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1.
Natl Sci Rev ; 10(4): nwad008, 2023 Apr.
Artigo em Inglês | MEDLINE | ID: mdl-36960219

RESUMO

Contrasting views exist on timing and mechanisms of Tertiary crustal uplift in the NE Tibetan Plateau based on different approaches, with many models attributing surface uplift to crustal shortening. We carry out a comprehensive investigation of mid-Tertiary stratigraphy, sedimentology, and volcanism in the West Qinling, Hoh Xil and Qaidam basin, and the results challenge previous views. It was held that the discordance between Oligocene and Miocene strata is an angular unconformity in the West Qinling, but our field observations show that it is actually a disconformity, indicative of vertical crustal uplifting rather than crustal shortening at the Oligocene to Miocene transition. Widespread occurrence of synsedimentary normal faults in mid-Tertiary successions implicates supracrustal stretching. Miocene potassic-ultrapassic and mafic-ultramafic volcanics in the Hoh Xil and West Qinling suggest a crucial role of deep thermomechanical processes in generating crust- and mantle-sourced magmatism. Also noticeable are the continuity of mid-Tertiary successions and absence of volcanics in the Qaidam basin. Based on a holistic assessment of stratigraphic-sedimentary processes, volcanic petrogenesis, and spatial variations of lithospheric thicknesses, we speculate that small-sale mantle convection might have been operating beneath northeast Tibet in the mid-Tertiary. It is assumed that northward asthenospheric flow was impeded by thicker cratonic lithosphere of the Qaidam and Alxa blocks, thereby leading to edge convection. The edge-driven convection could bring about surface uplift, induce supracrustal stretching, and trigger vigorous volcanism in the Hoh Xil and West Qinling in the mid-Tertiary period. This mechanism satisfactorily explains many key geologic phenomena that are hardly reconciled by previous models.

2.
Artigo em Chinês | MEDLINE | ID: mdl-22096849

RESUMO

OBJECTIVE: To investigate the effects of the cadmium chloride on the DNA damage and the expression of the gadd153 and gadd45beta promoter and mRNA in HepG2 cells. METHODS: DNA damage induced by cadmium chloride was detected by comet assay. The plasmids (pGADD153-Luc and pG45-Luc) containing DNA damage and repair inducible gene 153 and 45 (gadd153 and gadd45beta) promoter and luciferase and gadd45beta reporter gene were constructed. The activity of gadd153 and gadd45beta promoter were represented by the luciferase activity, the inducible luciferase activities was detected by bioluminescence. The expression of gadd153 and gadd45beta mRNA was detected by RT-PCR. RESULTS: The results of comet assay indicated that Olive Tail Moment induced by the cadmium chloride increased significantly at the dose of 100, 300 micromol/L, compared with the control (P < 0.05). The luciferase activity analysis showed that the expression levels of gadd153 promoter increased significantly in 1, 5, 10 micromol/L treatment group, compared with the control (P < 0.05). The expression levels of gadd45beta promoter in 5, 10 micromol/L treatment group were significantly higher than that in control group (P < 0.05). The expression levels of gadd153 mRNA induced by cadmium chloride at the doses of 1, 5, 10 micromol/L and the expression levels of gadd45beta mRNA induced at the doses of 5, 10 micromol/L were significantly higher than thoae in control group (P < 0.05). CONCLUSION: The cadmium chloride can induce the DNA damage and increase the expression levels of the gadd153 and gadd45beta promoters in HepG2 cells.


Assuntos
Antígenos de Diferenciação/genética , Cloreto de Cádmio/toxicidade , Dano ao DNA/efeitos dos fármacos , Fator de Transcrição CHOP/genética , Ensaio Cometa , Genes Reporter , Células Hep G2 , Humanos , Plasmídeos , Regiões Promotoras Genéticas , RNA Mensageiro/genética
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