日本地球惑星科学連合2019年大会

講演情報

[E] 口頭発表

セッション記号 M (領域外・複数領域) » M-IS ジョイント

[M-IS02] 地球掘削科学

2019年5月27日(月) 13:45 〜 15:15 A07 (東京ベイ幕張ホール)

コンビーナ:山田 泰広(海洋研究開発機構 海洋掘削科学研究開発センター)、針金 由美子(産業技術総合研究所)、黒柳 あずみ(東北大学学術資源研究公開センター東北大学総合学術博物館)、山口 耕生(東邦大学, NASA Astrobiology Institute.)、座長:針金 由美子(産総研)、阿部 なつ江(海洋研究開発機構 海洋掘削科学研究開発センター)

14:45 〜 15:00

[MIS02-17] Exploring the deep subseafloor biosphere and biogeochemical carbon cycling beneath the Arctic ocean

*稲垣 史生1Steffen Leth Jørgensen2Rolf Birger Pedersen2 (1.国立研究開発法人海洋研究開発機構、2.ノルウェー・ベルゲン大学)

キーワード:Arctic ocean、scientific ocean drilling、deep subseafloor biosphere、biogeochemical carbon cycle

Despite the Arctic cryosphere is the most sensitive and vulnerable to the global environmental change, the nature of deep subseafloor arctic environments remains largely unknown. Active processes on the drastic climate change, including the anthropogenic global warming and subsequent ice melt, are presumably similar to those mechanisms that formed some of the major hydrocarbon resources we presently use, deeply buried in the subseafloor sediment over millions of years at high atmospheric CO2 and global warm conditions. Continuing to advance understanding of the natural analogues beneath the Arctic ocean through scientific drilling is a powerful approach for the discoveries and understanding of life and Earth co-operating systems, and consequently will illuminate the possible resilience and sustainable strategies adopted by human society towards the future. Here, we are keenly interested in the Arctic deep biosphere and biogeochemical carbon cycling, which presumably be tightly associated with tectonics and biotic/abiotic processes through paleoceanographic events of seawater stagnations, perturbations and fertilizations in the Paleogene to Cretaceous period, and perhaps still continuing in situ over geologic time. How is diagenetic activity and microbial diversity linked to variability in Cenozoic climate and environmental changes? To what degree is carbon diagenesis linked to biotic/abiotic and tectonic processes? What fluid flow and energy transformation processes support microbial activity in situ and govern carbon sink in the Arctic sedimentary basin? How does alternation of deep oceanic crust contribute to microbial life and biogeochemical carbon cycling in the shallower habitat? In addition, what is the nature of the Arctic basement? These important scientific issues on the most climate-sensitive place on Earth remain to be explored, but using the Chikyu’s riser-drilling and onboard facilities, it can be addressed by the state-of-the-art interdisciplinary analyses of core samples and the long-term borehole observatory.