摘要
The pelagic manganese nodules from the East Pacific Ocean have been studied using polarizing and electron microscope since 1994. Based on the surface morphology and the type of stromatolites in the coatings, these manganese nodules can be divided into smooth and knobbly ones. The coatings of smooth nodules are composed of Minima. The coatings of knobbly ones consist of Admirabilis. The authors have reported the first discovery of the beaded ultra-microfossils in the manganese nodules, but did not classify
The pelagic manganese nodules from the East Pacific Ocean have been studied using polarizing and electron microscope since 1994. Based on the surface morphology and the type of stromatolites in the coatings, these manganese nodules can be divided into smooth and knobbly ones. The coatings of smooth nodules are composed of Minima. The coatings of knobbly ones consist of Admirabilis. The authors have reported the first discovery of the beaded ultra-microfossils in the manganese nodules, but did not classify and
基金
Project supported by Foundation of the National Committee of Education, Foundation of the Center for Materials Analysis
Foundation of the Laboratory of Mineral Deposits, Nanjing University.
