PhytOC sequestration characteristics and phytolith carbon sink capacity of the karst grasslands in southwest China.

IF 8.2 1区 环境科学与生态学 Q1 ENVIRONMENTAL SCIENCES
Science of the Total Environment Pub Date : 2024-12-10 Epub Date: 2024-10-18 DOI:10.1016/j.scitotenv.2024.176949
Mengxia Luo, Linjiao Wang, Li Liu, Lukang Song, Xiaxia Lu, Maoyin Sheng
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引用次数: 0

Abstract

Grassland is an important component of terrestrial ecosystems and plays a crucial role in the global carbon cycle. PhytOC (phytolith-occluded organic carbon) is an extremely important long-term and stable carbon pool in terrestrial ecosystems. Southwest China karst soil exhibits obvious characteristics of alkalinity, high silicon content, and rich calcium, which can significantly influence the characteristics and mechanisms of PhytOC sequestration in vegetation. To elucidate the sequestration characteristics and mechanisms of PhytOC in the karst grasslands, three typical karst grasslands of tropical shrub tussock (TST), warm-temperate shrub tussock (WST), and mountain meadow (MM) from Guizhou province of southwest China were studied. The following results and conclusions were obtained that: 1) the range of PhytOC content of aboveground plant parts, underground roots, and soil in the karst grasslands was 4.03-16.54 g·kg-1, 10.67-33.92 g·kg-1, and 0.63-1.89 g·kg-1, respectively. The underground roots are an important site for phytolith carbon sequestration in grassland ecosystems, and the PhytOC content of underground roots may be higher than that of the aboveground parts. 2) The PhytOC sequestration rate of vegetation was 7.34-15.93 kg·ha-1·yr-1, and the annual sequestration amount of PhytOC of the whole grasslands in southwest China could reach 0.48 × 103-1.48 × 103 t CO2. Compared to grasslands in non-karst regions of China, karst grasslands in southwest China have a higher sequestration rate of PhytOC in vegetation and a greater capacity for phytolith carbon sequestration. 3) Soil available silicon, pH, and stoichiometric characteristics of C, N and P nutrients significantly affected the phytolith carbon sequestration of vegetation and the soil accumulation of PhytOC in the karst grasslands. The research results are of great significance for estimating the phytolith carbon sequestration capacity of grassland ecosystems and for grassland construction and management based on enhancing carbon sequestration.

中国西南喀斯特草地的植物碳封存特征和植物碳汇能力
草地是陆地生态系统的重要组成部分,在全球碳循环中发挥着至关重要的作用。植物有机碳(PhytOC)是陆地生态系统中极其重要的长期稳定碳库。中国西南岩溶土壤具有明显的碱性、高硅含量和富钙等特点,会对植被中植物固碳的特征和机制产生重要影响。为阐明岩溶草地植物有机碳的固碳特征和机制,研究了中国西南贵州省的热带灌木草丛(TST)、暖温带灌木草丛(WST)和山地草甸(MM)三种典型的岩溶草地。研究结果和结论如下1)喀斯特草地植物地上部分、地下根系和土壤中 PhytOC 的含量范围分别为 4.03-16.54 g-kg-1、10.67-33.92 g-kg-1、0.63-1.89 g-kg-1。地下根系是草地生态系统植物碳固存的重要场所,地下根系的 PhytOC 含量可能高于地上部分。2)植被的植物碳固存率为 7.34-15.93 kg-ha-1-yr-1,西南地区整个草原的植物碳年固存量可达 0.48 × 103-1.48 × 103 t CO2。与中国非喀斯特地区的草地相比,西南喀斯特草地植被中植物碳封存率更高,植物碳封存能力更强。3)土壤可利用硅、pH值以及C、N、P养分的化学计量特性显著影响喀斯特草地植被的植物碳固存率和植物碳有机碳的土壤积累。该研究成果对估算草地生态系统的植被固碳能力和基于提高固碳能力的草地建设与管理具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Science of the Total Environment
Science of the Total Environment 环境科学-环境科学
CiteScore
17.60
自引率
10.20%
发文量
8726
审稿时长
2.4 months
期刊介绍: The Science of the Total Environment is an international journal dedicated to scientific research on the environment and its interaction with humanity. It covers a wide range of disciplines and seeks to publish innovative, hypothesis-driven, and impactful research that explores the entire environment, including the atmosphere, lithosphere, hydrosphere, biosphere, and anthroposphere. The journal's updated Aims & Scope emphasizes the importance of interdisciplinary environmental research with broad impact. Priority is given to studies that advance fundamental understanding and explore the interconnectedness of multiple environmental spheres. Field studies are preferred, while laboratory experiments must demonstrate significant methodological advancements or mechanistic insights with direct relevance to the environment.
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