Nitrogen Availability and Microbial Communities of Canopy Soils in a Large Cercidiphyllum japonicum Tree of a Cool-Temperate Old Growth Forest

• Published in: Microbial ecology Vol. 82; no. 4; pp. 919 - 931
• Main Authors: Tatsumi, Chikae, Azuma, Wakana A., Ogawa, Yuya, Komada, Natsuki
• Format: Journal Article
• Language: English
• Published: New York Springer US 01.11.2021; Springer Nature B.V
• Subjects: Abundance; Ammonia; Availability; Biodiversity; Biomedical and Life Sciences; Canopies; Canopy; Cellulose; Cercidiphyllum japonicum; Ecology; Flowers & plants; Forests; Fungi; Geoecology/Natural Processes; Height; Herbivores; Life Sciences; Microbial activity; Microbial Ecology; Microbiology; Microbiomes; Microorganisms; Mineralization; Nature Conservation; Nitrification; Nitrogen; Old growth; Oligotrophic microorganisms; Organic soils; Oxidizing agents; Plant cover; Redundancy; Soil Microbiology; Soil microorganisms; Soil properties; Soils; Trees; Water Quality/Water Pollution; Fungi; Canopy humus; Nitrification; Ammonia-oxidizer; Prokaryote; Nitrogen availability; Organic soils
• ISSN: 0095-3628; 1432-184X
• DOI: 10.1007/s00248-021-01707-w

Canopy soils on large trees are important for supporting the lives of many canopy plants, and thereby increasing regional biodiversity. However, because of the less accessibility to canopy soils, there is insufficient knowledge on how canopy soils produce available nitrogen (N) for canopy plants through the activity of canopy soil microbes. Canopy soils usually have different soil properties from ground soils, so we hypothesized that canopy soils would have unique microbial communities compared to ground soils, but still provide available N for canopy plants. Here, we compared soil N availability, including net N mineralization and nitrification rate, and microbial communities between canopy soils (organic soils) collected at various heights of a large Cercidiphyllum japonicum tree and ground soils (organic and mineral soils) in a cool-temperate old-growth forest of Japan. The canopy soils had significantly different N availability (mass-based higher but volume-based lower) and microbial communities from the ground mineral soils. Among organic soils, the height of the soil had an impact on the microbial communities but not on the N availability, which agreed with our hypothesis. Despite the decrease in fungal abundance in the higher soils, the increase in certain components of the cellulose-decomposing fungi and oligotrophic bacteria may contribute to the available N production. Also, the abundance of ammonia-oxidizers did not change with the height, which would be important for the nitrification rate. Our study implied canopy soils could provide N to canopy plants partly through the functional redundancy within different microbial communities and constant population of ammonia-oxidizers.