Anthropogenic Impacts on Biological Carbon Sequestration in the Coastal Waters

The well-known biological mechanism for carbon sequestration in the ocean is the biological pump (BP)， which is driven by primary production initially in the surface water and then dependent on particulate organic carbon sinking process in the water column. In contrast microbial carbon pump (MCP) depends on microbial transformation of dissolved organic carbon (DOC) to refractory DOC (RDOC).Although the BP and the MCP are distinct mechanisms, they are intertwined. Both mechanisms should be considered regarding maximum sequestration of carbon in the ocean. Recent studies have showed that excess nutrients could facilitate the uptake of DOC and enhance both bacterial production and respiration. Bacterial growth efficiency increases with increasing nitrogen concentration to certain levels and then decreases thereafter, while the remaining DOC in the water usually decreases with increasing nitrogen concentration, suggesting that excess nitrogen could simulate uptake of DOC in the environment and thus have negative impacts on the ocean DOC storage.This is somehow against the case of the BP which is known to increase with increasing availability of nutrients. Another responsible factor is the nature of algal products. If it is labile, the organic carbon cannot be preserved in the environment.On top of that, labile organic carbon has priming effects for river discharged semi-labile DOC for bacterial respiration.That is, labile organic matter will become the incubator for bacteria. While bacteria respire DOC into CO₂, they consume oxygen, and finally result in hypoxia. Under anoxic condition, anaerobic bacteria successively work on the rest of the organic carbon and produce harmful gasses such as methane and H₂S. Such story did have happened during geological events in the history of the earth. The above processes not only result in ecological disasters but also reduce the capacity of carbon sequestration in the ocean. To achieve maximum carbon sinks, both BP and MCP should be considered in management, especially in the coastal waters where eutrophication and hypoxia are severe. Currently, farm over-fertilization is found world widely to be responsible for coastal water eutrophication. Therefore nutrients input must be under control for optimum outputs of the sum of BP and MCP towards sustainable coastal ecosystems.