Yin Chuntao, Schlatter Daniel C, Kroese Duncan R, Paulitz Timothy C, Hagerty Christina H
Department of Plant Pathology, Washington State University, Pullman, WA, United States.
Department of Botany and Plant Pathology, Oregon State University, Adams, OR, United States.
Front Microbiol. 2021 May 20;12:576763. doi: 10.3389/fmicb.2021.576763. eCollection 2021.
Liming is an effective agricultural practice and is broadly used to ameliorate soil acidification in agricultural ecosystems. Our understanding of the impacts of lime application on the soil fungal community is scarce. In this study, we explored the responses of fungal communities to liming at two locations with decreasing soil pH in Oregon in the Pacific Northwest using high-throughput sequencing (Illumina MiSeq). Our results revealed that the location and liming did not significantly affect soil fungal diversity and richness, and the impact of soil depth on fungal diversity varied among locations. In contrast, location and soil depth had a strong effect on the structure and composition of soil fungal communities, whereas the impact of liming was much smaller, and location- and depth-dependent. Interestingly, families Lasiosphaeriaceae, Piskurozymaceae, and Sordariaceae predominated in the surface soil (0-7.5 cm) and were positively correlated with soil OM and aluminum, and negatively correlated with pH. The family Kickxellaceae which predominated in deeper soil (15-22.5 cm), had an opposite response to soil OM. Furthermore, some taxa in Ascomycota, such as Hypocreales, and , were increased by liming at one of the locations (Moro). In conclusion, these findings suggest that fungal community structure and composition rather than fungal diversity responded to location, soil depth and liming. Compared to liming, location and depth had a stronger effect on the soil fungal community, but some specific fungal taxa shifted with lime application.
施用石灰是一种有效的农业措施,广泛用于改善农业生态系统中的土壤酸化问题。我们对施用石灰对土壤真菌群落影响的了解甚少。在本研究中,我们利用高通量测序(Illumina MiSeq),在太平洋西北部俄勒冈州两个土壤pH值递减的地点,探究了真菌群落对施用石灰的响应。我们的结果表明,地点和施用石灰对土壤真菌的多样性和丰富度没有显著影响,且土壤深度对真菌多样性的影响在不同地点有所不同。相比之下,地点和土壤深度对土壤真菌群落的结构和组成有强烈影响,而施用石灰的影响则小得多,且取决于地点和深度。有趣的是,Lasiosphaeriaceae、Piskurozymaceae和Sordariaceae科在表层土壤(0 - 7.5厘米)中占主导地位,与土壤有机质和铝呈正相关,与pH值呈负相关。在较深土壤(15 - 22.5厘米)中占主导地位的Kickxellaceae科,对土壤有机质的反应则相反。此外,在其中一个地点(莫罗),石灰施用增加了子囊菌门中的一些分类单元,如肉座菌目等。总之,这些发现表明,真菌群落结构和组成而非真菌多样性对地点、土壤深度和施用石灰有响应。与施用石灰相比,地点和深度对土壤真菌群落的影响更强,但一些特定的真菌分类单元会随石灰施用而发生变化。