ORIGINAL RESEARCH article
Front. Mar. Sci.
Sec. Marine Biogeochemistry
Volume 12 - 2025 | doi: 10.3389/fmars.2025.1503255
This article is part of the Research TopicThe Biological Pump: A Hunt For Microbial Key Players Involved in Ocean Carbon and Nutrient FluxesView all 6 articles
Temperature-dependent oxygen utilization rates of the mesopelagic water in the Southeast Asian basins
Provisionally accepted- 1Guangdong Ocean University, Zhanjiang, Guangdong Province, China
- 2College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang, China
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The Southeast Asian Seas (SEAS), characterized by interconnected basins separated by shallow sills, serve as a critical pathway for the Indonesian throughflow (ITF), regulating Indo-Pacific climate and biogeochemical exchanges. While temperature is a key driver of marine oxygen balance, its influence on mesopelagic oxygen dynamics in the SEAS remains underexplored. By combining the age estimation based on transient tracer with the Arrhenius equation, this study investigates temperaturedependent oxygen consumption processes in the SEAS mesopelagic zone (200 -1000 m), revealing an average apparent activation energy (Ea) of 100.9 kJ mol -1 . There is a robust positive correlation (R² > 0.64) between the oxygen utilization rate (OUR) and temperature in the mesopelagic, which is consistent with fundamental biochemical kinetics. A significant disparity in Ea was observed between the western (126.8 kJ mol -1 ) and eastern (89.8 kJ mol -1 ) ITF pathways, attributed to contrasting water masses from the North and South Pacific. The combination of temperature and organic matter can explain these regional differences. The stratified results show that a strong linear relationship still exists in the 200 -600 m. However, a deviation from the classical Arrhenius equation was observed in the 600 -1000 m, where physical processes such as mixing and water mass transport, along with biological factors like substrate availability and microbial community composition, might modulate oxygen consumption patterns. Projected warming scenarios indicated differential responses: a 2°C temperature rise amplified oxygen consumption by 30.7% (western ITF) and 45.9% (eastern ITF), underscoring temperature as a critical modulator of future oxygen loss.
Keywords: Transient tracer, oxygen utilization rate, temperature, Southeast Asian Seas, Arrhenius equation
Received: 28 Sep 2024; Accepted: 04 Aug 2025.
Copyright: © 2025 Liu and Huang. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence: Peng Huang, College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang, China
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