日本地球惑星科学連合2014年大会

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セッション記号 B (地球生命科学) » B-GM 地下圏微生物学

[B-GM22_30AM1] 地球惑星科学と微生物生態学の接点

2014年4月30日(水) 09:00 〜 10:45 415 (4F)

コンビーナ:*砂村 倫成(東京大学大学院理学系研究科地球惑星科学専攻)、木庭 啓介(東京農工大学大学院農学研究院)、高井 研(海洋研究開発機構極限環境生物圏研究センター)、座長:布浦 拓郎(独立行政法人海洋研究開発機構海洋・極限環境生物圏領域)、濱村 奈津子(愛媛大学)

09:15 〜 09:30

[BGM22-02] 微生物生態情報の把握は森林の窒素循環メカニズムの理解を深めるのか

*磯部 一夫1大手 信人1 (1.東京大学)

キーワード:微生物生態, 窒素循環, 森林

Forests cover approximately 70% of Japan's total land area, representing a largest reservoir of diversity of organisms including plants, animals, fungi, protists and prokaryotes on land. These organisms are closely associated each other in material cycles if not directly. Thus, we need to know how materials are cycling between the organisms in order to address a fundamental question in ecosystem ecology: why do forests have the richest biodiversity on land? However, it is not easy to understand the material cycles in a forest because the forest has the various environmental heterogeneity which greatly affect the cycle. For example, nitrogen dynamics can be different in soils around hills and valleys in forests. Such spatial heterogeneity of the dynamics in the soils has been explained mainly from phenomenological perspectives using abiotic information such as soil moisture, soil temperature or litter quality. However, these perspectives have not fully explained the dynamics. Here, we suggest that such heterogeneity need to be explained in the context of ecology of microbial communities which mediate the nitrogen dynamics. More specifically, we suggest that understanding the nitrogen dynamics based on the physiology, population dynamics and diversity of the microbial communities can provide the mechanistic insights into the nitrogen cycle in forests.We analyzed the spatial heterogeneity of nitrogen dynamics and associated microbial communities in natural and planted forest soils in Asia. Specifically, we focused on nitrification in which ammonium are oxidized to nitrate and found the close association between gross nitrification rates and population size of nitrifiers in the soils. Additionally, nitrification rates cannot be fully explained by using environmental properties including substrate supply, soil moisture, soil temperature and litter quality, but can be explained by using the population size of nitrifiers. This shows that the better understandings of the microbial ecology allows us to more accurately predict the spatial heterogeneity of material cycles. In this presentation, we would like to discuss how information on microbial ecology expands our understandings of nitrogen cycle in forests.