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增温对高寒灌丛土壤呼吸不同组分的影响机制
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  • 英文篇名:Influencing Mechanisms of Warming on the Soil Respiration Components in An Alpine Scrubland
  • 作者:马志良 ; 刘美 ; 赵文强
  • 英文作者:MA Zhiliang;LIU Mei;ZHAO Wenqiang;College of Life Science, China West Normal University;Key Laboratory of Mountain Ecological Restoration and Bioresource Utilization & Ecological Restoration/Biodiversity Conservation Key Laboratory of Sichuan Province/Chengdu Institute of Biology, Chinese Academy of Science;Ecological Security and Protection Key Laboratory of Sichuan Province/Mianyang Teacher' College;
  • 关键词:高寒灌丛 ; 增温 ; 土壤呼吸 ; 土壤碳循环
  • 英文关键词:alpine scrub;;warming;;soil respiration;;soil carbon cycling
  • 中文刊名:生态环境学报
  • 英文刊名:Ecology and Environmental Sciences
  • 机构:西华师范大学生命科学学院;中国科学院山地生态恢复与生物资源利用重点实验室/生态恢复与生物多样性保育四川省重点实验室/中国科学院成都生物研究所;生态安全与保护四川省重点实验室/绵阳师范学院;
  • 出版日期:2019-03-18
  • 出版单位:生态环境学报
  • 年:2019
  • 期:03
  • 基金:国家重点研发计划项目(2017YFC0505000);; 国家自然科学基金项目(31570476);; 国家科技基础性工作专项(2015FY110300)
  • 语种:中文;
  • 页:212-218
  • 页数:7
  • CN:44-1661/X
  • ISSN:1674-5906
  • 分类号:S154
摘要
陆地生态系统土壤呼吸对气候变暖的响应研究方面目前还没有一致的结论,其原因可能为土壤呼吸不同组分对土壤温度变化的敏感性及相应的非生物和生物机制存在显著差异。文章分别从非生物因素和生物因素系统地论述了增温对青藏高原东部窄叶鲜卑花(Sibiraea angustata)高寒灌丛土壤呼吸不同组分的影响机制,发现增温可通过提高土壤微生物群落和植物根系的生理活性直接促进土壤异养呼吸和根系呼吸。同时增温能通过改变非生物因子影响土壤呼吸各组分速率,如增温显著提高土壤养分含量和土壤酶活性,进而间接促进土壤呼吸;而增温引起土壤水分含量较小程度的降低不足以抑制土壤呼吸过程。增温还能通过改变植物群落生产和土壤微生物群落结构等生物因子影响土壤呼吸各组分速率,如增温导致植物细根生产量、死亡量和分解速率提高,非根际土壤微生物生物量与活性增加;增温还导致土壤微生物功能群向革兰氏阳性菌和放线菌群落转变,从而导致土壤微生物对土壤惰性有机碳的利用增加。受根际土壤可利用碳含量较高的影响,根际微生物呼吸对增温的响应不敏感,增温对根际微生物生物量的影响也不显著。由此可见,在青藏高原东部高寒灌丛生态系统中,气候变暖将通过改变非生物与生物因子影响土壤呼吸等碳释放过程。以上结果有利于更加全面地认识全球气候变暖背景下高寒灌丛土壤碳循环过程。
        To date, there are no consistent conclusions on the response of soil respiration of terrestrial ecosystem to climatic warming, which s likely due to the significant differences among the temperature sensitivity of soil respiration components and abiotic/biotic factors affecting soil respiration. This study systematically summarized the influencing mechanisms of warming on the soil respiration components in a Sibiraea angustata scrubland on the eastern Qinghai-Tibetan Plateau, China. We found that warming directly increased soil heterotrophic respiration and root respiration due to the significant increase in physiological activity of soil microbial community and plant root system. Simultaneously, warming influenced the rates of soil respiration components by changing the abiotic factors. For example, warming resulted in the significant increase in soil nutrient contents and enzyme activities,which indirectly increased soil respiration. While the decreased soil moisture caused by warming did not enough to inhibit soil respiration. Moreover, warming changed plant community production and soil microbial community structure, such as increased in plant fine root production, mortality and decomposition and soil microbial biomass and activities in the bulk soil, which indirectly influenced soil respiration rates. Furthermore, warming caused the transition of soil microbial functional groups to Gram-positive bacteria and actinomycetes. This phenomenon might lead to the acceleration of soil microbial utilization of soil recalcitrant organic carbon. Due to the higher available carbon contents in the rhizosphere soil, warming had no significant effect on rhizomicrobial respiration and rhizomicrobial community. This shows that climatic warming will affect the carbon release process by changing the abiotic/biotic factors relate to soil respiration in the alpine scrubland on the eastern Qinghai-Tibetan Plateau. These results will improve our understanding of soil carbon cycling process under global climatic warming in these alpine scrub ecosystems.
引文
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