Japan Geoscience Union Meeting 2023

Presentation information

[J] Online Poster

M (Multidisciplinary and Interdisciplinary) » M-ZZ Others

[M-ZZ44] Marine manganese deposits - Genesis, exploration and development

Fri. May 26, 2023 10:45 AM - 12:15 PM Online Poster Zoom Room (25) (Online Poster)

convener:Akira Usui(Marine Core Research Center, Kochi University), Katsuhiko Suzuki(Submarine Resources Research Center, Japan Agency for Marine-Earth Science and Technology), Yoshio Takahashi(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Takashi Ito(Faculty of Education, Ibaraki University)

On-site poster schedule(2023/5/25 17:15-18:45)

10:45 AM - 12:15 PM

[MZZ44-P02] Spatial characterization of 210Pb- and 14C-derived bioturbation activities in surface sediments at northwestern Pacific seamounts

*Yuki Ota1, Masahiro Suzumura1, Ayumi Tsukasaki1, Atsushi Suzuki1, Koji Seike1,2, Jumpei Minatoya3 (1.National Institute of Advanced Industrial Science and Technology, 2.Department of Natural Environmental Studies, Graduate School of Frontier Sciences, The University of Tokyo, 3.Japan Organization for Metals and Energy Security (JOGMEC))

Keywords:marine sediment, northwestern Pacific, bioturbation, seamounts, 210Pb, 14C

obalt-rich ferromanganese crusts are present on seamount summits in the northwestern Pacific at various water depths. International Seabed Authority has issued the environmental guidelines and requires contractors to conduct an environmental and biological baseline survey around the seamounts. In this study, 210Pb activity measurements and 14C dating were conducted in sediment cores collected from the seamounts to evaluate the spatial characteristics of bioturbation activity. The results indicate the shallower mixing layer depth and the smaller particle mixing coefficient of the surface sediment at the summit areas than at the foot of seamounts, which suggests a weak bioturbation activity in the peaks. This difference in bioturbation activity may be attributed to the differences in bottom-water dissolved oxygen and particulate organic matter concentrations between the summits and feet of the seamounts in the northwestern Pacific.