Dissolved oxygen is low when nitrate is high in ocean depth profiles due to remineralization
Oceanographic studies confirm that the decomposition and remineralization of organic matter at depth consume dissolved oxygen while releasing nutrients such as nitrate, resulting in inverse profiles of low oxygen and high nitrate.
The claim connects dissolved oxygen depletion at depth to nitrate accumulation driven by remineralization. Papers 3, 5, and 11 provide direct support for this fundamental biogeochemical coupling in ocean water columns. The remaining papers are irrelevant dental or material science studies.
Muchamad Al Azhar, Z. Lachkar, M. Lévy, Shafer Smith. Oxygen Minimum Zone Contrasts Between the Arabian Sea and the Bay of Bengal Implied by Differences in Remineralization Depth. 2017. https://doi.org/10.1002/2017GL075157
This study discusses how oxygen minimum zones are formed and maintained through organic matter remineralization processes, establishing the link between dissolved oxygen depletion and nutrient cycling.
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Helmuth Thomas. Remineralization ratios of carbon, nutrients, and oxygen in the North Atlantic Ocean: A field databased assessment. 2002. https://doi.org/10.1029/2001gb001452
This field-based assessment examines remineralization ratios of carbon, nutrients, and oxygen in the ocean, showing how oxygen consumption is coupled with nutrient (nitrate) release at depth.
Ding Li, Liping Wang, Fan Jiang, Xiang Zeng, Qinzeng Xu, Xuelei Zhang, Qiang Zheng, Zongze Shao. Prokaryotic community structure and key taxa in the Arabian Sea’s oxygen minimum zone. 2024. https://doi.org/10.3389/fmars.2024.1380819
This research highlights microbial communities and biogeochemical properties in ocean oxygen minimum zones where respiration and remineralization drive down dissolved oxygen while accumulating metabolic byproducts like nitrate.
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