Using δ13C and δ15N of sediments and mangrove leaves from Qi'ao island to reveal trophic status
        
            编号:1697
             稿件编号:2168            访问权限:仅限参会人
            更新:2021-06-17 14:16:28
                        浏览:1235次
            口头报告
        
        
        
            摘要
            Mangrove forests in tropical and subtropical regions are among the most productive and diverse ecosystems around the globe despite the usually limited nitrogen (N) availability. However, many waterways have experienced eutrophication as a result of intensive anthropogenic activities and it is unclear how the increased nutrient loads may affect nutrient status and nitrogen cycles in mangroves.
Analysis of the δ13C and δ15N isotope composition, coupled with the contents and stoichiometries of total organic carbon (TC), total nitrogen (TN), total phosphorus (TP), were performed on the water, sediments and plant leaves from the Qi’ao island mangrove reserve in order to assess the nutrient status. The overlying water of Qi’ao island was eutrophic, while low soil C:N ratios indicated high soil fertility and fast C and N mineralization rates. However, the low foliar N:P values appeared to be related to N limitation, though the high plant-soil discrimination in δ15N reflected high N use efficiency in Qi’ao mangrove ecosystem. Those preliminary findings suggested the poor nutrient status in a suburb mangrove ecosystem that is subject to intense human activities such as sewage discharge and fish farming.
 
         
        
            关键字
            Mangrove, Stoichiometry, Stable isotopes, Nutrient limitation, Nitrogen cycle
         
        
        
                稿件作者
                
                    
                                
                                                                                                            
                                王莹
                                中山大学大气科学学院
                            
                                
                                    
                                                                    
                                王凡
                                中山大学大气科学学院
                            
                 
                     
        
     
发表评论