Aridity-driven divergence in soil microbial necromass carbon in alpine grasslands of the Tibetan Plateau

IF 5.1 1区 农林科学 Q1 SOIL SCIENCE
Yunfei Zhao, Xia Wang, Yazhen Li, Menghan Yuan, Jia Li, Huawei Zhu, Zhuoyun Cheng, Wenhui Duan, Junwu Wang
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Abstract

Soil microbial necromass carbon (MNC) contributes to the long-term stability of soil organic carbon (SOC). However, the response of MNC across aridity gradients remains unclear, especially in vulnerable alpine ecosystems. Here, we examined alpine grasslands from 180 sites spanning a 3,500 km aridity gradient on the Tibetan Plateau to investigate how MNC abundance and composition (contributions of bacterial and fungal necromass carbon) vary with climate. MNC was variable, ranging from 0.55 to 26.95 g kg−1 soil, with higher content observed in humid and dry-subhumid regions than in arid and semiarid regions in the Western Tibetan Plateau. Soil properties were the dominant drivers of MNC, with soil fertility (cation exchange capacity and total phosphorus) and weathering products (clay, silt and iron/aluminum oxides) facilitating MNC accumulation, while a negative correlation was observed between MNC and soil pH. A pivotal aridity threshold of 0.60 underpinned a non-linear decrease in MNC with increasing aridity across soil condition gradients; MNC was negatively correlated with aridity below this threshold and showed no correlation beyond it. Given this pivotal aridity threshold, we delineated the drivers of MNC under conditions of low (aridity < 0.6) versus high (aridity > 0.6) aridity. In low-aridity conditions, MNC accumulation was governed by aridity, soil fertility, weathering products, and pH, whereas in high-aridity conditions, the interplay between soil properties and temperature took precedence. Species richness enhanced carbon accumulation from microbial residues under low-aridity conditions more so than under high-aridity conditions, with fungal necromass carbon consistently being a higher contributor to SOC than bacterial necromass carbon, particularly in humid regions. These findings highlight aridity-driven divergence in MNC and propose that conserving plant diversity may mitigate the adverse effects of aridification on MNC under low-aridity conditions in alpine grasslands.

Abstract Image

青藏高原高寒草地土壤微生物尸碳在干旱驱动下的分化
土壤微生物坏死碳(MNC)有助于土壤有机碳(SOC)的长期稳定。然而,MNC在不同干旱梯度下的反应仍不清楚,尤其是在脆弱的高寒生态系统中。在此,我们考察了青藏高原干旱梯度长达3500千米的180个地点的高寒草地,以研究MNC的丰度和组成(细菌和真菌尸碳的贡献)如何随气候而变化。青藏高原西部湿润和干旱半湿润地区的 MNC 含量高于干旱和半干旱地区。土壤特性是 MNC 的主要驱动因素,土壤肥力(阳离子交换容量和总磷)和风化产物(粘土、淤泥和铁/铝氧化物)有利于 MNC 的积累,而 MNC 与土壤 pH 值之间呈负相关。0.60 的关键干旱度阈值支撑着 MNC 随土壤条件梯度的干旱度增加而非线性减少;在该阈值以下,MNC 与干旱度呈负相关,超过该阈值则无相关性。鉴于这一关键的干旱临界值,我们划分了低干旱(干旱度为 0.6)和高干旱(干旱度为 0.6)条件下 MNC 的驱动因素。在低干旱度条件下,MNC积累受干旱度、土壤肥力、风化产物和pH值的影响,而在高干旱度条件下,土壤特性和温度之间的相互作用占主导地位。物种丰富度在低湿度条件下比在高湿度条件下更能促进微生物残体的碳积累,真菌残体碳对SOC的贡献一直高于细菌残体碳,尤其是在潮湿地区。这些发现凸显了干旱导致的MNC差异,并提出保护植物多样性可减轻干旱化对高寒草地低湿度条件下MNC的不利影响。
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来源期刊
Biology and Fertility of Soils
Biology and Fertility of Soils 农林科学-土壤科学
CiteScore
11.80
自引率
10.80%
发文量
62
审稿时长
2.2 months
期刊介绍: Biology and Fertility of Soils publishes in English original papers, reviews and short communications on all fundamental and applied aspects of biology – microflora and microfauna - and fertility of soils. It offers a forum for research aimed at broadening the understanding of biological functions, processes and interactions in soils, particularly concerning the increasing demands of agriculture, deforestation and industrialization. The journal includes articles on techniques and methods that evaluate processes, biogeochemical interactions and ecological stresses, and sometimes presents special issues on relevant topics.
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