A5101884606- Geology and Paleoclimatology Research
- Pleistocene-Era Hominins and Archaeology
- Archaeology and ancient environmental studies
- Groundwater and Isotope Geochemistry
- Geological formations and processes
- Karst Systems and Hydrogeology
- Air Quality and Health Impacts
- Atmospheric chemistry and aerosols
- Atmospheric Ozone and Climate
- Geochemistry and Elemental Analysis
South China Normal University
2019-2022
Ludong University
2015-2022
Hong Kong Polytechnic University
2000
Abstract. Stalagmite ky1, with a length of 75 mm and the upper part (from top to 42.769 depth) consisting 678 laminae, was collected from Kaiyuan Cave in coastal area Shandong Peninsula, northern China, located warm temperate zone East Asia monsoon area. Based on high-precision dating U–230Th technique continuous counting 1st 678th laminae have been confirmed be AD 1894 ± 20 1217 bottom, respectively. By measurement thickness δ18O ratios, we haved obtained time series data ratios 20,...
Abstract. Stalagmite ky1 was collected from Kaiyuan Cave in coastal areas of Shandong Peninsula, northern China, located at warm temperate zone and East Asia monsoon area, it 75 mm length, the top 42.77 developed 678 laminae. Based on high precision dating with U-230Th technique, by continuous laminae counting, can be confirmed that 1st 678th layer were 1217 1892 AD to bottom respectively. By measurement thickness δ18O values, we got data value time series AD, analyzed climatic significance...
Abstract. Abstract: Stalagmite KY-1 was collected from Kaiyuan Cave, which is in the warm temperate zone and East Asia monsoon area Shandong Peninsula, coastal Northern China. Based on results of U-230Th-dating, continuous counting laminae, linear interpolation/extrapolation, we determined that stalagmite grew over last 1 ka between AD 892 1894. This period includes Medieval Warm Period (MWP), Little Ice Age (LIA), an early stage Current (CWP), corresponds to a time late Tang Dynasty Qing...