Interactive effects of carbon and nitrogen fixation in two biocrust types in the Mu Us Sandland

IF 5.7 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Wenxin Zhang , Mengchen Ju , Shufang Wu , Chongfeng Bu , Jin Fan , Xinhao Li , Yingxin Wei , Jingwen Pang , Kadambot H.M. Siddique
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Abstract

Biocrusts, as pioneer organisms in dryland ecosystems, play a vital role in regulating carbon (C) and nitrogen (N) cycling. Understanding how precipitation gradients influence regional-scale variations in C and N components—and their coupling—is essential for effectively conserving and managing biocrusts. This study examined differences and interactions in C and N dynamics within moss- and cyanobacteria-dominated biocrusts and their underlying soils across three representative sites along a west–east precipitation gradient (262–476 mm) in the Mu Us Sandland. We also assessed the relationships between microbial diversity, functional genes involved in C and N cycling, and soil C–N content. Significant spatial heterogeneity was observed: biocrusts in the eastern region had the highest levels of dissolved organic carbon and particulate organic carbon (361.52 and 8.41 mg·kg−1, respectively), while nitrate-N and organic N concentrations peaked in the western region (6.68 and 1.02 mg·kg−1, respectively; P < 0.05). Bacterial diversity and C–N cycling-related genes strongly correlated with C and N accumulation and transformation, exhibiting distinct regional patterns. Partial least squares path modeling indicated that precipitation gradients drove divergence in C–N coupling (goodness-of-fit = 0.80 for moss crusts, 0.74 for cyanobacteria crusts). In moss crusts, N fixation functional genes enhanced C and N components. In contrast, in cyanobacteria crusts, N consumption functional genes negatively affected N content (β = −0.69, P < 0.05), contributing to N losses in wetter regions through leaching. Functional gene expression by Cyanobacteria and Proteobacteria was identified as a key regulator of C–N interactions. These findings provide mechanistic insight into the microbial basis of regional-scale C–N coupling, highlight the importance of moss crusts for nutrient retention under increased precipitation, and offer a scientific foundation for dryland ecosystem management and climate adaptation strategies.

Abstract Image

毛乌素沙地两种生物结壳类型碳氮固定的交互效应
生物结壳作为旱地生态系统的先锋生物,在调节碳(C)和氮(N)循环中起着至关重要的作用。了解降水梯度如何影响区域尺度上碳氮组分的变化及其耦合,对于有效地保护和管理生物结壳至关重要。本研究考察了毛乌素沙地西向东降水梯度(262-476 mm)三个代表性地点以苔藓和蓝藻为主的生物结皮及其下垫土壤中C和N动态的差异和相互作用。我们还评估了微生物多样性、参与碳氮循环的功能基因和土壤碳氮含量之间的关系。土壤中溶解有机碳和颗粒有机碳含量在东部地区最高(分别为361.52和8.41 mg·kg−1),硝态氮和有机氮含量在西部地区最高(分别为6.68和1.02 mg·kg−1);P & lt;0.05)。细菌多样性和碳氮循环相关基因与碳氮积累和转化密切相关,表现出明显的区域格局。偏最小二乘路径模型表明,降水梯度驱动碳氮耦合的发散(苔藓结壳的拟合优度为0.80,蓝藻结壳的拟合优度为0.74)。在苔藓结壳中,固氮功能基因增强了C和N组分。而在蓝藻菌壳中,氮消耗功能基因对氮含量有负向影响(β = - 0.69, P <;0.05),通过淋溶促进湿润地区氮的损失。蓝藻菌和变形菌的功能基因表达被确定为C-N相互作用的关键调节因子。这些发现为揭示区域尺度C-N耦合的微生物机制提供了新的视角,突出了降水增加条件下苔藓结皮对养分保持的重要性,并为旱地生态系统管理和气候适应策略提供了科学依据。
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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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