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半干旱草原土壤呼吸对干旱响应的季节性时间和植物功能类型的联合控制

Joint control of seasonal timing and plant function types on drought responses of soil respiration in a semiarid grassland.

作者信息

Qian Ruyan, Hao Yanbin, Li Linfeng, Zheng Zhenzhen, Wen Fuqi, Cui Xiaoyong, Wang Yanfen, Zhao Tong, Tang Ziyang, Du Jianqing, Xue Kai

机构信息

College of Life Sciences, University of Chinese Academy of Sciences, Beijing, China.

Yanshan Mountains Earth Critical Zone and Surface Flux Research Station, Chinese Academy of Sciences, University of Chinese Academy of Sciences, Beijing, China.

出版信息

Front Plant Sci. 2022 Aug 15;13:974418. doi: 10.3389/fpls.2022.974418. eCollection 2022.

Abstract

Globally, droughts are the most widespread climate factor impacting carbon (C) cycling. However, as the second-largest terrestrial C flux, the responses of soil respiration (Rs) to extreme droughts co-regulated by seasonal timing and PFT (plant functional type) are still not well understood. Here, a manipulative extreme-duration drought experiment (consecutive 30 days without rainfall) was designed to address the importance of drought timing (early-, mid-, or late growing season) for Rs and its components (heterotrophic respiration (Rh) and autotrophic respiration (Ra)) under three PFT treatments (two graminoids, two shrubs, and their combination). The results suggested that regardless of PFT, the mid-drought had the greatest negative effects while early-drought overall had little effect on Rh and its dominated Rs. However, PFT treatments had significant effects on Rh and Rs in response to the late drought, which was PFT-dependence: reduction in shrubs and combination but not in graminoids. Path analysis suggested that the decrease in Rs and Rh under droughts was through low soil water content induced reduction in MBC and GPP. These findings demonstrate that responses of Rs to droughts depend on seasonal timing and communities. Future droughts with different seasonal timing and induced shifts in plant structure would bring large uncertainty in predicting C dynamics under climate changes.

摘要

在全球范围内,干旱是影响碳(C)循环的最普遍气候因素。然而,作为陆地第二大碳通量,土壤呼吸(Rs)对由季节时间和植物功能类型(PFT)共同调节的极端干旱的响应仍未得到充分理解。在此,设计了一项控制性极端持续时间干旱实验(连续30天无降雨),以探讨干旱时间(生长季早期、中期或晚期)对三种PFT处理(两种禾本科植物、两种灌木及其组合)下Rs及其组分(异养呼吸(Rh)和自养呼吸(Ra))的重要性。结果表明,无论PFT如何,干旱中期的负面影响最大,而干旱早期总体上对Rh及其主导的Rs影响较小。然而,PFT处理对干旱后期的Rh和Rs有显著影响,这具有PFT依赖性:灌木及其组合处理中下降,而禾本科植物处理中未下降。通径分析表明,干旱下Rs和Rh的降低是通过土壤含水量降低导致MBC和GPP减少实现的。这些发现表明,Rs对干旱的响应取决于季节时间和群落。未来不同季节时间的干旱以及由此引起的植物结构变化将给预测气候变化下的碳动态带来很大不确定性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/316e/9421296/874d30794e89/fpls-13-974418-g001.jpg

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