scholarly journals Brine chemistry and mineral sedimentary characteristics of undersand salt lakes in Qaidam Basin:an example from the peripheral zone of Qarhan salt lake

1995 ◽  
Vol 7 (4) ◽  
pp. 327-333
Author(s):  
Hu Dongsheng ◽  
2021 ◽  
Vol 9 ◽  
Author(s):  
Jun Li ◽  
Xiying Zhang ◽  
Mingyue Hu ◽  
Wenxia Li ◽  
Weiliang Miao ◽  
...  

The fluid inclusion composition of halite can help track chemical composition of ancient fluids and, thus, serves as a reliable index to analyze ancient brine in salt lakes. Qarhan Salt Lake (QSL) is the largest potash brine deposit in China. Although the mixing of modern river water and Ca-Cl deep water is widely accepted as potassium formation, the mixing characteristics in the time domain and driving factors of deep water are still unclear. Here, the chemical composition of fluid inclusions in primary halite samples collected from the ISL1A borehole in QSL was measured by LA-ICP-MS technology. The analysis results show that, during the formation stage of the S4 salt layer in QSL, the main potassium salt layer, the contents of Ca2+ and Sr2+ in brine increased significantly. There is evidence confirming that Ca-Cl deep water is beneficial to the enrichment of potassium and the surrounding rivers generally develop terraces. It suggests that, during the formation stage of the QSL potassium salt layer, more Ca-Cl inflow water of the northern margin supplies the salt lake, inferring that it was driven by tectonic activities. In addition, the chemical composition of halite fluid inclusions shows that there is an anomaly in geochemistry at the early stage of salt formation in QSL. By combining the time of tectonic activities, it is inferred that the anomaly is not caused by tectonic activities but maybe caused by a salt-forming event. This work indicates that deep water and tectonic movement have a huge impact on the evolution of salt lakes. Therefore, it is necessary to consider the influence of deep water and tectonic activities on the salt-forming evolution stage of salt lakes when studying the salt-forming evolution stage of salt lakes and paleoclimate by using salt lake deposition.


Zootaxa ◽  
2021 ◽  
Vol 5082 (4) ◽  
pp. 393-400
Author(s):  
ZHENHUA LIU ◽  
ADAM ŚLIPIŃSKI ◽  
HONG PANG

Apalochrini comprises nearly half of the genera of Australian Melyridae, which are all recognized by male specific characters, and are commonly found on grasses, flowers and riverside or seashore rocks. Here we describe a new genus Salsolaius gen. nov. from Lake Way of Western Australia, representing the first known genus of Australian Melyridae inhabitating in salt lakes. The new genus can be easily distinguished by asymmetrically biserrate antennae and exposed apical abdomen from above in both male and female, the former characters is firstly found in Melyridae. Consequently, Salsolaius biserratus sp. nov. was described as the type species of this genus. An updated key to genera of Australian Apalochrini is provided.  


2015 ◽  
Vol 33 (6) ◽  
pp. 1426-1435 ◽  
Author(s):  
Xiaocan Yu ◽  
Chunlian Wang ◽  
Chenglin Liu ◽  
Zhaochong Zhang ◽  
Haiming Xu ◽  
...  

2021 ◽  
Vol 12 ◽  
Author(s):  
Junqing Luo ◽  
Zhechao Zhang ◽  
Yazhou Hou ◽  
Fengwei Diao ◽  
Baihui Hao ◽  
...  

Lake littoral zones can also be regarded as another extremely hypersaline environment due to hypersaline properties of salt lakes. In this study, high-throughput sequencing technique was used to analyze bacteria and fungi from different rhizocompartments (rhizosphere and endosphere) of four dominant plants along the salinity gradient in the littoral zones of Ejinur Salt Lake. The study found that microbial α-diversity did not increase with the decrease of salinity, indicating that salinity was not the main factor on the effect of microbial diversity. Distance-based redundancy analysis and regression analysis were used to further reveal the relationship between microorganisms from different rhizocompartments and plant species and soil physicochemical properties. Bacteria and fungi in the rhizosphere and endosphere were the most significantly affected by SO42–, SOC, HCO3–, and SOC, respectively. Correlation network analysis revealed the potential role of microorganisms in different root compartments on the regulation of salt stress through synergistic and antagonistic interactions. LEfSe analysis further indicated that dominant microbial taxa in different rhizocompartments had a positive response to plants, such as Marinobacter, Palleronia, Arthrobacter, and Penicillium. This study was of great significance and practical value for understanding salt environments around salt lakes to excavate the potential microbial resources.


1995 ◽  
Vol 7 (4) ◽  
pp. 321-326
Author(s):  
Liu Xingqi ◽  
◽  
Yu Shengsong ◽  
Shao Mingyu

2018 ◽  
Vol 497 ◽  
pp. 128-145 ◽  
Author(s):  
QiShun Fan ◽  
Tim K. Lowenstein ◽  
HaiCheng Wei ◽  
Qin Yuan ◽  
ZhanJie Qin ◽  
...  

2019 ◽  
Vol 55 (5) ◽  
pp. 3643-3653 ◽  
Author(s):  
Jiyan Li ◽  
Ling Zhou ◽  
Jialiang Yan ◽  
Xujia Cui ◽  
Yingying Cai

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