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Plant production, and carbon and nitrogen source pools, are strongly intensified by experimental warming in alpine ecosystems in the Qinghai-Tibet Plateau

机译:在青藏高原的高山生态系统中,实验性变暖极大地加强了植物的生产以及碳和氮源库。

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摘要

The aim of this study was to assess initial effects of warming on the nutrient pools of carbon and nitrogen of two most widespread ecosystem types, swamp meadow and alpine meadow, in the Qinghai-Tibet Plateau, China. The temperature of the air and upper-soil layer was passively increased using open-top chambers (OTCs) with two different temperature elevations. We analyzed air and soil temperature, soil moisture, biomass, microbial biomass, and nutrient dynamics after 2 years of warming. The use of OTCs clearly raised temperature and decreased soil moisture. The aboveground plant and root biomass increased in all OTCs in two meadows. A small temperature increase in OTCs resulted in swamp meadow acting as a net carbon sink and alpine meadow as a net source, and further warming intensified this processes, at least in a short term. On balance, the alpine ecosystems in the Fenghuoshan region acted as a carbon source.
机译:这项研究的目的是评估气候变暖对青藏高原两种最普遍的生态系统类型沼泽和高寒草甸碳氮养分池的初步影响。空气和上层土壤的温度通过使用具有两个不同温度升高的开放式顶棚(OTC)被动提高。我们分析了变暖2年后的空气和土壤温度,土壤湿度,生物量,微生物生物量以及养分动态。使用OTC明显提高了温度,减少了土壤湿度。在两个草甸的所有OTC中,地上植物和根系生物量均增加。 OTC的温度略有升高,导致沼泽草甸充当净碳汇,高山草甸充当净碳源,进一步的升温至少在短期内加剧了这一过程。总的来说,风火山山地区的高山生态系统是碳源。

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