三峡水库太湖新银鱼耳石日轮与生长的研究

对采自重庆长江江津江段的太湖新银鱼(Neosalanx taihuensis)耳石日轮与生长进行了研究。太湖新银鱼矢耳石形状近圆形,体长(Y)与耳石长半径(X)之间呈线性相关,其关系式为Y=0.1099X+16.986,R2=0.7626。耳石日轮环纹清晰,以中心核为起点圆形规则排列,其上具有明显的过渡轮纹。太湖新银鱼体长(Y)与日轮(X)呈线性关系,其关系式为Y=0.2631X+23.924,R2=0.8057;体重(Y)与日轮(X)呈指数关系,其关系式为Y=0.0446e0.0244X,R2=0.8104。太湖新银鱼体重(Y)与体长(X)间呈显著的幂函数关系Y=0.000001X3.3529,R2=0.9163。     

太湖中大银鱼_太湖新银鱼和寡齿新银鱼群体的遗传结构

利用ＲＡＰＤ技术对太湖中的大银鱼,太湖新银鱼,寡齿新银鱼的遗传结构进行了研究,共在太湖中的６个采样片采到大银鱼和太湖新银鱼样品,在两个采样片得到了寡齿新银鱼的样品。结果表明,太湖中不同水域的三种银鱼没有明显的遗传差异,三种银鱼中,大银鱼的遗传相似性指数显示最大,太湖新银鱼的次之,寡齿新银鱼的最小,说明大银鱼的遗传变异性最小,寡齿新银鱼的最大,太湖新银鱼的遗传变异性界两者之间。     

太湖新银鱼和寡齿新银鱼组织内氨基酸的含量

太湖新银鱼(Neosalanx taihuensis Chen)和寡齿新银鱼(N.oligodontis Chen)广泛分布于我国东部平原地区湖泊,为重要经济鱼类。目前,有关银鱼种群生态与生长特性、生物学特性、生殖发育及移植引种等方面的研究报道较多,但对银鱼鱼休营养成分及营养价值方面的研究尚未见报道。本文是对这两种银鱼肌肉及寡齿新银鱼整体的水解氨基酸和游离氨基酸进行测定,并初步比较分析的结果。     

用PAPD方法分析太湖大银鱼、太湖新银鱼和寡齿新银鱼的亲缘关系

１９９６￣１９９７年２年中在太湖６个水域采集到大银鱼（Ｐｒｏｔｏｓａｌａｎｘ ｃｈｉｎｅｎｓｉｓ）、太湖新银鱼（Ｎｅｏｓａｌａｎｘ ｒｅｇａｎｉｕｓ）和寡齿新银鱼（Ｎｅｏｓａｌａｎｘ ｏｌｉｇｏｄｏｎｔｉｓ）并发现其中有２个样品的ＲＡＰＤ图谱与其它样品的图谱有很大差异,进一步ＤＮＡ分析结果表明,这２个样品不属于大银鱼,太湖新银鱼和寡齿新银鱼的其它种银鱼,表明太湖中可能存在５种银鱼。     

大银鱼耳石日轮与生长的研究↑（*）

１９９５年对内蒙莫力庙水库的大银鱼耳石日轮与生长进行了研究。大银鱼人工受精卵孵出仔鱼、剖出其听囊内一时圆形矢耳石，其制片在光镜下观察，耳石形态经历了由圆形、椭圆形到梨形的变化过程。耳石长半径与鱼体长呈线性相关，其关系式为Ｙ＝４．７９８ｘ－２０．８８７（ｒ＝０．９６５０，Ｐ＜０．０１）。孵出后第二天耳石上出现第一个日轮，正常条件下，每天形成一轮。孵化后天数可用耳石日轮数加１表示，其表达式为Ｄ＝Ｎ＋１，耳石上的日轮数变幅为２６７－３４５。日轮间距有规律性变化，依据日龄和相关体长、体重资料进行了大银鱼生长特性研究。     

辽东湾安氏短吻银鱼的生物学

安氏短吻银鱼Neosalanx andersoni(Randahl)曾为辽东湾早春的重要捕捞对象。本文对该鱼的形态特征、繁殖、食性、洄游等进行了调查，并对其分布、精巢数目、资源下降的原因以及繁殖保护的措施作了分析和讨论．     

用RAPD方法分析太湖大银鱼、太湖新银鱼和寡齿新银鱼的亲缘关系

1996～1997年 2年中在太湖 6个水域采集到大银鱼（Protosalanx chinensis）、太湖新银鱼（Neosalanx mpnius）和寡齿新银鱼（Neosalanx oligodontis）,并发现其中有2个样品的 RAPD图谱与其它样品的图谱有很大差异,进一步的DNA分析结果表明,这2个样品不属于大银鱼、太湖新银     

徐家河水库近太湖新银鱼的胚胎发育

近太湖新银鱼受精卵对孵化条件要求不高,只要保证充足的溶氧,可以静水孵化。水温７－１０．６℃时,孵化期２３２．８ｈ,水温１０－１３．５℃时,孵化期１７４．３ｈ。鱼菌孵出后４ｄ,可以平游。不投饵情况下,鱼苗可１５ｄ以上。刚孵出鱼苗平均体长２．７ｍｍ,１周后可长到３．９ｍｍ,两周后长到５．３文章对胚胎发育的各主要阶段进行了描述。     

胭脂鱼早期生活史行为发育

以人工繁殖的胭脂鱼(Myxocyprinusasiaticus)脱膜仔鱼为研究对象,对其早期发育阶段在自然环境下的行为生态学及其早期生存的适应性进行分析。胭脂鱼脱膜仔鱼和1～3日龄的早期仔鱼对光照强度栖息地底质颜色没有选择性,栖息于水体底层,有喜好隐匿场所的倾向,但达不到显著性喜好的程度(P=0.654),不进行顺水漂流。4日龄以后的仔鱼开始趋光,选择白色底质,离开水体底层,并顺水漂流。14日龄以后,顺水漂流停止,选择白色底质的比例下降,几乎完全不选择隐匿场所,但仍然趋光。0～8日龄的仔鱼昼夜活动差异不明显(t=-1.48,P=0.142),9～14日龄时,夜间活动明显强于白天(t=-6.95,P=0),14日龄以后,昼夜活动差异不显著(t=0.05,P=0.96)。     

云南高原湖泊太源新银鱼的繁殖

采用常规方法调查了滇池和星云湖太湖新银生腺的周年发育情况和怀卵星。其繁殖期为当年冬至翌年春，盛期为１月初至２月中旬，届时水温约１１℃。     

中华倒刺鲃仔、稚鱼的耳石微结构与日轮形成特征

以中华倒刺鲃(Spinibarbus sinensis)亲鱼为材料,在实验室养殖条件下以人工孵化的丰年虫(Eubranchipus vernalis)为仔、稚鱼饵料,通过已知日龄法观察其耳石的微结构,分析其日轮形成特征。结果表明,仔、稚鱼的微耳石和矢耳石一般由1个中心核和1个耳石原基组成,少数存在多个中心核或原基现象,星耳石中心核和原基区分不明显。微耳石和矢耳石中心核直径分别为(37.73±5.34)μm和(39.78±7.11)μm,耳石原基直径分别为(16.29±3.46)μm和(17.09±3.88)μm。矢耳石和星耳石轮纹清晰度、规律性、周期性和完整性不及微耳石;微耳石第1条日轮在仔鱼出膜后第2天形成,以后每天沉积1轮。30日龄稚鱼微耳石轮纹数(N)与日龄(T)的关系符合直线模型,相关关系式为:N=1.0016T-0.8753(R2=0.9961,P<0.01,n=197),线性方程斜率与1无显著性差异(P>0.05)。在微耳石和矢耳石样本中共观察到孵化标记轮和转移标记轮2种,其中孵化标记轮的出现率分别为78.68%和83.33%,转移标记轮的出现率分别为29.95%和48.98%。60尾33日龄稚鱼微耳石的生长轮宽度变化范围0.522~2.244μm,平均为(1.087±0.231)μm。     

Early ontogeny of the spotted wolffish (Anarhichas minor Olafsen)

This study illustrates the embryo development of the spotted wolffish (Anarhichas minor Olafsen), an interesting candidate for cold‐water aquaculture. The egg morphology (semitransparent, yellow‐white with numerous oil droplets in the yolk), size (5.4–6.5 mm) and long embryogenesis (c. 800–1000 d°, depending on temperature) of A. minor are very similar to Anarhichas lupus. Cleavage is slow, and the first cell divisions take place at 12 h at 8°C. After 12 days the 2‐mm embryo with the first somites is laid down and the blastopore starts closing. The fat globules in the yolk fuse into one after 22 days, and after 30 days eye pigmentation is noticeable. After 44 days, eye pigmentation is strong, the digestive tract folded and a green gall bladder can be noted in the now 11‐mm‐long embryo. One week later the blood is brightly red, the intestine is pigmented and the lower jaw is well developed. Premature hatching may occur from this stage. After 58 days vascularization of the yolk is complete, capillaries are noted in the fin fold, the first ray rudiments are established in the tail and pectoral fins, and the four gill arches are covered by the operculum. The preanal finfold is reduced after 72 days, stomach and gill filaments are formed, and six pigmented rows are noted on the 17‐mm‐long embryo body. After 86 days all fin rays are seen and the digestive tract is intensely pigmented and folded. Hatching (normal) starts after 110 days and may last for 2–3 weeks. Late embryos and early larvae of A. minor have more distinct bands of pigment along the body compared with the closely related A. lupus. An increase in both length and weight of the embryos in individual batches occurs during the hatching period.     

Environmental determinants of growth rates for larval Japanese anchovy Engraulis japonicus in different waters

Do disparate mechanisms determine growth rates of fish larvae in the different regions? The relationship between growth rates and environmental factors (sea temperature and food availability) was examined for larval Japanese anchovy Engraulis japonicus in geographically and environmentally different waters, through sagittal otolith microstructure analysis. Recent 3‐day mean growth rates directly before capture were positively related with sea‐surface temperature (SST) but not with food availability (plankton density) for the larvae in the Kuroshio Extension and Kuroshio–Oyashio transition regions of the western North Pacific. On the contrary, variations in recent growth rates were attributed to food availability (plankton density) as well as SST for the larvae in the East China Sea. In the shirasu fishing ground in Sagami Bay, larval growth rates were variable under the influences of both SST and food availability (feeding incidence). On the surface, the growth–environment relationships seemed to differ among regions. However, a definite general pattern of the dome‐shaped relationship between recent growth rates and SST was observed when all the regions were combined. Growth rates were similar even among clearly different regions if at the same SST. Overall, growth rates roughly increased with SST until they reached the maximum at SST of 21–22°C (i.e. optimal growth temperature), and declined when SST went over 21–22°C. On the contrary, no clear relationship was observed between growth rate and plankton density or between SST and plankton density. Therefore, the apparent among‐region differences would be firstly caused by the differences in regional SST range. The systematic mechanism of growth determination for widespread pelagic fish species larvae would be run by primarily sea temperature and secondarily food availability, at the species level.     

Early life history of yellow puffer,Chonerhinos naritus (Richardson, 1848) from Sarawak,Northwestern Borneo

The growth and morphological development including fins, spine distribution and pigmentation of larval and juvenile of hatchery‐reared yellow puffer, Chonerhinos naritus were described to provide essential information on the early life history of this species. The total length (TL) of newly hatched larvae was 3.42 ± 0.23 (mean ± SD) mm, reaching 5.66 ± 0.38 mm on 5 days after hatched (DAH), 7.80 ± 0.28 mm on 11 DAH, 9.88 ± 0.40 mm on 27 DAH and 10.92 ± 0.58 mm on 30 DAH. The yolk was completely absorbed in preflexion larvae at 4 DAH. The mouth opening started at 3 DAH of yolk sac larvae, while the teeth appeared starting from preflexion larvae at 7 DAH. Overall aggregate fin ray numbers including caudal fin attained full complement in postflexion larvae at 27 DAH. Several melanophores with appearance of small stellate were first appeared dorsally on the head of flexion larvae at 13 DAH, expanded at the dorsal region of the head, above the eye in juveniles at 30 DAH. The spines first appeared in preflexion larvae of C. naritus at 7 DAH, covering the ventral skin region below pectoral fin base and expanded to the ventral part of the body and nearly covered the whole abdomen region before the anus and below the eyes in juveniles. C. naritus remain as larvae for approximately 29 days, during which they metamorphose to the juvenile stage prior to sexual maturation. Observations in larvae development of C. naritus revealed similar characteristics with other Tetraodontidae species.     

Variability in growth rates of larval haddock in the northern North Sea

The large-scale distribution of haddock ( Melanogrammus aeglefinus ) larvae in the northern North Sea was mapped in a grid survey carried out in late April 1996. A drifting buoy was deployed in the centre of one of the areas of concentration of larvae located off the east coast of the Shetland Isles, where intensive sampling was carried out for ≈ 10 days. Daily larval haddock growth variability, estimated from otolith microstructure analysis, was independent of the measured variability of the physical and biological environment of the larvae. The survey coincided with the onset of the spring plankton production bloom, and a likely explanation for the absence of environmental effects on larval growth was high food availability and larval feeding rates. Nevertheless, differences in growth were observed between cohorts, with larvae hatched later in the spring displaying higher growth at age than those hatched earlier. Particle-tracking modelling suggested that differences in temperature history between cohorts, on their own or compounded by a potential interaction between temperature and the development of plankton production, may explain the higher growth rate of the larvae hatched later in the season.     

金沙江一期工程对保护区圆口铜鱼早期资源补充的影响

2008、2010－2013年在金沙江下游水富／宜宾断面进行了鱼类早期资源调查,研究金沙江一期工程对长江上游珍稀特有鱼类国家级自然保护区圆口铜鱼早期资源补充的影响。共采获圆口铜鱼卵苗6190粒（尾）,其中鱼卵74粒、鱼苗6116尾;2013年向家坝水电站蓄水后在水富／宜宾断面未采集到圆口铜鱼卵、苗。各年圆口铜鱼卵苗江汛期和最大日径流量分别为：2008年6月12日－7月2日、3．79×107粒（尾）,2010年6月22日－7月10日、3．47×107粒（尾）;2011年6月23日－7月4日、9．58×107粒（尾）;2012年6月24日－7月13日、1．22×107粒（尾）。圆口铜鱼卵苗江汛与金沙江下游的水文流量持续增长相关,卵苗日径流量高峰值与洪峰过程较一致,最大日径流量基本先于最大水文流量前出现。圆口铜鱼繁殖盛期在6月中旬－7月上旬较短时间内（2～3周）。2008年向家坝水电站截流前长江上游珍稀特有鱼类国家级自然保护区的圆口铜鱼早期资源补充量为2．12亿粒（尾）;2010－2012年导流施工期间早期资源补充量分别为1．65亿、1．61亿、0．82亿粒（尾）,呈下降趋势;2013年无早期资源补充。溪洛渡、向家坝2个梯级大坝一定程度上阻隔了圆口铜鱼卵苗向下游漂流的途径。要合理制定水电梯级调度方案,促进或引起圆口铜鱼自然繁殖过程,并降低圆口铜鱼卵苗在库区的死亡率;加强圆口铜鱼现有栖息地保护,严格控制或禁止在产卵场捕捞亲鱼;开展圆口铜鱼在梯级大坝上下游间群体交流连通性的可能性研究和圆口铜鱼全人工繁殖技术研究。     

Understanding the life histories of amphidromous fish by integrating otolith‐derived growth reconstructions,post‐larval migrations and reproductive traits

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Otolith biochronologies as multidecadal indicators of body size anomalies in yellowfin sole (Limanda aspera)

Dendrochronology (tree‐ring analysis) techniques have been increasingly applied to generate biochronologies from the otolith growth‐increment widths of marine and freshwater fish species. These time series strongly relate to instrumental climate records and are presumed to reflect interannual variability in mean fish condition or size. However, the relationship of these otolith chronologies to fish somatic growth has not been well described. Here, this issue was addressed using yellowfin sole (Limanda aspera) in the eastern Bering Sea, for which a 43‐yr otolith chronology was developed from 47 otoliths and compared with body size for 6943 individuals collected in 1987, 1994, and 1999 through 2006. Among several metrics of size normalized for age and sex, average body mass index (defined as weight/length) had the strongest relationship to the otolith chronology, especially when the chronology was averaged over the 5 yr preceding fish capture date (R² = 0.88; P < 0.001). Overall, sample‐wide anomalies in otolith growth reflected sample‐wide anomalies in body size. These findings suggest that otolith chronologies could be used as proxies of body size in data‐poor regions or to hind‐cast somatic growth patterns prior to the start of fisheries sampling programs.     

An additional life-history tactic of masu salmon: Migration of parr to coastal habitats

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.