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The optimal CO(2) concentrations for the growth of three perennial grass species

BACKGROUND: Grasslands are one of the most representative vegetation types accounting for about 20% of the global land area and thus the response of grasslands to climate change plays a pivotal role in terrestrial carbon balance. However, many current climate change models, based on earlier results...

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Detalles Bibliográficos
Autores principales: Zheng, Yunpu, Li, Fei, Hao, Lihua, Shedayi, Arshad Ali, Guo, Lili, Ma, Chao, Huang, Bingru, Xu, Ming
Formato: Online Artículo Texto
Lenguaje:English
Publicado: BioMed Central 2018
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5799915/
https://www.ncbi.nlm.nih.gov/pubmed/29402224
http://dx.doi.org/10.1186/s12870-018-1243-3
Descripción
Sumario:BACKGROUND: Grasslands are one of the most representative vegetation types accounting for about 20% of the global land area and thus the response of grasslands to climate change plays a pivotal role in terrestrial carbon balance. However, many current climate change models, based on earlier results of the doubling-CO(2) experiments, may overestimate the CO(2) fertilization effect, and as a result underestimate the potentially effects of future climate change on global grasslands when the atmospheric CO(2) concentration goes beyond the optimal level. Here, we examined the optimal atmospheric CO(2) concentration effect on CO(2) fertilization and further on the growth of three perennial grasses in growth chambers with the CO(2) concentration at 400, 600, 800, 1000, and 1200 ppm, respectively. RESULTS: All three perennial grasses featured an apparent optimal CO(2) concentration for growth. Initial increases in atmospheric CO(2) concentration substantially enhanced the plant biomass of the three perennial grasses through the CO(2) fertilization effect, but this CO(2) fertilization effect was dramatically compromised with further rising atmospheric CO(2) concentration beyond the optimum. The optimal CO(2) concentration for the growth of tall fescue was lower than those of perennial ryegrass and Kentucky bluegrass, and thus the CO(2) fertilization effect on tall fescue disappeared earlier than the other two species. By contrast, the weaker CO(2) fertilization effect on the growth of perennial ryegrass and Kentucky bluegrass was sustained for a longer period due to their higher optimal CO(2) concentrations than tall fescue. The limiting effects of excessively high CO(2) concentrations may not only associate with changes in the biochemical and photochemical processes of photosynthesis, but also attribute to the declines in stomatal conductance and nitrogen availability. CONCLUSIONS: In this study, we found apparent differences in the optimal CO(2) concentrations for the growth of three grasses. These results suggest that the growth of different types of grasses may respond differently to future elevated CO(2) concentrations through the CO(2) fertilization effect, and thus potentially alter the community composition and structure of grasslands. Meanwhile, our results may also be helpful for improving current process-based ecological models to more accurately predict the structure and function of grassland ecosystems under future rising atmospheric CO(2) concentration and climate change scenarios.