Climate change amplifies gross nitrogen turnover in montane grasslands of Central Europe in both summer and winter seasons
Wang, Changhui1; Chen, Zhe; Unteregelsbacher, Sebastian; Lu, Haiyan; Gschwendtner, Silvia2; Gasche, Rainer; Kolar, Allison; Schloter, Michael2; Kiese, Ralf; Butterbach-Bahl, Klaus
刊名GLOBAL CHANGE BIOLOGY
2016
卷号22期号:9
关键词ammonia-oxidizing archaea ammonia-oxidizing bacteria freeze-thaw frozen soil gross N mineralization gross nitrification montane grassland
ISSN号1354-1013
DOI10.1111/gcb.13353
文献子类Article
英文摘要The carbon- and nitrogen-rich soils of montane grasslands are exposed to above-average warming and to altered precipitation patterns as a result of global change. To investigate the consequences of climatic change for soil nitrogen turnover, we translocated intact plant-soil mesocosms along an elevational gradient, resulting in an increase of the mean annual temperature by approx. 2 degrees C while decreasing precipitation from approx. 1500 to 1000mm. Following three years of equilibration, we monitored the dynamics of gross nitrogen turnover and ammonia-oxidizing bacteria (AOB) and archaea (AOA) in soils over an entire year. Gross nitrogen turnover and gene levels of AOB and AOA showed pronounced seasonal dynamics. Both summer and winter periods equally contributed to cumulative annual N turnover. However, highest gross N turnover and abundance of ammonia oxidizers were observed in frozen soil of the climate change site, likely due to physical liberation of organic substrates and their rapid turnover in the unfrozen soil water film. This effect was not observed at the control site, where soil freezing did not occur due to a significant insulating snowpack. Climate change conditions accelerated gross nitrogen mineralization by 250% on average. Increased N mineralization significantly stimulated gross nitrification by AOB rather than by AOA. However, climate change impacts were restricted to the 2-6cm topsoil and rarely occurred at 12-16cm depth, where generally much lower N turnover was observed. Our study shows that significant mineralization pulses occur under changing climate, which is likely to result in soil organic matter losses with their associated negative impacts on key soil functions. We also show that N cycling processes in frozen soil can be hot moments for N turnover and thus are of paramount importance for understanding seasonal patterns, annual sum of N turnover and possible climate change feedbacks.
学科主题Biodiversity Conservation ; Ecology ; Environmental Sciences
电子版国际标准刊号1365-2486
出版地HOBOKEN
WOS关键词AMMONIA-OXIDIZING ARCHAEA ; NITRIFICATION RATES ; N MINERALIZATION ; GAS FLUXES ; TEMPERATURE SENSITIVITY ; MICROBIAL COMMUNITIES ; SPECIES COMPOSITION ; SEMIARID GRASSLAND ; SATURATED SPRUCE ; OXIDE EMISSIONS
WOS研究方向Science Citation Index Expanded (SCI-EXPANDED)
语种英语
出版者WILEY
WOS记录号WOS:000381077300004
资助机构Helmholtz-BMBF TERENO initiative ; BMBF SUSALPS projectFederal Ministry of Education & Research (BMBF) ; FORKAST project of the Bavarian government ; Humboldt PostDoc Fellowship
内容类型期刊论文
源URL[http://ir.ibcas.ac.cn/handle/2S10CLM1/24508]  
专题植被与环境变化国家重点实验室
作者单位1.Karlsruhe Inst Technol, Inst Meteorol & Climate Res Atmospher Environm Re, D-82467 Garmisch Partenkirchen, Germany
2.Chinese Acad Sci IBCAS, State Key Lab Vegetat & Environm Change, Inst Bot, Beijing 100093, Peoples R China
3.German Res Ctr Environm Hlth GmbH, Res Unit Environm Genom, D-85764 Neuherberg, Germany
推荐引用方式
GB/T 7714
Wang, Changhui,Chen, Zhe,Unteregelsbacher, Sebastian,et al. Climate change amplifies gross nitrogen turnover in montane grasslands of Central Europe in both summer and winter seasons[J]. GLOBAL CHANGE BIOLOGY,2016,22(9).
APA Wang, Changhui.,Chen, Zhe.,Unteregelsbacher, Sebastian.,Lu, Haiyan.,Gschwendtner, Silvia.,...&Dannenmann, Michael.(2016).Climate change amplifies gross nitrogen turnover in montane grasslands of Central Europe in both summer and winter seasons.GLOBAL CHANGE BIOLOGY,22(9).
MLA Wang, Changhui,et al."Climate change amplifies gross nitrogen turnover in montane grasslands of Central Europe in both summer and winter seasons".GLOBAL CHANGE BIOLOGY 22.9(2016).
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