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1.
南极鱼类年龄与生长研究进展   总被引:4,自引:2,他引:2       下载免费PDF全文
朱国平  魏联 《水产学报》2017,41(10):1638-1647
南极鱼类生长相对缓慢,独特的生物学特性使其年龄鉴定较其他海区鱼类更为困难。但考虑到鱼类年龄鉴定是开展渔业资源评估的基础,因此过去一些年来,硬质部位,如鳞片、鳍条(棘)、脊椎骨以及耳石等仍成为南极鱼类的主要鉴龄材料。本文对南极鱼类年龄鉴定的方法和材料进行了总结回顾,将年龄鉴定的方法和材料进行比较,分析各自优缺点。结果显示:(1)对于具鳞的南极鱼类,因鳞片在鱼类生长过程中存在重吸收现象,因而利用鳞片及鳍条(棘)单独鉴龄所得出的结果通常小于耳石的鉴龄结果,缺乏精确性;(2)南极鱼类生活跨度较大,高龄鱼体长频次分布严重重叠,以致无法准确判断其年龄结构;(3)耳石重量法易受到特殊个体影响而误判年龄;(4)因鳍条易损坏,脊椎骨采集较为困难,且许多南极鱼类无鳞,目前大多数南极鱼类使用耳石鉴定年龄,其也成为目前最为精准的南极鱼类鉴龄方法,但同时利用鳞片和耳石重量等对鉴定结果进行验证;(5)南极鱼类尚存在无统一的鉴龄标准、人为主观性较强以及缺乏早期生活史研究等不足之处;(6)为了研究南极鱼类早期生活史,耳石微化学及微结构等方法将被广泛利用。  相似文献   

2.
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。  相似文献   

3.
基于耳石微化学分析的鱼类种群生态学研究进展   总被引:1,自引:0,他引:1       下载免费PDF全文
研究鱼类的种群生态学,破解其数量特征、生境利用、种群结构和动态变化等种群属性是保护和合理开发天然渔业资源的基础。耳石微化学分析是破解鱼类的种群生态学难题的新颖而有力的手段,不仅可以反演鱼类生活史过程中所经历的环境条件,还可溯源资源群起源的产卵场等关键生境,在鱼类资源种群空间结构形成机制研究及动态评估中具有优势。本文在分析耳石元素组成及其沉积特征的基础上,重点介绍了耳石微化学分析在鱼类种群生态学(如反演鱼类生活史、评估种群结构、把握关联性和破解混合群体的构成与来源等)中的应用进展,也客观评述了耳石微化学分析在鱼类种群生态学研究中的局限性与解决途径,并对今后相关技术的发展趋势及需要关注的科学问题进行了展望。  相似文献   

4.
鱼类早期生活史研究与其进展   总被引:128,自引:11,他引:117  
殷名称 《水产学报》1991,15(4):348-358
鱼类早期生活史的研究,主要涉及卵和仔鱼发育,仔鱼最佳饲养条件、饵料密度、营养、生长、临界期、饥饿、捕食、环境耐力和毒性反应等和渔业密切相关的诸因子,是鱼类自然资源繁殖保护和养殖业苗种培育的基础。近二、三十年来,鱼类早期生活史研究已成为水产科学的一个崭新领域,在国际上受到广泛重视并迅速发展。国际海洋开发理事会(ICES)曾三次举行鱼类早期生活史学术讨论会,  相似文献   

5.
研究中华倒刺鲃(Spinibarbus sinensis)耳石的发育和生长特征,补充早期生物学资料,为进一步研究该鱼野生资源的早期生活史特征提供基础数据。在实验室养殖条件下观察了乌江中华倒刺鲃仔、稚鱼及3种耳石的形态发育过程和生长特点。结果表明,在水温(26.0±2.1)℃下,初孵仔鱼微耳石和矢耳石已经形成,星耳石在仔鱼出膜后第6天出现。在形态发育过程中,微耳石由出膜时的近圆形经卵圆形发育成贻贝形,且中心核位置偏移到前端靠近背侧;矢耳石由近圆形经卵圆形发育成箭矢状;星耳石由逗号形发育成不规则四边形。3种耳石形态发育的各阶段与鱼体发育阶段存在一定的对应关系。在生长上,仔稚鱼鱼体、3种耳石的长径和短径与日龄均呈显著的线性关系(P0.001),鱼体全长与3种耳石长径呈现出显著的线性关系(P0.001),仔稚鱼鱼体、3种耳石的特定生长率随日龄增加均呈下降趋势。  相似文献   

6.
陈子越  陆化杰  刘凯  王芮 《水产学报》2023,47(7):079314-1-079314-14
耳石是研究头足类年龄与生长、种群结构和生活史的重要材料。根据2018年厄尔尼诺发生期冬季(12月)我国鱿钓船在西北太平洋日本海海域生产调查期间采集的530尾太平洋褶柔鱼(Todarodes pacificus)样本,首次对厄尔尼诺发生期太平洋褶柔鱼的耳石外形生长特征进行了报道。结果表明,日本海太平洋褶柔鱼的耳石具有宽大的背区、侧区和翼区,以及较狭长的吻区。主成分分析表明,耳石总长(TSL)、侧区长(LDL)、翼区长(WL)和最大宽度(MW)可以作为描述日本海太平洋褶柔鱼耳石外形生长特征的表征参数。协方差分析表明,耳石各外形表征参数与胴长、体质量间的生长关系不存在性别间显著性差异。赤池信息准则表明,TSL、LDL、MW与胴长、体质量的生长关系适用幂函数生长模型表示,WL与胴长、体质量的生长关系适用线性生长模型表示。随着太平洋褶柔鱼个体逐渐生长,其耳石整体外形轮廓的绝对尺寸生长逐渐减缓,但耳石整体外部轮廓的相对尺寸基本维持原状。本研究为后续利用耳石研究太平洋褶柔鱼的生活史过程提供了参考,也为研究异常气候事件对头足类硬组织生长的影响提供了科学依据。  相似文献   

7.
鱼类早期生活史一般可划分为胚胎期、仔鱼期和稚鱼期;但在鱼类早期生活史划分中,由于研究目的、研究方法、研究对象以及研究重点等方面的差异,对鱼类早期生活史发育时期的划分上存在着许多不同的观点,本文就这些不同的观点进行简要地阐述.  相似文献   

8.
进一步开展叶尔羌高原鳅(Triplophysa yarkandensis)不同地理群体分类判别、探明耳石与鱼类生活史的相关机制,本研究基于耳石形态学和鱼类生态学方法,对叶尔羌河、和田河和塔里木河的734尾叶尔羌高原鳅耳石与鱼体的形态指标进行了统计分析。结果显示,叶尔羌高原鳅耳石较小,左右微耳石形态无显著差异(P>0.05);叶尔羌高原鳅耳石形态指标与体长、体质量呈对数函数关系,R2范围在0.48~0.62;采用鱼体形态学、耳石形态测量法和椭圆傅里叶分析法分别对两两群体进行判别分析,和田河群体与塔里木河群体判别准确率分别为96.0%、61.4%和82.2%,叶尔羌河群体与和田河群体判别准确率分别为93.0%、79.5%和87.9%,叶尔羌河群体与塔里木河群体判别准确率分别为96.5%、77.5%和86.8%。叶尔羌高原鳅耳石形态与鱼体生长的关系极大程度地反映了其个体发育对栖息环境的适应性,且不同地理群体叶尔羌高原鳅耳石形态特征存在显著差异(P<0.05)。本研究将耳石形态学首次应用于叶尔羌高原鳅种群的鉴别分析,为进一步开展高原鳅属进化分类提供参考,为高原渔业种质资源保护提供了科学依据。  相似文献   

9.
头足类耳石微化学研究进展   总被引:3,自引:1,他引:2  
耳石是位于平衡囊内起平衡作用的一对钙化组织,它是头足类的加速度感应器,记录其生命周期内的生物和生态信息。随着鱼类耳石微化学研究及应用的日趋成熟与完善,头足类耳石的相应研究也逐渐兴起。目前头足类耳石微化学的研究内容主要包括无机和有机大分子、微量元素、同位素、微化学标记等方面,其中微量元素是应用研究的重点,在头足类种群识别、生活史分析及栖息环境重建等方面发挥了重要作用。分析认为,头足类微量元素在与栖息环境尤其水温关系的研究中取得了很好的结果,被认为是测定头足类生活水温的温度计。然而,涉及种群识别、生活史分析以及与盐度和食物关系的研究还不够充分,且多集中于Sr/Ca的研究。因此,建议在今后的研究中要综合多种研究方法按时间和空间序列从日轮水平分析多种微量元素的含量与变化。  相似文献   

10.
鱼类早期发育阶段是其生活史中的关键时期之一,生理、形态学变化剧烈,死亡率极高。研究鱼类早期发育阶段的生长规律及其生理特性,可为了解鱼类早期阶段的致死因子提供理论依据,有助于提高苗种阶段的生长率和成活率,也对制定合理的早期培育策略具有重要的指导意义。异速生长模式对确定仔鱼的养殖模式有重要的指示作用,鱼类在早期阶段会优先发育与生命活动关系较密切的器官,以期达到较高的早期成活率。RNA/DNA是评价鱼类早期发育阶段生长率的有效指标,也可用于评价仔稚鱼的生长潜力、营养状况、饲料营养水平以及确定关键期。研究仔稚鱼消化酶的发生和演变有助于深入了解鱼类在个体发育早期的消化生理,有助于选择适口饵料和制定投喂策略。因此,本文综述了鱼类早期发育阶段的异速生长模式、核酸及蛋白含量变化规律以及消化酶的发生和变化,为鱼类早期阶段健康养殖的发展提供依据。  相似文献   

11.
Juvenile walleye pollock of the Japanese Pacific population were collected from the Funka Bay [spawning ground; 16–64 mm fork length (FL)] in spring and the Doto area (nursery ground; 70–146 mm FL) in summer. Hatch dates were estimated by subtracting the number of otolith daily increments from sampling dates, and their early growth was back‐calculated using otolith radius–somatic length relationships. Interannual change of the hatching period was observed during 2000–02, and the peaks ranged from mid‐February in 2000 to early‐April in 2002. In 2000, when a strong year class occurred, early life history of the surviving juveniles could be characterized by early hatching and slower growth in the larval stage (<22 mm length). Higher growth rate in 2001 and 2002 did not always lead to good survival and recruitment success. Even though their growth was slow in 2000, the larvae hatched early in the season had larger body size on a given date than faster‐growing larvae hatched in later season in 2001 and 2002. Bigger individuals at a certain moment may have advantage for survival. The delay of hatching period may result in higher size‐selective mortality, and as a necessary consequence, back‐calculated growth in 2001 and 2002 could shift towards higher growth rate, although abundance of such a year class would be at the lower level. Variability in spawning period, early growth and their interaction might have a strong relation to larval survival through cumulative predation pressure or ontogenetic changes in food availability.  相似文献   

12.
This study examined otolith geochemistry as a natural marker of natal origins in young‐of‐the‐year (YOY) Cichla temensis in the Negro River Basin of Brazil. We analysed trace element and isotopic composition of otoliths of YOY collected off spawning nests from the main stem and major tributaries. These were compared with regional bedrock geologic composition to explore underlying mechanisms of differences in otolith geochemistry. Our results suggest that spatial differences in otolith geochemistry can be used to distinguish natal origins based on 87Sr/86Sr, Sr/Ca and Ba/Ca ratios. This approach allowed us to correctly classify 99% of juvenile fish to their natal streams using cross‐validation in a linear discriminant function analysis (LDFA). Patterns of otolith isotopic composition correspond with patterns in regional geology as expected based on previously demonstrated correlations, although some fine‐scale spatial differences cannot be accounted for by available geologic information. These results demonstrate that otolith chemistry is valuable as a natural marker of natal origins in this system and suggest that inferences from geologic maps may be useful for interpreting movements based on otolith geochemical signatures. This information provides the basis for future work to investigate the early life history and spatial ecology of this important cichlid.  相似文献   

13.
14.
This study investigated otolith shape, elemental chemistry of otolith cores (first 1-3 months of life), and stable isotope ratios (δ18O and δ13C) of whole otoliths as indicators of stock structure among three important southern Australian blue grenadier Macruronus novaezelandiae fishery regions; west Tasmania - WTAS, east Bass Strait - EBS, and Great Australian Bight - GAB. Comparisons were confined to two dominant cohorts of age 4+ and 13+ years, spawned in winter 2002 and 1993 respectively. Otolith shape varied significantly between the WTAS and GAB regions for the age 4+ cohort only. Cu:Ca of otolith cores was significantly higher for both cohorts from WTAS than EBS and GAB, and Ba:Ca of otolith cores higher for WTAS and EBS than the GAB region. Stable isotopic signatures showed greater variation among regions for the age 13+ cohort. In particular, otoliths of age 13+ fish from WTAS displayed significantly higher δ18O (indicative of lower temperature history) than age 4+ fish from all regions, and the same age fish from the GAB and EBS regions. δ18O of blue grenadier otoliths accurately predicted water temperature at their main capture depths of 400-600 m. Chemistry of otolith cores combined with whole otolith isotope ratios discriminated GAB and EBS samples from those collected on the known WTAS spawning ground with moderate to high (64-86%) accuracy. The results provide support for the hypotheses that the GAB fishery is based on a separate stock for management purposes, and that the EBS fishery is likely replenished both from local spawning and the major WTAS spawning region.  相似文献   

15.
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   

16.
Demography can have a significant effect on reproductive timing and the magnitude of such an effect can be comparable to environmentally induced variability. This effect arises because the individuals of many fish species spawn progressively earlier within a season and may produce more egg batches over a longer period as they get older, thus extending their lifetime spawning duration. Inter‐annual variation in spawning time is a critical factor in reproductive success because it affects the early environmental conditions experienced by progeny and the period they have to complete phases of development. By reducing the average lifetime spawning duration within a fish stock, fishing pressure could be increasing the variability in reproductive success and reducing long‐term stock reproductive potential. Empirical estimates of selection on birth date, from experiments and using otolith microstructure, demonstrate that there is considerable variation in selection on birth date both within a spawning season and between years. The few multi‐year studies that have linked egg production with the survival of progeny to the juvenile stage further highlight the uncertainty that adults face in timing their spawning to optimize offspring survival. The production of many small batches of eggs over a long period of time within a season and over a lifetime is therefore likely to decrease variance and increase mean progeny survival. Quantifying this effect of demography on variability in survival requires a focus on lifetime reproductive success rather than year specific relationships between recruitment and stock reproductive potential. Modelling approaches are suggested that can better quantify the likely impact of changing spawning times on year‐class strength and lifetime reproductive potential. The evidence presented strengthens the need to avoid fishing severely age truncated fish stocks.  相似文献   

17.
Martin J, Daverat F, Pécheyran C, Als TD, Feunteun E, Réveillac E. An otolith microchemistry study of possible relationships between the origins of leptocephali of European eels in the Sargasso Sea and the continental destinations and relative migration success of glass eels.
Ecology of Freshwater Fish 2010: 19: 627–637. © 2010 John Wiley & Sons A/S Abstract – Little is known about the extent to which Atlantic eels coming from different European rivers converge on the same spawning site. Our aim was to evaluate the spatial homogeneity of eel spawning area(s) with an otolith microchemistry approach. This work compared the elemental signatures of otolith’s core region of Anguilla anguilla leptocephali caught in the Sargasso Sea in 2007 with those of glass eels and elvers sampled in European estuaries during 2006, 2008 and 2009. Using laser ablation inductively coupled plasma mass spectrometry, the same annular ablation trajectory along the first feeding mark was applied on otoliths of glass eels, elvers and leptocephali. The concentrations of thirteen isotopes in the otoliths of glass eels/elvers did not vary among three annual cohorts collected in eleven European locations. However, otolith elemental fingerprints of leptocephali differed significantly from glass eels otolith’s signature. Although the mechanisms that regulate the differences in trace element signatures among leptocephali and glass eels/elvers are unknown, we propose that the sampled glass eels/elvers were born in a spawning site or region where favourable transport and/or feeding conditions occurred. Conversely, the leptocephali may have been sampled in a less favourable region in the Sargasso Sea, with a low probability of reaching continental growth areas.  相似文献   

18.
Alternative life-history tactics of masu salmon Oncorhynchus masou are well documented. Subsequent to the freshwater parr stage (age ≥ 1 + years), an anadromous form migrates to the sea after smolting, while a resident form matures without seaward migration. In addition to this typical migratory dimorphism, anecdotal reports based on field observations have indicated that some underyearling masu salmon use estuarine waters. However, no empirical evidence indicates saltwater utilisation and subsequent survival in the early parr stage. Here, we used otolith microchemistry to examine whether a portion of masu salmon parr in northern Japan enters coastal habitats. The otolith Sr:Ca ratios of most juveniles collected from six rivers had consistently low values, indicating that masu salmon parr inhabiting these rivers stay only in freshwater. In contrast, in individuals from a steep-gradient river the Sr:Ca ratios increased at about a 200-µm distance from the otolith core. These results suggest that some masu salmon parr might use brackish water or sea water temporarily. In addition, three masu salmon parr were found in another steep river where a culvert located only ten metres from the river mouth completely blocked upstream migration for spawning. The Sr:Ca ratios in these fish increased at about >200 µm from the otolith core, indicating the parr had immigrated to the non-natal river from the sea. Such flexible behaviour at an early life stage may contribute to the spatial expansion of masu salmon, and the movement could moreover help to stabilise its population dynamics.  相似文献   

19.
The poleward flowing East Australian Current (EAC) drives sporadic upwelling, entrains coastal water and forms the western Tasman Front (wTF), creating a mosaic of water types and larval transport routes along south eastern Australia. The spatial distribution, otolith chemistry and growth rates of larval sardine (Sardinops sagax) were examined to infer spawning location and larval transport. A gradient of increasing larval size from north to south along the shelf was not detected but was evident between the shelf and offshore in the wTF. Here larvae were larger and older. Based on the occurrence of newly hatched larvae, spawning by S. sagax between southern Queensland and mid New South Wales (NSW) was more extensive than previously reported. The otolith chemistry from two wTF larval size classes differed, implying different origins. The otolith chemistry of wTF post‐flexion larvae was similar to larvae from northern NSW, whereas wTF flexion larvae were similar to larvae observed nearby from mid‐NSW. Two possible larval transport routes, direct and indirect, are inferred from otolith chemistry, current velocities and a previously published particle tracking study. Either larvae from northern NSW were advected south and entrained with younger larvae directly into the wTF, or larvae from a range of shelf regions were advected around the southern edge of an anticyclonic eddy, to join younger larvae directly entrained into the wTF. Based on the co‐occurrence of larval ages and sizes in the wTF and their advection routes, the wTF appears to be an important larval retention zone.  相似文献   

20.
In order to understand better the recruitment variability in European anchovy in the Bay of Biscay, it is important to investigate the processes that affect survival during the early life stages. Anchovy juvenile growth trajectories and hatch‐date distributions were inferred over a 3‐year period based on otolith microstructure analysis. Otolith growth trajectories showed a characteristic shape depending on their hatch‐date timing. Earlier‐born juveniles had notably broader maximum increments than later born conspecifics, resulting in higher growth rates. This observation suggests that early hatching would be beneficial for larval and juvenile growth, and, therefore, survival. The estimated juvenile hatch‐date distributions were relatively narrow compared with the extended anchovy spawning season (March–August) in the Bay of Biscay and indicated that only individuals originated mainly from the summer months (June–August) survived until autumn. Hatch‐date distributions were markedly different among years and seemed to influence the interannual recruitment strength of anchovy. We conclude that years characterized by juvenile survivors originating from the peak spawning period (May and June) would lead to considerable recruitment success. Downwelling events during the peak spawning period seem to affect larval survival. Furthermore, size‐dependent overwinter mortality would be an additional process that regulates recruitment strength in the anchovy population in the Bay of Biscay.  相似文献   

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