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黄东海近代厌氧沉积物中鳀鱼鱼鳞沉积信息的空间分布及重建潜力
引用本文:黄建生,孙耀,贾海波,杨茜,唐启升.黄东海近代厌氧沉积物中鳀鱼鱼鳞沉积信息的空间分布及重建潜力[J].海洋学报(英文版),2014,33(12):138-144.
作者姓名:黄建生  孙耀  贾海波  杨茜  唐启升
作者单位:厦门大学, 海洋与地球学院;中国水产科学研究院, 黄海水产研究所;中国水产科学研究院, 黄海水产研究所;中国水产科学研究院, 黄海水产研究所;中国水产科学研究院, 黄海水产研究所;中国水产科学研究院, 黄海水产研究所
基金项目:The National Basic Research Program of China under contract Nos 2010CB428902 and 2006CB400007; the National Natural Science Foundation of China under contract No. 40876088.
摘    要:Many studies have revealed that anchovy has exhibited large variability in population size on decadal tim-escales. However, such works concerning anchovy population are mainly based on short historical catch records. In order to understand the causes of variability in fish stocks (natural and/or anthropogenic) and calibrate the error between catches and standing stocks, it is essential to develop long-term time series of fish stocks from the time when human impacts are minimal or negligible. Well preserved fish scales from sediment record are regarded as useful indicators revealing the history of fish population dynamics over the last centuries. Anchovy scales was first analyzed over the Yellow Sea and East China Sea and the largest abundance was found in the central South Yellow Sea where is regarded as the largest overwintering ground for Japanese anchovy (Engraulis japonicas). Thus in the central South Yellow Sea, two cores covering the last 150 years were collected for estimating fish scale flux. The scale deposition rate (SDR) records show that the decadal scale SDRs were obviously coherent between cores with independent chronologies. Thecalibration of downcore SDRs to the standing stocks of anchovy further validated that SDR is a reliable proxy to recon-struct the long-term anchovy population dynamic in the central South Yellow Sea where anoxic conditions prevail in the sediment. When assembled with other productivity proxies, it would be expected that SDR could be associated with changes in oceanic productivity and may make a contribution to determine the forcing factors and elucidate the mechanism of the process in future.

关 键 词:南黄海中部  东中国海  沉积物  鳀鱼  空间分布  沉积记录  日本  水垢
收稿时间:9/3/2013 12:00:00 AM
修稿时间:2014/3/25 0:00:00

Spatial distribution and reconstruction potential of Japanese anchovy (Engraulis japonicus) based on scale deposition records in recent anaerobic sediment of the Yellow Sea and East China Sea
HUANG Jiansheng,SUN Yao,JIA Haibo,YANG Qian and TANG Qisheng.Spatial distribution and reconstruction potential of Japanese anchovy (Engraulis japonicus) based on scale deposition records in recent anaerobic sediment of the Yellow Sea and East China Sea[J].Acta Oceanologica Sinica,2014,33(12):138-144.
Authors:HUANG Jiansheng  SUN Yao  JIA Haibo  YANG Qian and TANG Qisheng
Institution:1.College of Ocean and Earth Science, Xiamen University, Xiamen 361005, China;Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao 266071, China2.Yellow Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Qingdao 266071, China
Abstract:Many studies have revealed that anchovy has exhibited large variability in population size on decadal timescales. However, such works concerning anchovy population are mainly based on short historical catch records. In order to understand the causes of variability in fish stocks (natural and/or anthropogenic) and calibrate the error between catches and standing stocks, it is essential to develop long-term time series of fish stocks from the time when human impacts are minimal or negligible. Well preserved fish scales from sediment record are regarded as useful indicators revealing the history of fish population dynamics over the last centuries. Anchovy scales was first analyzed over the Yellow Sea and East China Sea and the largest abundance was found in the central South Yellow Sea where is regarded as the largest overwintering ground for Japanese anchovy (Engraulis japonicas). Thus in the central South Yellow Sea, two cores covering the last 150 years were collected for estimating fish scale flux. The scale deposition rate (SDR) records show that the decadal scale SDRs were obviously coherent between cores with independent chronologies. The calibration of downcore SDRs to the standing stocks of anchovy further validated that SDR is a reliable proxy to reconstruct the long-term anchovy population dynamic in the central South Yellow Sea where anoxic conditions prevail in the sediment. When assembled with other productivity proxies, it would be expected that SDR could be associated with changes in oceanic productivity and may make a contribution to determine the forcing factors and elucidate the mechanism of the process in future.
Keywords:anchovy  the Yellow Sea and East China Sea  population dynamic  reconstruction potential
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