1887

Abstract

Summary

Shallow-water hydrothermal vents release significant amounts of radiocarbon (¹4C)-depleted carbon, yet its fate in the marine carbon cycle remains poorly understood. This study investigates carbon uptake and transfer within the Kueishantao hydrothermal system (Taiwan) using a novel multi-isotope approach. By analyzing bulk d¹³C and ?¹4C values of particulate organic carbon (POC) from the water column and compound-specific d²H, d¹³C, and ?¹4C values of lipids from surface sediments, we trace the assimilation of vent-derived carbon.

Our results show that chemoautotrophic sulfur-oxidizing microbes are key drivers of ¹4C-depleted carbon fixation near the vent orifice, as indicated by the correlation between d¹³C and ?¹4C in fatty acids. Using d²H values, we identify a spatial shift from chemoautotrophy to photoautotrophy at the margins of the vent plume, while vent CO2 uptake remains stable. This study provides the first in-situ evidence of photoautotrophs assimilating vent-derived carbon in shallow hydrothermal systems, offering new insights into carbon cycling in these dynamic environments.

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/content/papers/10.3997/2214-4609.202533065
2025-09-07
2026-02-13
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