雄性四倍体与雌性二倍体杂交培育全三倍体长牡蛎(Crassostrea gigas)的研究

将美国雄性四倍体长牡蛎与中国北方海区雌性二倍体长牡蛎杂交 ,进行全三倍体长牡蛎培育研究。结果表明 ,四倍体与二倍体杂交的受精率为 47.4%─ 88.9% ,平均为 69.5 % ;来自同样雌贝的二倍体对照组的受精率平均为 91 .4%。杂交组和对照组面盘幼虫的平均孵化率分别为 5 3.9%和 61 .6% ;受精卵发育至稚贝的存活率 ,杂交组和对照组分别为 1 .3%和1 .9%。杂交组累计培育出眼点幼虫 8.32 4亿 ,稚贝 1 .843亿。杂交组幼虫的生长略快于对照组 ,但无显著差异。经流式细胞仪分析 ,杂交组的幼虫、稚贝、幼贝等均为 1 0 0 %三倍体。中国北方海区的长牡蛎可以与美国的雄性四倍体长牡蛎实现良好的杂交 ,产生 1 0 0 %三倍体。利用长牡蛎四倍体培育三倍体 ,方法简便高效 ,显示出四倍体在贝类三倍体商业生产中的巨大应用价值。     

诱导三倍体太平洋牡蛎群体发育过程中三倍体率的变化

借助染色体计数和流式细胞计数计对 6 - DMAP处理和冷休克两种诱导方法获得太平洋牡蛎 (Crassostrea gigas)三倍体群体在各个发育时期三倍体率进行了系统检测。结果发现 ,在 4～ 8细胞时期 ,6 - DMAP诱导三倍体率为 75 % ,冷休克诱导三倍体率为 5 0 % ,在发育至 D形幼虫期和稚贝期 ,两类三倍体群体的三倍体率均有所下降。如从 4～ 8细胞期发育至稚贝期 ,冷休克诱导群体下降了 5 3.0 8%以上 ,6 - DMAP诱导群体三倍体率下降了 2 7.36 %。养殖一年后 ,6 - DMAP诱导群体三倍体率仍保持在 6 0 %以上 ,而冷休克诱导群体三倍体率已下降至不足 10 %。这一结果说明 ,利用 6 - DMAP诱导来获得三倍体是比较理想的方法     

5-羟色胺刺激长牡蛎排放精卵在四倍体诱导中的应用

本文报道了用 5 羟色胺催产出的长牡蛎精、卵 ,人工授精后诱导四倍体的实验结果 .结果表明 :在 2 6℃水温条件下 ,受精后 7min ,用 0 .5mg/dm3细胞松弛素B处理2 5min ,获得长牡蛎的胚胎四倍体 ,其诱导率为 1 6.7%,D形幼虫孵化率为 2 7.0 %;诱导效果优于采用常规解剖法 .注射 5 羟色胺刺激长牡蛎亲贝排放精、卵的有效浓度分别为 1× 1 0 -6 ～ 1× 1 0 -2 mol/dm3和 1× 1 0 -5 ～ 1× 1 0 -3mol/dm3.     

利用四倍体与二倍体杂交规模化培育全三倍体太平洋牡蛎苗种

利用引进美国的四倍体太平洋牡蛎(Crassostrea gigas)雄贝与我国的二倍体雌贝杂交，规模化培育全三倍体牡蛎苗种。杂交组的平均受精率为48．27％，对照组为80．53％，杂交组较低的受精率可能与四倍体雄贝的精子活力及精子数量有关。杂交组的孵化率、幼虫成活率和变态率分别为81．10％，42．3％和1．82％，对照组分别为79．96％，37．0％和1.80％。杂交组共培育出稚贝1200万粒。不同时期取样的流式细胞仪分析结果表明，杂交组的三倍体率为100％。     

利用细胞松弛素B抑制第一极体排放诱导近江牡蛎(Crassostrea rivularis)四倍体

采用细胞松弛素B（CB）处理受精卵,抑制第一极体的排放,对近江牡蛎四倍体的诱导和培育进行了研究.结果表明,近江牡蛎在25-28℃时受精卵发育同步性较高.在28℃条件下,CB适宜处理剂量为0.6mg/L.在个别受精卵出现第一极体时实施处理,至对照组的第一极体出现率达到50%终止处理,四倍体的诱导效果较好.5个处理组D形幼虫的平均孵化率为11.0%,显著低于对照组72.4%的平均孵化率.在受精后4-12d期间处理组幼虫的存活率显著低于对照组.处理组胚胎和D形幼虫阶段四倍体的平均比例分别为41.8%和37.9%.四倍体的比例随着幼虫的生长发育呈下降趋势,至受精后12d在各处理组已检测不到四倍体.2组幼虫完成附着变态,从受精卵至稚贝的累计存活率平均为0.3%.本研究结果表明,使用CB处理抑制受精卵第一极体的释放可以有效诱导近江牡蛎四倍体,但所获得的四倍体幼虫存活力差,需要在未来的研究中解决.     

四倍体太平洋牡蛎(Crassostrea gigas Thunberg)自群繁殖的研究

2004年7~8月,利用诱导的1龄四倍体太平洋牡蛎做亲本,通过解剖取卵、人工受精的方法进行四倍体的自群繁殖。结果表明四倍体太平洋牡蛎自群繁殖的受精率为95.54%,孵化率为37.38%,采用同一雌体四倍体牡蛎与二倍体雄贝杂交产生的三倍体组(TD)的受精率为85.19%,孵化率为99.9%,而以二倍体做母本、四倍体做父本的杂交组(DT)的受精率为98.73%,孵化率为87.63%,二倍体对照组的受精率为96.39%,孵化率为99.9%。四倍体牡蛎经自群繁殖培育出稚贝1130粒。经流式细胞仪分析,四倍体太平洋牡蛎幼虫和稚贝的四倍体率均达到100%。幼虫培育过程中,从孵化出D-形幼虫到出现眼点,幼虫的成活率达11.86%,眼点幼虫的变态率高达16.1%。实验证明四倍体太平洋牡蛎可以进行自群繁殖,比诱导的方法简单高效。     

熊本牡蛎室内人工育苗技术研究

本文以熊本牡蛎为材料,在高温季节,通过强化亲贝营养和26℃以上高温促熟培育,使熊本牡蛎亲贝快速成熟,利用阴干流水刺激方法诱导产卵,并进行了不同盐度下受精卵孵化实验;通过合理控制幼虫密度、投喂新鲜无污染的单胞藻、及时分级筛选等系列技术措施,克服了熊本牡蛎育苗成功率低的技术难题;开展了栉孔扇贝壳、长牡蛎壳和栉江珧壳三种附着基的采苗试验,结果显示牡蛎壳是理想的附着基,可使稚贝的附着变态率达到60%以上,促进稚贝的生长和成活,提高稚贝产量,壳长2mm以上的稚贝单位水体出苗量超过10×10~4粒/m~3。     

肠道细菌对厚壳贻贝稚贝附着的作用研究

为探讨肠道细菌形成的微生物被膜对贝类附着的作用,从厚壳贻贝(Mytilus coruscus)成体肠道中分离10株肠道细菌,调查厚壳贻贝肠道细菌形成微生物被膜特性,分析微生物被膜密度、细菌种属与厚壳贻贝稚贝附着之间的相互关系。所有肠道细菌均可有效促进稚贝附着。其中,Paracoccus sp.1微生物被膜诱导的稚贝附着率最高(61%),且微生物被膜膜厚较厚,细菌分布较密集;仅5株肠道细菌Roseovarius sp.1、Winogradskyella sp.1、Tenacibaculum sp.4、Bacillus sp.5和Nonlabens sp.1的被膜密度与附着显著相关(P0.05)。系统发育分析发现肠道细菌诱导附着率与其种属无关。本研究表明源于厚壳贻贝成贝肠道细菌可以促进其稚贝的附着,说明肠道细菌对厚壳贻贝的生长发育具有一定的作用。本研究结果为深入探讨肠道细菌与厚壳贻贝相互作用和推动该种规模化养殖提供理论依据。     

两种东风螺幼虫附着和变态的化学诱导研究

在持续24h作用下,12×10-3mol/dm3 K+可有效地诱导台湾东风螺(Babylonia formosae)和方斑东风螺(B.aerolata)的浮游幼虫90%以上完全变态.持续作用24h,15×10-3mol/dm3 K+对方斑东风螺幼虫有毒害作用,但作用12h可取得较好的诱导效果.增加K+诱导变态的稚贝能正常活动和摄食.增加K+诱导的幼虫变态率随幼虫平均壳高的增大而提高.L-多巴、肾上腺素和去甲肾上腺素在5.5×10-6～5.5×l0-5mol/dm3时对方斑东风螺幼虫的变态无诱导活性,而多巴胺在10-4mol/dm3时可诱导较12×10-3mol/dm3 K+约少一半的变态率.钾通道阻滞剂TEA对K+诱导两种东风螺幼虫变态无阻抑作用.根据添加KCl诱导幼虫变态试验结果,初步认为幼虫获得变态能力时的壳高,在台湾东风螺是860.2～1009.8μm,在方斑东风螺是849.6～956.0μm.两种东风螺的浮游幼虫均有变态延迟现象.     

合浦珠母贝四倍体诱导过程中非整倍体的产生

合浦珠母贝Pinctadamartensii (Dunker)三倍体的卵与二倍体的精子授精 ,以细胞松弛素B(CB)抑制第一极体释放诱导四倍体 ,得到胚胎期非整倍体占 (88.1 8± 6 .79) % ,1龄贝中非整倍体约占 2 8.70 %。成贝非整倍体染色体数目有 2 9,3 0 ,40 ,41 ,43条 5种类型。非整倍体作为一个群体其壳长和体重与二倍体无明显差异 (p >0 .1 0 ) ,但与三倍体有显著差异 (p<0 .0 1 ) ;二倍性水平的非整倍体的壳长和体重明显小于二倍体 (p <0 .0 1 ) ,而三倍性水平的非整倍体与二倍体无明显差异 (p >0 .1 0 )。研究结果表明 ,合浦珠母贝能耐受约单倍体染色体数目 7%— 1 4%的增加或减少 ,且表明合浦珠母贝非整倍体在一定条件下是可以存活的。     

Assessing the Validity of Seismo-Acoustic Predictor Equations for Obtaining Seabed and Sub-Surface Sediment Physical Properties

The interdependence between the seismo-acoustic properties of a marine sediment and its geotechnical/physical parameters has been known for many years, and it has been postulated that this should allow the extraction of geotechnical information from seismic data. Though in the literature many correlations have been published for the surficial layer, there is a lack of information for greater sediment depths. In this article, a desktop study on a synthetic seafloor model illustrates how the application of published near-surface prediction equations to subsurface sediments (up to several tens of meters burial depth) can lead to spurious predictions. To test this further, acoustic and geotechnical properties were measured on a number of sediment core samples, some of which were subjected to loading in acoustically-equipped consolidation cells (oedometers) to simulate greater burial depth conditions. For low effective pressures (representing small burial depths extending to around 10 meters subsurface), the general applicability of established relationships was confirmed: the prediction of porosity, bulk density, and mean grain size from acoustic velocity and impedance appears generally possible for the investigated sedimentary environments. As effective pressure increases through, the observed relationships deviate more and more from the established ones for the near-surface area. For the samples tested in this study, in some instances increasing pressure even resulted in decreasing velocities. There are several possible explanations for this abnormal behavior, including the presence of gas, overconsolidation, or bimodal grain size distribution. The results indicate that an appropriate depth correction must be introduced into the published prediction equations in order to obtain reliable estimates of physical sediment properties for greater subsurface depths.     

海上大直径钢管桩打桩过程中桩周土强度弱化研究

海上大直径钢管桩打桩过程中,桩周土体受到强烈扰动而发生强度弱化,掌握桩周土体强度弱化规律对于准确预测打桩过程、保证工程安全具有重要意义。为研究土体强度弱化规律,开展了环剪试验模拟打桩对桩周土体的扰动,测试土体强度随剪切速率的变化规律,建立了描述土体强度弱化规律的拟合公式,引入到打桩分析软件中。研究结果表明：土体的强度折减程度不仅与土体本身的性质有关还受到土体的埋深和剪切速率的影响,埋深越深土体强度折减程度越低,剪切速率越高土体强度折减越高,在打桩分析中可采用这里推荐的线性折减方法来模拟不同深度处土体强度的折减规律。     

Interannual Sea Level Variations and Annual Tides in the Northwestern Pacific

Specific properties of the interannual sea level variations and annual tides in the Northwestern Pacific were studied. Several tide stations were monitored. The monthly mean sea level for the year of 1995 was analyzed at each tide station. A seismic event in 1995, some tectonic activity around the subject area, and the Kuroshio (the oceanic western boundary current) may possibly contaminate results which would have occurred from the astronomical annual tide alone.     

Flow Cytometric Analysis of Coastal Lagoon Bacterioplankton and Picophytoplankton: Fixation and Storage Effects

The effect of different fixation and storage protocols on the flow cytometric (FCM) simultaneous analysis of bacterioplankton and phytoplankton in coastal seawater samples (Mediterranean coastal lagoons) was investigated. FCM measurements (cell number, fluorescence and scatter characteristics) were obtained through DAPI staining. Three fixatives [glutaraldehyde (GA), formaldehyde (FA) and paraformaldehyde (PFA)] and two storage (3 months duration) methods (5 °C and −196 °C) were tested. Two dominant populations were detected in studied samples: bacteria and eukaryotic picophytoplankton. Adding fixatives (2% final concentration) appears necessary to obtain FCM exhaustive counts of all the bacteria and phytoplanktonic cells. This was related to the permeation effect of fixatives which allowed a better DAPI staining of the cells. Maximum fluorescence, i.e. optimal staining of the cells was obtained with FA or PFA, and significant lower fluorescences with GA. Fixed samples stored at 5 °C induced rapid cell loss. Only storage in liquid nitrogen of samples fixed with FA or PFA, allows mid-term (≥4 months) preservation of bacteria or picophytoplankton cell numbers, and limited evolution of DAPI-induced fluorescence and scatter characteristics.     

INFORMATION FOR AUTHORS

<正>Acta Oceanologica Sinica(AOS)is a comprehensive academic journal edited by the Editorial Committee of Acta Oceanologica Sinica and is designed to provide a forum for important research papers of the marine scientific community which reflect the information on a worldwide basis.The journal publishes scholarly papers on marine science and technology,including physics,chemistry,biology,     

Phylogenetic diversity and phenotypic characterization of cultivable bacterioplankton isolated from polar oceans

A set of 27 marine planktonic bacteria isolated from the polar regions was characterized by 16S rDNA sequencing and physiological and biochemical testing. More than half of these bacteria were positive for caseinase, gelatinase and 13-glucosidase, and could utilize glucose, maltose or malic acid as carbon source for cell growth. Twelve isolates expressed nitrate reduction activities. Except for one antarctic isolate BSwlO175 belonging to Actinobacteria phylum, these isolates were classified as γ-Proteobacteria, suggesting that γ-Proteobacteria dominated in cultivable marine bacterioplankton at both poles. Genus Pseudoalteromonas was the predominant group in the Chukchi Sea and the Bering Sea, and genus ShewaneUa dominated in cultivable bacterioplankton in the Prydz Bay. With sequence similarities above 97%, genus Psychrobacter was found at both poles. These 27 isolates were psychrotolerant, and significant 16S rDNA sequence similarities were found not only between arctic and antarctic marine bacteria （ 〉 99% ）, but also between polar marine bacteria and bacteria from other aquatic environments （ ≥ 98.8% ）, including temperate ocean, deep sea, pond and lake, suggesting that in the polar oceans less temperature-sensitive bacteria may be cosmopolitan and have a bipolar, even global, distribution at the species level.     

Net Sand Transport Direction in a Tidal Inlet, using Foraminiferal Tests as Natural Tracers

The relationship between the flux of exotic benthic foraminiferal tests (i.e. tests which are supplied from open-sea sources alone) in a tidal inlet and that of bulk sediment was analysed, which can be expressed as two first-order linear equations. According to this relationship, in order to determine net sediment transport directions in the entrance, the test concentration in surficial sediments of the tidal basin can be compared against a ‘ critical level ’. The critical level is determined for the conditions that no net transport of bulk sediment is present within the entrance. If the observed concentration (averaged over the tidal basin) is higher than the simulated critical level, then the net sediment transport is directed to landward. This method is applied to the analysis of net sand transport at Christchurch Harbour, a tidal inlet system located in southern England. In this investigation, concentrations of exotic foraminiferal tests in the surficial sediments of the tidal basin and ebb tidal delta area were obtained from the analysis of sea-bed sediment samples. A series of probable critical levels were calculated based upon the data sets with regard to: (1) sediment discharge from the rivers; (2) magnitude of sediment discharge within the entrance during the ebb; (3) the test concentration outside the harbour; (4) the thickness of the moving layer; and (5) two parameters associated with dispersive processes. The results show that the concentration in the tidal basin sediment is higher than a number of simulated critical concentrations for representative cases. Consequently, the high level of the concentration of exotic benthic foraminiferal tests within the harbour should be explained as a result of landward net transport of sands within the entrance.