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:669次 口头报告

报告开始:2021年07月11日 17:30 (Asia/Shanghai)

报告时间:5min

所在会议:[S4B] 4B、生态与可持续发展 » [S4B-3] 4B、生态与可持续发展-3

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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
报告人
王莹
研究生 中山大学大气科学学院

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
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