首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到18条相似文献,搜索用时 187 毫秒
1.
长江口水域四种鱼类的耳石微化学研究   总被引:2,自引:0,他引:2  
刘洪波  姜涛  邱晨  杨健 《海洋与湖沼》2018,49(6):1358-1364
利用X-射线电子探针微区技术(electron probe microanalysis, EPMA),对长江口不同水域中捕获的焦氏舌鳎、皮氏叫姑鱼、鮸鱼和光泽黄颡鱼耳石中的Sr含量进行耳石微化学研究,结果发现,焦氏舌鳎是典型的海水鱼类,不仅Sr:Ca比(按惯例标准化为Sr:Ca×10~3)的移动平均值高(7),而且Sr含量面分析图亦呈现为对应高盐度海水的黄色或红色图谱。虽然皮氏叫姑鱼和鮸鱼从出生直至被捕Sr:Ca比的移动平均值都在3—7间波动,总体上属河口半咸水栖息鱼类,但从Sr含量面分析图来看,皮氏叫姑鱼生活史履历更为复杂,可包括淡水(对应蓝色图谱)和半咸水生境(对应绿色图谱);而鮸鱼仅在长江口较高盐度半咸水或海水生境中活动,未见进入过淡水的履历。光泽黄颡鱼表现出仅利用淡水生境的履历,其Sr:Ca比的移动平均值仅在1.5—3间窄幅波动,整个生活史均在淡水区域里活动,表现为长江口典型的淡水栖息鱼类。本研究从新的角度提供了较为客观、直观和最新的信息,用以较为准确地重建和掌握长江口这些不同鱼类的生境利用特征。  相似文献   

2.
金岳  李楠  俞骏  方舟  陈新军 《海洋与湖沼》2021,52(6):1540-1548
根据2016年5月于南海北部采集的中国枪乌贼(Uroteuthis chinensis)和剑尖枪乌贼(U.edulis)样本,分析其不同时期耳石微量元素的差异,推测两种枪乌贼类可能的洄游路线。研究结果表明,选取的枪乌贼样本均孵化于2015年10月-2016年2月,其中主要分布于11-12月。中国枪乌贼耳石Sr/Ca随着月份推移呈现出先降低后回升的趋势;剑尖枪乌贼耳石Sr/Ca在不同月份间有更多的变化,稚鱼期的Sr/Ca为最低;中国枪乌贼耳石的Ba/Ca值随着生长而下降,成鱼期迅速上升,剑尖枪乌贼耳石Ba/Ca由仔鱼期后开始逐渐下降,至成鱼期逐步回升。根据耳石Ba/Ca与水深关系确定了不同生长时期对应的水层,随后将对应水层的平均温度与Sr/Ca建立关系,发现除1月孵化的中国枪乌贼外其耳石Sr/Ca与水温均呈正相关,而剑尖枪乌贼耳石Sr/Ca与水温均呈负相关。根据上述结果,最后推测两种枪乌贼的洄游方式均在大陆架范围内进行南北定向洄游。  相似文献   

3.
为了解日本有明海沿岸六角川和筑后川河口水域鳀科鲚属鱼类刀鲚(Coilia nasus)的洄游特征和生境履历,利用电子探针微区分析(EPMA)技术,对采于两水域刀鲚的矢耳石进行了锶(Sr)元素含量的X射线强度面分布及耳石最长轴锶钙元素比值(Sr:Ca)的定量线分析。结果发现10尾六角川刀鲚(LJC)中的7尾以及15尾筑后川刀鲚(ZHC)耳石核心区域的Sr:Ca比值≤ 3,显示出这些个体在淡水生境出生并早期生活于淡水的履历。紧邻核心区域随后的生长阶段,Sr面分布图谱显示出了多样对应于含量水平差异的不同颜色同心环轮变化样式,Sr:Ca比值的波动亦可相应地分成1-6个差异极其显著的阶段,显示出这些个体在随后生活史阶段中极富变化的生境转换状况。另外3尾六角川刀鲚耳石核心的Sr:Ca比值较高(3-6.7),对应于半咸水生境;但在核心区域之外,Sr:Ca比值则高低变化不一,显示出这些六角川刀鲚个体在河口半咸水生境孵化的特征。本研究表明,二维Sr元素含量面分布图谱和基于耳石最长轴的Sr:Ca比值完全可以作为重建日本有明海沿岸各河口水域刀鲚生境履历的有效工具。  相似文献   

4.
为探究中国近海大泷六线鱼(Hexagrammosotakii)耳石微化学成分特征及群体分化状况,采集了连云港、青岛、威海、烟台、秦皇岛、大连、丹东7个野生群体和1个威海养殖群体的大泷六线鱼样本。利用LA-ICPMS技术测定耳石中的微量元素,以微量元素与钙的比值进行了分析,结果显示大泷六线鱼耳石中, Na/Ca、Sr/Ca、Fe/Ca、Mg/Ca较高,而Mn/Ca、Ba/Ca、Zn/Ca、Li/Ca较低。耳石1龄前元素比值的组间比较(S-N-K检验)结果显示:Na/Ca、Sr/Ca、Fe/Ca在群体间具显著性差异(P<0.05)。耳石边缘区元素与环境中元素比较发现,Li、Mn元素在耳石中富集程度较大,Sr在耳石的中元素含量远远大于水环境中的浓度,说明耳石中的元素沉积与海水中元素并不是简单的线性关系。判别分析结果显示:耳石1龄前元素指纹的判别分析结果表明,大泷六线鱼群体的判别成功率为63.0%,判别正确范围为30.0%~80.0%,耳石边缘区元素的判别正确率为57.1%,判别正确范围20.0%~80.0%,秦皇岛群体有高的判别成功率80.0%。耳石元素指纹可以用于不同大泷六线鱼群体的...  相似文献   

5.
鮸鱼胚胎发育的研究   总被引:2,自引:0,他引:2  
研究了人工繁殖时鮸鱼(Miichthys miiuy)胚胎的发育过程。鮸鱼受精卵呈圆球形,浮性,卵径为0.99~1.15 mm,中央大多具有1个油球,少数为2~3个或较多个油球。在水温为24.5~24.7℃,盐度为24的天然海水中,鮸鱼胚胎发育历时约21h 48 min孵化出膜。整个胚胎发育分为5个阶段,共21个发育期。  相似文献   

6.
本研究以确认鱼类早期个体规模化耳石锶(Sr)标记的可行性及其时滞特征为目的,选择鲤(Cyprinuscarpio)仔鱼为实验对象,开展了六水氯化锶(SrCl2.6H2O)溶液2d的活体浸泡标记研究。结果显示,该浸泡标记过程对鲤存活、生长无显著影响。利用X射线电子探针微区分析(EPMA)技术进行分析:定量线分析结果显示对照组Sr/Ca比值(3.0左右)趋于稳定,标记组却均出现了明显的标记峰值(远3.0);面分布分析结果表明在标记组鲤耳石上均呈现出一圈明显、清晰可见的红色"高Sr标记环"。此外,对比对照组和标记组微化学结果发现,"高Sr标记环"在恢复续养250d后的鲤耳石仍然可见,说明Sr标记可长期存在。观察鲤仔鱼耳石微结构,发现Sr在耳石上存在明显的时滞效应。首次得出在开始浸泡后的第3天,耳石上才开始出现Sr标记,在浸泡结束后的第6天,耳石Sr标记区才会完全消失的结论。本研究首次揭示出,外源Sr标记的方法在鲤仔鱼种群大规模增殖放流标记和评价中将具有很强的稳定性、可靠性、可行性和应用潜力。  相似文献   

7.
作者对鮸鱼(Miichthys miiuy)的早期发育(从受精卵到45日龄幼鱼)形态特征及生态习性进行了描述。鮸鱼的受精卵在水温21.4℃~22.0℃,盐度25.7条件下,经过29 h30 min仔鱼孵出。从受精卵到仔鱼出膜可分为卵裂期、囊胚期、原肠期、胚体形成期等4个主要时期,然后进入胚后发育阶段。孵出后的3日龄仔鱼已能在水体中平游,极少数个体可开口摄食轮虫。4日龄仔鱼全部开口摄食,并对光反应敏感,出现明显的集群现象。22日龄的后期仔鱼各鳍鳍条发育形成,鳞片开始出现,进入到稚鱼期。39日龄后,鮸鱼全身披满细小的鳞片,全部分布于育苗池的底部,开始进入到幼鱼发育阶段。根据仔、稚、幼鱼形态特征和生活习性对鮸鱼的分类进行了探讨。  相似文献   

8.
为研究大麻哈鱼(Oncorhynchus keta)生活史特征及不同群组间的鉴别,本文采用电子微探针技术分析自然野生、人工增殖锶标记、人工增殖物理标记和人工养殖4组大麻哈鱼耳石样本的Sr浓度及Sr/Ca值,反演其生境履历。定量线分析结果表明,耳石Sr/Ca值波动显著,根据Sr/Ca值的特征划分了各群组大麻哈鱼淡、咸水间的生活史阶段。根据大麻哈鱼生活史特征及耳石径长参数差异的分析结果将各群组间个体进行了有效辨别。其中锶标记组个体耳石标记区Sr/Ca值达到17.033×10~3,显著高于其他组,证实了锶标记方法的有效性。对大麻哈鱼人工增养殖组和自然野生组早期淡水生活阶段耳石径长参数(R_(f1)、R_L)以及淡水系数(R_C)进行对比分析,结果显示:自然野生组中120μm≤R_(f1 )≤200μm, 20μm≤R_L≤30μm, 0.06≤R_C≤0.10;人工增养殖组中240μm≤R_(f1 )≤470μm, 80μm≤R_L≤200μm, 0.15≤R_C≤0.29。两群组间的参数差异显著,可作为群组间个体辨别的依据。本研究结果表明,耳石微化学分析技术能够有效分析大麻哈鱼的关键生活史特征,且可据此开展大麻哈鱼群组间的鉴别。研究结果可为大麻哈鱼生活史研究及增殖放流效果评估提供有效的方法。  相似文献   

9.
采用实验生态学方法,进行了鮸鱼仔稚鱼发育生长方式及其生态学意义研究。结果表明,鮸鱼的形态学变化和器官分化主要发生在仔鱼期。仔鱼期头部和尾部快于躯干部的生长。仔鱼头部(拐点:9.80mm体长)、眼径(8.87mm)和口径(23.40mm)的正异速生长为仔鱼的呼吸和摄食提供了有利条件;尾长(16.40mm)正异速生长为减少仔鱼运动能耗和成功逃避捕食者准备了条件;虽然躯干部生长比较缓慢,但是体高呈现正异速生长(11.20mm),这可能与仔鱼消化系统为满足其迅速发育的营养需要而快速生长及鳔的发育有关。结果表明,鮸鱼在早期发育阶段优先发育对生长生存起关键作用的器官,即运动、视觉和摄食器官。但在稚鱼阶段,其主要长度量度相对于体长指标均呈现负异速成长。  相似文献   

10.
陈朴贤 《海洋科学》2012,36(11):24-29
为了探索褐毛鲿(Megalonibea fusca)胚胎孵化和早期仔鱼生长发育最适宜的盐度条件,作者观察了其胚胎在6个盐度(35、30、25、20、15、10)海水中沉浮性、发育、初孵仔鱼分布状态.结果表明:胚胎在盐度35时完全上浮,盐度低于25完全下沉,在盐度30时处于半悬浮状态;不同盐度对胚胎发育有一定影响:在盐度30~15范围内,胚胎发育较快,孵化时间较为一致,在盐度35和10发育变慢,孵化时间延长2.5 h以上;初孵仔鱼在不同盐度海水中呈不同分布状态:在盐度35时完全上浮表层,盐度25~30分布于中下层至中上层,盐度25大部分仔鱼沉底,盐度低于20,初孵仔鱼全部沉底.观察了10个盐度(35、32、29、26、23、20、17、14、11、8)海水中胚胎孵化率和早期仔鱼存活率,结果表明:褐毛鲿胚胎在盐度35~8范围内孵化率达(76±2)%~(98±2)%,在较低盐度26~11区间,孵化率达(88±0)%~(98±2)%,显示低盐区更高的孵化率,而在较高盐度29~35区间,孵化率在(82±2)%~(84±2)%,并且具有明显趋向性,即盐度大于29,随盐度升高孵化率逐渐下降;盐度对早期仔鱼存活率有明显影响:孵化后40 h 正常仔鱼最高存活率在低盐度26~8区,为(89.4±2.2)%~(97.4±0.1)%,盐度大于29,随着盐度上升仔鱼死亡率骤然升高,在盐度29~35,升至(31.7±0.7)%~(38.1±1.5)%,畸形率升至(7.1±0.2)%~(10.7±0.5)%,正常仔鱼存活率下降至(61.0±1.0)%~(61.9±1.5)%.低盐度区仔鱼有更高的存活率.褐毛鲿胚胎最适孵化盐度在29~32,早期仔鱼最适培育盐度为26.  相似文献   

11.
Habitat use of the tapertail anchovy(Coilia mystus Linnaeus, 1758) from the Oujiang River Estuary and the Zhujiang(Pearl) River Estuary was studied by examining the environmental signatures of Sr and Ca in otoliths using electron probe microanalysis. Individuals from the Oujiang River had higher and varied Sr:Ca ratios(expressed as(Sr:Ca)×1 000, 3.83–13.0 average) in the otolith core regions, suggesting that they were born in brackish or sea waters, and that a freshwater habitat might not be necessary for egg hatching and larval growth.While, individuals from the Zhujiang River had lower Sr:Ca ratios(0.39–2.51 average) in the core regions,suggesting a freshwater origin. After hatching, anchovies from the Zhujiang River migrate downstream to the river estuary close to brackish water. Our results demonstrated varied habitat use for spawning during stages of early life history between the two populations, and suggested that such variations are promoting diversity of life history strategies of this species.  相似文献   

12.
13.
Habitat use by the European eel Anguilla anguilla in Irish waters   总被引:2,自引:0,他引:2  
The apparent use of marine and freshwater habitats by European eel Anguilla anguilla was examined by analyzing the strontium (Sr) and calcium (Ca) concentrations in otoliths of the eels collected from Irish coastal and fresh waters. The age and growth of eels were also examined using their otolith annuli. The sizes and ages of the female eels were greater than those of the males. The somatic growth rates ranged from 15 to 62 mm/year, which is typical for Ireland and other European countries. Analyses of Sr:Ca ratios along a life history transect in each otolith showed peaks (maximum more than 25 × 10−3) between the core and elver mark corresponding to the period of their leptocephalus and early glass eel stages in the ocean. Outside the elver mark, the Sr:Ca ratios indicated that eels had remained in different habitats that included freshwater (average Sr:Ca ratios, 0.98–1.78 × 10−3) and areas with relatively high salinities (average Sr:Ca ratios, 6.73–8.89 × 10−3). Some individuals showed clear evidence of shifts from sea to fresh waters. These findings suggest that Irish eels have the same behavioral plasticity regarding whether or not to enter freshwater or remain in marine environments as has been recently documented in this species and several other temperate anguillid species. However, patterns of habitat use in Irish waters were somewhat different than those previously reported for other habitats.  相似文献   

14.
牙鲆是太平洋西岸海水养殖、捕捞和自然增殖的主要鱼类,但是人工养殖病害多、生长慢,针对这一问题,从2003年开始开展了牙鲆选择育种。本文利用筛选和培育的F1、F2代牙鲆家系核心群体,构建了F3代家系52个,在生长到196d时,对家系1 560尾鱼苗全长、体宽、体质量、全长日增量和体重日增量5个生长性状进行测量和计算,获得7 800个数据。采用"加性-显性"线性模型、最小范数二阶无偏估计法(MINQUE)对以上生长性状的边际平均值、加性方差分量、显性方差分量、随机方差分量、狭义遗传力、广义遗传力、亲本加性效应、杂交随机效应等遗传参数进行了评估。结果显示:1202、1206、1226和1211家系以上生长性状的边际平均值同时显著高于其他家系。以上5个生长性状的加性方差分量比率为(0.099±0.01)~(0.24±0.02),显性方差分量比率(0.30±0.02)~(0.31±0.02),随机方差分量比率(0.48±0.02)~(0.61±0.01),5个性状狭义遗传力0.099~0.24,广义遗传力0.38~0.54,以上遗传参数均达极显著性水平(P0.01)。综合比较18个亲本5个性状的加性效应预测值,发现F0917、F0908、F0905、F0915、F09125和KS(韩国牙鲆)亲本在5个性状上都具有极显著的正向效应(P0.01),其他亲本5个性状都不同程度的表现为显著(P0.05)或极显著(P0.01)的负向加性效应。对42个杂交组合显性随机效应进行预测,D(2×6)、D(2×18)、D(3×4)、D(7×12)、D(7×14)和D(8×13)6个杂交组合在5个性状上都表现为极显著(P0.05)正效应,利用这些杂交组合建立家系将促进牙鲆以上5个性状的生长。本文研究结果,为牙鲆优良家系的建立及新品种的培育初步筛选出了性状优良的亲本、杂交组合和家系,同时为牙鲆进一步选择育种提供了理论和技术依据。  相似文献   

15.
江苏近岸海域鮸时空分布特征研究   总被引:3,自引:1,他引:3  
根据2006—2007年4个季度拖网专项调查数据,以鮸为目标种,以机轮底拖网禁渔区线内侧及毗邻海域为目标区域,对鮸资源时空分布特征进行分析,并探讨形成机制,结果表明:(1)江苏海域的鮸主要分布于34°00′N以南海域,主产卵区位于辐射沙脊群海域及周边近岸海域,春季为主要产卵期;(2)江苏省中南部海域为鮸早期幼体的过渡性索饵场所,幼鱼群体随时间推移呈逐步分散趋势;(3)鮸在江苏海域的栖息时间为春、夏、秋3个季节,冬季呈零星分布;(4)海底地形地貌、潮汐和海流类型、辐射沙脊群等特征要素是影响区域生物生态的重要因子。  相似文献   

16.
To further evaluate the potential use of Mg/Ca and Sr/Ca ratios as a paleothermometer in the shell carbonate of the blue mussel Mytilus edulis, we grew juvenile mussels (~15 mm shell height; <2 years old) collected from Maine, USA, in controlled environments for 4 months. The four-by-three factorial design consisted of four circulating temperature baths (7, 11, 15 and 19°C), and three salinity ranges (23, 28, and 32). During the experiment, water Mg/Ca and Sr/Ca molar ratios were monitored weekly, and showed little variation across all salinity and temperature ranges. Data from sampled shells including all salinity treatments yielded relatively poor relationships between shell elemental chemistry and water temperatures. However, if only the low salinity treatment data (23) are used, the relationships between shell elemental chemistry and water temperature improve moderately. Based on the data presented here, it may be possible to use Mg/Ca and Sr/Ca ratios from the shell carbonate of juvenile M. edulis to reconstruct paleotemperatures in estuarine settings (salinity below 24) with a corresponding RMSE (root mean squared error; 95% confidence interval) of ±2.4°C and ±2.8°C, respectively. In order for this methodology to be statistically meaningful, water temperature changes must be rather large, as the errors associated with using Mg/Ca and Sr/Ca ratios from the shell material of M. edulis are substantial. Further work is required to determine if the findings presented here can be duplicated, and if the potential salinity effect is pervasive.  相似文献   

17.
An experimental study on Phragmites australis leaf litter decomposition was conducted in the estuarine environment, Ria de Aveiro, Western Portugal, using the leaf-bag technique, with fine- (1 mm) and coarse-mesh (5 mm) bags. The leaf bags were placed in the field sites at day 0, covering a complete salinity gradient, and replicates were collected over time, at days 3 (leaching), 7, 15, 30 and 60. The biomass loss through the leaching phase, about 20% of the initial leaf mass, was independent of both the salinity and the bag mesh size. The biomass decay pattern along the salinity gradient varied through time and presented strong similarities between the two mesh sizes, with the remaining biomass always lower in the 5 mm mesh-size bags. At days 7 and 15, the lowest remaining biomass was observed at the head of the estuary, the preferential distribution area of P. australis. At day 30, the remaining biomass was higher in the marine area and diminished under a direct relationship with salinity, reaching the lowest value in the freshwater environment, with values ranging from 66% to 44% of the initial weight in 5 mm bags, and from 79% to 51% in 1 mm bags. The largest heterogeneity in the remaining biomass among the study areas positioned along the salinity gradient was found close to days 30 (5 mm) and 40 (1 mm). The overall results indicate that the relationship between leaf decay rate and salinity depends on the decay time considered (k15, k30 or k60) and, for the later stages (k60), also on the leaf-bag mesh size. This implies that the use of leaf litter decay rates as a functional indicator in transitional waters will need to take into consideration the factor location in the salinity gradient and leaf litter stage at which the decay rate is determined. The differences between the decay rates with the mesh size acted mainly at the level of the absolute k value and not at the level of the pattern along the salinity gradient. Even so, the data obtained at the mouth of the estuary, in the area closest to a fully marine environment, indicated that after the initial biomass loss through leaching, P. australis decayed either very slowly, in the 5 mm, or not at all, in the 1 mm mesh bags.  相似文献   

18.
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号