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EDITORIAL article

Front. Plant Sci., 15 May 2024
Sec. Functional Plant Ecology
This article is part of the Research Topic Carbon-Water-Nitrogen Processes and Mechanisms of Agricultural and Forest Ecosystems under Future Climate Change View all 11 articles

Editorial: Carbon-water-nitrogen processes and mechanisms of agricultural and forest ecosystems under future climate change

  • 1School of Water Conservancy and Hydropower, Hebei University of Engineering, Handan, Hebei, China
  • 2Institute of Applied Ecology, Chinese Academy of Sciences (CAS), Shenyang, China
  • 3School of Earth System Science, Institute of Surface-Earth System Science, Tianjin University, Tianjin, China
  • 4BNU-HKUST Laboratory for Green Innovation, Advanced Institute of Natural Sciences, Beijing Normal University at Zhuhai, Zhuhai, China
  • 5Guangdong-Hong Kong Joint Laboratory for Carbon Neutrality, Jiangmen Laboratory of Carbon Science and Technology, Jiangmen, China

It is well known that agricultural and forest ecosystems serve as vital carbon sinks in terrestrial ecosystems. Understanding the fundamental processes and mechanisms of ecosystem carbon cycles in face of climate change is critical for quantifying the carbon sinks of terrestrial ecosystems. Ecosystem carbon cycles cannot be separated from water and nitrogen cycles and thus the response and adaptation of carbon-water-nitrogen processes in agricultural and forest ecosystems to climate change demand further studies. This research topic published 10 papers to gain novel insights into the underlying mechanisms and processes of carbon-water-nitrogen interactions in agricultural and forest ecosystems in response to climate change.

Litter decomposition is a pivotal biogeochemical process, which profoundly influences carbon and nitrogen cycling in forest and grassland ecosystems. Climatic factors can significantly impact litter decomposition rates, carbon sequestration, and the emissions of greenhouse gases such as CO2 and N2O. Liu et al. conducted a comprehensive meta-analysis of 351 samples from 37 published studies to explore the interactive effects of solar radiation and precipitation on litter decomposition and CO2 emission on a global scale. They found that the solar radiation significantly increased litter decomposition which was dependent on precipitation regimes. Meanwhile, Li et al. investigated the effects of warming and reclamation on N2O emission flux through a long-term manipulative warming experiment on the Qinghai-Tibetan Plateau. Their results demonstrated that reclamation amplified the warming effects on N2O emissions by enhancing soil nitrification and related enzymatic activities in alpine meadows. Additionally, Lin et al.examined the long-term spatiotemporal variations in aboveground carbon sequestration rates in the eastern Tibetan Plateau using a forest landscape model under different climate change scenarios. Their study highlighted the variability in aboveground carbon sequestration rates across various forest types in response to climate warming.

The escalating frequency and duration of drought events under climate change have prompted heightened scrutiny of their impacts on temporal and spatial variations in evapotranspiration and water use efficiency. Yang et al. analyzed the inter-annual variations of evapotranspiration with eddy covariance fluxes in an urban forest in Beijing, China, revealing that spring and mid-summer droughts primarily drove inter-annual variations in evapotranspiration due to the reduced stomatal conductance. Furthermore, Xu et al. employed the ensemble empirical mode decomposition method to investigate spatial variations and mechanisms influencing the stability of water use efficiency in China. Their findings explored the role of precipitation and soil moisture in promoting stable water use efficiency, with unstable trends primarily driven by positive or negative reversals. In addition, Jiang et al. presented an in-depth analysis of the impact of seasonal drought on root distribution and water utilization patterns of forests in south China. Their findings highlighted the critical role of deep fine roots in utilizing deep soil water during the dry season, constituting a substantial portion of total water consumption.

Leaf photosynthesis, reliant on both photochemical and carboxylation processes, is central to terrestrial carbon fluxes. Accurate estimation of photochemical parameters and maximum carboxylation rates is essential for predicting carbon fluxes of terrestrial ecosystems. The article by Liu et al. found that the inferred values of the photochemical redox parameters varied with leaf macronutrient contents. The work of Li et al. evaluated the relationships between the leaf maximum rate of carboxylation and both leaf Narea and photosynthetic pigments of winter wheat in a farmland ecosystem in China. One of the study’s notable findings was the strongest correlation between leaf Vcmax and leaf Chlarea. Their findings suggest that photosynthetic pigment content serves as a predictor for estimating Vcmax, offering a novel approach for spatially continuous Vcmax estimation and enhancing simulation accuracy in ecological models.

In addition to the above articles from field studies, two papers elucidated the mitigated effects of elevated CO2 concentrations on environmental stressors such as drought and nutrient deficiency. Based on manipulative experiment with environmental growth chambers, Chang et al. examined the effects of elevated CO2 concentration and temperature on plant growth and leaf gas exchange of winter wheat along a soil water gradient, and found that elevated CO2 concentration substantially enhanced leaf photosynthesis by about 30% under water deficiency, suggesting the negative impacts of water deficiency on winter wheat might be partially mitigated by elevated CO2 concentration. Li et al.reported findings that the plant growth and leaf photosynthesis of annual ryegrass under phosphorus deficiency were enhanced by elevated CO2 concentration, indicating the impacts of phosphorus deficiency on annual ryegrass may be alleviated by elevated CO2 concentration under climate change.

This research topic presents the latest studies on how climate change affects the carbon-water-nitrogen processes of agricultural and forest ecosystems. Meanwhile, this research topic highlights the importance and uncertainty of ecosystem functioning in response to climate change. Therefore, fully exploring the potential mechanisms and processes of agriculture and forests to climate change is pivotal to projecting the potential risk of climate change on global grain yield and forest carbon sequestrations.

Author contributions

YZ: Writing – original draft, Writing – review & editing. QY: Writing – review & editing. HZ: Writing – review & editing. MX: Writing – original draft, Writing – review & editing.

Funding

The author(s) declare financial support was received for the research, authorship, and/or publication of this article. Ming Xu was supported by the Special Fund for Science and Technology Innovation Strategy of Guangdong Province, China under Grant No. 2022660500250009604.

Acknowledgments

The editors would like to thank the authors, reviewers, and the Frontiers in Plant Science team, whose efforts have led to the success of this Research Topic.

Conflict of interest

The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.

Publisher’s note

All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.

Keywords: global change, plant growth, carbon sequestration, crop yield, carbon budget, ecosystem structure and function, ecological process models

Citation: Zheng Y, Yang Q, Zhou H and Xu M (2024) Editorial: Carbon-water-nitrogen processes and mechanisms of agricultural and forest ecosystems under future climate change. Front. Plant Sci. 15:1423506. doi: 10.3389/fpls.2024.1423506

Received: 26 April 2024; Accepted: 06 May 2024;
Published: 15 May 2024.

Edited and Reviewed by:

Sebastian Leuzinger, Auckland University of Technology, New Zealand

Copyright © 2024 Zheng, Yang, Zhou and Xu. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

*Correspondence: Yunpu Zheng, zhengyunpu@hebeu.edu.cn; Ming Xu, 91122020071@bnu.edu.cn

Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.