温度和元素浓度对Sr在褐牙鲆仔稚鱼耳石中的沉积影响  

Temperature and Water Elemental Concentration Affecting Strontium Incorporation into Otoliths in Larval-Juvenile Flounder Paralichthys olivaceus

作　　者：田洪林 刘金虎 曹亮[1,2,4] 窦硕增[1,2,3,4] TIAN Honglin;LIU Jinhu;CAO Liang;DOU Shuozeng(CAS Key Laboratory of Marine Ecology and Environment Sciences,Institute of Oceanology,Chinese Academy of Sciences,Qingdao 266071;Laboratory for Marine Ecology and Environmental Science,Pilot National Laboratory for Marine Science and Technology(Qingdao),Qingdao 266071;University of Chinese Academy of Sciences,Beijing 100049;Center for Ocean Mega-Science,Chinese Academy of Sciences,Qingdao 266071)

机构地区：[1]中国科学院海洋研究所,中国科学院海洋生态与环境科学重点实验室,青岛266071 [2]青岛海洋科学与技术试点国家实验室海洋生态与环境科学功能实验室,青岛266071 [3]中国科学院大学,北京100049 [4]中国科学院海洋大科学研究中心,青岛266071

出　　处：《渔业科学进展》2020年第2期78-86,共9页Progress in Fishery Sciences

基　　金：国家重点基础研究发展规划项目(2015CB453302);国家基金委-山东省联合基金项目(U1606404)共同资助。

摘　　要：科学认识鱼类耳石中微量元素沉积与主要水环境因子的关系是基于耳石微化学方法重新构建鱼类生活史及反演其环境履历的重要前提。本研究以环境与耳石中重要元素Sr为例,研究在不同水温(16℃、19℃和22℃)和不同元素浓度(1×、2×和3×Sr)下Sr在褐牙鲆(Paralichthys olivaceus)仔稚鱼耳石形成生长过程中(孵化后15~93 d)的沉积(Sr∶Ca比)特征。结果显示,在不同水温下,耳石中Sr∶Ca比随水体中Sr浓度的升高呈线性增长,而元素分配系数(DSr)随元素浓度的升高先降低然后趋于稳定。在不同Sr浓度下,耳石中Sr∶Ca比及DSr均随水温升高呈增长趋势,二者在22℃时的值均显著高于在其他水温时的值。耳石中Sr沉积能够表征褐牙鲆仔稚鱼所经历的水环境中Sr浓度和水温的变化,可作为元素指纹应用于褐牙鲆早期生活史的重建和环境履历的反演。An understanding of the effects of aquatic environmental factors on elemental incorporation into otoliths is fundamental for reconstructing life and environmental histories of fish using otolith microchemistry analysis.This study investigated the effects of temperature(16℃,19℃,and 22℃)and water elemental concentration(1×,2×,3×Sr ambient baseline,6.5 mg/L)on the otolith elemental incorporation of Sr in larval-juvenile flounder,Paralichthys olivaceus(15~93 days post hatching).The results revealed that the otolith incorporation of Sr(Sr∶CaOtolith)was positively dependent on ambient Sr concentration(Sr∶CaWater)as well as water temperature.Sr∶CaOtolith values were significantly higher at 22℃than at 16℃and 19℃at all Sr concentrations.Partition coefficient of Sr(DSr,Sr∶CaOtolith/Sr∶CaWater)tended to decrease with increasing Sr∶CaWater but remained stable when Sr∶CaWater reached a certain level at each temperature.Sr was incorporated into the otoliths more efficiently at 22℃than at the lower temperatures.It appeared that the otolith elemental incorporation of Sr was closely related to the ambient elemental concentration and,thus,could reflect the water chemistry that fish experienced,suggesting that Sr could be used as an elemental fingerprint to reconstruct the life and environmental histories of the flounder during its early life stage in nature.

关 键 词：褐牙鲆 矢耳石 SR 温度 元素指纹 沉积 

分 类 号：S931.1[农业科学—渔业资源]