论文部分内容阅读
Low sea levels during Pleistocene glacial stages have been investigated in many studies of the topography and sediments of the world’s continental shelves. Melting of the glaciers was accompanied by a rise in sea level from perhaps 150m below the present level, a position that is indicated by the present depth of relict shore sediments and fossils. Approximate depths and dates of rising sea level are provided
Low sea levels during Pleistocene glacial stages have been investigated in many studies of the topography and sediments of the world’s continental shelves. Melting of the glaciers was accompanied by a rise in sea level from perhaps 150m below the present level, a position that is indicated by the present depth of relict shore sediments and fossils. Approximate depths and dates of rising sea level are provided