Geologically controlled intermittent gas eruption and its impact on bottom water temperature and chemosynthetic communities—A case study in the “HaiMa” cold seeps, South China Sea

2020 ◽  
Vol 55 (9) ◽  
pp. 6066-6078 ◽  
Author(s):  
Jiangong Wei ◽  
Jiwei Li ◽  
Tingting Wu ◽  
Wei Zhang ◽  
Jiangtao Li ◽  
...  
Keyword(s):  
South China Sea ◽  
Water Temperature ◽  
South China ◽  
Bottom Water ◽  
Cold Seeps ◽  
Bottom Water Temperature ◽  
China Sea

Variance of Bottom Water Temperature at the Continental Margin of the Northern South China Sea

2021 ◽  
Vol 126 (2) ◽  
Author(s):  
Peng‐Qi Huang ◽  
Xian‐Rong Cen ◽  
Shuang‐Xi Guo ◽  
Yuan‐Zheng Lu ◽  
Sheng‐Qi Zhou ◽  
...  
Keyword(s):  
South China Sea ◽  
Water Temperature ◽  
Continental Margin ◽  
South China ◽  
Bottom Water ◽  
Northern South China Sea ◽  
Bottom Water Temperature ◽  
China Sea

scholarly journals Distinct Bottom-Water Bacterial Communities at Methane Seeps With Various Seepage Intensities in Haima, South China Sea

2021 ◽  
Vol 8 ◽  
Author(s):  
Xiaopeng Li ◽  
Zehan Dai ◽  
Pengfei Di ◽  
Junxi Feng ◽  
Jun Tao ◽  
...  
Keyword(s):  
South China Sea ◽  
Bacterial Community ◽  
Water Column ◽  
South China ◽  
Bottom Water ◽  
Methane Content ◽  
Cold Seeps ◽  
Community Structures ◽  
Methane Seeps ◽  
China Sea

Methane seeps are chemosynthetic ecosystems in the deep-sea environment. Microbial community structures have been extensively studied in the seepage-affected sediments and investigation in the water column above the seeping sites is still lacking. In this study, prokaryotic communities in the bottom water about 50 cm from the seabed at methane seeps with various seepage intensities in Haima, South China Sea were comparatively studied by using 16S ribosomal RNA gene sequencing. These sites were assigned based on their distinct methane content levels and seafloor landscapes as the non-seepage (NS) site, low-intensity seepage (LIS) site, and high-intensity seepage (HIS) site. The abundances of the dominant phyla Proteobacteria, Bacteroidetes, and Actinobacteria differed significantly between NS and the two seepage sites (p < 0.05). Alpha diversity differed among the three sites with the HIS site showing the lowest community diversity. Principal component analysis revealed highly divergent bacterial community structures at three sites. Many environmental variables including temperature, alkalinity, pH, methane, dissolved organic carbon (DOC), and inorganic nutrients were measured. Redundancy analysis indicated that methane content is the key environmental factor driving bacterial community variation (p = 0.001). Linear discriminant analysis effect size analysis identified various differentially enriched genera at the LIS and HIS sites. Phylogenetic analysis revealed close phylogenetic relationship among the operational taxonomic units of these genera with known oil-degrading species, indicating oil seepage may occur at the Haima cold seeps. Co-occurrence networks indicated that the strength of microbial interactions was weakest at the HIS site. This study represents a comprehensive comparison of microbial profiles in the water column of cold seeps in the SCS, revealing that the seepage intensity has a strong impact on bacterial community dynamics.

scholarly journals A Quantitative Assessment of Methane-Derived Carbon Cycling at the Cold Seeps in the Northwestern South China Sea

Minerals ◽  
2020 ◽  
Vol 10 (3) ◽  
pp. 256 ◽  
Author(s):  
Junxi Feng ◽  
Niu Li ◽  
Min Luo ◽  
Jinqiang Liang ◽  
Shengxiong Yang ◽  
...  
Keyword(s):  
South China Sea ◽  
South China ◽  
Bottom Water ◽  
Cold Seep ◽  
Anaerobic Oxidation Of Methane ◽  
Cold Seeps ◽  
Dissolved Carbon ◽  
China Sea ◽  
Seafloor Observation ◽  
Gas Hydrate Formation

Widespread cold seeps along continental margins are significant sources of dissolved carbon to the ocean water. However, little is known about the methane turnovers and possible impact of seepage on the bottom seawater at the cold seeps in the South China Sea (SCS). We present seafloor observation and porewater data of six push cores, one piston core and three boreholes as well as fifteen bottom-water samples collected from four cold seep areas in the northwestern SCS. The depths of the sulfate–methane transition zone (SMTZ) are generally shallow, ranging from ~7 to <0.5 mbsf (meters below seafloor). Reaction-transport modelling results show that methane dynamics were highly variable due to the transport and dissolution of ascending gas. Dissolved methane is predominantly consumed by anaerobic oxidation of methane (AOM) at the SMTZ and trapped by gas hydrate formation below it, with depth-integrated AOM rates ranging from 59.0 and 591 mmol m−2 yr−1. The δ13C and Δ14C values of bottom-water dissolved inorganic carbon (DIC) suggest discharge of 13C- and 14C-depleted fossil carbon to the bottom water at the cold seep areas. Based on a two-endmember estimate, cold seeps fluids likely contribute 16–26% of the bottom seawater DIC and may have an impact on the long-term deep-sea carbon cycle. Our results reveal the methane-related carbon inventories are highly heterogeneous in the cold seep systems, which are probably dependent on the distances of the sampling sites to the seepage center. To our knowledge, this is the first quantitative study on the contribution of cold seep fluids to the bottom-water carbon reservoir of the SCS, and might help to understand the dynamics and the environmental impact of hydrocarbon seep in the SCS.

Ahead of Bit Pore Pressure Prediction using VSP - A Case Study in South China Sea

2010 ◽  
Author(s):  
Yuhong Xie ◽  
Jun Cai ◽  
Ling Xia Zhen ◽  
Hong Tian ◽  
Yan Hua Li ◽  
...  
Keyword(s):  
South China Sea ◽  
Pore Pressure ◽  
South China ◽  
China Sea ◽  
Pore Pressure Prediction

Towards a 90% renewable energy future: A case study of an island in the South China Sea

2017 ◽  
Vol 142 ◽  
pp. 28-41 ◽  
Author(s):  
Bin Ye ◽  
Kai Zhang ◽  
JingJing Jiang ◽  
Lixin Miao ◽  
Ji Li
Keyword(s):  
Renewable Energy ◽  
South China Sea ◽  
South China ◽  
The South China Sea ◽  
The South ◽  
China Sea
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