首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Negative responses of ecosystem autotrophic and heterotrophic respiration to experimental warming in a Tibetan semi-arid alpine steppe
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Negative responses of ecosystem autotrophic and heterotrophic respiration to experimental warming in a Tibetan semi-arid alpine steppe

机译:生态系统自养和异养呼吸对藏藏半干旱高原草原实验变暖的负响应

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摘要

Evaluating the responses of ecosystem respiration (Re) and its components to climate change is crucial for predicting terrestrial carbon cycling, particularly for the alpine grassland ecosystems. However, effects of climatic warming on ecosystem heterotrophic respiration (Rh) and autotrophic respiration (Ra) remain poorly understood in semi-arid alpine grasslands. A field manipulative experiment was conducted to investigate the effects of experimental warming on total Re, Rh and Ra in a Tibetan semi-arid alpine steppe during growing seasons of 2013 and 2014. Our results showed that warming decreased seasonal Re, Rh and Ra by 29%, 37% and 13%, respectively. However, warming tended to increase the contribution of Ra to Re (Ra/Re) but decrease that of Rh to Re (Rh/Re). Negative responses of Re was closely related to the changes in plant biomass and soil microbial biomass carbon. The apparent Q(10) values of Ra were higher than those of Re and Rh, with the Q(10) values ranked as Ra > Re > Rh. Warming decreased the apparent Q(10) values of Re and the two components. Our results emphasize that Re and its components respond negatively to experimental warming, and soil carbon loss has the potential to be less under future climatic warming in the Tibetan semi-arid alpine steppe.
机译:评估生态系统呼吸(RE)及其组件对气候变化的响应对于预测陆地碳循环至关重要,特别是对于高山草原生态系统。然而,气候变暖对生态系统异养呼吸(RH)和自养呼吸(RA)的影响仍然在半干旱高山草原中仍然知之甚少。进行了现场操纵实验,以研究2013年和2014年生长季节的藏半干旱高原干草原中实验升温的影响。我们的结果表明,温暖季节性re,Rh和Ra达到29 %,37%和13%。然而,加热倾向于增加RA至RE(RA / RE)的贡献,但将RH的贡献降低到RE(RH / RE)。 RE的负响应与植物生物质和土壤微生物碳碳的变化密切相关。 RA的表观Q(10)值高于RE和RH的值,Q(10)值排名为RA> RE> RH。变暖降低了Re和两个组分的表观Q(10)值。我们的结果强调RE及其组件对实验变暖的负面响应,土壤碳损失在藏族半干旱高原草原中未来气候变暖的可能性较少。

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