"nitrogen deposition" "climate warming"
212405271
Effects of climate warming and nitrogen deposition on subtropical montane ponds (central China) over the last two centuries: Evidence from subfossil chironomids.
Many remote montane ecosystems are experiencing biogeochemical changes driven by warming climate and atmospheric pollution. Compared with circumpolar and temperate lakes, the responses of subtropical montane lakes to these external stressors have been less investigated. Here we present sedimentary multi proxies records (i.e. chironomids, elements and stable isotope of carbon and nitrogen) in 210Pb dated cores from two montane ponds (central China) Before the 1900s, low biomass and the dominance of opportunistic species (e.g. Chironomus anthracinus type) in both ponds might be in response to cold and harsh condition. Thereafter, chironomid communities in both ponds experienced pronounced shifts. Nutrient tolerant/warm adapted species (e.g. Chironomus sp. Polypedilum nubeculosum type and Endochironomus impar type) proliferated and biomass increased synchronously after the 1900s, suggestive of favorable condition for chironomid growth. Redundancy analyses revealed that changes in chironomid communities in both ponds were significantly correlated with rising temperature and d15N depletion. Prolonged growing season and nitrogen subsidy would increase primary productivity, and hence enhancing food availability for chironomids. Catchment mediated indirect effects of warming and nitrogen deposition, such as hydrological changes and terrestrial organic matter inputs, would impose further influences on chironomid communities. Taken together, the combined effects of climate warming and nitrogen deposition have caused significant shifts in primary consumers of these montane ponds, and imposed cascading effects on structure and function of subtropical montane aquatic ecosystems.
Environmental pollution
Ting Zheng Yanmin Cao Jia Peng Xue Bai Xu Chen
229418476
Interactive effect of climate warming and nitrogen deposition may shift the dynamics of native and invasive species
Projections of invasive species expansion under a warmer world often do not explicitly consider the concurring nitrogen (N) deposition. It remains largely unknown how the convoluted effect of climate warming and N deposition will shift the native and invasive species dynamics. Here, we hypothesize that the concurring increases in N and temperature would promote growth of invasive species greater than that of native species. A controlled greenhouse experiment was conducted to quantify the growth response of an invasive species (Solidago canadensis L. and a co existing native species (Artemisia argyi Levl. et Van) under the effects of climate warming, N deposition and their interactions. Due to the strong positive effect of N addition, the interactive effect of temperature increase and N addition resulted in an overall significant increase in growth of both invasive and native species, demonstrating that these manipulations may make microhabitats more favorable to plant growth. However, the relative increases in biomass, height and diameter of invasive S. canadensis were significantly lower than those of native A. argyi. This suggests that the vegetative growth superiority of invasive S. canadensis over the native species A. argyi is reduced by the enhanced N availability in the warmer world. Therefore, the inclusion of N deposition may mitigate the projection of invasive species S. canadensis expansion under climate warming.
Guang-Qian Ren Chris B Zou Ling-Yun Wan Jacob H Johnson Jin-ru Li Lan Zhu Shanshan Qi Zhicong Dai Hai-yan Zhang Dao-Lin Du
109910171
Simulated climate warming and nitrogen deposition influence leaf traits and leaf trait spectrum in Solidago canadensis from China and North America
Temperature is a key factor that affects plant growth, and nitrogen (N) is an important resource for plant growth and photosynthesis. Changes in temperature and N may strongly influence the functional traits of invasive plants. The aim of this study was to predict the potential invasiveness of invasive plants in response to climate warming and atmospheric N deposition. We conducted a simulated warming and N deposition experiment at Chengdu. In this experiment, we selected Solidago canadensis from China and North America as the focal invader and set up four experimental treatments: 1) ambient, (2) warming (2degC above the ambient) (3) N addition (4 g N m a in the form of NH4NO3) and (4) warming plus N addition. We determined three leaf traits, leaf chlorophyll content, leaf area, and leaf dry matter content,
Zhou Xiao Hui Zhou Xiaohui Peng Pei Hao Peng Peihao Li Jing Ji Li Jingji
205110710
Nitrogen deposition but not climate warming promotes Deyeuxia angustifolia encroachment in alpine tundra of the Changbai Mountains, Northeast China.
Vegetation in the alpine tundra area of the Changbai Mountains, one of two alpine tundra areas in China, has undergone great changes in recent decades. The aggressive herb species Deyeuxia angustifolia (Komarov) Y. L. Chang, a narrow leaf small reed, was currently encroaching upon the alpine landscape and threatening tundra biota. The alpine tundra of the Changbai Mountains has been experiencing a warmer climate and receiving a high load of atmospheric nitrogen deposition. In this study, we aimed to assess the respective roles of climate warming and atmospheric nitrogen deposition in promoting the upward encroachment of D. angustifolia. We conducted experiments for three years to examine the response of D. angustifolia and a native alpine shrub, Rhododendron chrysanthum, to the conditions in which temperature and nitrogen were increased. Treatments consisting of temperature increase, nitrogen addition, temperature increase combined with nitrogen addition, and controls were conducted on the D. angustifolia communities with three encroachment levels (low, medium, and high levels) Results showed that 1) D. angustifolia grew in response to added nutrients but did not grow well when temperature increased. R. chrysanthum showed negligible responses to the simulated environmental changes. 2) Compared to R. chrysanthum, D. angustifolia could effectively occupy the above ground space by increasing tillers and growing rapidly by efficiently using nitrogen. The difference in nitrogen uptake abilities between the two species contributed to expansion of D. angustifolia. 3) D. angustifolia encroachment could deeply change the biodiversity of tundra vegetation and may eventually result in the replacement of native biota, especially with nitrogen addition. Our research indicated that nutrient perturbation may be more important than temperature perturbation in promoting D. angustifolia encroachment upon the nutrient and species poor alpine tundra ecosystem in the Changbai Mountains.
The Science of the total environment
Shengwei Zong Ying-hua Jin Jiawei Xu Zhengfang Wu Hongshi He Haibo Du Lin Wang
132976119
A model based investigation of the relative importance of CO2 fertilization, climate warming, nitrogen deposition and land use change on the global terrestrial carbon uptake in the historical period
In this paper, using the fully coupled NCAR Community Earth System Model (CESM1.0.4) we investigate the relative importance of CO2 fertilization, climate warming, anthropogenic nitrogen deposition, and land use and land cover change (LULCC) for terrestrial carbon uptake during the historical period (1850 2005) In our simulations, between the beginning and end of this period, we find an increase in global net primary productivity (NPP) on land of about 4 PgCyr 1 (8.2 with a contribution of 2.3 PgCyr 1 from CO2 fertilization and 2.0 PgCyr 1 from nitrogen deposition. Climate warming also causes NPP to increase by 0.35 PgCyr 1 but LULCC causes a decline of 0.7 PgCyr 1. These results indicate that the recent increase in vegetation productivity is most likely driven by CO2 fertilization and nitrogen deposition. Further, we find that this configuration of CESM projects that the global terrestrial ecosystem has been a net source of carbon during 1850 2005 (release of 45.1 2.4 PgC) largely driven by historical LULCC related CO2 fluxes to the atmosphere. During the recent three decades (early 1970s to early 2000s) however, our model simulations project that the terrestrial ecosystem acts as a sink, taking up about 10 PgC mainly due to CO2 fertilization and nitrogen deposition. Our results are in good qualitative agreement with recent studies that indicate an increase in vegetation production and water use efficiency in the satellite era and that the terrestrial ecosystem has been a net sink for carbon in recent decades.
Climate Dynamics
Narayanappa Devaraju Govindasamy Bala Ken Caldeira Ramakrishna R Nemani
32236296
Genotypic trait variation modifies effects of climate warming and nitrogen deposition on litter mass loss and microbial respiration.
Intraspecific variation in genotypically determined traits can influence ecosystem processes. Therefore, the impact of climate change on ecosystems may depend, in part, on the distribution of plant genotypes. Here we experimentally assess effects of climate warming and excess nitrogen supply on litter decomposition using 12 genotypes of a cosmopolitan foundation species collected across a 2100 km latitudinal gradient and grown in a common garden. Genotypically determined litter chemistry traits varied substantially within and among geographic regions, which strongly affected decomposition and the magnitude of warming effects, as warming accelerated litter mass loss of high nutrient, but not low nutrient, genotypes. Although increased nitrogen supply alone had no effect on decomposition, it strongly accelerated litter mass loss of all genotypes when combined with warming. Rates of microbial respiration associated with the leaf litter showed nearly identical responses as litter mass loss. These results highlight the importance of interactive effects of environmental factors and suggest that loss or gain of genetic variation associated with key phenotypic traits can buffer, or exacerbate, the impact of global change on ecosystem process rates in the future.
Global change biology
Jes Hines Marta Reyes Thomas J Mozder Mark O Gessner
54995915
Influence of climate warming and nitrogen deposition on soil phosphorus composition and phosphorus availability in a temperate grassland, China
Climate warming and nitrogen (N) deposition change ecosystem processes, structure, and functioning whereas the phosphorus (P) composition and availability directly influence the ecosystem structure under conditions of N deposition. In our study, four treatments were designed, including a control, diurnal warming (DW) N deposition (ND) and combined warming and N deposition (WN) The effects of DW, ND, and WN on P composition were studied by 31P nuclear magnetic resonance (31P NMR) spectroscopy in a temperate grassland region of China. The results showed that the N deposition decreased the soil pH and total N (TN) concentration but increased the soil Olsen P concentration. The solution state 31P NMR analysis showed that the DW, ND and WN treatments slightly decreased the proportion of orthophosphate and increased that of the monoesters. An absence of myo inositol phosphate in the DW, ND and WN treatments was observed compared with the control. Furthermore, the DW, ND and WN treatments significantly decreased the recovery of soil P in the NaOH EDTA solution by 17% 20% The principal component analysis found that the soil pH was positively correlated with the P recovery in the NaOH EDTA solution. Therefore, the decreased soil P recovery in the DW and ND treatments might be caused by an indirect influence on the soil pH. Additionally, the soil moisture content was the key factor limiting the available P. The positive correlation of total carbon (TC) and TN with the soil P composition indicated the influence of climate warming and N deposition on the biological processes in the soil P cycling.
Journal of Arid Land
Guangna Zhang Zhen-hua Chen Aiming Zhang Lijun Chen Zhijie Wu
21718494
BVOCs emission in a semi arid grassland under climate warming and nitrogen deposition
Biogenic volatile organic compounds (BVOCs) profoundly affect atmospheric chemistry and ecosystem functioning. BVOCs emission and their responses to global change are still unclear in grasslands, which cover one quarter of the Earth's land surface and are currently undergoing the largest changes. Over two growing seasons, we conducted a field experiment in a semi arid grassland (Inner Mongolia, China) to examine the emission and the responses of BVOCs emissions to warming and nitrogen deposition. The natural emission rate (NER) of monoterpene (dominant BVOCs here) is 107 16 mu g m( 2) h( 1) in drought 2007, and 266 53 mu g m( 2) h( 1) in wet 2008, respectively. Warming decreased the standard emission factor (SEF) by 24% in 2007, while it increased by 43% in 2008. The exacerbated soil moisture loss caused by warming in dry season might be responsible for the decrease of SEF in 2007. A possible threshold of soil moisture (8.2% (v/v) which controls the direction of warming effects on monoterpene emission, existed in the semiarid grassland. Nitrogen deposition decreased the coverage of Artemisia frigida and hence reduced the NER by 24% across the two growing seasons. These results suggest that the grasslands dominated by the extended Artemisia frigida are an important source for BVOCs, while the responses of their emissions to global changes are more uncertain since they depend on multifactorial in situ conditions.
Hongjun Wang Jianyang Xia Yujing Mu Linmei Nie Xingguo Han Shiqiang Wan
128224585
"Biogeochemical impacts of climate warming and atmospheric nitrogen deposition in peatlands: an aboveground belowground perspective "(Plenary speaker)
Luca Bragazza
128080344
Climate warming and atmospheric nitrogen deposition biogeochemical effects through plant soil interactions
Luca Bragazza