Conservative behavior of dissolved black carbon in the northwestern Pacific marginal seas

Dissolved black carbon (DBC) represents the largest molecularly identifiable slow-cycling organic carbon pool in the ocean. However, its behavior remains debated due to large differences between its radiocarbon ages and residence times based on mass balance estimations, suggesting considerable removal in the source regions. Here, we show that DBC is predominantly derived from riverine sources and behaves conservatively throughout the entire water masses of the northwestern Pacific marginal seas-including the East China Sea, the Yellow Sea, and the East Sea (Japan Sea)-which are characterized by extreme biogeochemical alterations and long water residence times (~100 years). This conservative behavior is evidenced by a strong negative correlation between DBC and salinity, consistent mass balance estimates, and a uniform B6CA/B5CA marker ratio. Thus, we suggest that the discrepancy between DBC ages and residence times in the ocean is more likely due to substantially enhanced contemporary DBC production rather than removal pathways.

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Publication Details

Journal
Nature Communications
Published
2025-12-01
DOI
https://doi.org/10.1038/s41467-025-65855-0
Citations
1
Primary Topic
Marine and coastal ecosystems
Type
article
Field-Weighted Citation Impact
1.79

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article

Conservative behavior of dissolved black carbon in the northwestern Pacific marginal seas

Hannelore Waska, Heejun Han, Guebuem Kim, Thorsten Dittmar et al.
1 citations
Nature Communications
Marine and coastal ecosystems
1.79
article

Conservative behavior of dissolved black carbon in the northwestern Pacific marginal seas

Hannelore Waska, Heejun Han, Guebuem Kim, Thorsten Dittmar, Marit Renken, Jihyun Park, Hojong Seo, Joon‐Soo Lee, In-Seong Han
article en
1 citations

Abstract

Dissolved black carbon (DBC) represents the largest molecularly identifiable slow-cycling organic carbon pool in the ocean. However, its behavior remains debated due to large differences between its radiocarbon ages and residence times based on mass balance estimations, suggesting considerable removal in the source regions. Here, we show that DBC is predominantly derived from riverine sources and behaves conservatively throughout the entire water masses of the northwestern Pacific marginal seas-including the East China Sea, the Yellow Sea, and the East Sea (Japan Sea)-which are characterized by extreme biogeochemical alterations and long water residence times (~100 years). This conservative behavior is evidenced by a strong negative correlation between DBC and salinity, consistent mass balance estimates, and a uniform B6CA/B5CA marker ratio. Thus, we suggest that the discrepancy between DBC ages and residence times in the ocean is more likely due to substantially enhanced contemporary DBC production rather than removal pathways.

Nature CommunicationsVol. 16(1)
Carl von Ossietzky Universität Oldenburg (DE), Korea Institute of Ocean Science and Technology (KR), Seoul National University (KR), Helmholtz Institute for Functional Marine Biodiversity (DE), National Institute of Fisheries Science (KR), National University College (PR)
National Research Foundation, Seoul National University, Ministry of Oceans and Fisheries, National Research Foundation of Korea, National Institute of Fisheries Science, Korea Institute of Marine Science and Technology promotion
Openalex Percentile: Top 12%
Marine and coastal ecosystems
1.79
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