共查询到18条相似文献，搜索用时 250 毫秒
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对伊犁河雅玛渡河段2010年1～4月采集的39尾伊犁裂腹鱼[Schizothorax (Racoma) pseudaksaiensis (Herzenstein)]样本进行了体表鳞片、臀鳞、脊椎骨、耳石和背鳍条共5种年龄鉴定材料的年轮特征研究。结果表明,体表鳞片没有明显的年轮特征,不能作为年龄鉴定材料,其他4种材料可作为伊犁裂腹鱼的年龄鉴定材料。样本为2+龄时,4种年龄材料鉴定结果的吻合率为100%;3+和4+龄鉴定结果吻合率较高,分别是87.3%和85.4%;5+～8+龄个体吻合率较低,为63.9%。伊犁裂腹鱼3+龄以上个体进行年龄鉴定时不能仅用1种鉴定材料,而应以耳石为主,其他年龄材料为辅。 相似文献
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利用2014年采自湖北长湖的378尾短颌鲚(Coilia brachygnathus)样本,去除包膜和黏液的矢耳石于55℃烘箱中烘烤24 h,电子天平称重(精确至0.001 g),成对t检验结果表明,短颌鲚左右矢耳石重量之间无显著差异(P0.05),数据分析以左右矢耳石重量的平均值计为矢耳石重量;采用直线、幂函数和多项式3种回归方程研究了其耳石重量与年龄的关系。结果显示,长湖短颌鲚的耳石和鳞片均可用于鉴定其年龄,且两者鉴定年龄的吻合度达到75.8%;根据222尾耳石与鳞片年龄一致的短颌鲚样本数据,发现耳石重量与个体的年龄呈显著相关(P0.05);按年龄组以耳石重量与相应的体长作图,可以初步判断所观测年龄的可靠性;利用建立的耳石重量-年龄关系函数估算得到的个体年龄,与直接读取耳石磨片获得的年龄结果无显著差异(P0.05),表明利用矢耳石重量直接推算其个体年龄,可以作为辅助短颌鲚年龄鉴定尤其快速鉴定的一种有效方法。 相似文献
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分析比较了元江越鳠(Mystus pluriradiatus)不同年龄鉴定材料的鉴定结果。结果显示:微耳石磨片、星耳石和脊椎骨材料为鉴定元江越鳠年龄的可利用材料,矢耳石细小且脆不适合用于越鳠的年龄鉴定。微耳石磨片和星耳石的年龄判别能力最高,均达到96.0%,脊椎骨的年龄判别能力为93.3%;最大年龄读数出现在微耳石磨片和脊椎骨上,读数为5+龄;微耳石磨片的同一鉴定者两次独立年龄读数的吻合率最高为94.5%、脊椎骨次之为91.7%、星耳石最低为88.1%;两种年龄材料读数之间的吻合率比较中,微耳石磨片与星耳石的吻合率较高为90.9%,两者的年龄读数在低龄组时吻合较好,微耳石磨片与脊椎骨的吻合率为89.3%,3+龄以上时二者的年龄读数吻合率高。结果表明,鉴定低龄个体选择星耳石材料(n+龄≤3+龄),高龄个体用微耳石磨片进行辅助鉴定的年龄鉴定方法对元江越鳠进行年龄鉴定较为准确。 相似文献
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根据2017-2019年在洞庭湖采集的228尾花[鱼骨](Hemibarbus maculatus)样本,使用耳石和鳞片研究其年龄、生长和资源现状。结果显示:耳石和鳞片是良好的年龄鉴定材料,鳞片上年轮特征以普通切割型为主,耳石重量可用于粗略、快速年龄鉴定。样本体长90~262 mm,优势体长组120~180 mm;体重11.0~399.0 g,优势体重组为20.0~80.0 g;年龄组成1~4龄,1龄为优势年龄组。体长体重关系:W=7.434×10^-6 L s 3.165,b值显著大于3,为异速生长鱼类。Von Bertalanffy生长方程:L t=301.4[1-e-0.471(t+0.341)],W t=522.0[1-e-0.471(t+0.341)]3.165,拐点年龄2.11龄(体长206.2 mm,体重156.9 g)。花[鱼骨]为典型的r-选择鱼类,总死亡系数3.321,自然死亡系数0.823,开发率为0.752,种群处于过度开发状态。建议起捕体长为172.2 mm,开发率降至0.601,同时在繁殖季节设置人工鱼巢,以恢复洞庭湖花[鱼骨]种群资源。 相似文献
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鱼类耳石研究和应用进展 总被引：6，自引：0，他引：6
鱼类耳石研究是鱼类生长和早期生活史研究的基础。文章阐述了鱼类耳石形态的研究方法及其在鱼类种类识别中的应用、耳石微结构在鱼类年龄鉴定、早期生长研究、产卵期、孵化期和产卵场的推算以及早期生活史中特殊事件的研究等方面的进展,探讨了耳石研究的存在问题并提出了进一步研究的建议。 相似文献
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2014年4—8月于凤鲚(Coilia mystus)的主要繁殖期在长江口采集仔稚鱼103尾。分析凤鲚仔稚鱼样本得出日龄范围为5~48 d,体长为4.20~26.21 mm。为研究长江口凤鲚早期发育不同阶段生长,测定了凤鲚仔稚鱼(5~48日龄)体长随日龄的生长变化,其变化分为3个阶段(5~11日龄、12~30日龄、31~48日龄)。不同日龄阶段,体长的生长速率差异性显著(P0.05)。耳石早期发育研究发现耳石长、耳石宽随鱼体的生长而增长,在17~19日龄之后其生长速率增大约2倍。采用分段回归方法分析耳石长、耳石宽与日龄的关系,发现二者异速生长的拐点均出现在19~20日龄,拐点前为慢速生长,之后为快速生长。研究发现凤鲚早期生长发育阶段的耳石形态有较为显著的改变:卵黄囊期、前弯曲期为圆形;弯曲期耳石长的生长大于耳石宽的生长,耳石逐渐变成椭圆形;耳石变成稳定形态后,长宽比基本保持稳定。 相似文献
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Abstract – We used laser ablation inductively coupled plasma mass spectrometry line scans to determine the elemental composition of otoliths, pectoral fin rays and scales of Arctic grayling. Elemental signatures of otoliths and pectoral fin rays effectively provide life-history information on individual fish, important for management of grayling, and potentially all freshwater teleosts. Bulk elemental signatures measured in the otoliths and fin rays were highly correlated to the stream chemistries where the fish were captured. A surprising result of this study was that fin rays showed the strongest relationship with water chemistry for strontium. Scale strontium concentrations were not correlated to water chemistries suggesting that other physiological mechanisms, or remobilisation, may be influencing the deposition of trace elements within scales. Linear discriminant function analyses for otolith and fin ray elemental signatures (and intriguingly also for scales) separated fish from different rivers for all three structures; thus, this technique can be used effectively as a means to discriminate origin of capture. 相似文献
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Abstract The suitability of three anatomical structures to determine age and growth of bull trout, Salvelinus confluentus (Suckley), was assessed. Scales and pelvic fin rays collected from recaptured bull trout 96–265 mm TL were used to validate annulus formation and assess the accuracy and precision of back calculation. Ageing precision and agreement of assigned ages were compared among scales, fin rays and otoliths from bull trout 52–711 mm TL. Annulus formation was validated for 88% (14 of 16 fish) of recaptured bull trout using pelvic fin rays and 68% using scales (15 of 22 fish). Annulus formation in fin rays occurred between late April to early June, and the hyaline (non-growth) band began forming in late August. Back-calculated length was not significantly different from measured length at initial capture either for fin rays or scales ( P ≥ 0.19), and absolute percent error was 7.2 ± 1.2 (mean ± SE; n = 14) for fin rays and 8.7 ± 1.9 ( n = 15) for scales. Consistency of back-calculated lengths at age between tag and recapture samples for individual fish was similar for fin rays (mean absolute difference = 8.2% ± 0.9; n = 33) and scales (9.4% ± 1.4; n = 40). However, fin rays (87% precision) and otoliths (90%) provided notably higher ageing precision than scales (68%) and closer agreement of assigned ages, particularly for fish older than age 4. Pelvic fin rays appear to offer more accurate and precise age and growth determinations than scales and a non-lethal alternative to otoliths, but further work is needed to validate the accuracy and precision of ageing large, migratory bull trout. 相似文献
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软骨鱼类(鲨、鳐和银鲛类)多位居海洋食物网的顶端或近顶端, 通过下行效应调控海洋生态系统结构和功能, 多为生态系统中的关键性物种。脊椎骨是软骨鱼类支撑身体的重要硬组织, 其生长贯穿整个生活史, 主要应用于鉴定年龄。随着微化学技术的兴起, 并结合脊椎骨轮纹的特殊结构, 可进而掌握鱼类整个生活史中摄食及洄游信息。目前, 国内外基于脊椎骨的微化学研究主要集中在稳定同位素和微量元素分析, 并已取得一定的进展。本文在归纳国内外应用脊椎骨在软骨鱼类生长、摄食及洄游中的应用案例基础上, 着重分析了脊椎骨应用于年龄鉴定及校正、摄食及洄游等核心问题上的研究现状和发展前景, 以期为今后学者展开基于软骨鱼类脊椎骨的相关研究提供参考。 相似文献
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为确定鉴定滇池鲤（Cyprinus carpio）年龄的适宜材料,对4种年龄鉴定材料（耳石、鳞片、胸鳍条和鳃盖骨）的形态和年轮标志进行了描述,并对这4种钙化组织鉴定鲤年龄的一致性进行了探讨。2013年5、6、8-11月以及2014年3-7月,使用拖网采集云南滇池鲤584尾,体长范围7.5~50.5 cm,体重范围17.2~3 211.3 g。其中耳石采集于584尾样本,鳃盖骨和鳞片分别采集于276尾样本,胸鳍条采集于274尾样本。微耳石磨片轮纹清晰,在反射光下呈明暗相间的条纹,年龄标志明显。同一鉴定者2次年龄读数的吻合率,微耳石磨片轮最高（88.0%),鳞片次之(84.1%),胸鳍条和鳃盖骨则分别为73.7%和72.1%。2次读龄的平均误差百分比,微耳石磨片和鳞片较小,分别为2.6%和2.9%;胸鳍条和鳃盖骨较高,分别为4.7%和5.9%。以微耳石磨片年龄读数为基准,鳞片年龄读数与其吻合率最高(77.5%),平均变异系数最低(6.14%);鳃盖骨和胸鳍条与其吻合率分别为61.9%和56.2%,平均变异系数均超过12%。综合分析认为,耳石是滇池鲤年龄鉴定的最佳材料,鉴定4龄以下个体年龄时可使用鳞片,鳃盖骨和胸鳍条则不适于滇池鲤的年龄鉴定。 相似文献
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以养殖群体为对照,研究了广东东江外来尼罗罗非鱼(Oreochromis niloticus)鳞片、腹鳍棘、鳃盖骨、脊椎骨和矢耳石5种年龄材料的年轮结构特征。与养殖群体相比,整体上东江种群年轮的清晰度及对比度更高。结合周年水温数据,推测东江尼罗罗非鱼在1 3月份低温期形成1个年轮标志,而其副轮较多的特征可能与繁殖活动有关。在5种年龄材料中,以矢耳石的轮纹特征最为明显,且规律性强,而鳃盖骨和鳞片受副轮影响,可读性最低。5种年龄材料的可读性由大到小顺序为矢耳石、脊椎骨、腹鳍棘、鳃盖骨、鳞片。 相似文献
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怒江细尾高原鳅生长特征与食性 总被引：1，自引：1，他引：0
对2008年从怒江采集到的172尾细尾高原鳅(Triplophysa stenura)进行了生长与食性的研究。并采用von Bertalanffy生长方程、Gompertz生长方程、Logistic生长方程以及三项式方程分别拟合了细尾高原鳅的生长。实验结果显示,耳石适合于细尾高原鳅的年龄鉴定。体长与体重关系式为W=0.9996×10-5L2.9762(R2=0.9680)。体长与耳石半径间关系式为L=0.0027R1.7230(R2=0.9542)。四种生长方程均能反映其生长规律,其中von Bertalan-ffy生长方程表达式为Lt=246.9430(1-e-0.05964(t-0.1689));Wt=132.0300(1-e-0.05964(t-0.1689))2.9762。体重、生长曲线的拐点为18.45龄。食性分析表明:细尾高原鳅为杂食性鱼类,食物组成主要是水生昆虫幼虫,着生藻类,原生动物及有机碎屑等。 相似文献
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Md Rakeb‐Ul Islam Daniel J. Schmidt David A. Crook Jane M. Hughes 《Ecology of Freshwater Fish》2019,28(2):229-240
A comprehensive knowledge of migratory behaviour is paramount for the effective management and conservation of fishes in coastal drainages. The Australian smelt (Retropinna semoni) is a common fish distributed throughout coastal and inland drainages in south‐eastern Australia. Multiple life history patterns (potamodromy, facultative diadromy, estuarine residence) in the southern regions of its geographic distribution have been reported, and it is possible that some of these differences reflect characteristic behaviours of cryptic species within the group. To elucidate the life history patterns of smelt at the northern extent of their range and to identify any differences in migratory behaviour between two genetically distinct lineages (“SEQ‐N”, “SEQ‐S”) in this region, the movement patterns of Australian smelt were assessed using otolith chemistry. No evidence of marine residence was found based on otolith Sr:Ca and Ba:Ca transects for either group, suggesting that both are non‐diadromous. Significant differences in multi‐elemental otolith chemistry signatures were found among rivers and between paired sites within some rivers, suggesting no connectivity among drainages and limited dispersal of individuals over large spatial scales within rivers. These findings provide key insights into the migratory patterns of northern Australian smelt populations and, in combination with previous research, suggest that life history variation in the Australian smelt complex may occur primarily at the intra‐population level rather than among genetically distinct lineages. Conservation and management strategies for Australian smelt should take limited dispersal and individual life history variation into consideration in order to protect the components of this important species complex. 相似文献