supported by the Project of State Oceanic Administration, China (908-01-BC15);the National Natural Science Foundation of China (41374073, 41025013 and40821091)
Magnetic minerals in sediments of the continental shelf are sensitive to environmental changes.Therefore,to determine the exact phases of magnetic minerals is the prerequisite to investigate the paleoenvironmental sig...
supported by the National Basic Research Program of China (2010CB428901);the National Natural Science Foundation of China (90211022 and 41020164005)
Sea surface temperature (SST) records in the South Yellow Sea during the last 6200 years are reconstructed by the unsaturation index of long-chain alkenones (K 37 U ') in sediment core ZY2 from the central mud area.Th...
Some features of the circulation in the YellowSea (hereafter referred to as YS) in the cold season (mid-November through mid-April) are analyzed emphatically by using the observations of several large-scale surveys i...
The gravity data from the sea region to the west of 124° E of the South Yellow Sea have been processed and the feature of gravity fields analyzed. An experience relationship formula on the filter wavelength and corre...
Since the Late Quaternary, eustatism has undergone great changes in the coastal area of eastern China. Sunk paleo-channels have been discovered in some regions at sea bottom of the China Sea. As a result of unequilibr...
In China, study on fossil Zygnemataceae has newly attracted the attention of palynologists. In our study of the bottom sediments in the East China Sea and Yellow Sea, Zygnemataeeae have for tthe first time been found ...