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变暖和添加氮对青藏高原高寒草甸生态系统呼吸的影响:冬季变暖的重要性

The effects of warming and nitrogen addition on ecosystem respiration in a Tibetan alpine meadow: The significance of winter warming.

作者信息

Zong Ning, Geng Shoubao, Duan Cheng, Shi Peili, Chai Xi, Zhang Xianzhou

机构信息

Lhasa National Ecological Research Station Key Laboratory of Ecosystem Network Observation and Modelling Institute of Geographic Sciences and Natural Resources Research Chinese Academy of Sciences Beijing China.

University of Chinese Academy of Sciences Beijing China.

出版信息

Ecol Evol. 2018 Sep 5;8(20):10113-10125. doi: 10.1002/ece3.4484. eCollection 2018 Oct.

Abstract

In recent decades, global warming has become an indisputable fact on the Tibetan Plateau. Alpine ecosystems are very sensitive to global warming, and the impact may depend on the degree of atmospheric nitrogen (N) deposition. The previous studies have paid more attention to year-round warming, but the effect of winter warming has been unstudied. In this study, a manipulative experiment was conducted, consisting of warming and N addition. It was carried out since 2010 in an alpine meadow, and three types of warming treatments were set up: no warming (NW), year-round (YW), and winter warming (WW). Warming significantly increased air and soil temperature, but decreased soil moisture. Under no N addition, YW showed significantly decreased ecosystem respiration (Reco) in 2012, and WW decreased Reco in 2014. Under N addition, neither YW nor WW had significant effects on Reco, indicating that N addition compensated the negative effect of warming on Reco. Annually, YW and WW decreased ecosystem carbon (C) emissions, and the extent of the reduction was even larger under WW. Under no N addition, both YW and WW significantly decreased aboveground biomass. Moreover, especially under no N, YW and WW significantly decreased soil inorganic N. WW also had negative effects on soil microbial biomass C. Structure equation modeling showed that soil moisture was the most important factors controlling Reco, and soil inorganic N content and microbial biomass C could explain 46.6% and 16.8% of the variation of Reco. The findings indicate that soil property changes under warming had substantial effects on ecosystem C efflux. The inhibitory effects of winter warming on ecosystem C efflux were mainly attributed to the decline of soil N and microbial biomass. Thus, the effects of winter warming on ecosystem C emissions in this semiarid alpine meadow are not as serious as expected and largely depend on N deposition.

摘要

近几十年来,全球变暖已成为青藏高原上一个无可争议的事实。高山生态系统对全球变暖非常敏感,其影响可能取决于大气氮(N)沉降的程度。以往的研究更多地关注全年变暖,但冬季变暖的影响尚未得到研究。在本研究中,进行了一项控制实验,包括增温与添加氮。该实验自2010年起在一个高山草甸中开展,设置了三种增温处理:不增温(NW)、全年增温(YW)和冬季增温(WW)。增温显著提高了空气和土壤温度,但降低了土壤湿度。在不添加氮的情况下,YW在2012年显著降低了生态系统呼吸(Reco),WW在2014年降低了Reco。在添加氮的情况下,YW和WW对Reco均无显著影响,表明添加氮补偿了增温对Reco的负面影响。每年,YW和WW都减少了生态系统碳(C)排放,且WW下的减少幅度更大。在不添加氮的情况下,YW和WW均显著降低了地上生物量。此外,特别是在不添加氮的情况下,YW和WW显著降低了土壤无机氮。WW对土壤微生物生物量C也有负面影响。结构方程模型表明,土壤湿度是控制Reco的最重要因素,土壤无机氮含量和微生物生物量C可以解释Reco变异的46.6%和16.8%。研究结果表明,变暖下土壤性质的变化对生态系统碳通量有重大影响。冬季变暖对生态系统碳通量的抑制作用主要归因于土壤氮和微生物生物量的下降。因此,冬季变暖对这个半干旱高山草甸生态系统碳排放的影响并不像预期的那么严重,且在很大程度上取决于氮沉降。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5ae2/6206223/a5467a93bfaf/ECE3-8-10113-g001.jpg

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