Bacterial influence on chromophoric dissolved organic matter in coastal waters of the northern South China Sea

2016 ◽  
Vol 76 (3) ◽  
pp. 207-217 ◽  
Author(s):  
X Yuan ◽  
W Zhou ◽  
H Huang ◽  
T Yuan ◽  
X Li ◽  
...  
Keyword(s):  
Organic Matter ◽  
South China Sea ◽  
Dissolved Organic Matter ◽  
South China ◽  
Coastal Waters ◽  
Northern South China Sea ◽  
Chromophoric Dissolved Organic Matter ◽  
China Sea

scholarly journals First records of the seamoth, Pegasus nanhaiensis (Actinopterygii: Syngnathiformes: Pegasidae), from the southern South China Sea, with notes on fresh coloration

2022 ◽  
Vol 52 (1) ◽  
pp. 1-8
Author(s):  
Takahiro Akaike ◽  
Sirikanya Chungthanawong ◽  
Hiroyuki Motomura
Keyword(s):  
South China Sea ◽  
South China ◽  
Coastal Waters ◽  
Northern South China Sea ◽  
Gulf Of Thailand ◽  
Malay Peninsula ◽  
Southern South China Sea ◽  
China Sea ◽  
Fish Market ◽  
First Time

Three seamoth specimens (45.5–56.9 mm standard length; SL) (Syngnathiformes: Pegasidae), originally identified as Pegasus laternarius Cuvier, 1829, but now recognized as representing P. nanhaiensis Zhang, Wang et Lin, 2020, a species recently described from the northern South China Sea off Yangjiang and Beihai, China, were obtained at a local fish market in Maha Chai, Samut Sakhon Province, Thailand on 6 July 2012, having been caught in the northern Gulf of Thailand. In addition, single specimens, reported as P. laternarius or Spinipegasus laternarius from Bidong Island, South China Sea off the Malay Peninsula (46.1 mm SL) and from Ko Kradat, Trat Province, eastern Gulf of Thailand (66.1 mm SL), were re-identified here as P. nanhaiensis. Thai specimens and Malaysian record represent the first records of P. nanhaiensis from Thailand and Malaysia, respectively, and from outside Chinese coastal waters. Additionally, the Bidong specimen is the southernmost record for the species. The fresh coloration of P. nanhaiensis is described for the first time.

Metaproteomic characterization of dissolved organic matter in the water column of the South China Sea

2011 ◽  
Vol 56 (5) ◽  
pp. 1641-1652 ◽  
Author(s):  
Da-Zhi Wang ◽  
Hong-Po Dong ◽  
Zhang-Xian Xie ◽  
Min-Han Dai ◽  
Hua-Sheng Hong
Keyword(s):  
Organic Matter ◽  
South China Sea ◽  
Dissolved Organic Matter ◽  
Water Column ◽  
South China ◽  
The South China Sea ◽  
The South ◽  
China Sea

scholarly journals An Areal Assessment of Subseafloor Carbon Cycling in Cold Seeps and Hydrate-Bearing Areas in the Northern South China Sea

Geofluids ◽  
2019 ◽  
Vol 2019 ◽  
pp. 1-14 ◽  
Author(s):  
Yanping Zhang ◽  
Min Luo ◽  
Yu Hu ◽  
Hongbin Wang ◽  
Duofu Chen
Keyword(s):  
Organic Matter ◽  
South China Sea ◽  
Carbon Cycling ◽  
South China ◽  
Northern South China Sea ◽  
Continental Margins ◽  
Cold Seeps ◽  
Carbonate Precipitation ◽  
Organic Matter Degradation ◽  
China Sea

Gas hydrates, acting as a dynamic methane reservoir, store methane in the form of a solid phase under high-pressure and low-temperature conditions and release methane through the sediment column into seawater when they are decomposed. The seepage of methane-rich fluid (i.e., cold hydrocarbon seeps) fuels the chemosynthetic biota-inhabited surface sediments and represents the major pathway to transfer carbon from sediments to the water column. Generally, the major biogeochemical reactions related to carbon cycling in the anoxic marine sediments include organic matter degradation via sulfate reduction (OSR), anaerobic oxidation of methane (AOM), methanogenesis (ME), and carbonate precipitation (CP). In order to better understand the carbon turnover in the cold seeps and gas hydrate-bearing areas of the northern South China Sea (SCS), we collected geochemical data of 358 cores from published literatures and retrieved 37 cores and corresponding pore water samples from three areas of interest (i.e., Xisha, Dongsha, and Shenhu areas). Reaction-transport simulations indicate that the rates of organic matter degradation and carbonate precipitation are comparable in the three areas, while the rates of AOM vary over several orders of magnitude (AOM: 8.3-37.5 mmol·m-2·yr-1 in Dongsha, AOM: 12.4-170.6 mmol·m-2·yr-1 in Xisha, and AOM: 9.4-30.5 mmol·m-2·yr-1 in Shenhu). Both the arithmetical mean and interpolation mean of the biogeochemical processes were calculated in each area. Averaging these two mean values suggested that the rates of organic matter degradation in Dongsha (25.7 mmol·m-2·yr-1) and Xisha (25.1 mmol·m-2·yr-1) are higher than that in Shenhu (12 mmol·m-2·yr-1) and the AOM rate in Xisha (135.2 mmol·m-2·yr-1) is greater than those in Dongsha (27.8 mmol·m-2·yr-1) and Shenhu (17.5 mmol·m-2·yr-1). In addition, the rate of carbonate precipitation (32.3 mmol·m-2·yr-1) in Xisha is far higher than those of the other two regions (5.3 mmol·m-2·yr-1 in Dongsha, 5.8 mmol·m-2·yr-1 in Shenhu) due to intense AOM sustained by gas dissolution. In comparison with other cold seeps around the world, the biogeochemical rates in the northern SCS are generally lower than those in active continental margins and special environments (e.g., the Black sea) but are comparable with those in passive continental margins. Collectively, ~2.8 Gmol organic matter was buried and at least ~0.82 Gmol dissolved organic and inorganic carbon was diffused out of sediments annually. This may, to some extent, have an impact on the long-term deep ocean carbon cycle in the northern SCS.

Dimethylsulfide and dimethylsulfoniopropionate production along coastal waters of the northern South China Sea

2016 ◽  
Vol 117 ◽  
pp. 118-125 ◽  
Author(s):  
Ping-Ping Shen ◽  
Ya-Nan Tang ◽  
Hua-Jian Liu ◽  
Gang Li ◽  
Yan Wang ◽  
...  
Keyword(s):  
South China Sea ◽  
South China ◽  
Coastal Waters ◽  
Northern South China Sea ◽  
China Sea
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