Academy of Sciences, Beijing 100049, China
| | - Zheng-Wen Wang
- Erguna Forest-Steppe Ecotone Research Station, CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China
| | - Xiao-Tao Lü
- Erguna Forest-Steppe Ecotone Research Station, CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China.
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He M, Tang L, Li C, Ren J, Zhang L, Li X. Dynamics of soil organic carbon and nitrogen and their relations to hydrothermal variability in dryland. JOURNAL OF ENVIRONMENTAL MANAGEMENT 2022; 319:115751. [PMID: 35982576 DOI: 10.1016/j.jenvman.2022.115751] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 01/22/2022] [Revised: 06/30/2022] [Accepted: 07/10/2022] [Indexed: 06/15/2023]
Abstract
Carbon (C) and nitrogen (N) cycles of terrestrial ecosystems play key roles in global climate change and ecosystem sustainability. In recent decades, climate change has threatened the nutrient balance of dryland ecosystems. However, its impact on soil organic carbon (SOC) and soil total nitrogen (STN) in drylands of China are still unclear. In this study, the structural equation model (SEM) was used to explain the relationship between environmental variables used by the best model and SOC or STN. Then Adaptive Boosting Regressor (AdaBoost), Gradient Boosting Regression (GBRT), Extreme gradient boosting Regression (XGBoost) and Random Forest Regression (RF) were used to establish the prediction model of SOC and STN based on soil samples along with environmental variables. The performance of these models was assessed based on a 10-fold cross-validation method using three statistical indicators. Finally, we predicted the SOC and STN of soil samples from 2000 to 2019 based on the best model. Overall, the RF model performed better at predicting SOC and STN in drylands than the other three prediction models (AdaBoost, GBRT, XGBoost). Climate factors were the main factors affecting SOC and STN in the study area. In the Alashan, a dryland in northern China, the precipitation in the growing season increased from 2000 to 2019, at a rate of 12.9 mm/decade. During the same period, the annual sunshine duration significantly decreased by 66 h/decade. Along with interannual hydrothermal variability, SOC showed a fluctuating upward trend at a rate of 0.04 g/kg/decade, while STN exhibited a fluctuating downward trend at 0.003 g/kg/decade from 2000 to 2019. Due to the effects of climate change, dryland were considered as potential sites for carbon sequestration. However, due to the annual hydrothermal variance causing dynamic annual changes, it was deemed unstable. Moreover, it would cause STN loss, which might reduce soil fertility. More attention should be paid to STN monitoring in dryland in the future.
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Affiliation(s)
- Mingzhu He
- Shapotou Desert Research and Experiment Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 730000, Lanzhou, Gansu, China.
| | - Liang Tang
- Shapotou Desert Research and Experiment Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 730000, Lanzhou, Gansu, China.
| | - Chengyi Li
- Shapotou Desert Research and Experiment Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 730000, Lanzhou, Gansu, China; University of Chinese Academy of Sciences, 100000, Beijing, China
| | - Jianxin Ren
- Hami Agricultural Product Quality and Safety Inspection and Testing Center, 839000, Hami, Xinjiang, China
| | - Libin Zhang
- Shapotou Desert Research and Experiment Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 730000, Lanzhou, Gansu, China; University of Chinese Academy of Sciences, 100000, Beijing, China
| | - Xinrong Li
- Shapotou Desert Research and Experiment Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, 730000, Lanzhou, Gansu, China
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8
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Harris E, Yu L, Wang YP, Mohn J, Henne S, Bai E, Barthel M, Bauters M, Boeckx P, Dorich C, Farrell M, Krummel PB, Loh ZM, Reichstein M, Six J, Steinbacher M, Wells NS, Bahn M, Rayner P. Warming and redistribution of nitrogen inputs drive an increase in terrestrial nitrous oxide emission factor. Nat Commun 2022; 13:4310. [PMID: 35879348 PMCID: PMC9314393 DOI: 10.1038/s41467-022-32001-z] [Citation(s) in RCA: 15] [Impact Index Per Article: 7.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/10/2022] [Accepted: 07/11/2022] [Indexed: 11/17/2022] Open
Abstract
Anthropogenic nitrogen inputs cause major negative environmental impacts, including emissions of the important greenhouse gas N2O. Despite their importance, shifts in terrestrial N loss pathways driven by global change are highly uncertain. Here we present a coupled soil-atmosphere isotope model (IsoTONE) to quantify terrestrial N losses and N2O emission factors from 1850-2020. We find that N inputs from atmospheric deposition caused 51% of anthropogenic N2O emissions from soils in 2020. The mean effective global emission factor for N2O was 4.3 ± 0.3% in 2020 (weighted by N inputs), much higher than the surface area-weighted mean (1.1 ± 0.1%). Climate change and spatial redistribution of fertilisation N inputs have driven an increase in global emission factor over the past century, which accounts for 18% of the anthropogenic soil flux in 2020. Predicted increases in fertilisation in emerging economies will accelerate N2O-driven climate warming in coming decades, unless targeted mitigation measures are introduced.
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Affiliation(s)
- E Harris
- Swiss Data Science Centre, ETH Zurich, 8092, Zurich, Switzerland.
- Functional Ecology Research Group, Institute of Ecology, University of Innsbruck, 6020, Innsbruck, Austria.
| | - L Yu
- Institute of Environment and Ecology, Tsinghua Shenzhen International Graduate School (SIGS), Tsinghua University, Shenzhen, 518055, China
- Laboratory for Air Pollution & Environmental Technology, Empa, Swiss Federal Laboratories for Materials Science and Technology, 8600, Duebendorf, Switzerland
| | - Y-P Wang
- Climate Science Centre, CSIRO Oceans and Atmosphere, Aspendale, VIC, 3195, Australia
| | - J Mohn
- Laboratory for Air Pollution & Environmental Technology, Empa, Swiss Federal Laboratories for Materials Science and Technology, 8600, Duebendorf, Switzerland
| | - S Henne
- Laboratory for Air Pollution & Environmental Technology, Empa, Swiss Federal Laboratories for Materials Science and Technology, 8600, Duebendorf, Switzerland
| | - E Bai
- Key Laboratory of Geographical Processes and Ecological Security of Changbai Mountains, Ministry of Education, School of Geographical Sciences, Northeast Normal University, Changchun, 130024, China
| | - M Barthel
- Department of Environmental Systems Science, ETH Zurich, 8092, Zurich, Switzerland
| | - M Bauters
- Isotope Bioscience Laboratory - ISOFYS, Department of Green Chemistry and Technology, Ghent University, Coupure Links 653, 9000, Ghent, Belgium
| | - P Boeckx
- Isotope Bioscience Laboratory - ISOFYS, Department of Green Chemistry and Technology, Ghent University, Coupure Links 653, 9000, Ghent, Belgium
| | - C Dorich
- Natural Resource Ecology Laboratory, Colorado State University, Fort Collins, 80523, CO, USA
| | - M Farrell
- CSIRO Agriculture and Food, Locked bag 2, Glen Osmond, SA, 5064, Australia
| | - P B Krummel
- Climate Science Centre, CSIRO Oceans and Atmosphere, Aspendale, VIC, 3195, Australia
| | - Z M Loh
- Climate Science Centre, CSIRO Oceans and Atmosphere, Aspendale, VIC, 3195, Australia
| | - M Reichstein
- Department of Biogeochemical Integration, Max Planck Institute for Biogeochemistry, Jena, Germany
| | - J Six
- Department of Environmental Systems Science, ETH Zurich, 8092, Zurich, Switzerland
| | - M Steinbacher
- Laboratory for Air Pollution & Environmental Technology, Empa, Swiss Federal Laboratories for Materials Science and Technology, 8600, Duebendorf, Switzerland
| | - N S Wells
- Centre for Coastal Biogeochemistry, Southern Cross University, Lismore, NSW, 2480, Australia
- Department of Soil and Physical Sciences, Agriculture and Life Sciences, Lincoln University, Lincoln, 7647, New Zealand
| | - M Bahn
- Functional Ecology Research Group, Institute of Ecology, University of Innsbruck, 6020, Innsbruck, Austria
| | - P Rayner
- School of Geography, Earth and Atmospheric Sciences, University of Melbourne, Parkville, VIC, 3052, Australia
- Melbourne Climate Futures Climate and Energy College, University of Melbourne, Parkville, VIC, 3052, Australia
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9
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Chen A, Zhang D, Wang H, Cui R, Khoshnevisan B, Guo S, Wang P, Liu H. Shallow groundwater fluctuation: An ignored soil N loss pathway from cropland. THE SCIENCE OF THE TOTAL ENVIRONMENT 2022; 828:154554. [PMID: 35302037 DOI: 10.1016/j.scitotenv.2022.154554] [Citation(s) in RCA: 4] [Impact Index Per Article: 2.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/29/2021] [Revised: 03/06/2022] [Accepted: 03/09/2022] [Indexed: 06/14/2023]
Abstract
Nitrogen (N) pollution originating from agricultural land is among the major threats to shallow groundwater (SG). Soil N losses due to the SG table fluctuation are neglected, although a large number of studies have been conducted to evaluate N losses through leaching and runoff. Herein, the characteristics of N losses driven by SG table fluctuation were investigated using the microcosm experiment and surveyed data from the croplands around Erhai Lake. According to the results achieved, the total N (TN) loss mainly occurred during the initial 12 days when the soil was flooded, then presented N immobilized by soil and finally, basically balanced between influent and effluent after 50 days. The results demonstrated that 1.7% of the original soil TN storage (0-100 cm) was lost. The alternation of drying and flooding could greatly increase TN loss up to 1086 kg hm-2, which was 2.72 times as much as that of continuous flooding flow. The amount of soil N losses to groundwater was closely related to the soil profile biochemical characteristics (water content, soil microbial immobilization, mineralization, nitrification, and denitrification processes). Soil N loss from crop fields driven by SG table fluctuation is 26 and 6 times of the runoff and leaching losses, respectively, while the soil N loss from the vegetable fields is 33 and 4 times of the runoff and leaching losses. The total amount of N losses from the croplands around the Erhai Lake caused by flooding of shallow groundwater (SG) in 2016 was estimated at 3506 Mg. The estimations showed that N losses would decrease by 16% if vegetables are replaced with staple food crops. These results imply that the adjustment of the planting structure was the key measure to reduce soil N storage and mitigate groundwater contamination.
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Affiliation(s)
- Anqiang Chen
- Agricultural Environment and Resources Institute, Yunnan Academy of Agricultural Sciences, Kunming 650201, China
| | - Dan Zhang
- College of Resources and Environment, Yunnan Agricultural University, Kunming 650201, China
| | - Hongyuan Wang
- Key Laboratory of Non-point Source Pollution Control, Ministry of Agriculture and Rural Affairs, Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing 100081, China.
| | - Rongyang Cui
- Key Laboratory of Mountain Surface Processes and Ecological Regulation, Chinese Academy of Sciences, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences and Ministry of Water Conservancy, Chengdu 610041, Sichuan Province, China
| | - Benyamin Khoshnevisan
- Key Laboratory of Non-point Source Pollution Control, Ministry of Agriculture and Rural Affairs, Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing 100081, China; Department of Chemical Engineering, Biotechnology and Environmental Technology, University of Southern Denmark, Denmark
| | - Shufang Guo
- Agricultural Environment and Resources Institute, Yunnan Academy of Agricultural Sciences, Kunming 650201, China
| | - Panlei Wang
- Agricultural Environment and Resources Institute, Yunnan Academy of Agricultural Sciences, Kunming 650201, China
| | - Hongbin Liu
- Key Laboratory of Non-point Source Pollution Control, Ministry of Agriculture and Rural Affairs, Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing 100081, China
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10
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The Coupling Response between Different Bacterial Metabolic Functions in Water and Sediment Improve the Ability to Mitigate Climate Change. WATER 2022. [DOI: 10.3390/w14081203] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 12/11/2022]
Abstract
Extreme climatic events, such as heat wave and large temperature fluctuations, are predicted to increase in frequency and intensity during the next hundred years, which may rapidly alter the composition and function of lake bacterial communities. Here, we conducted a year-long experiment to explore the effect of warming on bacterial metabolic function of lake water and sediment. Predictions of the metabolic capabilities of these communities were performed with FAPROTAX using 16S rRNA sequencing data. The results indicated that the increase in temperature changed the structure of bacterial metabolic functional groups in water and sediment. During periods of low temperature, the carbon degradation pathway decreased, and the synthesis pathway increased, under the stimulation of warming, especially under the conditions temperature fluctuation. We also observed that nitrogen fixation ability was especially important in the warming treatments during the summer season. However, an elevated temperature significantly led to reduced nitrogen fixation abilities in winter. Compared with the water column, the most predominant functional groups of nitrogen cycle in sediment were nitrite oxidation and nitrification. Variable warming significantly promoted nitrite oxidation and nitrification function in winter, and constant warming was significantly inhibited in spring, with control in sediments. Co-occurrence network results showed that warming, especially variable warming, made microbial co-occurrence networks larger, more connected and less modular, and eventually functional groups in the water column and sediment cooperated to resist warming. We concluded that warming changed bacterial functional potentials important to the biogeochemical cycling in the experimental mesocosms in winter and spring with low temperature. The effect of different bacteria metabolism functions in water column and sediment may change the carbon and nitrogen fluxes in aquatic ecosystems. In conclusion, the coupling response between different bacterial metabolic functions in water and sediment may improve the ability to mitigate climate change.
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11
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Maxwell TL, Canarini A, Bogdanovic I, Böckle T, Martin V, Noll L, Prommer J, Séneca J, Simon E, Piepho HP, Herndl M, Pötsch EM, Kaiser C, Richter A, Bahn M, Wanek W. Contrasting drivers of belowground nitrogen cycling in a montane grassland exposed to a multifactorial global change experiment with elevated CO 2 , warming, and drought. GLOBAL CHANGE BIOLOGY 2022; 28:2425-2441. [PMID: 34908205 DOI: 10.5281/zenodo.5597021] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.5] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Subscribe] [Scholar Register] [Received: 06/11/2021] [Revised: 10/26/2021] [Accepted: 11/28/2021] [Indexed: 05/26/2023]
Abstract
Depolymerization of high-molecular weight organic nitrogen (N) represents the major bottleneck of soil N cycling and yet is poorly understood compared to the subsequent inorganic N processes. Given the importance of organic N cycling and the rise of global change, we investigated the responses of soil protein depolymerization and microbial amino acid consumption to increased temperature, elevated atmospheric CO2 , and drought. The study was conducted in a global change facility in a managed montane grassland in Austria, where elevated CO2 (eCO2 ) and elevated temperature (eT) were stimulated for 4 years, and were combined with a drought event. Gross protein depolymerization and microbial amino acid consumption rates (alongside with gross organic N mineralization and nitrification) were measured using 15 N isotope pool dilution techniques. Whereas eCO2 showed no individual effect, eT had distinct effects which were modulated by season, with a negative effect of eT on soil organic N process rates in spring, neutral effects in summer, and positive effects in fall. We attribute this to a combination of changes in substrate availability and seasonal temperature changes. Drought led to a doubling of organic N process rates, which returned to rates found under ambient conditions within 3 months after rewetting. Notably, we observed a shift in the control of soil protein depolymerization, from plant substrate controls under continuous environmental change drivers (eT and eCO2 ) to controls via microbial turnover and soil organic N availability under the pulse disturbance (drought). To the best of our knowledge, this is the first study which analyzed the individual versus combined effects of multiple global change factors and of seasonality on soil organic N processes and thereby strongly contributes to our understanding of terrestrial N cycling in a future world.
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Affiliation(s)
- Tania L Maxwell
- Division of Terrestrial Ecosystem Research, Department of Microbiology and Ecosystem Science, Center of Microbiology and Environmental Systems Science, Vienna, Austria
- INRAE, Bordeaux Sciences Agro, ISPA, Villenave d'Ornon, France
| | - Alberto Canarini
- Division of Terrestrial Ecosystem Research, Department of Microbiology and Ecosystem Science, Center of Microbiology and Environmental Systems Science, Vienna, Austria
| | - Ivana Bogdanovic
- Division of Terrestrial Ecosystem Research, Department of Microbiology and Ecosystem Science, Center of Microbiology and Environmental Systems Science, Vienna, Austria
| | - Theresa Böckle
- Division of Terrestrial Ecosystem Research, Department of Microbiology and Ecosystem Science, Center of Microbiology and Environmental Systems Science, Vienna, Austria
| | - Victoria Martin
- Division of Terrestrial Ecosystem Research, Department of Microbiology and Ecosystem Science, Center of Microbiology and Environmental Systems Science, Vienna, Austria
| | - Lisa Noll
- Division of Terrestrial Ecosystem Research, Department of Microbiology and Ecosystem Science, Center of Microbiology and Environmental Systems Science, Vienna, Austria
| | - Judith Prommer
- Division of Terrestrial Ecosystem Research, Department of Microbiology and Ecosystem Science, Center of Microbiology and Environmental Systems Science, Vienna, Austria
| | - Joana Séneca
- Division of Terrestrial Ecosystem Research, Department of Microbiology and Ecosystem Science, Center of Microbiology and Environmental Systems Science, Vienna, Austria
| | - Eva Simon
- Division of Terrestrial Ecosystem Research, Department of Microbiology and Ecosystem Science, Center of Microbiology and Environmental Systems Science, Vienna, Austria
| | - Hans-Peter Piepho
- Institute of Crop Science, University of Hohenheim, Stuttgart, Germany
| | - Markus Herndl
- Agricultural Research and Education Centre Raumberg-Gumpenstein, Irdning-Donnersbachtal, Austria
| | - Erich M Pötsch
- Agricultural Research and Education Centre Raumberg-Gumpenstein, Irdning-Donnersbachtal, Austria
| | - Christina Kaiser
- Division of Terrestrial Ecosystem Research, Department of Microbiology and Ecosystem Science, Center of Microbiology and Environmental Systems Science, Vienna, Austria
| | - Andreas Richter
- Division of Terrestrial Ecosystem Research, Department of Microbiology and Ecosystem Science, Center of Microbiology and Environmental Systems Science, Vienna, Austria
| | - Michael Bahn
- Department of Ecology, University of Innsbruck, Innsbruck, Austria
| | - Wolfgang Wanek
- Division of Terrestrial Ecosystem Research, Department of Microbiology and Ecosystem Science, Center of Microbiology and Environmental Systems Science, Vienna, Austria
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12
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Maxwell TL, Canarini A, Bogdanovic I, Böckle T, Martin V, Noll L, Prommer J, Séneca J, Simon E, Piepho H, Herndl M, Pötsch EM, Kaiser C, Richter A, Bahn M, Wanek W. Contrasting drivers of belowground nitrogen cycling in a montane grassland exposed to a multifactorial global change experiment with elevated CO 2 , warming, and drought. GLOBAL CHANGE BIOLOGY 2022; 28:2425-2441. [PMID: 34908205 PMCID: PMC9306501 DOI: 10.1111/gcb.16035] [Citation(s) in RCA: 14] [Impact Index Per Article: 7.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/11/2021] [Revised: 10/26/2021] [Accepted: 11/28/2021] [Indexed: 05/13/2023]
Abstract
Depolymerization of high-molecular weight organic nitrogen (N) represents the major bottleneck of soil N cycling and yet is poorly understood compared to the subsequent inorganic N processes. Given the importance of organic N cycling and the rise of global change, we investigated the responses of soil protein depolymerization and microbial amino acid consumption to increased temperature, elevated atmospheric CO2 , and drought. The study was conducted in a global change facility in a managed montane grassland in Austria, where elevated CO2 (eCO2 ) and elevated temperature (eT) were stimulated for 4 years, and were combined with a drought event. Gross protein depolymerization and microbial amino acid consumption rates (alongside with gross organic N mineralization and nitrification) were measured using 15 N isotope pool dilution techniques. Whereas eCO2 showed no individual effect, eT had distinct effects which were modulated by season, with a negative effect of eT on soil organic N process rates in spring, neutral effects in summer, and positive effects in fall. We attribute this to a combination of changes in substrate availability and seasonal temperature changes. Drought led to a doubling of organic N process rates, which returned to rates found under ambient conditions within 3 months after rewetting. Notably, we observed a shift in the control of soil protein depolymerization, from plant substrate controls under continuous environmental change drivers (eT and eCO2 ) to controls via microbial turnover and soil organic N availability under the pulse disturbance (drought). To the best of our knowledge, this is the first study which analyzed the individual versus combined effects of multiple global change factors and of seasonality on soil organic N processes and thereby strongly contributes to our understanding of terrestrial N cycling in a future world.
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Affiliation(s)
- Tania L. Maxwell
- Division of Terrestrial Ecosystem ResearchDepartment of Microbiology and Ecosystem ScienceCenter of Microbiology and Environmental Systems ScienceViennaAustria
- INRAEBordeaux Sciences AgroISPAVillenave d'OrnonFrance
| | - Alberto Canarini
- Division of Terrestrial Ecosystem ResearchDepartment of Microbiology and Ecosystem ScienceCenter of Microbiology and Environmental Systems ScienceViennaAustria
| | - Ivana Bogdanovic
- Division of Terrestrial Ecosystem ResearchDepartment of Microbiology and Ecosystem ScienceCenter of Microbiology and Environmental Systems ScienceViennaAustria
| | - Theresa Böckle
- Division of Terrestrial Ecosystem ResearchDepartment of Microbiology and Ecosystem ScienceCenter of Microbiology and Environmental Systems ScienceViennaAustria
| | - Victoria Martin
- Division of Terrestrial Ecosystem ResearchDepartment of Microbiology and Ecosystem ScienceCenter of Microbiology and Environmental Systems ScienceViennaAustria
| | - Lisa Noll
- Division of Terrestrial Ecosystem ResearchDepartment of Microbiology and Ecosystem ScienceCenter of Microbiology and Environmental Systems ScienceViennaAustria
| | - Judith Prommer
- Division of Terrestrial Ecosystem ResearchDepartment of Microbiology and Ecosystem ScienceCenter of Microbiology and Environmental Systems ScienceViennaAustria
| | - Joana Séneca
- Division of Terrestrial Ecosystem ResearchDepartment of Microbiology and Ecosystem ScienceCenter of Microbiology and Environmental Systems ScienceViennaAustria
| | - Eva Simon
- Division of Terrestrial Ecosystem ResearchDepartment of Microbiology and Ecosystem ScienceCenter of Microbiology and Environmental Systems ScienceViennaAustria
| | | | - Markus Herndl
- Agricultural Research and Education Centre Raumberg‐GumpensteinIrdning‐DonnersbachtalAustria
| | - Erich M. Pötsch
- Agricultural Research and Education Centre Raumberg‐GumpensteinIrdning‐DonnersbachtalAustria
| | - Christina Kaiser
- Division of Terrestrial Ecosystem ResearchDepartment of Microbiology and Ecosystem ScienceCenter of Microbiology and Environmental Systems ScienceViennaAustria
| | - Andreas Richter
- Division of Terrestrial Ecosystem ResearchDepartment of Microbiology and Ecosystem ScienceCenter of Microbiology and Environmental Systems ScienceViennaAustria
| | - Michael Bahn
- Department of EcologyUniversity of InnsbruckInnsbruckAustria
| | - Wolfgang Wanek
- Division of Terrestrial Ecosystem ResearchDepartment of Microbiology and Ecosystem ScienceCenter of Microbiology and Environmental Systems ScienceViennaAustria
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13
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Zhang Y, Zhang F, Abalos D, Luo Y, Hui D, Hungate BA, García-Palacios P, Kuzyakov Y, Olesen JE, Jørgensen U, Chen J. Stimulation of ammonia oxidizer and denitrifier abundances by nitrogen loading: Poor predictability for increased soil N 2 O emission. GLOBAL CHANGE BIOLOGY 2022. [PMID: 34923712 DOI: 10.6084/m9.figshare.14370896] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Subscribe] [Scholar Register] [Indexed: 05/02/2023]
Abstract
Unprecedented nitrogen (N) inputs into terrestrial ecosystems have profoundly altered soil N cycling. Ammonia oxidizers and denitrifiers are the main producers of nitrous oxide (N2 O), but it remains unclear how ammonia oxidizer and denitrifier abundances will respond to N loading and whether their responses can predict N-induced changes in soil N2 O emission. By synthesizing 101 field studies worldwide, we showed that N loading significantly increased ammonia oxidizer abundance by 107% and denitrifier abundance by 45%. The increases in both ammonia oxidizer and denitrifier abundances were primarily explained by N loading form, and more specifically, organic N loading had stronger effects on their abundances than mineral N loading. Nitrogen loading increased soil N2 O emission by 261%, whereas there was no clear relationship between changes in soil N2 O emission and shifts in ammonia oxidizer and denitrifier abundances. Our field-based results challenge the laboratory-based hypothesis that increased ammonia oxidizer and denitrifier abundances by N loading would directly cause higher soil N2 O emission. Instead, key abiotic factors (mean annual precipitation, soil pH, soil C:N ratio, and ecosystem type) explained N-induced changes in soil N2 O emission. Altogether, these findings highlight the need for considering the roles of key abiotic factors in regulating soil N transformations under N loading to better understand the microbially mediated soil N2 O emission.
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Affiliation(s)
- Yong Zhang
- School of Resources and Environmental Engineering, Anhui University, Hefei, China
| | - Feng Zhang
- School of Resources and Environmental Engineering, Anhui University, Hefei, China
| | - Diego Abalos
- Department of Agroecology, Aarhus University, Tjele, Denmark
| | - Yiqi Luo
- Center for Ecosystem Science and Society and Department of Biological Sciences, Northern Arizona University, Flagstaff, Arizona, USA
| | - Dafeng Hui
- Department of Biological Sciences, Tennessee State University, Nashville, Tennessee, USA
| | - Bruce A Hungate
- Center for Ecosystem Science and Society and Department of Biological Sciences, Northern Arizona University, Flagstaff, Arizona, USA
| | - Pablo García-Palacios
- Departamento de Biología y Geología, Física y Química Inorgánica y Analítica, Escuela Superior de Ciencias Experimentales y Tecnología, Universidad Rey Juan Carlos, Móstoles, Spain
- Instituto de Ciencias Agrarias, Consejo Superior de Investigaciones Científicas, Madrid, Spain
| | - Yakov Kuzyakov
- Department of Soil Science of Temperate Ecosystems, University of Göttingen, Göttingen, Germany
- Agro-Technological Institute, RUDN University, Moscow, Russia
- Institute of Environmental Sciences, Kazan Federal University, Kazan, Russia
| | - Jørgen Eivind Olesen
- Department of Agroecology, Aarhus University, Tjele, Denmark
- iCLIMATE Interdisciplinary Centre for Climate Change, Aarhus University, Roskilde, Denmark
- Aarhus University Centre for Circular Bioeconomy, Aarhus University, Tjele, Denmark
| | - Uffe Jørgensen
- Department of Agroecology, Aarhus University, Tjele, Denmark
- Aarhus University Centre for Circular Bioeconomy, Aarhus University, Tjele, Denmark
| | - Ji Chen
- Department of Agroecology, Aarhus University, Tjele, Denmark
- iCLIMATE Interdisciplinary Centre for Climate Change, Aarhus University, Roskilde, Denmark
- Aarhus University Centre for Circular Bioeconomy, Aarhus University, Tjele, Denmark
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14
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Zhang Y, Zhang F, Abalos D, Luo Y, Hui D, Hungate BA, García‐Palacios P, Kuzyakov Y, Olesen JE, Jørgensen U, Chen J. Stimulation of ammonia oxidizer and denitrifier abundances by nitrogen loading: Poor predictability for increased soil N 2 O emission. GLOBAL CHANGE BIOLOGY 2022; 28:2158-2168. [PMID: 34923712 PMCID: PMC9303726 DOI: 10.1111/gcb.16042] [Citation(s) in RCA: 20] [Impact Index Per Article: 10.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/30/2021] [Accepted: 12/10/2021] [Indexed: 05/15/2023]
Abstract
Unprecedented nitrogen (N) inputs into terrestrial ecosystems have profoundly altered soil N cycling. Ammonia oxidizers and denitrifiers are the main producers of nitrous oxide (N2 O), but it remains unclear how ammonia oxidizer and denitrifier abundances will respond to N loading and whether their responses can predict N-induced changes in soil N2 O emission. By synthesizing 101 field studies worldwide, we showed that N loading significantly increased ammonia oxidizer abundance by 107% and denitrifier abundance by 45%. The increases in both ammonia oxidizer and denitrifier abundances were primarily explained by N loading form, and more specifically, organic N loading had stronger effects on their abundances than mineral N loading. Nitrogen loading increased soil N2 O emission by 261%, whereas there was no clear relationship between changes in soil N2 O emission and shifts in ammonia oxidizer and denitrifier abundances. Our field-based results challenge the laboratory-based hypothesis that increased ammonia oxidizer and denitrifier abundances by N loading would directly cause higher soil N2 O emission. Instead, key abiotic factors (mean annual precipitation, soil pH, soil C:N ratio, and ecosystem type) explained N-induced changes in soil N2 O emission. Altogether, these findings highlight the need for considering the roles of key abiotic factors in regulating soil N transformations under N loading to better understand the microbially mediated soil N2 O emission.
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Affiliation(s)
- Yong Zhang
- School of Resources and Environmental EngineeringAnhui UniversityHefeiChina
| | - Feng Zhang
- School of Resources and Environmental EngineeringAnhui UniversityHefeiChina
| | - Diego Abalos
- Department of AgroecologyAarhus UniversityTjeleDenmark
| | - Yiqi Luo
- Center for Ecosystem Science and Society and Department of Biological SciencesNorthern Arizona UniversityFlagstaffArizonaUSA
| | - Dafeng Hui
- Department of Biological SciencesTennessee State UniversityNashvilleTennesseeUSA
| | - Bruce A. Hungate
- Center for Ecosystem Science and Society and Department of Biological SciencesNorthern Arizona UniversityFlagstaffArizonaUSA
| | - Pablo García‐Palacios
- Departamento de Biología y GeologíaFísica y Química Inorgánica y AnalíticaEscuela Superior de Ciencias Experimentales y TecnologíaUniversidad Rey Juan CarlosMóstolesSpain
- Instituto de Ciencias AgrariasConsejo Superior de Investigaciones CientíficasMadridSpain
| | - Yakov Kuzyakov
- Department of Soil Science of Temperate EcosystemsUniversity of GöttingenGöttingenGermany
- Agro‐Technological InstituteRUDN UniversityMoscowRussia
- Institute of Environmental SciencesKazan Federal UniversityKazanRussia
| | - Jørgen Eivind Olesen
- Department of AgroecologyAarhus UniversityTjeleDenmark
- iCLIMATE Interdisciplinary Centre for Climate ChangeAarhus UniversityRoskildeDenmark
- Aarhus University Centre for Circular BioeconomyAarhus UniversityTjeleDenmark
| | - Uffe Jørgensen
- Department of AgroecologyAarhus UniversityTjeleDenmark
- Aarhus University Centre for Circular BioeconomyAarhus UniversityTjeleDenmark
| | - Ji Chen
- Department of AgroecologyAarhus UniversityTjeleDenmark
- iCLIMATE Interdisciplinary Centre for Climate ChangeAarhus UniversityRoskildeDenmark
- Aarhus University Centre for Circular BioeconomyAarhus UniversityTjeleDenmark
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15
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Fikri M, Joulian C, Motelica-Heino M, Norini MP, Hellal J. Resistance and Resilience of Soil Nitrogen Cycling to Drought and Heat Stress in Rehabilitated Urban Soils. Front Microbiol 2021; 12:727468. [PMID: 35002993 PMCID: PMC8727462 DOI: 10.3389/fmicb.2021.727468] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/18/2021] [Accepted: 11/12/2021] [Indexed: 11/21/2022] Open
Abstract
In the context of climate change and biodiversity loss, rehabilitation of degraded urban soils is a means of limiting artificialization of terrestrial ecosystems and preventing further degradation of soils. Ecological rehabilitation approaches are available to reinitiate soil functions and enhance plant development. However, little is known about the long-term stability of rehabilitated soils in terms of soil functions when further natural or anthropogenic perturbations occur. Based on rehabilitated urban soils, the present study sought to evaluate the resistance and resilience of soil functions linked to carbon cycling and phosphate dynamics in addition to nitrogen cycling and related microbial communities after a heat and drought stress. A laboratory experiment was conducted in microcosms under controlled temperature conditions, with four contrasted soils collected from a rehabilitated urban brownfield; an initial, non-rehabilitated soil (IS), a technosol with a high organic matter level (HO), and two technosols with less organic matter (LO1 and LO2), together with their respective controls (no stress). Changes in potential denitrification (PDR), nitrification (PNR) rates, and their interactive relationships with soil microbial activities and soil physicochemical properties were determined following a combined heat (40°C) and drought stress period of 21 days. Measurements were carried out immediately after the stress (resistance), and then also 5, 30, and 92 days after soil rewetting at 60% water holding capacity (resilience). Microbial activities involved in soil functions such as carbon cycling and phosphate dynamics proved to be of low resistance in all soils except for IS; however, they were resilient and recovered rapidly after rewetting. On the other hand, the microbial activities and gene abundances that were measured in relation to nitrogen cycling processes showed that for denitrification, activities were more rapidly resilient than gene abundances whereas for nitrification the activities and gene abundances were resilient in the same way. Results suggest that, unless the soils contain high amounts of organic matter, microbial communities in imported soils can be more vulnerable to environmental pressures such as drought and heat than communities already present. This should be considered when rehabilitating degraded soils.
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Affiliation(s)
- Mehdi Fikri
- BRGM, DEPA/GME, Orléans, France
- ISTO, UMR 7327, CNRS-Université d'Orléans-Brgm, Orléans, France
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16
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Shi Y, Wang J, Ao Y, Han J, Guo Z, Liu X, Zhang J, Mu C, Le Roux X. Responses of soil N 2 O emissions and their abiotic and biotic drivers to altered rainfall regimes and co-occurring wet N deposition in a semi-arid grassland. GLOBAL CHANGE BIOLOGY 2021; 27:4894-4908. [PMID: 34240513 DOI: 10.1111/gcb.15792] [Citation(s) in RCA: 15] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/16/2021] [Revised: 06/16/2021] [Accepted: 07/01/2021] [Indexed: 06/13/2023]
Abstract
Global change factors such as changed rainfall regimes and nitrogen (N) deposition contribute to increases in the emission of the greenhouse gas nitrous oxide (N2 O) from the soil. In previous research, N deposition has often been simulated by using a single or a series of N addition events over the course of a year, but wet N deposition actually co-occurs with rainfall. How soil N2 O emissions respond to altered rainfall amount and frequency, wet N deposition, and their interactions is still not fully understood. We designed a three-factor, fully factorial experiment with factors of rainfall amounts (ambient, -30%) rainfall frequency (ambient, ±50%) and wet N deposition (with/without) co-occurring with rainfall in semi-arid grassland mesocosms, and measured N2 O emissions and their possible biotic and abiotic drivers. Across all treatments, reduced rainfall amount and N deposition increased soil N2 O emissions by 35% and 28%, respectively. A significant interactive effect was observed between rainfall amount and N deposition, and to a lesser extent between rainfall frequency and N deposition. Without N deposition, reduced rainfall amount and altered rainfall frequency indirectly affected soil N2 O emissions by changing the abundance of nirK and soil net N mineralization, and the changes in nirK abundance were indirectly driven by soil N availability rather than directly by soil moisture. With N deposition, both the abundance of nirK and the level of soil water-filled pore space contributed to changes in N2 O emissions in response to altered rainfall regimes, and the changes in the abundance of nirK were indirectly driven by plant N uptake and nitrifier (ammonia-oxidizing bacteria) abundance. Our results imply that unlike wetter grassland ecosystems, reduced precipitation may increase N2 O emissions, and N deposition may only slightly increase N2 O emissions in arid and semi-arid N-limited ecosystems that are dominated by grasses with high soil N uptake capacity.
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Affiliation(s)
- Yujie Shi
- Institute of Grassland Science, Key Laboratory of Vegetation, Ecology of the Ministry of Education, Jilin Songnen Grassland Ecosystem National Observation and Research Station, Northeast Normal University, Changchun, P.R. China
- Jilin Provincial Key Laboratory of Ecological Restoration and Ecosystem Management, Northeast Normal University, Changchun, P.R. China
| | - Junfeng Wang
- Institute of Grassland Science, Key Laboratory of Vegetation, Ecology of the Ministry of Education, Jilin Songnen Grassland Ecosystem National Observation and Research Station, Northeast Normal University, Changchun, P.R. China
- Jilin Provincial Key Laboratory of Ecological Restoration and Ecosystem Management, Northeast Normal University, Changchun, P.R. China
| | - Yunna Ao
- Institute of Grassland Science, Key Laboratory of Vegetation, Ecology of the Ministry of Education, Jilin Songnen Grassland Ecosystem National Observation and Research Station, Northeast Normal University, Changchun, P.R. China
- Jilin Provincial Key Laboratory of Ecological Restoration and Ecosystem Management, Northeast Normal University, Changchun, P.R. China
| | - Jiayu Han
- Institute of Grassland Science, Key Laboratory of Vegetation, Ecology of the Ministry of Education, Jilin Songnen Grassland Ecosystem National Observation and Research Station, Northeast Normal University, Changchun, P.R. China
- Jilin Provincial Key Laboratory of Ecological Restoration and Ecosystem Management, Northeast Normal University, Changchun, P.R. China
| | - Zhihan Guo
- Institute of Grassland Science, Key Laboratory of Vegetation, Ecology of the Ministry of Education, Jilin Songnen Grassland Ecosystem National Observation and Research Station, Northeast Normal University, Changchun, P.R. China
- Jilin Provincial Key Laboratory of Ecological Restoration and Ecosystem Management, Northeast Normal University, Changchun, P.R. China
| | - Xinyuan Liu
- Institute of Grassland Science, Key Laboratory of Vegetation, Ecology of the Ministry of Education, Jilin Songnen Grassland Ecosystem National Observation and Research Station, Northeast Normal University, Changchun, P.R. China
- Jilin Provincial Key Laboratory of Ecological Restoration and Ecosystem Management, Northeast Normal University, Changchun, P.R. China
| | - Jinwei Zhang
- Institute of Grassland Science, Key Laboratory of Vegetation, Ecology of the Ministry of Education, Jilin Songnen Grassland Ecosystem National Observation and Research Station, Northeast Normal University, Changchun, P.R. China
- Jilin Provincial Key Laboratory of Ecological Restoration and Ecosystem Management, Northeast Normal University, Changchun, P.R. China
| | - Chunsheng Mu
- Institute of Grassland Science, Key Laboratory of Vegetation, Ecology of the Ministry of Education, Jilin Songnen Grassland Ecosystem National Observation and Research Station, Northeast Normal University, Changchun, P.R. China
- Jilin Provincial Key Laboratory of Ecological Restoration and Ecosystem Management, Northeast Normal University, Changchun, P.R. China
| | - Xavier Le Roux
- Microbial Ecology Centre LEM, INRAE UMR 1418, CNRS UMR 5557, VetAgroSup, Université de Lyon, Villeurbanne, France
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17
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Li H, Meng J, Liu Z, Lan Y, Yang X, Huang Y, He T, Chen W. Effects of biochar on N 2O emission in denitrification pathway from paddy soil: A drying incubation study. THE SCIENCE OF THE TOTAL ENVIRONMENT 2021; 787:147591. [PMID: 33991921 DOI: 10.1016/j.scitotenv.2021.147591] [Citation(s) in RCA: 7] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/29/2020] [Revised: 03/30/2021] [Accepted: 05/01/2021] [Indexed: 06/12/2023]
Abstract
N2O emission from paddy soil is a potential environmental risk, especially when the soil moisture content of paddy soil changes and excessive nitrogen retention occurs. Biochar is known to have a positive effect on reducing N2O emissions. However, the influence of different types of biochar on N2O emission with varying soil moisture contents is unclear. The objective of this study was to investigate the effects of biochar made from different feedstocks and at different pyrolysis temperatures on the release of N2O during drying process of paddy soil. An incubation experiment with four kinds of biochar (rice straw and rice husk biochar pyrolyzed at 400 °C and 700 °C, respectively) applied at 1% (w/w) was conducted on paddy soil with the same initial moisture content (105% water-filled pore space). The emission rate of N2O, concentrations of ammonium and nitrate, and the abundance of N2O related microbial functional genes (narG and nosZ) were monitored throughout the incubation period. Biochar amendments reduced cumulative N2O emissions by 56.8-90.1% compared to the control. Low-temperature rice straw biochar decreased nosZ gene abundance, downregulated the denitrification pathway, and reduced nitrogen loss and N2O emission. The low-temperature pyrolysis rice husk biochar and the control showed similar trends in narG and nosZ gene abundance and N2O emission. The high-temperature pyrolysis of rice straw and rice husk biochar showed opposite trends in narG gene abundance, but both increased nosZ gene abundance at the later incubation period. Different feedback on denitrification-derived N2O emission in biochar application was revealed in this study by establishing a link between biotic and abiotic factors, showing that caution should be exercised when considering the use of biochar to mitigate N2O emission under drying soil conditions.
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Affiliation(s)
- Han Li
- Liaoning Biochar Engineering & Technology Research Center, Shenyang Agricultural University, Shenyang 110866, China.
| | - Jun Meng
- Liaoning Biochar Engineering & Technology Research Center, Shenyang Agricultural University, Shenyang 110866, China.
| | - Zunqi Liu
- Liaoning Biochar Engineering & Technology Research Center, Shenyang Agricultural University, Shenyang 110866, China.
| | - Yu Lan
- Liaoning Biochar Engineering & Technology Research Center, Shenyang Agricultural University, Shenyang 110866, China.
| | - Xu Yang
- Liaoning Biochar Engineering & Technology Research Center, Shenyang Agricultural University, Shenyang 110866, China.
| | - Yuwei Huang
- Liaoning Biochar Engineering & Technology Research Center, Shenyang Agricultural University, Shenyang 110866, China.
| | - Tianyi He
- Liaoning Biochar Engineering & Technology Research Center, Shenyang Agricultural University, Shenyang 110866, China.
| | - Wenfu Chen
- Liaoning Biochar Engineering & Technology Research Center, Shenyang Agricultural University, Shenyang 110866, China.
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18
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Tarin MWK, Fan L, Xie D, Tayyab M, Rong J, Chen L, Muneer MA, Zheng Y. Response of Soil Fungal Diversity and Community Composition to Varying Levels of Bamboo Biochar in Red Soils. Microorganisms 2021; 9:microorganisms9071385. [PMID: 34202337 PMCID: PMC8306102 DOI: 10.3390/microorganisms9071385] [Citation(s) in RCA: 7] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/08/2021] [Revised: 06/21/2021] [Accepted: 06/23/2021] [Indexed: 11/16/2022] Open
Abstract
Soil fungi play a vital role in soil nutrient dynamics, but knowledge of their diversity and community composition in response to biochar addition into red soil is either limited or inconsistent. Therefore, we determined the impact of bamboo biochar (BB) with increasing concentrations (0, 5, 20, and 80 g kg−1 of soil, referred to as B0, BB5, BB20, and BB80, respectively) on soil physicochemical properties and fungal communities (Illumina high-throughput sequencing) in red soil under Fokenia hodginsii (Fujian cypress). We found that increasing BB levels effectively raised the soil pH and soil nutrients, particularly under BB80. BB addition significantly increased the relative abundance of important genera, i.e., Basidiomycota, Mucoromycota, and Chytridiomycota that could play a key role in ecological functioning, e.g., wood degradation and litter decomposition, improvement in plant nutrients uptake, and resistance to several abiotic stress factors. Soil amended with BB exhibited a substantial ability to increase the fungal richness and diversity; BB80 > BB20 > BB5 > B0. Basidiomycota, Mucoromycota, Glomeromycota, Rozellomycota, Aphelidiomycota, Kickxellomycota, and Planctomycetes were positively associated with soil pH, total nitrogen, phosphorous, and carbon, and available potassium and phosphorous. Besides, the correlation analysis between the soil fungal communities and soil properties also showed that soil pH was the most influential factor in shaping the soil fungal communities in the red soil. These findings have significant implications for a comprehensive understanding of how to ameliorate acidic soils with BB addition, as well as for future research on sustainable forest management, which might increase soil fungi richness, diversity, and functionality in acidic soils.
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Affiliation(s)
- Muhammad Waqqas Khan Tarin
- College of Landscape Architecture, Fujian Agriculture and Forestry University, Fuzhou 350002, China; (M.W.K.T.); (L.C.)
- College of Forestry, Fujian Agriculture and Forestry University, Fuzhou 350002, China; (L.F.); (D.X.); (J.R.)
| | - Lili Fan
- College of Forestry, Fujian Agriculture and Forestry University, Fuzhou 350002, China; (L.F.); (D.X.); (J.R.)
| | - Dejin Xie
- College of Forestry, Fujian Agriculture and Forestry University, Fuzhou 350002, China; (L.F.); (D.X.); (J.R.)
| | - Muhammad Tayyab
- College of Agriculture, Fujian Agriculture and Forestry University, Fuzhou 350002, China;
| | - Jundong Rong
- College of Forestry, Fujian Agriculture and Forestry University, Fuzhou 350002, China; (L.F.); (D.X.); (J.R.)
| | - Lingyan Chen
- College of Landscape Architecture, Fujian Agriculture and Forestry University, Fuzhou 350002, China; (M.W.K.T.); (L.C.)
| | - Muhammad Atif Muneer
- International Magnesium Institute, College of Resources and Environment, Fujian Agriculture and Forestry University, Fuzhou 350002, China;
| | - Yushan Zheng
- College of Landscape Architecture, Fujian Agriculture and Forestry University, Fuzhou 350002, China; (M.W.K.T.); (L.C.)
- College of Forestry, Fujian Agriculture and Forestry University, Fuzhou 350002, China; (L.F.); (D.X.); (J.R.)
- Correspondence:
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19
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Yue P, Zuo X, Li K, Cui X, Wang S, Misselbrook T, Liu X. The driving effect of nitrogen-related functional microorganisms under water and nitrogen addition on N 2O emission in a temperate desert. THE SCIENCE OF THE TOTAL ENVIRONMENT 2021; 772:145470. [PMID: 33581515 DOI: 10.1016/j.scitotenv.2021.145470] [Citation(s) in RCA: 2] [Impact Index Per Article: 0.7] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 11/05/2020] [Revised: 01/19/2021] [Accepted: 01/24/2021] [Indexed: 06/12/2023]
Abstract
Nitrous oxide (N2O) is an important greenhouse gas and a precursor of ozone depletion in the upper atmosphere, thus contributing to climate change and biological safety. The mechanisms and response characteristics of N2O emission in desert soils to precipitation and nitrogen (N) deposition are still unclear. To further elucidate this, an in-situ experiment was conducted in the Gurbantunggut Desert, a temperate desert in China, between June and September 2015 and 2016. The response in N2O flux to water addition (equivalent to 5 mm precipitation) was very transient in summer, only lasting one to two days. This was attributed to the rapid decrease in soil moisture following the water addition, due to the high temperature and drought conditions, and there was no significant change in N2O emission or in the abundance of N-related key functional genes. In contrast, N2O emissions increased significantly in response to N addition. This was associated with an increase in functional gene abundances of amoA (ammonia oxidizing bacteria (AOB)) and ammonia-oxidizing archaea (AOA), which responded positively to increasing soil NH4+-N content, but were inhibited by increasing soil NO3--N content. The abundance of the nirS (nitrate reductase) gene was significantly increased by increasing soil NO3--N content. Interestingly, the indirect effect of increased soil moisture in enhancing N2O emission by increasing the abundance of AOA was offset by a direct effect of soil moisture in inhibiting soil N2O emission. Overall, N2O emissions were mainly controlled by AOA rather than AOB in summer, and were more sensitive to soil available N than to soil moisture in this temperate desert.
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Affiliation(s)
- Ping Yue
- Urat Desert-Grassland Research Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; Naiman Desertification Research Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Science, Lanzhou, 730000, China; State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
| | - Xiaoan Zuo
- Urat Desert-Grassland Research Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; Naiman Desertification Research Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Science, Lanzhou, 730000, China
| | - Kaihui Li
- State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China
| | - Xiaoqing Cui
- College of Resources and Environmental Sciences, China Agricultural University, Beijing 100193, China
| | - Shaokun Wang
- Urat Desert-Grassland Research Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; Naiman Desertification Research Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Science, Lanzhou, 730000, China
| | - Tom Misselbrook
- Rothamsted Research, North Wyke, Okehampton, Devon EX20 2SB, UK
| | - Xuejun Liu
- College of Resources and Environmental Sciences, China Agricultural University, Beijing 100193, China.
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20
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Harris E, Diaz-Pines E, Stoll E, Schloter M, Schulz S, Duffner C, Li K, Moore KL, Ingrisch J, Reinthaler D, Zechmeister-Boltenstern S, Glatzel S, Brüggemann N, Bahn M. Denitrifying pathways dominate nitrous oxide emissions from managed grassland during drought and rewetting. SCIENCE ADVANCES 2021; 7:eabb7118. [PMID: 33547069 PMCID: PMC7864578 DOI: 10.1126/sciadv.abb7118] [Citation(s) in RCA: 31] [Impact Index Per Article: 10.3] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/12/2020] [Accepted: 12/07/2020] [Indexed: 05/19/2023]
Abstract
Nitrous oxide is a powerful greenhouse gas whose atmospheric growth rate has accelerated over the past decade. Most anthropogenic N2O emissions result from soil N fertilization, which is converted to N2O via oxic nitrification and anoxic denitrification pathways. Drought-affected soils are expected to be well oxygenated; however, using high-resolution isotopic measurements, we found that denitrifying pathways dominated N2O emissions during a severe drought applied to managed grassland. This was due to a reversible, drought-induced enrichment in nitrogen-bearing organic matter on soil microaggregates and suggested a strong role for chemo- or codenitrification. Throughout rewetting, denitrification dominated emissions, despite high variability in fluxes. Total N2O flux and denitrification contribution were significantly higher during rewetting than for control plots at the same soil moisture range. The observed feedbacks between precipitation changes induced by climate change and N2O emission pathways are sufficient to account for the accelerating N2O growth rate observed over the past decade.
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Affiliation(s)
- E Harris
- Plant, Soil and Ecosystem Processes Research Group, Department of Ecology, University of Innsbruck, Sternwartestrasse 15, 6020 Innsbruck, Austria.
| | - E Diaz-Pines
- Institute of Soil Research, University of Natural Resources and Life Sciences, Vienna, Peter-Jordan-Straße 82, 1190 Vienna, Austria
| | - E Stoll
- Plant, Soil and Ecosystem Processes Research Group, Department of Ecology, University of Innsbruck, Sternwartestrasse 15, 6020 Innsbruck, Austria
| | - M Schloter
- Research Unit Comparative Microbiome Analysis, Helmholtz Zentrum München, Ingolstädter Landstraße 1, 85764 Neuherberg, Germany
- Chair of Soil Science, Technical University of Munich, 85354 Freising, Germany
| | - S Schulz
- Research Unit Comparative Microbiome Analysis, Helmholtz Zentrum München, Ingolstädter Landstraße 1, 85764 Neuherberg, Germany
| | - C Duffner
- Research Unit Comparative Microbiome Analysis, Helmholtz Zentrum München, Ingolstädter Landstraße 1, 85764 Neuherberg, Germany
- Chair of Soil Science, Technical University of Munich, 85354 Freising, Germany
| | - K Li
- Department of Materials, Photon Science Institute, The University of Manchester, Oxford Road, Manchester M13 9PL, UK
| | - K L Moore
- Department of Materials, Photon Science Institute, The University of Manchester, Oxford Road, Manchester M13 9PL, UK
| | - J Ingrisch
- Plant, Soil and Ecosystem Processes Research Group, Department of Ecology, University of Innsbruck, Sternwartestrasse 15, 6020 Innsbruck, Austria
| | - D Reinthaler
- Plant, Soil and Ecosystem Processes Research Group, Department of Ecology, University of Innsbruck, Sternwartestrasse 15, 6020 Innsbruck, Austria
| | - S Zechmeister-Boltenstern
- Institute of Soil Research, University of Natural Resources and Life Sciences, Vienna, Peter-Jordan-Straße 82, 1190 Vienna, Austria
| | - S Glatzel
- Geoecology, Department of Geography and Regional Research, Faculty of Geosciences, Geography, and Astronomy, University of Vienna, Althanstraße 14, 1090 Vienna, Austria
| | - N Brüggemann
- Forschungszentrum Jülich GmbH, Institute of Bio- and Geosciences, Agrosphere (IBG-3), Wilhelm-Johnen-Straße, 52425 Jülich, Germany
| | - M Bahn
- Plant, Soil and Ecosystem Processes Research Group, Department of Ecology, University of Innsbruck, Sternwartestrasse 15, 6020 Innsbruck, Austria
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21
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Huang J, Xu Y, Yu H, Zhu W, Wang P, Wang B, Na X. Soil prokaryotic community shows no response to 2 years of simulated nitrogen deposition in an arid ecosystem in northwestern China. Environ Microbiol 2020; 23:1222-1237. [PMID: 33346392 DOI: 10.1111/1462-2920.15364] [Citation(s) in RCA: 5] [Impact Index Per Article: 1.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/10/2020] [Accepted: 12/15/2020] [Indexed: 11/30/2022]
Abstract
An arid ecosystem might be sensitive to nitrogen (N) deposition, but the associated ecosystem-specific response of soil microbes is not well studied. To assess the N enrichment effects on plant and prokaryotic community diversity, we performed a two-year NH4 NO3 treatment in a desert steppe in northwestern China. Results showed that N addition increased plant aboveground biomass and decreased plant Shannon diversity. A C4 herb (Salsola collina) became dominant, and loss of legume species was observed. The concentrations of soil NH4 + -N, NO3 - -N, microbial biomass N, and the plant aboveground biomass N pool increased in contrast to total N, suggesting that the N input into the arid ecosystem might mainly be assimilated by plants and exit the ecosystem. Remarkably, the α-diversity and structure of the soil prokaryotic community did not vary even at the highest N addition rate. Structural equation modelling further found that the plant aboveground N pool counteracted the acidification effect of N deposition and maintained soil pH thus partially stabilizing the composition of prokaryotic communities in a desert steppe. These findings suggested that the plants and N loss might contribute to the lack of responsiveness of soil prokaryotic community to N deposition in a desert steppe.
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Affiliation(s)
- Juying Huang
- Institute of Environmental Engineering, Ningxia University, Yinchuan, China
| | - Yixin Xu
- Institute of Environmental Engineering, Ningxia University, Yinchuan, China.,College of Resources and Environment, Ningxia University, Yinchuan, China
| | - Hailong Yu
- College of Resources and Environment, Ningxia University, Yinchuan, China
| | - Wanwan Zhu
- Institute of Environmental Engineering, Ningxia University, Yinchuan, China.,College of Resources and Environment, Ningxia University, Yinchuan, China
| | - Pan Wang
- Institute of Environmental Engineering, Ningxia University, Yinchuan, China.,College of Resources and Environment, Ningxia University, Yinchuan, China
| | - Bin Wang
- Research Institute of Subtropical Forestry, Chinese Academy of Forestry, Hangzhou, China
| | - Xiaofan Na
- School of Life Science, Lanzhou University, Lanzhou, China
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22
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Klaus VH, Friedritz L, Hamer U, Kleinebecker T. Drought boosts risk of nitrate leaching from grassland fertilisation. THE SCIENCE OF THE TOTAL ENVIRONMENT 2020; 726:137877. [PMID: 32481225 DOI: 10.1016/j.scitotenv.2020.137877] [Citation(s) in RCA: 6] [Impact Index Per Article: 1.5] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/06/2019] [Revised: 02/29/2020] [Accepted: 03/10/2020] [Indexed: 06/11/2023]
Abstract
Both climate change and agricultural intensification are drivers of global nutrient cycles and biodiversity loss. A potentially great environmental threat can arise when these two drivers interact, for example, when farmers try to compensate reduced soil nutrient availability due to drought by the application of liquid organic fertiliser. As dry soils don't hold back nutrients very well, this approach can lead to nitrate leaching and potentially also to the pollution of drinking water. However, little is known about leaching from dry but fertilised grassland soil, and how this is affected by land use intensity and plant diversity. In this mesocosm study, we transferred 60 grassland sods differing in past land use intensity to a greenhouse and treated them with severe drought, fertilisation and both together. Drought was induced by almost entirely stopping irrigation for seven weeks. Fertilisation was done by three applications of slurry summing up to 168 kg total nitrogen per hectare (111 kg NH4-N). We assessed nutrient leaching risk with ion-exchange resin (IER) bags installed in the soil of all mesocosms. IER bags were retrieved after drought and extracts were analysed for concentrations of nitrate, ammonium, phosphate and potassium. Fertilisation partially buffered drought-induced losses in yield. However, the interaction of fertilisation and drought resulted in a drastic increase in nitrate leaching risk when soils are rewetted (>300%), while neither drought nor fertilisation alone were significant. Ammonium concentrations followed the same trend as nitrate, but less pronounced. Phosphate and potassium concentrations were not affected by the treatments. Past land use was hardly related to soil nutrient concentrations, rather was plant diversity. However, results indicate that plant diversity was not driving nitrate and ammonium concentrations under drought and/or fertilisation. This study reveals grassland fertilisation during drought to be a severe environmental problem due to significantly increased nitrate leaching risk.
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Affiliation(s)
- Valentin H Klaus
- Institute of Agricultural Sciences, ETH Zürich, Universitätstr, 2, 8092 Zürich, Switzerland; Institute of Landscape Ecology, University of Münster, Heisenbergstr, 2, 48149 Münster, Germany.
| | - Lennart Friedritz
- Institute of Landscape Ecology, University of Münster, Heisenbergstr, 2, 48149 Münster, Germany
| | - Ute Hamer
- Institute of Landscape Ecology, University of Münster, Heisenbergstr, 2, 48149 Münster, Germany
| | - Till Kleinebecker
- Institute of Landscape Ecology, University of Münster, Heisenbergstr, 2, 48149 Münster, Germany; Institute of Landscape Ecology and Resource Management, University of Gießen, Heinrich-Buff-Ring 26-32, 35392 Gießen, Germany
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23
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Singh N, Abagandura GO, Kumar S. Short-term grazing of cover crops and maize residue impacts on soil greenhouse gas fluxes in two Mollisols. JOURNAL OF ENVIRONMENTAL QUALITY 2020; 49:628-639. [PMID: 33016385 DOI: 10.1002/jeq2.20063] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/17/2019] [Revised: 02/03/2020] [Accepted: 02/10/2020] [Indexed: 06/11/2023]
Abstract
An integrated crop-livestock system (ICLS), when managed properly, can help in mitigating soil surface greenhouse gas (GHG) fluxes, especially carbon dioxide (CO2 ), methane (CH4 ), and nitrous oxide (N2 O). However, the impacts of an ICLS on GHG fluxes are poorly understood. The present study was conducted at two sites (northern Brookings [Brookings-N] and northwestern Brookings [Brookings-NW]) established in 2016 and 2017, respectively, under loamy soils in South Dakota. The specific objective was to evaluate the impact of cover crops (CCs) and grazed CCs under oat (Avena sativa L.)-CCs-maize (Zea mays L.) rotation on GHG fluxes. Study treatments included the following: (a) a legume-dominated CC (LdC), (b) a cattle-grazed LdC (LdC+G), (c) a grass-dominated CC (GdC), (d) a cattle-grazed GdC (GdC+G), and (e) one without CC or grazing (NC). Greenhouse gas monitoring occurred weekly during the growing crop seasons in 2016 and 2017 for Brookings-N and in 2017 and 2018 for Brookings-NW. Data showed that cumulative CO2 and N2 O fluxes at Brookings-N were lower for GdC+G (4042 kg C ha-1 for CO2 and 1499 g N ha-1 for N2 O) than for LdC+G (4819 kg C ha-1 for CO2 and 2017 g N ha-1 for N2 O), indicating the superiority of GdC+G over LdC+G in reducing GHG fluxes. However, no effect from grazed CC on cumulative CO2 and N2 O fluxes were observed at the Brookings-NW site. Cumulative CH4 flux was not affected by an ICLS at either site. This short-term investigation showed that, in general, CCs and grazing of CCs and maize residue did not impact GHG fluxes.
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Affiliation(s)
- Navdeep Singh
- Dep. of Agronomy, Horticulture and Plant Science, South Dakota State Univ., Brookings, SD, 57007, USA
| | - Gandura Omar Abagandura
- Dep. of Agronomy, Horticulture and Plant Science, South Dakota State Univ., Brookings, SD, 57007, USA
| | - Sandeep Kumar
- Dep. of Agronomy, Horticulture and Plant Science, South Dakota State Univ., Brookings, SD, 57007, USA
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24
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Ullah MR, Corneo PE, Dijkstra FA. Inter-seasonal Nitrogen Loss with Drought Depends on Fertilizer Management in a Seminatural Australian Grassland. Ecosystems 2019. [DOI: 10.1007/s10021-019-00469-4] [Citation(s) in RCA: 3] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 10/25/2022]
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25
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Abstract
Climate change is causing shifts in precipitation patterns in the central grasslands of the United States, with largely unknown consequences on the collective physiological responses of the soil microbial community, i.e., the metaphenome. Here, we used an untargeted omics approach to determine the soil microbial community's metaphenomic response to soil moisture and to define specific metabolic signatures of the response. Specifically, we aimed to develop the technical approaches and metabolic mapping framework necessary for future systematic ecological studies. We collected soil from three locations at the Konza Long-Term Ecological Research (LTER) field station in Kansas, and the soils were incubated for 15 days under dry or wet conditions and compared to field-moist controls. The microbiome response to wetting or drying was determined by 16S rRNA amplicon sequencing, metatranscriptomics, and metabolomics, and the resulting shifts in taxa, gene expression, and metabolites were assessed. Soil drying resulted in significant shifts in both the composition and function of the soil microbiome. In contrast, there were few changes following wetting. The combined metabolic and metatranscriptomic data were used to generate reaction networks to determine the metaphenomic response to soil moisture transitions. Site location was a strong determinant of the response of the soil microbiome to moisture perturbations. However, some specific metabolic pathways changed consistently across sites, including an increase in pathways and metabolites for production of sugars and other osmolytes as a response to drying. Using this approach, we demonstrate that despite the high complexity of the soil habitat, it is possible to generate insight into the effect of environmental change on the soil microbiome and its physiology and functions, thus laying the groundwork for future, targeted studies.IMPORTANCE Climate change is predicted to result in increased drought extent and intensity in the highly productive, former tallgrass prairie region of the continental United States. These soils store large reserves of carbon. The decrease in soil moisture due to drought has largely unknown consequences on soil carbon cycling and other key biogeochemical cycles carried out by soil microbiomes. In this study, we found that soil drying had a significant impact on the structure and function of soil microbial communities, including shifts in expression of specific metabolic pathways, such as those leading toward production of osmoprotectant compounds. This study demonstrates the application of an untargeted multi-omics approach to decipher details of the soil microbial community's metaphenotypic response to environmental perturbations and should be applicable to studies of other complex microbial systems as well.
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26
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Hammerl V, Kastl EM, Schloter M, Kublik S, Schmidt H, Welzl G, Jentsch A, Beierkuhnlein C, Gschwendtner S. Influence of rewetting on microbial communities involved in nitrification and denitrification in a grassland soil after a prolonged drought period. Sci Rep 2019; 9:2280. [PMID: 30783152 PMCID: PMC6381133 DOI: 10.1038/s41598-018-38147-5] [Citation(s) in RCA: 9] [Impact Index Per Article: 1.8] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/11/2018] [Accepted: 12/18/2018] [Indexed: 11/11/2022] Open
Abstract
The frequency of extreme drought and heavy rain events during the vegetation period will increase in Central Europe according to future climate change scenarios, which will affect the functioning of terrestrial ecosystems in multiple ways. In this study, we simulated an extreme drought event (40 days) at two different vegetation periods (spring and summer) to investigate season-related effects of drought and subsequent rewetting on nitrifiers and denitrifiers in a grassland soil. Abundance of the microbial groups of interest was assessed by quantification of functional genes (amoA, nirS/nirK and nosZ) via quantitative real-time PCR. Additionally, the diversity of ammonia-oxidizing archaea was determined based on fingerprinting of the archaeal amoA gene. Overall, the different time points of simulated drought and rewetting strongly influenced the obtained response pattern of microbial communities involved in N turnover as well as soil ammonium and nitrate dynamics. In spring, gene abundance of nirS was irreversible reduced after drought whereas nirK and nosZ remained unaffected. Furthermore, community composition of ammonia-oxidizing archaea was altered by subsequent rewetting although amoA gene abundance remained constant. In contrast, no drought/rewetting effects on functional gene abundance or diversity pattern of nitrifying archaea were observed in summer. Our results showed (I) high seasonal dependency of microbial community responses to extreme events, indicating a strong influence of plant-derived factors like vegetation stage and plant community composition and consequently close plant-microbe interactions and (II) remarkable resistance and/or resilience of functional microbial groups involved in nitrogen cycling to extreme weather events what might indicate that microbes in a silty soil are better adapted to stress situations as expected.
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Affiliation(s)
- Verena Hammerl
- Research Unit Comparative Microbiome Analysis - Helmholtz Zentrum München, Ingolstädter Landstr. 1, 85764, Neuherberg, Germany
- Chair for Soil Ecology - Technische Universität München, Ingolstädter Landstr. 1, 85764, Neuherberg, Germany
| | - Eva-Maria Kastl
- Research Unit Comparative Microbiome Analysis - Helmholtz Zentrum München, Ingolstädter Landstr. 1, 85764, Neuherberg, Germany
| | - Michael Schloter
- Research Unit Comparative Microbiome Analysis - Helmholtz Zentrum München, Ingolstädter Landstr. 1, 85764, Neuherberg, Germany
| | - Susanne Kublik
- Research Unit Comparative Microbiome Analysis - Helmholtz Zentrum München, Ingolstädter Landstr. 1, 85764, Neuherberg, Germany
| | - Holger Schmidt
- Institute of Natural Sciences - Universität Koblenz Landau, Campus Koblenz, Universitätsstraße 1, 56070, Koblenz, Germany
| | - Gerhard Welzl
- Research Unit Comparative Microbiome Analysis - Helmholtz Zentrum München, Ingolstädter Landstr. 1, 85764, Neuherberg, Germany
| | - Anke Jentsch
- Disturbance Ecology - University of Bayreuth, Universitätsstr. 30, 95447, Bayreuth, Germany
| | - Carl Beierkuhnlein
- Chair of Biogeography - University of Bayreuth, Universitätsstr. 30, 95447, Bayreuth, Germany
| | - Silvia Gschwendtner
- Research Unit Comparative Microbiome Analysis - Helmholtz Zentrum München, Ingolstädter Landstr. 1, 85764, Neuherberg, Germany.
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Brenzinger K, Drost SM, Korthals G, Bodelier PLE. Organic Residue Amendments to Modulate Greenhouse Gas Emissions From Agricultural Soils. Front Microbiol 2018; 9:3035. [PMID: 30581429 PMCID: PMC6292959 DOI: 10.3389/fmicb.2018.03035] [Citation(s) in RCA: 14] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/10/2018] [Accepted: 11/23/2018] [Indexed: 01/08/2023] Open
Abstract
Organic fertilizers have been shown to stimulate CH4 uptake from agricultural soils. Managing fertilizer application to maximize this effect and to minimize emission of other greenhouse gasses offers possibilities to increase sustainability of agriculture. To tackle this challenge, we incubated an agricultural soil with different organic amendments (compost, sewage sludge, digestate, cover crop residues mixture), either as single application or in a mixture and subjected it to different soil moisture concentrations using different amounts of organic amendments. GHG fluxes and in vitro CH4 oxidation rates were measured repeatedly, while changes in organic matter and abundance of GHG relevant microbial groups (nitrifiers, denitrifiers, methanotrophs, methanogens) were measured at the end of the incubation. Overall the dynamics of the analyzed GHGs differed significantly. While CO2 and N2O differed considerably between the treatments, CH4 fluxes remained stable. In contrast, in vitro CH4 oxidation showed a clear increase for all amendments over time. CO2 fluxes were mostly dependent on the amount of organic residue that was used, while N2O fluxes were affected more by soil moisture. Several combinations of amendments led to reductions of CO2, CH4, and/or N2O emissions compared to un-amended soil. Most optimal GHG balance was obtained by compost amendments, which resulted in a similar overall GHG balance as compared to the un-amended soil. However, compost is not very nutrient rich potentially leading to lower crop yield when applied as single fertilizer. Hence, the combination of compost with one of the more nutrient rich organic amendments (sewage sludge, digestate) provides a trade-off between maintaining crop yield and minimizing GHG emissions. Additionally, we could observe a strong increase in microbial communities involved in GHG consumption in all amendments, with the strongest increase associated with cover crop residue mixtures. Future research should focus on the interrelation of plants, soil, and microbes and their impact on the global warming potential in relation to applied organic amendments.
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Affiliation(s)
- Kristof Brenzinger
- Department of Microbial Ecology Netherlands Institute of Ecology (NIOO-KNAW), Wageningen, Netherlands
| | - Sytske M Drost
- Department of Microbial Ecology Netherlands Institute of Ecology (NIOO-KNAW), Wageningen, Netherlands
| | - Gerard Korthals
- Department of Microbial Ecology Netherlands Institute of Ecology (NIOO-KNAW), Wageningen, Netherlands
| | - Paul L E Bodelier
- Department of Microbial Ecology Netherlands Institute of Ecology (NIOO-KNAW), Wageningen, Netherlands
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Soil bacterial networks are less stable under drought than fungal networks. Nat Commun 2018; 9:3033. [PMID: 30072764 PMCID: PMC6072794 DOI: 10.1038/s41467-018-05516-7] [Citation(s) in RCA: 631] [Impact Index Per Article: 105.2] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/04/2017] [Accepted: 07/11/2018] [Indexed: 12/13/2022] Open
Abstract
Soil microbial communities play a crucial role in ecosystem functioning, but it is unknown how co-occurrence networks within these communities respond to disturbances such as climate extremes. This represents an important knowledge gap because changes in microbial networks could have implications for their functioning and vulnerability to future disturbances. Here, we show in grassland mesocosms that drought promotes destabilising properties in soil bacterial, but not fungal, co-occurrence networks, and that changes in bacterial communities link more strongly to soil functioning during recovery than do changes in fungal communities. Moreover, we reveal that drought has a prolonged effect on bacterial communities and their co-occurrence networks via changes in vegetation composition and resultant reductions in soil moisture. Our results provide new insight in the mechanisms through which drought alters soil microbial communities with potential long-term consequences, including future plant community composition and the ability of aboveground and belowground communities to withstand future disturbances. Drought conditions can alter the composition of soil microbial communities, but the effects of drought on network properties have not been tested. Here, de Vries and colleagues show that co-occurrence networks are destabilised under drought for bacteria but not fungi.
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Effect of long-term fertilization strategies on bacterial community composition in a 35-year field experiment of Chinese Mollisols. AMB Express 2018; 8:20. [PMID: 29442257 PMCID: PMC5811423 DOI: 10.1186/s13568-018-0549-8] [Citation(s) in RCA: 14] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/28/2017] [Accepted: 02/05/2018] [Indexed: 11/10/2022] Open
Abstract
Bacteria play vital roles in soil biological fertility; however, it remains poorly understood about their response to long-term fertilization in Chinese Mollisols, especially when organic manure is substituted for inorganic nitrogen (N) fertilizer. To broaden our knowledge, high-throughput pyrosequencing and quantitative PCR were used to explore the impacts of inorganic fertilizer and manure on bacterial community composition in a 35-year field experiment of Chinese Mollisols. Soils were collected from four treatments: no fertilizer (CK), inorganic phosphorus (P) and potassium (K) fertilizer (PK), inorganic P, K, and N fertilizer (NPK), and inorganic P and K fertilizer plus manure (MPK). All fertilization differently changed soil properties. Compared with CK, the PK and NPK treatments acidified soil by significantly decreasing soil pH from 6.48 to 5.53 and 6.16, respectively, while MPK application showed no significant differences of soil pH, indicating alleviation of soil acidification. Moreover, all fertilization significantly increased soil organic matter (OM) and soybean yields, with the highest observed under MPK regime. In addition, the community composition at each taxonomic level varied considerably among the fertilization strategies. Bacterial taxa, associated with plant growth promotion, OM accumulation, disease suppression, and increased soil enzyme activity, were overrepresented in the MPK regime, while they were present at low abundant levels under NPK treatment, i.e. phyla Proteobacteria and Bacteroidetes, class Alphaproteobacteria, and genera Variovorax, Chthoniobacter, Massilia, Lysobacter, Catelliglobosispora and Steroidobacter. The application of MPK shifted soil bacterial community composition towards a better status, and such shifts were primarily derived from changes in soil pH and OM.
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Adaptation of soil nitrifiers to very low nitrogen level jeopardizes the efficiency of chemical fertilization in west african moist savannas. Sci Rep 2017; 7:10275. [PMID: 28860500 PMCID: PMC5578973 DOI: 10.1038/s41598-017-10185-5] [Citation(s) in RCA: 20] [Impact Index Per Article: 2.9] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/28/2017] [Accepted: 08/07/2017] [Indexed: 12/05/2022] Open
Abstract
The moist savanna zone covers 0.5 × 106 km2 in West Africa and is characterized by very low soil N levels limiting primary production, but the ecology of nitrifiers in these (agro)ecosystems is largely unknown. We compared the effects of six agricultural practices on nitrifier activity, abundance and diversity at nine sites in central Ivory Coast. Treatments, including repeated fertilization with ammonium and urea, had no effect on nitrification and crop N status after 3 to 5 crop cycles. Nitrification was actually higher at low than medium ammonium level. The nitrifying community was always dominated by ammonia oxidizing archaea and Nitrospira. However, the abundances of ammonia oxidizing bacteria, AOB, and Nitrobacter increased with fertilization after 5 crop cycles. Several AOB populations, some affiliated to Nitrosospira strains with urease activity or adapted to fluctuating ammonium levels, emerged in fertilized plots, which was correlated to nitrifying community ability to benefit from fertilization. In these soils, dominant nitrifiers adapted to very low ammonium levels have to be replaced by high-N nitrifiers before fertilization can stimulate nitrification. Our results show that the delay required for this replacement is much longer than ever observed for other terrestrial ecosystems, i.e. > 5 crop cycles, and demonstrate for the first time that nitrifier characteristics jeopardize the efficiency of fertilization in moist savanna soils.
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Mekala C, Nambi IM. Understanding the hydrologic control of N cycle: Effect of water filled pore space on heterotrophic nitrification, denitrification and dissimilatory nitrate reduction to ammonium mechanisms in unsaturated soils. JOURNAL OF CONTAMINANT HYDROLOGY 2017; 202:11-22. [PMID: 28549725 DOI: 10.1016/j.jconhyd.2017.04.005] [Citation(s) in RCA: 11] [Impact Index Per Article: 1.6] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/22/2016] [Revised: 02/23/2017] [Accepted: 04/09/2017] [Indexed: 06/07/2023]
Abstract
Irrigation practice will be effective if it supplies optimal water and nutrients to crops and act as a filter for contaminants leaching to ground water. There is always a scope for improving the fertilizer use efficiency and scheduling of wastewater irrigation if the fate and transport of nutrients particularly nitrogenous compounds in the soil are well understood. In the present study, nitrogen transport experiments for two different agricultural soils are performed under varying saturation 33, 57, 78% water filled pore space for sandy soil 1 and 52, 81 and 96% for loam soil 2. A HYDRUS 2D model with constructed wetland (CW2D) module could simulate aerobic nitrification and anoxic denitrification well for both soils and estimated the reaction kinetics. A hot spot of Dissimilatory Nitrate Reduction to Ammonium (DNRA) pathway has been observed at 81% moisture content for a loamy sand soil. The presence of high organic content and reductive soil environment (5.53 C/NO3- ratio; ORP=-125mV) results in ammonium accumulation of 16.85mg in the soil. The overall observation from this study is nitrification occurs in a wide range of saturations 33-78% with highest at 57% whereas denitrification is significant at higher water saturations 57-78% for sandy soil texture. For a loamy sand soil, denitrification is dominant at 96% saturation with least nitrification at all saturation studies. The greatest nitrogen losses (>90%) was observed for soil 2 while 30-70% for soil1. The slow dispersive subsurface transport with varying oxygen dynamics enhanced nitrogen losses from soil2 due to lesser soil permeability. This in turn, prevents NO3- leaching and groundwater contamination. This type of modeling study should be used before planning field experiments for designing optimal irrigation and fertigation schedules.
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Affiliation(s)
- C Mekala
- Department of Civil Engineering, Indian Institute of Technology Madras, 600036, India
| | - Indumathi M Nambi
- Department of Civil Engineering, Indian Institute of Technology Madras, 600036, India.
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Xu X, Liu X, Li Y, Ran Y, Liu Y, Zhang Q, Li Z, He Y, Xu J, Di H. Legacy effects of simulated short-term climate change on ammonia oxidisers, denitrifiers, and nitrous oxide emissions in an acid soil. ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH INTERNATIONAL 2017; 24:11639-11649. [PMID: 28324256 DOI: 10.1007/s11356-017-8799-6] [Citation(s) in RCA: 7] [Impact Index Per Article: 1.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/22/2016] [Accepted: 03/10/2017] [Indexed: 06/06/2023]
Abstract
Although the effect of simulated climate change on nitrous oxide (N2O) emissions and on associated microbial communities has been reported, it is not well understood if these effects are short-lived or long-lasting. Here, we conducted a field study to determine the interactive effects of simulated warmer and drier conditions on nitrifier and denitrifier communities and N2O emissions in an acidic soil and the longevity of the effects. A warmer (+2.3 °C) and drier climate (-7.4% soil moisture content) was created with greenhouses. The variation of microbial population abundance and community structure of ammonia-oxidizing archaea (AOA), bacteria (AOB), and denitrifiers (nirK/S, nosZ) were determined using real-time PCR and high-throughput sequencing. The results showed that the simulated warmer and drier conditions under the greenhouse following urea application significantly increased N2O emissions. There was also a moderate legacy effect on the N2O emissions when the greenhouses were removed in the urea treatment, although this effect only lasted a short period of time (about 60 days). The simulated climate change conditions changed the composition of AOA with the species affiliated to marine group 1.1a-associated lineage increasing significantly. The abundance of all the functional denitrifier genes decreased significantly under the simulated climate change conditions and the legacy effect, after the removal of greenhouses, significantly increased the abundance of AOB, AOA (mainly the species affiliated to marine group 1.1a-associated lineage), and nirK and nosZ genes in the urea-treated soil. In general, the effect of the simulated climate change was short-lived, with the denitrifier communities being able to return to ambient levels after a period of adaptation to ambient conditions. Therefore, the legacy effect of simulated short-time climate change conditions on the ammonia oxidizer and denitrifier communities and N2O emissions were temporary and once the conditions were removed, the microbial communities were able to adapt to the ambient conditions.
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Affiliation(s)
- Xiaoya Xu
- Institute of Soil and Water Resources and Environmental Science, College of Environmental and Resource Sciences, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou, 310058, China
| | - Xiaorui Liu
- Institute of Soil and Water Resources and Environmental Science, College of Environmental and Resource Sciences, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou, 310058, China
| | - Yong Li
- Institute of Soil and Water Resources and Environmental Science, College of Environmental and Resource Sciences, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou, 310058, China.
| | - Yu Ran
- Institute of Soil and Water Resources and Environmental Science, College of Environmental and Resource Sciences, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou, 310058, China
| | - Yapeng Liu
- Institute of Soil and Water Resources and Environmental Science, College of Environmental and Resource Sciences, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou, 310058, China
| | - Qichun Zhang
- Institute of Soil and Water Resources and Environmental Science, College of Environmental and Resource Sciences, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou, 310058, China
| | - Zheng Li
- Changzhou Industrial Technology Research Institute, Zhejiang University, Changzhou, China
| | - Yan He
- Institute of Soil and Water Resources and Environmental Science, College of Environmental and Resource Sciences, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou, 310058, China
| | - Jianming Xu
- Institute of Soil and Water Resources and Environmental Science, College of Environmental and Resource Sciences, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou, 310058, China
| | - Hongjie Di
- Institute of Soil and Water Resources and Environmental Science, College of Environmental and Resource Sciences, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou, 310058, China
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Gao M, Liu J, Qiao Y, Zhao M, Zhang XH. Diversity and Abundance of the Denitrifying Microbiota in the Sediment of Eastern China Marginal Seas and the Impact of Environmental Factors. MICROBIAL ECOLOGY 2017; 73:602-615. [PMID: 27924403 DOI: 10.1007/s00248-016-0906-6] [Citation(s) in RCA: 4] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 03/25/2016] [Accepted: 11/27/2016] [Indexed: 06/06/2023]
Abstract
Investigating the environmental influence on the community composition and abundance of denitrifiers in marine sediment ecosystem is essential for understanding of the ecosystem-level controls on the biogeochemical process of denitrification. In the present study, nirK-harboring denitrifying communities in different mud deposit zones of eastern China marginal seas (ECMS) were investigated via clone library analysis. The abundance of three functional genes affiliated with denitrification (narG, nirK, nosZ) was assessed by fluorescent quantitative PCR. The nirK-harboring microbiota were dominated by a few operational taxonomic units (OTUs), which were widely distributed in different sites with each site harboring their unique phylotypes. The mean abundance of nirK was significantly higher than that of narG and nosZ genes, and the abundance of narG was higher than that of nosZ. The inconsistent abundance profile of different functional genes along the process of denitrification might indicate that nitrite reduction occurred independently of denitrification in the mud deposit zones of ECMS, and sedimentary denitrification was accomplished by cooperation of different denitrifying species rather than a single species. Such important information would be missed when targeting only a single denitrifying functional gene. Analysis of correlation between abundance ratios and environmental factors revealed that the response of denitrifiers to environmental factors was not invariable in different mud deposit zones. Our results suggested that a comprehensive analysis of different denitrifying functional genes may gain more information about the dynamics of denitrifying microbiota in marine sediments.
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Affiliation(s)
- Minghong Gao
- College of Marine Life Sciences, Ocean University of China, 5 Yushan Road, Qingdao, 266003, China
| | - Jiwen Liu
- College of Marine Life Sciences, Ocean University of China, 5 Yushan Road, Qingdao, 266003, China
| | - Yanlu Qiao
- College of Marine Life Sciences, Ocean University of China, 5 Yushan Road, Qingdao, 266003, China
| | - Meixun Zhao
- Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Ocean University of China, Qingdao, 266100, China
- Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266071, China
| | - Xiao-Hua Zhang
- College of Marine Life Sciences, Ocean University of China, 5 Yushan Road, Qingdao, 266003, China.
- Laboratory for Marine Ecology and Environmental Science, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266071, China.
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Dai Z, Zhang X, Tang C, Muhammad N, Wu J, Brookes PC, Xu J. Potential role of biochars in decreasing soil acidification - A critical review. THE SCIENCE OF THE TOTAL ENVIRONMENT 2017; 581-582:601-611. [PMID: 28063658 DOI: 10.1016/j.scitotenv.2016.12.169] [Citation(s) in RCA: 171] [Impact Index Per Article: 24.4] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/24/2016] [Revised: 12/24/2016] [Accepted: 12/25/2016] [Indexed: 05/24/2023]
Abstract
A large number of soils, worldwide, are acid (normally pH<5.5) and suffering from on-going soil acidification. Acid soils or soils undergoing acidification generally have low fertility and low crop productivity. Biochars have been reported to be of potential value in agriculture for improving soil properties and in reducing the hazards caused by soil acidification and in naturally acidic soils. However, the ameliorant effects of biochars on acid soils and the mechanisms involved have not previously been critically reviewed. Here we summarize the phenomena, and mechanisms involved in the improvement of soil acidity by biochars, the alleviation of aluminum toxicity, the enhancement of nutrient availability, and changes in nitrification by collating data in the literature. In addition, the agronomic effectiveness and environmental concerns in the incorporation of biochar and other soil additives (i.e. lime, industrial by-products, organic wastes and plant residues) to acid soils are systemically compared. We conclude that biochar is a potentially effective amendment to reverse or to prevent acidification in acid soils. Finally, perspectives for further research in terms of soil acidification are presented to address some issues that are still poorly understood and/or highly controversial.
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Affiliation(s)
- Zhongmin Dai
- Institute of Soil and Water Resources and Environmental Science, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou 310058, China
| | - Xiaojie Zhang
- Institute of Soil and Water Resources and Environmental Science, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou 310058, China
| | - C Tang
- Department of Animal, Plant and Soil Sciences, La Trobe University, Melbourne Campus, Bundoora, VIC 3086, Australia
| | - Niaz Muhammad
- Institute of Soil and Water Resources and Environmental Science, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou 310058, China
| | - Jianjun Wu
- Institute of Soil and Water Resources and Environmental Science, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou 310058, China
| | - Philip C Brookes
- Institute of Soil and Water Resources and Environmental Science, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou 310058, China
| | - Jianming Xu
- Institute of Soil and Water Resources and Environmental Science, Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Zhejiang University, Hangzhou 310058, China; Department of Animal, Plant and Soil Sciences, La Trobe University, Melbourne Campus, Bundoora, VIC 3086, Australia.
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35
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Naylor D, Coleman-Derr D. Drought Stress and Root-Associated Bacterial Communities. FRONTIERS IN PLANT SCIENCE 2017; 8:2223. [PMID: 29375600 PMCID: PMC5767233 DOI: 10.3389/fpls.2017.02223] [Citation(s) in RCA: 222] [Impact Index Per Article: 31.7] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 08/17/2017] [Accepted: 12/18/2017] [Indexed: 05/20/2023]
Abstract
Root-associated bacterial communities play a vital role in maintaining health of the plant host. These communities exist in complex relationships, where composition and abundance of community members is dependent on a number of factors such as local soil chemistry, plant genotype and phenotype, and perturbations in the surrounding abiotic environment. One common perturbation, drought, has been shown to have drastic effects on bacterial communities, yet little is understood about the underlying causes behind observed shifts in microbial abundance. As drought may affect root bacterial communities both directly by modulating moisture availability, as well as indirectly by altering soil chemistry and plant phenotypes, we provide a synthesis of observed trends in recent studies and discuss possible directions for future research that we hope will provide for more knowledgeable predictions about community responses to future drought events.
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Affiliation(s)
- Dan Naylor
- Department of Plant and Microbial Biology, University of California, Berkeley, Berkeley, CA, United States
- Plant Gene Expression Center, United States Department of Agriculture-Agricultural Research Service, Albany, CA, United States
| | - Devin Coleman-Derr
- Department of Plant and Microbial Biology, University of California, Berkeley, Berkeley, CA, United States
- Plant Gene Expression Center, United States Department of Agriculture-Agricultural Research Service, Albany, CA, United States
- *Correspondence: Devin Coleman-Derr,
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Rughöft S, Herrmann M, Lazar CS, Cesarz S, Levick SR, Trumbore SE, Küsel K. Community Composition and Abundance of Bacterial, Archaeal and Nitrifying Populations in Savanna Soils on Contrasting Bedrock Material in Kruger National Park, South Africa. Front Microbiol 2016; 7:1638. [PMID: 27807431 PMCID: PMC5069293 DOI: 10.3389/fmicb.2016.01638] [Citation(s) in RCA: 18] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 06/08/2016] [Accepted: 09/30/2016] [Indexed: 11/13/2022] Open
Abstract
Savannas cover at least 13% of the global terrestrial surface and are often nutrient limited, especially by nitrogen. To gain a better understanding of their microbial diversity and the microbial nitrogen cycling in savanna soils, soil samples were collected along a granitic and a basaltic catena in Kruger National Park (South Africa) to characterize their bacterial and archaeal composition and the genetic potential for nitrification. Although the basaltic soils were on average 5 times more nutrient rich than the granitic soils, all investigated savanna soil samples showed typically low nutrient availabilities, i.e., up to 38 times lower soil N or C contents than temperate grasslands. Illumina MiSeq amplicon sequencing revealed a unique soil bacterial community dominated by Actinobacteria (20-66%), Chloroflexi (9-29%), and Firmicutes (7-42%) and an increase in the relative abundance of Actinobacteria with increasing soil nutrient content. The archaeal community reached up to 14% of the total soil microbial community and was dominated by the thaumarchaeal Soil Crenarchaeotic Group (43-99.8%), with a high fraction of sequences related to the ammonia-oxidizing genus Nitrosopshaera sp. Quantitative PCR targeting amoA genes encoding the alpha subunit of ammonia monooxygenase also revealed a high genetic potential for ammonia oxidation dominated by archaea (~5 × 107 archaeal amoA gene copies g-1 soil vs. mostly < 7 × 104 bacterial amoA gene copies g-1 soil). Abundances of archaeal 16S rRNA and amoA genes were positively correlated with soil nitrate, N and C contents. Nitrospira sp. was detected as the most abundant group of nitrite oxidizing bacteria. The specific geochemical conditions and particle transport dynamics at the granitic catena were found to affect soil microbial communities through clay and nutrient relocation along the hill slope, causing a shift to different, less diverse bacterial and archaeal communities at the footslope. Overall, our results suggest a strong effect of the savanna soils' nutrient scarcity on all microbial communities, resulting in a distinct community structure that differs markedly from nutrient-rich, temperate grasslands, along with a high relevance of archaeal ammonia oxidation in savanna soils.
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Affiliation(s)
- Saskia Rughöft
- Chair of Aquatic Geomicrobiology, Institute of Ecology, Friedrich Schiller University Jena Jena, Germany
| | - Martina Herrmann
- Chair of Aquatic Geomicrobiology, Institute of Ecology, Friedrich Schiller University JenaJena, Germany; German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-LeipzigLeipzig, Germany
| | - Cassandre S Lazar
- Chair of Aquatic Geomicrobiology, Institute of Ecology, Friedrich Schiller University Jena Jena, Germany
| | - Simone Cesarz
- German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-LeipzigLeipzig, Germany; Institute of Biology, Leipzig UniversityLeipzig, Germany
| | - Shaun R Levick
- Biogeochemical Processes, Max Planck Institute for Biogeochemistry Jena, Germany
| | - Susan E Trumbore
- Biogeochemical Processes, Max Planck Institute for Biogeochemistry Jena, Germany
| | - Kirsten Küsel
- Chair of Aquatic Geomicrobiology, Institute of Ecology, Friedrich Schiller University JenaJena, Germany; German Centre for Integrative Biodiversity Research (iDiv) Halle-Jena-LeipzigLeipzig, Germany
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37
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Niklaus PA, Le Roux X, Poly F, Buchmann N, Scherer-Lorenzen M, Weigelt A, Barnard RL. Plant species diversity affects soil–atmosphere fluxes of methane and nitrous oxide. Oecologia 2016; 181:919-30. [DOI: 10.1007/s00442-016-3611-8] [Citation(s) in RCA: 47] [Impact Index Per Article: 5.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/20/2015] [Accepted: 03/08/2016] [Indexed: 12/01/2022]
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38
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Simonin M, Le Roux X, Poly F, Lerondelle C, Hungate BA, Nunan N, Niboyet A. Coupling Between and Among Ammonia Oxidizers and Nitrite Oxidizers in Grassland Mesocosms Submitted to Elevated CO2 and Nitrogen Supply. MICROBIAL ECOLOGY 2015; 70:809-18. [PMID: 25877793 DOI: 10.1007/s00248-015-0604-9] [Citation(s) in RCA: 21] [Impact Index Per Article: 2.3] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 07/29/2014] [Accepted: 03/23/2015] [Indexed: 05/25/2023]
Abstract
Many studies have assessed the responses of soil microbial functional groups to increases in atmospheric CO2 or N deposition alone and more rarely in combination. However, the effects of elevated CO2 and N on the (de)coupling between different microbial functional groups (e.g., different groups of nitrifiers) have been barely studied, despite potential consequences for ecosystem functioning. Here, we investigated the short-term combined effects of elevated CO2 and N supply on the abundances of the four main microbial groups involved in soil nitrification: ammonia-oxidizing archaea (AOA), ammonia-oxidizing bacteria (AOB), and nitrite-oxidizing bacteria (belonging to the genera Nitrobacter and Nitrospira) in grassland mesocosms. AOB and AOA abundances responded differently to the treatments: N addition increased AOB abundance, but did not alter AOA abundance. Nitrobacter and Nitrospira abundances also showed contrasted responses to the treatments: N addition increased Nitrobacter abundance, but decreased Nitrospira abundance. Our results support the idea of a niche differentiation between AOB and AOA, and between Nitrobacter and Nitrospira. AOB and Nitrobacter were both promoted at high N and C conditions (and low soil water content for Nitrobacter), while AOA and Nitrospira were favored at low N and C conditions (and high soil water content for Nitrospira). In addition, Nitrobacter abundance was positively correlated to AOB abundance and Nitrospira abundance to AOA abundance. Our results suggest that the couplings between ammonia and nitrite oxidizers are influenced by soil N availability. Multiple environmental changes may thus elicit rapid and contrasted responses between and among the soil ammonia and nitrite oxidizers due to their different ecological requirements.
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Affiliation(s)
- Marie Simonin
- Institute of Ecology and Environmental Sciences - Paris, UMR 7618 Université Pierre et Marie Curie/CNRS/AgroParisTech, 78850, Thiverval Grignon, France
- Microbial Ecology Center, Université de Lyon/Université Lyon 1/CNRS/INRA, UMR CNRS 5557, USC INRA 1364, 69622, Villeurbanne, France
| | - Xavier Le Roux
- Microbial Ecology Center, Université de Lyon/Université Lyon 1/CNRS/INRA, UMR CNRS 5557, USC INRA 1364, 69622, Villeurbanne, France
| | - Franck Poly
- Microbial Ecology Center, Université de Lyon/Université Lyon 1/CNRS/INRA, UMR CNRS 5557, USC INRA 1364, 69622, Villeurbanne, France
| | - Catherine Lerondelle
- Microbial Ecology Center, Université de Lyon/Université Lyon 1/CNRS/INRA, UMR CNRS 5557, USC INRA 1364, 69622, Villeurbanne, France
| | - Bruce A Hungate
- Center for Ecosystem Science and Society and Department of Biological Sciences, Northern Arizona University, Flagstaff, AZ, 86011, USA
| | - Naoise Nunan
- Institute of Ecology and Environmental Sciences - Paris, UMR 7618 Université Pierre et Marie Curie/CNRS/AgroParisTech, 78850, Thiverval Grignon, France
| | - Audrey Niboyet
- Institute of Ecology and Environmental Sciences - Paris, UMR 7618 Université Pierre et Marie Curie/CNRS/AgroParisTech, 78850, Thiverval Grignon, France.
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Mariotte P, Robroek BJM, Jassey VEJ, Buttler A. Subordinate plants mitigate drought effects on soil ecosystem processes by stimulating fungi. Funct Ecol 2015. [DOI: 10.1111/1365-2435.12467] [Citation(s) in RCA: 30] [Impact Index Per Article: 3.3] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 01/08/2023]
Affiliation(s)
- Pierre Mariotte
- Centre for Carbon, Water and Food The University of Sydney 380 Werombi Rd Camden NSW 2570 Australia
- Department of Environmental Science, Policy and Management University of California Berkeley Berkeley California 94720 USA
| | - Bjorn J. M. Robroek
- Laboratory of Ecological Systems (ECOS) Ecole Polytechnique Fédérale de Lausanne EPFL School of Architecture, Civil and Environmental Engineering (ENAC) Station 2 1015 Lausanne Switzerland
- Swiss Federal Institute for Forest Snow and Landscape Research (WSL) Site Lausanne, Station 2 1015 Lausanne Switzerland
| | - Vincent E. J. Jassey
- Laboratory of Ecological Systems (ECOS) Ecole Polytechnique Fédérale de Lausanne EPFL School of Architecture, Civil and Environmental Engineering (ENAC) Station 2 1015 Lausanne Switzerland
- Swiss Federal Institute for Forest Snow and Landscape Research (WSL) Site Lausanne, Station 2 1015 Lausanne Switzerland
| | - Alexandre Buttler
- Laboratory of Ecological Systems (ECOS) Ecole Polytechnique Fédérale de Lausanne EPFL School of Architecture, Civil and Environmental Engineering (ENAC) Station 2 1015 Lausanne Switzerland
- Swiss Federal Institute for Forest Snow and Landscape Research (WSL) Site Lausanne, Station 2 1015 Lausanne Switzerland
- Laboratoire de Chrono‐Environnement UMR CNRS 6249 UFR des Sciences et Techniques Université de Franche‐Comté 16 route de Gray F‐25030 Besançon France
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40
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Xi N, Carrère P, Bloor JMG. Plant community responses to precipitation and spatial pattern of nitrogen supply in an experimental grassland ecosystem. Oecologia 2015; 178:329-38. [PMID: 25783490 DOI: 10.1007/s00442-015-3289-3] [Citation(s) in RCA: 13] [Impact Index Per Article: 1.4] [Reference Citation Analysis] [Abstract] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/23/2014] [Accepted: 03/03/2015] [Indexed: 11/24/2022]
Abstract
Recent work suggests that soil nutrient heterogeneity may modulate plant responses to drivers of global change, but interactions between N heterogeneity and changes in rainfall regime remain poorly understood. We used a model grassland system to investigate the interactive effects of N application pattern (homogeneous, heterogeneous) and precipitation-magnitude manipulation during the growing season (control, +50 % rainfall, -50 % rainfall) on aboveground biomass and plant community dominance patterns. Our study resulted in four major findings: patchy N addition increased within-plot variability in plant size structure at the species level, but did not alter total aboveground biomass; patchy N addition increased community dominance and caused a shift in the ranking of subordinate plant species; unlike community-level biomass, plant species differed in their biomass response to the rainfall treatments; and neither aboveground biomass nor community dominance showed significant interactions between N pattern and rainfall manipulation, suggesting that grassland responses to patchy N inputs are insensitive to water addition or rainfall reduction in our temperate study system. Overall, our results indicate that the spatial pattern of N inputs has greater effects on species biomass variability and community dominance than on aboveground production. These short-term changes in plant community structure may have significant implications for longer-term patterns of vegetation dynamics and plant-soil feedbacks. Moreover our results suggest that the magnitude of precipitation during the growing season plays a limited role in grassland responses to heterogeneous organic N inputs, emphasizing the need to consider other components of precipitation change in future heterogeneity studies.
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Affiliation(s)
- Nianxun Xi
- Grassland Ecosystem Research Unit, INRA-UREP, 5 Chemin de Beaulieu, 63039, Clermont-Ferrand, France
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41
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Thion C, Prosser JI. Differential response of nonadapted ammonia-oxidising archaea and bacteria to drying-rewetting stress. FEMS Microbiol Ecol 2014; 90:380-9. [PMID: 25070168 DOI: 10.1111/1574-6941.12395] [Citation(s) in RCA: 30] [Impact Index Per Article: 3.0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/23/2014] [Revised: 07/24/2014] [Accepted: 07/24/2014] [Indexed: 11/30/2022] Open
Abstract
Climate change is expected to increase the frequency of severe drought events followed by heavy rainfall, which will influence growth and activity of soil microorganisms, through osmotic stress and changes in nutrient concentration. There is evidence of rapid recovery of processes and adaptation of communities in soils regularly experiencing drying/rewetting and lower resistance and resilience in nonadapted soils. A microcosm-based study of ammonia-oxidising archaea (AOA) and bacteria (AOB), employing a grassland soil that rarely experiences drought, was used to test this hypothesis and also whether AOB were more resistant and resilient, through greater tolerance of high ammonia concentrations produced during drought and rewetting. Treated soils were dried, incubated for 3 weeks, rewetted, incubated for a further 3 weeks and compared to untreated soils, maintained at a constant moisture content. Nitrate accumulation and AOA and AOB abundance (abundance of respective amoA genes) and community composition (DGGE analysis of AOA amoA and AOB 16S rRNA genes) were poorly adapted to drying-rewetting. AOA abundance and community composition were less resistant than AOB during drought and less resilient after rewetting, at times when ammonium concentration was higher. Data provide evidence for poor adaptation of microbial communities and processes to drying-rewetting in soils with no history of drought and indicate niche differentiation of AOA and AOB associated with high ammonia concentration.
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Affiliation(s)
- Cécile Thion
- Institute of Biological and Environmental Sciences, University of Aberdeen, Aberdeen, UK
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Sgouridis F, Ullah S. Denitrification potential of organic, forest and grassland soils in the Ribble-Wyre and Conwy River catchments, UK. ENVIRONMENTAL SCIENCE. PROCESSES & IMPACTS 2014; 16:1551-1562. [PMID: 24690876 DOI: 10.1039/c3em00693j] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.1] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/03/2023]
Abstract
Soil denitrification activity can be highly variable due to the effects of varied land use management practices within catchments on the biogeochemical regulators of denitrification. To test this assumption in the context of mixed-use rural catchments, it was hypothesised that the relative magnitude of denitrification activity may be regulated, among others, by a gradient of soil nitrate (low to high) between organic (peat bog, heathland, and acid grassland), forest (coniferous and deciduous), and grassland (improved and semi-improved) rural land use types. The denitrification potential (DP) of organic, forest and grassland soils, in two UK catchments was measured in the laboratory. Land use type significantly (p < 0.05) influenced the DP, which ranged between 0.02 and 63.3 mg N m(-2) h(-1). The averaged DP of organic and forest soils (1.08 mg N m(-2) h(-1)) was 3 and 10 times less than the DP of semi-improved (4.06 mg N m(-2) h(-1)) and improved (12.09 mg N m(-2) h(-1)) grassland soils, respectively; and among others, nitrate correlated positively (p < 0.05) with the DP. The results indicated that the difference in soil nitrate concentration between organic (naturally low in nitrate availability) and grassland soils (nitrate enriched due to land management) partially regulated the extent of DP. In the absence of N fertilisation, except for the atmospheric N deposition, the relatively low net nitrification potential (as a source of nitrate for denitrifiers) of organic and forest soils alone seem to have resulted in lower denitrifier's activity compared to grassland soils. Moreover, the interactions between soil organic carbon, pH, bulk density, water filled pore space, and texture, as these are influenced by the relative degree of land management, exerted additional controls on the DP. The results suggest that land management can have significant effects on denitrification, and thus needs to be considered when modelling and/or predicting the response of denitrification to land use change.
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Affiliation(s)
- Fotis Sgouridis
- School of Physical and Geographical Sciences, Keele University, Staffordshire, ST5 5BG, UK.
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Merbold L, Eugster W, Stieger J, Zahniser M, Nelson D, Buchmann N. Greenhouse gas budget (CO2, CH4 and N2O) of intensively managed grassland following restoration. GLOBAL CHANGE BIOLOGY 2014; 20:1913-1928. [PMID: 24395474 DOI: 10.1111/gcb.12518] [Citation(s) in RCA: 40] [Impact Index Per Article: 4.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/26/2013] [Accepted: 12/02/2013] [Indexed: 06/03/2023]
Abstract
The first full greenhouse gas (GHG) flux budget of an intensively managed grassland in Switzerland (Chamau) is presented. The three major trace gases, carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) were measured with the eddy covariance (EC) technique. For CO2 concentrations, an open-path infrared gas analyzer was used, while N2O and CH4 concentrations were measured with a recently developed continuous-wave quantum cascade laser absorption spectrometer (QCLAS). We investigated the magnitude of these trace gas emissions after grassland restoration, including ploughing, harrowing, sowing, and fertilization with inorganic and organic fertilizers in 2012. Large peaks of N2O fluxes (20-50 nmol m(-2) s(-1) compared with a <5 nmol m(-2) s(-1) background) were observed during thawing of the soil after the winter period and after mineral fertilizer application followed by re-sowing in the beginning of the summer season. Nitrous oxide (N2O) fluxes were controlled by nitrogen input, plant productivity, soil water content and temperature. Management activities led to increased variations of N2O fluxes up to 14 days after the management event as compared with background fluxes measured during periods without management (<5 nmol m(-2) s(-1)). Fluxes of CO2 remained small until full plant development in early summer 2012. In contrast, methane emissions showed only minor variations over time. The annual GHG flux budget was dominated by N2O (48% contribution) and CO2 emissions (44%). CH4 flux contribution to the annual budget was only minor (8%). We conclude that recently developed multi-species QCLAS in an EC system open new opportunities to determine the temporal variation of N2O and CH4 fluxes, which further allow to quantify annual emissions. With respect to grassland restoration, our study emphasizes the key role of N2O and CO2 losses after ploughing, changing a permanent grassland from a carbon sink to a significant carbon source.
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Affiliation(s)
- Lutz Merbold
- Department of Environmental Systems Science, ETH Zurich, Universitaetsstr. 2, Zurich, 8092, Switzerland
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Rolli E, Marasco R, Vigani G, Ettoumi B, Mapelli F, Deangelis ML, Gandolfi C, Casati E, Previtali F, Gerbino R, Pierotti Cei F, Borin S, Sorlini C, Zocchi G, Daffonchio D. Improved plant resistance to drought is promoted by the root-associated microbiome as a water stress-dependent trait. Environ Microbiol 2014; 17:316-31. [DOI: 10.1111/1462-2920.12439] [Citation(s) in RCA: 339] [Impact Index Per Article: 33.9] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 09/23/2013] [Accepted: 12/20/2013] [Indexed: 11/28/2022]
Affiliation(s)
- Eleonora Rolli
- Department of Food, Environmental and Nutritional Sciences, DeFENS; University of Milan; Milan Italy
| | - Ramona Marasco
- Department of Food, Environmental and Nutritional Sciences, DeFENS; University of Milan; Milan Italy
| | - Gianpiero Vigani
- Department of Agricultural and Environmental Sciences - Production, Landscape, Agroenergy, DISAA; University of Milan; Milan Italy
| | - Besma Ettoumi
- Laboratory of Microbiology and Active Biomolecules (LMBA); Faculté des Sciences de Tunis; Campus Universitaire; Tunis Tunisia
| | - Francesca Mapelli
- Department of Food, Environmental and Nutritional Sciences, DeFENS; University of Milan; Milan Italy
| | - Maria Laura Deangelis
- Department of Agricultural and Environmental Sciences - Production, Landscape, Agroenergy, DISAA; University of Milan; Milan Italy
| | - Claudio Gandolfi
- Department of Agricultural and Environmental Sciences - Production, Landscape, Agroenergy, DISAA; University of Milan; Milan Italy
| | - Enrico Casati
- Department of Environmental Science; University of Milan Bicocca; Milan Italy
| | - Franco Previtali
- Department of Environmental Science; University of Milan Bicocca; Milan Italy
| | | | | | - Sara Borin
- Department of Food, Environmental and Nutritional Sciences, DeFENS; University of Milan; Milan Italy
| | - Claudia Sorlini
- Department of Food, Environmental and Nutritional Sciences, DeFENS; University of Milan; Milan Italy
| | - Graziano Zocchi
- Department of Agricultural and Environmental Sciences - Production, Landscape, Agroenergy, DISAA; University of Milan; Milan Italy
| | - Daniele Daffonchio
- Department of Food, Environmental and Nutritional Sciences, DeFENS; University of Milan; Milan Italy
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A tribute to Christian Körner for his 25 years of service on the Oecologia editorial board. Oecologia 2013; 171:605-11. [DOI: 10.1007/s00442-012-2586-3] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/23/2012] [Accepted: 12/18/2012] [Indexed: 10/27/2022]
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