[M-IS24] 冷湧水・泥火山・熱水の生物地球科学

[MIS24-03] 種子島沖海底泥火山群の総合調査（KS-21-27次航海）速報

*井尻 暁¹、土岐 知弘²、村山 雅史³、星野 辰彦⁴、瀬戸口 亮眞³、満留 由来²、宮本 洋好³、田代 昴士³、安村 幸真²、小林 祐大¹、山田 貫太郎¹、吉崎 結衣¹、大塚 宏徳¹、加藤 萌⁵ (1.神戸大学、2.琉球大学、3.高知大学、4.海洋研究開発機構、5.金沢大学)

キーワード：海底泥火山、種子島沖

Submarine mud volcanoes occur along the margins of convergent plates and are formed by the vertical intrusion of low density, deformable sediments from the deep subsurface to the seafloor. These migration pathways supplies subsurface-derived water, gaseous compounds such as methane, and even microbes to the overlying hydrosphere. In particular, methane emission from mud volcanoes is a significant source of fossil methane to atmosphere or hydrosphere. Around Japan, the Kumano forearc basin and off Tanegashima Island have been known as mud volcano fields. Several tens of mud volcanoes have been found off Tanegashima Island along the Ryukyu Trench. We surveyed three mud volcanoes, MV#8 (30º45´N, 131º36´E), MV#10 (30º23´N, 131º24´E), and MV#15 (31º03´N, 131º40´E), in this area during KS-21-27 cruise from December 2021 to January 2022 by R/V Shinsei-Maru. Our objectives for this cruise are 1) to investigate the activity of mud volcanoes off Tanegashima and clarify the relationship between mud volcano activity and the tectonic environment, and 2) to estimate the flux of carbon and microorganisms released from the mud volcanoes, and to clarify the impact of mud volcanism on the biogeochemical cycle in the ocean. To achieve the objectives, we obtained sediment cores from the summits, and seawater samples from the water column above these mud volcanoes. At MV#15, we succeeded in collecting methane hydrate in the sediment core sample. We present the preliminary report of this cruise including the result of chemical analysis of the methane hydrate sample.