Dynamics of dissolved organic carbon in the western North Pacific Ocean revealed by radiocarbon
ID:67 View Protection:ATTENDEE Updated Time:2026-04-22 15:55:14 Hits:48 Oral Presentation

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Abstract
Dissolved organic carbon (DOC) in seawater constitutes one of Earth’s largest organic carbon reservoirs (~662 Pg C) and plays a central role in long-term carbon sequestration and climate regulation. Recent studies suggest that DOC from marginal seas of the western North Pacific may serve as a carrier of trace nutrients, thereby influencing primary production in the open ocean. However, the source and transport pathways of this allochthonous DOC remain poorly constrained. In this study, we investigated the dynamics of DOC in the western North Pacific Ocean using radiocarbon (14C) as a tracer to constrain DOC sources and mixing relationships. Stable carbon isotope (13C) is additionally analyzed to provide complementary information on DOC origin. Seawater samples were collected during two cruises of Hakuho Maru in 2022 and 2023. DOC was extracted using a UV oxidation-based processing flow, and its radiocarbon signatures (Δ14C) were measured with a Single Stage Accelerator Mass Spectrometer. The Δ14C results revealed three DOC endmembers: refractory DOC as a background component, labile to semi-labile DOC derived from recent primary production in the surface, and an allochthonous DOC endmember characterized by a distinct Δ14C signature relative to ambient water masses. This allochthonous DOC signal is primarily confined to the density layer of σθ=26.6~27.5, consistent with transport along intermediate water pathways. By integrating multiple hydrographic and biogeochemical indicators together with radium isotopes, this allochthonous DOC is inferred to originate from the Bering Sea and its continental shelf, and is transported to the open ocean on decadal timescales. Our DOC partitioning further reveals the spatial distribution of DOC degradation and the short timescales of surface DOC cycling. This study presents the first extensive Δ14C constraints on DOC in the western North Pacific, providing new insights into carbon cycling processes and the connectivity between marginal seas and the open ocean.
 
Keywords
Dissolved organic carbon,Radiocarbon,western North Pacific
Speaker
JIANG Youwen
Student The University of Tokyo

Submission Author
JIANG Youwen The University of Tokyo
Yui Sakai The University of Tokyo
Yusuke Yokoyama The University of Tokyo
Yosuke Miyairi The University of Tokyo
Hiroshi Ogawa The University of Tokyo
Hajime Obata The University of Tokyo
Shigeyoshi Otosaka The University of Tokyo
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Important Date
  • Conference Date

    Jun 16

    2026

    to

    Jun 18

    2026

  • Apr 03 2026

    Draft paper submission deadline

Sponsored By
Hokkaido University
Organized By
Hokkaido University