AIM: To explore the effects of chlorogenic acid (CGA) on endothelial dysfunction in db/db mice and the possible mechanism. METHODS: Male db/db mice (n=12) were divided into control group and CGA group, with 6 mice in each group. The mice in CGA group were treated with diet containing 0.02% CGA, while the mice in control group were given normal diet only. The observation period was 12 weeks. Fasting blood glucose level, tail blood pressure and the body weight were analyzed each week. At the end of the 12th week, the mice were anesthetized and blood was taken from carotid artery. The plasma levels of heme oxygenase-1 (HO-1), catalase (CAT), NAD(P)H dehydrogenase quinone 1 (NQO1) and glutathione peroxidase-1 (GPx-1) were measured by ELISA. The mouse aortas were isolated, and the superoxide anion and nitric oxide (NO) levels were measured by DHE and DAF-2 DA staining, respectively. Wire Myograph System was used to detect the vasorelaxation of db/db mouse aorta. The protein levels of peroxisome proliferator-activated receptor α (PPARα), nuclear factor E2-related factor 2 (Nrf2), phosphorylated AMP-activated protein kinase (p-AMPK), phosphorylated endothelial NO synthase (p-eNOS), P22phox and P47phox were determined by Western blot. RESULTS: Dietary CGA decreased fasting blood glucose and body weight in db/db mice as compared with control group (P<0.01 or P<0.05). The plasma levels of HO-1, CAT, NQO1 and GPx-1 in CGA group were higher than those in control group (P<0.01 or P<0.05). Administration of CGA for 12 weeks attenuated superoxide anion level, increased NO level in the mouse endothelium and improved endothelium-dependent relaxation of the db/db mouse aorta. CGA also increased the protein levels of PPARα, Nrf2, p-AMPK and p-eNOS, and decreased P22phox and P47phox levels (P<0.01). CONCLUSION: Dietary CGA improves db/db mouse endothelium-dependent relaxation. This effect may be related to the increases in the levels of antioxidant molecules PPARα, Nrf2 and p-AMPK, and the up-regulation of antioxidant capacity, thus decreasing the oxidative stress, promoting eNOS phosphorylation, and increasing NO level. 相似文献
Floods and eolian activities are the dominant external agents to shape the topographic forms in ephemeral desert streams of drylands. So far, few studies have discussed the modern processes of eolian–fluvial interactions. To bridge this gap, we studied the modern interactions of eolian and fluvial process in a desert ephemeral river, the Maobula Gully in Inner Mongolia, which exhibits typical eolian–fluvial interactions.
Materials and methods
Multisource data such as integrated particle size data, hydrological data from the Tugerige Hydrological Station, high-spatial-resolution satellite images, and an eolian sediment saltation emission model were integrated to analyze the effects of eolian and fluvial delivery to the sediment on the riverbed, the eolian sediment feeding rate to the gully, the transport of sediment in flood events, and the interactions between eolian and fluvial processes.
Results and discussion
The desert reach of the Maobula Gully is a replacement reach between coarse sediment from the upper reaches and eolian sediment from the Kubuqi Desert. The annual eolian sediment feeding into the gully exhibited a significant decreasing trend. The eolian sediment into the gully increases the available sediment and the bed roughness, affecting the transport of sediment during floods. The sediment concentration and yields in flood events are mainly decided by the discharge and water yield, respectively. Through a comparison of the channel forms between 1970 and 2013, a recovery mechanism in the Maobula Gully was identified, which involves the equilibrium state between abrupt flood erosion and continuous dune migration.
Conclusions
This study analyzed the modern processes of eolian and fluvial processes and their interactions in a typical ephemeral desert stream named the Maobula Gully, and some interesting results were found. We believe that the methodology and results could provide references and evidence for understanding the mechanisms of fluvial and eolian interactions in other ephemeral desert streams around the world.