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1.
大连湾牡蛎的染色体数目   总被引:1,自引:0,他引:1  
以大连湾牡蛎的早期胚胎为材料。经染色体数目分析,首次提出大连湾牡蛎的染色体数目为2n=20。为牡蛎遗传育种工作提供依据。  相似文献   
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用冷热休克诱导三倍体近江牡蛎   总被引:1,自引:0,他引:1  
在近江牡蛎(Ostrea rivularis Gould)卵子授精后25分钟,分别用高温(35℃)和低温(10℃)持续处理20分钟,其胚胎发育初期的三倍体诱导率分别达到64%和69%。在这个高温点和低温点以外随着处理温度的升高或降低,三倍体诱导率均迅速减小。  相似文献   
4.
用冷热休克诱导四倍体近江牡蛎   总被引:1,自引:0,他引:1  
当近江牡蛎授精卵发育至第一次卵裂前3min或个别受精卵开始出现第一次卵裂时,分别用热体克(37℃,39℃,41℃)和冷休克(8℃,10℃,12℃)处理3min诱导四倍体。测定39℃热休克组胚胎早期的四倍体诱导率为28%,10℃冷休克组胚胎早期的四倍体诱导率为30%。温度过高(如42℃以上)可导致卵的高死亡率。  相似文献   
5.
从近江牡蛎肠道中分离出21株菌,其中, 9株为革兰阳性菌, 12株革兰阴性菌。为寻找能分泌多种酶的有益微生物,研究了它们蛋白酶、脂肪酶、淀粉酶、纤维素酶的产酶能力。结果表明,有61 .9%的菌株能分泌蛋白酶或淀粉酶(各有13株菌);有52. 4%的菌株能分泌脂肪酶(11株菌);有33. 3%的菌株能产纤维素酶(7株菌)。在这21株菌中,产4种酶的有5株菌,产3种酶的3株菌,产两种酶的5株菌,产1种酶的3株菌,不产酶的仅有5株菌。不产酶的菌株仅占细菌总数的23. 8%,而各种产酶菌则高达76. 2%,由此表明细菌在近江牡蛎对食饵消化过程的重要性。  相似文献   
6.
二倍体和三倍体牡蛎的外观鉴别   总被引:7,自引:1,他引:6  
对二倍体,三倍体僧帽牡蛎和太平洋牡蛎外套膜和生殖腺外部形态进行了周年观察。结果表明,从外套膜和生殖腺外观特征上的差异可鉴别出牡蛎二倍体和三倍体。1997年8月至1998年6月,分析了两种牡蛎样品266个,其鉴别准确率达96.99%。  相似文献   
7.
受试僧帽牡蛎(Ostreacuculata)暴露在含有久效磷农药的海水中养育7d,取鳃用空气干燥法制片,观察数千个早中期、中期细胞分裂相末发现微核、染色体结构变异及其它染色体畸变现象。但随久效磷浓度的增加细胞分裂相明显减少。处理过程中投饵和换水的僧帽牡蛎的细胞分裂相明显高于不投饵、不换水;但投饵和换水的僧帽牡蛎随久效磷浓度的增加细胞分裂被抑制的比率又快于不投饵、不换水。经久效磷处理的各组僧帽牡蛎核型与对照组的核型均为2n=20,20m,NF=40。研究结果指出:双壳类的僧帽牡蛎对久效磷农药的毒性不敏感,在所试浓度范围内,并不引起染色体损伤的遗传效应,但产生抑制鳃细胞分裂的效应  相似文献   
8.
Abstract. Oysters Ostrea chilensis P hilippi 1845. from a 40-month-old cohort which came from the natural population of the Quempillen River Estuary Southern Chile, were used as parental stock n = 600 for a hatchery-produced cohort. At 12 months of age this cohort was analysed physiologically filtration rate, organic ingestion rate, absorption rate, assimilation efficiency, excretion rate, respiration rate and electrophoretically multilocus heterozygosity MLH using four loci: LAP, GPI, PGM, CA. Most physiological variables were positively correlated with dry weight P < 0.05. with the exception of assimilation efficiency, excretion size and net growth efficiency P > 0.05. Also. there was a positive correlation between body size, ingestion rate, absorption rate and net growth efficiency with MLH. Respiration rate and consequently energy losses were negatively correlated with MLH. The energetic efficiency product of a lower metabolic cost in the heterozygous individuals in this cohort is reflected in a higher net growth efficiency and a positive correlation between growth and MLH. The genetic basis for the relationship between metabolic parameters and heterozygosity can be due to an overdominance in this 12-month-old cohort.  相似文献   
9.
Temporal patterns of larval brooding and settlement were investigated in a flat oyster (Ostrea chilensis) population in Tasman Bay, central New Zealand. The proportion of the population brooding larvae and larval settlement rates were monitored over 26 months. A peak period of brooding activity began in late spring and continued through summer. Maximum rates of 17% and 23% of adult oysters brooding larvae occurred in November and December, and an estimated 55–78% of adult oysters incubated larvae over the entire summer breeding period. These proportions of brooders are higher than those previously reported for Tasman Bay. A very low level of brooding activity (1%) occurred during winter. Temporal trends in larval settlement closely tracked brooding patterns. Settlement was greatest between November and January, and there were very low rates in winter. The seasonal breeding pattern in the population was intermediate between northern and southern populations, confirming a latitudinal gradient of reproductive behaviour for O. chilensis in New Zealand. Results are useful in optimising the timing of substrate deployment in an enhancement programme for the oyster fishery.  相似文献   
10.
Two multi-year oxygen isotope (δ18O) records were obtained from archaeological Ostrea angasi shells, confirming the potential of this species to provide valuable environmental records for the late Holocene period in southeastern Australia. High-resolution δ18Oshell samples from the O. angasi clearly display a seasonal variability, offering insight into past climate conditions in a region where such information is presently limited.

The oxygen isotope record in O. angasi reflects a combined temperature–salinity signal. Observations of δ18Oshell data from modern specimens are used as a point of reference to assist in decoupling these two influences, with the two archaeological samples compared with the δ18Oshell profile of four modern O. angasi. Assuming similar paleo- δ18Owater values at the collection sites, data from these archaeological shells present a record of temperatures during the period of their growth that are consistently lower than modern day, with mean annual temperatures ~2°C cooler.  相似文献   

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