4.7 Article

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

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FRONTIERS IN PLANT SCIENCE
卷 13, 期 -, 页码 -

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FRONTIERS MEDIA SA
DOI: 10.3389/fpls.2022.974418

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soil respiration; autotrophic respiration; heterotrophic respiration; climate extremes drought timing; function types; stability

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Globally, droughts have a significant impact on carbon cycling. However, the specific responses of soil respiration to extreme droughts, regulated by seasonal timing and plant functional types, are not well understood. In this study, a manipulative drought experiment was conducted to investigate the importance of drought timing and plant types on soil respiration. The results showed that mid-drought had the greatest negative effects on soil respiration, while early-drought had little effect. Plant functional types also had significant effects on soil respiration under late drought. This study highlights the importance of considering seasonal timing and plant communities in predicting carbon dynamics under future droughts.
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.

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