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水分动态对热带云雾林苔藓植物碳通量的影响。

Effects of moisture dynamics on bryophyte carbon fluxes in a tropical cloud forest.

机构信息

Department of Physical Geography and Ecosystem Science, Lund University, SE-223 62, Lund, Sweden.

Department of Ecology and Environmental Science, Umeå University, SE-901 83, Umeå, Sweden.

出版信息

New Phytol. 2019 Jun;222(4):1766-1777. doi: 10.1111/nph.15727. Epub 2019 Mar 4.

Abstract

Bryophytes play key roles in the ecological function of a number of major world biomes but remain understudied compared with vascular plants. Little is known about bryophyte responses to different aspects of predicted changes in moisture dynamics with climate change. In this study, CO fluxes and photosynthetic light responses were measured within bryophyte mesocosms, being subjected to different amounts, frequencies, and types (mist or rainfall) of water addition, both before and after different periods of complete desiccation. Bryophyte carbon fluxes and photosynthetic light response were generally affected by the magnitude and type, but not frequency, of watering events. Desiccation suppressed bryophyte carbon uptake even after rehydration, and the degree of uptake suppression progressively increased with desiccation duration. Estimated ecosystem-level bryophyte respiration and net carbon uptake were c. 58% and c. 3%, respectively, of corresponding fluxes from tree foliage at the site. Our results suggest that a simplified representation of precipitation processes may be sufficient to accurately model bryophyte carbon cycling under future climate scenarios. Further, we find that projected increases in drought could have strong negative impacts on bryophyte and ecosystem carbon storage, with major consequences for a wide range of ecosystem processes.

摘要

苔藓植物在世界上许多主要生物群系的生态功能中扮演着关键角色,但与维管植物相比,它们的研究仍不够充分。人们对苔藓植物对气候变化导致的水分动态变化的不同方面的反应知之甚少。在这项研究中,对苔藓植物中群进行了 CO2 通量和光合作用光响应的测量,这些中群分别经历了不同程度、频率和类型(雾或降雨)的水分添加,并且在经历完全干燥的不同时期前后都进行了测量。苔藓植物的碳通量和光合作用光响应通常受到浇水事件的大小和类型的影响,但不受频率的影响。干燥会抑制苔藓植物的碳吸收,即使在重新水合后也是如此,并且随着干燥持续时间的延长,吸收抑制的程度逐渐增加。估计该生态系统水平的苔藓植物呼吸作用和净碳吸收分别为该地点树木叶片相应通量的 58%和 3%。我们的结果表明,简化的降水过程表示法可能足以在未来气候情景下准确模拟苔藓植物的碳循环。此外,我们发现,预计的干旱增加可能会对苔藓植物和生态系统碳储存产生强烈的负面影响,对广泛的生态系统过程产生重大影响。

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