在65年的荒漠植被恢复时间序列中,植被和微生物条件的变化加速了土壤有机碳的积累

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Ting Zhang , Bin Niu , Yongli Wang , Zhifu Wei , Gen Wang , Xueyun Ma , Xinrong Li
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引用次数: 0

摘要

旱地植被恢复具有显著的有机碳固存潜力,不仅是遏制和扭转土地荒漠化的有效策略,也是缓解全球气候变化的有效途径。尽管通过植被恢复提高土壤有机碳(SOC)的研究取得了长足进展,但旱地碳储量的长期稳定性及其稳定机制仍不清楚。利用腾格里沙漠65年植被恢复时间序列,采用序贯化学提取法将土壤有机碳分离为功能不同的有机碳组分。土壤有机碳含量从11 a时的0.63 g/kg增加到65 a时的7.9 g/kg,并在34 a后加速增加。这个34年的阈值由分段函数确定,标志着积累速率和碳组分组成的变化。可提取的OC组分(如弱吸附OC、金属-OC配合物、碳酸盐-OC、铁-羟基氧化物-OC -OC)从34年的1.8 g/kg急剧上升到48年的3.9 g/kg,然后趋于稳定。34 ~ 65年,剩余OC从0.6 g/kg稳步增加到5.9 g/kg,成为优势。可萃取OC对有机碳的相对贡献从84%下降到47%,而剩余OC则从16%上升到53%。微生物生物量(磷脂脂肪酸,PLFAs)和群落组成(菌真菌比)与可提取的OC组分密切相关。剩余有机碳主要受植物属性(草本盖度、凋落物生物量)和生物结皮盖度的影响。这些结果表明,不同的生物和非生物因子调节不同的OC组分,导致长期植被恢复下不同的响应。总体而言,旱地的长期植被恢复加速了有机碳的积累,促进了更稳定的碳库的形成,有助于增强土壤恢复力和减缓气候变化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Shifts in the vegetation and microbial conditions accelerate soil organic carbon accumulation over a 65-year desert revegetation chronosequence

Shifts in the vegetation and microbial conditions accelerate soil organic carbon accumulation over a 65-year desert revegetation chronosequence
Revegetation in drylands is not only an effective strategy for curbing and reversing land desertification but also an effective approach to mitigating global climate change due to its significant organic carbon (OC) sequestration potential. Despite considerable progress in enhancing soil organic carbon (SOC) through revegetation, the long-term stability of carbon storage in drylands and the mechanisms underlying OC stabilization remain unclear. Here, we used a 65-year revegetation chronosequence in the Tengger Desert and applied sequential chemical extraction to separate SOC into functionally distinct OC fractions. SOC content increased from 0.63 g/kg at 11 years to 7.9 g/kg at 65 years, with a marked acceleration after 34 years. This 34-year threshold was identified by segmented function and signals a shift in both accumulation rate and carbon fraction composition. Extractable OC fractions (e.g., weakly adsorbed OC, metal–OC complexes, carbonate–OC, Fe-oxyhydroxide-OC–OC) rose sharply from 1.8 g/kg at 34 years to 3.9 g/kg at 48 years, then plateaued. In contrast, residual OC increased steadily from 0.6 g/kg to 5.9 g/kg between 34 and 65 years, becoming dominant. The relative contribution of extractable OC to SOC declined from 84 % to 47 %, while residual OC increased from 16 % to 53 %. Microbial biomass (phospholipid fatty acids, PLFAs) and community composition (fungi-to-bacteria ratio) were strongly associated with extractable OC fractions. In contrast, residual OC was primarily influenced by plant attributes (herb cover, litter biomass) and biocrust cover. These findings indicate that distinct biotic and abiotic factors regulate different OC fractions, leading to divergent responses under long-term revegetation. Overall, long-term revegetation in drylands accelerates SOC accumulation and promotes the formation of more stable carbon pools, contributing to enhanced soil resilience and climate change mitigation.
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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