Seasonal Gametogenesis of Host Sea Anemone (Entacmaea quadricolor) InhabitingHong Kong Waters

Studying gonadal development of annual cycle can reveal the process of gametogenesis and reproductive period, and evaluate fertility and source utilization of a species. Host sea anemones are conspicuous members of tropical and subtropical reef ecosystems, but little is known about its biology including reproductive seasonality. Here we reported a one-year study on the gametogenesis and reproduction of host sea anemone(Entacmaea quadricolor) inhabiting Hong Kong waters. E. quadricolor tissues were sampled in 12 occasions from 5 m and 15 m depths of water, respectively. Histological sectioning of the tissues showed that E. quadricolor was dioecious, and populational ratio of female to male was 1:1.6. The gonadal development was asynchronous within an annual cycle, which included proliferating, growing, maturing, spawning, and resting stages. The spawning occurred between August and October when surface seawater temperature reached the annual maximum(28℃), suggesting that temperature is an important factor modulating the gonadal development and mature of E. quadricolor.     

苏鲁榴辉岩带的矿物地球化学研究及意义

石榴石和单斜辉石作为榴辉岩的主要造岩矿物,其微量元素地球化学特征对深入研究化学组成等方面有重要意义。苏鲁榴辉岩带中石榴石和单斜辉石中的主要微量元素与全岩呈很好的正相关关系。石榴石和单斜辉石的轻重稀土元素含量呈相互消长的互补关系。Ga、Cr、Zn主要赋存于石榴石和单斜辉石中,重稀土、Y、Co、Sc主要赋存于石榴石中,V、Ni主要赋存于单斜辉石中,轻稀土和Sr在胶东榴辉岩中主要赋存于单斜辉石中,但在鲁南榴辉岩中可能赋存于磷灰石和绿帘石等矿物中。胶东榴辉岩为地幔成因,鲁南榴辉岩壳幔成因均有。苏鲁榴辉岩自西向东成岩温度逐渐升高,成岩压力增加。     

Simulated Heat Sink in the Southern Ocean and Its Contribution to the Recent Hiatus Decade

A set of numerical experiments is designed and carried out to understand a heat sink in the Southern Ocean in the recent hiatus decade. By using an oceanic general circulation model, the authors focus on the contributions from two types of forcing: wind stress and thermohaline forcing. The simulated results show that the heat sink in the upper Southern Ocean comes mainly from thermohaline forcing; while in the deeper layers, wind stress forcing also plays an important role. These different contributions may be due to different physical processes for the heat budget. The combination of these two types of forcing shows a significant heat sink in the Southern Ocean in the recent hiatus decade, and this is consistent with the observations and conclusions of a similar recently published study.     

植酸酶对凡纳滨对虾生长性能和体成分的影响

在凡纳滨对虾饲料中添加不同量微生物植酸酶(0,500,1000,2000 U/kg),观察虾的存活率、增重率、饲料系数及虾体和虾壳成分,研究饲料中添加植酸酶对凡纳滨对虾生长性能的影响。结果表明:饲养8周后,饲料中添加500~2000 U/kg植酸酶对凡纳滨对虾增重率、存活率和饲料利用无显著影响(P>0.05);植酸酶添加各组与对照组虾体的水分、粗蛋白、脂肪、灰分、总钙和总磷含量差异不显著;虾壳中粗灰分和钙含量在500和1000 U/kg组显著高于对照组和2000 U/kg组(P<0.05),虾壳磷含量在各饲料组间差异不显著。血清磷浓度在对照组和2000 U/kg组显著高于500 U/kg组(P<0.05),血清钙浓度在组间差异不显著,血清碱性磷酸酶活性以对照组最高,显著高于500和1000 U/kg组。结果说明,在特定试验条件下,饲料中添加植酸酶对凡纳滨对虾幼虾的虾壳和血清成分有显著影响(P<0.05),对幼虾生长性能影响不显著(P>0.05)。     

口蹄疫病毒VP1植物表达载体的构建

P1 T重组质粒上含有口蹄疫病毒 (FMDV)GD10分离株的p1cDNA片段 ,以此为模板 ,用PCR方法扩增其中的VP1基因 ,获得大小约 6 40bp的片段。该片段用BglⅡ和BstEⅡ酶切消化后克隆至表达载体 pCAMBIA130 5 .2 ,转化EcoliTOP10感受态细胞。重组质粒经PCR、酶切及序列分析 ,证实VP1基因处于CaMV35S启动子控制 ,且读码框正确     

西秦岭糜署岭岩浆混合花岗岩地球化学特征及构造意义

西秦岭糜署岭岩体是壳幔岩浆混合的产物。从寄主岩石和基性端元暗色微细粒镁铁质包体的主要元素、稀土元素岩石地球化学研究入手，深入探讨了糜署岭岩体是壳源和幔源两类岩浆混合形成的混浆花岗岩，其岩石地球化学特征介于壳源和幔源两个端元之间并有显著的过渡特征，表明二者在岩浆侵位过程中发生过不同程度地物质成分交换。这对研究西秦岭中生代壳幔混合作用和地壳增生有重要意义。     

Particulate organic carbon export flux by 234Th/238U disequilibrium in the continental slope of the East China Sea

234Th is widely used to quantify the magnitude of upper ocean particulate organic carbon(POC)export in oceans.In the present work,the rates of particulate organic carbon export were measured based on the distribution patterns of234Th/238U disequilibrium in the water column within the continental slope of the East China Sea(ECS)during May 2011.The profiles of particulate and dissolved234Th activities at all three stations showed a relative deficit with respect to238U in the upper 100 m of the water column.The dissolved234Th scavenging rates and the particulate234Th removal rates and their residence times were calculated by a one-dimensional steady state model.The results showed that the dissolved234Th scavenging rates and the particulate234Th removal rates ranged from 12.4–61.4 dpm/(m3·d)andfrom3.8–21.8 dpm/(m3·d),respectively.The residence times of dissolved and particulate234Th were in the range of 3.4–158 d and 63.7–96.5 d,respectively.Combined with the measurement of POC/234Th ratios of suspended particles,POC export flux(calculated by carbon)from the euphotic zone was estimated in the study region,which ranged from 4.14–14.7 mmol/(m2·d),withanaverageof8.21mmol/(m2·d),occupying35%oftheprimeproductivity in the study area.The results of this study can provide new information for better understanding the carbon biogeochemical cycle within the continental slope of the ECS.     

云南澜沦南现铜铅锌多金属矿成矿地质条件

铜铅锌矿赋存于中侏罗统花开左组浅色岩系和杂色岩系破碎带中,为受层位控制的砂页岩型铜矿及受构造控制的热液型铅锌多金属矿床.     

灌溉诱发型滑坡风险控制关键技术

长期灌溉引起地下水位上升诱发滑坡发生是灌溉诱发型滑坡的基本特征,有效控制地下水位是灌溉诱发型滑坡风险管理的根本措施.通过灌溉量控制、竖向混合孔疏排水、水平疏排水3种排水措施,可以实现灌溉诱发型滑坡的风险控制.采用数值模拟的手段,计算了不同灌溉量下地下水动力场及其对应的台塬斜坡稳定性,模拟了不同布井方式下的竖向混合井疏排地下水的效果,结果表明,灌溉量控制在350×10 4m3/a以下可实现滑坡风险控制,竖向混合排水井间距为40m时可提高单体斜坡的稳定性.统筹考虑各种因素,提出了以控制灌溉量为主,辅以竖向混合孔排水和水平排水的黑方台灌区滑坡的风险控制措施.