Sedimentary ladderane core lipids as potential indicators of hypoxia in the East China Sea  

作　　者：赵宗山 曹亚俐 李莉 宋国栋 杨红梅 刘素美 赵美训 

机构地区：[1]Key Laboratory of Marine Chemistry Theory and Technology,Ministry of Education [2]Ocean University of China

出　　处：《Chinese Journal of Oceanology and Limnology》2013年第1期237-244,共8页中国海洋湖沼学报（英文版）

基　　金：Supported by the National Basic Research Program of China (973 Program) (No. 2010CB428901);the National Natural Science Foundation of China (Nos. 21007062, 41020164005);the Ocean University of China Special Fund Projects for Young Teachers (No. 201013018)

摘　　要：Anammox （anaerobic ammonium oxidation） is an important process in many suboxic to anoxic marine environments for converting fixed nitrogen to N2, and has a major impact on the marine nitrogen cycle. Ladderane core lipids have been utilized as an indicator of the contribution of anammox to the marine nitrogen cycles. However, such studies have not been reported for the China seas and little is known about the importance of anammox within the nitrogen cycle of these marginal seas. In the research reported here, the ladderane core lipid contents of 17 surface sediment samples from the East China Sea are reported, and their spatial distribution is investigated. C^8-[5]-ladderane FAME, C20-[5]-ladderane FAME and C20-[3]- ladderane FAME have all been detected, suggesting that the anammox bacteria are widely present within the study area. The total contents of the three ladderane lipids （ZFAMEs） range from 24-355 ng/g （weight of dry sediments）, with higher contents occurring in the Minzhe Mud Zone and broadly coincident with the spatial distribution of hypoxia. It is suggested that the sedimentary ladderane core lipids are mainly produced in the water column and their sedimentary contents can be used as indicators of water column hypoxia.Anammox (anaerobic ammonium oxidation) is an important process in many suboxic to anoxic marine environments for converting fixed nitrogen to N 2 , and has a major impact on the marine nitrogen cycle. Ladderane core lipids have been utilized as an indicator of the contribution of anammox to the marine nitrogen cycles. However, such studies have not been reported for the China seas and little is known about the importance of anammox within the nitrogen cycle of these marginal seas. In the research reported here, the ladderane core lipid contents of 17 surface sediment samples from the East China Sea are reported, and their spatial distribution is investigated. C 18 -[5]-ladderane FAME, C 20 -[5]-ladderane FAME and C 20 -[3]- ladderane FAME have all been detected, suggesting that the anammox bacteria are widely present within the study area. The total contents of the three ladderane lipids (∑FAMEs) range from 24-355 ng/g (weight of dry sediments), with higher contents occurring in the Minzhe Mud Zone and broadly coincident with the spatial distribution of hypoxia. It is suggested that the sedimentary ladderane core lipids are mainly produced in the water column and their sedimentary contents can be used as indicators of water column hypoxia.

关 键 词：ANAMMOX ladderane core lipid HYPOXIA East China Sea water column 

分 类 号：P736.2[天文地球—海洋地质]