The OMZ and Its Influence on POC in the Tropical Western Pacific Ocean: Based on the Survey in March 2018

Jun Ma,Ning Li,Liqin Duan,Qidong Wang,Huamao Yuan,Jinming Song,Guorong Zhong,Xuegang Li

doi:10.3389/feart.2021.632229

Abstract

The hypoxia problem in the ocean is worsening, and the oxygen minimum zone (OMZ) continues to expand. The Tropical Western Pacific Ocean is one of the most sensitive areas in response to climate change and human activities, and the OMZ in this area has also expanded significantly. Based on a survey conducted in March 2018, the characteristics of OMZ in the Kocebu seamount area of the Tropical Western Pacific Ocean and its biogeochemical effects are discussed. The results showed that DO in the Kocebu seamount area first decreased and then increased, and the lowest value was 2.49 mg/L at a water depth of 750 m. Based on the oxycline and the threshold of 3.20 mg/L, OMZ in this area was located in the water column of 590–1,350 m. With the increase in water depth, the POC concentration decreased gradually and remained stable in the water column deeper than 1,000 m. The presence of OMZ reduced the decomposition rate of POC, causing more POC to sink into deeper waters. 38.77% of POC was decomposed in the water column of 150–300 m, whereas only 16.25% of POC was decomposed in the OMZ. In contrast to the vertical distribution of POC, δ13C-POC decreased rapidly in the water columns of 100–150 and 300–500 m, indicating the rapid decomposition of POC. This result suggests that POC and δ13C-POC should be combined in the evaluation of POC decomposition.

Highlights

The oxygen minimum zone (OMZ) refers to the water column in the ocean where dissolved oxygen (DO) is below a specific threshold
It is generally believed that the main structure of the OMZ in the ocean is located in the water column of 200–1,500 m, and there is a significant oxycline between the OMZ and the upper or lower waters (Paulmier and Ruiz-Pino, 2009; Breitburg et al, 2018)
The existence of OMZ shows a low-oxygen environment in the ocean, which has an important impact on marine organisms, global climate change, and the matter cycle

Summary

Introduction

The oxygen minimum zone (OMZ) refers to the water column in the ocean where dissolved oxygen (DO) is below a specific threshold. The existence of OMZ shows a low-oxygen environment in the ocean; there is no universal standard for its threshold. For different research areas and objects, the DO threshold of the OMZ varied from 0 to 100 μmol/kg. OMZ is widely distributed in the Central Atlantic Ocean, Northern Indian Ocean, Eastern Pacific Ocean, and Western Pacific Ocean and has important effects on marine organisms, global climate change, and matter cycles (Wright et al, 2012; Yao et al, 2020). OMZ causes some oxygen-sensitive organisms to escape from the area, which affects the diversity of marine organisms

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