日本地球惑星科学連合2025年大会

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[J] 口頭発表

セッション記号 A (大気水圏科学) » A-CC 雪氷学・寒冷環境

[A-CC32] 雪氷学

2025年5月28日(水) 13:45 〜 15:15 展示場特設会場 (4) (幕張メッセ国際展示場 7・8ホール)

コンビーナ:大沼 友貴彦(宇宙航空研究開発機構)、谷川 朋範(気象庁気象研究所)、渡邊 達也(北見工業大学)、波多 俊太郎(国立極地研究所先端研究推進系地圏研究グループ)、座長:大沼 友貴彦(宇宙航空研究開発機構)

13:45 〜 14:00

[ACC32-01] Diversity and dynamics of glacier microbiome revealed by metagenomic analyses

★招待講演

*村上 匠1瀬川 高弘2大沼 友貴彦3、薄羽 珠ノ介4、河合 繁5、広瀬 侑5竹内 望4、本郷 裕一1 (1.東京科学大学、2.山梨大学、3.宇宙航空研究開発機構、4.千葉大学、5.豊橋技術科学大学)

キーワード:氷河生態系、微生物学、メタゲノム解析

Glaciers and ice sheets, one of the Earth’s predominant freshwater environments, form a unique biome rich in microorganisms. Microbial activities on glacier surfaces, such as photosynthesis and inorganic nitrogen metabolism, play substantial roles in biogeochemical cycles in glaciers and downstream environments. However, details of biodiversity, functionality, and dynamics of glacier microbiota remain largely to be elucidated. To gain deeper insights into the ecosystem of microbes thriving on glaciers, we conducted metagenomic analysis, which involved sequencing and analyzing genetic information extracted from entire microbial communities.
Comparative metagenomics revealed that community structures of glacier microbiota varied significantly across the geographical regions, in particular between polar and midlatitude glaciers. For example, microbial communities in the midlatitude glaciers contained abundant bacterial species capable of denitrification, whereas such microbes were nearly absent in polar glaciers. Distribution of cyanobacterial species, key photosynthetic microorganisms, also differed between the two regions; a variety of cyanobacterial species were detected from the midlatitude glaciers, while a single dominant species prevailed in the polar glaciers.
Structural differences in microbial communities were observed not only across broad geographical regions but also within a single glacier. Our researches on an Alaskan glacier revealed that the structures of microbial communities changed along altitude. Furthermore, longitudinal analyses of the microbial samples collected from this glacier between 2001 and 2024 demonstrated the temporal shits of microbial communities, notably a recent increase in cyanobacterial abundance in the glacier’s upper area.
Our findings collectively suggest that microbes inhabiting glaciers dynamically change their distributions in response to local environmental conditions, such as nutrient availability and melting duration. Further interdisciplinary studies integrating biological, geological, and climatological data will uncover the mechanisms driving the dynamics of microbial ecosystems in glacier environments.