盘星藻在湖泊沉积中的成矿作用  

Pediastrum in Lake Sediment and Its Mineralization

作　　者：曾昭琪[1] 钱峰[2] 

机构地区：[1]南京大学生物科学与技术系,南京210093 [2]新加坡大学微生物系

出　　处：《湖泊科学》2000年第4期304-310,共7页Journal of Lake Sciences

摘　　要：常被作为淡水湖泊沉积相的指示植物———盘星藻 (Pediastrumspp .)亚化石 ,在许多国家均有发现 .我国新生代油田的岩芯中亦有较多的盘星藻化石的记载 (包括江苏、湖北、河北、西北和东北等地 ) .本文报告了盘星藻在湖泊中沉积成矿的探索性研究 ,证明盘星藻等浮游藻类在成矿或成油的过程中有一定的贡献 .A lot of algae fossils were found in Cenozoic lake sediments, especially Pediastrum fossil sedimentary deposits in some places of China and also in some nearby seacoasts. For imitating Pediastrum mine ralization in lake sediments, several species of Pediastrum are cultured using BBM medium and sea water with 18% salt. By optical and electronic microscope observation and photosyntheic pigment analysis, we found that Pediastrum boryanum, P.duplex var clathratum and P.tetras , etc. cannot grow well in sea water. If cultured in saline medium, the specimen will die in a short period of time. We consider that probably the Pediastrum fossil that appeared in marine sediments were transported to the sea by river. In order to prove the mineralization condition of in living organism and fossils of Pediastrum, the following analysis is made. The fat soluble substances are high and they contain a small amount of alkane, alkene fatty acid and a great deal of plant pigments. Pediastrum has high H/C and low O/C (atom number ratio) value. Therefore, it is a good resource of oil formation. The products of oxidative degradation of the insoluble cell wall of Pediastrum are similar to the production obtained by kerogen, which is known to be of algal origin. So, the insolable materials of cell wall are probably a source of kerogen during the deposition.

关 键 词：盘星藻 藻类 绿藻 成矿生物 湖泊沉积 指标植物 

分 类 号：Q949.2[生物学—植物学] P512.32[天文地球—地质学]