In recent years, some researchers have begun to use sediment cores in lakes to study the impact of historical primary productivity on the migration and enrichment of pollutants, and then analyze the "biological pump" role of phytoplankton. Outridge et al. (2005Outridge et al. ( , 2007 used the Rock-Eval pyrolysis parameters to study the primary productivity history in Arctic lakes, while also analyzing the mercury concentration in the deposition cores. They found that climate warming for algae growth played the role of a "biological pump" on mercury. Stern et al. (2009) investigated some lacustrine systems and also found the effect of algal "biological pump" on mercury concentrations in the sediment cores while emphasizing that historical changes in primary productivity were mainly due to global temperature warming. Carrie et al. ( 2009) also found the effect of global warming on lake historical productivity, while increased algae acted as a "biological pump" for mercury, enhancing its accumulation in sediments and aquatic fish. Söderström et al. (2000) found higher polychlorinated biphenyl (PCB) and dichlorodiphenyltrichloroethane sedimentary fluxes and higher PCB concentrations in the surface sediments of eutrophic lakes than those of oligotrophic lakes, and most of the transport depended on phytoplankton. Jeremiason et al. (1999) selected a pair of lakes of similar size and catchment area for comparison, and also found