Chemical and Physical Characteristics of Red Soils from Zhejiang Province, Southern China

2004 ◽  
pp. 63-87 ◽  
Author(s):  
Mingkui Zhang ◽  
Zhenli He ◽  
M. J. Wilson
2019 ◽  
Vol 32 ◽  
pp. 101427 ◽  
Author(s):  
Jiangping Ren ◽  
Jimin Sun ◽  
Zhengting Wang ◽  
Feng Ling ◽  
Xuguang Shi ◽  
...  

2016 ◽  
Vol 155 (3) ◽  
pp. 549-567 ◽  
Author(s):  
XILIN ZHAO ◽  
YANG JIANG ◽  
GUANGFU XING ◽  
ZHIHONG CHEN ◽  
KAI LIU ◽  
...  

AbstractThe Honggong pluton is the largest ferroan alkalic (A-type) granite intrusion emplaced along the Jiangshan–Shaoxing fault zone in southwestern Zhejiang Province, and has important implications for understanding the Late Mesozoic tectonic evolution of SE China. U–Pb ages of 138.7 ± 0.8, 134.2 ± 1.1, 128.5 ± 1.5 and 126.1 ± 0.9 Ma were obtained from zircon by laser ablation–inductively coupled plasma–mass spectrometry, indicating that the Honggong pluton formed in the Early Cretaceous. The Honggong pluton has a clear ferroan alkalic (A-type) granite geochemical signature with, for example, high total alkali contents and FeOt/(FeOt+ MgO) values. The Sr–Nd–Hf isotopic compositions suggest that there was juvenile material in the magma source. Geochemical evidence indicates that the pluton was derived through extensive fractionation of melts that contained both asthenospheric mantle and Mesoproterozoic crustal components. These rare granites in southern China were emplaced during five episodes at 235–225, 190, 165–155, 100–90 and 140–120 Ma. The age of the Honggong pluton suggests that localized extension in southwestern Zhejiang Province began as early as ~138 Ma and continued to 126 Ma. This Early Cretaceous extensional event was triggered by localized rollback of the subducting Pacific Plate.


2020 ◽  
Vol 222 (2) ◽  
pp. 1213-1223
Author(s):  
Yan Han ◽  
Xiuming Liu ◽  
Guoyong Zhao ◽  
Zhenke Zhang ◽  
Bin Lü ◽  
...  

SUMMARY The loess from the northern piedmont of the Dabie Mountains is in a transition area between loess from the Chinese Loess Plateau, the Quaternary red soils of southern China and the Xiashu loess. Despite its significant location, the study has been inadequate. In this study, the Guangshan section in the northern piedmont of the Dabie Mountains was selected for investigation. Environmental magnetism, geochemistry, colour reflectance and optical diffuse reflection spectroscopy analyses were applied to detect the magnetic variations in the loess. The results showed that (1) the magnetic minerals consisted mainly of magnetite, maghemite, hematite and goethite, which are the same as those in the Quaternary loess from the Chinese Loess Plateau, the Xiashu loess and the Quaternary red soils of southern China. The average magnetic particles were in the pseudo-single domain, like those of the Chinese Loess Plateau loess. (2) Unit III of the Guangshan section (2.4–4 m), with high chemical index of alteration and low Ba-index, was demonstrated as the most strongly developed palaeosol in the whole section, in agreement with field observations (more Fe-Mn films and weakly vermiculated development). However, it exhibited minimal susceptibility values and the lowest concentration of fine ferrimagnetic minerals. Simultaneously, the unit had low hematite to goethite ratio (Hm/Gt), suggesting that the pedogenic environment was humid; and it also had high values of b* and Gt%, implying that there was more goethite. Therefore, we can conclude that excessive soil moisture and intensive pedogenesis dissolved the fine ferrimagnetic minerals originally produced by pedogenesis and transformed them into goethite. These results could help to trace the palaeoclimatic evolution of the study area and clarify the magnetic variations of loess in different climates throughout China.


2015 ◽  
Vol 81 (9) ◽  
pp. 3086-3103 ◽  
Author(s):  
Xiaoxuan Guo ◽  
Ning Liu ◽  
Xiaomin Li ◽  
Yun Ding ◽  
Fei Shang ◽  
...  

ABSTRACTRed soils, which are widely distributed in tropical and subtropical regions of southern China, are characterized by low organic carbon, high content of iron oxides, and acidity and, hence, are likely to be ideal habitats for acidophilic actinomycetes. However, the diversity and biosynthetic potential of actinomycetes in such habitats are underexplored. Here, a total of 600 actinomycete strains were isolated from red soils collected in Jiangxi Province in southeast China. 16S rRNA gene sequence analysis revealed a high diversity of the isolates, which were distributed into 26 genera, 10 families, and 7 orders within the classActinobacteria; these taxa contained at least 49 phylotypes that are likely to represent new species within 15 genera. The isolates showed good physiological potentials for biosynthesis and biocontrol. Chemical screening of 107 semirandomly selected isolates spanning 20 genera revealed the presence of at least 193 secondary metabolites from 52 isolates, of which 125 compounds from 39 isolates of 12 genera were putatively novel. Macrolides, polyethers, diketopiperazines, and siderophores accounted for most of the known compounds. The structures of six novel compounds were elucidated, two of which had a unique skeleton and represented characteristic secondary metabolites of a putative novelStreptomycesphylotype. These results demonstrate that red soils are rich reservoirs for diverse culturable actinomycetes, notably members of the familiesStreptomycetaceae,Pseudonocardiaceae, andStreptosporangiaceae, with the capacity to synthesize novel bioactive compounds.


Geoderma ◽  
2003 ◽  
Vol 115 (1-2) ◽  
pp. 75-84 ◽  
Author(s):  
Renkou Xu ◽  
Anzhen Zhao ◽  
Qingman Li ◽  
Xiaoling Kong ◽  
Guoliang Ji

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