Literature DB >> 30308898

Hydrochemical properties and chemocline of the Sansha Yongle Blue Hole in the South China Sea.

Linping Xie1, Baodong Wang2, Xinming Pu1, Ming Xin1, Peiqing He1, Chengxuan Li1, Qinsheng Wei3, Xuelei Zhang3, Tiegang Li1.   

Abstract

Blue holes can provide valuable information regarding paleoclimate, climate change, karst processes, marine ecology, and carbonate geochemistry. The Sansha Yongle Blue Hole, located on Yongle Atoll in the Paracel Islands in the South China Sea, is the deepest blue hole in the world. A comprehensive investigation of the blue hole was conducted to determine the hydrochemical properties and associated redox processes active in the water column. Results indicate the presence of two thermoclines, one at 13-20 m and a second at 70-150 m, dividing the water column into five stratified water layers. Based on redox state, the water column can be divided into three layers: an oxic layer in the top 70 m, a chemocline at 70-100 m, which acts as a redox boundary, and an anoxic deep layer. In the oxic layer, photosynthesis in the oxic layer above the seasonal thermocline, results in nutrient uptake, transformation of inorganic carbon to organic carbon in the top mixed layer above the seasonal thermocline; Below the seasonal thermocline, organic matter degradation and nitrification, which are the main biological process at depths around 30 m and 50-70 m, lead to the accumulation of nitrate and a decrease in dissolved oxygen and pH; whereas photosynthesis is dominant at depths of 30-50 m, leading to increase in dissolved oxygen and pH. Within the chemocline, organic matter decays via a variety of reactions (e.g. aerobic mineralization, denitrification and anammox), leading to sharp decreases in the oxidizing chemical species (e.g., dissolved oxygen and nitrate) and corresponding increases in the reduced species (e.g., ammonium and sulfide). Within this layer, about 60% of the nitrogen is lost and chemoautotrophic/photoautotrophic production may contribute significantly to particulate organic carbon. Within the deep anoxic layer, sulfate reduction and degradation of organic matter result in accumulations of sulfide, dissolved inorganic carbon, and nutrients.
Copyright © 2018 Elsevier B.V. All rights reserved.

Entities:  

Keywords:  Blue hole; Carbon; Chemocline; Geochemistry; Nitrogen; South China Sea

Year:  2018        PMID: 30308898     DOI: 10.1016/j.scitotenv.2018.08.333

Source DB:  PubMed          Journal:  Sci Total Environ        ISSN: 0048-9697            Impact factor:   7.963


  5 in total

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Authors:  Jeffrey M Dick; Jingqiang Tan
Journal:  Microb Ecol       Date:  2022-05-03       Impact factor: 4.552

2.  Gulf of Mexico blue hole harbors high levels of novel microbial lineages.

Authors:  N V Patin; Z A Dietrich; A Stancil; M Quinan; J S Beckler; E R Hall; J Culter; C G Smith; M Taillefert; F J Stewart
Journal:  ISME J       Date:  2021-02-21       Impact factor: 11.217

3.  Diversity hotspot and unique community structure of foraminifera in the world's deepest marine blue hole - Sansha Yongle Blue Hole.

Authors:  Qingxia Li; Yanli Lei; Raphaёl Morard; Tiegang Li; Baodong Wang
Journal:  Sci Rep       Date:  2020-06-24       Impact factor: 4.379

4.  Microbial Diversity and Metabolic Potential in the Stratified Sansha Yongle Blue Hole in the South China Sea.

Authors:  Peiqing He; Linping Xie; Xuelei Zhang; Jiang Li; Xuezheng Lin; Xinming Pu; Chao Yuan; Ziwen Tian; Jie Li
Journal:  Sci Rep       Date:  2020-04-06       Impact factor: 4.379

5.  Environmental DNA Sequencing Reveals a Highly Complex Eukaryote Community in Sansha Yongle Blue Hole, Xisha, South China Sea.

Authors:  Yueteng Liu; Hui He; Liang Fu; Qian Liu; Zuosheng Yang; Yu Zhen
Journal:  Microorganisms       Date:  2019-11-28
  5 in total

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