TY - JOUR
T1 - Removal of dissolved organic carbon in the West Pacific hadal zones
AU - Chu, Mengfan
AU - Bao, Rui
AU - Strasser, Michael
AU - Ikehara, Ken
AU - Ding, Yang
AU - Liu, Kejian
AU - Liu, Mingzhi
AU - Xu, Li
AU - Wang, Yonghong
AU - Bellanova, Piero
AU - Rasbury, Troy
AU - Kölling, Martin
AU - Riedinger, Natascha
AU - Luo, Min
AU - März, Christian
AU - Jitsuno, Kana
AU - Cai, Zhirong
AU - McHugh, Cecilia
AU - Druffel, Ellen
N1 - Publisher Copyright:
© The Author(s) 2025.
PY - 2025/12
Y1 - 2025/12
N2 - The deep oceans are environments of complex carbon dynamics that have the potential to significantly impact the global carbon cycle. However, the role of hadal zones, particularly hadal trenches (water depth > 6 km), in the oceanic dissolved organic carbon (DOC) cycle is not thoroughly investigated. Here we report distinct DOC signatures in the Japan Trench bottom water. We find that up to 34% ± 7% of the DOC in the trench bottom is removed during the northeastward transport of dissolved carbon along the trench axis. This DOC removal increases the overall DOC recalcitrance of the deep Pacific DOC pool, and is potentially enhanced by the earthquake-triggered physical and biogeochemical processes in the hadal trenches. Radiocarbon analysis on representative oceanic transects further reveals that the Pacific deep-water DOC undergoes distinct removal compared to those in the Atlantic and Indian Oceans along the thermohaline transport. Our findings highlight hadal trenches as previously unrecognized DOC sinks in the deep ocean system, with varying dynamics that warrant further investigation.
AB - The deep oceans are environments of complex carbon dynamics that have the potential to significantly impact the global carbon cycle. However, the role of hadal zones, particularly hadal trenches (water depth > 6 km), in the oceanic dissolved organic carbon (DOC) cycle is not thoroughly investigated. Here we report distinct DOC signatures in the Japan Trench bottom water. We find that up to 34% ± 7% of the DOC in the trench bottom is removed during the northeastward transport of dissolved carbon along the trench axis. This DOC removal increases the overall DOC recalcitrance of the deep Pacific DOC pool, and is potentially enhanced by the earthquake-triggered physical and biogeochemical processes in the hadal trenches. Radiocarbon analysis on representative oceanic transects further reveals that the Pacific deep-water DOC undergoes distinct removal compared to those in the Atlantic and Indian Oceans along the thermohaline transport. Our findings highlight hadal trenches as previously unrecognized DOC sinks in the deep ocean system, with varying dynamics that warrant further investigation.
UR - https://www.scopus.com/pages/publications/85216056906
U2 - 10.1038/s41467-025-55883-1
DO - 10.1038/s41467-025-55883-1
M3 - Article
C2 - 39820746
AN - SCOPUS:85216056906
SN - 2041-1723
VL - 16
JO - Nature Communications
JF - Nature Communications
IS - 1
M1 - 733
ER -