scholarly journals Ubiquitous production of branched glycerol dialkyl glycerol tetraethers (brGDGTs) in global marine environments: a new source indicator for brGDGTs

2016 ◽  
Author(s):  
Wenjie Xiao ◽  
Yinghui Wang ◽  
Shangzhe Zhou ◽  
Limin Hu ◽  
Huan Yang ◽  
...  

Abstract. Presumed source specificity of branched and isoprenoid glycerol dialkyl glycerol tetraethers (GDGTs) led to the development of several biomarker proxies for biogeochemical cycle and paleoenvironment. However, recent studies reveal that brGDGTs are also produced in aquatic environments besides soils and peat. Here we examined three cores from the Bohai Sea and found distinct difference in brGDGT compositions varying with the distance from the Yellow River mouth. We thus proposed an abundance ratio of hexamethylated to pentamethylated brGDGT (IIIa / IIa) to evaluate brGDGT sources. The compiling of globally distributed 1354 marine sediments and 589 soils shows that the IIIa / IIa ratio is generally < 0.59 for soils, 0.59–0.92 and > 0.92 for marine sediments with and without significant terrestrial inputs, respectively. Such disparity confirms the existence of two sources of brGDGTs, a terrestrial origin with lower IIIa / IIa and a marine origin with higher IIIa / IIa, likely due to different pH influence. The application of the IIIa / IIa ratio to the East Siberian Arctic Shelf proves it a sensitive source indicator for brGDGTs, which is helpful for accurate estimation of organic carbon source and paleoclimates in marine settings.

2016 ◽  
Vol 13 (20) ◽  
pp. 5883-5894 ◽  
Author(s):  
Wenjie Xiao ◽  
Yinghui Wang ◽  
Shangzhe Zhou ◽  
Limin Hu ◽  
Huan Yang ◽  
...  

Abstract. Presumed source specificity of branched glycerol dialkyl glycerol tetraethers (brGDGTs) from bacteria thriving in soil/peat and isoprenoid GDGTs (iGDGTs) from aquatic organisms led to the development of several biomarker proxies for biogeochemical cycle and paleoenvironmental reconstructions. However, recent studies reveal that brGDGTs are also produced in aquatic environments besides soils and peat. Here we examined three cores from the Bohai Sea, and found distinct difference in brGDGT compositions varying with the distance from the Yellow River mouth. We thus propose an abundance ratio of hexamethylated to pentamethylated brGDGT (IIIa ∕ IIa) to evaluate brGDGT sources. The compilation of globally distributed 1354 marine sediments and 589 soils shows that the IIIa ∕ IIa ratio is generally < 0.59 in soils and 0.59–0.92 and > 0.92 in marine sediments with and without significant terrestrial inputs, respectively. Such disparity confirms the existence of two sources for brGDGTs, a terrestrial origin with lower IIIa ∕ IIa and a marine origin with higher IIIa ∕ IIa, which is likely attributed to a generally higher pH and the production of brGDGTs in cold deep water in marine waters. The application of the IIIa ∕ IIa ratio to the East Siberian Arctic Shelf proves it to be a sensitive source indicator for brGDGTs, which is helpful for accurate estimation of organic carbon source and paleoclimates in marine settings.


2013 ◽  
Vol 31 (4) ◽  
pp. 876-885 ◽  
Author(s):  
Shuqing Qiao ◽  
Xuefa Shi ◽  
Jingjing Gao ◽  
Yanguang Liu ◽  
Gang Yang ◽  
...  

2020 ◽  
Vol 236 ◽  
pp. 106639 ◽  
Author(s):  
Xingmin Liu ◽  
Lulu Qiao ◽  
Yi Zhong ◽  
Xiuquan Wan ◽  
Wenjing Xue ◽  
...  

2015 ◽  
Vol 14 (3) ◽  
pp. 433-445 ◽  
Author(s):  
Nan Wang ◽  
Guangxue Li ◽  
Jishang Xu ◽  
Lulu Qiao ◽  
Olusegun A. Dada ◽  
...  

2007 ◽  
Vol 27 (6) ◽  
pp. 854-871 ◽  
Author(s):  
Houjie Wang ◽  
Zuosheng Yang ◽  
Yunhai Li ◽  
Zhigang Guo ◽  
Xiaoxia Sun ◽  
...  

2011 ◽  
Vol 1 (32) ◽  
pp. 13
Author(s):  
Haibo Zong ◽  
Pingxing Ding ◽  
Fengyan Shi

Yellow River is famous for its high sediment concentration, which carries a huge amount of sediment into Bohai Sea during the flood season. In the mouth of Yellow River, the suspended sediment concentration (here after: SSC) are relatively high and the average depth is generally shallow. Recent studies indicated that in the shallow and micro-tide area, wave usually is a primary mechanism for bottom sediment resuspension. Most numerical studies of sediment transport in the Yellow River mouth didn't include the wave effects. To analyze the sediment transport in the Yellow River mouth with wave effect, a Coastal Sediment Transport Modeling System (CSTMS) was applied in this study.


2010 ◽  
Vol 11 (4) ◽  
pp. 491-497
Author(s):  
Chong HUANG ◽  
Gaohuan LIU ◽  
Hailong ZHANG ◽  
Kai SHAN

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