Uniformity and variance in the effects of moss crusts on soil properties, enzyme activities, and bacterial communities along a subtropical karst degradation gradient

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Xiaona Li , Xin Zhao , Dong Chen , Guanting Guo , Jiaojiao Wu , Mingzhong Long , Qimei Wu , Dengfu Wang , Hong Jiang , Linmei Long
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引用次数: 0

Abstract

Research on biocrusts in degraded subtropical karst ecosystems remains limited, and the few reports that are available focus on only one small area. Here, we assessed the effects of moss crusts on soil physicochemical properties, enzyme activities, and bacterial communities in four subtropical karst ecosystems experiencing varying degrees of degradation. We also explored the response mechanisms underlying moss crusts’ ecological functions along the same eco-degradation gradient. Our results indicate that moss crusts influence soil enzyme activities and physicochemical properties in the same way in each of the four karst ecosystems, regardless of the degree of degradation: moss crusts significantly improved soil physicochemical properties and enhanced aggregate stability (soil organic carbon, total nitrogen, alkali-hydrolyzable nitrogen, available kalium, silt + clay content, and soil aggregate mean weight diameter) and enzyme activities (N-acetyl-β-D-glucosidase, leucine aminopeptidase, β-glucosidase, and sucrase). Moss crusts greatly enhanced soil bacterial community species richness, except in HF with a much lower pH (5.35∼6.08), suggesting that the connection between moss crusts and bacterial species richness is most relevant in weakly alkaline (HJ and KD) and nearly neutral (YT) karst environments. Soil enzyme activities and chemical properties are more dominant drivers influencing bacterial communities within moss crusts in karst ecosystems with different degrees of degradation. Furthermore, moss crusts significantly enhanced the stability and complexity of soil bacterial networks in all study areas except HF. The influence of moss crusts on soil properties (total nitrogen, mean weight diameter, and sucrase) and bacterial network structure became stronger with an increasing degree of degradation, and interactions between soil bacterial taxa tended to become increasingly cooperative. This study deepens our understanding of the ecological functions of moss crusts in different ecosystems and offers a theoretical reference for the study of how biocrusts and their ecological functions respond to global climate change.
亚热带喀斯特退化梯度下苔藓结皮对土壤性质、酶活性和细菌群落影响的均匀性和差异性
对亚热带退化喀斯特生态系统中生物结皮的研究还很有限,而且仅有的几篇报道都集中在一个小区域。在4个不同程度退化的亚热带喀斯特生态系统中,研究了苔藓结皮对土壤理化性质、酶活性和细菌群落的影响。在相同的生态退化梯度下,探讨了苔藓结皮生态功能的响应机制。结果表明,无论退化程度如何,苔藓结皮对四种喀斯特生态系统土壤酶活性和理化性质的影响都是相同的。苔藓结皮显著改善了土壤理化性质,提高了团聚体稳定性(土壤有机碳、全氮、碱解氮、速效钾、粉土+粘土含量、土壤团聚体平均重径)和酶活性(n -乙酰-β- d -葡萄糖苷酶、亮氨酸氨基肽酶、β-葡萄糖苷酶和蔗糖酶)。除pH值较低的HF(5.35 ~ 6.08)外,苔藓结皮显著提高了土壤细菌群落物种丰富度,表明苔藓结皮与细菌物种丰富度的关系在弱碱性(HJ和KD)和近中性(YT)岩溶环境中最为相关。在不同退化程度的喀斯特生态系统中,土壤酶活性和化学性质是影响苔藓结皮细菌群落的主要驱动因素。此外,苔藓结皮显著提高了土壤细菌网络的稳定性和复杂性。苔藓结皮对土壤性质(全氮、平均重径和蔗糖酶)和细菌网络结构的影响随着降解程度的增加而增强,土壤细菌类群之间的相互作用趋于合作。该研究加深了我们对不同生态系统中苔藓结皮生态功能的认识,为研究生物结皮及其生态功能如何响应全球气候变化提供了理论参考。
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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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