Distribution of microplastics in bathyal- to hadal-depth sediments and transport process along the deep-sea canyon and the Kuroshio Extension in the Northwest Pacific

Masashi Tsuchiya*, Tomo Kitahashi, Ryota Nakajima, Kazumasa Oguri, Kiichiro Kawamura, Akimu Nakamura, Kengo Nakano, Yosaku Maeda, Masafumi Murayama, Sanae Chiba, Katsunori Fujikura

*Kontaktforfatter

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Abstract

Understanding microplastic (MP) behavior in oceans is crucial for reducing marine plastic pollution. However, the complex process underlying MP transportation to the deep seafloor remains unknown despite the deep sea being considered its major sink. We focused on MP distribution in Sagami Bay (adjacent to highly populated areas of Japan), the plate triple junction connected through the Sagami Trough, and the abyssal plain immediately below the Kuroshio Extension. We observed the highest number of MPs in the abyssal stations, more than previously reported. The polymer types and aspect ratio of MPs in the abyssal stations significantly differed from those in the bathyal/hadal stations. The study suggests that MPs accumulated in the open ocean surface layer sink to the abyssal plains immediately below it, while MPs from land sources accumulate in the bathyal depth and are transported to the hadal depth near the coast through turbidity currents along the submarine canyon.

OriginalsprogEngelsk
Artikelnummer115466
TidsskriftMarine Pollution Bulletin
Vol/bind199
Antal sider12
ISSN0025-326X
DOI
StatusUdgivet - feb. 2024

Bibliografisk note

Funding Information:
The authors thank the captain, officers, and crew of the R/V Yokosuka, the operational team of the manned submersible Shinkai 6500, M. Morioka, marine technician, Nippon Marine Enterprises, Ltd. We are grateful to the onboard scientists of the YK19-11 cruise, especially the principal scientist A. Yabuki. We also thank K. Iijima for his valuable comments on sedimentary rate estimation, H. Matsuda for her help in the data acquisition of blank samples, and the anonymous reviewers and editors for their valuable comments on the manuscript.

Funding Information:
This work was partially funded by the Environmental Research and Technology Development Fund (SII-2, JPMEERF18S20211) of the Environmental Restoration and Conservation Agency provided by the Ministry of Environment of Japan, and the funders had no role in the study design, data collection and analysis, decision to publish, or preparation of the manuscript.

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